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JOURNAL
OF THE
WASHINGTON ACADEMY
OF SCIENCES
VOLUME 49, 1959
PUBLISHED MONTHLY
BY THE
WASHINGTON ACADEMY OF SCIENCES
15380 P StREEt, N. W.,
WASHINGTON 5, D. C.
ACTUAL DATES OF PUBLICATION, VOLUME 49
No. 1, pp. 1-36, March 20, 1959.
No. 2, pp. 37-64, April 23, 1959.
No. 3, pp. 65-96, May 15, 1959:
No. 4, pp. 97-128, June 13, 1959.
No. 5, pp. 129-164, July 7, 1959.
No. 6, pp. 165-196, July 24, 1959.
No. 7, pp. 197-260, August 20, 1959.
No. 8, pp. 261-292, September 22, 1959.
No
No
. 9, pp. 293-332, November 25, 1959.
. 10, pp. 333-376, January 14, 1960.
ig
- fs
VOLUME 49 January 1959 NUMBER 1
wy oa A 2
= WwW a3
- Same
} 724
JOURNAL
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WASHINGTON ACADEMY
OF SCIENCES
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Ak 29 1959
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Published Monthly by the
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JOURNAL
OF THE
WASHINGTON ACADEMY OF SCIENCES
Vou. 49
JANUARY 1959
No. 1
SCIENCE ADMINISTRATION .—Pay plans and people. CRawFrorp R. BUELL,
U.S. Post Office Department, Washington, D.C. (Communicated by Waldo
L. Schmitt.)
(Received January 6, 1959)
Financial and psychic compensation of
scientists and engineers has long posed a
dilemma of no small proportions for all
government agencies which prosecute en-
gineering and scientific research and devel-
opment. World events within the past year
or two have emphasized the urgency of
reaching satisfactory conclusions. Toward
this end, the writer, during the past three
years, has studied the rank-status concept,
giving particular attention to scientists and
engineers engaged in research and develop-
ment. This study developed in some detail
the philosophical and historical background
of rank-status that had emerged as a con-
cept for civilian employment in the Federal
Government in the United States less than
20 years ago. The problems and situations
which give rise to consideration of the use-
fulness of a rank-status philosophy in the
administration of research are many. The
effect of the administrative climate upon the
scientist and, in turn, the attitudes of the
scientist and his effect upon that administra-
tive climate are matters that relate to the
quality of scientific and engineering achieve-
ments that are so necessary in this pre-
space age. Some of these elements and situa-
tions brought Reimer to the conclusion that,
“The futility of the fight against status is
gradually being recognized in the Western
world and, in certain forms at least, its con-
scious use is again respectable.”!
Appraisal of existing techniques used to
* Reimer, Everett, Modern personnel manage-
ment and the Federal service. The Federal Gov-
ernment Service: Its Character, Prestige, and
Problems, Sixth American Assembly, Arden House,
p. 161. Graduate School of Business, Columbia
University, New York, 1954
evaluate positions and to evaluate the peo-
ple in these positions or applying for them
is of especial importance to considerations
of rank-status. Considerable attention was
given, therefore, to the expressed opinions
of groups and of individuals concerning ap-
praisal of these techniques or tools. Evalua-
tion of positions includes job evaluation and
position classification. Evaluation of the
people includes such aspects of personnel ad-
ministration as merit rating and qualifica-
tions appraisal. From this aspect of the
study it was concluded that sophistication
of technique does not, by itself, lend validity
to any of these techniques. Sophisticated Job
evaluation and merit-rating techniques may
be no more valid and reliable than are some
of the less sophisticated tools that frequently
are used in rank-status plans.
This paper deals with a specific aspect of
rank-status—a comparison of six different
pay plans with the Classification Act of
1949, as amended. It is a summarization of
what the writer has found to be the methods,
techniques, and philosophies used in de-
termining the salary of scientists and re-
search and development engineers in various
private and government organizations. It
compares the techniques and policies used
in six important pay systems or research
organizations with those found existing un-
der the Classification Act of 1949, as
amended."
* Additional material prepared from the notes
of the writer concerning these six pay plans, and
other aspects of rank-status mentioned earlier, is
available from the writer for publication if deemed
desirable or to interested students of position
classification, pay administration, or research ad-
ministration.
Re aN MAR 2 4 1959
2 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
The term rank-status is used in this paper
to indicate systems where rank and pay are
based on the person rather than on the posi-
tion occupied by the person. It is used inter-
changeably with the terms rank-in-the-per-
son and personal-rank. Rank-status and job
evaluation systems each occur in many var-
lations—neither category should be thought
of as an absolute. Rank-status is used here
to refer to a system where the emphasis is
on the man, job evaluation to refer to a
system where the emphasis is on the posi-
tion.
Rank-status 1s a concept which is often
misunderstood and which, partly for that
reason, has evoked widespread claims, both
pro and con, that are as unrealistic as are
similar exaggerations concerning job evalua-
tion systems. “The only inherent feature of
the rank concept,” Stahl has said, “is that
status (pay, prestige, rights, ete.) inheres in
the individual regardless of the nature of his
assignments.’
In a rank-status system the various func-
tional areas of personnel administration are
oriented toward the man rather than toward
the position. Recruitment and selection, and
even salary, are based upon the long-range
needs of the agency. Recruitment and selec-
tion of the individual are based upon the
potential of the scientist or engineer rather
than upon his immediate usefulness. Hirings
and promotions under this concept look
toward accomplishing the agency’s over-all
objectives and goals even though Jobs and
programs may change from year to year. So
too, training emphasizes the next assign-
ment, at least, rather than increased ef-
fectiveness in the present assignment. A
forester could well characterize rank-status
as ‘“‘viewing the forest instead of the trees,”
while a social scientist might look upon it as
being based on the “inner man” rather than
upon the more mundane demands for food,
clothing, and a swept-wing motor car. The
rank-status concept gives more attention
to human relations and less to job relations.
It seeks to ‘oil the inner springs” of man, as
*Srauy, O. Gienn, Public personnel administra-
tion (4th ed.), p. 178. Harper & Brothers, New
York, 1950. See also pp. 181, 182, for the first sug-
gestion that the writer has found as to the useful-
ness of rank-status for scientific research work.
voL. 49, No. 1
someone has said, to motivate the man
rather than to emphasize reliance upon or-
ganization charts and other mechanistic de-
vices for facilitating the accomplishment of
the agency objectives. Rank-status may al-
most be thought of as a philosophy or a
“climate” within which men effectively work
toward a common goal, rather than to con-
sider it as a “system.”
The study covered selected plans for de-
termining the compensation of scientists
and of research and development engineers
in the field of mathematics, the physical and
biological sciences, and the medical and re-
lated sciences. In another sense, it was also
a study about people—the people who work
under the terms and conditions of those pay
systems—and the people of quality whom
the Government is seeking to attract to its
employment and to retain.
The pay plans which were compared with
the Classification Act of 1949 were:
The Los Alamos Scientific Laboratory
The Mellon Institute for Industrial Research
The British Scientific Service
The Public Health Service Commissioned Officer
Corps
Public Law 313, 80th Congress, Professional and
Scientific Service, Department of Defense
Public Law 692, 81st Congress, Public Health Sery-
ice
PAY SYSTEMS COMPARED WITH THE
CLASSIFICATION ACT OF 1949
I. LOS ALAMOS SCIENTIFIC LABORATORY
The Los Alamos Scientific Laboratory,
New Mexico, is an organization of the Uni-
versity of California which performs work
under contract for the Atomic Energy Com-
mission. Its personnel policies that have
been approved by the Atomic Energy Com-
mission are set forth in each contract. At the
time of this writer’s visit in 1953, raises of
$1,000 or up for persons receiving $12,000
or more per year could be approved by the ©
Los Alamos Field Office, A.E.C., without re- ~
ferral to the Atomic Energy Commission
headquarters office in Washington. The plan
here discussed covered some 50 senior staff
members and 845 staff members.
Under the contracts, salaries paid to per-
sons in the scientific categories must aver- |
age at the salaries or “‘salary line” computed |
JANUARY 1959
by least squares in terms of “dollars per
month” for up to 40 years beyond the last
degree granted. This permits hiring appli-
cants either above or below the salary line
or exactly on the line if management so
chooses. The supervisor is considered to be
the person best able to judge the merit of a
scientist or engineer and his contribution
to the program. “Supervisor” is here used
to indicate “levels of supervision” within
line management as differentiated from de-
terminations made by staff personnel as to
compliance with laws.
The conference of division leaders is the
key element in determining what monthly
salary will most nearly represent the value
of the individual scientist or engineer to the
laboratory for that year—all within the
frame of reference developed from the an-
nual survey of salaries and in terms of
equity with the salaries paid to other staff
members. In addition to various “salary.
line” measures, the personnel office prepares
‘“nictures” of the staff members in useful
eroupings through the use of mechanical
tabulating and other equipment. These
background data are then used by line
officials in conference in a very informal
manner. Part of this process has been de-
scribed to this writer as:
The technical organization is sensibly used to
provide an upward flow of ideas, feelings, and
arguments about the worth of individuals. We are
informal, very much so, but we do not operate in
a vacuum, nor do we play games with dollars and
people.
Very quickly, in such a process of looking at
people in terms of similar people, dollar-levels and
people levels become apparent; or reverse it 1f you
prefer: certain qualities of persons identify rather
precise dollar-levels. The exceptions leap to the
eye and demand correction. By slowing down of
money to people who are obviously overpaid and
the speeding up of money to those underpaid, a
“System” starts to be born. The factors are hu-
mans. The rating scales are humans. In all of this,
administration with a capital “A” supplies infor-
mation and assistance, maybe an idea now and
then, nothing more.
II. MELLON INSTITUTE OF INDUSTRIAL RESEARCH
The Mellon Institute of Industrial Re-
search, Pittsburgh, is an organization of the
*Personal correspondence from John A. Wood-
ward, wage and salary administrator, Los Alamos
oe Laboratory, Los Alamos, N. Mex., July
meLOOT
BUELL: PAY PLANS AND PEOPLE 3
University of Pittsburgh. At the time that
most of the information was obtained it was
organized for the purpose of “‘practical co-
operation between Science and Industry.”
Emphasis has subsequently shifted to fun-
damental research.
Salary levels for the Institute as a whole
were set in a manner somewhat similar to
that used at the Los Alamos Scientific Lab-
oratory. The salary lines were based upon
annual rather than monthly rates and com-
parison was based upon the age of the indi-
vidual rather than on the number of years
following the last degree.
Statistics were prepared each year. This
included sorting the employees according
to degrees held (bachelor, master, and doc-
tor) and then grouping according to the age
of the individual. The average salary of
each age group was plotted with respect to
age, and a straight line drawn to represent
approximately the average trend. This line
was used simply as a guide and not as a hard
and fast rule. The director of research ex-
plained that if an individual salary is above
or below the line by too great a distance
(particularly below), an adjustment 1s made
to minimize the discrepancy. The director,
subsequent to his retirement has recently
written:
There are always gross exceptions. But broadly
we have judged a man on the character of work
that he is doing, his accomplishments, on his per-
sonality, his relationship with his donor organiza-
tion, and of course in later years on the “cost of
living.” In research, as you know, it is the indi-
vidual and not the “position” that determines his
worth.’
III. THE SCIENTIFIC OFFICER CLASS
BRITISH CIVIL SERVICE
The scientific officer class is the highest
of the three classes of the scientific civil
service of Great Britain. It includes sci-
entists engaged in research, and scientists
and engineers engaged in research and de-
velopment. The fields of work covered are
substantially the same as those covered by
a large number of occupational specialties
which were under the professional service
of the Classifictaion Act of 1923 and now
are under the Classification Act of 1949.
Within the British service, however, the
OF THE
° Personal correspondence from E. Ward Tillot-
son, July 22, 1957.
4 JOURNAL OF THE
scientists and engineers are not ‘‘catalogued”’
either by themselves or by the personnel
system into as narrow specialties as is cus-
tomary in the United States. The Royal
Commission on the Civil Service, 1953-55,
reported some 3,400 employees in the seven
“srades” or ‘classes,’ each of which is
titled ‘‘scientifie officer’ with an adjective
being used to indicate the level.
There are two principles that constitute
the major base upon which the salary scales
for all British civil servants are built. How-
ever, the Royal Commission report stated:
It seems to us desirable that there should be one
set of principles of pay for the whole Service...
But this is not to say that there can be one short
formula that can by itself solve all wage and salary
problems.°
The principle of “fair comparison” (with
current remuneration of outside staffs em-
ployed on broadly comparable work, taking
account of differences in other conditions of
service) is the primary principle of pay. The
secondary principle is the maintenance of
‘Internal relativities.” Internal relativities
may be “vertical relativities’ between
grades within a class or service or may refer
to the relationship between classes engaged
on the same broad type of work. Internal
relativities may also be “horizontal relativi-
ties’ or comparisons between grades or
classes held to be of comparable status or of
roughly the same level of responsibility in
different hierarchies.
Most of the scientific officer grades have
a broad salary range wherein annual pro-
motion is customary and with fixed annual
increments. Some of the grades have a “bar”
in the middle of the range, beyond which
bar the scientific officer cannot pass without
affirmative action of a reviewing panel of
scientists. Once this action has been taken
he can proceed to the top of his grade range
by larger annual increments. For the chief
scientific officer grade there were two rates
of pay adopted, partly because there were
sufficient variations between the posts to
warrant it (job evaluation) and partly for
the advantage if it were necessary to recruit
* Royal Commission on the Civil Service, 1953-
55, Report, p. 23. Her Majesty’s Stationery Office,
London, 1955, Cmd. 9613.
WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. l
from outside the service. “Posts above chief
scientific officer” were ‘“‘broadbanded” on the
span of £3,500-£6,000 per year with no
stated intermediate steps.
Specialized posts in the higher grades are
occasionally filled from the outside. If the
applicant is from industry, the civil service
selection board (of scientists) will look at
his present salary and may appoint him at
one of the higher steps within the class to
which he would normally be appointed. It
could, if it wished, place him in a higher
grade if such action were needed in order
to recruit (or retain) a specific individual.‘
The principle of fair comparison makes
comparison with industry salaries feasible,
even though the government scientific offi-
cer salaries were considered by some to be
unfavorable compared with industry. In re-
cruiting for the very highest posts, public
advertisement is not favored. Instead,
...all government and other scientists of the
required standing are considered by high level sci-
entists and administrators, working in conjunction
with the Civil Service Commission, and the most
suitable individual available would be invited
[italics not in original] to accept the appointment ®
It may be noted in passing that the flexi-
bility in determining starting salaries for the
two lowest grades is limited to one salary
step. This flexibility in determining the
starting pay of scientists and engineers ac-
complishes in a direct manner that which so
often is achieved under the Classification
Act of 1949 only after a struggle—accom-
plished sometimes on merit as gauged by
job evaluation, but probably more often ac-
complished either with the connivance of po-
sition classification authorities, or by what
has been euphemistically called “outwitting”
the classification authorities.
Flexibility is also found in another pro-
cedure whereby under the “special merit
promotion scheme” posts may be created
outside the normal organizational hierarchy
for outstanding individual research workers.
This recognizes the value,
...of scientists of marked creative ability whose
advancement should not involve any break in their
7 Personal interview with H. J. Hadow, head of
United Kingdom Scientific Mission, July 31, 1957.
* Royal Commission, p. 130.
JANUARY 1959
scientific work; in such cases, subject to the recom-
mendation of a high-level selection board, the
Treasury may approve promotion on “individual
merit.”
An unusual characteristic of the British
scientific service is that the recruitment,
promotion, pay and other personnel proc-
esses are each scientist-oriented rather than
personnel technician-oriented.
IV. PUBLIC HEALTH SERVICE COMMISSIONED
OFFICER CORPS
The Public Health Service Commissioned
Officer Corps is composed of some 10 occu-
pational categories. The scientist officer
category includes those officers whose pri-
mary function is research, although others
may also do research to a lesser degree. The
research is both basic and applied, and may
be performed in the laboratory, in the field,
or in clinical situations. Some of the titles
carried by the officers include bacteriologist,
biochemist, psychologist, physiologist, and
protozoologist. There were somewhat more
than 200 scientist officers, as of August 1957,
of a total corps of close to 6,500.
The corps is a nonmilitary organization
of highly trained professional men and
women of many occupations. Personnel and
pay procedures are the same whether for the
scientist officer, the medical officer, or any
other category. The corps is made up of
officers who typically intend to spend most
or all of their working careers in the corps.
The pay system and the pay scales are
those of the military forces. Flexibility for
pay determination within a stated pay grade
does not exist. Judgments about an officer
applicant or about the promotability of a
Scientist officer are typically the result of
group judgment of his peers. Usually at
least one of those peers is in the same spe-
cialty field or the same professional field
as the person being judged. Provision exists
for “selection out” of the officers who are not
considered qualified for promotion by a
promotion board.
The organization rates and ranks the man
upon his over-all usefulness to the service.
This relieves the scientist officer of concern
as to whether an individual assignment
*McCrensky, Epwarp, Scientists in the British
! Civil Service. Science 124: 569. Sept. 28, 1956.
BUELL: PAY PLANS AND PEOPLE 5
might result in professional down-grading
such as might occur under the Classification
Act of 1949 for positions which are subject
to that Act. It is the responsibility of the
organization to place the scientist officer in
such assignments as are appropriate, when
possible. Thus rank—and assignments—fol-
low the man.
The rank-in-the-person follows length
of service in grade for permanent promo-
tions but it follows more closely the personal
ability of the man when it comes to tem-
porary promotions. Pay follows the rank to
which the officer is promoted, with the pay
grades being the same as for the military.
Although not tied directly to determining
annual salary, it is interesting to note that
sophisticated systems are used in applicant
rating by interview and file evaluation
boards and used in performance appraisal
and selection for promotion. While it 1s sig-
nificant that sophisticated systems are char-
acteristic of this corps, the fact that they are
used by typical scientist officers rather than
by personnel technicians or administrators
may be of equal significance to the corps
from the standpoint of morale.’®
V. PUBLIC LAW 313, 80TH CONGRESS,
DEPARTMENT OF DEFENSE
The act of August 1, 1947, usually known
as Public Law 3138, 80th Congress, estab-
lished a special pay system for professional
and scientific positions which were estab-
lished to effectuate research and develop-
ment activities of what were then known as
the War Department and the Naval Estab-
lishment.
Although World War II fighting had long
since ceased, the research and development
emphasis of national defense was not fully
achieved. Many competent scientists and
engineers were resigning from the activities
of the Department of Defense (then War
and Navy) for more lucrative positions out-
- side of the Federal Government. A one-day
hearing on H.R. 4084 brought testimony
from less than half a dozen officials, chiefly
military, that the work to be assigned em-
™® Basic material on the corps was obtained from
the writings of Sidney H. Newman, Ph.D., chief,
Officer Selection and Evaluation Program, and in-
terviews with him and with Paul M. Camp, chief,
Division of Personnel.
6 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
ployees under this proposal was of such
scope and responsibility as would normally
be assigned to an officer of the rank of
general. As to “why not make them gen-
erals?” Admiral Hussey replied that the
civilian scientists wouldn’t stand for it, that
they feared military regimentation. The
proposed positions were to be established
under a procedure “fully in accord’? with
section 13 of the Classification Act of 1923."!
Public Law 313 was a 3-paragraph act
which provided simply the following:
1. Each department was authorized to establish
fifteen positions in the professional and scientific
service, each being established to effectuate re-
search and development functions, and any and
all other activities which require specially qual-
fied scientific or professional personnel, provided
that the rates of compensation [then $10,000 to
$15,000] shall be subject to the approval of the
Civil Service Commission.
2. Appointments shall be made without competi-
tive examination upon approval of the proposed
appointee’s qualifications by the Civil Service
Commission or such officers or agents as it may
designate for this purpose. [It is noted that all
decisions have been made within the Commis-
sion, no delegation having been made to other
agencies. |
3. An annual report to Congress was required,
showing names of employees, functions per-
formed, and salaries.
At the time the rest of this statement was
prepared, Public Law 313 had been amended
to include not more than 120 positions in the
Department of Defense, 25 in the National
Security Agency, and 30 in the National Ad-
visory Committee for Aeronautics. Due to
Public Laws 85-462 (June 20, 1958) and 85-
568 (July 29, 1958), the present (January
1959) authorizations under Public Law 318,
as amended, are: Department of Defense,
292, National Security Agency, 50; Interior,
5; Agriculture, 5; Health, Education, and
Welfare, 5; and Commerce, 25. [In January
1959, in addition to the authorizations of
Public Law 318 listed above, there are some
380 other positions authorized under the.
same general philosophy. These include 85
in the Public Health Service, which are dis-
cussed under Public Law 692, and 260 in the
National Aeronautics and Space Agency.]
™“U. 8S. Congress, House of Representatives,
Committee on Post Office and Civil Service, Re-
port to Accompany H.R. 4084, July 16, 1947, House
Report 953, 80th Congress, Ist Session, 3 pp. (Not
printed.)
VoL. 49, No. l
The first review of a submission received
by the Civil Service Commission (typically
received as a “name case’) is in terms of
the Classification Act of 1949. Is it a scien-
tific or professional position established
within the requirements of P.L. 313 and
what would be the grade level of the position
if it were under the Classification Act of
1949? This preliminary evaluation includes
consideration of the following factors:
1. The nature, magnitude, and scope of the
agency’s research and development program and
its relation to the international situation.
2. The career of service and the scientific ac-
complishments of the incumbent.
3. The approximate comparison as to scope of
program and weight of responsibility with other
jobs which may be comparable.
4. The nature of the agency’s organizational
structure.
5. Whether during a transitional period there is
an attempt to maintain consistency between the
former pay rate and the proposed pay rate in the
total range of pay.
The second and fifth items are factors not
used in the evaluation of Classification Act
positions.
Following this, a comparison is made be-
tween the salary recommended by the
agency and the GS grade appropriate if it
were under the Classification Act. This is
done by dividing the P.L. salary range into
three subranges approximately equal, each
subrange to be roughly the equivalent of one
of the three ‘‘supergrade” levels, GS-16, 17,
and 18. Conformance to this rough guide
would result in recommendation by the
Personnel Management Review Division
that the salary be approved, subject to re-
view of the qualifications of the man by the
Examining Division. It is believed that no
case has been rejected on the qualifications
aspect that had been approved by the posi-
tion evaluation. Where disparity exists be-
tween salary range that would appear ap-
propriate from the position review and the
salary recommended by the agency, a con-
ference is held with agency officials, seeking ~
additional information concerning the man,
the program, or the scarcity of men of the —
required qualifications. A denial of an
agency recommendation would come only —
after such inquiries had been made. The -
Commission no longer determines on its own —
initiative what the appropriate salary is. It
JANUARY 1959
either accepts or rejects the recommendation
of the agency. An agency may resubmit a
case with a different recommendation if it
chooses.
While the Commission studiously avoids
taking original action that is the responsi-
bility of the agency, it appears to be equally
desirous of avoiding a rubber-stamp role,
requiring substantially equal justifications
for recommendations of changes of salary
downward that it requires on changes up-
ward.!?
As with super-grades, each military
agency has two administrative problems—
approval of a Public Law 313 “space” and
getting the man for the space. Approval of
the space is internal within the Depart-
ment of Defense, yet the layers of review
of proposals may be far more time-consum-
ing and hazardous than obtaining salary
and qualification approval from the Com-
mission.
VI. PUBLIC LAW 692, 81ST CONGRESS,
PUBLIC HEALTH SERVICE
The Act of August 15, 1950, was identical
to Public Law 313 except that it applied to
the Public Health Service.
Senate Report No. 1102 described the
reasoning back of this pay system that was
established outside of the Classification Act
of 1949, saying,
Authority to pay reasonable salaries to out-
standing scientific and professional persons en-
gaged in research is essential if the quality as well
as the quantity of medical research is to increase.
The full potentialities of the whole research
staff of the Public Health Service can be brought
out only if those who guide its research activities
combine research talents of the highest order with
ability to stimulate others and administer large
programs. This combination of talents is rare. Per-
sons who possess them command high salaries.
The personnel manual of the Public
Health Service contains statements con-
cerning the approving authority, general
policy, promotion policy, eligibility criteria
for individuals, determination of salary
levels, and processing procedures that are
“Most of the material concerning administra-
tion of P.L. 313 within the Commission was ob-
tained in interview with Ralph Remley, chief,
Classification Appeals and Special Services Office,
U.S. Civil Service Commission, April 2, 1957.
BUELL: PAY PLANS AND PEOPLE vi
unusual in setting forth useful criteria suc-
cinctly for all interested parties. The desig-
nation of these positions and the determina-
tion of salary levels are considered part of
the career development program that cannot
be met within the commissioned corps or the
Classification Act pay systems. The posi-
tion and the salary will be identified with
the incumbent or prospective incumbent and
will exist only during the period that the
position is occupied by the incumbent. This
recognizes administratively the rank-status
basis of Public Law 692, rather than con-
sidering it merely as an extension of the
Classification Act with the “position” con-
cept.
The manual contains criteria for de-
termination of salary levels. There are two
general guides that apply to all categories
of P.L. 692 personnel, these elements being:
1. An assessment of the demonstrated compe-
tence of the candidate, whether applicant or in-
cumbent.
2. The extent to which competition for scarce
manpower or other factors tends to raise non-
government salaries.
The three categories of personnel each have
a separate and additional criterion, as fol-
lows:
1. Independent Investigators
Up to $15,500—may be paid to those who are
fully competent, mature and highly produc-
tive.
Up to $17,500—may be paid to those of excep-
tional competence with international reputa-
tions.
Up to $19,000—may be paid to those who are, by
general consensus, recognized as fully compe-
tent to occupy the most distinguished aca-
demic chairs or to assume key research posi-
sions in industrial research.
2. Clinical Specialties—may be paid salaries gen-
erally comparable, within the $19,000 ceiling,
with the total earned income of their counter-
parts in academic teaching and research posts,
but not with the income of those engaged full
time in the practice of medicine.
3. Program Leaders—the importance and com-
plexity of the position, and the size and com-
plexity of the program for which the incumbent
is responsible.
The manual also provides that, in formu-
lating their reeommendations, chiefs of bu-
reau as well as chiefs of division may
utilize the technical advice of such groups
of professional peers or supervisors, of the
8 JOURNAL OF THE
sandidate or incumbent as they may de-
termine to be needed.'*
VII. OTHER SYSTEMS
The Battelle Memorial Institute, Colum-
bus, Ohio, has had a form of rank-status
since it was founded in 1929. Its former
metallurgist director has said,
The ideal criterion for personal recompense in
any business is productivity [italics im original].
The persons who produce the most deserve the
MOSt pay...
...In modern research this difficulty of meas-
uring productivity is imereased many fold....
To take the results of team research and to say that
this percentage is creditable to that person’s efforts,
is to destroy the structure that makes research
effective. Consequently, we must use empirical
rather than mathematically precise means to eval-
uate each man’s worth. We do this by appraising
other qualities of the imdividual that experience
tells us are usually related to his productivity.
These qualities determine the “merit” of the
technical man to the research organization, and
salary increases based on such evaluation are
called merit raises.”
Every staff member’s situation is reviewed
quarterly; there are no standard or auto-
matic increases of any type, and no arbi-
trary rules for determining the amount of
increases, if any, to be given at any one time.
These appraisals rely heavily upon evalua-
tion of personal traits. Among these are
initiative, willingness to put out some extra
effort, tenacity to follow through, and eco-
nomic ‘sense’ superimposed on the basic
technical knowledge required. Other traits
evaluated are salesmanship (including re-
port writing—because their only product is
the research report—and vocal presentation
and interpretations of the user’s needs), ad-
ministrative talent, and, importantly, sci-
entific integrity and selflessness.
The policy at Standard Oil Co. (of New
Jersey) apparently recognizes the inade-
quacy of job evaluation as a basis for pay
for research workers. In an answer to an
inquiry from the writer concerning rank-
status the manager of the Employee Rela-
tions Department wrote as follows:
** Basic material on administration within the
bureau was obtained during interview with Paul
es nD chief, Division of Personnel, August 15,
s WILLIAMS, CriybE, Bases research worker salary
structure on merit system. Industrial Science and
Engineering, January 1955: 33.
WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. l
Job evaluation does not seem to be appropriate
to professional engineers and scientists because
none of them perform according to a job descrip-
tion. Job classifications are based primarily on tra-
ditional relationships between jobs, skills required
and responsibility exercised. The professional em-
ployee’s effectiveness depends on his individual
contribution within a team effort. Perhaps a more
important factor determining pay is the condition
of supply and demand. It sets salaries far more
than a job classification. The very large turnover
among professional employees in research organiza-
tions 1s an indication of the dominance of economic
factors over rigid classification systems.”
During the summer of 1957 General Elec-
tric was in the process of changing some of
its personnel and pay policies, and so was
not in a position to discuss plans which it
expected would be installed. Bearing upon
the goal sought by some persons of having
a single pay system for all civilians in the
Federal service, the multiplicity of plans
within GE is of interest. A consultant with
GE has written,
As a part of our broad decentralization program,
substantial latitude is provided for managers of our
decentralized departments in establishing the par-
ticular practices they believe most appropriate for
their particular operations. As a consequence, it is
difficult to generalize and develop statements that
are truly accurate for the General Electric Co. as a
whole. We have, for example, more than 35 position
evaluation methods now in use in our Company.”
The consultant called attention to the
1957 report of the Defense Advisory Com-
mittee on Professional and Technical Com-
pensation, of which Ralph J. Cordiner
(president of General Electric) was chair-
man. The point was made that the report
contained statements of some of the basic
concepts which are considered, at General
Electric, to be important in the development
of compensation structures and suitable
compensation relationships. ;
The chart herewith, ‘Generalized Com-
parisons Between Various Aspects of Se-
lected Pay Systems,” is a summary of some
of the comparisons between the seven pay —
plans given major attention.
* Personal correspondence, a statement pre- |
pared by research people as an attachment to a ©
letter signed in the name of R. L. Mason, manager,
Employee Relations Department, Standard Oil
Con New Yorks NaN July 1955s ‘
*’ Personal correspondence from L. L. Ferguson, |
consultant, Employee Compensation Research, ©
General Electric Co., New York, July 17, 1957.
|
|
EN VaRrous ASPE
me instances base
+
Public Healt]©22 ( ae Health Service)
+
His. Pay is Pena aye 3 S. is usually based on the MAN.
Ss. enoirased: al? is same as for P.L. 313.
be specified ranks
in- tions.
pi-
Be
} Pay PA mistrate eo P.H.S. is geared to long-range
a career development program that
under P.H.S. Commissioned Officer
issification Act. Within C.S.C. it is
iate job, as is case with P.L. 313.
afic | Assignments are
ied tist officers.” I
to a few “‘resti
self.
Ae
pet | Assignments to 1)
reduction in ri
ticed—it reliev
individual assi
sef- | No immediate e}
by considered by
2d
for
6 : :
Pema pnlicants tor gupplicant is same as for P.L. 313.
is fecsional exani2s are made initially by chiefs of
lial Peeeennand. e| (professional men) who are encour-
be en teachalcal advice of groups of ‘‘peers”’ or
bt- eae writteed: All line officials over a P.L. 692
| le . Action in Dept. of Health, Educa-
| not learned.
jen Employees are ev
A choice rating |
attitudes & ja
used for prom
mine |Group Sealuatic® & determinations are made same
ich Fpeae Somme off that in C.S.C. a group—commis-
Lst Renoticers aremendations of an individual position
Ee Paar ale evaly *8ency recommendation. In P.H.S.
= Beem associq one) frequently acts wpon a recom-
ial Pee dalinuat of professional peers.)
selection boar}
Bre || Oriented towarke® toward position classifiers and
EL pee iasioned? C.S.C. level; and to professional
aS Be cengir scientists and engineers) at the
' —)
Pay Plan Aspects
1. Pay based primarily or entirely on the MAN or on
the JOB?
Los Alamos Se ee Laboratory
( |
Pay is based on the MAN,
R
2. Pay geared to accomplishment of long-range or
short-range objectives of agencies?
3. Assignments based on pay or rank—or pay or rank
based on assignments?
4, Effect of assignment to lower level work.
See
5, Bifect of assignment to higher level work,
EE
f. Methods of evaluating the MAN. a>)
A. Applicant evaluation based on: scholastic his:
tory, potential, or work-or-siliry history.
B, Bimployee evaluation based on: job performance
or empirical solutions designed to represent job
performance which is considered to be immensur
able directly.
7. Making of salary determinations or effective recom
mendations for sume:
A. As to person or group making thom,
B. As to extent to which they are made by “peers,”
ie., by scientists and engineers (S & 1's).
§. Orientation of salary plan and its administration,
Pay administration is geared to long-range program
with considerations of the man’s potential & expected
achievement at end of, say, next 5 years,
Assignments are based typically on pay of the scientist
or engineer, (High quality job performance miny |
enuse & salary increase? Lack of quality may couse
salary stagnation.)
No effect unless it is permanent or prolonged and due
to lack of competence,
No immediate effect, Quality of work done may result
in higher salary from next salary review.
Applicants ive evaluated on basis of education (kind
of degree) und comparison with curve of salaries of
other 8 & M's in U.S. for the same number of years
beyond Inst degree earned, Potential is included,
Employees’ evaluation includes the above, plus evalua
tion of last year's work and comparisons with other
employees.
Supervisory scientists initiate the salary recommenda
tions and the division lenders’ conferences make ef
fective review of these recommendations, though not
nocessurily having the last word,
Oriented toward line management, (Line Manage:
ment! here is a group composed of the senior scientists
or engineers.)
Mellon Institute
(
Pay based on the MAN
(Conelusions based upon study of the sy:
GENERALIZED COMPARISONS BETWEEN Vartous Aspects OF SELECTED Pay SYSTEMS
stems — in some instances based upon inference rather than specifie facts found)
British Scientific Service
(C)
Pay is based primarily on the MAN, for higher levels.
Broad job evaluation is used for most posts in B.S.S.
but at the higher levels
placed in « higher grade if nec
dustry or to retain. (Job evaluation for B.S
cally a means of determining posts to which men of spec-
ified rank are normally assigned.)
G
from in-
is typi-
ssary to recr
ntifie officers’ may be
|
Public Health Service Commissioned Officer Corps
(D)
Classification Act of 1949 as Amended
Pay is based primarily on the MAN. A job evaluation plan
is not used, although some specific higher posts carry |
Specified ranks «& may be filled through “‘spot’’ promo-
tions
Pay is based on the JOB. Job evaluation plan is based
on duties, responsibilities and qualifications required.
It is used to place the position in a “eclass’’ to which
is attached a specific pay range.
Apparently it is the same as for Los Alamos although
no direct information was obtained.
Same as Los Alamos
Same ns Los Alamos.
Same as Los Alamos
Easentinlly the same as for Los Alamos, except (1) sal-
ary history is based on age rather than on years since
last degree, and (2) the acceptability to (or relation-
ship to) the doner organization in regard to salary.
Salary recommendations
made by persons who were scientists or engineers. It
is not known whether group action was used in mak-
ing the determinations,
Same as Los Alamos,
Tr a = a syoereas nd Pe " oe . x = 2 5 rane
(Note: ‘Job Byaluation” is used in the general sense of analysis and evaluation of the dutios, responsibilities, and qualifications required for minimum satisfactory performance requ
Pay administration is geared to long-range objectives.
| eae
Pay administration
s geared to long-range objectives
Pay administration within D.O.D. agencies is geared to
short-range objectives—to the immediate job to be
done.
Assignments are based typically on rank of the scientific
officer. Occasionally for higher posts it will be reversed
and “spot”? promotions used.
Assignments are based typically on rank held by “‘scien-
tist officers.” However, rank and pay of those assigned
to a few “restricted’’ positions are based on the job it-
self.
Assignments to lower level work typically have no effect
on pay or on future assignments.
Assignments to lower-level work would not be the cause of
reduction in rank or pay. Career management is prac-
ticed—it relieves the man of concern as to whether an
individual assignment might harm his pay or career.
Pay is based on assignments which have been evaluated
by job evaluation & assigned to a class (including |
grade level). “Details” (supposedly of short dura
tion) involve no change in pay.
Grade and pay are lowered if found on survey or job
audit—unless management is given opportunity to |
reassign duties or employees. Pay is not lowe
few “savings” cases provided for in the Act.
Assignments to higher level work haye no immediate ef-
fect. Level and quality of work would be considered by
next promotion or selection board (for promotions to 2d
and 8d levels “without waiting for a vacancy,” or for
individual merit” positions).
promotion to
No immediate effect. Level and quality of work would be
considered by next selection board.
irade and pay would be raised if the S & If is legally
qualified for such grade
determinations
Applicants are evaluated, for entrance to lowest grades,
on basis of review of scholustic honors (unity. degree
with Ist or 2d class honors required) & on potential
for growth, by means of oral & written exams «& refer-
ence chec Tor higher levels, graduate work, accept-
able work history, & salary history are used, including
industry pay.
Employees are evaluated on basis of record obtained when
upplicants, plus annual job performance evaluation A
and B, seek to determine the man’s stage in growth.
Salary recommendations (usually tantamount to determi-
nations) are made by panels of senior scientists which
have some leeway in determining starting pay at lowest
two levels & may authorize placing an applicant from
industry, or an employee, in higher grade if necessary
to attract or retain in B,
merit posts (subject to Tr
S. May promote to spe¢ial
ury approval).
Applicants for first 2 levels always are given written pro-
fessional exam, un oral interview, a file exam (entire
background, education, training, & experience, & super-
visor & teacher reference checks). For full grade & above,
oral & written exams may be waived.
Pmployees are evaluated annually on job proficiency, forced
choice rating by worker-associates, & measures of work
attitudes & job performance items. Selection boards are
used for promotions «& selection-out.
NOT APPLICABLE:
eable, because the po:
from the MAN.
(A) nor (B) is appli
jon is evaluated separately
Group evaluations are used for pay & tenure determina-
tions. Some or all of applicant-interview panel of scien-
tist officers are in same professional category as the appli-
cant; file evaluation board members are scientist officers;
worker-associates ratings are by ‘“‘peers’’; investigation
boards must contain one member of same profession;
selection board is also a “‘peers”’ group.
Positions of S & B's typically are classified in agencios | Wffectiv
by position classifiers (who are not also S & 1's unless |
by chance) or by administrative or personnel officials
on classifier recommendations. Group evaluation is |
seldom used (P.H.S. uses). For supergride 8 & [po
sitions, C.S.C. commissioners have lately delegated
their authority to C.S.C. classifiers.
To a considerable degree it is oriented toward line manage-
ment scientists and engineers. In addition, the job eval-
uation used in part does not have the degree of orienta-
tion toward the personnel technician that is found in the
Classification Act of 1949,
red by a position)
Oriented toward line management which here is that of
commissioned officers of whom some are scientists and
some are engineers.
Oriented toward one specialty of personnel technician
the position classifier.
Public Law 313 (D.0.D. Agencies)
(PF)
Pay consideration in agencies of 1.0.1. varies. Tt may be |
either based on the MAN or the JOB. C.S.C. determins
tion is based primarily on JOB—with the MAN’s quali
ons sometimes influencing doubtful cases,
flew
Pay administration within D.O.D. agencies is geared usu
ally to long-range objectives; within C.S.C. it is geared
to the immediate job to be done
C.S.C. typically bases pay upon assignments, Once this
has been done, agencies typically assign S & Bs upon
the basis of salary and ability, (See 8. EB. concerning
“details.”)
| There is no known effect if assigned to lower-level work
except that if it appeared in position descriptions or cer
tifications required periodically by C.S.C, it would pre
sumably affect pay adversely, Management may initiate
aetion,
If duties are to remain of a higher level, presumably the
agency would request review by C.8.G. and a higher
alary. C.S.C. would not initiate it,
| ©.S.C. evaluation of applicant is based on S.10. 67, Appli
cation for Bederal Employment, plus agenoy letter
of transmittal-sometimes supplemented by addi-
tional information from applicant, ov from “Amerioan
Men of Science,”’ ete. Agency & D.O.1D, evaluations
vary greatly as to kind,
Sume as above, if not already in the file,
minations are made by the Con
trained, unless by chance.
Che total system partakes both of orientation toward po-
sition classifiers and, in some agencies, of orientation
toward administrative or military personnel (rather sol-
dom oriented toward scientists and engineers).
©.8.C. evaluation of applicant is same as for PT
recommendations are made by position clussifier
(if more than one, the others are reviewers), Final deter-
oners a8 & group.
No one in C.S.C. is a practicing scientist or engineer.
None who pass on these matters would haye been so
Public Law 602(Publie Health Service)
(G)
‘ty consideration in PHS, is usually based on the MAN,
©.S.C, determination issame as for PL, 318.
Pay administration within P.HLS. is geared to long-range
objectives as part ofa career development program that
oan not be achieved under PWS, Commissioned Officer
Corps or under Classification Act. Within G.S.C, it is
geared to the immediate job, as is onse with PL, 818.
me as for PL, 8th.
Sume as for PL, S18.
Samo as for PL. Shh,
PALS. recommendations ave made initially by chiefs of
Durenus ov divisions (professional men) who are encour=
aged to use the technionl advice of groups of “peors’’ or
of supervisors as needed, All line officials over a PL, 002
mun ave professional Action in Dopt, of Wealth, Mduen-
tion, & Welfare was not lenrned,
Sime ns above,
C.8.C. recommendations & determinations are made siine
us for PL, 818, (Note that in O.8.C, 2 group commis
sioners—acels on recommendationa of an individual position
classifier review of the agency recommendation, In PIS.
i line official (professional) frequently acta upon a recom
mendation of a group of proferxatonal peers.)
The system is oriented toward position classifiers and
ndministrators at the C.8.C, level; und to professional
personnel (including scientista and engineers) at the
P.ILS, level,
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Yb
JANUARY 1959
CONCLUSIONS AND RECOMMENDATIONS
The facts and opinions assembled during
this study furnished convincing evidence
that categorical and sweeping generaliza-
tions on the subject of rank-status for scien-
tists and engineers would be hazardous.
They might be as unsound as the chant,
“Four legs good, two legs bad,’ used by
some of George Orwell’s animal characters
as a means of differentiating the “good”
animals from the “bad” humans in his Life
on the animal farm. In one sense, rank-
status may be considered to be almost a
philosophy or a symbol of principle rather
than necessarily a pay plan.
Aside from the Classification Act of 1949,
as amended, all the pay plans studied in de-
- tail represent, to this writer, variations of
rank-status pay plans. The matters of prin-
cipal interest in this study are the variations
in the degree to which pay is based upon
the qualifications of the man or upon the
production of the man rather than the duties
and responsibilities of the position.
Although there is a common philosophic
approach to the problem of pay, in practice
there are restrictions of one kind or another
which result in a variety of methods used.
On the other hand, the Classification Act of
1949, as amended, which furnished the point
of departure for the study was the single
strictly job evaluation plan that was stud-
ied. More scientists and engineers in re-
search and development are paid under the
Classification Act of 1949 than under any
other pay system. It is useful, therefore, as
a specific against which to compare other
systems. But to consider the Classification
Act as being “THE” job evaluation plan and
representative of industrial job evaluation
plans would be grossly misleading. Indus-
trial plans for job evaluation not infre-
quently include evaluations of the contribu-
tions made by the individual as well as
evaluations of the duties and responsibili-
ties that are assigned by management and
of the working conditions as they are found
to exist. An example of such a composite
plan for evaluating creative engineers has
been described by Chaffee.1* In addition to
“ CHAFFEE, RANDOLPH W., Evaluating engineers
to recogmze talent and reward achievement. Ma-
chine Design, June 1951: 143-172.
BUELL: PAY PLANS AND PEOPLE 9
the duties and responsibilities of a position
that would be measured under the proce-
dures used in organizations whose positions
are under the Classification Act of 1949,
numerous personal qualities would be meas-
ured, as would job performance. The total
evaluation, if scored high enough, would
place the incumbent in a merit subgrade.
This technique is in accord with the more
generalized proposal of the Purvis commit-
tee for premium salary “which will give
recognition to the skills and _ abilities
brought to the job by the individual... over
and above job evaluation techniques now
used to determine an incumbent’s grade and
Payene?
This study may be considered to be a
comparison between one specific type of job
evaluation plan (the Classification Act of
1949, as amended) and several other pay
plans, each of which has some of the “flavor”
of rank-status.
SUMMARY OF CONCLUSIONS
1. Conclusion: Research and develop-
ment personnel is an unusually rapid grow-
ing occupational group in the work popula-
tion of the United States today, yet it 1s wn
short-supply when considered against cur-
rent needs—especially as the needs relate to
the defense of the nation. This group, with
its high professional standards and work-
ing habits and with a different kind of logic
from that characteristic of nonprofessional
personnel, has attitudes that are hostile to
many aspects of administration. Personnel
administration as it has been practiced on
them is typically anathema. Salary and
prestige associated with their professional
attainments mean much to scientists and
engineers—although not to the exclusion of
adequate salary. The “social handles of the
pay cup” concept which emphasizes the so-
cial aspects or prestige that follows the pay
itself is important to scientists and engi-
neers, although apparently not to the extent
found by Whiting a quarter-century ago in
his study of laboring groups.
Because of a combination of salary prob-
*%U. S. Congress, Senate Committee on Post
Office and Civil Service, Administration of the
Classification Act of 1949 and the compensation
process established by the act, Senate Document
34. 83d Congress, Ist Session, p. 22. 1953.
10 JOURNAL
lems (e.g., comparisons with the trades and
crafts) and lack of attention by manage-
ment to status and recognition for their
work, scientists and engineers are either ‘‘on
the move” or at least are preconditioned to
accepting an offer of employment from an-
other organization. Absurdities and _ ex-
tremes have existed in the use of status and
prestige symbols, ranging from the kind of
carafe available to an executive, to parking
lot privileges, to priorities in obtaining Asi-
atic flu vaccine, and to other more tangible
rewards. The fact that absurdities have
existed has not blinded many organizations
to the value of a reasoned use of status and
prestige. The conscious use of status in the
Western world is again becoming respect-
able. It will probably become increasingly
recognized now that the launching of the
Russian “‘sputnik”’ as the first earth satel-
lite has caused additional attention to be
focused, perhaps belatedly, upon the prob-
lems of training, recruiting, and retaining
an adequate supply of quality scientists and
engineers.
2. Conclusion: Different principles and
practices in personnel administration are
needed for scientists and engineers in re-
search and development than for persons in
other occupations and functions. Scientists
and engineers do not usually fit into the
administrative process either by personal
traits or by process or function. “Supervi-
sion” is a term that is anathema to them,
particularly so the closer one gets to basic
or “pure” research or to the higher levels of
research and development. Especially in
these areas the organizational structure
tends to emphasize the man rather than the
position. Personnel administration as de-
veloped by personnel administrators who
are not scientists or engineers is especially
obnoxious to them—they object to having
such personnel administration “applied to
them.” Because of these things, adminis-
trators attempt to adjust both the substan-
tive work organization and the facilitative
organizations to conform to the needs of the
personnel who are to accomplish the mission
of the work organization. In the facilitating
organizations which are responsible for the
personnel administration function this is
most noticeable in the reduction in proce-
OF THE WASHINGTON ACADEMY
OF SCIENCES VOL. 49, No. 1
dures and in the use of “committees of
peers” for decisions in the personnel areas.
As Boehm quoted a research director, “Re-
search can be managed in a businesslike
way, but not in a way like other business.””?”
3. Conclusion: The subject of rank-status
or rank-in-the-person has been discussed
for only about two decades in the United
States but neither the concept nor the ap-
plication is of recent origin. Extensive ap-
plication of the concept existed in the gov-
ernment of China during the early centuries
of the Christian Era. In the Western world
it appeared in the military, in the Catholic
Church, in the civilian governmental organi-
zations of European and other areas, and in
United Nations organizations before consid-
eration for use in civilian government situa-
tions in the United States. Beginning with
the proposal by Graham in 1939, the sub-
ject has come to be increasingly in the pub-
lic eye as a result of recommendations of
congressional and presidential committees,
and the writings and speeches of public-
spirited groups and individuals from many
walks of life who have broad knowledge of
public affairs. Among the groups which have
favored emphasis upon rank-status or at
least further study of the usefulness of rank-
status to the Federal Service are: the Ad-
visory Committee on Natural Scientists
(1942), the Senate Committee on Post Office
and Civil Service (1953, Purvis Commit-
tee), the Commission on Organization of the
Executive Branch of the Government (1955)
(the second Hoover Commission), the Sixth
American Assembly (1954), the Society for
Personnel Administration (1955), and the
Defense Advisory Committee on Profes-
sional and Technical Compensation (1957,
Cordiner Committee). Some of these groups
were studying government as a whole, while
others concerned themselves specifically
with the work of scientists and engineers or
with administrative personnel.
4. Conclusion: In research and develop-
ment the degree of development of the scien-
tists and engineers may be of more impor-
tance than their precise duties or the
particular work assignments by their super-
* BoEeHM, GerorcE A. A., Research management:
The new executive job. Fortune 54(4): 222. Octo-
ber 1957.
JANUARY 1959
visors. This is signally the case in basic re-
search done by an individual or by the team
approach to either research or development.
Assignments to a scientist, especially, may
be couched in the most general terms. They
may sometimes only name the area of study
that management is interested in. In other
instances, a general outline of study that is
defined by management may be deviated
from to a high degree because of the scien-
tist’s findings or because of lack of specific
findings at intermediate points. Deviations
may also occur because of ‘“‘fringe thoughts”
—random thoughts that have come to the
selentist, seemingly “‘out of the blue,” as a
result of his lifetime of preparation in col-
lege or university plus the complex of his
later experience. The work assignment to
two scientists or engineers may be the same,
especially under the team approach, but the
contributions of an Einstein may be far dif-
ferent from the contributions of a John Doe,
Ph.D. Classification of a research and devel-
opment position independent of an examina-
tion of an individual’s qualifications and
potential has been referred to, with some
justification, as an absurdity, and classifi-
cation without regard to performance as
nonsensical.
5. Conclusion: The job evaluation or po-
sition classification concept that “if work
(duties and responsibilities) can be assigned
at can be described and can be evaluated”
falls short of realization for research and
development positions.
This is either the conclusion or the gen-
eral implication of Graham (1939), Steel-
man (1947), the Senate Committee on Post
Office and Civil Service (the Purvis Com-
mittee—1953), the Chief, Bureau of Ord-
nance, Department of the Navy (1949),
Wengert (relating to job evaluation systems
in general—1950), Renzetti (1952), and
various technical directors of research.
Others who have also held similar opinions
include Mason (1955), Clyde Williams
(1955), and the Defense Advisory Commit-
tee (the Cordiner Committee—1957).
6. Conclusion: Job evaluation plans (in-
cluding the Classification Act of 1949) are
typically unsatisfactory tools with which to
determine the salary of scientists and engi-
neers in research and development. Measur-
BUELL: PAY PLANS AND PEOPLE let!
ing the duties and responsibilities of scien-
tists and engineers by job evaluation
techniques is difficult in itself and, when
obtained, often does not measure the value
to the organization of the scientist or engi-
neer. One of the reasons for this is that Job
evaluation plans used in the Federal Gov-
ernment, at least, are not designed to evalu-
ate the effect of the man. In research and
development the abilities of the scientist or
engineer so often have greater effect upon
his contribution to the research program
than do the assignments of work and respon-
sibility made by the supervisor.
It is difficult to evaluate scientific and
engineering research and development posi-
tions and to evaluate the qualifications and
the abilities of the scientists and engineers
themselves. It appears to be equally difficult
to appraise the value of the work product
of such scientists and engineers either when
engaged in individual research or team re-
search. It is difficult for scientists and engi-
neers themselves to make these evaluations
even if they are research and development
administrators in charge of the total work
operations. It is still more difficult in many
of those areas for a person to make valid
evaluations if he is not a scientist or engi-
neer.
There has been much criticism of the
Classification Act of 1949, as amended, as
a tool for measuring the difficulty and re-
sponsibility of positions—of work assign-
ments made to scientists and engineers.
There has also been criticism that the Clas-
sification Act is designed to measure only
the difficulty and responsibility of positions
with the objective of achieving “equal pay
for equal work,’ whereas what should be
measured is the total contribution of a man
to the research and developmént program
in which he is engaged. There also has been
much criticism of various systems used to
appraise the worth of individuals, whether
in meeting the qualification requirements of
the Civil Service Commission for appoint-
ment or promotion or in the area of per-
formance appraisal. Particular criticisms
and cautions have been voiced against plac-
ing too much reliance upon systems which
use techniques which involve numeric treat-
ment or obtain results which in some other
12 JOURNAL OF THE
way have an aura of exactness that is mis-
leading.
It would be hazardous to believe that
either simplicity or sophistication in evalu-
ation techniques is, by itself, either desir-
able or useful. Rules of thumb in these areas
would produce serious inequities as may
complicated systems, which produce ‘“reli-
able” though “invalid” results. So-called
“objective” systems (which frequently are
also sophisticated) are subject to the same
possibility of creating false illusions of ac-
curacy in measuring what they purport to
measure.
Job evaluation techniques and man eval-
uation techniques have been developed in
some few situations that afford promise of
much greater usefulness than is character-
istic of the Classification Act, for example.
Typically, however, reliance on any tech-
mique to the exclusion of the considered
judgment of operating personnel would be
unduly optimistic at this time.
7. Conclusion: The present inadequacies
of many sophisticated job evaluation plans
and man evaluation plans and the criticism
that results from such inadequacies empha-
size the need for much additional research
and development in these areas of personnel
administration. The fact that many tech-
niques fall far short of what is desirable in
measuring either research and development
positions or in measuring the scientists and
engineers themselves should not lead to the
conclusion that these decisions should in the
future be made as snap judgments or made
by intuitions without an array of informa-
tion available to the authority who is to
make the decisions. In the Los Alamos Sci-
entific Laboratory and the Mellon Institute
much material is gathered for the authori-
ties who recommend or determine what the
salaries will be for the individual scientists,
but so far as the actual evaluation of Scien-
tist John Doe is concerned the processes that
are used are unsophisticated. On the other
hand, some of the evaluation techniques
used within the Public Health Service are
sophisticated. In each of these organizations
and in the British scientific service the tech-
niques used are planned as azds to an evalu-
ation by man—not as a substitute for man’s
judgment. On this point Worthy and Ur-
wick each considered that the various meas-
WASHINGTON ACADEMY OF SCIENCES
vou. 49, no. 1
ures of the objective and sophisticated vari-
eties could be very useful to the executive,
but that they would be used to “sharpen
his judgment” rather than replace it.
8. Conclusion: The Classification Act of
1949, as amended, appears to be more criti-
cized for positions of scientists and engi-
neers in research and development than for
positions in other fields of work. The criti-
cism in this area comes from employees and
management alike. It was found, however,
that serious criticism of the Classification
Act was not universal, for in some cases
there was found the belief that the adminis-
tration of the Act was more to be criticized
than the Classification Act itself.
9. Conclusion: Rank-status pay plans for
scientists and engineers recognize (1) the
unsuitability of the usual job or position
evaluation techniques to research and devel-
opment work, and (2) the antagonism of
research and development scientists and en-
gineers to a job evaluation form of adminis-
trative stricture with its concomitant lack of
recognition for personal contributions. Part
of the unsuitability stems from the previous
conclusion which emphasizes the develop-
ment of the man rather than the job assign-
ment. This suggestion by Graham in 1939
was corroborated by the Advisory Commit-
tee on Natural Scientists which looked on
the caliber-of the job as being a reflection
of the man 2m the job and that the classifi-
cation should rest upon the research con-
tribution of each man. The unsuitability
question was again raised in 1947 by Steel-
man—unsuitability both as to present clas-
sification principles and classification tech-
niques for many research and development
positions. Renzetti differentiated between
the degree of unsuitability or suitability of
the Classification Act for research work as
compared with -nonresearch engineering
work which lends itself to a pyramidal
structure. The Purvis Committee cited Ein-
stein as an example of a man to whom ap-
plication of the Classification Act of 1949
would be unsuitable. Basing the salary on
the position tends to ignore the contribution
of a gifted engineer, in the view of Nichol- —
son.*° The survey of scientists and engineers ©
°° NICHOLSON, Scott, How much is an R/D boss |
worth? Research and Engineering, December 1956: —
6.
JANUARY 1959
in research and development made by the
Department of the Army indicated that
scientists and engineers in research and de-
velopment do not fall into the “readily iden-
tifiable levels” that are envisioned by the
Classification Act and that the precise duties
should not be the sole measure of value of
the individual. Adding weight to the con-
clusions as to unsuitability and antagonism
is the fact that the Committee on Scientists
and Engineers for Federal Government Pro-
erams found that nine out of ten scientists
and engineers considered that pay should
reflect substantial differences in quality of
work performed, something not permitted
by the Classification Act or by many other
job evaluation systems.
In arriving at his conclusion, the writer
was not unmindful that Chaffee attributed
to mental laziness and the lack of an or-
ganized demand the fact that job evalua-
tion had not (by 1950) really developed for
creative engineering, though Chaffee’s own
work indicated the technical feasibility of
such application of job evaluation. So also
Sykes, who saw merit in each of the two
concepts and appeared to lean toward the
Classification Act for areas he had con-
sidered.
10. Conclusion: Rank-status should not
carry the connotation of “unlimited license
for administrative indiscretion.” It should
not be thought of as the discredited system
that was not uncommon at the turn of the
century which saw the owner-manager’s son
“start at the bottom and rise to the top”
in three or four years. In each of the plans
studied there was some form of control over
_ the exact salary to be paid to an individual
scientist or engineer. Pay at a stated number
of years beyond his last degree was found
to be used as a guide for individual salaries
at the Mellon Institute of Industrial Re-
search and as a control measure for total
salary expenditures at the Los Alamos Sci-
entific Laboratory.?! At the latter labora-
tory, since it was engaged on government
work, there was also a review control exer-
cised by the Atomic Energy Commission to
see that individual salaries did not become
absurd. The British scientific service, oper-
ating under the principle of “fair compari-
*1 Pay at stated ages used at Mellon Institute.
BUELL: PAY PLANS AND PEOPLE it
)
son” with industry pay for comparable
work, has controls upon salary decisions
made by agency boards and officials through
two means. The first is the existence of sal-
ary standards with Civil Service Commis-
sion review and approval of entrance sal-
aries above the normal rate. The second is
the Treasury review and approval of recom-
mendations for special merit promotions of
outstanding individual workers. The scien-
tist officer class of the Public Health Service
commissioned officer corps has over-all con-
trols established in congressional legislation
and comparable to the military pay system.
Its uniqueness stems from the effectiveness
of the sophisticated modern techniques used
in evaluating personnel for appointment,
promotion, and selection-out, and from the
fact that the techniques are used by other
scientist officers—sometimes in board ac-
tions where other members of the board may
be from commissioned officer classes other
than the scientist officer class.
In the Department of Defense and in the
Public Health Service strong accent upon
rank-status exists in determining the sal-
aries of those scientists and engineers whose
positions come within the purview of Pub-
lic Law 318, 80th Congress (1947), and Pub-
lic Law 692, 81st Congress (1950), respec-
tively. With initial control invested in the
operating agencies, the Civil Service Com-
mission has review authority over the par-
ticular salary to be paid to an individual,
including the final determination by that
body as to the qualifications of an incum-
bent or proposed incumbent of a specific
position. These public laws were approved
with the intention that they would be “in
accord with” the compensation schedules
of the Classification Act of 1923, as
amended, specifically with section 13 which
described the then existing grade levels and
which prescribed the pay rates for those
grades. Although the preliminary review
within the Civil Service Commission consid-
ers the grade in which the position would be
placed, were it under the Classification Act,
the ultimate decision of approval or denial
of the agency recommendation is based
typically on the Commission review of
matching the qualifications of the individual
with the assigned duties and responsibilities.
14 JOURNAL OF THE
It was learned that in the Canadian civil
service the technique for determining the
salary of scientists and engineers is a posi-
tion classification plan but that the control
exercised by Treasury is flexible enough to
permit it granting salaries above the stated
range of salaries for the classification of the
position when there are exceptional circum-
stanees.7” Another recent step toward the
principle of recognition of the man in the
job, rather than the job alone, was the set-
ting up of some 300 different titles into three
classes for the purpose of achieving greater
flexibility of personnel and to enable a man
to receive the salary that he is worth with-
out always relating his job to a particular
classification.7*
11. Conclusion: The concept of rank-
status or rank-in-the-person—rather than
rank-in-the-position—is used successfully
as the basis for salaries of scientists and en-
gineers in the organizations of high repute
which were studied. In nongovernmental or-
ganizations such as the Los Alamos Scien-
tific Laboratory and the Mellon Institute
of Industrial Research and the Battelle Me-
morial Institute rank-status has been the
basis for pay plans that have been used ef-
fectively for many years. The British scien-
tific service is based upon this principle as
part of its integrated career service. The
Pubhe Health Service Commissioned Officer
Corps used many of the principles of rank-
status, though the specific salaries paid are
within the framework of the military pay
schedules. Both Public Law 313 positions
and Public Law 692 positions have princi-
ples of rank-status firmly imbedded in the
basic law. The Classification Act of 1949,
as amended, is still basically the Classifi-
cation Act of 1923 with respect to the princi-
ple under study. It disregards the qualifi-
cations of the “person” except insofar as
they are requirements for minimum satis-
factory performance of the work described
for the “position.” No account is taken of
unusual qualifications of a scientist or en-
gineer for the position which he is filling.
* Personal interview with David M. Watters,
Secretary of the Treasury Board, Department of
Finance, Ottawa, Canada, May 6, 1957.
** Personal correspondence from David M. Wat-
ters, October 16, 1957.
WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. l
12. Conclusion: A_ significant practice
that was found in most of the rank-status
type pay plans for scientists and engineers
that were studied was an “evaluation by
one’s peers.” This practice was found fre-
quently in some form of group appraisal of
the scientist or engineer as one of the tech-
niques used in achieving a final determina-
tion as to compensation. Although the eval-
uation methods varied greatly in the degree
of sophistication of the process, the signifi-
cance probably lay as much in the psycho-
logical value of the evaluation by one’s peers
as in the technical results.
13. Conclusion: Sophisticated systems for
evaluating men and jobs are useful to man-
agement but should supplement, rather than
be a substitute for, the considered judgment
of responsible research and development ad-
ministrators. Sophisticated systems of job
evaluation (e.g., the Classification Act of
1949) are of relatively greater use at the
lower levels of scientific and creative engi-
neering work than for the higher levels and
they are progressively of less use the more
the work proceeds from the routinized or
regularized toward the unknown. As Worthy
has succinctly expressed it, when referring
to executives, rather than to scientists or
engineers, ‘““As to methods of determining a
man’s contribution, I think there is no sub-
stitute for executive judgment.” And as to
measure of the men themselves, “...tech-
niques of this kind [test batteries] cannot
be used in isolation nor as a substitution for
executive judgment. They can, however, be
an excellent means for helping sharpen ex-
ecutive judgment.””4
14. Conclusion: Scientists and engineers
generally favor having their salaries include
considerations of their individual back-
grounds of education and training and their
contributions to the program. They are par-
ticularly antagonistic toward the practice
of having their pay based solely upon a po-
sition description—in part because the de-
scription so often bears relatively little re-
semblance to what the incumbent actually
does or what he must actually know.
15. Conclusion: Scientists and engineers
“Personal correspondence from James C.
Worthy, March 19, 1957.
JANUARY 1959
usually favor having their contributions to
the research and development programs
judged by persons with generally the same
backgrounds as they themselves have. Sci-
entists and engineers usually believe that a
person who is untrained in a particular field
of knowledge or work cannot classify posi-
tions in that area as well as if he were
trained in that work area. As in other con-
troversial matters, there are extreme opin-
ions on both sides of the question. A view
frequently held was described in the report
of the Committee on Engineers and Scien-
tists for Federal Government Programs as,
substantially, that eleven out of twelve Fed-
eral scientists and engineers believed that a
person could not classify satisfactorily Jobs
in a professional field unless he were trained
in that field. When scientists evaluate sci-
entists they frequently have their own par-
ticular disciplines represented. This is found
in the provisions of the Public Health Serv-
ice Manual for the use of the advice of
groups of peers in the making of recom-
mendations for the appointments and sal-
aries of scientists under Public Law 692. It
is also found in the interview boards used
in the Public Health Commissioned Officer
Corps and in the panels for fellowship
awards by the American Academy of Sci-
ence.
16. Conclusion: Rank-status pay plans
are more acceptable to management than is
the Classification Act of 1949, as amended,
even though controls in the use of rank-
status practices are exercised by some level
above the laboratory or office concerned.
The various writings examined and testi-
mony read indicated to the writer that it is
- now quite generally recognized that in Gov-
ernment, as well as in most industrial situ-
ations, there are few persons, indeed, who
make unreviewed and unreviewable deci-
sions in regard to salary and status matters.
17. Conclusion: The Classification Act of
1949 and its administration often exert a
degree of domination over the legitimate
needs and desires of management to the ex-
tent that operating officials resort to un-
ethical practices in an attempt to escape
such domination. Along with the growth of
“scientific management” during the 1920’s
came the dependence upon classification
BUELL: PAY PLANS AND PEOPLE 15)
specialists for carrying out most of the ad-
ministration of the Classification Acts of
1923 and 1949. Management rather willingly
abdicated to what has become an “elite
corps of classifiers,’”’*° to use the character-
ization of the Cordiner Committee. Empha-
sizing mechanics and process rather than
the people in the position, the administra-
tion of the Act gradually resulted in a sepa-
rateness from line management of the proc-
ess and the classification personnel which
in some cases was absolute. Position classi-
fiers either made final grade level decisions
themselves or served as staff to another
staff man, rather than to lhne management.
They were “on top” rather than ‘“‘on tap” as
staff assistance to line management. This
dominance appears to the writer to have
reached full-flowering in the Federal Gov-
ernment about the end of the Korean con-
flict.
It frequently happens that an adminis-
trator can not increase the salary of a scien-
tist or engineer whose position is under the
Classification Act unless he can “rewrite” a
position description that will get a higher
classification. Because of this, the adminis-
trator may covertly or overtly encourage
distortions in descriptions of duties. A con-
test between an administrator’s skill at
writing descriptions and a classifier’s skill
in ferreting out the facts through work au-
dits often results in disharmony that injures
both the work program and the classifica-
tion program. Even when harmony persists
there may be intense distrust on each ‘“‘side.”
Under such situations, position descriptions
may degenerate into “job sheets” which are
merely exercises in dissimulation. It is not
unusual, therefore, to find that the ‘job
sheets” are not believed either by the man
who wrote them or by those who read them.
In this connection it is recognized that
there is often a broad “zone” within which
it is difficult to determine whether the exag-
gerations and misleading statements of
many position descriptions are not only un-
*° Defense Advisory Committee on Professional
and Technical Compensation, Civilian Personnel.
Vol. 2 of “A Plan of Action to Attract and Retain
Professional, Technical, and Managerial Employees
for Defense.” Tab. J of Vol. 2 (of Vol. 2), “Problems
of Salary Administration Under the Classification
Act,” by Study Group II, p. 3. Washington, 1957.
16 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
ethical practices but are also illegal prac-
tices of falsification of a Government pay
record.
The writer has concluded that if adminis-
trators and employees together resort to un-
ethical practices, the position classifier can
usually only delay the action sought by the
administrator but can seldom prevent the
action from eventually taking place—even
though it takes a paper reorganization to
accomplish it.
RECOMMENDATIONS
1. The present importance of attracting
and retaining qualified scientists and engi-
neers in research and development calls for
the utmost in Congressional leadership in
authorizing the use of rank-status plans. It
also calls for the utmost in administrative
leadership and skill in developing and ad-
ministering one or more rank-status pay
plans for the higher level scientists and en-
gineers that will be acceptable to the scien-
tist and engineer and to management. Such
plans must meet the American philosophy
of pay based upon what the employee is
worth to the government organization which
hires him. The “worth” of a scientist or en-
gineer should be viewed as the contribution
toward the end result or program accom-
plishment rather than as “equal amount of
work” or “equal assignments.”’
2. The Civil Service Commission should
encourage agencies to make more of the
agency classification decisions (for posi-
tions under the Classification Act of 1949)
at top levels of line management rather than
in the personnel staff office. The emphasis
should be on extensive and intensive use of
personnel administrators and technicians as
consultants participating in the discussions
leading to line management decisions. The
Commission should also give added stimulus
to constructive interpretation by scientists
and engineers of the Classification Act of
1949, as amended, both in development of
sound classification standards and in the
appheation of those standards.
3. Legislation should be sought which
would:
a. Provide for a Research and Develop-
ment Corps, outside of the existing Classi-
fication Act, in which would be placed the
VoL. 49, No. 1
positions of scientists and engineers engaged
in research and development, which are now
under Public Laws 313 and 692 or which are
under the Classification Act of 1949, as
amended, at levels above grade GS-15, the
pay schedule of this corps to have a mini-
mum and a maximum rate that are at least
as high as those currently existing under
Public Law 313, but to have no specified
pay steps within the range. Provision should
be made that positions not initially to be
placed under this corps would be eligible
for such status upon review and approval
by the Civil Service Commission that each
position so recommended by an agency was
above the level that is characteristic of
grade GS-15 under the Classification Act of
1949. It is proposed that there be no statu-
tory ceiling placed upon the numbers of such
additional positions.
A case could be made for inclusion of all
levels of professional scientists and engi-
neers in the proposed corps.?® Initial limita-
tion, however, is believed to be more useful,
through inclusion of only those whose sal-
aries are above the salaries of the equiva-
lent of GS-15. The proposed corps would
thus cover the levels where rank-status is
most needed from the standpoint of salary
determination. These same levels are where
recruitment and retention of the highest
caliber personnel would be the most profit-
able in terms of the personal contributions
of the scientists and engineers to the sub-
stantive aspects of research and develop-
ment programs and of their effect as lode-
stones in drawing junior scientists and
engineers of promise into government or-
ganizations. This limitation would reduce
some of the serious criticisms that would
come from employees in other occupations
whose pay would continue to be fixed under
the Classification Act of 1949, and from
other interested parties such as Members
of Congress, the Civil Service Commission,
and others who would resist any attempt
to remove such a large group of positions
from the operation of the Classification Act.
°° See particularly Beitstey, G. Lyte, Notes for
the Hoover Commission Personnel Task Force on
subject of rank-in-the-person (written presenta-
tion to the task force dated March 5, 1954), pp. 2,
3. (Typewritten.)
JANUARY 1959
b. Place the determination of salary
levels for individual positions of the Re-
search and Development Corps upon the
executive department or agency authorized
to have such positions. The agency should
be required to file with the Civil Service
Commission a plan of administration of this
program which would utilize the concept of
a board of professional scientists and engi-
neers to make individual salary determina-
tions or recommendations to the head of the
agency. Provision should also be made for
agencies to change their plans when they
see fit, and to file the revised plan or a new
plan with the Commission within 30 days
after adoption.
The determinations as to salary for an
individual should not be subject to disap-
proval or change by any authority outside
the agency. As part of the salary determina-
tion process under the professional peer con-
cept proposed, provision could be made for
nonvoting participation by a representative
of the Civil Service Commission. This repre-
sentative could be required to file with the
agency head any disagreement with a sal-
ary decision of the board. The agency also
might well be required to transmit such
statements to an appropriate committee of
the Congress annually, with agency com-
ments, if the agency chooses to make any.
So also, the Civil Service Commission could
be required to make annual reports to the
same committee concerning its findings as
to over-all administration of the plan by
agencies that are operating under it.
c. Reduce the number of grades of the
Classification Act of 1949 to provide for
greater rate ranges within the grades to
which positions of the scientists and engi-
neers in research and development would
be assigned if not coming within the pur-
view of the Research and Development
Corps pay schedule. Theoretically this
would cover the levels from the present
erade GS-5 through grade GS-15. The
broader zones would reduce the number of
border-line controversial cases which often
create friction between line personnel and
position classifiers.
d. Revise the Classification Act of 1949
by abolishing specific step rates and pro-
vision for periodic step increases for grades
BUELL: PAY PLANS AND PEOPLE 17
GS-13, GS-14, and GS-15. Substitute for
those provisions salary increases on the
basis of not more than one per year and
make the amount of increase to be not less
than, say, $250 a year or more than one-
half the difference between the minimum
rate of the grade and the maximum rate.
e. Provide for an independent and non-
partisan advisory body of scientists and en-
gineers and public-spirited citizens to study
the operation of the pay systems for scien-
tists and engineers that are covered by these
recommendations, to study the need for an
integrated career corps of such scientists
and engineers (a collaborative study with
operating agencies), and to report to the
President its findings in these and related
matters. It is proposed that the study be
limited to the scientist and engineer areas
because of the present critical situations in
these areas and because different problems
exist in other areas.
4. Additional study by individuals or
committees could produce useful informa-
tion and recommendations on areas that
are closely related to, or intertwined with
rank-status pay plans for scientists and en-
eimeers, such as:
a. The possibility that entrance to a pro-
posed Research and Development Corps
should be planned as eventually beginning
at a level lower than that recommended for
immediate action.
b. The national effects, favorable and un-
favorable, of changing the salary basis for
scientists and engineers in research and de-
velopment to fair competition with nongov-
ernmental activities, either on a local or a
national prevailing rate basis.
c. The extent, if any, to which the na-
tional interests make it desirable to provide
a special pay raise under existing pay plans
for scientists and engineers that would be
different from the amount of any raise for
other groups.
d. The practicability of decentralizing to
agencies the authority currently residing in
the Civil Service Commission to pay new
recruits and present employees above the
minimum step of the grades—making it on
the basis of agency need and occupational
specialty rather than on the broad occupa-
tional coverage that is now used.
18 JOURNAL OF THE
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 1
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Scientists. Documents and Reports to Accom-
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AmeprtcAN AssemBLy. JUhe Federal Government
service: Its character, prestige, and problems,
Sixth American Assembly, Arden House. Co-
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Betstey, G. Lyte. Notes for the Hoover Commis-
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Brown, Auyin. The armor of organization: A ra-
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liminary thereto, an inqury into the origins
of existing military organization. Hibbert Print-
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Burcess, Carter L. Similarities and contrasts in
military and civilian career services. Personnel
Admin. 18 (September): 16-238. 1955.
BusH, Georcre P. The principles of administration
in the research environment. Ch. 23 of “Scien-
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Hattery, editors. American University Press,
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engineers in government and industry. Govern-
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Corson, JoHN J. Executives for the Federal service:
A program for action in time of crisis. Columbia
University Press, New York, 1952.
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TECHNICAL COMPENSATION. Civilian personnel.
Vol. 2 of “A Plan of Action to Attract and Re-
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DEPARTMENT OF THE ARMy. Office of the Deputy
Chief of Staff for Personnel. Office of Civilian
Personnel. Survey of civilian personnel man-
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and development activities, May—October 1956.
38 pp. and appendix. Department of the Army,
Washington, 1956.
Drucker, Peter F. Management and the profes-
sional Employee. Harvard Bus. Rev. 30
(May—June) : 84-90. 1952.
Frost, Connie Curtis. Supplementing pay with
recognition. Personnel Admin. 19 (Novem-
ber—December) : 18-20. 1956.
GRAHAM, GrEorGE A. Significant personnel practices
in business organizations. (In Vol. 3 [no title]
of “Documents and Reports to Accompany the
Report on Civil Service Improvement,” pp.
60-63. 3 vols.) Government Printing Office,
Washington, 1942.
GRAND, JoSepH A. Manpower crisis in Federal labs.
Chem. and Eng. News (April 1): 26-28. 1957.
Hensev, H. Struve. Ways and means of recruiting
capable Federal executives. Public Admin. Rey.
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Howe i, WiturAM F., and Fow.irer, Donatp D. Per-
sonnel programs of international organizations.
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1956.
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[Trytten report.|
MILuer, Devtsert C., and Form, Wiiuiam H. /n-
dustrial sociology: An introduction to the
study of work relations. Harper & Brothers,
New York, 1951.
Mosuer, FrepertcK and EpirH. Distinguishing
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Federal Government Service: Its Character,
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sembly, Arden House, pp. 113-151, Columbia
University, New York, 1954.
Parton, ArcH. Incentive compensation for execu-
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46. 1951.
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31-40. 1956.
SHEPHERD, Cuovis, and Brown, Pauta. Status, pres-
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Admin. Sci. Quart. 1 (December): 340-360.
1956.
Somers, Herman M. Some reservations about the
senior civil service.’ Personnel Admin. 19
(January-February) : 10-18. 1956.
STEELMAN, JoHN R. Administration for research.
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Government Printing Office, Washington, 1947.
The Editors Say ...Executive development con-
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1956.
Urwick, Lynpatt F. Management education in
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U.S. Commission ON ORGANIZATION OF THE EXECU-
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1950.
JANUARY 1959
DRAKH AND DAVIS: NEW LYGAEIDAE 19
ENTOMOLOGY .—A new subfamily, genus, and species of Lygaeidae (Hemiptera-
Heteroptera) from Australia.
CarRL J. DRAKE, Smithsonian Institution, and
Norman T. Davis, University of Connecticut.
(Received December 15, 1958)
The present paper designates a new sub-
family of bugs in the very large and hetero-
geneous family Lygaeidae to hold a remark-
able species and genus described as new
herein from Australia. The type series of
24 specimens of the new species were all
eollected by the Australian hemipterist
Henry Hacker in Queensland.
Since the hierarchal characters of the
undescribed species were found inapplicable
for its inclusion in any of the present sub-
familial taxa of Lygaeidae, it has been
necessary to erect a new genus and new
subfamily for its reception. These new
categories are being named in honor of the
lygaeid specialist Dr. James A. Slater, who
is now engaged in classifying and cata-
loguing this family of insects for the world.
In their comprehensive check-list of the
families and subfamilies of Heteroptera,
China and Miller (1955) recognize 15 sub-
families in the family Lygaeidae. The fun-
damental subfamily classification of Ly-
gvaeidae was established by Stal (1862, 1865,
1872) and has remained essentially the same
except for the addition of five subfamilies
by Berg (1879), Reuter (1878) Douglas and
Seott (1865), Breddin (1907), and Barber
and Bruner (1933). Additional subfamily
characters have been developed by Hutchi-
son (1934), Slater and Hurlbutt (1957),
Ashlock (1957), and Scudder (1957). Ana-
lytical keys to the subfamilies of Lygaeidae
for various regions of the world may be
found in the publications of Stal (1862,
1865, 1872, 1874), Walker (1872), Saunders
(1892), Barber (1917), and Stichel (1925,
1957).
For many helpful suggestions and advice
on phylogeny and classification, we wish to
express our sincere thanks to the following
hemipterists: Dr. W. E. China, British
Museum (Natural History), London; Dr.
J. Carayon, Muséum National d’Histoire
Naturelle, Paris; Dr. J. A. Slater, University
of Connecticut, Storrs, Conn.; and Dr. R.
I. Sailer, H. G. Barber, and P. D. Ashlock,
all of the U. $8. Department of Agriculture,
Washington, D.C. The illustrations were
prepared as follows: Figure 1 was drawn
by Arthur Smith, artist, British Museum
(Natural History), London; the photograph
of figure 2 is by Dr. J. Carayon, Muséum
National d’Histoire Naturelle, Paris; the
remainder were prepared by the junior
author.
MORPHOLOGY
In order to determine accurately the charac-
teristics and systematic position of this insect,
the following detailed analysis of its morphology
has been made:
Head: The general shape of the head may be
characterized as being distinctly broad and short
and moderately declivent (Figs. 1, 3). The com-
pound eyes are strongly protruding and widely
separated and have rather coarse facets. The
eyes are almost contiguous with the thorax. The
ocellii are present. The tylus is narrow and
strongly produced anteriorly, while the juga are
short, flat, and inconspicuous. The bueculae are
well developed and open in front, extending back
over about a third of the ventral surface of the
head. The beak is 4-segmented and straight and
reaches to just beyond the procoxae. The an-
tenniferous tubericles are moderately small, and
the antennae are short and 4-segmented. The
small segments are rather thick and subeylindri-
eal except for the last segment, which is fusiform
(Fig. 4).
Thorax: The prothoracic coxal cavities are
closed posteriorly (Fig. 6), and the pleural su-
ture is distinguishable only on the prothorax.
The meso- and metathoracic sterna are fused,
but the intersegmental suture is distinct. There
are well-developed scent gland ostioles (SgO)
on the metathorax. Internally the metathoracic
scent gland consists of a median, unpaired, res-
ervoir (Fig. 10, S¢R) into which lateral, branch-
ing scent glands open (Sg). The afferent ducts of
the scent-gland reservoir pass through the base
of the metasternal apophyses to their external
20 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
opening in the scent-gland ostioles. The struc-
ture of the scent gland is essentially the same as
is found in other lygaeids as well as in most other
families of Pentatomorpha except the aradids.
The metacoxal articulation is the trochalopo-
dous type. The tarsi are 3-segmented (Figs. 7,
8, 9), the second segment being small and in-
completely fused to the third; arolia are present.
Wings: The clavus and corium are distinct,
and the membrane appears to have a reticular
pattern of venation (Figs. 1, 2). However, there
are five distinct longitudinal veins extending
through the membrane, and the reticulation has
probably developed secondarily. The second and
third longitudinal veins are in some cases partly
coalesced at the base (Fig. 1), and in others they
are entirely separate.
The metathoraciec wing venation is greatly re-
duced (Fig. 11). The terminology used here for
the veins follows that of Leston (1953) and of
Slater and Hurlbutt (1957). The subcosta is ab-
sent; the radius (R) is well developed; the
hamus is not distinguishable except possibly as
a broad, indistinct veinlike thickening between
R and Cu near the base of the wing. The distal
branch of the media from R, characteristic of
the pentatomorphs, is in this insect only a small
stub. The cubitus (Cu) is distinct and is fol-
lowed by the bifureate vanal furrow (VF). The
intervanal veins are absent, and the vanal veins
(V) are present and fused basally. The so-called
jugum is absent.
Abdomen: The first abdominal segment is re-
duced in a manner characteristic of Heteroptera,
and thus only the median tergite of that segment
ean be distinguished (Fig. 12, I). Segments II
through VII are distinct, and all the pregenital
terga are fused to one another except for tergites
II and III, between which there remains an in-
tersegmental membrane. On the venter of the
abdomen the second, third, and fourth segments
are fused, but the intersegmental sutures are
distinet (Fig. 13). The remaining segments are
free ventrally. The connexiva are distinctly
formed, and the dorsal connexival sutures are
modified into convoluted membranes (Fig. 12,
CxM) which enable dorso-ventral expansion and
contraction of the abdomen. The ventral con-
nexival sutures are very indistinct (Fig. 13). The
first abdominal spiracles are apparently absent:
spiracles IT through VI are dorsal on the connexi-
vum (Fig. 12), and spiracle VII is ventral on the
connexivum (Figs. 13, 19). Spiracle VIII of the
VoL. 49, No. 1
female is also ventral and is normally concealed
under the seventh segment (Fig. 14); the eighth
spiracle of the male is absent. Two closely set
pairs of trichobothria are found on the venter of
segments III and IV; a widely separated pair
is found on each side of the fifth and sixth seg-
ments near the connexival suture, and a single
trichobothrial hair is found on each side of the
seventh segment (Fig. 13). Scars of the nymphal
scent glands are present between tergites IV
and V, and V and VI (Fig. 12, Sg).
Female genitalia and genital segments: The
eighth and ninth tergites are compressed ventrad
and lie in an almost vertical plane, and the tenth
segment is reduced to a small tubular sclerite
projecting from beneath the ninth tergum (Fig.
14, X). The seventh segment is very deeply cleft
santas ae: “!
wansesessea, ss) Zoe
1 HO et pe Zit ym
satiety
- (oP
ie:
ita x *
6" 8 oes
BAAS
ALR EK 7
{ASS Se es ‘
e
o'
a
.
e
>
Q
.
RZ
lia. 1—Slaterellus hackert, n. gen. and sp.
JANUARY 1959
mid-ventrally and normally overlaps the base
of the ovipositor (Fig. 13, VII). When the ovi-
positor is in use, its anterior end is extended
downward and posteriorly into the position
shown in Fig. 14. This manner of extension of the
ovipositor is especially characteristic of the
lygaeids. In this extended position the gonocoxo-
podites (valvifers) of the eighth segment are
seen to be large triangular sclerites (Fig. 14,
Gep 1). The gonocoxopodites of the ninth seg-
ment are not shown but are considerably reduced
and lie beneath the ventral margins of that seg-
ment. The gonapophyses (valvulae) of the eighth
segment extend from the anterior apex of the
gonocoxopodites and are joined ventrally by a
membrane (Fig. 14, Gap 1). The first gonapo-
physes are also attached to the ventral margins
of the ninth paratergites by means of sclerotized
rods, the inner rami, extending from their base
(not shown). The second gonapophyses are
joined for most of their length and are united to
the first gonapophyses by the usual tongue-in-
groove mechanism found in the heteropteron
ovipositors. The third gonapophyses (= styloids
of Dupuis, 1955) although usually present in
other Hemiptera, can not be distinguished.
Internally the female genital chamber consists
of a simple cuticular sac. Posteriorly its lumen
extends into the ovipositor, and the common
oviduct extends from it anteriorly. Arising from
the roof of the genital chamber there is a com-
plex tubular gland, the spermatheca (Fig. 15).
At the base of the spermatheca the roof of the
genital chamber is differentiated into a pouch-
like structure with a groove extending posteriorly
from it. This structure possibly functions to di-
rect the vesica of the phallus (see below) into
the spermatheca during copulation. The sper-
matheca consists of a double tube, the ductus
receptaculi (DR), at the end of which is a dis-
tinctive chamber, the capsula seminis (Ca 8).
Various studies of other Heteroptera show that
the spermatozoa are retained in the seminal cap-
sule. The distal portion of the duct is sclerotized
(PI) and is possibly equivalent to what has been
termed the pars intermedialis in the pentatomid
spermatheca (Dupuis, 1955). The proximal end
of this structure is encircled by a ridge which
presumably serves for the attachment of mus-
cles extending from it to the lower rim of the
seminal capsule. In the lumen of this duct there
is a second and much narrower duct which also
DRAKE AND DAVIS: NEW LYGAEIDAE
21
Fig. 2—Slaterellus hackeri, n. gen. and sp.
extends from the genital chamber to the seminal
capsule.
Male genitalia and genital segments: The
eighth segment of the male is reduced consider-
ably, and only the ventral portion of it is sclero-
tized (Fig. 19, VIII). This segment and the ninth,
or pygophore (Pg), are normally retracted com-
pactly into the seventh segment. The tenth and
eleventh segments are very reduced and are in-
corporated into the proctager, which lies over
the top of the pygophore (Fig. 16). The para-
meres (Fig. 17) are symmetrical and are similar
in form to those found in many lygaeids. The
phallus is extremely small, and it has been im-
possible to obtain it in the erect condition and
to study many of the details of its structure. At
its base is the usual stirrup-shaped plaque
basalis, or stapes (Fig. 18, BP). The phallus is
clearly differentiated into phallosoma (Ps) and
endosoma (Es), and the latter is in all probabil-
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, NO. 1
bo
Pir
Upiffe
Mf f/ fii
iy
SS
\
~
Ss BF
~ >
i]
Le
VES,
Hf
Yj
i f
//
Ay
ANS
f
tj
1,
/}
il Ui
Fig. 3-11.—Slaterellus hackeri, n. gen. and sp.: 3, Lateral view of head; 4, antenna; 5, lateral view
of labium and labrum; 6, ventral view of thorax with legs removed (CC, coxal cavity; SgO, scent-gland
ostiole); 7, left prothoracic leg; 8, right mesothoracic leg; 9, right metathoracic leg; 10, internal view
of meso- and metathorax showing scent-gland apparatus (Sg, scent gland; SgR, scent-gland reservoir) ;
11, metathoracic wing (Cu, cubitus; R, radius; V, vanal veins; VF, vanal fold).
JANUARY 1959 DRAKE AND DAVIS: NEW LYGAEIDAE 23
SS eee re
= &
/
SPQ yya eye 0d eV; a
7
a
|
9 |
re
0.125mm
ae
Fies. 12-19.—Slaterellus hackeri, n. gen. and sp.: 12, Dorsal aspect of female abdomen (CxM, con-
nexival membrane; Sgs, scent- gland scars); 13, ventral aspect of female abdomen (Gep 1, first gono-
peeodite) 14, lateral aspect of female abdomen with ovipositor extended (Gap 1, first gonapophysis;
Gap 2, second gonapophysis: Gep 1, first gonocoxopodite); 15, spermatheca (CaS, capsula seminalis;
Gch, genital chamber; DR, ductus receptaculi; PI, pars intermedialis) ; 16, pygophore from above; 17,
right paramere from later al aspect; 18, phallus from dorsal aspect (Bp, ‘basal plate; Ps, phallosoma; Es,
endosome); 19, ventral view of terminal s segments of male (Pg, pygophore).
24 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
ity differentiated into vesica and conjuctiva. The
phallosoma lacks processes.
SYSTEMATIC POSITION
The ventral trichobothria, the type of sperma-
theca, and the type of phallus are the principle
features relating this insect to the group of
families of Geocorisae designated as the Pentato-
morpha (Leston, Pendergrast, and Southwood,
1954). Of the several families of Pentatomorpha
this insect clearly belongs to the Lygaeidae, as
is indicated by its possession of the following
combination of characteristics: Ocelli present;
labium and antennae 4-segmented; tarsi 3-seg-
mented; antennae inserted below a line from the
middle of the eyes to the apex of the tylus; five
longitudinal veins in the membrane of the hem-
elytra.
This insect differs from all other lygaeids in
having the longitudinal veins of the membrane
irregularly connected to one another by cross-
veins which form a variable reticular pattern.
It also differs from all other lygaeids except the
Maleinae and Chauliopinae in having a vestiture
of short, scalelike hairs. However, in addition
to the characteristic venation of the membrane
it is unlike these subfamilies in having closed
coxal cavities and in having a different arrange-
ment of abdominal spiracles. It appears to be
most closely related to the Blissinae, since it has
the same pattern of distribution of abdominal
spiracles as the blissines as well as having a
head with similar proportions of width to length,
similarly shaped pronotum, and similar charac-
teristics of the clavus and claval commissure.
The unusually short corium of this insect is also
characteristic of some but not all blissines. In
addition to the very distinctive vestiture and
membrane venation, this insect differs from the
Blissinae in lacking swollen fore-femora and in
having a punctate corium and clavus.
The lack in this insect of certain additional
definitive characters of other subfamilies may
be noted. Unlike most Megalonotinae, the su-
ture between segments IV and V is straight and
complete, and the paired setae near the eyes are
lacking. Unlike the Lygaeinae and Cyminae the
hind margin of the pronotum is not convex. The
suleate tylus characteristic of most Geocorisae
is lacking and unlike the Megalonotinae, Oxy-
careninae, Heterogastrinae, and Pachygronthinae
the fore-femora are not armed.
vou. 49, no. l
Slaterellinae, n. subfam.
30dy clothed above and beneath and on ap-
pendages with a vestiture of short, scalelike
hairs; head with transocular width greater than
median length, inserted into pronotum almost to
eyes; eyes strongly convex, ocelli present, buc-
culae moderately short, high, open in front.
Forefemora unarmed, not incrassate; tarsi 3-seg-
mented and with arolia; metacoxae trochalopo-
dous; fore-coxal cavities closed. Metathoracic
scent gland ostioles distinct; pronotum not con-
stricted into anterior and posterior lobes. Meso-
thoracic wings with corium short and truncate,
forming approximately the basal fourth of the
wing, the membrane correspondingly longer;
sides of the clavus almost parallel, claval com-
missure short but more than half as long as
the scutellum; membrane with five longitudinal
veins that are irregularly connected to one an-
other by cross-veins so as to form a variable and
indefinite network. Metathoracic wings with
distal branch of media vestigal, hamus reduced
or absent, and with intervanal veins and jugal
lobe absent. Spiracles dorsal on connexival seg-
ments II through VI and ventral to the connexi-
vum on segments VII and VIII, and with VIII
absent in the male. Segments II through IV
fused but with sutures distinct and straight.
Segment V and VI narrowed and segment VII
completely divided midventrally in the female.
In the male segment VI and VII narrowed mid-
ventrally and segment VIII and IX of the fe-
male reduced and mostly concealed beneath
tergite VII. Pygophore of male concealed be-
neath tergite VII and with symmetrical para-
meres. Spermatheca of female terminating in a
bulb.
Type genus, Slaterellus, n. gen.
Slaterellus, n. gen.
Head depressed, sloping gently forward, trans-
ocular width slightly greater than anterior width
but less than posterior width of pronotum, and
with tylus conical and projecting, jugum short
and flat, antenniferous tubercles small, ocelli
widely separated, bucculae extending backward
forming very low obliquely converging carinae,
eyes exserted, large, and widely separated. An-
tennae thick, very short, scarcely longer than
the head. Pronotum depressed, punctate, with
lateral margins gradually converging anteriorly,
hind margin roundly excavated. Legs with sec-
JANUARY 1959
ond tarsal segment reduced and fused to third.
Hemelytra not extending to the apex of the ab-
domen nor covering the connexival segments;
clavus and corium sparcely punctate. Ventral
trichobothria on segments III and IV consisting
of two patches with a pair of closely set hairs, on
segments V and VI a pair of patches on each
side with a single hair, and a single patch with
one hair on each side of segment VII.
Type species, Slaterellus hackeri, n. sp. This
monobasic genus is known only from the Aus-
tralian mainland.
Slaterellus hackeri, n. sp. (Figs. 1, 2)
Small, oblong, fuscous-brown tinged with gray-
ish or testaceous, with blackish patches on head
and pronotum, usually also with broad, blackish
fuscous; hemelytral membrane grayish with
veins fuscous. Antennae (Fig. 4) dark fuscous.
Legs (Figs. 7, 8, 9) brownish fuscous with fe-
mora largely blackish fuscous. Modified hairy
vestiture of body and appendages whitish.
Length 2.90 mm (male), 3.34 mm (female) ;
width 1.30 mm (male) and 1.50 mm (female).
Head wider across eyes (0.80 mm) than me-
dian longitudinal length (0.55 mm), interocular
space slightly longer (0.60 mm) than median
length of head (0.55 mm), apex extending
slightly beyond tips of first antennal segments;
eyes moderately large, strongly excerted, slightly
less than half of their width extending laterally
beyond front margin of the pronotum; ocelli
widely separated, with space between them twice
that between an eye and an ocellus. Antennae
short, stout, moniliform, 0.54 mm long, sub-
equal in length to width of vertex, segmental
measurements: I, 13; II, 10; III, 9; IV, 13; (80
units equal 1 mm.). Labium moderately stout,
4-segmented, extending to base of prosternum.
Bucculae very broad, very short, with cariniform
bases converging sharply inward. Orifice of meta-
thoracic stink gland plainly visible on meta-
pleura and provided with an upright channel
(Fig. 10). Legs short, stout, the anterior pair
apparently subfossorial.
Pronotum trapezoidal (Fig. 1), slightly de-
pressed, coarsely but not very closely punctate,
broadly roundly excavated behind, wider across
base (1.25 mm) than front margin (0.85 mm).
Abdomen 1.25 mm long, widest a little behind
middle; connexiva wide, very thick, moderately
reflexed so as to form a fairly deep trough with
DRAKE AND DAVIS:
NEW LYGAEIDAE 25
abdominal tergites; hemelytra (Fig. 1) not ex-
tending to tip of abdomen or covering most of
connexival segments; basal coriaceous part very
short, extending less than half its length beyond
apex of scutellum. Membrane overlapping api-
cally so as to be jointly rounded behind, cover-
ing very little of connexival segments and of
seventh abdominal tergite (Fig. 1). Scutellum
moderately large, triangular, wider across base
than median length (38:22), with median carinae
and rimmed edges prominently raised. Venation
of metathoracic wings as in Fig. 11. Male geni-
talia as in Figs. 17 and 18. Female genitalia as
in Figs. 14 and 15.
Holotype (male) and allotype (female),
Goodna, Queensland, Australia, December 12,
1926, Drake Collection (U.S. Nat. Mus.). Para-
types: 20 specimens same data as holotype; 2
specimens, Manjo District, Queensland, Novem-
ber 1927, and 2 specimens, Forest Hills, Queens-
land, January 19338; all collected by Hacker.
Paratypes have been deposited in the British
Museum (Natural History) London; California
Academy of Science, San Francisco; Muséum
National d’Historie Natural, Paris; U.S. Na-
tional Museum, Washington, D.C., and the col-
lections of Drs. J. A. Slater and N. T. Davis,
Storrs, Conn., and T. W. Woodward, Brisbane,
Australia.
This singular species is named in honor of the
eminent entomologist Henry Hacker, whose large
collection of insects contains many rare and un-
described species of Australian Hemiptera.
LITERATURE CITED
AsHLock, P.D. An investigation of the taronomic
value of the phallus in the Lygaeidae (Hemip-
tera-Heteroptera). Ann. Ent. Soc. Amer. 50:
407-426. 1957.
BarBer, H. G. Synoptic keys to the Lygaeidae
(Hemiptera) of the United States. Psyche 24:
129-135. 1917.
. (Continuation of the above.) Psyche 25:
71-88. 1918.
Hemiptera-Heteroptera (excepting the
Miridae and Corixidae). In “Insects of Puerto
Rico and the Virgin Islands.” New York Acad.
Sci. 14(3): 263-441. 1939.
Barser, H. G., and Bruner, 8. C. A new sub-
family of Lygaeidae including a new genus
and two new species of Pamphantus Stal (He-
muptera-Heteroptera: Lygaeidae). Journ. New
York Ent. Soc. 41: 531-542. 1933.
Bere, C. Hemiptera Argentina. Enumeravit Spe-
cieque Novas: 1-816. Bonariae, 1879.
Cuina, W. E., and Miuuer, N. C. E. Check-list
of family and subfamily names in Hemiptera-
26 JOURNAL OF THE
Heteroptera. Ann. Mag. Nat. Hist., ser. 12, 8:
257-267. 1955.
Dova.as, J. W., and Scort, J. The British Hemip-
tera 1. Ray Society, London, 1865.
Dupuis, C. Les genitalia des Hemipteres Heterop-
teres. Mém. Mus. Nat. Hist. Nat., ser. A, 6:
183-278. 1955.
Hurcuinson, G. E. Report on terrestrial families
of Hemiptera-Heteroptera: Yale North India
Expedition. Mem. Connecticut Acad. Arts Sci.
10: 119-146. 1934.
Leston, D. Notes on the Ethiopian Pentato-
moidea (Hemiptera): XVI, an acanthosomid
from Angola, with remarks wpon the status
and morphology of Acanthosomidae Stal. Publ.
Cult. Comp. Diam. Angolia 16: 121-132. 1953.
Leston, D., PeNpreRGRaAST, J. G., and SouTHwoop,
T. R. E. Classification of the _ terrestrial
Heteroptera (Geocorisae). Nature 174: 91.
1954.
Reuter, O. M. Note sur une nouvelle espéce
d’ Hemiptera. Ann. Ent. Soc. France, ser. 5, 8:
144. 1878.
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, No. 1
Saunpbers, E. The Hemiptera-Heteroptera of the
British Islands. London, 1892.
ScuppEr, G. G. E. New genera and species of
Heterogastrinae (Hemiptera, Lygaeidae) with
a revision of the genus Dinomachus. Opus. Ent.
22: 161-183. 1957.
Siater, J. A., and Hurtsutt, H.W. A compara-
tive study of the metathoracic wing in the
family Lygaeidae. Proc. Ent. Soc. Washington
59: 67-79. 1952.
STAL, C. Synopsis Coreidum et Lygaeidum Sue-
ciae. Ofv. Vet.-Akad. Férh. 22: 203-225. 1862.
Hemiptera Africana 2: 1-200, Stockholm,
1865.
—. Genera Lygaeidarum Europae disposutt.
Ofv. Vet.-Akad. Forh. 29 (pt. 7): 37-62. 1872.
. Enumeratio Hemipterorum, Pt. IV.
Svenska Vet.-Akad. Hand]. 12(1): 1-186. 1874.
SticHEL, W. Jllustrierte Bestimmungs Tabellen
der Deutschen Wanzen, Pt. III. Berlin, 1925.
Waker, F. Catalogue of the specimens of He-
miptera-Heteroptera in the collection of the
British Museum, Pt. V. British Museum, Lon-
don, 1872.
It is the great destiny of human science, not to ease man’s labors or pro-
long his life, noble as those ends may be, nor to serve the ends of power, but
to enable man to walk upright, without fear, in a world which he at length
will understand and which is his home. Charles Darwin did not kill the
faith of mankind. He wrought mightily, and others with him, for a newer
and greater faith—faith in universal order, whose secrets open themselves
to men truly free to question, to communicate, and to arrive at agreement
as to what they have seen.—PAut B. SHARS.
JANUARY 1959
MATSUBARA AND IWAI: A NEW SANDFISH 27
ICHTHYOLOGY —Description of a new sandfish, Kraemeria sexradiata, from
Japan, with special reference to its osteology.: Kryomatsu MatsuBaRra and
Tamotsu Iwai, Kyoto University, Maizuru, Japan. (Communicated by
Leonard P. Schultz.)
(Received November 6, 1958)
The sandfishes referred to the genus
Kraemeria are inhabitants in the sandy
shallow waters of the tropical Pacific and
are by no means familiar even to ichthy-
ologists. Remarkably enough, the members
of this inconspicuous little group, attaining
about 40 mm in total length, appear to
exhibit a high endemism, and no one has
found them before in the Japanese area.
Although the genus Kraemeria has been
included in the family Trichonotidae or
Gobiidae or sometimes placed in the inde-
pendent family Kraemeriidae, their system-
atic position was in a state of confusion
until Gosline’s (1955) paper placed the
family Kraemeriidae in the suborder Gobioi-
dei based upon the results of his osteological
studies.
The recent expedition to the Amami
Islands, Kagoshima Prefecture, greatly aug-
mented our limited knowledge of the ichthy-
ological fauna of the southernmost district
of Japan. Among a number of fishes col-
lected, there were three specimens of the
genus Kraemeria possessing sufficient dis-
tinctive characters to warrant the erection
of a new species. The descriptions presented
below are based on the material obtained
from the sandy tide pools at Ankyaba and
Usyuku, Amami Oshima, the largest island
of Amami Islands.
In order to make a comparison of osteo-
logical features of the species with those of a
known species, K. samoensis, a study of
the bones of the present new species was
undertaken. Counts and measurements of
the bodily parts were made according to
standard practice as outlined by Matsubara
(1955, pp. 60-69). In the osteological ex-
amination the skeletal elements were stained
* Contributions no. 1 from the Marine Biologi-
cal Institute of Kyoto University. The Institute is
located at Tannawa, Sennan-gun, Osaka Prefec-
ture. It was established for our Department by
the Nankai Electric Railway Co., Ltd., on March
20, 1958. We wish to acknowledge generous finan-
cial assistance from the Company.
with alizarin red and cleared with potassium
hydroxide and glycerol.
Kraemeria sexradiaia, n. sp. (Fig. 1)
SUNA-HAZE (new Japanese name)
Ho.totypeE—MIKU (Marine Biological Institute of
Kyoto University) no. 1744, a mature male speci-
men, 33.0 mm in standard length (38.0 mm in
total length), collected in the tide pool of
Usyuku, Amami Oshima, on July 10, 1958.
PARATYPES —2 specimens, MIKU no. 1745, 30.2 and
30.5 mm (36.5 and 36.0 mm), collected in the tide
pool of Ankyaba, on June 30, 1958.
Diagnosis —K. sexradiata is a dwarf species,
full-grown ova are found in a small female meas-
uring 36.0 mm in total length. The body 1s
slender and compressed laterally. The eye is
very small. The lower jaw strongly projects far
beyond the upper jaw. The pectoral fin consists
of 6 rays, the lower 5 are branched. Scalloped
flaps on the lower edge of the gill-cover number
3 to 5. In the fresh condition prior to preserva-
tion, the body is transparent. Counts and pro-
portional measurements of bodily parts of types
are shown in Table 1.
TABLE 1.—CouNTS AND PROPORTIONAL MEASURE-
MENTS IN TYPES OF KRAEMERIA SEXRADIATA
Items ee Paratypes
Standard length in mm........... 33.0 30.5 30.2
Dorsalltitiml ket eo eer he ee Vie 14 V, 14 V, 14
Ata efi sve Mere a eer ee Tt, 313 IL, i183 V9 3g}
iRectorall fink: eer caer aces: 6 6 6
Wentralsiiny ss) cept rss. 1, & 1, & 1, &
Gnill=rakers/eacagee eye ee 9 — 9
Vertebracw mek peta. aes ee ee — — 26
SS Kes pe ek hte adie ar ak rel Piet dG male female male
In standard length:
leadulenio thee eae tle ae ces 4.1 3.8 3.8
Depthvotsbod yas sees ceee eee 8.5 6.2 8.6
iPredorsall(distancess.25-e. ose. o. Boll Bor Ball
iPreanalydistances. 4.5.25. -205 05. 1.8 1.8 1.8
Length of pectoral fin........... 22, ere oI
Depth of caudal peduncle....... 16.5 11583 11
Length of caudal peduncle...... 16.5- 16.9 16.8
In head length:
SnOilbss seer Hae ce eee Gad 6.7 6
IDTENTTGUE OF EM@acdcescescousedac 26.7 26.7 26
Imterorbita)liwaGit heer ree 20.0 20.0 20.0
Length of upper jaw............ 3.8 4.0 4.2
Length of lower jaw.....2....... Poll Beil 2.7
28 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
Description of the holotype-—Body slender
and compressed laterally, without scales. Head
rather broad, about twice as wide as body.
Opercle relatively large and the lower edge
armed with 5 scalloped flaps. Posterior margin of
membranous gill-cover extending over base of
pectoral. A series of minute sensory papillae pres-
ent along lower edge of preopercle, upper lip
fold, and mandibular fold. Small nasal tube
midway between tip of snout and eye. Eye very
small. Mouth moderately large and obliquely
directed. Lower jaw projecting far beyond tip
of upper jaw when mouth is closed. Gill-mem-
branes extend forward and narrowly joined to
isthmus before a vertical through posterior mar-
gin of preopercle. Nine gill-rakers on cerato-
branchial bone of first gill-arch, but no rakers
on epibranchial and hypobranchial. No gill-
rakers on other gill-arches. Pseudobranchae ab-
sent. Branchiostegal rays slender and 5 in num-
ber. Small conical teeth closely set on both upper
and lower jaws, slightly curved, directed inward.
Dorsal fin consisting of 5 anterior spines and
14 soft rays, the posteriormost one _ bilobed.
First dorsal spine originating above a vertical
through posterior end of pectoral. Anal fin with
1 spine and 13 soft rays, the last one bilobed.
Anal spine arises below membrane between sec-
ond and third soft dorsal rays. Pectoral fin rays
6, all branched except the uppermost simple one.
Pelvic fin with 1 spine and 5 branched soft rays,
inserted below a vertical through posterior mar-
gin of opercle. Caudal fin 6 + 7 + 6+ 6.
Anal papilla slender, the posterior tip pointed.
In fresh condition prior to preservation body
and fins transparent.
Description of paratypes—The systematic
characters of paratypes generally agree with
those of the holotype except for scalloped flaps
on the lower edge of the opercle, the flaps being
3 Mm one specimen and 4 in the other.
Remarks —In some characters this new species
Y VA VA VA Y VA 4 po y, 4
/ ff // VA A ff ff Le 5 =
42 i he Oohe penal 3 aes RECS a eet cme ine a Ste SS BB ==
, < Tay : € i 2S = = ?
vou. 49, No. l
closely resembles K. cunicularia Rofen but dif-
fers in having 6 pectoral rays (8 or 9 in cunicu-
laria) and slender anal papilla with pointed
posterior tip (flat anal papilla with notched pos-
terior tip). Compared with the other species,
K. nudnum, K. sexradiata is seen to differ in the
fewer number of pectoral fin rays, 6 as against
8 (Regan, 1908, p. 246), and in having the
scalloped flaps on the opercle (3-5 versus none).
Although Rofen (1955, p. 182) utilized the
number of scalloped flaps on the lower edge of
the opercle as an important character in dis-
tinguishing the species of this group, our speci-
mens show a rather extensive variation in this
character as aforementioned.
Name.—kK. sexradiata is named in reference
to the six pectoral rays of this fish. The Japanese
name Suna-haze means sand-goby, in reference
to its habitat.
OSTEOLOGY
In this section the skeletal system of K.
sexradiata is described based upon the dis-
section of a specimen, 30.2 mm in standard
length.
Jaws (Fig. 2, A) —The upper jaw consists of
a premaxillary and maxillary. There is no supra-
maxillary. The premaxillary is a stout bar form-
ing the anterior half of the upper edge of the
gape, and armed with about 20 small conical
teeth directed slightly inward. The maxillary is a
well ossified curved bone overlying the dorsal
surface of the premaxillary. The posterior end
reaches to the lower prong of the dentary.
The lower jaw consists of a dentary, articular
and angular. The dentary is the largest bone,
bearing about 23 small conical teeth on the upper
surface. At the anterior end the bone strongly
projects downward. Posteriorly the dentary is
bifureated, the lower prong is longer than the
upper one. The articular is a slender forked bone
attaching to the posterior border of the dentary
re =
2
Fic. 1.—Lateral aspect of holotype of Kraemeria sexradiata, n. sp. Scale bar indicates 10 mm.
JANUARY 1959
and abuts on the condyle of quadrate posteriorly.
The lower wing of the bone becomes slenderer
anteriorly and reaches to below the middle of
dentary. The angular is a small heavy bone
lying on the posterior end of the articular.
Suspensorium (Fig. 2, A) —The hyomandibu-
lar is roughly triangular in shape. Its dorsal bor-
der articulates along the ventrolateral margin of
the pterotic. Posteriorly it articulates with the
opercle by a small condyle. Anterior to the hyo-
mandibular there extends a slender metaptery-
MATSUBARA AND IWAI: A NEW SANDFISH 29
goid. The quadrate is a relatively large bone,
bearing 3 projections. The first projection on the
dorsal surface abuts against the pterygoid. The
second one on the dorsoposterior edge meets the
anterior end of the metapterygoid, and the last
one on the posterior edge extends posteriorly
along the dorsal border of the preopercle. The
bone bears a heavily ossified condyle at its ven-
tral corner for the articulation of the articular
of the mandible. It is a remarkable fact that
there is a broad interosseous space between the
i
Si = —
=_-— — ee
—-—---—- ~- 7 SS — i
Se See ea ae
Fic. 2.—Lateral aspects of jaws, suspensorium (A), lower half of branchial arches (B), upper pharyn-
geal teeth (C), hyoid arch (D), shoulder girdle (EK), and caudal skeletons (F) of K. sezradiata. (Each
sale bar indicates 1 mm. ac, actinost; an, angular; ar, articular; 6b, basibranchial; br, branchiostegal
ray; cb, ceratobranchial; ch, ceratohyal; cl, clavicle; d, dentary; eh, epihyal; ep, epural; gh, glossohyal;
hb, hypobranchial; hm, hyomandibular; hoc, hypocoracoid; hp, hypural plate; hrc, hypercoracoid; zh,
interhyal; zo, interopercle; lp, lower pharyngeal; mp, metapterygoid; mz, maxillary; op, opercle; pa,
aay pm, premaxillary; po, preopercle; pr, pectoral fin ray; pt, pterygoid; g, quadrate; so, suboper-
cle.
30 JOURNAL OF THE
hyomandibular - metapterygoid - quadrate strut
and the preopercle (dotted area in Fig. 2, A).
Symplectic and mesopterygoid could not be
detected, although it is difficult to manifest the
absence of these bones.
The pterygoid is a thin, slender, rodlike bone
lying between the quadrate and the palatine.
Anteriorly it overlies the posterior portion of the
palatine. The palatine is a small and edentulous
T-shaped bone. Its dorsoanterior condyle articu-
lates with the ethmoid region of the cranium
with an intervention of the cartilagenous band.
Opercular series (Fig. 2, A) —All four opercu-
lar elements are present. The preopercle is a
slender bone tapering anteriorly. The anterior
half of it abuts against the ventral border of the
quadrate. Dorsally it meets the ventroposterior
border of the hyomandibular. The opercle is the
largest bone among the opercular series. On the
anterior edge, it bears a small condyle for the
articulation of the hyomandibular. Posteriorly
it is bifurcated into two sharp projections. The
subopercle is quadrant in shape, and lies between
the opercle. and the interopercle. The inter-
opercle, resembling the preopercle in shape, is
attached to the lower edge of the preopercle.
Hyoid arch (Fig. 2, D)—The interhyal is a
small bone, rodlike in shape, and capped with
cartilagenous band at each end. The upper end
of the bone is inserted on the proximal side of
the juncture between the hyomandibular and the
preopercle, and the lower end is attached to the
dorsoposterior end of the epihyal. The epihyal is
a flat, nearly triangular bone. The ceratohyal is
a well ossified bone. The anterior half is slender,
but the posterior half is abruptly expanded, be-
ing nearly as wide as long and about three times
wider than the anterior half. The posterior end is
sturdily jomed with the epihyal. The hypohyal
is not discernible.
There are 5 long branchiostegal rays, the last
of which articulates with the junction between
the epihyal and ceratohyal. Another 4 are set
on the ceratohyal, the anteriormost one of which
is attached to the slender portion of the bone
and widely separated from the other 3 which are
attached to the wider section.
The glossohyal is edentulous. It is a flat, fan-
shaped bone having a shallow notch at the tip
(Fig. 2, B, gh). Posteriorly it articulates with the
first basibranchial. se
Branchial arch (Fig. 2, B)—The branchial
apparatus consists of five branchial arches di-
WASHINGTON ACADEMY OF
SCIENCES VOL. 49, No. l
minishing in size posteriorly. The median floor
of the arches is composed of 3 basibranchials
which he longitudinally behind the glossohyal.
All bones are rodlike in shape. There are hypo-
branchials on the first three branchial arches.
The hypobranchial of the first arch is a slender
bone with a projection at the anterior bend, an.
meets the first basibranchial. That of the second
arch is similar to the first bone in shape, but about
half as long as the first one. The third one is
modified into a small tridentate bone. There are
five slender ceratobranchials decreasing in length
posteriorly. Only the first ceratobranchial is
armed with a single row of short gill-rakers. The
fifth one is modified into the lower pharyngeal
bone bearing three rows of small conical teeth,
apparently separated from the fellow of the op-
posite side (Fig. 2, B, lp).
Epibranchials are present on the first three
arches. Since all of these bones are not well
ossified, their detailed structures are obscure.
The upper pharyngeal teeth are confined to a
small patch on bony plate extending on the
third and fourth branchial arches. The plates on
two sides are not fused together along the me-
dian line (Fig. 2, C).
&
Sp
bo
Fic. 3—Cranium of K. sexradiata: (A) Dorsal
aspect and (B) ventral aspect. (Scale bar indicates
1 mm. as, alisphenoid; bo, basioccipital; ep, epiotic;
ex, exoccipital; fr, frontal; me, mesethmoid; pf,
prefrontal; po, prootic; ps, parasphenoid; pt, ptero-
tic ; ptm, posttemporal; so, supraoccipital; sp, sphe-
notic; v, vomer.
po
JANUARY 1959
Cranium.—oOn the dorsal aspect (Fig. 3, A),
the anterior corner of the cranium is occupied
with an unpaired thin bone which is thought to
be mesethmoid. Anteriorly it is broadened and
extends ventroanteriorly to the dorsal surface of
the vomer.
' The prefrontals are merely small rodlike bones
on the lateral edges of the mesethmoid and not
joined directly with the mesethmoid, but at-
-tached with the latter by an intervention to the
eartilagenous patch.
The frontals are the largest flat bones cover-
ing a vast part of the top of the cranium. At
the interorbital region, they are abruptly con-
stricted in width and so securely fused together
along the midline that the suture is not apparent
on this region (Fig. 3, A, fr). The anterior end
of the fused frontal overlies the mesethmoid. Be-
hind the orbit each frontal expands and abuts
against the sphenotic and pterotic laterally, and
against the supraoccipital and epiotic posteriorly.
The dorsal surface of the sphenotic is nar-
rowly exposed along the lateral border of the
frontal.
The pterotics are slender bones lying behind
the sphenotics. Each bone meets the frontal lat-
erally and epiotic posteriorly. The latero-poste-
rior end of the bone is pointed.
The parietals appear to be absent.
The supraoccipital is a median dorsal bone
extending between the frontals and also epiotics.
Its rhombic dorsal portion is well ossified. It is
separated from the exoccipital by an intervention
ct the epiotic.
The epiotics form a portion of posterolateral
edge of the cranium. The dorsoposterior part of
each bone receives the anterior end of the post-
temporal. The bone is bounded with the pterotic
and frontal anteriorly and with the exoccipital
posteriorly. Mesially it meets the counterpart
of the opposite side at the midline, and separates
the supraoccipital from the exoccipital.
The exoccipitals contribute to form most of
the posterior surface of the cranium. They meet
along the dorsal median line. Dorsally the bone
slightly overlies the epiotic. In the ventral aspect
they curve ventroanteriorly to meet the dorso-
posterior edge of the basioccipital.
On the ventral aspect (Fig. 3, B),. the vomer
forms the anterior corner of the cranium. It is a
fanlike bone with a rather deep notch at the
tip. Posteriorly it becomes abruptly narrower,
sliding under surface of the anterior part of the
MATSUBARA AND IWAI: A NEW SANDFISH 1
parasphenoid. No teeth could be found on the
vomer.
The parasphenoid, running along the midline
of the ventral surface of the cranium, is a long
narrow bone. From near the bilobed posterior
end over the basioccipital the bone widens ante-
riorly and sends the lateral wings on both sides
extending toward the prootics. Then it becomes
narrow between the orbits and the anterior end
is inserted between the vomer and the ethmoid
cartilage.
The median basioccipital forms the posterior
end of the ventral surface of the brain case. An-
teriorly, it 1s deeply excavated and each arm
attaches to the parasphenoid and prootic. Poste-
riorly it is thickened to form a condyle for the
articulation of the atlas.
There is no opisthotic. The portion of the otic
bulla is covered by the interosseous membrane
(posterior dotted area in Fig. 3, B).
Each prootic forms a suture for the alisphe-
noid anteriorly, for the parasphenoid ventrally,
for the pterotic dorsally, and for the basioccipital
posteriorly.
The alisphenoids are slender elements and they
are united dorsoanteriorly under the frontals.
There is no basisphenoid.
Shoulder girdle (Fig. 2, E) —Although almost
all the skeletal elements are present in the shoul-
der girdle, the ossification is imperfect. The post-
temporal, hyperecoracoid, and hypocoracoid are
much reduced in size. The posttemporal is a
simple strut and is bound tightly to the upper
edge of the epiotic. Ventrally it articulates with
the dorsal edge of the supraclavicle which is
slender in shape.
The dorsal extremity of the clavicle is shal-
lowly furcated. It extends ventroanteriorly and
is forklke in general appearance.
The hypercoracoid, rectangular in shape, lies
behind the clavicle. The dorsoposterior edge
meets the lowermost actinost.
The hypocoracoid is roughly triangular in
shape and attached to the posterior edge of the
lower bend of the clavicle. It is well separated
from both the hypercoracoid and actinosts.
There are 3 large actinosts with a large fora-
men between each of them, all of them lying a
short distance behind upper portion of the clav-
i@le (ine, 2, 18, Ge).
No postelavicle could be recognized.
Caudal skeletons (Fig. 2, F)—AIl hypural
bones are fused together and modified into a
32 . JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
fan-like plate (Fig. 2, F, hp). It is deeply ex-
cavated at the middle of the posterior border.
The suture between the urostyle and hypural
plate is obscure. There is a single epural above
the upper border of the hypural fan. The neural
process of the urostyle is separated from the
hypural plate and directed upward. There is a
splint-like bone between the hypural plate and
the last haemal spine. The last two vertebrae
contribute to support the caudal fin rays.
There are 26 vertebrae including hypural
plate.
CONSIDERATIONS AND CONCLUSION
In general, the osteological features of K.
sexradiata agree with those of K. samoensis
as given by Gosline (1955, pp. 158-170),
with the exception of some minor points.
The differences between them are as fol-
lows: (1) Gosline drew a large symplectic
bone below the metapterygoid, but so far as
our observations go, the bone recognized by
him as symplectic appears to be a bony
shelf extending from the metapterygoid.
Evidence that the interhyal bone articulates
with the juncture between the preopercle
and the posterior end of the quadrate
strongly suggests that the reduced sym-
plectic bone, if present, may lie near this
area. (2) Although Gosline stated that the
alisphenoid appears to be lacking, in our
specimen this paired bone is recognizable
in front of the prootic. (3) Lower pharyn-
geals are evidently separated in our species
versus they are entirely fused without su-
ture in samoensis. That the individual bones
of the skeletal system in such small fishes
as Kraemeria are not sufficiently demar-
cated owing to unsatisfactory ossification
might explain these differences.
Koumans (1931, p. 14) included the
Psammichthyidae (=Kraemeriidae) in the
order Gobioidea. Schultz (1941, p. 269)
stated that Kraemeria has features that re-
semble the trichonotids more than the go-
bids.
Gosline (1955, p. 165) placed Kraemeria
in a distinct family Kraemeriidae and as-
signed the latter to the suborder Gobioidei
on the basis of the following features: (1)
the parietals are absent, (2) the branchio-
stegal rays are 5 in number, the first one of
which is far separated from the others, (3)
there is a broad interosseous space between
vou. 49, No. 1
the metapterygoid and preopercle, and (4)
the hypural plate bears detached splint-like
bone on both dorsal and ventral sides. He
concluded that these features of Kraemeria
agree with those of gobioid fishes but dis-
agree with those of both blennid and tri-
chonotid fishes.
Results of our osteological observation,
as well as such peculiar external features as
steeply projected lower jaw and scaleless
body would be sufficient to justify the re-
tention of Kraemeria in a separate family.
On the other hand, the fishes of the genus
Kraemeria seem to be closely related, in
general physiognomy, to those of the family
Trichonotidae. But, at the present, there is
no adequate information on the osteological
features of the trichonotid fishes, which will
enable us to compare both groups. Accord-
ingly, the decision whether the family Krae-
merlidae belongs to the suborder Gobioidei
or other separate suborder, should be with-
held until such a time as more information
becomes available concerning the anatomi-
cal features of the trichonotid fishes, al-
though the fact that the pelvic fins are
united for one-fifth the length of inner rays
by a membrane in Kraemeria tongaensis
and for their full length in Gobitrichinotus
radiocularis (Rofen, 1958, p. 182), both of
which are referred to Kraemeriidae, may
support Gosline’s conception concerning the
allocation of Kraemeriidae to the gobioid
eroup.
REFERENCES
GostinE, WitiiAM A. The osteology and rela-
tionships of certain gobioid fishes, with particu-
lar reference to the genera Kraemeria and
Microdesmus. Pacific Sci. 9(2): 158-170, 7
figs. 1955.
Koumans, F. P. A preliminary revision of the
genera of the gobioid fishes with united ventral
fins: iv + 174 pp. Lisse, 1931.
Martsupara, Kryomatsu. Fish morphology and
hierarchy 1: xi + 789 pp., 289 figs. Tokyo, 1955.
Recan, CuHarutes Tate. Report on the marine
fishes collected by Mr. J. Stanley Gardiner in
the Indian Ocean. Trans. Linn. Soc. London,
Zool. (2) 12(13): 217-255, 10 pls. 1908.
Roren, Ropert R. The marine fishes of Rennell
Island. In “The natural history of Rennell
Island, British Solomon Islands’ 1: 149-218,
1 fig., 11 pls. Copenhagen, 1958.
ScHuitz, Leonatp P. Kraemeria bryani, a new
species of trichonotid fish from the Hawaiian
Islands. Journ. Washington Acad. Sci. 31(6):
269-272, 1 fig. 1941.
JANUARY 1959
NOTES AND
NEWS 33
“NIGHT-GOWNED” FISHES
There are fish that wear “nightgowns.” They
are among the most resplendent of all sea crea-
tures. They have teeth in their throats. These are
the “parrotfishes,” a family distributed world-
wide through tropical waters where they fre-
quent coral reefs. The first systematic zoological
description of this group as a whole, by Dr.
Leonard P. Schultz, U. S. National Museum
curator of fishes, has recently been published by
the Smithsonian Institution.
The strange practice of donning night robes
before retiring, cited in the report, is an ob-
servation by Dr. Howard E. Winn, of the Uni-
versity of Maryalnd, and presumably is re-
stricted to one or two species found in West
Indian waters. These fishes pass the hours of
darkness resting on the shallow sea bottom. They
lean against rocks, arms of coral, or other stable
objects. Sometimes they retire inside conch shells.
But as night approaches the fish starts secreting
a transparent mucous envelope from a special
secretory system. It starts with the mouth and is
extended backward, until the transparent enve-
lope completely encloses the body. There is a
little flap with a hole in the center in front of
the open mouth. There is another small hole at
the rear. The mouth flap moves back and forth
as the animal breathes. The openings assure a
constant flow of water around the gills, without
which the animal could not live.
The entire process of nightgown-making re-
quires from a half hour to an hour-and-a-half.
It stops entirely, Dr. Winn observed, whenever
hight was turned on the aquarium but was re-
sumed immediately with darkness. As the folds
progress the breathing rate is reduced. The pur-
pose of wearing nightgowns can only be sur-
mised. The thin garments, he believes, may afford
some sort of protection against nocturnal en-
emies. Also it may protect the body from be-
coming surrounded by silt.
The gown-weaving, as well as the practice of
spending the night leaning against some solid
object, apparently is dictated by some nervous
mechanism which is set off by darkness. So far
as known, the practice is unique in nature. But,
as cited by Dr. Schultz, this is only one of the
parrotfish curiosities. Colors, of males, become
more and more brilliant as adulthood is ap-
proached, and a fully matured individual of some
species 1s one of the handsomest denizens of the
deep. Females of some species, however, may re-
main throughout life rather drab individuals.
“Many species,’ says Dr. Schultz, “pass
through from one to three color phases. In gen-
eral these are Juvenile, in which the color may
consist of two or three alternating dark and
light streaks, or spots that are dark or mottled
pale and dark; immature, in which the color pat-
tern is usually some shade of red, brown, or
purple; and adult, in which the color pattern
seems to be reached somewhat before or at sexual
maturity, with the predominating colors gen-
erally green, blue, pink, red, orange, and yellow.
A few species are brownish. Some of these are
females, but the males predominate in shades
of green or blue and with green teeth.”
Color changes, it is explained, are a factor
which makes species classification quite difficult.
Living in the shelter of coral banks and quite
secretive in their ways of life these parrotfishes,
or Secaridae, have remained among the least
known of the fish groups.
Their food, for the most part, consists of
algae which are scraped from the coral branches.
This necessitates the so-called pharyngeal mill,
or teeth in the throat, designed to crush coralline
algae, coral fragments, and other food items. The
upper pharyngeal teeth are paired and fit snugly
against the base of the skull. The number of rows
on each upper pharyngeal bone varies from one
to three, according to genera. The lower pharyn-
geals consist of a single bone with a toothed sur-
face. This arrangement constitutes a grinding
mill operated by powerful muscle attached to the
shoulder girdle and base of the skull.
Some species, Dr. Schultz points out, appar-
ently have a very wide distribution, while others
have very restricted habitats, but more collect-
ing in numerous island groups will be required
before the distribution of individual species can
be determined.
Major regions where these strange animals
are found are the central and west Pacific,
Hawaiian and Johnston Islands, some offshore
islands of the east Pacific adjacent to the Ameri-
can continents, west Atlantic and Bermuda, east
Atlantic, the Indian Ocean, Andaman Islands,
and Ceylon. There are about 80 valid species for
the whole world, the report says.
34 JOURNAL OF THE
COMPRESSIVE PROPERTIES OF
For many years the National Bureau of Stand-
ards dental research laboratory has investigated
the basic properties of dental materials in co-
operation with the American Dental Associ-
ation and the Federal dental services. As part
of this program, a study was recently under-
taken by J. W. Stanford and G. C. Paffen-
barger, research associates of the American
Dental Association, and J. W. Kumpula and
W. T. Sweeney of the Bureau staff to obtain
precise data on the compressive properties of
human enamel and dentin.* Data derived from
the work will be used in evaluating dental fill-
ing materials, in designing cavity preparations,
and in demonstrating physical changes in teeth.
In the past, abundant information has been
compiled on the properties of restorative ma-
terials used in dentistry, but relatively few data
have been published about hard tooth tissue, the
foundation for these materials. An obvious ex-
planation for this lack is the limited supply of
human enamel and dentin available, and the
difficulties inherent in testing small specimens.
However, since a successful dental restoration
depends equally on the restorative material and
the tooth, knowledge of both is necessary.
In the Bureau tests of human enamel, the
highest strength, modulus of elasticity, and pro-
portional limit were obtained for specimens of
cusp enamel, the tapering projections on the
crown of the tooth. Intermediate values for
these properties were found for specimens pre-
pared from the sides of teeth; and lowest values
for the occlusal surface or chewing part of molar
teeth. Although dentin showed a higher com-
pressive strength than did enamel, it had a lower
modulus of elasticity.
The specimens used in the tests were prepared
from freshly extracted teeth. Made in the shape
of cylinders 0.044 inch in diameter and from
0.075 to 0.082 inch in length, they were ground
from block sections of enamel, dentin and combi-
nations of the two. All cutting and grinding
operations were accomplished under a steady
dripping of water on the field of cutting.
After the specimen ends were made plane and
parallel, the specimen was placed upright in a
* For further technical details, see Determination
of some compressive properties of human enamel
and dentin, by JoHN W. StTanrorpD, G. C. PAFFEN-
BARGER, JOHN W. Kumpua, and W. T. SWEENEY,
Journ. Amer. Dental Assoc. 57: 487. 1958.
WASHINGTON ACADEMY OF SCIENCES
voL. 49, no. l
HUMAN ENAMEL AND DENTIN
testing machine between two hardened steel
platens. Because of the small size of the speci-
mens, two optical strain gages had to be fastened
across the specimen length on the sides of the
platens (rather than on the specimen). These
strain gages were used to determine the deforma-
tion occurring in the specimens under load. In
conducting the tests, the 0-1,000-pound range
of a 2,000-pound-capacity testing machine was
uesd to measure the loads as they were applied.
The strain measurements included errors re-
sulting from deformations in those portions of
the steel platens within the gage length, and
possible non-parallelism of the platens. To evalu-
ate these errors, tests were conducted on metals
for which the moduli of elasticity are well known.
Small cylinders of carbon steel, aluminum alloy,
and magnesium alloy, were prepared in a manner
similar to that used in preparing the tooth speci-
mens, and were tested in compression. The re-
sults obtained with these metals were used to
correct the experimentally determined moduli of
elasticity of the hard tooth tissues.
Stress-strain diagrams derived from the data
showed an important difference between the
enamel and the dentin. The enamel, largely in-
organic, showed little plastic flow in comparison
with the more organic dentin. This is also shown
by the data in Table 1. It was found that the
more brittle enamel broke at a load slightly
higher than its proportional limit, while the
dentin exhibited plastic flow from its propor-
tional limit of approximately 25,000 psi up to
its compressive strength of about 50,000 psi.
Average values computed for the three enamel
areas range from 1.8 X 10° to 8.2 x 10° psi for
modulus of elasticity; 15,000 to 34,000 psi for
TABLE 1.—CoOMPRESSIVE PROPERTIES OF
Human ENAMEL AND DENTIN
| Modulus | Propor- | Compres-
Material of tional sive
elasticity | limit strength
10 psi} psi psi
Enamel:
Caspers Seen ke 8.2 | 34,200 | 40,200
roid (sevens «eRe 1 ged 21,200 | 28,200
Occlusal surface...| 1.8 | 15,400 | 18,200
Denting Ass ar ee 25,100 | 50,400
Dentin and enamel... 3.6 | 23,900 | 34,200
JANUARY 1959
proportional limit; and 18,000 to 40,000 psi for
compressive strength. In tests of dentin speci-
mens, values determined for these three proper-
ties, in the same order, are 2.2 X 10° psi; 25,000
psi; and 50,400 psi. These values for dentin
are comparable to values previously found by
Peyton, Mahler, and Hershenov.* The crushing
NOTES AND NEWS 39
strength of both enamel and dentin earler re-
ported by G. V. Black® is not inconsistent with
the values for compressive strength derived from
the present study.
* Physical properties of dentin, by F. A. Peyton,
D. B. Mauer, and B. HersHenov, Journ. Dent.
Res. 31: 366. 1952.
® Physical characters of the human teeth, by G.
V. Buack, Dental Cosmos 37: 353. 1895.
EXPERIMENTAL MAP PAPERS CONTAINING SYNTHETIC FIBERS
The National Bureau of Standards, in work
sponsored by the Army Engineer Research and
Development Laboratories, has investigated the
strength characteristics of synthetic-fiber map
paper. Tests for dimensional stability, folding
endurance, and bursting and tearing strengths
were made on specimens of three experimental
handsheets and two commercially produced pa-
pers. Results show that a polyester-cellulose
sheet has high dimensional stability, a pre-
requisite for military map paper, and better
strength properties than commercial map paper.
A paper containing polyamide fibers has low
dimensional stability, but exceptional folding,
tearing, and bursting strengths.’
For many years the Bureau has conducted re-
search on the properties of paper and related
materials. In previous experiments a dimen-
sionally stable paper, that is, a paper with low
moisture expansivity, was developed by laminat-
ing two thin sheets to a backing of polyester film-”
G. L. McLeod of the Bureau staff undertook the
present study to find out whether synthetic
fibers with less affinity for water than cellulose
could impart the desired moisture stability to
map paper. Also, while cellulose is and probably
will remain the backbone of the paper industry,
erowing interest is being displayed in the use of
synthetic fibers to improve the properties of
special-purpose papers.
Initial attempts to prepare handsheets from a
suspension containing 100 percent synthetic fi-
bers were unsuccessful. The sheets tore and dis-
integrated when removed from the mold. A
suspension was then prepared containing cellu-
1¥For further technical details, see Properties of
some experimental map papers containing syn-
thetic fibers, by G. L. McLznop, TAPPI 41: 430.
1958.
“Improved dimensional stability in laminated
paper, by G. L. McLzrop and THrEtma L. Works-
MAN, TAPPI (in press); and Improved map paper,
NBS Tech. News Bull. 42: 148. 1958.
lose fibers and synthetic fibers in a 1-to-3 pro-
portion. From this suspension it was possible to
produce handsheets that could be manipulated
and treated with an acrylic binding agent. After
treatment, the sheets were dried for 1 hour in a
forced-air oven, and cured in a flat-bed press at
160°C with a pressure of 300 lb/in.’ for 45 sec-
onds. The synthetic fibers in the three different
handsheets were poylester, polyacrylate, and
polyamide (nylon). Table 1 shows the results
of tests on these handsheets compared with re-
sults obtained from all-cellulose sheets made with
the same handsheet apparatus.’
Similar tests were conducted on machine-made
paper containing 40 percent synthetic fiber, 40
percent cellulose rag fiber, and 20 percent acrylic
binder. Only two of the synthetic fibers, poly-
ester and polyamide, were used in the machine-
made paper. Table 2 gives the results of these
tests compared with identical tests on commer-
cial map paper. Included in this table are the
Federal specifications for map paper.
In general, test results of the handsheets and
the machine-made paper follow the same pat-
tern. The polyester-cellulose sheets are superior
in dimensional stability to moisture, and have
higher bursting, folding, and tearing strengths
than does regular map paper. The polyacrylic-
cellulose sheets, tested only in the form of ex-
perimental handsheets, are superior to the poly-
amide-cellulose and the all-cellulose sheets in
dimensional stability but inferior to the poly-
ester-cellulose sheets. The polyamide-cellulose
paper has the lowest dimensional stability of all
the papers tested, which makes it unsuitable for
map paper. However, because of its exceptional
folding endurance and high tearing strength, this
paper map prove to be valuable for other pur-
poses.
No difficulties were encountered in printing on
3Preparation of fiber test sheets, by M. B.
SHaw, G. W. Bickine, and L. W. Snyper, Paper
Trade Journ. 90(16): 7.S. 69. 1930.
36 JOURNAL OF THE
the synthetic-fiber papers, in either black and
white, or in the regular five-color lithographic
process used for Army maps. The smoothness
and opacity ratings of the synthetic fiber sheets
are lower than those of regular map paper, but
these are minor deficiencies which can be easily
WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. 1
overcome. That the synthetic-fiber papers have
less dry tensile strength than commercial map
paper is attributed to the low fiber-to-fiber bond-
ing in the synthetics. Dry tensile strength, how-
ever, 1s a relatively unimportant factor in papers
used for military maps.
TABLE 1.—COMPARISON OF TEST RESULTS FOR HANDSHEETS FROM BLENDS OF 75 PERCENT SYNTHETIC
FIBER AND 25 PERCENT CELLULOSE FIBER WITH 100 PERCENT CELLULOSE HANDSHEETS
Tests performed
Test results
ae Seco One 75% nylon |75% polyacrylate alee
Basis weight (17 X 22-500), in pounds.......... 23.8 34.6 30.2 31.9
‘Thickness,an" intchese ys. oes ee eh ee 0.0054 0.0118 0.0059 0.0108
Expansivity for relative humidity change be-
tween oo and’ 507; sim percent. ner ae et 0.25 0.037 0.014
Folding endurance, Schopper, double folds..... Approx. 1200) 100,000 4260 31,600
Bunshine streneGhrm points aerate ae eee 46 122 86 76
Tensile strength, kg/15 mm:
| DO GaN al nt Ue les rien Lt Ne eis | nailer 25.6 6.1 5.8 4.4
VSG ERPs Seay Pin ate i acto cen Ee etl sen ee ae 2.9 2.0 13 3.5
Teanine strengthenn yeramsway. kee eee 156 864 323 590
TaBLE 2.—TEsT RESULTS OF MACHINE-MADE POLYESTER-RAG,
NYLON-RAG, AND COMMERCIAL Map PAPER
50:50
Tests performed Polyester-rag
Basis weight (17 X 22-500), in
OUTS, Hayate OO sete ee ci ee nee 26.2
Expansivity for relative humidity
change between 65 and 50%:
Machinew direction se see ee 0.059
Cross®directione ee, ae ee 0.10
Brightness, in percent’ 9.) 55.5.4. 83.1
Aciditivs pr hothextractione 4.9: 4.8
Smoothness (Bekk), in seconds..... 33
Water resistance, dry indicator, in
SECOMGS SA HUW, pet ets ee MR Gna eg ieee 94
aLhickness sinminchesp saa ere 0.0052
Folding endurance, Schopper,
double folds:
Machinemdinrection eases) see nner 14,300
Crosseaineciloneatsee se ee 11,300
Bursting strength, in points:
ID) Ci gaee Oe eRe a Meche cats Reni nae da 8 49
WG ti pha geen UN Rd oh rand ae ee 46
Tensile strength, dry, in kg./15 mm:
Machinesdirection..cea5 45a CD
Cross) direction’) nee sare 77
Tensile strength, wet, in kg./15 mm:
Machimedirectione ae a4 see 5.3
Crossidinectionn a. eee 4.2
Tearing strength, in grams:
Machimesidirectionmas a. e 151
Crosse dinectioney ser eae eee 141
Opacity. mapercentaae ee eee 75.8
50:50 Commercial map Federal specification
Nylon-rag paper requirements
22.6 23.7 2 + 5%
0.196 0.071 0.075 max
0.28 OFZ 0.25 max
82.1 CATE 70.1
a.7 5.0 4.5
8 60 50-100
77 70 55
0.0054 0.0041 0.0042 + 0.0005
40 , 000 1410 1000
13.500 1300 1000
50 50 50
30 30 20
6.5 ES 1130
4.5 6.8 6.0
3.4 4.4 3.9
2.3 2.8 2.5
168 85 95
108 94 95
67.1 93 .2 91.0
@ All figures are minimum values unless otherwise designated.
Vice-Presidents of the Washington Academy of Sciences
Representing the Affiliated Societies
Bunesepmical Society of Washington ................26.cecceeeeseees MicHAEL GOLDBERG
muaeepelerical Society of Washington.................---2.--se0e-- FrANK M. SETZLER
mraestiecmcicty Of Washington................0ccee0ccccee le seeee HERBERT FRIEDMANN
wnemmeneseeiety of Washington................-.-ceeeeeececeeeee Aunen L. ALEXANDER
Mamanelorical Society of Washington. ....................00..e80es Haroup H. SHEPARD
BemmnEeUSEAPNIC SOCIELY....5... 00052. c cece eee e ce eeusyes ALEXANDER WETMORE
Pemmeetewuoociciy of Washington.....0..........002-ccnecceeedeenceeces Care H. DANE
Medical seciety of the District of Columbia........................-. FREDERICK O. CoE
MmmmrrreLtisrOnical SOCIety..... 2.2.61... cee ee cee cc ene nee cuesaee U.S. Grant, 3p
Pereaecinemeicry Of Washington.............. 06.0.0. 0 cece c eee enews: CaRROLL E. Cox
Washington Section, Society of American Foresters. ...................-- G. F. GRAVATT
PMP society Of Mngineers..............0.0 0 cece eee eee ecees Howarp S. RAPPLEYE
Washington Section, American Institute of Electrical Engineers....RoBERT D. ELBoURN
feimimpnolerical Society of Washington.......................000% CaRLTon M. Herman
Washington Branch, Society of American Bacteriologists.................. BERNICE Eppy
Washington Post, Society of American Military Engineers......... ALBERT J. HosKINSoN
Washington Section, Institute of Radio Engineers................. Rosert D. HuntToon
National Capital Section, American Society of Civil Engineers....Howarp 8S. RAPPLEYE
D. C. Section, Society of Experimental Biology and Medicine...... KaTHRYN KNOWLTON
Washington Chapter, American Society for Metals.................... JoHn A. BENNETT
Washington Section, International Association for Dental Research..ALPHONSE FoRzIATI
Washington Section, Institute of the Aeronautical Sciences.............. F. N. FRENKIEL
D. C. Branch, American Meteorological Society.................-.--- Jack C. THOMPSON
Washington Section, American Society of Mechanical Engineers...... WiuuraM G. ALLEN
Washington Chapter, Acoustical Society of America................... RicHarp K. Coox
imeeeuerme society of Washington..............02c ces cee eee ee neces FRANK L. CAMPBELL
CONTENTS
Page
ScIENCE ADMINISTRATION.—Pay plans and people. Crawrorp R.
ENToMOLOGY.—A new subfamily, genus, and species of Lygaeidae (Hemip-
tera-Heteroptera) from Australia. Cart J. Drake and NormMan
TODAVIS. 220 a a Re Sn ee 19
IcHTHYOLOGY.—Description of a new sandfish, Kraemeria sexradiata,
from Japan, with special reference to its osteology. Kryvomatsu
MaTsuBara and Tamotsu Iwat. .. .:..-+.:).9.%. 7. 4) 27
Notes anD NEws:
“Night-@owned”’ fishes... . 10.52 ms «he a igectlt oye tet 33
Compressive properties of human enamel and dentin.............. 34
Experimental map papers containing synthetic fibers............. 35
VOLUME 49 Feebruary 1959 NUMBER 2
JOURNAL
OF THE
WASHINGTON ACADEMY
OF SCIENCES
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aS
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A A i ip i
ee ee
bl Bl il i ie ik
t i bee iv
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2 ii TEE ELL ia
= ir ial! A. Had Uepa ———
——<—<—<$—$—$——————
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JOURNAL
OF THE
WASHINGTON ACADEMY OF SCIENCES
Vou. 49
FEBRUARY 1959
No. 2
THE ACADEMY MEMBERSHIP COMMITTEE
The organization of the Membership
Committee of the Washington Academy of
Sciences has been altered to increase its
effectiveness. The Committee now consists
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FEBRUARY 1959
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“DE-LOUSING” SHRIMP
There is a tiny blue-and-white shrimp in the
Bahamas that lives on the “lice” that infest
fishes, sets up permanent de-lousing stations to
which louse-plagued fish make regular visits
like men to barber shops, and which advertises
its places of business by swaying from side to
side and vigorously waving its exceptionally
long white antennae in the water to attract
transient customers.
Specimens of this shrimp, discovered by
Vern and Harry Pederson and collected a few
months ago in the Bahamas by Conrad Lim-
baugh of the Scripps Institution of Oceanogra-
phy of La Jolla, Calif., have just been added
to the marine invertebrate collections of the
Smithsonian Institution.
The phenomenon of fish de-lousing by other
sea organisms often has been described and
probably is world-wide. This, however, is by far
the most complex case ever reported. The
shrimp, as described by Mr. Limbaugh, “sets
up shop” on the head of a sea-anemone, flower-
like member of the coral family, whose petals
are stinging tentacles. These tentacles protect
VoL. 49, NO. 2
FEBRUARY 1959
the tenant from all natural shrimp predators.
The anemone, in turn, cannot survive without
the presence of another species of shrimp at its
base.
The de-lousing shrimp cleans its fish customer
meticulously from head to tail of parasitic cope-
pods, the so-called “lice of the sea,’ often al-
most invisibly minute, which infest most marine
higher organisms. It also removes other minute
parasites and cuts away small patches of dead
tissue. It works inside and out. The fish helps
the shrimp to forage within its gill cavities,
mouth, and throat by opening them one at a
time as the forager approaches them. It also
allows the “barber” to make minor incisions
in its skin to get at parasites which have bored
into the flesh.
Apparently such a shrimp always does a
rushing business. The fish cleaned react to the
waving tentacles by approaching the cleaner,
stopping or slowing down. They even assume
awkward positions, seemingly as if hypnotized.
Sometimes certain varieties may change colors.
Often they will fight for the right to be cleaned,
or “having firsts” on the barber chair, and there
are vicious battles. More docile forms crowd one
another, sometimes completely obliterating the
cleaner from view.
Mr. Limbaugh is engaged in an essentially
world-wide study of fish-cleaner organisms.
There is, he reports, considerable variation in
the complexity of the phenomenon which seems
to have arisen, in its various forms, over long
periods of evolution. Nothing hitherto reported,
however, has approached the complexity of the
Bahama case. There may be, however, other
organisms that maintain permanent cleaning
stations. These, indeed, may constitute a very
important phase of sea biology. The stations
may be set up on individual coral heads, on
reef formations, in sea floor depressions, or
merely in certain general areas.”
Certain species of fish and other organisms,
as well as shrimp, engage in this cleaning ac-
tivity. “In general,” Mr. Limbaugh reported
DE-LOUSING SHRIMP 4]
recently to the Western Society of Naturalists,
“the concept may be expanded to include very
large areas or physical features. I am now
convinced that this is one reason fish visit the
edges of kelp beds, where species of cleaner
fish dominate the fauna. I believe also that many
famous fishings grounds (off the Pacific coast)
may be cleaning stations. Among these I would
include certain islands and shoals.’ He con-
tinues:
Visiting fishes at the small cleaning stations in
the Bahamas showed a definite time pattern in
their daily arrival, obviously related to a diurnal
patterned life. Longer term studies undoubtedly
would have shown seasonal trends. The number
of fish processed at a small station during a six-
hour daylight period may be large, up to 300 for
one cleaning fish. In areas inhabited by thousands
of cleaner organisms, the numerical significance
begins to take on meaning. Often a fish will visit
more than one station and return many times
during the day. This is particularly true of an
injured or sick fish.
In an experiment in the Bahamas, I removed
all the known cleaners from two small isolated
reefs where fishes were particularly abundant.
Within a few days the numbers of fish were
drastically reduced. Within two weeks all except
territorial fishes had disappeared. Many of these
developed white fuzzy blotches, swelling, ulcerated
sores and ravaged fins. Later small shrimp and
juvenile fish cleaners appeared. Most of the original
fish did not return but were replaced by juveniles.
Known organisms involved as cleaners in the
sea include eight families of 21 species of fishes,
several families of shrimps, involving six species,
a worm, a bird, and a crab. Relationships of
cleaners to the cleaned organisms frequently are
so casual as to seem accidental, but in other cases
it involves integrated and complex behavior. In
warm seas, cleaning organisms generally are col-
ored to contrast with their environment. In gen-
eral they are solitary, paired or slightly gregarious.
In temperate waters they are not brightly colored
or contrastingly marked. Often they are highly
gregarious. They are more numerous than in
warmer waters but there are fewer species.
$e ——_ i —
42 JOURNAL OF THE
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 2
GENERAL SCIENCE.—Moon bound.| RaymMonp J. SkeEGEeR, National Science
Foundation.
(Received January 2, 1959)
Man always has been and still is moon
bound. From earliest times he has been fas-
cinated by the very appearances of the
moon. The baby in his crib reaches for the
bright moon; the child in the nursery won-
ders at the “man in the moon.” A Hebrew
story tells that this man was banished to
the moon because he picked up sticks on the
Sabbath; his sticks are now the shadows
on the moon. Young men yearn for a “lady
in the moon,” and old men dream of “‘the old
moon in the new moon’s arms.” Literature?
abounds in fanciful speculations about the
moon, for example, writings of Dante,
Ariosto (“Orlando Furiosa’’), Milton, Jon-
son (‘‘News from the New World Discovered
in the Moon’’), Shakespeare, Donne, Keats
(“Endymion”), Rostand (“Cyrano de Ber-
gerac”). Men have always been susceptible
to wonderful stories about this wonderland.
One of the most celebrated was the so-
called “moon hoax,” which appeared in an
August issue of “The Sun” in 18385. R. A.
Locke, a newspaperman, reported that Sir
John Herschel had just discovered flying
men and animals on the moon by means of
a new large telescope in Africa. The only
truth about the whole account was the rapid
increase in the newspaper circulation. Nev-
ertheless, beneath man’s superficial stories
is a genuine curiosity as to just what is on
the surface of the moon.
As man became interested in nature for its
own sake, he felt a burning desire to “save
the appearances,’ to uncover the ¢vaus
(physies) beneath the dawoyuera (appear-
ances). For example, in Plato’s educational
program for the future leaders of his Re-
public, he discussed the merits of astronomy
*Luncheon address given at the “Unveiling of
the Moon Building,” Sheraton-Carleton Hotel,
Washington, D. C., October 28, 1958.
> Gopwin, F. The man in the moon. 1638; Wit-
KINS, J. The discovery of a world in the moon.
1638; Boon, A. The emperor in the moon. 1687;
Fow er, G. A flight to the moon. 1813; WELLS,
H. G. First man in the moon. 1901; Corriy, C. M.
John Donne and the new philosophy. 1937; Atuor,
K. Jules Verne. 1941; Nicotson, M. Voyages to the
moon. 1948.
as a possible subject, not for its applica-
tions in agriculture or in navigation, but
because of its relation to the intelligible
principles behind phenomena. For centuries
man had been observing the irregular plane-
tary and lunar motions. He saw chaos, he
sought to unveil cosmos; he looked for
order amid the apparent disorder. It was the
fall of a meteorite near Aegos Potamoi in
467 B.C. that stimulated Anaxagoras’s in-
terest in the heavens as a sequence of under-
standable events. He visualized moonlight
as reflected sunlight; he explained the phases
and eclipses of the moon. Above all, he re-
garded the surface of the moon as earth-
like. For this very reason this first philoso-
pher of distinction in Athens was banished
in the so-called golden age of Pericles for
impiety. It was Hipparchus of Nicea who
determined later (about 129 B.C.), par-
allactically, the distance of the moon from
the earth (within 0.1 percent of the modern
value).
The telltale telescope of Galileo revealed
the nature of the heavens in a dramatic way
comparable to that of the visible Sputnik—
far more compelling than any theoretical
speculation. The announcement of the
moon’s appearance was made in the Siderius
Nuncius. In the church of Santa Maria
Maggiore in Rome, a portrait of the Virgin
shows a small picture of the moon as first
glimpsed by Galileo. There one sees out-
lined the mountains of the moon; for ex-
ample, the Apennine range, 450 miles long
and with 3,000 peaks such as Huygens
(19,000 feet high). Galileo himself estimated
the mountains to be about 4 miles in height.
All these ranges have familiar European
names; for America had not yet been ex-
plored in detail. If the moon’s hidden face is
ever revealed to us, mountain ranges there
will undoubtedly be named after those on
our Western Hemisphere. One observes also
many large flat regions, which have been
given fanciful names: the Sea of Serenity,
the Ocean of Storms, the Bay of Rainbows,
the Lake of Death, et al. A moot scientific
FEBRUARY 1959
question today persists as to whether these
areas are actually lava flows or dust bowls.
Particularly striking are craters such as
Archimedes, which is 40 miles in diameter
and which could have been formed by a
meteorite having a weight of 25 billion tons.
For comparison, we think of Meteor Crater
in Arizona, which is less than a mile wide
and which is supposed to have been pro-
duced by a meteorite of only 200,000 tons.
Sad to relate, Galileo too suffered imprison-
ment at the end of his life of research of
the heavens. His view of the moon and other
celestial phenomena did not agree with the
socially accepted doctrine of his times.
There is an apocryphal story that Newton
conceived his theory of gravitation when he
was struck by an apple falling from a tree.
There might have occurred to him the
thought: “Suppose it had been the moon;
suppose the moon were an apple!” “In such
a case,” he might have surmised, “moons
and apples would be subject to the same law
of gravitation—a universal law.” In any
event we have all come to believe that we
do live in a universe with laws that apply
equally to moons and to apples.
In more recent times, a Washingtonian,
Simon Newcomb (1835-1909), director of
the Nautical Alamanac from 1877, became
so fascinated by lunar motions as to in-
vestigate them in considerable detail. You
recall that tidal slowing of the rotating
earth (about 0.001 second in a century) re-
sults in an increasing angular acceleration
and consequential recession of the moon
about ten centimeters each month. Even to-
day lunar motions still present a formidable
challenge to man, including the earth-moon
enigma that these two bodies might have
been closely associated about 5 billion years
ago. More amazing than our ignorance,
however, is our knowledge about the moon
and other astronomical phenomena. How
unbelievably well has man succeeded in
“saving the appearances’ —without ever go-
ing to the moon! Laplace’s remark is still
worth considering: ‘Because of the majesty
of its subject and the perfection of its the-
ories astronomy is the most beautiful monu-
ment of the human spirit, the noblest claim
of its intelligence.”
It is not surprising, therefore, that much
SEEGER: MOON BOUND 43
science fiction has been written with respect
to our nearest neighbor in space. A partic-
ularly interesting book was written in 1900
by Newcomb himself.® It tells of a Harvard
professor of molecular physics who began
about 1941 a secret project in a brickyard
on a nearby Potomac Island. Later he ex-
panded his operations to the island of Elba,
where he built Uraniberg (a heavenly city)
in the tradition of Tycho Brahe. His unique
invention was a space ship, which had been
made possible by the discovery of a new
material called etherene. Its reaction with
ether vibrations was conceived to be analo-
gous to that of the wings of a bird with the
air through which it flies. A new source of
energy, therm, akin to electricity, was also
available. The time came for the unveiling
of the motes, as these space ships were called
(hi motes traveled a hundred miles high).
Newcomb noted that Professor Gale, an
English physicist, believed such motion to
be impossible owing to air friction. He over-
came this difficulty by flying the ships above
the atmosphere, the height of which was
found on flight to be greater than that pre-
viously calculated. On the occasion of the
unveiling, formal invitations were sent to
the President of the United States, to the
heads of the several Government depart-
ments, to members of the Judiciary, to high
officials of the Army and Navy, as well as
to presidents and professors of various uni-
versities. A dinner was arranged in their
honor prior to the unveiling ceremony.
About one-third of the individuals offered
excuses for not coming, another third came
in order to see who the third third really
were that could be seriously interested in
such a subject. The book concluded by re-
vealing the true motivation of the project
and its secrecy; it was aimed at the estab-
lishment of a “defender of the peace of the
world.”’ In the same spirit, United States
satellites today are rightly called Explorers
and Pioneers, for they are much more sig-
nificant as rockets for peace than as mis-
siles for war. So much for the superscience
of Newcomb’s fiction!
In a strictly technical paper* on “The
Outlook for the Flying Machine,” Newcomb
* Newcomp, S. His wisdom—the defender. 1900.
* Newcoms, 8S. Sidelights of astronomy. 1906.
4+ JOURNAL OF THE
reviewed later (1906) Langley’s aircraft
failure. He concluded, “Let us discover a
substance a hundred times as strong as
steel, and with that some form of force un-
suspected which will enable us to utilize
this strength, or let us discover some way
of reversing the law of gravitation so that
matter may be repelled by the earth in-
stead of attracted—then we may have a
flying machine. But we have every reason
to believe that mere ingenious contrivances
with our present means and form of force
will be as vain in the future as they have
been in the past.”
Truth has once again turned out to be
stranger than fiction. The accomplishments
of our age surpass not only the sober ex-
pectancy of great scientists of yester years
but even their science fiction. I wonder what
Simon Newcomb would say if he knew that
we are now shooting for the moon.
In all our technological development,
however, we need to distinguish carefully
both between science and science fiction,
and between science and technology. We
speak of these times as a space age. Yester-
day it was an atomic age. In neither case
has it been truly a scientific age. At a meet-
ing of the Federal Schoolmen’s Club in
Washington last year, a talk was given
about satellites. At the end two educators
asked these questions: (1) ‘““What keeps the
satellite up?” (2) “What keeps it going?”
Mind you, 300 years after Newton had told
clearly how well-behaved moons travel in
public space!
What is science? It is not information,
please! It is not mysterious gadgetry! It is
not powerful magic! Science, 1.e., knowledge,
is the result of the use of the scientific
method, a method that is peculiar to the
scientist. May I stress again that the “what”
of science is less important than the “how”
of the scientific method, all of which is
meaningless except in terms of the “who,”
the scientist that observes, that relates, that
imagines. As Henri Poincaré once said,
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, NO. 2
“Science is no more a collection of facts than
a house is a collection of stones.” The end
of science is a comprehensive view, an 1m-
aginative vista, an interpretive theory. Its
means is a workshop, 1e., a laboratory.
Work, let us remember, can and should be
adventuresome; it can and should be won-
der-full; it can and should be joy-full. The
scientist in his laboratory is akin to the
artist in his studio; to the child in his
kindergarten. Science, above all, can and
should be fun-full; for science is explora-
tion. With our modern satellites we are now
abel to reach the upper atmosphere, the very
edge of the earth, where we meet incoming
cosmic rays and meteors from outer space.
The surface of the moon is a member of
our planetary family that affords unusual
physical conditions. The very lack of an
atmosphere, as indicated by the sharpness
of the moon’s shadows, allows incoming
radiation there to be free from atmospheric
influences. The surface, too, is free from
erosion although it undergoes large tempera-
ture changes from minus 243° F. to plus
214° F. on a single day. It is evident that
any design for building on the moon must
necessarily be quite different from that on
the earth. For example, gravitational force
there is only one-sixth as great so that the
weight of building materials will actually
be less on the moon than on the earth.
The inertial mass, however, remains the
same. Consequently, vibrational phenom-
ena, which involve both gravitational
stresses and inertial masses, will behave
quite differently from those upon the earth.
We moderns are literally moon bound.
We dream of Luniberg, a city on the moon,
with buildings that are truly out of this
world. We visualize a lunar observatory for
man’s penetration into the space about him
and his reflection upon the earth he has left
behind him.
Meanwhile, as we stand moon bound on
the earth, let us all insist upon a scientific
outlook!
Frespruary 1959
RUDD: STUDIES IN AESCHYNOMENE 45
BOTAN Y.—Supplementary studies 1n Aeschynomene, I: Series Viscidulae, includ-
ng a new species and fwe new varieties. VELVA E. Rupp, U. S. National
Museum.
(Received February 13, 1959)
A considerable number of Aeschynomene
specimens have come to my attention since
publication of “The American Species of
Aeschynomene” (Contr. U.S. Nat. Herb.
32: 1-172. 1955). Some of these specimens
are old, representing collections that have
been ascribed to “familiar,” widespread
species without critical examination or that
have spent years in the limbo of “indet”’
folders. Others are types and historical col-
lections that I did not have access to earlier.
Among such specimens I find a few that
I believe to represent new taxa and others
that amplify the concepts of the old. This
paper is essentially a recapitulation of the
Viscidulae series of the genus Aeschynom-
ene, but without repetition of detailed de-
scriptions and explanations of synonymy
given before. Included in this treatment is
the description of one new species and five
new varieties, presentation of a new specific
name for an old variety, and reinstatement
of two old specific names that have been
kept in synonymy for a century or so. Ma-
terial from the Old World is also considered.
A revised key is provided.
For the material on which this study is
based, I am deeply grateful to the curators
of the herbaria cited, for their help in pro-
viding types and other pertinent specimens.
The initials of the herbaria, as cited, are
those of Lanjouw and Stafleu (Index Her-
bariorum, ed. 3. 1956).
This series, named for the earliest de-
scribed species of the group, Aeschynomene
viscidula Michx., includes a few closely re-
lated species of the section Ochopodium
Vog. The plants are disconcertingly similar
in appearance, all prostrate to suberect her-
baceous or suffrutescent perennials arising
from woody roots. The leaves, flowers, and
fruits are relatively small, the leaflets rang-
ing from about 2 to 30 mm long, the flowers
from 5 to 13 mm long, and the articles, or
joints, of the loments from 2 to 5 mm in
diameter. The stipules are attached at the
base, and the calyx is campanulate with five
subequal lobes, or teeth.
In general, characters of the fruit are
the most useful for separating the taxa. The
number of articles can be counted, the
length of the stipe and the dimensions of
the articles can be measured. The kind and
degree of pubescence is distinctive in a few
species. Unfortunately, there is some insta-
bility, especially in certain species, that
casts suspicion on the genetic composition
and presents difficulties in key construction.
Since full descriptions are not included
in this paper, except for new taxa, the fol-
lowing rather detailed key is presented.
KEY TO SPECIES AND VARIETIES
Fruit (1-) 2- or 3- (rarely 4- or 5-) articulate and
short-stipitate, the stipe commonly 1-4 mm
long, scarcely extending beyond the calyx, or,
in a few cases, 5-7 mm long; bracteoles usually
about half as long as the calyx or longer.
Leaves 5-9-foliolate, the leaflets obovate to cu-
neate; articles of fruit (3-) 4-5.5 mm in di-
ameter.
Articles densely white-tomentulose and usually
also beset with glandular hairs, sometimes
the terminal article glabrate, 35-4 mm in
diameter; stipe of fruit 1-3 mm _ long,
mostly contained within the calyx (south-
ern United States to northern and eastern
South America)......... 1. Ae. viscidula
Articles glabrous to moderately appressed-pu-
bescent, (3-) 4-5.5 mm in diameter; stipe
of fruit 2-7 mm long, usually extending
1-4 mm beyond the calyx.
Fruit with articles 4-55 mm in diameter,
glabrous, the stipe 4-7 mm long; brac-
teoles about as long as the calyx (Mex-
1G Olay ae ores act St ie 2. Ae. acapulcensis
Fruit with articles about 3-4 mm in diame-
ter, appressed-pubescent to glabrate, the
stipe 2-7 mm long; bracteoles about
one-half as long as the calyx (South
Africa; Madagascar; Mauritius; Ré-
union; eastern Australia)
3. Ae. brevifolia
Leaves 10-32-foliolate, the leaflets obovate to lin-
ear-oblong, occasionally some leaves with
fewer leaflets; articles of fruit 2-3 (-5) mm in
diameter.
Stipe of fruit 3-7 mm long, commonly hispidu-
lous with hairs about 1 mm long.
46 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
Surface of articles crisp-pubescent to subgla-
brous and also best with glandular hairs;
stipe 3-4 (-5) mm long; leaves mostly
10-20-foliolate, the leaflets obovate to ob-
long.
Fruit 2- or 3-articulate, rarely 4-articulate,
the stipe 3-4 mm long; leaves predomi-
nantly 10-14-foliolate, the leaflets obo-
vate or obovate-elliptic.
Flowers 5-8 mm. long; articles of fruit 2.5—-
3 mm long, 2-3 mm wide (widespread
in tropical America)
4a. Ae. brasiliana var. brasiliana
Flowers about 10 mm long; articles of
fruit 4-5 mm long, 3-4 mm wide (Up-
per Orinoco, Venezuela)
4b. Ae. brasiliana var. carichanica
Fruit 4- or 5-articulate, the stipe 4-5 mm
long; leaves 14-20-foliolate, the leaflets
oblong or obovate-oblong (northern
Venezuela)
4c. Ae. brasiliana var. venezolana
Surface of articles crisp-puberulent to glabrate ;
stipe 5-7 mm long; leaves about 20-32-
foliolate, the leaflets elliptic (Minas Ge-
LATS SEAZI) epee eae a 5. Ae. vogelii
Stipe of fruit 15-3 mm long, hispid, the hairs
2-4 mm long, concentrated at base of the
first article; surface of articles glabrous to
moderately pubescent but lacking glandular
hairs.
Articles of fruit 2-2.5 mm in diameter; flowers
4-7 mm long; leaflets entire, oblong-ellip-
tic, rarely somewhat obovate.
Leaflets 4-6 (-8) mm long, 1.5-8 mm wide;
stipules linear-lanceolate, about 1 mm
wide at the base, 4-5 mm long; stems
usually prostrate.
Fruit with articles glabrous to moderately
crisp-puberulent; stems and leaves
moderately pubescent or often gla-
brate (widespread in Central and
South America)
6a. Ae. histrix var. histrix
Fruit with articles appressed-pubescent ;
stems and leaves canescent (Central
and South America; one collection
from Florida)
6b. Ae. histrix var. incana
Leaflets 7-12 mm long, 2-4 mm wide; stip-
ules broadly lanceolate, usually 2-3 mm
wide at the base, 5-15 mm long; stems
suberect (Mexico to South America)
6c. Ae. histrix var. densiflora
Articles of fruit 2.6-3 mm in diameter; flowers
7-9 mm long; leaflets setiferous, ovate or
linear-oblong, or sometimes entire and
linear-oblong.
Leaflets 2-5 mm long, 1-2 mm wide, ovate
to elliptic-oblong, each bearing one or
more yellowish, bulbous-based, glandular
setae (Paraguay; Missiones, Argentina)
6d. Ae. histrix var. multijuga
VoL. 49, No. 2
Leaflets 5-10 mm long, 15-2 mm wide, lin-
ear-oblong, entire of ciliate (Paraguay)
6e. Ae. histrix var. apana
Fruit 4-9-(infrequently fewer) articulate and long-
stipitate, the stipe (4-) 5-15 mm long; brac-
teoles about 1 mm long, or one-third as long
as the calyx.
Articles of fruit 2-25 mm in diameter; stipe
commonly 10-15 mm long; leaves mostly
10-18-foliolate, the leaflets obovate or obo-
vate elliptic (widespread in tropical Amer-
ICL) ee 7a. Ae. elegans var. elegans
Articles of fruit 3-5 mm long, 25-4 mm wide.
Leaves predominantly 9-32-foliolate.
Flowers 5-10 mm long; fruit with articles
3-4 mm long and 3 mm wide.
Leaflets obovate or obovate-elliptic;
leaves 5-14-foliolate; stipe of fruit
(4-) 5-8 mm long.
Fruit with articles 3-4 mm long and 3
mm wide; flowers 8-10 mm long;
leaflets about 10-20 mm long, 5-10
mm wide (Goyaz, Brazil)
7b. Ae. elegans var. robustior
Fruit with articles about 3 mm in diame-
ter; flowers 5-7 mm long; leaflets
3-10 mm long, 24 mm wide
(coastal Brazil; Puerto Rico)
8. Ae. gracilis
Leaflets elliptic or oblong-elliptic, 5-15
mm long, 3-4 mm wide; leaves 16—20-
foliolate; flowers 7-10 mm long; arti-
cles of fruit 3-4 mm long and 3 mm
wide; stipe 7-10 mm long (southeast-
ern Colombia; western Brazil)
9a. Ae. foliolosa
Flowers 10-15 mm long; fruit with articles
about 5 mm long and 4 mm wide; leaf-
lets elliptic or obovate-elliptic, 7-20 mm
long, 5-10 mm wide (Rio de Janeiro,
Brazil) 05. 22 10. Ae. bradei
Leaves 5-8-foliolate.
Leaflets obovate or obovate-elliptic, obtuse,
entire, 3-15 mm long, 2-6 mm wide.
Flowers 7-10 mm long; leaves not more
than 8-foliolate; fruit usually 6—-8-ar-
ticulate, the stipe 6-14 mm long.
Fruit with articles about 3-4 mm long,
2.5-3.5 mm wide; flowers 7-9 mm
long (widespread in tropical South
America)
lla. Ae. faleata var. faleata
Fruit with articles 4-5 mm long and
3-4 mm wide; flowers 8-10 mm long
(Paraguay)
llb. Ae. faleata var. hassleri
Flowers 5-7 mm long; leaves 5-12-folio-
late; fruit (3-) 4-7-articulate, the
stipe (4-) 5-8 mm long (costal Bra-
zil; Puerto Rico)... ... 8. Ae. gracilis
Leaflets elliptic-oblong, acute, 12-30 mm
long, 5-10 mm wide, the margins closely
ciliate; fruit 3- or 4-articulate, the stipe
about 5-7 mm long, the articles about 3
mm in diameter (Minas Gerais, Brazil)
12. Ae. warmingii
FEBRUARY 1959
1. Aeschynomene viscidula Michx. Fl. Bor. Am.
2: 74. 1803, non Roxb. ex Willd. 1809.
Aeschynomene prostrata Poir. in Lam. Encyc.
Suppl. 4: 76. 1816.
Secula viscidula (Michx.) Small, Fl. Miami 90,
200. 1913.
Aeschynomene eriocarpa Standl. & Steyerm.
Field Mus. Publ. Bot. 23: 9. 1948.
This species is easily recognized by its short-
stipitate, densely tomentulose fruits. Even
though geographically widespread, the morpho-
logical characters are generally uniform in all the
material observed. The chief instability appears
to be in the fruit indument; the glandular hairs
may fail to develop, or sometimes the terminal
one or two joints of the loments may be glabrous.
2. Aeschynomene acapulcensis Rose, Contr. US.
Nat. Herb. 5: 191. 1899.
Aeschynomene picachensis Brandeg. Univ. Cal-
ifornia Publ. Bot. 6: 181. 1915.
On the basis of the fruit characters indicated
in the key, this glabrous-fruited Mexican species
has been retained as separate from the pube-
scent-fruited Ae. brevifolia which occurs in the
Old World. It is my strong feeling, however, that
the two taxa might ultimately be proved conspe-
cific. The geographic separation could be explain-
able in terms of early sailing routes and the prac-
tice of transporting animals and fodder, but the
evidence is scanty. Thus far I have seen only
three collections from Mexico and but shghtly
more material from Africa, Madagascar, and the
other known localities for Ae. brevifolia.
Vegetatively, the plants of Ae. acapulcensis
and Ae. brevifolia are virtually indistinguishable.
They may range from glabrous to pubescent,
and there is considerable variation in stipe length
of the fruit, even on individual specimens.
3. Aeschynomene brevifolia L. ex Poir. in Lam.
Encye. 4: 451. 1797.
Hedysarum micranthos Poir. in Lam. Encyc. 6:
446. 1806.
Aeschynomene micrantha (Poir.) DC. Prodr. 2:
321. 1825.
Patagonium racemosum E. Mey. Comm. PI.
Afr. Austr. 1: 123. 1835.
As already indicated in the key and in the
comments under the preceding species, Ae. brev-
ifolia, based on a collection from Madagascar, is
scarcely distinguishable from Ae. acapulcensis
from Mexico. Except for differences in fruit in-
dument, some of the specimens with glabrate
leaflets and fruits, from Madagascar and Ré-
union, for example, are quite similar to material
RUDD: STUDIES IN AEKSCHYNOMENE AT
of the type collection of Ae. acapulcensis. Other
specimens with more glandular development,
such as most from South Africa, vegetatively
resemble the type collection of Ae. picachensis,
which I consider referable to Ae. acapulcensis.
I have seen a sheet from L that I presume to
be an isotype of Patagonium racemosum E. Mey.
collected by Drege in Africa. It is essentially
identical with other collections of Ae. brevifolia
from Africa.
The collections from Australia seem to belong
to this species but approach Ae. gracilis in longer
leaf axis, and Ae. falcata in fruit characters,
having longer stipes and sometimes four or five
articles instead of the customary two or three.
The bracteoles are slightly shorter than average.
Bentham (Fl. Austral. 2: 227. 1864) considered
this material as “quite identical” with Ae. falcata
var. paucijuga from Brazil, and cited Ae. mi-
crantha as a synonym.
There has been a question as to the correct
name for this taxon. Apparently Poiret validated
the Linnaean name Ae. brevifolia, based on a
collection by Commerson in Madagascar, and
then, later, published Hedysarum micranthos
based on material of presumably the same col-
lection. I have not yet learned the circumstances
of Linnaeus’s connection with the Commerson
collection, nor has a sheet been located with
“brevifolia”’ in Poiret’s handwriting.
From P I have seen isotypes of H. micranthos
and a photographic negative of the type. One
sheet with Commerson’s handwriting attests to
the authenticity of the collector’s name and lo-
eality. The type and one of the isotypes have
been annotated by Poiret as Hedysarum mi-
cranthos. On two other sheets, including one
from Desvaux’s herbarium, are the three names,
Hedysarum micranthos, Aeschynomene micran-
tha, and Aeschynomene brevifolia. It would ap-
pear that Desvaux’s interpretation of the three
names as synonymous would be correct and that
the name Ae. brevifolia should have priority.
Unfortunately, the sheet in the Lamarck her-
barium, labeled as the type of Ae. brevifolia,
appears to be incorrect. A fragment of ample
size for determination, lent me from P, is iden-
tical with type material of Hedysarum falcatum,
based on a Commerson collection in Brazil. There
must have been an error in labeling this par-
ticular sheet.
There are additional labels on this putative,
but apparently erroneous, type sheet. Annota-
48 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
tions “du bresil,’ “de Commerson,”’ and “Aes-
chinomene brevifolia. Dict. No. 10” are in
Lamarck’s hand. Desvaux added the names
“hedysarum faleatum Poir. ene. en Desy.” That
Desvaux recognized a confused situation is in-
dicated by other labels, “hedysarum micranthos
Poir. enc. en Desv.” and “Ces deux plantes
etoient sous un seul nom dans cet herbier Aesch.
brevifolia mais j’ai la certitude que la brevifolia
est Phedys. micranthus du meme auteur et que
Vautre qui n’est pas de Madagascar mais du
brésil est ’hedys. faleatum Poiret.”
I am greatly indebted to Dr. Alicia Lourteig
for,doing considerable research for me in locating
the pertinent specimens, transcribing certain
labels, and photographing types that could not
be lent.
4a. Aeschynomene brasiliana (Poir.) DC. var.
brasiliana.
Aeschynomene brasiliana (Poir.) DC. Prodr. 2:
322. 1825.
Cassia biflora Mill. Gard. Dict. ed. 8, no. 14.
1768, non L. 1753.
Hedysarum brasilianum Poir. in Lam. Encycl.
6: 448. 1804.
Cassia houstoniana Collad. Hist. Nat. Med.
Cass. 132. 1816.
Aeschynomene paucijuga DC. Prodr. 2: 321.
1825.
Aeschynomene paucijuga var. subscabra DC.
Prodr 227321) 13825:
Hedysarum hirtum Vell. Fl. Flum. 319. 1825;
eon. 72) talos 1511835:
Aeschynomene brasiliana B Vog. Linnaea 12:
90. 1838.
Aeschynomene biflora (Mill.) Fawe. & Rendle,
Fl. Jam. 4: 27. 1920.
Aeschynomene guaricana Pittier, Bol. Teen.
Minist. Agric. & Cria, Serv. Bot. Caracas 5:
41. 1944, without Latin diagosis.
This widely distributed species is readily iden-
tifiable by the fruit, flower, and leaf characters
given in the key. The material is generally uni-
form, with minor variation in size of vegetative
parts due, probably, to habitat factors. A few
specimens show reduction in fruit indument.
What appear to be more significant variations
are indicated in the following two taxonomic
varieties.
4b. Aeschynomene brasiliana (Poir.) DC. var.
earichanica Rudd, var. noy.
A varietate typica floribus fructibusque ma-
joribus differt.
The plants are more robust and the flowers
and fruits significantly larger than those of the
typical variety, the flowers about 10 mm long,
voL. 49, NO. 2
the articles of the fruit 4-5 mm long and 3-4
mm wide.
Type in the U.S. National Herbarium, no.
2167562, collected on the north end of Cerro
Carichana (Cerro Gavilan), elevation 100-300
m, December 21, 1955, by J. J. Wurdack and
J. V. Monachino (no. 40885). Duplicates at NY
and VEN.
4c. Aeschynomene brasiliana (Poir.) DC. var.
venezolana Rudd, Contr. U.S. Nat. Herb.
32: 80. 1955.
This variety, known only from northern Ven-
ezuela, differs from the typical variety in leaf
and fruit characters, the leaves consistently nar-
rower and the fruits with longer stipes and more
numerous articles.
5. Aeschynomene vogelii Rudd, nom. et stat. noy.
Aeschynomene podocarpa var. B Vog. Linnaea
12: 89. 1838.
Aeschynomene falcata var. y multijuga Benth.
in Mart. FI. Bras. 15(1): 68. 1859.
This taxon appears to warrant specific status,
and designation of a new name is necessary. The
epithet vogeli is chosen in honor of Dr. J. R.
Theodor Vogel, the author of many of the taxa
of this series, including the variety on which this
species is based.
In my earlier paper I treated Ae. podocarpa
and its var. 8 as synonymous. Since then I have
had the privilege of examining additional speci-
mens and have concluded that the fragment at
F, labeled as Aeschynomene podocarpa, must be
a portion of the Sellow collection on which var.
8 was based, rather than typical Ae. podocarpa.
The identity of typical Ae. podocarpa is prob-
lematic, but I now believe that it is referable to
Ae. elegans.
Bentham based his Ae. falcata var.y multijuga
on Ae. podocarpa var. 8 and cited two Brazilian
collections. One, the type, is the Sellow collection
from Serra Itambé, Minas Gerais, and is the
basis of my Ae. vogelii. The other, collected by
Weddell “in arenosis maritimis Rio de Janeiro,”
is represented by a sheet at P, annotated in
what appears to be Bentham’s hand, but it
actually is Ae. elegans and is quite unlike the
Sellow collection.
There are two additional collections from
Minas Gerais that seem to belong to this taxon:
Riedel 943, from Serra de Lapa (NY), and
Markgraf, Mello Barreto, & Brade 3455, from
Serra do Grao Mogol (RB; US, fragment). The
FEBRUARY 1959
material is essentially like the specimens of the
Sellow collection except that the leaflets average
a little smaller in size and exhibit more glandular
development, with the margins mostly glandular-
denticulate.
6a. Aeschynomene histrix Poir. var. histrix.
Aeschynomene histrix Poir. in Lam. Encyc.
Suppl. 4: 77. 1816.
2? Aeschynomene cassioides Desv. in Ham.
Prod. Pl. Ind. Occ. 51. 1825.
? Aeschynomene echinus Vog. Linnaea 12: 92.
1838.
Aeschynomene conferta Benth. Ann. Nat. Hist.
3: 433. 1839.
Aeschynomene mucronulata
Journ. Bot. 2: 56. 1840.
Aeschynomene histrix var. mucronulata Benth.
in Mart. Fl. Bras. 15(1): 69. 1859.
Secula hystrix (Poir.) Small, Man. Southeast
Fl. 728. 1933.
Aeschynomene pineticola Standl.
Ceiba. 1: 79. 1950.
This species sensu latior is polymorphic and
fairly widespread in Tropical America. The
principal variations are indicated in the key.
In this paper I am following Bentham who
assigned Ae. echinus to Ae. histrix “ex descr.”
Although I am tentatively placing Ae. echinus
under the typical variety of Ae. histriz, it is
possible that it is the same as Ae. histrix var.
densiflora. The specimens that I previously de-
termined as Ae. echinus are referred in this
paper to two other varieties of Ae. histrix, var.
apana, and var. multijuga.
Presumably Vogel in his examination of the
Sellow specimens from Brazil made few com-
parisons with specimens from beyond that coun-
try’s borders. He must have disregarded Ae.
histrix from French Guiana (Ae. densiflora from
British Guiana was not yet published) and in-
itiated the new species Ae. echinus. In his de-
scription of Ae. echinus he states that the
stipules, racemes, and flowers are as in the pre-
ceding species, which is his Ae. incana, another
variety of Ae. histrix, according to the present
treatment.
Benth. Hook.
& . Wms.
6b. Aeschynomene histrix Poir. var. incana
(Vog.) Benth. in Mart. Fl. Bras. 15(1): 69.
1859 (As Ae. hystrix var. incana).
Aeschynomene puberula DC. Prodr. 2: 321.
1825.
Aeschynomene incana Vog. Linnaea 12: 90.
1838, non G. F. W. Mey. ex DC. 1825, as
synonym.
As indicated in the key, var. incana is very
RUDD: STUDIES IN AESCHYNOMENE 49
similar to the typical variety, differing chiefly
in indument.
6c. Aeschynomene histrix Poir. var. densiflora
(Benth.) Rudd, Contr. U.S. Nat. Herb. 32:
84. 1955.
Aeschynomene densiflora Benth.
Journ. Bot. 2: 56. 1840.
in Hook.
Although there is intergradation between viri-
eties of Ae. histriz, the specimens of var. densi-
flora usually are readily distinguished, especially
from those of the typical variety, by their robust
habit, and larger leaflets and stipules.
6d. Aeschynomene histrix Poir. var. multijuga
(Chod. & Hass.) Rudd, comb. et stat. nov.
Aeschynomene brasiliana (Poir.) DC. forma
multyjuga Chod. & Hass. Bull. Herb. Boiss.
II. 4: 882. 1904.
This taxon, originally published as a form of
Ae. brasiliana, has the principal characteristics,
especially the dolabriform fruit structure, of
Ae. histrix. It differs from typical Ae. histrix in
having slightly larger flowers and fruits, and
leaflets that are mostly denticulate with bulbous-
based glandular setae.
Specimens of the type collection of this vari-
ety indicate a rather luxuriant, suffrutescent
herb, 0.5-1.5 m tall. It was collected by Hassler
(No. 5814) “in campo pr. flumen Carimbatay,”
Paraguay. I have seen isotypes from GH, MO,
and NY.
The three other collections that I am assigning
to this variety are from Missiones, Argentina, as
follows: “On the Parana 26°—27° S. Lat.,” Parodi
100 (K); Loreto, Ekman 1720 (NY); San Ig-
nacio, Burkart 15344 (US). They apparently
are from lower, more compact plants, with
shorter internodes and slightly smaller leaflets.
In the character of the fruits, flowers, and glan-
dular setae, however, they appear to be essen-
tially the same as specimens of the type collec-
tion.
In my earlier paper I interpreted this material
as representing Ae. echinus. While the exact
identity of Ae. echinus is still in doubt, I now
think that it is more likely to be the same as
typical Ae. histrix, or possibly Ae. histriz var.
densiflora. The type locality of Ae. echinus also
is not exactly known but on the basis of what is
known of Sellow’s itinerary, presumably it is
from farther south or east than the above cited
specimens. So far I have seen nothing like var.
multijuga from the range of Sellow’s travels.
5O JOURNAL OF THE
6e. Aeschynomene histrix Poir. var. apana Rudd,
var. NOV.
A varietate typica foliolis elongatis, floribus
fructibusque majoribus differt.
The specimens of this variety, because of the
linear-oblong leaflets, 5-10 mm 1.5-2 mm wide,
have an aspect quite different from others of Ae.
histrix, yet the flowers and fruits are all essen-
tially the same. Occasional leaflets of var. apana
have a few marginal glandular setae such as are
found in var. multijuga.
Type in the U. 8. National Herbarium, no.
1177243, collected near the Rio Apa, at Cen-
turion, Paraguay, December 9, 1908, by K.
Fiebrig (no. 4387). Duplicate at GH. Additional
material is the Hassler collection no. 11021 (F,
GH,NY,US), also from near the Rio Apa, Para-
guay.
7a. Aeschynomene elegans Schl. & Cham. var.
elegans.
Aeschynomene elegans Schl. & Cham. Linnaea
5: 583. 1830.
Aeschynomene tecta Vog. Linnaea 12: 87. 1838.
Aeschynomene falcata Vog. var. plurijuga
Benth. in Mart. Fl. Bras. 15(1): 68. 1859.
Aeschynomene falcata Vog. var. elegans (Schl.
& Cham.) O. Ktze. Rev. Gen. 1: 158. 1891.
Aeschynomene falcata Vog. var. elegans (Schl.
& Cham.) O. Ktze. forma glabrior O. Ktze.
Rey. Gen. 1: 158. 1891.
Aeschynomene arenicola Brandeg. Univ. Cali-
fornia Publ. Bot. 10: 408. 1924.
This species is easily recognized by its slender,
long-stipitate, small-jointed, moniliform fruits.
It is one of the most widespread of the series,
ranging from Mexico to southern Brazil.
Many of the collections annotated and cited
by Bentham as Ae. falcata actually are speci-
mens of Ae. elegans. His Ae. falcata var. plu-
rijuga, based on Ae. tecta and Ae. podocarpa,
certainly must be the same as Ae. elegans. Sellow
specimens from Brazil annotated as Ae. tecta,
presumably isotypes, are Ae. elegans.
The identity of typical Ae. podocarpa still is
in question. I have seen no Sellow specimens
annotated as such or any that I can relate to the
original description.
Previously, on the basis of characters in the
original description and examination of a small
photographic negative of type material, I de-
cided that Ae. gracilis should be placed in syn-
onymy under Ae. elegans. I have now seen iso-
types of Ae. gracilis and conclude that it should
be reinstated as a distinct species.
WASHINGTON ACADEMY OF SCIENCES
vou. 49, NO. 2
7b. Aeschynomene elegans Schl. & Cham. var.
robustior Rudd, var. nov.
A varietate typica foliolis fructibusque ma-
joribus differt.
As characterized in the key, this more robust
variety of Ae. elegans is recognized by its rela-
tively larger leaves with 10-14 leaflets, 10-20
mm long and 5-10 mm wide, and fruit with
larger articles, 3-4 mm long and 3 mm wide. The
fruit stipe is about 5-8 mm long, in contrast to
the 10-15 mm long stipe that is customary in
typical Ae. elegans.
Type in the Herbarium of the Royal Botanic
Gardens, Kew, collected at Brejon, near Santa
Cruz, Goyaz, Brazil, by J. E. Pohl, in 1820.
There are two other sheets at K that appear
to belong to the same collection, labeled no. 1101,
but without collector’s name.
8. Aeschynomene gracilis Vog. Linnaea 12: 89.
1838, non Miq. 1844.
Aeschynomene portoricensis Urb. Symb. Antill.
1: 325. 1899.
After examining isotypes of Ae. gracilis from
Brazil and Ae. portoricensis from Puerto Rico,
it seems appropriate to combine the two species.
Their close similarity was mentioned by Urban
in connection with his publication of Ae. porto-
ricensis. The former species is known only from
the type collection by Sellow in Brazil between
Campos, Rio de Janeiro, and Victoria, in Es-
pirito Santo. The latter species, which has been
frequently collected in Puerto Rico, is somewhat
variable as to leaf size, number of articles per
fruit, and stipe length, but several specimens
are essentially identical with the Sellow collec-
tion from Brazil.
There is some similarity to Ae. falcata in fruit
characters but the stipe of Ae. gracilis is usually
shorter and the loments have fewer, obliquely
semioval joints. The flowers are smaller. The
leaves seem to be intermediate between Ae. ele-
gans and Ae. micrantha.
9. Aeschynomene foliolosa Rudd, Contr. US.
Nat. Herb. 32: 91. 1955.
This is a distinctive species with panicles of
small flowers and slender long-stipitate fruits.
The leaves are relatively long with 16-20 oblong-.
elliptic leaflets.
In the original description only two localities
are cited, both from the outer periphery of the
Amazon Basin. Recently another collection from
a somewhat intermediate area has been recog-
FEBRUARY 1959
nized, Ducke [Herb. No.] 12382 (MG), collected
December 14, 1912, at Campo da Frequezia
Velha, Coary, Brazil.
10. Aeschynomene bradei Rudd, sp. nov. Fig. 1
Suffrutex diffusus, ad sectionem Ochopodium
pertinet, foliis 3-5 em longis, 9-16-foliolatis, fo-
liolis ellipticis, adpresse pubescentibus; Ae. ele-
gans var. robustior affinis sed imprimis floribus
fructibusque majoribus differt.
Stems suffrutescent, rusty-tomentose when
young, somewhat glandular-hispidulous, glabres-
cent; stipules lanceolate or lanceolate-ovate,
about 5-8 mm long, attenuate, 1-2 mm broad
at the base, pubescent like the stem; leaves
about 3-5 em long, 9-16-foliolate; leaflets el-
liptic or obovate-elliptic, 7-20 mm long, 5-10
mm broad, obtuse, mucronulate, entire, moder-
ately appressed-pubscent on both surfaces, the
hairs colorless or sometimes rusty; inflorescences
axillary, racemose, slightly longer than the sub-
tending leaves; bracts deltoid-ovate, about 1
mm in diameter, pubescent, the bracteoles ovate,
about 2 mm long and 1 mm wide; flowers
yellow, 10-15 mm long; calyx 3-5 mm long
campanulate with 5 subequal lobes about 2 mm
long, ciliate, subglabrous to glandular-hispidu-
lous; standard 10-15 mm long, the claw 2-5 mm
long, the blade suborbicular, 8-10 mm in di-
ameter, pubescent on the outer face; wings and
keel slightly shorter than the standard, the wing
blades oblique, 4-5 mm broad, the keel blades
about 2 mm broad, bent at about a 90° angle;
stamens 8-12 mm long, monadelphous, the fila-
ments united from base to midlength, the sheath
open on the carinal side; ovary 5-ovulate, pu-
bescent; fruit 2—-5-articulate, the stipe subgla-
brous, 7-10 mm long, the articles crisp-pubes-
cent, about 5 mm long and 4 mm wide; seed
brownish black, sublustrous, 3 mm long, 2 mm
broad, and compressed to 1 mm or less in thick-
ness.
Type in the herbarium of the Jardim Botanico
do Rio de Janeiro, no. 28707, collected at Pedra
Dubois, Santa Maria Madalena, Rio de Janeiro,
Brazil, altitude 1,100 m. February 27, 1935, by
Santos Lima and A. C. Brade (no. 14220). Frag-
ment and photograph at US.
Only one other specimen is known, a unicate
at RB, collected at Pedra das Flores, Santa
Maria Madalena, Rio de Janeiro, Brazil, altitude
1,200 m, March 4, 1934, by Santos Lima and A.
C. Brade (no. 13273). Fragment at US
RUDD: STUDIES IN AESCHYNOMENE Syl
Fic. 1—Aeschynomene bradei: a, Portion of
stem with leaf, immature flower, and fruit (nat.
size); b, standard; c, wing; d, keel; e, calyx and
stamen filaments; f, one article of fruit, open,
showing seed. (b-f, <2.)
This species, represented by the two collec-
tions cited above, is readily referable to series
Viscidulae of section Ochopodium. In general
structure it resembles such related species as
Aeschynomene falcata, Ae. elegans, Ae. vogelii,
and Ae. foliolosa. In aspect it is rather distinc-
tive due to more robust, woody growth, larger
flowers and fruits. The critical characters are in-
dicated in the key.
lla. Aeschynomene falcata (Poir.) DC. var. fal-
cata.
Aeschynomene falcata (Poir.) DC. Prodr. 2:
322. 1825.
Hedysarum falcatum Poir. in Lam. Encye.
Meth. Bot. 6: 448. 1804.
Hedysarum diffusum Vell. Fl. Flum. Text 320.
S25 eltconbie plese sao:
Aeschynomene falcata (Poir.) DC. var. pauci-
juga Benth. in Mart. Fl. Bras. 15(1): 67.
1859.
Aeschynomene apoloana Rusby, Bull. New
York Bot. Gard. 6: 511. 1910.
An isotype and a photographic negative of
the type of Hedysarum falcatum Poir., on which
Ae. falcata is based, have recently been sent to
me from Paris. This authentic material, in the
Jussieu Herbarium, was collected by Commerson
in Brazil. It has characteristic faleate fruit and
5-8-foliolate leaves, and confirms our concept of
the species.
As explained under Ae. brevifolia, material
from a sheet in the Lamarck Herbarium and
labeled as the type of Aeschynomene brevifolia
L. ex Poiret, appears to be identical with the
type material of H. falcatwm. According to the
description, Ae. brevifolia was collected by Com-
merson in Madagascar. There must have been
52 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
an error in labeling the collection, however, as
this specimen does not fit the description of
Ae. brevifolia, and must really be a duplicate of
Commerson’s Brazilian collection of Hedysarum
falcatum.
1lb. Aeschynomene falcata (Poir.) DC. var. hass-
leri Rudd, var. noy.
A varietate typica foliolis fructibus floribusque
majoribus differt.
In comparison with material of typical Ae.
falcata, the specimens of this variety are out-
standing in appearance due to more vigorous
growth, especially their larger flowers, fruits,
and leaves. The differences apparently are in
degree rather than structural pattern.
This is another example of specimens from
VoL. 49, No. 2
Paraguay being significantly more robust and
with larger organs than their closest relatives.
Type in the Herbarium of the Royal Botanic
Gardens, Kew, collected in a thicket near Con-
cepcion, Paraguay, September 1901, by E. Hass-
ler (no. 7461). Isotype at NY.
There is an additional sheet at K, also col-
lected by Hassler (no. 10977), “In altaplanitie,
Sierra de Amambay,” Paraguay, 1913.
12. Aeschynomene warmingii Micheli, Vid. Medd.
Nat. Foren. Kj¢gbenhayn 68. 1875.
As indicated in the key, this species from
Lagoa Santa, Minas Gerais, Brazil, is distinctive
with its fairly large, 5-7-foliolate leaves. Un-
fortunately, it is known only from the type
collection.
INSECTS AS FLYERS
Insects are the most efficient flying animals.
They surpass both birds and bats. They are
superior in some ways to any “flying machine”
yet invented by man. The air was their exclusive
domain for at least 100 million years before any
rival winged creatures appeared. During this
time they developed two flight systems, direct
and indirect, which are in use today, although
the former is confined to a few groups such as
the dragonflies.
This is the claim of Dr. R. E. Snodgrass, re-
search associate of the Smithsonian Institution,
in a report on arthropod evolution recently pub-
lished by the Institution. The earliest known in-
sects, with highly developed jumping mecha-
nisms, were wingless. There are some wingless
forms today. But, Dr. Snodgrass points out, the
earliest known winged insects in the fossil record
had the flying mechanism fully developed so that
its evolutionary development largely is a matter
of conjecture.
The first step, as deduced by Dr. Snodgrass,
was the emergence from the sea of some long
extinct many-footed wormlike creature. The feet
were fleshy lobes by means of which it had
moved clumsily along the sea bottom. A first
evolutionary step was the elimination of these
lobes on all but the first three segments of the
body behind the head. These gradually evolved
into legs.
The earliest insects, Dr. Snodgrass says, to
come on land presumably were provided with
so-called “paranotal lobes,’ small appendages
attached to the back in the region of the thorax.
These are not hypothetical structures which
since have disappeared, he says, since there are
traces of them in various modern insects and in
others; during the nymph stage, wings first ap-
pear as lobelike extensions from the back.
“Presumably,’ says Dr. Snodgrass, “when
these paranotal lobes became sufficiently large
in the primitive insects they first served as
gliders. If the at first rigid lobes became flexible
at their bases they could then, by action of the
thoracic muscles, be flapped up and down, thus
enabling the gliding insect to sustain itself longer
in the air. Even this simple wing movement,
however, involved modifications of the thoracic
skeleton and some degree of adaptation in the
musculature.”
Eventually, he points out, the back muscles
became differentiated to the poimt where they
could move the wings without the help of any
wing muscles per se. This is the “indirect” sys-
tem of most insects.
Development of wings was evidently a re-
sponse to demand. The first winged insects ap-
pear very shortly after the appearance of the
first tall plants in the primeval swamps.
FEBRUARY 1959
The direct up-and-down movement, with vari-
ous modifications, continues in the “direct flight”’
system, best exemplified by the dragonflies.
During the long period of their undisputed
domain of the air both systems developed. Then
came the birds and bats to dispute their aerial
INSECTS AS
FLYERS 5S
supremacy. They fed chiefly on insects whose
only defense was the development of greater
speed and flying accuracy.
As a result the less efficient systems tended to
become eliminated and the present methods of
insect flight better developed.
NEWS OF MEMBERS
Dr. Bernard Frank is the new forestry officer, Forest Research Institute, Dehra Dun,
Uttar Pradesh, India.
Mr. Thomas G. Digges has been honored with the first annual George Kimball Burgess
Memorial Award of the Washington Chapter of the American Society for Metals.
Mr. Conrad V. Morton, curator of the division of ferns, U. S. National Museum, Smith-
sonian Institution, is one of two American botanists who have been awarded honorary life
memberships in the American Gesneria Society for their important contributions to the
world’s knowledge of the plant family Gesneriaceae, which includes the African violet and
gloxinia.
To understand Nature we must first study man thoroughly, because there 1s nothing
in the universe which is not to some degree hidden in man’s nature. Man is verily a
universe in miniature —PLINY THE ELDER.
D4 JOURNAL OF THE
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 2
ZOOLOGY .— A review of the gorgonacean genus Placogorgia Studer, with a descrip-
tion of Placogorgia tribuloides, a@ new species from the Straits of Florida.
FREDERICK M. Baysr, U.S. National Museum.
(Received December 5, 1958)
The extensive dredging operations of the
U.S. Fish Commission steamer Albatross
brought to hght a great many zoological
novelties, not a few of which are still await-
ing description. Among these is a new gor-
gonian coral of the genus Placogorgia, which
is now described and figured.
The genus Placogorgia as presently con-
stituted contains four species in the At-
lantic Ocean. All are characterized by calic-
ular thorn-scales with a rather broad,
branched, basal root and a stout, more or
less laciniated but usually blunt spine, which
projects above the surface of the calicles,
giving them a thorny appearance. Although
the thorn-scales of the four species are
not identical, they are so similar that only
exhaustive descriptions could point out the
differences between them, and the species
are distinguished mainly upon differences in
the size and ornamentation of the cortical
spindles.
The new species of Placogorgia that is the
subject of this paper differs rather strikingly
from the four previously known Atlantic
species in the huge size of its calicular
thorn-seales, which, moreover, have a quite
acute spine and therefore bear a strong re-
semblance to the thorn-seales of Para-
muricea. In this study, it has been necessary
to reexamine all the Atlantic species of
Placogorgia and to reappraise their position
in respect to Paramuricea and related
genera with calicular thorn-scales.
Genus Placogorgia Studer
Placogorgia Studer, 1887, Arch. Naturg. 53(1): 56.
[No species described.]
Placogorgia Wright and Studer, 1889, Challenger
Zool. 31 (part 64): 113. (Type species, Placo-
gorgia atlantica Wright and Studer, fixed by
subsequent monotypy.)
Placogorgia Nutting 1910, Siboga Exped.
Monogr. 13b: 76. [= Discogorgia Kikenthal.]
Placogorgia Nutting, 1912, Proc. U.S. Nat. Mus.
43: 83.
Pseudothesea Kiikenthal, 1919, Ergebn. deutschen
not
Tiefsee-Exped. 13(2): 843. (Type species,
Thesea placoderma Nutting, by original desig-
nation.)
As described, Placogorgia is difficult to sepa-
rate from Paramuricea and Echinomuricea. Most
of the species of Placogorgia, including some
from the Indo-Pacific assigned to Thesea by
Nutting (= Pseudothesea Kikenthal), have
large, rude spindles that often become platelike,
with strong external spines, and small, rather
blunt calicular thorn-scales. Paramuricea has
large, sharp thorn-scales (sometimes with the
basal part much reduced), and small spindles
usually without external spines—rarely flat
scales with a central projecting process or boss.
Unfortunately, the type species of Placogorgia
has small cortical spindles with little or no indi-
cation of external spines, and rather sharp, but
small, calicular thorn-scales (both characters like
Paramuricea); and Paracuricea multispina
Deichmann has cortical plates with a projecting
process, and blunt calicular thorn-seales (char-
acters approaching Placogorgia). Except for E.
atlantica, Echinomuricea has stellate thorn-
scales with a smooth or nearly smooth spine; its
distribution is primarily Indo-Pacific. I] am in-
clined to think that the Echinomuricea atlantica
described and figured by Thomson (1927, p. 40,
pl. 4, fig. 3) is actually Johnson’s Acanthogorgia
grayt (Johnson 1862, p. 195) rather than at-
lantica—compare the spicules!—and that it be-
longs to Placogorgia and not to Echinomuricea
or Paramuricea. Its calicular thorn-scales and
cortical plates are similar to those of the new
Placogorgia described herein, but Thomson gives
no measurements and the magnification of his
figures is not indicated, so its identity remains
uncertain. Ktikenthal (1924, pp. 225-226) sug-
gested that both atlantica and grayi are refer-
able to Paramuricea. This disposition is contra-
indicated in the case of gray: (Thomson’s
atlantica) by the large plates with several pro-
jecting spines, but could be valid for the true
atlantica. There seem to be no species in the
Atlantic Ocean that can be assigned to the genus
FEBRUARY 1959
Echinomuricea as defined by most authors, which
is characterized by calicular thorn-scales of a
particularly distinct type.
Nutting (1910) described a number of East
Indian species under the generic name Placo-
gorgia, but most of them have been referred to
other genera, notably Discogorgia (Kiukenthal
1924, p. 212). He also described some muriceids
with calicular thorn-scales and large, spinose
cortical spindles and plates, which he placed in
Thesea. Since they had nothing to do with the
original Thesea of Duchassaing and Michelotti,
Kiikenthal in 1919 established for them the genus
Pseudothesea, with Thesea placoderma Nutting
as its type species. The character of its calicular
thorn-scales leaves no doubt that T. placoderma
is congeneric with Placogorgia atlantica Wright
and Studer, and its cortical plates are not unlike
those of Placogorgia rudis Deichmann. Most,
perhaps all, of the other species described by
Nutting in his monograph of the S:boga Muri-
ceidae belong to other genera. Thesea sanguinea
and T. simplex, of which I have seen type mate-
rial, are referable because of their thorn-scales
(which are of the “leaf-club” type) to Echino-
gorgia, a genus which perhaps should be ranked
among the Plexauridae (Bayer, 1958, pp. 43, 48).
The paramuriceid species characterized by
thorn-seales in the calicle are a closely inter-
related complex, within which the generic dis-
tinctions—if such exist—must be drawn upon
highly arbitrary grounds, at least until detailed
studies can be made upon all pertinent type
specimens. Until adequate studies can be under-
taken there is no alternative but to recognize at
least the most distinct of the genera that have
been established. These genera are based mostly
upon the form of the calicular thorn-scales. The
thorn-seales of some genera, such as Villogorgia,
Trachymuricea, and Echinogorgia (which pos-
sibly belongs in quite another family), are very
distinctive, whereas those of other genera are
only modifications of a simple, basic type, be-
tween which it is almost impossible to draw hard
and fast boundaries.
The accompanying chart (Fig. 1) shows the
major types and varieties of calicular thorn-
scales (A-G) and cortical sclerites (H-N) found
in the genera of Paramuriceidae sensu lato. (Ex-
cluded are Bebryce and Acanthacis, which are so
distinctive that they need not enter into the
present discussion.) The combinations of these
BAYER: REVIEW OF PLACOGORGIA STUDER 979)
types that occur in the various genera are indi-
cated by the numbered connecting lines.
CALICULAR THORN-SCALES
A. The Menella-type (genus Menella Gray:
Kukenthal, 1924, p. 184)—A single smooth,
tapered spine rises from a root-part consisting
of irregularly diverging branches. So far as I
can tell from the literature, this type is always
associated with cortical spindles that may pro-
duce strong external spines (J). I have seen only
Menella rubescens Nutting, whose thorn-scales
are illustrated (A); final definition of the genus
will depend upon a reexamination of the type
species, MW. indica Gray, the holotype of which
must be in the British Museum of Natural
History.
B. The Echinomuricea-type (genus Echino-
muricea Verrill: Kukenthal, 1924, p. 185) —A
single smooth, tapered spine originates abruptly
from a root-part consisting of four or five widely
diverging branches, the whole producing a stel-
late body. These are usually, if not always, com-
bined with simple, symmetrically sculptured
spindles in the cortex (K). Similar thorn-scales,
but with shorter projecting spine, are found in
the genus Hubrandella, established by Deich-
mann (1936, p. 128) to replace Verrill’s Lisso-
gorgia, which was based on a single specimen
said to have come from Florida; nothing like it
has ever again been found in Florida, suggesting
that it may have originated elsewhere—most
likely in the Indo-Pacific. It resembles some of
the species of Echinomuricea from that region.
C. The Paramuricea-type (genera Paramuri-
cea Kolliker and Placogorgia Studer: Deich-
mann, 1936, pp. 134, 141) —Large thornscales
with a stout, acute, more or less aculeate spike
arising from a complicated, branched or lobed
basal root. In combination with very large spin-
dles and plates with (1) or without (H) spines,
it is found in Placogorgia japonica (6) and P.
tribuloides (3) ; with smaller spindles, sometimes
knee-bent, it occurs in Paramuricea placomus
(aN
D. The Villogorgia-type (genus Villogorgia
Duchassaing and Michelotti, including Acampto-
gorgia Wright and Studer, Brandella Gray, Para-
camptogorgia Kiukenthal, and Perisceles Studer,
all synonyms: Aurivillius, 1931, p. 204) —A
projecting part that consists of a cluster of
fingerlike processes, or thin radiating folia, arises
vou. 49, No. 2
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
Fic. 1.—(See opposite page for legend).
FEBRUARY 1959 BAYER: REVIEW
from a widely diverging pair of flattened roots
curved to fit the calicular walls. The various
modifications that prompted the establishment
of several genera were shown by Aurivillus
(1931) to represent but a single type of spicule.
Always associated with small 4-armed bodies
having a pyramidal or winged central process
(M, middle figure), sometimes with two arms
suppressed to form a spindle with a median pro-
jection (M, top and bottom figures).
E. The Placogorgia-type (genera Placogorgia
Studer and Paramuricea Kolliker: Deichmann,
1936, pp. 134, 141) —Similar to the Paramuri-
cea-type but usually the root is more strongly
developed laterally and somewhat curved to fit
the calicular wall, and the spine is thick, com-
paratively blunt, and conspicuously serrated or
laciniated. Usually smaller than the typical
thorn-scales of Paramuricea (C, upper figure)
but occasionally surpass them in size, in which
cases the root is more complicated and its
branches coalesce more or less completely. In
Placogorgia they are found in combination with
simple spindles both small (K) and excessively
large (H), large and small unilaterally spinose
spindles (1, J, and L, lower figure), and margin-
ally lobate scales (N, lower figure). Some spe-
cies of Paramuricea have Placogorgia-type thorn-
scales combined with lobated scales (N, the two
npper figures), indicating that some generic
allocation may be necessary.
F. The Trachymuricea-type (genus Trachy-
muricea Deichmann, 1936, p. 182) —The lacini-
ated spine projects obliquely from a root that
is only a simple spindle. Always in combination
with small spindles having a conical external
process (L, upper two figures) much like some of
the cortical sclerites of Villogorgia. Only two
species known at present, both of them further
dis‘inguished from species of Paramuricea and
Villogorgia by a very high collaret.
G. The Echinogorgia-type (genera Hchino-
OF PLACOGORGIA STUDER 7
gorgia Kolhiker, Plexauroides Wright and Studer,
and Paraplexaura Kikenthal: Ktkenthal, 1924,
pp. 124, 130, 198) —A simple, stellate type of
thorn-scale in which the projecting spine is
greatly expanded into a thin leaf as in Hchino-
gorgia and Plexauroides (three stages of modifi-
cation are shown in G, bottom to top) and some-
times much thickened as in Paraplexaura. Since
it is possible to trace the development of the
folate thorn-scales found in Plexauroides and
some species of Hchinogorgia, and the massive
thorn-scales of Paraplexaura from the simple,
stellate type of some Echinogorgias, it seems ob-
vious that these genera are inseparable. The
thorn-scales may be the predominant type of
sclerite, or they may be combined with simple
or unilaterally developed spindles (I and K).
The generic distinctions are somewhat vague
and dependent largely upon the development of
the anthocodial armature, which is said to rele-
gate Hchinogorgia to the Paramuriceidae, and
Plexauroides and Paraplexaura to the Plexauri-
dae. Inasmuch as the anthocodial spiculation
may be reduced in those species of Hchinogorgia
that have a thick rind into which the polyps
retract fully, just as it is in the species of
Plexauroides and other plexaurids that have
thick rinds, it is a character of no value at the
generic and familial levels. At this time it re-
mains a moot point whether all of these species
should be transferred to one family or the other;
it is certainly improbable that they will continue
to span two families.
CORTICAL SCLERITES
The basic type of cortical spicule is the simple
spindle (K), which may grow excessively large
(H), and by flattening and expansion of the
margins develop into thick plates or thin scales
(N). Simple spindles usually occur even in those
species that have characteristically modified
cortical sclerites, although in certain species they
Fic. 1.—Types of calicular thornscales (A-G) and cortical sclerites (H-N), and their various com-
binations (1-14): A, Calicular thorn-seales of Menella rubescens; B, of Echinomuricea indomalaccensis;
C, of Placogorgia tribuloides (left) and Paramuricea placomus (right); D, of Villogorgia zimmermani
(above) and V. nigrescens (below); E, of Placogorgia tenuis (above) and P. atlantica (below); F, of
Trachymuricea hirta; G, of Echinogorgia flerilis (top and middle) and E. pseudosassapo (bottom); H,
cortical sclerite of Placogorgia mirabilis; I, of Placogorgia tribuloides; J, of Placogorgia rudis (above)
and Thesea flezilis (below); K, of Paramuricea placomus (above) and Placogorgia atlantica (below); L,
of Trachymuricea kiikenthali (top and middle) and Placogorgia tenuis (bottom); M, of Villogorgia zim-
mermani (top and middle) and V. nigrescens (bottom); N, of Paramuricea grandis (top), P. echinata
(middle), and Placogorgia dendritica (bottom). 1, spicular combination found in the genus Menella; 2,
in Echinomuricea; 3, in Placogorgia (some species); 4, in Placogorgia (some species); 5, in Placogorgia
(some species); 6, in T’rachymuricea; 7,in Placogorgia (some species); 8, in Placogorgia and Paramuricea
(some species); 9, in Placogorgia (some species); 10, in Placogorgia (some species); 11, in Echinogorgia;
12, in Echinogorgia; 13, in Villogorgia; 14, in Paramuricea and some species of Placogorgia.
58 JOURNAL OF THE
may be largely suppressed by the thorn-scales
of the ealicular region, which then dominate
throughout the rind (Lchinomuricea and Echino-
gorgia). A common sculptural modification found
in several genera and species is the unilaterally
spinose spindle (J, L) which may become very
large (1).
It may be useful to summarize the types of
thorn-seales in the form of a dichotomous key
to serve as a guide to the holaxonian genera
having these peculiarly modified sclerites. As
in the discussion above, Bebryce is not included
because its superficial layer of rosettes and deeper
layer of stellate plates render it absolutely un-
mistakable.
1. Cortex consisting of a single layer of spicules in
the form of large, flattened spindles or plates.
Thorn-seales around calicular aperture with
a stout, rough, sometimes branched spine -
arising from a rather small, tuberculate base
Genus AcanTHacis Deichmann
Cortex consisting of an outer layer of spicules,
large or small, and a more or less complete
mner layer of smaller spicules surrounding
GIVE RATS Fei RS ee ee re eh Ure SR ee 2
2. Calicular thorn-scales noticeably broader than
high, the root-part developed mostly at right
angles to axis of calicle, with two main, spread-
ing branches curved to fit the calicular wall;
projecting portion consisting of several radi-
ating folia or a laciniated, digitate process
(Fig. 1, D). Cortex containing 4-armed bodies
with a pyramidal, sometimes foliate central
process; sometimes modified into simple spin-
dles with median process (Fig. 1, M)
Genus ViLtLocorciA Duchassaing and Michelotti
Calicular thorn-scales typically higher than
wide, not with two main diverging roots
curved! tomit- the calicular walls! a. s2-—9" 3
3. Calicular thorn-scales are spindles with an ob-
liquely set, more or less laciniated, pyramidal
process near the distal end (Fig. 1, F)
Genus TracHyMurRIceEA Deichmann
Calicular thorn-scales with a flattened, branched,
lobed tor Ssplatelike. basess- "2 =. ee: 4
4. Projecting portion of the calicular thorn-scales
Isausually, aasIMeleySpINere 246 a4 ee eee 5
Projecting portion of the thorn-scales is a folate
expansion sometimes lobed or cleft into broad
fingers (Fig. 1, G), sometimes thickened into
a massive head..Genus Ecurnocorota Kolliker
5. Projecting spine of the calicular thorn-scales is
a smooth or nearly smooth, tapered spike. ..6
Projecting spine of the thorn-scales is an echinu-
=
late or laciniate digitate process........... 7
WASHINGTON ACADEMY OF
SCIENCES VOL. 49, NO. 2
6. Projecting spike of calicular thorn-scales gradu-
ally merging into root portion, which consists
of several irregularly divided branches (Fig. 1,
AO eee ee eae er Genus MENELLA Gray
Projecting spike of thorn-scales abruptly set off
from the root portion, which consists of four
or five widely diverging, slender branches
Chige lB) e. Genus Ecurnomuricea Verrill
7. Root portion of the calicular thorn-scales con-
sists of several tuberculate lobes more or less
completely fused together; projecting spine
echinulate or strongly laciniate (Fig. 1, E).
Cortical plates and spindles often with one or
more strong spines. .Genus PLAcocorciA Studer
Root portion of the thorn-scales consists of sev-
eral diverging branches not extensively fused
together; projecting spine echinulate (Fig. 1,
C, right hand figure). Cortical spindles usually
without spinous projections
Genus ParaMurRIceA Kolliker
PLACOGORGIA TRIBULOIDES, n. sp.
Figs. 2-9; 15
Diagnosis —Calicular thorn-scales nearly 2
mm in length, projecting spine about 1 mm. Cor-
tical spindles large (1.5 mm-+), flattened, espe-
cially near branch tips, with several stout pro-
jecting spines. A single pair of large bent spindles
and some small accessory rods in each opercular
sector; collaret with 3-6 rows of transverse
spindles. Branching dichotomous.
Description —The type is a small, nearly com-
plete colony measuring 5 cm from base to tip of
the tallest branch. Ramification is in one plane
and dichotomous; the main stem _ bifurcates
within 5 mm of the base and both branches
again bifureate at about 10 mm from the first
division. Further dichotomies are asymmetrical,
since not all the branches subdivide. The trunk
has a diameter of 2.6 mm, the major branches
1.5 mm (exclusive of calicles), and the terminal
twigs about 1.0 mm (excluding calicles). Most of
the calicles are inclined toward one face of the
colony (the “front’’), and are closely set, their
bases almost touching one another. The calicles
are low cylinders filled with very stout, acute,
imbricating thorn-scales (Fig. 2). The antho-
codiae are armed with a prominent, conical oper-
culum consisting of a ringlike collaret usually
3-5 spicules in height, surmounted by eight
points each made up of one pair of large, bent
spindles of subequal size, and some small ac-
cessory rods.
The coenenchyme has a dense outer layer of
glassy, irregularly tuberculate spindles, the larg-
Frpruary 1959 BAYER: REVIEW
est of which bear one to several strong, sharp,
projecting spikes. Toward the branch tips some
of these become broad and platelike, with sev-
eral spines, closely resembling the sclerites of
certain species of Paracis. Between and beneath
the large outer sclerites there are small, irregu-
lar spindles that form a discontinuous inner
layer.
Spicules—(a) Cortex: roughly tuberculate,
coarse spindles with one or several outward pro-
jecting, finely echinate processes (Fig. 3). Near
the calicles these sclerites increase in size, reach-
ing a length of 1.5 mm or longer, and bearing
OF PLACOGORGIA STUDER 59
several stout processes some of which may be
marginal (Fig. 4). Toward the branch tips, the
large deposits may become quite broad and
platelike, after the manner of Paracis. Lying be-
tween and beneath the large deposits are numer-
ous smaller spindles, more or less flattened and
with irregular edges (Fig. 5), forming a discon-
tinuous axial sheath.
(b) Calicles: large thorn-seales with a stout,
sharp, echinulate spine arising from the distal
margin (Fig. 6). The broad, tuberculate basal
part of the scale may have a width of 0.8 mm,
and the spine may exceed a length of 1 mm.
Figs. 2-9.—Placogorgia tribuloides, n. sp.: 2, Side view of calicle with operculum; 3-4, cortical
sclerites; 5, spindles of axial sheath; 6, calicular thorn-scale; 7, spindles of collaret and 8, of points; 9,
spicules from the tentacles. All spicules enlarged to scale shown beneath Fig. 4.
60 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
Their appearance in situ on the calicles is shown
in Higs2:
(c) Polyps: the collaret contains about 5
transverse rows of curved spindles, in smaller
polyps as few as 3 rows, in larger individuals as
many as 5 or ozcasionally 6 rows. In polyps of
average size they have a length of 0.5 mm (Fig.
“UU GO
|
|
OA So,
Sere Res
VOL. 49, No. 2
7). Surmounting the collaret, the eight opercu-
lar points contain one pair of large, bent spin-
dles about 0.5 mm long (Fig. 8) and another
pair or two of smaller but similar accessory rods.
The appearance of the closed operculum, partly
retracted within the calicle, is shown also in Fig.
2. The tentacles contain the small, flat, bent rod-
ral
Par N +
MEE a
Fies. 10-15.—Spicules of Placogorgia: P. mirabilis (10a, ealicular thorn-seale; 10b, cortical spindle) ;
P. atlantica (lla, calicular thorn-scale; 11b, cortical spindle); P. tenuzs (12a, crutch-shaped rod from
opercular sector; 12b, calicular thorn-scale; 12c, cortical sclerite); P. rudis (13a, calicular thorn-seale;
13b, cortical sclerite); P. placoderma (14a, cortical sclerite; 14b, calicular thorn-scales); P. trzbuloides
(15a, cortical sclerite; 15b, calicular thorn-scale).
FEBRUARY 1959
lets with laciniated edge that are characteristic
of paramuriceid genera (Fig. 9).
Color —White, the light brown axis showing
through the translucent spicules.
Holotype—US.N.M. no. 10204. Straits of
Miowoa on Havana, Cuba: 23° 10’ 39” N.,
82° 20’ 21” W., 204 fathoms, January 19, 1885;
collected by tangles. Albatross station 2335.
Remarks—Four other species of Placogorgia
are known to occur in the Atlantic: Placogorgia
atlantica Wright and Studer, P. mirabilis Deich-
mann, P. rudis Deichmann, and P. tenuis (Ver-
rill). Placogorgia tribuloides differs from all these
species in the large size of its thorn-scales, which
approach the type found in Paramuricea. That
genus, however, lacks the large cortical spindles
or plates with serried processes. P. tribuloides
further differs from P. mirabilis in the absence of
excessively large (4 mm) spindles in the cortex;
from P. rudis, which has similar cortical spindles,
by its large and sharp thorn-scales; and from
P. tenuis by the frequent development of sev-
eral spies on the cortical spindles and the lack
of the single large, crutch-shaped rod in the
opercular segments. These differences may be
set forth in the form of a dichotomous key:
1. Cortex contains large spindles up to 4 mm in
length, clearly visible to the unaided eye
(Fig. 10b). Anastomosis of branches frequent
Placogorgia mirabilis Deichmann
Largest spindles of cortex less than 2 mm in
length. Anastomosis of branches infrequent
SY BESET. 0 4 ot re een 2
2. Operculum usually with a single large, crutch-
shaped rod (Fig. 12a) in each sector. Cortical
spindles up to approximately 0.6 mm in length,
usually with only one projecting process (Fig.
12c), sometimes none
Placogorgia tenuis (Verrill)
Operculum with at least two large, bent spin-
dles in each sector, not a single crutch-
SiZDEC) (GG). so a a 3
3. Cortical spindles small, usually not exceeding
a length of 0.5 mm, without a row of promi-
nent external spines (Fig. 11b). Thorn-scales
0.5 mm long, spine 0.38 mm, sharp and aculeate
(Fig. 11a)
Placogorgia atlantica Wright and Studer
BAYER: REVIEW OF PLACOGORGIA STUDER 61
Cortical spindles larger, up to 1.5 mm in length,
many of them with a row of spines (Figs. 138b,
15a)
4. Calicular thorn-scales large, 1.7 mm _ over-all,
with a strong, sharp spine as much as 1 mm in
length (Fig. 15b)
Placogorgia tribuloides, n. sp.
Calicular thorn-scales smaller, usually not more
than 0.5 mm over-all, spine stout, mostly blunt
or moderately sharp (Fig. 18a), commonly
0.2-0.25 mm long and rarely up to 04 mm,
often with several prominent terminal sub-
GINAISIOINS). on one Placogorgia vudis Deichmann
REFERENCES
AvrRIvILLIus, Macnus. The gorgonarians from Dr.
Sixten Bock’s expedition to Japan and Bonin
Islands 1914. Kungl. Svenska Vet.-Akad.
Handl. (3)9(4): 337 pp., 65 figs., 6 pls. 1931.
Bayer, Freperick M. Les octocoralliaires plex-
aurides des cdtes occidentales d’ Amérique.
Mém. Mus. Nat. Hist. Nat., Paris, nouv. sér.
(A)16(2): 41-56, 6 pls. 1958.
DEICHMANN, EisaBeTH. The Alcyonaria of the
western part of the Atlantic Ocean. Mem. Mus.
Comp. Zool. 53: 317 pp., 37 pls. 1936.
JOHNSON, JAMES YATE. Descriptions of some new
corals from Madeira. Proc. Zool. Soc. London
1862: 194-197, 14 figs. 1862.
KUKENTHAL, WILLY. Gorgonaria. Wiss. Ergebn.
deutschen Tiefsee Exped. 13(2): 946 pp., 318
figs., pls. 30-89. 1919.
Gorgonaria. Das Tierreich 47: xxvii +
478 pp., 209 figs. Berlin, 1924.
Nvuttine, CHARLES CLEVELAND. The Gorgonacea of
the Siboga Expedition. III. The Muriceidae.
Siboga-Exped. Monogr. 13°: 108 pp., 22 pls.
1910.
Descriptions of the Alcyonaria collected
by the US. Fisheries steamer “Albatross,”
mainly in Japanese waters, during 1906. Proc.
US. Nat. Mus. 43: 1-104, pls. 1-21. 1912.
StupER, THEOPHILE. Versuch eines Systemes der
Alcyonaria. Arch. Naturg. 53 Jahrg. (1): 1-74,
folio dl, Iessyi
TuHomson, J. ArtHUR. Alcyonaires provenant des
campagnes scientifiques Prince Albert I°" de
Monaco. Rés. Camp. Scient. Albert I°* Monaco
1a he Pps Oo pls. 1927.
WricHtT, EpwarD PERCEVAL, and STUDER, THEOPHILE.
Report on the Alcyonaria collected by H.MS.
Challenger during the years 1873-1876. Repts.
Voy. Challenger, Zool., 31 (part 64): Ixxi +
314 pp., 438 pls. 1889.
62 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 2
ARCHEOLOGY SALVAGE PROGRAM IN CHATTAHOOCHEE VALLEY
Five thousand years of buried history are
represented in the lower valley of the Chatta-
hoochee River of Alabama and Georgia, which
soon will be inundated by a group of dam-
created reservoirs. This is indicated in a pre-
liminary survey by archeologists of the River
Basin Surveys—joint project of the Smithsonian
Institution, National Park Service, and Corps
of Engineers—to explore sites of archeological
and historic significance which will be flooded
in extensive dam-building plans.
Largest of the areas to be inundated will be
the Walter F. George Basin, named for the late
senior senator from Georgia. The survey re-
vealed 117 sites in Georgia and 90 on the Ala-
bama side of the Chattahoochee, and they are to
be explored more thoroughly—the most worth-
while with extensive excavations—before the
Army engineers complete their work.
These sites range from simple Indian village
locations to areas containing remains of several
different cultures, and from single mounds in
which Indians buried their dead to multiple
groups of mounds surrounding ceremonial pla-
zas. There also are two historic sites of consider-
able importance. One is the Spanish fort of
Appalachicola, dating from 1689 to 1691, and the
other the historic Creek Indian town of Ro-
anoke, which was occupied by white settlers and
then attacked and burned by the Indians in
1736. The fort will lie just outside the pool area,
but, because the exact dates of its occupancy are
known, it will be tested as it should provide an
important check point in working out the chron-
ology of the area. The remains of Roanoke also
will be helpful in that respect and should be
quite productive of archeological specimens.
Plans are being made to start excavations there
this spring.
The Indian sites in the Walter F. George
Basin date from about 4,000 B. C. to relatively
late Creek villages of the period from 1675 to
1836. These latter present the possibility of a
specific identification of sites from ethno-histor-
ical and other documentary evidence.
Two other Chattahoochee Valley dams are
also under construction—the Columbia Dam,
which is another project of the Army Engineers,
and the Oliver Dam of the Georgia Power Co.
The basins to be flooded by these reservoirs are
an integral part of the picture and must be
studied in conjunction with the Walter F.
George Basin. Work is just beginning at the
Columbia Dam, while the Oliver Dam is virtu-
ally completed and will be closed in April. Two
River Basin Survey parties will start excava-
tions at the Columbia Dam site in February.
Complete coverage of that Basin was not pos-
sible in the preliminary survey, but 14 sites were
located. One, a major mound probably dating
from about 300 years before Columbus, already
is half destroyed by the river and will be the
scene of operations of one of the field parties.
The University of Georgia is cooperating in the
salvage program and since last fall has been test-
ing a series of sites in the Oliver Basin. Much
useful information has been obtained. The work
there has been supported by a grant from the
Georgia Power Co.
Only sporadic archeological work has been
done in the Chattahoochee area in the past, and
an extensive program of excavations is indicated.
In addition to the University of Georgia, Ala-
bama and Florida institutions probably will co-
operate with the Smithsonian Institution and the
National Park Service in the salvage program.
——$—<$_ $e —_—$§_ i _—
GRASS PRIMER REPRINTED
The Smithsonian Institution announces the
publication of a new edition of First Book of
Grasses, by Dr. Agnes Chase, one of the world’s
foremost agrostologists. Formerly botanist of the
United States Department of Agriculture and
now honorary Fellow of the Smithsonian Insti-
tution, Mrs. Chase will observe her ninetieth
birthday on April 20, 1959. Much of her scientific
work has appeared in this JOURNAL.
Since it first appeared in 1922, this book has
been the companion of succeeding generations of
FEBRUARY 1959
beginning students of grasses. It has been out of
print for several years. The present revised (3d)
edition, 150 pages in length, contains 94 of the
author’s drawings of grasses, plus a frontispiece
OBITUARY 63
reproduced in color of Albrecht Diirer’s painting
“Das grosse Rasenstiick.” Dr. Leonard Car-
michael, Secretary of the Smithsonian Institu-
tion, has contributed a new Foreword.
Clarence Rapmond Shoemaker
March 12, 1874—December 28, 1958
Love of the outdoors and natural history ran
strong in the Shoemaker family, staunch, thrifty,
purposeful Quaker farming folk who originally
settled in Cheltenham, Pa., in the days of Wil-
ham Penn. Some became businessmen, others
millers; a few became well-known naturalists.
Clarence Shoemaker’s grandfather, George,
who left Pennsylvania for Georgetown in 1818,
was a miller, who controlled the former Co-
lumbia Flour Mills. He served as local flour
inspector for 48 years and, interestingly enough,
was an amateur horticulturist and fruit grower.
Clarence’s first cousin, Ernest (1866-1957), be-
came a well-known coleopterist. His exception-
ally fine personal collection of beetles, butter-
flies, and moths was bequeathed to the U. 8.
National Museum, while his extensive collection
of American Indian arrowheads went to the
American Museum of Natural History in New
Work,
Clarence’s bent for natural history developed
early on spacious grounds graced with forest
trees, ornamental shrubbery, and gardens sur-
rounding his home in then bucolic Georgetown.
The place was always alive with birds far beyond
what one can find today in that now more settled
area. Here he lived from the age of seven until
his death, December 28, 1958, at the age of 84.
It was quite natural that in his teens he should
become one of the very early members of the
Washington Audubon Society. As one of its most
dedicated and ornithologically knowledgeable
members, he was much sought after as a bird-
walk leader. Equally interested in native wild
flowers, he was also for many years an active
and enthusiastic participant in the botanical “‘ex-
cursions” conducted by the Wildflower Preserva-
tion Society. Moreover, the Foundry Flour Mill,
managed by his father, Francis Dodge Shoe-
maker, and his uncle, David, which supplied
large quantities of flour to the Federal Govern-
ment during the Civil War, was situated on
Foundry Branch near the erossing of the first
Potomac aqueduct, between the river and the
Chesapeake and Ohio Canal, from which it drew
its waterpower. Though scarcely a quarter of a
mile beyond the town that then was Georgetown,
it was an unspoiled wooded area where wildlife
and flowers abounded and where virtually all the
local species of either could be found at one
season or another.
Shoemaker was educated in a private school
in Georgetown. From this he went for a year to
the Western High School but graduated from
Central three years later, in 1897. In this latter
school he received his first formal instruction in
biology. He also took (1910-1911) collegiate
work in that subject at George Washington Uni-
versity but did not continue, for, as he expressed
it, he already knew more zoology than was then
taught to undergraduates there. That rather
comprehensive knowledge he had gained in the
field and through his long association with the
Smithsonian Institution.
It was quite natural that, as a young man
born in Washington and with his interest in
natural history, he should turn to the Nation’s
pioneer scientific establishment nearby in search
of a future. The first opening that came his way,
however, was a clerkship in the Smithsonian’s
International Exchange Service of which an
older cousin, Coates W., was the chief. Given this
opportunity, he further developed another in-
terest—spiders—that he had earlier acquired on
the home and mill grounds. Not only did he
continue assiduously to collect them and build
up an extensive library of arachnid literature,
but he so well mastered the systematics of the
group that he was soon recognized as an au-
thority on the local fauna. As a consequence, he
was frequently called upon by the U.S. Depart-
ment of Agriculture and others to identify
spiders. Later his spider collection was left to
64 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
the National Museum and is incorporated in its
larger study collections.
In 1910 Dr. Mary J. Rathbun, in charge of
the marine, aquatic, and terrestrial invertebrates
in the National Museum, gave him his first op-
portunity for full-time zoological work as sci-
entific aide in her division. He was promoted to
assistant curator in 1921 and associate curator
in 1942. Retiring in 1944 at the age of 70, he was
given the honorary title of research associate in
the Smithsonian Institution. It was Miss Rath-
bun who assigned to him the study of the vast
and largely, at the time, unworked collection of
amphipod crustaceans to which he thereafter
rather closely devoted the rest of his life. Though
relinquishing his interest in spiders and giving
somewhat less attention to his fieldwork with
birds and flowers, he continued to maintain his
very colorful iris garden. In its heyday it was one
of the show places in Old Georgetown.
Throughout his life Mr. Shoemaker was an
active member of the Audubon and the Wild-
flower Preservation Societies already mentioned,
the Biological Society of Washington, the Wash-
ington Biologists’ Field Club, the American As-
sociation for the Advancement of Science, and
the Washington Academy of Sciences to which
he was elected in 1939. He was also a member of
the American Ornithologists’ Union and a char-
ter member of the American Society of the
Mammalogists and of the Society of Systematic
Zoology.
His scientific reports on the Amphipoda fig-
uratively covered the world, for, because of his
very special knowledge of that group of crus-
taceans, he received collections for study from a
number of important scientific expeditions.
Among these expeditions are to be numbered the
South Georgia and Belgian Congo Expeditions
vou. 49, NO. 2
and the biological survey of Porto Rico and the
Virgin Islands of the American Museum of Nat-
ural History in New York; the Bermuda Ex-
peditions of the New York Zoological Society;
the Canadian Cheticamp and Hudson Bay Ex-
peditions; the Canadian Arctic Expedition, the
U. S. Antarctic Expedition of 1939-1941; the
Point Barrow, Alaska, Expedition; various West
Indian expeditions, including his own to the
Florida Keys and the American Virgin Islands;
the Johnson-Smithsonian Expedition to the
Porto Rican Deep; and the Presidential Cruise
to the Galapagos Islands. Up to the time of his
retirement he had published 56 papers on these
forms, and since that occasion some 14 others.
Beyond these, by the time of his first serious
illness preceding his death by a bare three weeks
he had completed and illustrated several addi-
tional manuscripts that are about ready for the
printer except for typing. The very last of these
contained the descriptions of two new and un-
usual species of amphipods taken on the Smith-
sonian-Bredin Caribbean Expedition in the
spring of 1958.
He was a meticulous worker. His desk and
laboratory table (they were one), his instru-
ments and optical equipment, notes, card files,
and publications were left in excellent order.
There have been few specialists on amphipods
who knew them as well, loved them as much, and
described and figured them as carefully as Mr.
Shoemaker. He was his own artist, and his draw-
ings were exceedingly clear and accurate; no es-
sential detail was ever glossed over or overlooked.
As a kindly, unassuming friend, and a sci-
entifically productive individual, he will long be
remembered by his colleagues in this Museum
and coworkers elsewhere around the world—
Watpo L. ScHmirt.
Officers of the Washington Academy of Sciences
SDE...) FRANK L. CampBEtL, National Research Council
Pepeereart CIert. 2... ee LAWRENCE A. Woop, National Bureau of Standards
JiR i. re Heinz Specut, National Institutes of Health
RINE oe. 8. oo. ee ee W. G. BromBacHEeR, National Bureau of Standards
EPRPMAOESE >= =.->.-.- Morris C. Lmixinp, Armed Forces Institute of Pathology
Custodian of Publications............... Haratp A. Renper, U.S. National Museum
SEM ee ee CuesteR H. Pacs, National Bureau of Standards
(2) LBS LD Deh) H. A. Borruwicrx, T. D. Stewart
emmaersie 196) |... we Bourpon F. Scrisner, Keita C. JOHNSON
CRS S22 4 ee Puitip H. ABELSON, Howarp S. RAPPLEYE
Board of Managers....All the above officers plus the vice-presidents. representing the
affiliated societies
CHAIRMEN OF COMMITTEES
Standing Committees
SIE ao ks sk he tees es FRANK L. CAMPBELL, National Research Council
Meetings..... eee RatpH B. KENNARD, American University
Membership............ LawreNncE M. KusHNER, National Bureau of Standards
Monographs........... Peer os Dean B. Cowie, Carnegie Institution of Washington
Awards for Scientific Achievement....... FRANK A. BIBERSTEIN, Catholic University
Grants-in-aid for Research...... B. D. Van Evera, George Washington University
Policy and Planning.............. MarcGaret Pitrman, National Institutes of Health
Encouragement of Science Talent.............. Leo ScuusertT, American University
Science Education............ RayMoNpD J. SEEGER, National Science Foundation
Miavaaua Means...........:.. RussELL B. Stevens, George Washington University
MIC UEPCINOEONS. ... 2... 5.2 eee cece Joun K. Taytor, National Bureau of Standards
Special Committees
2 OS... Harotp H. SHeparp, U. 8. Department of Agriculture
Mireecieye.............. James I. HAMBLETON, U.S. Department of Agriculture (Ret.)
emwetty On GONPTESS............-....--- Joun A. O’Keere, National Aeronautics and
Space Administration
CONTENTS
Page
The Academy Membership Committee.................-...-.-00005- St
GENERAL SCIENCE.—Moon bound. RAYMOND J. SEEGER.............. 42
Botrany.—Supplementary studies in Aeschynomene, I: Series Viscidulae,
including a new species and five new varieties. VaivaA E. Rupp.... 45
Zootocy.—A review of the gorgonacean genus Placogorgia Studer, with
a description of Placogorgia tribuloides, a new species from the
straits of Florida. FREDERICK Mi. BAYER. ..\.[722..... 2 seo 54
Notes:and INEWS. Vs eu's ho oe ee a ee ee 40, 52, Ss, 62
| ee ey ay .
OBITUARY: Clarence*B.. Shoemaker..°°.0......-. 2.0). 3 ee 63
i s by a “ate SS
‘ See week
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VOLUME 49 March 1989 NUMBER 3
JOURNAL
OF THE
WASHINGTON ACADEMY
OF SCIENCES
————_—_T
oo
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JOURNAL
OF THE
WASHINGTON ACADEMY OF SCIENCES
Vou. 49
Marcu 1959
No. 3
mar STOOMPRISING A SYMPOSIUM:ON THE SUBJECT EXTRA-
MURAL SCIENCE PROGRAMS OF THE FEDERALGOVERNMENT,”’
ARRANGED BY A COMMITTEE OF THE WASHINGTON ACADEMY
OF SCIENCES (GEORGE W.IRVING, CHAIRMAN) AND PRESENTED
SUNDAY MORNING, DECEMBER 28, 1958, AT THE SHERATON-
miviewHtOrEl, WASHINGTON, D.C. AS THE ACADEMY’S CON-
iminwiON TO THE 125TH MEETING OF THE AMERICAN
ASSOCIATION FOR THE ADVANCEMENT OF SCIENCE
Introductory Remarks by Dr. A. T. McPherson, Presiding
It is a great pleasure for me, as the Presi-
dent of the Washington Academy of Sci-
ences, to welcome you to the symposium on
“Extramural Science Programs of the Fed-
eral Government.” This symposium is the
Washington Academy’s contribution to the
125th meeting of the American Association
for the Advancement of Science. As you
know, Washington is the scientific as well
as the political Capital of the United States.
Every major scientific activity in our Gov-
ernment has its headquarters in or nearby
Washington. Moreover, several of the na-
tional scientific societies have established
their national headquarters here in Wash-
ington, owing at least in part to their desire
to be near the scientific activities being con-
ducted here at the seat of Government.
Among these is, of course, our own Associa-
tion.
Since Washington is unique in being the
center of Federal scientific activity, 1t was
felt in planning this symposium that our
most useful contribution would be to have
representatives of the principal agencies of
the Federal Government describe some as-
pect of the research supported by them. In-
asmuch as many who attend the AAAS
meetings have conducted research under
65
Federal support or may wish to, it occurred
to us that the aspect that would be of most
interest to the greatest number would be
the extramural science programs each
agency sponsors. It is particularly appro-
priate, we feel, that the Washington Acad-
emy of Sciences has been given the oppor-
tunity to do this since it is the one scientific
society in the Nation’s Capital that counts
among its membership representatives of all
the scientific disciplines. Included in its
membership also are many of the policy-
making scientists of the Federal Govern-
ment.
Perhaps it 1s appropriate at the outset
to indicate what we mean by “extramural”
science programs. We mean, simply, any
programs that are conducted outside of the
physical facilities of an agency and staffed
predominantly by non-Federal employees.
This includes scholarships, fellowships,
grants, grants-in-aid, loans, contracts and
cooperative programs.
It would be impossible in the time allotted
this session to include a description of every
extramural program that is now in effect in
the Federal Government. We have selected,
rather, the six Federal agencies which, to-
gether, support the majority of extramural
SME TION | MAY 8 2 one
66 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
research and science education programs in
the country. They are, as your program in-
dicates, the National Science Foundation,
the National Institutes of Health, the U.S.
Department of Agriculture, the Department
of Defense, the Atomic Energy Commission,
and the National Aeronautics and Space
Administration. The representatives of
these agencies here with us today can speak
authoritatively on the extramural programs
for which their agencies are responsible,
since they occupy in each ease high positions
in their respective agencies.
VoL. 49, NO. 3
The order of presentation is immaterial
except for the first. We have asked the rep-
resentative of the National Science Foun-
dation to lead off since the NSF, in addition
to its responsibility for its own direct ex-
tramural programs, has certain coordinating
responsibilities for science programs in all
Federal Government agencies as well.
We hope that this symposium will give
you a clear picture of the extramural re-
search and science education program of the
Federal Government in its entirety.
EB
Extramural Science Programs of the National Science Foundation
By Rosert B. Brove, Associate Director for Research, National Science Foundation
We are here as representatives of several
of the Federal agencies to discuss the nature
and scope of our respective agencies’ extra-
mural programs for research and education
in science. The National Science Foundation
conducts no research or education programs
itself. All the support of education and re-
search by the Foundation is through extra-
mural grants and contracts.
The nature of the activities of the Foun-
dation and its objectives are adequately de-
scribed in the Act of Congress which was
approved by the President in May 1950 and
led to the establishment of the National
Science Foundation as an independent Fed-
eral agency. Section 3 of this Act states
that the Foundation is authorized and di-
rected “to develop and encourage the pur-
suit of a national policy for the promotion
of basic research and education in the sci-
ences; to initiate and support basic scientific
research...; to appraise the impact of re-
search... .”
In carrying out these directives the Foun-
dation is itself forbidden to operate any
laboratories or pilot plants. The Act permits
the making of contracts or grants for sci-
entific research through the utilization of
appropriations available in such a manner
as will best realize the objectives of the
Foundation. There is very great freedom
given to the Foundation in the choice of
organizations or institutions to which grants
or contracts may be given. While nonprofit
organizations are particularly identified, the
Foundation is not exclusively restricted to
this type of agency. It may make grants to
such institutions, individuals, agencies of
the United States, and the several States
as are qualified to best realize the objectives
of the Foundation—in particular, the ad-
vance of basic research.
A very substantial part of the business of
the National Science Foundation is the sup-
port of basic research in science through
institutions and individuals that are best
qualified to pursue such research. Advisory
panels and program officers of the Founda-
tion consider many factors in assessing re-
search proposals: the qualifications and
promise of the investigator; the nature of
the proposed research project; and the fa-
cilities and support provided by the institu-
tion. |
The Foundation is very conscious of the
outstanding contributions made by a small
number of scientists with exceptional abil-
ity. These men, together with a much larger
number of good but not remarkable workers,
will create the new developments in basic
science. The Foundation is constantly look-
ing for the young scientist who shows signs
of real originality and boldness in his ap-
proach to scientific research.
|
|
|
|
|
Marcu 1959 EXTRAMURAL PROGRAMS OF THE NATIONAL SCIENCE FOUNDATION 67
In some areas of research the scientist’s
needs are easily met—books, pen, and paper
may satisfy the mathematician. In most
fields, however, the success of basic research
in science depends on the accessibility of the
necessary tools and assistants. Some of the
modern research facilities are very costly
and require large staffs of scientists and
technicians for their operation. Nuclear re-
actors, cyclotrons, computers, radio and
optical astronomy observatories have been
built in part or wholly by Foundation
grants.
In addition to providing the equipment
required, Foundation support of research
projects provides employment opportunities
as research assistants for more than 6,000
eraduate students studying for the Ph.D.
degree.
Most of the basic research in this country
is carried forward by our colleges and uni-
versities. It is therefore not surprising that
nearly all the Foundation support of basic
research is given to institutions of higher
learning. This support is provided in almost
every case through the use of a grant rather
than by a contract.
In addition to its support of basic re-
search, the Foundation supports a substan-
tial program for the promotion of education
in the basic sciences. The Foundation is di-
rected by Congress to develop and encour-
age a national policy for the promotion of
education in the sciences and in particular
to award scholarships and fellowships. The
award of fellowships to graduate students
appears to have been an unusually success-
ful enterprise, and thousands of scientists
have been assisted by this program. Fellow-
ship support has been extended to post-
doctoral research workers and even to jun-
ior and senior faculty to assist them in
developing new research programs or to en-
hance their competence as teachers. The
competition for National Science Founda-
tion fellowships is severe, and the award of
a fellowship is considered as recognition of
very high scholastic achievement and re-
search promise.
Foundation support of education in the
sciences extends to universities and colleges
in all States through establishment of sci-
ence teacher institutes. These are designed
to improve the training of science teachers,
especially secondary-school teachers, in the
subject matter of science. Approximately
300 summer institutes will be functioning
under this program in the summer of 1959.
In addition, about 35 academic year insti-
tutes will begin in the fall of 1959, as well
as some 200 in-service institutes designed
to benefit the teacher who lives in the vi-
cinity of the college or university by offering
courses taught at night or on Saturdays.
The Foundation has developed several
experimental programs in education; most
of these are built upon patterns established
either by the fellowship or the institute
program. The Foundation is also extending
substantial support to curriculum improve-
ment programs for secondary-school science
courses, in physics, mathematics, chemistry,
and biology, but extending as well to many
of the other sciences.
Knowledge is society’s most precious pos-
session, and a very important and rapidly
growing area of knowledge is basic science.
The value and use of knowledge can be as-
sured for future generations only if we re-
cord in publications the results of our re-
search. The critical problem of scientific
literature is illustrated by the tremendous
volume that must be assimilated. If the
auditorium were full, all of the people in
this room reading 24 hours a day could not
keep up with our present output of scientific
literature. The rate of increase of literature
is such that the world’s output in pages per
year will double in the next 8.5 years. The
National Science Foundation has contrib-
uted substantially to this flood of scientific
literature by making grants to scientific so-
cieties to aid in the establishment of new
journals or in the expansion in size of exist-
ing publications. The importance of Soviet
scientific developments has been recognized
in our program for English translations of
important journals and books that are avail-
able only in the Russian language.
Not only is it necessary to print and store
in our libraries the full account of our total
knowledge, but we must also develop the
means of identification and retrieval of this
knowledge. We are assisting abstract jour-
nals as well as general studies of new means
of searching for information. The Office of
68 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
NATIONAL SCIENCE FOUNDATION
Millions of Dollars
GROWTH OF MAJOR
FOUNDATION SUPPORT
00 PROGRAMS...FY 1952-59
DOLLARS
= =
HB international Geophysical Year
BS Focilities
| Eis} Education in the Sciences
ce = Research
|
40 |
20 |
1952'53 '54 '55 '56 '57 '58 '59
Fiscal Years Est
Cuart 1
Science Information Service is a division of
the Foundation that provides assistance and
coordination to Government and private ab-
stracting and information-handling services.
It is not a Government office set up to an-
swer requests of the general public or of
Government agencies for information about
specific technical questions.
There have been two events since the in-
itiation of the Foundation in 1950 which
have appreciably changed the anticipated
growth of Federal support for this agency.
The International Geophysical Year, which
officially ends next Wednesday, has been an
intensive burst of scientific effort with a
year of preparation and an 18-month year
of coordinated observations. For some years
to come the results and deductions from this
period of observation will be published in
scientific journals. The second event that
affected the Foundation’s budget was the
awakening of the world by the Russian
Sputnik. We have suddenly realized that
leadership can be substantially influenced
by the intellectual and technical attain-
VoL. 49, No. 3
ments of a nation. This leadership requires
not only adequate support for the research
of its talented scholars but also an educa-
tional system that identifies potential schol-
ars and gives them the best possible prep-
aration for their careers. Chart *1 shows
the growth and magnitude of the support
given the Foundation.
The National Science Foundation makes
grants to scientists on the basis of proposals
submitted to it and reviewed by panels of
specialists and by the Foundation’s program
offices. Some of these grants assure support
for three to five years, while others are for
one or two years. The funds provided by
Congress have only been sufficient to enable
the Foundation to grant less than a third
of the proposals it receives. It is quite nat-
ural that the scientist who has won the
competition for an award will return after
a year or two for further support and he
will then, because of the greater opportunity
provided by the Foundation funds, present
an even better justification for his support.
The percentage of proposals for research
support to which grants were awarded is
shown in Chart *2. This is by no means an
established pattern of support. Many mer-
itorlous proposals are now refused grants.
At times we have been able to grant less
than one-third of the requests considered
worthy of support by the review panels.
The use of substantial funds by the Foun-
dation has enabled it to support the con-
struction of such facilities as the National
Radio Astronomy Observatory, Green
Bank, W. Va., and the Kitt Peak National
Observatory, Tucson, Ariz. These national
laboratories and institutes carry with their
creation an implied commitment for con-
tinued operating budgets. The Foundation
is indeed concerned with the problem of
providing adequate support for the major
facilities, and for the continued support of
able scientists who justify essentially life
time support. To this committed support
load must be added the encouragement and
opportunity which the Foundation must be
prepared to offer to the young scientist be-
ginning his independent research activity.
Congress has directed that the Founda-
tion avoid undue concentration of research
and education activities. A measure of the
Marcu 1959 EXTRAMURAL PROGRAMS OF THE NATIONAL SCIENCE FOUNDATION 69
needs for basic science research support may Support for education through fellow-
be indicated by the number of graduate stu- ships and institutes for teacher training has
dents or by the dollar grants. Chart %3 been nationwide but not in all cases as well
shows that the grants given are in reason- distributed as would be desired for a na-
able balance with these two measures of tionwide program. We have attempted to
need. correct these discrepancies as they are iden-
NATIONAL SCIENCE FOUNDATION
PERCENTAGE OF GRANTS AWAKDED
TO PROPOSALS RECEIVED-FISCAL YEARS (963-1989
Millions of Dollars Fiscal Years 1953-1959
150
Ul Proposals Received
HE Gronts Awarded
Percentages indicate proportion
of grants awarded to proposals
received in the Fiscal Year
1953 1954 1955 1956 I1957 1958 1959
Fiscal Years
CuHart 2
NATIONAL SCIENCE FOUNDATION
REGIONAL COMPARISON OF PROPOSALS RECE/VED(NUMBER)
GRANTS AWARDED (NUMBER), ana! GRADUATE STUDENT POPULATION
(Expressed in % of total of each index)
07% 07% 0.5%
BB Proposals (FY /952-58/
[] Grants (FY /952-56/
Eee) Graduate Students (/955-56/
Cuart 3
70 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
tified. A program of cooperative fellowships
is being introduced this year which will pro-
vide a much wider distribution of fellows
throughout the Nation, but still permit the
applicant to select freely the institution
through which he seeks to compete for the
fellowship.
The activities of the Foundation are not
restricted entirely to this country. Fellow-
ships are granted only to citizens, but they
may use their grants for study at foreign
universities. Funds in support of research
have frequently been used by grantees to
carry on their studies in foreign countries;
and in exceptional cases grants have been
made to a few foreign investigators whose
work was considered essential to our own
programs or involved the active participa-
tion of American scientists or students. We
have responsibilities for assistance to par-
ticipants in international conferences and
congresses. In our Office of Science Informa-
tion Service we arrange for the exchange of
VoL. 49, NO. 3
publications and for the translation of some
of these so that they will be generally avail-
able to scientists.
The principal objective of the National
Science Foundation is the development of
basic science in the United States. We are
attempting to do this by direct support of
the scientist in his research program, by
supplying him with the means of publishing
his results, with ready access to the results
of the work of other scientists, and by 1m-
proving our educational system so that
promising scholars are given a better foun-
dation for their future careers. Some very
valuable and exciting advances have al-
ready been made in science through our
support, but the major impact of such a
broad program as we have undertaken will
not be measured by the visible splashes but
rather by the rising tide of general basic
science development and the technological
benefits that later come to society through
their application and use.
Extramural Science Programs of the Department of Defense
By GrorGE D. LuxKss, Hzecutive Secretary, Defense Science Board, Office
of the Director of Defense Research and Engineering!
I appreciate the invitation of the Wash-
ington Academy of Sciences to participate
in this symposium and to make the Defense
contribution on extramural science pro-
grams of the Federal Government. We in
Defense find a symposium of this nature an
excellent opportunity to get across to the
scientific community at large the nature and
scope of our scientific research activities
and, particularly in the theme of today’s
session, how our extramural activities con-
tribute to the achievement of Defense ob-
jectives. Within this framework I shall also
weave some of the more significant aspects
of our policy on basic research in the hope
of furthering understanding.
*Formerly Office of the Assistant Secretary of
Defense (Research and Engineering).
DOLLAR MAGNITUDE, PERFORMANCE COMPO-
NENTS, AND RESEARCH SUPPORT LEVELS
It is important to provide, first, a back-
drop of the total dollar effort of Department
of Defense scientific research and develop-
ment. The first chart shows graphically the
DOD obligations for fiscal year 1959 in re-
lation to those of the other Federal Govern-
ment agencies. Something like 62 percent of
all Federal funds devoted to research and
development represents the Defense De-
partment’s share of the Federal effort. The
second chart displays the approximate dis-
tribution of these funds in terms of the three
major performance components: Govern-
ment laboratories, industrial contractors,
and university and other nonprofit institu-
Marcu 1959 EXTRAMURAL SCIENCE PROGRAMS OF THE DEPARTMENT OF DEFENSE 71
tions. You will note that industry performs
about 60 percent of the total effort sup-
ported from the research and development
appropriations of the Department of De-
fense, universities and other nonprofit in-
stitutions conduct about 9 percent, and
Government laboratories perform the bal-
ance of 31 percent. Of funds for in-house
performance, approximately 14 percent is
for research and development per se con-
ducted internally by Government scientists
and engineers, 13 percent is for test and
evaluation, and 4 percent is for contract
monitoring.
I should now hasten to add that an addi-
tional source of funds is available for sup-
port of scientific and engineering activities
of the Department of Defense, primarily
the latter. These, in appropriation language,
are principally the Procurement and Pro-
duction funds, of which something like $3.2
billion in fiscal year 1959 go to the support
of development, test, and evaluation of new
weapons of the distinctively hardware vari-
ety—the B-58 and the IRBM and ICBM
programs are good examples. The charts
presented do not include the funds from
this source; within the theme of this sym-
posium—extramural science—their omis-
sion is of little consequence, however.
Now let us discuss the scientific research
activity of the Defense effort. The third
chart displays the character distribution of
the Defense research and development pro-
gram. Of our fiscal year 1959 research and
development programs, 15 percent, or $391
million, is devoted to research; and of this
$109.6 million is for basic research. The
balance, 85 percent of the total program, is
for development. We estimate that almost
two-thirds of the $391 million of research
funds supports extramural activities, and at
least 70 percent of the $109.6 million basic
research funds is devoted to extramural
support of basic research.
NATURE AND SCOPE OF DEFENSE SCIENTIFIC
RESEARCH ACTIVITIES
The science programs of the Department
of Defense comprise activities in the physi-
cal and engineering sciences, in the life sci-
|
BASIC RESEARCH
Cuart 1. Estimated Distribution of FY 1959
Federal Government Research and Development
Obligations.
NAT'L AERONAUTICS
AND SPACE
ADMINISTRATION
HEALTH, EDUCATION,
, DEPARTMEN — AND WELFARE
j OF DEFENSE
AGRICULTURE
1.2% INTERIOR
0.7% COMMERCE
1.5% NAT'L SCIENCE
FOUNDATION
ALL OTHER
Cuart 2. Where Defense Research and
Development is Performed.
UNIVERSITIES AND
OTHER NONPROFIT
INSTITUTIONS 9%
OVERNMEN
ABORATORIE
:INDUSTRIA
ONTRACTOR
Cuart 3. Character of Defense Research and
Development Program for FY 1959.
72 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
ences, in psychology and the social sciences,
and in operations research.
About 80 percent of the funds devoted to
scientific research support activities in the
physical and engineering sciences; this
amounts to about $313 million in fiscal year
1959 Defense program. Within this broad
category the typical fields of endeavor and
the program objectives are as follows:
In physics the objective is the advance-
ment, through systematic and exploratory
research, of those selected aspects of pure
and applied physics which contribute to an
increase in military capability. The present
program, totaling about $33 million in ex-
tramural effort, includes solid-state physics,
extreme-temperature physics, statistical
physies, physics of atoms and molecules, nu-
clear physics, physical acoustics, upper-air
physics, electron physics, optics, magnetism,
instrumentation for physical measurements,
and electromagnetic radiation.
In chemistry the objective of the program
may be divided into two parts: (1) a bal-
anced effort of selected fundamental re-
search which serves as a foundation for the
varying needs of the military and (2) spe-
cific applied projects aimed at satisfying
short-term defense needs. The present pro-
gram includes research support in relevant
areas of analytical, inorganic, organic, phys-
ical, polymer and radiation chemistry. The
extramural support runs about $31 million
yearly.
In mathematics the objective is the sys-
tematic advancement of this science, closely
geared to the objectives of the other scien-
tific programs, and in response to expanding
needs for direct qualitative information
about the design and operations of weapons
and weapons systems. The present program
includes algebra, analysis, geometry, topol-
ogy, probability, statistics, logistics, com-
munications, and computers. Extramural
support runs about $5 million yearly.
With respect to those fields of endeavor
that are more characteristically the engi-
neering sciences, the scope of the programs
and the broad objectives are as follows:
Mechanics: The objective of the research
program in mechanics is the systematic ad-
vancement of engineering knowledge and
principles bearing directly upon design eri-
VoL. 49, No. 3
teria for the development of new weapons
systems and components. Studies on the fol-
lowing are included in the present program:
the dynamics of gases, liquids and solids;
aerodynamic problems; problems involving
structural design, strength of solids, hydro-
mechanics, propulsion, heat and mass trans-
fer, soil mechanics; and problems involving
the development and synthesis of mecha-
nisms. Extramural support runs about $25
million yearly.
Materials: The objective of the research
program is the systematic advancement of
knowledge on the fundamental properties
and behavior of materials to provide the
best possible selection for designers and
fabricators of military weapons and equip-
ments. The present program includes studies
on metals, minerals, ceramics, elastomers,
adhesives, transparent materials, organic
structural materials, fibers and fibrous ma-
terials, insulating materials, and dielectric
and magnetic materials. Extramural sup-
port runs about $27 million yearly.
Combustion: The objective of the re-
search program in the field of combustion
is to gain an increased understanding of the
total process of transforming the chemical
energy of reactants into thermal and kinetic
energy of reaction products, so the design
of military propulsion devices can be put
on an increasingly rational basis. The pres-
ent program includes investigations of basic
phenomena in selected areas of physics,
chemistry, fluid mechanics, thermochemis-
try, and thermodynamics; and also funda-
mental investigations of processes that are
interrelated combinations of these phenom-
ena. Extramural support runs about $6 mil-
lion yearly.
Electronics: The objective of the research
program in electronics is to ensure maxi-
mum extension and acceleration of all our
senses for military purposes. The present
program includes acoustics and underwater
sound; antenna theory, electromagnetic
propagation and reflection; communica-
tions, data handling, and information the-
ory; electronic instrumentation and
standards; electronic countermeasures and
counter-countermeasures; IFF theory; in-
frared; navigation; radar; electronic tubes,
parts, and semiconductors; and electron and
Marcu 1959 EXTRAMURAL SCIENCE PROGRAMS OF THE DEPARTMENT OF DEFENSE Me
ion plasma. Extramural support runs about
$43 million yearly.
In the geophysical sciences the objective
is the advancement through systematic and
exploratory research of those selected as-
pects which will increase the capability of
the military to utilize, predict, and control
the natural environment. Included in the
present program are meteorology, climatol-
ogy, oceanography, marine geology, geo-
chemistry, cartography, geodesy, geog-
raphy, astronomy, astrophysics, magnetism,
and gravity studies. Extramural support
runs about $19 million yearly.
Turning now to the broad category of life
sciences, the DOD supports major programs
in the medical sciences and in biology. The
scope and the objectives are:
In the medical sciences, to provide sup-
port of the mission of military medicine by
studies in—
(a) Preventive medicine: research on
methods of physical examination and health
surveillance, promotion of physical fitness,
preventive dentistry; nutrition, environ-
mental physiology and pathology, disease
and injury prevention, toxicology; protec-
tion against radiation and blast, the effects
of chemical and biological agents, with
methods of casualty prevention; industrial
and public health studies.
(b) Studies relating to the medical prob-
lems of aviation, astronautics, submarine
and diving medicine, man in relation to the
machines of war in all media, terrain and
climates; and survival techniques.
(c) Improved methods of medical, surgi-
eal, dental and psychiatric care and re-
habilitation of the sick and injured.
The medical sciences program runs about
$24 million yearly, of which about $15 mil-
lion is the extramural effort.
In the biological sciences the objective is
the systematic development of this field in
areas of military interest. The present pro-
gram includes hydrobiology, biogeography,
ecology, the biomechanism of complex data
reception and control in living systems, bac-
terial fungal, viral genetics and nutrition,
the ecology of disease vectors, the mecha-
nism of infection, and the survival of micro-
organisms. Extramural support runs about
$7 million yearly.
As to the psychological and social sci-
ences, the support level is about $21 million,
of which $15 million is the extramural effort.
Program content and the objectives are:
the advancement through systematic and
exploratory research of those selected as-
pects of pure and applied psychological and
social sciences which contribute to an in-
crease in the military capability. The pres-
ent program includes studies leading to new
concepts, techniques, devices, and principles
applicable to the solution of military prob-
lems, including military manpower needs
and the availability, selection, classification,
assignment and proficiency measurement of
personnel; education; training and training
devices; motivation; morale; leadership;
human organization; human engineering;
psychological and unconventional warfare;
intelligence operations; and civil affairs and
military government.
Finally, coming to operations research as
a field of scientific activity in its own right,
the objective is to provide quantitative
bases for executive decisions on military
and related scientific matters. The present
program includes contracts totaling about
$28 million in support of work with RAND,
the Operations Research Office, the Opera-
tions Evaluation Group, the Combat Opera-
tions Research Group, the Institute for De-
fense Analyses, the Human _ Resources
Research Office, the Naval Warfare Analy-
sis Group, and the Naval Warfare Research
Center.
In total, these scientific research pro-
grams comprise a fiscal year 1959 Defense
effort amounting to about $391 million, pro-
viding about $137 million to the conduct of
intramural effort and $254 million to the
support of extramural science activities.
DEPARTMENT OF DEFENSE POLICY ON
BASIC RESEARCH
Let us turn now to objectives stated even
more broadly. About a year ago Secretary
McElroy issued a strong policy directive
setting forth the principles governing the
support of a Department-wide basic re-
search program, conceived and anchored
in imaginative long-term planning and
long-term funding. This policy recognizes
that “the needs of national defense are
74 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
uniquely characterized by pressing demands
for new facts and knowledge very close to
the frontiers of science” in order to protect
the security of the United States and its
vast Defense investment against both tech-
nological surprise and obsolescence. It em-
phasizes also that the costs of basic research
are small in proportion to the potential mili-
tary strength to which basic research is ca-
pable of contributing and that “sustained
support of basic research offers one of the
most promising opportunities for effecting
long-range economies in other aspects of the
military program.”
Specifically, the directive states:
A. It is the policy of the Department of De-
fense:
1. To support a broad and continuing basic
research program to assure the flow of the
fundamental knowledge needed by the
military departments as prime users of
scientific facts and to evolve novel weap-
ons of war; and
2. To maintain, through such a broad sup-
port program, an effective contact between
the military departments and the scien-
tists of the country so that the military
departments are continuously and grow-
ingly aware of new scientific developments
and the scientists are aware of the mili-
tary needs.
B. It is further the policy of the Department of
Defense to coordinate its basic research pro-
gram with the National Science Foundation
and to encourage the support of sound basic
research programs by government and pri-
vate agencies, recognizing that these pro-
grams are essential to the full development,
utilization and growth of the nation’s scien-
tific resources and, hence, to national defense.
Within the guidance of this policy, the
Department of Defense substantially in-
creased fiscal year 1958 funding for some
research programs judged critical for the
improvement of military weaponry. The
increased funding for each field was: $31.6
million for the physical, medical, and geo-
physical sciences; $10 million for materials
research; and $12.5 million for the vital
areas of electron tubes and electronic parts.
$30 million of these funds went to the sup-
port of basic and supporting research pro-
grams at academic institutions. The main
VOL. 49, NO. 3
effect was to restore research to the level
from which it had sagged over the past sev-
eral years owing to inflation and the in-
creased costs of modern instrumentation. In
addition to the above funds, $12 million was
made available to the Army and Air Force
in June of this year for the explicit purpose
of financing certain contractual research
programs for periods longer than the an-
nual program increment or to provide for
program longevity.
NEW GRANTS AUTHORITY UNDER PUBLIC
LAW 85-934
The recent session of Congress saw the
passage of Public Law 85-934, an act to au-
thorize the expenditure of funds through
grants for the support of scientific research.
Heretofore the Department of Defense has
been limited to the use of a research con-
tract in engaging the services of an educa-
tional or other nonprofit organization. The
Grants Act provides the authority to make
grants to such institutions or organizations
for the support of basic scientific research,
where such action is deemed to be in fur-
therance of the objectives of the agency; it
also grants discretionary authority to vest
title of research equipment in the organiza-
tion carrying out such research. Increased
flexibility will accordingly result from this
authority in Defense support of basic sci-
entific research. A directive is presently be-
ing drafted in the Department of Defense
to establish a uniform policy among all
military agencies in the awarding and ad-
ministration of research grants and the
transfer of title to research equipment ac-
quired under such grants.
This, I believe, covers the highlights of
Defense science programs and our broad
objectives in their support, the program
content and technical objectives of our sci-
entific effort in some discrete fields, and
certain aspects of Defense policies designed
to be constructive, forward-looking, and to
lend stimulation and sustenance to science
from the Defense end of the Federal Goy-
ernment.
Marcu 1959 EXTRAMURAL PROGRAMS OF THE NATIONAL INSTITUTES OF HEALTH
~I
Or
Extramural Science Programs of the National Institutes of Health
By C. J. VAN SLYKE, Deputy Director, National Institutes of Health; Assistant
Surgeon General, Public Health Service, U. S. Department of
Health, Education, and Welfare
It is a pleasure to appear in this sympo-
sium on the extramural science programs of
the Federal Government.
The program chairman has asked that I
cover briefly the objectives and nature of
the National Institutes of Health with re-
spect to our extramural activities, leaving
time for questions and discussion. What I
shall present, therefore, is a thumbnail
sketch of the NIH grants and awards pro-
grams.
I shall not attempt to include the NIH
intramural program—its conduct of re-
search—nor all the extramural programs of
the U. S. Public Health Service, of which
the NIH constitutes the principal research
branch. Nor will this outline cover extra-
mural scientific activities of other compo-
nents of the Department of Health, Educa-
tion, and Welfare, in which the Public
Health Service is a part.
Now to turn to the NIH extramural pro-
gram. The objective of the National Insti-
tutes of Health and of the Public Health
Service is contained in the public laws which
form our enabling legislation and which im-
pose upon us grave obligations and duties.
The purpose of all our activities is stated,
in simplest terms, in public law as being “to
improve the health of the people of the
United States.”
The methods for achieving this objective
are, again in the shortest words, the conduct
and support of research and training and
aid in the application of knowledge.
In the legislation upon general duties,
there is a charge to “conduct in the (Public
Health) Service, and encourage, cooperate
with, and render assistance to other appro-
priate public authorities, scientific institu-
tions, and scientists in the conduct of, and
promote the coordination of, research, in-
vestigations, experiments, demonstrations,
and studies relating to the causes, diagnosis,
treatment, control, and prevention of phys-
ical and mental diseases and impairments
Ole maeinaeers
In legislation establishing the Institutes
which compose the NIH, such as the NHI,
NCI, and so on, there are mandates direct-
ing the conduct and support of research and
training and other activities aimed at the
acquisition and application of knowledge
concerning cancer and heart disease and
other “categorical” disease fields.
Additionally, through the Health Re-
search Facilities Act of 1956, there is pro-
vided a program of support for the construc-
tion of research facilities in the sciences
related to health.
NATURE OF THE PROGRAM
These, then, are the objective and the
methods of NIH extramural activities in
general, legislative terms. What has been
built upon this framework, what is it for,
how does it operate, what are its character-
istics, what is it accomplishing, what is its
future? These and other broad questions
occur, and the answers, though they be
partial, will portray the nature of our grants
and awards programs.
To begin the answers upon a historical
note, I was privileged to author a paper,
upon the real beginning of the NIH extra-
mural program, in the issue of Science for
Friday, December 13, 1946. The day and
the date have turned out to be more aus-
picious than the general belief holds about
enterprises connected with Friday the thir-
teenth. The paper began with these words:
A large-scale, nationwide, peacetime program of
support for scientific research in medical and re-
lated fields, guided by more than 250 leading sci-
entists in 21 principal areas of medical research,
is now a functioning reality. The program, based
on U.S. Public Health Service Research Grants
financed by public funds, supports research—con-
ducted without governmental control—by inde-
pendent scientists. The purpose of these grants is
to stimulate research in medical and allied fields
76 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
by making available funds for such research and
by actively encouraging scientific investigation of
specific problems on which scientists agree that
urgently needed information is lacking. Accom-
panying this purpose is complete acceptance of a
basic tenet of the philosophy upon which the
scientific method rests: The integrity and inde-
pendence of the research worker and his freedom
from control, direction, regimentation, and outside
interference.
The U. S. Public Health Service Research
Grants, in operation as a medical research program
of scientists and by scientists, may have early and
profound effects upon the course of medical history
and the national health.
The program, both in principle and as admin-
istered, has been welcomed and approved whole-
heartedly by leaders in medical research.
ORGANIZATIONS OF ACTIVITIES
The organization, programming, and ap-
propriations responsibilities of the NIH ex-
tramural activities today fall into the fol-
lowing categorical Institutes and Divisions:
National Cancer Institute, National
Heart Institute, National Institute of Al-
lergy and Infectious Diseases, National In-
stitute of Arthritis and Metabolic Diseases,
National Institute of Dental Research, Na-
tional Institute of Mental Health, National
Institute of Neurological Diseases and
Blindness, Division of General Medical Sci-
ences, Division of Hospital and Medical
Facilities, Division of Nursing Resources,
Division of Sanitary Engineering Services,
and Division of Special Health Services.
Noneategorical or general research and
training grant funds are available from the
Division of General Medical Sciences for
scientists whose interest do not fall within
the scope of responsibility of the categorical
Institutes and Divisions. The Division of
Research Grants of the National Institutes
of Health has administrative responsibility
for the management of the research grants
programs, and for the Health Research Fa-
cilities construction grants.
NATIONAL ADVISORY COUNCILS
By Federal law, nine National Advisory
Councils have been established as advisers
to the Public Health Service. No research
or training grant may be paid by the Sur-
geon General unless recommended for ap-
proval by one of these Councils. Seven of
the Councils advise the seven so-called cat-
VoL. 49, NO. 3
egorical Institutes on their respective pro-
grams, in addition to reviewing and recom-
mending appropriate action on applications
for grant support. The National Advisory
Health Council reviews applications for
general or noncategorical research grants
and advises the Surgeon General on matters
relating to health activities and functions of
the Service. The Federal Hospital Council
advises the Surgeon General on matters re-
lating to the Administration of the Hospital
Survey and Constructions Program and re-
views applications for grants in aid of proj-
ects in research, experiments, or demonstra-
tions relating to the development utilization,
and coordination of hospital services, fa-
cilities, and resources.
The National Advisory Council on Health
Research Facilities, established in July
1956, reviews and recommends appropriate
action on applications submitted by uni-
versities or other nonprofit institutions for
assistance in the construction and/or equip-
ping of additional facilities for the conduct
of research in the sciences relating to health.
The Federal share can not exceed 50 percent
of the total cost of building of research
space.
SCIENTIFIC STUDY SECTIONS
In view of the large number of applica-
tions which must be evaluated, and the need
for skilled scientific review covering the
entire range of medical and biological re-
search, more than 30 Study Sections of spe-
cial nonfederal consultants expert in various
fields of research have been established.
These study sections act as technical ad-
visers to the National Advisory Councils
and to the Surgeon General. They accept
responsibility not only for providing tech-
nical advice on applications for research
support but also in conjunction with the
Councils, for surveying as scientific leaders
the status of research in their particular
fields in order to determine areas in which
additional activity should be initiated or
expanded.
TYPES OF EXTRAMURAL ACTIVITIES
The grants and awards of NIH are com-
prised in four main categories: (1) research
grants, (2) research fellowships, (3) train-
Marcu 1959 EXTRAMURAL PROGRAMS OF THE NATIONAL INSTITUTES OF HEALTH Li
ing grants and traineeships, and (4) health
research facilities grants. I shall discuss
each in a highly summary fashion, sketching
their general functions.
1. Research Grants
These grants are made to universities,
medical schools, hospitals, laboratories, and
other public or private institutions and to
individuals for support of research in health,
medicine, and allied fields. The major ob-
jectives are: to expand medical and bi-
ological research in scientific institutions
throughout the country; to stimulate new
investigations in fields needing exploration;
and to provide, incidentally, on-the-job
training for scientific personnel in connec-
tion with the research being conducted. The
funds provide for salaries, equipment, sup-
plies, travel, overhead, and certain other ex-
penses.
Research grants are financed from ap-
propriations made to each of the seven In-
stitutes concerned with “categorical” dis-
ease fields and from an appropriation to the
NIH (for general research and services) to
support needed research lying outside the
“categorical” disease fields.
Grants are made on a yearly basis. How-
ever, continuity and stability, both for the
work and the man, are of paramount im-
portance and have been so considered since
the beginning of the program. Therefore, the
duration of the investigation is a vital con-
sideration of the Study Sections and Ad-
visory Councils in their decisions regarding
recommendations for action. These bodies
have consistently provided for continuity
and have indicated to grantees continued
favorable action as long as congress ap-
propriates necessary funds. The Congress
has recognized the importance of these
moral commitments and has sustained them
in principle and practice.
That we have steadily progressed toward
greater stability is shown in the fact that,
early in the life of the program, the average
duration of a grant was about two years.
Today, the average duration is some five
years, and many meritorious investigators
have received support since 1946.
Research under the program is conducted
by the investigator with full independence
and autonomy. Support of research through
the use of research grants does not imply
in any way any degree of Federal control,
supervision, or direction of the research
studies. Although the investigator submits
a proposal in his application, he is free to
pursue the project in any manner he deems
most promising. The autonomy of the in-
dividual researcher implied in this philoso-
phy does not, however, exclude self-imposed
guidance entailed in the over-all plan of an
organized, cooperative research project in
which several groups of investigators may
collaborate.
In order not to divert the time of the re-
searcher unnecessarily from the actual con-
duct of the research, he is requested to sub-
mit only informal annual progress reports,
and their distribution is limited to the re-
viewing consultants.
Neither these advisers nor those who ad-
minister the program in the NIH review
grantee papers proposed for publication.
Grantees, fellows, and trainees may publish
results of any work supported by grant or
award when and where they wish, and re-
sponsibility for direction of the work is
never and should never be ascribed to the
NIH, Public Health Service. This does not
indicate any lack of interest in the results
of research projects, but is aimed solely at
avoiding any degree of governmental re-
striction. Grantees are requested, however,
to provide 10 copies of reprints after papers
have been published. It is also requested
that published papers carry footnote ac-
knowledgment of the financial assistance
through the grant.
The research grants program has grown
steadily. While financial figures are far from
being the only factor which shows growth,
they are at least easily apparent. In fiscal
year 1949, some 10.8 million dollars was ap-
propriated for the purpose; in fiscal year
1959 the appropriation for research grants
is 141.5 million dollars. This year there will
be some 7,000 or more research grants
awards, so dispersed geographically that
every corner of the country where there is
real research potential will be reached and
the nation will be aided with this support.
Some 5,000 or so professional papers will be
published by these grantees in a wide range
78 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
of journals, and it is these fruits of the work
that best testify to the quality of the en-
deavors supported.
This is research in the public interest and
in which the public is vitally interested for,
as we all know, medical research is a sub-
ject which the public eagerly devours when
presented through the media of public com-
munication. Since studies done with research
erants are supported with public funds,
there is no desire on the part of NIH to as-
sume credit for this work; credit belongs to
the investigator and his institution and to
the people who, through their Congress and
Administration, make possible today so
much more medical research than used to be
conducted. Therefore, it is of public interest
to say that, year by year, many of the
medical research findings hailed in the press
and among the professions have received
NIH grant support. The quality of the pro-
gram and the quality of the judgment ex-
ercised by the Study Sections and Councils
is reflected, for example, in the fact that a
total of 27 Nobelists in medicine and phys-
iology have been recipients of NIH-PHS
grant support, including this year’s winners.
2. Research Fellowships
Research fellowships are intended to in-
crease the number of scientists qualified to
carry on independent research. Seven types
of fellowships are presently available:
(1) Predoctoral research fellowships are
awarded to students with a bachelor’s de-
gree or equivalent, for the pursuit of grad-
uate research training in the fields related
to the health sciences. Stipend rates are
$1,600, $1,800, and $2,000 for the first, sec-
ond, and third years, respectively. Allow-
ances for dependents, travel, and tuition are
added to the stipend.
(2) Postdoctoral research fellowships are
awarded to qualified persons holding a Doc-
tor’s degree in medicine, dentistry, or re-
lated fields. Stipend rates are $3,800, $4,200,
and $4,600 for the first, second, and third
years, respectively. Allowances for depend-
ents, tuition, and travel are added to the
stipend.
(3) Special research fellowships are
awarded to qualified candidates who have
demonstrated unusual competence in re-
VOL. 49, No. 3
search or who require specialized research
training. The stipend, including necessary
allowances, is determined at the time of the
award.
(4) Student part-time research fellow-
ship grants are awarded to schools of med-
icine, dentistry, nursing, and public health.
The awards are designed to give students in
the health sciences an opportunity to ex-
plore the research field in the hope that
many of those supported will enter into full
or part-time research careers. Units of $600
are provided for part-time research work
during the school term, or for full-time re-
search work for two months during any time
when curriculum work is not scheduled for
the student.
(5) Senor research fellowship grants are
awarded to schools of medicine, dentistry,
and public health in support of competent
scientists who wish to conduct research and
teaching in the preclinical sciences. These
fellowships provide support between the
completion of postdoctoral training and the
time of eligibility for appointment to per-
manent or higher academic posts. The
awards are made for 5-year periods, are re-
newable, and provide for salary, plus partial
research expenses not exceeding $2,000. Sen-
ior Research Fellows may also apply for ad-
ditional support for their research needs.
(6) Post-sophomore research fellowship
grants are awarded to schools of medicine
and dentistry for support of students who
wish to obtain research training prior to
completion of their professional degrees.
Participants must be willing to drop out of
regular courses for one, two, or three years.
The stipend is set by the school in amounts
not to exceed $3,200 annually. Allowances
for dependents and tuition are added to the
stipend.
(7) Foreign research fellowships are
awarded to a limited number of scientists
who wish to study in United States lab-
oratories. The purpose of the program is to
provide an opportunity to strengthen med-
ical research by mutual exchange of re-
search methods, scientific philosophy, and
cultural values. Nominations will be made
by respective National Research Organiza-
tions in each Western European country.
Candidates must have (a) completed a doc-
Marcu 1959 EXTRAMURAL PROGRAMS OF THE NATIONAL INSTITUTES OF HEALTH 79
toral degree in one of the medical or related
sciences, and demonstrated proficiency in
research, (b) made satisfactory arrange-
ments with the laboratory in the United
States where training will be obtained, and
(c) acquired a workable reading and speak-
ing knowledge of the English language.
Scientists will be brought to the United
States on an exchange-visitor’s visa, which
requires return to the homeland for a period
of at least two years at the end of the train-
ing period. Stipends are $3,800 for the first
year and $4,100 for the second year. De-
pendency, travel and certain other allow-
ances are added to the stipend.
In fiscal year 1957, over 2,000 research
fellowships were provided in a total amount
of $5,300,000.
3. Training Grants and Traineeships
Training grants are intended to augment
the nation’s supply of qualified scientific
investigators by assisting in the establish-
ment, expansion, and improvement of train-
ing and instructional programs in univer-
sities and other institutions. Aid to the
institution is provided by grants in two
general classes—undergraduate and grad-
uate.
Traineeships to individuals may be
awarded either through one of the graduate
training grants or directly to the individual
in training. Traineeships are intended to in-
crease the number of qualified investigators
by encouraging advanced training in spe-
cialized areas of medical and related re-
search, as well as in the fields of public
health and nursing. Stipend rates vary ac-
cording to the nature and requirements of
the different fields covered.
(1) Undergraduate training grants are
awarded to schools of medicine, dentistry,
nursing, and public health to assist in de-
veloping expanded and better integrated
undergraduate instruction relating to the
prevention, diagnosis, and treatment of can-
cer, mental illness, and cardiovascular dis-
eases. It is the responsibility of the institu-
tion to determine the most appropriate use
of the funds.
(2) Graduate training grants are awarded
to public and private nonprofit institutions
interested in providing special training for
researchers, teachers, and prospective prac-
titioners interested in public service. Funds
may be used to improve facilities and to
provide salaries for faculty and staff, sti-
pends for trainees, and necessary supplies
and materials.
In fiscal year 1957, over 1,100 training
erants were made in a total amount of
$25,000,000. Approximately 1,950 trainees
were supported under these grants. In ad-
dition, 405 direct traineeships in a total
amount of $1,857,000 were made.
4. Health Research Facilities Grants
Under the Health Research Facilities Act
of 1956, the Congress authorized the estab-
lishment of a program to assist in the con-
struction of additional facilities for the con-
duct of research in the sciences relating to
health. The program provides grants in aid
on a matching basis to public and private
nonprofit institutions. The amount of Fed-
eral funds awarded may not exceed 50 per-
cent of the total costs of the research portion
of the facility, and the remaining sum must
be provided from non-Federal sources. The
sum of $30,000,000 has been appropriated
yearly for this program since its inception
and to date, and meritorious applications
submitted to the National Advisory Council
on Health Research Facilities have re-
quested funds far in excess of the appropria-
tions, even though the applicants must, as
indicated, match the Federal dollars. Sev-
eral hundred awards have been made to in-
stitutions in all parts of the country under
this program, and already new research fa-
cilities are in operation that would not
otherwise have been made possible.
Here it is well to point out that the pro-
grams described above, for research, for
training, and for facilities, supplement and
complement each other—and help achieve
the balance that always must be sought be-
tween these necessary components of re-
search: funds for skilled investigators to
do research with, facilities in which to work,
and training to develop scientific manpower
to do research.
In the above, I have portrayed most of
the major components of the NIH extra-
mural program. I should mention that I
have not included a relatively new area for
80 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
us, that of contract research, because it is
in developmental stages and is concerned
largely only with the specialized area of
cancer chemotherapy. Many of you, of
course, know the program of our National
Cancer Institute’s National Cancer Chemo-
therapy Service Center. Through this Cen-
ter a large endeavor is underway, employing
contract work as one of the mechanisms, to
screen many, many thousands of compounds
for possible anticancer effects and to de-
velop, ultimately and hopefully, chemother-
apeutic agents useful against human can-
cers.
The future is bright for not only this but
also the other extramural programs which I
have discussed, in the opinion of the more
than one thousand representatives of Amer-
ica’s scientific community who advise upon
and guide these programs. This summer a
final report was issued by a group of con-
sultants to the Secretary of the Department
of Health, Education, and Welfare who had
been appointed to study and advise upon
the advancement of medical research and
education through programs of the Depart-
ment. This group, known as the Bayne-
Jones Committee since it was chaired by
Dr. Stanhope Bayne-Jones, foresaw and
recommended a future of strong growth
and development for medical and related
research and medical education.
VoL. 49, NO. 3
In the final analysis, of course, the con-
tinued success of the NIH program, as one
of the partners in the nation’s medical re-
search enterprise, rests upon the human and
economic benefits that accrue from pro-
ductive scientific investigation. That the
past decade has seen many such benefits, in
terms of new drugs and other therapies, for
example, is well known.
In the paper to which I referred earlier,
presented in 1946, these thoughts were ex-
pressed:
The great benefits from all medical research,
wherever conducted, are received by the millions
of people whose lives are made healthier, happier,
and longer through widespread application of
knowledge gained in research larboratories. Con-
versely, research not conducted for want of funds
is very costly to the same millions. The essence
of these facts, as related to the Research Grants
program, has been stated by the National Advisory
Health Council: “There are few purposes for which
public funds could be used more appropriately
than to discover ways to prevent and cure illness
and to prolong useful years of life.” The function
of the Research Grants is to make it possible for
workers in medical and allied sciences to expedite,
extend, and intensify health-saving and life-saving
research.
The function of the whole extramural
program of NIH, comprising today 80 per-
cent of this year’s total of $324.4 million
in public funds, remains essentially the same
in 1958 as in 1946.
Marcu 1959
EXTRAMURAL SCIENCE PROGRAMS OF THE U. S. D. A. 81
Extramural Science Programs of the United States
Department of Agriculture
By Byron T. SHaw, Administrator, Agricultural Research Service
Some of the other representatives on this
panel may contradict me, but I believe that
the Department of Agriculture administers
the oldest extramural science program in
the Federal Government. We have actually
had such a program since 1887. But before
discussing our extramural research, I want
to say a few words—by way of background
—about our intramural or regular research
program.
As you know, the Department has the
responsibility in the Federal Government
for agricultural research. This responsibility
goes back to 1862, when the Department
was established “to acquire and diffuse use-
ful information on subjects connected with
agriculture in the most general and compre-
hensive sense of the word.” Beginning in a
small way, and expanding as the needs of
agriculture and the Nation increased, the
Department’s research program today cov-
ers all phases of production, marketing, and
utilization of agricultural products. It uti-
lizes all the life sciences, nearly all the phys-
ical sciences, and to an increasing extent
the social sciences as well.
Our intramural science program is a dis-
persed cooperative endeavor, involving
some 10,000 employees and an appropri-
ation of approximately $90 million. We
have research locations in every State, rang-
ing in number from 1 to 28 and in size from
small 1-man field stations to the large re-
gional utilization laboratories and the Re-
search Center at Beltsville, Md. We are
also doing a limited amount of regular re-
search in other countries—in Latin America,
Europe, and Africa.
About 90 percent of our research is co-
operative with other public and private
organizations—including Federal and State
agencies, private research institutions, and
farmer and industry groups. More than half
of the work is in cooperation with State
agricultural experiment stations.
Through the years, the States have also
provided increasing support for agricultural
science. At the present time State agricul-
tural experiment stations are spending an
estimated $100 million of non-Fedreal funds
for State and regional research. In addition,
they are spending $311 million made avail-
able by Congress as Federal grants. These
Federal-grant funds are appropriated to the
Department for payment to the States and
constitute our oldest and largest extramural
science program.
The Federal-grant program had its origin
in the Hatch Act of 1887, which authorized
an annual Federal grant of $15,000 to each
State for the partial support of State agri-
cultural experiment stations. Additional acts
successively increased the amounts of these
payments, each act setting up its own for-
mula for distributing the funds. In 1955,
Congress consolidated these acts into one
statute, which now serves as the authority
for all Federal-grant payments to State
experiment stations.
Administration of these funds is delegated
by the Secretary to the Agricultural Re-
search Service, and we have a Deputy Ad-
ministrator for Experiment Stations—Dr.
EK. C. Elting—who is responsible for this
activity. Dr. Elting and a small scientific
staff prescribe standards for Federal-grant
research, approve projects to be supported
by Federal-grant funds, and determine that
the funds are spent in accordance with the
purposes intended by Congress.
Each State experiment station director
develops his own State research program in
terms of State and Federal resources avail-
able to him. He submits to the ARS well-
defined projects for which he proposes Fed-
eral-grant support. Projects that are
approved then become an integral part of
the State program and may or may not be
carried out in cooperation with the Depart-
ment. Publication of results and any patent-
able materials that may develop in Federal-
erant research are entirely the property of
82 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
the State experiment station and are not
subject to Federal printing or patent regu-
lations. Close to 6,000 State experiment
station projects are currently being sup-
ported entirely or in part by Federal-grant
funds.
The department’s role in the Federal-
erant research program is primarily one
of service. Although we must assure that
certain legal requirements are met, a far
more important responsibility is the techni-
cal assistance we’re called on to give. This
assistance includes comprehensive reviews
of Federal-grant research, participation in
planning of regional research, and coordina-
tion of research effort among the States as
well as between the States and the Depart-
ment. This broad review and coordinating
service helps all of us to avoid duplication
of effort, to recognize gaps that need to be
filled, and to plan and carry out a more ef-
fective Federal-State program of agricul-
tural research.
Our second extramural science program
was initiated about 10 years ago under the
Research and Marketing Act of 1946. This
act for the first time gave us authority to
contract for research outside the Depart-
ment, when such work can be done more
rapidly, more effectively, or at less cost
than it can be done within the Department.
Originally, this contracting authority ap-
plied only to utilization and marketing
research, but in 1954 it was broadened to
include all phases of Department research.
At the present time, we have approximately
200 research contracts in force, totaling
close to $4 million, and divided roughly
fifty-fifty, in terms of public and private
organizations doing the work.
I mentioned that in Federal-grant re-
search, the States make most of the deci-
sions. In contrast, we make most of the
decisions in our contract research program.
We determine what research needs to be
done, what will be done, and, by mutual
agreement with the contractor, how it will
be done. In each case, we negotiate as to
terms, conditions, length of time, and cost
of the research to be undertaken. Research
results must be published in a manner ap-
proved by the Department, and any patent-
VoL. 49, No. 3
able materials developed are assigned to the
Secretary of Agriculture for public use.
Although, in a few cases, we have con-
tracts involving basic research, it is ex-
tremely difficult—because of the very na-
ture of basic research—to negotiate this
type of contract. And we were pleased when
the recent Congress, recognizing this prob-
lem, gave the Department authority, for the
first time, to make discretionary grants for
basic research. No special money has been
appropriated for such grants, however, and
our present funds are all obligated. But we
hope, through future adjustments in our
program, to make funds available for this
purpose.
We are convinced that through both con-
tracts and grants, we can help to obtain
more efficient use of our Nation’s scientific
manpower and facilities and thus make
faster progress in agricultural research.
The same kind of thinking is the basis
of our third extramural science program,
which has been initiated during the past
year. This time we are undertaking—also
through contract and grant arrangements—
a rather extensive program of research by
foreign scientists in foreign scientific insti-
tutions. Authority and funds for this work
come from the Agricultural Trade Develop-
ment and Assistance Act of 1954generally
called public Law 480. As you know, under
this Act, our Government sells surplus agri-
cultural commodities to foreign countries
and receives payment in foreign currencies.
It is these currencies that we are using for
our overseas research. The Act originally
limited use of these funds to research that
would extend our markets for agricultural
commodities. Last spring, Congress added a
new authority, and we can now use Public
Law 480 funds for all phases of agricultural
research.
We expect to obligate something like $10
million (in foreign currency equivalent)
during this fiscal year, to be spent over a
period of 5 years. These obligated funds
represent money now available, and they
will cover the entire cost of grants and con-
tracts negotiated. This is to assure that we
will have enough money to complete any
overseas research jobs that we start.
Marcu 1959
The program is being developed by three
survey teams, who are visiting the various
countries to evaluate the potential of their
scientists and facilities and to determine the
willingness of their governments to sanction
the research. One team is working in Europe
and the Middle East, the second in the Far
Hast, and the third will be in Central and
South America after the first of the year.
Several grants have already been exe-
cuted for work in the United Kingdom and
Israel, and we are well along with our ne-
gotiations in France, Italy, Spain, and Fin-
land. Other countries—including Poland,
Yugoslavia, Pakistan, Indonesia, India, and
Chile—are in the survey stage. And still
others will probably become eligible for
participation, as additional sales of surplus
products are made and additional foreign
currencies become available.
Both basic and applied research, as well
as developmental work, will be included in
this foreign program. All basic studies will
be done through grants, and all develop-
mental work will be carried out under con-
tract. Both grants and contracts will be used
for applied research; each proposed project
will be considered on its own merits.
Although no hard and fast rule has been
established, we expect to concentrate the
basic research in Europe, because European
scientists are especially noted for their con-
tributions in this area of research. The ap-
plied and developmental work will be done
in all the countries participating in the pro-
gram.
We know there is a vast reservoir of
scientific manpower in the free world. And
we believe, through the P. L. 480 program,
that we can help to make more effective use
of this manpower—to our own benefit as
well as that of the countries concerned.
I want to stress that this foreign research
is supplementary to our own domestic pro-
gram. We are looking for institutions having
scientific personnel with specialized experi-
ence and facilities that will enable them to
carry out needed research more rapidly or
more effectively than can now be done here
in the United States.
EXTRAMURAL SCIENCE PROGRAMS OF THE U. S. D. A. 83
In the utilization, marketing, and home
economics research, we hope to develop
new uses and new markets for agricultural
products, both in the United States and in
the country concerned. These studies will
include quality evaluation of farm commod-
ities, biochemical changes that occur in ma-
turing fruits and vegetables, market disease
and insect problems, and consumer habits
and preferences in foreign countries.
In the farm and forestry studies, we will
give special attention to foreign diseases,
insects, and other pests that constitute po-
tential threats to American agriculture. We
also want to study the genetic traits of for-
eign livestock breeds, potential new crop
plants under native conditions, and old-
world soils, which may help us find out how
to halt soil deterioration in this country.
Results of this overseas research will be
made available to the United States public
in the same way results of our domestic
research are made available. And we reserve
the right to publish results in other coun-
tries, including the country where the work
is done, if the contractor fails to do so. All
patentable materials will be assigned to the
Secretary of Agriculture for United States
use anywhere in the world. Rights to the use
of such patents in other countries will of
course be in accordance with the patent
policies of those countries.
Needless to say, we are quite optimistic
about this new world-wide resource for agri-
cultural research. We believe it has great
potentials for helping us solve some of our
important farm problems.
Taken all together, our extramural sci-
ence programs—aincluding Federal grants to
the States and the domestic and foreign
contract-and-grant programs—constitute a
powerful supplement to the Department’s
research effort. They not only represent ad-
ditional manpower and facilities for getting
ahead faster—they also promote better un-
derstanding and closer cooperation among
all groups working to advance agriculture.
And I am convinced that where we have un-
derstanding and cooperation, we have an
environment for outstanding progress.
84 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 3
Extramural Science Programs of the Atomic Energy Commission
By Cuarues L. Dunnam, Director, Division of Biology and
Medicine, U. S. Atomic Energy Commission
The Atomic Energy Commission has well-
defined responsibilities for the conduct of
scientific research and development pro-
erams. Its science programs with the nota-
ble exception of its Health and Safety Lab-
oratory in New York City are almost
exclusively accomplished by contract and
so contain practically no intramural activi-
ties in the usual sense of the word. Its na-
tional laboratories, such as the Oak Ridge
National Laboratory, the Brookhaven Na-
tional Laboratory, and the Argonne Na-
tional Laboratory, and its other major re-
search and development facilities such as
Los Alamos Scientific Laboratory and the
Ernest O. Lawrence Radiation Laboratories
at Livermore and Berkeley, are largely
government-owned but contractor operated,
in fact, chiefly by universities or groups of
universities. Exceptions are the Oak Ridge
National Laboratory and the research and
development activities at the Hanford
Works which are under contract with in-
dustrial firms. I have assumed for purposes
of this symposium that my remarks should
be directed primarily toward that part of
our science program carried out in non-Goy-
ernment owned facilities, 1.e., our offsite re-
search program.
In order to get a proper picture of our
total effort, one must bear in mind that the
onsite and offsite aspects of our programs
are closely integrated. In general, work at
the major AEC laboratories 1s work especi-
ally appropriate to the unique facilities and
talents at hand. Interdisciplinary research
and research projects involving large col-
laborative efforts by many scientists have
proved especially effective in such an en-
vironment. This is not to say such projects
can not or should not be undertaken at uni-
versities. In fact the AEC does support this
type of work in its offsite programs where
the situation is favorable and we have not
hesitated to provide major items of equip-
ment, building modifications and the like to
universities and independent or private-
owned laboratories so as to further such
efforts.
Before sketching our program, and our
program interests, I should give you some
background.
The AEC emerged from the Manhattan
Engineering District with a total monopoly
in this country of nuclear-weapons research
and nuclear reactor research, practically all
of which was being conducted at Govern-
ment-owned but contractor-operated insti-
tutions. It also found itself supporting di-
rectly or in collaboration with the Office of
Naval Research a large share of the coun-
try’s nuclear physics and nuclear chemistry
research whether conducted at Government
facilities, universities, or independent labo-
ratories. In addition, it was supporting a
program of radiobiological research. Almost
all the latter was being conducted in Goy-
ernment-owned facilities. This was the situ-
ation at the time the Atomic Energy Act of
1946 was passed.
Section 1(a) of the Act concluded as fol-
lows: “Accordingly, it is hereby declared to
be the policy of the people of the United
States that, subject at all times to the para-
mount objective of assuring the common
defense and security, the development and
utilization of atomic energy shall, so far as
practicable, be directed toward improving
the public welfare, increasing the standard
of living, strengthening free competition in
private enterprise, and promoting world
peace.”
The Act went on in Section 1(b) to define
the purpose of the Act as follows:
Purpose of Act—It is the purpose of this Act to
effectuate the policies set out in Section 1(a) by
providing, among others, for the following major
programs relating to atomic energy.
(1) A program of assisting and fostering private
research and development to encourage maximum
scientific progress;
(2) A program for the control of scientific and
technical information which will permit the dis-
Marcu 1959
semination of such information to encourage scien-
tific progress, and for the sharing on a reciprocal
basis of information concerning the practical in-
dustrial application of atomic energy as soon as
effective and enforceable safeguards against its use
for destructive purposes can be devised;
(3) A program of federally conducted research
and development to assure the Government of ade-
quate scientific and technical accomplishment.
It then went on to say that the AEC was
established to accomplish these objectives.
In order to implement these parts of the Act,
recognizing that nuclear science and radio-
biology must advance as rapidly and as free
of security restrictions as possible under the
Act, the AEC developed its research pro-
gram in such a way as to encourage extra-
mural research activities at universities,
colleges and independent laboratories
throughout the country. In the first few
years of both its physical research and its
biomedical research programs the AEC
leaned heavily on the ONR through cooper-
ative arrangements with that agency for
rapid implementation of the program.
The reactor program continued for the
most part at AEC laboratories and at AEC
facilities operated by contracts with in-
dustry until the Atomic Energy Act of 1954
was passed which directed the AEC to re-
move from classification restrictions data
whose publication and dissemination would
not cause undue risk to the common defense
and security. The weapons development
program has continued almost exclusively
in AEC installations and on a classified ba-
sis to date.
Our physical-research program exclusive
of work on controlled thermonuclear reac-
tions has grown on the basis of annual oper-
ating cost from about $21,000,000 in 1948 to
about $89,000,000 in the current fiscal year.
Meanwhile over and above what was in-
herited from the MED the AEC has spent
for construction for physical research fa-
cilities more than $100,000,000, roughly
three-fourths of which was spent for major
research machines and associated housing,
a number of which were located on univer-
sity campuses. At present some $34,000,000
of the Division of Research’s $89,000,000
total annual operating funds go to support
work not conducted at AEC-owned major
research centers. Through all its activities
EXTRAMURAL SCIENCE PROGRAMS OF THE A. E. C. 85
whether concerned with onsite or offsite re-
search this Division shapes the programs in
such a way as to foster the development of
new talent for its future needs.
Work in basic physical research breaks
down into four major areas: physics and
mathematics, controlled thermonuclear re-
actions, commonly known as “Sherwood,”
chemistry, and metallurgy and materials.
In physics, the major effort centers
around attempts to learn all that can be
learned about the fundamental properties
of nuclear matter through research with
high energy particle accelerators as well as
through the use of high flux research reac-
tors and low energy accelerators. Although
the Nation’s two largest particle accelera-
tors are located at AEC laboratories, more
than one-third of the AEC funds support-
ing high-energy physics and nuclear struc-
ture research goes into offsite programs.
Mathematics research and research in the
field of computers are sponsored for what
they may contribute to advancing knowl-
edge and in the case of computers for what
these machines may contribute to a great
increase in research per scientific man-year.
Work performed under the _ so-called
Sherwood project is aimed at the develop-
ment of a controlled thermonuclear reaction
for the ultimate purpose of generating eco-
nomic power for industrial and civilian use.
This effort, currently costing between
$35,000,000 and $40,000,000 annually, is
limited by our present incomplete under-
standing of the fundamental properties of
plasmas. Hence more and more work is de-
voted to understanding cooperative phe-
nomena in a completely ionized gas. The
major costs in this program except for the
stellerator project at Princeton University
are incurred at AEC laboratories.
Chemistry research includes work de-
voted to such very practical problems as
solvent extraction and ion-exchange tech-
niques, analytical techniques for process
control and methods for producing usable
amounts of rare earth salts, pure metallic
uranium, thorium, zirconium, hafnium, ni-
obium, tantalum, and the like as well as
transuranic elements, all of interest to the
atomic-energy program. Geochemical and
geophysical research is supported princi-
86 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
pally at universities and the U. 8S. Geologi-
cal Survey. Fundamental research in the
program category “Chemical properties and
reactions,” with considerable emphasis on
the nuclear and chemical properties of the
heavy elements, takes place under heavy
AEC support at universities, as well as at
the AEC laboratories.
Finally, our physical research program
includes heavy emphasis on metallurgy and
materials. Research in this area falls into
the categories of production, treatment, and
properties of metals, alloy theory, and ir-
radiation effects.
The science program of the Division of
Reactor Development includes research and
development activities categorized under
AEC’s civilian power and supporting pro-
grams and costing this fiscal year about
$162,000,000. These activities are directed
towards development of nuclear reactors
for economic, electrical power, space heat,
gasification of coal, polymerization proc-
esses, and for the propulsion of merchant
vessels. This Division also administers the
military reactor program which includes
nuclear propulsion units for submarines,
surface vessels, aircraft and rockets as well
as package power units for military instal-
lations.
The civilian power program is for the
most part carried out at AEC installations
and at industrial establishments with some
university and independent laboratory par-
ticipation. The program includes not only
the design and construction of research re-
actors and reactors for testing purposes, ex-
perimental and prototype reactors, but in
addition there is a research program con-
cerned with fuel element development, sepa-
rations systems development, i.e., fuel ele-
ment processing for recovery of fissionable
material, radioactive waste treatment and
waste disposal development, and reactor
safety development.
The Atomic Energy Commission has re-
cently inaugurated a program for accelerat-
ing the development of the industrial uses
of radioisotopes. This year it will spend
about $4,000,000 for applications develop-
ment, high-intensity radiation studies, and
to increase training opportunities for prac-
ticing industrial scientists and engineers.
VoL. 49, No. 3
In the biomedical field AEC’s offsite sci-
ence program is closely related to and sup-
plements its onsite program. Of the
$43,000,000 operating funds for the current
fiscal year for biomedical research about
one-third goes for the support of over 500
separate totally unclassified contracts with
universities and independent laboratories
for work in the following areas; the biologi-
cal effects of the various ionizing radiations
including acute and delayed effects, and ei-
fects produced by various beam intensities.
Objects for study include the gamut from
effects on simple biological systems to the
most complex organisms including wherever
possible effects on man himself. A major ef-
fort is directed to the genetic and ecarcino-
genic effects of ionizing radiations whether
from external sources or from radionuclides
incorporated into the living organism. An-
other important area for research support
is in the development of methods for alter-
ing or combatting radiation effects and for
removing deposited radionuclides from the
body. A third area of scientific effort is the
monitoring of radioactive materials dis-
tributed around the world as fallout from
nuclear weapons testing, and studies of the
movement of radionuclides in the strato-
sphere, troposphere, the soil, plants and ani-
mals and animal products. All this is in an
effort to gain an understanding of the mech-
anism of transport and incorporation into
the food chain of these materials. The fourth
category concerns work carried on at field
tests, at AEC laboratories and to a lesser
extent at private institutions on problems
concerned with understanding and estimat-
ing effects of radiation, including radioac-
tive fallout, thermal radiation effects and
primary and secondary blast effects from
nuclear weapons. A fifth category is radia-
tion dosimetry and instrumentation. The
last category we call the beneficial uses of
atomic energy. Except for our cancer re-
search program, it is very largely carried
out in university laboratories and is devoted
to exploiting the tools of atomic energy—
reactors, and accelerators, and the byprod-
ucts of atomic energy—radioisotopes, in the
advancement of knowledge in medicine,
agriculture, and biology generally.
In addition to these research and develop-
MarcuH 1959 EXTRAMURAL SCIENCE AND RESEARCH ACTIVITIES OF N. A. S. A. 87
ment programs the AEC science program in-
cludes training and education activities.
This year we are spending approximately
$15,500,000 for this purpose. We have spe-
cial fellowship programs in industrial medi-
cine, industrial hygiene, and radiological
physics all carried out principally on uni-
versity campuses. In addition there are re-
actor engineering fellowships. The training
for these is partly at universities and partly
at AEC laboratories. We sponsor jointly
with the National Science Foundation a
number of programs aimed at improving
science teaching in secondary schools. This
latter category includes summer workshops
in radiobiology and radiological physics for
high school science teachers. Finally, AEC
has a program of grants for radiation equip-
ment to be used in colleges and universities
in courses in reactor engineering, courses in
radiation health, and courses in the life sci-
ences and physical sciences generally.
In summary: The AEC program in sci-
ence is accomplished almost exclusively by
contract with universities, groups of uni-
versities, industry, and independent labora-
tories. Its major operations are carried out
for the most part in Government-owned
facilities but contractor operated. Its offsite
research involves the support of many hun-
dred totally unclassified research projects
chiefly in university laboratories and
planned to supplement the work of the large
laboratories. In physical science the goal is
to keep the United States at the forefront in
the atomic energy field. In reactor engineer-
ing—to produce economic and safe nuclear
power plants for a variety of purposes.
In biology and medicine its goal is to
produce as complete as possible a body of
knowledge concerning the effects of ionizing
radiations on biological systems and how
to alter and to protect against these effects.
It also aims to exploit the tools and by-
products of atomic energy activities for the
benefit of mankind in medicine, biology and
in agricultural sciences.
Finally the AEC devotes a considerable
effort to strengthening education and train-
ing in the fields of its principal interests.
a a
Extramural Science and Research Activities of the National Aeronautics
and Space Administration
By Ira H. Apsort, Assistant Director of Research, NASA
The National Aeronautics and Space Ad-
ministration will be three months old in a
few days. With the agency at this tender
age I am certain that you will appreciate
the difficulty of my speaking in detail about
the nature and scope of our extramural sci-
ence and education activities and the con-
tribution made by these activities to the
achievement of our objectives. We do, how-
ever, have some fairly definite thoughts
and plans about these activities.
The NASA was formed with the old Na-
tional Advisory Committee for Aeronautics
as its nucleus. The NASA is not merely an
enlarged NACA but is a new agency which
includes the former NACA and other organ-
izations which have been transfered to it.
I believe it would, nevertheless, be appro-
priate to say a few words about the former
NACA for the benefit of those of you who
may not be familiar with it.
The NACA was established in 1915 to
conduct research in the fields of aeronautics.
Its main responsibilities were:
1. Foresight in the planning of research
that would produce new research informa-
tion when needed,
2. The conduct of such research, mainly
in its own laboratories, and
3. Effective communication in making its
research results rapidly and generally avail-
able.
The NACA fostered close contact and co-
operation with other Government agencies,
with industry, and with the scientific com-
munity. Its advisory committees served the
88 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
broader purpose of providing a mechanism
for the exchange of scientific information
and opinion, and thus encouraged the in-
formal coordination of research through
this exchange of information.
The NACA started its research activities
through contracting with others for the
eonduct of research. In the first five years
of operation, 82 technical reports were 1s-
sued of which only 7 were prepared by the
NACA staff, and 5 of these were in the fifth
year. Through a combination of circum-
stanees which I need not dwell upon, the
NACA was unable to extend this program
of contract research to meet the needs of
the country, and it established its own lab-
oratories to conduct most of its research.
The total contract research program of the
NACA never exceeded one million dollars
a year and was usually much smaller. Even
this small program was of great value in
supplementing its own research because it
permitted the utilization of special skills
and talents that existed only in the univer-
sities and research institutions.
Because of the small size of the NACA
extramural research program, the agency
only occasionally sought out people or or-
ganizations to undertake research on prob-
lems proposed by itself, and limited the
program to nonprofit organizations. Usually
selection was made from the numerous pro-
posals made by people who desired spon-
sorship for the research they wished to un-
dertake. This system worked well for such
a small program because it assured a high
degree of enthusiasm and competence by
the research workers. In this program the
NACA operated within a rather narrow au-
thorization. Consequently, the program was
conducted with one-year fixed-price con-
tracts. Within this hmitation a sincere at-
tempt was made to keep the program as
flexible as possible. The contracts called
only for work of a certain type or within
an area, and a report on the results. Con-
tinuity was obtained to such a degree that
a few institutions have worked continuously
on certain problems for a dozen years or
more.
The National Aeronautics and Space Act
of 1958 creating the NASA continued all
the functions of the NACA and added the
vou. 49, No. 3
direct responsibility for research in space
technology, for the design, development,
construction, and operation of space vehi-
cles for peaceful purposes, and for the con-
duct of scientific research in space. These
are grave responsibilities involving the pres-
ervation of the role of the United States as
a leader in aeronautical and space science
and technology.
We plan to continue our research pro-
grams at the Langley, Ames, and Lewis Re-
search Centers to support both aeronautical
and space activities. In this work we shall
continue to cooperate as in the past with
other Government agencies, the industry,
and with educational and research institu-
tions. With regard to our new functions in
space technology, we intend to develop in
our own staff a relatively small but highly
skilled organization with the technical ca-
pabilities fully to meet our responsibilities
in planning and conducting our programs.
We expect to contract with industry for the
design, development, and construction of
space vehicles and components. We intend
to conduct an intensive program of scientific
research in space, both to assist in the de-
velopment of space technology and to ex-
plore and study the natural phenomena
occurring outside the earth. This program
will offer unique opportunities for coopera-
tive activity between NASA and the educa-
tional and research institutions in conduct-
ing scientific experiments using sounding
rockets, satellites, deep space probes, and
interplanetary vehicles.
It is obvious that the proper discharge of
our responsibilities will require the full and
efficient utilization of all the scientific and
technical skills that should be brought to
bear on this task, wherever they may exist.
Consequently, the NASA plans to sponsor
a greatly increased program of research in
educational and research institutions. The
NASA is aided in these plans by having a
broad authorization for the conduct of this
program. It will be under the direction of
Dr. Lloyd Wood of our Headquarters staff.
Our preliminary planning has established
the following general principles:
1. The research may be either basic or
apphed
Marca 1959 EXTRAMURAL SCIENCE AND RESEARCH ACTIVITIES OF N. A. S. A. 89
2. The research should be relevant to the
mission of the NASA
3. The research should be coordinated
with and supplementary to NASA Research
Center programs
4. The research should be coordinated
with that sponsored by the National Science
Foundation and other Government agencies.
5. Continuity of support should be pro-
vided so the investigators can plan their
research most effectively and make the com-
mitments necessary to retain capable as-
sistants.
In order to implement point 5, it is
planned to make the initial obligation of
funds to cover costs for periods up to three
years. Insofar as practicable, notice of ter-
mination or extension of support will be
given at least one year in advance. Over-
head will be paid according to approved
Government practices with the intent of
paying the indirect cost of research activi-
ties. It is also planned to use both contracts
and grants as appropriate to support the
research.
It is apparent that research relevant to
the mission of the NASA will include many
branches of science. In addition to the usual
physical and engineering sciences, we shall
be interested in the cosmological sciences,
the life sciences, and, at least to some de-
eree, socio-economic studies.
I would lke to emphasize the new op-
portunities the NASA offers for educational
and research institutions to participate as
full partners in the conduct of scientific
research in space. The law specifically pro-
vides that one of our functions is to ‘“‘ar-
range for participation by the scientific
community in planning research measure-
ments and observations to be made through
use of aeronautical and space vehicles and
conduct or arrange for the conduct of such
measurements and observations.”
We are confident that the educational and
research institutions will be fertile sources
of ideas for worth-while experiments to be
conducted in space. Within the limit of our
resources we shall be happy to contract with
such institutions to follow up on their ideas
and to reduce them to properly instru-
mented experiments. In some cases the en-
gineering and operating problems may be
entirely within the capabilities of the con-
tracting institution. Such may be the case,
for example, with sounding rockets. In other
cases the NASA itself, either through its
own resources or through industrial con-
tracts, will necessarily play a major role
in the engineering and operating phases of
the program. Obvious examples would be
relativistic clock experiments to study the
gravitational effect and orbiting astronom-
ical laboratories. In these cases we shall
assist In such work as appropriate by ar-
ranging for instrumentation and for instru-
mentation packaging, by providing the ve-
hicles, by launching and tracking them, by
obtaining the data and reducing them to
understandable form so that the contracting
institution can analyze and interpret the
information and report the results.
The coming space age is opening up vast
new avenues of scientific exploration and
achievement. Where they will lead I cannot
say because our imaginations are too lim-
ited for us to foresee the potentials ahead.
I am certain that the exploration of these
avenues is a task that we must all under-
take together in a spirit of scientifie coop-
eration. We in the NASA intend to under-
take our work in this spirit and to pursue
it as vigorously and rapidly as will be pos-
sible with the resources made available to
=
ia
90 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 3
PROCEEDINGS OF THE ACADEMY AND AFFILIATED SOCIETIES
GEOLOGICAL SOCIETY
782D MEETING
The 782d meeting of the Society was held in
the John Wesley Powell Auditorium, January 8,
1958, President Carte H. Dane presiding.
Informal communication—Joun B. MERTIE,
Jr.: A monazite lode in South Africa.
Program—Harry Kurmic, A. V. HEYL, A.
R. Taytor, and Jerome Stone: Rare earth
deposit at the Scrub Oaks mine, Morris County,
New Jersey.
IsiporE ZieTz, G. EK. ANDREASEN, and AR-
THUR GRANTzZ: An aeromagnetic study of the
Cook Inlet area, Alaska.
Twenty-seven east-west aeromagnetic trav-
erses were flown across the Cook Inlet depression
at a flight elevation of approximately 2,500 feet
above mean sea level. The northernmost line
crosses the area between Willow and Kashwitna,
and the southernmost line crosses Cook Inlet at
about Homer. The lines traverse part or all of
four Mesozoic tectonic elements that dominate
the structure of the Cook Inlet area. These are
the Talkeetna geanticline, the Matanuska geo-
syncline, the Seldovia geanticline, and the Chu-
gach geosyncline.
The aeromagnetic data, compiled as total in-
tensity magnetic profiles, show several signifi-
cant features that are consistent with the struc-
tural grain of the area. A 2-dimensional anomaly
is observed near the eastern edge of the area on
all profiles except the southernmost lines where
the feature becomes obscure. Geologic evidence
strongly suggests that this feature, called the
Knik Arm anomaly, is produced by granitic
rocks that have been intruded along the axis of
the Seldovia geanticline.
Near the western shore of Cook Inlet the
magnetic pattern changes abruptly. This line of
abrupt change implies a lithologic contact trend-
ing approximately northeast. This inferred con-
tact joins the Castle Mountain high-angle re-
verse fault, which has been mapped along the
north side of the Matanuska Valley and which
separates the rocks of the Talkeetna geanticline
to the north and northwest from the rocks of
the Matanuska geosyncline to the south. The
southern end of the inferred contact joins a
similar fault. This contact, which has been
named the Moquakie contact, marks the western
edge of the Matanuska geosyncline; it is in-
terpreted as a possible major fault or fault zone.
A structural basin lies between the Moquakie
contact and the Chugach-Kenai Mountains. This
basin is wide at the southern end of Cook Inlet
and narrows to the northeast. The few anomalies
over the basin area suggest depths to the base-
ment rocks of 2 to 4 miles. A 2-dimensional,
broad anomaly of about 200 gammas in mag-
nitude trends northeast from the Richfield well,
northeast of Nikishka, to the Susitna Flats area.
This anomaly, called the Point Possession anom-
aly, is believed to be produced by a rock mass
buried about three to four miles. The data sug-
gest that this trend also continues southwest
from the well.
783D MEETING
The 783d meeting of the Society was held in
the John Wesley Powell Auditorium, January
22, 1958, President Carte H. Dane presiding.
Program—D. M. Kinney, W. J. Hatt, JR.,
and A. D. Zapp: Latest Cretaceous and earliest
Tertiary rocks between Castlegate and Green
River, Utah.
W. L. Newman, A. T. Migescu, and E. M.
SHOEMAKER: Chemical composition as a guide
to the size of sandstone-type uranium deposits,
Colorado Plateau. Concentrations of uranium,
yttrium, sodium, iron, zirconium, manganese,
calcium, and nickel in 75 mill pulp samples of
uranium deposits in the Salt Wash member of
the Morrison formation on the Colorado Plateau
seem to be significantly related to the sizes of
the deposits represented by the samples. Linear
correlation coefficients between element concen-
trations, as determined by semiquantitative
spectrographic analysis, and sizes of deposits in
tons, range from /0.37/ for uranium and yttrium
to /0.24/ for nickel. The lowest significant cor-
relation coefficient for the 75 samples at the 95
percent level of confidence is 0.228. Three meth-
ods of size estimation were developed: one based
on simple linear regression theory and two based
on multiple regression theory. About 80 percent
of the size estimates based on simple linear re-
gression theory are within a factor of 12 to
14 of the true size. Estimates based upon
multiple regression theory range within approxi-
Marcu 1959
mately the same orders of magnitude. Although
the error of the estimates may be quite large,
the methods permit classification of the deposits
within reasonable confidence limits into the fol-
lowing size groups: very large deposits (10,000
to more than 100,000 tons), large deposits (1,000
to 10,000 tons), medium deposits (100 to 1,000
tons), small deposits (10 to 100 tons), and very
small deposits (1 to 10 tons). These methods
will be useful in estimating the sizes of deposits
where exposures of ore are limited, or where an
estimate is desired that is independent of other
estimates.
CHarLtes Mitton, Mary E. Mross, and
E. C. T. Cuao: Recent developments on the
mineralogy of the Green River shales.
784TH MEETING
The 784th meeting of the Society was held in
the John Wesley Powell Auditorium, February
12, 1958, President Carte H. DANE presiding.
Informal communication—PRESTON CLouD:
Mode of locomotion of an Upper Cambrian
trilobite.
Program.—RaupH L. MILusr: Faulting in the
southern Appalachians. Davin M. Raup: The
effect of environment on echinoid morphology.
The scutellid echinoid genus Dendraster L.
Agassiz has a geologic range from Pliocene to
Recent. Sand-dollars of this genus live now from
central Baja California to Vancouver Island,
British Columbia. Fossils occur in central and
southern California and in Baja California. In
the past, Dendraster has been classified into 25
species, subspecies, and varieties. In all these
forms, the apical system is posteriorly eccentric.
Variations in the eccentricity of the apical sys-
tem figure prominently in approximately two
out of every three taxonomic distinctions within
the genus.
The position of the apical system in D. ez-
centricus (Eschscholtz) varies widely. Variation
in this character between adjacent populations
of this single living species often exceeds varia-
tion between species in the fossil record. Fur-
thermore, variation in the eccentricity of the
apical system in D. excentricus is correlated with
water turbulence. In areas of high water tur-
bulence, such as those just beyond the surf zone
along the exposed coast, sand-dollars of this
species exhibit high eccentricity; that is, the
apical system is located near the posterior mar-
gin of the test. In quiet water, whether it be
PROCEEDINGS: GEOLOGICAL SOCIETY 91
at depth along the exposed coast or in shallow
protected bays, sand-dollars have a nearly cen-
tered apical system (low eccentricity). In in-
termediate environments, intermediate morphol-
ogy obtains. The correlation between turbulence
and morphology is interpreted as nongenetic
variation (nonheritable) resulting from the ef-
fect of environmental forces. The high degree
of eccentricity enables sand-dollars living under
turbulent conditions to be stable in the feeding
position and still have the madreporite exposed
(in the feeding position, they are inclined to the
sea bottom with the anterior portion of the test
buried).
Variation in eccentricity in fossil Dendraster
is interpreted in light of the above findings. The
three prominent Pliocene species, D. coalingaen-
sis Twitchell, D. ashleyi (Arnold), and D.
gibbsu (Rémond), have previously been dis-
tinguished from each other partially on the basis
of this character. Statistical analysis of these
forms shows D. ashleyi and D. gibbsii to be in-
distinguishable on the basis of this character.
Further, the amount of difference in eccentricity
between D. coalingaensis and D. gibbsii—D.
ashleyi is of the same order of magnitude as
that between populations of the living species
occurring under conditions of differing water
turbulence. Thus, the eccentricity differences
between D. coalingaensis and D. gibbsi-D.
ashley: are interpreted as the result of differing
water turbulence and not genetic change. This
does not mean that the three species are syn-
onymous but only that the differences in ec-
centricity are not genetic. The mean eccentricity
of the three Phocene forms, on the other hand,
is greater than that of the living species, D.
excentricus. Thus, there appears to have been
evolution toward a less eccentric apical system
between Pliocene and Recent.
Therefore, the eccentricity of the apical sys-
tem shows genetic change over time whereas at
a given point in time, it shows non-genetic
change and hence is an indicator of past envi-
ronmental conditions.
R. A. Bacnoup: Correlation between wind
and sand-dune directions in the light of present-
day conditions.
785TH MEETING
The 785th meeting of the Society was held
in the John Wesley Powell Auditorium, Febru-
92 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
ary 26, 1958, Vice-President Luoyp G. HENBEST
presiding.
Program.—JouHN C. Reep, Jr.: Crystalline
rocks of the Potomac River Gorge near Wash-
ington, D. C. Below Great Falls, about 10 miles
northwest of Washington, the Potomac River is
entrenched in a spectacular gorge which affords
unexcelled exposures of the crystalline rocks of
the Piedmont. The major rock types exposed
between Great Falls and Stubblefield Falls are:
(1) Mica schist and arkosie quartzite, assigned
by Keith (1901) to the Carolina gneiss, and by
Cloos (1953) to the Wissahickon formation, (2)
amphibolite bodies, probably representing sills
or lava flows, interlayered in the schist and
quartzite sequence, (3) granitized schist (in part
the Sykesville formation of Cloos, 1953), and
(4) sodie quartz diorite or granodiorite in small
discordant intrusive bodies. The age of the rocks
is problematical: the quartzite-schist sequence
has been considered by some geologists to be
Precambrian, and by others to be an eastern
metamorphosed equivalent of lower Paleozoic
rocks in the Blue Ridge.
The quartzite occurs in massive beds as much
as 40 feet thick, and as thinner beds, commonly
regularly interlayered with schist. Locally,
graded bedding and crossbedding are preserved.
Bedding in the schist has been largely obliterated,
and the only conspicuous planar structures are
sets of S-planes marked by parallel orientation of
micaceous minerals. The earliest of these is par-
allel to bedding in the associated quartzites,
whereas the younger set is subparallel to axial
planes of folds. Locally the axial plane cleavage
is a closely spaced slip or fracture cleavage, but
generally it is marked by a parallelism of new
micas. In many places formation of the new
cleavage has destroyed all trace of the older
bedding plane foliation.
Petrographic evidence indicates that the
quartzite-schist sequence has undergone at least
two periods of metamorphism. Large bent and
ragged books of biotite and muscovite, very rare
relicts of andalusite, and indeterminate sericite
pseudomorphs, probably after andalusite or
other aluminum silicate minerals, are believed
to be relicts of the early stage. During the later
metamorphism new biotite, muscovite, and gar-
net were formed, and the earlier aluminum sili-
cates were almost completely altered to sericite.
In the interlayered mafic rocks the earlier met-
VOL. 49, NO. 3
amorphism produced the assemblage andesine-
green hornblende-clinozoisite, which during the
later metamorphism was locally converted to an
assemblage of oligoclase-epidote-biotite with
green hornblende as a relict. Perhaps these two
metamorphic episodes can be correlated with
the formation of the two sets of S-planes in the
schist.
The granitized schist was apparently produced
by interaction of the normal schist with soda-
rich solutions, probably at a late stage in the
second metamorphic cycle. All gradations exist
between schist with thin oligoclase-quartz fila-
ments along the two sets of S-planes to rocks in
which thin micaceous wisps, still preserving the
orientation and relationships of the S-planes in
the adjacent schist, appear “suspended” in a
granitic matrix of quartz and oligoclase.
Field relationships indicate that small dis-
ecordant plugs and dikes of leucocratic quartz
diorite, identical in mineralogy with the quartz-
feldspathic components of the granitized schist,
may represent local intrusion of material derived
from the granitized schist. Small granitic bodies
may have originated by migration of material
into regions of low pressure near brittle am-
phibolites and quartzites, while still others may
have been formed entirely by metosomatic re-
placement.
It is hoped that this brief outline will en-
courage others to continue studies in this easily
accessible and extremely well exposed area.
REFERENCES CITED
Cioos, Ernst. Geologic map of Montgomery
County, Maryland. Maryland Department of
Geology, Mines, and Water Resources. 1953.
Coos, Ernst, and ANDERSON, J. L. Geology of Bear
Island, Potomac River, Maryland. Johns Hop-
kins Univ. Studies in Geology, no. 16, pt. 2.
Baltimore, 1950.
KeituH, ArtHur. Description of the Piedmont Pla-
teau, in Washington folio, U. S. Geol. Survey
Folio 70. 1901.
F. G. Hourermans: Effects of cosmic radi-
ation in meteorites and the earth’s atmosphere.
786TH MEETING
The 786th meeting of the Society was held
in the John Wesley Powell Auditorium, March
12, 1958, President Carte H. DANE presiding.
Communication—JoHN B. Mertie: A me-
morial to Fred H. Moffit.
Marcu 1959
Program—U. S. Geological Survey investi-
gations at the Nevada test site: KE. B. EckEL
and ©. B. Reap: Geological phase; W. H.
Diment and others: Geophysical phase.
787TH MEETING
The 787th meeting of the Society was held in
the John Wesley Powell Auditorium, March
26, 1958, President Carte H. Dane presiding.
Program——M. Gorpon WoLMAN and LUCIEN
M. Brush, Jr.: Laboratory study of equilibrium
channel shape in noncohesive material.
J. T. Hack: The relation of manganese to
surficial deposits in the Shenandoah Valley, Vir-
ginia. Manganese mines and prospects in a nar-
row zone at the northwest foot of the Blue Ridge
occur in residual clays of the Cambrian Toms-
town dolomite and Waynesboro formation. They
are covered by a mantle of quartzite cobbles
washed from the mountain slopes. The deposits
are thought by some to have formed on the
Harrisburg peneplain in Tertiary time under
conditions of lesser relief and warmer climate,
as residual concentrates from carbonate rocks.
Mapping of the surficial deposits of the Shen-
andoah Valley reveals no evidence to support
the concept of multiple erosion cycles or of a
valley floor peneplain that might have provided
a site for manganese concentration. The features
of the region are better explained as the result
of long-continued and deep erosion of a folded
area that is now close to isostatic equilibrium.
Alluvium occurs where streams enter the lime-
stone valley from areas of resistant sandstone
and quartzite and is spread by laterally migrat-
ing and degrading streams that form pediment-
like aprons near the mountain foot. The spread-
ing is aided by piracies of the main streams by
their own tributaries. Residuum, or saprolite,
occurs on limestone where the insoluble residues
are protected from erosion by a resistant cap-
ping of either transported gravel or of coarse-
grained chert residual from the limestone itself.
The manganese deposits are residual concen-
trates in the clay, preserved not because they
are uneroded remnants on a Tertiary surface but
because they have been formed under an armor
of alluvial cobbles and gravel. The process of
manganese concentration is a continuous one
and may possibly be going on at the present time.
Earu IncErRSon: The Moscow symposium on
petrochemistry, December 1957.
PROCEEDINGS: GEOLOGICAL SOCIETY 93
788TH MEETING
The 788th meeting of the Society was held
in the John Wesley Powell Auditorium, April
9, 1958, President Carte H. Dane presiding.
Program —G. W. WETHERILL, G. R. TILTON,
and G. L. Davis: Age of the Baltimore gneiss.
Davip LANDEN: New developments in photo-
grammetric measurements for geologists. One of
the recent developments in the Geological Sur-
vey has been the introduction and use of modern
photogrammetric mapping equipment in geo-
logic investigations. While aerial photographs
have long been one of the most important tools
of the geologist, the use of modern double-pro-
jection stereoscopic plotting equipment has
taken place only within the last few years. As
a result of recurring problems which concerned
the application of photogrammetric techniques
to geologic mapping, the chief topographic engi-
neer and the chief geologist in 1953 formed an
Interdivision Committee on Photogrammetric
Techniques in Geology. This group cut across the
lines of the largest Divisions in the Survey and
soon became a potent force in the advancement
of photogrammetry in geology through instru-
ment development, training, publications, and
technical assistance.
Advances in the design and use of stereo-
scopes, simple photogrammetric measuring
equipment, and the use of modern double-pro-
jection plotting equipment such as the Multi-
plex, Kelsh, and ER-55 for geologic use are de-
scribed. Several new instruments, useful for
making measurements under a stereoscopic plot-
ter, were sponsored by the Interdivision Com-
mittee; these included the photogrammetric pro-
file plotter, the photogrammetric dip-and-strike
indicator, and others. The stereoplotted grid was
designed to facilitate transfer of geologic data
from photograph to map. The orthophotoscope
machine and its product, the orthophotograph,
were developed primarily for geologic use. The
orthophotograph is a photograph in which es-
sential detail has been rectified to an ortho-
graphic, or plan, projection. It has become today
one of the great advances in surveying and
mapping technology. A new photographic tech-
nique, useful to paleontologists, was also de-
veloped—photographs of fossils in orthographic
projection.
It is concluded that one of the best means of
advancing a science such as geology is to advance
94 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
its measuring and mapping techniques. Aerial
photographs and photogrammetry, by their
very nature, should be among the geologist’s
most fundamental operations—that of making
accurate measurements.
Vincent C. Kexuey: Structure and fracture
systems of the Colorado Plateau. The Colorado
Plateau is a relatively undeformed structural
segment within the Cordilleran orogenic systems.
It consists of irregularly interspersed uplifts,
basins, platforms, and lesser fold belts of mild
or moderate intensity. Most of the deformation,
however, is concentrated along great monoclinal
flexes which bound certain parts of the uplifts
and basins.
Fracture sets have been mapped on a scale of
1:62,500 on photomosaics for a large part of the
Plateau. The joint sets range greatly in strati-
graphic and areal extent, in spacing, in orienta-
tion, and in numbers. Dominant joint sets are
nearly vertical in areas of low-dipping rocks, but
inclined longitudinal and oblique joint sets are
common along monoclinal flexes. From this
relationship and from the fact that the fracture
systems reveal little regular relationship to folds
in most places, it is concluded that many of the
sets are older than the Laramide folding. Some,
however, are clearly younger than the principal
folding.
The fracture systems of the several major
uplifts are largely dissimilar. The lack of simi-
larity of uplift fracture patterns may be due to
(1) differences in the uplift forms and their
regional settings, (2) differences in stratigraphy,
(3) differences in rate an® manner of uplift
growth, and (4) the fact that many of the sets
appear by areal distribution to be related to
crustal disturbances of much greater extent
than the uplifts and of quite different mechanics
of deformation.
Numerous joints probably formed early for
nonorogenic reasons such as differential com-
paction, differential loading, original-dip gliding,
and epeirogenic warping. Nevertheless, the ex-
istence of some consistency of orientation of
dominant regional sets in northeasterly, north-
westerly, and easterly directions makes it ap-
pear that there were over-all deep-seated stress
systems, responsible, in complicated ways, for
many of gross aspects of the fracture pattern.
Three east-west lineaments of fracture zones,
the Cache Valley, Rico, and Rattlesnake, are
“rooted” in part in the Precambrian structures
VoL. 49, NO. 3
to the east and are thought to be reflections of
shearing before and during Laramide in the
basement.
Two phases of Laramide deformation on the
Plateau are postulated. The first resulted from
a major stress oriented easterly or southeasterly
which formed the northerly and northeasterly
trending monoclines. The second phase resulted
from a major regional stress oriented southwest-
erly which formed the northwesterly trending
folds and uplifts.
789TH MEETING
The 789th meeting of the Society was held
in the John Wesley Powell Auditorium, April 23,
1958, President Carte H. DANE presiding.
Informal communications: EDwIN ROoEDDER
reported on the Science Fair held in Georgetown
on April 19, at which he had been a judge, and
introduced a prize winner, Philip Perkins.
L. T. AupricH reported the seismic detection
in the Washington area and in New York State
of the Ripple Rock blast in the Seymour Nar-
rows, British Columbia.
Program.—Gorpon E. ANDREASEN, ISIDORE
Zietz, and ARTHUR GRANTZ: Structural inter-
pretation of aeromagnetic data observed in the
Copper River Basin, Alaska.
Z.S. ALTSCHULER and E. J. Youna: Relations
between Tertiary sedimentation and structural
history in west-central Florida.
RicHarp H. JAHNs and C. WAYNE BURNHAM:
Preliminary experimental evidence on pegmatite
crystallization.
790TH MEETING
The 790th meeting of the Society was held in
the John Wesley Powell Auditorium, October 8,
1958, President Carte H. DANE presiding.
Program —tThe deferred presidential address
of W. D. Jonnston, Jr.: Outside Interior, or the
Geological Survey’s part in foreign technical
assistance, 1940-1958.
791ST MEETING
The 791st meeting of the Society was held
in the John Wesley Powell Auditorium, October
22, 1958, President Carte H. Dane presiding.
Program—ApDRIAN RicHaRDs: Eruption of
Capelinhos Volcano, Faial Island, Azores, a
report of the Cranbrook Expedition, 1958.
Irnvinc FrrepMAN: Deuterium and the age of
Arctic sea ice. The deuterium fractionation that
Marcu 1959
occurs upon the change of state of liquid water
to ice has been measured under natural condi-
tions. The ice is enriched in deuterium by 2 per-
cent relative to the water in equilibrium with it.
Consecutive samples from an ice-core collected
near ice island T-3 (80°N, 113°W) was analyzed
for its relative deuterium content. A plot of
relative deuterium content versus depth in the
10-foot core shows several minima. These min-
ima are interpreted to be due to the freezing
of snow melt water that runs off the surface of
the ice in summer. If this thesis is correct, the
ice flow represents the accumulation of 4 years of
winter ice.
D. F. Hewett: Deposits of the manganese
oxides. The program of field work on manganese
deposits during the war permitted the collection
of many specimens of manganese oxides over the
entire nation as well as in Cuba and Mexico. X-
ray analyses of about 250 specimens from the
United States, 150 specimens from Cuba, and
100 from Mexico have been made by Richmond
and Axelrod of the Geological Survey to de-
termine mineral character, and partial and com-
plete chemical analyses have been made of many
specimens by Fleischer of the Survey. Some of
the results of this work have been announced
by Fleischer and Richmond. Recently, Hewett
has continued the study of the manganese oxides
by interpreting the geological environment under
which the 250 specimens from the United States
were formed.
From this review of the mode of occurrence
of the oxides of manganese, 33 in number of
which 27 are known in the United States, the
conclusion has been reached that (1) some of
the oxides are uniformly supergene throughout
the United States, (2) another group is unl-
formly hypogene, and (3) another group that
includes the common oxides, psilomelane, hol-
landite, cryptomelane, coronadite, hetaerolite
and pyrolusite, is supergene in some places and
hypogene in others. To reach this conclusion,
a group of criteria to distinguish between super-
gene and hypogene origin was set up.
The study indicates that in the broad arc
from central New Mexico across Arizona into
southern California and Nevada there are many
veins of the manganese oxides, at least 100, of
which at least 30 are extensively explored,
largely made up of psilomelane, hollandite with
minor cryptomelane, coronadite, and pyrolusite,
which are hypogene in origin. Most of the veins
PROCEEDINGS: GEOLOGICAL SOCIETY 95
follow fractures and breccia zones in layered
voleanic rocks of middle Tertiary age. Associ-
ated with the manganese oxides, in some places
younger and in other places older, are opal,
chalcedony, quartz, zeolites, fluorite, barite, and
calcite, in part hydrothermal in origin. In the
same broad are there are numerous deposits of
stratified manganese oxides which contain small
but noteworthy amounts of tungsten, lead, and
copper, which are also found in the vein oxides.
It is concluded that the veins of oxides are re-
lated to the stratified oxides; that hot waters
from depth contained manganese which was
deposited as oxides in the veins where the solu-
tions met the shallow zone of ground water con-
taining oxygen. The remaining manganese was
carried to the surface where flocculent oxides
were formed and carried as sediments to nearby
basins. This interpretation is supported by the
presence in the region of hot springs that are
now depositing oxides of manganese that contain
the same minor metals as the veins and strati-
fied oxides.
792D MEETING
The 792d meeting of the Society was held
jointly with the Paleontological Society of Wash-
ington in the John Wesley Powell Auditorium,
November 12, 1958, Vice-President ALIcE ALLEN
presiding.
Program.—ALFRED 8S. RomEr: Rocks, fossils,
and Darwin.
793D MEETING
The 793d meeting of the Society was held in
the John Wesley Powell Auditorium, December
10, 1958, Vice-President Liuoyp G. HENBEST
presiding.
Program —tThe Presidential address; CARLE
H. Dane: The New Mexico geologic map—a
summary of 30 years of geologic progress. Pre-
liminary versions of the geology of the north-
western and southeastern parts of New Mexico,
by Carle H. Dane and George O. Bachman, have
been published by the U. 8. Geological Survey,
and first compilation has been completed for
the remainder of the State. These preliminary
maps were assembled and exhibited as a new
summary picture of the geology of New Mexico,
30 years subsequent to the issuance of the pre-
vious U. 8. Geological Survey geologic map of
New Mexico by N. H. Darton. The new map
will show many more geologic units than were
96 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
previously recognized, hundreds of faults and
intrusive dikes not previously shown, and much
greater detail of geology, summarized from more
than 150 different sources of data, published and
unpublished. During the 30-year interval be-
tween the two maps, vertical air photographic
coverage of the whole State has become avail-
able, and the reconnaissance and semidetailed
phase of geologic mapping of the State has been
nearly completed. During this interval the con-
cepts of intertonguing and of facies changes
have become firmly established in geologic think-
ing, in part as a result of detailed studies of
the Permian, Cretaceous, and Tertiary rocks
in New Mexico, and these concepts are reflected
in the new map.
The general geology of the State was briefly
described with particular reference to the dis-
tribution of units selected for discrimination on
the compilation, and the geology of six selected
areas was described more fully to illustrate the
more detailed geologic mapping that is now
available for generalization and to show the
variety of sources from which data was derived.
Some new facts about the geology of the State
discovered in recent years and during reconnais-
sance in connection with the State map project
were mentioned. The excellent record of geologic
assistance and guidance in the discovery and
development of mineral resources in New Mexico
Was summarized, and it was pointed out that
the annual value of production of mineral re-
sources in the State has increased more than
VoL. 49, No. 3
tenfold in the last 30 years, due chiefly to spec-
tacular increases in the value of oil and gas,
potash, and uranium produced. The geologist
has thus made a substantial contribution to the
improvement of the general welfare in the State.
66TH ANNUAL MEETING
The 66th annual meeting was held immedi-
ately following the 793d meeting, President
CarLE H. Dane presiding. The reports of the
secretaries, treasurer, and auditing committee
were read and approved. The Awards Committee
presented first prize to G. W. WETHERILL, G. R.
Titton, and G. L. Davis for their paper Age
of the Baltimore gneiss and second prize to
IstipoRE ZiptTz, G. E. ANDREASEN, and ARTHUR
Grantz for their paper Aeromagnetic study of
Cook Inlet, Alaska. The Sleeping Bear Cup was
presented to W. H. Brapuey for his devastating
demolition of a special Cloud effect.
Officers for the year 1959 were then elected:
President: JosepH W. GREIG
First Vice-President: CHARLES A. ANDERSON
Second Vice-President: Louis C. Conant
Secretary (2 years): J. THomas Dutro
Treasurer: HELEN F. WEISSENBORN
Members-at-large of the Council (2 years):
CHARLES S. DEenNy, JoHN E. JoHNSON, Rospert C.
STEPHENSON.
The Society nominated Carte H. Dane to be
a Vice-president of the Washington Academy of
Sciences for the year 1959.
If our scholars would lead more earnest lives, we should not witness
those lame conclusions to their ill-sown discourses, but their sentences
would pass over the ground like loaded rollers, and not mere hollow and
wooden ones, to press in the seed and make it germinate.—THOREAU.
Vice-Presidents of the Washington Academy of Sciences
Representing the Affiliated Societies
Emilesepuical Society of Washington................................ MICHAEL GOLDBERG
puparopolorieal Society of Washington...................02-ceeeeee: FraNK M. SETZLER
Femeriea society of Washington.....................00.sceeceeess HERBERT FRIEDMANN
urrateresaciery of Washineton.................5cecneceeecseece ed ALLEN L. ALEXANDER
Pepamolomtes) Society of Washington. ................-..-2.eeee0-- Haroup H. SHEPARD
Menai oearrapmic SOCIety........ 02... 62.002. Seen caw eeeeeeuees ALEXANDER WETMORE
Poameeeesnmcicty of Washington............0..0..6ceeeececcceesuees ees Car.LE H. Dane
mreuten) paciety of the District of Columbia......................-.6-- FREDERICK O. CoE
SUE TECISRINCAL SOCIETY... <5. sa oe cle ce pees ede vecceteteceseeecs U.S. Grant, 3p
Peermaeeansortery OF Washington.............5..ce cece cece we eee seccees CARROLL E. Cox
Washington Section, Society of American Foresters. ....................- G. F. Gravatt
Weemmeton mociety of Engineers. ................. 0. cece cee eecees Howarp S. RAPPLEYE
Washington Section, American Institute of Electrical Engineers....RoBert D. ELBoURN
hem ntoolesical Society of Washington.........................-- CarRLTon M. HERMAN
Washington Branch, Society of American Bacteriologists.................. BERNICE Eppy
Washington Post, Society of American Military Engineers......... ALBERT J. HOSKINSON
Washington Section, Institute of Radio Engineers. ................ Rosert D. HuntTooNn
National Capital Section, American Society of Civil Engineers....Howarp S. RAPPLEYE
D. C. Section, Society of Experimental Biology and Medicine...... KaTHRYN KNOWLTON
Washington Chapter, American Society for Metals.................... JoHN A. BENNETT
Washington Section, International Association for Dental Research.. ALPHONSE ForRzIaATI
Washington Section, Institute of the Aeronautical Sciences.............. F. N. FRENKIEL
D. C. Branch, American Meteorological Society...................... Jack C. THOMPSON
Washington Section, American Society of Mechanical Engineers...... WiuiraM G. ALLEN
Washington Chapter, Acoustical Society of America................... RicHarpD K. Coox
ieeceneme society of Washington.............0... cece ween nce eees FranK L. CAMPBELL
CONTENTS
Page
SyMPosium ON “Extramural Science Programs of the Federal Govern-
ment’’:
Introductory remarks. A. T. McParrson....-...>))seeeeeeee 65
Extramural science programs of the National Science Founda-
tion. Roprrt B. BRope. ». 2104 2...5. eee 66
Extramural science programs of the Department of Defense.
Grorce_ D. LUEKES. . oo. 24.02 a. dees ee A 70
Extramural science programs of the National Institutes of
Health. C. J. VAN SEYKE.....0....o<....2. Dee 75
Extramural science programs of the United States Department
of Agriculture. Byron T. Saaw......--.... 02) see eee 81
Extramural science programs of the Atomic Energy Commission.
CHARLES L. DUNHAM......... . hace «es. ere 2 Se 84
Extramural science and research activities of the National
Aeronautics and Space Administration. Ira H. Apspott.. 87
PROCEEDINGS: Geological Society of Washington.:................... 90
ae Fe
| DAW2S
VOLUME 49 April 1959 eee a
JOURNAL
OP AH
WASHINGTON ACADEMY
OF SCIENCES
Published Monthly by the
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Journal of the Washington Academy of Sciences
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TOW rN AE
OF THE
WASHINGTON ACADEMY OF SCIENCES
Vou. 49
APRIL 1959
No. 4
Science and Education in the Washington Area
By FrRanK L. CAMPBELL
President, Washington Academy of Sciences
(A radio address delivered on Engineering News-Report, March 1, 1959)
Yesterday in Washington three scientific lectures
for high school students and teachers were given at
10:30 a.m.: one by Dr. Raymond J. Seeger, of the
National Science Foundation, entitled “Faster Than
Sound”; the second by Dr. R. Kenneth Lobb, of the
Naval Ordnance Laboratory, on “Hypersonic Flight
in the Frontiers of Space”; and the third by Dr.
Sterling B. Hendricks, of the US. Department of
Agriculture, on the “Action of Light on Plants.”
They spoke at the Carnegie Institution of Washing-
ton, the U.S. National Museum, and the National
Institutes of Health, respectively. All three are
outstanding scientists, particularly Dr. Hendricks,
who is a member of the National Academy of Sci-
ences and who recently received an award from
the President of the United States in recognition
of his scientific work.
Why were these distinguished men lecturing on
a Saturday morning when they might have been
resting? Because, like hundreds of other scientists
and engineers in the Washington area, they feel
that it is their civic duty to give freely of their time
and experience in order to transmit to younger
people some understanding of their work and of
their enthusiasm for it. Call it free advertising, if
you like, for these men are selling science and en-
gineering to students who have yet to choose a
career. They do it not only because they know
that our country needs an ever-increasing number
of persons skilled in science and technology but also
because they believe in their work as a deeply satis-
fying way of life. So they speak partly as mis-
sionaries, trying to convert those who do not under-
stand the ethical values of work that requires great
devotion and absolute honesty.
The lectures just mentioned were part of a series
of nine. How were they arranged and how in gen-
eral is the great scientific and engineering talent
of the Washington area brought to bear on young
people? It is done by joint effort of two federations
of local societies; one is called the Washington
Academy of Sciences, the other the D. C. Council
of Engineering and Architectural Societies. The
Academy unites 26 scientific and engineering soci-
eties; the Council 29 engineering and architectural
97
societies. Six engineering societies are common to
both. It would have been chaotic if each of the 49
local societies had tried to do its own proselyting in
the schools of the Washington area; even inde-
pendent action by the Academy and the Council
would have been inefficient if not irritating. The
problem was solved in 1955 by the creation of the
Joint Board on Science Education; i.e., joint be-
tween the Academy and the Council, but to a con-
siderable degree independent of both. The Joint
Board has many other functions beside the arrange-
ment of the lecture series first mentioned. Its most
remarkable feature is its Secondary School Con-
tacts Committee. This is an organization of eight
divisions covering junior and senior high schools in
Six areas in and around the District of Columbia as
well as parochial and private preparatory schools
in the whole Washington area. For each of the 150
schools of the area there is a scientist or engineer
who had volunteered to help the science and mathe-
matics teachers and students of his chosen school
in any way he can. Through the Contacts Com-
mittee he may get Career Day speakers, speakers
for science clubs, films on science and engineering
topics, advice and assistance on science projects, and
assistance for local science fairs. Occasionally the
science or mathematics teachers of the area wish to
go to national science teachers’ meetings on school
days. Then the Contacts Committee arranges for
their classes to be taken by professional scientists
and engineers, who, though inexperienced in teach-
ing, are willing to brave hostile or indifferent stu-
dents in order to carry their message to the students
willing to listen.
I could tell you of many other achievements of
the Joint Board and of its parents, the Academy and
Council, but time is lacking. We scientists and en-
gineers in the Washington area are proud of what
we are doing for our successors. Looking at the fine
membership of our Junior Academy of Sciences,
at the science fairs held here, and at other evidence
of scientific interest and competence of many of our
young people, we are optimistic about the future of
science and engineering in this community.
a
ITHSONIAN 1 5 1959
SN ETITUTION JUN 15 1
QS JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 4
PHYSICS.—Men and electrons! L. Marron, National Bureau of Standards.
(Received February 18, 1959)
Several months ago I came to the conclu-
sion that the history of the electron (or of
electrons) might be a good subject for the
address of the retiring president of this so-
ciety. In the meantime, I had ample oppor-
tunity to study the subject and found, to my
surprise, that there is even more historical
material than I ever imagined. Under the
circumstances it seems preposterous to add
one more history of the electron to the exist-
ing ones unless one can say something new.
I take courage, however, from the fact that
my interpretation of one or the other phase
of the development does not seem to agree
entirely with those derived from earlier pa-
pers. I present here, therefore, a slightly dif-
ferent version of the history of the electron
or, to be more precise, some fragments of the
history of the electron.
To start, I should like to show a tabula-
tion of the properties of electrons, as we
know them now. Though incomplete this
represents a few of the salient facts we have
acquired in the past and allows us to look
at the different aspects of the behavior of
the electron. At the same time this permits
us to group our discussion around certain
conceptual aspects of this development, and
the first of these conceptual aspects is the
PROPERTIES OF ELECTRONS AND
RELATED DEFINITIONS
GHARGE. 3 eee e==its&X 10 ¥es.u.
Rese MASS oe mo = 9.1 X 102g
Masse Pe eae wot m = moll — @/e2)R®#
Raprics (CLassIcAL).......- r = e2/moc? = 2.8 X 10°32 cm
Virtioqie sn esa eee t
MOMENTUM: 326095 902 FF p= mp
Kiwetic FINERGY.......2-. E = 2(m — mo)
Wave LENGTH. ..._......2- AX = h/p
SIE ee eee oe cele aes s= 16
MaGNeTic MOMENT.....__. pu = 0.93 X 102° erg/gauss
SPATISTICS «2.8 te ee ee Fermi
corpuscular nature of the electron. We shall
try to examine, therefore, how the concept of
the elementary charge emerged and who are
its originators. In other words, my presenta-
tion of the history of the electron will not be
a strictly chronological one. However, within
1 Address of the Retiring President of the Philo-
sophical Society of Washington, delivered on
January 16, 1959.
the framework of whatever conceptual de-
vice I may follow, I shall use a more or less
chronological development.
It is customary to start the history of the
electron with the famous utterings of Ben-
jamin Franklin. These appeared first in
1756 and are as follows: “The electrical
matter consists of particles extremely subtle,
since it can permeate common matter, even
the densest metals, with such freedom and
ease as not to receive any appreciable resis-
tance.” This statement is usually taken as a
clear proof that Benjamin Franklin for the
first time conceived the idea of electricity
consisting of very small particles and was
aware of this corpuscular nature of electric-
ity. I can not agree entirely with that view-
point. Let us examine this statement in the
light of what was known when Franklin an-
nounced it and what kind of background
existed. In those times the commonly ac-
cepted theory described electricity in terms
of two fluids; one so-called vitreous and one
resinous. In case someone should be inclined
to take this 2-fluid theory as a precursor of
the present conception of electrons and of
positrons, | must warn you that the two
fluids had to be present in equal quantities
to describe the phenomena known at that
time. Franklin took the very important step
of replacing this 2-fluid theory with a 1-fluid
theory in which all known phenomena could
be described in terms of one type oi electric-
ity or by the lack of it. This was a tremen-
dous step forward, and its importance can
not be sufficiently underlined. It paved a
way toward our modern conception oi elec-
tricity, and indeed it paves a way toward
the electron concept, but—and here comes a
very important ‘“but’’—the fact that the de-
scription was in terms of “particles” does
not have the same meaning as when we talk
today of particles of electricity.
In a chapter of the first edition of the
Handbuch der Physik, Walter Gerlach com-
pared the role played by Franklin in the
development of electron theory to that of
Democritos in the development of the
atomic theory of matter. I would agree par-
AprRIL 1959
tially with this viewpoint. Both Democritos
and Franklin used the atomistic concept in
describing certain phenomena: Democritos,
those of matter; Franklin, those of electric-
ity. Neither man had very ample experi-
mental material at hand on which to base
such a conception. In both cases the concept
of smallest possible particles was an ex-
tremely vague one, so in one sense their
roles were very similar, but here the analogy
ends. Whereas Democritos’s atomistic con-
ception remained alive through the writings
of Lucretius, that of Franklin was forgotten
for quite a while. In fact, I have no evidence
that Franklin’s utterances were remembered
at all until the time of the emergence of the
corpuscular concept. They were not resus-
citated until J. J. Thomson dug them out of
oblivion in his Silliman lectures in 1903
given at Yale University. Nowhere in the
famous papers preceding that of Thomson,
dealing with the subject of the electron,
could I find any trace of their being aware
of Franklin’s prediction, and in that sense
Franklin’s statement was without very
much influence on the subsequent develop-
ment. In the Silliman lectures Thomson,
speaking of the determination of e/m, the
charge to mass ratio of the elementary
charge, says:
These results lead us to a view of electrification
which has a striking resemblance to that of Frank-
lin’s “One-Fluid Theory of Electricity.” Instead
of taking, as Franklin did, the electric fluid to be
positive electricity we take it to be negative. The
“electric fluid” of Franklin corresponds to an as-
semblage of corpuscles, negative electrification be-
ing a collection of these corpuscles.
One more remark about the use of the
word “particles” in Franklin’s famous state-
ment. At the time of Franklin the atomistic
concept of matter was already quite well
advanced. In fact, at least a century earlier
the famous natural philosophers had con-
ceived of heat in terms of what we would
regard nowadays as a kinetic theory. Bacon,
Boyle, and Hooke professed surprisingly
modern views about the nature of the heat.
Take, for instance, Hooke in his Micro-
graphia: “Heat is a property of a body
arising from the motion or agitation of its
parts.” Or listen to Boyle: “Nature of heat”
consists in “a various, vehement, and in-
MARTON: MEN AND ELECTRONS 99
testine commotion of the parts among them-
selves.” It is hardly surprising, therefore,
that, when matter has been considered as
being constituted of small particles, Franklin
should borrow the expression “‘particles” for
a supposed fluid. We must remember that
Franklin’s fluid was something material and
tangible. Another interesting parallel is
that, like Franklin’s views that were forgot-
ten for so long, the kinetic views of Bacon,
Boyle, Hooke, and others were also forgot-
ten for quite a while. Take this quotation
from Whittaker’s remarks in his History of
the theories of aether and electricity:
Perhaps nothing in the history of natural phi-
losophy is more amazing that the vicissitudes of
the theory of heat. The true hypothesis, after hav-
ing met with general acceptance throughout a
century, and having been approved by a succession
of illustrious men, was deliberately abandoned by
their successors in favor of a conception utterly
false, and, in some of its developments, grotesque
and absurd.
Franklin’s 1-fluid theory found slowly a
universal acceptance. It became a good
working theory for Faraday, who created
the next important step in the theory. In
January 1834 Faraday wrote as follows:
The theory of definite electrolytical or electro-
chemical action appears to me to touch immedi-
ately upon the absolute quantity of electricity or
electric power belonging to different bodies. It is
impossible, perhaps, to speak on this point without
committing oneself beyond what present facts will
sustain; and yet it is equally impossible, and per-
haps would be impolitic, not to reason upon the
subject. Although we know nothing of what an
atom is, yet we cannot resist forming some idea
of a small particle, which represents it to the mind;
and so we are in equal, if not greater, ignorance of
electricity, so as to be unable to say whether it is
a particular matter or matters, or mere motion of
ordinary matter, or some third kind of power or
agent, yet there is an immensity of facts which
justify us in believing that the atoms of matter are
in some way endowed or associated with electrical
powers, to which they owe their most striking
qualities, and amongst them their mutual chemical
affinity.
There are two important details to be re-
tained from this statement. One is that there
is no mention at all of either Franklin or of
any other predecessor. The second is that
gradual emergence of the notion of the ele-
mentary charge. This elementary charge
does not yet exist separately from matter.
100 JOURNAL OF THE
It is linked to the atom or atoms and exists
only in the electrolytic exchange of electric-
ity. There is no prediction about the exist-
ence of such an elementary charge in the
normal conditions of conductivity.
The first instance of attributing the phe-
nomena of electrodynamics to the agency of
moving electric charges is that of Weber. In
1873 Maxwell, writing on the work of his
predecessors, said:
The electromagnetic speculation which was orig-
inated by Gauss and carried on by Weber, Rie-
mann, J. M. C. Newmann, Lorenz, etc. is founded
on the theory of action at a distance, but depend-
ing either directly on the relative velocity for the
particles, or on the gradual propagation of some-
thing, with a potential or force, from one particle
to the other.
This I have quoted from the foreword of the
first edition of Maxwell’s famous Treatise
on electricity and magnetism. No wonder
that on page 312 of the same volume, in a
section dealing with electrolysis, I find the
following quotation:
Suppose, however, that we leap over this diffi-
culty by simply asserting the fact of the constant
value of the molecular charge, and that we call
this constant molecular charge, for convenience in
description, one molecule of electricity.
Eight years later Helmholtz went even fur-
ther in his Faraday memorial lecture de-
livered before the Royal Institution of
Great Britain. In this year of 1881 Helm-
holtz formulated his thought as follows:
Now the most startling result of Faraday’s law
is perhaps this; if we accept the hypothesis that
the elementary substances are composed of atoms,
we cannot avoid concluding that electricity also,
positive as well as negative, is divided into definite
elementary portions which behave like atoms of
electricity.
All these statements taken together could be
interpreted as a clear conception of the cor-
puscular nature of the elementary charge
of electricity. I am somewhat skeptical of
this view. None of these statements men-
tions the evidence obtained in gaseous dis-
charges and for that type of evidence we
have to go back almost 20 years.
Exactly 100 years ago, in 1859, the Ger-
man mathematician and physicist Plicker
made a rather surprising discovery. He was
investigating the discharge of electricity
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, NO. 4
through a rarefied gas. He was in a better
position to investigate that type of phenom-
enon than were any of his predecessors, be-
cause his institution had an outstanding
technician named Geissler who invented a
new pump for producing a better vacuum.
The Geissler tubes, as they soon became
known, showed surprisingly beautiful col-
ored phenomena in the discharge which took
many forms and shapes. Pliicker was in the
fortunate position of being the first investi-
gator of this behavior. One particular fact
emerged: that there exists a kind of recti-
lineal propagation of part of the electrical
discharge, originating on the negative elec-
trode, hence the name “cathode rays.” With-
out attempting any explanation of their na-
ture, Pliicker, and later his pupil Hittorff,
observed that these rays can be deflected by
a magnetic field. Pliicker was originally pro-
fessor of mathematics and was recognized
as one of the leading geometers of his time.
When he took over the physics chair, he con-
ducted all his physics research in a remark-
ably unquantitative way. I deliberately use
the word unquantitative, instead of qualita-
tive, because one would expect from a
leading mathematician an attempt at a
somewhat quantitative formulation of the
phenomena he is investigating. Plucker did
nothing of the kind, and his successor Hit-
torff followed in the same way. The German
physicist Goldstein did quite a bit to in-
vestigate these discharge phenomena, and
so did the British physicist Crookes. Slowly,
however, people started to speculate about
the nature of these strange rays and gradu-
ally two views emerged. One was that of
Crookes, who maintained that in an elec-
trical discharge, particularly in the cathode
rays, matter finds itself in what he called a
fourth state of aggregation—a state of ag-
eregation beyond the known three: solid,
liquid, and gaseous. The German school of
thought was somewhat opposed to this view.
Based upon the experiments of Hertz and
his pupil Lenard, the view became pre-
ponderant on the eastern side of the Rhine
that cathode rays consist of some kind of an
ether vibration. Lenard found that cathode
rays can penetrate through a thin film of
aluminum, or other thin material, and can
even enter the outer atmosphere. No cor-
APRIL 1959
puscle, it was thought, would be able to
penetrate through dense matter like this,
and that is why the electromagnetic wave
explanation was preferred by the Ger-
mans. Apparently nobody thought that this
strange substance could be electricity in free
flight, and nobody tried to identify it with
electrolytic phenomena or with the conduc-
tion of electricity in matter.
The naming day of the electron did not
occur until 1874, or 1881, depending on
which year is taken as the proper date. In
1874, before the Belfast meeting of the
British Association, J. Johnstone Stoney
read a paper in which he proposed that the
elementary charge of electricity be called
the electron. His paper, however, was not
published until 1881. Stoney’s proposal was
a reasonably logical one. Faraday used the
word ion quite often in his electrolytical and
electrochemical investigations, and ion was
accepted for quite a long time. But the noun
electron was not derived from the ion; it
was derived from the Greek word for amber,
from which the word electricity itself has
been derived. It was, however, responsible
for the introduction of the ending t-r-o-n in
our language. This fateful event did not oc-
cur until the first or second decade of our
century when the magnetron and kenotron
were so named. From then on, all kinds of
devices were given names ending in “tron,”
through the somewhat mistaken idea that
t-r-o-n means something. I should have pre-
ferred that this ending be reserved for ele-
mentary particles like the positron and the
meson, which was originally called meso-
tron. However, as the “tron” ending has now
been taken over by all kinds of gadgets, it
may be just as well that the mesotron has
been renamed meson and cannot be con-
fused with the perhapsatron and the swin-
deltron. Still, I sometimes wonder what some
people may think of the electron who are
familiar only with the various complicated
instruments ending in “tron.” Perhaps they
think of the electron too as a complicated
gadget.
Another remark may be pertinent at this
point. At the beginning of the century, par-
ticularly in European countries, the word
electronics was used to describe the physics
of the free electron. Here is another sad in-
MARTON: MEN AND ELECTRONS
101
stance of the corruption of a word that was
reasonably straight-forward and _ reason-
ably short. Nowadays, particularly in this
country, electronics is completely devoted
to the description of high-frequency phe-
nomena, and nobody who wants to speak of
the free electron can ever use the word elec-
tronics without it being misunderstood.
The real emergence of the modern con-
cept of the elementary charge or elementary
particle had to wait until the closing days
of the last century. Stoney’s electron was
still the elementary charge associated with
the electrolytic process. The discovery of
the photoelectric effect in 1888 by Heinrich
Hertz, and its later further development by
Hallwachs, did not contribute in any man-
ner to the identification of the gaseous ion
with the electrolytic one. This great event
did not occur until 1895-1897. Those years
saw three very essential steps. First was
Perrin’s identification of the charge carried
by cathode rays with the negative charge.
The next extremely important step was the
theoretical work of Lorentz, who in 1897
interpreted the then quite new observations
of Zeeman and showed that their only possi-
ble interpretation was in terms of the action
of electrons associated with the atoms. Lo-
rentz also calculated the famous equation
of Lorentz force. Later in the same year
came the extremely important work of J. J.
Thomson, who determined quantitatively
for the first time the deflection of an elec-
tron beam and determined in this manner
the ratio of the charge to the mass of the
elementary particles carrying the elemen-
tary quantity of electricity. These were the
essential steps necessary for formulation of
the modern concept, and of the three I
should be inclined to say that Lorentz’s con-
tribution was perhaps the greatest, although
I do not want to belittle Thomson’s and
Perrin’s contributions either. The early part
of the twentieth century saw determination
of the elementary charge by Millikan. This
achievement, however, did not change the
conceptual formulation which by that time
had been acquired.
The word electron did not find immediate
acceptance, and even as late as 1906, the
date of the second edition of Thomson’s
famous book Conduction of electricity
102 JOURNAL OF THE
through gases, the word never appears. In
that book Thomson always calls the ele-
mentary charge negative ion. Even slower
was the acceptance in certain circles of the
notion of the elementary charge, and to
many the famous struggle waged by Ehren-
haft against Millikan and many others re-
mains still vivid. Ehrenhaft was convinced
that smaller charges than those measured
by Millikan and others exist, and he put up
a long, hard fight to prove that subelectrons
can exist. Ehrenhaft, although somewhat a
strange character, was a very good physi-
cist, and he devised many beautiful experi-
ments in an effort to prove the existence of
subelectrons. He was very much hurt when
his own students became convinced of the
futility of his views. He was too stubborn
to recognize it, and stories are still going
around about his complaint that he has sent
one of his best students to California to con-
vince Millikan and instead of that his best
student was corrupted by Millikan. I have
to thank Dr. DuMond for an anecdote il-
lustrating this controversy. One day Muilli-
kan was asked by a lady: “Dr. Millikan, do
you spend your whole time proving that
electricity consists of electrons?” He an-
swered with a smile that thanks to Dr. Eh-
renhaft there was getting to be more truth
than pleasantry in that question.
When I said that the twentieth century
saw essentially the consolidation of the con-
ception of elementary particles, I did not
mean to imply that nothing has happened.
Since the turn of the century several very
important investigations occurred which
should be mentioned here. One was the dis-
covery by Kaufmann that the mass of the
electron varies with its velocity. This be-
came a splendid confirmation of the special
relativity theory. The second important se-
ries of investigations demonstrated the inert
mass of the electron through the so-called
evyromagnetic effects. Four such effects have
been listed in the literature. One was Max-
well’s proposed experiment, which would
show that a magnet, rotated around any
axis not coinciding with the direction of
magnetization, must act as a gyroscope. The
second is the Barnett effect of magnetiza-
tion by rotation. The famous Einstein—de
Haas effect is third: it consists of rotation
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 4
by magnetization. And last is gyroscopic
magnetization by the rotation of a magnetic
field, investigated by Fisher and by Bar-
nett.
The last important new feature of twenti-
eth-century work which can be derived es-
sentially from Lorentz’s equation of force
is known nowadays under the generic term
of electron optics. As it is impossible to dis-
cuss electron optics without referring at
least briefly to the dual nature of the elec-
tron, it may be better at that point to close
the particle chapter and start the wave
chapter.
In concluding my remarks about the cor-
puscular aspects of the electron, I should
like to give a few short quotations. One is
drawn from Rosenfeld’s book Theory of
electrons:
When Thomson’s estimate of the specific charge
of the cathodic corpuscles became available, no
doubt was left as to the identity of Lorentz oscil-
lators with electrons in harmony with Thomson’s
atomic model.
My other quotation comes from Weisskopf,
a review called Recent Developments in
the theory of electron, which was published
in April 1949 in the Reviews of Modern
Physics:
There was hardly any other discovery which left
the understanding of so many and varied phe-
nomena as the discovery of the electron...It was
mainly H. A. Lorentz who brought the classical
electron theory into a consistent frame. These were
his fundamental assumptions: the electron is an
elementary particle with a charge e and a mass m;
the motion of the electrons is determined by clas-
sical mechanics if the force acting on the electron
is given by the expression:
F = eR —_— (e/c)(v xX H)
where e and v are the e charge and velocity of the
electron and E and AH are the electric and mag-
netic field strengths. The electromagnetic field in
turn is given by the Maxwell equations. -
And last but not least a few words from
Albert Einstein:
No longer ...do physicists of the younger gen-
eration fully realize, as a rule, the determinant
part which H. A. Lorentz played in the formation
of the basic principles of theoretical physics. The
reason for this curious fact is that they have ab-
sorbed Lorentz’ fundamental ideas so completely
that they are hardly able to realize to the full the
boldness of these ideas, and the simplification
AprRIL 1959
which they brought into the foundations of the
science of physics.
I should like to return now to the tabula-
tion shown at the beginning of this presenta-
tion. As we know now, the chief character-
istic of the electron, or for that matter of
any elementary particle, is the duality of
its nature. Depending upon the experiment
we carry out, it can behave either as a cor-
puscle or as a wave. It is logical now that
we consider the wave properties of the elec-
tron. I briefly mentioned earlier that the
late nineteenth century saw a clear division
of opinion about the nature of the electron
between physicists east of the Rhine and
west of the Rhine. In that respect it is in-
teresting to quote the foremost representa-
tive of the western opinion. In his classical
paper in 1897, J. J. Thomson wrote as fol-
lows:
The most diverse opinions are held as to these
rays; according to the almost unanimous opinion
of German physicists they are due to some process
in the aether to which—inasmuch as in a uniform
magnetic field their course is circular and not
rectilinear—no phenomenon hitherto observed is
analogous: another view of these rays is that, so
far from being wholly aetherial, they are in fact
wholly material, and that they mark the paths of
particles of matter charged with negative electric-
ity.
Yet Thomson’s investigations disposed of
the wave nature of the electron only tempo-
rarily. In 1924, in his famous thesis, de
Broglie reintroduced the wave concept in
the fundamental properties of the electron.
This wave, however, is something different
from that of Hertz and of Lenard. The
early wave was a truly electromagnetic
phenomenon. De Broglie’s wave is a guide
wave of the particle, not electromagnetic in
nature; it is always linked with a particle,
it cannot be dissociated from it. The ques-
tion then may legitimately arise: who were
the predecessors of this conception and how
was it born? As usual we do find ancestors
of the idea, as they are most generously
acknowledged in the same thesis of de Brog-
lie. Part of the concept goes back to Ein-
stein. Einstein in his famous paper of 1905
introduced the concept of the dual nature
of light where light behaves both as a parti-
cle and as a wave. The “needle radiation”’
concept of Einstein was hard to accept for
MARTON: MEN AND ELECTRONS
103
his contemporaries. Nevertheless, it paved
the way for de Broglie, who acknowledges
it handsomely. But this is only part of the
picture. The more important part of it is
that two important fundamental principles
of physics—that of Fermat and that of
Hamilton—Maupertuis—show more _ than
formal resemblance. On page 24 of his the-
sis, de Broglie says:
Guided by the idea of a profound identity of
the principle of least action and that of Fermat,
from the beginnings of my researches on this sub-
ject I was led to admit that,...the dynamically
possible trajectories of a mov “ine particle coincide
with the possible rays of its wave.
He is even more positive on page 35:
Fermat’s principle, applied to the phase-wave,
is identical with the principle of Maupertuis, ap-
plied to the moving particle.
The conclusion is simple:
The preceding results...establish a link be-
tween the movement of a moving particle and the
propagation of a wave.
The experimental verification was not
long in coming. The wonderful work of
Davisson, Germer, and of G. P. Thomson
is well known to everyone and does not need
to be repeated here. What needs perhaps to
be repeated is the role Elsasser played in
these investigations. Elsasser was, at the
time of de Broglie’s thesis, a young research
student, and he was the first one who found
that there may be some experimental evi-
dence in the work of Davisson and Kuns-
man for the physical existence of de Brog-
lie’s waves. In a manner of speaking, this
observation by Elsasser stimulated Davis-
son and Germer to their now classical re-
sults. I deliberately used the words “in a
manner of speaking”’ because Davisson em-
phasized that the first interpretation of El-
sasser was not quite right. I am quoting
from a note countersigned by Davisson and
published in a biography of Davisson by
K. K. Darrow.
The attention of C. J. Davisson was drawn to
W. Elsasser’s note of 1925, which he did not think
much of because he did not believe that Elsasser’s
theory of his (Davisson’s) prior results was valid.
This note had no influence on the course of the
experiments. What really started the discovery was
the well-known accident with the polycrystalline
104
mass, which suggested that single crystals would
exhibit interesting effects. When the decision was
made to experiment with the single crystal, it was
anticipated that “transparent directions” of the
lattice would be discovered. In 1926 Davisson had
the good fortune to visit England and attend the
meeting of the British Association for the Ad-
vancement of Science at Oxford. He took with
him some curves relating to the single crystal, and
they were surprisingly feeble (surprising how rarely
beams had been detected!). He showed them to
Born. to Hartree and probably to Blackett; Born
called in another Continental physicist (possibly
Franck) to view them, and there was much discus-
sion of them. On the whole of the westward trans-
atlantic voyage Davisson spent his time trying to
understand Schroedinger’s papers, as he then had
an inkling (probably derived from the Oxford dis-
cussions) that the explanation might reside in
them. In the autumn of 1926, Davisson calculated
where some of the beams ought to be, looked for
them and did not find them. He then laid out a
program of thorough search, and on 6 January 1927
got strong beams due to the line-gratings of the
surface atoms, as he showed by calculation in the
same month.
Nevertheless we have to recognize that
Elsasser’s ideas were brilliant. He men-
tioned them at that time to different people,
one of them being Einstein. Einstein’s an-
swer was: ‘Young man, you are sitting on
a gold mine.”
It so happened that the year 1924 was
also the year I finished my studies. During
the years that followed I saw an extremely
rapid change in our picture of the nature of
the electron, and with it the whole founda-
tion of physics changed. Let me mention
just a few highlights from the five years
1924 through 1928. Following de Broglie’s
thesis came Schrodinger’s famous wave
equations. The next year, 1926, saw the in-
troduction of the electron spin concept by
Uhlenbeck and Goudsmit. The years 1926
and 1927 saw the birth of electron optics,
and 1928 was the year in which Dirac pre-
sented his famous theory of the electron.
There were so many things happening in
those years that one almost forgets that
during those same years Heisenberg an-
nounced his famous indeterminacy princi-
ple.
T should like to examine a little closer one
or two aspects of this rapid evolution. First
of all, most of these discoveries affected a
much greater area of physics than the elec-
tron itself. This is in keeping with the older
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 4
tradition: many years earlier the investiga-
tions of J. J. Thomson led into considera-
tions about the structure of the atom. In a
similar way the discovery of the wave equa-
tion led Schrodinger to a much wider
investigation and much more important con-
sequences than the wave behavior of a par-
ticle alone.
An interesting example of the application
of present-day concepts is the case of elec-
tron optics. Electron optics nowadays cov-
ers a very wide field. The common interpre-
tation of this expression corresponds to the
ray optics of light and covers all phenom-
ena of the interaction of electrons with
macroscopic fields of forces. I rather like to
distinguish, in close analogy to light optics,
between two kinds of electron optics: geo-
metrical and physical electron optics. Geo-
metrical optics considers everything that
can be explained with a simple ray concept.
Physical optics requires the application of
wave principles. In this manner electron
optics, in its wider conception, represents
a very beautiful example of our present-day
concept of the electron at large. At the time
of the conception of geometrical electron
optics, some beginnings of physical elec-
tron optics existed. Scattering had been
known for a long time, and electron diffrac-
tion was just being discovered. Electron in-
terference was far in the future and so was
electron polarization. Geometrical electron
optics could very adequately have been de-
scribed in terms of particle concepts alone.
Electron ballistics could be created using
the particle concept and all the interactions
of the electron in a macroscopic field were
properly described in terms of very general
equations derived from the Lorentz equa-
tion. This description is quite adequate for
macroscopic considerations, but it cannot
represent the observed phenomena when
we reach microscopic dimensions. To ex-
plain the resolving power of an electron
microscope we must have recourse to the
wave concept. This concept also leads to the
highly satisfactory give and take which one
finds in other branches of physics. The wave
concept led us to the discovery of electron
interferences and vice versa; the observa-
tion of electron interferences gives a more
beautiful demonstration of the wave con-
Aprit 1959
cept than we had before. The recent inven-
tion of the electron interferometer at the
National Bureau of Standards and its fur-
ther development in Germany and elsewhere
is a good case in point. It shows that very
fruitful analogies can be drawn from other
branches of physics and applied to the
physics of the electron. Here an applica-
tion of electron interferometer principles
taken over from light optics has shown that
the optical path difference concept can be
extended to electron optics.
Much more could be said about the his-
tory of the electron without exhausting the
subject. I have not even touched, for in-
stance, such important matters as how Di-
rac’s theory led to the discovery of the posi-
tron or Yukawa’s theory to the discovery of
the meson. Both particles were discovered
by Anderson. The meson was originally
known under the name of “heavy electron.”
It is interesting to note that this concept is
being resuscitated in a recent note by M.
Goldhaber, who suggests that the electron
and the »-meson are two states of the same
particle. Here I am attaching a label to the
meson, and so we must distinguish between
the z- and the »-mesons. The meson theory
of nuclear forces, as we know it today, ap-
plies to the z-meson. At the time of its dis-
covery it was thought that the p»-meson
would satisfy Yukawa’s theory.
These are extremely fruitful and interest-
ing speculations, and one could spend an
enormous amount of time on them. My re-
marks may be summarized in the following
fashion: Three names stand out above the
MARTON: MEN AND ELECTRONS
105
others as the chief architects of the present
conception of the electron. These are H. A.
Lorentz, J. J. Thomson, and Louis de Brog-
lie. In emphasizing their names I do not
mean to minimize the contributions of many
others. However, I believe that conceptually
we owe these three more than we do any
other investigators.
This is the end of my story, but not that
of the electron. After having spent the even-
ing reviewing some phases of the past, I
should like to spend one more minute on the
future. For me some of the most fascinating
aspects of future work on the electron con-
cept lie in the directions indicated by the
current fight between the ‘Copenhagen
school” and the ‘“‘determinists” or ‘“positiv-
ists.” As is well known, the Copenhagen
school’s interpretation of quantum events
is a statistical one, while the opposing
school wishes to ascribe a “physical reality”
to the microevent. The arguments used in
this fight range all the way from physics
to metaphysics; from philosophy to dialec-
tical materialism. Some of the arguments
sound like a quotation from Lewis Carroll’s
The hunting of the snark:
Just the place for a Snark! I have said it twice:
That alone should encourage the crew.
Just the place for a Snark!—TI have said it thrice:
What I tell you three times is true.
My hope is, however, that this sometimes
acrimonious debate will lead us to a reform-
ulation of the concept which will be accept-
able both to the determinist and to the in-
determinist.
OO —
Wherever modern Science has exploded a superstitious fable or a pic-
turesque error, she has replaced it with a grander and even more poetical
truth—GEORGE PERKINS MARSH
106
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 4
MYCOLOGY.—Two new species of Harposporium parasitic on nematodes.
CHARLES DRECHSLER, Crops Research Division, Agricultural Research Serv-
ice, United States Department of Agriculture.
(Received February 27, 1959)
In Petri-plate cultures prepared with de-
caying plant detritus, eelworms were ob-
served undergoing destruction by two mu-
cedinaceous fungi markedly different from
any hyphomycetous parasite hitherto re-
corded as attacking nematodes. The two
fungi are herein described as new species
of Harposporium Lohde (1874) though ne1-
ther of them produces conidia of the dis-
tinctive crescentic shape signalized in the
name of that genus. However, both fungi
resemble H. anguillulae Lohde emend. Zopt
(1888), the widespread species on which the
genus was erected, in forming their conidia
for the most part on minute slender sterig-
mata arising from globose cells borne later-
ally on hyphal elements extended from
parasitized animals.
1. Harposporium baculiforme sp. nev.
Hyphae assumentes incoloratae, intra vermic-
ulos nematoideos viventes evolutae, simplices
vel ramosae, plerumque 2-4.5 crassae, primo
parce septatae sed postea ex magna parte in
cellulis 3-20y longis constantes ; genitabiles rami
externi, incolorati, clavati, saepius 4-15, longi,
basi 0.6-1.0p, lati, apice 1.5-2.5y lati, ibi aliquot
(fere 2-12) cellulas conidiferas (phialas)
ferentes; cellulae conidiferae vulgo globosae sed
interdum elongato-ellipsoidae vel obovoideae,
2.5-6u longae, 2.64, crassae, 1-2 sterigmatibus
praeditae; sterigmata vulgo 1-3, longa, circa
0.6 crassa; conidia incolorata, baculiformia, ali-
quando sursum leviter attenuata, basi et apice
rotundata, plerumque 2.5-5u4 longa, 0.7-1.5p
crassa.
Vermiculos nematoideos interficiens habitat in
foliis arborum putrescentibus prope Durango et
Steamboat Springs in Colorado.
Assimilative hyphae colorless, growing within
living nematodes, in small host animals simple
or only sparingly ramified but in larger animals
forming moderately branched mycelia, mostly 2
to 4.54 wide, at first rather scantily septate
though later becoming divided into cells mostly
3 to 20u long, from some of which lateral
branches are extended that narrowly perforate
the host integument and elongate externally into
conidiophores; conidiophores colorless, some-
what club-shaped, 4 to 1l5y long, 0.6 to 1.0yu
wide at the base, 1.5 to 2.54 wide at the tip,
whereon are borne several (mostly 2 to 12)
conidiuferous cells in loosely capitate and some-
times partly in catenulate arrangement; coni-
diuferous cells commonly globose though some-
times elongate-ellipsoidal or inverted egg-shaped,
2.5 to 4, wide and 2.5 to 6y long exclusive of
the 1 or 2 sterigmata; sterigmata commonly 1
to 3u long, about 0.64 wide; conidia colorless,
cylindrical or tapering very slightly toward the
apex, always with rounded ends, 2.5 to 5y long
and 0.7 to 1.54 wide.
Type of species: Figs. 1-14.
Harposporium baculiforme came to light in
several maize-meal-agar plate cultures which af-
ter being permeated with mycelium of Pythium
ultimum Trow had been further planted with
small quantities of leaf mold collected in woods
near Durango in southern Colorado early in July
1958. Later it appeared also in some maize-meal-
agar plate cultures that after being overgrown
by Pythium_debaryanum Hesse were further
planted with leaf mold gathered in woods near
Steamboat Springs in northern Colorado on
July 23, 1958. In both sets of cultures it sub-
sisted by parasitizing eelworms referable to a
species of Plectus. Mostly it attacked relatively
young individuals, in each instance extending
through the small animal host a single assimila-
tive hypha with scarcely any vegetative branches
(Figs. 1-5). Moderate ramification was usual
when a more robust animal was invaded (Fig.
6). An assimilative hypha could in some in-
stances be seen to have originated from a conid-
ium lodged in the forward region of the stoma
(Figs. 1, a; 5, a). A manner of initiating attack
corresponding to that found usual in my JH.
bysmatosporum (Drechsler, 1946, 1954; Asch-
ner and Kohn, 1958) was thus disclosed. Many
infected eelworms, however, did not show any
recognizable conidium within the stoma, and in
these animals the avenue of attack remained con-
jectural.
ApRIL 1959
The conidiophores of Harposporium baculi-
forme differ markedly in their small dimensions
from the robust filamentous conidiophores found
in all known congeneric forms as well as in all
known nematode-destroying members of the re-
lated Cephalosporium-Verticillium-Acrostalag-
mus series. Soon after they have been extended
from an infected animal they commonly give rise
directly from the slightly expanded tip to globose
conidiiferous cells in numbers varying from 1
to 5 (Figs. 1, b, ec; 2, a-f; 3, a-g; 4, a, b; 5, b;
6, a-c; 7-11). Some of the globose cells may give
rise to 1 or 2 others, so that usually 5 to 12 conidi-
iferous cells, interspersed with a few sterile
cells of similar subspherical shape, become as-
sembled in a loose irregular cluster. Although
the globose cells in relatively young clusters
most often bear only a single sterigma, many
cells in older clusters are provided with two
sterigmata (Fig. 11).
If left undisturbed the conidia produced on
individual sterigmata tend to cohere side by
side in compact sheaves (Fig. 12). Since usually
a large proportion of them are moved short
distances in different directions by roving eel-
worms and protozoans they commonly are seen
lying separately in haphazard disorder (Figs.
13, 14) around infected eelworms. On careful
scrutiny some appear to have a very slightly
tapering shape—a spore lp, wide at its base, for
example, diminishing to a width of 0.94 at its
rounded tip.
2. Harposporium sicyodes sp. nov.
Hyphae steriles incoloratae, intra vermiculos
nematoideos viventes evolutae, parce vel medio-
criter ramosae, primo parce septatae sed postea
in cellulis plerumque 5-20, longis et 2-4u crassis
constantes; hyphae fertiles extra animal emor-
tuum evolutae, interdum in materia animal am-
biente omnino immersae interdum omnino vel
ex magna parte procumbentes vel ascendentes,
in axe simplices vel ramosae, saepius 10-200u,
longae, in cellulis plerumque 4-25, longis et
2-3.5u latis constantes, cellula terminalis vulgo
conidia ex 1-2 sterigmatibus gignens, aliae cel-
lulae saepius 1-6 ramulos conidiferos ferentes;
ramuli conidiferi saepissime globosi sed interdum
lageniformes, plerumque 2.8-3.74 crassi, 1-2
sterigmatibus 1.2-3.74 longis et 0.6-0.8u latis
praediti, in toto vulgo 4-8, longi; conidia in-
colorata, cylindrata, recta vel leviter curvata,
DRECHSLER: NEW SPECIES OF HARPOSPORIUM
107
basi et apice rotundata, ita cucumiformia (fruc-
tui Cucumers sativi similia), plerumque 3-5y
longa, 0.9-1.2u lata.
Vermiculos nematoideos interficiens habitat in
foliis arborum putrescentibus in Arlington, Vir-
ginia.
Assimilative hyphae colorless, growing within
living nematodes, in young condition rather
sparingly septate, later becoming divided into
segments mostly 5 to 204 long and 2 to 4u
wide; conidiophores developed outside of dead
host animal, sometimes submerged and some-
times in varying measure procumbent or ascend-
ing, simple or sparingly branched, mostly 10 to
200 long, composed of cells mostly 4 to 25y
long and 2 to 3.54 wide—the terminal cell often
producing conidia on 1 or 2 sterigmata whereas
some or all of the other cells bear 1 to 6
conidiuferous branches (phialides) ; conidiuferous
branch often globose, then 2.8 to 3.7 in diam-
eter and provided with 1 or 2 sterigmata 1.2 to
3.7m long, but sometimes variously flask-shaped
and 4 to 8u in total length—the sterigma in
either instance often becoming widened at the
tip; conidia colorless, somewhat cylindrical
though tapering slightly toward both broadly
rounded ends, straight or slightly curved, hence
resembling cucumber (Cucumis sativus L.)
fruits in shape, mostly 35 to 5 long and 0.9 to
1.24 wide.
Harposporium sicyodes was found in a maize-
meal-agar plate culture that after being over-
grown with mycelium of Pythium vexans deBary
had been further planted with leaf mold taken
from woods bordering a watercourse in Arling-
ton, Virginia, on October 11, 1958. It subsisted
by parasitizing a sharp-tailed nematode which
A. L. Taylor, who kindly examined several in-
fected specimens, held probably referable to
a species of Panagrobelus. In many infected
animals a tubular connection was discernible,
though usually with some difficulty, between an
assimilative hypha and a conidium lodged in the
stoma (Figs. 15-18). Some parasitized eelworms
showed one or two ellipsoidal bodies lodged
within the oesophagus 20 to 50u from the an-
terior end. These bodies may have been swollen
infective condia but owing to their deeply im-
bedded positions the presence of hyphal con-
nections with any assimilative hypha could be
neither established nor disproved. Invasion of
the eelworm was accompanied often by pro-
nounced withdrawal of the musculature from the
108 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, No. 4
C. Drechsler
Fies. 1-14.—Harposporium baculiforme from leaf mold gathered in Colorado, partly near Steamboat
Springs (1, 4, 5, 8, 13) and partly near Durango (2, 3, 6, 7, 9-12, 14), drawn to a uniform magnification
with the aid of a camera lucida, X 1000: 1, eelworm (Plectus sp.) with infecting conidium, a, in its stoma,
and with 2 conidiophores, a and b; 2, infected eelworm (Plectus sp.) with 6 conidiophores, a-f; 3, infected
eelworm (Plectus sp.) with 7 conidiophores, a-—g; 4, infected eelworm (Plectus sp.) with 2 conidiophores,
a and b; 5, forward portion of eelworm (Plectus sp.) showing origin of assimilative hypha from conidium,
a, lodged in stoma, and a young conidiophore, b; 6, middle portion of infected eelworm (Plectus sp.)
with branched assimilative mycelium and 3 conidiophores, a—c; 7-11, conidiophores; 12, conidia cohering
in sheaves; 13, 14, two assortments of conidia, each assortment being from a separate infected eelworm.
APRIL 1959 DRECHSLER: NEW SPECIES OF HARPOSPORIUM 109
Ee
re
re
te
:
eS = om ee,
I GO Ge, gy,
ro)
See ee RTD ITD,
20 30 40u
C. Drechsler
del.
Fies. 15-25.—Harposporium sicyodes developing parasitically on an eelworm (probably Panagrobelus
sp.), drawn to a uniform magnification with the aid of a camera lucida, X 1000: 15, forward portion of
infected eelworm showing origin of assimilative mycelium from conidium lodged in stoma; 16-18, for-
ward portions of 3 infected eelworms, each showing an assimilative hypha connected with a conidiophore
and with a conidium lodged in the stoma; 19, median portion of infected eelworm with 3 conidiophores,
a-c; 20, middle portion of infected eelworm with a branched conidiophore; 21, posterior portion of a
large eelworm showing a simple conidiophore; 22-24, three assortments of conidia, each assortment being
taken from a separate eelworm; 25, eight conidia ingested by a proteomyxan rhizopod (probably Lep-
tomyxa reticulata).
110 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, NO. 4
oe \
2'e, Sell 30 e 7
Fics. 26, 27.—Proximal portions of two conidiophores of Harposporium helicoides showing, respec-
tively, 17 conidiiferous cells, a-q, and 3 conidiiferous cells, a-c, at different stages of development,
xX 1,000. Fie. 28—Detached conidia of H. helicoides, a-n, X 1,000. Fic. 29—Detached conidia of H.
oxycoracum, a-u, X 1000. Fra. 30.—Indurated hyphae of H. diceraewm within integument of an eelworm
(Plectus sp.) in a culture 65 days old, X 1,000. Fra. 31. Portions of indurated hyphae of H. diceraeum
that have given rise within integument of an eelworm to 4 new conidia about 45 days after production
of conidia on external conidiophores had ceased in the 65-day-old Petri-plate culture, X 1,000.
-
nF
pe
Ek
7
Aprit 1959
integument (Figs. 15, 16, 19, 20, 21). Develop-
ment of assimilative hyphae, especially in pos-
terior regions of large eelworm hosts (Fig. 21),
appeared rather less abundant than in nema-
todes attacked by most related parasites.
The conidiophores of Harposporium sicyodes,
like those of all congeneric species other than H.
baculiforme, are moderately stout filamentous
hyphae whether they are short (Figs. 16; 18;
19, c) or long (Figs. 17; 19, a, b; 20; 21). They
usually remain simple, yet axial branching (Fig.
20) is not exceptional among them. Their uni-
cellular conidiuferous branches, or phialides, are
mostly shaped like a Florence flask, with the
globose main part being abruptly distinct from
the narrow sterigma arising from it. In more
than a few instances, however, the distended
main part tapers upward and merges with a
distal sterigma, so that the conidiiferous cell ap-
pears transitional to the type of phialide familiar
in species of Cephalosporium and Verticillium.
The slight distension often noticeable at the
tip of a sterigma would seem to come about in
the abscission of the first conidium.
Harposporium sicyodes, like nearly all of its
known congeners, conveniently continues to pro-
duce conidia while exposed to microscopical ex-
amination in an agar slab under a cover glass.
Assortments of its conidia formed on conidi-
ophores extended from separate individual ani-
mals (Figs. 22, 23, 24) show only moderate
variability in shape and size. In my culture a
large proportion of the detached spores were
being constantly ingested by a proteomyxan
rhizopod (Fig. 25) provisionally identified as
Leptomyza reticulata Goodey (1914).
SUPPLEMENTARY OBSERVATIONS ON THREE OTHER
SPECIES OF HARPOSPORIUM
Several maize-meal-agar plate cultures which
had been planted with leaf mold of the same
collection that yielded Harposporium sicyodes
permitted abundant development of H. helicoides
Drechsler (1941). Occasion was taken to study
more closely the manner in which the phialides
of the latter species give rise to conidia (Figs.
26, a-q; 27, a-c). The individual phialide orig-
inates as a wart-like protuberance (Fig. 26, i)
that continues to grow until it reaches a di-
ameter of 3.5 to 4.54 (Fig. 26, f, 1, p, q). It then
puts forth a sterigma usually 0.7 or 0.84 wide
(Fig. 26, ec, h), which soon appears to swell
distally in forming a terminal globular knob
DRECHSLER: NEW SPECIES OF HARPOSPORIUM
JEU
often about 1.54 in width (Fig. 26, b, e). From
this globular knob is now extended a slender
outgrowth, approximately 0.54 wide, whose tu-
bular membrane is clearly continuous not with
the globular contour but with a somewhat nar-
rowing tube passing centrally through the knob
(Figs. 26, a, d, g, k, n, 0; 27, a). The outgrowth
elongates first with gradually increasing and
later with gradually diminishing width, at the
same time describing a helicoid spiral of left-
handed rotation (Figs. 26, }, m; 27, b, ce). Ulti-
mately the helicoid filament is cut off by a cross-
wall at the lower boundary of the knob and then
readily becomes detached as a conidium (Fig.
28, a-n). Manifestly the peripheral substance of
the knob is of plastic consistency, since in de-
tached spores it covers the basal membrane, and
thus persists as a minute deposit of mucus that
clothes the very slightly widening proximal end.
In all cultures the conidia of H. helicoides are
given to pronounced variations with respect to
size, some measuring as much as 48u in length
and 1.7 in greatest width, while others have
corresponding dimensions of only 20u and 0.7p,
respectively.
The conidia of Harposporium oxycoracum
Drechsler (1941) resemble those of H. helicoides
in having the slightly expanded basal end en-
veloped in a small quantity of mucus. They
often show considerably greater dimensions than
were assigned to them in the original account of
the species. Thus, among the conidia produced
by the fungus (Fig. 29, a-u) in Petri plate
cultures that had been planted with forest de-
tritus collected near Beltsville, Maryland, in
April 1958, some measured no less than 60 in
total length and fully 2.34 in greatest width.
Moreover, in many of the larger conidia not
only the tip but also a proximal portion, usually
2 to 5u in length, appeared to be filled solidly
with wall material.
The lot of forest detritus from southern Col-
orado that yielded Harposporium baculiforme
supphed also some development of H. diceraeum
Drechsler (1941) in several Petri plate cultures.
Destruction of the nematode (Plectus sp.) para-
sitized by H. diceraewum was apparently com-
pleted about 20 days after the cultures had been
prepared. When the cultures were 65 days old
all external conidiophores of the fungus, together
with all the conidia they had borne, had dis-
appeared, but within the integuments of many
parasitized animals could be seen variable por-
112
tions of somewhat indurated living mycelium
(Fig. 30). Some of the integuments loosely in-
closed a few living conidia of H. diceraewm (Fig.
3l), which in each instance must have been
recently formed on a small conidiophore ex-
tended from a single indurated segment. As the
hyphal segments here had undergone only slight
thickening of their walls and showed only faint
yellowish coloration they seemed less strongly
modified for endurance than the chlamydospores
always produced within eelworms destroyed by
H. anguilulae.
REFERENCES
AscHner, M., and Koun, S. The biology of Harpo-
sporium anguillulae. Journ. Gen. Microbiol.
19: 182-189, pls. 1-2. 1958.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 4
Drecusier, Cuartes. Some hyphomycetes para-
sitic on free-living terricolous nematodes. Phy-
topathology 31: 773-802. 1941.
. A species of Harposporium invading its
nematode host from the stoma. Bull. Torrey
Bot. Club 73: 557-564. 1946.
. Production of aerial arthrospores by Har-
posporium bysmatosporum. Bull. Torrey Bot.
Club 81: 411-413. 1954.
GoopEy, T. A preliminary communication on three
new proteomyxan rhizopods from soil. Arch.
Protistenk. 35: 80-102. 1914.
Loupe [Georc]. Ueber einige neue parasitische
Pilze. Versamml]. Deut. Naturf. und Aerzte
47: 203-206. 1874.
ZorF, WILHELM. Zur Kenntnis der Infections-
Krankheiten mnederer Thiere und Pflanzen.
Nova Acta Leop.-Carol. Deut. Acad. Naturf.
52: 314-376. 1888.
———————
GRAPHICAL DIAGNOSIS OF INTERLABORATORY TESTS
A simple way to analyze the discrepancies be-
tween different testing laboratories that presum-
ably use the same test procedure was recently
worked out at the National Bureau of Standards.’
Devised by W. J. Youden of the NBS applied
mathematics laboratory, the method employs
a graphical presentation of the test data which
allows each laboratory to tell at a glance how
its performance compares with that of others.
The graph can point the way to corrective
action to eliminate the bias, if any, in the tech-
nique used by a particular laboratory; or it may
indicate the need for an improved test pro-
cedure—one that lends itself better to uniform
application by all laboratories. In addition, it
provides an estimate of the precision of the
test-procedure results.
DISCREPANCIES, NORMAL AND ABNORMAL
Duplication of tests by two or more labora-
tories is constantly being undertaken in science
and industry in order to verify results, to de-
tect systematic errors, and in general to monitor
the techniques of measurement. Sooner or later
all important results in the physical sciences
are checked by other laboratories. In industry,
* For further technical details see the following
articles by W. J. Youden: Presentation for action,
Ind. and Eng. Chem. 50: 91A. Oct. 1958; Circum-
stances alter cases, ibid. 50: 77a. Dec. 1958; What
is a measurement? ibid. 51: Feb. 1959.
the same quality-control tests may be used by
the various plants of a single company and—
perhaps alternatively—the same acceptance tests
are performed by laboratories at different depots
of the purchaser.
In all such cases, discrepancies in the results
from different laboratories are not only expected,
but inevitable. It is basic to all measurement
processes (except those of the crudest sort or
those involving only simple counting) that when
the same procedure is repeatedly carried out
on the same specimen with the same equipment
and personnel, the results are not all identical
but are scattered over a certain range of values.
When the same measurements are made by a
number of different laboratories, using nominally
identical equipment, the scatter is even greater.
In any case, the more precise the procedure, the
narrower the range of scatter.
However, when the scatter is unusually large
or when a particular laboratory differs markedly
from most of the others, something must be
wrong. The problem—which the present method
of analysis is intended to help solve—is to deter-
mine just where the difficulty lies. The difficulty
may be due to a number of factors, some of the
most important being (1) intrinsic lack of pre-
cision in the procedure; (2) faulty technique
in carring out the procedure; (3) ambiguity or
vagueness in the formulation of the procedure,
Aprit 1959
causing differences in the way it is applied by
different laboratories; (4) differences in the
specimens measured; and (5) simple mistakes,
such as misreading a dial.
COORDINATING INDUSTRIAL TESTS
The importance of identifying the factors
responsible for the discrepancies is clear enough
in scientific research. In industry, undiagnosed
errors in the carrying out of quality-control
tests and errors intrinsic to the test procedure
itself are a severe handicap to efficient produc-
SAMPLES
OF A
OF B
MATERIAL OR BATCH B
TESTING LABORATORIES ——>
RESISREQUETS << —<—<————>
PLOT ONE POINT FOR
EACH LABORATORY,
USING ITS TEST RE-
SULTS AS COORDINATES
ee od
"B" SCALE
GRAPHICAL DIAGNOSIS OF INTERLABORATORY TEST
113
tion. To allow for testing errors, the usual prac-
tice is to aim at a higher quality product than
the specifications call for. The larger the test
errors, the greater the amount of excess quality
needed to insure that a reasonable proportion
of the finished items will pass the tests—which
are still based on the same specifications. Even
a modest improvement in the precision or in the
uniformity with which tests are carried out
could thus lead to a substantial drop in costs.
Under the stimulus of a high rate of new-
product development, much attention has re-
SSS
SIF
Lit | | |e
TO CORRESPONDING
POINTS
"AY SCALE
Fic. 1.—Statistical design for diagnosing discrepancies in results from different testing laboratories.
The interlaboratory design was developed by the National Bureau of Standards.
114
cently been given to the problem of coordinating
quality-control or acceptance tests in different
laboratories. These schemes often use advanced
statistical techniques to attack the problem with
various degrees of thoroughness, but the practi-
eal results have been generally disappointing.
Part of the difficulty seems due to the very
sophistication of the methods used. Though mod-
ern mathematical techniques have added many
powerful tools to the statistical analyst’s arsenal,
their use demands considerable skill. In contrast,
experience with the present method indicates
that in a large majority of cases it provides data
that “speak for themselves.’ However, there are
circumstances that require a more elaborate or
comprehensive interlaboratory test design; but
even in such cases the present method might
well be used for a preliminary survey of the
situation.
THE STATISTICAL DESIGN
In the present statistical design, samples of
two fairly similar materials, A and B, are sent
to the various laboratories; and each laboratory
is asked to carry out the test procedure on each
sample. The test results may be single readings
or averages, provided that the same number of
readings are used for each average. (If there are
only a few laboratories, a second pair of samples
is distributed later; this is of advantage even
when not required by the fewness of the labora-
tories.)
When the results come in they are used to
prepare a graph. The two test measurements
from each laboratory are interpreted as the
coordinates of a single point; the x-coordinate
is the test result on sample A and the y-co-
ordinate the result on sample B. There is thus
one point for each laboratory (Fig. 1).
A horizontal median line is then drawn; 1e.,
a line parallel to the x-axis and placed so that
there are as many point above the line as there
are below it. A second median line is drawn ver-
tically; i.e., parallel to the y-axis and so that
there are as many points to its left as to its
right.
For example, when two cement samples were
sent to 25 laboratories for tests of 7-day tensile
strengths, the results gave the graph shown in
Fig. 2. Here two of the laboratories were so
definitely separated from the other 23 that they
were not used in locating the median lines.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
TENSILE STRENGTH, psi
VoL. 49, No. 4
450
400
350
300 350 400
TENSILE STRENGTH, psi
Fic. 2—Plot of 7-day tensile strength of two ce-
ment samples as reported by 25 laboratories.
450
INTERPRETATION OF GRAPH
The most important general feature of the
graph is the way the points are distributed
among the four quadrants into which the graph
paper is divided by the median lines. If only
random errors of precision were present the
points should be equally numerous in all quad-
rants.
However, in all cases to which the method has
been applied thus far, there has been a more or
less definite tendency for the points to concen-
trate in the upper right and lower left quadrants.
In view of the way the points were obtained,
this means that some laboratories tend to get
high results on both samples and other labora-
PHTHALIC ANHYDRIDE ,%
(op)
6 Te 8
PHTHALIC ANHYDRIDE ,%
Fic. 3—Results of phthalic anhydride determi-
nations reported by 15 laboratories in two samples
of paint.
APRIL 1959 GRAPHICAL DIAGNOSIS
tories get low results on both samples. That is,
it indicates the presence of individual laboratory
biases. Evidence of this state of affairs is seen,
for example, in the cement tests (Fig. 2).
The more pronounced the individual labora-
tory biases, the greater the departure from uni-
form, circular distribution of the points about
the intersection of the medians. Fig. 3 illustrates
a case in which the points (with a few excep-
tions) lie in a long narrow oval with its long axis
at about 45° with the x-axis. These points were
plotted from phthalic anhydride determinations
reported by 15 laboratories on two samples of
Results of the kind shown in Fig. 3 suggest
rather clearly that the test procedure needs more
careful formulation. In its present form the pro-
cedure is apparently open to individual modi-
fications that produce differences in the results
obtained. Indeed, the more carefully each labor-
atory follows its own interpretation of the test
procedure, the more closely the points will
cluster along the 45° line.
DEVIANT LABORATORIES
Points that deviate far from the intersection
of the medians tend to fall into two categories.
Either they are far out but close to one of the
median lines or they are far out but close to the
45° line (see, e.g., Figs. 3 and 4).
In the first case, the result is fairly good on
one material and rather bad on the other. A
single instance of this kind might be due to a
simple mistake or blunder; but if the same
laboratory obtains similar results in succeeding
pairs of materials, carelessness may be the
reason.
A quite different explanation applies to a point
for out on the 45° line. Here the laboratory in
question is doing very consistent, careful work;
but it has introduced some modification into
the procedure so that the results are all too high
(or too low). A thorough check on its procedure
to discover the source of the bias is in order.
In the copy or the interlaboratory test report
that is sent to a particular laboratory, it might
be helpful to circle its point in red. This would
save the laboratory the trouble of consulting
its files to locate itself and would present a vivid
picture of its position in respect to the other
laboratories.
When an individual point is exceptionally far
from the intersection of the medians it is better
not to compress the scale in order to include it
OF INTERLABORATORY TEST
115
in the graft. As was done in the example of the
cement tests (Fig. 2), such points should be
ignored in locating the median lines.
INSOLUBLE RESIDUE ,%
) 0.1 0.2 0.3 0.4 0.5 0.6
INSOLUBLE RESIDUE ,%
Fic. 4——Percent insoluble residue in two samples
of cement as reported by 29 laboratories. Circle
has radius equal to 2.5 times the standard devia-
tion. According to elementary statistical theory,
95 percent or more of the points are expected to
fall inside the circle if there are no systematic dif-
ferences in the techniques used by the different
laboratories.
ESTIMATING PRECISION
The graphical presentation of test results,
as described above, may also give information on
the standard deviation (oc) of a single result.
An estimate of a can be obtained rather simply
if it is assumed that (1) the two materials are
sufficiently alike so that the dispersion among
the results for A should be about the same as
that for B; and (2) the differences in precision
among the various laboratories are relatively
unimportant in comparison to other sources of
difference. The first condition can be satisfied by
proper choice of the materials and experience
shows that as a rule the second condition is then
also fulfilled.
One way to get the desired estimate, under
the assumptions mentioned, is to find the aver-
age distance of the points from the 45° line
through the intersection of the medians, and then
to multiply this average by +~/ a/2 or 1.2533.
Alternatively, the same estimate can be found
by simple numerical calculations from the given
results for A and B, without having to measure
distances on the graph.
According to elementary statistical theory,
a circle centered on the intersection of the medi-
ans and having a radius of 2.5 « should contain
95 percent or more of the points provided there
are no constant errors. Laboratories whose points
116
fall outside such a circle almost certainly are
erratic or are following a procedure which de-
viates substantially from that followed by the
other laboratories.
POSSIBILITY OF SAMPLE VARIATION
Could a pattern of points like that of Fig. 2
be caused by differences in the samples? It is not
difficult to see that the answer must be in the
negative. If the stock from which the A samples
were taken were inhomogeneous, and similarly
for the B samples, then the pairs of samples
distributed to the laboratories would be of four
kinds:
high in A, high in B
high in A, low in B
low in A, high in B
low in A, low in B
Since any one of these combinations is as likely
to occur as any other, the points representing
the test results should be nearly equally divided
among the four quadrants. A concentration of
points along the 45° line can not be charged to
variation among the samples.
Cao IN CEMENT
Cao IN CEMENT
Fic. 5—Determinations by eight laboratories of
CaO in cement. The number of laboratories being
so few, each was asked to make determinations on
two pairs of samples. Hollow symbols show results
for first pair and corresponding solid symbols show
results of same laboratories on second pair of
samples. The graph indicates that the test pro-
cedure is vulnerable to individual bias. Thus, two
of the laboratories appear in the same region for
both pairs. The “circle” laboratory is very consis-
tent—and gets the highest results. The “square”
laboratory gets very low results and is not very
precise as shown by the fact that its two points
(hollow and solid squares) are farther apart than
are the pairs for other laboratories.
JOURNAL OF THE WASINGTON ACADEMY OF SCIENCES
VoL. 49, No. 4
However, if there is a roughly circular dis-
tribution of points, but with a disappointly wide
scatter, the diagram does not reveal whether this
arises from sampling difficulties or from poor
precision in testing. Further light on this prob-
lem can be obtained by a modification in the
method of assigning samples. If there are 2N
laboratories, N double-size samples of each ma-
terial are prepared. By mixing or otherwise, it
should be possible to divide each double-size
sample into two closely matching halves. The
samples are now distributed in such a way that
if the two halves of a particular double sample
of A go to laboratories X and Y, then these
same laboratories receive the two halves of a
double sample of B.
If sample variation is the trouble, the points
in the new graph will tend to appear as N closely
spaced pairs—like double stars in the heavens.
On the other hand, if the points corresponding
to the two halves of a double-size sample are
separated as much (on the average) as points
from different double samples, the scatter cannot
be ascribed to sample heterogeneity.
SUMMARY OF ADVANTAGES
The present interlaboratory test scheme re-
quires of each laboratory the relatively light task
of measuring only two samples; and the colla-
tion of test results involves a minimum of com-
putation. Interpretation of the graph requires
no professional statistical background to follow
the reasoning; yet it permits a fairly searching
examination of the test procedure itself and of
the way it has been carried out by the individual
laboratories.
Directions for improvement are clearly indi-
cated. A long narrow ellipse directs attention to
a more careful description of the procedure or
even to the need for its modification. Points far
out and near one of the medians indicate erratic
work; points far out along the 45° line are
strong evidence of deviations from specified pro-
cedure. Use of a circle with a radius of 2.5 o
shows the individual laboratory whether or not
its technique has in some way become saddled
with .a substantial constant error. Experience
has already shown that a certain few labora-
tories turn up all too frequently in the most
distant positions from the intersection of the
medians. Improved performance from those few
laboratories may go far to restore confidence in
a test procedure.
Aprit 1959
GURNEY: A NEW GRASSHOPPER
ilsty/
ENTOMOLOGY.—A new grasshopper of the genus Achurum from eastern Texas
(Orthoptera: Acrididae). ASHLEY B. GurRNEY, Entomology Research Division,
United States Department of Agriculture.
(Recieved February 18, 1959)
One of the most distinctive genera of
North American grasshoppers is Achurum
Saussure,! characterized by a very slender
and elongate body and an _ extremely
oblique, or ventrally “undercut,” face. An
individual clinging parallel to a grass stem
with its antennae extended forward would
scarcely be distinguishable from the vegeta-
tion. Since the publication of Hebard’s re-
view of the genus (Trans. Amer. Ent. Soc.
48: 89-93. 1922), the genotype, A. sumi-
chrastt (Saussure), has been the only in-
cluded species. It was shown in habitus il-
lustration by Ball et al. (Univ. Arizona
Techn. Bull. 93: 287. 1942). The characters
of the genus were also treated by Hebard in
his key to Nearctic genera of Acridinae
(Trans. Amer. Ent. Soc. 52: 47-59. 1926).
Though of distinctive appearance, speci-
mens of Achurum are uncommon, and in the
United States swmichrasti is known only in
southeastern Arizona and _ southwestern
Texas.
For the privilege of studying the new spe-
cies here described I am very grateful to
John R. Hilliard, of the staff of McMurry
College, Abilene, Tex., who collected all the
material, and to whom I am glad to dedicate
the species in recognition of his unpublished
studies of grasshoppers and in appreciation
of his cooperation. I am also grateful to
J. A. G. Rehn, Academy of Natural Sciences
of Philadelphia, for the loan of specimens
of sumichrasti needed for comparative pur-
poses to supplement specimens in the U. 8.
National Museum.
The new species averages larger than
sumichrasti, and it is separated by differ-
ences which in the main are subtle rather
than striking. The most noticeable differ-
ences are that the male subgenital plate of
hillardi is more elongate and acute and the
fastigium of the vertex has wider marginal
areas.
1 Saussure (Rev. Mag. Zool. 1861:313) adapted the
name Achurum from the “Greek” achyron, mean-
ing chaff, husk, or scale.
Achurum hilliardi, n. sp.
Figs. 1,2, 6, 8, 9, 11, 18
Male (holotype): General appearance much
as in sumichrasti; fully winged. Apex of fastig-
ium in dorsal view angulate rather than evenly
rounded (usually but not always true of swmi-
chrasti), and with marginal areas laterad of im-
pressed longitudinal grooves (Figs. 5, 6, /g) wider
than in sumichrasti, in lateral view with lateral
margins decurved at apex (Fig. 1, Jm) and with
portion of frontal costa (fc) anterior to anten-
nal bases obtuse-angulate rather than more
broadly rounded as usual in swmichrastz.
Pronotum, tegmina, and wings essentially as
in sumichrasti; hind femur with both mesal and
lateral dorsal and ventral genicular lobes pro-
duced toothliike somewhat longer than in sumi-
chrasti (Figs. 2, 3); hind tibia with variable
number of spines (left: 17 lateral, 22 mesal, one
apical on mesal only; right: 16 lateral, 19 mesal,
one apical on each side), apical spurs similar to
those of swmichrastz.
Subgenital plate apically produced, not es-
sentially triangularly acute in lateral view as in
sumichrasti (Figs. 7, 8); supra-anal plate (epi-
proct) elongate (Fig. 9); cercus slender, elon-
gate, as in sumichrasti; (phallic complex not
extracted, described under variation below from
paratypes).
Coloration: In general pale brown; antennae
and compound eyes reddish brown; dorsal sur-
faces of closed tegmina much paler than lateral
surfaces; dorsal surface of pronotum somewhat
paler than lateral lobes, latter with conspicuous
blackish spot near anterior margin, another spot
near posterior margin (Fig. 1); hind femur with
tiny dark spots (10 left, 12 right) along the mid-
longitudinal line of the lateral (outer) paginal
area, both mesal and lateral genicular disk with
blackish spot at anterior margin (Fig. 2, sp.).
Measurements (length in millimeters) : Body,
32.2; antenna, 14.0; fastigium anterior to com-
pound eyes, 2.5: pronotum, 4.7; tegmen, 28.0;
hind femur, 14.5; greatest width of hind femur,
1S:
Variation among other specimens: The shape
118 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, NO. 4
Fries. 1-13.—1, Achurum hilliardi, n. sp., lateral view of head and prothorax of holotype, only bases
of antenna and leg shown; 2, A. hilliardi, apical portion of left hind femur of holotype; 3, A. swmichrasti
(Saussure), same view as Fig. 2, male from Cuernavaca, Mexico; 4, A. sumichrasiz, laterial view of apical
portion of head of male from Baboquivari Mountains, Ariz.; 5, A. swmichrasti, dorsal view of anterior
portion of head, same specimen as Fig. 4; 6, A. hilliardz, same view as Fig. 5, holotype; 7, A. sumichrastz,
lateral view of apical portion of abdomen, male from Fort Grant, Ariz.; 8, A. hilliardz, same view as
Fig. 7, holotype; 9, A. hilliardi, dorsal view of apex of abdomen, holotype; 10, A. swmichrastz, dorsal
view of epiphallus, KOH preparation, male from Baboquivari Mountains, Ariz.; 11, A. hilliardi, same
view as Fig. 10, paratype; 12, A. swmichrasti, lateral view of aedeagus, KOH preparation, same specimen
as Fig. 10; 13, A. hilliardi, lateral view of aedeagus, KOH preparation, paratype. (fc, frontal costa;
ig, longitudinal groove of fastigium; /k, lateral knob of epiphallus; lm, lateral margin of fastigium;
mk, mesal knob of epiphallus; sp, dark spot on genicular disk.) (Drawings by author.)
Aprit 1959
of the fastigium in dorsal view varies somewhat
among the paratypes, but in none is it evenly
rounded at the apex as is usual in swmichrasti.
In lateral view the position of the frontal costa
anterior to the antennal bases is always decidedly
obtuse-angulate, but specimens of swmichrasti
occasionally are sufficiently angulate so that this
feature is not a constant separating character.
Spines along the hind tibia vary as follows as
regards extremes and averages: Lateral, 13-18,
av. 16.1; mesal, 17-21, av. 18.9. In contrast, the
tibial spines of 9 males of swmichrasti from
Texas, Arizona, and Mexico have been examined
with the following corresponding results: Lat-
eral, 13-16, av. 14.8; mesal, 16-20, av. 17.7. The
apex of the supra-anal plate is weakly sclerotized
and consequently the length of the organ varies,
but in most specimens an acute apical portion
is moderately developed. This organ in sumi-
chrasti is very similar, not always as short and
blunt as might be inferred from Hebard’s de-
scription (Trans. Amer. Ent. Soc. 48: 93. 1922).
The female nymphs (not considered paratypes)
show a very elongate second portion of the su-
pra-anal plate similar to that described and
figured for suwmichrasti by Hebard.
The phallic complex of four paratypes has
been examined and compared with examples of
sumichrasti. The shapes of the aedeagal valves
may differ slightly in the two species (Figs. 12,
13), but individual variation in preparations ap-
pears to render separation on this basis uncer-
tain. Figs. 10 and 11 depict epiphalli of swm-
chrasti and hilliardi, and the limited dissections
made indicate that differences occur in the mesal
and lateral knobs of the lophus. The lateral
knob of hilliardi (Fig. 11, /k) is more evenly
rounded when seen in lateral view than that of
sumichrasti, which is rather abruptly terminated
at its anterior margin. The mesal knob of hilli-
ard: (mk) apparently is less produced mesally
than that of swmichrasti.
The general coloration of the paratypes is
comparatively uniform, but two specimens lack
dark spots on the lateral paginal area of the
hind femur, and one of them has the two dark
spots on the lateral lobe of the pronotum ob-
solete.
Measurements (extremes and averages, in
millimeters) of the paratypes are as follows:
Body, 29.0-33.0, av. 31.6; antenna, 13.5-15.5,
av. 14.1; fastigium anterior to eyes, 2.3-2.6, av.
2.5; pronotum, 4.3-4.9, av. 4.6; tegmen 27.4—
GURNEY: A NEW GRASSHOPPER
119
30.5, av. 28.7; hind femur, 14.5-15.0, av. 14.8;
greatest width of hind femur, 1.6-1.8, av. 1.75.
To show the average larger size of hilliardi, 14
males of sumichrasti from localities throughout
the latter’s range have been measured for three
dimensions, with results as follows: Pronotum,
3.6-4.6, av. 4.1; tegmen, 22.0-28.0, av. 25.8;
hind femur, 11.5-14.0, av. 13.1. It should be
noted that tegmen length has been measured
“from the distal extremity of the tubercle formed
by the junction of the subcostal and radial veins”
to the extreme tip. (Proc. 4th Internat. Locust
Conference, Cairo: 97. 1937). Dirsh (Anti-
Locust Bull. 16, fig. 1. 1953) illustrated this di-
mension.
Type: U.S. National Museum no. 61125.
Type locality: A bog 2 miles south of Warren,
Tyler Company, Tex.
The holotype male, 8 male paratypes, and 3
females apparently in the instar preceding ma-
turity bear identical data, having been taken
at the type locality April 24, 1955, by J. R. Hilh-
ard. Paratypes will be deposited in the collec-
tion of Mr. Hilliard, and those of the Academy
of Natural Sciences of Philadelphia, the Univer-
sity of Michigan, and the U. S. National Mu-
seum.
Mr. Hilliard has furnished the following eco-
logical notes:
The site is located just off U. S. Highway
287/69. The lumber road leading to the collection
site turns off the main highway 2 miles south of
Warren, Tyler, Tex. The specific area is a low, wet,
boggy meadow just across the Texas and New
Orleans Railroad tracks and includes the railroad
right of way. The area is an open meadow dotted
with crayfish chimneys. The fine, light sandy soil
supports a lush growth of sedges, grasses, and nu-
merous clumps of the pitcherplant Sarracenia
sledget McFarlane. The adjacent wooded area con-
sists of pine, oak, and magnolia.
This locality 1s a part of Tharp’s region no. 1,
the Longleaf Pine Region of Texas (Vegetational
Regions of Texas, in Texas range grasses, by B. C.
Tharp, 1952). According to Tharp’s map of the
average annual precipitation, which is adapted
from Climate and man (Yearbook of Agriculture,
1941), the average annual precipitation in this re-
gion would be between 48 and 50 inches.
The habitat of hilliardi apparently contrasts
sharply with that of swmichrasti; the latter has
seldom been discussed, but so far as recorded it
is much different from the boggy environment
occupied by hilliardi. Hebard (1. ¢.: 93) stated
that Rehn captured a single specimen while
beating bear grass (Nolina sp.) in the Sierritas
120 JOURNAL OF THE
Mountains, Ariz. Ball (Journ. Econ. Ent. 29:
680. 19386) said that it feeds on broom rape
(Andropogon barbinodis Lag.), and in 1942
(Ball et al., 1. c.: 286) stated that it is found on
“coarse grasses on rocky slopes in desert grass-
land of the Lower and Upper Sonoran zones of
southeastern Arizona.” In the Chinati Moun-
tains near Shafter, Tex., Tinkham (Amer. Midl.
Nat. 40: 565, 574. 1948) found a localized colony
in tall grass at the bottom of a steep cut on the
slope of a high plateau at about 5,500 feet ele-
vation, and his figure 24 is a photograph of the
habitat.
The distribution of suwmichrasti was stated
by Ball et al. (1. c.: 286) as “Southeastern Ari-
zona west to the Baboquivari and Quinlan
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, NO. 4
Mountains; north to the Catalina and Pinaleno
Mountains ...southwestern Texas, and south to
Mexico and Guatemala.” Texas records are
limited to Jeff Davis, Brewster, and Presidio
Counties. Specimens from El Salvador (L. Olo-
mega, Dept. San Miguel) and Nicaragua (Ma-
nagua) are in the U. 8. National Museum, but
there is no information about the ecological con-
ditions of the localities where they were taken.
Saussure (1. c.: 313) originally described sumi-
chrasti from temperate Mexico, and Tinkham
(1. c.: 646) regarded it in the United States as
belonging to the Mexican Upper Sonoran fauna.
Coahuila and Veracruz are nearer to eastern
Texas than any other Mexican areas from which
sumichrasti has been recorded.
a i
BIRD MIGRATION STUDIES
Some of the familiar present-day mass bird
migrations in spring and autumn may stem from
habit developed during forced ebb and flow of
avian populations in the Pleistocene or Ice Age,
which ended 30,000 years or less ago. In some
way the migratory instinct seems to have been
built into the annual life cycle of the species.
This thesis is discussed by Dr. Alexander Wet-
more, Smithsonian Institution research associate,
in a publication recently issued by the Institu-
tion. It appears to be corroborated, he says, by
the route patterns of migrations from different
parts of North America.
“Among the multitudes of migrants that come
south into Central America,’ Dr. Wetmore says,
“eastern and western species mix in abundance
as far as southern Guatemala. Farther south,
eastern species predominate, and comparatively
few of those that nest between the Rocky Moun-
tains and the Pacific coast reach the Isthmus of
Panama.
“The ice front of the last glacial period in the
eastern half of North America extended south
to Long Island, the Ohio Valley, and the Missouri
River above St. Louis, with consequent displace-
ment of Temperate Zone conditions far south-
ward. In the west, where the ice front lay a
relatively short distance below the United States-
Canadian boundary, pressures toward the south
would have been far less severe. Eastern species
either had to cross the water barrier of the Gulf
or to follow the shoreline west and southwest,
and so tended to penetrate farther into Central
America. Western populations on the other hand
had necessity for shifts of less extent.”
One interesting migration, Dr. Wetmore says,
is that of certain species of vireos. The red-eyed
vireo breeds commonly over a wide area from
British Columbia to Nova Scotia and south to
Texas and central Florida. In the fall this vast
group of individuals goes south to winter in the
upper basin of the Amazon. A closely related
species, the yellow-green vireo, nests in the Trop-
ics from Mexico to Panama. This bird certainly
has no need for a seasonal migration because of
climate. But it migrates also in September and
October to join the redeyes in the upper Amazon.
Another, the black-whiskered vireo, nests in
southern Florida and the West Indies, where cold
of changing seasons is never a problem. But most
of these birds also migrate into the same general
region as their relatives.
“We may theorize,’ says Dr. Wetmore, “that
there is some tie for this habit back to Pleistocene
climatic conditions. This appears clear in the
case of the red-eyed vireo, but obscure with the
others that now nest in regions that are tropical.
It seems possible that during the period of the
Wisconsin ice sheet temperature conditions in
these areas of the northern Tropics were so dif-
ferent that an annual migration was established
which now continues though there is no apparent
present necessity for it.”
History of the northward surges of bird popu-
lations may be repeating itself today, the orni-
thologist points out. During the past century
weather records in the Northern Hemisphere
APRIL 1959
show a slight but steady advance of warmer
temperatures toward the north. The shift seems
to have been accelerated in the past 30 years.
Slowly birds are following the change that this
brings. In Iceland it is reported that due to
warmer conditions in the past 50 years, indicated
by retreat of glacial ice and the decrease of the
ice pack on the northern coast, seven species of
birds have been added to the breeding popula-
tion. These include such diverse forms as the
starling, short-eared owl, herring gull, and tufted
duck. There also has been an increase in migrant
species and in those that remain through the
winter.
EXCAVATIONS AT LA VENTA
121
In Greenland there has been recorded a more
interesting instance. Twenty years ago there
was a chance invasion of a flock of fieldfares, an
Old World thrush that nests in birch and conif-
erous forests of northern Europe and north-
western Siberia, ranging north nearly to the tree
line. Wanderers remained in southern Greenland
to establish a breeding colony, thus populating
a land area quite remote from their previous
range. Some Greenland birds migrate in fall to
return in spring, but the fieldfare, although a
migrant in its proper home in northern Eurasia,
remains a resident in southern Greenland.
EE
EXCAVATIONS AT LA VENTA
On an inland island, a dry land area of about 2
square miles surrounded by a jungle swamp in
southeastern Mexico, stood, between 2,000 and
3,000 years ago, one of the great religious centers
of the aboriginal New World. It consisted of a
stone pyramid 103 feet high and with a base of
more than 10,000 square feet, a ceremonial court
where rites were conducted and sacrifices made to
a fantastic jaguar god, and various other struc-
tures. This was the La Venta site in the Tabasco
province near Veracruz, chief extant monument
of the mysterious Olmec people who apparently
evolved a civilization roughly contemporaneous
with, but quite distinct from, those of the Mayas
and Incas to the south. They preceded by many
centuries the Aztecs whose culture was dominant
in Mexico at the time of the first European ex-
plorations.
The La Venta site has been the scene of ex-
eavations by archeologists for nearly 20 years.
Latest of these was the uncovering of the cere-
monial court, just north of the great pyramid,
by a cooperative expedition of the Smithsonian
Institution, the National Geographic Society, and
the University of California, under the direction
of Dr. Philip Drucker, Smithsonian archeologist,
and Dr. Robert F. Heizer of the University of
California. It was a mammoth job, carried out
with pick, shovel, and wheelbarrow—for machin-
ery could not be brought into the site—by a labor
force of 50 men in 100 days. Helpful advice and
assistance were provided by the Instituto Na-
cional de Antropologia e Historia and the Museo
Nacional de Antropologia of Mexico.
The joint report on this work, by Drs.
Drucker, Heizer, and Robert J. Squier, has re-
cently been published by the Smithsonian’s
Bureau of American Ethnology. The findings
throw considerable new light on the ways of life,
especially the religious practices, of the Olmec
people. Datings by the carbon-14 technique show
that artifacts found there covered a range be-
tween about 2,300 and 3,000 years ago. This is
essentially contemporaneous with the Maya cul-
tures of Yucatan and Guatemala. Still, very
little is yet known as to the vanished Olmecs who
had disappeared long before the 16th century,
essentially “without a history” and leaving almost
no clues as to their identity. A little, however,
can be reconstructed from the results of these
investigations. La Venta, the authors hold, was
a ceremonial center operated by a small group of
priests, or priest-kings—and their personal ser-
vants, supported by tributes from villages in the
general vicinity and with large labor forces re-
cruited from these same villages. Even after the
original construction, the excavations show, much
labor was essential for repair and maintenance.
The fact that the site was in continuous use for
about 400 years is a clear indication of extraordi-
nary cultural stability and singleness of purpose.
The Olmec religion must, at the time of the begin-
ning of the site, have already been a well-worked-
out system which had sufficient meaning, tradition,
and purpose to insure its continuance for nearly
half a millennium.
That the society which built and gloried in the
La Venta site had an agricultural economy seems
quite likely, although we have no direct evidence.
No actual remains of maize have been found al-
though the mano and metate, usually associated
with maize agriculture, do occur. That this culture
group had master artisans who could sculpture
basalt, work jade, and polish metallic mirrors is
established. But all this tells us little else than the
fact that...some rather elaborate sociopolitical]
or socioreligious organization was in existence.
JOURNAL OF THE
ZOOLOGY
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 4
Taxonomy of the copepod genera Pherma and Pestifer. R. U. Goop-
ING, University of Washington. (Communicated by Fenner A. Chace, Jr.)
(Received February 2, 1959)
In 1923, C. B. Wilson instituted the genus
Pherma for a new species of copepod, P.
curticaudatum, specimens of which had been
collected from an annelid off the coast of
Lower California. He placed it in the
Clausiidae, a family containing a number
of other annelid associates. However, in
revising this group, M. 8S. Wilson and Illg
(1955: 135) considered that “it would be
impossible to assign (Pherma) to any fam-
ily, since C. B. Wilson omitted a description
of the oral appendages.”
Twenty-one years later, in a paper pub-
lished posthumously, C. B. Wilson (1944)
described another new genus, Pestifer (with
genotype P. agilis also from an annelid but
in the Gulf of Mexico), which he referred
this time to the Clausidiidae. Again the
mouthparts were not discussed.
His descriptions of these two species were
sufficiently similar for Wilson and Illg (loc.
cit.) to suggest an investigation into their
possible congeneracy. Accordingly, advan-
tage was taken of a visit to the United
States National Museum in September 1958
to pursue this problem (as part of a tax-
onomic analysis of the Clausidiidae, on
which I am currently engaged) Examination
of the type material available there of both
Wilson’s genera indicated that a single spe-
cies is represented; this is redescribed.
Pherma curticaudatum C. B. Wilson, 1923
Synonym.—Pestifer agilis C. B. Wilson, 1944:
546-547, pl. 31, figs. 165-171.
Material examined —The syntypes are “three
adult females, one of which bore egg strings...
from the parapodia of an unnamed annelid,
dredged from a depth of 645 fms. by the Bureau
of Fisheries steamer ‘Albatross’ off the coast
of lower California in April, 1911. These ...are
deposited in...the American Museum of Natu-
ral History (Cat. No. 4617). (Wilson, 1923.)
Two specimens—one ovigerous but without
maxillipeds, the other lacking the cephalosome
and one of each of the three pairs of swimming
legs—were found in the U.S. National Museum
collections (no. 59354: the label with them also
lists the Albatross station number as D5685) ;
both were dissected for study. The third is still
in the original repository. It was examined with-
out dissection after clearing in methyl] salicylate.
This specimen lacks only the right maxilliped
and caudal rami but unfortunately, in the course
of preparation, broke in half.
The other specimens studied were two females,
from the skin of an annelid dredged near the
Tortugas Islands, Gulf of Mexico, in 380 fath-
oms, July 18, 1932; USNM no. 79641. Although
Wilson (1944) lists one of these as the holotype
of Pestifer agilis, both were included in the same
vial. It is possible that the female which I dis-
sected is the one on which most of Wilson’s
drawings were based, since it was devoid of one
of each pair of the appendages he figured and
both maxillipeds. The other was examined as a
temporary whole mount in lactic acid; one max-
illiped and both ovisaecs have been removed dur-
ing the course of this investigation.
To simplify reference to these specimens,
the following abbreviations are used: “Ph. 1,”
the ovigerous Pherma female; “Ph. 2,” the muti-
lated Pherma female; “Ph. 3,” the Pherma fe-
male in the American Museum; “Pe. 1,” the
relatively undamaged Pestifer female; and “Pe.
2,” the Pestifer female which I (and Wilson?)
have dissected.
Female —Wilson’s figure of the habitus (1923,
fig. 1)* is better than any which could be at-
tempted with the existing material; it shows
very well the delimitation of the first pedigerous
segment both from the second and from the
cephalosome,’ the remainder of the metasome
swollen and fused into a single mass whose
three constituent segments are indicated by con-
strictions at approximately equidistant intervals
along the body, and the abrupt narrowing at the
origin of the 3-segmented urosome. Lacking,
however, is any clear indication that the first
segment of the urosome is set off from the last
* All references to figure numbers from C. B.
Wilson’s papers have here been placed in boldface
type.
* The latter division, as he mentions in the text,
is absent on the ventral side.
APRIL 1959
metasomal segment; a definite line of thickening
does in fact occur at this point. The dorsal
boundary between the genital and anal segments
is also less well defined than shown in his draw-
ings.
Another fact which he does not mention or
indicate in his figures is that the genital segment
can be seen in ventral view (Fig. 16) to have an
irregular thickened line, running transversely
just anterior to the openings of the oviducts,
which divides it into an anterior and a posterior
part. In the latter of these, two dark areas
(which may represent paired seminal recepta-
cles) show up very distinctly even in cleared
specimens.
The caudal rami (Fig. 9) are neither “jointed”
(Wilson, 1944) nor “destitute of setae” (Wilson,
1923). This confusion has evidently arisen be-
cause the middle seta of the three terminal ones
on each ramus is enlarged nearly to the diameter
of the ramus itself. There is a slight transverse
constriction in its proximal portion which prob-
ably corresponds to the end of the basal “peg”
characteristic of one or two of the terminal
caudal setae in less modified copepods. The other
two setae at the end of each caudal ramus are
slender and, in most of the specimens, lie close
to the shaft of the main one, so that it is not
easy to determine their exact lengths. There are
also two short setae on the outer face of the
ramus, both in the distal half, and one dorsally—
all slender and inconspicuous.
The considerable difference between the
lengths which Wilson gives for the body of
curticaudatum (440 mm) and of agilis (6.24
mm) is not shown by the specimens. It was
difficult to make measurements since the only
whole animals curved; rough estimates, for
which a ruler and dissecting microscope were
used, indicate that Ph. 3 was about 4.5 mm long
(without caudal rami) and Pe. 1 more than 3.7
mm. Since the metasome and urosome of Pe. 2
are of comparable size to those of Pe. 1, it is
probable that Wilson’s first figure is the more
accurate.
In all the specimens which possessed a cepha-
losome there is a groove separating the anterior
part of the ventral surface from the wide, non-
protuberant rostrum (Fig. 10). The “ventral
cephalic shield” so delimited partially overhangs
(in ventral view) the lateral depressions where
the antennules and antennae insert, and its
border continues thereafter as a thickened ridge,
GOODING: TAXONOMY OF PHERMA
123
terminating eventually at the extreme posterior
corner of each maxilla (Fig. 11).
No postoral protuberance, between the max-
ilipeds and first pair of legs, could be distin-
guished.
The antennules are slender structures with six
podomeres (Fig. 1). No evidence could be found
for the division of the basal podomere into the
two short ones shown by Wilson (1944, pl. 31,
fig. 167)—no doubt the reason why he termed
this appendage 7-segmented—nor for his claim
(loc. cit., p. 547) that “the only setae are termi-
nal on the end segment.” The pattern appeared
to vary among the specimens; its most complete
form (Ph. 1, left) was—proximal to distal podo-
meres: 2, 6, 3, 2, 2 plus 1 aesthete, and 7 plus
1 aesthete.
The antennae (Fig. 2) may have three or
four podomeres, since the division between the
third and fourth—a line at best—is sometimes
completely absent. The terminal armature ac-
cords well with what I consider to be basic
among poecilostomes: a row of curved setae
(here three instead of the more usual four)
between, on the one side, two more slender setae,
which are located in a depression behind the tip
of the appendage toward its outer face, and one
more distally placed on the other; but that on
the third podomere is reduced to a single seta,
usually accompanied by three small elements.
Nothing could be found on the first two podo-
meres. It is possible that Wilson (1944) partially
confused the antennae with the maxillipeds since,
in his generic diagnosis of Pestifer (p. 546), he
speaks of them as “prehensile” and figures (pl.
31, fig. 168) what is obviously the other append-
age under the title “second antenna”.
The mouth is placed more anteriorly than is
usual in copepods (under the median part of
the labrum in Fig. 11). In ventral view the
labrum forms a shallow, wide area with thick-
ened exoskeleton; its posterior edge is broken
by three projections. The middle one of these
has heavily sclerotized sides but a thin ventral
surface, so that it generally appears medially
incised rather than, as is in fact the case, pos-
teriorly acuminate especially if viewed from be-
hind instead of ventrally. In the latter aspect
it may be seen to be divided for most of its
length by a line parallel to the sides. This medial
structure appears to correspond to the labral
area of more typical poecilostomes, while the two
lateral “hooks,” which extend backward nearly
124
to the maxillae, are a distinctive feature of
curticaudatum. Under each is a local modifica-
tion of the ventral exoskeleton (its outline shown
dashed on the right side of Fig. 11) which fits
into the depression in the anterior surface of the
mandible. A fleshy, protuberant structure aris-
ing just posterior to the angle of the maxillae
(and presumably preventing excess posterior
movement in these) is believed to represent the
labium. The heavily sclerotized borders around
the bases of the maxillae fuse medially to delimit
the labrum from an anterior, triangular area
which continues uninterrupted to the mouth. In
it, at the level of the median maxillar insertions,
is a longitudinal ridge bearing, like the surround-
ing parts of this surface, a few tiny spinules.
Nothing resembling characteristic paragnaths
could be found but two small flaps clothed in
short cilia occur—one on either side of the mid-
line—under the inner lobes of the maxillules
(and thus hidden by them in Fig. 11).
The mandible is oriented with its flat surface
almost parallel to the plane of the mouth re-
gion, the main shaft extending forward at an
angle of about 45° to the transverse and the tip
curving backward (Fig. 11). Terminally (Figs.
3, 4) it bears a stout curved spine, with a
toothed flange on its ventral side, and a short
fimbriate lamella, both articulating with the
body of the appendage and pointing somewhat
posteriorly. As is typical in clausiids, the ap-
pendage is small and, in an undissected specimen,
very difficult to distinguish under the labrum
and inner lobe of the maxillules.
The maxillules (Fig. 5) are unimerous but
bilobed: the outer, bearing three setae, is thinly
sclerotized and protrudes in a transversely pos-
teroventral direction from the lower side of the
appendage, while the two setae of the inner lobe
—one covering the other in a ventral view—
extend toward the mouth. One or more of these
setae on both lobes sometimes could not be dis-
cerned: this is presumed due to variation, to the
hazards of dissection, or to difficulties in obser-
vation.
The maxillae (Fig. 6) insert over a consider-
able area of the cephalosome. They appear to
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 4
resemble closely the same pair of appendages
in Clausia (Giesbrecht, 1893), and, like these,
their segmentation is difficult to distinguish. It
seems probable that each has two podomeres, the
basal being greatly expanded, the distal inserted
eccentrically upon it and bearing a thickly spinu-
lose dorsal lobe. Neither podomere is armed in
the conventional fashion, but it is possible that
the dorsal lobe, which appears to articulate at
its base, represents a modification of the terminal
armature. One may speculate that, by grinding
the tips of this pair of appendages together, the
animal could triturate the relatively soft skin
of its host and feed on the resultant debris.
The maxillipeds form the main prehensile
apparatus. Each is strongly developed and te-
tramerous (Fig. 7). The first two podomeres are
somewhat inflated and the fourth produced into
a strong, tapering, hooklike structure. Patches
of fine spinules on the inner surface of the first
and second podomeres represent the only orna-
mentation. The armature consists of a short seta
on the inner surface of the fourth podomere and
a small element near the inner curvature of the
hook.
Despite Wilson’s statement (1944: 546, 547),
there are only three pairs of legs on the meta-
some, no trace being found of the fourth. Each
is small and is borne just anterior to the middle
of its respective somite. The legs are biramous,
the two rami and the protopodite having two
podomeres respectively, although the division
between those of the endopodite is sometimes
very difficult to distinguish. The armature is
somewhat irregular: the basic pattern appears
to be:
prot. endp. exop.
1 2 1 2 1 2
Leg 1 ==, 7 1: 1-. 6-. => 4Ve
Leg 2 -- -1. = 2 2bn— -I. 4 III.
Leg 3 == =1. 1-. 4-. = 1. kee
but, as shown in Figs. 12-14, this may vary even
between the legs of a single pair. The main dif-
ferences occur in the second legs, where the last
podomere of the endopod may have four (Ph. 2,
left leg), five (Ph. 1, L; Ph. 3, both legs; Pe. 1)
B; Pe. 2, L), or six setae (Ph. 1, R) and that
Fies. 1-9.—Pherma curticaudatum Wilson, female: 1, Left antennule, ventral; 2, left antenna, dorsal;
3, tip of left mandible, ventral; 4, left mandible, dorsal; 5, left maxillule, dorsal; 6, left maxilla, dorsal;
7, right maxilliped, medial aspect; 8, right sixth leg and adjacent structures, ventral; 9, left caudal
ramus, dorsal. (Figs. 1, 2, 4-6, 9, and 12-16 are of Ph.1; 10 of Ph.3; 11 of Pe.1; and 3, 7, and 8 of Pe. 2.
A camera lucida was used for Figs. 10 and 11; the others were drawn with a carbon-arc type of projection
apparatus. Scales refer to the figure (or figures) nearest them, and were made from a stage micrometer.)
125
GOODING: TAXONOMY OF PHERMA
ApRIL 1959
(See opposite page for legend).
Figs. 1-9.
126
of the exopod three (Ph. 1, R; Ph. 2, L) or
four (Ph. 1,09; Pi. 3,8; Pesta Pee ee)
It is interesting to note that on the exopod spines
of all the legs distal setules—so characteristic a
feature in a number of poecilostome genera that
they may represent a primitive tendency in this
group—are present (Fig. 15).
The fifth pair of legs is completely lacking,
but sixth legs are considered to be represented
in some of the specimens by a small stout seta
just anterior to the origin of the ovisacs on either
side of the genital segment (Fig. 8).
Male—No male was present in either of the
collections, and I know of no account in the liter-
ature of a copepod which could be so assigned.
This is unfortunate since a knowledge of the
morphology of males from each locality might
do much to clear up the taxonomic dilemma
posed in the next section.
Remarks—There seems little doubt that the
genera Pestifer and Pherma are synonymous, but
I should like to consider briefly the reasons why
I have identified Pe. agilis with Ph. curticauda-
tum. As noted in the description, the available
specimens exhibit differences in the armature of
the antennules, antennae, maxillules, and met-
asomal legs, in the segmentation of the antennae
and legs, and in the shape of the ovisacs. None
of the first six characters is apparently consist-
ent within the specimens of one species, and vari-
ation may occur even between the appendages
on opposite sides of the same animal. In some
of the cases where changes in armature are in-
volved it has been possible to infer accidental
loss of certain setae.
The last of the differences (shape of the ovi-
sacs) 1s evident from a comparison of Wilson’s
(1923) fig. 1 and (1944) pl. 31, fig. 165, and
borne out by my examination of his specimens.
Although there is usually considerable variation
in the form of the ovisaes even in a single popu-
lation of a particular copepod, the mean may
prove valid as one of the complex of characters
which distinguishes that species. But here only
one representative in each collection possessed
intact ovisaes. I should not like to diagnose two
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 4
species on such a basis, particularly since the
specimens are from different geographical areas
and might thus be expected to show some slight
variation.
Comparative zoogeography, however, suggests
that the two collections are more likely to rep-
resent different species than to compromise a
single one and, although this argument is purely
inferential, it seems suitable to consider it here.
According to Ekman (1953), archibenthal ani-
mals (both curticaudatum and agilis fall into
this category) show only limited distribution
patterns. If one assumes that the depth at which
these copepods were found represents their
lower limit, then there still exists evidence that
the tropical shelf fauna on either side of Central
America possesses many more pairs of closely
related species than forms with an amphi-
American range, and that the latter are all very
ancient. (Paleontological information about
copepods is almost nonexistent.) Even if these
copepods extend into the abyssal region, a con-
tinuous distribution is not very probable. Nor
do their hosts provide more assistance on this
topic since neither was identified further than
to group.
The position is, then, that on morphological
grounds the available material appears to repre-
sent a single species whose phenotypic variation
is not in excess of that to be expected in an
animal modified for a strictly associated exist-
ence, nor does it provide a basis for specific
separation. On the other hand, the locations
from which the specimens were collected might
lead one to expect the presence of two similar
species. The number of specimens is too small
to decide conclusively between these alternatives.
But, since copepod taxonomy is still dependent
almost entirely on morphological criteria, the
former has seemed preferable. I shall thus leave
to some future worker, with more material at his
disposal, the onus of proving that speciation or
subspeciation has occurred in Pherma curticau-
datum (in which case Wilson’s name agilis may
be revived for the West Indian form).
It seems possible now to refer Pherma to the
Fries. 10-16.—Pherma curticaudatum Wilson, female: 10, View of the anterior part of the cephalosome
from the left side, showing groove between rostrum and mouth area, and insertions of the antennule and
antenna; 11, ventral view of the anterior part of the cephalosome: the mandible and framework around
the base of the maxilla are shown on the right side of the figure; the bases of the antennule and antenna,
the maxillule and maxilla on the left; 12, first pair of legs and coxal plate, ventral; 13, second pair of
legs and coxal plate, ventral; 14, third pair of legs and coxal plate, ventral; 15, detail of tip of terminal
exopod spine on leg 3; 16, part of urosome, ventral. (In Figs. 12-14, certain elements of the armature
whose absence in the specimen from which they were drawn is presumed to be accidental have been
indicated by dashed outlines. Figs. 10 and 11 are somewhat diagrammatic.)
APRIL 1959
12
GOODING: TAXONOMY OF PHERMA
O-lmm
Fias. 10-16.—(See opposite page for legend).
128
Clausudae, a step which makes some changes
necessary in the present definition of that family
(M. 8. Wilson and Illg, 1955). Treatment of
this will be deferred to a later paper.
This study was begun at the U.S. National
Museum and completed in the Department
of Biology, Boston University; it has been
supported in part by a research grant to
Dr. Paul Illg from the State of Washington
Initiative 171 Fund for Research in Biology
and Medicine. My thanks are due to the
authorities of the institutions mentioned
for the use of their facilities, and to Dr.
Libbie Hyman and Dr. Thomas Bowman
for their assistance in obtaining type ma-
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 4
terial on loan. Dr. Illg and Dr. Arthur
Humes have been kind enough to read and
criticize the manuscript.
LITERATURE CITED
EKMAN, SVEN. Zoogeography of the sea: xiv + 417
pp. London, 1953.
GresBRECHT, WILHELM. Mittheilungen iiber Cope-
poden. Mitt. zool. Stat. Neapel 11: 56-106. (5.
Clausia lubbockii Claparéde: S. 79-83.) 1893.
WILson, CHARLES BrancH. A new genus and species
of parasitic copepod from Lower California.
Amer. Mus. Novit. 81: 4 pp. 1923.
. Parasitic copepods in the United States
National Museum. Proc. U. S. Nat. Mus. 94:
529-582. 1944.
Wixson, Miprep S., anp Inte, Paut L. The family
Clausudae (Copepoda, Cyclopoida). Proc. Biol.
Soc. Washington 68: 129-142. 1955.
EEE
DR. FRIEDMANN AWARDED ELIOT MEDAL
Dr. HerBerRT FRIEDMANN, acting head cura-
tor, department of zoology, U. 8S. National Mu-
seum, Smithsonian Institution, has recently re-
ceived the Daniel Giraud Elhot Medal of the
National Academy of Sciences for his book The
honey-guides. The Elliot Medal is awarded for
the most meritorious work in zoology or paleon-
tology published each year.
Dr. Friedmann’s studies of the honey-guide,
issued by the Smithsonian, clarified several puz-
zling problems about these birds. Prior to this
work it was thought that the birds fed chiefly on
the honey and bee larvae in wild bees’ nests, but
being unable to open such nests by themselves,
the birds led or guided humans to the hives
(hence the name honey-guide), and then after
the men had taken their fill, they came back to
feed on the remnants left strewn about. Since
the only use to the bird of the guiding habit de-
pended upon the cooperation of a totally inde-
pendent creature, man, the habit could not have
had any value until it was perfected by both
participants, and in such a way as to help the
birds. It was found that the African natives de-
liberately substituted themselves for the original
“partner” of the bird, the ratel or honey-badger.
The guiding behavior, which appears so pur-
posive, is merely an excitement reaction of the
bird when it meets with a potential foraging as-
sociate, and which calms down when it sees or
hears bees. Since this usually happens near a
bees’ nest, the effect is that the follower is usually
led to a hive. Many observations show that the
behavior is purely instinctive and involves no
“planning” or preknowledge by the bird. It was
also found that the birds’ interest in the hives was
in the wax of the comb not in the honey or bee
larvae. Studies showed that the birds depend on
was-splitting microbes in their digestive tracts to
make the wax digestible.
Born in New York City April 22, 1900, Dr.
Friedmann took his undergraduate training at
City College in New York and received his Ph.D.
in ornithology from Cornell University in 1923.
He was a National Research Council fellow at
Harvard University from 1923 to 1926, an in-
structor at Brown University, 1926-27, and at
Amherst College, 1927-29. He has been a curator
in the Division of Birds at the U. S. National
Museum since 1929. He is the author of many
ornithological works, including The parasitic
cuckoos of Africa, Monograph No. 1 of the Wash-
ington Academy of Sciences.
Officers of the Washington Academy of Sciences
WeMUStUCHE...--+......... Py oe: FRANK L. CamMpBELL, National Research Council
President-elect................ LAWRENCE A. Woop, National Bureau of Standards
2) FIG. oc poten ee Heinz Specut, National Institutes of Health
LLU. ag W. G. BrompBacHerR, National Bureau of Standards
NRERUUPSE 265.1... 5. - Morris C. Lrrxinp, Armed Forces Institute of Pathology
Cusiodrvan of Publications............... Haraup A. REHDER, U.S. National Museum
LOST ue aco deee CuestER H. Paces, National Bureau of Standards
LOPES 0 1 a er H. A. Bortuwick, T. D. Stewart
OES 1) Bovurpon F. ScriBNeR, KeitrH C. JOHNSON
NGHORGETS (OT9O". .0 0. oe wee eens Puitip H. ABELSON, Howarp S. RApPpLEYE
Board of Managers....All the above officers plus the vice-presidents representing the
affiliated societies
CHAIRMEN OF COMMITTEES
Standing Committees
OO 2 PLS oh eee FRANK L. CAMPBELL, National Research Council
. PCT. RatpH B. KENNARD, American University
Membership............ LAWRENCE M. KusHNER, National Bureau of Standards
POMGPTAPUS, ..'............. ..Dran B. Cowir, Carnegie Institution of Washington
Awards for Scientific Achievement....... FRANK A. BIBERSTEIN, Catholic University
Grants-in-aid for Research...... B. D. Van Evera, George Washington University
Policy and Planning.............. MarGARET Pittman, National Institutes of Health
Encouragement of Science Talent.............. Leo ScHusertT, American University
Science Education............ RayMonp J. SEEGER, National Science Foundation
Wiaveraud Meéans.............. RussELL B. STEVENS, George Washington University
Pee eIALIONS. ........5. 00 cece cence JouN K. Taytor, National Bureau of Standards
Special Committees
Lo LEWES ool Oa Harotp H. SHEeparp, U. 8. Department of Agriculture
MPeetOry.....:......... JamMES I. HamBueton, U.S. Department of Agriculture (Ret.)
ihibrary of Congress......... ee ee Joon A. O’Kerrre, National Aeronautics and
Space Administration
CONTENTS
Page
SCIENCE AND EDUCATION in the Washington area. FRANK L. CAMPBELL. 97
PHysics.—Men and electrons. L. MARTON................ ee 98
Myco.tocy.—Two new species of Harposporium parasitic on nematodes.
CHARLES DRECHSLER. ..!i¢2... 5. ..44 0. poate 106
ENToMoLoGy.—A new grasshopper of the genus Achurum from eastern
Texas (Orthoptera: Acrididae). AsHLEY B. GURNEY............ 117
ZooLtocy.—Taxonomy of the copepod genera Pherma and Pesizfer.
R. Us -Goopin@ 2.03 ee ore i ee a eee 122
Notes anp NEws:
Graphical diagnosis of interlaboratory tests.................... 112
Bird migration studies... 2.52)... 4% a0 0-a hee Boe ee 120
Excavations at. La, Venta... 2. $2 6s. yn sco) bee 2 pA
“Ho,
JY:
Da
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JOURNAL
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Vou. 49
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No. 5
HISTORY OF SCIENCE—Franklin as a physicist! RAyMonp J. SEEGER, Na-
tional Science Foundation.
(Received April 17, 1959)
There are many souvenirs of Benjamin
Franklin (1706-1790) .?
There are also many portraits, some of
them famous. For example, the White House
library contains the 1759 portrait done by
Benjamin Wilson (1721-1788) in Philadel-
phia, the only nonpresidential one there. It
was taken by Maj. John André during the
American Revolution and then sent to Eng-
land. The family of Sir Charles Grey, who
had been in charge of the troop evacuation
from Philadelphia at that time, presented it
in 1906 to the White House. Harvard Uni-
versity boasts the earliest known (Sumner)
portrait, made in 1748 by Robert Febe in
1Based upon talks given at meetings of the
American Association for the Advancement of Sci-
ence (Section L, 1936) and the Philosophical So-
ciety of Washington (1956).
2 Pamphlets by the National Franklin Commit-
tee of the Franklin Institute (Philadelphia, 1956) :
Life of Benjamin Franklin (year by year, 1706-
1790); H. B. Auten, Philosopher with a twinkle in
his eye; E. T. Benson, The foundation for peace
grows on the farm; Benjamin Franklin, innovator ;
Benjamin Franklin: Printing and the graphic arts ;
Benjamin Franklin, the well-doer; Benjamin
Franklin and aeronautics; Benjamin Franklin and
business; Benjamin Franklin and economics ; Ben-
jamin Franklin and education; Benjamin Frank-
lin and electricity ; Benjamin Franklin and meteor-
ology; Benjamin Franklin and the mutual
philosophy. ;
Convorcet, M. J. A. N. pr, Hloge de M. Franklin
lu a la séance publique de lV Académie des Sciences.
Paris, 1790.
Crane, V. W., Benjamin Franklin. Baltimore,
1936.
Van Doren, C., Benjamin Franklin. New York,
1938
Forp, P. L., The many-sided Franklin. New
York, 1899.
FRANKLIN, W. T., Wemoirs of the life and writ-
ings of Benjamin Franklin. London, 1833.
SmitH, W., Eulogium on Benjamin Franklin.
Philadelphia, 1792.
Philadelphia. In the Pennsylvania Academy
of Fine Arts there is David Martin’s
“thumb” portrait, done in 1767. The New
York City Metropolitan Museum of Art has
the portrait by Joseph S. Duplessis of Paris,
a picture of Franklin in 1778, the year of his
presentation at the Versailles Court. In 1955
the Duplessis 1779 portrait was placed in
Independence Hall by Harry 8. Truman;
it had been given in 1945 by Charles de
Gaulle. This picture had originally belonged
to Madame Claude Adrien Hevetius, who
had received it from Franklin. The famous
portrait done by J. Wright in 1782 hangs in
the Royal Society of London.
Franklin statues, too, adorn our public
squares and parks throughout the nation.
In front of the City Hall of Boston a statue
portrays Franklin the printer in the front
and the kite experiment in the rear, the 1783
Treaty of Paris and the Declaration of In-
dependence on the sides. The statue at the
Philadelphia Post Office in 1906 honored
Franklin as “admired for talent’; a large
one is in Franklin Hall of the Franklin In-
stitute. In Washington a statue commemo-
rates Franklin, on one side as a philosopher,
on another as a patriot, on the third as a
philanthropist, and in the front as a printer.
In the east room of the White House, there
is a Limoge porcelain bust of Franklin to-
gether with busts of Washington, Jefferson,
and Lincoln; they were presented by France
to Theodore Roosevelt during his term as
President. The choice of a statue of Frank-
lin to guard the entrance of the Palmer
Physical Laboratory together with one of
Joseph Henry (1797-1878) presents an in-
teresting enigma. Henry’s association with
129
SMITHSC
meri rE
INS TIT :
130
Princeton University is well known. What,
if any was Franklin’s connection?
Perhaps the most personal souvenirs of
Franklin are his writings.? At the age of 23
he suggested for his own epitaph: “The
Body of Franklin, Printer.” In his will he
declared, “I, Benjamin Franklin, Printer,
Late Minister Plenipotentiary for the U.S.A.
to the Court of France.” John Bartram once
remarked that Franklin was the only person
in Philadelphia who had made a success of
the printing trade. He was appointed public
printer for the Middle Atlantic States. Poor
Richard’s Almanac (1733, et al.) could well
be taken as an American symbol of a local
boy making good—without the benefit of
formal education. We are all familiar with
his Autobiography, called by Carl Van
Doren “‘a masterpiece of memory and hon-
esty.” (Unfortunately, it was left incom-
plete as of 1757.) The Saturday Evening
Post, which owed its origin to the Pennsyl-
vania Gazette established in 1728, still car-
ries the caption ‘Founded by Benjamin
Franklin.” I wrote recently to Ben Hibbs,
its editor, to inquire if the Post had ever
published an article on Franklin’s interest
in physics. The answer was, “No record in
our files!” To me this is prima-facie evi-
dence of the neglect of Franklin as a physi-
cist. Because of a general fear of his un-
predictable puns, he was not invited in 1776
to participate in writing the Declaration of
Independence; although he was the oldest
member of the Second Continental Con-
gress. Incidentally, he was also the oldest
member of the Constitutional Convention
(1787). Honoré de Balzac (1799-1850) once
remarked that Franklin was the inventor
of the lightning rod, the hoax, and the re-
publi.
In connection with science Franklin is
commonly regarded as a gadgeteer. We re-
eall the Franklin stove, or Pennsylvania
* Sparks, J.. Works of Benjamin Franklin. Bos-
ton, 1844.
Franklin Papers, including I. Minis Hays’s Cal-
endar (1908), at the American Philosophical So-
nee W.C., list of the Benjamin Franklin Pa-
pers in the Library of Congress. 1905.
George Simpson Eddy Collection of Princeton
University on Benjamin Franklin. —
_ Benjamin Franklin Collection of Yale Univer-
sity.
JOURNAL OF THE WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 5
fireplace, which he invented in order to re-
tain heat and at the same time to provide
fresh air by converting most of the smoke
into flame. It was his first invention (1742).
The Metropolitan Museum of Art has a
1795 model of such a stove that was com-
pleted in 1773. Another famous invention
of Franklin was his modification (1759) of
the so-called armonica, a specimen of which
is in the Boston Museum of Fine Arts. It
consisted of 37 glass hemispheres, of differ-
ent diameters, attached to an iron spindle
controlled by a belt and treadle. By means
of a finger or light drum stick one could
cause these glass hemispheres to vibrate (a
keyboard was added later). Wolfgang
Amadeus Mozart (1756-1791) and Ludwig
van Beethoven (1770-1827) both composed
music for it; for example, Mozart’s Adagio
and Rondo in C. Franklin’s mahogany chair
with a ladder beneath the cowhide seat is
an equally famous invention; the American
Philosophical Society has one that was con-
structed in 1785. Most of us, however, are
more familiar with the bifocals which were
made in 1784 for Franklin by a Paris op-
tician, after he had been using ordinary
spectacles for 25 years. Franklin wrote hu-
morously to George Whately the next year,
“T understand French better by the help of
my spectacles.” At the age of 80 he invented
an instrument for taking down books from
high shelves—later used frequently by gro-
cers,
His formal education having been com-
pleted at the age of 10, Franklin then
learned his trade—and thus acquired some
important skills. He said later, “It has been
useful to me to construct little machines
for my experiments, while the intention of
making the experiments was fresh and warm
in my mind.” (See the Franklin machine at
the Franklin Institute and the one at the
American Philosophical Society in Philadel-
phia—invented by Philip Syng (1703—-
1789), Junto member.) Some instruments
invented by him for the lectures of Ebe-
nezer Kinnersley are at Harvard Univer-
sity*; for example, the profile of a house
* KINNERSLEY, E., A course of experiments in
electricity. Philadelphia, 1764.
CouHEN, I. B., Some early tools of American sci-
ence. Cambridge, 1950.
May 1959
that had a lightning rod grounded by means
of a square that popped out in case of an in-
complete circuit. The celebrated “Thunder
House,” purchased in 1789 from the Rev.
John Prince of Salem, contained a small
charge of gunpowder that made the house
collapse if a short circuit occurred from the
lightning rod to the ground.
Even when we do think of Franklin as a
scientist we are apt to regard him primarily
as an amateur. In “The Amateur in Sci-
ence,” of the July 1956 issue of Endeavour,
an amateur was defined as ‘‘one for whom
the pursuit of science is a secondary activity
in life.” In this sense Franklin was certainly
an amateur. In those days, however, the
frontiers of many sciences were so vaguely
defined by the newly developing profes-
sional domains that it was easy for amateurs
to reach vantage points in a relatively short
time and to direct important advances. It is
still possible today in those scientific areas
where observational experience is still more
necessary than precise experiments. As we
have accelerated the expansion of knowl-
edge with refined and quantitative appara-
tus, it has become less probable for ama-
teurs to make much headway—for instance,
nowadays in physics and in chemistry—but
a phenomenon like tribo-electricity (cf. Jo-
han C. Wilcke’s (1732-1796) tribo-electric
series, 1757) still challenges our understand-
ing.
As an amateur Franklin was particularly
active in the formation of learned societies,”
notable among these being his Junto (cor-
rupt for Junta, 1.e., council), which was or-
ganized in 1727 and which met Friday
evening as does the present Philosophical
Society of Washington. There were only 10
members; increase in membership was pro-
vided through the organization of subordi-
nate clubs. This group, sometimes called the
Leather Apron Club, did represent a re-
markable combination of mechanics and
sages. For example, it included Thomas
Godfrey, a glazier; Michael Scull, a sur-
veyor; William Parsons, a shoemaker; and
William Maueridge, a joiner. These individ-
uals were wont to discuss questions of natu-
ral philosophy, politics, and morals. They
° Lince.pacH, W. E., Franklin and the scientific
societies. Journ. Franklin Inst. 261. 1956.
SEEGER: FRANKLIN AS A PHYSICIST
151
prepared and read papers. (The compara-
tively rare informal communications of the
Philosophical Society of Washington are in
the same tradition.) They would discuss
such questions as: “What is the reason the
tides rise higher in the Bay of Fundy than
the Bay of Delaware? Why does the flame
of a candle tend upward in a spiral? Whence
comes the dew that stands on the outside of
a tankard that has cold water in it in the
summer-time?” To nonmembers they ad-
dressed this mind-searching question: ‘Do
you love truth, for truth’s sake?” In 1748,
with the Royal Society of London as a
model, there was a “proposal for promoting
useful knowledge among the British Plan-
tations in America.” In this document it was
argued “that one society be formed of vir-
tuosi or ingenious men residing in several
colonies to be called the American Philo-
sophical Society, who are to maintain cor-
respondence.” The Penn family proceeded
later to “pack” the society, so that it de-
clined about 1762 and had to be revived
about 1766. Meanwhile, however, in 1750 a
young Junto, including two of Franklin’s
sons, became organized as the ‘“American So-
ciety for Promoting and Propagating Useful
Knowledge.” It combined in 1768 with the
other organization to form the present Amer-
ican Philosophical Society for Promoting
Useful Knowledge; Franklin was the first
president of the enlarged group.
Sometimes we forget that Philadelphia,
being the second largest city in the whole
British Empire, was a significant cultural
center during this colonial period. The Li-
brary Company of Philadelphia (organized
in 1731) had one of the best collections of
scientific books in the country. For example,
its first order, in 1732, included William J.
’sGravesande’s Mathematical elements of
natural philosophy (1726), Herman Boer-
haaves’s A new method of chemistry (1727),
Hayes’s Fluxions, Drake’s Anatomy,
L’Hospital’s Conic sections, and Deshall’s
EKuclid. Despite his apparently poor prepar-
atory education, Franklin read much. Peter
Collinson presented him with the Philoso-
phiae naturalis mathematica principia of
Sir Isaac Newton (1642-1727). By 1740 he
had read ’sGravesande’s book on natural
philosophy and Boerhaave’s one on chemis-
JOURNAL OF THE
try, as well as Stephen Hale’s Statical essays
(1738), J. T. Desagulier’s A course of natu-
ral philosophy (1738), and Newton’s Optics
(1728). It may be recalled that he and Ben-
jamin Thompson, Count Rumford (1753-
1814), both attended lectures of John Win-
throp (1714-1779) at Harvard.®
Notable among Franklin’s scientific ac-
tivities were the contacts he maintained
with European scientists.‘ Prior to 1728,
seven of the eight Americans elected to the
Royal Society of London had been Bos-
tonians. (It is truly remarkable that Boston
did not develop science more at that time.)
During this period, to be sure, the Royal
Society elected nonscientists as well as sci-
entists, in a ratio of about two to one. Physi-
cians were the largest single group (their
election was a tribute to the broad scientific
training they had received); they included
such individuals as Sir William Watson
(1715-1787), Sir John Pringle (1707-1782),
John Fothergill (1712-1780), and John Mit-
chell (1680-1772). On Franklin’s first trip
abroad he met Sir Hans Sloane (1660-1753),
physician, naturalist, and secretary and
later president of the Royal Society, and
sold him an asbestos purse. About the same
time he met also Henry Pemberton (1694—
1771), Gresham professor of physics and
editor of the third edition of the Philoso-
phiae naturalis mathematica principia, and
popularizer of Newton’s ideas. Another
noted European was Peter Collinson (1694—
1768), gentleman, Quaker, gardner, botanist,
and a merchant of cloth; he became a fellow
of the Royal Society in 1728 and a member
of its council in 1732. Franklin’s friends in-
cluded Fothergill; Erasmus Darwin (1731-
1802), physician and botanist, poet, and
“The Sage of Lichfield’—not to mention
his being the grandfather of Charles Dar-
win; Capt. James Cook (1728-1779), for
whose letter of safety he received in 1779 a
Cook gold medal from the Royal Society;
James Watt (1736-1819); Joseph Black
(1728-1799) ; Sir Wilham Herschel (1738-
1822) ; and the Reverend Dr. Joseph Priest-
* BrascH, F. E., John Winthrop, America’s first
astronomer and the science of his period. Astron.
Soc. Pacific. 1916.
“METROPOLITAN MuvusEUM oF ArT,
Benjamin
Franklin and his circle. New York, 1936.
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 5
ley (17338-1804), a kindred devotee of in-
tellectual, political, and religious freedom,
who claimed to have become interested in
science by meeting Franklin in 1765 and
who was urged by him to write a famous
history of electricity.®
Franklin was equally active in maintain-
ing contacts with American scientists.® For
example, he was the one who first sent from
Europe seeds of Chinese rhubarb, Scotch
cabbage, and kohlrabi. He encouraged John
Bartram (1699-1777), whom Carolus Lin-
naeus (1707-1778) called “the greatest liv-
ing natural botanist.” In 1749 an electrical
machine was given by him to Yale Uni-
versity ; 1t had to be replenished in 1789 and
is now in the collection there. In 1758 a
machine was sent to Winthrop; it was lost
in the Harvard Hall (library) fire of 1764.
Wherever Franklin lived he became a source
of scientific communication. He _ corre-
sponded with almost every scientist of note
on the two continents.
If we do think of Franklin as more than
an amateur in science, we are inclined to
stress his interest in useful knowledge.!® He
is regarded as a utilitarian par excellence. In
this connection one quotes from Franklin’s
1749 “Opinions and Conjectures” in the
April 29, 1750, letter to Collinson, two years
after his beginning experiments with electric
phenomena: “Nor is it of much importance
to us to know the manner in which nature
executes her laws; it is of real use to know
that china left in the air unsupported will
fall and break, but how it comes to fall, and
why it breaks, are matters of speculation.
Tis indeed a pleasure indeed to know them,
but we can preserve our china without it,”
and, in the last paragraph, ‘‘Chagrined a
little that we have been hitherto able to
produce nothing in this way of use to man-
kind.” In a letter (September 20, 1761) to
Mary Stevenson he wrote: ‘What signifies
philosophy that does not apply to some
use?” It will be recalled that Francis Ba-
con,'' the great promoter of science, was
* PRIESTLEY, J., The present state and history of
electricity. London, 1767.
° HENDLE, B., The pursuit of science in Revolu-
tionary America. Chapel Hill, 1956.
** PLEDGE, H.8., Science since 1500. London, 1940.
za FARRINGTON, Be Francis Bacon, philosopher of
industrial science. New Y ork, 1949.
May 1959
also a prophet of the usefulness of science.
It became an article of faith in the eight-
eenth-century age of enlightenment that
science should be applicable to the improve-
ment of the natural conditions of life. More-
over, the British wars, which had been going
on with Spain since 1739 and with France
since 1744, emphasized economic needs.
With respect to pupils in academies, Frank-
lin once remarked, “It would be well if they
could be taught everything that is useful
and everything that is ornamental.” As to
the current Harvard education, he did ob-
serve, “They learn little more than how to
earry themselves handsomely and enter a
room genteely and from whence they return,
after an abundance of trouble and change, as
great blockheads as ever, only more proud
and self conceited.” Colleges in those days
were created primarily for the dissemination
of knowledge (particularly theological) and
not for creative research. In his own think-
ing, however, Franklin was concerned first
of all with the quest for knowledge and then
only with a search for its usefulness. He
was not purely utilitarian, otherwise he
would not at all have become interested in
electrical phenomena. In June 1783 in con-
nection with the first balloon experiment of
Jacques Etienne Montgolfier (1745-1799)
and Joseph Michel Montgolfier (1740-
1810), we recall his celebrated comment:
“What is the use of a balloon? What is the
use of a new born baby?” Franklin certainly
did not follow his investigations primarily
for personal gains.!* He refused the invita-
tion of the Pennsylvania Governor to patent
his stove. He was a genuine scientist, al-
though he was undoubtedly first of all a
citizen. For example, his “Plain Truth” grew
out of his concern about the French and
Spanish privateers which were harboring
within 20 miles of Philadelphia in 1747.
Let us look briefly at Franklin as he was
viewed by his contemporaries. As for honors,
he received a master of arts degree from
Harvard in July 17583, its first honorary de-
gree in the European sense. In September of
that same year he received a master of arts
degree from Yale and in 1756 a master of
arts degree from the College of William and
” CoHEN, I. B., Franklin and the twentieth cen-
tury. Journ. Franklin Inst. 261: 289. 1956.
SEEGER: FRANKLIN AS A PHYSICIST
133
Mary'?—the only honorary degree granted
by that institution prior to the Revolution.
In 1759 he received an LL.D. from St.
Andrews and in 1762 a D.C.L. from Oxford.
On November 30, 1753, he became the first
foreigner to receive the Sir Godfrey Copley
Medal of the Royal Society of London. In
1756 he became a member of the Royal
Society through the initiative of Watson.
His admission, indeed, was somewhat unique
in that he was able to qualify without peti-
tioning, without signing the charter book,
and even without paying the normal fee. He
was made a council member in 1760, 1765,
1766, and 1762. In 1772 he became one of
the eight foreign associates of the Académie
Royale des Sciences—the next American to
become a member was the Swiss-born Jean
Louis Rodolphe Agassiz (1807-1873), 100
years later (1872). He was elected to 24
scientific and educational societies, includ-
ing the Russian Academy of Sciences. Many
claims were made on behalf of Franklin. He
was called the “modern Prometheus” by
Immanuel Kant (1724-1804), the “father of
electricity” by the Reverend William Stuke-
ley (1685-1765), the “Newton of the age,”
the “Newton of electricity.” The physiocrat
Anne Robert Jacques Turgot, Baron de
PAulne (1727-1781), wrote, “Eripuit coelo
fulmen, sceptrumque tyrannis.” John Adams
(1735-1826) said, ‘His reputation was more
universal than that of Leibniz or Newton,
Frederick or Voltaire; and his character
more beloved and esteemed than any or all
of them.” Priestley remarked that the kite
experiment was “‘the greatest that has been
made in the whole compass of philosophy
since the time of Newton.” Franklin, it must
be emphasized, was investigating electricity
when world-wide knowledge of it had public
interest at a peak. Electrical phenomena
were awe-inspiring; they produced an effect
on the public mind akin to that of the atomic
bomb and more recently of Sputnik. In a
letter of April 15, 1759, van Musschenbroek
advised Franklin, “I should wish, however,
that you would go on making experiments
entirely on your own initiative, and thereby
pursue a path entirely different from that of
the Europeans, for you shall certainly find
many other things which have been hidden
8 William and Mary Quart. 2: 208. 1894.
154
to natural philosophers through the space
of centuries.”” Franklin was not hampered
by conventions, by concepts, or even by
language itself. But the glamor of lightning
flashes, of cloud electrification, and of the
lightning rod has always overshadowed his
real contributions.
How has Franklin been regarded in the
light of history? There is an anonymous
letter to Benjamin Franklin, LL.D., F.RS.,
1777, entitled “In which his Pretensions to
the Title of Natural Philosopher are Con-
sidered.” The writer compared Franklin and
Newton; he felt the latter better qualified as
a scientist because he was ‘skilled in the
science of magnitude and number.” It is
noteworthy that the Newtonian period in
American science was much more prevalent
in Boston than in Philadelphia. I. Bernard
Cohen has written a suggestive article on
Franklin as a Newtonian scientist.1* He
focused attention to two seemingly different
Newtons. The one personality apparently
was responsible for the Principia; a work
couched in Latin, a work concerned with
theory and mathematics, a work which con-
cluded with the system of the world. The
other Newton evidently wrote the Optics in
English; he dealt essentially with experimen-
tal observations; he ended it with queries
and hypotheses. In short, the Optics was not
a completed theoretical synthesis based upon
established experimental optical facts.
Franklin’s own misunderstanding of New-
tonian mechanics was notorious (ef. his 1747
letter to Cadwallader Colden (1688-1776) ).
Franklin, it is true, did emphasize the im-
portance of experiments. In this sense he was
truly a Newtonian; some of his speculations
were similar to Newton’s queries. I am con-
vineed, however, that Newton was Newton
—a single, but complex personality. The ap-
CoHeN, I. B., Benjamin Franklin: An experi-
mental Newton scientist. Bull. Amer. Acad. Arts
and Sci. 2. Jan. 1952.
Subsequent to my talks I read with interest
Cohen’s more recent publication on Franklin and
Newton (Philadelphia, 1956). He makes a plausi-
ble case for the eighteenth-century high regard of
Franklin as a Newtonian in the Optics tradition—
perhaps, at the expense of depreciating Newton as
a mathematical physicist. In this instance I my-
self am inclined to weigh more heavily the unique-
ness of the individual’s imagination than the de-
velopment of social speculations, although I
recognize everyone’s indebtedness to his philo-
sophical heritage and to his cultural environment.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 5
parent difference in his approaches to me-
chanics and to optics was inherent more in
the subject matter than in himself. In both
cases he started with experimental concepts,
sought simple relations and then attempted
to create a deductive system from a few ax-
iomatie first principles.
In later years Franklin’s work has not
always been held in the highest esteem.
William Whewell (1794-1866) ,!° who fa-
vored the two-fluid theory, accordingly was
opposed to Franklin. Even in 1928 Willis
Steel concluded in his Benjamin Franklin of
Paris that “the man of science regards quiz-
zically this ancient’s inventions and _ so-
called discoveries.” In the first presidential
address!® of the American Physical Society,
Henry Augustus Rowland (1848-1901) ob-
served that there had been only four signifi-
cant contributions to physics by Americans
in the early days, namely, those made by
Franklin, Rumford, Henry, and Mayer. At
the fiftieth anniversary of the Society, Gor-
don Ferrie Hull commented thus on the in-
clusion of Franklin: “Never heard of as a
scientist 1f not known as publisher, states-
man and publicist.” Basil F. J. Schonland,
on the other hand, has argued that the “‘one-
fluid theory—is today the electron theory of
matter.”?* John Trowbridge (1848-1923) **
noted in 1917, ‘‘The position of Franklin
among the greatest men of electricity in the
estimation of scholars is as follows; Frank-
lin, Cavendish, Maxwell, Faraday.” Sir
Joseph John Thomson (1856-1940) has
emphasized that “the service which Frank-
lin’s one-fluid theory has rendered to the
science of electricity by suggesting and co-
ordinating researches can hardly be over-
estimated.” I doubt if many of us would
agree with Robert Andrew Millikan (1868—
1953)1® that “The world has recently and
properly celebrated the year 1947 as both
the 200th anniversary of Franklin’s dis-
1 WHEWELL, W., History of inductive sciences,
ed. 3. New York, 1865.
76 Row.anpD, H. A., Bull. Amer. Phys. Soe. 1: 4.
1899.
Hutu, G. F., Fifty Years of physics—a study in
contrasts. Science 104: 238. 1946.
* ScHONLAND, B. F. J., Benjamin Franklin:
Natural philosopher. Proc. Roy. Soc. 236. 1856.
** Trowsripce, J., Franklin as a scientist. Col.
Soc. Massachusetts 18. 1917.
® Mituikan, R. A., Franklin’s discovery of the
electron. Amer. Journ. Phys. 16: 369. 1948.
May 1959
covery of the electron and the 50th anni-
versary of J. J. Thomson’s unambiguous
establishment of the electron theory of
matter.” Incidentally, is it not strange that
Thomson? did not even mention Millikan
and the oil-drop experiment in his book???
In his Introduction to Modern Physics (ed.
2, 1935) Floyd Karkas Richtmyer (1881-
1939) listed Franklin with Boyle, Galileo,
Gilbert, Huygens, and Newton. He then
qualified this endorsement by noting, “The
Franklin theory can hardly be called the
forerunner of all-modern theory which grew
out of experiments of a very different kind.”
Through painstaking experiment, through
scrupulous accuracy, through refusal to sur-
mise what carefully observed facts did not
warrant, Franklin did “find electricity a
curiosity and leave it a science.’”’ I agree
with Thomson that Franklin was “a physi-
cist of the very first rank.”
From this point of view let us review?
the state? of electricity B.F. (before Frank-
lin). There are, I believe, four basic facts
and one commonly accepted theory. First,
the phenomenon of electric attraction has
been known for ages; Thales of Miletus
(640-546 B.C.) had noted the attraction of
amber. Theophrastus of Eresus (371-287
B.C.) had called attention to a similar at-
traction of jet and onyx. Jerome Fracastro
(1478-1553) added diamond to the list. In
1551 Jerome Cardan (1501-1576) had noted
the difference between this kind of attrac-
tion and that of magnetism. William Gilbert
*” THomson, J. J., Recollections and Reflections.
London, 1936.
27m an informal communication of December
1958 Sir George Paget Thomson wrote the follow-
ing in reply to my question about this omission:
“Millikan’s work on the electron came quite a long
time after my father’s, and indeed Millikan’s
method was an adaption of that of H. A. Wilson
in the Cavendish Laboratory. The beauty of Muil-
likan’s work, apart from its accuracy 1s, of course,
the fact that for the first time it was possible to
see charges on a drop changing by definite steps.
While this was an interesting and, indeed, fascinat-
ing confirmation of what everybody has believed,
it was, I think, only a confirmation.”
~ We are concerned here with the historical facts
of logical discovery rather than with their socio-
logical developments and significance, either then
or now.
*8 WuHiTTaker, EH. T., A history of the theories
of aether and electricity. Edinburgh, 1951.
Srecer, R. J., On understanding electric break-
down wm solids. Journ. Washington Acad. Sci. 36:
285. 1946.
SEEGER: FRANKLIN
AS A PHYSICIST 135
(1540-1603) of Colchester, a physician to
Queen Elizabeth I, mentioned in his 1600
De magnete, magnetisque corporibus et de
magnete tellure a large** number of so-
called electrics (like amber) such as glass,
sealing wax, and precious stones. Substances
that did not exhibit this behavior he called
an-electrics (not like amber). In each in-
stance he detected the effect by means of a
versorium, 1.e., an insulated, pivoted, metal
needle. It was generally believed at this
time that friction released electricity as a
fluid similar to body humors such as blood,
phlegm, choler (yellow bile), and melan-
choly (black bile). Attraction for a body
would then be produced by its contact with
the effluvia atmosphere stirred up by rub-
bing (cf. Query 22 in Newton’s Optics).
Contributions came to be more frequent
after Gilbert. Sir Thomas Browne (1605-
1682), who first used the word electricity,
pointed out in 1646 additional substances.
In 1675 Robert Boyle (1627-1691), who in-
vented the word fluid, produced the effect in
a vacuum. Newton himself observed it
through a plate of glass. Charles-Francois
de Cisternay du Fay (1698-1737), botanist
and superintendent of the King’s gardens,
concluded that most nonmetallic substances
behaved similarly. Otto von (Guericke
(1602-1686) made an electric machine in
1660. A 6-inch sulphur ball was mounted on
a wooden axle; it could be rubbed by hand
to produce an electric effect. He noted that
pointed objects were more easily attracted.
Newton had a similar one made of glass in
1675. Francis Hauksbee (d. 1713), curator
of instruments for the Royal Society, used
a glass globe which was rubbed with flannel
and which was attached by a chain to an
insulated metal such as a gunbarrel. All this
work was neglected until 1740, when it was
revived by some Germans. For example, in
1744 Johann Heinrich Winkler (1703-1770)
made a machine which had leather stuffed
with cushions. The electrostatic machine
soon became an important instrument for
studying electrical effects.
The second primary fact known about
electric phenomena was the electric repul-
2 GILBERT, W., De magnete. Mottelay transla-
tion 1893; reprint New York.
Linpsay, R. B., William Gilbert and magnetism
wn 1600. Amer. Journ. Phys. 8: 271. 1940.
156 JOURNAL OF THE
sion of a freely suspended object after con-
tact with an electrified body. Nicolo Cabeo
(1585-1650), an Italian Jesuit, first ob-
served this effect about 1629 or 16380; but
von Guericke was the first to publish it
(1672). Du Fay noted that rubbed amber,
when pivoted, could experience either at-
traction or repulsion with other electrified
objects. Accordingly, he suggested in 1733
an explanation based upon two different
electric fluids, vitreous and resinous. His
theory involved cartesian vortices. Abbé
Jean Antoine Nollet (1700-1776) ,?° pupil of
du Fay, preceptor to the Royal Family of
Louis XV, and teacher of physics at the
Ecole de Méziéres, produced a series of
papers in the memoirs of the Académie in
1745. According to his view an electric fluid
had two currents that moved in opposite
directions, i.e., in and out of a body; they
were said to be either affluent or effluent,
respectively. He compared electrical effects
with thermal properties. Franklin, who
praised Nollet in a letter to him, incurred
his distrust and enmity by having this in-
advertently omitted by Collinson and Foth-
ergill in the subsequent publication of his
correspondence. In 1746 George Louis Le-
clere, Comte de Buffon (1707-1788), a natu-
ralist, summarized the status of electricity
as “not yet sufficiently ripe for the estab-
lishment of the court of laws, or indeed of
any one fixed, and determinate in all its
circumstances.”
The third basic fact was electric conduc-
tion. Von Guericke had found that attrac-
tion took place to some degree through a
linen thread. Stephen Gray (1666/7-1736) ,
a pensioner of Charterhouse, performed par-
ticularly interesting experiments, including
the derivation of sparks from a boy’s nose
(1730), the boy being suspended while hay-
ing his feet rubbed with glass. This experi-
ment was repeated in 1744 at Philadelphia.
It was Gray who differentiated experimen-
tally between a conductor and an insulator,
which he associated with a nonelectric and
an electric, respectively. He found, for ex-
ample, that when wires replaced silk threads
no electric effects were observed, but that
they could be transmitted from rubbed glass
*° NoututeT, J. A., Lettres sur lVélectricité. Paris,
53.
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 9
by a stick attached to an ivory ball (and
thus influence a feather used as an electro-
scope). In this manner he was able to pro-
duce an effect over a distance as great as
765 feet. He noted that the transfer of the
emanation could be accomplished inde-
pendently of the electrified body; accord-
ingly, he introduced the concept of a true
fluid for the first time. Static electricity had
been so-called because it was regarded as
stationary. Leakage that occurred fre-
quently because of poor insulation had only
made electrical phenomena appear to be
somewhat capricious and even more mys-
terious.
The fourth fundamental fact was con-
cerned with electric storage. We are all
familiar with Pieter van Musschenbroek’s
(1692-1761) famous experiment of 1746 in
which he tried to store electric charges in a
phial containing a gun barrel in water. He
received a severe shock, which in a letter to
René Antoine Ferchault de Réaumur (1683-
1757) he insisted he “would not receive
again for the Kingdom of France.” Priest-
ley called this the act of a “cowardly pro-
fessor.” On the contrary, many people
wished to be thrilled by just such shocks.
Spectacular experiments were performed
everywhere. You will recall the Paris ex-
periment with its 900-foot line-up of hand-
in-hand Carthusian Monks. Sometimes a
jar was filled with mercury or with shot.
Ewald George von Kleist (d. 1748), Bishop
of Pomerania, who had made the discovery
independently and possibly earlier, filled a
phial with alcohol containing a nail. Wat-
son, apothecary as well as physician, noted
that the shock to a human went through the
arm and chest because this was the shortest
path. He coated a Leyden jar with tinfoil
both inside and out and thus obtained more
powerful effects. People exposed themselves
to shock treatments for paralysis (cf.
Franklin’s Dec. 21, 1757, letter to Pringle).
In 1750 a hot enough spark, obtained
through a wire 2 miles long, set ether afire.
The Leyden jar soon became another power-
ful new tool for investigating electrical phe-
nomena.
Franklin’s one-fluid theory was a major
contribution to the whole problem. In 1768
in a letter to Michael Collinson upon the
May 1959
death of Peter Collinson, his father, Frank-
lin told of the receipt of a 3-foot sealed
glass, the size of a fist, which could be
rubbed with a piece of flannel, as the be-
ginning of his own interest in electrical
phenomena. On March 28, 1747, he had
written a thank-you letter to Collinson for
this apparatus. In the former letter he ad-
mitted that ‘this was the first notice I ever
had of that curious subject.” In his Auto-
biography he apparently corrected himself
to note that Dr. Adam Spence(r), a physi-
cian from Edinburgh, who was supposed to
have given some phenomenological lectures
in Boston in 1748, and who actually gave
them in Philadelphia in 1744, had sold him
all the electric apparatus. The basic letter
containing the essence of Franklin’s one-
fluid theory was written to Collinson on
July 11, 1747, a year after his retirement
from printing. In it he described a funda-
mental experiment, which has been called
by Millikan “the most wonderful thing ever
done in the field of electricity.” Two men
were placed on wax. The one man rubbed a
glass tube and passed a spark to the other.
Each one was then able to produce a spark
to a third (neutral) man; but they became
neutralized by contact with each other. Here
for the first time we have exemplified the
conservation of electric charge (cf. later
work with Leyden jar), which became
a foundation stone for the mathematical
theory of electricity. Assuming the equality
of the charges, Franklin then gave the fol-
lowing explanation: The electric fluid, subtle
and particulate, elastic and self-repellent,
did not result from rubbing; rather it was
the normal content of neutral matter, which
attracted it and behaved like a saturated
sponge. An excess or deficiency of the fluid
would exhibit itself as positive or negative
electricity, respectively. The excess would
then produce an atmosphere on the surface,
as the smoke from a body with dry resin
about it. His single fluid eliminated the
problem of annihilation of effects upon con-
tact of the two kinds of electricity. The
most significant aspect of this mechanical
theory was the economic association of mat-
ter and electricity (two fundamental sub-
stances rather than three). It must be ad-
mitted that the nature of Franklin’s fluid
SEEGER: FRANKLIN AS A PHYSICIST
137
was very nebulous—little understood even
by himself. He was wont to compare it with
fire. In his 1748 letter to Collinson he specu-
lated: “Perhaps they may be different modi-
fications of the same element; or they may
be different elements. The latter is by some
suspected.” In a letter of March 10, 1773,
to Jacques Barbeu Dubourg (1709-1779)
he discarded the notion of any relation be-
tween electricity and magnetism on account
of their difference with respect to heating
and jarring. In a letter of June 25, 1784, he
mused on the possibility of a universal fluid
associated with fire, light, and electricity.
On June 20, 1788, at the American Philo-
sophical Society he even read a paper with
similar ideas, viz., “Loose Thoughts on a
Universal Fluid.”
Why should the vitreous fluid be regarded
as positive? Why not the resinous? Franklin
had reasoned about this choice, too (cf.
Mar. 16, 1752, letter to Kinnersley). The
vitreous charge seemed to spread over an op-
posite conductor. Moreover, a candle flame
appeared to be blown away by a vitreous-
charged body, but toward a_ resinous-
charged body. He admitted, however, some
uncertainty in this conclusion. As today we
evaluate the one-fluid theory, we note that
Franklin could not resolve a major diffi-
culty, namely, the repulsion of two fluid-
less, 1.e., negatively charged, bodies. To an-
swer this question, Franz Maria Ulrich
Theodor Aepinus (1724-1802) insisted in
1759 that one had to postulate additionally
repulsion between particles of negative mat-
ter, which effectively became a second elec-
trical substance, but one that was not fluid.
Thus the original simplicity was lost in an
undefined haze. He eliminated effluvia, too,
inasmuch as electric fluid did not seem car-
ried off with air that was blown away. Con-
sequently, without effluvia, action at a dis-
tance became plausible and gave rise to the
mathematical theory of electrostatics. In
1759 Robert Symmer (d. 1763) suggested
that electrification merely separated the
neutral mixture of the two fluids. For ex-
ample, glass, regarded as ordinarily con-
taining both vitreous and resinous electric
fluids, was supposed to lose some of the res-
inous electricity and thus be left with a sur-
plus of the vitreous. No reason, however,
138 JOURNAL OF THE
was advanced as to what determined the
fluid. Physical relations, including the na-
ture of the forces exerted by these massless
fluids, were disregarded, although the re-
sultant neutralization of their effects upon
mixing seemed reasonable. It is interesting
that Antoine Laurent Lavoisier (1743-1794)
included electricity as a chemical element
along with heat and hght in his 1789 La
traité élémentaire de la chimie. The chief
difference between the two-fluid theory and
one-fluid theory was then virtually the flu-
idity of the negative state. The theory itself,
which seemed simple, became readily ac-
cepted in France by prominent individuals:
for instance, by Charles Augustin Coulomb
(1736-1806), who was largely responsible
for discovering the law of force between
electrostatically charged bodies, and for
defining electric charges quantitatively
(1785); and by Siméon Denis Poisson
(1781-1840), who established the mathe-
matical theory of electrostatics (1812). It
was opposed, however, in Holland by Mar-
tin van Marum (1750-1837)—and in Italy
by Alessandro Volta (1745-1827). The di-
lemma persisted until the discovery of the
electron.”®
The law of force between electrified bod-
ies became evident in another Franklin ex-
periment (Mar. 18, 1755, letter to John
Lining (1708-1760)). In this case a cork
was placed inside a charged silver can and
found to be unaffected (cf. Faraday’s 1843
ice-pail experiment). In 1766, Priestley, who
immigrated to the United States in 1794,
repeated this experiment and inferred the
inverse-square law of force in analogy with
that of gravitation. It was he, indeed, who
pointed out the need for instruments (no
good measurements were possible up to
1760). Gray had previously noted that hol-
low and solid oak tubes would give the same
effect which he therefore concluded in the
case of repulsion, was more of a surface than
°° HELMHOLTZ, H. von, On the modern develop-
ment of Faraday’s conception of electricity. Journ.
Chem. Soc. 39: 277. 1881.
MaxweELL, J. C., A treatise on electricity and
magnetism, ed. 3. Oxford, 1892.
Mi.uikan, R. A., Electrons (+ and —), protons,
photons, neutrons, mesotrons, and cosmic rays,
rev. ed. Chicago, 1947.
BirkHorF, G. D., Electricity as a fluid. Journ.
Franklin Institute 226: 315. 1938.
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, No. 5
a height (or volume) effect. By no means
could this surmise be considered an experi-
mental confirmation of the inverse-square
law, done first by John Robison (1739-
1805) of Edinburgh, who obtained an actual
value of 2.06 and guessed it to be theoreti-
cally 2.0. Meanwhile, John Michell (1724—
1793) had suggested a torsion balance for
precise investigations. Coulomb used a tor-
sion balance to establish the relation quan-
titatively; in 1785 for like (positive)
charges, and in 1787 for unlike charges; he
thus eliminated all further vortex specula-
tions. Henry Cavendish (1731-1810) also
made such investigations in 1779, but he
failed to publish them (done in 1879 by
James Clerk Maxwell (1831-1879)). In
conclusion, Franklin’s conservation of elec-
tric charge, plus the establishment of the
inverse-square law, made possible the for-
mulation of an exact science of electricity—
insofar as an “exact” science may be said
to exist.
In his September 1, 1747 and 1748, let-
ters to Collinson he noted certain new facts
which he himself had observed, namely,
electrostatic induction, the significance of
erounding which made it possible to obtain
a permanent state of electrification, and the
determination of the induced charge on a
grounded body. Franklin applied his theory
of induction to a dissectible condenser, spe-
cifically, to a Leyden jar (cf. 1748 letter to
Collinson). Incidentally, he sent Philadel-
phia-made Leyden jars on various occasions
to James Bowdoin in Boston. Kinnersley, a
teacher of English in the Academy, had
showed that a jar charged inside was
charged also outside, with equal and oppo-
site effects, but that the water itself was not
electrified. Moreover, this phenomenon was
reversible. Thus, if a cork were placed so
that it could make contact alternately with
the inside and with the outside, it would
continue to oscillate until neither was
charged. There appeared to be a balance of
‘the two charges, not an accumulation of
either one. On the other hand, small sparks
were produced if the separating glass of a
parallel-plate condenser was removed, but
a very large spark occurred when the plate
was replaced. This effect depended upon the
thickness of the glass. Another interesting
May 1959
fact was that the glass was impermeable to
electric flow but not to electric influence;
the electric fluid was able to pass through
a dielectric like glass only if it were punc-
tured or heated. He noted what we would
now call the variation of capacitance as a
chain was removed from a can (cf. Sept.
1753 letter to Collinson). In a letter dated
June 14, 1783, Franklin wrote, “I would
recommend it to you to employ your time in
making experiments, rather than in making
hypotheses, and forming imaginary sys-
tems.”
In conclusion, Franklin did discover
many new curious facts, but, more impor-
tant, he showed a mastery of experimental
techniques including the design of experi-
ments and the testing of hypotheses. He did
not merely collect random facts; he searched
for significant scientific facts; experimenta-
tion must be vectorial, not scalar. Above
all, he formulated a simple conceptual
scheme. As J. J. Thomson remarked, “A
collection of electrons would resemble in
many respects Franklin’s electric fluid.” It
is still useful today for qualitative thinking.
How many of us sophisticated moderns
would immediately set down Poisson’s par-
tial differential equation and attempt to
solve it if asked what would happen if a
piece of hard rubber rubbed with a cat’s
fur would be brought near another piece
of hard rubber rubbed with cat’s fur?
Let us now consider what I would desig-
nate as the Franklin experiment. Fothergill
in his preface to Franklin’s book empha-
sized the scientific discussion of lightning
as contrasted with unbridled speculation.
The so-called age of enlightenment had
references only to a few leaders, not to most
people. The majority of folks still had per-
petual fear of the unleashing of natural
forces, like lightning and earthquakes (cf.
current ideas of atomic energy, rainmaking,
etc.). In New England, for example, light-
ning was regarded by some as a personal
act of an angry god. In this connection we
recall Titus Lucretius Carus’s (96-55 B.C.)
astute remark2? (book 6) dealing with “the
very nature of fire-fraught thunderbolt”:
27'T Lucretius Carus, On the nature of things
(translation by W. E. Leonard). New York, 1950.
SEEGER: FRANKLIN AS A PHYSICIST
139
If Jupiter
And other gods shape those refulgent vaults
With dread reverberations and hurl fire
Whither it pleases each, why smite they not
Mortals of reckless and revolting crimes—
Nay, why, then aim they at eternal wastes,
And spend themselves in vain?
And, lastly, why with devasting bolt
Shakes he asunder holy shrines of gods
And his own thrones of splendor?”
In a sermon on “Earthquakes, the Work
of God,” the Reverend Thomas Prince con-
sidered lightning as focusing in the ground
and thus producing a series of violent earth-
quakes**—a common notion in the spring
of 1750. On November 26, 1755, Winthrop
lectured in Harvard Chapel on earth-
quakes”? being “neither objections against
the order of Providence, nor tokens of God’s
displeasure, but necessary consequences of
natural laws.” In Europe bells were often
inscribed with the words “Fulgura Frango”’
(I break the lightning). Abbé Nollet, for
instance, advised people to ring bells during
a storm. In 1784 Fisher of Munich com-
pleted a 33-year study of heghtning and
found that 386 church towers had been
struck and 103 bell ringers killed. In 1787
the Parhament of Paris had to renew Char-
lemagne’s edict against bell rimging in
storms. Nevertheless, a hundred years ago
bells were still being rung for this purpose.
It was natural to compare lightning with
electric sparks and to speculate about their
possible relation. An electric spark had first
been noticed by von Guericke. Its similarity
to lightning had been noted individually by
Hawksbee (1705), William Wall (1708),
Newton (1716), Winkler (1746), John
Freke (1746), and Nollet (1748). Gray, in-
deed, stated in 1734, “Electric fire seems to
be of the same nature with that of thunder
and lightning.” Franklin himself wrote on
July 11, 1747, “We represent lightning, by
passing the wire in the dark over a china
plate that has gilt flowers.” Later (1749-
1752) he associated the aurora borealis, too,
°8 Prince, T., Improvement of the Doctrine of
Earthquakes.
°° WinTHROP, J., Lectures on earthquakes. Bos-
ton, 1755.
140
with electric discharge. The age of super-
stition, however, has not been left wholly
behind us. We moderns are still accustomed
to believing that lightning never strikes
twice in the same place, although the Em-
pire State Building has been struck as often
as 68 times in three years—not to mention
the Washington Monument.
What was needed in order to identify
lightning unquestionably with an electric
spark was a critical experiment—the design
of such an experiment was one of Franklin’s
most important contributions. He did not
make the first analogy, nor even a correct
interpretation. The basic facts were all
known in 1747 (cf. July 11 letter to Collin-
son). With Thomas Hopkinson (1703-1751)
he had observed, by means of a similarly
charged cork in the neighborhood, the loss
of electric charge on a cannon ball due to a
steel bobkin held 6 to 8 inches away. Dis-
charge for a blunted needle, however, oc-
curred only when it was brought much
closer. In his July 27, 1750, letter to Collin-
son, Franklin called attention to the St.
Elmo fire associated with a pointed object.
St. Elmo (Erasmus) may be recalled as be-
ing the patron saint of the Mediterranean
sailors. His fire was considered a good omen,
inasmuch as a storm would end soon after
its appearance (cf. Columbus’s encourage-
ment of his shipmates). Franklin made a
complete list of 12 apparent similarities be-
tween lightning and electric sparks in his
March 18, 1755, letter to Lining, which he
had copied from his own November 7, 1749,
notebook. The characteristics were light,
color, crooked path, swift motion, metal
conduction, explosion crack, passage through
ice and water, bending of a body at the base,
destruction of animals, melting of metals,
fire in inflammable substances, and sulphu-
rous smell. But what about the action with
respect to a point? Said Franklin,... “Let
the experiment be made!” “It might have oc-
curred to any electrician,’ he remarked in
the letter. It might have but it didn’t.
In the July 29, 1750, letter to Collinson,
which contained 56 “Opinions and Conjec-
tures” of 1749, Franklin first noted, “I
would propose an experiment’’—sometimes
called the sentry-box experiment. In this
case an insulated man was to be placed in a
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 5
sentry box having an upright, 20-80-foot,
pointed, iron rod. Expressed interest by
King Louis XV of France (1710-1774) in
this suggestion led to three secret attempts
to perform it. Jean Francois D’Alibard, a
botanist (1703-1799), was the first to do the
experiment on May 10, 1752, at Marly-la-
Ville, 18 miles from Paris; he used an iron
rod 40 feet high, 1-inch thick, with a brass
point, connected to a bottle. A soldier by
the name of Coiffier first noted some action;
he called a priest, Raulet, who observed the
effect six times. On May 18, DeLor, a maker
of physical instruments, made a rod 99 feet
long with a resin base 2 feet square by 3
inches thick, at the Chateau de St. Germain.
Buffon repeated the experiment on May 19.
Franklin himself might have received the
news of these events in June. The King in-
structed Abbé Guillaume Mazéas (1712-
1776) to write a letter (May 20, 1752) to
Benjamin Franklin via Stephen Hales
(1677-1788). English experiments by John
Canton (1718-1772) on July 20, by Benja-
min Wilson on August 12, and by John
Bevis (1693-1771), were announced by
Watson to the Royal Society in December.
The second type of lightning experiment
involved the celebrated kite. Alexander Mc-
Adie®® has raised some questions as to
whether this experiment was ever actually
performed. Franklin, however, did describe
it in detail in his letter of October 19, 1782,
to Collinson. Priestley, too, cited it in his
book® which had been read in manuscript
by Franklin himself. This experiment was
possibly done on June 6, 1752, near 18th
and Spring Garden Street in Philadelphia
between the Delaware and Schuylkill Riv-
ers where Franklin was wont to walk. The
choice of such a spot may have been owing
in part to the delay in waiting for suitable
conditions at the Christ Church spire—or
possible fear of ridicule. Questions have
been raised as to whether the rod was close
enough to the cloud. The apparatus was
certainly simple; a silk kite having a
sharply pointed wire protruding one foot,
was attached by twine to a key; a dry silk
ribbon was tied to the end of the twine and
held in the hand. The observer was to hold
°° McAnpig, A. G., The date of Franklin’s kite ex-
perument. American Antiquarian Society, 1924.
May 1959
the silk in a sheltered area and bring his
knuckle toward the key to test for a spark.
(The popular picture showing Franklin’s
son as a boy assistant is, to say the least,
exaggerated inasmuch as the latter was 21
years of age at the time.) The Royal So-
ciety, which was said to have previously
(1750) laughed at the suggestion of such
action by lightning on a point, and had re-
fused its publication in the Transactions,
was favorably impressed in December 1752
by the announcement of the successful at-
tempt.
Newton H. Black*! cautions, “Perhaps
the most wonderful part of it was that
Franklin was not killed at once.” George
Wilhelm Richmann (1711-1753), a Swedish
physicist, was killed August 6 at the St.
Petersburg Imperial Academy when he at-
tempted to repeat the D’Alibard result. The
kite experiment was done in 1754 by John
Lining, in 1756 by Abbé Giacomo Battista
Beccaria (1716-1781), and by van Mus-
schoenbroek. In May 1753 Jacques de Ro-
mas used a kite which was supposed to have
produced 10-foot sparks—due to interwoven
wire and hemp. He also claimed priority.
On June 15, 1954, Czechoslovakia cele-
brated the 250th anniversity of the birth of
Father Procopius Divis, the so-called Euro-
pean Franklin, the scientist who erected in
his garden a multiple-pointed, grounded rod
as a protective device. There seems to be no
way now to determine whether Franklin or
this European was the first®* to invent the
lightning rod. Franklin’s own suggestion®*®
occurred in his July 29, 1750, letter in which
he described an experiment which would
permit bells to be rung in his house when-
ever lightning would be conducted via a
lightning rod nine feet above the chimney
to some Leyden jars. His own house, for
which such a device was made in September
3 Buack, N. H., An introductory course in col-
lege physics. New York, 1941.
2 CoHEN, I. B., and ScHorietD, R., Did Divis
erect the first European protective lightning rod,
and was inventing independent? Isis 43: 358. 1952.
Huser, K., Father Procopius Divis—the Euro-
pean Franklin. Isis 43: 351. 1952.
3 CoHEN, I. B., The two hundredth anniversary
of Benjamin Franklin’s two lighining experiments
and the introduction of the lghtning rod. Proc.
Amer. Phil. Soc. 16: 331. 1952; Prejudice against
the introduction of lightning rods. Journ. Franklin
Inst. 253: 393. 1952.
SEEGER: FRANKLIN
AS A PHYSICIST 141
1752, was actually struck in 1787. Two
methods of performing a critical experiment
were also outlined. In one case the rod was
to be erected so as to reduce the effect
through a continuous point discharge of the
clouds. In the other instance the hghtning
rod was to be grounded so as to permit suc-
cessful conduction to the earth. Franklin,
of course, expected to draw a charge from
the clouds; actually he only induced a
charge and obtained virtually the same re-
sult, both for the grounded and ungrounded
experiments. All the 1752 experiments were
with ungrounded test rods, but the records
were not always clear on this matter. What
we can definitely say is that lightning rods
were early placed upon the Academy and
the State House in Philadelphia.
In 1762 there were comparatively few
lightning rods in England. Watson’s house
at Payne’s Hill had been the first one so
protected. In 1761 and 1767 St. Paul’s Ca-
thedral in London had been struck; in 1771
it was protected with a conductor. St.
Bride’s was hit in 1764. In 1769 heghtning
struck the magazine at Brescia and de-
stroyed one-sixth of the people of the town.
In 1772 the Powder Magazine at Purfleet
was struck. The Royal Society appointed a
committee consisting of B. Franklin, H.
Cavendish, J. Robertson, W. Watson, and
B. Wilson to look into the matter of protec-
tion for Purfleet—pointed conductors with
good metallic connections to the ground
were recommended in the August 21, 1772,
report (Wilson dissented). Keen partisian-
ship developed with respect to the report.
Wilson?* was subsequently appointed by
King George III (1738-1820), to succeed
Wilham Hogarth (1697-1764) as Sergeant
Painter to the Board of Ordnance. Political
pressure from the King was supposed to
have forced the resignation of Sir John
Pringle as President of the Royal Society.
Pringle commented that the King ‘could
not reverse the laws and operations of na-
ture.” Pointed rods were soon replaced by
round rods on Kew Palace and other Gov-
ernment installations. Nevertheless, Purfleet
itself was struck a few years later—even af-
ter these rods had been erected. In France
* Witson, B., Observations on lightning. Lon-
don, 1773; Further observations on lightning. Lon-
don, 1774
142 JOURNAL OF THE
Jean Paul Marat (1744-1793) and Max-
milien Marie Isidore de Robespierre (1758—
1794) approved the use of lightning rods; in
Italy Pope Benedict XIV recommended
them (they were used in some churches
there). Abbé Nollet, however, contended
that it was “as impious to ward off God’s
lightning as for a child to resist the chasten-
ing rod of the father.” Some people went
about with unsheathed swords overhead to
simulate lightning rods—the clerics were
evidently at a disadvantage. As we look
back at the situation, both groups were par-
tially right. Nollet was correct in that a
cloud did not produce an appreciable in-
ductive effect on a point and Wilson was
correct in that a point was probably no bet-
ter for the same purpose than a blunted ob-
ject owing to the scale of the objects in-
volved. On the same basis, however, both
were partially wrong; the rod itself was
definitely not harmful.
Considerable attention was soon given to
the protection of public buildings. The 340-
foot campanile at St. Mark’s in Venice was
struck nine times (on three occasions com-
pletely destroyed), but not after its protec-
tion by proper hghtning rods. Likewise, Si-
ena Cathedral, struck in 1771, received no
further lightning blows after rods were ap-
propriately erected. The New York Dutch
Church finally sought protection in 1765 af-
ter damage had been done in 1750 and then
again in 17638. St. Martin’s-in-the Fields in
London was unprotected when it was struck
in 1842.
Even more significant are those buildings
that were never struck.®® First in impor-
tance 1s Solomon’s Temple built in Jerusa-
lem about 1000 years B. C. The roof of this
building was covered with metal both inside
and outside, and in addition it had iron
spikes as a protection against birds and
thieves; these were all connected by iron
pipes to a cistern. The 202-foot-high monu-
ment in commemoration of the great London
fire of 1677 was protected from lightning
by virture of its pointed metal flame-figures
fixed to an iron base used as steps. St.
Peter’s Cathedral in Geneva, it is true,
had a wooden tower, but it was shielded
*° SCHONLAND, B. J. J., The flight of thunderbolts.
Oxford, 1938.
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 5
owing to the covering of tinned iron plate
connected to the ground by metal. The fa-
mous Pantheon of Rome had a roof of
bronze. Various roofs of churches and pal-
aces were made of lead and copper sheets.
The Eiffel Tower was found to be uniquely
protected from lhghtning owing to its having
virtually a Faraday cage.
In the United States today 90 percent of
the lightning flashes take place in the coun-
try. Nevertheless, about 500 persons are
killed and 1,300 injured annually. There is
also considerable property loss each year.
Yet, only one-fifth of the United States
buildings that could profit from lightning
protection are so protected.
Of greater scientific significance, however,
is the whole matter of atmospheric elec-
tricity. In Franklin’s letter of April 29, 1749,
to Mitchell on thundergusts, he discussed
model experiments of clouds. In the 1949
Opinions and Conjectures (#20) of the
July 29, 1750, letter a cloud was simulated
by a 10-foot by 1-inch pasteboard tube cov-
ered with gilt; it was discharged silently by
a needle one foot away, but it produced a
crack with a blunt object only 3 inches
away. Incidentally, this model was wanting
in that it involved essentially a surface ef-
feet, whereas the cloud represented a vol-
ume distribution of charge.
Franklin ingeniously employed his light-
ning rod chimes to determine the kind of
charge on a cloud by charging a Leyden jar
(Oct. 19, 1752, and Apr. 18, 1754, letters to
Collinson). In this way he found that a
cloud was usually charged negatively on the
bottom. Toward the end of a storm, how-
ever, the upper positive charge would de-
scend so that the bottom became positively
charged. Such an experiment indicates that
Franklin was “no vague amateur.” Schon-
land observes that Franklin’s work was the
only direct and reliable information on at-
mospheric electricity for a period of one
hundred and seventy years. Pierre Charles
Lemonnier (1715-1799) had noted further
in 1752 that atmospheric electricity may
exist even without a cloud.
Noteworthy among recent (1902) devel-
opments has been the work of Sir Charles
Vernon Boys (1855-1944), whereby he was
able to use a camera in connection with
May 1959
the activity of lightning rods. Furthermore,
electric fields have been obtained as the
result of having pointed rods attached to
recording galvanometers. The quantity of
electricity moving to and from the earth
has been actually measured by means of
a water voltameter. The sign and amount
of charge in the very heart of the cloud
has been determined by the use of points
on balloons. Paradoxically enough, we are
now studying lightning more as a means
of determining the nature of electric charges
than vice versa. An important by-product
of this information is some help in our un-
derstanding of cosmic rays, as well as the
upper atmosphere.
In conclusion, let us look once more at
Franklin, the natural philosopher. The pur-
suit of science was certainly very close to
his heart; his scientific curiosity became
manifest in many areas. In his March 28,
1747, letter to Collinson he confessed his
enthusiastic interest in electrical phenom-
ena: “I never was before engaged in any
study that so totally engrossed my atten-
tion and my time as this has lately done...
I have, during some months past, had little
leisure for anything else.” He had under
varying conditions investigated charged ob-
jects. They became discharged by having
sand sifted upon them, by being breathed
upon, by being surrounded with smoke, by
having a candle burnt near them; he noted
a difference between candlelight and sun-
light with respect to the loss of charge by
iron shot (cf. July 11, 1747, letter). Later
he expressed a hope to study the possible
production of electrification by evapora-
tion.
His broad curiosity led him to investigate
also thermal phenomena. In his Apri 14,
1757, letter to Lining, he noted that a silver
teapot should preferably have a wooden
handle. He mentioned an experiment for de-
termining relative thermal conductivity. He
discussed also insulation properties of cloth-
ing. On the 20th of September 1761, he wrote
in a letter to Mary Stevenson about experi-
ments®® he had done about 1729 and which
had been repeated about 1786 by Joseph
°° Conen, I. B., Franklin, Boerhaave, Newton,
Boyle and the absorption of heat. Isis 46: 99. 1955;
Franklin's experiments on heat as a function of
color. Isis 34: 404. 1943.
SEEGER: FRANKLIN AS A PHYSICIST
143
Breitnal, a member of the original Junto.
Broadcloth squares were placed on sunny
snow in the morning. The various colors
used were black, deep blue, light blue, green,
purple, red, yellow, and white. The black
cloth sunk the deepest, whereas the white
one was still on the surface at the end of the
experiment. He observed, too, that beer be-
fore a fire was warmer in black mugs than in
bright silver tankards. We are familiar with
Franklin’s pulse glass (German origin),
which contained water at a lower boiling
point owing to air having been blown out.
Boiling, therefore, could be made to occur
from the heat of one’s palm in contact with
the glass.
In his April 28, 1752, letter to C. Colden
he disagreed with Newton’s corpuscular the-
ory of hight and favored a wave theory; his
opinion was refuted in 1780 by Governor
James Bowdoin (1727-1790), first president
of the American Academy of Arts and Sci-
ences, in the inaugural address entitled “A
Philosophical Discourse.” Incidentally,
Franklin became a member of that organi-
zation in 1781.
Franklin found dehght in investigating
various meteorological phenomena. A north-
east storm spoiled his view of a lunar eclipse
expected in Philadelphia at 9 p.m. on Octo-
ber 21, 1748. Nevertheless, the same eclipse
was visible in Boston one hour later. He
realized that such a storm must have begun
in the southwest and been rotating about a
moving center. In 1755 he followed a whirl-
wind in Maryland, where he again noted
that the circular motion was more impor-
tant than the linear one. Franklin, to be
sure, accepted the common notion that wa-
ter spouts were composed of ocean water. In
1783 he noted that the dust which resulted
in a fog during summer had a cooling effect.
Cleveland Abbe (1838-1916) remarked, “If
he had done nothing else but his work on
meteorology that would have entitled him
to the highest rank.”
Of particular significance was his obser-
vation (May 10, 1768, letter to Pringle) of
the change in barge speed with the depth of
a canal. He discussed the courses of rivers
in his September 20, 1761, letter. About
1773-74 Franklin found interesting the use
of oil to calm wave motion on Serpentine
144 JOURNAL
Pond in Hyde Park (Nov. 7, 1773, letter to
S. Brownrigg). In his August 1785 letter to
Julien David LeRoy (1724-1803) of Paris
he noted that the fogs off Newfoundland
were probably produced by the Gulf Stream.
He showed some interest also in ocean-
ography. In 1726 on his first ocean voyage,
or at least on the return, he had measured
the ocean currents, including their tempera-
ture, and observed various astronomical
phenomena as well as meteorological con-
ditions. On his last voyage in 1786 (at the
age of 80) he compared the currents and
the winds with observations of the Gulf
Stream; he determined the temperature at
different depths. He devised experiments to
improve navigation.
In his September 9, 1782, letter to Sir
Joseph Banks (1743-1820), successor to
Pringle, he said, “I long earnestly for a re-
turn of those peaceful times, when I could
sit down in sweet society with my English
philosophic friends, communicating to each
other new discoveries and proposing im-
provements of old ones.” In his April 29,
1785, letter to Jan Ingenhousz (1730-1799)
with respect to his plans for a return to
Paris, he remarked hopefully, “We'll make
plenty of experiments together.”
Not only was Franklin truly a philoso-
pher of nature, but he was equally a popu-
larizer of science in the best sense of that
word. He was able to expound his ideas so
they could be generally understood. To John
Perkins he wrote in 1753, “If my hypothe-
sis is not the truth, it is at least naked. For
I have not with some of our learned moderns
disguised my nonsense in Greek, clothed it
in algebra, or adorned it in fluxions. You
have it in puris naturalibus.”’ Moreover, he
spread continually popular interest in sci-
ence through the Chronicle, the Gazette, and
the Journal, which he published. Van Doren
said in 1930, “He was the best writer in
America.” Franklin’s letters were not just
personal letters, but more like Leonard Eu-
ler’s “Letters to a German Princess,” i.e.,
public letters to be read by all interested in
the subject matter. He wrote to Collinson
in September 1755, “You are at liberty to
communicate this paper to whom you
please; it being of more importance that
OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 5
knowledge should increase then that your
friend should be thought an accurate phi-
losopher.”
Franklin is responsible for the famous
book on Experiments and observations on
electricity made at Philadelphia by Mr.
Benjamin Franklin (London, 1751). It be-
gan with his first (July 11, 1747) letter to
Collinson, read by a circle of friends ineclud-
ing Watson, who discussed it on January 21,
1748. On February 5, 1750, Collinson asked
Franklin if he might send this letter and
other material to a printer; he sent it all
in April. The book was published in April
1751 and announced in the magazines of
that time. It received a generous reception
in England. It is true that in January 1750
the publisher Edward Cave already had one
paper in The Gentleman’s Magazine, as well
as one of the articles. Denis Diderot (1713—
1784) remarked that this book taught man
the nature of experimental art. It truly rep-
resented the “vade mecum of electrical dis-
course” by virtue of its logical presentation
of experiments and ideas. Abbé Nollet, how-
ever, regarded the book as an affront by his
own Paris enemies. The book went through
ten editions in four languages: five of them
were in English (1st,1751; 2d,1754; 3d,1760;
4th,1769 with notes by Franklin himself;
oth,1774) ; three in French (1st by D’Al-
lard,1752; 24,1756; 3d by Dubourg,1773) ;
one in German (by Welcke, 1758), and one
in Italian (1774). It is remarkable that
there was no American edition until 1941°*
—the sources then being the 5th English
edition and the 1751 Bowdoin manuscript
of a copy of the book, which had been made
up by Franklin himself. The book could
serve even now as an excellent illustration
of scientific research and teaching for both
students and teachers—particularly the ex-
cellent edition by Cohen with its helpful
“Critical and Historical Introduction.”
What, however, is the use of this Ameri-
can classic of science today? In introductory
courses in physics there is a great careless-
ness about persons, places, and times (his-
torical clues) and hence, more significantly,
* FRANKLIN, B., Benjamin Franklin’s experi-
ments, ed. by I. B. Cohen. Cambridge, 1941.
May 1959
about the evolution of ideas—owing par-
tially to our cultural neglect of the history
of science. Of seven texts on electricity and
magnetism, five make no mention of Frank-
lin’s one-fluid theory or of his lightning ex-
periment. Of 26 modern (after 1940) college
physies textbooks, I happen to have at hand,
14 do not even mention Franklin’s name; 5
find noteworthy his naming the electric
charges; 4 include the one-fluid theory; 2
complain of his wrong choice of the movable
fluid. The palm glass is noted by one, the
bifocals by someone else, and electrotherapy
by still another. Only two persons consider
the important modern principle of conserva-
tion of electric charge. Only three discuss
lightning (two the kite, one the lightning
rod). Nevertheless, many of Franklin’s
ideas are unnamed commonplaces in physics
today ; for example, the use of a semicircular
wire with an insulated handle for discharg-
ing—and much of our electrical terminol-
ogy.
We fail as teachers, I believe, in depriv-
ing our students of their rightful and joyous
heritage. They should know who did what
and when in physics; they should learn to
be proud of their American scientific tradi-
tion in pure science—and thankful. Ameri-
can culture, past and present, should be
recognized for its scientific aspects. We
should not permit narrow historians who
may not appreciate science—much less un-
SEEGER: FRANKLIN
AS A PHYSICIST 145
derstand it—to distort the conception of its
role in our society.
In evaluating a scientist we may ask per-
sonally, “What did he himself do?” Or we
may inquire socially, “What did he receive
from previous ages? What did he contribute
to his own age? What did he transmit to
future ages?” In various ways®* one can
thus view Franklin. From all viewpoints,
however, I always see Franklin as a physi-
cist—not the triumphing Franklin of the
1778 engraving by Jean Honoré Fragonard,
painter to the King, but the thoughtful
Franklin of the Mason Chamberlin portrait
(1762), observing his bell-equipped light-
ning detector.
ABBE, C., Benjamin Franklin as a meteorolo-
gist. Proc. Amer. Phil. Soc. 45. 1906.
Bett, W. J., Early American science. Williams-
burg, 1955.
CoHEN, I. B., Benjamin Franklin as scientist and
citizen. Amer. Scholar 474. 1943.
CoHEN, I. B., The defense of Benjamin Frank-
lin. Sci. Amer. 179. 1948.
CrowTHER, J. G., Famous American men of sci-
ence. New York, 1937.
Diuter, T., Franklin’s contribution to medicine.
Brooklyn, 1912.
Goopman, N. G., The ingenious Dr. Franklin.
Oxford, 1931.
Houston, E. J., Franklin as a man of science and
inventor. Journ. Franklin Inst. 159: 16. 1906.
JAFFE, B., Men of scvence in America. New York,
1944 and 1958.
_ Mituikan, R. A., Benjamin Franklin as a scien-
tast. “Meet Dr. Franklin,” Franklin Institute, Phil-
adelphia, 1943.
Pepper, W., The medical side of Benjamin
Franklin. Philadelphia, 1811.
Appeal for Back Numbers
The Academy would deeply appreciate the donation of copies of the following issues of
this JOURNAL:
Vol. No.
48 6
45 1
44 2,9
43 Das
41 iS
40 9,1
Vol. No.
38 i
37 1
36 1
30 8-12 incl.
34 9
30 4
Copies should be sent to the Academy office at 1530 P Street, NW., Washington 5, D. C.
146 JOURNAL OF THE
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 5
ARCHEOLOGY .—Relationship between Plains Early Hunter and Eastern Archaic.
Wiuu1AM J. Maypr-Oaxss, University of Toronto. (Communicated by Waldo
R. Wedel.)
(Received March 9, 1959)
This paper is a revised version of one pre-
pared for the Archaic Conference held at
Bloomington, Ind., in May 1955. It is es-
sentially the original paper with several ad-
ditions and corrections resulting from both
the discussions held at this conference and
the papers prepared by other participants.
Some of the information presented in a
later paper on the “Plains Archaic Concept”
(Mayer-Oakes, n.p.b) has been included
here, as well as certain additional data
which have become available since Febru-
ary 1957 when this paper was cast into its
present form.
From the experience of the conference
and especially the evidence released since
then, two major points of the paper have
become more clearly the burden of my argu-
ment. Support for both of these points came
from several participants in the conference.
Most simply stated, these two main conten-
tions are as follows:
(1) The cultures called “Archaic” in east-
ern North America are considerably longer-
lived than previously considered and are
part of a widespread culture base which
covered much of the New World at a very
early time, considerably earlier than it was
previously thought to be.
(2) The cultures called ‘“paleo-Indian,”
while less varied in nature and content than
“Archaic,” are nonetheless varied in typol-
ogy and cover a considerable span of time in
a rather restricted area of North America.
They are at least partly contemporaneous
with “Archaic.”
I consider this paper an exploratory one
to be followed by more detailed investiga-
tion of some of the points examined. In this
presentation we shall concern ourselves pri-
marily with North American manifestations,
especially those in the United States east of
the Rockies.
TERMINOLOGY
In North America east of the Rocky
Mountains, the term “Archaic” has fairly
general usage in at least two main ways. In
one sense, Archaic is considered to be a de-
velopmental stage and generally connotes
the presence of a diversified hunting-gather-
ing-fishing type of economy accompanied
by a social organization reflecting the earli-
est stages of semisedentary life. The pres-
ence of ceramics, agriculture, or a developed
magico-religious structure is not expected in
such a stage.
The other main sense in which Archaic
is used is as the name for a period of time,
and as such it may crosscut the first usage.
In the ideal case a developmental stage
would correlate directly with a time period.
Such a correlation is evidently often as-
sumed in the unspecified usage of the term.
Actually, complicating factors such as the
presence of cultural centers and the his-
torical facts of cultural isolation may oper-
ate to make the stage and the time period
disagree. An example of this kind of disa-
greement is the interpretation originally
given to the Eva focus of western Tennessee
by Kneberg (1952).
Likewise, the term ‘‘paleo-Indian” has
been used in these two main ways. As a de-
velopmental stage, the term paleo-Indian
has been applied to small nomadic hunting
groups many of which give some evidence
for a specialization in the game killed. In
the temporal sense, paleo-Indian has been
reserved for units the extreme age of which
could be fairly definitely established. The
geological or paleontological dating factors
for this period have been supplemented re-
cently by radiocarbon dating.
While there have been differences in Ae
usage of the two terms, not all of the result-
ing confusion can be ascribed to the de-
velopmental and temporal aspects of these
usages. There is still a third factor implicit
in the current usage of the terms. This is the
factor of a genetic cultural relationship or
tradition and is most frequently expressed,
for example, in terms of the exclusive as-
sociation of fluted projectile points with the
May 1959
paleo-Indian unit. For Archaic an associa-
tion of ground and polished stone tools with
a rather heterogeneous assemblage of pro-
jectile points is most often posited. The
terms have thus come to connote not only
stages of culture and periods of time but
actual cultural inventories.
There are valid objections to the con-
tinued use of each of the two terms. “Ar-
chaic” is far from the oldest cultural mani-
festation and is just as inappropriate as was
the early denomination of Valley of Mexico
Formative cultures as “Archaic.” With
“naleo-Indian” we have a loaded word, “In-
dian” as yet relatively unsubstantiated by
physical evidence. I have no immediate sug-
gestions for the former but would definitely
prefer to use the term “Early Hunter”
rather than “paleo-Indian.”
ARCHAIC MANIFESTATIONS
Let us turn now to a brief consideration
of some of the units called Archaic.
In the Northeast, Ritchie (1944 and paper
presented at the 1955 Archaic Conference)
has defined a series of apparently local de-
velopments which are fairly well placed in
time and cultural stage in both the local
relative sequence and by radiocarbon dates.
In the Southeast and in the lower Ohio
Valley, Webb (1950a) and others have de-
scribed what must have been not only a
series of local developments, but also the
most intensive early occupation of North
America at the time period of 3000 B.C.
There is little evidence for actual contact
between these two groups although it is
generally agreed that they were at the same
developmental stage and equivalent abso-
lute and relative time periods.
Some evidence for connecting links be-
tween these main Archaic areas has come
to hght in the upper Ohio Valley where we
have found shellheap campsites (Mayer-
Oakes, 1955a). The inventory of artifacts
and the general characteristics of these sites
indicate a relationship to the Southeastern
materials. Within this “Panhandle Archaic”’
complex we are beginning to get evidence
for sequent steps in both developmental and
temporal terms. Major complexities begin-
ning to appear in the Panhandle complex are
the typological distinctiveness of the pro-
MAYER-OAKES: PLAINS EARLY HUNTER AND EASTERN ARCHAIC
147
jectile points in an early unit and the factor
of northern relationships in a later unit.
In addition, in the upper Ohio Valley,
there are other Archaic complexes within
which developmental steps are beginning to
be recognized.
Several years ago I suggested a third
major area of Archaic culture—the Plains—
and have recently discussed this in detail.
(Mayer-Oakes, n.p.b). A summary of per-
tinent information from this area is pre-
sented below.
This picture of an increasingly complex
internal structure recognized for various re-
gional Archaic units will probably apply to
most of the area under consideration. And
here we can bog down in a welter of specific
typological and other considerations of arti-
facts or traits. But before that happens, let
us push on back to the time of the Early
Hunters.
EARLY HUNTER MANIFESTATIONS
Until fairly recent years there has been
a tendency to equate fluted points with
paleo-Indian and let it go at that. Now,
however, there have been enough additional
finds and enough evidence for develop-
mental steps within paleo-Indian to war-
rant a reexamination of the whole question.
The old term “Yuma” has been fairly
successfully supplanted by names for the
more discrete projectile point types known
as “Eden” and “Scottsbluff.”” No new type
name has been applied to the parallel-flaked
lanceolate point unless we consider the “An-
gostura”’ point or the “Plainview” in this
category. Actually all four of these are dis-
tinct types.
Sellard’s (1952) study is an important
and comprehensive recent work on the sub-
ject of the paleo-Indian. (Wormington’s
most recent edition, 1957, has been released
since this paper was first prepared.) Per-
haps the biggest contribution it makes is
the suggestion of a specific sequence within
the general Early Hunter category. At
Blackwater Draw Locality Number 1 the
sequence of Clovis to Folsom to Portales
has been established by stratigraphy and
typology. There is even the hint of speciali-
zation in game animals; Clovis points are
associated with elephant; Folsom with Bi-
son taylorz; Portales with Bison.
148
In the southern High Plains, Clovis and
Folsom type points are perhaps easily segre-
gated. In other parts of North America very
few fluted points qualify as classic Folsom
type, so naturally most are called Clovis.
Because the Clovis point is more variable in
size, form and character of fluting, need
for more precise typological work is indi-
cated.
The Portales complex is interesting since
it apparently includes not only Eden and
Scottsbluff types, but also Plainview and
possibly Clovis types. Two radiocarbon
dates that apply to Plainview have been re-
leased=—5150)B ©; ==160) (O=i71) anda7220
B.C. +500 (Lamont, unpublished; Krieger,
1957). Two samples (0-169 and 0-170)
place the Portales complex at 43850 B.C.
+150 and 4280 B.C. £150, respectively.
With this rather solid stratigraphic foun-
dation let us consider other situations indi-
cating relative sequence within the Early
Hunter unit. Forbis and Sperry (1952) re-
port a stratigraphic sequence of points in
Montana that runs from Folsom to Scotts-
bluff to Signal Butte II. Davis (19538) has
described materials from the Red Smoke
and Lime Creek sites in Nebraska that con-
stitute a sequence from Scottsbluff to Plain-
view types. An average radiocarbon date of
7574 B.C. +450 (C-471) for the Lime Creek
site suggests contemporaneity with Folsom.
Holder and Wike (1949) report the ma-
terials for the Allen site on Medicine Creek
in Nebraska to be similar to Signal Butte I.
The radiocarbon date for the Allen site, 85438
B.C. £1500 (C-470) , is at considerable vari-
ance with the date for Signal Butte I—1495
B.C. +120. (L-104A, Kulp, Feely, and
Tryon, 1951: 566.)
Eden and Scottsbluff types were found at
the Finley site (Moss, 1951) which has been
dated geologically as between 5000 and 7000
B.C. This dating agrees roughly with the
culturally similar Sage Creek site for which
the average of two radiocarbon dates is
4926 B.C. +250 (C-302).
Hughes (1949) has reported on South Da-
kota materials characterized by a lanceolate
point he designates as the “Long” type, but
which is now known as the “Angostura”’
point. Radiocarbon dating places this com-
plex at 5765 B.C. +740 (C-454). A more
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 5
recent test for this unit yielded the date of
7430 B.C. £500 (M-370).
The Signal Butte finds (Strong, 1935)
have been somewhat controversial. Current
interpretations are based on a reexamination
by Bliss (1948) and a rather late radio-
carbon date (L-104A, average of two, 1495
B.C. +120, Kulp, Feely, and Tryon 1951:
566) for the early stages of this unit. These
facts indicate a late time position rather
than the originally suggested Karly Hunter
time.
A provocative unit recently mentioned in
print is the Lucy site in central New Mexico
(Roosa, 1956). Early Hunter in stage, the
blowout context of the site has produced
Clovis, Folsom and Sandia points as well
as mammoth and bison bones. Aside from
the presence of the rare Sandia type the site
iS unique in producing two fluted Sandia
points. Significance of this combination of
point styles is not clear but it may be evi-
dence for cultural as well as temporal cor-
relation of two otherwise distinct point
styles.
Without an attempt to examine in detail
these few situations, two conclusions seem
obvious. First, a real variety in forms of
projectile point definitely represents the
Early Hunter stage and period. Secondly,
we appear to have evidence for a series of
typologically developmental steps, in effect
a dynamic projectile point style tradition:
(1) fluted points of general or Clovis type;
(2) fluted point of special or Folsom type;
(3) lanceolate point; (4) stemmed point.
This sequence of types, however, appears at
variance with some of the chronologic data,
for example, the early Nebraska materials;
the Scottsbluff and Angostura points with
mammoth remains in central Mexico and
Clovis points with the Portales complex.
The Sandia point, moreover, cannot easily
be fitted into this sequence.
A fact to remember here is that at this
early period there are apparently complexes
of artifacts and points, especially in the
Southwest and Far West, which seem to be
of totally unrelated types (Jennings, 1957;
Haury, 1950).
Perhaps a consideration of types of points
of the Early Hunters in a fashion similar to
that applied to pottery types, using popu-
149
May 1959 MAYER-OAKES: PLAINS BARLY HUNTER AND EASTERN ARCHAIC
AREAS WEST PLAINS EAST TIME
(CALIFORNIA) (GREAT BASIN) Sage
: 2 PRESENT
/ \
re ‘ of %
4 ‘\ ? .
“ .
2.000
? SIGNAL BUTTE I
1 LAURENTIAN 4,000
PANHANDLE LAMOKA
STARVED ROCK OLD COPPER INDIAN KNOLL ;
ARCHAIC 6,000
COCHISE PORTALES
i] EVA
! ANGOSTURA EDEN SCOTTSBLUEF
1 PLAIN VIEW MODOC RUSSELL 8,000
\
: €— LEHNER => LIME CREEK \ wf
/
1 ? : ioeserny/—— NACo FOLSOM\\ GRAHAM CAVE \ (ARCHAIC) / 10,000
' OAK hi FRONTIER | NOP 4
\ GROVE i oped £1 y SUbZ,
\ n Ves < 3 wr
\ q “ i ? NO7, ?
\ 4 ” | 20,000
] '
- i SANDIA
/ TULE SPRINGS <——?——> |
ae $ ?
—<$—_—— 9? —________»
ROSA - eae 30,000
I
‘ Hi S pn?
ea
? gS 3
CLOVIS ee
we ¢
Sa,.07 40,000
TRADITIONS + EARLY MILLERS EARLY COLLECTORS
EARLY BIG GAME HUNTERS
EARLY FORAGERS
Ines al
larity history charts would help us to under-
stand the meaning of current data. It cer-
tainly seems reasonable to expect both
geographic and temporal variations in the
popularity of forms of points rather than
rigid conformance to a simplistic typological
formulation. Because of the extreme paucity
of data the statistical significance of this
approach may not be impressive but it
seems worth a try.
In addition to the variety of materials
classified without much question as of Early
Hunter origin, there are interesting units
in the Prairies and eastern Plains which
should be mentioned here. At Graham Cave
in Missouri, Logan (1952) has reported a
stratified sequence the lowest levels of
which (because of the presence of fluted
points) would in part unquestionably be
classed as Early Hunter in stage or in type.
Because, however, of a probable continuity
with and development into the upper parts
of the deposit (a generally eastern Archaic
unit) the possible antiquity and significance
of this site have not been stressed.
The preceramic complex which I first re-
ported in 1949, from Starved Rock, IIl., is
typologically oriented to the Plains area at
the level of the Early Hunter stage rather
than at the eastern Archaic stage. As a con-
servative pre-radiocarbon guess my range
of 3000 B.C. to 500 B.C. was intended to
convey a sense of time equality and slight
priority to the eastern Archaic period. In
the same mental operation, however, I have
never been able to shake the impression
that this Plains-oriented complex not only
had roots back to earlier times but may it-
self have existed at an earlier time. The
presence of a copper point at Starved Rock
has led some students to postulate connec-
tions with the nearby Old Copper complex;
some have seen this as a general indication
of lateness within the Archaic stage.
150 JOURNAL OF THE
ORIGIN AND DEVELOPMENT OF THE
PLAINS ARCHAIC CONCEPT
Perhaps the earliest publication pertinent
to our discussion is the report of excava-
tions at Signal Butte, Nebr., by Strong
(1935). Temporal interpretation in this re-
port is based on geological factors. The
original conclusion that the earliest levels
at the site were of great antiquity would
place them in an Early Hunter time period.
In 1950 Bliss criticized the interpretation of
Signal Butte I as an early complex. On the
basis of limited testing he split Signal Butte
I into three sequent typological stages and
suggested an alternative and much younger
dating. His contention is now supported by
a radiocarbon date of 1495 B.C. +120
(L-104A, Kulp, Feely, and Tryon, 1951:
566).
Excavations conducted in Nebraska in
1948 by Holder and Wike (1950) resulted
in the definition of the Frontier complex,
compared by the excavators to Signal Butte
I and other early Plains units, some of
which were just being discovered. Holder
and Wike (1949) suggest that the Frontier
complex is part of a larger Plains Archaic
unit. I believe this is the first published use
of the phrase to denote the present inter-
pretive concept. A subsequent radiocarbon
date on the Frontier complex of 8543 B.C.
+1500 (C-470) aligns this unit with the
earliest known on the Plains and is com-
pletely at variance with the recent date as-
signed to Signal Butte I.
Initial studies of the prepottery unit
found at Starved Rock in 1947 and 1948
indicated the cohesiveness of the unit as
well as the distinctiveness of the projectile
point complex. Examination of projectile
point specimens from the Plains area dis-
played at the 1948 and 1949 Plains Archaeo-
logical Conferences, and in museums at
Lincoln impressed me with resemblances be-
tween the Starved Rock Lanceolate type of
projectile point and points from the Angos-
tura reservoir in South Dakota, the Frontier
and Lime Creek complexes, and the Nebo
Hill complex.
The final season of excavations at Starved
Rock, in 1949, was carried out with a view
to establishing the prepottery complex sug-
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 5
gested by the testing of the previous two
years. Conclusions derived from it did sub-
stantiate and expand our knowledge of the
complex I called “Starved Rock Archaic”
(Mayer-Oakes, 1951). In order to fit this
unit into the general framework of known
units I was compelled to make use of an
idea latent in much archeological discussion
of the time—the concept of a Plains culture
area on an Archaic stage or time level. I
did, as a matter of fact, draw specific com-
parisons between Starved Rock and Fron-
tier, Angostura, Nebo Hill, and Signal Butte
I. None was blessed at that time with ab-
solute dates, so comparisons of typology
and stage were paramount within the gen-
eral framework of prepottery times.
The concept was invoked to explain an
Illinois complex of material traits which had
primary similarities to early stone industries
in the Plains but contained, as well, traits
also found in eastern Archaic or other units.
The area was conceived of as a zone of inter-
change between East and West during the
relatively recent Archaic period.
Subsequent to my specific suggestion of
a Plains Archaic, several finds gave support
to the concept. Rowe (1952) has reported
Plains Archaic materials from southwestern
Iowa. Graham Cave (Logan, 1952) docu-
ments the progressive change from a Plains-
oriented unit to an eastern Archaic unit. The
lower levels of Graham Cave are definitely
units to be understood as part of the Plains
Archaic, both typologically (in the sense
of combining Early Hunter and Archaic
styles) and geographically. Dates range
from 7750 B.C. +500 (M-130) and 6680
B.C. +500 (M-131) both for Level 6, to
5950 B.C. +500 (M-132) from Level 4, a
recognizable Eastern Archaic assemblage.
Baerreis has reported an Early Archaic
site near Madison, known as the Airport
Village. This site is considered to be tran-
sitional, typologically, between paleo-Indian
and Early Woodland. The “mixed” assem-
blage is tentatively interpreted as a unit
with closest affinities to Starved Rock Ar-
chaic. Here again, is a unit ascribable both
typologically and geographically to Plains
Archaic.
McGregor (1954) specifically aligns an
Archaic complex at the Chrisman site in
May 1959
southern Illinois with Starved Rock Ar-
chaic, and further suggests that both are
parts of an Illinois River aspect of a Plains
phase within the broad Archaic pattern.
This is one of the few published extensions
of the concept.
The type of point from the Angostura
reservoir which Hughes (1949) called the
“Long” point, and is now known as the
Angostura point, has become a key type in
the Plains. Because its form is identical
with that of the Starved Rock Lanceolate
type. I feel it is highly significant to a dis-
cussion of the Plains Archaic concept. This
type is widespread; it occurs in southern
Texas (Orchard and Campbell 1954) and
northwestern Canada (MacNeish, 1955).
The Angostura type site is dated at 5765
B.C. =740 (C-454) and 7430 B.C. +500
(M-370). While the occurrence in Texas is
not dated, the point occurs in an uncertain
context which may be early Archaic, at
about 4000 B.C. The point found by Mac-
Neish in Pit 2, site N.W.T.53, and assigned
to the Great Bear River complex is placed
im 2o00Nb.©. ==230 (MacNeish, 1955).
Two points found with the second mam-
moth at Iztapan (Aveleyra, 1956) are par-
ticularly interesting because they are not
fluted. Rather, they were lanceolate points,
one a fair example of an Angostura, the
other a “laurel leaf.” While this find ex-
tends the geographic range of the Angostura
type far to the south, the time factor here is
unknown. The association with extinct
fauna is important, however, since Angos-
tura points are rarely in such a context.
The most recent southward extension of
North American Plains point styles is re-
ported by Cruxent and Rouse (1956) from
Venezuela. A lithic complex termed “El
Jobo” contains a number of points of An-
gostura and Plainview (or Nebo Hill and
Lerma) style together with scrapers. The
stylization is close enough to the North
American types to suggest historical rela-
tionships. This in turn lends support for ac-
ceptance of the crude Folsom-like fluted
point reported from Costa Rica (Swauger
and Mayer-Oakes, 1952).
A recently reported unit which fits our
concept of Plains Archaic is the Havey site
near Madison, Wisconsin. A surface collec-
MAYER-OAKES: PLAINS EARLY HUNTER AND EASTERN ARCHAIC
151
tion from this site is interpreted by Nero
(1955) as belonging to a complex transi-
tional between paleo-Indian and Early Ar-
chaic. Although not cited as such by the au-
thor, the Havey site is a good candidate for
Plains Archaic from the point of view of
both typology and geographical location.
The most recent field work relating to the
Plains Archaic concept was carried out in
southeastern Saskatchewan during 1957.
Here, at a deep stratified site (BDR 6) on
Long Creek, a tributary to the Souris River,
several sequent units of an appropriate age
have been excavated (Mayer-Oakes, N.D.c;
Wettlaufer, n.p.). Three levels of occupation
at depths of from 4 feet to 8 feet beneath the
present surface provide evidence for a bison-
hunting archeological complex characterized
by Duncan and Hanna points plus some lan-
ceolate forms in the lowest level. Radio-
carbon dates for the lowest level give an
antiquity of 5000 years. Here, then, is an as-
semblage generally similar to the eastern
Archaic, but existing in the mixed-grass
northern plains at 3000 B.C. when the La-
moka and Laurentian peoples were estab-
lished in New York State. We have here end
dates for the Plains lanceolate point tradi-
tion in this area.
RECENT DEVELOPMENTS
In a broad developmental synthesis of
New World archeology, Willey and Phillips
(1957) have recently made use of the Plains
Archaic Concept in an effort to interpret var-
lous components known from the Plains and
Prairies. They have recognized that several
of these units give better evidence for a
Lithie stage of development than an Archaic
stage, but prefer to interpret all as basically
on an Archaic level. In the light of several re-
cent radiocarbon dates and information pre-
sented at the recent Archaic Conference, I
feel this position needs revision.
For some time the well known Old Copper
complex of Wisconsin has been considered a
late Archaic unit and thus it was striking to
note the early radiocarbon dates released in
1954 (Ritzenthaler, 1954). Two samples
gave dates of 3650 B.C. +600 (C-836) and
5560 B.C. +600 (C-837, C-839) respectively.
One of the sites early considered as an 1m-
portant Plains Archaic unit is Graham Cave.
152 JOURNAL OF THE
Radiocarbon dates indicate that Level 6 was
occupied from 7750 B.C. +500 (M-130) to
6880 B.C. £500 (M-131). The intermediate
level 41s dated at 5950 B.C. +500 (M-132).
In view of the rather complete previous ac-
ceptance of this material as “Plains Archaic”
the dates seem surprisingly early.
Radiocarbon dates on Tennessee Archaic
units indicate that the early Eva complex
goes back to 5200 B.C. +500 (M-357). This
date is some 2000 years older than other
eastern Archaic dates and apparently corre-
lates with level 4 at Graham Cave wherein
the Missouri complex has taken on a de-
cidedly eastern flavor.
Still a third series of important radiocar-
bon dates was published by Fowler, Winters,
and Parmalee (1956: 31) in their report on
the Modoc Rock Shelter. This deep stratified
site produced a range of eastern Archaic ma-
terials throughout its 26 feet of deposit, with
average dates ranging from 3657 B.C. to
7922 B.C. An important correlate of these
dates is the observation that polished stone
is present at the earliest surely Archaic level
and dates to 6210 B.C. Fowler concludes that
the Modoe finds extend the period of eastern
Archaic culture back to at least 6000 B.C.;
he sees these dates as support for and in turn
supported by the dates on Old Copper. There
is, however, no suggestion of a Plains Ar-
chaie connection with the Modoc materials.
The most recently released early eastern
Archaic date comes from Russell Cave in
northeastern Alabama (Miller, 1956). From
the 14-foot level in a deep stratified deposit
not yet excavated to bottom has come a date
of 6210 B.C. £300 (L-344; Miller, 1957).
The associated cultural material is not fully
reported but it appears to be early south-
eastern Archaic with point styles very much
like the “Steubenville Stemmed” and “‘Steu-
benville Lanceolate” points of the Ohio
Valley Panhandle complex.
In a recent description of an Early Ar-
chaic complex from the Upper Ohio Valley
(Mayer-Oakes, 1955a) I have suggested
that the typology of Panhandle Archaic pro-
jectile points is derived from late paleo-
Indian complexes. A subsequent site report
and seriation study of these points (Mayer-
Oakes, 1955b) indicates the western affinities
of this Early Archaic shellmound complex.
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 5
Several geographers and ecologists (Borch-
ert, 1950) have pointed out the existence of
a “Prairie Peninsula” which extended east-
ward into Ohio, Pennsylvania, and New
York during the Post-Glacial Thermal Max-
imum (or Altithermal) about 6000 to 3000
B.C. This wedgeshaped corridor of grassland
extending into the eastern Woodlands was a
convenient ecological zone for exploitation
by the western hunters when and if the High
Plains became too arid for normal activities.
Powell (1955) has recently suggested that
we look for natural migration routes in at-
tempting to explain movements of Early
Man in North America. The Canadian gla-
cial lakes and Great Lakes as well as the
waterways of the northern Mississippi Val-
ley form a logical route from northwest to
southeast which, at the time of the eastern
grassland extension, would have increased
the lkelhhood of general movement from
west to east.
This idea of a prairie peninsula is impor-
tant in understanding the nature of the ear-
liest Archaic unit in the Upper Ohio Valley.
It consists of a complex of subsistence traits
with emphasis on hunting, and of tools, ex-
pressed in styles of projectile points, which
was brought in from the west via the Prairie
Peninsula by units of the Plains Archaic.
Contact with neighboring resident early Ar-
chaie units and adaptation to riverine life
resulted in local development of a distinctive
Archaic culture. This Panhandle Archaie
continued to be influenced by northern Ar-
chaic units and gradually lost its western
orientation. It changed, thus, from the most
eastern component of the Plains Archaic to
a unique local Archaic.
In addition to the various lines of recent
evidence cited above which suggest that Ar-
chaic cultures are longer-lived than previ-
ously considered, there have also been signs
in recent years that the Early Hunter ecul-
tures are quite varied in typology. Whereas
the term has often been restricted to units
characterized by use of fluted points, radio-
carbon dates and geological dating factors
indicate that various nonfluted point sites
are equivalent in age to Folsom and that the
general lanceolate point horizon covers a
large area of North America for a span of
several thousand years. I refer here to the
May 1959
following expressions: the Scottsbluff and
Angostura points found associated with
mammoth remains in the Valley of Mexico;
the Early Hunter sequence at Blackwater
Draw showing Clovis, Folsom, and Portales
units in stratigraphic succession; the Mon-
tana stratigraphic sequence of points run-
ning from Folsom to Scottsbluff to Signal
Butte II; the Lime Creek sequence of Scotts-
bluff to Plainview and the Red Smoke se-
quence of Frontier to Plainview; the early
radiocarbon date on the Frontier complex;
the radiocarbon dates for Eden and Scotts-
bluff points at Sage Creek; and the radio-
carbon date on the Angostura type site.
The age of more than 37,000 years (0-235,
0-248) for hearths near Lewisville, Tex.,
with an associated Clovis fluted point has
caused understandable consternation. Krie-
ger (1957) discusses this find in detail. Sig-
nificant to our problem in this paper is the
stretching back in time of the Early Hunter
stage far beyond our expectations of 1955.
It is hard to believe that one point style ex-
isted for a period of at least 28,000 years. If
accepted, this date certainly points up the
need for defining types within the broad
Clovis fluted category.
DISCUSSION
The question of Archaic origins has not
yet been satisfactorily answered. In many
areas of the New World, Archaic cultures
appear as the first occupation for which
there is much detailed evidence. Although
Griffin (1946) suggested lumping Archaic
and paleo-Indian together under the latter
term, there do seem to be good reasons for
retaining at least these two categories. Cer-
tainly the amount of time involved would
indicate this; the development from a simple
hunting to a diversified hunting-gathering-
fishing, semisedentary pattern would also in-
dicate such a dichotomy.
While, as Griffin suggests, there no doubt
are strands of cultural continuity from the
earlier to the later units, these have not yet
been recorded in any detail.
Perhaps the most convincing explanation
for an Archaic source is Spaulding’s (1946)
suggestion of an Old World impetus for the
Northeastern Laurentian. While there are
many aspects of the Archaic for which Old
MAYER-OAKES: PLAINS EARLY HUNTER AND EASTERN ARCHAIC
153
World parallels and sources have not yet
been suggested, it seems reasonable to as-
sume that strong LEurasiatic influences
helped formulate the distinctive eastern Ar-
chaic as well as subsequent Woodland com-
plexes.
What can we say about local sources for
the Archaic? One line of thought has us
looking to the preceding Early Hunter stage.
The area east of the Mississippi has so far
not been productive of evidence for this.
Most of the definite Early Hunter complexes
here are not tied into any local sequence and
most of them show no signs of continuity
with or influence on later Archaic complexes.
There are three main exceptions to this: (1)
Coe (communication from Witthoft) has
found a stratified sequence of points in North
Carolina which apparently stretches far
back into the Early Hunter time period, yet
bears no obvious relationship to the Plains
“sequence” or the fluted point complexes of
the east. (At this site we apparently get into
problems of Early Hunter period complexes
that are in the tradition of the Southwest
and Far West rather than the fluted and
lanceolate point.) (2) Ritchie (1953) has re-
ported a paleo-Indian site in Vermont with
a point inventory that includes both fluted
and unfluted forms, some quite similar to
the Starved Rock Lanceolate type, and thus
suggestive of Plains Archaic contacts. (3)
The Panhandle complex in its earliest stages.
There is one site in the east which gives
fairly good evidence for the priority of fluted
points to Archaic points. Aside from this
unit—the Parrish site (Webb, 1951)—there
is only typological evidence for the place-
ment in time of the eastern fluted points.
The apparent gap in occupation of the
Plains from about 5000 B.C. to 2000 B.C.
has prompted Krieger (1950, 1953) to evoke
climatic factors as explanation. This is an
attractive theory and seems not only to fit
the data but also to have some bearing on
the problem of Archaic origins.
INTERPRETATIONS
On the basis of the recent developments
sketched above, we are beginning to see the
eastern Archaic as a longer-lived and more
broadly conceived stage of cultural develop-
ment, having continent-wide relationships.
154
The Early Hunter cultures are seen as a spe-
cialized development partly preceding and
partly contemporaneous with the earliest
part of the Archaic period and related to Ar-
chaic units in at least one well established
way, as expressed in the concept of a Plains
Archaie.
Taking a broad view of the cultural va-
riety present in North America at the time
period of 10,000-12,000 years ago, Sauer
(1957) proposes three basic patterns of en-
vironmental adjustment. These he calls:
“Old Bison Hunters” (Folsom-Yuma
units) ; “Old Basketmakers” (Great Basin
units); “Ancient Millers” (California Oak
Grove and Cochise units).
While I feel that the third pattern is the
least acceptable and most controversial one,
it is equally possible to consider the eastern
Archaic as a fourth major pattern of hunt-
ing and gathering—foraging—related by
subsistence and traditions of technology to
both the “Old Bison Hunters” and “Old
Basketmakers,” but existing as a distinctive
combination of the two.
So far I have avoided qualifying the
phrase ‘Plains Archaic.” I have used it to
imply both time period and stage as well as
tradition. Originating as a simple space-
time concept, it has developed both his-
torical and developmental significance. At
the present time the most reasonable use
for the concept is as an historical con-
tinuum, comprising a tradition (in the sense
of the term as defined in Willey and Phillips)
of basic hunting-gathering economy ex-
pressed materially in a restricted range of
projectile point styles and associated, al-
though poorly known, tools. Out of the vari-
ous styles of lanceolate points present at the
earliest part of the Early Hunter period, a
small number were continued for lengths of
time varying with the specific area. In gen-
eral, the “unfluted Folsom” style and the
broad-stemmed Scottsbluff style were car-
ried from the central Plains to the north,
east, and south as Postglacial time and
ecological changes went on. Contacts with
resident local Archaic units resulted in com-
plexes which can be explained and under-
stood on the basis of this Plains Archaic
lithic tradition.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 5
The Plains Archaic concept is thus seen
to comprise a cultural unit of historical con-
tinuity over a period of perhaps 7000-8000
years within the Plains and Prairies geo-
graphic areas. Roots of the tradition are in
the earliest Plains lithic complexes. There
is apparently no fundamental change in
basic hunting-gathering economy although
there is probably a change in degree to
which big game herds were utilized as a
major means of subsistence.
In trying to apply their “Lithic” and “Ar-
chaic”’ developmental stages to the Plains
area, Willey and Phillips recognized the di-
lemma posed by the available evidence. On
the basis of this evidence, I think it is prac-
tically impossible to define or segregate,
meaningfully, these two stages. The rela-
tionship among all Plains preceramic units
are too strong. However, by assuming that
there was a development towards an Ar-
chaic stage, we can align some of the other-
wise floating units into a schematic order
based on this concept of the Plains Archaic,
or more simply, a Plains tradition.
Perhaps the earliest well-established units
of the Plains tradition series would be the
Frontier complex followed by Scottsbluff
and Plainview units. All these could be
classed as Early Hunter in period, but since
they are more generalized in typology than
the fluted point units they are the best basis
for the general tradition. With the increas-
ing popularity of a complex distinguished
by Angostura points we are fully into the
time period characterized by units of Plains
tradition, which continues on as at Graham
Cave, Starved Rock, Nebo Hill, Airport
Village, Havey site, and Signal Butte I.
The most eastward thrust of this tradi-
tion is expressed in the Panhandle Archaic
of the Upper Ohio Valley, in which there
is a unique combination of Plains projectile
point traditions and local seasonal adapta-
tions to a riverine ecology. Interestingly
enough, the crude Plainview-like lanceolate
points seem to drop out of style by late Ar-
chaic times in the east, but the Scottsbluff-
like Steubenville Stemmed points continued
to be a favorite style, moving eastward to
the Atlantic coast (Ritchie, 1958) and form-
ing in the Ohio Valley the basic Early Wood-
land style.
May 1959
SUMMARY
In this paper we have briefly discussed
some features of Early Hunter and Archaic
relationships, restricting our geographic
area of interest to the region east of the
Rockies and considering only a selection of
the possibilities. We have indicated how the
subject terms can be used in the temporal,
developmental and typological or tradi-
tional sense and have attempted to distin-
guish these in our discussion.
Major points proposed are:
1. Eastern Archaic is seen as part of a
fairly homogeneous cultural stage—Early
Foragers—incorporating both temporal and
typological variety on a broadening geo-
graphic basis, but with a longer time span
than was hitherto believed possible. It over-
laps, in part, the time period characterized
by Early Hunter remains.
2. Plains Early Hunter is seen as part of
a cultural stage—Harly Big Game Hunters
—inecorporating significant temporal and
typological varieties, the latest and eastern-
most of which reflect some contact with the
eastern Archaic.
3. The concept of Plains Archaic has been
suggested as the concrete expression of the
contact between the Plains tradition and
the eastern Archaic. Plains Archaic may be
considered as the pattern characteristic of
the late period of Early Hunter culture, ex-
pressed materially as an acculturation proc-
ess between two coexisting great cultural
eroups, the Karly Foragers and Early Big
Game Hunters.
An alternative approach at a more general
level, making use of continent-wide data is
eraphically presented in Fig. 1. Here, four
basic early subsistence patterns are repre-
sented as traditions rather than as stages.
All but “Early Foragers” may in fact
qualify as “Lithic” in the sense of Willey
and Phillips’s stages. There is difficulty in
consistently distinguishing ‘Early Millers”
from some of the “Early Collectors”; there
may be basic direct relationships among
all of these units. I feel, however, that the
simple dichotomy proposed by Jennings and
others (1956) is inadequate. A “Desert” cul-
ture and a “Plains paleo-Indian” as the
basic early units need to be supplemented
MAYHR-OAKES: PLAINS EARLY HUNTER AND EASTERN ARCHAIC
155
by the units proposed here in our chart. In
doing this I admit to being strongly in-
fluenced by the early dates on eastern Ar-
chaic and Sauer’s suggestion of an “Ancient
Miller” pattern.
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May 1959
LOOMIS: MILLIPEDS COLLECTED FROM FLORIDA TO SAN ANTONIO
157
ZOOLOGY—Miullipeds collected enroute from Florida to San Antonio, Texas,
and vicinity. H. F. Loomis, Miami, Fla.
(Received March 26, 1959)
In the latter half of December 1958, the
writer and his wife visited San Antonio,
Tex., spending some time collecting milli-
peds on the way and in the region about San
Antonio. One day was devoted to searching
the Kerrville area in the hope of rediscover-
ing several of the more unusual species de-
seribed from there by Prof. R. V. Chamber-
lin alone or in conjunction with Stanley
Mulaik, and some success was had. The col-
lection as a whole resulted in the finding of
five new species, one of which represents a
new genus, and in establishing further lo-
calities for several known species. Descrip-
tions and data on these are here presented
as well as descriptions of three other new
species received following our return to
Florida. Unless otherwise stated all collec-
tions reported were made by E. M. and H.
F. Loomis.
Type specimens of all species described
are deposited in the U.S. National Museum.
Family DESMONIDAE
Genus Desmonus Cook
Desmonus Cook, Proc. U. S. Nat. Mus. 21: 463.
1898.
Ethocyclus Chamberlin and Mulaik, Journ. New
York Ent. Soc. 49: 58. 1941.
Specimens of this genus from five localities
within a radius of approximately 100 miles of
San Antonio present several interesting features.
None of these millipeds appear to have been de-
scribed as belonging to this genus, and all have
certain characters in common that probably are
generic but may be only specific; a question that
can not be determined with any degree of satis-
faction without additional and more widely col-
lected material. From experience in making the
present collection this should become available
upon proper search.
The discovery of Desmonus between Bandera
and Helotes came during the return from Kerr
County to find additional specimens of species
collected there by Mr. and Mrs. Stanley Mulaik
and described in the paper by him and Professor
Chamberlin (loc. cit.). It had been hoped to ob-
tain snecimens of Ethocyclus atophus, but no
cyclodesmids were found. However, with the
finding of the Desmonus and subsequent speci-
mens in the region a careful reexamination of
the description of Hthocyclus forced the con-
clusion that it is a desmonid rather than a cyclo-
desmid.
While the first three segments are of quite
similar shape in the Cyclodesmidae and Des-
monidae, the fourth segment in Ethocyclus is
described as laterally broader and less acute than
the fifth segment, a normal condition for the
latter family but applying in only the smaller of
the two genera of the former. The first segment
of E'thocyclus is said to bear two transverse rows
of setae and “on typical segments the posterior
portion of tergite elevated above level of anterior
portion and divided into low tubercular swellings
which appear to have born(e) setae forming a
transverse series.” These are characters of Des-
monus attributed to no other cyclodesmid than
Ethocyclus, and hence the latter genus is placed
as a synonym of the former.
The Texas specimens, representing three spe-
cles, are in the group having 20 segments; all
are essentially white in color but have a coating
of organic matter; pits are at the anterior junc-
tion of carimae and dorsum of segments 3 through
20; head with a definite low ridge beginning
between the antennae and extending upward
halfway to segment 1, where it terminates and is
succeeded by an impressed sulcus across the ver-
tex; segments 1 to 4 with two transverse series
of short, well-separated setae which are reduced
to a single series on ensuing segments; segment
4 with outer margin of lateral keels elongate,
sometimes slightly rounded, in shape intermedi-
ate between the keels of segments 8 and 9; dor-
sal tubercles usually beginning on segment 5
and continuous through segment 19 but lacking
or very indefinite on segment 20; males with
lateral keels of segments 5 to 15 at least, more
oblique than those of female, the dorsal tubercles
also more prominent.
In the accompanying descriptions and illus-
trations it will be seen that the three species are
very closely related and a wider range of speci-
mens may show that one or two of them will
have to be reduced in rank. The dorsal tubercu-
158
lation varies greatly in amount in specimens
within the species but seems to be typical for
each of them. None of the specimens of dis-
tinctus has the tubercles of segment 19 coalesced
to form two enlarged swellings as occur in the
other two species, and conjunctus does not have
the tubercles of the midbody segments as high
or inclined as in crassus but does have those of
segment 19 larger than on preceding segments.
Differences of the gonopods are slight between
the species, as Dr. Causey has observed’ for the
other species in a recent paper on the family,
while within the present species considerable
variation has been noted. For none of the previ-
ously described species has mention been made
of the distinct cephalic ridge, which may be a
feature limited to the new forms.
Desmonus conjunctus, n. sp.
Male type and female from between Bandera
and Helotes, Tex., December 26, 1958, co-collec-
tor J. C. Loomis; a male and 3 females from
Landa Park, New Braunfels, and 2 males from
Lake Placid, between New Braunfels and Seguin,
Tex., December 29, 1958.
Description—Largest specimen, a female, 9
mm long and 1.7 mm wide. Dorsal swellings or
tubercles usually first evident on segment 6,
rarely on segment 5, and increasing slightly in
prominence thereafter, becoming strongest on
segments 17, 18, and 19, on the latter of which
the three innermost tubercles on each side are
united imto a single large rounded boss sur-
mounted by the three setae of the individual
tubercles (Fig. 1). In an extreme variant in
sculpturing the male from New Braunfels shows
much more prominent tubercles than any other
specimen, and on segments 17 and 18 the three
innermost ones on each side are united as on
segment 19. In none of the specimens are any
lateral tubercles evident below the compound
Proc. Biol. Soe. Washington 71: 173-78. 1958.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 5
ones on segment 19. Last segment without tu-
bercles. Gonopods as shown in Figs. 2 and 3.
Desmonus crassus, Nl. sp.
Five males (1 the type) and 8 females from
Victoria County, Tex., labeled “8-06 J. D. Mitch-
ell” sent me for examination by Richard L. Hoff-
man from the National Museum collection.
Description—This is a stouter species than
either of the other two described here, attaining
a length of 8 mm and a diameter of 1.9 to 2 mm.
Tubercles generally more prominent than in the
other two species, beginning on segment 5, where
frequently they are quite distinct, and increasing
in size thereafter and on the most strongly sculp-
tured specimens they are considerably raised, in-
clined caudad, with setiferous apex devoid of
coating and shining; segments 18, 19, and some-
times 17 with the three inner tubercles on each
side united into a single large inclined tubercle
with that on segment 19 smaller than that on
18; segments 18 and 19 without other lateral
tubercles.
Gonopods with anterior arm showing two or
three teeth, the posterior arm more slender at
apex than in the other species (Fig. 4).
Desmonus distinctus, n. sp.
Five males (1 the type) and 5 females “‘col-
lected under rocks and logs in closely grazed pas-
ture land with a few oaks and cedars on the
Beauregard Road about 5 miles SSW. of Boerne,
Tex., January 31, 1959,” by J. C. Loomis.
Description —Largest specimen, a female, 8.5
mm long and 1.5 mm in diameter. In general the
tubercles are more prominent than those of
conjunctus but less so than in crassus, although
in one or two females the tubercles are not in-
dividually indicated except by the location of
the setae; the males, however, have tubercles
beginning on segment 5, becoming stronger
thereafter and quite uniform in size from seg-
Figs. 1-23.—1-3, Desmonus conjunctus, n. sp.: 1, segments 19 and 20 of male, posterior view; 2, right
gonopod, lateral view; 3, apex of left gonopod of Landa Park male, lateral view.
n. sp., left gonopod, lateral view.
4, Desmonus crassus,
5, Desmonus distinctus, n. sp., apex of right gonopod, lateral view.
6, 7, Ilyma digitata, n. sp.: 6, right gonopod, lateral view; 7, apex of right gonopod, lateral view. 8,
Pseudopolydesmus bidens, n. sp.: left gonopod, mesal view.
right gonopod, mesal view.
9, Pseudopolydesmus minor (Bollman):
10-14, Mecistopus varicornis, n. sp.: 10, joints 6 and 7 of female antenna;
11, joints 6 and 7 of male antenna; 12, right anterior gonopod, lateral view; 13, ninth male legs, posterior
view; 14, basal joints of tenth male legs, anterior view. 15-18, Aniulus vestigialis, n. sp.: 15, left
mandibulary stipe of male; 16, left anterior gonopod, lateral view; 17, left posterior gonopod, mesal
view; 18, left posterior gonopod, caudolateral view. 19-23, Ziniulus ambiguus, n. sp.: 19, stipe and
first two segments of male, lateral view; 20, right anterior gonopod, lateral view; 21, right posterior
gonopod, lateral view; 22, apex of right posterior gonopod, caudal view; 23, apex of uncate blade of same
gonopod, mesal view.
May 1959 LOOMIS: MILLIPEDS COLLECTED FROM FLORIDA TO SAN ANTONIO 159
17 20
19 2 |
Figs. 1-23.—(See opposite page for legend).
ZS
160
ment 7 to 17, although not so high or sharply
marked as in crassus, those on segment 18
slightly larger, but only the second from within
larger on segment 19, which has 2 to 5 distinct
tubercles on each side with none coalesced as in
the other species. Last segment with two very
low, indefinite tubercles sometimes present.
Gonopods as shown in Fig. 5.
Desmonus atophus (Chamberlin and Mulaik)
In order to allow absolute verification of its
family and generic position and its relationship
to the species here described, a specimen of
atophus was requested of Professor Chamberlin,
but word has been received that he was unable
to find the original material; hence, these mat-
ters await finding of the lost specimens or col-
lections from the type locality, presumably
Raven Ranch, although only Kerr County was
so designated.
A NEW NAME IN CYCLODESMIDAE
In studying the original description of Des-
monus (Cyclodesmus) atophus (Chamberlin and
Mulaik), Dr. Carl’s notes and illustration of
Cyclodesmus aztecus Humbert and Saussure, the
genotype, were reviewed in Rev. Suisse Zool. 10:
678-9, pl. 12, fig. 109, 1902. The conclusion was
reached that the West Indian species heretofore
included under Cyclodesmus belong in a differ-
ent genus for which the name Caribocyclus is
proposed, with the Haitian Cyclodesmus angusti-
pes Loomis as the genotype. This genus is dif-
ferentiated from the Mexican Cyclodesmus by
having each gonopod composed of one or two
more or less slender branches rising above the
basal jomt. In the species having 2 branches
these may be separated, partially fused, or com-
pletely united. The illustration of C. aztecus
shows the gonopod with an expanded and curved
outer jomt sheathmg the simple and evenly
curved seminal one.
Family STYLODESMIDAE
Genus Ilyma Chamberlin
Ilyma Chamberlin, Bull. Univ. Utah 31(11): 24.
1941.
KEY TO THE SPECIES ILYMA
1. Segment 1 with 12 primary tubercles in two
transverse series of 6 each
colotlipa Chamberlin
Segment 1 with 10 primary tubercles arranged
essentiallyein 2 onOwSiaes = to - eae 2
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 5
2. Segment 1 with outermost primary tubercle on
each side larger than any of the others
orizaba Chamberlin
Segment 1 with outermost primary tubercle on
each side not so large as or no larger than the
Others 2. owe. e eo sew n> ee 3
3. Segment 19 with posterior processes greatly ex-
ceeding the tip of segment 20...cajuni Loomis
Segment 19 with processes shorter, only equal-
ing the tip of segment 20...°. 22a. oe eee 4
4. Processes of segment 19 broad, the sinus between
them rather shallow and U-shaped
morela Chamberlin
Processes of segment 19 narrow, the sinus be-
tween them deep and V-shaped.
digitata n. sp.
A mexican species, potosina Chamberlin, was
established on a single fragmentary female, lack-
ing two molts of maturity! Its juvenile charac-
ters are not comparable with the mature ones
of the other species, and its true identity will be
difficult to determine.
Ilyma cajuni Loomis
Three males and 5 females collected by Leshe
Hubricht, December 12, 1954, in Cameron
County, Tex., at “Rabb Ranch, near southmost
(?), under palm logs,” and sent me by Richard
L. Hoffman.
These specimens were compared with para-
types of cajuni without finding specific differ-
ences. The species has the primary tubercles of
segment 1 arranged as in the following species
except that the space between the two median
tubercles of both rows is much wider than that
between any of the other tubercles.
Ilyma digitata, n. sp.
A male (type) and 4 females, one immature,
found beneath logs beside U.S. Highway 190
between Kinder and LeBlanc, La., December 20,
1958.
Diagnosis —Relationship with morela is indi-
cated by the size of the body, the short processes
of segment 19, and certain characters of the
gonopods, although these differ materially in the
two species.
Description—Length of male and largest fe-
male 6 mm, width 0.9 mm. Vertex, first segment,
and posterior divisions of other segments black;
front of head, antennae, anterior subsegments,
segment 20, and all ventral surfaces, including
the legs, colorless.
Head with vertex not greatly raised above the
front but with 20-28 sharply rounded tubercles
May 1959 LOOMIS: MILLIPEDS COLLECTED FROM FLORIDA TO SAN ANTONIO
of various sizes, the largest at the lateral margins
behind the antennae but the margins not raised
into a granular ridge as in cajuni.
First segment with only the four large, equi-
distant, primary tubercles in front forming a
distinct row; the other six primary ones also
equidistant from each other, one on each side
of middle at posterior margin, a second latero-
cephalad of it and the third still further forward
and outward, behind and laterad of the outer
tubercle of the front row. In addition there are
many smaller tubercles of varying sizes including
a dozen or more along the posterior margin,
standing erect and not projecting beyond it.
Body with lateral carinae quite narrow, de-
scending more obliquely than in cajuni, the pores
opening from blunt and cylindrical tubercles as
long as thick, not in the least conical. Dorsum
of segments with customary 4 rows of primary
tubercles extending from segment 2 to 19, the
median rows on the latter elevated but not thick-
ened, and produced backward into 2 outwardly
parallel processes that equal but do not exceed
the tip of segment 20 which is visible in the
deep V-shaped sinus between them. Secondary
tubercles about 6 in number between the median
primary rows but lacking behind segment 16;
the 3 secondary ones between the outer and in-
ner primary rows on the anterior four-fifths of
body lacking on the posterior fifth. Last seg-
ment as in cajuni.
Gonopods as shown in Figs 6 and 7.
Family PoLyDESMIDAE
Dixiedesmus erasus (Loomis)
Two males and 6 females from east side of
Blakely River, Ala., before entering the flats
east of Mobile, on U.S. Highway 90, December
19, 1958.
Pseudopolydesmus bidens, n. sp.
Seven males (1 the type) and 5 females from
beside U.S. Highway 190, between Kinder and
LeBlanc, La., December 20, 1958.
Diagnosis —A small species, broader and flat-
ter than minor (Bollman), with anterior corners
of carinae dentate from segment 2 through 18,
and with distinctive gonopods.
Description—Largest specimen of each sex 12
mm long and 1.7 mm wide. Living color dark
brown, shining. Dorsum quite flat, the lateral
carimae broad, thin vertically at junction with
body; anterior corners scarcely rounded and
161
each with a distinct tooth on segments 2 through
18; lateral margins nearly straight, the porifer-
ous ones with 3 setae plus 1 on the posterior
angle, the nonporiferous ones with 2 plus 1 on
the angle; posterior angles larger and more pro-
duced on all segments, including 19, than in
minor. Last segment triangular in dorsal view,
its sides straight, not slightly emarginate as in
minor. Gonopods (Fig. 8) with only 2 triangular
lobes or teeth on the distomesal edge, the small
papillose process located more than halfway to
the tip of the gonopod.
Dr. Nell B. Causey kindly sent me a male and
female of P. minor, collected 1.5 miles west of
Conway, Faulkner County, Ark., December 24,
1953, by M. A. Jackson, which allowed me to
make direct comparisons with bidens. P. minor
is more slender and convex, with narrower lat-
eral carinae which are relatively thicker where
they join the body. Since a complete gonopod
of minor has not been illustrated previously, one
is shown in Fig. 9, in which the small papillose
area or tubercle shown a short distance above
the basal one is lacking from the opposite gono-
pod.
Pseudopolydesmus serratus (Say)
Male and many females from beside US.
Highway 190, at Kinder, La., December 20, 1958.
Family EURYMERODESMIDAE
Eurymerodesmus melacis Chamberlin and
Mulaik
Specimens collected in following Texas locali-
ties in December 1958: Kerrville-Bandera;
Landa Park, New Braunfels; McQueeney;
Schertz.
Family STRONGYLOSOMIDAE
Oxidus gracilis (Koch)
Numerous specimens from J. O. Vaughan
Ranch, Schertz, and from McQueeney, Tex.,
December 1958.
Family LysiopETALIDAE
Abacion tesselatum creolum (Chamberlin)
Male and female from Ponce de Leon, Holmes
County, Fla., December 19, 1958.
Abacion texense (Loomis)
Numerous specimens from Kinder-LeBlanc,
La., December 20, 1958; and following Texas lo-
162 JOURNAL OF THE
calities, December 1958: J. O. Vaughan Ranch,
Schertz; Kerrville-Bandera; McQueeney; Landa
Park, New Braunfels.
Family RHISCOSOMIDIDAE
Tingupa sp.
Two specimens, 4 mm long, with 28 segments
each and having essentially black markings col-
lected beside U.S. Highway 190 at Walker, La.,
December 20, 1958.
Family CLEIDOGONIDAE
Cleidogona sp.
Two females near Blakely River before enter-
ing flats east of Mobile, Ala., on U.S. Highway
90, December 19, 1958.
Mecistopus, n. gen.
Type—Mecistopus varicornis, n. sp.
Diagnosis—Included among genera having
ninth male legs 5-jointed but differmg in the
coxal joint and in having jomts 4 and 5 very
small. Relationship with Rhabdarona Chamber-
lin and Mulaik is indicated but the gonopods
reach back along the body, when at rest, with
tips inserted between the separated sterna of
legs 12 and 13. Sexual differences of the last
joint of the antennae also are unique.
Description—Body of intermediate size,
smooth and strongly shining with the outer dor-
sal seta on each side of segments 2 to 8-13
borne on a subconic tubercle set off above by a
distinet longitudinal impression.
Head with labral area convex and raised above
the front; last joint of antennae differing in size
and shape in the sexes.
Gonopods unusually long, bent strongly cau-
dad and lying in close contact with each other
and with the ventral side of body between the
coxae of legs 9 to 12 which have their sterna
broadened; tips of gonopods curving up toward
body between the well separated sterna of legs
12 and 138, the latter wider than the sterna that
follow.
Males with legs 1 and 2 shorter and more
slender than legs 3 to 7, which are crassate but
have no other special modification except that
the ventral face of the last joint of each leg is
papillose; ninth legs 5-jointed, basal joint large
and apically continued into a long, slender, erect
and acute process, jomts 4 and 5 very small;
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 9
legs 10 and 11 with the poriforation of each
coxal joint opening from a cylindrical process
behind which, on leg 11, is a conic tubercle;
twelfth legs lacking either process or tubercle.
Mecistopus varicornis, nN. sp.
Many specimens, including male type, col-
lected in collaboration with J. C. Loomis be-
tween Kerrville and Medina, Tex., along High-
way 16, December 26, 1958; a male from beside
the Beauregard Road, 5 miles SSW. of Boerne,
Tex., collected January 31, 1959, by J. C.
Loomis; and a male from Landa Park, New
Braunfels, Tex., December 29, 1958.
Description —Length 14 to 17 mm, the males
shorter than females. Fully colored living speci-
mens are shining dark chestnut-brown with a
very narrow longitudinal median light line, a
tiny light spot surrounding base of first dorsal
seta, and a larger oval light spot between the
two outer setae; the hyaline dorsal setae are
conspicuously silvery in daylight on the living
animal, giving it a coarsely fuzzy appearance.
Head with broad labral area convexly elevated
above the front and with lateral margins behind
it also elevated for a considerable distance; front
hispid, much more densely so adjacent to the
labrum; eyes well developed, triangular, in series
of ocelli arranged 7, 6, 5, 4, 3, 2, 1, from above;
antennae very long and slender, joint 3 longest,
joint 7 differing in both length and shape in the
sexes as shown in Figs. 10 and 11.
On segments 2 to 8 or 9 of female and 2 to
10-13 of male the outer seta on each side of dor-
sum is near the posterior margin and borne on
a distinct tubercle, largest in male, which is set
off from the surface above it by a conspicuous
furrow extending forward halfway across the
subsegment.
Anterior gonopods as shown in Fig. 12. Pos-
terior gonopods small, reaching only to about
the middle of the coxal joint of ninth legs and
consisting of 2 apically thickened structures re-
sembling wooden golf clubs on short shafts with
the heads directed outward. Ninth legs 5-jointed,
as shown in Fig. 13, the tiny, subhemispherical,
fifth joint almost black in contrast to the nearly
colorless preceding joints. Legs 10 (Fig. 14) and
11 as in generic description, the anterior face of
the broad sternum of each smooth whereas the
anterior median face of twelfth sternum has a
strong vertical ridge with sterna thereafter hav-
ing similar but smaller ridges.
May 1959 LOOMIS: MILLIPEDS COLLECTED FROM FLORIDA TO SAN ANTONIO
Family PARATULIDAE
Aniulus adelphus Chamberlin
Numerous Texas specimens from J. O.
Vaughan Ranch, Schertz; and McQueeney, De-
cember 1958.
Aniulus eraterus Chamberlin
Many specimens collected along Highway 16
between Kerrville and Bandera, Tex., in collab-
oration with J. C. Loomis, December 26, 1958.
Aniulus vestigialis, n. sp.
Male (type), female, and several immature
females from Landa Park, New Braunfels, Tex.,
December 29, 1958.
Diagnosis —Related to austinensis Chamber-
lin but differing from it and all others of the
genus in having the accessory blade of posterior
gonopods reduced to a vestige near the base of
the broad seminiferous blade.
Description—Male 36 mm long with 58 seg-
ments; female 31 mm long with 53 segments;
both 2.6 mm in diameter. Living color mostly
yellowish brown with a lateral series of dark
spots at the pores.
Head with mandibulary stipes of male as
shown in Fig. 15.
First segment of male about as long as seg-
ments 2 and 3 together as measured either along
the dorsum or lateral margins; a single strongly
raised rim along the broadly emarginate lateral
margin. Second segment with two strong lateral
ridges, its lateral margin little if any lower than
that of segment 1; ensuing segments with more
lateral striations but the intervals not raised into
ridges. Apex of last segment somewhat surpassing
the valves, more acute than a right angle, its
sides straight, not emarginate.
Gonopods as shown in Figs. 16-18. Sternum of
tenth male legs with a rounded surface swelling
on each side and medianly its anterior portion
developed into a long vertical ridge projecting
between the posterior gonopods.
Ethoiulus oreines (Chamberlin)
Aniulus oreines Chamberlin, Bull. Univ. Utah 30
(11): 6, figs. 18, 19. 1940.
The figures cited above clearly indicate neces-
sity of the transfer.
Ziniulus ambiguus, n. sp.
Two males (1 the type), a female, and three
163
immature specimens collected along the Beau-
regard Road, about 5 miles SSW. of Boerne,
Tex., January 31, 1959, by J. C. Loomis.
Diagnosis—While the anterior gonopods
closely resemble those of Hakiulus, the posterior
ones are more typical of Ziniulus, especially Z.
medicolens, and the mandibulary stipes are typi-
cal of the latter genus.
Description—Color dark, approaching black,
with minor lighter markings. Type with 48 seg-
ments, body 20 mm long, 1.7 mm wide; other
specimens with 47 to 51 segments.
Mandibulary stipes of male (Fig. 19) sub-
quadrate, with both angles of nearly equal size;
dorsal edge with a raised rim.
First segment of male unusually short, the
lateral margin but little longer than that of seg-
ment 2 (Fig. 19) which may have 1, 2, or 3 lat-
eral striations. Segments with transverse sulcus
broadly bowed forward where it passes in front
of the pore which is separated from it by about
its own diameter. Last segment with apex
shightly exceeding the anal valves but not de-
flexed.
Anterior gonopods (Fig. 20) resembling those
of Hakiulus, the posterior ones (Figs. 21-23)
with the flattened, uncate, blade rising from near
the base of the bifurecate blade rather than dis-
tad of its middle, as in medicolens. Sternum of
segment 8 lacking a median projection in front.
Ziniulus medicolens Chamberlin
Numerous specimens of both sexes from J. O.
Vaughan Ranch, Schertz, Tex., December 1958.
Family ATOPETHOLIDAE
Eurelus kerrensis Chamberlin and Mulaik
A mature female, thought to be this species,
from beside Highway 16, between Kerrville and
Bandera, Tex., collected December 26, 1958, in
collaboration with J. C. Loomis.
The specimen has 52 segments and is 8 mm in
diameter, similar in this respect to soleatus Cook,
but is larger than is given for kerrensis, the
smaller size of which was one of the characters
on which the two species were separated.
Family SIPHONOPHORIDAE
Siphonophora sp.
A young female, 8 mm long and with but 41
segments, collected by Leslie Hubricht, March
12, 1955, in Zilker Park, Austin, Tex., and sent
me by Richard L. Hoffman.
164
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 5
National Science Foundation Makes Educational Grant to
Washington Academy of Sciences
The National Science Foundation has made a
grant of $32,250 to the WasHINGTON ACADEMY
or ScreNcEes to conduct a several-faceted pro-
eram in science education. This a part of a half-
million dollar program of grants to 17 State
academies and similar organizations — to
strengthen their educational activities.
The AcaprMy’s program consists of four
projects, which may be summarized as follows:
To establish a community consultation service ;
to participate in curricular experiments inte-
erating instruction in science and mathematics;
and to organize round-table discussions among
secondary school teachers, college instructors,
and local scientists. The program is under the
supervision of the Joint Board on Science Educa-
tion, which will administer and coordinate all its
phases.
With reference to the consultation service, a
central office will be established, with appropri-
ate files to catalogue the scientific resources of
the community. This file in the hands of a trained
clerk will serve as a means for making these re-
sources readily available to the various schools.
The round-table discussions will be designed to
create a better liaison between teachers, in both
secondary schools and colleges, with local sci-
entists in the several scientific disciplines.
The curricular experiments will be conducted
at both elementary and secondary school levels.
Their objective will be to explore to what extent
instruction in science and in mathematics may be
coordinated to complement and supplement each
other. Four public and two private schools in
the local area have indicated their intention to
participate in this program and conduct experi-
mental courses. The grant makes it possible to
reimburse these cooperators for direct costs in-
curred by their participation in the program.
Dr. John K. Taylor, of the National Bureau
of Standards, has been named as director of the
program and as such will have general responsi-
bility for its total operation. Dr. Taylor has had
a long and continuing interest in science educa-
tion and has been a member of the Joint Board
on Science Education since its inception in 1955.
Dr. William T. Read, recently retired as scien-
tific adviser to the Department of Defense, will
be retained as executive secretary. In this ca-
pacity he will be responsible for administration
and implementation of the program. Dr. Read
was one of the leaders in the cooperative effort
by the D. C. Council of Architectural and En-
gineering Societies and the WASHINGTON ACAD-
EMY OF SCIENCEs to coordinate the educational
activities of the local technical societies which
resulted in the formation of the School Contacts
program and finally the Joint Board on Science
Education. Dr. Read has also other extensive
educational experience and is a former dean of
the School of Chemical Engineering at Rutgers
University.
The Joint Board has appointed special ad-
visory committees to give technical assistance to
the participants in the projects. Thirty distin-
guished scientists representing the disciplines of
biology, chemistry, physics, engineering, mathe-
matics, and geology, and affliated with the ma-
jor scientific and educational institutions of the
area, will work in cooperation with the Joint
Board’s Curriculum Committee to this end. Dr.
Raymond J. Seeger is chairman of this latter
committee.
The program will have its headquarters in the
office of the Academy at 1530 P Street, NW.,
Washington 6, D. C. The telephone number is
ADams 4-5323. One of its projects 1s concerned
with the establishment of a roster of scientists
who can assist school teachers and their students
by speaking to science clubs, consulting on sci-
ence projects, and performing related activities.
Dr. Read would be glad to hear from all who are
interested in participating in this aspect of the
program.
Officers of the Washington Academy of Sciences
OEE FRANK L. CAMPBELL, National Research Council
Presiden) Clech..............-. LAWRENCE A. Woop, National Bureau of Standards
(PROTO) Heinz Specut, National Institutes of Health
PREETI es ee ws W. G. BrompBacHEeR, National Bureau of Standards
PeReUPOIst..6..5........ Morris C. Lerxinp, Armed Forces Institute of Pathology
Gusroazan of Publications............... Haratp A. REHDER, U.S. National Museum
ETS oo CHESTER H. Page, National Bureau of Standards
(el STE Le H. A. Bortuwick, T. D. Stewart
Memaners £0 196)... ee Bourpon F. ScrisNer, Keita C. JoHNSON
MPT S TO POG! 2. ee ee eee Puitip H. ABELSON, Howarp S. RapPplEYE
Board of Managers....All the above officers plus the vice-presidents representing the
affiliated societies
CHAIRMEN OF COMMITTEES
Standing Committees
ec 2 2) FRANK L. CAMPBELL, National Research Council
ULL UL iS 2 RautpH B. KENNARD, American University
Membership............ LawrencE M. KusHNER, National Bureau of Standards
MEGUSECAGHS................- Dean B. Cowir, Carnegie Institution of Washington
Awards for Scientific Achievement....... FRANK A. BIBERSTEIN, Catholic University
Grants-in-aid for Research...... B. D. Van Evera, George Washington University
Pomey ana Planning.............. MarGARET PiTrMan, National Institutes of Health
Encouragement of Science Talent.............. Leo Scuusert, American University
Science Education............ Raymond J. SEEGER, National Science Foundation
ieyoaned Means.............. RussELL B. Stevens, George Washington University
PoC EWGIAGIGHS. .............0000005- Joun K. Tartor, National Bureau of Standards
PURE fos es. ce ales Haroip H. SHeparp, U. 8S. Department of Agriculture
MIECEGOPY............... James I. Hamsieton, U.S. Department of Agriculture (Ret.)
Eubrary of Coneress.................... Joun A. O’Krere, National Aeronautics and
Space Administration
CONTENTS
Page
History or Science—Franklin as a physicist. Raymonp J.SEEGER.. 129
ARCHEOLOGY.—Relationship between Plains Early Hunter and Eastern
Archaic. ( William J.‘ Mayer-Oakes.........0......:s 025 er 146
ZooLocy.—Millipeds collected enroute from Florida to San Antonio,
Texas, and vicinity. H: F. Loomis...:..........3 - 3.332 157
ACADEMY ANNOUNCEMENTS: |
Appeal for back numbets of JoURNAL.............. 232 145
National Science Foundation makes educational grant to WASH-
INGTON ACADEMY OF SCIENCES
: Was
MeuME 40 June 1959 NUMBER 6
JOURNAL
OF PRHE
WASHINGTON ACADEMY
OF SCIENCES
ceneecececeeecet
AMMA ANN
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JOURNAL
OF THE
WASHINGTON ACADEMY OF SCIENCES
Vou. 49
June 1959
No. 6
ASTRONAUTICS—The exploration of space. HucH L. DryprEN, National Aero-
nautics and Space Administration.
(Received May 29, 1959)
The surging tide of technological develop-
ment has brought us to a new frontier, the
frontier of space exploration and travel. We
are at approximately the same stage in the
development of space vehicles as the Wright
Brothers were in the development of the air-
plane in 1904. In those days few people were
interested in the fragile wood, wire, and cloth
vehicles which were the fore-runners of our
modern jet transports and military air-
planes. In fact, as a nation, we were so un-
interested that the Wrights took their inven-
tion to Europe. When World War I broke
out, we found that we had no airplanes of our
own. We were compelled to build copies of
airplanes developed by other nations.
Today the situation is different. There is
widespread public interest. The competition
is evident. Many now have faith in the great
potentialities of space exploration to benefit
mankind. It is a privilege for me to tell you
about the steps that are being taken to insure
that the United States will occupy its proper
role as a leader in space research, develop-
ment, and operation for peaceful purposes.
The space age began with the launching
of Sputnik I by the U.S.8.R. on October 4,
1957. The United States launched its first
satellite, Explorer I, on January 31, 1958. At
present ten earth satellites have been
launched into orbit successfully. Three space
probes penetrated to distances of 63,000 to
71,000 miles from the earth. Two space
probes reached a velocity high enough to
* Address delivered before the Cosmos Club of
Washington on April 13, 1959, and substance of a
lecture delivered at the 442d meeting of the Wash-
ington Academy of Sciences on May 21, 1959.
escape from the earth’s gravitational field to
enter orbits around the sun as man-made
planets. Instrumentation on board these
space vehicles provided new information
about the environment of nearby space, in-
formation which increases our understanding
of the earth and its atmosphere; of cosmic
rays, other particles and radiations en-
countered by our earth in its journey through
space; in fact, of the physical universe in
which we live. From the data already re-
turned to earth from satellites and space
probes containing equipment developed by
Dr. James A. Van Allen, head of the physies
department of the University of Iowa, have
come the discovery and description of the
Great Radiation Belt. This belt consists of
clouds of charged particles whose impact on
the satellite produces radiation of high in-
tensity harmful to man and capable of dam-
age to film and other photosensitive appa-
ratus. There are in fact two radiation belts
believed to be of different origins. The first
has its maximum intensity at a height of
about 2,400 miles and is believed to be pro-
duced as a result of the impingement of cos-
mic rays on air molecules. The second, reach-
ing its Maximum intensity at about 10,000
miles above the earth is believed to consist
of particles from the sun, whose atmosphere
now appears to reach to the earth and be-
yond. In both cases the particles are trapped
by the magnetic field of the earth and per-
sist for a long time until as they travel back
and forth in spiral paths from pole to pole
they collide with air molecules releasing
some of their energy to form the imposing
auroral lights of the far north and south.
165
166 JOURNAL OF THE
In addition to this fascinating discovery
which I am not competent to describe in de-
tail, the four U.S.8.R. and eleven U.S. space
vehicles so far launched successfully have
produced exploratory data on the distribu-
tion of matter and magnetic fields en-
countered in space, as well as data on solar
radiation, electric field, photons, heavy nu-
clei, positive ions, and the physiological re-
actions of a dog which are as yet reported
only in part by U.S.S.R. scientists. Truly an
imposing record for the first year and a half
of the space age.
In the early months there was wide public
discussion of the organization of U.S. activ-
ities in space research, development, and
operation. As an interim measure cognizance
over all space programs was assigned to the
Department of Defense and a study of US.
requirements in space science and technology
was undertaken by the President’s Science
Advisory Committee under the leadership of
Dr. James R. Killian. As a result of this
study the President on April 2, 1958, recom-
mended to the Congress the formation of a
civilian agency to be responsible for space
activities concerned with problems of civil
space flight, space science, and space tech-
nology. Military programs associated with
military weapons systems and military op-
erations were continued as the responsibility
of the Department of Defense. The Presi-
dent further recommended that the new
agency be based on the existing National
Advisory Committee for Aeronautics. The
responsibilities of NACA in aeronautical re-
search and services in support of military
aeronautics and missiles programs were to be
continued by the new agency and extended
to military space programs. The functions of
the new agency were to be considerably ex-
panded over those of NACA to include the
development and operation for research pur-
poses of space vehicles.
After extensive hearings and consideration
by the Congress the National Aeronautics
and Space Act of 1958 became law on July
29, 1958, with most of the features recom-
mended by the President. This Act expresses
an important national policy with respect to
activities in space, and the National Aero-
nautics and Space Administration was es-
tablished to implement this policy. Section
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 6
102(a) reads as follows: ‘‘The Congress
hereby declares that it is the policy of the
United States that activities in space should
be devoted to peaceful purposes for the bene-
fit of all mankind.” In Section 102(¢c) the Act
states the objectives of the aeronautical and
space activities of the United States under
this policy. In paraphrased form they are:
1. The expansion of human knowledge of atmos-
pheric and space science ;
2. The improvement of aeronautical and space
vehicles ;
3. The development and operation of space ve-
hicles;
4. The study of the potential benefits to be
gained for mankind through space activities;
5. The preservation of the role of the United
States as a leader in aeronautical and space science
and technology and in application thereof to peace-
ful activities;
6. The interchange of information between ci-
vilian and national defense agencies;
7. Cooperation with other nations in aeronauti-
cal and space activities and in peaceful application
of the results; and
8. The most effective utilization of the scientific
and engineering resources of the United States in
achieving these goals.
The Act, in addition to the formulation of
the policy and these objectives and the es-
tablishment of NASA, created an Aero-
nautical and Space Council to advise the
President on all significant aeronautical and
space activities and on the assignment of
responsibility for specific projects. A Civil-
ian-Military Liaison Committee was also
established as a channel for advice and con-
sultation between NASA and the Depart-
ment of Defense.
On August 8 the President appointed Dr.
T. Keith Glennan, president-on-leave of
Case Institute of Technology, as NASA’s
first administrator, and myself as deputy ad-
ministrator. NASA began operations on Oc-
tober 1, 1958, at which time it absorbed the
personnel and facilities of the National Ad-
visory Committee for Aeronautics, thus end-
ing the 43-year existence of NACA by meta-
morphosis. NASA thus began with nearly
8,000 scientists and engineers, and technical
and administrative personnel and five field
laboratories: Langley Research Center at
Langley Field, Va.; Ames Research Center,
Moffett Field, Calif.; Lewis Research Cen-
ter, Cleveland, Ohio; Wallops Island Sta-
tion, Wallops Island, Va.; and the High
JUNE 1959
Speed Flight Station, Edwards, Calif. To
carry the new responsibilities there was
added to the organizational structure space
flight development in addition to aeronauti-
cal and space research and business adminis-
tration. The new responsibilities for devel-
opment and operation of space vehicles will
be carried largely by contract with existing
industry and educational groups.
On October 1, as a result of prior review,
the President transferred to NASA from the
Department of Defense the original US.
scientific earth satellite project, Project
Vanguard, with more than 160 scientists and
technologists of the Naval Research Labora-
tory; five space probes and three satellite
projects which were under the direction of
the Advanced Research Projects Agency of
the Department of Defense, and a number of
engine development programs from the Air
Force and ARPA. On December 3 the Presi-
dent transferred the functions and facilities
of the Jet Propulsion Laboratory, Pasadena,
Calif., from the Department of the Army to
NASA. At the same time NASA entered into
an agreement with the Army whereby the
Army Ballistic Missile Agency, Huntsville,
Ala., will carry out certain NASA projects.
In the seven months of NASA’s existence
we have been working with a high sense of
urgency on a fourfold task, (1) carrying out
the on-going satellite and space-probe pro]-
ects transferred to the new agency; (2)
planning and initiating new projects; (3)
establishing long-range plans and objec-
tives; and (4) building an organization ade-
quate to carry out the over-all program. In
our remaining discussion together I wish to
outline our over-all plans and objectives.
In our present appearances before Con-
eressional committees we are asked to sol-
emnly swear that our testimony will be the
truth, the whole truth, and nothing but the
truth. Dr. Homer Newell, NASA assistant
director for space sciences, after taking this
oath, remarked that we do not always know
the truth in science and we can only try to
tell the truth as we see it today. Space science
and technology represents a new and un-
known area of knowledge, and no person can
now foresee the aeronautical and space ac-
tivities of the future any more than the
Wrights could foresee the aeronautical ac-
DRYDEN: THE EXPLORATION OF SPACE
167
tivities of today in 1903. As you recall,
Wilbur stated that “it is not necessary to
look too far into the future; we see enough
already to be certain that it will be magnifi-
cent.”
In hne with U.S. policy as expressed in the
Act, NASA has established objectives which
carry out the application of space science
and technology to peaceful purposes. Some
of the most important relate to the applica-
tions of earth satellites to meteorology, com-
munications, navigation, and geodetics. In
some of these fields we expect that, after a
period of subsidized development, the earth
satellite techniques will prove less costly yet
more effective than presently available
methods.
The objective of NASA’s meteorological
satellite program is to provide the knowl-
edge, experimental data, and component de-
velopment required for an operational satel-
lite system for weather observation, analysis,
and forecasting. To accomplish this objec-
tive requires research and development on
vehicles, instrumentation, data-handling
techniques, and satellite flights. The in-
creased knowledge obtainable by such a sys-
tem may well lead to the possibility of doing
something about the weather as well as ob-
serve and experience it.
The first meteorological satellite, a very
primitive one, was Vanguard II, successfully
launched on February 17, 1959. It carried
two infrared photocells to sean the earth’s
cloud cover. The instrumentation worked
well, and excellent electronic signals were
received and recorded on the ground
throughout the life of the satellite’s bat-
teries. However, the satellite acquired a
complex wobbling motion which has greatly
complicated the reduction of the data. This
satellite was the first toddling step toward
our final objective. A second more sophisti-
cated satellite is under construction and later
versions are in the planning stage.
Our present concept of the system which
is our objective comprises six satellites in
polar orbits at altitudes of 500 to 1,000 miles
and three satellites in 22,000 mile equatorial
orbits which travel at the same speed as the
earth’s surface and so remain over fixed
points on the earth’s surface. The satellites
will be provided with instrumentation to
168
observe cloud formations, hurricanes, torna-
does, thunderstorms, temperatures at vari-
ous levels (inferred from spectral distribu-
tion of radiated energy), incoming and
reflected solar radiation, ete. The data re-
ceived from the satellites will be transmitted
quickly (perhaps by communication satel-
lites described below) to a central weather
computing center, an enlarged version of
that operated now by the U.S. Weather Bu-
reau at Suitland, Md., near Washington,
which is now engaged in numerical weather
prediction. The operational system will be
operated by the Weather Bureau, perhaps
with NASA assistance in the satellite
launchings.
A second NASA objective for the peaceful
application of satellites is the development
of the knowledge, experimental data, and
component development required for a
world-wide communication system capable
of transmitting wide band messages includ-
ing television pictures. The accomplishment
of this objective requires development of
vehicles, transmitters, antennas, receivers,
and experimental data on operating equip-
ment. The final system might be operated by
an industrial group or by government mo-
nopoly as later determined by Congressional
policy. One type of system, the passive sys-
tem described below, permits use of the
satellite component by any nation or person
providing the necessary ground equipment.
NASA’s first experiments are devoted to
the development of components of the pas-
sive system. It is well known that the moon
may be used as a reflector of radio and radar
signals if very powerful transmitters and
sensitive receivers are used on the ground
and the geometrical relations are correct.
Satellites provide smaller moons nearer the
earth which require less transmitter power
and less expensive equipment. According to a
study by Dr. John Pierce of the Bell Tele-
phone Laboratories a passive satellite sys-
tem may prove economically competitive
with ocean cable for transatlantic commu-
nication. Television transmission would be
possible over this system.
The first passive satellite for experiments
on this method of communication is sched-
uled by NASA during this year. Its launch-
ing has been delayed by lack of an adequate
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 6
launching vehicle. The passive satellite con-
sists of a large inflatable sphere 100 feet in
diameter which is made of aluminized mylar
plastic. The sphere weighs less than 100
pounds and will be placed in a 700- to 1,000-
mile orbit. It can be packed for launching
is a sphere only two feet in diameter. The
satellite should be readily visible with about
the brightness of Venus. In use a strong radio
signal is reflected from the satellite in all
directions, reaching the earth as a weaker
signal which can be received by a highly
sensitive receiving antenna pointing toward
the satellite.
Our present concept of a passive satellite
communications system involves 10 to 20
such satellites in orbits at about 3,000-mile
altitude. Any nation could use the satellites
as reflectors without interference with use by
any other nation. Thus the launching of pas-
sive communications satellites would be an
important contribution to the peaceful uses
of satellites by all nations.
Time will not permit discussion of other
plans and objectives for practical applica-
tions of satellites to problems of trade and
commerce. I turn now briefly to the uses of
satellites and space probes for the advance-
ment of scientific knowledge of the space
environment. The NASA space science pro-
gram has its roots in the sounding rocket
program for exploration of the upper atmos-
phere which began some 12 years ago with
the use of captured V-2 rockets and the
subsequent development of special sounding
rockets. During the International Geophysi-
cal Year this program received great 1m-
petus, and the U.S. fired about 200 sounding
rockets and launched its first satellites and
space probes.
With the cooperation of the Space Science
Board of the National Academy of Sciences—
National Research Council and the National
Science Foundation, NASA has formulated
long-range objectives in the space science
program and established a definitive pro-
gram for the next few years. The term “space
science” has been coined to denote scientific
investigations carried out in space through
the use of satellites, space probes, and other
space vehicles. It is not a scientific discipline
in itself. Though emphasis at present is on
the physical sciences, it is clear that bio-
JUNE 1959
logical science investigations will also be in-
cluded.
Our program includes a number of areas
and their relations one with the other. One
area is that of study of the atmospheres of
the earth, sun, moon, and planets with re-
spect to chemical composition, density, mo-
tions, diffusive processes, absorption of solar
radiation, etc. A second area is that of study
of the ionospheres. For the earth this region
is that from say 50 to a few hundred miles.
The presence of the ionosphere permits re-
flection of radio waves for communication
beyond the horizon. The state of the iono-
sphere is as important to long-range radio
communication as is the state of the weather
in the lower atmosphere to transportation
and other human activities.
A third area of study has already been
mentioned, the cosmic rays in interplanetary
space, the Great Radiation Belt of Van
Allen, and the auroral particles.
A fourth covers the fascinating subjects
of magnetism, electricity, and gravity.
A fifth is that of astronomy. Satellite ob-
servations place the observer of the sky
above the distortion effects of the earth’s
atmosphere and its absorption of a large
part of the radio waves, gamma rays, ultra-
violet rays, X-rays, and visible light. As one
scientist remarked, satellites permit obser-
vation of the universe in full color compared
to his present black-and-white picture. Thus
in the field of astronomy we are planning to
establish and operate unmanned astronomi-
cal observatories orbiting above the absorb-
ing atmosphere of the earth and to measure
with precision the emission and absorption
features of the sun, stars and nebulae in the
unexplored ultraviolet, infrared, and X-ray
regions of the electromagnetic spectrum.
The nearest object to us in space is the
moon. NASA’s plans and objectives include
unmanned lunar exploration as a prelimi-
nary to ultimate manned exploration, and to
investigate the surface and interior of the
moon and the nearby space, including at-
mosphere and ionosphere if the moon ex-
hibits such features. The space vehicles used
will include lunar probes, lunar orbiters, and
vehicles for rough landings, and soft land-
ings of instruments. These vehicles are listed
in accord with the estimated order of avail-
DRYDEN: THE EXPLORATION OF SPACE
169
ability of the necessary vehicles and guid-
ance systems.
The next nearest neighbors of the earth are
the planets Venus and Mars. NASA’s plans
include exploratory probes of the space near
these planets as our capabilities permit. At
present our payload capacities are so small
that only very limited data are obtainable
even if the mission is otherwise successful.
But as will be described now steps are under
way to remedy this situation.
In order to accomplish the long-range ob-
jectives outlined and others to be described
it is essential that we develop rocket boosters
and vehicles capable of putting much larger
payloads into space. This is the one area
where our competition is definitely ahead.
NASA and the Department of Defense have
planned a program extending over the next
10 years to provide the vehicles required for
foreseen military and nonmilitary space
missions. Time permits only a brief sketch
of these developments.
At present, except for Vanguard, we are
using assemblies of components and vehicles
that were designed for other purposes to
launch satellites and space probes. They are
inefficient and expensive. Improved vehicles
will soon be available such as the Discoverer
satellite based on the Thor ballistic missile
booster and the Hustler engine originally de-
veloped for a ground to air missile. NASA is
developing a 4-stage solid-propellant satel-
lite vehicle to carry about 150 pounds into a
300-mile orbit. This vehicle, called the
Seout, will be much more economical than
existing vehicles and will satisfy many of the
needs of our scientific program. It will be
very useful in international cooperative pro-
orams.
NASA has under development the Vega, a
3-stage vehicle using a modified Convair
Atlas as first stage, a second stage incorpo-
rating a modified General Electric engine
which was used in the Vanguard first stage,
and a JPL third stage using storable propel-
lants. The Vega will enable us to put several
tons in a 3800-mile orbit and to send 1,000
pounds to the neighborhood of the moon.
Later vehicles in the program are the
Centaur, Saturn, and Nova. Centaur is simi-
lar to Vega except that the second stage uses
high-energy propellants, liquid hydrogen
170
and liquid oxygen. The first stage of Saturn
is being developed by the Army Ballistic
Missile Agency as a cluster of existing rocket
engines giving over one million pounds
thrust. Nova will be based on a single cham-
ber rocket of over one million pounds thrust,
which is being developed by the Rocketdyne
Division of North American under NASA
contract.
The Atomic Energy Commission and
NASA jointly are developing nuclear rockets
for application to space missions as the state
of development permits and on the study of
nuclear power plants for use in satellites.
Finally, NASA’s long-range objectives in-
clude the exploration of the solar system by
man himself. Enroute to this objective are
the milestones of orbital flight of man in the
simplest vehicle (Project Mercury, much in
the public eye), in advanced maneuverable
vehicles, in larger satellites carrying several
men, in permanent manned orbiting space
laboratories, manned flight to the vicinity of
the moon and back, and manned landing on
the moon and return. The objective of Pro-
ject Mercury is to begin the manned explora-
tion of space by developing the technology
needed to place a man in orbit about the
earth for a short time and recover him safely,
and by studying man’s physiological and
psychological performance. By restricting
the altitude to a height well below the Great
Radiation Belt, no heavy shielding is re-
quired. By planning for only a few orbits
before recovery, existing life support sys-
tems are adequate.
As you know from the public and technical
press, the man will travel in a capsule sub-
stituted for the nose cone of an interconti-
nental ballistic missile. The man is supported
in a reclining position on a couch for pro-
tection against the accelerations imposed
by launching and by reentry into the atmos-
phere. The capsule is provided with equip-
ment to supply oxygen and remove carbon
dioxide, communications and navigation
equipment, attitude control jets, heat shield
to protect from reentry heating, and a para-
chute for final landing on water. Reentry is
initiated by firmg a small rocket to slightly
reduce the speed of the capsule in orbit.
The orbiting flight of the first Mercury
Astronaut will be preceded by extensive
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 6
tests and qualifications of the capsule and
training of the astronaut extending over the
next two years. Ballistic flights over short
distances, instrumented ballistic and orbital
flights, animal passenger flights, are included
in this program of testing and evaluation.
The seven Mercury Astronauts were se-
lected from an original group of 100 military
test pilots who met the general qualifica-
tions. When 80 percent of the first 69 inter-
viewed volunteered to proceed, the inter-
views were terminated. The list was then
narrowed to 32 who were given extensive
physical and psychological tests. The seven
astronauts will receive the most intensive
course of training ever offered to a party of
prospective explorers. Every conceivable
characteristic of space flight that can be
simulated on the ground or in the air will be
made a part of their personal experience.
Every detail of the launching, guiding, and
tracking procedures will be taught them by
ground crews, until they know the operation
as we know the working of an office in which
we have spent the better part of our profes-
sional lives. Only one can be first, but there
will be several flights in the program.
All this training of the selected pilots, and
all this repeated testing of the rocket and
its component parts, are directed toward
one end: that the first orbital flight of the
Mercury vehicle shall be as nearly routine as
human ingenuity and practice can make it.
We are determined that the risks to the pilot
will be no greater than those experienced
during the first flights of a new high-per-
formance airplane.
The Mercury project will be followed by
others. In due course a permanent manned
satellite will be placed in orbit around the
earth, to conduct research, and possibly as a
station from which to organize deeper pene-
trations into space. As we master the re-
quired technology we will send an expedition
to the moon, and later on to Mars, to Venus,
and to more distant reaches of the solar sys-
tem.
May I recall to your mind the vast extent
of the reaches of space as mapped by the
astronomers. The most important object in
our part of the universe is the sun, source
of our heat, our light, and in the last analy-
sis our food supply. In its neighborhood are
JUNE 1959
nine planets which travel in orbits around
the sun and accompany the sun in its motion
through space. The earth is number three,
at just the right distance for our delicate
bodies so that we neither roast nor freeze, at
a distance of 93 million miles. Our nearest
neighbor, as previously mentioned, is the
moon, about 240,000 miles away on the aver-
age, moving in an orbit about the earth and
accompanying us on our yearly journey
around the sun. The nearest planet to us 1s
Venus, 26 million miles, the next Mars, 49
million miles away. The farthest planet,
Pluto, is 3,680 million miles from the sun.
To comprehend these tremendous dis-
tances let us suppose that we now had space-
craft able to travel at 10 miles per second,
approximately the initial velocity required
to escape from the solar system or 60 times
the speed of a jet transport. It would take us
6 hours 40 minutes to travel the average
distance to the moon, 24 days to Venus, 58
days to Mars, 108 days to the sun, 11-2
years to Pluto.
The nearest star 1s 25 million million miles
away, and travel to it at 10 miles per second
would require 80,000 years. It is evident
PHOTOGRAPHS OF VANGUARD I IN ORBIT
7a
that our exploration will be confined to the
solar system for some time.
The greatest speed we know is that of
light, 186,000 miles per second. We call the
distance hght travels in one year, a lght
year; it is nearly 6 million million miles.
Thus the nearest star is a little over 4 light
years away. Our sun is 26,000 hght years
from the center of our galaxy, the Milky
Way. Such distances become almost beyond
our comprehension.
Is then the travel of man to the stars a fu-
tile dream? You remember the verse:
The world will last when gone are we
Without a trace of thee or me.
Before we came there was no void,
And when we're gone the same ‘twill be.
I wonder. Since the invention of writing
the thoughts, the knowledge, and the in-
fluence of men who lived thousands of years
ago are still available. Each age builds on
the shoulders of the past. Who then dares
to mit the horizons of the physical universe
to be ultimately explored by man? The ex-
ploration of space has begun; who knows
where it will end?
Cll
TRACKING CAMERA PHOTOGRAPHS VANGUARD I IN ORBIT
The Smithsonian Optical Tracking Station at
Woomera, Australia, has successfully photo-
graphed the Vanguard I earth satellite at the
apogee of its orbit, nearly 2,500 miles from the
earth. The Woomera station is operated for the
National Aeronautics and Space Administration
as a part of the civilian space agency’s world-
wide network of tracking stations. The Baker-
Nunn precision satellite tracking camera, manned
by personnel of the Woomera Missile Range, took
pictures of Vanguard I on three occasions, May 1,
3, and 4, 1959. No other object as small as this
6-inch sphere has been photographed from such
a distance. It is comparable to aiming a camera
at a golf ball 600 miles away.
The tracking camera, one of 12 located around
the world, was especially designed for tracking
earth satellites during the International Geo-
physical Year. The Woomera station is operated
under the technical direction of the Smithsonian
Astrophysical Observatory for the NASA. Equip-
ment at the station is furnished by the United
States; staff and buildings are supplied by the
Australian Government.
In a congratulatory note to the staff at the
station, Dr. Hugh L. Dryden, NASA’s deputy
administrator, said the tracking team’s efforts
demonstrated the true capabilities of the Baker-
Nunn camera, thus paving the way for more ac-
curate optical satellite tracking data, essential
to precise orbital calculations.
The Vanguard I, developed by the U.S. Naval
Research Laboratory for the IGY, was launched
on March 17, 1958. It was the second scientific
satellite launched by the United States. With a
perigee of 402 miles, the satellite is currently
making 76 orbits a week. During the week of May
17, 1t completed 4,590 revolutions around the
earth since it was launched. The Vanguard pro-
gram was transferred from the Naval Research
Laboratory to the NASA on October 1, 1958.
The other 11 camera stations are located at:
Organ, N. Mex.; Olifantsfontein, South Africa;
Cadiz, Spain; Tokyo, Japan; Naini Tal, India;
Arequipa, Peru; Shiraz, Iran; Curacao, N.W.L.:
Hobe Sound, Fla.; Villa Dolores, Argentina; and
Haleakala, Maui, Hawaii.
172 JOURNAL OF THE
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, No. 6
GEOLOGY .—Sulphide mineralization and associated structure in northern. Union
County, Illinois. GEORGE A. DESBOROUGH, Southern Illinois University, Car-
bondale, Ill. (Communicated by David Nicol.)
(Received April 20, 1959)
Minor amounts of sulphide mineralization
in Union County of southwestern Illinois
have been known for many years, but no at-
tempt has been made to study this outlying
occurrence in detail. The area lies midway
between the Illinois-Kentucky fluorspar dis-
trict and the southeastern Missouri lead
district and exhibits some characteristics of
both. The occurrence is in the complex fault-
zone along the Rattlesnake Ferry (Ste.
Genevieve) fault and appears as dissemi-
nated deposits and as vein filling of frac-
tures in the Backbone limestone of Devonian
age. The mineralization consists of galena
and sphalerite with subordinate chaleopy-
rite plus their associated alteration prod-
ucts. The occurrence has characteristies nor-
mally attributed to deposits regarded as
being of epithermal origin. All features in-
dicate marked structural and stratigraphic
control. Subordinate faults with small dis-
placement along the major fault zone seem
most favorable for mineralization. Although
no systematic prospecting or exploration has
been conducted in the area, structural and
stratigraphic relationships are favorable for
sulphide mineralization.
Since the early 1900’s several small-scale
operations have been unsuccessfully at-
UNION COUNTY, SOUTHERN ILLINOIS
RATTLESNAKE
a ~~ FERRY FAULT
F
AREA O
N STUDY
ie) 5 ite)
MILES
Fic. 1—Index map of area
temped to extract lead ore from mineralized
zones along faults in northern Union County,
Il]. These mineralized locales occur along the
Rattlesnake Ferry (Ste. Genevieve) fault
zone in the 8. % of sec. 1, T. 11 8., R.3 W.
(Alto Pass quadrangle), about 5 miles east
of the Mississippi River in the Shawnee Hill
Section of southwestern Illinois (Fig. 1).
The area is complexly faulted and, ac-
cording to Weller and Ekblaw (1940, p. 25),
displacement along the Rattlesnake Ferry
fault may exceed 1,500 feet. In some areas
the numerous faults occur in a zone one-half
mile wide; however, in the vicinity of Grassy
Knob (just east of the Big Muddy River
and south of Rattlesnake Ferry) the zone is
only a few yards wide.
On the south side of the major fault zone,
the strata are almost exclusively Lower and
Middle Devonian. The strata exposed on
the north side of the fault are dominantly of
Chesteran age (late Mississippian), al-
though many of the hills are capped by
Caseyville (Lower Pennsylvanian) outliers.
In the area immediately north of the
major fault zone and west of Alto Pass,
numerous north-south trending faults com-
plicate the structural and stratigraphic re-
lationships (Ekblaw, 1925; Desborough,
1957). At least two periods of faulting are
evident in this area, one prior to Pennsyl-
vanian deposition, and the other during post-
Pennsylvanian time (St. Clair, 1917; Ekb-
law, 1925; J. M. Weller and Ekblaw, 1940;
Weller, 1940; Desborough, 1957).
STRATIGRAPHY
The mineralization and associated struc-
tures are apparently restricted to the Back-
bone limestone and the Clear Creek chert,
both of Devonian age. About one-half mile
north of the mineralized area Mississippian
rocks of Meramecian and Chesteran age are
exposed. The complete Chester series is ex-
posed, as well as the Ste. Genevieve forma-
tion of the Meramec group. The Chester
JUNE 1959
_. MISSISSIPPIAN
WN (Undifferentiated)
DESBOROUGH: SULPHIDE MINERALIZATION
GRAND TOWER LIMESTONE SSea\
[TT] cLEAR CREEK CHERT
BACKBONE LIMESTONE
[_] ALLUViIUM
-". STREAM
FAULT
INFERRED FAULT
STRIKE & DIP
=
INDEX MAP
SEC. |
LOCALITY, Ie
et
~
~
--
--22-"—
<= oe = =
5S ie 70
CROSS SECTION
Oo
500
1000
SCALE IN FEET
Fig. 2.—Areal geologic map and cross-section of area in Sec. 1, T. 118., R. 3W., Alto Pass quadrangle,
Ulinois.
strata are overlain unconformably by Lower
Pennsylvanian clastic sediments. The strati-
graphic relationships of the Backbone lime-
stone and the Clear Creek chert are as fol-
lows:
Middle Devonian
Dutch Creek sandstone (not exposed)
Clear Creek chert.......... 300 feet thick
Lower Devonian
Backbone limestone........ 200 feet thick
Grassy Knob chert (not exposed)
PAST AND PRESENT STUDIES
The general geology of this area has been
studied by Worthen (1868), St. Clair (1917),
Savage (1920), Poor (1923), Basset (1925),
174 JOURNAL OF THE
Ekblaw (1925), S. Weller and J. M. Weller
(1939), J. M. Weller and Ekblaw (1940),
and J. M. Weller (1945). Recently, Brad-
bury (1957) wrote a brief description of the
mineralized area. He summarized the data
obtained in the past and added new observa-
tions. Subsequently, local interest im the
mineralization has been stimulated. As a re-
sult several prospect pits were made in the
bedrock of sec. 1 (Fig. 2).
The blasting and removal of overburden
during the late fall of 1957 and the early
winter of 1958 exposed the nature of the
mineralization as well as interesting struc-
tural relations. During the period of ex-
cavating and blasting, the writer frequently
visited, examined, and photographed some
of the significant geologic features, several
of which have been obscured by later ex-
cavations. Thin sections of the wallrock and
the mineralized rock were prepared and
studied.
This paper attempts to describe and ex-
plain in some detail the nature of the min-
eralization and structure. In some aspects
my interpretations differ from those of
earlier writings.
Two locales of mineralization will be dis-
cussed herein, designated as Locality 1 and
Locality 2. Locality 1 refers to the mineral-
ized area at the normal fault near the stream
junction (Fig. 2). Locality 2 refers to the
mineralized area at the junction of the two
faults exposed near the stream in the south
valley wall of Hutchins Creek (Fig. 2).
LOCALITY 1
Locality 1 was apparently referred to as
the “third caved shaft or prospect pit” by
Bradbury (1957, p. 2). He implied that this
prospect pit is situated on a northwesterly
trending fault, based on Weller and Ek-
blaw’s geologic map (1940, pl. 1). Recent
excavations have revealed the mineraliza-
tion to be along an approximately vertical
K-W striking fault which involves only the
Backbone limestone at the surface. The dis-
placement is probably small. The breccia-
tion and drag features of the northern fault
block indicate it is downthrown.
The host, Backbone limestone, is a light
gray, dense limestone, part of which has
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 6
been altered to ocherous material. A few
hundred feet north of the fault, the Back-
bone limestone contains inch-thick beds of
chert. Alteration of the host rock by min-
eralizing solutions is not evident.
Mineralization is concentrated in the
downthrown block and consists of vein cal-
cite and subordinate galena, sphalerite, and
chalcopyrite. Smithsonite and limonite oc-
cur locally as oxidation products. Galena is
found in the calcite as masses up to 6 inches
long and as small euhedral crystals dissemi-
nated in the limestone. Sphalerite is found
as crystalline encrustations upon calcite
crystals and as linings in small vugs. Chal-
copyrite occurs as small disphenoids en-
closed by calcite. The smithsonite is sparsely
scattered between the calcite crystals in
small, green, crystalline masses. Limonite
occurs as pseudomorphs after chalcopyrite.
Contact relations between mineral grains
indicate the following sequence of deposi-
tion: (1) calcite I, (2) chalcopyrite, (3a)
calcite II, (3b) sphalerite-galena, (3c) cal-
cite II. Calcite I is very coarse-grained and
semitransparent, and it contains disphenoids
of chalcopyrite. Because small disphenoids
of chalcopyrite are found upon calcite I
crystals in vugs, as well as included within
large calcite crystals, deposition of calcite I
must have begun prior to and ended after
the chalcopyrite stage. Calcite II is repre-
sented by a medium-grained, white to gray
variety ; its contact relations with galena in-
dicate the calcite is younger. However, sub-
hedral crystals of sphalerite are found upon
calcite Il. These factors suggest the calcite
II stage preceded the sphalerite-galena stage
and continued after the cessation of the
latter.
LOCALITY 2
Locality 2 is in the center of the W.%,
H.%, SE.4, of sec. 1 (Fig. 2). According to
Bradbury’s report (1957, p. 2), the exact
location of the exposure is uncertain since
there are many prospect pits in the vicinity.
Possibly it was this exposure that Bradbury
referred to as the “first shaft,” because min-
eralization here is apparently restricted to
the Backbone limestone. Bradbury probably
based his locations upon Weller and Ek-
blaw’s preliminary geologic map (1940, pl.
JUNE 1959
1), which is generalized because of its small
scale.
Excavations at this location within the
past year have revealed minor sulphide min-
eralization in the Backbone limestone and
complex structural and stratigraphic rela-
tionships.
Structural and stratigraphic relationships.
——The fault at Locality 2 which strikes
N.45—50°W. is a normal one (Fig. 2, 3). It
dips about 80° NE., and the stratigraphic
displacement is probably less than 5 feet;
however, a vein about 3 feet wide occupies
the fracture on the north side of the N.80°W.
fault (Fig. 3).
The Clear Creek chert and Backbone
limestone lie in normal contact on the south
side of the major fault (Fig. 3, 4). This fault
strikes about N.80°W. and dips 60°SW. (Fig.
3). About 25 feet of Backbone limestone is
exposed above the creek bed (Fig. 2). The
exposures of Backbone limestone on each
side of the fault are apparently in place, and
they are almost identical in thin section and
hand specimens. To establish whether or not
the limestone beneath the Clear Creek chert
was a calcareous component of the lower
Clear Creek formation, a thin section of the
Clear Creek limestone from the locality de-
scribed by Weller (1940, p. 24) was studied.
Mineralogically, the Clear Creek limestone
contains abundant glauconite and is much
more siliceous than the Backbone limestone
at the mineralized locale. Both chalcedony
and euhedral to subhedral quartz grains are
abundant in the Clear Creek limestone,
whereas the Backbone limestone thin sec-
tions are essentially quartz-free. At the min-
eralized locale the Clear Creek chert is not
calcareous and is in beds 2 inches to one foot
thick, whereas the Backbone limestone is
chert-free and conspicuously styolitic. The
latter has also been recrystallized by min-
eralizing solutions or tectonic stress.
The structural and stratigraphic relation-
ships discussed above show that the fault
block on the south must have moved down
relative to the opposite block (Fig. 3). This
is contrary to what one might expect, as the
relative displacement along the major fault
zone shows that most fault blocks on the
southwest side of northwesterly trending
DESBOROUGH: SULPHIDE MINERALIZATION
175
faults are upthrown. Also, the regional dis-
placement along the Rattlesnake Ferry fault
zone demonstrates that the north side is
downthrown. It is not likely that the fault in
question is an antithetic fault since it 1s not
in the downthrown block relative to the
major displacement along the large fault
zone (de Sitter, 1956, p. 154). It has been
pointed out that movement in opposite di-
rections along the same fault plane during
two periods of faulting may have occurred a
few miles northeast of the area discussed
ta
ae
Ba
Y
No a
See ill: sere
SERS BE i
XS S55 ee:
Om
°» SEES ee
en
Oo 5 10 20
SCALE IN FEET
Fa] CLEAR CREEK CHERT
FE “BACKBONE LIMESTONE
Fase MINERALIZED ZONES
Fic. 3—Diagrammatic sketch of structural and
stratigraphic relationships of the Backbone lime-
stone and Clear Creek chert at Locality 2.
here (Desborough, 1957, p. 201). This writer
proposes that the fault is probably due to
normal fault movement along a former re-
verse fault plane.
Weller and Sutton (1940, p. 852) have also
suspected movement along faults “at several
different times and in several different di-
rections, with complete reversal in some
places” several miles to the east in the flu-
orspar district of southeastern Illinois and
western Kentucky. Weller and Ekblaw
(1940, p. 26) recognized the existence of
high-angle thrust faults in southern Illinois
and attributed these to compressional forces.
The following observations collectively
suggest at least two movements, In opposite
directions, along the N.80°W., 60°SW. fault
176 JOURNAL OF THE
plane at Locality 2: (1) Stratigraphic rela-
tionships signify the south fault block is
downthrown (Fig. 3). (2) The major re-
eional displacement along the northeast side
of the Rattlesnake Ferry Fault shows the
south side is upthrown. (3) Empirical knowl-
edge of the area indicates nearly all north-
westerly trending faults have their north
fault block downthrown. (4) Dip of strata
adjacent to the fault plane due to drag ef-
fect indicates reverse fault movement be-
cause the strata dip north whereas the fault
plane dips south (Fig. 3). (5) Directional
Fic. 4—Slickensides (lower left) developed along
N.80°W. fault in Backbone limestone just below
Clear Creek-Backbone contact (at pick handle).
Locality Two.
smoothness along well-developed slicken-
sides indicates the south fault block to be
upthrown (Fig. 4).
The N.45-50°W. fault intersects, con-
tinues across, and displaces the N.80°W.
fault plane (Fig. 3), indicating the N.45—
50°W. fracture occurred later than the last
displacement (normal fault movement)
along the N.80°W. fault. The N.45-50°W.
fault was present before the deposition of the
mineralizing solutions which are contained
in its fracture. This suggests that the min-
eralization emplacement may have occurred
(a) later than that period of faulting during
which the reverse fault occurred and (b)
after the normal fault movement along the
existing reverse fault plane.
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 6
Studies in the Pomona Area a few miles
to the northeast have shown that two sepa-
rate periods of faulting occurred in the
area: | post-Chesteran—pre-Pennsylvanian
and later post-Pennsylvanian displacements
along the same fault-plane (Desborough,
1957, p. 201). Evidence suggesting move-
ment along the same fault plane, in opposite
directions during separate periods of fault-
ing, has been presented (Desborough, 1957,
p. 201).
Weller and Ekblaw (1940, p. 26) imply
that thrusting forces originating in the
Ozark region resulted in the formation of
the Rattlesnake Ferry Fault. The writer
agrees. They also suspected this structure
“originated in post-Mississippian—pre-
Pennsylvanian time and has subsequently
been accentuated” (Weller and Ekblaw,
1940, p. 25).
On the assumption that the first displace-
ments along the Rattlesnake Ferry Fault
originated during the post-Mississippian
interval, reverse-fault movement along the
N.80°W. fault at Locality 2 probably oc-
curred at that time. According to Weller’s
observations (1940, p. 51), local compres-
sional forces would cause reverse fault dis-
placement. The displacement now evident
along the N.80°W. fault (Fig. 3) is ap-
parently due to normal-fault movement.
This movement suggests tensional forces
which were accommodated because a pre-
viously formed fault was present.
Mineralization —The rock at Locality 2
is not appreciably brecciated as it is at Lo-
eality 1. Mineralization here consists of vein
calcite with minor amounts of galena, sphal-
erite, and sparsely scattered euhedra of chal-
copyrite. Vein calcite occurs abundantly
only along the N.45-50°W. fault plane, the
mineralized portion of which is not more
than 3 feet wide. Galena occurs in chunks up
to 6 inches across with well developed cube
faces. Replacement is indicated by the ran-
dom distribution of sphalerite in the Back-
bone limestone. It is also present as cavity
fillings in the form of veinlets an inch in
width. The veinlets probably formed along
joints, as they are generally parallel to the
N.40-50°W. fault. Sphalerite also occurs as
cavity fillings along the styolites. It is par-
JUNE 1959
ticularly conspicuous along both fault
planes, including the slickensides in the
Backbone limestone (Fig. 4). Galena is pres-
ent as cavity fillings in the form of veinlets
with the same strike as those with sphalerite.
They have not been found together in the
same veinlet. Some of the veinlets have been
oxidized to limonite and exhibit boxworks.
Excavations along the N.45-50°W. fault in
the creek bed revealed abundant vein calcite
and chunks of galena as large as 6 inches
in diameter with sphalerite in lesser
amounts. No smithsonite was observed here.
The paragenesis at Locality 2 is vague. In
one small veinlet contact relations of min-
erals suggest that some calcite is older than
galena. Where sphalerite and calcite are
found in veins the sphalerite is older. On the
other hand, where sphalerite is randomly
distributed in limestone and not in veins, it
is younger than the associated calcite. Age
relationships between galena and_ sphal-
erite are not clear. As at Locality 1, two
generations of calcite are inferred if 1t may
be assumed that in usual sequence, sulphides
are deposited later than one stage of calcite
(McKinstry, 1948, p. 149).
Late in the fall of 1957 an exploration
hole 80 feet deep was drilled about 300 feet
northeast of Locality 2. It is reported to
have penetrated 80 feet of valley fill which
consisted mostly of sand and gravel. This
suggests that the slope of the hill on the
south valley wall may continue downward
as much as 100 feet vertically with the same
steep gradient now exhibited by the hill
above the valley-fill (cross-section, Fig. 2).
CONCLUSIONS
(1) Mineralization is concentrated along
both E-W and NW-SE trending faults.
(2) The glauconite content and abun-
dance of silicic (chalcedony and quartz)
material in the Clear Creek limestone of this
area permits its differentiation from upper
Backbone limestone.
(3) Evidence strongly suggests move-
ment along the same fault plane in opposite
directions during two separate periods of
faulting.
(4) Reverse fault movement along the
Rattlesnake Ferry fault zone is suggested.
DESBOROUGH: SULPHIDE MINERALIZATION
177
(5) The upper Backbone limestone may
be a host for sulphide mineralization in ad-
jacent areas where it is not siliceous and
faults are present.
ACKNOWLEDGMENT
I wish to thank Dr. and Mrs. David
Nicol and Dr. Stanley Harris, Jr., for eriti-
cism of the manuscript and Dr. Dewey Amos
for helpful suggestions during the investiga-
tion. I also acknowledge the assistance of
K. Dean Mellravy in preparing the illustra-
tions.
REFERENCES
Basset, C. F. The Devonian strata of the Alto Pass
quadrangle. Trans. Illinois Acad. Sci. 18: 360-
368, 3 figs. 1925.
BraDBuRY, JAMES C. Outlying occurrences of galena,
sphalerite, and fluorite in Illinois. Geol. Surv.
Illinois, Ind. Min. Notes 7: 4. 1957.
DessorouGH, GrorcE A. Faulting in the Pomona
Area, Jackson County, Illinois. Trans. Illinois
Acad. Sci. 50: 199-204, 3 figs. 1957.
De Srrter, L. U. Structural geology: 522, 309 text
figs. New York, 1956.
ExsBLaw, GeorcE E. Post-Chester, Pre-Pennsyl-
vanian faulting in the Alto Pass Area. Trans.
Illinois Acad. Sci. 18: 378-382, 1 fig. 1925.
Mckinstry, H. E. Mining geology: 680, 3 pls., 145
text figs. New York, 1948.
Poor, R. S. The stratigraphy of the Mississippian
System in the Alto Pass quadrangle. University
of Illinois master’s thesis, unpublished mss.
SavacE, T. E. The Devonian formations of Illinois.
Amer. Journ. Sci. 49 (4): 169-182, 1 pl., 3 figs.
1920.
Sr. Cruatr, Stuart. Oil investigations in part of
Williamson, Union, and Jackson Counties.
Geol. Surv. Illinois 35: 53, 3 pls., 2 figs. 1917.
WELLER, J. Marvin. Geology and oil possibilities of
extreme southern Illinois. Geol. Surv. Illinois,
Rept. Inv. 71: 71, 1 pl. 1940.
. Geologic map of Illinois. 1945.
WELLER, J. Marvin, and Exsiaw, Georce FE. Pre-
luminary geologic map of part of the Alto Pass,
Jonesboro and Thebes quadrangles. Geol. Surv.
Illinois, Rept. Inv. 70: 26, 1 pl. 1940.
WELLER, J. Marvin, and Sutton, A. H. Mississippian
border of the Eastern Interior basin. Bull.
Amer. Assoc. Petroleum Geol. 245 (5): 765-
858, 10 figs. 1940.
WELLER, S., and Wetter, J. Marvin. Preliminary
geologic maps of the pre-Pennsylvanian forma-
tions in part of southwestern Illinois. Geol.
Surv. Illinois, Rept. Inv. 59: 1 pl., 2 figs. 1939.
WortHEN, A. H. Geology of Alexander, Union, and
Jackson Counties. Geol. Surv. Illinois 3: 20-83,
3 pls. 1868.
178 JOURNAL OF THE
ENTOMOLOGY.
BuaKE, Arlington, Va.
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 6
Seven new galerucid beetles from the West Indies. Doris H.
(Received April 21, 1959)
Six of the seven new species of Galeru-
cinae from the West Indies described in this
paper were collected by Fernando de Zayas
in Cuba. He has been collecting insects there
for many years until he has a large number
which may in time form the nucleus of a
National Collection of Cuba.
Monocesta cubensis, n. sp.
Fig. 4
About 6 mm in length, elongate oblong, the
elytra covered wth fine pale pubescence, pro-
thorax with a transverse groove, dirty yellowish
brown, the head with a piceous band on either
side, leaving only a narrow pale vertex; elytra
with broad dark humeral vitta having a violet
lustre and extending to the apex and uniting
with a narrow marginal vitta, a shorter sub-
sutural vitta uniting across the base with the
others but not reaching the apex; breast and
abdomen except tip dark, legs and antennae bi-
colored.
Head with a broad piceous band extending on
either side from occiput about eye, leaving a
narrow pale yellow brown stripe down front;
mouthparts deep brown, occiput smooth with a
few short hairs at base of head, frontal tubercles
distinct. Antennae with only the six basal joints
present in the single specimen, these pale at base,
piceous at apex, second and third joints subequal,
fourth as long as second and third together,
fifth shorter than fourth. Prothorax approxi-
mately twice as broad as long, almost rectangu-
lar with a strong tooth at each angle, a trans-
verse median sulcus and a smaller one in the
middle over the occiput; surface shining, im-
puncate, yellowish brown. Scutellum dark with a
violaceous luster, densely pubescent. Elytra
elongate, not perceptibly wider apically, humeri
prominent, a short intrahumeral sulcus, faint
subcostate ridges along the middle, surface shin-
ing feebly beneath the very fine and appressed
pale pubescence, and densely, finely, and shal-
lowly punctate; pale yellow-brown with a broad
subsutural dark vitta having a violaceous luster
and not reaching apex, a broad lateral vitta from
humerus to apex and a marginal vitta uniting at
humerus and apical curve with the lateral vitta.
30dy beneath with breast and abdomen except
the tip dark. Legs having the anterior and middle
femora pale with a median and apical dark area,
the posterior femora dark at apex, anterior tibiae
dark on one side, middle and posterior tibiae
dark at base and apex, tarsi with apex of each
joint dark. Length 6 mm; width 2.3 mm.
Type, female, in collection of F. de Zayas, from
La Brena, Moa, Oriente Province, Cuba, col-
lected by Fernando de Zayas and Pastor Alayo.
Remarks —One species of Coelomera has been
described from Cuba by Suffrian, C. liturata, and
although the description resembles somewhat the
present species, the beetle is evidently a true
Coelomera in that the third antennal joint is
twice as long as the second. In addition only
two washed-out pale vittae are on the elytra, and
the elytra are somewhat widened behind, which
is not the case in the present species. This is the
first Monocesta known from the West Indies. In
Clark’s classification of the genus it belongs to
Division B, the smaller, more parallel-sided bee-
tles, with the elytra not postmedially dilated.
Galerucella melanocephala, n. sp.
Fig. 7
About 5 mm in length, oblong oval, covered
with short, pale, closely appressed pubescence,
the elytra more densely and coarsely punctate
than the prothorax, the prothorax depressed at
sides and middle; pale yellow-brown, the head
more or less black over occiput, antennae with
apices of joints 1 to 7 black, rest dark; femora,
tibiae and tarsi dark at apices, elytra with three
pale reddish brown vittae on each, becoming in-
distinct before apex.
Head with interocular space more than half
its width, a median line down occiput to frontal
tubercles, upper part of head dull, closely punc-
tate, and covered with pale pubescence; inter-
antennal area flat, upper part of head dull black
usually, sometimes dark on either side with a
pale area between, from tubercles to labrum
pale, labrum dark. Antennae not extending to
middle of elytra, stout, the third joint longest,
pale with the apices of jomts 1 to 7 black,
es oo
Rieter SAN
ms
3.Ectmesopus nigrolimbatus —
6. Chthoneis vittata
i
2.Ectmesopus zayas
By -Leptonesi ofes quadrimaculata
1. Galerucella spi lopte ra
A.Monocesta cubensis
8. Chthoneis vittata q4
Fies. 1-8—wWest Indian Galerucinae.
7.Galerucella melanocephala
180 JOURNAL OF THE
S to 11 entirely dark. Prothorax twice as wide
as long, widely depressed at sides and down
the middle, lateral margin somewhat angulate,
a small tooth at basal and apical angles; surface
punctate, and covered with pale appressed pu-
bescence, entirely pale. Scutellum squarish, pale.
Elytra densely and strongly punctate, covered
with short pale pubescence, through which on
the pale yellow brown surface the punctures are
apparent; three rather narrow pale reddish
brown vittae on each elytron, becoming indistinct
before apex, remnants of another below humerus
on the side, not apparent from above. Body
beneath pale with the breast and area about
coxae a little darker; legs pale, the apices of fem-
ora, knee of tibiae and apices of tibiae and tarsi
black. Length 5.8 to 5.8 mm; width 2.2 mm.
Type, male, U.S.N.M. type no. 64684, taken
at La Brena, Moa, Oriente Province, Cuba, in
June 1954 by F. de Zayas and Pastor Alayo. A
second specimen was taken at Yunque, Oriente
Province, in July 1955 by Zayas, and a third at
Piloto, Moa, Oriente Province, June 1954, by
Zayas and Alayo.
Remarks —This is distinguished from the other
Cuban species of Galerucella by the black or
partly black occiput (one specimen from Piloto
has the occiput and tubercles black with a pale
area between).
Galerucella spiloptera, n. sp.
Fig. 1
About 4 mm in length, oblong oval, covered
with fine pale pubescence, punctate beneath, pale
yellow brown, the elytra with deep brownish
spots and remnants of vittae along suture, middle
of elytra and along the sides; antennae pale with
apices of joints a little darker.
Head with interocular space more than half
its width, a median depressed line down occiput
to inconspicuous frontal tubercles, area between
antennal sockets flat, lower front short, labrum
small, a short, closely appressed pale pubescence
covering occipital sculpture. Antennae stout, ex-
tending below humeri but not to middle of elytra,
third joint longest, all joints pale with apices a
little darker. Prothorax approximately twice as
wide as long with slightly rounded sides, surface
widely depressed on sides and in middle, covered
with short, closely appressed pale pubescence
hiding the punctation beneath; entirely pale.
Scutellum pale. Elytra densely and strongly
punctate, the punctures visible through the
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 6
dense, fine, closely appressed pubescence, a long
incurving intrahumeral depression, another along
the suture below scutellum, and another along
the side before the apex; yellow brown with
cinnamon brown spots and fragments of vittae
along the suture, a spot near base in middle,
another half way down and two elongate ones
before apex, a spot covering humerus and ex-
tending down the side, more or less interrupted to
apical curve. Body beneath a little deeper brown
than upper surface, shining, thinly pubescent.
Legs entirely pale. Length 4.2 mm; width 1.8
mm.
Type, male, U.S.N.M. type no. 64683, taken in
Miami, Fla., from a plane from Curacao, Dutch
West Indies, via Jamaica, B.W.1., collected by
W. F. Buren on March 29, 1946.
Remarks—The spotted markings, or inter-
rupted elytral vittae, differentiate this small
species from the others in the West Indies. It
somewhat resembles G. interrupta Jacoby from
South America, a larger, less pubescent species.
Chthoneis vittata, n. sp.
Figs. 6, 8
About 5 mm in length, oblong oval, shiny,
densely punctate, the elytra faintly costate, dirty
yellow brown, the head and breast deeper brown,
antennae, except the basal joints, brown, each
elytron with four more or less interrupted brown-
ish vittae, tibiae and tarsi bicolored.
Head with interocular space approximately
half width of head, frontal tubercles large and
distinct, a large shallow fovea on each side near
eye, a short, narrow carina between antennal
sockets, lower front short; deep brown in color
with the labrum darker brown. Antennae long
and slender, the three basal joints pale, rest dark
brown, second and third joints together equal
fourth in length, rest long but not so long as
fourth, and gradually diminishing a little. Pro-
thorax almost twice as wide as long, widest
apically with a broad tooth at apical angle,
disk a little uneven with a slight bump on either
side near margin, surface shiny, finely punctate,
entirely yellow-brown. Scutellum dark brown.
Elytra rather depressed, several costae more dis-
tinct in apical half; surface shiny, densely and
somewhat rugosely punctate; yellow brown with
four deep reddish brown vittae on each elytron,
the second and third being interrupted before
apex, and the lateral one broadening to cover
humerus. Epipleura vanishing soon after the
JUNE 1959 BLAKE: SEVEN NEW
middle. Body beneath pale with breast in part
deep brown and tibiae at knee and towards apex
dark, the tarsal joints pale at base and dark at
apex. Coxal cavities open, claws appendiculate.
Length 5.2 mm; width 2 mm.
Type, male, U.S.N.M. type no. 64685, from
Piloto, Moa, Oriente Province, Cuba, collected
in June 1954 by F. de Zayas and Pastor Alayo.
One paratype in collection of F. de Zayas.
Remarks —tThis third species of Chthoneis has
been collected by Zayas and Alayo in the moun-
tains of Oriente Province, Cuba. This one differs
from the other two West Indian species in being
vittate, but is of the same dirty yellowish brown
coloration otherwise. The aedeagus bears a
strong resemblance to that of C. insulae Blake,
also from Cuba. A specimen collected at Gran
Tierra, Moa, Oriente Province, on June 5, 1951,
by Zayas is considerably larger (length 7 mm;
width 2.8 mm), and darker in coloring. The pro-
thorax in relation to the elytra is not so wide.
Unfortunately only one specimen, a female, is at
hand, and it is not clear from this single specimen
whether this is a distinct species or merely a large
female specimen of C. vittata. A drawing has
been made of it.
Ectmesopus zayasi, n. sp.
ie. 2
About 2 mm in length, narrowly oblong, shin-
ing, deep blue above except for the wide pale
margin on the prothorax and the pale lower part
of the face, the legs pale with apices of middle
and posterior tibiae and tarsi brownish; lower
surface pale, the breast a bit darker. Antennae in
male with the two terminal joints enlarged and
middle tibiae notched near apex.
Head with interocular space approximately
half width of head, upper part piceous with fine
punctures, tubercles and lower front pale yellow;
tubercles distinct, a narrow carina down lower
front. Antennae in male with tenth and eleventh
joints enlarged, dark brown, the basal joints a
little paler. Prothorax narrow, a little wider than
long, with nearly straight sides, without depres-
sions, shining deep piceous with a bluish luster,
the margins pale yellow; impunctate. Scutellum
dark. Elytra shining deep blue with distinct punc-
tation. Body beneath pale, the breast a little
darker, legs pale with the apical half of middle
and posterior tibiae and tarsi deeper brown. Mid-
dle tibiae in male notched. Length 2 mm; width
0.9 mm.
GALERUCID BEETLES 181
Type, male, from Somorrostro, San José de las
Lajas, Havana Province, Cuba, collected by F.
de Zayas, and in his collection.
Remarks—None of the other species of Ect-
mesopus so far described except E. tristis Blake,
which is entirely dark, has so nearly dark a pro-
notum, in this case only the margin on the sides
is pale. The usual abnormality of the male an-
tennae is in the last two thickened joints.
Ectmesopus nigrolimbatus, n. sp.
Fig. 3
About 3.5 mm in length, elongate oblong-oval,
shining, the elytra densely and distinctly punc-
tate, pale reddish yellow with the eight basal an-
tennal joints darker, the femora with a dark
streak above, tibiae and tarsi dark, sides of pro-
notum narrowly dark, elytra deep blue.
Head with interocular space half width of head,
occiput shining and smooth, very finely punc-
tate, frontal tubercles well defined, a narrow
carina between antennal sockets running down
front. Antennae not reaching the middle of the
elytra, third joint a little longer than second,
about half as long as fourth; basal eight joints
deep brown, apical three reddish yellow. Pro-
thorax nearly as long as wide, with slightly curved
sides, disk not depressed but smoothly convex,
basal angles oblique; pale reddish yellow with
sides narrowly piceous, the dark area wider an-
teriorly, surface shining, impunctate. Scutellum
reddish brown. Elytra slightly wider apically,
with distinct intrahumeral sulcus and well marked
humer1; shining, densely and distinctly punctate,
deep blue. Body beneath reddish yellow, the fem-
ora pale with a dark streak above and at apex,
front tibiae dark on upper side, pale beneath,
middle and hind tibiae entirely dark, tarsi dark.
Length 3.7 mm; width 1.7 mm.
Type, female, from Piloto, Moa, Oriente Proy-
ince, Cuba, collected in June 1954 by Fernando
de Zayas and Pastor Alayo, and in the collection
of Zayas.
Remarks —Although only a female of this spe-
cles is known, I am pretty sure that the male has
notched middle tibiae and probably some deform-
ity of the antennal joints. The only two other
species having a close resemblance to this are
from Haiti and the Dominican Republic, £.
angusticollis Blake and E. leonardorum Blake.
Both species have dark sides to the prothorax
but differ from the rest of the genus in being more
slender.
182 JOURNAL OF THE
Leptonesiotes quadrimaculata, n. sp.
Big. 5
~
About 5.5 mm in length, elongate oblong oval,
the elytra finely and confusedly punctate, pale
reddish, the antennae, tibiae and tarsi deeper
brown, the femora in basal half with a metallic
luster, the abdomen also metallic, the elytra with
a large basal fascia interrupted at the suture, and
an apical one covering apical half, these spots
being bluish green.
Head with interocular space half its width, oc-
ciput well rounded, smooth, shining, nearly im-
punctate; frontal tubercles distinctly marked, a
short carina between antennal sockets; head en-
tirely pale reddish. Antennae not extending to the
middle of the elytra, gradually thickening to-
ward apex, third joint shorter than fourth, basal
joints pale, the remaining ones deeper brown.
Prothorax a little wider than long, with nearly
straight sides, apical angle obtusely truncate,
disk smoothly convex, without depressions, en-
tirely pale reddish, shining, 1mpunctate. Scutel-
lum pale. Elytra wider than prothorax and
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 6
shghtly wider apically, a short intrahumeral sul-
cus, surface finely punctate, shining, pale reddish
with a broad basal fascia narrowly interrupted
at the suture of lustrous bluish green, and an-
other even broader area covering apical half of
elytra. Body beneath reddish brown with the
middle of the breast and abdomen darker brown,
the abdomen having a metallic lustre, femora
also with metallic lustre, except at apex which
is pale; tibiae and tarsi brown. Anterior coxal
cavities open. Claws appendiculate. Length 5.7
mm; width 2 mm.
Type, female, collected at Rancho Luna, Cien-
fuegos, Las Villas Province, Cuba, in June 1955,
by Fernando de Zayas, and in his collection.
Remarks—Al\though no male has been ex-
amined, I believe that this is closely related to
Leptonesiotes cyanospila (Suffrian) and that the
male has notched middle tibiae and possibly en-
larged hind femora. It has a color pattern similar
to that species but instead of the small basal and
apical spots, the present species has spots so large
as to form basal and apical fasciae.
ti
AMERICAN INSTITUTE OF CHEMISTS HONOR AWARD
THomas R. Henry, the Washington Star’s sci-
ence columnist, was recently presented with the
annual honor award of the Washington Chapter,
American Institute of Chemists. Mr. Henry was
cited for his service to science as a professional
writer and author and for his ability and untiring
efforts in keeping the public informed of impor-
tant and noteworthy advances in science through
the medium of the press.
The presentation was made by Dr. Emil Ott,
past-president of the American Institute of
Chemists, at a dinner held at the Army-Navy
Club on May 27, 1959. Dr. Ott emphasized Mr.
Henry’s contributions to science reporting and
his efforts in the education of editorial writers
on the importance of disseminating science news
to the public.
The invitation address was delivered by Ben-
jamin McKelway, editor of the Evening Star. He
praised Mr. Henry for his ability as a reporter
who has written articles on many important news
events. He also praised Mr. Henry’s style and
firm grasp of his subjects.
In his acceptance address, Mr. Henry outlined
the progress made in science reporting over the
past 30 years. Further, he pointed out that jour-
nalism and science have been accepting each other
and as a result have contributed to public under-
standing and progress of science itself.
JUNE 1959
SETTY: HIP AND THIGH MUSCLES OF THE EMPEROR PENGUIN
183
ZOOLOGY —M uscles of the hip and thigh of the emperor penguin. L. R. SErry,
School of Medicine, Howard University. (Communicated by Herbert Fried-
mann.)
(Received March 11, 1959)
Some emperor penguins, Aptenodytes fos-
teri, recently brought from the Antarctic
to the zoo at Portland, Oreg., died from an
epidemic of aspergillosis. After autopsy,
some parts of the bodies of the dead birds
were in a satisfactory condition for ana-
tomical study. The musculature of the hip
and thigh was one of such parts.
METHOD
One specimen was prepared to show the skele-
ton of the region; another, the musculature. The
latter was preserved in a solution made of a
mixture of equal parts of 4-percent formalde-
hyde, glycerine, and 95-percent alcohol. This
specimen was used for the dissection of the
muscles.
The function of each muscle was determined
by pulling on the muscle from near the point of
insertion toward the point of origin.
The descriptions of the muscles of the hip
and thigh of a penguin, Hudyptes chrysocome,
by Watson (1883) were used as a guide.
Although Watson in his work on Eudyptes
chryosocome considered the trunk to be in a
horizontal position, the natural vertical position
of the trunk is taken as the basis of orientation
in the present study.
RESULTS
The bones serving for the attachment of the
muscles of the hip and thigh are shown in the
accompanying labeled photograph (Fig. 1).
In both the fresh and the preserved condi-
tions, the muscles are very dark red-brown. Their
strong fishy odor remains even after the addi-
tion of the above preservative.
The superficial muscles of the lateral aspect
of the hip and thigh (Fig. 2) are the following:
Sartorius. This is a very large, elongated mus-
cle and the most cephalic of all the muscles of
the thigh. It originates by an aponeurosis from
about 2.5 em of the cranial end of the coalesced
splnous processes of the lumbosacral portion of
the vertebral column and the spinous process of
the four thoracic vertebrae immediately above.
It arises also along the dorsolateral edge of the
cephalic end of the ilium. The fibers pass ob-
liquely to the insertion of the muscle on the
anterocephalic part of the patella.
Sartorius flexes the thigh and extends the leg.
Rectus femoris. The cephalic portion of the
musculoaponeurotic sheet that covers the lateral
surface of the thigh is rectus femoris. It arises by
an aponeurosis from the coalesced spinous proc-
esses of the lumbosacral portion of the vertebral
column. The fibers run transversely to the in-
sertion which is by a tendon in common with the
tendon of extensor cruris (Fig. 3) to the poste-
rior side of the patella.
Rectus femoris flexes the thigh and extends
the leg.
Tensor fasciae femoris. The caudal portion of
the musculoaponeurotic sheet that covers the
lateral surface of the thigh is tensor fasciae
femoris. It originates from the coalesced spinous
processes of the lumbosacral vertebrae by an
aponeurosis shared with rectus femoris. The
fibers take a transverse course, and the insertion
is by a tendon into the posterocaudal part of
the patella and the cephalic end of the lateral
upper tibial crest (Fig. 1).
This muscle extends the thigh and flexes the
leg.
Biceps femoris. This is a large muscle immedi-
ately caudad of tensor fasciae femoris. It origi-
nates along the posterior border of the innomi-
nate bone and on the caudal margin of the
tendon of origin of the tensor fasciae femoris. Its
fibers run laterally and shghtly caudally to the
insertion which is made by a tendon on a tu-
bercle on the outer side of the fibula at the junc-
tion of the upper and middle thirds of that bone
(Fig. 1). The tendon of insertion passes through
a loop of a band-like tendon extending from the
distal end of the lateral surface of the shaft of
the femur to the tendinous outer head of origin
of a leg muscle (gastrocnemius). The loop is
thickened where it makes a sharp bend around
the caudal border of the tendon of biceps fem-
Oris.
The sciatic nerve lies just below biceps fem-
184 JOURNAL OF THE
oris and runs almost parallel to the long axis of
this muscle. As soon as the nerve makes its exit
from the pelvis, it sends branches into biceps
femoris (Fig. 3).
Biceps femoris is an effective flexor of the leg.
Semitendinosus. Semitendinosus is a_ large
muscle situated immediately caudad of biceps
femoris and is essentially as wide as that muscle.
Semitendinosus arises from the most posterior
part of the caudal processes of the innominate
bone. It also arises from the transverse processes
of the third, fourth and fifth caudal vertebrae.
Most of the fibers pass essentially in the trans-
verse plane. Insertion is by a ribbonlike tendon
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 6
about 3.75 em long and 1.25 em wide into the
distal end of the medial upper tibial crest (Fig.
Lye
This muscle flexes the leg and extends the
thigh. If the knee joint be flexed, the posterior
fibers depress the tail.
The deep muscles of the hip and thigh (Fig. 3)
are as follows:
Gluteus medius. Gluteus medius is a large
muscle. It arises from the whole posterior sur-
face of the ium and from the lateral surface of
some of the coalesced spinous processes of the
lumbosacral region. The fibers run caudolaterad
and are inserted by a tendon on the greater tro-
1h:
0
oo :
Fic. 1.—Lateral aspect of the portion of the skeleton of A ptenodytes fosteri to which muscles of the
hip and thigh have attachment. Not all the thoracic vertebrae involved are shown. 1, Shaft of the femur.
2, Groove on the patella for the tendon of musculus ambiens. 3, Medial upper tibial crest. 4, Lateral
upper tibial crest. 5, Tubercle of the fibula. 6, Groove on the fibula for the tendon of musculus ambiens.
7, Obturator foramen. 8, Pubic portion of the innominate bone. 9, Cartilaginous tip of the pubic bone.
10, Pygostyle. 11, Transverse process of a caudal vertebra. 12, Ischium portion of the innominate bone.
13, Greater trochanter. 14, Coalesced spinous processes of the lumbosacral portion of the vertebral col-
umn. 15, Ilium portion of the innominate bone. 16, Spinous process of a thoracic vertebra.
JUNE 1959
Fic. 2—Superficial muscles of the lateral aspect
of the hip and thigh of Aptenodytes foster. 1, Sar-
torius. 2, Rectus femoris. 3, Tensor fasciae femoris.
4, Semitendinosus. 5. Biceps femoris.
chanter of the femur and to a lesser extent on
the articular capsule of the hip joint.
The cephalic third of gluteus medius is con-
cealed by sartorius; the caudal two-thirds are
covered by the aponeurosis of origin common
to rectus femoris and tensor fasciae femoris.
Gluteus medius rotates the hip joint medially.
Gluteus minimus. Gluteus minimus is smaller
than gluteus medius. It originates along the
lateral border of the ilium and from a tendinous
sheet between it and gluteus medius. The fibers
run caudolaterad and insert by a tendon on the
greater trochanter of the femur anterolaterad
of the insertion of gluteus medius.
Much of the posterior surface of gluteus mini-
mus is covered by gluteus medius.
Gluteus minimus rotates the hip joint medi-
ally.
A third gluteal muscle has not been recognized
In penguins.
Extensor cruris. Extensor cruris is a large mus-
cle mass which originates from the lateral and
cephalic surfaces of the shaft of the femur. The
part on the cephalic surface is much larger than
the part on the lateral surface, and it arises
about 2.56 em more proximally than that on the
SETTY: HIP AND THIGH MUSCLES OF THE EMPEROR PENGUIN
185
lateral surface. The cephalic part inserts into the
upper truncated extremity of the patella. The
lateral part inserts into the tendon of tensor
fasciae femoris and hence reaches the lateral
surface of the patella and the cephalic end of
the lateral upper tibial crest.
Extensor cruris is covered laterally by the
musculoaponeurotic sheet formed by rectus fem-
oris and tensor fasciae femoris.
Extensor cruris functions as an important ex-
tensor of the leg.
Adductor longus. This muscle arises from
about 3 em of the posterior border of the ischium
portion of the innominate bone. The fibers run
obliquely to the point of insertion near the dis-
tal end of the caudal border of the shaft of the
femur.
Adductor longus is crossed laterally by the
sciatic nerve. This nerve and adductor longus
are concealed by biceps femoris. At its origin,
the adductor longus crosses obturator externus;
CS
ar a T
Ls aa
Ni 3
6
Fic. 3—Lateral surface of the deep muscles of
the hip and thigh of Aptenodytes fostert. Sartorius
has been cut off at its insertion. Rectus femoris and
tensor fasciae femoris have been entirely removed.
Also biceps femoris and semitendinosus have been
bisected and their cut ends reflected. 1, Gluteus
medius. 2, Gluteus minimus. 3, Adductor magnus.
4, Extensor cruris. 5, Sartorius. 6, Semimembrano-
sus. 7, Crurococcygeus. 8, Semitendinosus. 9, Biceps
femoris. 10, Adductor longus. 11, Sciatic nerve. 12,
Obturator externus.
186 JOURNAL OF THE
at its insertion, it makes contact with adductor
magnus. Its tendon of insertion unites with that
of crurococcygeus.
The action produced by adductor longus 1s
extension of the thigh.
Crurococcygeus. Crurococeygeus is a_ long
muscle, tapering at each end and measuring
over 22.5 em from the origin to the insertion. It
arises by a flat tendon for a distance of 1.25 em
from the cephalolateral border of the pygostyle.
The tendon becomes slender and rounded before
joining the muscle proper. The muscle fibers take
an oblique course; and insert by a long, narrow
tendon into the lateral side of the shaft of the
femur distad to the tendon of insertion of adduc-
tor longus to which it is fused. Just distad to the
Fic. 4—Superficial muscles of the medial aspect
of the hip and thigh of Aptenodytes fosteri. 1, Sar-
torius. 2, Extensor cruris. 3, Musculus ambiens. 4,
Gracilis. 5, Semimembranosus (abdominal head).
6, Semimembranosus (pubic head). 7, Adductor
magnus. 8, Gluteus minimus.
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 6
insertion of crurococcygeus is the attachment
of the upper end of the fibrous pulley through
which the tendon of insertion of biceps femoris
passes.
Crurococcygeus is covered by semitendinosus
and biceps femoris laterally and by semimem-
branosus and adductor magnus medially.
Acting with its fellow of the opposite side,
crurococcygeus depresses the tail. If the tail be
fixed, the muscle is an extensor of the thigh.
Obturator externus. Obturator externus arises
from the whole lateral surface of the innominate
bone caudad of the acetabulum, exclusive of the
pubic part of this bone. The fibers run cephalo-
laterad to the tendon of insertion on the greater
trochanter of the femur just caudad of the ten-
don of insertion of gluteus minimus.
Laterally the muscle is crossed by adductor
longus and the sciatic nerve.
Obturator externus rotates the thigh laterally.
It is an antagonist of gluteus medius and gluteus
minimus.
Obturator internus. Obturator internus (not
shown in the figure) is an elongated oval mus-
cle. It arises from the greater part of the medial
surface of the ischium, the pubis and the mem-
brane between these two bones. The fibers pass
cephalad and end on a tendon which passes
through the obturator foramen and which is in-
serted on the greater trochanter of the femur
mediad of the insertion of obturator externus.
Since this muscle lies on the inner side of the
bony pelvis, only its tendon is in contact with
obturator externus.
Obturator internus assists obturator externus
in lateral rotation of the thigh.
Gemellus. Gemellus (not sho'yn in the figure)
is small and quadrilateral. It arises from the
lateral side of the innominate bone close to the
margin of the obturator foramen. The muscle
is divided into two slips by the tendon of in-
sertion of obturator internus. The fibers run
laterad to the insertion on the caudal border of
the greater trochanter of the femur just mediad
to the tendon of insertion of obturator internus.
The muscle is concealed by the insertion of
obturator externus.
Gemellus is a lateral rotator of the thigh.
The superficial muscles of the medial aspect
of the hip and thigh (Fig. 4) are the following:
Musculus ambiens. This is a flat, superficial
muscle on the medial side of the thigh. It has
JUNE 1959
an origin of about 3.75 em from the lateral
margin of the cephalic end of the pubic bone. It
extends toward the knee and tapers to a tendon
which is 0.6 em wide and 11.25 em long. This
tendon crosses the front of the knee joint in a
groove on the patella and in a groove on the
lateral side of the proximal one third of the
fibula (Fig. 1). Then this tendon passes medially
to the tendon of insertion of biceps femoris and
joins the head of a leg muscle (flexor perforatus
digitorum) which arises from the lateral side
of the distal end of the femur. The part of the
tendon that passes over the surface of the groove
on the patella has a marked thickening.
On its deep side, musculus ambiens makes
contact with gracilis. The part of the tendon of
insertion that lies in the groove on the patella
is concealed by the distal end of sartorius.
Musculus ambiens adducts the thigh and ex-
tends the leg.
Gracilis. Gracilis is a slender muscle that arises
from the whole medial surface of the shaft of
the femur. It inserts by a tendon on the medial
side of the proximal end of the medial upper
tibial crest.
This muscle lies between the origin of exten-
sor cruris and the insertion of adductor magnus.
The medial surface of the major part of it is
covered by musculus ambiens.
Gracilis extends the thigh.
Adductor magnus. This is a large, thick mus-
cle. It arises from the lateral side of the pubis,
ischium and the membrane between these two
bones for a distance of 9.37 em from the ob-
turator foramen to a point 1.25 cm distant from
the cartilaginous tip of the pubic bone. The fi-
bers pass transversely to the insertion on the
caudal surface of the distal half of the femur.
Some of the insertion is by a special tendon on
the area just above the internal condyle of the
femur. To this tendon some fibers of a leg mus-
cle (gastrocnemius) are attached.
Laterally the muscle makes contact with ad-
ductor longus and crurococcygeus.
SETTY: HIP AND THIGH MUSCLES OF THE EMPEROR PENGUIN
187
Adductor magnus adducts and extends the
thigh.
Semimembranosus. Semimembranosus is a
large, flat muscle. It has two heads of origin:
pubic and abdominal. The pubic head arises
from the following: (1) the lateral side of the
distal end of the pubic bone, including a part
of the cartilaginous tip of that bone; (2) the
lateral side of the adjacent distal end of the
ischium; and (3) the lateral side of the caudal
end of the membrane between the pubis and
ischium. The abdominal head arises from the
lateral surface of the abdominal wall where it
is attached to the aponeurosis of the abdominal
muscles for a distance of about 12.5 em running
parallel to the long axis of the body.
The fibers of both heads of origin extend to a
common insertion which is on the medial side of
the medial upper tibial crest. This insertion is a
linear one of 5 em, with additional fibers at the
cephalic end attached to the medial side of the
patella.
Laterally the pubic head makes contact with
crurococcygeus and semitendinosus. Cephali-
cally it is in contact with adductor magnus.
Semimembranosus extends the thigh and flexes
the leg.
SUMMARY
1. The morphology of the muscles of the
hip and thigh of the emperor penguin, Ap-
tenodytes fosteri, 1s very similar to that
given by Watson for Eudyptes chrysocome.
However, the muscle which he described as
pectineus was found to be represented in
Aptenodytes fosteri by only a ligament.
2. As suggested by Watson the possession
of an abdominal head by semimembranosus
is possibly a unique feature in the anatomy
of penguins.
LITERATURE CITED
SHUFELDT, R. W. Osteology of the penguins. Journ.
Anat. and Phy. 35. 1901.
Watson, M. Report on the Spheniscidae. Zool.
Voy. Challenger, pt. 18. 1883.
LSS JOURNAL OF THE
ZOOLOGY
WASHINGTON
ACADEMY OF SCIENCES — VOL. 49, No. 6
Noles on Mecistocephalus in the Americas, with a redescription of
Mecistocephalus guildingii Newport (Chilopoda: Geophilomorpha: Mecisto-
cephalidae). R.
E. .Crabill, ir. tice:
National Museum.
(Received April 7, 1959)
Heretofore four centipede species properly
referable to the genus Wecistocephalus have
been reported from the tropics of the New
World. These are: mavzillaris (Gervais),
1837; punctifrons Newport, 1842; guildingu
Newport, 1845; and janeirensis Verhoeff,
1938. Although I have never seen a neo-
tropical specimen of the first, I do not doubt
that it occurs in Central and South America:
maxillaris is probably pantropical. Whether
the true punctifrons, an Indian and south-
east Asian form, is established in the Neo-
tropics at all seems questionable, for there
is reason to suspect that most or all of those
neotropical specimens that have been called
punctifrons are in fact referable to an his-
torically obscure species, one which I believe
may be peculiar to the New World Tropics.
I submit that gwildingu and janeirensis both
refer to the same zoological entity and sug-
gest further that it may be very widely dis-
tributed in the tropical and parts of the sub-
tropical American continents. Indeed, it
may very well prove to be as representative
of the Americas as are mazillaris and in-
sularis (Lueas), 1863, of the Old World
tropics and subtropies.
This species was initially described as
guildingu from the Antillean island of St.
Vincent by George Newport in 1845 (p.
429). But inasmuch as the original charac-
terization was quite superficial, the identity
of guildingu has remained in obscurity un-
til the present time.
Dr. Chamberlin we know synonymized
guldingu under mazillaris (1920, p. 185),
so that whenever he reported the latter in
the Neotropics, as he did most recently from
southern Florida (1958, p. 14), we may be
sure that his specimens were either guild-
ingu or maxillaris, and usually the former.
In 1893 (p. 470) R. I. Pocock reported hav-
ing seen specimens, which he called guwild-
ingu from the West Indies; he expressed the
belief that they were not in any case con-
specific with punctifrons and thereby dis-
agreed with Meinert and Bollman who had
thought they were. These men had seen
specimens from St. Croix, Cuba, and Ber-
muda, and T. D. A. Cockerell had collected
others on Jamica. It seems probable that all
were referable to guildingu. Subsequently
no topotypical material from St. Vincent
was ever described, so that in his great
monograph of 1929 (p. 156) the Count von
Attems-Petzenstein was obliged to set aside
guildingu pending clarification.
The first adequate description—it 1s,
however, not without errors—of this centi-
pede appeared in 1938 (p. 383) when Karl
W. Verhoeff redescribed it from Rio de
Janeiro, Brazil, as a new species, janeirensis.
Topotypes of janeirensis from Rio de Ja-
neiro that I have seen are, however, essen-
tially indistinguishable from the St. Vincent
topotype of guildingu described below.
Equally similar to the St. Vincent topotype
are: a series of Florida specimens recently
acquired'; a specimen from the Panama
Canal Zone; eight individuals from the is-
land of Martinique lying in the Lesser An-
tilles not far to the south of St. Vincent. If
it is true that (a) my topotype is really con-
specific with the original cotypes, and (b)
all are conspecific with the specimens cited
above, then all must take the Newport
name. What we understand of distribution
in the genus and what we know about this
particular case strongly suggest both in-
ferences to be true.
Finally, in 1942 Wolfgang Bucherl re-
ported the presence of punctifrons and ja-
neirensis in Brazil, synonymizing guildingu
under the former but admitting he had never
seen a specimen of the latter. I suspect that
all these specimens were actually referable
to guildingit.
‘IT should lke to express my thanks to Dr.
Howard V. Weems, Jr., and to his colleagues of the
State Plant Board of Florida at Gainesville for their
kindness in placing these and many other specimens
in my hands for study.
JUNE 1959 CRABILL: NOTES
It seems to me that the evidence suggests:
(1) that the representative and possibly
endemic Mecistocephalus of the New World
tropics is guildingu, and further; (2) that
this species 1s very widely distributed from
southern Florida, throughout the Caribbean
and Central America, southward at least as
far as southern Brazil.
The following description is based upon a
single female topotype from St. Vincent. To
the best of my knowledge it is the first such
specimen known since the time of the origi-
nal description of the Newport species in
1845. Unfortunately his original cotypical
series cannot be identified in the British
Museum collections today and so must be
presumed to be unavailable.?
In the underlying description I have uti-
lized a number of new characters and have
attempted to refine some old ones. In both
cases it has often seemed desirable to devise
new terms to describe them, both to avoid
imprecision and to propose an interlinguistic
uniformity of unambiguous usage.
Imprecision of designation and the com-
mon failure of one worker to understand
exactly what another meant by loose and
variant usage have injected much confusion
into our present, often jumbled heritage. We
need to be exhaustive rather than merely
minimally (and highly subjectively) ana-
lytical in describing typical material; we
need to establish an unambiguous terminol-
ogy and then abide by it. New terms and
characters are signalized in the description
and then are treated separately at the end
of the paper: in addition all are illustrated
in the labeled figures.
Mecistocephalus guildingii Newport, 1845
On the basis of published descriptions one
could come to the conclusion either that (a)
insularis and guildingiw are conspecific, or (b)
they are not, but are very similar to one another.
On the basis of African material of insularis I
suggest they are very similar but not conspecific.
Briefly, they differ at least as follows. In insularis
(compare with data on guildingu below): clyp-
eal plagulae are as long as or somewhat longer
than the anterior areolate clypeus; buccal spic-
=I am indebted for this information to Dr. G.
Owen Evans, who is in charge of the arachnid and
myriapod collections at the British Museum.
ON MECISTOCEPHALUS
189
ula are deflected anteromedially and reach or
nearly reach anterior head margin; body suf-
fused with subsurface blackish-green pigment
flecks and patches; basal plate not centrally sul-
cate; Ist pedal tergite not bisuleate; ultimate
pedal tergite very long, sides regularly conver-
gent, posterior margin narrowly rounded.
Topotype: female. British West Indies, St.
Vincent Island. (Exact locality, collector, and
date are unknown.) U.S. National Museum
Myriapod Collection 2546.
IntRopucTion. Length, 33 mm. Pedal seg-
ments, 49. Body shape: anterior five-sixths of
body approximately parallel sided, final fifth
gradually narrowing. Color: head, prosternum,
and prehensors orange-brown; antennae, basal
plate, and first pedal tergite concolorous, lightly
orange-brown; tergites and sternites of anterior
body third white-yellow, becoming paler poste-
riorly; legs essentially white to very faintly yel-
low-white.
ANTENNAE. Length, 3.7 mm in Hoyer’s moun-
tant. Distally shghtly attenuate, each article dis-
tinctly longer than greatest width. First 4 slightly
indented at outer basal corner, the remaining
articles not so. First 7 clothed sparsely with very
long setae, the Sth suddenly densely shortly
setose as are those following. Ultimate article on
outer and inner surfaces of distal half with
elongate patches of short club- or spoon-shaped
setae, these short and not set into depressions.
CrepHatic PLATE. Dimensions: length 1.16 mm,
greatest width 0.62 mm, ie., 1: 1.187. Shape:
long and very narrow; sides straight but con-
verging very slightly posteriorly. Frontal suture
conspicuous, evenly curved posteriorly. From
straight posterior margin two diverging setiger-
ous sulci pass forward for about a third the
length of the plate. Prebasal plate not detected.
Ciypeus (Fig. 1). Paraclypeal sutures distinct,
complete (Note D). Each bucca (Note B) an-
teriorly areolate but posterior to spiculum (Note
H) smooth and consolidated; buccal spicula well
developed, bluntly pointed; buccal stili (Note
I) long and curved, anterior incisures (Note A)
distinct, deep; approximately the anterior half
of each bucca glabrous, as a group the long stiff
setae fall far short of the labral area and the
anterior incisures of the stili. A typical elypeal
area absent, in its position the areolate figures
are somewhat smaller and paler. Clypeal plagu-
lae (Note F) much shorter than the anterior
areolate clypeal portion; anterior margins
L9O
rounded, not square; separated posteriorly from
labrum by a thin membranous suture and from
each other by a thin areolate strip; their surface
nonporous, smooth except for small rugose pos-
teromedial corner. Setae: posterior geminate
setae (Note E) essentially paramedian and just
anterior to plagulae, with large alveolate sockets ;
midelypeal setae long and stiff, three on each
side, not set into sclerotized islands. LaBRUM
(Fig. 1). Midpiece not projecting below side-
pieces, its sides very narrowly overlapped by
sidepieces medially. Anterior division of each
sidepiece separated by suture from adjacent
plagula; posterior divisions each with a distinct
indentation laterally on posterior margin; labral
posterior margin smooth, not roughened or serru-
late. MANDIBLE. With 6 pectinate lamellae and
one membranous hyaline projection (an incipient
pectinate lamella?); the comb-teeth of each
lamella from 5 (on the first) to 11 (on one of the
medials) ; all teeth hyaline, broad, about equal
in length. First Maxinuazt (Fig. 6). Coxo-
sternum with a prominent midlongitudinal su-
ture, this margined anteriorly by a few stout
setae; each anterolateral corner extended into a
blunt projection, posterior to each a prominent
sinuous incisure or suture (Note C) ; lappets ab-
sent. Medial lobes shghtly shorter than telopo-
dites; both very long, curved; telopodite lappets
absent. Seconp MaxinuaE (Fig. 6). Without
medial suture or sign of division; coxosternum
medially and posterolaterally coarsely areolate,
anterolaterally smooth, essentially consolidated;
most setae set into strongly sclerotized semi-
alveoli confluent anteriorly with a large vacant
or membranous lacuna. Telepodite first article
very long, curved, bicondylic basally; apical
claw straight, small, very sharply pointed. Pro-
STERNUM (Fig. 5). Without sclerotic lines;
sparsely setose; shallowly areolate; midlongi-
tudinally very shallowly suleate. Anteriorly shal-
lowly diastemate, with two pale small sharp
denticles. Ventral condyles displaced far to each
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 6
ing front of head. First article with two rounded
prominent denticles; femoroid and tibioid each
with a rounded denticle; tarsungula with a mi-
nute pointed basal denticle. Ungular blades not
serrulate. Poison calyx extremely long and thin,
the digitiform appendices minute, beginning at
the pigmented base of the ungula proper. Poison
gland extending posteriorly to level midway be-
tween denticles of first article.
TERGITES (except ultimate pedal). Basal plate
with a midlongitudinal elongate elliptical sulcus.
First pedal tergite with a pair of deep para-
median sulci, these extending from posterior
margin not less that three-fourths the distance
to the anterior margin but not attaining it. Re-
maining tergites each deeply completely bi-
suleate. SPIRACLES. On anterior body third ver-
tically broadly elliptical, thereafter gradually
tending toward subcircular. Lecs. Dorsally very
sparsely shortly setose, ventrally and laterally
moderately setose, the setae long and straight.
Pretarsi ventrally evidently not concave, at most
flat basally; accessory claws acicular, not more
than one-third as long as pretarsus. STERNITES
(Figs. 2, 3). Rhachides (Note G) anteriorly bi-
fureate, subtended angles of first three or so ap-
proximately 90° when measured at base, there-
after widening slightly to subtend more than 90°
(to approximately 110°); bifureate rhachides
detected on sternites 2 through approximately
25, these very weak posterior to the tenth.
Sternites of about the anterior body third each
with a very long metasternite extending far
under the succeeding sternite.
ULTIMATE PEDAL SEGMENT (Fig. 4). Pre-
tergite separated from each of its pleurites by a
pronounced suture. Tergite with perfectly
straight sides and an evenly rounded posterior
margin; width to greatest length = 1:1.35. Pre-
sternite distinctly divided medially. Sternite sub-
triangular, the sides very strongly convergent,
the posterior margin rounded and very densely
clothed with fine setae, with very dense under-
side. TELopopiTEe (Fig. 5). Flexed, well surpass- lying, apparently glandular tissue; posterior
Fries. 1-6.—Mecistocephalus (M.) guildingii Newport, topotype: 1, Clypeus and bucca; ventral. AlJ
setae shown; areolation of left side shown. a, Right paraclypeal suture. 6, Right buccal spiculum. c,
Right plagula. d, Anterior end of right buceal stilus. e, Anterior incisure of stilus. f, Indentation on right
labral sidepiece. 2, Rhachis of third pedal sternite. 3, Rhachis of eighth pedal st2rnite. 4,
Ultimate pedal and postpedal segments; ventral. All setae of sternite and left coxopleuron shown; those
of postpedal segments deleted. 5, Prosternum and right prehensor; ventral. All setae deleted. Dashed
outline of poison calyx shown inside that of poison gland. 6, First and second maxillae; ventral. All
setae of left side shown; setal alveoli and lacunae of right side shown. Areolation of right side shown,
those of left deleted. a, Anterolateral projection of first maxillary coxosternum. b, Right lateral incisure
of first maxillary coxosternum. c, Setae with alveoli and lacuna in situ and enlarged.
Fics. 1-6.—(See opposite page for legend).
192 JOURNAL OF THE
rounded margin followed by a_ cushionlike
mound, this also densely finely setigerous. Each
swollen, not extending anteriorly
beyond rear margin of penultimate pedal seg-
ment; pores large and slightly smaller, dis-
tributed uniformly but absent ventromedially,
ventroposteriorly, dorsomedially, and dorsopos-
teriorly; ventromedial edge raised and swollen,
densely finely setose and with dense underlying
glandular tissue. Ultimate legs very thin and
long, with long stiff setae; pretarsus represented
by a microscopic terminal bristle. PosTPpEDAL
SEGMENTS (Fig. 4). Gonopods well separated;
basal article broad and flat; second article mi-
nute, nipplelike, only indistinctly separated from
the basal. Terminal pores conspicuous.
The other specimens that I have examined all
agree very closely with one another and with the
St. Vincent topotype. In the males the ultimate
sternite seems somewhat broader and shorter,
the coxopleura shorter than the corresponding
parts of the females.
Lengths (in mm): 5 males: 19, 21, 29, 30, 33;
11 females: 27, 28, 28, 30, 30, 30, 32, 33, 33, 33,
36. FiortpA: Miami, South Miami, Rockdale,
Key West. PanaMa Cana ZONE: Frijoles. Mar-
TINIQUE: Riviere Pilote. BRAziL: Rio de Janeiro.
coxopleuron
NOTES
A. Anterior Incisure (of the Stilus); New
Character. The anterior cleft or break on the
medial side of the buecal stilus, q.v. (Fig. le.)
B. Bucca; New Term (pl. = buccae, L.
“cheek”). The so-called cephalic pleuron; that
portion of the ventral head capsule bounded an-
teriorly by the paraclypeal sutures, q.v., and
laterally by the folded lateral margin of the
cephalic plate; a neutral descriptive term pro-
posed to replace the morphologically implicative
“pleuron” of authors. (See also stilus, spiculus,
anterior incisure.) (Fig. 1.)
C. Lateral Incisure (of First Maxillae); New
Character. The cleft on each side of the 1st
maxillary coxosternum. Its presence, absence,
development, and position are all significant sys-
tematically. (Fig. 6b.)
D. Paraclypeal Sutures; New Character. -The
sutures or grooves in most Geophilomorpha that
pass from the antennal sockets shortly laterally,
then ventroposteriorly usually to terminate in
the vicinity of the outer end of each labral side-
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 6
piece. When present they may be taken to de-
fine the lateral limits of the clypeus and the an-
terior limits of each bucca, g.v. The degree of
development, the course, the termination of these
sutures all have significance. (Fig. 1a.)
E. Posterior Geminate Setae; New Term. The
persistent pair of setae located posteriorly on the
clypeal midline. (Fig. 1.)
F. Plagula (of the Clypeus) ; New Term (pl. =
plagulae; L. “a small flat surface or area”). The
so-called clypeal or preclypeal consolidated
area(s), or in Mecistocephalidae the posterior
clypeus; widespread in the order, though in
many families much smaller in size. When pres-
ent, so far as is known always paired and bi-
lateral, each occupying a position just anterior
to the labrum on the posterior part of the
elypeus. (Fig. 1c.)
G. Rhachis (or Rachis); New Term (pl. =
rhachides, rachides, G. “a ridge, axis, back-
bone’). In Mecistocephalidae the elongate, mid-
longitudinal sternital thickenings, especially char-
acteristic of the more anterior sternites. The
rhachis is apparently in reality a very narrowly
inverted sternital fold whose surfaces, in any
case, serve as areas of muscular attachment. An-
teriorly the rhachis is bifureate or not; if bi-
fureate, the size of the angle subtended by the
bases of the anterior arms, within limits, has
systematic significance. (Figs. 2, 3.)
H. Spiculum (of the Bucca); New Term
(pl. = spicula, L. “a small spike or sharp
point”). In Mecistocephalidae, the pigmented
spikelike point on the anterior part of the bucea,
q.v. (hig ib;)
I. Stilus (of the Bucca); New Term (pl. =
stili, L. “a pointed writing instrument”). The
heavily sclerotized, elongate, usually blunt and
thickened inner edge of the bucca; at midlength
giving attachment to the maxillae. (Fig. 1d.)
REFERENCES
AttEeMs, Cari. Das Tierreich 52: 1-388. 1929.
BtcHEerRL, Wo.trcanc. Mem. Inst. Butantan 15:
1-372. 1941 (=1942).
CHAMBERLIN, RaLpH V. Can. Ent. 52(8): 184-189.
1920.
. Ent. News 69(1): 13-14. 1958.
Newrort, Gerorce. Trans. Linn. Soc.
19(4): 349-439. 1845.
Pocock, ReeinaLp I. Journ. Linn. Soc. London 24:
454-544. 1893.
VERHOEFF, Kart W. Zool. Jahrb. (Syst.) 71(4/6):
339-388. 1938.
London
JUNE 1959
GRICEKE A NEW SPECIES OF HALOPTILUS
193
ZOOLOGY—A new species of Haloptilus (Copepoda: Calanoida) from equator-
zal and subtropical waters of the east-central Pacific Ocean!. GkorGE D. GRICE,
Woods Hole Oceanographic Institution, Woods Hole, Mass.
eated by Paul L. Illg.)
(Communi-
(Received April 3, 1959)
The new species of Haloptilus described
below was found while examining a series of
plankton samples which had been collected
by the U. S. Fish and Wildlife Service as
part of their oceanographical and marine
biological studies in the Pacific Ocean.
Haloptilus austini, n. sp.
Figs. 1-18
Localities and materials —Latitude 28°00’N.,
longitude 159°03’W. (U.S. Fish and Wildlife
Service Hugh M. Smith Cruise 27, station 67,
February 19, 1955, 100-0 m depth of tow, 1 fe-
male); latitude 00°11’S., longitude 119°58’W.
(Hugh M. Smith Cruise 31, station 94-2, No-
vember 7, 1955, 146-72 m depth of tow, 2 fe-
males). Physical oceanographic and other data
for Cruise 27 are summarized by McGary and
Stroup (1958) and that for Cruise 31 by King,
Austin, and Doty (1957).
Types—All three specimens have been de-
posited in the U.S. National Museum. A female
from Cruise 31 was selected as the holotype
(U.S.N.M. no. 102742). Paratype numbers are
as follows: U.S.N.M. no. 102744 (1 female,
Cruise 31) and U.S.N.M. no. 102743 (1 female,
Cruise 27).
Description—Female (Figs. 1-18). The ceph-
alothorax is much longer than the abdomen, the
ratio of these two body parts being approxi-
mately 8 to 1 (Fig. 1). The head is rounded and
considerably produced anteriorly (Figs. 1 and
2). A convex protrusion is present on each side
at a poimt adjacent to the origin of the second
antennae. The rostral filaments (Figs. 2 and 3)
arise from two small elevations which are situ-
ated a short distance in front of the origin of the
first antennae.
The abdomen (Figs. 4, 5, and 6) consists of
4 segments. The genital segment is longer than
the combined lengths of the succeeding 3 seg-
menis.
*Contribution No. 116 Hawai Marine Labora-
tory, University of Hawai.
* Fellow of the John Simon Guggenheim Memo-
rial Foundation, 1958-1959.
The first antennae of all three specimens are
broken off at sezment 22. When held against the
body, segment 20 reaches to approximately the
end of the caudal furcae. The endopod of the
second antennae (Fig. 7) is a little less than
twice the length of the exopod. The exopod con-
sists of 7 segments. Segment 1 has 2 setae. Seg-
ments 2 through 6 are furnished with a single
seta. There are 4 setae on segment 7. The first
segment of the endopod has 2 setae situated
just beyond the mid-point of this segment. The
external lobe of the second endopodal segment
has 6 large and 1 minute seta. The internal lobe
has 8 setae, 4 of which are notably small.
The exopod of the mandible (Fig. 8) is a little
more than one-half the length of the endopod.
The former apparently consists of 5 segments,
the first 4 of which are furnished with a seta.
The terminal segment has 2 setae. Segment 1 of
the endopod has 2 setae distally, and segment 2
is provided with 8 terminal setae. The gnathal
lobe of the mandible is shown in Fig. 9.
The first maxilla is shown in Fig. 10. The
exopod is elongate and furnished with 11 setae.
Four of the setae on the distal margin are quite
small and slender (Fig. 11). The endopod carries
5 setae, and the second basal segment bears 4
setae. Inner lobes 1, 2 and 3 bear 7, 2 and 4
setae, respectively. The external lobe has 6 large
and 5 small setae.
The second maxilla (Fig. 12) has 6 lobes.
Lobes 1 through 4 and lobe 6 have 3 setae. Lobe
5 has 2 setae. The distal part of this appendage
is furnished with 7 setae.
The maxilliped (Fig. 13) consists of 2 basal
and 5 endopodal segments. The first basal seg-
ment has 2 setae near the proximal end, 3 setae
near the center, and 3 setae near the distal end.
The second basal segment is furnished with 2
setae near the center and 2 setae on the disto-
lateral corner. Endopodal segments 1 and 2 have
4 setae and segments 3 and 4 have 3 setae. The
fifth segment is furnished with 1 seta and 3
bristles.
The first to fourth pairs of swimming feet are
194 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, No. 6
nn SCALES
an WA) __1.0MM._i FG. |
a WY) A
; \! ) Ti
WD -O.OSMM. 4 FIGS. 9,11
=> -OIMM + FIGS. 6,8,10,12-14,18
| (i
[ rc WY, ea OIMM, FIGS. 2-5,7,15-I7
ae y
_ Fires. 1-18.—Haloptilus austint, n. sp., female: 1, Dorsal; 2, forehead, lateral view; 3, forehead, ventral
view; 4, abdomen, dorsal view; 5, abdomen, lateral view; 6, genital segment, ventral view; 7, second
antenna; 8, mandibular palpus; 9, gnathal lobe of mandible; 10, first maxilla; 11, terminal part of exopod
of first maxilla; 12, second maxilla; 13, maxilliped; 14, first foot; 15, second foot; 16, third foot; 17, fourth
foot; 18, fifth foot. Fig. 11 drawn from paratype. All other figures drawn from holotype.
JUNE 1959
shown in Figs. 14 through 17. The first pair
of feet is smaller than the succeeding 3 pairs.
There is 1 seta on the internal margin of basi-
podal segment 1 and 1 seta on the external mar-
gin of basipodal segment 2. Both exopod and
endopod consist of 3 segments. Segments | and
2 of the exopod have 1 long external spine and
1 internal seta. Segment 3 has 2 external spines
and 4 internal and 1 terminal seta. Endopodal
segment 1 has 1, segment 2 has 2, and segment
3 has 5 setae.
The second, third, and fourth pairs of feet
are similar. Basipodal segment 1 has an internal
seta. Basipodal segment 2 of the second and
third feet is naked. This segment of the fourth
feet is furnished with an external seta. Segments
1 and 2 of the exopod have a small external spine
and a single internal seta. The third exopodal
segment has a terminal, finely serrate spine.
There are 3 small external spines and 5 internal
setae on this segment. In the second and fourth
pairs of feet, endopodal segment 1 has 1 seta,
segment 2 has 2 setae, and segment 3 has 7 setae.
In the third pair of feet the numbers of setae
on these respective segments of the endopod are
if 2,.and 8.
The fifth pair (Fig. 18) of feet is smaller than
the preceding 3 pairs. Basipodal segment 1 has
1 internal seta. Basipodal segment 2 is furnished
with 1 seta which exceeds the tip of the terminal
exopodal spine. Exopodal segment 1 has 1 ex-
ternal spine, segment 2 has 1 external and 1 in-
ternal spine, and segment 3 has 2 external and
1 terminal spine. Segment 3 is also furnished with
3 internal setae. Endopodal segments 1, 2, and
3 are provided with 1, 1, and 6 setae, respectively.
Total length of the three specimens is as fol-
lows: 3.33 mm (holotype), 3.16 mm (paratype,
Cruise 31) and 3.06 mm (paratype, Cruise 27).
No male has been found.
Remarks—tThis species resembles H. chier-
GRICE: A NEW SPECIES OF HALOPTILUS
195
chiae (Giesbrecht) but may readily be dis-
tinguished from it by the shape of the head and
the structure of the first maxillae and fifth pair
of feet. The head of H. austini is considerably
more produced anteriorly. In regard to the first
maxilla of H. austini, the second basal segment
has 4 setae, the exopod has 11 setae, and the
endopod has 5 setae. The corresponding parts
of the first maxilla of H. chierchiae, as figured
by Giesbrecht (1892) and Sars (1924), have 5
setae, 8 setae, and 7 setae. The seta on the second
basal segment of the fifth pair of legs of H.
austini exceeds the tip of the terminal exopodal
spine. In H. chierchiae this seta, as figured by
Sars (1924), does not reach the distal end of the
second exopodal segment. This new copepod is
named in honor of Thomas 8. Austin, oceanog-
rapher, Honolulu Biological Laboratory, U. 8.
Fish and Wildlife Service.
Acknowledgments—The Honolulu Biological
Laboratory, U.S. Fish and Wildlife Service, pro-
vided laboratory space during the course of the
investigation. Dr. W. Vervoort has kindly read
the manuscript.
REFERENCES
GIESBRECHT, W. Systematik und Faunistik der
pelagischen Copepoden des Golfes von Neapel
und der angrenzenden Meeresabschnitte.
Fauna und Flora des Golfes von Neapel.
Monogr. 19: 831 pp., 54 pls. 1892.
Kane, J. E., Austin, T. S:, and Dory, M. S. Pre-
liminary report on expedition EASTROPIC.
U.S. Fish and Wildlife Service Spec. Sci. Rep.,
Fisheries 201: 155 pp. 1957.
McGary, J. W., and Stroup, E. D. Oceanographic
observations in the central North Pacific, Sep-
tember 1954-August 1955. U.S. Fish and Wild-
life Service Spec. Sci. Rep., Fisheries 252: 250
pp. 1958.
Sars, G. O. Copépodes particuliérement bathy-
pélagiques provenant des campagnes scien-
tefiques du Prince Albert ler de Monaco. Res.
Camp. Sci. Monaco 69: text (1925), 408 pp.,
atlas (1924), 127 pls. 1924-1925.
rr ———_§_
They will tell you to try to prove you are right; I tell you to try to prove you
are wrong.—LovuIs PASTEUR.
196
JOURNAL OF THE WASHINGTON ACADEMY OF
SCIENCES VOL. 49, NO. 6
James Herbert Hibben
JAMES H. Hispsen, for 20 years chief of the
chemical division of the U. 8. Tariff Commission
and one of the foremost chemical consultants in
the United States, died suddenly on June 15,
1959, at George Washington University Hospital
after a fall at his home.
Dr. Hibben, the son of Thomas E. and Jeanie
Ketcham Hibben, was born in Indianapolis, Ind.,
on May 14, 1897. He attended public schools in
Indianapolis; was a graduate of the University
of Illinois, receiving his B. 8. in 1920 and his
M. 8. in 1922; and of the University of Paris
(1924) with the degree of D. Sc. He has been
a fellow of the International Education Board at
Paris (1924), a National Research Fellow at
Princeton University (1925-27), consultant to
the Bureau of Standards and to various chemical
industries, and a member of the research staff
of the Geophysical Laboratory of the Carnegie
Institution of Washington (1928-1939). During
World War I Dr. Hibben enlisted in the Army as
a private and served with the A.E.F., being dis-
charged in 1919 with the rank of sergeant. Deco-
rations and awards: St. Mihiel and Marne De-
fense Sector.
Dr. Hibben was a member of the Washington
Academy of Science (vice pres.); New York
Academy of Sciences; the Cosmos Club; Ameri-
can Chemical Society; the Chemical Society of
Washington (treas., sec., pres.; Hillebrand Prize
award) ; Sigma Xi and Sigma Chi; and a former
fellow of the American Institute of Chemists.
He was the author of several books and many
papers. One of his best-known works was the
book entitled The Raman effect and its chemical
application (1939). This was one of the first de-
finitive works on this subject. It brought together
all the then known information on a new type
of secondary radiation information by which the
behavior of atoms within the molecules and the
molecules themselves may be determined inde-
pendently of their state of aggregation. Many
applications of this effect have been made, both
to physics and chemistry, and Hibben’s “Raman
Spectra” is still used as the starting point for
much of this work.
At the Tariff Commission Dr. Hibben carried
out many complex and important responsibilities
which, by law or Executive order, the Com-
mission is charged with making. He provided
basic and authoritative information to the Com-
mission, to top ranking officials of Government
agencies, executives of industry, and, when neces-
sary, to members and committees of Congress
and the Office of the President on matters re-
lating to United States tariffs and foreign trade
pertaining to chemicals and chemical products.
During World War II he was chairman or mem-
ber of many intra agency committees and com-
missions. He was directly responsible for the
organization and publication of the Tariff Com-
mission’s annual report on Synthetic organic
chemicals, U.S. production and sales.
Dr. Hibben is survived by his wife, the former
Louise Douglas of Indianapolis; a daughter, Mrs.
Phyllisann Courtis; a granddaughter, Lisa; and
two sisters, in Indianapolis.
— $a ——_—__
FISHER AWARD
Dr. James I. Hoffman, chief, metallurgy division, National Bureau of Standards, is the re-
cipient of the 1959 Fisher Award in Analytical Chemistry. This award is the highest recog-
nition for work in analytical chemistry in the United States and Canada. It consists of
$1,000 and an etching. Presentation of the award was on April 6, 1959, at the meeting of
the Society in Boston.
Officers of the Washington Academy of Sciences
2075 TEs ao Oe eee ee FrRaNK L. CamMpBELL, National Research Council
PAEESTOCTIL-CLCCL. 5.02.2. 0 ese ss LAWRENCE A. Woop, National Bureau of Standards
(Dag EM TPO on Heinz Specut, National Institutes of Health
LU EROUCG 2 n Ao eee ee W. G. BromBacHer, National Bureau of Standards
PUFONTUUSE. 3.0 55.5.2..--- Morris C. Lerxinp, Armed Forces Institute of Pathology
Custodian of Publications............... HaratD A. REHDER, U.S. National Museum
ULE. ooo LS aa CHESTER H. Pace, National Bureau of Standards
WOME Se Cr H. A. Bortruwicx, T. D. Srewart
WEGIUGCRS COLIC]... os ee ec es Bourpon F. Scrispner, Keita C. JOHNSON
LUA OOG 0) LS Puitip H. AsBentson, Howarp S. RappLEYE
Board of Managers....All the above officers plus the vice-presidents representing the
affiliated societies
CHAIRMEN OF COMMITTEES
Standing Committees
LS AYCUI C5 pe FraNK L. CAMPBELL, National Research Council
(URC TIDES yy oh e RautpH B. KeNNaRD, American University
Membership............ LawRENcCE M. KusuHNnerR, National Bureau of Standards
MUGMOPTHOUS 0... 5. cs ec eee Dean B. Cowiz, Carnegie Institution of Washington
Awards for Scientific Achievement....... FraNK A. BIBERSTEIN, Catholic University
Grants-in-aid for Research...... B. D. Van Evpra, George Washington University
Foney and Planning.............. MarGARET Pittman, National Institutes of Health
Encouragement of Science Talent.............. Leo Scuusert, American University
Science Education............ Raymond J. SEEGER, National Science Foundation
Ways and Means.............. RussELL B. StEvENS, George Washington University
Fee eVOlatiONS. .... 2.0.60 5..00 0. eee. JOHN K. Tartor, National Bureau of Standards
Special Committees
UOVL ESS dios Haroutp H. SHeparp, U. S. Department of Agriculture
Wirectory......-........ JaMEs I. HamBieton, U.S. Department of Agriculture (Ret.)
iiprary of Congress.......:............ Joun A. O’Keere, National Aeronautics and
Space Administration
CONTENTS
Page
Astronautics.—The exploration of space. Hucu L. DrypEN....... 165
GxroLoGy.—Sulphide mineralization and associated structure in northern
Union County, Illinois. Grorce A. DESBOROUGH: .............. 172
ENTOMOLOGY.—Seven new galerucid beetles from the West Indies.
Doris’ H., BEA BB: 9 ocs.505 8 oes 45 th da vee oe a er 178
Zootocy.—Muscles of the hip and thigh of the emperor penguin. L. R.
SETEY 0. 0 3 gs SESE 6 RS won ba tie, Be 183
ZooLocy.—Notes on Mecistocephalus in the Americas, with a redescription
of Mecistocephalus guildingii Newport (Chilopoda: Geophilo-
morpha: Mecistocephalidae). R. E. CRABILL, JR................. 188
ZooLtocy.—A new species of Haloptilus (Copepoda: Calanoida) from
equatorial and subtropical waters of the east-central Pacific Ocean.
GEORGE D,. GRICE 6 e403 08 ou eb . Ls Pe ee 193
Notes AND NEWS: |
Tracking camera photographs Vanguard I in orbit.............- 171
American Institute of Chemists Honor Award................. 182
Fisher Award in Analytical Chemistry..............>2. 3a 196
OBITUARY: James Herbert: Hibben. 22)... 3.4. .:. 22... ee 196
Qw23
foLuME 49 July 1959 NUMBER 7
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JOURNAL
OF THE
WASHINGTON ACADEMY OF SCIENCES
VoL. 49 JULY 1959 No. 7
SYMPOSIUM ON THE HISTORY OF AMERICAN GEOLOGY
* * *
Prefactory Statement
The papers published in this issue of the JoURNAL were presented as a part of a Sympo-
sium on the History of American Geology at the Washington meeting of the American Asso-
ciation for the Advancement of Science, December 27 and 28, 1958. The Symposium was
arranged by Edgar W. Owen, of the University of Texas, and was sponsored jointly by
AAAS Section E (Geology and Geography), Section L (History and Philosophy of Science),
and the Geological Society of America.
The Symposium aimed to examine the current state of investigation into the history of
the science and its applications and to stimulate interest in the subject. Of the 224 Ameri-
ean colleges giving majors in geology, only 18 offer courses in the history of geology. The
scarcity of historical publications during the period when the science has undergone phe-
nomenal development of its basic concepts and practical applications indicate the existence
of a fertile field for mature and discriminating research.
The following papers, not made available for inclusion here, were also presented at the
Symposium:
Dirk J. Struik, Massachusetts Institute of Technology: Science in America before 1830. Published
in Science, April 24, 1959.
Kirttey F. Marner, Harvard University: Geology, geologists, and the AAAS. Published in Science,
April 24, 1959.
F. C. MacKnieut, University of Pittsburgh: A university course in history of geology for seniors and
graduates.
Erwin F. Lanes, Portland (Oregon) State College: Dr. John Evans, U.S. geologist to the Oregon and
Washington Territories. Published by American Philosophical Society, 1959.
Herman R. Frits, National Archives: Highlights in the history of the development and use of topographic
maps as a base for delineating geological information by agencies of the Federal Government, 1800-
1879.
SMITHs
INSTITUTIgnN AUG 2 ¢ 195@
eT
LOS JOURNAL OF THE
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 7
Notes on the Earliest Geological Maps of the
United States, 1756-1832
By Joun W. Wetts, Cornell University
Here I propose to consider briefly a still
poorly understood aspect of American geol-
ogy, that of the earliest geological maps.
Published listings and accounts of these
early maps are very few, and all are incom-
plete. The best are Jules Marcou’s Mapoteca
geologica Americana (1884) and Ireland’s
History of the development of geologic maps
(1943). Important also is Leighton’s One
hundred years of New York State geologic
maps (1910). There are a few notices of
early maps in Merrill’s Contributions to the
history of American geology (1906). Stan-
ton’s Evolution of the geologic map of the
United States (1934) mentions only two
maps prior to 18438 (Maclure’s maps of 1809
and 1817). At least 11 maps are known that
show the geology of this country as it then
was understood before 1843.
It is assumed that there is agreement on
the essential characteristics of a geological
map as contrasted with other types of maps.
They are attempts to show symbolically the
distribution of the different kinds of rock at
or near the earth’s surface. Thus, Lewis
Evans’s maps of 1749, 1751, and 1755 can
not be considered as geological, although his
Analysis of 1755 indicates that he could
have produced a most creditable one.
In 1756, however, a genuine geological
map of America appeared in France. This
was In a memoir on the mineralogical com-
parison of Canada and Switzerland by the
ereat French naturalist Jean-Etienne Guet-
tard, who had never been in North America.
This map has generally been dismissed as
merely showing by various symbols the lo-
ealities of some 39 kinds of “earths,” rocks,
minerals, and fossils, but it is truly a geo-
logical map, for like all geological maps it
exhibits a generalization of the distribution
of the rocks. By even modest standards it
is a poor map, and while it is probable, as
White (1951) has suggested, that Lewis
Evans could have produced a better one
based on extensive first-hand knowledge, he
did not, and Guettard’s effort must stand as
the oldest geological map of the continent as
well as one of the oldest of geological maps
in general. It was as good in its time as
many of the later ones, but unlike many of
them it was almost wholly ignored, was
never a source of information, and had not
their wider distribution, especially in the
land to which it referred. An English version
appeared in the Literary Magazine, or Uni-
versal Review in 1757, which was reprinted
later in Fuller’s Naval Chronicle (1760)
(Ireland, 1948, p. 1257).
Guettard’s map developed from a memoir
he read before the Académie Royale des
Sciences in Paris in 1752, a date often
quoted as its publication date. First based
largely on information in Charlevoix’s His-
torie et déscription générale de la Nouvelle
France, it was considerably augmented by
the time it was first published in 1756;
Comte de la Galissionére and M. Gautier,
the latter King’s Physician at Quebec, had
in the meantime sent him specimens and
notes. He may also have gotten some infor-
mation from the Jesuit Relations. Guettard
undertook the compilation from a desire to
see 1f other countries showed the same sys-
tematic arrangement of rocks, minerals, and
fossils that he had already made out for
France, where he recognized three terreins or
bandes. He thought he demonstrated this for
Canada and Switzerland, and marked the
extent of the bandes on his maps. He sug-
gested that they could be traced into Mexico
and into Greenland, and thereby be linked to
their counterparts in England, probably the
earllest attempt at intercontinental correla-
tion. The first of his bandes was the Bande
Sableuse: sands, marls, and sandstones that
extended along the continental shelf from
the Gulf of Mexico to Newfoundland and
the Grand Banks. The Bande Marneuse,
with limestones with no other metal than
iron, is shown along the Gulf and Atlantic
Coastal Plains, including eastern New York,
JuLyY 1959
New England, and eastern Quebec. The
Bande Schisteuse ou Meétallique, with
shales, slates, sandstone, coal, marble, gran-
ite, ete., with many metals and hot springs
but few fossils, covered all the continent
then known westward from the Bande
Marneuse, including the Maritime Prov-
inces. On the map these three Bandes are
labeled by name and the middle one is
shaded.
Guettard regarded fossils as important,
especially is showing the geological sim-
ilarities of one continent with another. It
may be noted is passing that the first figures
of American Paleozoic (Ordovician) fossils
appeared in his memoir.
This first attempt to map the geology of
America and correlate it with Europe, based
upon what were later developed anew as
working principles when Wernerian con-
cepts failed, deserves the premier place in
the history of American geology in ways
other than merely chronological.
Some 40 years later, Constantin-Fran-
cois Chasseboeuf, later Comte de Volney,
traveled extensively for several years in the
United States, and in 1803 he published his
then famous but now almost forgotten T'ab-
leau du climat et du sol des Etats-Unis
d’ Amérique, an attempt to assess the rela-
tion of the soil and climate to the economy,
politics, and viability of the new Republic.
A year later two englished versions ap-
peared in London and Philadelphia which
have been the source of most references to
Volney’s geology. There were several later
editions in French, one in German, and one
in Italian. It is curious that this work
should be so little known today, for it first
brought an idea of American geology widely
to the notice of Europeans.
Volney’s ideas on American geology were
not wholly original. His classification of the
rocks was derived from that of Samuel L.
Mitchill (1798-1802), who in turn owed
much to Lewis Evans. He recognized five
regions, each characterized by certain types
of rocks: (1) a Granitic region, from Long
Island to the mouth of the St. Lawrence and
the Thousand Islands, separated by the
Mohawk Valley from (2) the Catskill Sand-
stone region (Les grés de Katskill) , extend-
ing west of the Hudson Valley as far as the
WELLS: EARLIEST GEOLOGICAL MAPS OF THE U. S&S.
iy)
“Genesee lakes,” (3) a Limestone region in
the “West or Back country,’ (4) marine
sands of the coastal plain, and (5) the [Pied-
mont] region between the fall-line (“sillon
d’isinglass,” a term first used by Lewis
Evans) and the sandstone or granite moun-
tains.
An anonymous review, probably by
Mitchill, of Volney’s book appeared in that
fascinating omnium gatherum of doings in
American science, the Medical Repository,
in 1804-05. It noted that Volney’s terrains
corresponded to Mitchill’s, and that Volney
“possesses a discriminating as well as gen-
eralizing mind” and “beheld with an ob-
serving eye the tracts over which he trav-
elled” (p. 189). The geological eye-opener to
the reviewer, however, was Volney’s geo-
logically colored map: “This is a beautiful
and obvious manner of expressing the prev-
alence of any of the great strata of the
earth, as over-spreading or underlaying [sic]
an extensive tract of country. It is a pity
that map-makers have not more generally
observed it” (p. 411).
This appears to be the first and only pub-
lished reference to the important fact that
Volney’s map, to us misleadingly titled
Carte des Etats-Unis de ’ Amérique-Nord,
pour servir au tableau du climat et du sol
par C. F. Volney (40 X 53 cm, lacking any
geological legend), was geologically colored.
And indeed in very few copies of the original
French edition and in none of the later edi-
tions is the map colored, although all have
geological indications such as the trace of
the outcrop of the “Isinglass Vein” and the
“Limestone Band” in Virginia. The only
colored copy I have yet seen is William
Maclure’s large-paper copy which is now in
the library of the Academy of Natural Sci-
ences of Philadelphia, a small portion of
which is shown in Fig. 1. But that the map
was to be colored has always been obvious
from this note printed on the errata page
(p. 534) of the 1803 edition:
Avis au Lecteur
Dans la grande Carte qui est coloriée, le sol
caleaire est designée par la couleur verte; le
granitique, par la couleur rouge; et le grés, par le
bistre; et dans la petite carte [climatic] l’orange
marque le lit du vent; le verd-d’eau, indique le
courant du Golfe.
voL. 49, NO. 7
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This extraordinary synthesis, the second
geological map of the United States and one
of the very earliest of published colored
geological maps, surely deserves as much
respect as Maclure’s attempt six years later.
A parenthetical note may be added here:
Volney, who had visited Thomas Jeffer-
son several times at Monticello, sent him a
copy of the Tableau. Jefferson acknowl-
edged it early in 1805 in a lengthy letter
(Chinard, 1923, p. 171-175), in the course
of which he sniffed at the geological part:
Of the first [geological] part I am less a judge
than most people... [not] having indulged myself
in geological inquiries, from a belief that the
skin-deep scratches which we can make or find
in the surface of the earth, do not repay our time
with as certain and useful deductions as our pur-
suits in some other branches.
So much for geology from the first of dem-
ocrats!
The year 1809 is, of course, memorable
for the appearance of William Maclure’s
map of the United States. While this is
only the third, it is the earliest well-known
geological map of this country, and Mac-
lure has been overpraised as the “father
of American geology” and the “Wilham
Smith of America.” Many have taken his
memoir and map as the starting point of
our geology. Maclure introduced the Wer-
nerian classification to American geology, a
classification that was to dominate as well
as to hinder its progress for two decades.
Although Maclure certainly made observa-
tions in much of the country east of the
Alleghenies, he was obviously greatly in-
debted—an unacknowledged debt1—to the
published details and observations made
earlier by Evans, Schoepf, Larochefoucauld-
Liancourt, Mitchill, and especially to Vol-
ney as evidenced by the geological coloring
of his map. His classification was hardly
more than Mitchill’s put in Wernerian ter-
minology; and his almost total disregard of
fossil evidence scarcely warrants his being
1Maclure rarely referred to the work of others.
His theory of the origin of the secondary rocks of
the Mississippi basin in a vast inland sea or lake
impounded behind the Appalachians, solemnly ad-
vanced so late as 1823, makes no mention of the
fact that this had been previously elaborated by
Mitchell and Volney, and according to White (1951)
the idea can be traced back to Lewis Evans.
WELLS: EARLIEST GEOLOGICAL MAPS OF THE U. S.
201
placed even near William Smith. But his
map was good, the best of its time consider-
ing the large area covered, especially since
it reputedly represented the results of little
more than a year’s work. In 1809 Mitchill
noted Maclure’s forthcoming map in the
Medical Repository and mentioned that
Maclure had returned to the United States
in 1808 (others say 1807) after 9 or 10 years
in Europe (where he had been an agent of
the United States government), that he had
started working on American geology in the
summer of that year, and that he had al-
ready delineated the principal strata on a
map. It is entirely likely that Maclure al-
ready had his map outlined before he re-
turned to this country and went into the
field. Two bits of evidence suggest this. One
is the sour comment of Gilbert Chinard
(1923, p. 101, footnote) to the effect that
Maclure, who had been in Paris in 1801 on
affairs of the American government, ob-
tained much unacknowledged information
from Volney:
Maclure fit autre chose que de recueillir des
observations pour le compte du gouvernement
américain; il receuillit auprés de Volney les ma-
tériaux pour ses Observations on the geology of
the United States...., et qui lui ont value la rép-
utation d’étre l’auteur de la premiére étude géo-
logique sérieuse sur les Etats-Unis,....
The second is found in the second version
of Maclure’s map, published in the Journal
de Physique in Paris in 1811. This map was
prepared in France from a colored map that
Maclure had sent to J.-C. Delamétherie,
editor of the Journal in 1809 together with
his memoir. As published this map has the
same color scheme as the 1809 map, colors
different from those on the map sent to
Paris. Most remarkable, however, is that
the base map is Volney’s 1803 map, with
re-engraved title but retaining all other de-
tails including Volney’s route trace and con-
tact lines. Either Maclure sent Delamétherie
a copy of Volney’s map with his own geo-
logical coloring, or Delamétherie had Mac-
lure’s data transferred to pulls from the re-
engraved plate of Volney’s map. Also, the
curious caterpillar bands of granitic or pri-
mary color in Canada, found on Volney’s
map but not on Maclure’s 1809 map in the
Transactions of the American Philosophical
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Society, appear on the 1811 version. Were
they added by Delamétherie from Volney’s
map or were they on the map Maclure sent
Delamétherie?
A version of Maclure’s map that has gen-
erally been overlooked, except by Marcou
(1893, p. 6), appears in L. A. F. de Beau-
jour’s Apercu des Etats-Unis ..., published
in Paris in 1814 and englished the same year
by William Walton. This is colored in Wer-
nerian fashion only along the contact lines,
and admittedly is based wholly on Maclure.
Two other versions of the Maclurean
map appeared in the two editions of Parker
Cleaveland’s Elementary treatise on min-
eralogy and geology, 1816 and 1822. They
were no improvement on Maclure and
scarcely warrent mention except for their
wide circulation of Maclure’s work.
In 1817 and 1818 Maclure published re-
vised editions of his memoir and map. The
1817 edition appeared as a book in Phila-
delphia; that of 1818 was published in the
Transactions of the American Philosophical
Society. The geology on both is essentially
the same and these maps are generally listed
as if they were the same. They were printed,
however, on different bases and only the
1818 issue carries a geological legend. Geo-
logical details on both are only a slight im-
provement over the 1809 map. The base
maps for both were very poor for the time.
In a critical notice of Maclure’s memoir and
map of 1817 Rafinesque clearly pointed out
the path to be followed:
... We must especially collect and describe all
the organic remains of our soil, if we ever want to
speculate with the smallest degree of probability
on the formation, respective age, and history of
our earth. (1818, p. 48).
The eleventh and last map (Fig. 2) con-
sidered here is almost completely unknown,
except for listing in two catalogues of the
Library of Congress and mention by Ireland
(1943, p. 1260). It appeared in John How-
ard Hinton’s History and topography of the
United States, published in London in 1832
and also in the same year in an Atlas of the
United States of North America, published
in London and Philadelphia. The atlas was
made up of the maps from Hinton’s History
with condensed text. The geological map
and sections and most of the other maps
WELLS: EARLIEST GEOLOGICAL MAPS OF THE U. 8S.
203
were not included in the several American
editions of this popular work.
This map deserves particular notice, for
it was the first to show anything of the
geology west of the Mississippi Valley. The
gveology east of the Mississippi was obvi-
ously taken from Maclure’s maps, and that
of the region westward to the “Chippe-
wayan Mountains” could only have been
developed from Edwin James’s geological
results of Long’s Expedition to the Rocky
Mountains published in 1822-23. The plate
following the map in both Hinton’s book
and the atlas is a copy of James’s geological
sections across the United States, and the
legend on the map uses James’s geological
nomenclature. Although James did not pub-
lish a geological map, his route map has a
few geological boundaries indicated for the
western section, and might be considered a
geological map of the western part of the
United States. Unfortunately there is no in-
dication in Hinton’s work as to just who,
among the “several literary gentlemen in
America and England” who are mentioned
as having contributed to the book, compiled
the map and accompanying geological text.
Both are skilfully done, evidently by some-
one who had some acquaintance with ge-
ology but who added little or nothing be-
yond information already published.
Eleven years after the appearance of this
eleventh geological map of the United
States saw the publication of James Hall’s
far better and more detailed map of the
Northeastern States (1848). This was fol-
lowed two years later by Lyell’s beautifully
executed map of the eastern half of the
country. With these the pioneer era of
American geological maps came to a close.
REFERENCES
Brausour, L. A. F. Apercu des Etats-Unis, au com-
mencement du XIX*° stécle, depuis 1800
jusqu’au 1810 avec des tables statistiques: 274
pp.; map, 17 tables. Paris, 1814.
CurnarD, G. Volney et lTAmérique, daprés des
documents inédits et sa correspondance avec
Jefferson. Johns Hopkins Stud. in Romance
Lit. and Lang. 1: 206 pp., portr. 1923.
CLEAVELAND, P. An elementary treatise on mineral-
ogy and geology,...: xil, 668 pp., 5 pls., map.
Boston, 1816. Second ed.: 2 vols., xu, pp. 1-480,
481-818, 5 pls., map, Boston, 1822.
Evans, L. An analysis of a general map of the Mid-
204
dle British Colonies in America... : 1v, 32 pp.
Philadelphia, 1755.
Fuuuer, J. The Naval Chronicle: 3 vols. London,
1760.
GueEtTTArD, J.-E. Mémoire dans lequel on compare le
Canada a la Suisse, par rapport a ses minérauz.
Mém. Acad. Roy. Sci. (Paris), Ann. 1752: 189-
220, pl. 7; 323-860, pls. 8-12; Addition, 524-
538. 1756. Also: duodecimo edition, t.2: 281-
328, pl. 7; 480-538, pls. 8-12. Amsterdam, 1761.
Hai, JAMES. Geology of New York. Part 4, com-
prising the survey of the Fourth Geological
District: 683 pp., map, 19 pls., 74 figs. Albany,
1843.
Hinton, J. H. The history and topography of the
United States: edited by John Howard Hinton,
A.M., assisted by several literary gentlemen mn
America and England ..., 2 vols. (Geology,
vol. 2, p. 45-89, geological map opposite p. 45).
London, 1832. See also: An atlas of the United
States of North America, corrected to the pres-
ent period,...: 58 pp., 16 maps, 1 pl. London
(third map is geological). (The atlas sold for 2
guineas plain, 3 guineas colored.)
IRELAND, H. A. History of the development of geo-
logic maps. Bull. Geol. Soc. Amer. 54: 1227-
1280. 1943.
James, E. P. Account of an expedition from Pitts-
burgh to the Rocky Mountains performed wm
the years 1819 and ’20... under ...command
of Major Stephen H. Long, 2 vols. (1823), 503
pp.; 442, xevui pp. Atlas (1822), 2 maps, 8 pls.,
pl. of sects. Philadelphia.
LeicHton, H. One hundred years of New York
State geologic maps, 1809-1909. Rep. Director
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1910.
LYELL, C. Travels in North America: with geologi-
cal observations on the United States, Canada,
and Nova Scotia, 2 vols. London, 1845.
Macuure, W. Observations on the geology of the
Umted States, explanatory of a geological map.
Trans. Amer. Phil. Soc. 6: 411-428, map
(43.5 X 53.5 cm). 1809. .
. Observations sur la géologie des Etats-Unis,
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98-102. 1823.
Marcou, J., AND Marcou, J. B. Mapoteca geologica
Americana, 1762-1881. U. S. Geol. Surv. Bull.
no. 7 (with supplement). 1884.
Marcou, J. Second supplement to Mapoteca geo-
logica Americana. Amer. Geol. 11: 95-99, 1933.
Merritt, G. P. Contributions to the history of
American geology. Rep. U. S. Nat. Mus. for
1904: 189-734, 37 pls., 141 figs. 1906.
Mircuii, S. L. A sketch of the mineralogical his-
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445-452 (1798); 3, no. 4: 325-335 (1800).
_A sketch of the mineralogical history of the
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Agriculture, Arts, and Manufactures (New
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cultural Society on the mineralogy of New-
York. Medical Repository 5: 212-215. 1802.
—. (Review of Volney’s Climat et Sol des
Etats-Unis.) Medical Repository 8: 172-196;
410-420. 1804-05.
. Maclure’s geological enquiries. Medical Re-
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RaFINESQUE, C. 8. (Review of Maclure’s Observa-
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America, 1817.) Amer. Monthly Mag. and Crit.
Rev. 3: 41-44. 1818.
Stanton, T. W. The evolution of the geologic map
of the United States (abstract). Journ. Wash-
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VoLney, C.-F. CHASSEBOEUF, Comte de. J'ableau du
climat et du sol des Etats Unis d’Amérique;
suivt d’eclaircissemens sur la Floride, sur la
colonie francaise au Scioto, sur quelques colo-
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Wuits, G. W. Lewis Evans’ contributions to early
American geology, 1743-1755. Trans. Illinois
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. Lewis Evans (1700-1756) : a scientist m co-
lonial America. Nature 177: 1055-1056. 1956.
JuLty 1959
BACK: EMERGENCE OF GEOLOGY AS A PUBLIC FUNCTION
205
Emergence of Geology as a Public Function, 1800-1879
By Wiuu1AM Back, U. S. Geological Survey
———————
The congressional act of March 3, 1879,
that created the U. S. Geological Survey
marked the acceptance of geology as a sci-
ence having permanent value for and de-
serving permanent support from the Amer-
ican people. Even earlier, organization of
the four western surveys which were con-
solidated by the act of March 3, 1879, dem-
onstrated a change in the public attitude
toward their national government. This
change prompted Henry Adams (1918, p.
312) to refer to the congressional authoriza-
tion for the exploration of the fortieth par-
allel as “almost its first modern act of leg-
islation.” In this paper I attempt to indicate
some of the political and administrative at-
titudes that accounted for a delay of nearly
100 years after the Constitutional Conven-
tion before geology achieved this recogni-
tion. Part of the answer lies, of course, in
the slowness of development of geology it-
self, because the growth and public sup-
port of a science progress concurrently. The
science can not be actively supported until
it develops, nor can it develop until it is
actively supported.
Another reason for the delay was that
during the Jeffersonian period, 1801-29, the
climate of the time was not favorable to the
extension of Federal Government functions
and expenditures. The policy was stated by
Jefferson in his first annual message: “Ag-
riculture, manufactures, commerce, and
navigation, the four pillars of our prosper-
ity, are then most thriving when left most
free to individual enterprise” (White, 1951,
p. 23). It was a period of consolidation and
growth but not of expansion. Jefferson’s and
Adam’s interest in the appreciation of sci-
ence was generally not shared by others
who, through their political positions, could
have facilitated the promotion of scientific
studies.
Nor was the philosophical attitude as to
the proper functions of the Federal Govern-
ment significantly changed during the Jack-
sonian period of 1829-61. President Van
Buren stated the underlying Democratic
philosophy clearly and unequivocally in his
message to Congress in 1837. “All commu-
nities,” he declared, “are apt to look to
eovernment for too much... But this ought
not to be. The framers of our excellent Con-
stitution and the people who approved it
with calm and sagacious deliberation acted
at the time on a sounder principle. They
wisely judged that the less government in-
terferes with private pursuits the better for
the general prosperity ...its real duty...
is...to leave every citizen and every in-
terest to reap under its benign protection
the rewards of virtue, industry, and pru-
dence.”’ Governmental policy followed this
philosophy consistently (White, 1954, p. 6).
While the National Government was used
by its citizens hardly more in 1860 than it
was in 1800, the States and their subdivi-
sions were actively pushing into new fields,
unhampered by the constitutional doubts of
statesmen on the national scene, although
restrained in some measure by the dominant
philosophy of laissez faire (White, 1954,
Preface).
The movement for public education, in-
spired and led by Horace Mann, reflected
the desire for more informed public opinion.
A convention of organized workingmen
meeting in Boston in 1833 resolved that no
person would receive the votes of its mem-
bers “but such as are known to be openly
and decidedly favorable to a system of
general education, by means of manual
labor schools, supported at public expense,
and open alike to the children of the poor
as well as to the rich...” This resolution
was symptomatic of the future, as Amer-
icans came to realize that government could
make positive, constructive contributions to
the needs of the people without necessarily
creating either a threat to liberty or a drain
on the Nation’s resources (White, 1954, p.
10). Coming as it did in 1833, this resolu-
206
tion may be a manifestation of the same
intellectual forces, the same general awak-
ening of the desire for knowledge, that
prompted the organization of the State geo-
logical surveys—l17 of them during the
period 1830-40 alone (Fig. 1).
As to more positive contributions by the
Federal Government, however, it 1s doubt-
ful that much could have been accomplished
even if the prevailing attitude had been
more favorable. The years of the Jackso-
nians, from 1829 to 1861, were years of
almost uninterrupted excitement, tension,
crisis, and apprehension. Nullification in
South Carolina, the resolution censuring
Jackson and its final erasure from the Sen-
ate Journal, the panic of 1837, the contro-
versy with Great Britain over Oregon, the
war with Mexico, the problem of slavery in
the newly acquired territories leading to the
Compromise of 1850, the moral and admin-
istrative crises precipitated by the Fugitive
Slave Act, the panic of 1857, John Brown’s
raid—all these events gave neither the pol-
iticians nor the people any peace (White,
1954, p. 18). Congress and the administra-
tors had little time for expanding the fune-
tion of science In government.
Another reason, as we have said, is that
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
geology was a young science which, at least
so far as the Federal Government was con-
cerned, had not yet proved its practical
value and was considered theoretical and
academic. The general intellectual environ-
ment in the United States was not conducive
to active participation in theoretical sci-
ences. We have the clearest description of
the attitude of the times in Tocqueville’s
perceptive writings where he states (1900,
vol. 2, p. 43), “In America the purely prac-
tical part of science is admirably under-
stood, and careful attention is paid to the
theoretical portion which is immediately
requisite to application. On this head the
Americans always display a clear, free,
original, and inventive power of mind. But
hardly anyone in the United States devotes
himself to the essentially theoretical and
abstract portion of human knowledge.”
Thus we see that the political and ad-
ministrative philosophy was not compatible
with support of geology on the Federal level,
and that whatever was to be done with
public support necessarily became the re-
sponsibility of the State governments. The
defeat of John Quincy Adams in 1828
marked the climax of his effort to use na-
tional power and resources for what he con-
GRAPH SHOWING DATE
OF ADMISSION OF EACH
STATE AND PERIGBS
OF AC TIVE Sai
GEOLOGICAL SURV Es
TO=IVOO
JuLy 1959
ceived to be national purposes. I think this
may have brought about the general re-
alization that the States would have to as-
sume greater responsibilities, and it is par-
ticularly significant to geology in that it
happened immediately before the first State
surveys were formed in the 1830's.
This is not to imply that the Federal
Government was completely inactive in ge-
ologic exploration but only that the States
were taking the lead and dominating that
part of geology supported directly by public
funds. As we know, we had the expeditions
of Schoolcraft, Lewis and Clark, Pike, Long,
Wilkes, and Frémont; the Pacific Railway
Survey; and others during the period 1803
to 1860. Geologic knowledge was gained
from all these expeditions, but geology was
not their primary purpose. The authoriza-
tions of the surveys of Featherstonhaugh in
1834-35 and of David Dale Owen in 1839
were the first Federal attempts to support
geologic investigations.
It is interesting to speculate on the pos-
sible causes of the flourishing of the State
surveys in the 1830’s (Fig. 1). Of the 13
original States only two did not start a sur-
vey during the decade 1830-40; one of
these, North Carolina, had had a token sur-
vey a few years earlier, and the remaining
State, South Carolina, began its survey only
two years after the end of this decade. (It
is also of interest to note that the Geological
Survey of Great Britain was organized in
1835.) Were these States only imitating
Massachusetts and North Carolina, the
early birds, or had geology truly become a
science, as Smallwood suggests? He states
(1941, p. 441), “Geology, the third large
department of natural history, stands out in
rather marked contrast to botany and zo-
ology. During the period designated as ‘the
passing of the naturalist’ (1830-40), in
which the naturalist, after acquiring great
influence, rather rapidly declined, geology
became very prominent in the making of
State surveys. The naturalists’ emphasis
was being replaced by the adoption of sci-
entific criteria that any geologist could ap-
ply.”
I think we cannot completely disregard
the role of chance in the nearly simultane-
ous beginning of the surveys. That is to say,
BACK: EMERGENCE OF GEOLOGY AS A PUBLIC FUNCTION
207
there was enough general activity in geol-
ogy to permit this sudden development. The
establishment of the American Journal of
Science in 1818 and of the American Geo-
logical Society in 1819, the publication of
Eaton’s Index to the Geology of the North-
ern States in 1818, and the organization of
the Geological Society of Pennsylvania in
1832 were significant items in bringing ge-
ology to the forefront.
Nor do I think we can overlook the role
of individual personalities as contributing
factors. We see the rise of strong leaders
such as Edward Hitchcock, who was re-
sponsible for the conception and establish-
ment of the first State geological survey,
that of Massachusetts; the Rogers brothers,
responsible for three of the early surveys;
W. W. Mather, who made the Ohio and
Kentucky surveys; C. T. Jackson, also re-
sponsible for three State surveys; David
Dale Owen, who started the Indiana sur-
vey; and Amos Eaton, whose lectures to the
New York State Legislature no doubt were
the beginning of that State’s survey.
Regardless of which of the several possi-
bilities was dominant, we see from Fig. 1
that the early State surveys were short-
lived, not only those that began during the
early period but even those that began later.
The short life of these surveys no doubt
could be explained by many reasons, such
as adverse economic conditions, internal po-
litical changes, or shortage of competent
personnel. But I think none of these come as
close to the truth as that suggested by the
Federal Survey’s Director Mendenhall in
describing the tremendous task confronting
the men who undertook the first survey of
Pennsylvania: “An adequate study of
45,000 square miles of extremely varied and
complex geology and the revelation of the
wide variety of mineral resources that it
contains, would tax the capacity of a large
modern staff, trained according to modern
standards, and equipped with complete
modern maps. It couldn’t be done promptly,
of course, a century ago. Base maps were
lacking; trained geologists were very few.
Principles had to be established and meth-
ods devised as the work proceeded. The
magnitude of the task was tremendous and
dawned only slowly on the workers. Results
208
came in slowly so that the State lost pa-
tience and in six years appropriations
ceased”? (Mendenhall, 1936, p. 17).
It was no doubt this same impatience
that caused nearly continuous difficulty in
establishing permanent State surveys. Toc-
queville apparently recognized this char-
acteristic of our society and in effect pre-
dicted the difficulty that activities such as
State geological surveys would face in gain-
ing general acceptance. He comments, “The
man of action is frequently obliged to con-
tent himself with the best he can get, be-
cause he would never accomplish his pur-
pose if he chose to carry every detail to
perfection... The world is not led by long
or learned demonstrations” (Tocqueville,
vol. 2, p. 44).
Therefore, when geology did not yield
results immediately capable of application
to current wishes, the “men of action” saw
no need for further support and the surveys
ceased. As the reports were later published
and use could be made of the geologic
knowledge from the surveys, most of the
States again organized surveys, the later
ones generally being longer lived than the
earlier ones. The State surveys continued to
dominate the public activity in geology un-
til the Civil War.
Although three States started surveys
during the Civil War, this generally was a
period of disruption in geology, lost records,
and diversion of personnel. After the war we
see a great increase in geologic interest and
activity by the Federal Government. Merrill
states, “The period of the Civil War had
brought to light a considerable number of
men...of great physical and moral cour-
age. It was but natural, therefore, particu-
larly when the necessity for military routes
in the west and public land questions were
taken into consideration, that such should
turn their attention toward western explo-
ration. Further, the surveys made in 1850’s,
in connection with routes for the Pacific
railroads, and the work done by Evans,
Hayden, and Meek in the Bad Lands of the
Missouri had whetted the desires of numer-
ous investigators. Willing workers were
abundant and Congress not difficult to per-
suade into granting the necessary funds”
(Merrill, 1924, p. 500).
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 7
This change in the attitude of Congress
marks a significant step in the emergence of
geology as a public function. Only a few
years before, in 1852, Congress specified
that no new geological surveys be under-
taken unless authorized by law. I think this
change in attitude may be attributed at
least in part to a gradual shift in the point
of initiation of new functions in the Govern-
ment. In the early periods we see the Presi-
dent taking a very active role in developing
new functions. For example, Thomas Jeffer-
son wrote detailed instructions for Lewis
and Clark to follow on their expedition. A
few decades later Congress is perplexed with
the problem of doing something constructive
with Smithson’s estate. The act creating
the Smithsonian Institution was one of the
earliest modern acts of Congress to take a
positive and constructive attitude toward
a new function. Still later, as the tasks and
responsibilities of the Government in-
creased, I believe we can see the initiation
of new functions taking place in the newly
organized and expanding departments. Here
the debates are not among the members of
Congress as much as between the Congress
and the administrators. Therefore, as the
potential leaders of western surveys sought
Congressional appropriations, the logic of
their arguments added force to govern-
mental processes and facilitated the begin-
ning of new functions. As these western sur-
veys gained in strength and popularity it
was only a step in the direction of more eco-
nomical operation to create the U. 8. Geo-
logical Survey by combining their purposes
and personnel.
In summary, I have attempted to outline
the political and administrative philosophy
from about 1800 to 1879 as it bears on the
emergence of geology as a public function.
I have ignored almost entirely the force of
geology itself. Nor have I considered the
very significant contributions made by the
land-grant colleges and other publicly sup-
ported educational institutions. Other items
I have ignored, in deference to other papers
in this symposium, are, for example, the
role of the Smithsonian Institution, the ac-
tivities of the AAAS, the effect of Darwinian
concepts, the popularization of geology, and
the development and use of topographic
Juty 1959
maps. Indeed, every contribution to the ad-
vancement of geology must be considered a
part of the story of the emergence of geol-
ogy as a public function.
ACKNOWLEDGMENTS
This paper was developed from several
term reports prepared for courses in public
administration at Harvard University. The
stimulation and guidance of Prof. John M.
Gaus in the study of the historic connection
of science and government and the helpful
suggestions of C. L. McGuinness of the
United States Geological Survey are grate-
fully acknowledged.
BACK: EMERGENCE OF GEOLOGY AS A PUBLIC FUNCTION
209
REFERENCES
ApamMs, Henry. The education of Henry Adams:
517 pp. Boston, Houghton Mifflin Co., 1918.
MeENDENHALL, W. C. Establishment of Pennsylvania
survey—an outstanding event in development
of science in U. S. Pennsylvania Dept. Internal
Affairs Monthly Bull. 2(1): 17-18. 1936.
Merri, G. P. The first one hundred years of Amer-
ican geology. Yale University Press. 1924.
SmaLLwoop, W. M. Natural history and the Amer-
wcan mind: 445 pp. New York, Columbia Uni-
versity Press, 1941.
TocQUEVILLE, ALEXIS DE. Democracy in America 1:
442 pp.; 2: 399 pp. New York, Colonial Press,
1900.
Wuite, L. D. The Jeffersonians: 572 pp. New York,
Maemillan Co., 1951.
. The Jacksonians: 593 pp. New York, Mac-
millan Co., 1954.
The United States Geological Survey and the Advancement
of Geology in the Public Service
By Tuomas B. Nouan, Director, U. S. Geological Survey
The Geological Survey will be 80 years
old on March 3, 1959. It came into being that
date in 1879, when President Hayes signed
an appropriation bill that contained an item
giving the Director of the Geological Survey
the responsibility of administering a new
organization, which was directed to classify
the public lands and to examine the “geo-
logical structure, mineral resources, and
products of the national domain.”
This rather oblique method of creating
the new organization was perhaps an appro-
priate conclusion to the struggle for support
—especially financial support—by four
predecessor exploratory surveys which were
by this action combined into one. The union
was accomplished largely through the ac-
ceptance by the Congress of the major rec-
ommendations of a committee set up by the
National Academy of Sciences at its request.
The infant bureau thus, at its inception, en-
joyed the sponsorship of the leading scien-
tific group of the country. It has been for-
tunate since that time to have had continued
assistance in the selection of its directors,
through recommendations by this same
Academy.
The four predecessor surveys were each
established in the years following the Civil
War. They were to aid in developing the
West, through the acquisition of additional
knowledge of its geography and of its re-
sources. Their objectives, and those of the
young Geological Survey, were primarily
the practical ones of exploring the geo-
graphic frontier, in part to learn about new
or better routes by which it might be tra-
versed; in part to discover and appraise the
natural wealth of the new territory. Empha-
sis was, of course, laid upon the mineral
wealth, but the soils, the water and forest
resources, and even the scenic features had
to come under scrutiny if the objectives were
to be attained.
To achieve success in this sort of an ex-
ploration of a physical frontier, it is now
apparent that it was necessary to develop
both new concepts and new techniques. It
was fortunate that the members of the early
surveys and of the new Geological Survey
210
had the capacity to do this; they were able,
in a sense, to use the results of their explora-
tion of intellectual frontiers in the attain-
ment of their practical objective of delimit-
ing the geographic one.
The record of the Survey in subsequent
years seems to me to illustrate a continuing
ability to utilize the products of intellectual
curlosity in the solution of the practical
problems that arise in our economy. The in-
dustrialization of the country, following the
development of the West; participation in
two World Wars; and currently the need to
resolve difficult and perplexing problems in
water and mineral supply have each been
accompanied by reorientations in the re-
search programs of the Survey, with con-
comitant applications of research results to
the problems themselves.
I believe this ability to recognize, or an-
ticipate, national needs and to use research
results in their solution has been the most
significant contribution by the Survey to
the “advancement of geology in the public
service.”
With this preface, I should like to review
very briefly the history and activities of the
Geological Survey since its founding. Clar-
ence King was the first director; he served
for only two years, but in that brief period
a staff of outstanding scientists was gath-
ered, several geologic studies were begun, a
chemical laboratory was set up in Denver,
topographic surveys were begun in Nevada,
the Survey’s first geophysical work was
started as part of the study of the Comstock
Lode, and, in cooperation with the Census
Bureau, the collection of statistics on yearly
mineral production in the region west of the
100th meridian was begun. Thus, from the
very beginning both practical and theoreti-
eal investigations, or applied science and
basic research, were part of the Survey pro-
eram.
Establishment of the Survey did not put
an end to the controversy over the function
of a Government bureau engaged in scien-
tifie activities. John Wesley Powell, who
had been instrumental in the founding of
the Survey and who had succeeded King as
director, had as his goal the establishment
of the Survey as a great scientific and tech-
nical bureau with emphasis on research in
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, NO. 7
all its functions. Shortly after he assumed
office, paleontological laboratories were es-
tablished, a physical laboratory was set up
for research on the effect of temperature,
pressure, and related phenomena on rocks,
and studies of metamorphism and the para-
genesis of minerals were begun. In 1882 con-
gressional authorization was given “to pre-
pare a geologic map of the United States,”
thus leaving no doubt as to the national ex-
tent of the Survey’s work; and to procure
statistics in relation to mines and mining,
thus placing on a permanent basis work that
had been undertaken in cooperation with
the Tenth Census. And the Survey was
making a topographic map of the United
States because, as Powell pointed out, sound
geologic research is based on geography.
By 1884 this vigorous prosecution of work
and rapid expansion of the Survey had pro-
voked considerable discussion in both public
and private circles, and a Congressional
committee undertook an investigation of the
several scientific bureaus to attain greater
efficiency and economy in their administra-
tion. In his appearances before this com-
mittee Powell established a philosophy
which has become the guiding principle of
the Survey in later years that a Government
research agency should promote the wel-
fare of the people by investigations in those
fields most_vitally affecting the great in-
dustries in which people engage, should have
the broadest possible territorial base, and its
work should not be undertaken in those
fields where private enterprise may be re-
lied on for good and exhaustive work. The
majority report was favorable, and Con-
gress, by specific appropriation, endorsed
the chemical, physical, and paleontologic
work of the Survey.
In addition to its regular scientific work,
three major problems in conservation oc-
cupied the Survey during the first third of
its history. In 1888 Congress authorized the
Survey to undertake a study of the arid re-
gions where irrigation Was necessary to agri-
culture. In 1894 and in subsequent years
the Survey received appropriations for
gaging streams and determining the water
supply of the United States. When the Rec-
lamation Act was passed in 1902, its ad-
ministration was assigned to the Survey
Juty 1959
until the work changed from planning to
construction. In 1907 the Reclamation Serv-
ice became an independent bureau and the
chief of the Geological Survey’s Hydro-
graphic Branch became its first director.
In the course of its geologic and topo-
graphic surveys, the Survey had gathered
data related to forests, and in 1891 Congress
authorized creation of forest reserves on the
public lands. A comprehensive study of for-
est reserves was begun in 1897, and land
classification maps were prepared to form
the basis for regulations governing the re-
serves. In 1905 the Forest Service was es-
tablished in the Department of Agriculture
and took over the further examination and
classification of forest reserves as well as
the administration of regulations.
Mining geology and mining technology
had been an important part of the Survey’s
work from the start. Beginning in 1888, an
annual volume of statistics on the mineral
resources had been prepared. Public in-
terest in a separate division of mines to
serve the needs of the mining industry de-
veloped fairly early. But 1t was some years
later (1908) when the Survey was author-
ized to undertake an investigation of mine
safety. These activities were somewhat out-
side the normal work of the Survey and were
later transferred to the Bureau of Mines,
which was established by congressional act
of May 16, 1910, along with the Technologic
Branch of the Survey, whose chief became
the first director of the Bureau.
Meanwhile the regular geologic work of
the Survey had progressed. Investigations
had been undertaken in Alaska, Hawaii,
Puerto Rico, and Cuba. Nearly a third of
the country had been mapped topographi-
eally, at least in reconnaissance, geologic
folios had been published, and some 400 re-
ports had been published on such topics as
Lake Bonneville, the Paleozoic fishes of
North America, the glacial gravels of Maine,
borax deposits in Death Valley, and tin in
Alaska, on the chemical composition of ig-
neous rocks, the form of sea level, earth-
quakes in California, and the compressibil-
ity of liquids. Its investigation in the
Leadville district had shown the practical
importance of geologic studies in mining,
those in the Lake Superior region had an
NOLAN: UNITED STATES GEOLOGICAL
SURVEY 2A
effect on discovery and development, and
studies in the Appalachian coal field were
pointing the way toward a scientific basis
for development of natural fuel resources.
The middle third of the Survey’s history
is nearly coincident with the directorship of
George Otis Smith. It was Smith’s idea that
a scientific bureau should collect and ar-
range facts upon which the Nation could
base its plans for future development and
should make its science useful to the public.
Basic research was encouraged but there
was increased emphasis on and a widening
of the Survey’s usefulness in applied science.
During his first decade in office the gen-
eral public was in closer touch with the Sur-
vey and made more use of its scientific re-
sults than ever before. In one year it was
reported that approximately 50,000 letters
of inquiry were handled in the different sci-
entific branches. In a special publication,
Bulletin 599, entitled Our mineral reserves,
the country’s ability to meet emergency de-
mand was summarized and the Survey of-
fered to serve as an agent in bringing con-
sumer and producer into touch with each
other. In recognition of its responsibility to
make its work intelligible to the layman,
nontechnical descriptions of the physical
features and their origin were printed on
the backs of several topographic maps, and
guides covering points of scenic or unusual
geologic interest in some of the national
parks and along several transcontinental
routes were prepared.
Efforts to assist in discovering and de-
veloping new oil reserves were intensified,
field studies seeking a better understanding
of the principles and conditions governing
the origin, movement, and segregation of oil
and gas were begun, and field investigations
of the oil shale reserves were also under way.
After Germany gained a monopoly of the
potash supply, Congress directed the Sur-
vey to explore for domestic deposits, and
intensive and ultimately successful explo-
ration was carried out in the western States.
Another notable contribution to geology in
its broadest sense was the study by G. K.
Gilbert of hydraulic mining debris in the
Sierra Nevada which involved mining, agri-
culture, and navigation problems as well as
geology.
212
With the advent of the first World War,
scientific knowledge and methods were ap-
plied to the technology of weapons, and the
need for basic raw materials brought to the
Survey an important role in the war effort.
Scientific data already available in the
Survey formed the basis of special investiga-
tions of certain mineral deposits and an in-
creased exploration for new deposits. The
strategic minerals concept was first devel-
oped at this time, and a beginning was made
in military geology as information on po-
tential mineral and water resources of other
countries was gathered.
The war had shown the need for increased
development of power sources. During the
war Survey hydraulic engineers had made
a countrywide survey of the power situation
to determine where water power could be
substituted for steam-generated power.
Aiter the war a survey of sources of energy
in the Washington-Boston area, the so-
called Superpower Survey, was undertaken
by congressional authorization. The Federal
Coal Commission was set up in 1922 and
took the director away from the Survey for
a year; in 1924 he was appointed to a Fed-
eral Oil Conservation Board and to a naval
oil supply commission; in 1925 he was dele-
gate to the World Power Conference, and
in 1930 the newly established Federal Power
Commission took him permanently from
the Survey.
The last third of the Survey’s history has
been one of relatively rapid and great
changes and an even more intimate involve-
ment of the Survey with the national de-
velopment. During the depression years of
the early 30’s, appropriations were so re-
duced that many were forced to leave the
Survey and many projects were suspended.
Through allocation of funds from the Public
Works Administration and other agencies
some of the Survey programs, notably topo-
graphic mapping and investigations of min-
eral resources in the Southeastern States,
were continued, and in 1936 increased ap-
propriations made possible more normal op-
erations.
In 1939, with the threat of approaching
war, Congress authorized the beginning of
strategic mineral investigations, and when
JOURNAL OF THE WASHINGTON ACADEMY
OF SCIENCES VOL. 49, NO. 7
the war started a high proportion of Survey
men were shifted to this work. A military
geology group was formed immediately after
the United States entered the war and grew
rapidly as its work became more and more
useful to the armed services. Appraisals of
characteristics of enemy terrain were made
for use in strategic planning, and Survey
scientists went into the war theaters to aid
in planning tactical operations. An investi-
gation of fissionable raw materials begun at
the request of the Manhattan Engineer Dis-
trict was expanded after the war on behalf
of the Atomic Energy Commission to a ma-
jor program that involved both exploration
and basic research in the geology of fission-
able materials.
In the post-war years, also, engineering
geologic investigations have been under-
taken in support of the program of the De-
partment of the Interior for river-basin
development, and geologic mapping of fast-
growing industrial areas has provided data
needed in many types of engineering con-
struction in expanding urban areas. Re-
search has also been undertaken on geologic
processes, such as the development of land-
slides, that affect the safety of engineering
structures.
In the Survey’s traditional fields of geo-
logic mapping and appraisal of the mineral
resources of the Nation there has been a
constant awareness of the need for continual
development of new exploratory tools and
improvement of techniques as the expanding
economy calls for ever-increasing amounts
of raw materials and advancing technology
creates demands for new materials. Geo-
chemical prospecting methods have been de-
veloped to aid in the discovery of mineral
deposits. New, rapid, sensitive, and imex-
pensive analytical methods suitable for use
in the field have been developed, and geo-
botanical and hydrogeochemical techniques
have been investigated. Geophysics has
taken to the air, and magnetic and radio-
activity surveys have been made of many
thousands of square miles. Geologic map-
ping techniques are being improved notably
by the development of photogeology to ob-
tain greater coverage more rapidly and at
less cost.
JuLty 1959
More than ever before we need to de-
velop an understanding of the processes by
which mineral deposits are formed in order
to develop the scientific techniques required
to guide the search for new sources. As part
oi a long-range minerals program, more and
more data are being sought on the physical
properties of rocks, on the nature of the ore-
forming fluids, on the physical, chemical,
and biochemical changes that take place in
weathering.
Geologic facts and techniques are being
used in an ever-increasing variety of prob-
lems. Airborne radioactivity surveys de-
veloped to aid in exploration for new sources
of uranium are being adapted to monitoring
the effects of nuclear explosions on atmos-
pheric radioactivity, and both geophysical
and geochemical methods are being used in
a study of the relation of environmental
factors to the development of cancer, and
measurements of the temperature in frozen
ground turn out to be significant in the de-
sign of buildings, roads, and other construc-
tion and the location of water supplies in
our forty-ninth State.
This recital of activities and policies since
1879 is in part abridged from the excellent
historical summary prepared by John and
Mary Rabbitt on the occasion of the
seventy-fifth anniversary of the Geological
Survey; it was published in Science in 1954.
The chronological recital alone, I think, re-
cords the very considerable contributions
that the organization has made to the “‘ad-
vancement of geology in the public service.”
I should like, though, to further summarize
by pointing out four broad categories in
which these activities have been especially
productive.
One might be categorized as the develop-
ment or refinement of new fields or new
principles. I believe that it is fair to say, for
example, that mining geology as it is prac-
ticed today is very largely the product of
Survey work. This began with Clarence
King who, in addition to his own activities,
sponsored the work of Becker in the Com-
stock and S. F. Emmons in Leadville, con-
tinued through the widespread activities and
generalizations of Lindgren and the timely
analysis of the newly developed porphyry
NOLAN: UNITED STATES GEOLOGICAL SURVEY
213
copper deposits by Spencer and Ransome,
and is operative to the present day through
the field development of airborne and geo-
chemical exploration methods, and the lab-
oratory researches of the Geochemistry and
Petrology Branch. An even stronger case
might be made for the new field of ground-
water hydrology with the early work of
Mendenhall in southern California, the long
period of development under Meinzer, and
the more recent investigations by Sayre,
Theis, and others.
Contributions to geologic thinking and to
the development of principles are basically
made by individuals, rather than organiza-
tions, but the latter can provide an environ-
ment in which individual contributions may
flower. I believe this has been true in the
Geological Survey; certainly our basic con-
cepts in sedimentation and stream dynamics
have been continuously influenced by the
work of Gilbert, Rubey, and, most recently,
by Leopold. Similarly, glacial geology has
been influenced by Survey authors from T.
C. Chamberlain through Alden and Mat-
thes; structure, from Dutton to Gilluly,
petrology from Hague through Cross to E.
S. Larsen, Jr. The list could be greatly ex-
panded.
Less glamorous, perhaps, but certainly of
inestimable value to the profession have
been the numerous new or improved tools
or techniques that have resulted from the
Survey’s work. The Bibliographies of North
American geology, Lexicon of geologic
names, and Data of geochemistry are ex-
amples of published contributions that are
invaluable to the practicing geologist, while
a whole series of proposals or developments
from the standardization of cartographic
methods for geologic maps to the devising of
the numerous instruments and methods of
photogeology have made it possible for ge-
ologists to do their field work and write their
reports more accurately and more effec-
tively.
The third category has been alluded to in
previous paragraphs. It might be called the
recognition, and sponsoring, of new and de-
sirable areas of endeavor in fields related
to geology and earth science. The establish-
ment of such Federal agencies as the Forest
214
Service, Bureau of Reclamation, Bureau of
Mines, and the Grazing Service (now a part
of the Bureau of Land Management) and
the non-Federal Geophysical Laboratory,
resulted directly from activities initiated
in the Geological Survey. I suppose some
may feel that the creation of additional
Federal agencies is a dubious contribution,
but I believe most thoughtful observers will
concur in the belief that the part played by
the Survey in the creation of professional
agencies in the resource management field
with the high standards that characterized
the parent agency has been a significant
contribution to the Nation’s wellbeing.
Finally, I feel that the Survey has played
a large and beneficial role in education in
this country that is in addition to the con-
tributions to geologic thinking that I have
mentioned. In part this has been the result
of its personnel policies and in part of its
extensive publication program. In regard to
the first, the bureau has from the beginning
encouraged an interchange of personnel be-
tween its staff and that of university facul-
ties in geology as well as in the summer
employment, as field assistants, of advanced
students in geology. This policy has led to
the widespread use of the so-called “w.
a.e.” appointments; these are operative only
when the individual, usually a university
teacher, is actually employed—commonly
during the summer field seasons. Among
the earliest appointments recorded in the
Survey archives are those of T. C. Chamber-
lain (who received the magnificent sum of
“£10 per diem, paid only when actually
employed”), J. P. Iddings, O. C. Marsh, and
a number of others. Utilization of men such
as these not only benefited the Survey
through the individual skills thus made
available but also inevitably contributed
to the universities and to geologic education,
by making available promptly as instruc-
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
tional material the results of field and labo-
ratory work of not only the w. a. e. teachers
but of the Survey staff with whom they were
in contact. This interchange of personnel
and the widespread utilization of ‘‘w. a. e.”
appointments is still a major element in
Survey policy.
Possibly even greater assistance to geo-
logic education has been provided by the
several series of publications which record
the results of the Survey’s work. I suspect
that directly, through the use of such clas-
sics as Gilbert’s Lake Bonneville mono-
graph, and indirectly, through the contribu-
tions of Survey material in textbooks and
lectures, almost all of us in the geologic
profession are indebted, more than we rec-
ognize, to this long series of reports on the
Survey’s field and laboratory work.
It is apparent that I believe the Geologi-
cal Survey has contributed significantly to
both the advancement of geology and the
public service. To me the real and lasting
contribution made by the Survey, and by
the other Federal scientific agencies, is the
part they have played in securing general
recognition, throughout the country, not
only that scientific and professional work of
the highest quality 1s possible in the Federal
Government, but that it has been one of the
essential contributions to the development
of this Nation to the international power
that it is today.
I observed earlier in this paper that a
transition from an exploration of a geo-
graphic frontier to an intellectual one char-
acterized the early work of the Geological
Survey. In recent months, some of our more
inquisitive younger members have proposed
various studies of the geography of the
individual components of “outer space.”
Perhaps we are about to see the beginning of
a new cycle in the history of the Geological
Survey in the public service.
JuLY 1959
OEHSER: SMITHSONIAN IN EARLY AMERICAN GEOLOGY
The Role of the Smithsonian Institution in
Early American Geology
By Pauu H. Oruser, Smithsonian Institution
The concern of the Smithsonian Institu-
tion with the science of geology began very
early in its history. It was, indeed, inherent
in its very foundation; for James Smithson,
the Englishman who left his fortune to the
United States of America ‘“‘to found at
Washington an Institution for the increase
and diffusion of knowledge among men’’—
this disappointed, lonely man who had
never been to America but somehow caught
the vision of the potential of such an es-
tablishment on American soil—was himself
something of a geologist. While still a young
Oxford student he geologized through the
British Isles and thereafter assembled a
large collection of gems and minerals and
made noteworthy studies of them. Today,
on entering the beautiful new Hall of Gems
and Minerals at the Smithsonian, one can
read this label accompanying a colorful
specimen of smithsonite (zinc carbonate):
“This mineral was named [by Beudant]
in honor of its discoverer, James Smithson,
distinguished English chemist and mineral-
ogist and founder of the Smithsonian In-
stitution. Despite the primitive chemical
apparatus and crude reagents which Smith-
son had to use, he was able to achieve an-
alytical results of the most creditable char-
acter and to enlarge our knowledge of many
mineral species. Before his time zine carbo-
nate and zinc silicate were confused as a
single mineral species under the name cala-
mine, but his researchers distinguished the
two minerals which are now known as
smithsonite and hemimorphite.”’
When the Smithsonian Institution was
finally established by act of Congress in
1846, on the basis of a broad interpretation
of the provisions of Smithson’s will, geology
and mineralogy were included among the
Institution’s concerns. In fact, James Smith-
son’s personal collection of minerals came as
a nucleus of the great national collections
in this field that have accumulated through
the years.
The first Secretary of the Smithsonian
was Prof. Joseph Henry. He was a “natural
philosopher” and made his principal con-
tributions to science in the field of electric-
ity; but he began as a geologist in his
native New York State in the days of Amos
Eaton under whose influence he came.
When, in 1820, Eaton was commissioned to
conduct an agricultural and geological sur-
vey of Albany County, N. Y., he chose the
23-year-old Joseph Henry as an assistant.
Six years later, Henry received an appoint-
ment as engineer on a survey for an east-
west road through New York State, an as-
signment in which he notably acquitted
himself. It is said that “his labors in this
work were exceedingly arduous and respon-
sible. They extended far into the winter, and
the operations were carried on in some in-
stances amid deep snows in primeval for-
ests.’ He was offered the job of directing the
construction of a canal in Ohio, but the va-
cant chair of mathematics at the Albany
Academy beckoned, and this budding geolo-
gist-engineer abandoned canal-building for
the classroom. His third published scientific
paper, Topographical sketch of the State of
New York; designed chiefly to show the gen-
eral elevations and depressions of its sur-
face, which appeared in the Transactions of
the Albany Institute in 1829, capped this
phase of this career. Henry too was a life-
long friend of James Hall, the eminent State
geologist of New York, from whom he must
have assimilated considerable geologic nour-
ishment.
I dwell on Henry here because a few
years later it was put into his power to
organize and shape the destiny of the
Smithsonian Institution, and there can be
little doubt that his knowledge of geology
and its methods and his understanding of
the importance of the science of geology to
the growth of the country had its impact on
the course the Institution was to take. This
knowledge and understanding were reflected
216
particularly in two directions—exploration
and publication.
Henry had as his Assistant Secretary a
man as thoroughly trained in the natural
sciences, particularly biology, as he himself
was in the physical sciences—Spencer Ful-
lerton Baird. Before Baird came to Wash-
ington, and up to the time the Smithsonian
was founded, there had been at least half a
dozen principal Western exploring expedi-
tions, beginning with Lewis and Clark in
1804 and ending with Frémont’s explor-
ations of Oregon and California. But these
were only the beginning. Soon the Bad
Lands were being explored by Dr. John
Evans and Thaddeus A. Culbertson. In
1849-50 Capt. Howard Stansbury led an
exploring and surveying expedition to Great
Salt Lake. Capt. Lorenzo Sitgreaves (1852)
was exploring the Zuni and Colorado River
region. The Mexican boundary survey was
in progress (1854-56) under May. W. H.
Emory. Several parties were in the field sur-
veying for a railroad route to the Pacific.
There were expeditions, also, to Chile, the
La Plata region, the Amazon Valley, Green-
land, and Bering Sea.
The Smithsonian’s part in these efforts
was considerable. In his 1854 annual report
Baird described 26 important explorations
undertaken during the preceding two years,
including six Pacific Railroad surveys.
“With scarcely an exception,” he wrote,
“every expedition of any magnitude has re-
ceived more or less aid from the Smith-
sonian Institution. This has consisted in the
supply of instructions for making observa-
tions in meteorology and natural history,
and of information as to particular desider-
ata; in the preparation, in part, of the
meteorological, magnetical, and natural his-
tory outfit, including the selection and pur-
chase of the necessary apparatus and
instruments; in the nomination and training
of persons to fill important positions in the
scientific corps; in the reception of the col-
lections made, and their reference to indi-
viduals competent to report upon them; and
in employing skillful and trained artists to
make accurate delineations of the new and
unfigured species. Much of the apparatus
supphed to the different parties was in-
vented or adapted by the Institution for this
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, NO. 7
special purpose, and used for the first time,
with results surpassing the most sanguine
expectations.”
All this represented the type of aid the
Smithsonian rendered throughout the excit-
ing decades of western exploration and ex-
pansion. It paid off in many ways, and all
the natural sciences, including geology,
benefited. The Nation benefited. Two spec-
tacular instances are enough to mention.
On June 16, 1874, Maj. John Wesley
Powell laid on the desk of Secretary Joseph
Henry the manuscript of his Exploration of
the Colorado River of the West and its
tributaries, culminating Powell’s explora-
tions up to that time. The Smithsonian
among others had aided the Powell expedi-
tions in various ways, and it was the Smith-
sonian that sponsored the publication of the
Exploration. With remarkable speed, it
came off the press the following year. Its
importance to American geology needs no
recounting before this audience.
Another Smithsonian-nurtured venture of
far-reaching significance was the Kennicott
Expedition that in 1864 set out to explore
Russian America for the Western Union
Telegraph Co., which undertook to run a
telegraph line to Europe by way of Alaska
and Siberia after the failure of the Atlantic
cable. Directing the scientific corps was the
young Robert Kennicott, of the Chicago
Academy of Sciences, who died of a heart
attack near Nulato in May 1866. A geolo-
gist, William Healey Dall, was then put in
charge. Soon afterward, Cyrus Field’s At-
lantic cable was assured and the Western
Union dropped the whole project of an over-
land telegraph line, and the exploring party
was disbanded. In their few months in the
Far North, however, they had done remark-
able work, penetrating territory never be-
fore seen or traversed by white men and
gathering a wealth of natural-history data.
Two of the party—Henry M. Bannister and
Ferdinand Bischoff—had returned to Wash-
ington in 1867, about the time when the
United States Congress was considering the
purchase of Alaska from Russia. Their pres-
ence was most opportune, for they were
probably the only persons in the Capital
with firsthand knowledge of Russian Amer-
ica. Bannister, Bischoff, and Baird were
JuLY 1959
called to testify before the Senate Commit-
tee on Foreign Relations. Their story of
Alaska’s wealth of furs, fish, and timber,
gold and copper, its unbelievable mountains
and glaciers and forests, must have been a
thrilling one to hear. Bannister himself later
remarked: “The annexation was ridiculed
at the time, but we could testify that the
country was worth the price asked. Time
has sufficiently proved that we were right
and I can safely say that we did not over-
state anything... The project of the West-
ern Union Telegraph Company...was a
failure but its greatest result was the annex-
ation of Alaska.” Almost immediately an-
other expedition was organized by the
Treasury Department to obtain additional
information concerning the new ‘Territory
of Alaska, and at the request of the Secre-
tary of the Treasury the Smithsonian fur-
nished instructions ‘“‘for research into the
physical and natural history of the coun-
try.” Among these instructions the following
is of special interest: “Full collections
should be made of the rocks and minerals of
the country at the different stopping points,
as well as of any fossil remains that may be
found to occur. Notes should accompany
these specimens showing their relationship
to each other and the country itself, and il-
lustrated by diagrams indicating the num-
ber, inclination, and relative thickness of
any strata that may be observed.”’
There was another aspect to the Smith-
sonian’s role of catalyst whose importance
should not be minimized. It was the at-
mosphere it provided young scientists in
Washington for study and research. In those
early days the Smithsonian’s funds had to
be spread thin. It could not build up a large
staff of geologists, biologists, physicists, an-
thropologists. But it could provide some of
them with facilities and even living quar-
ters. The be-towered, owl-haunted Smith-
sonian Building, designed by the church-
building architect James Renwick, was a
mecea for them. Joseph Henry and his
family occupied the east “apartments” of
the building. Encouraged by both Henry
and Baird, many a young hopeful was al-
lowed to occupy some unused upper room in
one of the towers. One group called itself
the Megatherium Club, taking its name
OEHSER: SMITHSONIAN IN EARLY AMERICAN GEOLOGY
217
from the field of vertebrate paleontology.
The geologist Fielding Bradford Meek lived
in a north-tower room from the time he went
to Washington in 1858 until his death in
1876, and within the Smithsonian walls were
carried on his patient and conscientious la-
bors “by which the paleontology of the
United States was so greatly advanced.”
The visiting Louis Agassiz spent many a
night in the building as a guest of the
Henrys, and there still is circulated the
probably not apocryphal story of how, one
night, some of the resident “boys” loosened
the slats of Agassiz’s bed. It is not recorded
just what effect this downfall had on the
future career of the famous glaciologist.!
Two other geologists who were the bene-
ficiaries of Smithsonian hospitality were
William Healey Dall and Lester F. Ward.
Neither, so far as I know, ever lived in the
building or was ever on the payroll of the
Smithsonian; but Dall, explorer, paleontol-
ogist, conchologist, spent a lifetime in the
National Museum’s division of mollusks;
while Ward, the paleobotanist who finally
became the patron saint of sociology, was
similarly given the keys to the Institution
and did some of his finest work under its
aegis. A little later, Charles Doolittle Wal-
cott became similarly attached to the
Smithsonian, where he helped to build up
its invertebrate collections, particularly the
Cambrian. All this provided the kind of en-
couragement that scientific research always
needs. Throughout the latter half of the
nineteenth century the Smithsonian was
perhaps its most generous dispenser; and
certainly, as Prof. William North Rice long
ago stated, until the time the U. 8. Geologi-
cal Survey was organized in 1879, the
Smithsonian Institution was the headquar-
ters of the geologists in the service of the
Government. In geology, as in other fields,
the Smithsonian created a salubrious cli-
mate for scientific work.
In 1846 when the Smithsonian was
founded, there were few outlets for the pub-
lication of sizable scientific manuscripts.
* Dr. T. 8. Palmer, biologist and necrologist who
pervaded W ashington scientific circles for many
years until his death in 1955, tried to find out just
which room in the Smithsonian Building “the bed
fell with Agassiz.” If he ever discovered this bit of
esoterica, the secret died with him.
218
As Henry said, “The learned societies in
this country have not the means, except in
a very limited degree, of publishing mem-
oirs which require expensive illustrations,
much less of assisting to defray the cost of
investigations by which the results have
been attained.”’ Henry felt, therefore, that
the Smithsonian could make a real contri-
bution to science by allotting a part of its
income to such publication, and he provided
for this in his initial program. “The publi-
cation of original memoirs and periodical
reports,” he said, “will act as a powerful
stimulus on the latent talent of our country,
by placing in bold relief the real laborers
in the field of original research, while it will
afford the best materials for the use of those
engaged in the diffusion of knowledge.” This
program was immediately initiated, and
Henry through the Smithsonian not only be-
gan a series of monumental publications but
also organized a scheme (the International
Exchange Service) by which scholarly pub-
lications in general could be distributed
throughout the world.
Geology benefited tremendously, as did
anthropology, astronomy, mathematics, bi-
ology, and other disciplines. The quarto
volumes of the Smithsonian Contributions
to Knowledge began to appear in the li-
braries and laboratories of the learned
world, their large illustrations, ample print,
and careful editing distinguishing them. Be-
fore 1860 there had appeared such pioneer
works as Joseph Leidy’s Ancient fauna of
Nebraska; J. W. Bailey’s Microscopical
examinations of soundings, made by the
United States Coast Survey off the Atlantic
coast of the United States; and Edward
Hitcheock’s Illustrations of surface geology.
There followed such works as Meek and
Hayden’s Paleontology of the Upper Mis-
sourt (1865); Charles Whittlesey’s On the
fresh-water glacial drift of the Northwest-
ern States (1866); Raphael Pumpelly’s
Geological researches in China, Mongolia,
and Japan (1866); J. G. Barnard’s On the
internal structure of the earth (1877); and
many others.
The effect of these publications was inde-
terminable but pervasive, and over the years
the Smithsonian’s publications in geology,
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 7
in all its branches, have constituted perhaps
the greatest contribution of the Institution
to that science. It did not, of course, end
with the cessation of the Smithsonian Con-
tributions to Knowledge in 1916, but has
continued to the present day in other Smith-
sonian series, particularly the Smithsonian
Miscellaneous Collections and the Bulletins
of the United States National Museum.
One should mention here too, the free
public lectures that Joseph Henry rather
reluctantly inaugurated in the early days
of the Smithsonian and which had their
special heyday up to the time the Institu-
tion’s lecture-room was destroyed by the
fire in the Smithsonian Building in 1865.
The best scientific and literary talent of the
country was brought to Washington for
these lectures, and geology was well repre-
sented. The very first lectures given in the
Smithsonian Building were a series of six
on Geology, by Edward Hitchcock, presi-
dent of Amherst College. Other geological
lecturers included the elder Benjamin Silli-
man and James D. Dana of Yale; Joseph
LeConte, then of Georgia; T. Sterry Hunt,
of Canada; Fairman Rogers, of Philadel-
phia; and Louis Agassiz, of Harvard. To
quote again Professor Rice: ‘““When science
had searcely naturalized itself in the coun-
try, these lectures in the national capital,
and under ~quasi-authoritative auspices,
served a most valuable purpose in stimulat-
ing public interest in scientific subjects.”
The United States National Museum is
the largest of the “bureaus” of the Federal
Government administered by the Smith-
sonian. Its Department of Geology, housed
in the Smithsonian’s Natural History Build-
ing, is the Nation’s great geological deposi-
tory, and has been ever since 1846, when by
act of Congress the custody of the Nationa!
Cabinet of Curiosities was transferred to
the Smithsonian Institution. The act stipu-
lated that ‘all objects of natural history,
plants, and geological and mineralogical
specimens belonging or hereafter to belong
to the United States,” and which were then
in the City of Washington, should be de-
livered to the Regents of the Smithsonian
Institution and together with new specimens
obtained by exchange, donation, or other-
JuLty 1959 OEHSER: SMITHSONIAN IN
wise, should be so arranged and classified
as best to facilitate their examination and
study. An act of March 3, 1879, decreed that
“all collections of rocks, minerals, soils, fos-
sils, and objects of natural history, archeol-
ogy, and ethnology, made by the Coast and
Geodetic Survey, the Geological Survey, or
by any other parties for the Government of
the United States, when no longer needed
for investigations in progress, shall be de-
posited in the National Museum.” By the
operation of these authorities, augmented
by the efforts of the National Museum’s
staff geologists, the national collections in
geology have grown in all divisions—verte-
brate paleontology, invertebrate paleontol-
ogy, paleobotany, micropaleontology, pe-
trology, mineralogy. Indeed, in some fields,
such as Foraminifera, they are matchless
anywhere in the world. Scientists from all
over the world have studied these collec-
tions, and hundreds of technical papers
based on them have been published, particu-
larly in taxonomic paleontology. Many
eminent geologists, such as William Henry
Holmes, O. C. Marsh, Charles A. White,
George Perkins Merrill, and Charles D.
Walcott, have identified themselves with
this Department of Geology of the Museum.
The last-named, in fact, became the third
Director of the United States Geological
Survey and later the fourth Secretary of the
Smithsonian Institution. His influence on
American geology, both scientific and phi-
lanthropic, has been great and would make
an interesting story in itself.
And another result of these Museum col-
lections that we have been discussing is an
educational one. The collections have been
drawn upon through the years as the basis
of geological exhibits that have been viewed
by millions of people. Today this exhibition
phase is being developed to a high level in
the modernized and expanded displays that
are being built, a most notable example be-
ing the new Gems and Minerals Hall opened
to the public in July 1958. We surmise that
James Smithson would be surprised but
pleased if he could walk into this hall to-
day, captioned by his name on a block of
smithsonite. Perhaps, however, we are get-
EARLY AMERICAN GEOLOGY
219
ting away from our limitation of “early
American geology.”
In summary, then, we should say that
during the third of a century between the
establishment of the Smithsonian Institu-
tion 1846 and the founding of the United
States Geclogical Survey in 1879, the Smith-
sonian served as a focus, headquarters, and
catalyst for geology in America. Its con-
tribution to the science of geology was
manifested along several lines: (1) the
encouragement, stimulation, and facilities
offered by the Institution to young scien-
tists who gathered in Washington in those
early days; (2) the publication and world-
wide distribution of geological works at a
time when expensive monographic publi-
cation was difficult to obtain; (3) aid that
the Smithsonian rendered in the western
explorations and surveys; (4) its promo-
tion of the science of paleontology and its
necessary concomitant, taxonomy; (5) the
building up of the great geological collec-
tions in the U. 8. National Museum; and
(6) education in geology through the Mu-
seum exhibits emanating from these col-
lections.
REFERENCES
Basster, Ray 8S. The Smithsonian: Pioneer in
American geology. Science 104 (2693) : 125-129.
1946.
GILMORE, CHARLES W. A history of the division of
vertebrate paleontology in the United States
National Museum. Proc. U. 8S. Nat. Mus. 90:
305-377. 1941.
JAMES, JAMES ALTON. The first scientific exploration
of Russian America and the purchase of Alaska.
Northwestern Univ. Studies in Social Sci. 4:
276 pp. 1942.
MerriLu, GrorGce Perkins. Contributions to the his-
tory of American geology. Rep. U.S. Nat. Mus.
for 1904: 189-738, illus. 1906.
OrHser, Paut H. Sons of science: The story of the
Smithsonian Institution and its leaders: xvii +
220 pp., illus. New York, 1949.
Rice, Witi1aAM NortH. Geology and mineralogy. In
“The Smithsonian Institution, 1846-1896: The
History of its First Half Century,” edited by
George Brown Goode: 631-646. Washington,
1897.
SMITHSONIAN InsTITUTION. Annual reports of the
Board of Regents, 1847-1878.
Unitep States Concress. A memorial of Joseph
Henry: 528 pp. Washington, 1880. (Published
also in Smithsonian Misc. Coll. 21: 1879.)
iw)
1)
—_)
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49) wor
Geology Plus Adventure: The Story of the Hayden Survey
By J. V. HowE.u, Tulsa, Okla.
The period 1840 to 1880 was one of ex-
pansion on a scale never before experienced
in North America. Population density of the
area east of the Missouri had reached a
point at which the supply of cheap land was
near exhaustion as a result of 250 years of
exploration and settlement. Yet the desire
for land and the spirit of adventure were
in no wise diminished, and the stage was set
for the explosive westward movement which,
in 35 years, resulted in settlement of all that
area from the Missouri River to the Pacific.
Transportation here was a problem vastly
different from that in the eastern half of the
country, where rivers, lakes, and mountain
passes were readily traversed, wood was
generally available for fuel, pastures were
plentiful, and the Indians were soon con-
quered or driven to the northward and
southward. But on the Western plains the
streams were few and seasonal and flowed
in the wrong direction. The Indian tribes
were warlike and well mounted, and main
trails were lacking. Nevertheless, the feat
was accomplished, and in a remarkably
short time.
First, as usual, came the fur traders and
trappers; then the military explorations
with their emphasis on wagon roads and
railroad routes to the Pacific, and with
them the geological and natural history sur-
veys. In seeking a reason for their pro-
liferation, one needs only to consider the
temper of the people and the reasons cited
above. Both government and its citizens
were avid for news of the West.
Alone of all the various explorations of
the period, the Hayden Survey and its im-
mediate predecessors, staffed by Ferdinand
V. Hayden and a handful of assistants, have
failed to receive full recognition and ade-
quate description. Meanwhile, those of King,
Powell, Frémont, Gunnison, Marcy, Long,
and others have produced a spate of books.
For this there are many reasons, none of
which seems wholly justified. The last four
were Army expeditions, each assigned to
the search for a major route to the Pacific.
Geology and natural history were secondary
to pathfinding, the civilian scientists being
strictly subordinates. King’s Survey of the
40th Parallel gained prestige and acclaim
not only by reason of its undisputed geo-
logical results but also because of its color-
ful, articulate leader. That of Powell be-
came famous first through the impact of the
Grand Canyon Voyage, the adventurous
character of which largely overshadowed
its very real geological discoveries. Hayden,
on the other hand, had little flair for per-
sonal publicity and depended on a work-
manlike job, prompt publication of results,
and an efficient liaison with the newspapers
to publicize his expeditions.
Ferdinand V. Hayden was born in West-
field, Mass., on September 7, 1829, to Asa
and Melinda Hawley Hayden, and he lived
there until his twelfth year. At this time his
parents separated, the father moving to
Rochester Depot, Ohio, and the mother to
Rochester, N. Y. Each remarried and each
had children by the second spouse. Ferdi-
nand lived with an uncle at Rochester De-
pot, and at the age of 18 entered Oberlin
College, 15 miles distant, from which he
was graduated in the spring of 1850. He then
entered Albany Medical College where he
came under the influence of James Hall and
of Dr. J. 8. Newberry, who combined the
practice of medicine in Cleveland, Ohio,
with the study of paleobotany.
It should be mentioned here that only
through a medical course could the student
of that day obtain an adequate training in
science. Hayden seems to have had no urge
to practice medicine and never did so, except
during the Civil War, when he served as a
surgeon in the Union Army. Shortly before
eraduation in 1853, Hayden, sponsored by
James Hall, made a trip up the Missouri
Riven in search of vertebrate fossils in the
Badlands. In this venture he was Joined by
F. B. Meek, and thus began an association
that ended only with Meek’s death in 1876.
The complete story of Hayden and the
Hayden Survey has never been told and is
JuLY 1959
beyond the scope of this paper. But an ap-
praisal of the work is possible, and many
hitherto unemphasized features will be
pointed out. Previous authors, concerned
with Hayden’s rivals, have been careless in
their statements, and some of these, too, will
be refuted.
After their first trip up the Missouri, an
expedition financed by James Hall and by
Pierre Chouteau, Jr., Alex Culbertson and
J. B. Sarpy of the American Fur Co., Meek
and Hayden returned in late autumn and
spent the winter at Albany, preparing their
collections and writing a report.
In the spring of 1854, Hayden again as-
eended the Missouri under the auspices of
the American Fur Co. and Maj. A. J.
Vaughan, the Indian agent for the Upper
Missouri tribes. This time he remained
through the winter, living at Fort Pierre and
making trips as weather permitted. During
this period he was able to visit the posts at
Forts Sarpy, Benton, and Union, returning
to St. Louis on November 5, 1855.
In 1856, attached to the exploring party
of Lt. G. K. Warren, Hayden again ascended
the Missouri, traveling upriver by steamer,
and visited the valley of the Yellowstone,
part of the time in company with the famous
guide Jim Bridger.
Again in 1857, he accompanied Lieutenant
Warren to the Black Hills and for the first
time discovered their domal structure.
Wines to Prof. S. F. Baird from Fort
Laramie on August 21, he said, ‘Success
has attended all our efforts, but we have had
a hard time. My discoveries in a geological
way are wonderful,” and “I have got the key
to the mountain area,” and “I am making
good use of it, so that this trip will not by
any means be a failure.”
The following year, 1858, under the aus-
pices of the Department of the Interior
(General Land Office), and with an appro-
priation of $5,000, Hayden made a survey
of western Kansas, traveling by wagon and
on horseback. In 1859-60 he was attached
to the expedition led by Col. W. F. Raynolds
to the headwaters of the Missouri and Yel-
lowstone Rivers. This party wintered at
Deer Creek, Wyoming (1% mile southwest
of Glenrock), and under the guidance of Jim
Bridger made an unsuccessful attempt to
reach the geyser area of the Yellowstone.
\
HOWELL: GEOLOGY PLUS ADVENTURE: THE HAYDEN SURVEY
221
Bridger had been with the party during most
of its travels, and there is no doubt that
Hayden was well acquainted with the “tall
tales” of that famous raconteur. Certain it
is that on the 1871 expedition the route
taken to the Park area followed that of the
1860 attempt which had been foiled by the
deep snow in the mountain passes.
The Civil War brought to a close all
Western explorations, and Hayden entered
the Army as acting assistant surgeon, was
advanced to surgeon of volunteers, and was
discharged with the rank of brevet leuten-
ant colonel on June 22, 1865. His Army
service involved duty in hospitals at Beau-
fort, S$. C.; West Philadelphia, Pa.; and Win-
chester Field Hospital at Winchester, Va.
Immediately after his discharge from the
Army, Hayden again headed for the Upper
Missouri, this time with one assistant and
under the auspices of the Academy of Natu-
ral Sciences of Philadelphia. Starting from
Fort Randall, S. Dak., on August 3, he made
a circuit of 650 miles in 52 days, his party
consisting of James Stevenson, a guide, an
Indian hunter, and a military escort of five
troopers.
The years 1867-68, Hayden, under aus-
pices of the General Land Office, devoted to
a survey of Nebraska Territory and eastern
Wyoming, but he was able to make trips
into North Park, Colorado, and westward
along the Union Pacific Railroad almost to
Salt Lake City and to spend two weeks in
the San Luis Valley. All this travel was on
foot or on horseback.
In the year 1869, again under the General
Land Office, Hayden traveled from Chey-
enne southward along the foothills to Santa
Fe, returning through South, Middle, and
North Parks. As a result of this trip he was
able to state for the first time that (1) the
main range of the Rockies is a huge anti-
clinal; (2) the Tertiary Lignite beds from
New Mexico to Canada are parts of one
basin, interrupted by uplifts; (3) the Rocky
Mountains are Post-Cretaceous in age; and
(4) the lower ranges are monoclinal, de-
scending toward the plains in steps.
By this time he had seen much of the
present States of Montana, North and South
Dakota, Wyoming, Kansas, Nebraska, and
northeastern Utah. A “Grand Plan” was
now shaping up, which involved the map-
222 JOURNAL OF THE
ping of these States as a unit, embracing the
mountains and plains, and studying the re-
lationships between them. With the recon-
naissance completed, detailed study and
mapping were now the object of his efforts.
In 1870 there was created, under the De-
partment of the Interior, the U. 8. Geo-
logical and Geographical Survey of the
Territories with Hayden as director. The
work of the first year was in Wyoming, the
starting point Cheyenne, and, with an ap-
propriation of $25,000, it was possible to
utilize 12 assistants, 8 teamsters and cooks,
and sufficient horses and wagons. In this
season Hayden first described and named
the Dacota, Fort Pierre, and Fox Hills units
of the Cretaceous.
The next year, 1871, the expedition took
the field at Ogden, Utah, to which the tracks
of the Union Pacific Railroad had then been
extended. An appropriation of $40,000 per-
mitted an increase in personnel to 32 and
included the photographer W. H. Jackson
and the artist Thomas Moran, and the sum-
mer was spent in what is now Yellowstone
Park. Paintings and photographs resulting
from their work were widely circulated and
certainly aided greatly in obtaining in-
creased support for the succeeding year. In-
cidentally, the edition of 12,000 copies of the
1871 report was exhausted by 1874.
The season of 1872 was spent in the Yel-
lowstone Park area where two large parties
totaling 56 men, 117 horses and mules, and
5 guests were able to explore thoroughly the
valleys of the Yellowstone, Gallatin, Madi-
son, and Snake Rivers and the Teton Moun-
tains. There is little doubt that the photo-
graphs and reports of this year did much to
cause the establishment of the Park.
Indian troubles in Wyoming led the War
Department to forbid geological work there
in 1873, and so attention was directed to
Colorado, where three divisions covered
Middle Park, South Park, and the San Luis
Valley. In this year also triangulation and
topography were begun under James T.
Gardiner, previously associated with Dr. J.
D. Whitney on the Survey of California.
Again in 1874, 1875, and 1876 work was
continued in Colorado and resulted in the
great Atlas of the geology of that State,
published in 1877, as well as the usual an-
nual reports.
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, NO. 7
In general, Hayden’s relations with the
Indians were good, but the large Survey
parties on occasion proved an irresistible
temptation. Thus in 1872 a party had some
difficulty with Bannocks near Fort Hall. In
1875 a party under J. T. Gardiner lost most
of their animals and equipment near the
Sierra La Sal after holding off an attack for
several hours and finally escaping during
the night. Meanwhile, W. H. Holmes lost
his animals to a band of Utes on Monte-
zuma Creek in southwestern Colorado.
Holmes and his packer, Tom Cooper, pur-
sued the Indians and recovered their stock
on Recapture Creek, so named by Holmes
in commemoration of this episode.
Again in 1877, A. D. Wilson’s party in
the Yellowstone area lost all their stock, ap-
parently to Chief Joseph’s band, while in
the final year of 1878 a topographical party
in the Teton area lost all its animals and
part of its equipment. Several other minor
attacks were repelled and no losses occurred,
but diaries and letters of the period 1870-
78 indicate that all parties posted guards
each night in strict military fashion. Inci-
dentally, a goodly number of the packers
and guides were familiar with the Indian
type of warfare, and a considerable number
of packers, cooks, geologists, and topogra-
phers were veterans of the Civil War; and
pictures, letters, and diaries agree that Hay-
den was the only one who habitually went
unarmed.
In 1877, work again was in Wyoming,
Utah, and Idaho but was rudely interrupted
in September by the depredations of Chief
Joseph. Next season an attempt was made
to conclude the work in the Wind River and
Yellowstone areas, and the personnel num-
bered 68. Despite loss of all the horses of the
Yellowstone party, much was accomplished,
particularly by A. C. Peale and. W. H.
Holmes in the Park area.
On June 30, 1879, the Hayden Survey
ended. Hayden himself moved to Phila-
delphia where he owned a home, where his
wife’s family lived, and where there was ac-
cess to library facilities then superior to
those in Washington. Here he closed out
the Survey affairs and completed his 2-
volume final report. By now his health had
begun to fail, and although in the summers
of 1883-1886 he made several trips to Mon-
JuLty 1959
tana with his close friend Peale, his condi-
tion grew rapidly worse, and he died in De-
cember 1887.
It may be of interest to note that on
December 30, 1930, six surviving members
of the Hayden Survey, W. H. Holmes,
George B. Chittenden, Ernest Ingersoll, W.
H. Jackson, Story B. Ladd, and Frederick
D. Owen, met in Washington to unveil a
memorial to the Survey. This took the form
of a bronze plaque located in the ground-
floor lobby of the new Washington Evening
Star Building, at the corner of Eleventh
Street and Pennsylvania Avenue, NW., site
of the old Star Building on whose third floor
were the offices of the Survey from 1870 to
1875.
An institution should be judged by the
quantity and quality of its work, and in
this respect the Hayden Survey and its
director have not received adequate recog-
nition. One may look well at the “firsts”
attributed to them, as follows:
1. Developed the plan of having topogra-
pher and geologist work together, a method
carried over to the U.S.G.S. and continued
down to the recent past.
2. First reported the domal structure of
the Black Hills.
3. Made the first scientific exploration of
the Yellowstone Park.
4. First determined age of the Rocky
Mountains.
5. First reported presence of Potsdam
sandstone west of the Missouri.
6. Made the first geological map of the
Black Hills.
7. First to report thrusting in the Rockies.
8. First to delimit and name 29 strati-
graphic units of the Cretaceous and Tertiary
of the Western United States, which are still
valid and used in their original sense.
9. First to recognize and explain the ter-
races in the Salt Lake Basin (in 1869).
10. First to recognize and explain lacco-
liths (but not to name them).
11. First to point out the anticlinal struc-
ture of the Main Range of the Rockies.
12. First to make extensive use of photo-
eraphs to illustrate geologic features.
13. First to show the existence of the
ereat Tertiary basin extending from Mexico
to Canada.
Other features that should be noted in-
HOWELL: GEOLOGY PLUS ADVENTURE: THE HAYDEN SURVEY
223
clude Hayden’s invariable custom of pub-
lishing the report of one season’s work be-
fore taking the field for the following year.
No backlog of manuscripts was allowed to
accumulate. And here it may be well to
point out that the Survey during the nine
years of its existence published 21,142 pages
of reports, while Hayden alone, or with F.
B. Meek, published a grand total of 1,306
pages bearing his name.
During these same 25 years from 1853 to
1878 there were employed 14 geologists (in-
cluding Hayden) whose total man-years of
field work were 55 in number. The area
mapped by all Hayden expeditions and
colored on the final map of 1882 included
417,000 square miles, which indicates an
output of 7,582 square miles per man—per
year. Admittedly, this was largely recon-
naissance, but the work was good to ex-
cellent and shows everyone was working.
Other statistics concerning personnel may
be of interest also. Of 219 members of Hay-
den’s various expeditions, 38 are listed in
Who Was Who, Dictionary of American Bi-
ography, and American Men of Science. Ap-
proximately 70 streams, mountains, towns,
lakes, and gulehes were named for Survey
members. At least 10 men wrote books other
than technical reports, and one became a
Congressman. Eighteen employees, after the
Survey closed, joined U.S.G.S. or other Gov-
ernment departments.
Here may be mentioned a feature of the
personnel which was much criticized by his
opponents. This pertained to Hayden’s em-
ployment each season of a few ‘general
assistants” who were sons, nephews, or pro-
tegees of Senators and Congressmen. Recall-
ing that there was then no Civil Service, that
Hayden’s relations with Congress were gen-
erally good, and that most of these assist-
ants were college students or graduates and
did a man’s work, in addition to having a
ereat adventure, one cannot be too critical.
Besides, what else could Hayden do if, as is
shown by the record, one application was
signed by 32 Senators and Congressmen!
Incidentally, this young man wrote a very
creditable book for boys detailing his ex-
periences of that summer. It is entitled In
the trail of the pack-mule, and the author is
Sid H. Nealy, who was an assistant in 1872
and 1873.
224 JOURNAL OF THE
The Hayden Survey, its members and
Hayden himself, left behind a vast store of
nearly 12,000 unpublished letters, diaries,
and journals, scattered widely. No full biog-
raphy of Hayden, or a history of his Survey,
has yet been published. However, Dr. F. M.
Fryxell and the writer, after many years of
searching, have brought all this together on
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, NO. 7
microfilm or photostatic copy; and they
hope eventually to write the detailed history
which the man and his Survey deserve. The
story is one that will require a large volume,
and in this brief paper only a glimpse can be
given of geology plus adventure as revealed
by the participants themselves.
rr ____
A History of the Popularization of Geology in America:
A Bibliographical Survey
By Marx W. PANGBORN, JR., U.S. Geological Survey
The history of the public relations aspects
of our science reveals that in this country,
during the 1830’s and 1840’s, geology held a
high position in public esteem, that our pro-
fession lost that position by default, and
that, by the same token, it is reestablishing
geology as a subject worthy of strong public
support and interest, and that an effective
and abundant popular literature plays a
large role in such a rennaissance.
During the Colonial and early Federal
periods the study of geology was largely
limited to the educated aristocracy. Such
public figures as Jefferson and Gallatin were
considerable students of geology, and their
interests were often parlayed into worthy
public enterprises, such as the explorations
of Lewis and Clark, Pike, and Long.
It was in the 1830’s and 1840’s, however,
that geology really came into its own. This
was the great age of the lyceum, or public
lecture series, that so impressed Agassiz
when he arrived in Boston in 1846. Geology
rode high on the wave of self-culture and
interest in natural history that got under
way about 1820, propelled by the ardent
proselyting activities of a sizable percentage
of the most prominent geologists, including
Eaton, Silliman, H. D. Rogers, Lyell, and
Agassiz. Amos Eaton alone made 3,000 lec-
tures outside the classroom, and it was in
part due to the boundless enthusiasm of such
men that a number of State legislatures were
inspired to finance early surveys.
The layman’s literature of the time was
largely that used by the geologists them-
selves. Concepts were still simple, and the
specialized geological terminology of 1840
was limited to a few hundred words. The
textbooks of Eaton (1), J. D. Dana (2),
Hitchcock (3), and Lyell (4) sold well
among those hungry for learning, and Man-
tell’s Medals of creation (5) and Hugh
Miller’s Old Red Sandstone (6) were vastly
popular informal books. The volumes of the
early State surveys were also well received
by laymen. Yet even this enlightened age
had its share of potboilers by nongeologists,
and we must admit that the works of 8. G.
Goodrich (Peter Parley) are horrible ex-
amples of the genre.
Public interest in geology declined during
the period from the Civil War to the turn of
the century, despite interest in the great
bonanzas and in Western exploration. Part
of the decline may be blamed on the fact
that during this period geologists began to
use their special and often unnecessary tech-
nical terms, a trend which continues to the
present day and renders unacceptable, to the
layman, far too much of the professional
literature. Equally significant was the very
sharp decline in the proportion of geologists
interested in popularizing their science.
Some of the most famous exceptions were,
of course, John Wesley Powell and Clarence
King. Exploration of the Colorado (9) and
Mountaineering in the Sierra Nevada (8)
went through many editions and helped to
keep alive the tradition of Western scien-
tific exploration. Perhaps the biggest selling
book was Darwin’s Origin of species (7),
JuLY 1959
which caused almost as much uproar and
intellectual ferment in this country as it
did in England. Other geologist-writers in-
cluded J. D. Dana, whose easier texts, like
The geological story briefly told (12), were
fine for high school and layman’s use, and
N. 8. Shaler, who turned out a number of
nontechnical introductions to physiography,
such as Aspects of the earth (10) and Sea
and land. Another gifted popularizer was
Alexander Winchell, whose vividly written
Walks and talks in the geological field (11)
was, for many years, on the reading lst of
the Chautauqua Association, an organiza-
tion whose subscribers numbered 5 million
in the year 1900. Among nongeologist
writers, the best was probably H. N. Hutch-
inson, a liberal English clergyman whose
books Extinct monsters (13) and Creatures
of other days were free of the theological
controversy of earlier times.
From 1900 to World War II, it is no
coincidence that geology and physiography
all but disappeared from the high schools
at the same time that interest in populariza-
tion all but disappeared within our profes-
sion.
On the credit side, between 1910 and 1930
the U. 8. Geological Survey undertook a
modest public education program, publish-
ing guidebooks (14) covering some of the
western railroad routes, and some booklets
on the national parks, by men like Arnold
Hague, M. R. Campbell, and W. T. Lee.
Francois Matthes, in his Geologic history
of the Yosemite Valley (17), proved that a
scientific classic could be written in plain
English. The National Park Service became
a potent educational force in the 1920’s as
its public education program began to de-
velop. Some State surveys, notably New
York, Pennsylvania, and Kentucky, began
to issue popular publications, as did the
American Museum of Natural History. Pop-
ular interest in mineral collecting, to be-
come so strong in the 1950’s, began to revive
with the founding of the journals Rocks and
Minerals, in 1926, and Mineralogist, in 1933.
Among the few layman’s books that sold
well were F. B. Loomis’s Field book of com-
mon rocks and minerals (15) and astrono-
mer W. M. Reed’s The earth for Sam (16).
Two other authors, who are still turning out
big sellers, were Roy Chapman Andrews,
PANGBORN: POPULARIZATION OF GEOLOGY
225
whose books on dinosaur hunting (19) were
well received, and Carroll Lane Fenton, who
was establishing his reputation as a popu-
larizer with works like Our amazing earth
and The rock book (18).
Since World War II, the outlook for pop-
ularizing geology has become generally
brighter. Geology courses are being reintro-
duced into a number of high schools, and
school libraries, by now rather common, fea-
ture the better-known geological texts and
popular works, as well as such fine journals
as Natural History and Scientific American.
Some States have stepped up their educa-
tional and publishing programs, including
California (22), Kansas, Oklahoma, and
Illinois, and the U. 8. Geological Survey
now prints geological descriptions on the
backs of its National Parks maps (23).
The National Park Service remains pre-
eminent as the great popularizer of geology
in the country. Perhaps 10 million young
people of school age see geological wonders
first hand every year, and take home scores
of thousands of earth science books from
park concessions.
Interest in caves has burgeoned since
1941, when the National Speleological So-
ciety was formed; now its 1,700 members
and perhaps 15,000 other young spelunkers
spend their weekends underground. Even
more spectacular has been the spread of in-
terest in mineral collecting and cutting; H.
C. Dake authoritatively estimates the mini-
mum number of devotees at 250,000.
With the publication of the successful
new Merit Badge pamphlet on geology (27),
the Boy Scouts have become an important
agent for promoting the earth sciences. Over
50,000 copies of this pamphlet have been
sold since introduction in 1953, and geology
badges earned have risen from 300 to 3000
per year. Geology month among the Scouts,
October 1957, featured “The biggest show
on earth,” during which 4,000 geologists as-
sisted 38,000 scout units to make it by far
the largest public relations program ever
put on by our profession.
Geology now has an over-all public rela-
tions organization in the American Geologi-
cal Institute, founded in 1948. Its publica-
tions include a career booklet, of which a
modest 18,000 copies have been given away,
and a layman’s guide to the nontechnical
226 JOURNAL OF THE
literature (29). Yet A.G.I.’s operations are
still on a small scale compared with those of
the American Petroleum Institute and of
certain oil companies, which distribute free
career materials and teachers’ pamphlets
by the millions.
In the past few years there has been a
noticeable increase in the sales of popular
geology books, both absolute and in relation
to other technical subjects; only aviation
and rocketry attract more young readers
now than do the earth sciences. The Fen-
tons’ Rock book, for example, has been sell-
ing twice as well since 1945 as it did when
published in 1940, and Zim and Shaffer’s
new Rocks and minerals (30) is the run-
away leader in the fabulously successful
Golden Guide series.
In addition to established names like
Andrews (25) and the Fentons (31), a new
eroup of outstanding popularizers is now at
work. Among them are journalist Ruth
Moore (28), physicist George Gamow (21),
geologists O. P. Jenkins (22) and F. M.
Fryxell, paleontologists G. G. Simpson and
EK. H. Colbert (20), and mineralogists R.
M. Pearl (26) and F. H. Pough (24).
Although lack of objective data makes
it difficult to contrast the status of popular
geology in recent years with its status in the
1840’s, it 1s clear that in 1840 a high per-
centage of the most prominent geologists
participated in public lectures and similar
services; by 1940 surely no more than one
or two percent of our profession lectured,
counselled, or wrote for the public.
I am glad to say, however, that since
World War II an increasing number of ge-
ologists have become aware that geology
must be brought to the layman if public in-
terest and support for geological enterprises
are to grow, and if a supply of future geolo-
gists is to be assured. Let us hope that our
profession fills the gaps in the popular lit-
erature. New illustrating and publishing
techniques promise more attractive books,
and new marketing methods are providing
far wider audiences. If our geologists them-
selves can engender the proselyting enthusi-
asm of Amos Eaton and Agassiz, and are
willing to grant their popularizations the
same care that they put into their profes-
sional work, then geology will indeed hold
the American public’s interest and approval.
WASHINGTON
_
15.
16.
18.
a
“SYELG,
ACADEMY OF SCIENCES VOL. 49, NO. 7
BIBLIOGRAPHY
Eaton, Amos. Geological text book, prepared
for public lectures on North American geol-
ogy ...: 63 pp. Webster and Skinners, Al-
bany, 1830.
. Dana, JAMES Dwicut. A system of mineralogy:
144 pp. Durrie & Peck, New Haven, 1837.
. Hitcucock, Epwarp. Elementary geology, ed.
2: 346 pp. Dayton & Saxton, New York,
1841. (Went through 30 editions in 20 years;
Hitchcock tried to reconcile the Bible and
geology.)
Cuaries. Elements of geology, 1st
American ed. James Kay, Philadelphia, 1839.
(Lyell’s numerous textbooks went through
many editions.)
. MANTELL, GipEon ALGERNON. The wonders of
geology, 2 vols. A. H. Maltby, New Haven,
1839. (This and Medals of creation were in-
tended for the layman.)
. Mitier, Hucu. The Old Red Sandstone. Edin-
burgh, 1841.
. Darwin, CHARLES Rosert. Origin of species, 1st
American ed.: 432 pp. Appleton, New York,
1860. (Appleton issued this book in the face
of hundreds of threatening letters; it was a
best seller for years.)
. Krnc, CLARENCE Rivers. Mountaineering in the
Sierra Nevada. J. R. Osgood, Boston, 1872.
. PowELL, JoHN Wes.ey. The exploration of the
Colorado River of the West...: 291 pp.
Government Printing Office, Washington,
1875.
. SHALER, NATHANIEL SOUTHGATE. Aspects of the
earth: 344 pp. Scribner, New York, 1889.
. WINCHELL, ALEXANDER. Walks and talks in the
geological field: 329 pp. Chautauqua Press,
New York, 1886.
. Dana, James Dwicut. The geological story
briefly told: 302 pp. American Book Co.,
New York, 1895.
. Hutcuryson, Henry NEVILLE. Extinct mon-
sters ...: 254 pp. Appleton, New York, 1892.
. Lee, Witutis THomas. Guidebook of the West-
ern United States, Part B, The Overland
route...: 244 pp. Government Printing Of-
fice, Washington, 1915. (U.S. Geol. Surv. Bull.
612.)
Loomis, FREDERIC BREwsTER. Field book of com-
mon rocks and minerals: 352 pp. Putnam,
New York, 1923. (100,000 copies of this steady
best seller have been printed over the years.)
Reep, WiLL1AM Maxwe Lu. The earth for Sam:
390 pp. Harcourt Brace, New York, 1930.
(52,000 copies in print.)
. Matrues, Francois Emite. Geologic history of
the Yosemite Valley: 137 pp. Government
Printing Office, Washington, 1930. (U.S. Geol.
Surv. Prof. Paper 160.)
FENTON, Carrot LANE, and Fenton, M. A. The
rock book: 357 pp. Doubleday, New York,
1940. (Over 40,000 copies sold.)
AnpDREWS, Roy CHapMan. Under a lucky star; a
lifetime of adventure: 300 pp. Viking, New
York, 1948. (Sold 30,000.)
Juty 1959
20. CoLtpert, Epwin Harris. The dinosaur book:
156 pp. American Museum of Natural His-
tory, New York, 1945. McGraw-Hill, 1951.
(Nearly 25,000 copies of this model popu-
larization have been bought.)
21. Gamow, GerorcE. Biography of the earth: 194
pp. Viking, New York, 1948. (8,000 of the
hard cover edition and a quarter million pa-
perbacks have been sold.)
22. JENKINS, OuaF Pitr. Geologic guidebook along
highway 49—Sierran gold belt...: 164 pp.
San Francisco, 1948. (California Div. Mines
Bull. 141. Leads all state-issued publications
with 20,000 copies sold.)
23. U.S. GrotogicaL Survey. Topographic map of
the Denver mountain area, scale 1:190,680.
Washington, 1948. (Top seller among Park
maps which have a geological text on the
back; over 3,000 per year.)
24. PoucH, FreperiIcK Harvey. A field guide to
rocks and minerals: 333 pp. Houghton Mif-
flin, Boston, 1953. (Like Loomis, a tremen-
dous seller.)
25. ANDREWS, Roy CuHapMan. All about dinosaurs:
146 pp. Random House, New York, 1953. (A
leader even in the highly successful “All-
about” series of children’s books, with sales
over 160,000.)
DUPREE: ASA GRAY AND AMERICAN GEOLOGY
227
26. Peart, RicHarp Maxwe.u. How to know the
minerals and rocks: 192 pp. McGraw-Hill,
New York, 1955. (Another title which has
passed the quarter million mark, in all edi-
tions.)
27. Boy Scouts or America. Merit badge series:
geology, ed. 2: 35 pp. New York, 1956.
28. Moorr, RutH. The earth we live on: 416 pp.
Knopf, New York, 1956. (This history of ge-
ology has had a fine reception.)
29. PaNcBorN, Mark W.., Jr. Harth for the layman;
a list of nearly 1400 good books..., ed. 2:
68 pp. Washington, 1957. (American Geol.
Inst. Report no. 2.)
30. ZiM, HERBERT SPENCER, and SHAFFER, PAUL.
Rocks and minerals: 160 pp. Simon & Schus-
ter, New York, 1957. (Numerous sales out-
lets, high quality, and low price enable this
title to sell at the rate of half a million copies
per year, surely the all-time high for a sci-
ence book.)
31. FENTON, CARROLL LANE, and Fenton, M. A. The
fossil book: 496 pp. Doubleday, New York,
1958. (Prepublication orders of this expensive
book totalled nearly 4,000, a phenomenon
that could hardly have been conceived a few
years ago.)
OO
Asa Gray and American Geology
By A. Hunter Dupren, University of California
American geologists as a group did not
occupy a theoretical position which could
help them much to understand what was
happening when the Origin of species broke
over them in 1859. In spite of their number
and the quality of the precise stratigraphi-
cal work which they were doing, their the-
ories were as crude as they were hotly con-
tested within the group itself. As examples,
the brothers William Barton Rogers and
Henry Darwin Rogers will serve as well as
any. They were able geologists, but their
theories, depending heavily on such cata-
clysms as sudden floods, were far-fetched.
Louis Agassiz had imported the idea of a
glacial epoch to North America, but his
ideas of organic development were domi-
nated by an extreme idealism. Even the
acclaim of Europe was not sufficient to es-
tablish his glacial hypothesis firmly in
America, where many geologists still talked
of icebergs as the main depositors of the
drift. Virtually the only general theoretical
agreement in American geology in 1859 was
a propensity to catastrophism. The one man
with the stature to resolve these difficulties
and to bring American concepts into line
with Darwinian theories, James Dwight
Dana, did not perform this expected role
both because his own thoughts on species
were distinctly idealistic and because his
health broke in 1859, preventing him from
even reading the Origin of species for sev-
eral years.
Within 15 years, or at the very most 20
years, the picture had changed completely.
Not only did American geology stand near
the forefront in its accomplishments, glory-
ing and suffering in the great age of pale-
ontology with O. C. Marsh and E. D. Cope,
the glacial theories of T. C. Chamberlain,
and the Great Basin studies of able men
228 JOURNAL OF THE
such as G. K. Gilbert. Whatever theoretical
difficulties remained, though they were for-
midable, were those which faced the men at
the frontiers of the science rather than those
of provincials caught in a backwater. Who
was responsible for this sudden clearing of
the ground, this rapid assimilation of de-
scent with modification on the organic side
of the geologic scale as required by Dar-
winian theory? Who dethroned the great
catastrophist Louis Agassiz from the pinna-
cle of American geology in the very period
that his glacial hypothesis was winning the
vindication of overwhelming evidence? The
answer to these questions is the name of
a man who had the distinct advantage of
knowing very little geology—the botanist
Asa Gray.
While Gray’s role as the protagonist of
Darwin in America is widely if uncritically
recognized, the specific contribution which
he made toward adapting geologic phenom-
ena to a Darwinian sequence of life forms
has often been overlooked. And the imphca-
tions which his work had for the reorganiza-
tion of geologic theory among Americans
have been almost totally ignored.
Gray began his scientific life in the late
1820’s, when the old-style naturalist still
had a place in the upstate-New York in-
tellectual milieu in which he lived. Hence he
collected, in addition to plants and insects,
trilobites and minerals. His first paper in
the American Journal of Science concerned
the mineralogy of St. Lawrence County,
N. Y. But Gray was a good example of a
most important change which came across
American science in the 1830’s—the trend
toward specialization. The old-style natu-
ralist was vanishing, Gray becoming in-
creasingly identified with the science of
botany. Soon after he went to Harvard as
Fisher Professor of Natural History he
donated to the College his mineral collection
in an almost symbolic act of renunciation.
That he had withdrawn from active re-
search in any phase of geology made it
easier for him to adopt general views of the
subject without entering the controversies
which raged among the professional geolo-
gists. Thus when Sir Charles Lyell lectured
before the Lowell Institute in Boston in
1845, Gray attended regularly even though
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
he considered Lyell “not a good lecturer at
all.”’ But he spoke of an Englishman “oc-
cupyinge—though under a rather different
aspect the ground I am to take up...on
Geographical Botany.” Thus effortlessly and
without fanfare Gray absorbed Lyell’s point
of view even if he did not use his oppor-
tunities to become a friend and correspond-
ent of the British geologist.
Undoubtedly the arrival of Agassiz in
America in 1846 stimulated Gray to a
friendly reception of the Swiss scientist’s
glacial theory as well as his views on natural
history. The two cooperated cordially to
combat the idea of Vestiges of the natural
history of creation, which had a considerable
vogue in America as well as Europe. Yet
even in 1846, subtle differences showed up
between the thought of the two men, and
Gray never assented either to Agassiz’s
idealistic views of species as ‘“‘a thought of
the Creator” or to his catastrophism.
By 1855 Gray was aware of a funda-
mental antagonism between his whole view
of nature and that of Agassiz. Although the
zoologist dominated the scene in America
and commanded an overpowering European
reputation, the quiet botanist had unusual
facilities for tapping those minds of Europe
who were shaping the coming revolution.
He, and not Agassiz, was collaborating with
Joseph D. Hooker and Alphonse De Can-
dolle in creating a science of the geography
of organisms on a world scale. Through
Hooker he was brought into the circle of
Charles Darwin, who might most aptly be
described in 1855 as a geologist of first 1m-
portance who had also prepared an admira-
ble monograph on the barnacles. But be-
hind the sharp questions concerning the
world distribution of plants which Darwin
put to Gray seemed to lurk a consistent set
of doctrines. The trend of these doctrines,
as they gradually became apparent in Dar-
win’s letters, reinforced Gray’s belief in the
law of genetic connection among all the
members of a species. They not only re-
sembled one another, they were also the
actual descendents from a single pair and
had radiated from a single center of crea-
tion. Agassiz, on the other hand, maintained
that species had been created in great num-
bers, occupying essentially the same geo-
Juty 1959
graphic areas throughout their existence.
Thus he denied both a genetic connection
among the members of the same species and
among similar organisms which occurred in
different geologic strata. Gray increasingly
felt dissatisfied with Agassiz’s formulation,
but until 1858 he bided his time, hoping to
assemble a specific case with which to chal-
lenge his renowned colleague.
Gray found his facts with which to con-
struct a challenge among the botanical col-
lections coming in to him in large quantity
from the American exploring expeditions,
which were the characteristic research or-
ganizations of the 1850’s. Disjunct distribu-
tions, that is, plants peculiar to two widely
separated geographical localities, had been
among the favorite arguments of those who
believed in multiple as well as special crea-
tion. Gray found a large number of plants
in the first collections to come in from Japan
in 1857 and 1858 which were to be found
also in eastern North America and nowhere
else. To assume that a Philadelphus, say,
which was reported only in Japan and the
southern Appalachians, had been created
in those two localities independently, seemed
to Gray to answer the problem only by pre-
venting its being posed. If he could, on the
other hand, come up with a material con-
nection between the two similar plants found
half a world away, he would have a case
which fairly refuted Agassiz’s whole con-
ception of biology.
The key to Gray’s solution of the prob-
lem of disjunct distributions between eastern
Asia and eastern North America lay in ge-
ology, and here his own ignorance placed
him in the hands of others. Consulting both
James Dwight Dana and Charles Darwin,
he came up with a conception of geologic
history which would explain the present
distribution of plants. In the Tertiary period
a temperate flora had extended all the way
around the North Pole. With the glaciation
of the Pleistocene epoch this flora had been
pushed far southward, its remnants forming
the disjunct distributions which Gray’s evi-
dence should. Thus a flora continuous across
the Bering Strait area in the Tertiary pro-
vided a material and genetic connection be-
tween the plants with which Gray hoped to
refute Agassiz. Gray had no fossil evidence
DUPREE: ASA GRAY AND AMERICAN GEOLOGY
229
of this Tertiary flora, and precious few in-
dications of the climate, but his reasoning
established an unbroken chain of events.
That his paper on this subject was in-
tended as a full-scale assault on Agassiz and
not a fragmentary report on collections from
Japan is clear from the dramatic circum-
stances of that meeting of the American
Academy of Arts and Sciences in Boston
early in 1859, many months before the
publication of the Origin of species. Agassiz
was present in person to contest and rebut
Gray’s effort at every point. Yet the very
construction of Gray’s argument bears the
marks of the debate. His strategy avowedly
was to “hoist Agassiz on his own petard.”
At three points especially, this strategy led
Gray to make choices momentous for
American geology.
In the first place, he was one of the first
Americans to accept publicly and unquali-
fiedly Agassiz’s conception of the Ice Age.
An ice sheet which spread generally over
both the old and the new worlds was the
agent which Gray needed to accomplish his
distributions. It could not at the same time
serve, however, as the catastrophe which
Agassiz required. The very completeness of
Gray’s acceptance is a landmark in the his-
tory of glacial theory in America which
must have infuriated Agassiz by its very
cordiality.
In the second place, Gray was well aware
that Agassiz, who believed that no Tertiary
species existed in the present, would take
advantage of Gray’s lack of fossil evidence
for a circumboreal temperate flora in the
Tertiary. Agassiz had also made much of
the length of time during which present spe-
cies had remained unchanged. Therefore
Gray, in choosing geologic advice, rejected
that of Darwin in favor of Dana, who ad-
vocated a very warm period after the Pleis-
tocene glaciation. Gray could thus postulate
a second mingling of his species across the
Bering Strait area after the Pleistocene as
well as before, establishing a material con-
nection even if one accepted with Agassiz
the catastrophic nature of the Ice Age.
In the third place, Gray pointed out, be-
sides the identical species which followed
his pattern of distribution, a number of
genera which did the same. Thus genera
230 JOURNAL OF THE
peculiar to Eastern Asia and Eastern North
America which were represented only by
distinet species in the two places, suggested
to Gray that the vicissitudes of geologic
history had produced sufficient modifica-
tions in the pristine stock to lead to distinct
species which nevertheless had descended
from a single pair. This was descent with
modification through geologic time, and lest
anyone misunderstood the general bearing
of his theories, he pointed to the Linnaean
Society publication of 1858 which first pre-
sented Darwin and Alfred Russel Wallace
to the world.
Agassiz never effectively answered Gray,
despite his continued eminence in American
science. When the Origin of species ap-
peared, Gray introduced it to the American
scientific public in a review in the American
Journal of Science, speaking not for himself
but for the whole board of editors, which
included both Dana and Agassiz. When
Gray retired as president of the American
Association for the Advancement of Science
in 1872 he presented his theories in new and
elegant form in Sequoia and its history,
which extended the formulation to Western
North America. Before the end of his life
in 1888 he was able to point to the research
of Oswald Heer, Saporta, and others as pro-
viding fossil evidence from Arctic Tertiary
flora to support his hypothesis.
Thus Gray, a botanist who knew little
geology but only understood its implica-
tions, provided a secure base for a Dar-
winian geology in America even before the
publication of the Origin of species. He
ranged descent with modification in the
organic scale alongside the geologic record
and found in their coincidence a key to the
present distribution of organisms. That
Agassiz’s whole conception of nature dis-
appeared so promptly from American sci-
ence, even among his own students, must
be credited largely to Gray. At the same
time, the equally rapid triumph of Agassiz’s
Ice Age theory received from the botanist
a marked impetus. The Darwinian way of
looking at the relation of geology and biol-
ogy became common coin in America among
geologists who never cited Gray in their
publications. The very pervasiveness of this
fundamental shift made it more anonymous.
WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. 7
Lest this sweeping conclusion be set down
as the circumstantial adulation of a biogra-
pher, let me call your attention to a signifi-
cant piece of contemporary evidence.’ Of
all those who commented on Gray’s career
at the time of his death in 1888, the one
who most fully plumbed the significance of
his introduction of organic evolution into
geology was Lester Ward. As a paleobota-
nist, Ward is under a professional shadow
because he spent so much of his time and
intellect on sociology. But in 1888 Ward was
speaking from the headquarters of Ameri-
can geology. As paleobotanist at the U.S.
Geological Survey he was the fellow worker
of John Wesley Powell, Gilbert, Clarence
Dutton, and the rest.
Ward felt that “history will doubtless
fully bear out the statement that, whether
we look at England or to the United States,
no man has done as much to remove appre-
hension from, and inspire respect for Dar-
winism, and therefore really to help its tri-
umphal march, as the modest American
botanist, Dr. Asa Gray.” Concerning Gray’s
Sequoia and its history, Ward was even
more specific. “Although possessed _ of
scarcely any of the abundant facts of pale-
ontology now known in support of his views,
he saw with unerring ken and portrayed
with a precision which had defied subse-
quent criticism, all the steps in the weary
pilgrimage of these giant denizens of the
Sierras, as they were driven southward by
the advancing ice sheet, or lured northward
by the return of cosmical summer... and he
saw how, in this protracted and unequal
struggle with the elements, this grand race
of beings...had been gradually decimated
in number and circumscribed in habitat...”
The idealist and catastrophic views of
Agassiz, although not the influence of his
magnetic personality, had so completely dis-
appeared by 1888 that only a few could rec-
ognize in Gray a major actor at a crucial
juncture in the history of science, a deft and
able theoretician who with one thrust of his
polished stiletto of a pen—the phrase is
Darwin’s—deflated one view of nature and
aided in the substitution of another.
‘Warp, Lester F., Asa Gray and Darwinism.
New Monthly Mag., August 1888: 85-92.
Juty 1959
WILSON: DARWINIAN NATURAL SELECTION Do
Darwinian Natural Selection and Vertebrate Paleontology
By JoHn A. Wiuson, University of Texas
The close correlation between form and
function as seen by the vertebrate paleon-
tologists in North America prevented the
adoption of Darwin’s proposal of natural
selection as the primary operating force in
evolution. This resulted in a schism between
paleontologists and neontologists that did
not close until the 1940’s. Cope in the im-
mediately post-Darwin period led in the
formation of a Neo-Lamarckian school to
which most North American vertebrate pa-
leontologists belonged. All the members of
this school were enthusiastic supporters of
evolution and their contributions furnished
an enormous amount of the paleontologic
evidence for evolution. But it was this pa-
leontologic evidence consisting of oriented
sequences of mammalian phylogenies that
prevented their accepting the randomness
of Darwinian natural selection as the pri-
mary operating force.
A few quotations will, I hope, substanti-
ate my thesis.
In North America Joseph Leidy was the
most prominent vertebrate paleontologist in
the Darwinian period. The Origin of species
did not fall on infertile ground; Leidy had
already in 1848 expressed earlier a general
belief in evolution:
The study of the earth’s crust teaches us that
very many species of plants and animals became
extinct at successive periods, while other races
originated to occupy their places. This probably
was the result, in many cases, of a change in ex-
terior conditions incompatible with the lfe of
certain species and favorable to the primitive
production of others... There appears to be but
trifling steps from the oscillating particles of in-
organic matter to a bacterium; from this to a
vibrio, thence to a monas, and so gradually up
to the highest order of hfe! The most ancient
rocks containing remains of living beings indi-
cate the contemporaneous existence of the more
complex as well as the simplest of organic forms;
but, nevertheless, life may have been ushered
upon the earth, through oceans of the lowest
types, long previously to the deposit of the old-
est paleozoic rocks as known to us.
It will be seen from this quotation that
Leidy certainly had a concept distinctly
above that of the “scale of nature.” He be-
lieved in the extinction of forms, of course,
and plainly expresses the germ of evolution,
even the development of living matter from
nonliving matter.
Leidy, one of the most competent verte-
brate paleontologists North America has
produced, confined most of his paleontologi-
cal writing to the description of new types.
While he firmly believed in the doctrine of
descent, he refrained from theorizing as to
the manner in which such descent came
about. In many ways this is understandable,
since Leidy’s period of work coincides with
the beginning of the discovery of the verte-
brate paleontological treasures of the West.
The vast tonnages of specimens and the
discovery of the sedimentary sequence of
the Tertiary did not come until Marsh and
Cope took over the field. At any rate, Leidy
did not theorize or speculate in print con-
cerning the Darwinian proposal of natural
selection.
Of his two successors Marsh and Cope,
the latter became the leader of a group
which until quite lately had _ survivors
known as the Neo-Lamarckists. Of the two
Cope wrote more extensively and expressed
his ideas on natural selection more freely
than did Marsh. However, from the few
statements on this subject made by Marsh
it is quite obvious that he was a member of
the same school. In Marsh’s vice-presiden-
tial address before the American Associa-
tion for the Advancement of Science meeting
at Nashville, Tenn., on August 30, 1877, he
says:
As a cause for many changes of structure in
mammals during the Tertiary and Post-Tertiary,
I regard as the most potent, natural selection, in
the broad sense in which that term is now used
by American evolutionists. Under this head I in-
clude not merely Malthusian struggle for life
among the animals themselves, but the equally
important contest with the elements and all sur-
rounding Nature. By changes in the environ-
ment, migrations are enforced, slowly in some
cases, rapidly in others, and with change of lo-
cality must come adaption to new conditions, or
232 JOURNAL OF THE
extinction. The life history of Tertiary mammals
illustrates this principal at every stage, and no
other explanation meets the facts.
I think it very likely that Marsh herein re-
ferring to “natural selection, in the broad
sense in which that term is now used by
American evolutionists” is referring to the
Neo-Lamarckian school as conceived by
Cope, but about this I cannot be certain.
In Marsh’s retiring presidential address
before the same organization at Saratoga,
N. Y., August 28, 1879, Marsh is not even as
explicit as he had been the previous year.
He states:
Just 20 years ago, science had reached a point
when the belief in “special creations” was deter-
mined by well established facts, slowly accumu-
lated. The time was ripe. Many naturalists were
working at the problem, convinced the Evolution
was the key to the present and the past. But
how had Nature brought this change about?
While others pondered, Darwin spoke the magic
word—“‘Natural Selection,” and a new epoch in
science began.
A little farther along in the address Marsh
continues:
The publication of Charles Darwin’s work on
the “Origin of Species,”” November, 1859, at once
aroused attention, and started a revolution which
has already in the short space of two decades
changed the whole course of scientific thought.
The theory of “Natural Selection,” or as Spencer
has happily termed it, the “Survival of the Fit-
test,” had been worked out independently by
Wallace, who justly shares the honor of the dis-
covery. We have seen that the theory of evolu-
tion was proposed and advocated by Lamarck,
but he was before his time. The anonymous au-
thor of the “Vestiges of Creation,” which ap-
peared in 1844, advocated a somewhat similar
theory which attracted much attention, but the
belief that species were immutable was not sensi-
bly affected until Darwin’s work appeared.
Beyond Marsh’s magnificent contribu-
tions to the documentation vertebrate pale-
ontology furnishes to evolution these are the
only two short statements in which he ap-
pears to give forth his views concerning
natural selection. Neither is_ sufficiently
complete to furnish any great light concern-
ing Marsh’s view on the mechanics of evolu-
tion, and although he does hp service to
natural selection the telling remark in the
first quote: “natural selection, in the broad
sense in which that term is now used by
American evolutionists,’ seems to make him
a follower of the Neo-Lamarckists school.
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, NO. 7
Cope, on the other hand, left absolutely
no question concerning his views on the
mechanics of evolution. More than 50 titles
concerning evolution are cited by Osborn in
his biography of Cope. From these it is nec-
essary to choose only one as illustrative of
the later concepts of Cope with regard to
natural selection. I quote from The primary
factors of organic evolution, 1896, on p. 474:
That natural selection cannot be the cause of
the origin of new characters, or variation, was
asserted by Darwin'; and this opinion is sup-
ported by the following weighty considerations:
1. A selection cannot be the cause of those
alternatives from which it selects. The alterna-
tives must be presented before the selection can
commence.
2. Since the number of variations possible to
organisms is very great, the probability of the
admirably adaptive structures which character-
ized the latter, having arisen by chance, is ex-
tremely small.
3. In order that a variation of structures shall
survive, 1t 1s necessary that it shall appear simul-
taneously in two individuals of opposite sex. But
if the chance of its appearing in one individual is
very small, the chance of its appearing in two
individuals is very much smaller. But even this
concurrence of chances would not be sufficient to
secure its survival, since it would be immediately
bred out by the immensely preponderant number
of individuals which should not possess the varia-
tion.
4. Finally, the characters which define the or-
ganic types, so far as they are disclosed by Pale-
ontology, have commenced as minute buds or
rudiments, of no value whatever in the struggle
for existence. Natural selection can only effect
the survival of characters when they have at-
tained some functional value.
In order to secure the survival of new char-
acter, that is, of a new type of organism, it is
necessary that the variation should appear in a
large number of individuals coincidentally and
successively. It 1s exceedingly probable that this
is what has occurred in past geologic ages. We
are thus led to look for a cause which affects
equally many individuals at the same time, and
continuously. Such causes are found in the chang-
ing physical conditions that have succeeded each
other in the past history of our planet, and the
changes of organic function necessarily produced
thereby. (Italics mine.)
Cope and Marsh were shortly followed by
Scott and Osborn as leaders in the field
of vertebrate paleontology in the United
States. Scott in 1926 in his book entitled The
theory of evolution (from the Westbook
Lectures delivered before the Wagner Free
"Origin of species, ed. 1872, p. 65.
“Juxx 1959
Institute of Science, Philadelphia) on page
_ 151-152 has this to say:
OF late years, a host of experimenis have been
_ performed upon animals, the larger number of
them with the object of determining whether
few characters, acquired during the liciime of
_ the parenis, can. under any circumsiances, be
transmitted io the ofispring. This is one oi the
most hotly dispuied questions of modern biology
and our whole conception of the efficient factors
which have brought about evolution hinges upon
the answer io this question. The same exper-
menis are mierpreied m diameirically opposite
_ senses by different writers according to their pre-
_ disposition and general pomt oi view. Ai the
present imme, ii 1s probable that a very con-
siderable majority of zoologisis and boianisis,
especially m this couniry, are meclined io deny
the hereditary iramsmission of characiers ac-
quired m the posi-embryonic life of the parents,
but the problem is still far from definite solution.
Important as this problem is im an atiempi io
. explain evolution and the manner in which it has
_ been efiecied, i has no bearmg upon the que>
tion which I have been endeavoring io answer
m these lectures, as to the probable truth of the
_ evolutionary theory. Thai theory is held quite
as strongly by those who affirm the transition of
acquired characters. Whatever interpretation be
put upon the significance of the expermenis.
presenily to be mentioned. as io the problem of
acquired characters, they do, ai all events, show
that hereditanly transmissible modifications may
be artificially produced m both animals and
planis.
_ Seott proceeds im pages following this
_ quotation to enumerate experimental evi-
dence of the inheritance of acquired charac-
_ teristics as Cope had done before. In Scott’s
Tevision of The history of land mammals in
the Western Hemisphere oi 1937 his diseus-
sion oi evolution is somewhat modified:
While the theory of evolution is Ss accepied by
Naturalists with subsiantial unanimity. there is
great divergence oi opinion among them con-
cermmg ithe efficient causes of the marvelous
transformations which the fossils reveal. Darwin’s
theory oi Naiural Selection does offer an ex-
planation, though he himself was iar from ai-
tmbutime io that agency the exclusive importance
which his modern followers (“Neodarwmians’)
asembed to 1t_ He also attached much significance
to the direct action of the environment and io
the effects of use and disuse and, toward the end
of his hie, he was mclimed io the belief that he
had underestimaied these factors and overesii-
mated Naiural Selection. According io the mod-
em version oi Darwim’s theory, random varia-
tions supplied the maierial from which Naiural
Selection picks the favorable ones, just as does
the breeder of animals or planis m esiablishing
WILSON: DARWINIAN NATURAL SELECTION
233
a new variety. Natural Selection, m Darwin’s
view, was the exact analogue oi the breeders
artificial selection.
This is not the place to present the argumenis,
pre and con, over this famous theory, which is
sull upheld by many high authorities, further
than io say that, m the writer’s opmion the ob-
served facts oi parallelism and convergence are
fatal to 1%t. The chances than random variations
should bring about the astonishimg lkeness be-
tween the marsupial Thylacosmilus, the carnivore
Eusmilus, and the ungulaie Umiathertum, or the
conversion of hoois mio claws m three unrelated
groups, are mathematically ml. Few paleoniolo-
gists have felt that the direct, unswervimg, sitep-
by-siep development of the ammoniies studied
by von Waagen and Neumayr, or of the many
mammahan series, which have been described m
the precedmg chapiers, were satisiacionly ac-
counted for by Natural Selection. In giving up
this theory, it must be admitied, there is nothing
to put m iis place. Darwm’s theory does offer
an explanation of the evolutionary process and
this no other theory does, but the question re-
maims: is it an adequate explanation?
The answer to Scott’s question so far as
the vertebrate paleontologists were con-
cerned was no. It was certainly inadequate
for Osborn because he proposed a further
alternative, aristogenesis, which was vitalist
in-its essential form although Osborn denied
this.
Vertebrate paleontology is an observa-
tional and deseriptive science, and the North
American workers were busily observing
and describing the spectacular material dis-
covered with the opening of the West. Ge-
netics, an experimental science, was born a
hitle later, and during the 1920’s and 1930's
its workers were busily acquiring experi-
mental proof of the mechanics of evolution.
During this period of the marshaling of the
evidence in both fields the chasm between
them grew.
The turning pomt when the chasm began
to narrow goes back, in my opinion, only to
the publication of J. Huxley’s Evolution:
The modern synthesis in 1942. The chasm
closed, so iar as vertebrate paleontologists
are concerned (with some exceptions) only
mn 1944 with the publication of G. G. Simp-
son’s Tempo and mode in evolution. Within
the synthesis Darwinian natural selection
has been modified somewhat. With this
modification both the oriented and random
aspects of evolution are satisfactorily ex-
plamable, at least for the present.
234
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
Impact of the Development of Photogrammetry upon Geology
By Davin LanpEN, U.S. Geological Survey
The modern specialized scientist, 1m-
mersed in the particular problems of his own
field, needs to raise his head at opportune
times and see what is going on in other
fields. What he sees when he looks about is
a vast complex of progress In many scien-
tific disciplines. This progress offers both a
challenge and an opportunity. The scientist
can often save himself costly and tedious
work by discovering the useful tools scien-
tists have already developed in other fields
and adapting them to his special purposes.
In the marriage of the disciplines of pho-
togrammetry and geology, we have an excel-
lent illustration of this point. Scientists, op-
erating in the specialized field of geology,
have recognized the challenge of photogram-
metry and have seized the opportunity to
espouse it. The linking of photogrammetry,
the science of making reliable measurements
by means of photographs, to the science of
geology was for many years a slow process;
only in the last decade has it experienced a
rapid acceleration.
EARLY USE OF PHOTOGRAPHY FOR RECORDING
SCIENTIFIC DATA
As iar back as 1853, a famous scientific
expedition, under the leadership of Col.
John C. Frémont, employed a photographer
to obtain reliable records of geologic and
geographic features encountered on a route
of exploration. This expedition set out from
Westport, Mo., with the objective of cross-
ing the Rocky Mountains near the thirty-
eighth parallel, in quest of a direct route to
California. A key member of Frémont’s
party was Solomon N. Carvalho,! a daguer-
reotypist and artist from Baltimore, who
was the first official photographer to ac-
company a Western expedition. In his ac-
count of the journey, Incidents of travel
and adventure in the Far West (New York,
1858), Carvalho describes the intricate
* WaLLace, E.S., The great reconnaissance: 126-
137. Little, Brown & Co., 1955.
process of mixing chemicals and preparing
daguerreotype plates while standing waist
deep in snow with the thermometer register-
ing 20° below zero.
Between 1854 and 1860 at least four more
exploration parties employed photographers,
with varying degrees of success. The out-
break of the Civil War halted expeditionary
photography for the duration. Following the
cessation of Civil War hostilities, several
separate Government-organized geological-
survey expeditions were created to further
knowledge concerning national resources in
the West. The most important of these were
the Hayden, King, Wheeler, and Powell sur-
veys; each of these parties included a pho-
tographer. The photographic work of these
survey expeditions was considerably more
successful than that of the earlier expedi-
tions, owing largely to three factors: the
superiority of the wet-plate process over the
daguerreotype process, the availability of
commercially prepared collodion, and the
experience acquired by the photographers
during the Civil War years. An important
product of these surveys, made between
1865 and 1880, was the large amount of ac-
curate geologic and geographic data col-
lected, which were represented largely in the
form of maps, with photographs serving to
illustrate geologic features in detail. Robert
Taft gives a list of photographers of this
period.”
The growing recognition of the value of
photography in recording scientific data
such as that gathered by the early western
surveys led to the formation, in 1890, of a
Committee on Photographs of the Geologi-
cal Society of America. In the first report of
this committee® we see the first known ref-
erence to a new activity: photogeology. The
object of the new movement, according to
the committee report, was ‘‘to make a
photo-geologic survey, and to secure for the
> Tart, Ropert, Photography and the American
scene: 308. 1938.
* Geol. Soc. Amer. Bull. 2: 616-6—30. 1890.
Juty 1959 LANDEN:
Society a national collection of photographs
illustrating the geology of the country.” The
stated uses for such a collection were “first,
to furnish to teachers better illustrations in
teaching geology, and second, to furnish to
investigators
study.”
material for comparative
=
\
Fic. 1—Panoramic camera. The first panoramic
camera used by the Geological Survey was con-
structed by C. W. Wright and F. E. W right in 1904.
Later, beginning in 1910, J. W. Bagley improved
this camera and extended its use in a program for
producing topographic maps.
PHOTOTOPOGRAPHIC SURVEYS
To understand properly the intensive
mapping activities by field parties inter-
ested primarily in geology, it 1s important
to realize that mapping was considered to
be a means to an end. The object was to
facilitate the understanding of geology;
maps were needed as a base on which geo-
logic data could be plotted.
In 1904, two members of the U. 8. Geo-
logical Survey staff, C. W. Wright and F. E.
Wright,* pioneered the use of photogram-
metric methods for the development of topo-
graphic maps needed specifically as a base
for geologic studies. The Wrights, operating
in an area of Alaska completely devoid of
maps, devised a spring-driven, revolving,
panoramic camera (Fig. 1) which afforded
a very large field of view. Level bubbles and
scales fitted to the camera provided a basis
* LANDEN, Davin, History of photogrammetry in
the United States. Photogrammetric Eng. 18(5):
857. December 1952.
DEVELOPMENT OF PHOTOGRAMMETRY
239
for photogrammetric measurements. Begin-
ning in 1910, James W. Bagley, a topo-
graphic engineer of the Geological Survey,
developed and improved the panoramic
camera with the object of extending its use
to the Survey’s regular program of produc-
ing general-purpose topographic maps. Bag-
ley also designed a panoramic photoalidade
(Fig. 2) which enabled the operator to use
the photograph for the determination of di-
rections and elevation differences in the
same manner in which a topographer oper-
ates the telescopic alidade on a plane table
in the field. This afforded a basis for draw-
ing planimetry and contours in the con-
struction of a map.
Meanwhile, the use of photographs for
mapping had been stimulated by two im-
portant advances: (1) the discovery in
1892 by F. Stolze,®> in Germany, of the prin-
ciple of the stereoscopic floating mark, and
its practical development later, and (2) the
advent of the airplane. The floating mark
principle offered a satisfactory method of
making measurements in the three-dimen-
sional ‘“‘model” observed when overlapping
photographs are viewed stereoscopically.
The airplane offered an excellent platform
on which a camera could be moved rapidly
from exposure station to exposure station;
furthermore, aerial photography offered a
practical means of obtaining a vertical view
of the terrain, with its inherent superiority
over terrestrial photography, for mapping
purposes. These events opened the way to
the widespread use of aerial photographs in
stereoscopic plotting equipment; maps could
now be produced by continuous plotting in-
stead of the old tedious point-by-point
methods. The two advances also accelerated
the development of a large number of accu-
rate stereoscopic plotting instruments for
mapping. Eventually, it was found that, in
general, maps of comparable accuracy could
be obtained at lower costs with the new
aerophotogrammetric techniques than with
the older ground methods.
In 1916, after studying the work of
Scheimpfiug, the Austrian inventor of a mul-
tiple-lens camera, Bagley and another mem-
> Von Gruser, O., Photogrammetry: 163. Ameri-
ean Photographic Publishing Co., Boston, 1932.
THE
JOURNAL OF
WASHINGTON ACADEMY
OF SCIENCES VOL. 49, NO. 7
Fig. 2.—Panoramic photoalidade.
ber of the Geological Survey, J. B. Mertie,
undertook the task of developing a tri-lens
camera (Fig. 3). Meanwhile, another col-
league, F. H. Moffit, designed a transform-
ing printer (Fig. 4) as a companion piece to
the camera. After Bagley was commissioned
a major in the Engineer Reserve Corps, in
1917, he continued his interest in phototopo-
eraphic mapping. The first aerial photo-
graphs taken with the tri-lens camera were
made at Langley Field in 1917-1918 with
the cooperation of the Air Service. This
event marks the actual beginning of aerial
surveying in the United States; the tests led
to a program of producing aeronautical
charts of the terrain between flying fields.
Multiple-lens cameras are in use for ob-
taining mapping photography to this day,
notably the nine-lens camera of the U. 8.
Coast and Geodetic Survey which has been
in use since 1936. For the great majority of
modern photogrammetric mapping projects,
Fic. 3.—Tri-lens camera. Designed in 1916-17 by J. W. Bagley, with the assistance of J. B. Mertie
and F. H. Moffit, and developed by the Corps of Engineers, U.S. Army. Later, cameras of this general
design were built with 4- and 5-lens combinations.
JuLYy 1959 LANDEN: DEVELOPMENT OF PHOTOGRAMMETRY UB
Fic. 4.—Transforming printer. Designed by F. H. Moffit in 1916-17, this transforming printing-
camera was used to project the side negatives of the tri-lens camera so as to bring the photographs to
the same plane and scale of the center photograph.
Fic. 5.—Plan view of the stereoautograph.
JOURNAL OF THE
however, aerial photography is obtained
with a single-lens camera or a combination
of single-lens cameras.
AMERICAN USE OF STEREOSCOPIC
MAPPING INSTRUMENTS
In the early 1920’s the Brock and Wey-
mouth Co. of Philadelphia designed and
built the first American stereoscopic plot-
ting equipment, and in 1923 they compiled
the first topographic map produced commer-
cially on such a machine in the United
States.
Meanwhile, in 1921, a semiautomatic
plotting machine, the stereoautograph (Fig.
5), was received (on loan) from Germany
for testing by the Geological Survey’s newly
established Section of Photographie Map-
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 7
ping. This instrument employed terrestrial
photographs only, and while workable, did
not prove to be economical. A second in-
strument, the Hugershoff aerocartograph
(Fig. 6), was imported from Germany by
the Geological Survey in 1927; this was the
first precise stereoscopic plotting instrument
utilizing aerial photography to be owned by
the United States Government.
Although the aerocartograph produced
satisfactory contour maps, its initial cost
was high and it was mechanically complex.
The multiplex aeroprojector, manufactured
by Zeiss in Germany, overcame these disad-
vantages, and in 1935 the Geological Survey
purchased its first multiplex equipment.
(See Fig. 7, Principle of multiplex.) Once
the value of the multiplex was demon-
Fic. 6.—The Hugershoff aerocartograph. The (German) aerocartograph is a complex stereoplotting
instrument using the optical-mechanical projection principle. While it is capable of producing good
maps from either vertical or terrestrial photographs, its use, together with narrow-angle photographs is
now considered obsolete, as it was replaced by more modern wide-angle plotting instruments.
JuLy 1959
strated, it was put into widespread use, first
in topographic mapping in the Tennessee
River Valley, then in the topographic map-
ping of other areas throughout the country.
During World War II this equipment was
used in carrying out formidable strategic
mapping assignments of high importance.
LANDEN: DEVELOPMENT OF PHOTOGRAMMETRY 239
Following World War II, two important
new plotting instruments were developed by
the Geological Survey: the Kelsh plotter
(Fig. 8) and the ER-55 plotter (Fig. 9).
Both of these instruments embody the gen-
eral principle of the multiplex but have fea-
tures which result in greatly superior per-
=
Saves
_—~ “MANUSGRIPT
__ MAE
Fie. 7.—Principle of multiplex.
“I
240 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, NO.
Fig. 8.—Kelsh plotter. Conceived by H. T. Kelsh in 1948, the Kelsh plotter was developed by him in
1947 and later by members of the Geological Survey technical staff. The main advantages of this plotter
over previous double-projection plotters are the swinging light source; correction, when necessary, of
cou lens distortion by means of an arm-and-cam arrangement; and contact (negative) size diaposi-
tive plates.
Fic. 9.—ER-55 plotter. Two ER-55 optical projectors are shown mounted on a standard
multiplex supporting frame. The projectors are arranged for convergent photography.
Juty 1959
formance. Commercial versions of these two
instruments are now the leading American-
made instruments of this type on the Ameri-
can market.
In addition to the American-made instru-
ments, numerous foreign-made instruments
are to be found in use for high-precision
topographic mapping in this country. (See
Fig. 10, Wild plotter.) Among these are
numerous instruments made by Zeiss Aero-
topograph (Germany), Henry Wild (Swit-
zerland), Officine Galileo (Italy), and Ot-
tica Mecanica Italiana (Italy). Despite
their complexity and high first cost, these
instruments find an important use because
of their versatility and increased capability.
RATE OF PROGRESS OF THE UNITED STATES
MAPPING PROGRAM
In view of the need for good topographic
maps on which to plot geologic data, the
LANDEN: DEVELOPMENT OF PHOTOGRAMMETRY
241
rate of progress of the United States map-
ping program is of vital importance to the
geologic profession. The lack of a suitable
map of the area of interest can delay a ge-
ologist’s operations by weeks or months.
Fortunately, Congress has recognized the
vital importance of the national topographic
mapping program and has, in recent years,
appropriated the funds needed to permit an
increase of several times in the annual map
output as compared to that of a decade ago.
At the current rate, about 100,000 square
miles of U.S.G.S. quadrangle maps at the
scales of 1:24,000 and 1:62,500, are com-
pleted annually.
As of 1958, the Geological Survey dis-
tributes some 20,000 separate topographic
maps produced by Federal agencies. These
maps are published at various scales rang-
ing from 1:24,000 to 1:250,000 (see Fig. 11,
Status of topographic mapping).
Fre. 10.—Wild autograph A-7 (Swiss). The autograph is a complete stereoplotting instrument of the
mechanical projection class. The instrument can be used for control extension by aerotriangulation as
well as for map compilation. Despite the initial high cost and complexity, its versatility and high order
of accuracy make it suitable for a wide range of special projects, with long-range economies in opera-
tion.
242 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, NO. 7
Fic. 11.—Status of topographic mapping (at scales ranging from 1:24,000 to
1:250,000) (January 1958).
INDEX TO TOPOGRAPHIC MAPS OF THE
UNITED STATES
PUBLISHED AT THE SCALE OF 1 250 000
NOVEMBER 1958
[] eustisneo
i=
BLACK AND WHITE ADVANCE PRINT_OF UNEDITED BAS
*= COMPILATION. 1:250,000 SCALE, AVAILABLE AT $3.50
(SHOWS CULTURE, DRAINAGE, AND CONTOURS.
{es BUT NO NAMES).
Fre. 12.—Index to topographic maps of the United States, published at the
scale of 1:250,000 (November 1958).
JuLty 1959
Quadrangle maps at a scale of 1:250,000
are also available, in a preliminary series,
for the entire State of Alaska. In addition,
more detailed mapping of a type that may
be termed ‘‘adequate” is already available
for about 29 percent of Alaska’s tremendous
land area. When Arizona, the last State to
be admitted previously, entered upon state-
hood in 1912, only 1 percent of its area was
adequately mapped.
The new series of 1:250,000-scale topo-
graphic maps of the United States, origi-
nally prepared by the Army Map Service,
but now being published in civilian editions
by the Geological Survey, is of particular
interest because it provides nearly complete
coverage of the country. (See Fig. 12, Index
to 1:250,000-scale maps.) In addition to the
1:250,000-scale maps themselves, geologists
have access to the rather recent high-alti-
tude aerial photography and other source
materials used in preparing the maps. These
materials, obtainable from the Geological
Survey, may provide detailed information
in areas of interest not covered by larger-
scale quadrangle maps. Much of this topo-
eraphic mapping is a result of the use of
high-altitude aerial photography flown at
heights as high as 36,000 feet.
PHOTOGRAMMETRY AND ACCURACY STANDARDS
Not only does photogrammetry provide a
means of increasing the rate of topographic
mapping but it also provides the means
whereby accuracy standards can be estab-
lished on a practical basis for maps of all
types of terrain.
The practical value of geologic informa-
tion, however well catalogued, may be seri-
ously limited if the location of the items
described is not accurately known. It is
therefore quite important to the geologist
that he recognize the characteristics of the
topographic map on which geologic data is
to be plotted, with respect to the accuracy
of the positions and elevations of features
shown on the map.
The idea of producing topographic maps
conforming with specified standards of ac-
curacy has long been known, and indeed
many maps meeting rigid specifications have
been prepared over the years, by classical
methods, where such procedure was eco-
LANDEN: DEVELOPMENT OF PHOTOGRAMMETRY
243
nomically justified. It was not until the ad-
vent of photogrammetric techniques and
parallel advances in related field-survey
procedures, however, that attainment of
standard accuracy in nearly all of the quad-
rangles of the National Topographic Map
series became economically feasible. Since
the early 1940’s, most topographic maps
produced by or for the Federal mapping
agencies have been prepared to comply with
standard specifications for horizontal and
vertical accuracy. Maps made in accordance
with these specifications are so designated
by the following statement printed on the
bottom of the sheet: “This map complies
with National Map Accuracy Standards.”
This statement assures the geologists, for-
ester, engineer, or other user that the map
has been made under carefully controlled
conditions and that the information given
can be relied on within the provisions of the
accuracy specifications.
SPECIAL-PURPOSE MAPS
The general-purpose topographic maps
produced by the Federal agencies cannot be
expected to meet all the specialized require-
ments of all the map users with respect to
scale, contour interval and map content. To
meet such requirements, photogrammetry
offers a valuable means for producing spe-
cial-purpose maps at relatively low cost.
Several government agencies, having spe-
cialized map requirements for studies in ge-
ology, forestry, agriculture and other fields,
maintain their own photogrammetric facili-
ties for producing the needed special-pur-
pose maps. Likewise, a number of commer-
cial organizations, such as oil companies,
operate photogrammetric installations for
producing needed geologic and other scien-
tific data.
The organization or individual that needs
special-purpose maps but is not in a posi-
tion to operate photogrammetric facilities
may wish to consider the services of the
various commercial firms that are equipped
to perform such tasks. Firms of this type are
to be found in all parts of the United States;
in general, they operate their own photo-
graphic aircraft and photogrammetric plot-
ting equipment.
244 JOURNAL OF THE
SOME EXAMPLES OF SPECIAL-PURPOSE
MAPPING
Some representative examples of the use
of photogrammetric techniques in geology
are shown by the following illustrations:
a. A structure contour map (Fig. 13)
b. An isopachous map (Fig. 14)
c. A compilation of photogeology and
surface geology is shown in Fig. 15—a pho-
togeologic map of the Notom-15 quadrangle,
Garfield County, Utah. The only available
control information was outside the area
mapped, and all the photogeologic data was
derived from photographs. The structure
contours shown are based on measurements
obtained with a multiplex plotter.
Two additional examples of large-scale
special-purpose mapping further illustrate
the use of photogrammetry for the solution
of scientific and engineering problems:
d. A beach-erosion study (Fig. 16). A
large-scale map of a heavily eroded beach
at Gay Head, Massachusetts, was compiled
from aerial photographs flown at 1,500 feet
above ground. The scale of the required map
was 1:600 (50 feet to the inch). Two-foot
ONE MILE
Fic. 13—Portion of a structure contour map.
This figure shows an enlarged portion of a structure
contour map of Discovery Anticline in northern
Alaska (U. S. Geol. Surv. Spec. Rep. 42, pl. 1,
1:40,000 scale). Measurements that were used to
develop the structure contours were made from
aerial photographs with a stereometer. (A structure
contour is a contour line drawn through points of
equal elevation on a stratum, key bed, or horizon,
in order to depict the attitude of the rocks.) The
contour interval is 200 feet, and the reference
datum is approximately sea level.
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
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Fic. 14—Example of isopachous map. Portion
of an area in Monument Valley, northeastern Ari-
zona, showing isopach intervals of 10 feet. (Iso-
pachous line are contour lines which show the
thickness of a formation.) A Kelsh plotter was used
to measure the thickness of the formation and to
plot the location of these measurements on a base
map.
contours were plotted with the Kelsh plot-
ter. It is planned to remap the area chrono-
logically on a yearly basis to record the rate
of erosion and its relation to the topography
and resistance of surficial materials.
e. Photogrammetric mapping of sand
beds in a hydraulic test flume® (Fig. 17). In
connection with a wide range of studies of
phenomena relating to the problems of wa-
ter shortages and soil erosion, an unusually
large-scale map was made of sand dune con-
figurations, resulting from flowing water in
a hydraulic test flume. Contour maps (Fig.
18) were prepared at 1:2 scale (half-size)
with a contour interval of 0.01 foot, from
photographs taken at a height of 65 inches
(5.4 feet). A Wild A-8 plotter was employed.
The cyclical recurrence of ridges and de-
pressions in the sand dune pattern is plainly
evident. Wavelengths and amplitudes of the
configuration can be easily determined. This
map was tested and was found to comply
with standard-accuracy specifications.
SOME EXAMPLES OF PAPER-PRINT PLOTTERS
Many of the less-exacting tasks required
in the plotting of data compiled on or from
photographs can be performed with less
*THompson, M. M., Photogrammetric mapping
of sand beds. Photogrammetric Eng. 24(3): 468
475. June 1958.
JuLy 1959
LANDEN: DEVELOPMENT OF PHOTOGRAMMETRY
245
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Fig. 15.—A compilation of photogeology and surface geology. Portion of Notom-15
quadrangle, Garfield County, Utah.
costly and less complicated instruments than
those required for high-precision topo-
graphic mapping. These instruments are
generally characterized as “paper-print
plotters,’ as contrasted with the precision
mapping plotters which invariably use
glass-plate diapositives (positive photo-
graphs printed on glass instead of on paper).
Among the more popular paper-print stereo-
scopic plotters are the Kail radial plani-
metric plotter, the K.E.K. Plotter, and the
Ryker-Wernstedt-Mahan plotter. (See Fig.
19, K.E.K. plotter.)
Another simple instrument, the sketch-
master, based on the camera lucida princi-
ple, permits the transfer of detail from the
photograph to the map. (See Fig. 20, Verti-
eal sketchmaster. )
Until recently, the paper-print plotters
constituted the prevailing type of instru-
ment for use in photo-geologic operations.
Lately, however, there has been an increas-
ing use by geologists of modern precision
stereoplotting instruments, such as the
Kelsh plotter, for making quantitative
measurements, for transferring geologic data
from the photographs to the map, and for
photointerpretation.
SOME EXAMPLES OF SPECIAL-PURPOSE PHOTO-
GRAMMETRIC INSTRUMENTS FOR MAKING
QUANTITATIVE MEASUREMENTS
In addition to providing a variety of gen-
eral-purpose and _ special-purpose maps,
photogrammetry has already provided a
large number of special instruments for
making quantitative measurements that are
useful in scientific studies. Geologic map-
ping, for example, employs basic measure-
ments such as distance, elevation, or direc-
tion, as intermediate steps in the solution
of some larger problem. Some of the instru-
ments described herein can be used to ob-
tain measurements such as dips, strikes,
thickness of beds, profile elements and the
like; measurements heretofore largely made
246
on the ground. The forester, for example,
‘an use photogrammetric measurements for
obtaining heights of trees; the hydrologist
can make use of these instruments for wa-
tershed and gradient studies; the engineer,
for example, makes use of these measure-
ments in highway design and construction,
41° 21° 00° +
GAY HEAD,
MASS.,
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Scale | 600
Contour Interval 2 Feet
Compiled by Branch of Special
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June 1958
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JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
etc. A few of these special-purpose photo-
grammetric measuring instruments are de-
scribed below:
The parallax-bar, or stereometer (Fig. 21)
is both the oldest as well as the most simple
photogrammetric instrument available. It is
used for measuring parallax differences.
Fic. 16.—Large-scale map for beach erosion study, Gay Head, Mass. Scale 1:600; contour
interval 2 feet. Made with Kelsh plotter.
JuLY 1959 LANDEN: DEVELOPMENT OF PHOTOGRAMMETRY 247
(The parallax of an object is its apparent
displacement due to its being viewed from
two different viewpoints.) By measuring the
horizontal separation between individual
dots placed at the bottom of an object to be
measured, then measuring the separation,
or parallax, at the top of the object, the dif-
| ference between the two parallax readings
can be directly related to the height of the
object. With the stereometer shown parallax
can be measured to hundredths of a milli-
meter.
The photogrammetric dip angle indicator
(Fig. 22) is a device for making direct meas-
urement of dip, or angle of slope, in the
Fig. 17.—Photogrammetric mapping of sand
beds in a hydraulic test flume. (The white spots
are heads of tacks used as vertical accuracy test Fic. 18—Contour map of sand beds compiled on
points. ) Wild A-8. Contour interval, 0.01 foot.
248 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, NO. 7
Fig. 19. _KEK (Kail, Elliot, King) plotter. The KEK nlotten consists of a stereoscope for viewing a
pair of photographs mounted upon two tables, a pair of floating marks scribed on glass disks, and a
plotting device attached to a pantograph. By raising or lowering the plate-carriers the floating mark is
placed in contact with the ground in the stereoscopic model so that planimetric detail can be plotted on
the map. Elevations are read on a drum scale linked to the plate-carriers. The floating mark can be set
to any desired contour interval and permits contouring when the photographs are well controlled. Since
the instrument is based on certain approximations and does not produce a geometrically true model, it
is not intended for precision work.
Fig. 20.—Vertical sketchmaster. This portable instrument based on the camera-lucida principle was
designed by J. L. Buckmaster of the U. 8. Geological Survey in 1931. By means of a mirror arrangement,
the sketchmaster permits the photograph and the plotting sheet to be viewed simultaneously, thus
making possible the transfer of detail from the vertical photograph to the plotting sheet. Adjustments
are provided for scale changes and approximate tilt correction.
JuLY 1959
LANDEN: DEVELOPMENT OF PHOTOGRAMMETRY
Fic. 21.—The parallax-bar, or stereometer.
stereoscopic model of a double projection
plotter. The surface of the platen shown is
eridded with suitable stereoscopic floating
marks. A vertical angle arc, passing through
a slot in the platen, is used for making di-
rect measurements of angles of slope. A
strike line can be plotted graphically, at
right angles to the plotted direction of dip.
A photogrammetric profile plotter’ (Fig.
23) is an instrument for plotting profiles di-
rectly from multiplex-type stereoplotting
equipment. Profiles are often used, in com-
bination with geologic data, to show geo-
graphically the inclination, structural rela-
tions and thickness of rock units at the sur-
face or subsurface of the ground. The pro-
file plotter plots the profile directly upon a
sheet of graph paper mounted in a vertical
plane.
ORTHOGRAPHICALLY RESTITUTED AERIAL
PHOTOGRAPHS
One of the important problems of the ge-
ologist working with aerial photographs is
how to relate, or transfer, information from
the photograph which is in a perspective
form, to a map which is in an orthographic,
or plan, projection.
A new photographic material that has
aroused much interest is the orthographi-
cally restituted aerial photograph. This new
photographic material is called an ortho-
photograph and the photogrammetric ma-
chine which produces it is called an ortho-
photoscope.®
*LanDEN, D., A photogrammetric profile plotter
for geologic use. Photogrammetric Eng. 22(5):
953-956. December 1956.
*“SoutHarD, R. B., Orthophotography. Photo-
grammetric Eng., June 1958.
The orthophotoscope (Fig. 24) employs
the anaglyphic principle to form a stereo-
scopic model under a double-projection ster-
eoplotter. The model is mechanically
scanned in contiguous strips by a moving
aperture which is controlled by an operator
to rise and fall while in stereoscopic contact
with the terrain being viewed. Photographic
detail, located by the intersection of ho-
mologous optical rays in true orthographic
position, is rephotographed upon a new
sheet of film placed directly under the mov-
ing aperture and rising and falling with it.
The film is sensitive only to the blue hght
of the red and blue rays forming the ana-
glyph. After the scanning is complete, the
film is removed and orthographic paper
prints are made (Fig. 25).
Fig. 22.—Photogrammetric dip (or slope)
indicator.
250 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, NO.
Fic. 23.—Photogrammetric profile plotter.
Fig. 24.—1956 model orthophotoscope with ER-55 projectors. The orthophotoscope, developed in the
research laboratory of the Geological Survey, under the direction of R. K. Bean, is an apparatus for
converting perspective photographs to the eauivalent. of arthographic photographs.
~I
Juty 1959 LANDEN: DEVELOPMENT OF PHOTOGRAMMETRY
iti
h (left) and an orthophotograph (right).
s of a perspective photograp
ked, while in the orthophotograph it is
In the perspective photograph the powerline appears to be croo
shown in its true, straight alignment.
Fig. 25.—Corresponding portion
252
Experience with orthophotographs by ge-
ologists shows that the photographic detail
is uniformly in position within nominal ac-
cepted tolerances. The orthophotograph fa-
cilitates the transferring of geologic details
from photograph to map. This can now be
done in a simple fashion by tracing; or, the
orthophotograph itself can be used as a
map.
A somewhat related photographic product
is called the photo-contour map.® This prod-
uct provides a topographic map whereon
elevations are shown by contours, while
planimetry is shown by photographie detail.
° Manan, R. O., The photo-contour map. Photo-
grammetric Eng. 24(3): 451-457. 1958.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
CONCLUSION
We have seen how photographs and pho-
togrammetry, over a period of a hundred
years, have made and continue to make a
profound impact on the science of geology.
This development has improved the work
of the geologist, through its effect in two
fields. One was an indirect effect, that of
improving the availability, quality, and va-
riety of photo-topographic maps. The other
was a direct effect, that of making available
in photographic form, a vast amount of
quantitative and interpretative data relat-
ing to the earth’s surface. Geologists have
been alert to the possibilities of applying
this sister science to the solution of their
own problems.
Development of Geologic Thought Concerning
Ulster County, New York
By JuLesS FRIEDMAN, U.S. Geological Survey
In the history of American geology, cer-
tain areas have been outstanding in the role
they have played in the development of geo-
logic thought. Such an area is Ulster
County, N. Y., situated west of the Hudson
River and halfway between the igneous and
metamorphic highlands of the Hudson and
the limestone Helderberg escarpment of the
Capitol District. Although more widely
known for the geology of its Catskill Moun-
tains, the county also includes part of the
Shawangunk Mountains and the Rondout
and Wallkill Valleys.
The geomorphic setting of the area,
known three centuries ago as the Esopus
territory, has exposed it to geologic specula-
tion since the earliest colonial days. By the
late nineteenth century, geologic thinking
in America was concerned with several
stratigraphic problems—the real boundaries
of the Ordovician, Silurian, and Devonian
systems—for which rock exposures in Ulster
County provided many of the problems and
some of the solutions. After several mid-
nineteenth century developments in mining
and quarrying, technological advances
opened the way, though inadvertently, for
stratigraphic and structural field investiga-
tion. During the present century, the area
has served_as a training ground in Paleozoic
stratigraphy for hundreds of American ge-
ologists.
Settlement of the Esopus territory of the
seventeenth century was controlled largely
by geographic factors. The fertile Rondout
and Wallkill Valleys, colonized and farmed
by the Huguenot French and Dutch, had
been occupied by Minsi and Delaware In-
dians in earlier times. That these Algonkian
Indians were as least as aware of their geo-
logic environment as the first European set-
tlers is suggested by their recognition and
use of Pleistocene glacial deposits of the
Rondout Valley for military strongpoints
and for burial grounds, by scores of Indian
place names derived from and incorporating
rock and landform names, and by their rec-
ognition of landforms and drainage in the
alignment of their trails. The original in-
habitants may also have discovered the
JULY 1959
sphalerite-galena ore bodies emplaced in
the Shawangunk conglomerate. William
Mather, in 1848, wrote, “There are tradi-
tions that lead ore has been cut out of
Shawangunk Mountain in many places by
the Indians and hunters of former days with
their hatchets, and melted to make their
bullets. Traditions of this kind,” continued
Mather, “are said to have led to the discov-
ery of the lead ores at Ellenville.”
Settlement of the old Indian lands and
rapid growth of the sparse population occu-
pied several decades after the American
Revolution, and then, in 1828, the Delaware
and Hudson Canal was completed between
the newly opened anthracite mines near
Honesdale, Pa., and Kingston, on the Hud-
son. Ten miles southwest of Kingston, at the
village of High Falls, dark beds of a previ-
ously unknown limestone formation were
exposed during excavation for the canal.
The discovery of these natural cement beds,
now recognized as part of the Rondout lime-
stone of Silurian age, made possible the de-
velopment of a natural cement industry un-
paralleled elsewhere in the United States.
Throughout the remainder of the nineteenth
century the industry was concentrated at
Rosendale and Rondout. By 1892 more than
a dozen major plants produced nearly
3,000,000 barrels of cement annually—90
percent of all cement consumed in the
United States at that time. But just before
the close of the century the introduction of
the portland process caused the natural ce-
ment industry to decline and then all but
disappear. Ironically, as the old quarries
and kilns at Rosendale fell into disuse, the
new portland cement industry thrived in
northern Ulster County, where nonmagne-
sian, crystalline limestones of Devonian age,
the Alsen and Becraft formations, as well as
the Coeymans and Manlius limestones, were
exploited.
The Rosendale area, nevertheless, had in-
fluenced the development of a standard sec-
tion for the Silurian and Devonian systems
in North America. When the four geologic
districts of New York State were delimited
in the 1830’s, Ulster County was included in
the First District, and William Mather was
chosen to report on the geology of this area,
FRIEDMAN: ULSTER COUNTY, NEW YORK
253
FULTON |
( Sean =
as
LmoivAarene NE
> ~L_ MONTGOMERY” \J
SS Evins a
=a
Fie. 1.—Index map of southeastern New York
showing the location of Ulster County.
including the cement belt. His Geology of
the First Geological District, published in
1848, but preceded by several preliminary
reports, is the first comprehensive work con-
cerned with the stratigraphy of Ulster
County. The rocks of Mather’s New York
system, his classification of the Paleozoic of
southeastern New York, are well displayed
in the Rosendale segment of the Rondout
Valley. The New York System corresponds
to parts of the Devonian, Silurian, and
Ordovician systems of the present day. De-
spite this work, the structure of the cement
belt was not to be unraveled until the ce-
ment industry itself had declined after 1893.
The geology of the Rondout-Whiteport-
Rosendale region had drawn geologists by
the score, and the stratigraphic positions of
the Silurian and Devonian limestones were
eventually worked out in detail by Darton,
Van Ingen and Clark, Grabau, Hartnagel,
and many others at the close of the century.
By 1910, faunal lists had been published for
254 JOURNAL OF THE
nearly all the fossiliferous formations, and
the top boundary of the Silurian system in
North America was drawn at the top of the
Manlius limestone and below the overlying
Coeymans limestone, the base of the Devon-
ian system in Ulster County.
As commercial interest switched to the
structurally complex belt between the Cats-
kill escarpment and the Hudson River
north of Kingston, so did the interests of
contemporary geologists; the first geologic
maps published on U. 8. Geological Survey
topographic base maps for this area were
prepared by George Chadwick and Rudolf
Ruedemann in the early 1940’s for the Cats-
kill and Kaaterskill quadrangles which in-
clude part of northern Ulster County. With
a few notable exceptions, all the detailed ge-
ologic maps painstakingly done in the ce-
ment belt south of Kingston during the
nineteenth century have either been lost or
have never appeared on adequate topo-
graphic base maps. It was not until R. M.
Logie restudied the natural cement lime-
stones in detail in the 1930’s that the in-
ternal stratigraphy of the Rondout lime-
stone was deciphered, but this study has not
been published and large-scale geologic
maps of the cement belt are still lacking.
Construction of the Ashokan Reservoir
and Aqueduct for the water supply system
of the City of New York provided the incen-
tive for Charles Berkey’s Geology of the
New York Aqueduct, the first work on the
valleys of the upper Rondout and Esopus
to use modern stratigraphic terminology
and to base structural interpretations on
diamond drill core measurements. It was
published as a New York State Museum
Bulletin in 1911. Again, technological re-
quirements had preceded and initiated an
advance in geologic techniques.
Before the 1920’s, very little information
was published on the Silurian Shawangunk
conglomerate below the cement limestone
sequence; moreover, a clear structural de-
scription of the intricately deformed Ordo-
vician clastic rocks below the Ordovician
and Silurian unconformity was unavailable.
In 1929, however, Bradford Willard pro-
vided stratigraphic evidence suggesting that
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 7
the Taconic disturbance occurred during the
interval represented by the unconformity
below the Shawangunk conglomerate; in the
following year C. K. and F. M. Swartz
traced the Tuscarora and Clinton units of
Swatara Gap, Pa., eastward and found that
they merged into the Shawangunk conglom-
erate at the Delaware Water Gap, and that
the conglomerate continued without inter-
ruption into Ulster County. They concluded
that the age of the formation was early
Middle Silurian and reinforced the concept
that a major hiatus exists below the base of
the Silurian system in much of eastern New
York.
In 1932, Charles Schuchert and Chester
Longwell summarized structural and strati-
graphic facts from Kingston and the Cats-
kill cement belt, indicating at least two epi-
sodes of deformation, Taconic and Acadian,
during Paleozoic time in the mid-Hudson
Valley region. It became clear, indeed, that
a single orogeny at the close of the Paleozoic
could not have been responsible for all
northern Appalachian structures and that
there was a series of smaller orogenic dis-
turbances distributed throughout Paleozoic
time. It also was learned that the disturb-
ances were possibly not correlative with
similar events in Europe, Asia, and Africa.
Between 1930 and 1945, stratigraphic
publications by Winifred Goldring, G. A.
Cooper, Rudolf Ruedemann, Rousseau
Flower, George Chadwick, and several other
geologists clarified much of the older work
and prepared the way for a new and more
realistic understanding of the lower Paleo-
zoic section of eastern New York.
Since 1945, synthesis and mild revision
have characterized the most recent work.
Detailed studies by W. A. Oliver, Jr., have
enhanced our knowledge of the facies rela-
tionships of the Onondaga limestone. Vari-
ous workers have divided the Shawangunk
conglomerate into three or even five mem-
bers. Lawrence Rickard, Jean Berdan, and
other contemporary stratigraphers have new
evidence that several long-recognized strati-
graphic units, e.g., the Manlius and Coey-
mans limestones, each transgress time lines
so sharply that they may actually be, at
least in part, facies of each other. This new
Juty 1959
work is reminiscent of the studies published
by G. A. Cooper and George Chadwick in
the 1930’s in which they demonstrate the
importance of facies relationships in the
Middle and Upper Devonian rocks of east-
ern New York. If facies changes are as
marked in the Lower Devonian and Silurian
part of the section as in the Upper Devo-
nian, the recognized contact between the
Silurian and Devonian systems may be in-
validated, 1.e., the Manlius limestone may
actually be the base of the Devonian sys-
tem. The base of the Silurian system, the
lowest member of the Shawangunk con-
glomerate, also may be of different age in
different places, suggesting the possibility
of several different ages for the Taconic
orogeny even within Ulster County.
Since Ruedemann’s death, however, pub-
lished papers on the deformed Ordovician
rocks below the Taconic unconformity in
the area have been few; it is in this subject
that work for the future could be most
profitable.
In retrospect, the most recent work in
geology in Ulster County, as elsewhere in
America, indicates the need for more com-
plete information on tectonic history as an
aid to stratigraphic correlation. It suggests,
moreover, the necessity for critically re-
viewing some of the most widely held con-
cepts of American geology.
REFERENCES
Berkny, C. P. Geology of the New York Aque-
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CuHapwick, G. H. Revision of “the New York
series.” Science, new ser., 28: 346-348. 1908.
. Catskill formation. Bull. Geol. Soc. Amer.
42(1): 242-243. 1931.
Great Catskill Delta.
60(2): 91-107. 1933a.
Hamilton red beds in eastern New York.
Science, new ser., 77: 86-87. 1933b.
. Upper Devonian of the New York region.
Bull. Geol. Soc. Amer. 44: pt. 1: 177. 1933c.
Geology of the Catskill and Kaaterskill
quadrangles. New York State Mus. Bull. 336,
Wie os.
Cuarkk, J. M. Classification of New York series
of geologic formations. New York State Mus.
Handbook 19: 29 pp. 1903.
Pan-Amer. Geol.
FRIEDMAN: ULSTER COUNTY, NEW YORK
259
and ScHucHeErT, C. The nomenclature of
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Cooper, G. A. Stratigraphy of the Hamilton group
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Stratigraphy of the Hamilton group of
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26: 537-551. 1934.
Darton, N. H. Preliminary report on the geology
of Ulster County. New York State Mus. Rep.
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Davis, W. M. The nonconformity at Rondout,
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395. 1883.
GotprRInc, W. Geology of the Coxsackie quad-
rangle, New York. New York State Mus. Bull.
332. 1943.
and Frowrr, R. H. Restudy of the Scho-
harie and Esopus formations of New York
State. Amer. Journ. Sci. 240: 673-694. 1942.
HartnaceL, C. A. Notes on the Siluric or Ontaric
section of eastern New York. New York State
Mus. Bull. 107: 39-54. 1907.
. Classification of the geologic formations
of the State of New York. New York State
Mus. Handbook 19. 1912.
MatHer, W. W. Geology of New York: Report
on the First District. 1843.
Mencuer, H. Catskill facies of New York State.
Bull. Geol. Soc. Amer. 50(11): 1761-1793. 1939.
Ouiver, W. A., Jr. Stratigraphy of the Onondaga
limestone in eastern New York. Bull. Geol.
Soc. Amer. 67: 1441-1474. 1956.
RUEDEMANN, R. Geology of the Catskill and Kaa-
terskill quadrangles. Pt. 1. New York State
Mus. Bull. 331: 7-188. 1942.
ScHucHErT, C. Silurian formations of southeast-
ern New York, New Jersey, and Pennsylvania.
Bull. Geol. Soc. Amer. 27: 531-534. 1916.
and Lona@weLi, C. R. Paleozoic deforma-
tions of the Hudson Valley region, New York.
Amer. Journ. Sci., ser. 5, 23: 305-326. 1932.
Swartz, C. K., and Swartz, F. M. Silurian of the
central Appalachians. Bull. Geol. Soe. Amer.
51(2): 148-149. 1929.
Age of the Shawangunk conglomerate
of eastern New York. Amer. Journ. Sci., ser. 5,
20: 467-474. 1930.
Van INGEN, G., and Ciark, P. KE. Disturbed fossil-
iferous rocks in the vicinity of Rondout, New
York. New York State Mus. Bull. 69: 1176—
1227. 1903.
Wiuarp, B. The age and origin of the Shawan-
gunk formation. Journ. Paleont. 1(4): 255—
258. 1928.
Stratigraphic aspect of Taconic disturb-
ance. Pan-Amer. Geol. 51(2): 93-96. 1929.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
Remarks on the History of American Petroleum Geology
By Epaar W. Owen, University of Texas
These remarks do not pretend to consti-
tute a history of petroleum geology. They
are merely an attempt at a perspective
which seems to have been elusive.
The year 1859 may well be considered the
beginning of modern times. Petroleum acti-
vated a new period of power and maneu-
verability for man at the same time that
Darwin’s Origin of species freed his mind
from the shackles of dogma. The Drake well
at Oil Creek, Pa., was completed in August
1859, producing 25 barrels per day at a
depth of 69 feet. It is generally recognized
as the beginning of the oil industry, al-
though petroleum had long been used in
many parts of the world. The American ori-
gin of the industry is anomalous, as western
Europe was much more industrialized and
had greater familiarity with the occurrence,
character, and uses of oil.
Many of the basic concepts of petroleum
geology were stated during the first decade
after the Drake discovery. In 1860 Henry
D. Rogers noted the occurrence of gas and
oil on anticlines. In the same year Alexander
Winchell recognized the role of reservoir
porosity. In 1861 T. Sterry Hunt and E. B.
Andrews emphasized the significance of
anticlines, and Andrews began working as
an exploration consultant while teaching at
Marietta College. H. D. Rogers in 1863 ad-
vanced a carbon-ratio theory as a criterion
of oil habitats. In 1865 Hunt elaborated the
anticlinal theory and Briggs explained un-
derground fluids mechanics. These concepts
are basic to petroleum geology, but their
enunciation did not add up to a workable
doctrine for oil exploration. E. DeGolyer
has stated the case admirably: “The anti-
clinal theory of the first half-century of the
oil industry was a speculative generaliza-
tion, determined empirically upon misun-
derstood and inadequate data.”
Organization of geological observations
into a disciplined science of petroleum ge-
ology has come slowly. In 1885 I. C. White,
after an important consulting job for Forest
Oil Co., restated the anticlinal theory
clearly enough to establish it as a guiding
exploration principle, but little practical ap-
plication was made of it for a quarter cen-
tury. Edward Orton published classic re-
ports on the Oil sands of southwestern Ohio
in 1886 and on The Trenton limestone as a
source of petroleum in 1887. M. J. Munn in
1909 made a major contribution to our un-
derstanding of the migration of oil.
Following the organization of the Ameri-
can Association of Petroleum Geologists and
the employment of thousands of profes-
sional geologists by the oil industry, our
concepts of the origin, migration, and accu-
mulation of oil and gas advanced rapidly
from 1918 to 1926. During those years hun-
dreds of important descriptive studies were
published and major contributions to the
philosophy of the discipline were made by
Alex. W. McCoy, E. G. Woodruff, L. F.
Athy, John L. Rich, F. M. Van Tuyl, R. C.
Beckstrom, R. Van A. Mills, W. H. Em-
mons, and others. More than 50 years after
its basic principles were first stated, petro-
leum geology had finally grown into a fairly
mature discipline, with an organic litera-
ture of comprehensive observations and
usable working hypotheses.
Some of the most important later scien-
tific milestones were: 1929, E. Russell
Lloyd’s exposition of the nature and role of
reef limestones; 1932, Parker D. Trask’s
work on source sediments; 1934, W. E.
Wrather and F. H. Lahee, editors, Problems
of petroleum geology; 1927-1941, A. I. Le-
vorsen’s work on stratigraphic traps; 1942,
Wallace Pratt’s spacious concept of Ozl in
the earth; and 1940-1950, M. King Hub-
bert’s studies in the mechanics of fluid
movement. No major contribution to the
science of geology has been the creation
solely of its author. All these important
works were syntheses, incorporating the ob-
servations and ideas of many other workers.
The employment of geology in petroleum
exploration and exploitation has been conso-
JuLY 1959
nant with the development of the science.
Although I. C. White, E. B. Andrews, and a
few others were employed briefly by oil
operators in the last century, the first or-
ganized geological department in the oil in-
dustry was established by E. T. Dumble for
the Southern Pacific Railroad in 1897. W.
W. Orcutt formed a department for Union
Oil Co. of California in 1898. A. C. Veach
was a full-time geologist for Houston Oil
Co. in 1901 and 1902, and H. B. Goodrich
did pioneer consulting work during 1899 to
1902 in many areas from New Brunswick to
Texas and Mexico. In 1907 and 1908 F. G.
Clapp, Ralph Arnold, W. T. Griswold, and
C. A. Fisher resigned from the U. 8. Geo-
logical Survey to do commercial geological
wark. In 1909 several able American geolo-
gists were doing phenomenally successful
work in Mexico. They were associated with
Europeans who had gained experience in
foreign areas, where oil companies had em-
ployed geology more actively than in the
United States. By 1912 several other men
were engaged in consulting practice. This
tardy application of known, effective sci-
entific techniques to the costly and hazard-
ous operations of oil exploration and de-
velopment is beyond understanding. But
suddenly geology became fashionable. Most
of the major American oil companies es-
tablished geological departments between
1913 and 1915. These were greatly expanded
in 1916 and have grown at an irregular rate
ever since.
As an art, petroleum geology has re-
sponded more quickly to technological de-
velopments than to new abstract scientific
concepts. Its practices and methods have
undergone constant transformaiton as ge-
ologists have applied, improved, and even
initiated a wide variety of new techniques.
Direct surface indications were the domi-
nant guide to oil prospecting until about
1910 and were used by geologists as well as
by the wildeat drillers who scorned geology.
These consisted of surface seepages, unusual
topographic features, drainage anomalies,
“ereekology,” and directional trends from
known fields. Surface structure mapping was
the dominant exploration method from 1910
to 1925. It had been used as early as 1883
when I. C. White surveyed with a spirit
OWEN: AMERICAN PETROLEUM GEOLOGY
257
level. W. T. Griswold introduced the more
efficient alidade in 1901. Every petroleum
geologist who worked between 1910 and
1925 had an intimate acquaintance with the
rocks on the ground and with the amiable
qualities of the telescopic alidade. Unfor-
tunately, surface mapping went into almost
total disuse by the oil companies after 1925.
The use of aerial photographs in the field,
and laboratory photogeology, have revived
some of the dignity of the surface geologist
in recent years.
Petroleum geology is essentially a sub-
surface inquiry. J. F. Carll was studying
well cuttings and plotting sample logs for
the Pennsylvania Geological Survey in 1875.
F. W. Minshall published cross sections of
the Burning Springs anticline as early as
1878. Orton’s Trenton Lime report of 1887
would be a creditable subsurface study by
today’s standards. But the oil companies
did not begin organized subsurface work
until 1917, when Alex. McCoy initiated the
first program for the Empire Gas & Fuel
Co. Other companies adopted the methods
promptly, and core-drilling was introduced
in 1919 to obtain additional subsurface in-
formation. The early emphasis was on struc-
tural attitude, and stratigraphy was mainly
a means to that end. The first general rec-
ognition of the importance of subsurface
stratigraphic studies resulted from the pub-
lication in 1921 of two classic papers by
Fritz Aurin, Glenn Clark, and Earl Trager
and by Luther White and Frank Greene.
Recognition of the economic importance of
stratigraphic traps resulted in rapid expan-
sion of the studies. Since World War II
several large research departments have
grown up in the oil industry, and their at-
tention has turned increasingly to stratig-
raphy.
The seismograph dominated petroleum
exploration from its successful application
on the Gulf Coastal Plain in 1924 until
recent diminishing economic effectiveness
has forced its more efficient integration with
other geological techniques. It was intro-
duced almost simultaneously by Alex. Deu-
ssen, L. P. Garrett, and E. DeGolyer for
their respective companies, quickly followed
by most other operators. The refraction
258
method of Mintrop was used until it was
largely supplanted by the reflection method
perfected by J. C. Karcher in 1926. Seismo-
graph surveys have now covered almost
every acre of prospective areas in the United
States; some areas have been surveyed
many times. Gravity methods have also had
an important, but lesser, role. The magne-
tometer has had wide use for rapid recon-
naissance. Many other geophysical tech-
niques have been tried without much
success, but new methods are constantly
under study. Geophysical instruments are
used in petroleum exploration only as tools
to obtain subsurface geological data. The
interpretation of their data has been left
largely in the hands of the technicians,
whose knowledge of geological structure and
of the formations they were exploring was
only rudimentary. The results of geophysi-
eal exploration have been phenomenal in
spite of this costly absurdity, but continued
success will be measured largely by the de-
gree of coordination with other information.
The principal effort of the petroleum ge-
ologist has always been directed to cbtain-
ing new data on earth science. His demand
for information is insatiable and often ex-
ceeds his ability to assimilate it. The most
reliable source of information, as well as
the ultimate test of his ideas, has always
been the drilling well. He soon replaced the
drillers’ well logs of early days with sample
logs of his own making. The rotary drilling
rig, which had been introduced in the Corsi-
cana field in 1895, gradually supplanted the
eable tool rig, which had furnished him
rather clean cuttings from the bottom of the
hole. By 1906 the rotary had reached Calli-
fornia and in 1918 moved into Oklahoma.
It reduced drilling time of individual wells
from years to days, but only the concerted
efforts of many geologists, engineers, and
drillers supplied the inventions of tools and
techniques which converted it into a satis-
factory medium for getting geological data.
The core barrel in 1921, later the wire-line
core barrel, the side-wall core, and the drill-
stem test tool, became direct sampling de-
vices. Use of the shale shaker, and control
of drilling mud viscosity, pump pressure,
and other physical factors made the cuttings
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, NO. 7
more intelligible samples. Introduction on
a commercial scale of Schlumberger elec-
trical logging into the United States in 1932
began a new cycle of data collection.
Instrumental logging of wells has be-
come universal practice, conducted simul-
taneously with drilling, or run at the time
of completion of the well. A wide range of
physical characters has been recorded di-
rectly or measured indirectly by recording
the response to various induced impulses.
No less than a dozen logging methods have
been developed and widely applied. The re-
sulting accumulation of accurate, detailed
measurements of multiple characters in bil-
lions of feet of geological section in hun-
dreds of thousands of deep wells has ex-
ceeded the capacity of all employed
geologists, engineers, and technicians to an-
alyze and interpret them.
Appheation of the acquired information
to problems of petroleum exploration has
required the use of many scientific pro-
cedures in addition to standard geological
and geophysical field methods. Micropale-
ontology was first applied by E. T. Dumble
in 1920. It was originally used for correla-
tion purposes in mapping subsurface struc-
ture, but broadened into environmental and
ecological studies. Macropaleontology, both
invertebrate and vertebrate, has been used
consistently in surface work and sparingly
in subsurface. The usual orthodox petro-
logic methods have recently been supple-
mented by more sophisticated techniques
which are still in an early stage of develop-
ment. Late discoveries in physical chemistry
have had some attention, and isotope ge-
ology has been appled to some of the
broader problems of geologic dating. Almost
every recent advance in geology and related
sciences has found some application to pe-
troleum geology. )
The contributions of petroleum geologists
to the basic science of geology have been
surprisingly meager, although their informal
impact on the philosophy of the science has
been far greater than is usually appreciated.
Several reasons account for this deficiency.
The requirement for immediate economic
employment of their studies usually pre-
vents definitive completion of their work.
Many of their results must remain confi-
JuLY 1959
dential until after the interest of the worker
and his contact with the work have sub-
sided. For most other scientists the litera-
ture of their science is their sharpest tool;
with petroleum geologists it is the most neg-
lected. Until recently, the bachelor’s degree
was considered adequate for the profes-
sional training of many petroleum geolo-
gists; 1t is not sufficient preparation for the
science of today.
The abundance of the data which the pe-
troleum geologists have accumulated has
passed their ability to marshal it, and will
require new statistical and electronic sort-
ing techniques for satisfactory analysis. Pe-
troleum geologists generally command a
more comprehensive three-dimensional view
of large segments of the earth than do any
other scientists. Their detailed knowledge
of the character of thick sections of the
geologic column is unique. Many of their
concepts are far in advance of anything
published. Many of the ideas in the current
geological literature relating to sedimenta-
tion, stratigraphy, structure, geologic his-
tory, and physiography look silly in the
light of their information. But their neglect
of effective communication has resulted in
continual duplication of basic studies. No
scientists are more liberal in the informal
sharing of their knowledge by oral discus-
sion, but no others have made as small con-
tributions per capita to the literature of
their science. The neglect, or even disdain,
of the data of petroleum geology by ge-
ologists outside the oil industry is equally
indefensible. The efficient employment of
the accumulated geological information and
the optimum advancement of the science
await a vast Improvement in the means and
habits of communication. As the cost of oil
finding in the United States has increased
to almost prohibitive levels this need has
assumed critical economic importance.
The role of the petroleum geologist has
changed continually with the development
of the oil industry and of the general econ-
omy. The imposition of conservation meas-
ures and State control of production during
and after the depression changed petroleum
exploration from a gambling game to an
orderly business. The growth of many large
OWEN: AMERICAN PETROLEUM GEOLOGY
259
oil operators and their tenacity in acquiring
and holding leases in prospective oil terri-
tory have now made acreage acquisition the
limiting factor i every new exploration
campaign. Diversity of ownership in small
tracts has magnified both the problems and
the costs. Unitization of drilling activities,
elimination of excessive drilling, and co-
operation in exploration have become more
pressing needs than improved technological
efficiency.
The role of petroleum geologists in the
building of the massive and complex modern
economy has been so great as to receive
general recognition. But the great impact
of these men on the world’s ethical climate
has been little appreciated. Into the tradi-
tionally selfish morals of the marketplace
has been injected the influence of thousands
of men educated in an idealistic atmosphere
and dedicated to scientific discipline. Most
of them had become geologists because of
an inherent adventurous and _ pioneering
spirit. They entered industry at a time when
operational control of most big corporations
was passing into the hands of trained, pro-
fessional management. Their energy and the
practical experience of their active, strategic
profession carried many of them quickly
into positions of authority in the industrial
world. Their success and that of their com-
panies came to be as closely related to the
degree of their integrity and the support
and cooperation which they commanded as
to their technological ability. In a single
generation, under their leadership and that
of other men of similar training, the United
States has evolved a pattern of business
ethics superior to any the world has ever
seen. Although piracy and rapacity are by
no means extinct, and we shall never be
able to dispense with the policeman, no man
today can afford ethical practices inferior
to the standards of his industry or profes-
sion. There even appears the anomalous
suggestion that, over the long term, self
interest is best served by unselfishness. For-
tunately this ethical transformation has co-
incided with the phenomenal growth of
modern industry, if it has not in fact been
largely responsible for that growth. This
has come to be a day of bigness, big busi-
260 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, No. 7
ness, big labor, government, science, even there is hope that for the first time in
big universities. Great power without strong history we need not be afraid of bigness for
checks and balances and high ethical re- its size alone. If that hope is realized the
straint is unendurable. But in the United credit will belong to the teachers of this new
States, if nowhere else yet in the world, generation of leaders.
Columbus alleged as a reason of seeking a continent in the West,
that the harmony of nature required a great tract of land in the
western hemisphere, to balance the known extent of land in the
eastern; and it now appears that we must estimate the native values
of this broad region to redress the balance of our own judgments, and
appreciate the advantages opened to the human race in this country,
which 1s our fortunate home. The land is the appointed remedy for
whatever is false and fantastic in our culture. The continent we in-
habit rs to be physic and food for our mind, as well as our body. The
land, with its tranquillising, sanative influences, is to repair the errors
of a scholastic and traditional education, and bring us into just re-
lations with men and things RALPH WALDO EMERSON.
Officers of the Washington Academy of Sciences
2 MOR i ow Je FRANK L. CAMPBELL, National Research Council
RESIHEME-CIECL.... 0... .2..+-- LawrRENcE A. Woop, National Bureau of Standards
Sold Dae U0 Heinz Specut, National Institutes of Health
_ UTS GS W. G. BrompacHer, National Bureau of Standards
MUEMEUESE fo ioe oc es on Morris C. Lerxinp, Armed Forces Institute of Pathology
Custodian of Publications............... Harautp A. ReHDER, U.S. National Museum
io. CuHresteER H. Page, National Bureau of Standards
EEE a MS) re H. A. Bortuwick, T. D. Stewarr
MMMIEMETSUO IGG! 222. ce oa ee Bourpon F. Scripner, KeitH C. JOHNSON
DTG 6 CY ra Puitip H. ABEetson, Howarp S. RapPLEYE
Board of Managers....All the above officers plus the vice-presidents representing the
affiliated societies
CHAIRMEN OF COMMITTEES
Standing Committees
a2 2 FRANK L, CaMPBELL, National Research Council
02 US. oo RautpH B. KENNARD, American University
Membership............ LAWRENCE M. KusHner, National Bureau of Standards
DeMOgraphs.................. Dean B. Cows, Carnegie Institution of Washington
Awards for Scientific Achievement....... FRANK A. BIBERSTEIN, Catholic University
Grants-in-aid for Research...... B. D. Van Evera, George Washington University
Poucy and Planning.............. MarGareET Pitrman, National Institutes of Health
Encouragement of Science Talent.............. Leo ScHusEertT, American University
Science Education............ RayMonpD J. SEEGER, National Science Foundation
Ways and no RussEtL B. Stevens, George Washington University
Pueie Helations...................... Joun K. Taytor, National Bureau of Standards
Special Committees
- Llu oe Haroitp H. SHEeparpD, U. 8. Department of Agriculture
MeECeLOry............... James I. HamBuLETON, U.S. Department of Agriculture (Ret.)
mvorary of Congress.................... Joon A. O’Krere, National Aeronautics and
Space Administration
CONTENTS
Page
Symposium on the History of American Geology
Prefatory statement. . a... Jeos os. J.P. . 2. ate ae 197
Notes on the earliest geological maps of the United States, 1756-1832.
JOHN Wr. WELES «ooo sg oesepas oaus 6 0 eins ens ws as a 198
Emergence of geology as a public function, 1800-1879. Wuti1aAm Back. 205
The United States Geological Survey and the advancement of geology
in the public service. THomas B. NOLAN................-++20:- 209
The role of the Smithsonian Institution in early American geology.
Pat. OBHSER.. . 6 c.g004 ws ss os 215
Geology plus adventure: The story of the Hayden Survey. J. V. HowE.t 220
A history of the popularization of geology in America: A bibliographic
survey. Mark. W. PANGBORN, JRB...¢.,. jc)... 3......) soe 224
Asa Gray and American geology. A. HUNTER DUPREE............... 227
Darwinian natural selection and vertebrate paleontology. JoHN A.
WUIESON bos. oc cetera de ete clo Wee oo ot soca a oa 231
Impact of the development of photogrammetry upon geology. Davin
TOANDION ow. oo ake Sele Os ee eo ee et 234
Development of geologic thought concerning Ulster County, New York.
JULES FRIEDMAN... 2.00): ) hota ek ee 252
Remarks on the history of American petroleum geology. EpGar W.
COWIEND «5 scape. ¥.2 asa oy Sie se js ps Sia Sa ee a es ee ee 256
2wW23
VOLUME 49 August-September 1959 NUMBER 8
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JOURNAL
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Vou. 49
AUGUST-SEPTEMBER 1958
No. 8
BOTANY .—Adventitious bud and stem relationship in apple. Hare DERMEN, Crops
Research Division, U. 8. Department of Agriculture, Beltsville, Md.
(Received May 12, 1959)
Under a title as of the present article
some details relating to adventitious bud
development on the stem of apple were re-
ported at the 1956 meeting of the Botanical
Society of America. The following note on
this subject appeared in the mimeographed
“Abstracts” assembled for the abstracts of
the papers presented at the meetings of the
General Section of the Botanical Society:
“In early March of this year 10 one-year-
old apple trees of the variety Maiden Blush
were cut back to about 12”, planted in 10”
pots and disbudded to induce adventitious
bud development on the stem. A number of
buds developed endogenously on the stems
adjacent to scars of cut-off buds as well as
in internodal regions. Buds were examined
by making serial tangential cuts under
them. Under the normal buds, three leaf
traces and a bud trace could be followed
into the stem pith but no trace of any na-
ture was observed in the stem behind the
adventitiously induced buds. Adventitious
buds which developed near normal bud
sears had no connection with any leaf or
bud trace. The results reported here verify
and extend conclusions made _ previously
with similar material.”
General information on the subject here
discussed appeared in earlier publications
(Dermen, 1948, 195la, 1955a). Some addi-
tional details with illustrative material are
presented here. This article will also formal-
ize the note quoted from the mimeographed
abstract.
Fig. 1-A shows a l-year-old tree of
Maiden Blush apple disbudded to induce
i»)
a
development of adventitious buds on the
stem. Round scars along the stem mark the
nodal regions where normal buds were cut
off. Arrows a and 6 point to two adventi-
tious buds that developed several weeks af-
ter normal buds were excised. The same two
buds are shown in the enlarged photograph
in Fig. 1-B indicated by arrows. The same
portion of the stem, shown in Fig. 1-C from
side view 1n respect to the buds, shows the
upper bud already grown into a shoot and
the lower one barely grown through the
bark.
Fig. 2 shows an adventitious bud (indi-
cated by an arrow) from another tree of
Maiden Blush hfted from the stem with a
piece of bark attached and sectioned by the
free-hand method with a razor blade. The
bud was still inside the bark when lifted
from the stem and the bark over the bud
was barely cracked. In Fig. 2 the centrally
located darkened region, appearing irregu-
larly inside the bark, is where the bulk of
the adventitious bud had developed. The
curved portion at the upper side of the en-
dogenous growth indicated by the arrow is
the shoot apex of the bud. Sometimes from
such endogenously proliferating growth
more than one shoot emerged.
At the stage of adventitious growth shown
in Fig. 2 no mark of any sort was detectable
on the wood surface at the point of the ad-
ventitious bud growth when the bark was
lifted; whereas behind all true nodal buds
there were clearly visible marks of vascular
tissue connection between leaf and bud at
a node and the wood under the bark.
61
SMITHSONIA
INSTITUTION. SEP 3 0 1958
262
Figure 3-A shows an enlarged view of the
scar of a normal bud. Figure 3-6 shows vas-
cular tissue markings on the wood of the
stem when the bark at the bud sear (Fig.
3-A) is lifted from the stem. In this view
there are on the stem four major vascular
connecting points. Three vascular points
marked a, b, and c are in a straight line;
they indicate the three points of vascular
connection between a leaf and the stem. The
point of vascular connection between an
axillary bud and the stem, marked d, 1s in-
dicated by an arrow. The four markings in
Fig. 3-6 (a, b,c and d) are transverse views
of traces of vascular tissue bundles from a
leaf and a bud at a node of the apple stem
extending through the wood to the pith of
the stem. The few small dots around trace
d are trace marks of scales and young
leaves of the axillary bud.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 8
Figure 4-A shows the view of the area of
the shoot grown from the adventitious bud
ain Fig. 1-C after the bark of the area was
lifted. Arrow a points to the scar in the
wood where a piece of fresh wood tissue had
pulled off when the bark with the shoot was
lifted, indicating the amount of wood tis-
sue which had grown on the stem since the
adventitious bud a (Fig. 1-A and B) had
grown into the shoot in Fig. 1-C. In Fig.
4-A arrow 6 points to the central middle
trace of the leaf at the node. Arrow c points
to the left trace of the leaf. The right leaf
trace cannot be seen in the view of the stem
shown. Arrow d points to the main axillary
bud trace. The small trace at the left of the
main bud trace is one of the traces of the
axillary bud scales.
Figure 4-6 shows the stem at the same
position in Fig. 4-A. Here is shown what re-
Fic. 1—Two adventitious buds on the stem of a one-year-old tree of variety Maiden Blush apple.
A, Two adventitious buds are indicated by arrows a and b. X 14. B, Enlarged view of the portion of
stem of the same tree with the two adventitious buds. X 114. C, Upper adventitious bud grown into a
shoot, lower one barely emerged through the bark. x 1.
AUGUST-SEPTEMBER 1959 DERMEN: BUD AND STEM RELATIONSHIP IN APPLES 263
Fic. 2.—A highly enlarged view of cross section of bark with an adventitious bud or buds developing
inside of it. X about 30.
SESS
Fig. 3.—A, Large sear at a stem node after nodal bud was excised. B, The same node region as in A
with the bark removed; a, b, c indicate transverse view cf three vascular traces of leaf; arrow at d indi-
cates transverse view of the vascular trace of the axillary bud. X 5.
264 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES — VOL. 49, No. 8
mains when the wood in the area marked was examined similarly. Figure 5-A shows
by arrows a and ¢ in Fig. 4-A was shaved the region of bud 6b after the bark was
off with a razor blade. There was no vascu- lifted. There was hardly any mark on the
lar trace connection beyond the depth of wood underneath the bud b. The location
the scar on the wood. In contrast to the situ- of bud 6 is indicated by an arrow on the
ation just described, there was present the back of the lifted piece of bark (Fig.
vascular trace of the leaf trace at arrow c. 5-6). Other marks are those of the three
The traces of the leaf and the normal axil- leaf traces and that of the axillary bud
lary bud could be followed through the wood trace. In Fig. 5-C the arrow points to the
tissue to the stem pith. right trace of the leaf. No other markings
The adventitious bud b, shown in Fig. 1, could be found in the vicinity of the leaf
Fic. 4.—A, Area of adventitious bud a in Fig. 1-A and B. Arrow at a indicates the place from which
a piece of wood tissue was pulled when bark and with it the shoot which had developed from bud a was
removed. Arrows at 6 and c point to two vascular traces of the leaf at the node. Arrow at d points to
the vascular trace of the axillary bud. B, The same area as in A. In B the area at a and c was shaved
off. The figure shows the vascular trace at ¢ is present, but there was no trace of vascular tissue back
of the region a. X 5.
Fig. 5.—Illustration of absence of vascular trace behind adventitious bud 6 in Fig. 1. Other details
in text. A and B enlarged X 215; C, X 44.
trace which would have indicated connec-
tions with the adventitious bud b.
The features just described give further
evidence that bud development on the apple
stem previously reported was truly of ad-
ventitious and endogenous origin and that
such buds were not latent buds which could
have been forced into shoot growth by
heavy pruning (MacDaniels, 1953).
The method here followed to demonstrate
whether a bud is of adventitious or of nor-
mal origin is useful and reliable, but not the
only method, as results previously reported
(Dermen 195la, 1955a) indicated. Occa-
sionally buds may originate in the nodal
area where a scar has resulted from dis-
budding operation to induce adventitious
bud growth. In such eases cuts in the scar
area tangential to the stem surface would
not reveal whether the vascular traces pres-
ent were those of an adventitious bud or
those of the axillary bud and the leaf which
had been removed. If a bud appears in the
scar region resulting from a cut carefully
made, or in close proximity to a scar, and it
has appeared in the manner described pre-
viously (Dermen, 1948, 1951a, 1955a) weeks
or months after the disbudding operation,
it surely must have originated adventi-
tiously and endogenously through meriste-
matic activity of cells of the callus tissue
forming after a cut.
A tree of Winesap apple variety was de-
termined to have a cytochimeral complex in
which at the shoot growing point the two
outermost cell layers, designated as L-I and
L-II, were diploid (2x) and inner cell layers
tetraploid (4x). This kind of chimeral plant
is designated as 2-2-4 (diploid, diploid, tet-
raploid) type and functions sexually as dip-
266 JOURNAL OF THE
loid (Dermen, 1951b). Some twigs and
branches of this Winesap apple tree were
found to have reverted to a completely dip-
loid condition (Dermen, 1951b).
A number of attempts were made to ob-
tain a completely tetraploid form of Wine-
sap apple, along with some other varieties,
by the adventitious budding method but
failed (Dermen, 1955a). In previous experi-
ments as many as two dozen trees had been
used. Hoping that eventually success might
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, No. 8
be achieved with the chimeral Winesap, the
number of experimental plants was in-
creased to 60 one-year-old trees. Even then
not a sing!e adventitious bud growth oc-
curred on the internodal regions of any of
the trees. However, on many of them a large
mass of callus grew in the scarred areas at
the nodes from where normal buds had been
cut. One such callus growth is shown in Fig.
6-A. The growth reached the size shown in
6 months, at the end of which two shoots
Ue A
‘ ;
ma
Fig. 6.—A, Large callus formation at a node of stem of Winesap apple with 2-2-4 type chimeral com-
plex. Arrow at calloused region points to a swelling suspected of being an adventitious bud. X 2. B, Two
diploid shoots from the calloused region. X about normal.
AUGUST-SEPTEMBER 1959
DERMEN: BUD AND STEM RELATIONSHIP IN APPLES
bo
or)
|
Fic. 7.—A, At the lower calloused node arrow points to bud developed adventitiously at the node of
a stem of 2-2-4 chimeral Winesap tree. B, Shoot growth from adventitious bud. C, A leafy shoot growth
from the adventitious bud; the shoot was entirely tetraploid. A, Slightly enlarged; B and C, normal size.
had begun to emerge (Fig. 6-6). The arrow
in Fig. 6-A points to one adventitious bud
with a smooth layer of tissue over it. On
cytological examination both shoots were
found to be homogeneously diploid.
One shoot also developed on another of
the 60 disbudded trees. It also developed in
a callused nodal region. In Fig. 7-A the ar-
row points to a swelling suspected of being
an adventitious bud and growing into a
shoot. In Fig. 7-B is shown a young shoot
developed from the “bud” in Fig. 7-A, and
in Fig. 7-C is shown the leafy shoot; it was
totally tetraploid (Dermen, 1955c). This
was the only instance in all the experiments
that a tetraploid shoot was isolated from a
2-2-4 chimeral type of plants by the dis-
budding method (Dermen, 1955a).
SUMMARY AND CONCLUSION
When tangential cuts are made behind
the normal buds at the stem nodes, there
are found in the wood a definite number of
markings which are easily recognizable;
these are the three vascular traces of a leaf
and one major vascular trace of the axillary
bud at a node seen at transverse sections.
These markings represent cross-sectional
views of vascular tissue bundles which con-
nect a leaf and a bud at a node with the
wood tissue. These traces can be followed
through the wood tissue to the pith of the
stem as cuts transverse to the traces are
made successively. Similar tangential cuts
were made into the wood behind what were
judged to be adventitiously originating
268 JOURNAL OF THE
buds. There were no such marks of vascular
traces in the wood behind any of the ad-
ventitious buds. A bud or branch trace was
present only in the amount of wood tissue
erown after the adventitious buds have
started growing into shoots. The present
study confirms earlier reports concerning
initiation of adventitious bud on the stem of
apple by following disbudding method pre-
viously described. This study also makes it
obvious that other methods followed dem-
onstrating the nature of the adventitious
buds developed on some apples were reli-
able. It is concluded that when 1- to 2-year-
old apple trees, potted in 10- to 12-inch pots,
are cut to stumps about 10 to 12 inches high
and all the buds at all the nodes are re-
moved, adventitious buds may appear either
along the internodal space on the stem or
near or 1n the nodal region. In the internodal
and near the nodal regions adventitious buds
originate in phloem tissue. In the nodal
region they originate in the callused tissue.
They appear as small swellings with a
smooth surface. The smooth surface is rup-
tured and a shoot slowly grows from such
an endogenously developed bud. The ap-
pearance of the swellings and emergence of
a bud and its growth into a shoot may take
weeks or months. Buds appearing in the
manner just described are truly adventitious.
Wellensick (1952) obtained adventitious
bud growth on apple, pear, beech, birch and
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 8
oak. MacDaniels (1953) failed to obtain
such buds on the apple. At the base of a
propagated shoot there are normal small
buds close together, and some of them are
difficult to see with naked eye. Bud and
shoot growth from these buds which nor-
mally remain latent should not be confused
with the true adventitious buds. When such
buds show growth into shoots following dis-
budding of stems they should be destroyed
so that they will not interfere with the in-
itiation of adventitious growth.
LITERATURE CITED
DerMEN, Hata. Chimeral apple sports and their
propagation through adventitious buds. Journ.
Hered. 39: 235-242. 1948.
. Tetraploid and diploid adventitious shoots
from a giant sport of McIntosh apple. Journ.
Hered. 42: 144-149. 195la.
. Ontogeny of tissues in stem and leaf of
cytochimeral apples. Amer. Journ. Bot. 38:
753-760. 1951b.
. Three additional endogenous tetraploids
from giant apple sports. Amer. Journ. Bot.
42: 837-841. 1955a.
_A 2-4-2 chimera of McIntosh apple. Journ.
Washington Acad. Sci. 45: 324-327. 1955b.
. A homogeneous tetraploid shoot from a
2-2-4 type chimeral Winesap apple. Journ.
Hered. 46: 244. 1955c.
MacDantets, L. H. Anatomical basis of so-called
adventitious buds in the apple. Cornell Univ.
Agr. Exp. Stat. Mem. 325: 3-22. 1953.
WELLENSICK, 8. J. Rejuvenation of woody plants
by formation of sphaeroblasts. Proc. Nederl.
Akad. Wetensch. Amsterdam C. 55(5): 567-
573. 1952.
It is the creatures which have their independent emotional life that give
us the great lesson of our kinship with the lower stages of living. This les-
son is sorely needed. I have known famous naturalists who had never
come by either an intellectual or emotional understanding of their place
in the chain of intelligence, and without this a man remains a stranger in
this world.—NATHANIEL SOUTHGATE SHALER.
AUGUST-SEPTEMBER 1959 CUATRECASAS: NEW CHIROPTEROPHILOUS SOLANACEAE
269
BOTANY.—New chiropterophilous Solanaceae from Colombia. José CUATRECASAS,
U.S. National Museum, Smithsonian Institution.
(Received May 27, 1959)
Dr. Stefan Vogel, accompanied by the
entomologist Dr. Helmut Sturm, both from
the University of Mainz, Germany, spent
one year, from 1955 to 1956, in northern
South America (Colombia and Panama)
conducting ecological research on pollina-
tion in the field. The main topic of the
investigation was the pollination of flowers
by bats. On this kind of fertilization there
existed at the time positive information on
about 20 genera, mostly of South Asian
plants, but only scarce data were available
from the American tropics. Before Dr.
Vogel’s studies, the existing reliable observa-
tions on fertilization by bats in the New
World were limited to Crescentia cujete by
Porsch in Central America and to Eperua
falcata and Bauhinia megalandra by Hart
in Trinidad; Porsch had quoted several
genera, the flowers of which were supposedly
visited by bats.
During his stay in Colombia and Panama,
Dr. Vogel checked the visiting of flowers of
about 17 species by long-tongued vampires
of the subfamily Glossophaginae. He ob-
tained on infrared film an amazing and fine
documentation on the subject clarifying
many details concerning the performance of
bats. The species of Glossophaginae which
were observed are: Glossophaga soricina,
Lonchophylla concava, and Anoura geof-
froyr peruana. The chiropterophilous plants
and flowers studied by Vogel mainly were
Bignoniaceae (Kigelia aethiopica, Cres-
centia cujete), Solanaceae (Trianae,
Markea), Gesneriaceae (Campanea), Gen-
tianaceae (Symbolanthus), Polemoniaceae
(Cobaea), Melastomataceae (Purpurella),
Papilionaceae (Mucuna), Bombacaceae
(Ochroma), Cucurbitaceae (Cayaponia),
Marcegraviaceae (Marcgravia), Lythraceae
(Lafoensia), and Capparidaceae (Cleome
anomala).
A detailed and illustrated report on his
research has been published by Dr. Vogel,
which is recommended to the reader inter-
ested in this subject: Fledermausblumen in
Suedamerika, Oecsterreich. Bot. Zeitschr.
104 (4/5): 491-530, 10 figs. 1958.
Among the Colombian collections of
chiropterophilous plants made by Vogel and
Sturm, which I received for identification,
three of the Solanaceae proved to be new
taxa. Their descriptions follow. The illus-
trations are originals of Dr. Vogel.
Markea vogelii Cuatr., sp. nov.
Frutex epiphyticus caudice tuberculato l-
gnoso ramis scandentibus prodeunti. Rami ramu-
lique griseo-virides glabri.
Folia alterna integra crassiuscula chartacea.
Petiolus glaber 4-8 mm longus semiteres tan-
tum basi paulo incrassatus. Lamina oblongo-
ovata vel oblongo-elliptica velsubelliptica basi
rotundata vel obtusa apice attenuata acumina-
taque acutissima, margine sublaevis plana vel
paulo revoluta, 5.5-9 em longa 3-4.5 em lata;
supra in sicco griseoviridis glabra sed minute
papilosa costa filiformi nervis secundaris paulo
visibilibus venulis obsoletis; subtus viridulis
costa eminenti nervis secundarus 6-8 utroque
latere tenuibus prominentibus ascendentibus
prope marginem arcuate-anastomosatis, venulis
obsoletis parcissimis minutis pilis sparsis vel
glabra, leviter papillosula. .
Inflorescentia simplicissima floribus solitarius
axilaribus ad terminationem ramulorum pendu-
lorum. Pedicelli 1-1.5 em longi glabri apicem
paulatim inerassati eum brevi pedunculo articu-
lati. Calyx crasse membranaceus circa 4 em lon-
gus glaber prismatico-tubulosus supra medium
lobatus lobis triangularibus acutis, tubo pris-
matico circa 2 cm lato comissuris sepalorum
angulatis apparente carinatis; sepalis ovato-
oblongis acutis uninervis 12-16 mm latis. Corolla
luteo-viridis glabra crasse membranacea com-
panulata basi tubulata in totidem 6.5-7.5 em
longa, tubo crasso circa 1.8 em longo 0.8-1 cm
diamitenti, limbo ecampanulato circa 3 em diami-
tenti lobis oblongo-ovatis obtusis 1.5-1.8 cm
longis latisque reflexis; petalis trinervis venulis
laxi reticulatis Inconspicuis. Stamina 5 filamentis
apice teneris basim versus incrassatis robustisque
basi barbulatis reliquis glabris 2.5-2.8 em longis
0
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, No. 8
Ni
Fic. 1.—a, 6, d, e, Trianaea spectabilis Cuatr. var. brevipes Cuatr., var. nov.;
c, Markea vogelii Cuatr., sp. nov.; f, Markea sturmi Cuatr., sp. nov.
AUGUST-SEPTEMBER 1959 CUATRECASAS: NEW CHIROPTEROPHILOUS SOLANACEAE
ad faucem corollam (apicem tubi) insertis; an-
theris basifixis pendulis crassis oblongis 1.6-1.8
em longis circa 3 mm crassis birimosis usque ad
basin dehismentibus. Discus crassus_ planus.
Ovarium oblongo-ovoideum glabrum biloculare
multiovulatum. Stylus circa 5.5 em longus cras-
slusculus erectus apice 2 stigmatibus bilobatis
decurrentibus. -
Typus: Colombia, Cundinamarca: Cordillera
Oriental, forests 1,800 m alt. above Monterre-
dondo, between Guayabetal and Limoncito, 138-
X-1956, Stefan Vogel 159. Holotypus US.
Markea vogelu, because of its life form, rather
large flowers, and greenish corolla, is in some way
closely related to M. viridiflora, but its tubulous-
campanulate corolla is more similar to that of
M. venosa and M. neurantha. The new species
could be placed near numbers 6 and 7 in my
key of the genus Markea (Feddes Repertorium
Sp. Nov. 61: 83. 1958), differing by its sub-
chartaceous or submembranaceous leaves, its
glabrescence, the shape and size of the calyx and
corolla, and the yellow-greenish color of the
corolla.
Markea sturmii Cuatr., sp. nov.
Frutex epiphyticus ramis tortuosis cortice
pallido-griseo corrugato rhitidomatoso ramulis
ultimis angulatis tenuibus glabris.
Folia alterna integra crassiuscule membra-
nacea glabra. Petiolus subteres leviter incrassatus
3-4 mm longus. Lamina elliptico-lanceolata vel
oblongo-lanceolata basi attenuata obtusa vel
subacuta apicem versus angustata longe acute-
que acuminata vel caudata margine laevi, 6.5—
12.5 em longa 1.8-4 em lata, acumine 2-20 mm
longo; supra sublaevis tantum costa filiformi
notata reliquis nervis inconspicuis; subtus costa
prominenti angusta nervis secundaris 6-8 utro-
que latere tenuibus prominulis patulis prope
marginem arcuatis anastomosatisque leviter con-
spicuis venulis obsoletis reliqua superficie laevi.
Inflorescentiae pauciflorae ad ramulos pendu-
los ex axillas foliorum supremum, pedunculo 6-8
em longo valde teneri sed rigidulo angulato
glabro subapicem brevem ramulum orienti, ad
apicem et in ramulo paulo incrassato 3-4 flores
sessiles ferenti. Pedicelli in specimine absenti.
Calyx crasse membranaceus viridis glaber sub-
prismatico-campanulatus circa 1.8 em longus 5-
lobatus, lobis oblongo-ovatis subacutis uninervis
S—-9 mm longis 6-7 mm latis (ad basim), tubo
271
prismatico comissuris sepalorum angulatis cari-
nata-prodeuntibus, venulis laxe reticulatis incon-
spicuis. Corolla crasstuscula viridis campanulata
basi tubulosa in totidem 3-3.5 em longa; tubo
circa 7 mm longo 4-5 mm diamitenti; limbo late
campanulato cirea 1.5 em diamitenti apice lobis
reflexis ovalibus vel subrotundatis 7-9 mm longis
latisque, petalis uninervis (costis) et laxe obsole-
teque reticulato venosis, intus fauce (apice tubi)
sparsissime pilosula reliqua omnino glabra. Sta-
mina 5, filamentis crassis 1.5-2 mm longis sub-
apicem tubi insertis parcis minutis pilis praedi-
tis; antheris inclusis erectis crassis oblongis
conniventibus 6 mm longis glabris 2-rimosis usque
ad basim dehiscentibus. Discus crassus obtuse
pentagonus fere planus. Ovarium ovato-conicum
glabrum circa 3 mm longum, biloculare loculis
multi-ovulatis. Stylus erectus glaber 1.2-1.3 mm
longus apice stigmatibus duobus oblongis de-
currentibus. Fructus ignotus.
Typus: Colombia, Huila: ridge of the Cordil-
lera between Guadalupe and Florencia, forests
1700 m alt., 9-VI-1956, Helmut Sturm 178. Holo-
typus US.
M. sturmu belongs to the section Merintho-
podium (D. Smith) Cuatr. and differs from all
other species essentially by its very short sta-
minal filaments. The size and shape of the calyx
and corolla and the thin, rather small and lance-
olate leaves also are unique. Although the thin
peduncles of the inflorescences are not flexuose,
these are pendant, because the terminal branch-
lets which bear them, are more or less flexuose
and pendulous.
Trianaea spectabilis Cuatr. var. brevipes Cuatr.,
var. NOV.
Frutex epiphyticus caudice tuberculato ramis
scandentibus elongatis. Lamina foliorum late
ovato-elliptica vel obovato-elliptica 20-29 cm
longa, 9-13 em lata. Stamina circa 8 mm supra
basim corollae inserta. Stigmata 5 oblonga conni-
ventia basim coalita. Ovarium 8-10 loculis. A
species typica pedicelli tantum 3.5-6 em longi
differt.
Typus: Colombia, Cundinamarea: Monterre-
dondo between Guayabetal and Limoncito, Cor-
dillera Oriental, forests 1,8C00—2,100 m alt., 6-XII-
55. “Vermutlich epiphytisch aehnlich Markea
wachsend mit grosser verholzter Knolle. An
Baeumen von dieser Knolle aus lange kletternde
verholzte, bis 15 m. hoch steigende Triebe aus-
272 JOURNAL OF THE
bildend. Blueten einzeln, axillaer, haengend, oder
gehaeuft am Ende beblaetterter Sprosse. Bis-
weilen Tetramerie meist pentamer. Wasserkelche.
Blueten bei dieser Art die Kelchzipfel nur wenig
ueberragend, Kronlappen spitz, Farbe gruenlich
gelb. Blaetter lederartig. Unreife Fruechte beere-
nart.” Stefan Vogel 6. Holotype, US; isotype, M.
These specimens are cited by S. Vogel in his
extremely interesting studies on chiropterophi-
lous flowers (p. 506, fig. 4-1). The only difference
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 8
the long flexuose pedicels are characteristic of
the genus.
Trianaea was described from flowering speci-
mens. Recently I received for study other collec-
tions with developed fruits which gave me the
opportunity to study the seeds. These prove to
be reniform, minutely alveolate and with a
curved semicircular embryo. This character ex-
cludes the genus Trianaea from the tribe Ces-
treae and indicates that it belongs to the Datu-
reae. (See also Cuatrecasas, J. Notes on
American Solanaceae, Feddes Repertorium 61:
83. 1958.)
I ean find between these and the regular typical
Trianaea spectabilis are the short pedicels of the
Vogel plants; this feature is remarkable, because
FORMER ACADEMY PRESIDENT MEMORIALIZED
A bust of Dr. AleS Hrdliéka (1869-1943), world-famous anthropologist who was asso-
ciated with the Smithsonian Institution for 40 years, was recently presented to the Smith-
sonian’s National Museum by Dr. Miloslad Ruzek, Ambassador of the Czechoslovak Re-
public to the United States. The gift was made on behalf of several educational and cultural
groups of Czechoslovakia as a memento of the recent observances in that country marking
the 15th anniversary of Hrdliéka’s death and the 90th anniversary of his birth.
The bust is the work of the Czech sculptor Milan Knobloch, based in part on a death
mask of the scientist made by Andreas J. Andrews, Smithsonian sculptor. The original of
the bust was unveiled last September in the entrance of the school that now bears Hrdliéka’s
name in Humpolec, Czechoslovakia, the town where he was born.
Hrdli¢ka came to America with his father in 1882. He studied medicine in New York and
anthropology in Paris, and in 1903 was called to Washington to set up a division of physical
anthropology in the U. 8. National Museum. Here he spent the rest of his life and built up
the collections in that department to rival those anywhere else in the world. He was founder
and first editor of the American Journal of Physical Anthropology, and founder and first
president of the American Association of Physical Anthropologists. He encouraged anthro-
pology in Czechoslovakia, especially at Charles University, Prague, by gifts of books and
money, one result of which is the Hrdli¢ka Museum in the Anthropological Institute of that
institution. He served as president of the Washington Academy of Sciences in 1929.
HONORARY MEMBERSHIP
D. E. Parsons, chief, Building Technology Division, National Bureau of Standards, has
been elected to honorary membership in the American Society for Testing Materials, ‘an
recognition of long and distinguished service to the Society in both technical and adminis-
trative work, and for eminent leadership in the field of building materials and building tech-
nology involving both research and standardization.”
AUGUST-SEPTEMBER 1959
SHOEMAKER: THREE NEW CAVE AMPHIPODS
273
ZOOLOGY—Three new cave amphipods from the West Indies. CLARENCE R.
SHOEMAKER,! U. S. National Museum.
(Received March 27, 1959)
During the Smithsonian-Bredin Carib-
bean Expedition of 1958, caves of several of
the Lesser Antilles were investigated. The
first two of the new amphipods described be-
low were collected by Desmond Nicholson,
captain of the Expedition’s vessel, Pree-
lance, from a fresh-water stream in Dark
Cave, Barbuda, on April 25, 1958. The third
new species, the type of a new genus, was
collected by Gilberto Silva Taboado during
his investigations of the fauna of Cueva
Grande, a large cave in Las Villas Province,
Cuba.
Family BocipIELuipAE Hertzog, 1936
Genus Bogidiella Hertzog, 1933
Bogidiella bredini,’ nu. sp.
Hie, 1
Material examined—Two specimens, a male
and a female, from Dark Cave, Barbuda.
Description—FEMALE: Side lobes of head
prominent and distally rounding; eyes absent.
Antenna 1 less than half the length of the body;
first joint of peduncle a little stouter and longer
than second; second joint twice as long as third;
flagellum about equal in length to the peduncle,
and consisting of about 12 joints; accessory fla-
gellum of 3 or 4 joints and reaching a little be-
yond the second joint of primary flagellum. An-
tenna 2, a little shorter than 1; gland-cone
prominent; third joimt half the length of the
fourth; fourth joint a little stouter and a little
longer than the fifth; flagellum shorter than fifth
peduncular joint and consisting of 5 joints which
decrease in length consecutively.
Mandible, cutting-edge with few teeth; ac-
cessory plate well developed, broad distally, with-
out teeth, but with crenulate distal margin; 5
spines in spine-row; molar low and conical with
*Mr. Shoemaker died on December 28, 1958,
leaving this manuscript nearly completed. It was
prepared for publication by Thomas E. Bowman,
U. S. National Museum, who added Fig. 2, 7, to
those drawn by Mr. Shoemaker.
* Named in honor of J. Bruce Bredin, sponsor of
the Expedition.
a very small triturating surface which is armed
with several slender teeth and a long seta; palp,
3-jointed, the second joint the longest. Mawilla 1,
inner plate broad and bearing 2 plumose setae;
outer plate with 7 spine-teeth which are nearly
simple; palp 2-jointed, second joint bearing 3
slender terminal spines. Maxilla 2, inner plate a
little wider but shorter than outer plate and
armed with 7 spines; outer plate with 5 spines.
Maxilliped, inner lobe reaching little beyond
base of outer lobe, and armed distally with 3
slender spine-teeth and 3 setae; outer lobe
reaching only to base of second joint of palp,
armed distally with 3 spine teeth and 1 seta, on
the inner margin with 4 setae; palp 4-jointed,
fourth joint well developed, with a comb of fine
spinules on inner surface, and bearing a slender
nail having a spine and a seta at its base. Up-
per lip symmetrical. Lower lip with inner lobes
poorly developed; side lobes short and blunt.
Gnathopod 1, longer and stronger than 2; sec-
ond joint rather short, not as long as the sixth,
somewhat, expanded for the greater part of its
length; third joint short; fourth joint about as
long as the fifth and with a brush of fine setae
on lower margin; fifth joint produced below into
a narrow lobe carrying a few spines; sixth joint
very large and strong, widest proximally and
converging to a narrow apex, rear margin short;
palm very oblique and without defining angle,
shghtly convex, on the outside armed with about
20 short slender submarginal branched spines,
and with a group of 3 slender spines at center, a
row of 10 rather stout branched spines beginning
on the rear margin of the joint and extending a
short distance into the palm, each of these spines
having a slender spine springing from its base; on
the inside of palm there is a groove into which the
seventh joint fits, defined by a row of 3 stout
spines and a group of slender spines, below which
is another row of 4 spines (Fig. 1, 7); seventh
joint long, ending in a short nail, on the inner
margin are 2 short spinules distally and 1 spinule
near the center, on the outer margin are 2 short
setae. Gnathopod 2, second joint not as much ex-
panded as that of gnathopod 1, and about as long
as the sixth joint; fifth joint half the length of the
274 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, No. 8
Fic. 1.—Bogidiella bredini, n. sp., female holotype: a, Entire animal, lateral; 6, antenna 1, showing
accessory flagellum; c, antenna 2; d, mandible; e, maxilla 1; f, maxilla 2; g, maxilliped; h, maxilliped
enlarged, showing outer lobe; 7, maxilliped enlarged, showing inner lobe; j, lower lip; k, gnathopod 1;
1, gnathopod 1, sixth joint, inside of palm; m, gnathopod 2; n, gnathopod 2, inside rear margin of sixth
joint; 0, peraeopod 1; p, peraeopod 3; q, peraeopod 5, distal end; r, pleopod 1; s, uropod 3; ¢, telson.
AUGUST-SEPTEMBER 1959
sixth, with the lower lobe rather broad and carry-
ing a few spines and a brush of fine scales or setae
on rear margin; sixth joint widest in the middle,
rear margin with 7 groups of spines; palm about
as long as the rear margin of joint, very oblique,
slightly convex, without defining angle, but hav-
ing a row of 5 or 6 spines where the palm curves
into the rear margin of joint; on the outside of
the palm is a row of 15 or 16 slender curved
bifureate submarginal spines extending almost
the entire length of the palm, and a group of 3
long slender spines near the center; on the inside
of the palm near its juncture with the rear margin
of the joint are 3 rows of spines, the first or distal
of group consisting of 3 spines, the second group
of 4 spines, and the third of 5 spines, below these
spines are 2 groups of slender spines (Fig. 1, 7)
and a narrow brush of fine setae adjacent to the
rear margin of the joint; seventh joint fitting
palm, and resembling that of gnathopod 2.
Peraeopods 1 and 2 are alike and carry rather
few spines. Peraeopod 2, second joint much longer
than any of the following joints and little ex-
panded; fourth jomt not quite as long as the
fifth and sixth combined; seventh joint short,
nearly straight, with a spinule on the inner mar-
gin, and bearing a small nail with a seta at its
base. Peraeopod 38, about as long as 2, but shorter
than 4; second joint. little expanded and much
longer than any of the succeeding joints; fourth
joint not quite as long as the fifth and sixth com-
bined; seventh joint like that of peraeopods 1 and
2 but a little longer and having 2 spinules on inner
margin. Peraeopod 4, like 3, but longer; seventh
joint broken, so the number of spinules could
not be determined. Peraeopod 5 very much like
4, but much longer and with longer and more nu-
merous spines; second joint about as long as the
fourth, which is about equal in length to the
fifth; fifth jomt a little shorter than the sixth;
seventh joint nearly half as long as the sixth,
slender, with 8 slender spinules on inner margin,
a sensory seta on outer margin, and having a
small nail with a seta at its base.
Uropods 1 and 2 reaching back about the same
distance. Uropod 1, much longer than 2; peduncle
nearly twice as long as the subequal rami, a spine
on lower margin near the proximal end, and a
spine at the distal end of the outer and inner mar-
gin; rami without lateral spines, but with distal
spines. Uropod 3, very long, peduncle not half as
long as the subequal rami, and bearing a spine
on the upper outer margin and one at the distal
SHOEMAKER: THREE NEW CAVE AMPHIPODS
2795
end of the lower margin; outer ramus with 3
groups of lateral spines, and a group of terminal
spines; inner ramus with 3 spines on inner mar-
gin, 2 on outer margin, and a group of terminal
spines. Telson short, broader than long, sides
convex, rear margin nearly straight and with 2
spines and 2 setae at either side.
Pleopods alike, but the third is the shortest.
Pleopod 1, peduncle much longer than outer
ramus, which consists of 3 joints, each consecu-
tively shorter, and each bearing 2 plumose setae;
inner ramus reduced to a very small single joint
bearing a long terminal plumose seta. Pleopod 2
is like pleopod 1. Pleopod 3 is like 1 and 2, but
shorter.
The coxal plates are all shallow and are as
shown in Fig. 1, a. The metasome segments are
as shown in Fig. 1, a. The branchiae occur on
gnathopod 2 and peraeopods 1-4, and are rather
narrow simple sacs. Marsupial plates occur on
gnathopod 2 and peraeopods 1-3. The marsupial
plates are narrow and rather short, and carry
very few setae. Length of animal from front of
head to the end of uropod 3, about 7 mm.
Maue: Length 5.8 mm. Its characters agree
closely with those of the female, but several
peraeopods are missing. A pair of small genital
papillae is present on the ventral surface of the
seventh peraeon segment; to the right one is at-
tached a slender filament, coiled distally. Under
high magnification the filament is seen to be made
up of minute granules, which appear to be sper-
matozoa.
Types—Holotype, female, US.N.M. no.
102418. Allotype, male, U.'S.N.M. no. 102419.
Two species of Bogidiella have been described
from the Americas, B. neotropica by Sandra
Ruffo (1952) from a small brook, tributary to the
Rio Cupari, Brazil, and B. brasiliensis by Rolf
Siewing (1953) from Bahia and Ilhabela, Brazil.
B. neotropica, described from a single specimen
about 3 mm in length, is the largest species here-
tofore described, but it is much smaller than the
present species which measures about 7 mm. In
some of its characters B. bredini is much like B.
neotropica, and whether the disagreements which
occur are due to greater maturity of B. bredini
or differences in sex, cannot be determined from
the known material. The pleopods of B. neotrop-
ica have only one ramus each, while in B. bredini
each has a well-developed outer ramus and a very
much reduced inner one. In B. neotropica the ac-
cessory flagellum has 2 well-developed joints and
276
a smaller terminal joint, while in B. bredini there
are 3 well-developed joints and a smaller terminal
joint. No spines or setae are shown on the dactyls
of the peraeopods of B. neotropica, but in B. bre-
dini all of the dactyls have them, the last having
as many as eight. B. brasiliensis, while less than
2 mm in length, has two rami to the pleopods,
with the inner ramus much less reduced than in
B. bredini. The telson is long in proportion to its
width, and has a small median lobe distally. The
first antenna is nearly twice as long as the second,
and bears a unisegmental accessory flagellum.
Of the remaining three species of Bogidiella,
only B. skopljensis (Karaman, 1935) from
Skoplje, Yugoslavia, has biramous pleopods, and
it differs markedly from B. bredini in the form
and armature of the antennae, peraeopods, and
telson.
Family GAMMARIDAE
Genus Metaniphargus Stephensen, 1935
Metaniphargus nicholsoni,’ n. sp.
Figs. 2, 3, a-o
Material examined—Thirty specimens from
Dark Cave, Barbuda, collected during the Smith-
sonian-Bredin Expedition. Also, more than 100
specimens collected in Dark Cave by G. A. Sea-
man in November 1955 and donated by him to
the U.S. National Museum.
Description—-Ma.E: Head and antennae are
as shown for the female (Fig. 2,a), but possibly
the antennae are a little longer in the male; ac-
cessory flagellum as long as the first jot of the
primary flagellum and consisting of one long
joint and a very short terminal joint. Eyes not
present.
Upper lip symmetrical. Mandible, cutting-edge
toothed; accessory plate strong, 3-pronged;
spine-row of 2 stout plumose spines and several
slender spines; molar strong, triturating surface
narrow with a tuft of setae at the front end and
a long plumose seta at the rear end; palp 3-
jointed, first joint over half the length of the
second, which is about equal in length to the
third; third joint is pectinate on the lower mar-
gin and carries a distal group of long spines.
Maxilla 1, inner plate broad and carrying about
20 long plumose setae on its straight outer mar-
5 Named in honor of Desmond Nicholson, captain
of the Expedition’s vessel, Freelance, who collected
the amphipods here described.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 8
gin; outer plate armed with 11 strong pectinate
spine-teeth; palp 2-jomted, and armed distally
with 6 strong spine-teeth and one long slender
seta. Maxilla 2, outer plate wider, but a little
shorter than the inner; inner plate carrying a
diagonal row of closely-set plumose setae, besides
the distal and marginal spines. Maxilliped, inner
plate reaching beyond the middle of the outer
plate, armed distally with 3 rather stout spine-
teeth and a row of subdistal plumose setae which
continues part way down the inner margin; outer
plate reaches to about two-thirds the length of
the second joint of the palp, armed distally with
3 long plumose spines, and on the inner margin
with a row of about 11 stout spime-teeth and a
submarginal row of slender spines; palp 4-
jointed, fourth joint about two-thirds the length
of the third, armed with a nail and carrying a
diagonal row of 5 closely set ridges or setae on
the inner surface. Lower lip without inner lobes,
and with short blunt side lobes.
Gnathopod 1 (Fig. 2, f), shorter than 2; second
joint expanded, a little longer than the fifth joint,
a few short spines on front margin, 4 groups of
long spines of 2 spines each on rear margin, and
3 long backward-directed submarginal spines
near the proximal end of rear margin. Third and
fourth joints short and rather stout, the fourth
with a brush of setae on lower margin; fifth joint
much longer and a little wider than the sixth,
lower margin bearing 5 or 6 groups of spines,
some of which are bifurcate at apex; front mar-
gin with a group of spines near the middle and a
distal group; sixth joint about two-thirds as long
as the fifth, widest in the middle, front margin
shg¢htly convex and bearing an apical and a sub-
apical group of spines, rear margin straight and
bearing three groups of spines, the longer of which
are bifureate at apex; palm transverse, slightly
convex, smooth, defined on the outside by 3 slen-
der bifureate spines, with 3 shorter straight sub-
marginal spines between these and the hinge of
the seventh joint, and a curved spine just before
the hinge, at the defining angle on the inside of
palm are 2 short, stout bifurcate spines, 2 straight
spines near the middle and a curved distal spine;
seventh joint fitting palm, bearing a nail, which
is about one-third the length of the joint, at the
base of which are a forward-pointing tooth and a
seta, Inner margin with a submarginal seta, outer
margin of joint with a forward-curving seta.
Gnathopod 2 (Fig. 2, h) a little stouter and much
longer than 1, second joint expanded, about as
AUGUST-—SEPTEMBER 1959 SHOEMAKER: THREE NEW CAVE AMPHIPODS DUG
SK
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MWA NN XS .
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Fic. 2.—Metaniphargus nicholsoni, n. sp., a-e, g, 7-1, female; f, h, male: a, Anterior end, lateral; b,
mandible; c, maxilla 1; d, maxilla 2; e, maxilliped; f, gnathopod 1; g, gnathopod 1; h, gnathopod 2; 2,
gnathopod 2; 7, distal end of gnathopod 2; k, peraeopod 2; /, peraeopod 3.
278
long as the sixth, with a small spine on front
margin, and 5 groups of 2 spines each on rear
margin; third and fourth joints short and stout;
fifth joint a little shorter and a little wider than
the sixth, widest distally, outer margin with a
small median spine and a distal group, rear mar-
gin convex, with a brush of fine spinules or setae
and 10 or 11 groups of spines, the longest member
of each being bifureate at apex; sixth joint long
and narrow, widest in the middle, both front and
rear margin slightly convex, front margin with 2
short spines and a distal group, inner margin with
a brush of 5 setae and 4 groups of spines, some of
which are serrate and the longest one in each
group is serrate and bifurcate at the apex; on the
inside of the sixth joint are 6 groups of spines
near the front margin; palm very oblique, nearly
as long as the rear margin of joint, nearly straight,
smooth, without defining angle, grooved along its
length, the edges of the groove bearing a series of
blunt spines, a group of long setae at either end
of the groove; seventh joint fitting palm, with a
seta on the outer margin near the proximal end,
inside margin of joint has what appear to be a
number of slender forward pointing teeth, but
they are so closely appressed to the margin that
at first they appear to be part of the cuticle.
Peraeopods 1 and 2, slender and about equal in
size and form. Peraeopod 2, second joint not much
expanded and as long as the fourth and fifth
joints combined, front margin bearing about 6
short spines, rear margin with 4 short spines on
lower half and 3 long spines on upper half; fourth
joint scarcely at all expanded and a little longer
than the fifth; fifth and sixth joints not ex-
panded and equal in length; seventh joint short
and bearing a short nail with a spinule and a seta
at its base. Peraeopod 3, much longer than 2;
second joint considerably expanded, about four-
fifths as wide as long, front margin convex and
armed with about 11 spines, rear margin nearly
straight, with an upper and lower lobe; fourth
joint little expanded and a little shorter than the
fifth; fifth jomt very little shorter than the
sixth; fourth to sixth jomts bearing groups of
spines on their front and rear margins; seventh
joint short and like that of the second peraeopod.
Peraeopod 4, second joint considerably expanded,
nearly as wide as long, front margin less convex
than in 3 and armed with 10 spines, rear margin
slightly convex and with an upper and lower lobe;
the third to seventh joints are like those of perae-
opod 3, but longer and a little stouter. Peraeopod
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 8
5 (Fig. 3, f), second joint narrower in proportion
than that of 3 or 4, about three-fourths as wide
as long, front margin a little convex and armed
with 7 spines, rear margin a little convex and with
an upper and lower lobe, the upper lobe being
not as pronounced as in peraeopod 3 or 4, and
the spines in the serrations being stouter than in
3 or 4; the third to seventh joints are like those
of peraeopod 4, but are a little stouter.
Uropod 1 and 2 extending back about the same
distance; uropod 3 extending back much farther.
Uropod 1, peduncle a little longer than the inner
ramus, upper outer margin with 2 lateral and 2
distal spines, the lower of which is the stouter,
inner margin with 2 lateral spines and one distal
spine, lower margin with one spine; outer ramus
without lateral spines but with a terminal group;
inner ramus with one lateral spine and a terminal
group. Uropod 2, peduncle as long as the inner
ramus, without spines on upper outer margin,
and with one distal spine on the upper inner mar-
gin; outer ramus shorter than the inner and with-
out lateral spines but with a terminal group;
inner ramus with one lateral spine on outer and
one on inner margin and a distal group. Uropod
3, peduncle much shorter than outer ramus, but
about two-thirds as long as the inner ramus,
upper outer margin with 2 distal spines, and inner
margin with one; outer ramus with a small second
joint, first jot with 3 groups of spines on the
outer margin, inner margin with 6 groups of
spines, 2 in each group being short and stout, and
one longer and plumose, distal margin with a
group of spines; second joint short, narrow and
conical, with a lateral spinule and 2 apical spi-
nules; inner ramus slender, about half as long as
outer ramus, and with sides converging to a sharp
apex, outer margin with one lateral spine and a
very small spinule near the apex; inner margin
with 3 spines. Telson short, extending to about
the end of the peduncle of uropod 3, divided to its
base, each lobe converging to a narrow, sharp
apex, outer margin of each lobe with one spine,
inner margin of each lobe with 2 lateral spines
and 2 apically, all spines being branched at apex
(Fig. 3, 0).
Coxal plates 1-5 are deeper than their body
segments. Coxal plate 1, front margin convex and
rear margin concave, with a few spines on the
front and lower margin. Coxal plate 2 like that
of 1, but a little wider and deeper. Coxal plates
3 and 4 much alike, a little deeper than 2, and
with lower margin evenly rounding. Coxal plate
AUGUST-SEPTEMBER 1959
5 is the largest and deepest, the front lobe is
twice as deep as the rear lobe and extends down
about two-thirds the length of the second joint
of the peraeopod (Fig. 3, 6). Coxal plate 6 with a
small front lobe (Fig. 3, e). Coxal plate 7 is as
shown by Fig. 3, f. Metasome segments are as
shown for the female by Fig. 3, h.
Urosome segment 1 with a single small spinule
on either side of the rear dorsal margin, and uro-
some segment 2 with 2 spinules similarly placed.
Pleopods all well developed. There does not ap-
pear to be any unusual character at the base of
the outer ramus of the third pair, such as occurs
in M. curasavicus. The branchiae occur on gna-
thopod 2 and peraeopods 1-4, and are large, oval,
simple and attached to the limb by a peduncle.
Length of the male about 7 mm.
FEMALE: The female is very much like the male
and differs only in detail. All of the figures here
given of the female or of a fully developed ovi-
gerous specimen. The head, antennae and front
part of the female are shown by Fig. 2, a. Gnatho-
pod 1 is proportionately shorter and stouter than
in the male; fourth joint with a brush of fine
setae on lower margin; the palm of the sixth
joint is transverse, smooth, with 3 short median
spines, a curved spine at the base of hinge, and 3
short stout bicuspid spines on the outside at the
defining angle, and on the inside at the defining
angle are 3 long slender spines which appear to
have 3 apical branches; the seventh joint has on
the outer margin a sensory seta, and on the inner
margin one or 2 small teeth or spines proximally,
and a long nail with a forward-pointing tooth and
a seta at its base. Gnathopod 2 is a little stouter
than that of the male.
Peraeopods 1 and 2 very much like those of
the male. Peraeopod 3 much like that of the
male; longer than peraeopod 2, but shorter than
4, which is about as long as 5; the front lobe of its
coxal plate is even larger in proportion than that
of the male. Peraeopods 4 and 5 much like those
of the male, but the second joint is longer and
narrower in proportion, and that of 4 has the
upper rear lobe more developed. The metasome
segments are as shown by Fig. 3, h. The first
urosome segment has one dorsolateral spinule on
either side, and the second segment has 3 on either
side (Fig. 3, 7). The pleopods are like those of
the male.
Uropods 1 and 2 are alike in both sexes. Uropod
3 is like that of the male, but is somewhat less
spinose. The telson is very similar to that of the
SHOEMAKER: THREE NEW
CAVE AMPHIPODS ZS
male; outer margin of each lobe with 2 marginal
spines, inner margin with one lateral spine and
one just below the apex, all the spines being
branched apically (Fig. 3, n). The branchiae are
like those of the male, and occur on gnathopod 2
and peraeopods 1-4. The marsupial plates are
narrow, and carry few setae (Fig 2,1, k). The fe-
male reaches a length of 7.5 mm.
Types —Holotype, male, U.S.N.M. no. 102424;
allotype, female, U.S.N.M. no. 102425; and 28
paratypes, all from Dark Cave, Barbuda, col-
lected by Desmond Nicholson, April 25, 1958.
M. nicholsoni is very similar to M. beattyi
Shoemaker, 1942, from slightly brackish water in
a deep well, St. Croix, Virgin Islands.‘ It differs
in details of the armature of the appendages and
most obviously in the shape and armature of the
telson. In M. beattyi the telson is relatively
shorter and broader; each lobe bears two apical
spines and a single spine on the distal part of the
outer margin; there are no spines on the margins
of the cleft as in M. nicholsoni. In M. curasavicus
Stephensen, 1933, however, the armature of the
telson is more similar to that of 1. nicholsoni.
Paraweckelia, n. gen.
Head with prominent lateral lobes, and without
eyes. Antenna | longer than antenna 2, with a
4-jointed accessory flagellum. Upper lip sym-
metrical. Mandible with toothed cutting-edge,
strong accessory plate, well-developed molar, and
a 3-jointed palp. Manilla 1 with a row of plumose
setae on inner plate, 9 spine-teeth on outer plate,
and a 2-jointed palp. Maxilla 2 without a diagonal
row of spines or setae on inner plate. Maxilliped
with inner and outer plates well developed, and
with a 4-jointed palp. Lower lip with inner lobes.
Gnathopod 1 smaller than 2; both subchelate.
Gnathopod 1 with fifth joint longer than the
sixth; palm of sixth joint only slightly oblique.
Gnathopod 2 with fifth joint much shorter than
sixth and with a rear lobe. Peraeopods 3-5 with
expanded second joint. Coxal plate 4 incised in
rear. Pleopods normal, not reduced. Uropods nor-
mal and with all rami well developed. Uropod 3
with 2-jointed outer ramus. Branchiae simple,
not attached by a pedicel. Marsupial plates nar-
row, with few setae. Telson cleft to base. Type,
P. silva, n. sp.
*Stephensen (1948) considered M. beattyi to be
identical with M. curasavicus Stephensen, 1933,
from Aruba, Curacao, and Bonaire. It has not been
possible to determine from Mr. Shoemaker’s notes
whether he agreed with Stephensen—T. E. Bow-
MAN.
280 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES — VOL. 49, NO. 8
Fic. 3.—a-o0, Metaniphargus nicholsoni, n. sp.: a, Peraeopod 2, male; 6, peraeopod 3, male; c, peraeo-
pod 4, female; d, peraeopod 5, female; e, peraeopod 4, male; f, peraeopod 5, male; g, pleopod 1, female;
h, metasome segments, lateral, female; 7, urosome segments, lateral, male; 7, uropod 1, female; k, uropod
2, female; /, uropod 3, female; m, telson, female; n, left half of telson, female; o, right half of telson,
male. p-t, Paraweckelva silvat, n. sp., female: p, Mandible; q, lower lip; 7, maxilla 1, palp; s, gnatho-
pod 1; ¢t, palm of gnathopod 2.
AUGUST-SEPTEMBER 1959
Paraweckelia silvai, n. sp.
Figs. 3, p-t; 4
Material examined—Ten specimens, collected
by Gilberto Silva Taboada in a fresh-water lake,
Lago Marti, in Cueva Grande, the largest of the
Caguanes Caves, a group of five caves located in
Punta Caguanes, north coast of Las Villas Proy-
ince, Cuba, February 1958.
Description—FrmMa.e: Head with prominent
rounding lateral lobes. Without eyes. Antenna 1,
longer than 2; first joint equal in length to the
second; third joint nearly half the length of the
second; flagellum composed of about 30 joints;
accessory flagellum of 4 joints. Antenna 2, first
joint nearly circular and very prominent, gland-
cone prominent; third joint about one-third as
long as the fourth, which is equal in length to the
fifth; flagellum not as long as the peduncle and
composed of about 12 joints, the first of which is
the longest.
Upper lip, symmetrical. Mandible, cutting-
edge toothed, accessory plate, strong, armed with
2 distal teeth, a row of smaller teeth on outer
margin and a brush of setae on inner margin
(Fig. 3, p); spine-row of seven spies; molar
prominent, its base produced forward into a nar-
row prominent process which extends beyond the
base of the palp; triturating surface rather long
and narrow and carrying a long plumose seta;
palp 3-jointed, second joint longest, first and
third being equal in length, second and third
joints with very few spines. Manilla 1, mner plate
with 7 plumose setae; outer plate with 9 toothed
spine-teeth; palp 2-jointed, and armed distally
with 8 slender spines. Maxilla 2, inner and outer
plate about the same size and length and each
carrying very few spines; inner plate without
diagonal row of spines. Maxilliped, inner plate
reaching to about the base of the second Joint
of the palp and armed distally with 5 shghtly
curved spine-teeth and a row of plumose spines
or setae which extends part way down the inner
margin; outer plate not extending to the middle
of the second joint of palp, armed distally with
several spines, inner margin armed with rather
stout spine-teeth and a few slender spines; palp,
with 4 joints, the second of which is much the
longest; fourth joint almost as long as the third,
with a comb of fine setae or spinules on inner
5 Named in honor of Gilberto Silva Taboada,
who collected the new species and donated them
to the U. S. National Museum.
SHOEMAKER: THREE NEW CAVE AMPHIPODS
281
surface, and with a small nail. Lower lip with
broad outer lobes, narrow inner lobes, and with
short blunt lateral processes.
Gnathopod 1, smaller than 2, second joint ex-
panded and not quite as long as the fifth and
sixth combined; fourth joint with a brush of
setules and a few spines on rear margin; fifth
joint longer than the sixth and with about 9
groups of long spines on rear margin; sixth joint
widening distally, front margin with a few spines,
rear margin with 2 groups of spines, palm con-
vex, very finely toothed throughout, defined by
a spine with a long thin branch, armed with
about 7 submarginal branched spines, and with
a curved spine just before the hinge of the
seventh joint; inside of palm with a group of 5
spines at the defining angle, and with about 12
submarginal branched spines; seventh joint fit-
ting palm, a sensory seta on the outer margin
and 3 setules on inner margin. Gnathopod 2,
second joint not much expanded and not as long
as the sixth; fourth joint with rear margin pro-
duced forward rather sharply; fifth joint, front
margin with one median spine, lower margin with
a few spines; sixth joint very large, widest
through the center, front margin with a few scat-
tered spines and a distal group, rear margin with
4 groups of spines, palm convex, longer than the
rear margin of the joint, crenulate, armed with
about 18 short branched spines and defined by
a long spine on the outside and one on the in-
side, each of which has a long slender branch
(Fig. 3, t); seventh joint fitting palm, and ap-
parently unarmed.
Peraeopods 1 and 2 slender and nearly equal
in form and length. Peraeopod 1, second joint
very little expanded, as long as the fourth and
fifth combined; fourth joint very little expanded
and about as long as the sixth; fifth joint shorter
than the sixth; seventh joint about a third as
long as the sixth, with a spinule on inner margin,
and with a curved nail. Peraeopod 3, longer than
1 or 2, but shorter than 4, second joint expanded,
front margin convex and spinose, rear margin al-
most straight, shghtly serrate, spose, and with
a lower lobe; fourth joint little expanded and
not as long as the fifth; fifth joint not as long as
the sixth; seventh joint about a fourth as long
as the sixth joint, and much like that of peraeo-
pod 1. Peraeopod 4, shorter than 5; front and
rear margins of second joint convex and spinose,
rear margin with a rather shallow lower lobe;
fourth, fifth, and sixth joints proportionately
bo
ee)
bo
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, No. 8
Fie. 4.—Paraweckelia silvai, n. sp., female: a, Anterior end, lateral; 6, maxilla 1; c, maxilla 1, apex of
outer plate (only 6 of the 9 spines shown); d, maxilla 1, inner plate; e, maxilla 2; f, maxilliped; g, maxilli-
ped, outer plate; h, maxilliped, inner plate; 7, peraeopod 1; 7, peraeopod 2; k, peraeopod 3; 1, peraeopod
4; m, peraeopod 5; n, 0, p, metasome segments 1, 2, and 3, respectively, lateral; g, pleopod 3; r, uropod
1; s, uropod 2; ¢, telson.
AUGUST-SEPTEMBER 1959
as in peraeopod 3, but longer; seventh joint
about a third as long as the sixth. Peraeopod
5, proportionately much like 4, but longer;
second joint with upper rear margin straight;
seventh joint straight, about a third as long as
the sixth, and is as shown by Fig. 4, m.
Coxal plates 1-4 deeper than their body seg-
ments, the first three with evenly rounding spi-
nose lower margins. Coxal plate 4 much broader
than the preceeding, rear margin deeply incised.
Coxal plate 5, with a shallow front lobe. Coxal
plates 5-7 as shown in Fig. 4, k, 1, m.
Branchiae are simple oval sacs, without pedi-
cels, and occur on gnathopod 2 and peraeopods
1-4. The marsupial plates are narrow, carry
few setae and are attached to gnathopod 2 and
peraeopods 1-3. The metasome segments are as
shown by Fig. 4, n, 0, p. Metasome segments 1-3
and urosome segment 1 each has two postero-
median dorsal setae, and urosome segment 2 has
a small spine on either side of the posterodorsal
surface.
Pleopods, normal and well developed, outer
ramus the shorter.
Uropod 1 reaches back a little farther than
2, and uropod 3 much farther than 1. Uropod
1, peduncle much longer than inner ramus, which
is longer than the outer; the armature of spines
is shown by Fig. 4, r. Uropod 2, much like uropod
1, but there are no spines on the peduncle except
the distal one. Uropod 3, peduncle about a third
as long as the outer ramus, which has small, nar-
row second joint; inner ramus a little shorter
than the outer, and the spine arrangement of
the uropod is shown by Fig. 4, s. Telson reaches
back to about the end of the peduncle of uropod
3, about as broad as long, cleft nearly to its
base, each lobe converging to a narrow indented
apex containing a spine and a seta, and each outer
lateral margin bearing 2 plumose setae. Length
from front of head to end of uropod 3, about 12
mm.
Mate: The male is like the female, and can be
distinguished only by the absence of marsupial
SHOEMAKER: THREE NEW CAVE AMPHIPODS
283
plates and the presence of male genitalia. The
males in the present lot are about the size of
the females except the male type which measures
about 15 mm.
Types—Holotype, male, U.S.N.M. no. 102461.
Allotype, female, U.S.N.M. no. 102462, and
eight paratypes.
The new genus, Paraweckelia, is closely related
to the genus Weckelia Shoemaker, 1942, contain-
ing the single species W. caeca (Weckel) from
Modesta Cave, near Canas, Cuba. The most im-
portant difference is in the structure of the man-
dibular palp, which consists of the usual three
joints in Paraweckelia, but is reduced to a single
small joint in Weckelia. In addition, the oblique
row of setae on the inner plate of the second
maxilla of Weckelia is absent in Paraweckelia.
LITERATURE CITED
Hertzoc, Louts. Bogidiella albertimagni sp. n., ein
neuer Grundwasser amphipode aus der Rheine-
bene ber Strassburg. Zool. Anz. 102: 225-227.
1933.
. Crustacés des biotopes hypogées de la
Vallée du Rhin d Alsace. Bull. Soc. Zool.
France 61: 356-372. 1936.
KaraMANn, Stanko. Uber zwei newe Amphipoden,
Balcanella und Jugocrangonyx, aus dem Grund-
wasser von Skoplje. Zool. Anz. 103: 41-47.
1933.
RurFro, Sanpro, Bogidiella neotropica n. sp., NUOVO
Anfipodo dell’ Amazonia. Riv. Svizzera Idro-
logia 14: 129-143, 1952.
SHOEMAKER, CLARENCE R. Notes on some American
fresh-water amphipod crustaceans and de-
scriptions of a new genus and two new species.
Smithsonian Misc. Coll. 101 (9): 1-31. 1942.
Srewinc, Roir. Bogidiella brasiliensis, e2n newer
Amphipode aus dem Kiistengrundwasser Bra-
stliens. Kieler Meeresforschungen 9 (2): 243-
247. 1953.
STEPHENSEN, Knut. Fresh- and brackish-water Am-
phipoda from Bonaire, Curacao, and Aruba.
Zool. Jahrb. (Abt. Syst.) 64 (3/5): 415-436.
1933.
. Amphipods from Curacao, Bonaire, Aruba
and Margarita. Studies on the Fauna of Cura-
cao, Aruba, Bonaire and the Venezuelan Islands
3 (11): 1-20. 1948.
284 JOURNAL OF THE
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 8
ZOOLOGY .—Antrogonodesmus, a new chelodesmoid genus from Cuba, and a re-
description of Amphelictogon dolius Chamberlin (Polydesmida, Chelodesmidae).
Ricuarp L. Horrman, Blacksburg, Va.
(Received June 16, 1959)
So far less than 80 species of Diplopoda
have been recorded from Cuba, a small
number which reflects inadequate collecting
rather than an impoverished fauna. More
than half of the known species have been
taken in the mountains of Oriente Province,
and it seems reasonable to presume that
attention to other parts of the island will
ereatly augment our knowledge of the milli-
peds of Cuba. The first large contribution
to this general subject was made in 1918,
when R. V. Chamberlin described a con-
siderable number of Cuban species (un-
fortunately without illustrations), the ma-
jority of which are still known only from
the original types. In recent years H. F.
Loomis has added a large number of new
species to the list, and redescribed some of
the older ones.
Two separate collections of Cuban dip-
lopods, received by the U. 8. National Mu-
seum and kindly transmitted to me for
study by Dr. Ralph E. Crabill, are of ex-
ceptional interest. One includes a remarka-
ble new genus of the Chelodesmidae without
close relatives elsewhere in the family; the
other contains male specimens of Amphelic-
togon dolius, a species originally based on
females and not subsequently rediscovered.
Family CHELODESMIDAE Cook
The status of this name has been the subject
of much dissention ever since its proposal in
1895, but with the recent discovery that the
type genus is subjectively synonymous with the
older name Eurydesmus, plus the latest (Copen-
hagen, 1953) decisions concerning the formation
of family names, there ean hardly be any doubt
that it is the correct name for the group of
genera which has long been called the family
Leptodesmidae by most European workers. A
detailed study of classification within the limits
of this huge group and its satellite families is in
preparation at this time, and should settle the
question of how much ground should be covered
by the name Chelodesmidae in a stricter sense
than now employed.
On the basis of work completed to date, it can
safely be said that of the two genera here dis-
cussed, at least Amphelictogon is very closely
related to both Eurydesmus and Leptodesmus,
falling in the same family with the former and
in the same subfamily or tribe with the latter
genus. This association is made on the basis of
comparison with material of species strictly
congeneric with the type species of the three
genera named, including newly-found characters
of antennal structure, form of the 2nd leg pair,
body shape and proportion, paranotal configura-
tion, and formation of the male genitalia. Less
can be said concerning the status of Antrogono-
desmus although it is obviously a member of
the Chelodesmidae in a restricted sense.
Antrogonodesmus, nD. gen.
Type species —Antrogonodesmus curiosus, 0.
NM
Dp:
Diagnosis ——A remarkable chelodesmid genus
differmg from all other known genera by the
form of the gonopods. The coxae are normal for
the family in shape, mode of connection, and
presence of-a long coxal process, but the pre-
femora are greatly enlarged and impressed on
the ventral side into a deep cavity densely
beset with long macrosetae. The prefemoral
process is short and distally biramous, one of the
divisions forming a shield for the solenomerite.
The latter is short and laminate, slender, un-
modified, largely concealed by the prefemoral
process and by a femoral process which is some-
what expanded and functioning as a solenophor.
Body form chelodesmid, e.g., with the an-
terior four of five segments broadest and the
following paranota becoming gradually reduced
IN size in going caudad and well separated from
each other by the large prozonites which are
only partly included by the preceeding meta-
zonites. A distinct interzonal furrow in the seg-
mental constriction. Pore formula normal, the
pores opening near the end of slender elongate
peritremata. Tergites, pleurites, and sternites
all smooth and glabrous, without any surficial
modifications. Legs long and slender, virtually
glabrous, those of the male sex with distinct
AUGUST-SEPTEMBER 1959
tibial pads extending back as far as the eighth
segment.
Antrogonodesmus curiosus, 0D. sp.
Fics. 1-4
Type specimens—Male holotype and female
paratype, U.S. Nat. Mus. (Myriapod Type no.
2581), from San Vicente, Pinar del Rio Province,
Cuba, collected in June 1956, by N. L. H.
Krauss.
Diagnosis—With the characters of the genus.
Specific characters probably are reflected in the
size, color pattern, and gonopod configuration.
Description—Male holotype: an elongate,
slender, caudally attenuate chelodesmoid, the
paranota of segments 2-4 rather broad, trans-
verse, almost horizontal, subrectangular, those
following gradually decreasing in size. Length,
approximately 34 mm., widths of selected seg-
ments as follows:
Collum
2d
3d
4th
6th
10th
16th
18th
.lmm
CO He He He Or Or Or Or
Nore om ©
Body chiefly tan to a light testaceous-brown,
the intersegmental constriction more darkly pig-
mented across dorsum. Caudolateral corners of
paranota, the entire collum, and large mid-
dorsal spots on the 2d and 3d segments chalky
white. Antennae, legs, and underparts hight tan
to nearly colorless.
Head convex, smooth, polished, the vertigial
groove very distinct and extending down to
middle of interantennal isthmus. latter broad,
twice length of first antennal article. Frons and
clypeus with numerous scattered setae, these
extending laterad well onto the genal surfaces,
latter only slightly convex without flattened
margins, a little smuate. Labrum with about 28
stout setae, the series merging into the 3 large
genal marginal setae on each side.
Antennae moderately long (5.0 mm) and slen-
der, reaching back to 3rd segment; all of the
articles moderately setose but vestiture imcreas-
ing distally; article 7 cylindrical, apically
rounded, the free margin inturned between and
separating the 4 sensory cones, outer (dorsal)
side of article with a small rounded sensory area.
Relative lengths of antennal articles, in de-
creasing order: 2-3-4-5-6-1-7 (perhaps abnor-
mal).
HOFFMAN: A NEW CHELODESMOID GENUS 285
Collum broader than head, smooth, convex,
anterior margin an even arc, almost a semi-
circle; median fourth of caudal margin rather
deeply concave. Anteriolateral edge of set off by
a fine groove extending dorsad as far as base of
mandibles. Lateral corners almost rectangular.
A row of six widely spaced submarginal micro-
setae along the rear edge of the segment.
Second segment slightly broader than the
others, the paranota broad and only slightly de-
pressed, not tilted cephaloventrad; the paranota
margined only on anterior edges, lateral and
caudal edges continuous with dorsal surface.
Segments 2-4 with small but distinct scapular
dentations, these segments all essentially similar
in size and shape. In going caudad from 5th seg-
ment the paranota become increasingly reduced,
the anterior corners become more oblique and
the posterior more acutely produced. On all
poriferous segments the peritremata are elongate
and slender, the pores opening dorsolaterally
almost at their posterior ends.
Prozonites and metazonites of equal size, sepa-
rated by a broad, smooth, interzonal furrow in
the convexity of a distinct intrasegmental con-
striction. Surface of segment smooth and _ pol-
ished, without granulations or perceptible setal
sockets.
Paranota of 19th segment rudimentary lobes
just large enough to carry the pores, scarcely
extending beyond caudal margin of the segment.
Anal segment small, the epiproct short, bluntly
conical, bent slightly ventrad. Anal valves
smooth, with a median setiferous convexity, the
mesial edges produced as raised rims, the mar-
ginal setiferous tubercules small, set quite high
on the valves, and separated from the marginal
rims. Hypoproct large, subcircular, the median
projection broad and low but distinct between
the small paramedian tubercules.
Pleural areas entirely smooth, unadorned;
stigmata small and opening almost flush with
the surface just above and in front of the coxae.
Sterna broad, glabrous, unmodified, the legs
inserted into an abruptly elevated podosternum,
this not produced into subcoxal spines or knobs,
but distinctly notched between the coxae on each
side and with the caudal side deeply concave
between the last legpair of each segment.
Legs long and slender, the joints virtually
glabrous except for a ventral macroseta on each
coxa and prefemur, and some microsetae on the
following three joints. Tarsus sparsely invested
with fine slender setae, these distinctly procum-
286 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, No. 8
PFP 2
PFP |
Fias. 1-9.—1, Antrogonodesmus curiosus, n. sp., mesial aspect of left gonopod of male holotype; 2,
lateral aspect of same; 3, telopodite of right gonopod seen from the coxal side; 4, telopodite of left
gonopod in ventral aspect; 5, Amphelictogon dolius Chamberlin, mesial aspect of left gonopod; 6, ventral
aspect of right gonopod; 7, lateral aspect of right gonopod; 8, ventral aspect of basal two joints of tenth
and eleventh leg pairs; 9, left paranotum of tenth segment. (Abbreviations: CX, coxa; CXP, coxal
process; F, femur; FP, femoral process; PF, prefemur; PFP, prefemoral process; SLM, solenomerite.)
AUGUST-SEPTEMBER 1959 HOFFMAN: A
bent. Pretarsus small, short, slightly curved. Leg
joints in decreasing order of length: 3-6-5-2-4-1.
Tibiae of legs 1-10 with extruded arthrodial
subtarsal pads, apparently a few others behind
the 10th can be extruded also. Seminal processes
of second coxae rudimentary, they open through
a low conical swelling of the coxae. Sterna of
anterior segments broad and without any trace
of subcoxal knobs or processes. Anterior pre-
tarsi also small and similar to the others.
Pleurae of segments 2-7 modified by a distinct
groove from the caudal margin of the segments,
curving cephaloventrad to form an arc just above
the coxae, thence fading out toward the inter-
zonal furrow. The low ridge formed by this
groove is entirely smooth.
Gonopod aperture quite small, broadly trans-
versely oval, about three times as wide as long,
its edges produced distally into a complete cir-
cumgonopodal rim of moderate height. Aperture
entirely confined to the metazonite of the seventh
segment, not infringing even onto the course of
the interzonal furrow.
Telopodites of gonopods, seen in situ, very
small, not extending beyond prozonite of seg-
ment although the coxae of normal size for
the bulk of the animal. Coxae attached by a
very small, elongate sternal remnant, and with
long slender apodemes, produced on the cephalic
surface into an elongate subconical coxal process
(CXP). Prefemora greatly enlarged especially
on the ventral surface, which is largely occupied
by a deep subcircular cavity, lined with long
setae (Figs. 2 and 3), unlike anything now
known in other chelodesmids. In mesial aspect,
prefemora are short and broad, with a straight
seminal groove proceeding distad to the base of
the solenomerite. A large prefemoral process
(PFP), distally expanded and divided into two
subequal laminate lobes, the outer of which is
terminally reflexed and curved to form a hood-
hke structure covering the solenomerite (PFP
2) as seen in ventral aspect, Fig. 3. Two other
gonopod processes, probably postfemoral in
structure, are the solenomerite (SLM), a simple,
shghtly curved, mostly concealed blade carrying
the seminal groove, and the femoral process
(FP), which originates near the base of the
solenomerite, and shields it on the ventral side.
Female paratype: similar to the male in most
structural details, but the body somewhat larger
with wider sterna and narrower paranota, and
with the interzonal furrow more deeply im-
pressed. The antennae are longer (5.8 mm), with
NEW CHELODESMOID GENUS 287
articles 2-6 almost identical in size and shape.
The color pattern is identical except that the
3rd segment lacks the median spot. The body
form is less attenuated caudally. Length, 35.0
mm, widths of selected segments:
2d 5.0mm
10th 4.9
16th 4.9
18th 3.8
Remarks :—Heretofore two chelodesmoid gen-
era have been known from Cuba: Amphelictogon
and Cubodesmus, both abundantly represented
by species from the eastern half of the island.
Antrogonodesmus is perhaps endemic to the
western part of the island, geographically vi-
cariating for the other two, but apparently not
closely related to either of them. There is, in
fact, no known genus with which it can be com-
pared. The large prefemoral cavity is unique,
and the relationship of the terminal processes
almost so.
As regards body forms and details, Antro-
gononodesmus seems to have no close ties with
Central American forms such as the dominant
chelodesmid genus Chondrodesmus. Tibial pads
on the male legs occur in numerous genera of
South America, but the systematic significance
of these structures has yet to be proven at least
as regards tracing affinities of genera so pro-
vided.
With most of the collecting which has been
done in Cuba restricted to the mountains of
Oriente, it would be premature to speculate on
the likelihood of a distinctive endemic fauna in
the hills of Pinar del Rio, yet such is suggested
by the discovery of an unusual chelodesmid.
Perhaps the intervening lowlands of Cuba have
been largely submerged through the Tertiary to
enhance the development of two distinct faunas.
Further exploration west of Havana is certainly
much to be desired.
Genus Amphelictogon Chamberlin
Amphelictogon Chamberlin, 1918, Bull. Mus. Comp.
Zool. 62: 224—Loomis, 1938, Bull. Mus. Comp.
Zool. 82: 460—Attems, 1938, Das Tierreich 68:
157; 1940, zbid. 70: 552—Loomis, 1941, Psyche
A8: 35.
Type species —Amphelictogon cubanus Cham-
berlin, by orthotypy.
Diagnosis—Amphelictogon is characterized
primarily by the structure of the gonopods,
which are rather small and project from a
strongly modified sternal aperture. The coxae
288
are connected by a small but distinct, attenuate
sternite, and are produced into a triangular pro-
jection partly concealing the lateral face of the
prefemur. The telopodite projects directly distad
from the prefemur as a rather straight stalk
which, however, is bent abruptly retroproximad,
strongly attenuated, and drawn out into a long
coiled flagellum. Prefemoral process set off by a
distinct articulation, extending distad as far as
the geniculum of the telopodite, where it nor-
mally curves proximad as a slender falcate
blade, occasionally with a terminal expansion or
a subterminal accessory process.
Body form slender, collum and second seg-
ment widest, segments posterior to 4th becoming
gradually narrower to end of body. Paranota
widely separated by the large exposed prozonites,
the two subsegments separated by a well defined
interzonal furrow. Prozonite of 7th segment of
males complete, not reduced in front of the
gonopod aperture. Legs long and slender, with-
out tibial pads, the pretarsi short and slender,
unmodified. Pore formula normal, peritremata
usually specialized and set off from margin of
paranota.
Coloration variable, the dorsum dark brown
with spots or bands or red, yellow, or white.
Species —22, most of them from Oriente Prov-
ince, Cuba, one from the Bahamas and one from
Isle of Pines.
Amphelictogon dolius Chamberlin
Figs. 5-9
Type specimens—Female holotype and para-
types, M. C. Z. nos. 5024-25, from Punta de
Judas, 40 miles east of Caibarién, Santa Clara
Province, Cuba, collected by Thomas Barbour
in 1917-18.
Diagnosis—The color pattern alone sets this
species off from the other known species of
Amphelictogon. On the basis of the gonopods,
dolius is allied to bidens Loomis and strwmosus
Loomis in having the prefemoral process distally
arcuate and slender and the telopodite femur
with two marginal teeth. It differs from both in
details of gonopod structure as well as color
pattern.
Description—Male: body elongate, slender,
widest across collum and attenuate caudally;
outline of body strongly moniliform, the prozo-
nites large and broadly separating the meta-
zonites. Paranota set high on sides and nearly
horizontal. Length of specimen approximately
30 mm., widths of selected segments as follows:
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 8
Collum 4.5mm
5th 4.2
10th 4.0
17th 3.5
Segments rich chestnut-brown, head and an-
tennae lighter brown; legs brownish pink, be-
coming reddish distally. Dorsum of paranota
and adjacent part of the metatergites as well
as tip of epiproct chalky white, each white spot
wider than the brown of the intervening mid-
dorsal area.
Head capsule normal in appearance, convex,
smooth; median groove of the vertex well de-
fined. Clypeal region set with numerous long fine
setae, the upper edge of the area limited by a
transverse row of larger setae, above which only
a few scattered setae occur on the lower frons.
A pair of subantennal setae, and two pairs on
the vertex is a transverse row, the setae of each
pair set close together. Labrum fringed with
about 40 long setae, intercalated with much
shorter ones. Genae rather flat, evenly convex.
Antennae long (5.8 mm) and unmodified, ar-
ticles 2-6 similar in size and shape, 1 very short,
7 subhemispherical, its distal edge turned in
mesially between each of the 4 sensory cones
and almost completely separating them; dorsal
(outer) side of article 7 with a small rounded
convex sensory area.
Collum broadly transverse, wider than head,
surface evenly arched and smooth. Anterior
margin evenly rounded through almost a half
circle, posterior margin strongly bisinuate, 1.e.,
with a median and two paramedian emargina-
tions, the latter emphasizing the lateral corners
of collum. Both edges set off by a submarginal
groove, deepest at the lateral ends and obsolete
across middorsum.
Second, third, and fourth tergites subsimilar
in appearance but narrowing in width, paranota
broadly transverse; anteriorly the margins are
evenly rounded and set off by a distinct ridge,
posteriorly the margins are bisinuate and set
off with a fine ridge; caudolateral corners dis-
tinctly produced. Surface of metatergites smooth
and polished, of prozonites finely shagreened, the
two subsegments separated by a deep sharply
defined interzonal furrow.
Segments 5 through 19 narrower than the
preceeding, the anterior paranotal corners in-
creasingly reduced along with width of the para-
nota, the prozonites proportionately more con-
spicuous along middle of body. Lateral margins
of segments 17-19 scarcely divergent from me-
dian body axis, paranotal angles directed caudad,
AUGUST-SEPTEMBER 1959 HOFFMAN: A
abruptly smaller on segment 19. Poriferous seg-
ments (5, 7, 9, 10, 12, 13, 16-19) simular to
others except for the strongly differentiated
peritremata, these elongate pyriform, the upper
surface flattened, pore directed dorsolaterad
(Fig. 9). Caudal edges of paranota margined,
but none produced into marginal dentations.
Epiproct subconical in dorsal aspect with a
small cylindric truncate apex beyond the ter-
minal whorl of macrosetae; lateral tubercules of
both whorls large and interrupting the curve of
the sides. Disc of anal valves convex, smooth,
surface of basal third of valves vertically striate,
mesal edges very strongly compressed, each valve
with an oblique secondary ridge projecting from
about the basal sixth and extending cephalo-
ventrad to near the lateral ends of the hypo-
proct. Latter about twice as wide as long, with
the ends acutely rounded and the distal edges
nearly straight, and with a large and distinct
median terminal lobe. Setiferous tubercules small
and removed from the edges.
Pleural and ventral surfaces smooth and
nearly glabrous, the former without pleural
carinae or other modifications. Interzonal furrow
continues well-defined around the segments in
a strong constriction between prozonites and
metazonites.
Legs inserted upon a distinctly elevated podo-
sternum, which is not produced into subcoxal
processes, and glabrous except for a row of 10-14
setae across the anterior surface above the inter-
zonal furrow and a few scattered setae in general
located near the coxal sockets. Legs long (up to
52 mm) and slender, the joints in decreasing
order of length: 3-6-5-4-2-1. Basal two joints
elabrous except for a few long ventral macro-
setae, distally the joints are increasingly setose.
Most legs are similar in proportion except the
9th and tenth pairs, the femora of which are
conspicuously enlarged with the ventral surface
flat or subconcave, ornamented with numerous
flat tubercules each of which bears a tiny curved
seta (Fig. 8).
Anterior legs smaller than the others but
similar in form, without tibial pads or other
modifications. Seminal ducts open flush with the
surface of the 2d coxae. Sterna between the
3d legs (4th segment) produced into two con-
tiguous elongate mounds; sterna between fourth
legs produced into 2 low subconical knobs; the
other sterna unmodified. Pretarsi short, slightly
curved, somewhat compressed.
Prozonite of seventh segment not infringed
NEW CHELODESMOID GENUS 289
upon by the small aperture of the gonopods and
generally similar to adjoining segments. The
aperture with the edges produced distad forming
a cireumgonopodal sheath, the rim of which is
flared and recurved toward the body. Gonopods
large, extending cephalad onto the 6th segment,
not in contact mesially or but slightly so; the
coxae joined by a small elongate sternal remnant,
without a coxal process, but extending some-
what behind the prefemora on the lateral side.
Prefemora rather small, densely setose. Pre-
femoral process elongate, as large as main part
of telopodite, terminating distally in a slender,
simple, attenuated curved process, the inner
edge of the process provided just beyond the
midlength with three rounded projecting lobes.
Femora short, flat, glabrous, separated from the
more distal part of the telopodite by a deep
(flexible?) groove or cingulum. Postfemur elon-
gate, slender, the basal half with two acute pro-
jections along the mesial edge; just beyond the
distalmost projection the telopodite is abruptly
reflexed proximad and drawn out into a long
coiled flagellum (Figs. 5-7).
Female: similar in structure to the male but
somewhat larger, the tergites wider (4.6 mm at
tenth segment, 5.0 mm at second). Color pattern
similar to that of male except that the collum
is completely ringed with white.
Remarks—This species has heretofore been
known only from the type locality. The material
described originated at the Cueva de Colon, in
Matanzas Province, Cuba, extending the known
range about 130 miles to the west.
Amphelictogon dolius appears to be remarka-
ble for the enlargement of the femora of legs 9
and 10. Whether such modification is unique in
this species or merely overlooked in others I
cannot guess. In the form of the gonopods dolius
is very much like Loomis’s species bidens and
strumosus, but differs so much in color pattern
from both that subspecifie status seems unlikely.
Probably actual comparison of specimens of the
three will provide various points of difference not
apparent from the published descriptions.
REFERENCES
CHAMBERLIN, R. V. The Chilopoda and Diplopoda
of the West Indies. Bull. Mus. Comp. Zool.
62(5): 149-262. 1918.
. Notes on West Indian Miullipeds. Proc.
U.S. Nat. Mus. 61(10): 1-19, pls. 1-6. 1922.
Loomis, H. F. New and noteworthy millipeds
from Cuba, collected by Dr. P. J. Darlington
in 1936. Bull. Mus. Comp. Zool. 82(6) : 427-480,
figs. 1-27. 19388.
290
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 8
ICHTHYOLOGY .—Bathypterois pectinatus, a new bathyal iniomous fish from the
eastern Pacific. GILES W. Map, United States Fish and Wildlife Service.!
(Received May 29, 1959)
The holotype of the distinctive species de-
scribed below has been available during my
review of the western Atlantic fishes of the
family Bathypteroidae. It was compared
with all known north Atlantic species
(Mead, 1959: 369); with the type or syn-
types of the Pacific Bathypterois ventralis
Garman, Bb. pectoralis Garman, and B.
antennatus Gilbert; with specimens repre-
senting B. longipes Ginther and several
variations of the cosmopolitan but poorly-
understood groups of species now known as
B. antennatus and B. atricolor. The study of
a second specimen, caught by the Vema, has
shown clearly that this form is not an ex-
tralimital subspecies or variant of the
Atlantic B. quadrifiis Giinther but a dis-
tinct although related species.
Bathypterois (Bathypterois) pectinatus, n. sp.
Fig. 1
Holotype —A specimen 142.1 mm in standard
length caught by the U. 8. Fish Commission
steamer Albatross at station D. 4654, 24 miles off
Aguja Point, Peru (lat. 05°46’ S., long. 81°32’
W.) on November 12, 1904, at a depth of 1,036
fathoms. U.S. National Museum no. 150029.
Paratype—A 123.0-mm specimen taken by
the R. V. Vema of the Lamont Geological Ob-
servatory from L.G.O. Biotrawl no. 122, Panama
Bay (lat. 07°25’ N., long. 79°23’ W.) on Novem-
ber 14, 1958, at a depth of 956 fathoms (cor-
rected). American Museum of Natural History
no. 20401.
Diagnosis —Posterior ventral procurrent cau-
dal ray modified into a hook or notch. Upper pro-
longed and stiffened pectoral rays fused basally
*One of the specimens on which this account
was based was caught by the 1958 eastern Pacific
cruise of the Vema, research vessel of the Lamont
Geological Observatory, Columbia University, and
was made available by Dr. Robert J. Menzies of
that laboratory through Dr. Vladimir Walters of
the American Museum of Natural History. Partial
support for this cruise of the Vema was obtained
from the U.S. Navy, Office of Naval Research, the
Bureau of Ships, and the National Science Founda-
tion. This paper constitutes contribution no. 363
of the Lamont Geological Observatory and no.
11 of the Biology Program.
but divided from one another at a point anterior
to the origin of the dorsal fin; these upper strong
rays followed by at most one rudimentary pec-
toral ray. Base of lowermost pectoral fin ray
about as thick as that of the adjacent ray. Scales
beneath proximal part of pectoral fin strongly
pectinate. Body black and without pattern; the
edges of the scale pockets white. Caudal fin
white; dorsal, anal, and ventral fins dusky.
Bathypterois pectinatus is closely related to
B. quadrifilis, a species known from the western
Atlantic (off Brazil, in the Gulf of Mexico and
the western Caribbean, and off Grenada and St.
Vincent in the British West Indies) at depths
from 470 to 655 fathoms. It differs from B. quad-
rifilis in the thickness of the lowermost pectoral
ray, by its colorless caudal fin and dusky dorsal
and anal fins (all are black in B. quadrifilis), by
its less-deep body, and in the extent of the scaly
covering over the proximal part of the caudal fin
(this covering extends out on to the caudal lobes
in B. quadrifilis but is restricted to the area over
the bases of the caudal rays in B. pectinatus).
Description—tThe following counts and meas-
urements (expressed in percent of standard
length) are those of the holotype (142.1 mm) fol-
lowed, in parentheses, by those of the paratype
CBO)
D—14 (14). A—9 (9). P. (upper part)—2,0/
2,1 (2,1/2,1). P. (lower part)—9/9 (9/9). V—
8/9 (9/9). C—I-16-II. Gill rakers (first arch)—
12+ 1+ 29 (12+ 1+ 30). Branchiostegal rays
—4+ 8 (5+ 8). Scales in lateral lime—about 62.
Vertebrae—d9.
Length of head 21.8 (21.3), of snout 7.1 (6.7),
of upper jaw 13.6 (13.3). Diameter of eye 2.0
(2.4); width of bony interorbital 7.9 (8.3).
Greatest depth of body 14.6 (14.4), depth at or-
igin of anal fin 10.6 (10.7), least depth of caudal
peduncle 7.1 (7.0). Greatest width of body 8.2
(8.1). Snout to origin of dorsal fin 40.1 (41.3), to
origin of anal fin 55.4 (55.7), to insertion of pec-
toral fin 18.3 (19.4), to msertion of ventral fin
35.5 (37.3). Base of last dorsal ray to insertion
of adipose fin 23.7 (22.6); insertion of adipose
fin to dorsal procurrent caudal ray 21.5 (22.2);
base of last anal ray to ventral procurrent caudal
AuGusT-SEPTEMBER 1959 MEAD: A NEW BATHYAL INIOMOUS FISH
ray 33.8 (32.6); insertion of ventral fin to anus
13.0 (11.8) ; anus to origin of anal fin 6.8 (7.6).
Length of base of dorsal fin 13.2 (13.7), of anal
fin 8.2 (8.1). Length of longest pectoral fin ray
89.6 (96.0), of longest ventral fin ray 32.2 (28.1).
Body compressed, snout depressed. Body deep-
est at origin of dorsal fin, this depth 1.5 in length
of head. Depth at origin of anal fin 2.0 in head;
least depth of caudal peduncle 3.0 in head. Great-
est width of body, anterior to dorsal fin, 1.8 in
greatest depth.
Cheeks, top of head posterior to eye, and body
covered with scales. Most body scales cycloid;
those beneath anterior end of lower part of pec-
toral fin strongly pectinate and more adherent
than most body scales. Body scales extend onto
caudal fin; all other fins scaleless. One or two
lateral line scales on caudal fin above the mid-
caudal ray.
Head 4.7 in standard length, depressed and
slightly convex above and before eye. Snout 3.0
to 3.2 in length of head. Sensory pores of head
well developed, 4 to 6 in the horizontal series be-
low the eye, about 8 along the lower outer surface
of the mandible, and about 4 in each longitudinal
series on top of head. Olfactory organ slightly
closer to eye than to tip of snout, the nostrils
separated by a thin membrane which bears a
short flap.
Eye minute but larger than that of several
other bathypteroid species, its greatest diameter
equal to or greater than the combined width of
the upper jaw bones (maxillary and supramaxil-
lary) at their widest point. Pupil elliptical, but
SEANAD
COLKIOR SON
EXE SOK EAE HEN
se sapenas:
A
291
not keyhole-shaped. Interorbital broad and con-
vex, 2.5 to 2.7 in length of head.
Branchiostegal membrane extending posteri-
orly beyond operculars, supported by 12 or 13
branchiostegal rays of which four or five originate
on the epihval. The membranes overlap ante-
riorly and are covered by a thick transverse gular
fold. Gill rakers on all four arches, of the usual
lathlike shape, spiny, and moderately long. Those
near the angle of the first arch are about twice as
long as the opposite gill filaments. No pseudo-
branchiae.
Maxillary broad and flat posteriorly, extending
beyond posterior end of the premaxillary and
surmounted by a slender supramaxillary which
extends forward nearly or quite to beneath the
posterior edge of the eye. Teeth on premaxillary
minute, mostly depressible, and in a single band
which is broader anteriorly than posteriorly.
Symphysis of upper jaw without teeth. A patch
of minute teeth on each side of the vomer, and a
row of smaller teeth on each palatine. Mandible
broad and heavy, with a bony toothless boss at
the symphysis, the anterior half not included
within or opposed to the upper jaw when the
mouth is closed. Teeth in mandible small but
larger than those in upper jaw, depressible and
forming a band which is broader anteriorly than
posteriorly. No teeth on the small tongue.
Dorsal fin inserted well behind axil of ven-
tral fin, the length of its base 1.6 in length of head.
Predorsal distance 2.4 or 2.5 in standard length.
First two dorsal rays unbranched, the rest
branched, the last divided to its base. Adipose
IEEE NOIOSORER KOK KOIDE
* 7a 8
VAT ATS TAS ASAD So
ee
Fig. 1.—Bathypterois (Bathypterois) pectinatus, holotype, U.S.N.M. no. 150029. The figured scale was
taken from beneath the anterior third of the lower part of the pectoral fin. (Drawn by Mildred H. Car-
rington.)
292
dorsal fin located about midway between poste-
rior end of base of dorsal fin and first dorsal pro-
current caudal fin ray, or slightly closer to end
of base of dorsal fin. (The position of the adipose
fin is variable in several bathypteroid species.)
Preventral distance 2.7 or 2.8 in standard length,
the length of the fin 3.1 to 3.6 in length of fish.
Ventral fin normally with nine rays, but one side
of the type has but eight. (The number of ventral
rays 1s constant in the western Atlantic species.)
The outer two ventral rays are simple, the rest
branched. Base of second ventral ray about the
same thickness as that of the third. Origin of
anal fin behind a vertical from end of base of dor-
sal fin, the preanal distance 1.8 in standard length.
First anal ray unbranched, the rest branched,
the last divided to its base. (All fins except the
ventrals and the adipose are broken in both speci-
mens.) Upper two pectoral fin rays stiffened and
elongate and fused basally, separating from one
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 8
another anterior to the origin of the dorsal fin and
extending beyond end of base of dorsal fin nearly
to base of caudal. One or no rudimentary rays
below these two fused and prolonged upper pec-
toral rays. All rays in lower part of pectoral fin
broken.
Anus located about midway between insertion
of base of inner ventral ray and origin of anal
fin. A small urogenital papilla present, preceded
by the ovopore.
Body black and without pattern. Edges of
scale pockets white. Caudal and adipose fins
white. All other fins, snout and under surface of
lower jaw dusky.
LITERATURE CITED
Meap, Gites W. Three new species of archibenthic
momous fishes from the western North At-
lantic. Journ. Washington Acad. Sci. 48: 362-
372. 1959.
Happy is he who has knowledge
That comes from inquiry. No evil he stirs
For his townsmen, nor gives himself
To unjust doings,
But surveys the unaging order
Of deathless nature, of what it is made,
And whence, and how. tear
In men of this kind the study
Of base acts never finds a home.
— EURIPIDES.
Eprror’s Note.—The August and September numbers of the Journal are combined in
one issue, as will also be the October and November numbers. Only 10 issues will be pub-
lished in Volume 49.
Officers of the Washington Academy of Sciences
SO ob eae 2 eee FranK L. CaMpBELL, National Research Council
Presaent-elect...............: LAWRENCE A. Woop, National Bureau of Standards
Daly IVY bo yee ee Heinz Sprecut, National Institutes of Health
LOAD UG) Soe W. G. BrompBacHer, National Bureau of Standards
LO) Morris C. Leixinp, Armed Forces Institute of Pathology
Custodian of Publications............... Harartp A. Resper, U.S. National Museum
LUE. oe Soe CHESTER H. Pace, National Bureau of Standards
2G OS Pa AOL a H. A. Bortruwickx, T. D. Stewart
WITEGETS AO 1961... 26... ce nee Bourpon F. Scrisner, Keita C. JOHNSON
MUO Ue Puitip H. Assuson, Howarp S. RappLErE
Board of Managers....All the above officers plus the vice-presidents representing the
affiliated societies
CHAIRMEN OF COMMITTEES
Standing Committees
UME GS SE FrankK L, CamMpBELL, National Research Council
1 SECT oS 6 Oo RatpH B. KENNARD, American University
Membership............ LawrENcE M. KusHner, National Bureau of Standards
Miemogranhs.................. Dean B. Cowiz, Carnegie Institution of Washington
_ Awards for Scientific Achievement....... FraNK A. BIBERSTEIN, Catholic University
Grants-in-aid for Research...... B. D. Van Evera, George Washington University
Policy and Planning.............. MarGaRET Pitrman, National Institutes of Health
Encouragement of Science Talent.............. Leo Scuusert, American University
Science Education............ RayMonD J. SEEGER, National Science Foundation
Ways and Means.............. RussELL B. Stevens, George Washington University
bite Helations................00000- Joun K. Taytor, National Bureau of Standards
Special Committees
OTD 5 Harotp H. SHeparp, U. S. Department of Agriculture
MOOGGLOTY.)..2.-......... James I. Hamsieton, U.S. Department of Agriculture (Ret.)
EiGrary o: Coneress.................... Joun A. O’Keere, National Aeronautics and
Space Administration
CONTENTS
Page
Botany.—Adventitious bud and stem relationship in apple. Hate
DERMEN «2.05 Psi. Re cent a. oS eee oe 261
Botany.—New chiropterophilous Solanaceae from Colombia. Jos#
CUATRECASAS. 2.602. c cc: 06 aise ae eile ie Pee oie, ee
ZooLocy.—Three new cave amphipods from the West Indies. CLAR-
ENCE’ R. SHOBPMAKER. .. 00.5 0% o2 0 0c oe oon eee 1s 2) er 273
ZooLocy.—Antrogonodesmus, a new chelodesmoid genus from Cuba,
and a redescription of Amphelictogon dolius Chamberlin (Poly-
desmida, Chelodesmidae). RicHarp L. HOFFMAN................ 284
IcutHyoLocy.—Bathypterois pectinatus, a new bathyal iniomous fish
from the eastern Pacific. Gites W. MEAD.......-.) eee 290
Notes aND News... 32.020) BR eee ee 272, 292
VOLUME 49 October—November 1959 NUMBER 9
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WASHINGTON ACADEMY
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DEC 9 59
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JOURNAL
OF THE
WASHINGTON ACADEMY OF SCIENCES
Vou. 49
OcTOBER-NOVEMBER 1959
No. 9
EDUCATION —Education for the Age of Technology 8S. B. INcram2 (Commu-
nicated by F. L. Campbell.)
I have chosen for a title around which to
organize the thoughts I wish to put before
you today Education for the Age of Tech-
nology. I should like first to talk about our
technical manpower needs and then go on to
some implications that these have for our
American educational system.
THE AGE OF TECHNOLOGY
The first point I wish to make is that to-
day is indeed the Age of Technology in
which educated, technically trained people
are at a premium as never before. The im-
pact of science upon our civilization has
been so great that it is the controlling fac-
tor, whether we like it or not, in our culture.
The technological character of our civiliza-
tion has the profoundest effect on our poli-
tics, on our international relations, on our
economic institutions, on our daily lives
and finally, our particular interest here to-
day, on our educational system.
The rate of social progress is paced by
the rate of technological progress. Within
our own country we experience the stresses
and strains of trying to adjust our social
structure to the rapid changes which have
occurred in our material way of life. Exter-
nally, we find ourselves caught up in a con-
test between two competing ideologies. We
know that the laurels will ultimately go to
the side that can establish and maintain
the greatest rate of technological advance,
* Presented at a meeting sponsored by the D.C.
Council of Engineering and Architectural Socie-
ties and the Washington Academy of Sciences on
Engineers, Scientists, and Architects Day at Wash-
mgton, D. C., on February 25, 1959. Published
jointly with the Journal of Engineering Education.
* Director of education and training, Bell Tele-
phone Laboratories, Inc., Murray Hill, N. J., and
vice-chairman, Engineering Manpower Commis-
sion of Engineers Joint Council.
293
and we know that this is true whether the
goal of the contest is the peaceful one of
providing the highest standard of living for
all the people of a nation or the grim one of
military victory in the ultimate struggle of
modern nuclear and electronic war.
Education plays a key role in determining
the rate of technological advance because it
is through our educational system that we
develop the abilities of those members of
society whose numbers and quality are crit-
ical in this determination, our scientists and
engineers. Less and less is the work of the
world done by unskilled and semiskilled
labor. More and more are highly skilled and
highly trained people needed by our society.
Our greatest need has shifted from man-
power to brainpower, and since we are
concerned with the rate of technological
progress our need is more and more for tech-
nological brainpower.
POTENTIAL OF TECHNOLOGICAL MANPOWER
The second point I wish to make is that
our potential of technological manpower has
a very definite limit, and we are not far
from reaching this limit at the present time.
I shall illustrate the point specifically by
some figures with respect to our capacity
to produce people trained in engineering,
since the same line of reasoning can be ap-
phed with equal force to those trained in
other technological fields like science and
architecture.
At the present time only about 9 percent
of our college entrants or 15 percent of our
male college entrants have the interest, the
aptitude, and the necessary preparation to
embark on engineering courses and only
about half of these graduate. Engineering
educators estimate that only those young
SMITHSONIAN
INSTITUTION
NOV 2 0 1959
294 JOURNAL OF THE
people scoring above 120 on the Army Gen-
eral Classification Test are capable of suc-
cessfully completing engineering training.
This is about 17 percent of the age group.
Now this does not mean, by any stretch of
the imagination, that all these 17 percent
may be regarded as potential engineers. Far
from it. In the first place, half of these are
women, and while experience has shown
that we can get a small number of scientists
and a smaller number of engineers from this
eroup, barring a social revolution, we can
not count on them to contribute in substan-
tial numbers to our reservoir of potential
engineers. This brings us from 17 percent
down to 82 percent. Now we have to con-
sider that this remainder has to supply not
only the engineers we have in our society
but also members of the other professions
and occupations which make the same high
demands on intellectual capacity that engi-
neering does. In the past, engineering has
succeeded in getting about one-fourth of
these. It is a question of how much higher
this figure can go. We certainly can not put
all our highly intelligent people in engineer-
ing, and very many of them would not be
successful at it even if they tried. It takes
a lot of other things besides intelligence to
be an engineer. It takes a mathematical
mind. It takes an interest in physical things
and physical phenomena. Engineering does
not give an adequate outlet for some of the
other basic aptitudes and interests which
intelligent people have. Many a successful
lawyer, journalist, or social scientist would
be wasted as an engineer, and besides our
society needs these people in those fields
into which their aptitudes and interests
properly channel them. So if we assume that
we will not be able to increase this fraction
of one-fourth substantially, we conclude
that about one-fourth of the 8% percent or
about 2 percent of the 2,200,000 young peo-
ple coming of college age each year is our
potential capacity for the production of en-
gineering graduates. This number is 44,000.
It is not far above the 35,000 engineers we
oraduated last year. Even this 2 percent
figure does not represent ultimate additions
to our national engineering foree because it
takes no account of losses of trained engi-
neers to other occupations. Dael Wolfle (1)
WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 9
reports a study made in 1953 on a large
sample of college graduates of the classes of
1930, 1940, and 1951. Of this group of engi-
neering graduates, only 64 percent were do-
ing professional engineering work as of
1953. We thus lose about one-third of those
we graduate as engineers from our engineer-
ing schools and in return we gain compara-
tively few to the profession from other
sources. A more realistic figure then for our
capacity to add to the engineering segment
of our labor force is 143 percent, and this,
I believe, is one we can hope to exceed only
with considerable difficulty.
NEED FOR TECHNOLOGICAL MANPOWER
My third point is that our need for tech-
nically trained people has increased con-
tinuously in the past and may be expected
to do so in the foreseeable future. A National
Science Foundation study on our scientific
personnel resources (2) traces the growth in
the percentage of our population engaged in
professional work in science and technology
over an 80-year period from 1870 to 1950.
This percentage was, in 1870, 1910, and
1950, 0.08, 0.2, and 0.7, respectively. The
basis for this steady increase, of course, has
been the continuous growth in the complex
technological nature of our civilization over
this 80-year period. Certainly, we can say
that this growth has continued over the dec-
ade since 1950. I know of nobody, certainly
no responsible spokesman for science, who
is willing to predict any cessation in this
trend. It, therefore, seems a valid procedure
to extrapolate this curve upward.
PERMANENT SHORTAGE OF TECHNOLOGICAL
MANPOWER
My fourth point, which is a corollary of
my points 2 and 3, is that our needs for
technically trained people, which we have
always been able to satisfy in the past, may
shortly be expected to outrun permanently
our ability to satisfy them. This means that
our shortage of scientists and engineers has
become chronic.
It is interesting to compare the 0.7 per-
cent figure, which I just quoted, and which
since 1950 may well have increased to
nearly 1 percent with the 1/3 percent fig-
ure for our capacity to produce engineers,
Ocr.—Nov. 1959
which I cited previously. The figures are not
directly comparable since the first one in-
cludes not only engineers but also all pro-
fessional technical people, and the second
one is our rate of production of engineers
and not their total number. Nevertheless,
I believe, that with a more careful analysis
of these figures than I am prepared to make
here, one can satisfy himself that we will
very shortly reach the point where we will
always need more scientists and engineers
than we are able to produce. This does not
say that in times of business recessions, like
last year, there may not appear to be tem-
porary easing of the shortage, but this is a
transient market condition associated with
the business cycle and we should not be mis-
led by it. When business turns upward
again, the engineer and scientist shortage
will be back with us once more and in a
more acute form than ever.
IMPLICATION FOR EDUCATIONAL SYSTEM
So much for our needs for technically
trained people in the Age of Technology.
What are the implications of the Age of
Technology for education? Actually, it has
implications for every phase and at every
level of our educational system.
To begin with, in assessing our educa-
tional system, it is important to do so with
respect not to the world of today but to that
of tomorrow. For it is in tomorrow’s world
that the school children and the college stu-
dents of today will take their places as con-
tributors to our society. Education must,
therefore, take a long range point of view.
Specifically, what can we do to educate ade-
quate numbers of scientists and engineers
to fill the needs which, I hope I have con-
vinced you, exist today and are going to
erow more acute as time goes on? How long
it takes to observe any noticeable change in
our output of engineers, after we take spe-
cific action to increase it is illustrated by
an experience only too fresh in the minds
of many of us. Between World War II and
the Korean War we misjudged our techno-
logical manpower needs. Official govern-
ment sources, as well as general public opin-
ion, supported the view that our needs for
engineers were amply provided for and that
opportunities in the engineering profession
INGRAM: EDUCATION FOR THE AGE OF TECHNOLOGY
295
were limited. It was not until after the out-
break of hostilities in Korea in 1950 that
we awoke to the fact that we were facing an
engineer shortage instead of an engineer
surplus. Although the nature of the shortage
immediately became obvious to employers
of engineers, to placement officers of engi-
neering colleges and to those in Govern-
ment concerned with manpower problems,
it was not until six years later, in 1956, that
the curve of engineering graduates turned
upward. It took two years of market stimu-
lation, government-backed publicity, and
strong public leadership to overcome the in-
ertia of the public attitude toward the pro-
fession and its opportunities, plus four more
years, the length of an undergraduate col-
lege course, before any effective increase in
the rate of production of engineers could be
observed. In other words, the lead time for
the production of engineers is at least six
years.
Since we must be looking at least 6 years
ahead it is obvious that we should not allow
ourselves to fall into the trap of responding
to the short-term fluctuations of the busi-
ness cycle. As far as national policy is con-
cerned, we can hope for a basic enough un-
derstanding of the problem on the part of
those who determine it to prevent this, but
unfortunately, we do not determine as a
matter of national policy, as for example
they do in Soviet Russia, how many high-
school graduates enter engineering school
in a given year. This is done by the high-
school graduates themselves. There is some
recent disturbing evidence that they may
be very sensitive to the immediate state of
the market. The first Russian sputnik went
up in October 1957. Something like a near
panic gripped the nation. Science and engi-
neering and their national importance were
brought into the focus of public attention
as never before. General expectation was
that engineering freshman _ enrollments
which had been slowly and steadily increas-
ing in recent years would take a sudden
spurt upwards in the fall of 1958. What
happened? They actually turned downward.
The United States Office of Education tells
us (3) that freshman engineering enroll-
ment decreased 11.1 percent below that of
1957, whereas total college first-time en-
296
rollments inereased 7.0 percent. What
turned the graduates away from engineer-
ing? Nobody has the answer for sure, but
among the various possible answers the
most likely one seems to be that it was the
result of the recession of 1957-58 and the
wide publicity that attended the slight eas-
ing of the tight market for engineering tal-
ent that had prevailed continuously since
1950.
In the guidance of these young students,
the high-school teachers of science and the
high-school guidance counsellors play a vi-
tal role. The teachers can stimulate the in-
terest of the promising students in scientific
careers and direct them into the right
courses to prepare them adequately for col-
lege entrance in engineering or science. The
counsellor can make the students aware of
the opportunities in these fields. The actual
beginning of a career in science is in the
early years of high school. A mathematics
or science course, not taken then, may bar
the student from the college science course
he may wish to elect later. There is a trend
in the engineering colleges toward raising
admission standards. Too often in the past,
the colleges have had to make up deficien-
cies left by inadequate high school prepara-
tion. The pressures on the modern engineer-
ing curriculum are great and there is no
room in the college curriculum for high
school mathematics. This puts the responsi-
bility squarely where it belongs—on the
high school.
ELEMENTARY AND HIGH SCHOOL
Actually the conditions of the Age of
Technology will require, I believe, in the
long run, a reorientation of the objectives
of our system of free public education. For
many years, the emphasis has been on per-
sonality development and social adjustment
of the school child. Little has been done to
stimulate, intellectually challenge and de-
velop the gifted child. We will not much
longer be able to tolerate the waste involved
in moving all of our students through the
same curriculum at the same pace, the
gifted along with the dull.
Particularly is this true at the high-school
level. Personality development and social
adjustment may well be the most important
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 9
considerations in the early grades of ele-
mentary school, but when we come to the
high-school level, in my opinion, the pri-
mary function of the school should be to
teach subject matter, and we should make
much greater demands on the scholarship of
the students than we do today. Academic
standards should be strictly maintained and
there should be greatly increased emphasis
on mathematics and science. Opportunities
should be provided for the better students
to progress at a more rapid rate in separate
classes and their subject matter should be
greatly extended. We simply cannot afford
to spend four years of the precious time of
those members of society who form our
most critical national resource coasting
along in academic low gear as we do now.
HIGHER EDUCATION
Turning now to higher education in sci-
ence and engineering, we find that the engi-
neering schools, being very close to the tech-
nological developments of recent years and
in many cases playing an important role in
them, as partners with government and in-
dustry, have responded much more quickly
to changing educational needs than have
the high schools. The result 1s that in the
case of undergraduate engineering educa-
tion the reorientation toward new objectives
is already far along. Our American engi-
neering education has traditionally been
one of schooling the young engineer heavily
in engineering practice. The new trend is to
give him a good solid foundation of mathe-
matics and pure and engineering sciences
as a base for his later work in engineering
practice. Engineering practice changes rap-
idly and soon becomes obsolete in the com-
plex and rapidly developing technology of
today. Furthermore, the multiplicity of the
specific fields of engineering practice is
ereat. The young engineer cannot be trained
in all of them while he is in college, and if
he is trained in one he quite probably will
end up working in another. Finally the en-
gineering colleges are not in a good position
to train In engineering practice, because the
seat of knowledge of engineering practice is
in industry and not in the colleges. It is
more important for the engineering student
to gain a comprehensive understanding of
Oct.-Nov. 1959
the laws of nature and a facility in the use
of the mathematical and scientific tools by
which engineering problems are attacked
than to master their detailed application in
a specific field. Experience shows that it is
not possible for him to do both in the short
span of a four-year undergraduate course.
Along with the changes occurring in un-
dergraduate engineering education has come
a greatly increased emphasis on graduate
work. A 4-year college training is inade-
quate in depth to equip an engineer to un-
dertake successfully much of the work he
is called upon to perform in the Age of
Technology. This is particularly true in the
creative work of research and development,
which now absorbs the efforts of over 30
percent of our total professional technologi-
eal force. The shortage of engineers is acute,
but that for engineers trained to the gradu-
ate level is doubly so. In this area the pure
sciences are far ahead of engineering, the
number of doctorates granted annually in
physics alone approximately equalling those
granted in all fields of engineering. Much is
being done by the fellowship and loan pro-
grams of the Federal Government and oth-
ers as well as by the provision of opportu-
nities for part-time employment during
graduate study to enable qualified engi-
neering students to continue for graduate
work. The kernel of the problem here is to
support our institutions of higher educa-
tion so that they may attract adequate
numbers of highly qualified faculty mem-
bers in competition with private industry.
EDUCATION IN INDUSTRY
The final segment of the educational sys-
tem is the newest part of our formal educa-
tional structure, education in industry. It
is a segment which might have been ignored
as recently as a few decades ago, but which
certainly cannot be ignored today. It is one
which may be expected to expand rapidly
in the future. It is a phenomenon of the Age
of Technology.
Formal technical educational programs
in industry have grown up in response to
two needs. The first is that of industry to
train its own employees in its own technol-
ogy. I have already noted that the engineer-
ing schools are now emphasizing fundamen-
INGRAM: EDUCATION FOR THE AGE OF TECHNOLOGY
297
tal science at the expense of engineering
practice. Where then does the young engi-
neer learn his engineering practice? The
answer 1s in industry. Employers today ac-
cept the need for training their new engi-
neering employees as a necessary step in the
development of their engineering staffs.
There is no clamor that I can detect to per-
suade the colleges to relieve them of this
burden. The reason is that they prefer to
give their own employees their own kind of
training in their own field.
The second need which brings educational
programs into being in industry is the need
to keep engineering staffs up to date. In
today’s rapidly developing technology, we
know that our physical equipment will be-
come obsolete soon enough. What we should
be concerned about is the obsolescence of
our engineers and scientists. Obsolescence
is the fate of any engineer or scientist who
allows his own field of technology to pass
him by or who allows himself to be out-
flanked by a competing technology. The
preventive is continuing education. No en-
gineer can afford to neglect his continuing
education. Industry and the nation faced in
the future, as I hope I have convinced you,
with a chronic shortage of engineers and
scientists cannot afford to neglect it either.
An engineer kept in technological mid-
stream by continuing education rather than
being swept into the eddy of obsolescence
may not increase our technological nose-
count, but he certainly does increase our
technological potential. Quality counts as
well as quantity.
By no means all this industrial educa-
tional effort 1s vocational in nature or is
specific training in engineering practice.
Particularly in the second area, that of con-
tinuing education, the great need is for the
upgrading of long service technical person-
nel in the fundamentals which have come
into the engineering curriculum since they
went to school. Here the universities can be
of great service and here too a reorientation
of our thinking in higher education is called
for. Our present higher educational system
is largely built on the assumption that once
a student is educated to a certain level and
has received certification for this in the
form of a degree, that he is equipped for life
298
with a level of technical competence cor-
responding to the degree. Nothing could be
further from the truth. A master’s degree of
1940 is not the equivalent of a master’s de-
eree of 1960, unless a lot has gone on in be-
tween in the form of continuing education.
Whole new fields of knowledge and whole
new technologies have grown up. The typi-
cal engineer or scientist has specialized and
kept up through his own efforts with the
new developments in his own specialty. But
increasingly, he finds himself less and less
able to understand what goes on about him
outside of that specialty. When called upon
to change his field, as he sooner or later
probably will be, he finds himself in a poor
competitive position with respect to the
younger men with more modern educations.
This is a problem in which we have only
begun to scratch the surface. I predict that
as our present technological labor force
whose age distribution is now so heavily
peaked at the younger years, ages and as
the shortage of technical manpower be-
comes more acute, we are going to have to
do much more about it than we do now.
Training programs in industry, not for new
employees, but for longer service ones, co-
operative programs with universities for
older technical employees, I feel sure will
see a great growth in future years. These
will often be nondegree programs, and when
done by universities industry will be pre-
pared to foot the bill. I can cite you several
examples of such programs taken from our
own company which are in existence at the
present time. In Bell Telephone Labora-
tories we have an extensive program of out-
of-hours courses taught by the members of
our own technical staff, as well as tuition
refund plans to encourage and facilitate
the continuing education of our employees
at universities. Each year the operating
telephone companies of the Bell System
send to us about 50 young engineers to learn
the latest developments of the communica-
tions art. The New York Telephone Co. and
the Southern Bell Telephone & Telegraph
Co. have joint programs with Cornell Uni-
versity and Clemson College to which their
engineers are sent to be brought up to date in
the fundamentals underlying the technology
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. 9
of telephone transmission. The Bell Tele-
phone Co. of Pennsylvania has a program
with similar objectives, but does it for itself.
The Western Electrie Co., the manufactur-
ing arm of the Bell System, sends its ex-
perienced engineers at intervals, to training
centers, where with the help of universities,
it offers them courses in the fundamentals
underlying important new areas of tech-
nology. Other Bell System companies and
other companies outside the Bell System are
also active in this field. Industry will move
to solve its own problems as they become
acute, but I think there is little apprecia-
tion in university circles of the magnitude of
this field of education and the part that
they are going to be called upon to play
in it. Coming on top of the foreseeable de-
mands on them for supplying undergraduate
education, resulting from the population
bulge following World War II and the need
for great expansion in graduate engineering
education, this educational responsibility
will not be easy to discharge and yet, I
believe, is one which it is proper for our
system of higher technical education to as-
sume.
CONCLUSION
These are exciting times in which we live.
Perforce we are all gamblers because the
one thing we can be sure of in the Age of
Technology is change—rapid change.
Statesmanship, business management, edu-
cational administration, have become
largely a matter of trying to anticipate the
direction and rate of this change. I have
made bold to try to look into the future in
several directions which seem to me to be of
importance to some who may be in this
audience. If I am right, I hope that what I
have said may be useful. If I am-wrong, I
hope that at least it has not been dull.
REFERENCES
(1) Wotrie, DaEL. America’s resources of special-
ized talent: 332 pp. Harpers, 1954.
(2) NationaL Science FounpaTion. Scientific per-
sonnel resources: 86 pp. Washington, 1955.
(3) U.S. DeparRTMENT oF HEALTH, EDUCATION, AND
WELFARE, Office of Education, Circular 554.
December 1958.
Oct—Nov. 1959
ROSS: NEW SPECIES OF FUSULINIDS
299
GEOLOGY .—The Wolfcamp Series (Permian) and new species of fusulinids, Glass
Mountains, Texas.1 CHARLES A. Ross, Peabody Museum, Yale University.
(Communicated by Herbert H. Ross.)
(Received May 29, 1959)
INTRODUCTION
The Wolfcamp Series in the Glass Moun-
tains, Tex., is represented by a sequence of
diverse lithologies and includes a regional
unconformity. A detailed study of these
strata reveals that two formations can be
recognized in the field and that both units
are within the “Zone of Pseudoschwagerina”
(Fig. 1). Each formation has a distinct
and characteristic fusulinid fauna. The
Nealranch formation embraces the upper
part of beds originally called Wolfcamp by
Udden (1917) in the Wolf Camp Hills and
is renamed to retain this widely used name
for the time-stratigraphic unit, the Wolf-
camp Series. The Lenoxhills formation un-
conformably overlies the Nealranch forma-
tion and is the upper formation of the
Wolfcamp Series in the Glass Mountains. It
was In part included in the Wolfcamp forma-
tion of King (1931), where it crops out in the
western Glass Mountains and is now known
to be present across the southern escarp-
ment of the eastern Glass Mountains, and
is the lower 200 to 300 feet of the Hess for-
mation of Udden (1917). The correlation of
these stratigraphic units with strata in other
regions is determined on the basis of their
fusulinid faunas.
The exact placement of the top of the
Pennsylvanian system in the Glass Moun-
tains has long been a major controversy.
Fusulinid faunas of Cisco (Virgil) age are
known from strata as high as the “grey
limestone” of King (1931 and 1937). In the
Wolf Camp Hills the Nealranch formation
(300 to 470 feet thick) unconformably over-
lies the “grey limestone” and contains the
oldest Schwagerina and Pseudoschwagerina
faunas thus far discovered in the Glass
Mountains. The boundary between the Per-
mian and Pennsylvanian systems is taken
at this unconformity. The Nealranch forma-
“From a dissertation submitted to the Depart-
ment of Geology, Yale University, in partial ful-
filment of requirements for Ph.D.
tion is truncated and has been removed for
some distance east of the Wolf Camp Hills
by pre-Lenoxhills erosion. At Gap Tank,
about 10 miles east of the Wolf Camp Hills,
90 feet of Nealranch strata have been
preserved from pre-Lenoxhills erosion in
a faulted syncline which formed before
Lenoxhills deposition.
In the western part of the Marathon
Basin at the foot of the Lenox Hills, 6 miles
west of Marathon, faulted and folded strata
locally contain Pseudoschwagerina uddeni
(Beede and Kniker), Schwagerina puguncu-
lus,n. sp., and Triticites uddent Dunbar and
Skinner. Thus the Nealranch formation was
deposited in the western part of this area
prior to the last major tectonic pulse of the
Marathon orogenic belt.
The Wolf Camp Hills, Gap Tank, the foot
of the Lenox Hills, and probably the base of
the Hess ranch horst have the only known
outcrops of the Nealranch formation in the
Glass Mountains.
The Lenoxhills formation unconformably
overlies the Nealranch, Gaptank, and older
strata of the Marathon orogenic belt. The
type section of the Lenoxhills formation is
in the Lenox Hills west of Marathon, where
it is composed of 130 feet of conglomerate at
its base succeeded by 160 feet of sandstone,
clastic limestone, and shale. To the south-
west in the Lenox Hills the entire formation
changes facies into conglomerate. Further to
the southwest at Dugout Mountain, the
conglomerate changes facies into sandstone
and shale (150 feet thick) and finally into
limestone and shale. Throughout the Glass
Mountains the Lenoxhills formation is
marked by a persistent basal conglomerate,
but the strata above change facies within
short distances.
Northeast of the Lenox Hills, the forma-
tion changes into a shale facies and is thin
(120 feet) just west of Iron Mountain. At
Leonard Mountain the Lenoxhills formation
forms the southern and eastern facies. Here
the shale units intertongue eastward into
JOURNAL OF THE
eries
Period
THIS wale
PAPER &
W E
LEONARD FM.
d
Leonar
LENOXHILLS FM.
PERMIAN
NEALRANCH FM.
Wolfcamp
WOLFCAMP_ FM.
| grey paney ys
x llimestone limestone z
=) | f o|¢
t | Uddenites . Uddenites o| 2
= : zone iz shales" D
© = 2
| < x
a
<
oO
Fic. 1—Stratigraphic terminology as used by
King (1937) and in this paper. In the table W rep-
resents the western Glass Mountains and E the
eastern Glass Mountains.
biohermal limestones which form the east-
ern face. Farther to the east from the Hess
ranch house to the vicinity of the Wolf
Camp Hills these biohermal strata inter-
tongue into silty thin-bedded limestones,
200 to 300 feet thick. Eastward from the
Wolf Camp Hills, the thin-bedded lime-
stones of the Lenoxhills formation inter-
tongue with red and varicolored shales, and
green cross-bedded sandstones of the mar-
ginal marine facies. Throughout much of
this eastern area the basal conglomerate of
the Lenoxhills formation fills valleys cut
into the limestone beds of the Gaptank for-
mation.
The Leonard formation unconformably
overlies the Lenoxhills formation in the
western Glass Mountains. Locally pre-
Leonard erosion has removed most of the
Lenoxhills formation and as at the south-
west end of Dugout Mountain and in the
northern part of the Lenox Hills the base of
the Leonard formation rests on the trun-
cated edges of the folded and faulted beds
of the Marathon orogenic belt. In the east-
ern part of the Glass Mountains the Leon-
ard formation overlies the limestone and
WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. 9
shale of the Lenoxhills formation with no
apparent unconformity, being rather a
sharp change in facies into thick units of
thin bedded limestone.
The “grey limestone” of King (1931) con-
tains the youngest Pennsylvanian fauna in
the Wolf Camp Hills and includes T'riticites
comptus n. sp., T. ventricosus (Moller), T.
pingus Dunbar and Skinner, and 7. kosch-
manni Skinner (Fig. 2).
The fusulinids which characterize and are
restricted to the Nealranch formation in the
Wolf Camp Hills include: Triticites uddeni
Dunbar and Skinner, Schwagerina emaciata
(Beede), S. pugunculus, n. sp., Pseudo-
schwagerina udden: (Beede and Kniker),
Paraschwagerina acuminata Dunbar and
Skinner, and P. gigantea (White). In ad-
dition the following species range into the
Nealranch formation: Triticites ventricosus
(Moller), 7. pinguis Dunbar and Skinner
T. koschmanni Skinner, Pseudoschwagerina
beeder Dunbar and Skinner, and P. texana
Dunbar and Skinner.
Fusulinids which characterize and are re-
stricted to the Lenoxhills formation in the
western Glass Mountains are: Schwagerina
extumida, n. sp., S. lineanoda, n. sp., S.
dispansa, n. sp., S. laxissima Dunbar and
Skinner, S. bellula Dunbar and Skinner,
Pseudoschwagerina tumidosus, n. sp., and
P. robusta (Meek). In addition the follow-
Ing species range into the Lenoxhills forma-
tion: Schwagerina compacta (White), S.
tersa, n. sp., S. crebrisepta, n. sp., S. nelsoni
Dunbar and Skinner, S. knight: Dunbar and
Skinner, S. diversiformis Dunbar and Skin-
ner, Paraschwagerina plena, n. sp., Pseudo-
schwagerina beede: Dunbar and Skinner, P.
terana Dunbar and Skinner, Parafusulina
linearis (Dunbar and Skinner), and P. schu-
cherti Dunbar and Skinner.
Descriptions of the new species mentioned
above follow.
Triticites comptus, 0D. sp.
PIA ests ao
Description—This_ elongate, subcylindrical
species commonly reaches a length of 9.2 mm
and a diameter of 2.0 mm in six to seven volu-
tions. The tightly coiled compact early whorls,
regularly and highly folded septa, rudimentary
Oct.-Nov. 1959 ROSS: NEW SPECIES OF FUSULINIDS 301
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T. vENTRICOSUS T. comprtus
Fie. 2.—Composite stratigraphic section (vertical scale: 1 inch = 100 feet) showing typical fusulinid
faunas (all X 5).
302 JOURNAL OF THE
chomata, and curved axis of coiling are distinc-
tive of this species (Pl. 1, figs. 1, 5).
In specimens examined the proloculi are small,
averaging 0.10 mm outside diameter. The first
two or three volutions are tightly coiled and
elongate, attaining form ratios of 2.5 to 3.2.
Succeeding volutions are higher and become
greatly extended along the curved axis of coil-
ing; the form ratio in the sixth or seventh volu-
tion generally exceeds 4.5. The long polar ex-
tremities are narrow and unevenly rounded and
overlap irregularly the preceding half volution
(Pl. 1, figs. 2, 5). The chambers increase slightly
in height laterally away from the midplane. The
shape of the lateral slopes is regular but tends to
be convex in most volutions.
The wall is composed of a thin tectum and a
thin, indistinct keriotheca. The wall thickness
gradually increases from 0.005 mm in the pro-
loculus to 0.05 mm in the sixth or seventh volu-
tion. The wall thickness remains nearly constant
from the midplane to the polar extremities.
The septa are thin and highly fluted into
closely spaced, nearly regular folds, which ex-
tend laterally across the entire chambers (PI. 1,
fig. 5). As seen in the sagittal section (PI. 1,
fig. 3), the septa are extremely numerous per
volution and are inclined steeply from the ante-
theca towards the floor of the chamber. The
folds often reach the top of the chamber and
have steep nearly parallel flanks and acutely
rounded crests.
The tunnel, narrow in the first three or four
whorls, expands gradually in later whorls. The
tunnel angle measures 18° in the first volution,
25° in the third, and 40° in the fifth or sixth
whorl. The tunnel is well defined by either low
chomata or breaks in the closely spaced, highly
folded septa throughout all but the outer volu-
tion (Pl. 1, figs. 1, 5). The path of the tunnel
includes the midplane of the shell. The antetheca
beneath the tunnel is often thinner than the
antetheca on the lateral slopes and apparently
has been slightly resorbed by the tunnel. Cho-
mata are rudimentary in the shell and form as
thin, high deposits connecting adjacent septal
folds of the successive chambers (Pl. 1, fig. 3).
Secondary axial deposition, common in the first
two or three whorls, gives this portion of the
shell a dense, dark appearance. These deposits
form as septal thickening in the lateral regions
of the early whorls.
Discussion —Triticites comptus, n. sp., is simi-
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, No. 9
lar in shape and general internal structures to
T. joensis Thompson, T. osagensis Newell, T.
tenuis Merchant and Keroher, T. plicatula Mer-
chant and Keroher, 7. ohioensis Thompson, and
T. collus Burma. From these species T. comptus
differs in lacking well-defined chomata and hay-
ing more regularly and highly folded septa
across the shell.
The stratigraphic occurrence of this highly
specialized species of Triticites, T. comptus, indi-
cates that it is probably similar to the unde-
scribed species mentioned by Thompson (1957,
p. 300) from the lower Virgil of the Midcontinent
region. The species takes its name from the Latin
comptus, meaning ornamented, elegant, refer-
TABLE OF MEASUREMENTS
YPM specimens
| Vo-
_lu- | 20550 | 20551 | 20555 | 20554 | 20552
tion
—=—= |
radius vector) 0 05mm) .05mm) .06mm| oun .05mm
t cOy 08 | 41 ee
2 1-10 12°. | a eas
See 20 © | 230) = jhean 5:
Ah Sat .30 .48 | .30 32
5 | .53 48 70 = ae ee
6 | .7 70° |1200° Pee eee
7 — .98 = GiEoon .88
|
half length 1 19mm} .19mm .28mm| 12mm) (12
Zee P| as AS.) 238 Sie
Bos on 62 {1.00 | .65 | 22
3 |1.15° |1.01 |1.90 ~—‘{1.20 +193
“B~|2.40 {2.00 |3.40 1.40 |27
6 |3.60 |2.40 [5.30 1.90 32
7 — [460 | — [3-90 | 29
formratio | 1 |2.7 |2.4 (2.5 1.5
221220 372 2.4 3.2
3 12.8 3.1 3.3.
4 13.3 3.3 4.0 4.0
5 14.5 4.2/4.9) SS
6 |4.7 3.4 5.3 2.9
7 — (4.7 — |4.3
| |
tunnelangle| 1 26° 18° |) = —
| 2 28 24" eras 18°
3 30 26. | 30 }ee20
eo ee 29 | 44:7 | Bias
5 — 39 45 | 28
6 = 43 — =) 20a
i ou —-— | — | =
wall thick- | 0 |.003mm .007mm .02mm '.007mm|
ness 1 /.003 |.009 |.005 |.008 |
2 1.005 |.01 007 |.01
3 |.01 01 01 01
4 |.02 02 005.01
5 |.02 .03 01 1.02
6 | .05 .04 03 06
7 — |.05 We bir
* Number of septa.
Speen 1959
ring to the close, regularly folded septa seen in
thin-section.
Occurrence-—Upper part of the Gaptank for-
mation in the Wolf Camp Hills, at Leonard
Mountain, and in the syncline four miles west of
Marathon, Tex.
-Holotype—YPM 20551, Yale Peabody Mu-
seum, illustrated Pl. 1, fig. 5, Gaptank formation,
Wolf Camp Hills.
Schwagerina crebrisepia, n. sp.
Pl. 4, figs. 1-3, 5
Description—This large, elongate species
commonly reaches 13 mm in length and 3 mm
in diameter in seven volutions. In thin section
specimens show a marked division between early
and late growth patterns; the young shell is
tightly coiled with secondary deposits and the
adult shell is loosely coiled with secondary de-
posits in irregular patterns along the axis.
The proloculus of the holotype (PI. 4, fig. 3) is
0.10 mm outside diameter and is spherical. The
size of the proloculi in other specimens ex-
amined is remarkably consistent averaging 0.10
mm in diameter with little variation. The first
three to four volutions are tightly coiled and
growth during this stage is mainly along the
axis. Form ratios of 3.0 to 4.0 are common in
the first four volutions. The fifth volution shows
a distinctive increase in chamber height as well
as a considerable increase in length. The form
ratio remains constant or decreases slightly in
this volution, but in later volutions it increases
reaching as much as 4.3 in the seventh one. The
chamber height in the adult whorls increases
gradually in the center of the shell, but in the
lateral and polar extremities the height in-
creases greatly giving the shell a subcylindrical
shape.
The wall is thin in the proloculus, 0.005 to 0.01
mm thick, and in the early whorls reaches only
0.03 mm. The adult whorls thicken gradually to
about 0.10 mm in the last whorl.
The septa are thin and highly folded (Pl. 4,
fig. 3). These folds have steep sides, reach to the
top of the chambers, and are rounded to sub-
acute at their crests in the adult whorls. In the
early whorls the folds are flattened across their
crests. Throughout the shell, the closely spaced
folds show a regular pattern, each septum having
folds of uniform height. The septa form parallel
to the axis of coiling.
ROSS: NEW SPECIES
OF FUSULINIDS 303
The tunnel angle ranges between 15° and 25°
in young shells, but increases gradually to a
width of 30° in the sixth volution and is one-
third the height of the adult chambers. The tun-
nel path deviates as much as 10° out of the
midplane of the shell. Chomata are rudimentary
in the early whorls and completely lacking in
the adult whorls. Secondary deposits fill the
young volutions except near the midplane and in
the first three adult whorls these deposits fill
the axial extremities. The septa in the remaining
portions of the shell show evidence of secondary
deposition at the crests of their folds. False walls
are common in the specimens examined; how-
ever, they are not present in whorls with axial
fillings.
TABLE OF MEASUREMENTS
YPM specimens
vole: 20634 20632 20631 20630
radius vector 0 .05mm 05mm | .05mm .05mm
1 ai aif | .09 | .09
2 .19 .20 .12 ll
3 30 .32 .20 sel
4 52 51 32 | .40
5 80 86 600 "70
6 ss 1.20 / 1.00 1 1.10
7 1.50 1.50 1.40 1.45
half length 1 .25mm .22mm -llmm -10mm
2 .65 -50 .38 .20
ee ee 1.10 52 | .50
4 2.10 1.95 .90 eS
5 3.10 2.80 | 1.85 | 2.15
6 | 4.65 4.00 3.40 | 2.80
7 | 6.40 5.75 | 4.20 | 4.70
form ratio 1 | 2.0 2.0 1.2 1.1
2 3.4 225 ae 1.8
3 3.8 3.4 2.6 2.4
4 4.0 3.8 2.8 2.9
5 3.9 Ee 3561 a1
6 4.0 oue 3.4 ae
7 4.3 | 3.8 | 3.0 | 3.2
tunnel angle 1 20° 18° 15° 245
2 20 17 18 28
3 25 22 28 28
4 30 25 24 25
5 30 21 17 23
6 29 28 23 30
7 =a wes as ee
wall thick- | 0 .01mm -Olmm | .0lmm | .005mm
ness emt -O1 -O1 | .008 _ .005
2 01 .02 -O1 .008
3 .02 .03 01 -O1
4 04 .05 -03 .03
5 09 .08 -03 .09
6 Gl 12 .06 Bi Ut
i
.10 a2 08 | .10
5304 JOURNAL OF THE
Discussion—Schwagerina crebrisepta is simi-
lar in general internal structure to S. franklinen-
sis Dunbar and Skinner but has distinct young
and mature regions, a larger size per volution,
and notable axial deposition. S. complexa
Thompson is similar in size and ontogeny but
has greater inflation in the adult chambers, less
tightly and less regularly folded septa, and is
more fusiform. The specific name crebrisepta
from the Latin, many septa, refers to the abun-
dant septa seen in thin sections of this species.
Occurrence -—Lenoxhills formation in western
Glass Mountains, Tex., reworked specimens in
lower part of the Leonard formation.
Holotype —YPM 20634, Yale Peabody Mu-
seum, illustrated Pl. 4, fig. 3; from Lenoxhills
formation, north of Hess ranch horst.
Schwagerina dispansa, DN. sp.
Pl. 2, figs. 7-12
Description—The shell of this species com-
monly attains a length of 9.5 mm and a diam-
eter of 3.5 mm in seven to eight volutions. The
outer two or three whorls are greatly extended
along the axis and give the shell long winglike
projections. The inner whorls are shorter and
more loosely coiled. The regularly folded septa,
early globose volutions and later extension of the
shell along the axis, and medium to small size
distinguish this species.
In specimens examined, the proloculi are
aspherical to spherical and range in size from
0.04 to 0.16 mm outside diameter. As shown in
Pl. 2, fig. 8, the initial whorl is often highly in-
flated and irregular, with a form ratio of 2.0.
The succeeding two or three volutions have thick
fusiform outlines and increase in height and
length proportionally, retaining form ratios of
2.0. In the outer two or three whorls the cham-
bers extend laterally along the axis as long ex-
tended polar extremities, and the form ratio in-
creases to 3.0 (Pl. 2, fig. 7, 12). The poles of
these mature volutions are evenly rounded and
the lateral slopes concave. The chambers in the
early whorls are nearly constant in height from
the center to the poles, but in later whorls they
show a great increase in height in the extended
polar extremities.
The wall is composed of a tectum and a thick,
coarsely alveolar keriotheca. The wall remains
constant in thickness from the center of the shell
to the polar extremities. It is commonly 0.01 mm
thick in the proloculus and gradually increases
to 0.10 mm thickness in the last volution. In
WASHINGTON ACADEMY
OF SCIENCES VOL. 49, No. 9
specimen YPM 20628 (PI. 2, fig. 7) the wall in
the minute proloculus is 0.003 mm thick.
The septa are strongly and regularly folded
throughout the shell. The folds are symmetrical
with nearly straight sides and rounded crests and
they are evenly spaced across the entire cham-
bers. The basal margin of folds of one chamber
generally touches the opposing folds in adjacent
chambers. Cuniculi are not observed in these
shells, but as shown in specimen YPM 20627
(Pl. 2, fig. 10) the formation of the tunnel re-
sults in resorption of the base of the septa and
this gives the impression of one well-developed
cuniculus on each side of the tunnel.
TABLE OF MEASUREMENTS
YPM specimens
|
Volu- | 20628 | 20629 | 20625 | 20626
radius vector 0 .04mm .12mm .16mm -14mm
1 09 .20 Ia aah
2 10 .39 47 41
3 .19 .70 2s .65
4 .30 1b JES 1.10 | .90
5 sar 1.55 1.35 1.30
6 .95 1.80? — 1.70?
7 1.35 — — --
8 1.60 — — --
half length 1 09mm 45mm .45mm .65mm
2 20 85 ete -90
3 32 1.50 1.35 1.30
4 .60 2.55 2.00 1.90
5 1.00 3.65 2.95 2.95
6 1.60 5.35 _ 4.30
7 2.80 — — —
8 4.90 _ — _—
form ratio 1 1.0 Dae, ey, 2.4
2 2.0 DE? tee 222
3 ise! 7d: 1.9 2.0
4 2.0 De 1.8 Zed
5 1.9 2.4 72 2.3
6 bs7/ 3.02 — Deen
7 Dell - — —
8 Roll — — _—
tunnel angle 1 28° iW 7X Ne 22
2 30 27 23 27
3 32 24 17 27
4 32 31 — 36
5 24 — _ —
6 29 — — —
7 38? —_— _— —
wall thick- 0 003mm O0lmm | .007mm | .02mm
ness 1 .003 01 .02 .02
2 .008 03 .02 -03
3 01 03 .07 03
“4 02 10 .08 .06
5 04 a .08 -08
6 07 .10 — .09?
7 .09 = = =
Bi eat) -- -- _
Oct-Nov. 1959
The straight tunnel is of medium width, the
tunnel angle is 20° in the first whorl with a
gradual increase to 35° in the fourth or fifth
whorl. The septa are resorbed to about one-half
chamber height to form the tunnel. Chomata
are rudimentary and are present only on the
outer surface of the proloculus. Secondary de-
posits occur in about two-thirds of the speci-
mens examined, and may be thick in the axial
region or thin coatings on the septa throughout
the shell. Falsewalls are common in shell cham-
bers which lack axial fillings (Pl. 2, fig. 7, 12).
Discussion—Schwagerina dispansa is a rare
species that is seemingly closely related to S.
knighti Dunbar and Skinner. S. knighti is much
larger and has several more highly globose volu-
tions than does S. dispansa, but variation within
S. knighti is poorly known. Axial deposits when
present in S. dispansa are apparently distinctive.
S. dispansa is similar in shape to S. nelsoni Dun-
bar and Skinner but is smaller when mature and
has a considerably different ontogeny.
The species takes its name from the Latin
dispansa, meaning stretched out, and refers to
the extended polar extremities in the mature
shell.
Occurrence—Lenoxhills formation in western
and central Glass Mountains, Tex.
Holotype—YPM 20628, Yale Peabody Mu-
seum, illustrated Pl. 2, fig. 7; from the Lenoxhills
formation, north of the Wolf Camp Hills.
Schwagerina extumida, n. sp.
Pl. 3, figs. 4-7, 9
Description—This thickly fusiform species
commonly attains a length of 9 mm and a diam-
eter of 4 mm in seven to eight volutions. The
form of the early whorls is globose and chamber
height increases proportionally faster than axial
elongation until the fifth volution. The later
whorls become more elongate and have concave
lateral slopes in the seventh and eighth volutions.
The poles are small and acutely rounded. The
wall in the outer whorls is extremely thick for
shells of this size but it changes thickness ap-
preciably from a maximum near the center to a
minimum near the poles, a distinctive feature
in this species (Pl. 3, fig. 6).
The proloculi are subspherical and in speci-
mens examined range between 0.14 and 0.18 mm
outside diameter. The first two whorls are low
and in most specimens have a form ratio of 2.4
in this portion of the shell. The third, fourth, and
ROSS: NEW SPECIES
OF FUSULINIDS 305
fifth whorls increase notably in height but rela-
tively little in length, giving form ratios of about
1.8. The chamber height remains constant, or
nearly so, across the entire shell in these volu-
tions. The sixth, seventh, and eight whorls show
a considerable increase in length. The height of
these chambers increases toward the poles to
give the lateral slopes a slight concave outline
(Ries siesi6.67)e
The spiral wall is composed of a well-defined
tectum and a thick, coarse keriotheca. In the
center of the shell the wall thickness increases
notably in the last two whorls to a maximum of
0.19 mm. In the lateral regions, the wall thins
evenly toward the poles.
The septa are regularly and highly folded
throughout the shell. They are closely folded in
TABLE OF MEASUREMENTS
YPM specimens
Your 20648 20649 20646 20650
radius vector 0 .07mm -09mm 08mm .09mm
1 pli allt el2 19
2 srl sel 57 .38
3 .36 Oe 45 .59
4 yl .70 -70 90
5 STA 1.20 1.00 1.30
6 1.21 1.70 1.40 1.60
7 1.65 2.00 — ao
half length 1 .20mm .25mm . 25mm 45mm
2 45 50 50 80
3 65 75 70 1.20
4 .95 1.20 1.30 e75
5 115834) 2.00 2.10 2.65
6 1G: 3.30 — 3.80
7 3.10 4.60 = =
form ratio 1 2.4 15 Well 2.4
2 Boll 1.6 Det pall
3 1.8 1.4 1.6 2.0
4 MZ 6 2/ 1.8 1.9
5 1.9 ted Dil 2.0
6 1.8 1.9 2.0 2.4
U 1.9 28 — =
tunnel angle 1 15° 20° ASS 22°
2 15 20 25 22
3 15 20 20 20
4 20 20 20 20
5 20 20 20 —
6 15 —- — a+
7 au a as ae
wall thick- 0 .008mm 01mm 007mm Olmm
ness 1 . 009 .015 . 008 .03
2 .015 .02 .012 -06
3 .025 .07 .03 .07
4 .080 09 .08 .09
5 .110 Ealtay 5 IH 5}
Gian \as1S0 Si .14 ?
7 .190 -19 —_ —
506
the first five volutions but the folds are spaced
slightly farther apart in the outer whorls where
the axis becomes elongate. Also the septa are
somewhat farther apart in the outer whorls (PI.
3, fig. 6) and the center of the septa lags behind
the lateral portions during growth.
The tunnel is narrow throughout the shell.
The tunnel angle reaches 25° in only one speci-
men examined, the average is about 20°. The
tunnel is well defined by secondary deposits on
the basal margin of the septa (pseudochomata)
and occasionally as minor axial fillings (Pl. 3, fig.
9).
Discussion—The rapid thinning of the wall
toward the poles and the placement and type of
secondary deposits make this species distinct
from most other species of Schwagerina. S. hes-
sensis Dunbar and Skinner is similar, however
the large proloculus, elongate form, and nearly
constant wall thickness of that species are dis-
tinetly different. S. hawkins: Dunbar and Skin-
ner is larger, more globose throughout the shell,
and has secondary deposits reinforcing the septa
throughout the entire shell. White (1932, Pl. 6,
fig. 6) illustrates a form which is similar to this
species and calls it Triticites plummeri, however
that form is smaller, has well-developed chomata
in the early whorls and is only superficially simi-
lar to S. extumida. Species derives its name from
the Latin extumida, meaning swelled up.
Occurrence —Lower part of the Lenoxhills
formation in Hess ranch horst.
Holotype—YPM 20649, Yale Peabody Mu-
seum, illustrated Pl. 3, fig. 9; Lenoxhills forma-
tion; Hess ranch horst.
Schwagerina lineanoda, n. sp.
Ri2 hess 1=G
Description—This small, subeylindriecal spe-
cles commonly reaches a length of 7.5 mm and a
diameter of 2.5 mm in six volutions. The shape
of the shell remains nearly constant during
growth with only a gradual elongation along the
axis of coiling. The poles are bluntly rounded
and succeeding whorls form smoothly rounded
poles without over hanging lips.
In specimens examined the proloculi are com-
monly aspherical and range in size from 0.16 to
0.24 mm outside diameter. The early whorls are
low and establish the general shape of the shell
by the second volution. The succeeding volutions
increase gradually in height. The chambers, how-
ever, show an increase in height toward the polar
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 9
extremities which causes gradual elongation of
the shell along the axis and gives the shell a more
cylindrical form in the outer volutions. The
lateral slopes are convex throughout the shell.
The form ratio increases from about 2.0 in the
first or second whorl to about 3.0 in the sixth.
The wall is fairly thick for shells of this size
and increases from 0.009 mm thick in the pro-
loculus to 0.06 mm in the sixth volution. The
wall is composed of a tectum and a finely alve-
olar keriotheca. It remains constant in thickness
from the center of the shell along the lateral
slopes to poles.
The septa are thick and tightly fluted into
close, regular folds. In thin sections these folds
are subcircular in outline, the greatest width of
the folds being slightly above the floor of the
chamber (Pl. 2, figs. 1-4). In axial section the
folds appear as series of knots aligned on the
floor of the chamber. The septal folds lap over
TABLE OF MEASUREMENTS
YPM specimens
Volu-| 20677 | 20675 | 20676 | 20674
radius vector 0 .12mm .07mm .llmm .08mm
1 rye .20 .19 BAZ
2, 38) .30 .29 .20
3 -48 .48 -42 .30
4 si? al .70 -00
5 1.00 .95 .95 .65
6 1.20 1.20? — —
half length 1 .55mm 30mm .40mm 20mm
2 1.00 .70 -70 45
3 1.60 1.00 1.35 80
4 2.50 1.70 2.15 As
5 3.30 2.45 2.80 1.60
6 3.90 3.10 — —
form ratio 1 3.3 1383 Deal 17
2 3.0 2.3 2.4 Does
3 Bo8) el 22% 2e0:
4 Boh 2.4 Sill Zan
5 See 2.6 2.9 2-5
6 Bor 2.6 = =
tunnel angle 1 28° 30° 28° 33°
2 29 34 30 35
3 29 35 35 32
4 30 33 32 —_
5 =— — —— —
6 — — —— —
wall thick- 0 .008mm 009mm 009mm 0imm
ness 1 .01 .02 01 01
% .03 02 .02 02
3 .05 .04 03 04
4 .07 -05 -07 06
5 05 07 05 07
6 .06 .06 —_ _
Oct—Nov. 1959
one another in the lateral regions of the early
whorls, but this is not so in the central region.
Cuniculi have not been observed. Although the
septa touch each other (Pl. 2, fig. 5), the septal
wall apparently is not resorbed at the point of
junction. In the fourth and later whorls, the
septa are widely spaced in many specimens and
do not always touch one another.
The tunnel is wide in this species, 28° in the
first volution, and gradually increases to about
30° in the third or fourth. Beyond the fourth
whorl where the septa become widely spaced, the
tunnel is difficult to trace in thin sections. Rudi-
mentary chomata are common on the outer sur-
face of the proloculus and in the first whorl,
but are lacking in the rest of the shell. Secondary
thickening of the septa in the axial region is
common in adult specimens, but generally lack-
ing in immature specimens (compare PI. 2, fig. 1,
with fig. 4, both specimens from the same sam-
ple).
Discussion —Schwagerina lineanoda, n. sp., 1s
similar to S. crassitectoria Dunbar and Skinner,
but is more elongate, has more rounded septal
folds, and a thicker spiral wall. Parafusulina
linearis (Dunbar and Skinner) is more elongate,
has heavier axial fillings, and more regularly
folded septa.
The morphologic position of S. lineanoda be-
tween Parafusulinea linearis and S. crassitectoria
suggests the three species are more closely re-
lated than previously suspected. The name,
lineanoda from the Latin, having lined knots,
refers to the appearance of the subround septal
folds in thin section.
Occurrence —Lenoxhills formation at Dugout
Mountain and north of the Wolf Camp Hills,
Tex.
Holotype—YPM 20675, Yale Peabody Mu-
seum, illustrated Pl. 2, fig. 3; Lenoxhills forma-
tion, north of Wolf Camp Hills.
Schwagerina pugunculus, n. sp.
iplones: 8) 912513
Description—This large, fusiform species
reaches a length of 11 mm and a diameter of 4
mm in six to seven volutions. The flat lateral
slopes, small pointed poles, and highly folded
septa are distinctive (Pl. 1, fig. 18).
The proloculi in specimens examined range
between 0.12 and 0.26 mm outside diameter and
are generally spherical. The first two or three
volutions have low, long chambers which give
ROSS: NEW SPECIES OF FUSULINIDS
307
form ratios between 2.0 and 3.7 depending on the
individual specimen. The succeeding volutions
become elongate along the axis of coiling. The
chamber height increases markedly from the
midplane toward the poles, and the lateral
slopes are straight or slightly convex; in YPM
20777, however, one slope is slightly concave in
the last volution. After the third whorl the volu-
tions expand evenly and slowly having an early
tightly coiled portion and late more loosely coiled
portion that gives the shell a zoned appearance.
The wall gradually thickens from 0.01 mm in
the proloculus to 0.10 mm in the seventh volu-
tion. It is composed of a tectum and well de-
veloped keriotheca with coarse alveoli. The
keriotheca thins gradually toward the poles and
is almost completely lacking around the poles.
TABLE OF MEASUREMENTS
YPM specimens
VE | 2k. | ie | Ra | aa
radius vector| 0 06mm 07mm .13mm .llmm
1 aliZ B2 54k allt
2 28 26 .38 30
3 50 48 65 50
4 80 .62 1.00 80
5 eal 1.10 1.42 1.20
6 1.45 1.60 a7) —
7 — 1.90 — —
half length 1 20mm 45mm 45mm .3d5mm
2 60 80 30153 .70
3 1.10 1.30 1.45 1.20
4 2.20 1.80 2.20 Dells
5 3.10 3.00 3.50 3.00
6 5.20 4.50 5.00 —
7 = 5.50 — —
form ratio 1 Zee Bo fl 2.0 Dol
2 Dil 3.0 2.0 2.3
3 Dee, D2 22 2.4
4 2.8 2.9 ere, Doe
5 Dt etl 28 20
6 3.6 2.8 2.8 --
7 — 2.9 — --
tunnel angle 1 165° TUS? iy? DBS
2 15 17 21 19
3 15 21 24 20
4 17 19 25 32
5 — 27 ~- —
6 fest = es zoe
7 ns ale aes ma
wall thick- 0 01mm .01mm 02mm .01mm
ness 1 01 .02 03 .02
2 02 04 03 03
3 04 .08 07 03
4 07 09 10 06
5 10 10 09 09
6 .10 silt — —_—
7 — 10 — —
308
The septa are thick and are highly fluted from
pole to pole (Pl. 1, fig. 12, 18). The sides of the
folds are steep and nearly parallel along their
basal margins. The crests of the folds are acutely
rounded and extend to the top of the chambers.
Small septal pores are common and are evenly
distributed over the septal face.
The tunnel angle ranges between 15° and 32°
in specimens examined and seems to expand
gradually from a narrow beginning to its great-
est width in the fourth or fifth volution. The
path of the tunnel is slightly irregular, varying
about 5° out of the midplane. Rudimentary
chomata are common on the outer surface of the
proloculus and in the first and second whorls.
Slight secondary deposition is common along the
axis as septal thickening which generally does
not completely fill the chambers. False walls are
not observed.
Discussion—This species is similar in general
size and form to Paraschwagerina gigantea
(White) but lacks the tightly coiled juvenarium
of that genus. Schwagerina pugunculus is similar
in size to S. hessensis Dunbar and Skinner but
lacks the thick walls, closely spaced, dense septa,
and the early inflated whorls of that species. S.
pugunculus differs from S. diversiformis Dunbar
and Skinner, S. compacta (White) and S. cras-
sitectoria Dunbar and Skinner by the lack of
heavy axial deposits and differences in ontogeny.
S. thompsoni Needham is smaller and more in-
flated in its later volutions than is this species,
but in other respects these two species appear
closely related. At a given volution S. elkoensis
Thompson is about half the size of S. pugunculus.
S. complexa Thompson, which is similar in size
and shape to S. pugunculus, has more highly in-
flated early adult chambers, more irregularly
folded septa, less pointed poles and is smaller
per volution.
Study of the Dunbar and Skinner collection
shows that Dunbar and Skinner refer specimens
of this species from the Nealranch formation (at
Wolf Camp) to S. franklinensis Dunbar and
Skinner. However, S. franklinensis is more slen-
der and delicate in appearance and has a differ-
ent ontogenetic growth. (S. franklinensis is pres-
ent in the Glass Mountains but considerably
higher in the stratigraphic section.) The species
takes its name from the Latin pugunculus, short
dagger, and refers to the short daggerlike ap-
pearance of the lateral slopes.
Occurrence—Nealranch formation in the
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. 9
Wolf Camp Hills and at the base of the Lenox
Hills, Tex.
Holotype-—YPM 20716, Yale Peabody Mu-
seum ; illustrated Pl. 1, fig. 18; Nealranch forma-
tion, Wolf Camp Hills.
Schwagerina tersa, 0. sp.
Pl. 1, figs:.4,;/6;. 7.1073
Description—This small, fusiform species
commonly attains 7.5 mm in length and 2.5 mm
in diameter in six to seven volutions. Throughout
the shell the shape is ellipsoidal, the poles gently
rounded, and lateral slopes convex.
In specimens examined, the proloculi range
in size from 0.08 to 0.16 mm outside diameter,
and the first two whorls are low and extend
rapidly along the axis of coiling. After the shell
has reached a length of 0.8 mm, the next volu-
tion increases markedly in height giving the shell
the appearance of two growth stages. The lateral
slopes are convex throughout the shell and the
chambers remain constant in height from the
center to the pole. Succeeding volutions overlap
at the poles, but without forming a prominent
lip; instead the underside of the whorls joins
with and continues the profile of the preceding
half volution (PI. 1, fig. 4, 6, and 11).
The wall is composed of a tectum and a
coarsely alveolar keriotheca. The wall in the pro-
loculus is 0.007 mm thick and increases gradually
to 0.09 mm in the sixth or seventh volution,
and shows little or no decrease in thickness
laterally away from the center of the shell.
The septa are highly fluted into closely spaced
folds which extend to the top of the chambers
(Pl. 1, fig. 4, 6, 11). The folds have steep flanks
and gently rounded crests. Septal folds of one
chamber overlap opposing folds of the preceding
chamber only near the poles.
The tunnel is of medium width in the early
whorls and gradually expands in later whorls;
it measures 25° in the first volution and 40°
in the fourth. The path of the tunnel follows the
midplane of the shell with little deviation. Cho-
mata, 1f present, are found only in the first and
second volutions and on the outer surface of the
proloculus, and are always rudimentary. Other
secondary deposits are apparently lacking in
this species.
Discussion—Schwagerina tersa is a nonde-
seript species which has all the characteristics
of an idealized primitive Schwagerina species.
These features include the medium to small size,
_— one iat
Oct—Nov. 1959
TABLE OF MEASUREMENTS
YPM specimens
Volu- | 20685 | 20684 | 20680 | 20682
radius vector} 0 07mm 08mm 08mm 04mm
1 sill alt .19 .09
2 .19 nell -O2 31133
3 .30 43 .55 24
4 .48 .67 .80 -46
5 .70 .95 1.10 ey (ili
6 .90 11,834) = 1.00
if = — — LESS
half length 1 .23mm 30mm 42mm .20mm
2 -50 5 1.10 45
3 .70 1.20 1.70 BOD
4 1845) 1.90 2.10 .95
5 2.20 2.95 3.30 1.45
6 3.20 3.702 — 2.20
uf = — — 2.95
form ratio 1 Zrall 8) 2 1.8
2 2.6 2.8 3.4 3300)
3 B33 2.8 oll 2.3
4 2.8 oll 2.6 Weil
5 Bal etl 33 (1) 2.0
6 3.6 ? — Dae
7 = — — Ded,
tunnel angle 1 25M 24° AGE Tie
2 31 29 45 28
3 29 34 48 ?
4 38 30 46 29
5 55? — a _
6 = — — ——
7 pa ae 2 zs
wall thick- 0 008mm | .006mm ? .006mm
ness 1 .008 .009 .0lmm .008
2 .O1 -O1 .02 01
3 .02 .02 .03 -O1
4 04 .05 06 .03
5 - 06 .07 .08 04
6 .07 -08 — .08
7 _ — — 09
the even, elliptical outline of the volutions,
the regularly folded thin septa, and the wide tun-
nel. It is similar to S. emanciata (Beede) but is
larger, lacks well developed chomata, and has
more closely and regularly folded septa. S.
grandensis Thompson and S. colemani Thompson
are about the same size and shape as S. tersa, but
the walls of the early whorls in those species are
thicker and the septal folding less intense. S.
vervillei Thompson is similar in general shape,
size, and interior structure but is notably smaller
per volution.
This species incorporates a number of closely
similar specimens from a thick stratigraphic
sequence.
Occurrence —Lenoxhills, Leonard and Word
formations, Tex.
ROSS: NEW SPECIES OF FUSULINIDS
309
Holotype—YPM 20684, Yale Peabody Mu-
seum, illustrated Pl. 1, fig. 6; from Lenoxhills
formation, southwestern side of Leonard Moun-
tain, Glass Mountains, Tex.
Pseudoschwagerina tumidosus, N. sp.
Pl. 3, figs. 1-3, 8
Description—This large elongate species
reaches a length of 11 to 14 mm and a diameter
of 5 to 8 mm in six volutions. The apices of this
form are rather acutely pointed for a Pseudo-
schwargerina and lack the knobs common in
some of the more highly inflated forms.
The proloculus is relatively large (Pl. 3, figs.
1-3, 8) and average outside diameter is 0.25 mm.
YPM 20761 (Pl. 3, fig. 2) from a different lo-
eality, has a smaller proloculus of 0.18 mm, out-
side diameter. YPM 20760 (PI. 3, fig. 8) has an
irregular proloculus but other specimens have
near spherical proloculi. The juvenarium has
three to four volutions and a form ratio of 2.2,
but the adult shell inflates within a quarter volu-
tion to a form ratio of 1.6 to 1.7. The form ratio
gradually diminishes to 2.4 in the last volution.
The height of the last volution is considerably
lower than those of the early adult volutions
(GRE Ste, Is By 3)
The spiral wall is 0.03 to 0.09 mm thick in the
juvenarium, decreases in thickness slightly in
early adult whorls, but finally attains a thickness
of 1.1 to 1.2 mm in the last volution. It is finely
alveolar throughout the shell.
The septa are numerous, highly folded, ani
thick (probably as a result of secondary deposi-
tion) in the juvenarium (PI. 3, fig. 8). In the
early adult whorls they are thinner, irregularly
folded, but commonly overlap one another, es-
pecially away from the center of the shell. The
lower margins of the septa in the early adult
region are folded shghtly up to one-half chamber
height and the septa do not always parallel the
axis of coiling. In the last volution the septa are
more numerous, more tightly folded and overlap
each other across the shell. Septal pores are com-
monly seen in slightly oblique sections and are
distributed evenly over the entire septal face
(PLS Bs, ier, 2)
The tunnel is narrow in the Juvenarium (tun-
nel angle 17°), where it is well defined by cho-
mata. In later volutions it is not possible to trace
the tunnel with any degree of accuracy but it
apparently widens, having angles of 25° or 30°.
Discussion —Pseudoschwagerina tumidosus is
310
TABLE OF MEASUREMENTS
YPM specimens
Vol} 20760 | 20759 | 20761 | 20758 | 20757
radius vector| 0 .12mm)} .13mm)| .09mm| .13mm } .llmm
1 .20 Pl .18 .30 45
2 .38 aoD .30 aN) .70
3 .64 90 60 80 il 6/5959
Aiea 2.00 1.10 2.00 2.20
By hil S53 12.60 1.90 3.10 —
6 |2.30 _— — — =
half length 0 .20mm)} .13mm) .09mm
1 .40 20 35 11 17
2 70 .70 .60 24 20
3 .90 1.20 1.20 ay Pal 19
4 {1.80 2.00 2.50 19 18
5 |3.50 3.40 4.25 20 18
6 15.50? 4.50? 7.00 — 29
form ratio 1 |2.0 1.0 2.0
4 Wplats 2.0 2.0
a (lad! 7) 2.0
AS 16 De 2.3
5 /1.9 LZ 1 We
6 {2.4 oe 2.8
tunnel angle} 1 lee ie 15°
2 17 18 20
3 25 22 —
4 30 — —
5 bith ae a
6 Tah a ves
wall thick- 0 .03mm| .03mm)} .03mm
ness 1 04 .03 .03
2 06 .09 .09
3 08 10 .09
4 09 09 04
5 .10 .08 .10
6 .10 09 12
rare in my collections from the Glass Mountains
but those specimens examined suggest it is a
distinct species from others in the collections.
This species compares most closely with P. tex-
ana var. ultima Dunbar and Skinner but differs
in certain important aspects. The inflation after
the Juvenarlum is more pronounced and the
septa are more irregularly folded in the early
adult whorls in this species than in P. texana var.
ultima.
P. beedei Dunbar and Skinner, and P. texana
Dunbar and Skinner are smaller and less elongate
than this species. P. uddeni (Beede and Kniker)
and P. robusta (Meek) are more inflated and
have smaller juvenaria. P. convexa Thompson is
similar in respect to the juvenarium, but differs
markedly in the adult stages by having more>
regularly, tighter, and more highly folded septa
and a less pronounced inflation.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. 9
YPM 20759 and YPM 20760 differ from YPM
20761 in the septal folding in the early adult
region, mature form ratio, and the size of the
proloculus. As these may represent slight genetic
differences in a population, these specimens are
included in this species. Certainly the general
form of these shells suggests a close taxonomic
relationship and their stratigraphic distribution
suggests an approximate age equivalence. This
species takes its name from the Latin, tumidosus,
meaning swollen, and refers to the shape of shell.
Occurrence -—Lenoxhills formation in the
western Glass Mountains, Tex.
Holotype—YPM 20760, Yale Peabody Mu-
seum, illustrated Pl. 3, fig. 8; Lenoxhills forma-
tion, Dugout Mountain, Tex.
Paraschwagerina plena, nt. sp.
Pl. 4, figs. 4, 6-8
Description—This inflated species commonly
attains a length of 10 mm and a diameter of 5
mm in six volutions. The highly inflated central
portion of the shell and the nearly straight lat-
eral slopes tapering toward acutely rounded to
pointed poles are characteristic of this species
(PIS4 tie. "4. 7,78):
In specimens examined the proloculi are
spherical and small, ranging between 0.04 to 0.06
mm outside diameter. The first two or three
whorls are greatly elongate along the axis of coil-
ing and have form ratios of 3.3. After the shell
reaches a length of 0.09 or 1.00 mm, it rapidly
expands for two volutions with form ratios de-
creasing to 1.7. The last one or two volutions
show a decline in chamber height and a slight
elongation along the axis, this increases the form
ratio to 2.0. Each chamber is nearly constant in
height and shows little change laterally toward
the poles. The lateral slopes are generally highly
convex in the inflated portion of the shell and
become either straight or slightly concave in the
extended portion of the mature region.
The wall is composed of a tectum and a well-
defined coarse keriotheca and increases gradually
from 0.005 mm thick in the proloculus to 0.10
mm in the sixth whorl. The wall remains of con-
stant thickness from the center of the shell
nearly to the poles. The septa are strongly folded
throughout the shell. The early or juvenile
whorls have high septal folds reaching to the top
of the low chambers. The inflated whorls show
high but irregular septal folds and the outer one
I
Oct-Nov. 1959
TABLE OF MEASUREMENTS
YPM specimens
ee |) 20725 20723 20722
radius vector 0 04mm .05mm 06mm
1 09 .09 11
2 13 mill) 25
3 40 -o2 75
4 95 .94 1.40
5 1.60 1.70 2.00
6 2.30 — 2.502
half length 1 12mm 20mm 29mm
2 42 .50 65
3 95 . 80 1.20
4 1.70 1.70 2.20
5 2.90 2.95 3.70
6 4.50 — 5.00
form ratio 1 8! pal 2A6
2 Bo" BoB) 2.6
3 2.4 Pact) 1.6
4 1.8 1.8 1.6
5 1.8 Mae 1.8
6 2.0 —_ 2.0
tunnel angle 1 SDM 28° 29°
2 38 32 —
3 = — as
4 = — —=
5 = — —
6 —— a pases
wall thickness 0 005mm. 007mm. 009mm
1 .004 . 009 .008
W 008 .02 01
3 01 . 04 01
4 04 07 04
5 .08 5 1 10
6 .10 — —
or two mature whorls indicate a return to
closely spaced, regular septal folds.
The tunnel is wide in the Juvenarium, meas-
uring 30°, but it cuts few septa in the inflated
and mature portions of the shell and can not be
traced in this outer region. Rudimentary cho-
mata in the juvenarium are thin and may be
lacking in a few specimens. The rest of the shell
lacks chomata. Secondary deposition is appar-
ently rare in this species; Pl. 4, fig. 8, shows
secondary deposition on the septa only in the
mature region; other specimens show no de-
position.
Discussion—Paraschwagerina plena, n. sp., 18
ROSS: NEW SPECIES OF FUSULINIDS
oll
structurally between a typical Paraschwagerina
and a typical Pseudoschwagerina. The inflation
of the chambers in the early adult shell and their
reduction in height in the late adult shell com-
pare favorably with Pseudoschwagerina. How-
ever, the elongate juvenarium with closely folded
septa and only rudimentary chomata, and the
well-developed although irregular septal foldings
in the adult shell are more suggestive of Para-
schwagerina. P. plena is similar to P. yaber
(Staff), but P. plena has highly folded septa
throughout the shell and differs in size and shape.
Both of these species occur in rocks younger than
Wolfeampian and apparently are the aberrant
continuation of this lineage into the Middle
Permian. Paraschwagerina acuminata Dunbar
and Skinner is less inflated with more evenly
folded septa throughout the shell; P. kansasensis
(Beede and Kniker) is more globose and has
more regularly folded septa; and P. gigantea
(White) is longer and less inflated and has more
regular septal folds in comparison to P. plena.
The species takes its name from the Latin
plena, full or plump, and refers to the greatly in-
flated volutions of this species.
Occurrence —Lower part of the Leonard for-
mation in the Lenox Hills and the Lenoxhills
formation in the Hess ranch horst.
Holotype —YPM 20722, Yale Peabody Mu-
seum; illustrated Pl. 4, fig. 8; from lower part of
Leonard formation, Lenox Hills.
REFERENCES
Dunsar, C. O., and Skinner, J. W. The geology of
Texas 3 (pt. 2), Permian Fusulinidae of Texas.
Texas Univ. Bull. 3701: 517-825, 1937.
Kine, P. B. The geology of the Glass Mountains,
Texas, pt. 1. Texas Univ. Bull. 3038: 1-167.
1931.
———. Geology of the Marathon region, Texas.
US. Geol. Survey Prof. Pap. 187: 1-148. 1937.
Tuompson, M. L. Northern midcontinent Missour-
tan fusulinids. Journ. Paleont. 31: 289-328.
1957.
Uppen, J. A. Notes on the geology of the Glass
Mountains. Texas Univ. Bull. 1753: 3-59. 1917.
Wuirts, M. P. Some Texas Fusulinidae. Texas Univ.
Bull. 3211: 1-104. 1932.
312 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES VOL. 49, No. 9
EXPLANATION OF PLATES
All figures & 10
PLATE 1
Figs. 1-3, 5.—Triticites comptus, n. sp., Gaptank formation:
1. Axial section, ‘‘grey limestone,’’ Wolf Camp Hills, YPM 20555.
2. Axial section, 5 miles northeast of Wolf Camp Hills, YPM 20550.
3. Sagittal section, ‘‘grey limestone’’, Wolf Camp Hills, YPM 20552.
5. Axial section, holotype, ‘‘grey liimestone,’’ Wolf Camp Hills, YPM 20551.
Fras. 4, 6, 7, 10, 11.—Schwagerina tersa, n. sp., Leonard and Lenoxhills formation:
4. Axial section, southwestern end of Dugout Mountains, YPM 20680.
6. Axial section of holotype, 2!4 miles west of the Wolf Camp Hills, one-third the distance up the
slope, YPM 20684.
7. Axial section, 214 miles northeast of Wolf Camp Hills, YPM 20681.
10. Sagittal section, 2!'4 miles west of Wolf Camp Hills, one-third the distance up the slope, YPM
20679.
11. Axial section, 244 miles northeast of Wolf Camp Hills, YPM 20682.
Fias. 8, 9, 12, 13.—Schwagerina pugunculus, n. sp., Nealranch formation, Wolf Camp Hills:
8. Axial section, YPM 20721.
9. Sagittal section, YPM 20720.
12. Axial section, YPM 20719.
13. Axial section of holotype, YPM 20716.
PLATE 2
Frias. 1-6.—Schwagerina lineanoda, n. sp., Lenoxhills formation:
1. Axial section, southwest end of Dugout Mountain, YPM 20677.
2. Axial section, north of Wolf Camp Hills, YPM 20676.
3. Axial section of holotype, north of Wolf Camp Hills, YPM 20675.
4. Axial section, north of Wolf Camp Hills, YPM 20674.
5. Tangential section, north of Wolf Camp Hills, YPM 20673.
6. Sagittal section, north of Wolf Camp Hills, YPM 20678.
Figs. 7-12.—Schwagerina dispansa, n. sp., Lenoxhills formation north of the Wolf Camp Hills:
7. Axial section of holotype, YPM 20628.
8. Axial section, photographed with oblique lighting, YPM 20629.
9. Sagittal section, YPM 20624.
10. Tangential section showing a single false cuniculus resorbed by tunnel, YPM 20627.
11. Axial section, YPM 20625.
12. Axial section, YPM 20626.
PLATE 3
Figs. 1-3, 8.—Pseudoschwagerina tumidosus, n. sp., Lenoxhills formation.
1. Oblique section, Hess ranch horst, YPM 20751.
2. Shghtly oblique section, Hess ranch horst, YPM 20761.
3. Axial section, Dugout Mountain, YPM 20759.
8. Axial section of holotype, Dugout Mountain, YPM 20760.
Frias. 4-7, 9.—Schwagerina extumida n. sp., Lenoxhills formation, Hess ranch horst.
4. Sagittal section, YPM 20651.
5. Axial section, YPM 20650.
6. Axial section, YPM 20648.
7. Axial section, YPM 20646.
9. Axial section, holotype, YPM 20649.
PLATE 4
Fries. 1-8, 5.—Schwagerina crebrisepta, n. sp., Lenoxhills formation in the Lenox Hills:
1. Axial section, YPM 20682.
2. Axial section, YPM 20631.
3. Axial section, holotype, YPM 20634.
5. Sagittal section, YPM 20633.
Figs. 4, 6-8.—Paraschwagerina plena, n. sp., lower part of the Leonard formation, Lenox Hills:
4. Axial section, YPM 20723.
6. Oblique section, YPM 20726.
7. Axial section, YPM 20725.
8. Axial section, holotype, YPM 20722.
313
ROSS: NEW SPECIES OF FUSULINIDS
Oct-Nov. 1959
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BJORNSSON: RESPONSES OF CERTAIN FUNGI TO LIGHT
O17
PLANT PHYSIOLOGY .—Responses of certain fungi, particularly Trichoderma
sp., to light. Ipa P. Brornsson,? University of Maryland. (Communicated by
Harry A. Borthwick.)
(Received June 16, 1959)
The importance of lhght for growth and
development of fungi is evident from the
widely scattered observations in the litera-
ture and the increasing number of recent
studies. Its importance for processes other
than photosynthesis is well demonstrated for
higher plants (Hendricks and Borthwick,
1955) and has also been demonstrated for
ferns (Mohr, 1956) and algae (Finkle, Ap-
pleman, and Fleischer, 1950; Killam and
Myers, 1956). Owing to fundamental dif-
ferences in structure and development
among these groups of plants, their responses
to light are expressed quite differently. De-
spite the differences, careful studies of the
way light acts to induce each response can
show whether the same or different photore-
actions are involved.
The purpose of the present study was to
explore the types of response of several fungi
to light and to study in detail the response of
one of them which appeared to be best suited
for this type of investigation—viz., Tricho-
derma sp.
MATERIALS AND METHODS
Potato-dextrose-agar was generally used
as the culture medium, and the cultures were
erown at 21° C. Test tubes were used as cul-
ture vessels, except for Trichoderma sp.,
which was grown in petri dishes. The cul-
tures were standardized by starting each
from a single spore when possible—other-
wise from a hyphal tip. For qualitative ob-
servations, photographic records and visual
estimations were made. For the quantitative
determinations, spores were counted or per-
cent transmissions of light by the spore sus-
pensions were determined with a spectro-
photometer.
*Scientific article A638, Contribution 2821, of
the Maryland Agricultural Experiment Station,
Department of Botany. This paper is based on a
thesis which was submitted to the Graduate School
of the University of Maryland in partial fulfillment
of the requirements for the Ph.D. degree, 1956.
* Present address: Department of Biology, New
Mexico Highlands University, Las Vegas, N. Mex.
Cool, white, fluorescent tubes, at distances
of 48 or 100 cm, gave illuminances of 78 or
4 f.c., respectively. For isolation of blue and
red wavelength regions, two layers of blue
or two layers of red cellophane were used
with these tubes or with blue or red fluores-
cent tubes at the same distances when higher
energies were desired. The fluorescent tubes
were used as blue and red sources because
they emitted very little of the far-red wave-
lengths (7,000 to 8,000 A). The far-red
wavelength region from four inecandescent-
filament lamps (125-watt) was isolated by
a filter consisting of two layers each of blue
and red cellophanes (Piringer and Heinze,
1954). Radiant energy from such lamps was
rich in the far-red wavelengths. Radiant
energy was varied either by varying the dis-
tance of the cultures from the source of light
or by interposing neutral filters consisting
of different numbers of layers of cheesecloth.
The action spectrum for Trichoderma sp.
was determined with the spectrograph de-
scribed by Parker, Hendricks, Borthwick,
and Scully (1946).
RESULTS
Twelve species of fungi were grown in
light and in darkness and examined for re-
sponses, such as production of sexual and
asexual fruiting bodies, growth of mycelium,
and formation of pigments. Cultures of one
of these species, Mucor sp., formed a mat of
mycelium in the dark and under all condi-
tions with light, but it did not fruit under
any condition. Lack of fruiting suggested
that there was lacking in the culture medium
some compound necessary for the further de-
velopment of the fungus. The other 11 spe-
cies, including Trichoderma sp., which 1s dis-
cussed in detail in the last part of this
section, showed one or more responses to
light.
Stemphylium _ sp.
(a yellow mycelial
strain) did not sporulate in 4 weeks in dark-
ness. This finding verified earlier work on
other species or isolates of Stemphylium
318 JOURNAL OF THE
(Weber, 19380; Hannon and Weber, 1955)
which also required heht for sporulation.
When cultures were grown on potato-su-
crose-agar at 21° C., maximal spore pro-
ducted was obtained when light was given
26 to 72 hours after inoculation with a sin-
+ sgatneeneapers:
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 9
gle spore. For sporulation, darkness prior
to exposure to hght was apparently unnec-
essary and, once initiated, spores apparently
matured in light or darkness. After 50 hours
of growth of the cultures in darkness, the
shortest period of continuous white fluores-
3
Fig. 1.—Top row: Sporulation of Stemphylium in response to various durations of white fluorescent
light of 78 f.c. intensity. From left to right groups of three tubes received no light, 48 hours, 72 hours,
and continuous light. Middle row: Formation of sclerotia in cultures of Botrytis gladiolor um in response
to blue (first tube), far-red (second tube), red (third and fourth tubes), and darkness (fifth and sixth
tubes). Bottom row: Sporulation of Trichoderma sp. in response to darkness (left), 1-minute exposure of
sector at top of culture (center), and 1-minute exposure of whole culture (right) to 34 f.c. of white
fluorescent light.
Oct.Nov. 1959 BJORNSSON: RESPONSES OF CERTAIN FUNGI TO LIGHT
cent light (34 f.c.) that induced sporulation
was 18 to 23 hours and the number of spores
increased with duration (Fig. 1, upper row)
and intensity of light. The least amount of
white fluorescent light (78 f.c.) that induced
spore formation, when given in daily cycles,
was | hour per day for 4 or 5 days. With con-
tinuous white fluorescent light, saturation
for sporulation was obtained in 7 days.
During that period the intensity of the light
was alternated (500 f.c. for seven hours and
78 f.c. for 17 hours). Red and far-red wave-
lengths were ineffective or much less effec-
tive for inducing sporulation than were the
shorter wavelengths of the visible spectrum.
Mycelial growth of Stemphyliwm was
stimulated by about 5 f.c. of continuous
white fluorescent light at 21° C., but was
retarded at 28° C. All wavelengths of the
visible spectrum appeared to be effective for
mycelial growth. In darkness the culture
medium and the mycelium were yellow. In
light there was a negative correlation be-
tween the number of spores and the inten-
sity of yellow color; in no case was an ir-
radiated culture as deep a yellow as those
grown in the dark. The concentration of the
yellow pigment in the medium was high
under conditions unfavorable for spore for-
mation—exposure to red, far-red, or low-
intensity white light, increase in sugar con-
centration of the medium, or a temperature
of 28° C. The pigmentation of the mycelium
and medium might have been directly de-
pendent on light or indirectly dependent
through the action of hght on growth and
sporulation of the organism.
Cultures of Botrytis gladiolorum Tim-
merm. showed three responses to lght—
sporulation, ridging, and formation of scle-
rotia. The number of spores formed in
response to exposure to white fluorescent
light (78 f.c.) increased with duration of
exposure from 7 to 70 hours. Mycelial
ridges, consisting of aggregations of erect,
aerial, spore-bearing hyphae, alternating
with areas of sparse, prostrate hyphae bear-
ing few spores, occurred in cultures exposed
to certain daily alternations of 34 or 78 f.c.
of white fluorescent light and darkness
which followed not more than 3 days of
darkness. Ridges were formed in cultures
that received at least eight but not more
319
than 23 hours of light in 24-hour cycles for
4 or 5 days. Ridges were not formed in cul-
tures in continuous light or darkness. Con-
tinuous light resulted in a dense uninter-
rupted layer of spores and darkness resulted
in a thick layer of nonsporulating myce-
lum. Blue light promoted spore formation
and ridging.
Sclerotia did not form in cultures in con-
tinuous white fluorescent light (78 f.c.), but
a few formed in continuous darkness. The
best conditions for the formation of sclero-
tia were provided by a 30-minute irradia-
tion with white fluorescent hght after the
cultures had grown in darkness 4 days. The
cultures were returned to darkness and ob-
served 8 days later. In three experiments,
that tested the relative effectiveness of red
and blue hehts, more sclerotia were formed
in cultures exposed to red light; the response
to blue light was about the same as to dark-
ness (Fig. 1, middle row). A promotive ef-
fect of red hght has not been previously
reported, but blue light has been observed
to be inhibitory for sclerotium formation by
Botrytis cinera (Reidemeister, 1909), five
species of Aspergillus (Tatarenko, 1954),
and Verticillium alboatrum (McClellan,
Borthwick, Bjornsson, and Marshall, 1955).
Sporulation of Curvulana trbolu
(Kauff.) Boed. and a dark mycelial strain
of Stemphylium sp. was promoted in cul-
tures exposed to continuous white fluores-
cent light (78 f.c.) as compared with that
of cultures in darkness.
Peniciluum gladioli MeCull. et Thom.
produced an abundance of aerial mycelium
but no spores in continuous far red or in
darkness. Cultures grown in continuous red
light formed a few spores but considerable
aerial mycelium; those grown in blue light
formed an abundance of spores but no aerial
mycelium. These results agree with earlier
reports on several species of Penicillium
(Tatarenko, 1954).
Stromatinia gladioli
(Drayton) Whez.
formed a greater number of sclerotia when
erown in continuous white fluorescent, blue,
or red light for 4 weeks than in continuous
darkness. Blue light appeared to be the
most promotive.
Rhizoctonia carotae Rader produced scle-
rotiumlike bodies when grown in continuous
320
white fluorescent light (34 f.c.) either un-
filtered or filtered with two layers of blue
or red cellophane, but did not form these
structures in the dark.
Diplodia sp. from cotton did not form
pycnidia during 27 days in the dark, but
produced these structures under all light
treatments. Cultures in red light formed
fewer, larger, and longer-necked pyenidia
than did those in either blue or white fluo-
rescent light (78 f.c.).
Rhizopus sp. formed sporangia abun-
dantly when exposed continuously to un-
filtered white fluorescent light or filtered
blue light from blue fluorescent tubes, but
both of these kinds of hght depressed spo-
rangiophore elongation. Cultures in red
light or darkness formed long sporangio-
phores, only a few of which developed spo-
rangia. Cultures grown in an alternation of
eight hours of white or blue fluorescent light
and 16 hours of darkness produced fewer
sporangia but somewhat longer sporangio-
phores than did cultures in continuous light.
Lenzites trabea (Fr.) Fr. did not form
basidiocarps during 12 months in darkness.
Cultures, each started from a hyphal tip
and grown in continuous white light for 4
weeks, also failed to produce fruiting bodies.
However, if such cultures were given an ad-
ditional 6 weeks in the light, small, incom-
pletely developed basidiocarps were formed
during an additional 4 weeks in darkness.
They were also formed when filtered red or
blue fluorescent light—but not far-red—was
used. Cultures grown on malt agar gave the
same results. Cultures left in darkness for
4 or 6 weeks prior to an exposure to filtered
blue fluorescent light for 11 days or 4 weeks
produced larger and better-developed ba-
sidiocarps than did cultures in filtered red
fluorescent or unfiltered white fluorescent
light (78 f.c.). An 11-day exposure to light
was as efficient as a 4-week exposure; 4
weeks of darkness prior to and subsequent
to treatments with light were sufficient for
the response. Ten minutes, 60 minutes, 24
hours, 7 days, or 14 days of high-intensity
blue, red, or unfiltered white fluorescent
light given after 3 weeks of darkness did
not induce basidiocarp formation, but 14
days of blue light after 6 weeks of darkness
effectively induced their formation. L. tra-
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
voL. 49, No. 9
bea apparently requires 4 to 6 weeks of
growth to reach the stage of greatest sensi-
tivity to light for basidiocarp formation. An
exposure to high-intensity blue lght for at
least 11 to 14 days is required for this in-
duction.
An isolate of Trichoderma sp. was ob-
tained from Raymond Lukens, Department
of Botany, University of Maryland. Its
growth and coloration were the same in
light and in darkness. Cultures sporulated
abundantly in light but did not produce
spores during 96 hours in the dark. The
growth rate of the mycelium increased with
increasing temperatures above 4.5° C. until
at 32° C. the mycelium became atypical.
Growth at 21° C. proved satisfactory and
that temperature was used for the experi-
ments with light. Alternation of tempera-
ture induced sporulation of certain species
of fungi, but sporulation was not induced
in cultures of Trichoderma grown in dark-
ness at 21° C. by exposing them to 2° C. for
one-half hour to 6 hours at the time of their
greatest responsiveness to light. A pretreat-
ment at 2° or 27° C. of one-half hour to 6
hours in the dark did not affect the number
of spores produced at 21° C. during a sub-
sequent exposure to light. Cultures started
from small uniform-size pieces of agar with
vegetative mycelium or _ single spores
reached the stage or size for maximal re-
sponse when the colony had a diameter of
about 1.5 em. This was attained after 26
or 40 hours, respectively, at 21° C. With a
% TRANSMISSION
RELATIVE
INTENSITY
Fic. 2—Sporulation of Trichoderma sp. as a
function of different relative energies (value of 1 =
1.5 f.c.) of white fluorescent light given for 1 min-
ute. Sporulation expressed in terms of percent
transmission of light by spore suspension.
Oct-Nov. 1959
% TRANSMISSION
30
3800 4000 4200 4400 4600 4800 5000 5200 5400
WAVELENGTH IN ANGSTROMS
Fic. 3—Action spectrum curve for sporulation
of Trichoderma sp. at energies of 6 X 10* ergs/cm’.
Sporulation expressed in terms of percent trans-
mission of light by spore suspension.
1-minute exposure to light, the number of
spores increased linearly with a logarithmic
increase in intensity from 1.5 to 50 f.c. of
white fluorescent light (Fig. 2). At least
100 times as much energy was required for
cultures of 1.0-cm diameter as for those of
1.5-em diameter. Twenty-four hours after
exposure to light the first visible sign of
sporulation was the occurrence of a white
ring of swollen hyphal tips 0.6 em wide.
The outer edge of the ring corresponded to
the periphery of growth of the culture at
the time the light was given. In an addi-
tional 24 hours this ring took on the charac-
teristic blue-green of fully developed spores.
With exposure times above saturation for
sporulation, the spores matured earlier. If
a portion of the ring of hyphal tips was ex-
posed to light, sporulation was localized to
those tips actually receiving light and the
stimulus was not translocated to the unex-
posed but otherwise receptive hyphal tips
(Fig. 1, lower row). Localized responses
have been reported for the light-stimulated
formation of pyenidia of Physalospora ob-
tusa (Fulkerson, 1955) and the initiation
of fruiting of Coprinus lagopus (Madelin,
1956).
Other workers reported that blue light
was more effective than red for spore pro-
BJORNSSON: RESPONSES OF CERTAIN FUNGI TO LIGHT
o21
duction in cultures of Trichoderma l-
gnorum (Lilly and Barnett, 1951) and one
isolate of Trichoderma sp. (Krietlow, 1938).
Preliminary experiments with cellophane
filters demonstrated the ineffectiveness of
the red and far-red wavelengths, and this
ineffectiveness was verified with the spec-
trograph. The action spectrum (with inci-
dent energies of 6 X 10* ergs/em?) showed
that the most effective wavelengths for in-
ducing sporulation were 4,300 to 4,900 A.
A sharp break occurred near 4,800 A and
sporulation was not induced by wavelengths
longer than 5,200 A (ince, 3).
DISCUSSION
Numerous reports in the literature clearly
show that fungi, although heterotrophic, re-
quire light for control of many features of
their growth and reproduction. The wide-
spread sensitivity of fungi to light 1s em-
phasized by the results of this study, in
which 11 of 12 species exhibited one or
more responses to light. These organisms,
moreover, were selected at random as far
as prior knowledge of their sensitivity to
light was concerned and they were not sub-
jected to a wide range of conditions during
their culture.
The stage of development, age, or size of
the fungus colony required for maximal re-
sponse to light, as well as the total energy
needed for a response, appears to vary with
type of response and species. The amount
of energy required for asexual sporulation
in Trichoderma, for example, differed strik-
ingly from that required for the same re-
sponse in Stemphylium, Botrytis and Peni-
culium. Trichoderma sporulated after a
short exposure to low-intensity light, and
the reaction was easily saturated. These
results resemble those reported for fruiting
of Coprinus lagopus (Madelin, 1956). On
the other hand, spore formation by Stem-
phylium sp. increased with increase in dura-
tion of exposure to relatively high-intensity
light and saturation was difficult to attain.
Blue light was the most effective for sporu-
lation of both Trichoderma and Stemphy-
lium—indicating that a similar pigment or
pigment system absorbs the energy. The
difference in the total energy requirement
might be the result of differences in con-
322 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
centration of the absorbing pigment, differ-
ent pathways of metabolism, or still other
factors.
Sporulation of the above-mentioned fungi
did not require a dark period prior to expo-
sure to light. Responses of certain of the
others appeared to be preconditioned by a
dark period. For example, Botrytis gladio-
lorum responded differently depending on
its age or stage of development when ex-
posed to light. Selerotia were not formed in
cultures exposed continuously to light, but
continuous heht ultimately induced the
ereatest number of spores. Sclerotia were
formed in the greatest number if, starting
from a single spore, cultures received five
or six days of darkness prior to a 30-minute
exposure to light. It is not known whether
the formation of sclerotia was precondi-
tioned by the dark period or the dark period
served to suppress the other responses and
this suppression permitted the formation of
sclerotia.
Ridging of Botrytis cultures in response
to daily cycles of light and darkness oc-
curred only when more than one cycle was
used. Reports on this kind of response are
rare for fungi (Sagromsky, 1952b). Such a
response resembles photoperiodism in higher
plants. Photoperiodic responses of higher
plants, however, are controlled by red and
far-red wavelength regions of the spectrum,
whereas cyclic phenomena of fungi appear
to be elicited by blue light.
Except for sclerotium formation in Bo-
trytis, which was stimulated by red lheht,
all responses of these fungi were promoted
best by the blue region of the spectrum. The
action spectrum for sporulation of Tricho-
derma showed a peak in the blue wave-
lengths and a sharp cutoff near 5,000 A.
These features are similar to those of other
action spectra reported for fungi, such as
conidiophore elongation in several isolates
of Penicillium and Verticilliwm (Sagrom-
sky, 1952a; Sagromsky, 1952b), sporophore
elongation (Bunning, 1953) and trophocyst
formation (Page, 1956) in Pilobolus kleinai,
giant conidiophore formation in Aspergillus
giganteus (Gardner, 1955), formation of
macroconidia in Sclerotinia fructigena (Sa-
gromsky, 1952b), fruiting of Coprinus lago-
pus (Borris, 1934; Madelin, 1956), and ca-
VoL. 49, No. 9
rotenoid produc.ion in \eurospora crassa
(Zalokar, 1955). The action spectra resem-
ble the action spectrum of phototropism and
the absorption spectra of carotenoids and
riboflavins. Several pigments from both of
these groups, along with other pigments,
have been reported in various species of
fungi. Recent works (Bunning, Dorn,
Schneiderhohn, and Thorning, 1953; Zalo-
kar, 1955), especially those on metabolic
inhibitors (Page, 1956) and mutants (Can-
tino and Horenstein, 1956), appear to favor
a flavoprotein as the absorbing pigment for
such reactions to light.
Further research is required in this field
to establish similarities and dissimilarities
between fungi and other groups of plants,
but fungi appear to have pigment systems
absorbing mainly in the blue wavelengths,
whereas green plants appear to possess
these, for nonphotosynthetic reactions, as
well as pigment systems absorbing in the
red and far-red wavelengths.
SUMMARY
Light elicited the following responses in
certain species of fungi: Spore production,
mycelial growth and coloration, and colora-
tion of the medium in cultures of a yellow
mycelial strain of Stemphylium sp.; spore
production, ridging and formation of scle-
rotia by Botrytis gladiolorum; and spore
production by Curvularia trifolu, Penicil-
hum gladioh, and a dark mycelial strain of
Stemphylium sp.; formation of pyenidia by
Diplodia sp.; basidiocarp formation by Len-
zites trabea; formation of sporangia by
Rhizopus sp.; formation of sclerotia by
Stromatinia gladioli; and, the formation of
sclerotiumlike bodies by Rhizoctonia ca-
rotae.
Spores were not formed by Trichoderma
sp. within a 96-hour period of growth in
darkness, but they were formed after a 1-
minute exposure to white fluorescent light
(1.5 f.c.). Alternation of temperatures nei-
ther induced sporulation nor increased the
number of spores produced upon subsequent
exposure to light. Spores were localized to
that portion of the ring of hyphal tips ex-
posed to light. Spore production increased
linearly with a logarithmic increase in inten-
sity from 1.5 to 50 f.c. of white fluorescent
Oct.—Nov. 1959
light. The action spectrum for sporulation
showed a peak of response to wavelengths
of 4,300 to 4,900 A, a sharp break near
4.800 A, and ineffectiveness of wavelengths
longer than 5,200 A.
With a possible exception of red-light-
induced sclerotium formation in Botrytis
gladiolorum, these responses were induced
with the shorter (less than 5,200 A) wave-
lengths of the visible spectrum.
These findings corroborate the researches
of other workers concerning the greater ef-
fectiveness of the shorter wavelengths of
the visible spectrum and the widespread
importance of light in the life cycle of fungi.
ACKNOWLEDGMENTS
The author wishes to express very sincere
appreciation to Dr. H. A. Borthwick, Crops
Research Division, Agricultural Research
Service, U. S. Department of Agriculture,
Plant Industry Station, Beltsville, Md., for
his interest, guidance, and assistance
throughout this work; and to her adviser
Dr. H. G. Gauch, Department of Botany,
University of Maryland, College Park, Md.,
for his aid, including the preparation of the
manuscript. Grateful acknowledgment is
made to Dr. S. B. Hendricks, Dr. W. D.
McClellan, Mr. Otis Greeson, and person-
nel of the Photoperiod Project, U. 8. De-
partment of Agriculture, Plant Industry
Station, Beltsville, Md.; and the Depart-
ment of Botany, University of Maryland.
The present study was supported in part
by a grant from the North American Com-
mercial Gladiolus Growers. The author is
grateful for this support.
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324 JOURNAL OF THE
WASHINGTON
ACADEMY OF SCIENCES VOL. 49, NO. 9
ZOOLOGY .—A new Floridan Pectiniunguis, with re-appraisal of its type species
and comments on the status of Adenoschendyla and Litoschendyla (Chilopoda:
Geophilomorpha: Schendylidae). R. EK. Crasiuy, Jr., U.S. National Museum,
Smithsonian Institution.
(Received May 27, 1959)
In 1889, the year of his untimely death,
Charles Harvey Bollman proposed a new
venus, Pectiniunguis, for the reception of
two species, one of which had been collected
at Pichilinque Bay,! near La Paz, at the
southern end of Baja California; he called
his new centipede Pectiniunguis americanus
and declared this species to be the type of
the genus. This was only the second generic
name referable to a group subsequently to
be recognized as a family and called Schen-
dylidae.
The Bollman species was reported for the
second time in 1889 when O. F. Cook col-
lected what he took to be americanus on the
Florida Keys; subsequent workers until the
present time have accepted the validity of
his identification. It was, however, in error,
as a recent comparison of the rediscovered
Bollman type with the Cook material re-
veals. Final confirmation was possible fol-
lowing the study of a series of fresh speci-
mens generously donated to the USS.
National Museum by Dr. H. V. Weems, Jr.,
of Gainesville, Fla. These specimens con-
stitute the typical series of the new species
described below.
Pectiniunguis (as it is defined here) may
be. distinguished from other schendyline
genera by its possession of the following
characters: Each coxopleuron has two gland
pits of the heterogenous type; sternital
porefields present; second maxillary claw
bipectinate, the coxosternites not fused
posterolaterally and posteriorly with the
postmaxillary sclerites; ultimate pretarsus
is either absent or minutely tuberculate. In
1912 Broelemann and Ribaut in a splendid
monograph employed the same diagnostic
features and added their own discovery that
specimens so characterized display two
kinds of labra. Some of the species, includ-
ing americanus, they believed, have medial
* The type locality was originally given as “Pi-
chiliungue Bay,” a misspelling for Pichilinque Bay.
labral undulations instead of true alveolate,
rooted and discrete teeth. They ascribed the
possession of true medial teeth to other
species to which they assigned (1911) a new
generic name, Adenoschendyla; geayi is the
type species (by subsequent monotypy).
Following an extended discussion (1912,
p. 69), they summarized the differences be-
tween the two labral types as follows: “Are
médian 4 ondulations superficielles, appuyé
a des piéces latérales peu dévelopées en
avant...” for Pectiniunguis; versus “Arc
médian composé de dents tuberculeuses pres-
que individualisées et munies d’une racine
appuyé a des piéces latérales plus or moins
distinct de la zone prélabiale...” for some
others including Adenoschendyla. In 1923
Professor Chamberlin, in the belief that
americanus has true medial labral teeth,
showed that Adenoschendyla must fall as
the junior synonym of Pectiniunguis and
that this action would leave the species with
midlabral undulations without a generic
name. For them he proposed a new name,
Intoschendyla, designating insulanus (Bro-
elemann and Ribaut) as its type species.
In his monograph of 1929 Attems accepted
the Chamberlin resolution, and the matter
was apparently closed. The case seems sim-
ple and convincing; however, the recent ex-
amination of Bollman’s type and of the six
types of the present new species provides a
basis for doubt which is implicit in two
questions. (1) Since the only intergeneric
character is said to be the labral one de-
scribed by the French workers and accepted
by Chamberlin and Attems, is it really sig-
nificant and, if so, practical; that is, does
it represent an intergroup repeatable dif-
ference in kind as the French authorities
maintained (and if so will it assist rather
than confuse the generic assignment of spe-
cies), or, on the other hand, does this char-
acter represent a difference 7n degree which
is quite variable among closely similar spe-
cies and even intraspecifically (and if so
Oct-Nov. 1959
would its use weaken the function of the
genus as a collective category)? (2) And in
case the labral character is really significant
intergenerically, then to which of the two
labral types is Pectiniunguis americanus as-
signable, for the resolution of this question
determines the zoological content and the
nomenclatural disposition of all three ge-
neric names.
It cannot be denied that in some species,
e.g., geayl, there are some, or is at least one,
specimen with relatively long, discrete me-
dial teeth, and that in other species the
medial teeth are blunter, lower, wholly or
partly fused with each other, e.g., insulanus,
halirrhytus, n. sp. On the other hand, two
factors cannot be avoided, interpretative
subjectivity and inter- or intraspecific vari-
ability. The labrum is normally directed
ventroposteriorly, so that looking down upon
it one sees it at an angle and not in perfect,
flat outline; consequently the interdental fis-
sures can appear shorter than they are, or
absent when they are present, or they may
not even be recognized as fissures. There-
fore one person might decide that the teeth
are labral undulations that are connected
with each other or continuous; another, see-
ing the same specimen but under different
conditions of preparation and magnifica-
tion, could report quite a conflicting 1m-
pression. The character, then, is capable of
being interpreted in quite a highly sub-
jective manner. Secondly, in my series of
halirrhytus I have observed considerable
labral variability, ranging from a typically
“undulate” condition to one in which the
medial structures seem typically toothlike,
being discrete and apparently rooted. Yet
five of the six specimens were collected at
the same time from the same pile of sea-
weed, and all agree most minutely in other
significant respects. I suggest that the labral
difference, at least in some species and con-
celvably in many or in all, is one of de-
gree, not of kind; that is, in some species
(A) the teeth are long and tend to be or are
well separated (e.g., geayz), whereas in some
others (B) the teeth are shorter, blunter and
are discrete or quite variously fused (e.g.
msulanus, halirrhytus). Given a suitable
series of any species, considerable varia-
CRABILL: A NEW FLORIDAN PECTINIUNGUIS 320
~
bility within each of these two categories,
A and B, might reasonably be anticipated.
It seems most significant to me that, guided
by the Broelemann-Ribaut criteria as ap-
phed to halirrhytus, one could, if he had
only one specimen at his disposal and not a
series, assign the holotype to Litoschendyla,
some paratypes to Pectiniunguis and feel
quite uncertain of the allocation of some
others. If it is really the case that this labral
character is a concomitant of supraspecific,
e.g. generic, grouping, then either it is not
now sufficiently refined, or else no degree of
refinement can make of it a reliable indicator
of supraspecifie affinities. The reasonable
solution seems provisionally to be to unite
both kinds of species within one genus, de-
fining the labral characters rather broadly
and characterizing them as involving mid-
labral teeth that are either (A) low, blunt,
nodular, separated or variously fused; or
(B) longer, more or less well defined, es-
sentially or clearly discrete. This is not to
suggest that two monophyletic groups, gen-
era let us say, are not actually involved,
only that if they are, existing criteria seem
inadequate for distinguishing them in a sat-
isfactory manner. For practical purposes of
preliminary classification it seems best for
the time being to include all under the senior
generic name.
The second question concerns the affinity
of americanus, the type species of Pec-
tiniunguis. Without any question its mid-
labral area is much more like that of insula-
nus and halirrhytus than that of geay7. Its
midlabral teeth are low, rather nodular,
some have interdental fissures but some do
not (Fig. 5). The very distinct fissures sepa-
rating the most central teeth from those
adjacent seem to be artifacts owing their
existence to the fact that the greatly arched
labrum was crushed perfectly flat in the
preparation of the microscopic slide by
Cook or Collins. Therefore the present opin-
ion is that careful scrutiny at high magnifi-
cations (450 X) favors the original arrange-
ment of Broelemann and Ribaut, so that if
future studies provide new support for a
division of Pectiniunguis into two genera,
like that of 1912, one would be Pectiniun-
guis Bollman, 1889, type species americanus
326 JOURNAL OF THE
Bollman, 1889 (teeth nodular, short, vari-
ously fused); the other, Adenoschendyla
Broelemann and Ribaut, 1911, type species
geayt Broelemann and Ribaut, 1911 (teeth
longer, more or less discrete, typically denti-
form rather than nodular): Litoschendyla
Chamberlin, 1923, type species imsulana
(Broelemann and Ribaut), 1911 (teeth nod-
ular or undulate, interdental fissures ob-
scure or absent), would then fall as a junior
subjective synonym of Pectiniungws.
Pectiniunguis halirrhytus, n. sp.
On the basis of the limited evidence in the
literature and the direct evidence derived from
study of the type of americanus, it seems proba-
ble that the new species is most like the Bra-
ailian geayi (Broelemann and Ribaut), the
Colombian chazaliei (Broelemann), the Cuban
insulanus (Broelemann and Ribaut), the Guianan
gaige. (Chamberlin), and the Lower Californian
americanus Bollman. In all, the leg-pair range
is roughly similar, and the sternital porefields
are undivided and extend in an unbroken series
to one of the latter body segments.
In both geayi and gaigei the basal prehensorial
article bears a tiny denticle, the porefields are
subcircular or circular on all sternites, the mid-
labral teeth are, at least in the types, relatively
long, narrow and apparently typically dentiform ;
at least geay? lacks a clypeal area: in halirrhytus
no prehensorial article has any denticle what-
ever, the porefields are transversely elliptical to
subtriangular becoming subcircular only on the
rear sternites, the midlabral teeth are in some
specimens typically dentiform but in others
erenulate or undulate, in all they are nodular,
short and broad. Like the new species, insulanus
and chazalie: have short, broad midlabral teeth,
but in both there are four mandibular dentate
blocks, whereas in halirrhytus there are consis-
tently only three. Moreover, in chazaliei the
clypeus is not separated from the buccae by
(paraclypeal) sutures, but in halirrhytus these
sutures are prominent and complete, so that
clypeus and buccae are separated; in insulanus
the porefields are absent on the last four ster-
nites, but in halirrhytus there is a tiny poregroup
on the penult sternite.
Perhaps Bollman’s americanus is most like
halirrhytus; though the two are quite similar in
many respects, they also differ rather strikingly
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 9
in certain characters. In americanus: there is
prominent subsurface dark pigmentation mani-
festating itself dorsally as a geminate longi-
tudinal band, ventrally and laterally as dark
blotches; the pretarsal accessory claws are equal
in length and are not more than half as long
as the claw proper which is robust, rather blunt
and only slightly curved; the legs’ femora and
tibiae ventrally are only sparsely setose and
are not more setose than the other articles;
the ultimate sternite is relatively broader and
shorter; the ultimate pretarsus is small but
evidently discrete and distinctly tuberculate. In
halirrhytus: there is in the typical series’ no
dark subsurface pigmentation whatever; the
pretarsal accessory claws differ markedly in
length, the larger of the two being more than
three-fourths the length of the claw proper
which is quite thin, well curved and pointed
apically; the legs’ femora and tibiae ventrally
are clothed very densely with fine setae but
the other articles are not; the ultimate is rela-
tively longer and narrower; the ultimate pre-
tarsus Is intimately fused with the tarsus (or else
it is absent) but in any case is not discrete and
typically tuberculate. It seems unlikely that
there are pleural differences too. The Cook and
Collins representation of the pleural region of
americanus (their Fig. 3) shows 4 gamma to
be absent, but a re-examination of the Bollman
tvpe shows that it is present, Just as it is in
halirrhytus.
Holotype :—female. Florida: Monroe County,
Big Pine Key; in beach seaweed; December 30,
1957, H. V. Weems, Jr., leg. In U.S. National
Museum Myriapod Collection, no. 2548.
Inrropuctory. Total length, ca. 49 mm. Pedal
segments, 59. Body shape: anterior quarter of
body slightly attenuate, posterior third more
conspicuously so. Color: head antennae and pre-
hensorial segment pale orange-yellow; tergites,
“In 1899 Cook reported that some of his Florida
Key specimens of what he called Pectiniunguis
americanus had dorsal dark geminate bands. Hav-
ing re-examined his material, I find that apart from
the specimens of halirrhytus, all pale in color, there
are at least two other species, the banded Poly-
cricus marginalis (Meinert), and another species of
Pectiniunguis which is weakly banded but whose
identity is quite questionable owing to the ex-
tremely poor condition of the material. These spec-
imens seem rather like the true americanus; how-
ever their present state of preservation precludes
a confident assignment to that or any other spe-
cles.
Oct-Nov. 1959
picurites paler yellow; legs and sternites varying
from very dilute yellow to white; body entirely
without subsurface dark bands or blotches of
pigmented cells.
ANTENNAE. Length (in Hoyer’s mountant),
4.9 mm. Shape: distally very shghtly attenuate ;
each article but the first slightly longer than
wide. Setae (dorsal aspect): first 4-5 articles
with few short setae, each with 2 circlets of long
setae; articles 5 or 6 through 14 each densely
finely setose. Special sensilla: fourteenth article
with an elongate patch of spatulate setae on
outer distal half (these absent on medial sur-
face); a dorsal patch of short stiff special setae
on articles 14, 9, 5, (2?). CepHatic PuatE (Fig.
12). Length, 1.3 mm; greatest width, 1.2 mm.
Shape: dorsal surface inflated or domed, not
flat; anterior margin essentially rounded; sides
very slightly incurved and distinctly convergent
posteriorly; posterior margin straight. Setae
very few, these moderately long. Areolation:
coarse and deep on anterior dorsal lateral third,
approximately the dorsal and lateral two-thirds
smoothly shallowly areolate. Frontal suture en-
tirely absent; with two essentially parallel para-
median sulei passing from posterior margin of
plate forward for about half its length. Prebasal
plate exposed for its entire width, very narrowly
laterally, widely at middle. CLyprus. Paraclypeal
sutures conspicuous, wide, complete from an-
tennal sockets to outer edge of each labral
fultura (Kommandibulares Geriist). Surface
swollen ventrally especially in region of labrum.
Each bucea (pleuron of some authors) glabrous,
well defined, with a prominent transbuccal su-
ture running perpendicular to long head axis at
level of fultura. Clypeus anterocentrally with
a large, well-defined but essentially elongate
ovate to flask-shaped clypeal area, this identified
by its smaller, much paler areolate figures be-
tween which minute glandular pores open (seen
only at 450 x). Without areas of consolidate
areolation (plagulae). Setae: postantennals, 2;
posterior geminate setae (just anterior to la-
brum), 2, minute; midelypeals rather robust,
9 on each side, in two poorly defined transverse
rows on anterior quarter of clypeus, the two
medialmost setae occupying the aforementioned
clypeal area. Clypeus adjacent to labrum swol-
len, the areolation here heavier, darker. LaBRUM
(Fig. 7). In situ its free margin is strongly di-
rected posteroventrally, the lateral ends bulg-
ing laterally, cleft, heavily sclerotized. Central
CRABILL: A NEW FLORIDAN PECTINIUNGUIS
BY
are separated from clypeus by a narrow mem-
branous suture, with 4 low, irregular, blunt,
nodular teeth, some of these not distinctly sepa-
rated from each other, vaguely anchored to
clypeus, the 4 nodular teeth flanked on each side
by one weakly pointed tooth. Lateral part of
labrum on each side indistinctly separated from
central are but fused without suture to adjacent
elypeus and continuous with it, each side of
labrum with about 7 teeth, each tooth firmly
anchored, broad, essentially separated from the
one adjacent, each with a relatively long and
very sharp medially directed extension. MAn-
DIBLE (Fig. 1). Dentate lamella in 3 distinct,
heavily sclerotized blocks, dentition 2-3-3, the
innermost block (in situ, ventralmost) partly
overlapped by the row of simple hyaline
teeth, these numbering some 23, each sharply
pointed. Frrst MaxiLuaE (Fig. 10). Coxoster-
num coarsely areolate, without medial sulcus or
suture; setae as shown. Coxosternal lappets
thick, short, mostly concealed, reaching level
of base of second telopodite article; areolate,
not fibrous or squamulate. Medial lobes sub-
triangular, without apical nipples, distal half
membranous. Telopodite biarticulate, broad, api-
eal rounded; lappets concealed, thick, curved,
areolate, not fibrous or squamulate, not ex-
ceeding end of telopodite. SEcoND MAxXILLAE
(Figs. 6, 10). The coxosternites very broadly
joined by an isthmus, this medially narrowly
continuous with Ist maxillary coxosternum.
Postmaxillary sclerites (pleura of some authors)
separated from posterior outer corners of max-
illae by a broad membranous suture on each
side; inner corner not reaching metameric pore
opening, outer part not surpassing level of afore-
mentioned suture. Telopodite: Ist article basally
with a ventral and a dorsal condyle, inner and
outer margins essentially parallel; third article
much longer than second; apical claw robust,
very long, distally strongly attenuate and api-
cally incurved, with a dorsal and a ventral comb
of long thin flat hyaline teeth. ProsterNum (Fig.
11). Anteriorly broadly diastemate, not denticu-
late; entirely without midlongitudinal sulcus.
Pleura very broad; pleuroprosternal suture
strongly oblique, the adjacent prosternal margin
thickened as shown; sclerotic lines absent. Setae
few and moderate in length. Anterolateral cor-
ners smoothly areolate, the remainder coarsely
deeply so. PREHENSORIAL TELOPODITE (Fig. 11).
When closed, not exceeding front margin of
328 JOURNAL OF THE
head. Ist article rather short and broad, with-
out a denticle; second and third articles with-
out denticles; tarsungula basally with a typical
denticle but with a broad pale fold somewhat
resembling a denticle; claw relatively long and
curved, neither its dorsal nor ventral edges
serrulate. Poison calyx extremely long and thin,
the lower end abruptly deflected laterally; poi-
son gland long and pointed, terminating pos-
teriorly near base of trochanteroprefemur.
TerrGITES. Basal plate centrally neither fove-
ate nor suleate; peripherally darker yellow, the
areolation smoother, centrally whiter, the areo-
lation coarser and deeper. Remaining pedal
tergites (except the ultimate) each shallowly
but distinctly bisuleate, sparsely setose. PLEU-
RITES (Fig. 14). Coarsely areolate, very sparsely
setose. All spiracles strongly elliptical, their axes
horizontal. Series 1, 2, and 3 complete; 1 alpha
is divided; 4 alpha evidently not discrete (1..,
not present); 4 gamma and 5 gamma are pres-
ent, conspicuous. Legs (except ultimate) (Fig.
3). Ventral vestiture: femora and tibiae of legs
3 through penults very densely, finely setose;
setae of remaining articles long and notably
fewer in number. Posteriorly the legs become
progressively thinner and longer. Pretarsi very
thin (compressed side-to-side), distally strongly
curved and apically sharply pointed; anterior
accessory claw very long, at least three-fourths
as long as claw proper, posterior accessory claw
conspicuously shorter than the anterior, both
accessory claws robust and pointed. STERNITES
(Fig. 2). Porefields absent on the first but pres-
ent on pedal sternites 2 through penultimate;
last two porefields minute, each consisting of a
few pores; porefields all undivided, those of
anterior body third subelliptical to subtriangu-
lar, becoming wider side-to-side and developing
rather pointed lateral ends, on posterior body
WASHINGTON ACADEMY
OF SCIENCES VOL. 49, No. 9
third becoming rounder and smaller. Ventro-
pleural subcoxal sclerites without porefields.
Sternites of anterior one-third to one-half of
body each with a very shallow transverse de-
pression.
ULTIMATE PEDAL SEGMENT (Figs. 9, 13). Pre-
tergite concealing anterior portion of coxapleu-
ron; broadly fused with its pleurites, laterally
not suturate. Tergite much broader at midlength
than long; sides essentially straight and strongly
convergent posteriorly; rear margin truncate.
Presternite distinctly suleate medially. Sternite
width at midlength about equal to greatest ex-
posed length; sides essentially straight, rear
margin broadly evenly excavate; whole surface
considerably swollen; rather densely clothed
with short stiff setae, especially posteriorly, as
shown. Coxopleuron as seen above exposed pos-
terolaterally; the whole structure slightly swol-
len; posterior ventral half densely setose, the
anterior lateral and dorsal parts with many
fewer setae; each coxopleuron with 2 large ven-
tral, concealed glandular pits, each pit with a
large concealed exit and internally with numerous
inclusive canals and glands (heterogenous type).
Ultimate leg with 6 articles distal to coxopleuron ;
tarsus biarticulate, the articles thin and long; pre-
tarsus either absent or so intimately fused with
tarsus as to be indistinguishable; femur and tibia
slightly flattened dorsally and moderately swol-
len ventrally; all articles dorsally with moder-
ate vestiture but trochanter, prefemur, femur
and tibia ventrally very densely finely setose,
setae of tarsi long and less numerous.
POSTPEDAL SEGMENTS (Fig. 9). Gonopods uni-
articulate, flat, wide, medially contiguous. Ter-
minal pores absent.
Allotype :—male. See collection data for holo-
type. The male allotype agrees closely with the
holotype but differs significantly as follows.
Fies. 1-14.—Holotype (HT) and paratype (PT) of halirrhytus and holotype (HT) of americanus: 1,
halirrhytus (HT): mandible. 2, halirrhytus (HT): sixth pedal sternite. All setae shown. 3, halir-
rhytus (AT): representative pretarsus from anterior third of body. 4, americanus (HT): representa-
tive pretarsus from anterior third of body. 5, americanus (HT): central portion of labrum. Ventral
aspect. 6, halirrhytus (HT): left claw of second maxillae. 7, halirrhytus (HT): central portion of
labrum. Ventral aspect. 8, hallirrhytus (PT): left half of labrum. Ventral aspect. 9, halirrhytus (HT):
ultimate pedal segment and postpedal segments. Ventral. Setae shown only on right presternite, sternite,
postpedal segments, and femur. Hidden glands and gland pits shown in dashed lines. 10, halirrhytus
(HT): first and second maxillae with postmaxillary sclerite and adjacent cephalic plate; left side. All
setae of maxillae shown. 11, halirrhytus (HT): right prehensor and right side of prosternum; ventral
aspect. Setae deleted. Poison calyx and poison gland outlined in dashes within prehensor. 12, halir-
rhytus (HT): cephalic, prebasal, and basal plates. Cephalic paramedian sulci shown in stipples. Setae
14, halir-
and antennae deleted. 13, halirrhytus (HT): tip of second tarsal article of ultimate leg.
rhytus (HT): left pleural region of tenth pedal segment. All setae shown.
Oct.—Nov. 1959 CRABILL: A NEW FLORIDAN PECTINIUNGUIS 329
a
ie
Oy"
|
ay)
12
Fies. 1-14.—(See opposite page for legend).
JOURNAL OF THE
Length, 49 mm. Pedal segments, 55. Clypeus:
midelypeal setae 9 + 10; posterior geminate
setae absent. Labrum: medial are wider, with
S-9 nodular undulate teeth, the interdental fis-
sures between some absent, between others very
vague, the suture separating the central arc
from clypeus proportionately longer; lateral
teeth about 5 on each side. Ultimate pedal seg-
ment: all leg articles conspicuously swollen ven-
trally and laterally, the prefemur, femur and
tibia markedly flattened dorsally; all articles
very densely finely clothed ventrally with stiff
setae. Postpedal segments: gonopods biarticu-
lare, long, projecting well beyond rear of body,
basally widely separated.
The following paratypes differ from the holo-
type in the significant characters cited:
Paratype A: female. See collection data for
holotype. Length, 62 mm. Pedal segments, 57.
Prebasal plate very broadly exposed. Midelypeal
setae right 12, left 7; posterior geminate setae
present, minute. Labrum: central are with 7-9
blunt, low broad teeth, these sharply separated
from each other by deep, narrow interdental fis-
sures; each lateral part with 8-10 broad, weakly
pointed teeth. Mandibular dentate blocks 3, den-
tition 2-3-3.
Paratype B: male. See collection data for
holotype. Length, 52 mm. Pedal segments, 57.
Prebasal plate very narrowly exposed. Mid-
elypeal setae right 7, left 7; only one minute
posterior geminate seta present. Labrum: central
are with 8-10 blunt low teeth, these with short,
narrow but distinct interdental fissures; each
lateral labral part with about 8 teeth, some with
long apical points, some lacking them. Man-
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 9
dibular dentate blocks 3, dentition 3-3-3. Coxo-
pleural pits fully exposed, not concealed.
Paratype C: female. See collection data for
holotype. Length, 42 mm. Pedal segments, 55.
Prebasal plate very narrowly exposed, nearly
concealed. Milclypeal setae 9 + 9; only one
posterior geminate seta present and this seems
vestigial. Labrum: 8 teeth on central are, these
with shallow interdental fissures, blunt, low,
broad; lateral teeth about 7 on each side. Man-
dibular dentate blocks, 3, dentition 2-3-3 (left),
3-3-3 (right).
Paratype D:—female. Florida: Monroe
County, Flamingo; May 3, 1958; R. S. Swanson
and C. F. Dowling, leg. Length, 64 mm. Pedal
segments, 57. Prebasal plate well exposed. Mid-
clypeal setae right 11, left 9: with two minute
posterior geminate setae. Labrum: central are
with 4-5 blunt broad teeth, the interdental fis-
sures very shallow or else absent (Fig. 8); lat-
eral teeth strongly pointed, 9-10 on each side.
Mandibular dentate blocks 3, dentition 2-3-3.
REFERENCES
AtteMs, C. graf. Das Tierreich, Lief. 52: 1-388.
1929.
Botiman, C. H. Proc. U.S. Nat. Mus. 12: 211-216.
1889.
BrRoFLEMANN, H., and Risaut, H. Bull. Soc. Ent.
France no. 8: 191-193. 1911.
Ibid- no. 10; 219-322 19
. Nouv. Arch. Mus. Hist. Nat. Paris (5)4:
53-183. 1912.
CHAMBERLIN, R. V. Proc. California Acad. Sci.
12(18) : 389-407. 1923.
Cook, O. F. Proc. Ent. Soc. Washington 14(3) : 303-
312. 1899.
Coox, O. F., and Cotiins, G. N. Proc. US. Nat.
Mus. 13: 383-396. 1891.
The beliefs which we have most warrant for, have no safeguard to rest on,
but a standing invitation to the whole world to prove them unfounded. If the
challenge is not accepted, or is accepted and the attempt fails, we are far
enough from certainty still; but we have done the best that the existing state
of human reason admits of; we have neglected nothing that could give the
truth the chance of reaching us: if the lists are kept open, we may hope that
if there be a better truth, it will be found when the human mind is capable of
receiving it; and in the meantime we may rely on having attained such ap-
proach to truth, as is possible in our day. This is the amount of certainty at-
tainable by a fallible being, and this is the sole way of attaining it.—JOoHN
STUART MIL.
Oct.-Nov. 1959
NOTES AND NEWS
dol
R. E. SNODGRASS HONORED
The Smithsonian Institution has recently pub-
lished a volume, Studies in invertebrate mor-
phology, m honor of Dr. Robert Evans Snod-
grass, one of the world’s leading insect
morphologists, on the occasion of his 84th birth-
day, which occurred last July 5. Longtime en-
tomologist of the Bureau of Entomology of the
U.S. Department of Agriculture, Dr. Snodgrass
officially retired in 1945, but he has continued
his scientific work at the U.S. National Museum,
holding the position of honorary collaborator of
the Smithsonian. He has been active in the sci-
entific life of Washington for more than half a
century and was one of the prominent contribu-
tors to this JourNaAL’s predecessor, the Pro-
ceedings of the Washington Academy of Sci-
ences.
The Festschrift just published contains a bio-
graphical account of Dr. Snodgrass written by
Dr. Ernestine B. Thurman, who also compiled
his bibliography, covering the years from 1896
to 1958. These are followed by contributions
from 17 of the some of world’s most eminent
scholars in the field of invertebrate morphology.
One outstanding chapter in the series, for ex-
ample, is by Prof. C. 8. Carbonell, of the Uni-
versidad de la Republica, Uruguay, who de-
scribes the anatomy of the South American
grasshopper Marella remipes. This strange in-
sect, at least from an evolutionary viewpoint, in
the process of changing from a land to a water
animal. It has acquired, chiefly through changes
in body structure, ability to swim easily both on
or under the surfaces of ponds and stagnant
streams. It passes considerable time totally sub-
merged among aquatic plants, to whose stems it
clings to avoid floating back to the surface. Its
eggs are laid under water, where they adhere to
the under surfaces of floating leaves. Thus far
specimens of this water grasshopper have been
found in Argentina, Uruguay, eastern Peru,
British Guiana, and Surinam, and it probably
is actually much more widely distributed but
ordinarily would not attract notice. It is nor-
mally an air-breathing creature which lives on
the floating leaves of water lilies. It eats these
leaves from the flat surfaces—never from the
edges as would be characteristic of most grass-
hoppers. The peculiar aspect of the partially
eaten leaves is so characteristic as to betray the
presence of the insects before they actually can
be seen, Dr. Carbonell says. From an anatomical
viewpoint, he says, the creatures show notable
adaptations to locomotion in water, especially in
the structure of the hind legs which are “oar-
shaped.” Other changes from the conventional
grasshopper form are less striking, but all are in
the direction of adaptation to aquatic life.
oo
Another noteworthy contributor to the Snod-
grass volume is Dr. K. D. Roeder, of Tufts Uni-
versity. His thesis is that insects can not afford
to “learn,” that there is not room in their bodies
for the spare nerve cells that apparently are
essential for learning—that is, modification of
behavior due to individual experience. Hence
their quite limited nervous systems are con-
structed for extremely rapid, quite stereotyped
innate responses to avoid predators or to capture
their own prey. Admittedly, Dr. Roeder says,
there is little understanding of the neurological
basis for the process known as learning in higher
animals. It is generally believed, however, that it
involves the capacity for a very great number
of combinations, or interactions, between neu-
rons, the basic units of the central nervous sys-
tem. The number of such interactions which is
theoretically possible must depend to a great
extent on the actual number of nerve units
which are available. There must be a very great
number of these in organisms with a high learn-
ing capacity.
The insect, however, apparently has no neu-
rons to spare. It must depend on an all-or-none
response to a stimulus. Dr. Roeder compares it
with the ringing of an alarm bell in a fire station.
The firemen do not know whether it is a big fire
or a little fire. They spring to action at once.
Their behavior is modified later, of course, by
the kind of fire—a blaze in a trash barrel or the
conflagration of a city block. They have
“learned” from experience.
Notable in the insect anatomy are giant nerve
fibers—considerably larger than any individual
fibers found in mammals or birds—leading from
the outside of the body to the brain. Such an
“axon” can transmit only one impulse at a time.
In higher animals a nerve transmitting “wire”
is made up of many much finer fibers, each of
which can carry its own message. But the insect
does not need a lot of description of the cause of
its alarm. It does not need to know color, shape,
size, odor, ete. It is recognized, says Dr. Roeder,
that a single large fiber transmits a nerve im-
pulse more rapidly than a bunch of fibers. In the
insect nervous system abundance of information
has been sacrificed for speed of response. The
response itself is built into the nervous system
OL JOURNAL OF THE
of the particular insect race, presumably the re-
sult of millions of generations of evolution. It 1s,
by and large, invariable after the nerve impulse
is received. The insect need not think what to do.
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 9
This would take time, measured in thousandths
of seconds. This the insect cannot afford, for in
its world the difference of a millisecond may be
the difference between destruction and survival.
SS
KATMAI AREA DESCRIBED
Nearly half a century ago a large Alaskan
valley was covered completely with the debris
and hot ashes of one of history’s greatest volcanic
eruptions. All vestiges of life were consumed by
fire. At the most, a bare trace of vegetation in
a few sheltered spots may have survived. Thus
was created an area believed quite comparable
to the ancient surface of the earth before the
most primitive forms of plant life first appeared.
Plants presumably constituted the base from
which has been built through a billion or more
years the great pyramid of terrestrial life. The
steaming, smoking, lifeless valley offered sci-
entists an opportunity to observe firsthand an
obviously telescoped re-enactment of the funda-
mental phenomenon of replacement of life on
the planet. The area was the Valley of Ten
Thousand Smokes, now part of the Katmai
National Monument in southwestern Alaska.
The progress through half a century is re-
corded in a report recently published by the
Smithsonian Institution of a systematic biologi-
cal survey of the region by Victor H. Cahalane,
former chief biologist of the National Park Serv-
ice, and now Assistant Director of the New York
State Museum. It results from a survey of the
Katmai area by the National Park Service,
starting six years ago and financed largely by
the Office of Naval Research. One of the im-
portant objectives of the survey was to gather
data on useful or poisonous plants, dangerous
animals, and other information that might serve
military needs from the survival aspect.
The first surveys, started about five years
after the voleanic eruption, were carried on by
a series of National Geographic Society expedi-
tions. It was found that in this relatively brief
period life had started to reassert itself amid
the smoking desolation. The National Geo-
graphic Society explorers found in favorable
spots patches of the quite primitive form of
mosses known as liverworts. Through successive
expeditions up to about 20 vears ago these liver-
worts and a few other quite primitive plant
forms expanded luxuriantly as the ashes cooled.
For the next two decades the progress was
not followed by scientific observers. Mr. Caha-
lane and his associates resumed where the former
explorers had concluded their work. They found,
according to the Smithsonian report, that the
ancient mosses had almost completely disap-
peared. The gradual cooling of the soil pre-
sumably had produced a condition unfavorable
for their survival. But higher plants, including
some flowering species, have gained a precarious
foothold. Altogether 35 species were collected,
including several grasses, dwarf willows, and the
lovely Arctic poppy and dwarf fireweed. Most
of these, according to the report, apparently are
holding their own. From year to year conditions
presumably will become more favorable for
them.
In most cases, it 1s likely, seeds were blown in
from outside the area. The investigator, however,
found several “plant islands.” These are in areas
that presumably were slightly protected from
the fall of hot ashes and may be survivals of the
original vegetation of the region, concerning
which nothing is known.
Henceforth the re-vegetation of the valley
will be followed from year to year. Plots, each
with its own limited plant growth, have been
staked out and will afford bases for observing
the development under the varying conditions
which now obtain.
The animal life present before the eruptions
was unable to survive them, but since then the
area has been increasingly re-invaded by the
same species from nearby areas. In due time it
may be expected to show once more a faunal pic-
ture more or less like the original one. So far as
human beings were concerned, the report says,
there could have been at the most only a few
scattered Eskimo villages farther away, the in-
habitants of which had sufficient warning of the
coming catastrophe so that they were able to
escape.
Officers of the Washington Academy of Sciences
JS oIS hic) 42, 19 FraNK L. CAMPBELL, National Research Council
Pyestdent-clect:............... LawRENCE A. Woop, National Bureau of Standards
ES ET O0 ee Heinz Specut, National Institutes of Health
. PISS. 65000 eee W. G. BrompBacHer, National Bureau of Standards
PERCIEDESE....2.-..--..- Morris C. Lerxkinp, Armed Forces Institute of Pathology
Gusmaran of Publications............... Haratp A. REHDER, U.S. National Museum
Sacto.) CHESTER H. Paces, National Bureau of Standards
22RD S 0D La) ae ee H. A. Bortuwick, T. D. Stewart
Weeeweers to 196! ... «2... ee eee Bourpon F. Scripner, Keita C. JoHNSON
WIERD NICS... ee we ee Puitip H. ABELSON, Howarp S. RapPpLlEYE
Board of Managers....All the above officers plus the vice-presidents representing the
affiliated societies
CHAIRMEN OF COMMITTEES
Standing Committees
LUE . FRANK L. CAMPBELL, National Research Council
LSE ES. 0 5 RatpH B. KENNARD, American University
Membership............ LAwrRENCE M. KusHner, National Bureau of Standards
DiMEEADHS..........:....... Dean B. Cowig, Carnegie Institution of Washington
Awards for Scientific Achievement....... FRANK A. BIBERSTEIN, Catholic University
Grants-in-aid for Research...... B. D. Van Evera, George Washington University
Poucy and Planning.............. MarGaret Pitrman, National Institutes of Health
Encouragement of Science Talent.............. Leo ScHusEerT, American University
Science Education............ RayYMonp J. SEEGER, National Science Foundation
Ways and Means.............. RussELL B. Stevens, George Washington University
Pele ETGlAtIONS... 0.2... 2.05. ce eee eee JouN K. Taytor, National Bureau of Standards
Special Committees
LOGOS =: 9: Oe Haroutp H. SHEeparpD, U. 8. Department of Agriculture
MMECCUOLY.-=............ JAMES I. HamsBieton, U.S. Department of Agriculture (Ret.)
Pibenry at Congress.................... Joun A. O’Kerere, National Aeronautics and
Space Administration
CONTENTS
Page
EpucatTion.—Education for the Age of Technology. 8S. B. Incram.... 293
GroLtocy.—The Wolfcamp Series (Permian) and new species of fusu-
linids, Glass Mountains, Texas. CHARLES A. Ross.............. 299
PLANT PatHoLtocy.—Responses of certain fungi, particularly T77-
Ehoderma sp., to light. Ipa P. BJORNSSON....~ .- 22. . 7:2 317
ZooLocy.—A new Floridan Pectiniunguis, with re-appraisal of its type
species and comments on the status of Adenoschendyla and Lito-
schendyla (Chilopoda: Geophilomorpha: Schendylidae). R. E.
CRABID, IR. Secu a. Sago tied ot s+ So eee geal 324
NotTEs AND NEws:
hy. Hi: Snodgrass ‘honored: . .. . Fa... eee ae os se Se
Katmai area described. .........2... Sapo ee 332
VOLUME 49 December 1959 NUMBER 10
me. 72
Bia W/2 2
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JOURNAL
OF THE
WASHINGTON ACADEMY OF SCIENCES
Vou. 49
DECEMBER 1959
No. 10
ASTRONOMY —Cepheid variables and the period-luminosity relation.! C. PAYNE-
GAPOSCHKIN, Harvard College Observatory. (Communicated by Charles M.
Herzfeld.)
The period-luminosity relation has al-
most reached its fiftieth anniversary. To-
day it is being studied more actively than
ever, and its observed complexities and
theoretical implications are still far from
exhausted. In fact I hope to show that what
we know and understand at present about
the period-luminosity relation is far less
than what remains to be discovered and
interpreted.
Introduction.—The diagram derived by
Miss Leavitt (1)? from 25 Magellanic Ceph-
eids, reproduced in Fig. 1, already shows
several of the features of current interest:
the linear relationship between the apparent
magnitude and the logarithm of the period,
the seatter of the points about the curve,
and the variety of amplitudes. Each, as I
shall describe, has been verified and ampli-
fied by later work.
The earlier work of Bailey (2) on the
variable stars in globular clusters laid the
foundation for the recognition of an equally
striking relationship between period and ap-
parent brightness within any one globular
cluster. Although the variables with periods
shorter than a day showed no marked cor-
relation between period and brightness, the
few with longer periods were always
brighter. On the simple assumption that all
the short-period variables were of similar
luminosity, Shapley (3) constructed a pe-
riod-luminosity curve from the data for all
globular clusters that contained variables
with periods longer than a day, and con-
*The 28th Joseph Henry Lecture of the Philo-
sophical Society of Washington, delivered before
the Society on May 22, 1959.
* Italic numbers in parentheses refer to the Bib-
hography, pp. 349-350.
309
cluded that it had the same slope as the
relation for the Magellanic Cepheids.
If the identity of the two period-lumi-
nosity relationships is granted, the con-
version from apparent to absolute magni-
tude can be effected by the establishment of
absolute magnitude for some one contribu-
tor to the curve. The short-period variables
in globular clusters were identified with
the RR Lyrae stars of the galactic field,
many of which have periods and light
curves exactly like those of the cluster vari-
ables. Accordingly the absolute magnitudes
of the RR Lyrae stars were intensively
studied, and the generally accepted value
0.0 was used to fix the zero point of the
period-absolute magnitude relation.
The immediate application of this con-
clusion by Shapley led to his epoch-making
study of the dimensions of the galaxy. Later
revisions of this work have resulted from
improvements in the scale of apparent mag-
nitudes and from corrections for obscura-
tion, not from revisions in the zero point of
the absolute magnitudes.
The upper part of the period-luminosity
curve was used to derive the distances of
the Magellanic Clouds, and when Hubble
(4) discovered Cepheids in NGC 6822,
Messier 33, and Messier 31, the distances
of these galaxies were similarly derived.
These applications of the period-luminosity
curve depended on the original working as-
sumption that the relationships among the
stars in globular clusters and those in the
Magellanic Clouds and other galaxies were
not only parallel but identical. That this
assumption is not justified was shown by
Baade (5) in his study of the Andromeda
galaxy. The zero point of the period-lumi-
ITHSONIAN : |
SNSTiTUTION SAN 1°8 1960
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 10
d
Ei
ng
Fic. 1—Miss Leavitt’s period-luminosity relation (maximum photographic magnitude above, min-
imum below). Left: period plotted against magnitude; right, logarithm of period plotted against mag-
nitude. From Harvard Circular 173. 1912.
nosity curve for classical Cepheids was thus
revised upward by about 1.5 magnitudes,
and all distances derived by the use of the
upper part of the curve were accordingly
also revised upward.
Within any one globular cluster there is
very little correlation between the apparent
magnitude and period of the RR Lyrae
stars, but the photographic (though not the
photovisual) magnitude has been shown for
example by Roberts and Sandage (6) to be
slightly brighter for the variables of shortest
period in Messier 3. That the absolute mag-
nitudes of RR Lyrae stars may differ
slightly in different globular clusters is sug-
gested by Sandage (7) and the possibility
that the accepted absolute magnitude of
RR Lyrae stars may require downward re-
vision is discussed by Arp (8).
The period-luminosity relations for vari-
ables in globular clusters and for Cepheid
variables have been convincing separated
by the work that has been briefly sketched
in the preceding paragraphs. Another
equally striking correlation that might well
have pointed in the same direction many
years ago is the Hertzsprung relationship
between the periods and the forms of the
light curves (9). The classical Cepheids
of the galaxy show a progression in the
form of a light curve (10), such that stars
of the shortest periods show a smooth rise
and fall, at longer periods (about 5 days) a
hump appears on the declining side, and
becomes more pronounced up to periods be-
tween 8 and 9 days. Between 9 and 10 days
the curves abruptly become more symmetri-
eal, with a more or less well-marked hump
between two shoulders, and generally small
amplitude. At rather longer periods the
light curve has a more abrupt and asym-
metrical rise, with a small hump just pre-
ceding the main brightening, and at the
longest periods the curve is again found to
be smooth and uncomplicated. The light
curve thus runs through one complete cycle
of changes between the shortest and long-
est periods. Cepheids in the Magellanic
Clouds also display the Hertzsprung rela-
tionship (11).
An analogous relationship between period
and light curve is shown by the short-
period variable stars in globular clusters:
in any one cluster, the stars of shortest pe-
riod have light curves that are almost sine
curves, and there is a rather abrupt transi-
tion at some longer period (not the same
in all clusters) to a highly asymmetrical
light curve, usually with a small hump be-
fore the main rise. Stars of the longest pe-
riods (less than a day) have less asym-
metrical light curves. This relationship was
DECEMBER 1959
pointed out by Bailey, who designated the
curves by the letters c, a, b, in order of in-
creasing period.
The Hertzsprung relationship for galactic
classical Cepheids and RR Lyrae stars is
illustrated in Fig. 2.
PAYNE-GAPOSCHKIN:
CEPHEID VARIABLES Odo
The globular cluster stars with periods
over a day do not conform to the Hertz-
sprung relationship; those with periods be-
tween 10 and 20 days show a broad maxi-
mum or a hump on the downward slope
(12). A few galactic variable stars of simi-
Fig. 2—The Hertzsprung relationship: means for Classical Cepheids (left); means for galactic RR
Lyrae stars (right).
From Harvard Annals, 113. 1954.
336
lar period, which differ from classical Ceph-
eids in lying far from the galactic plane,
in motion, and in other ways, show similar
light curves. In particular, a group of Ceph-
eids associated with the galactic center
shows a period-light curve pattern similar
to that of the stars in globular clusters (13).
These galactic variable stars are clearly to
be associated, like those in globular clusters
(14), with Population II, whereas the classi-
cal Cepheids are members of Population I
(15);
The period - luminosity relationship.—
Miss Leavitt’s period-luminosity relation-
ship showed considerable scatter about the
mean curve, and all later studies of the
variables in a single system (the Magellanic
Clouds, Messier 31, and so forth) also show
a dispersion. As the periods are determined
with adequate accuracy, it is usual to con-
sider whether the observed dispersion can
be a result of factors that have affected the
magnitudes. Shapley (16) enumerated pos-
sible contributors: errors of the magnitudes,
effects of unresolved doubles, effects of gen-
eral background brightening, obscuration
within the system, galactic obscuration,
Eberhard effect. Erroneous periods would
produce the same effect, but their contribu-
tion is certainly negligible.
In the early days of the application of the
period-luminosity relation, there was a
tendency to assume that a great part of
the dispersion was due to observational
causes and that the stars actually lay very
close to the curve. Recent work by Arp
(17) on the Small Magellanic Cloud leads
him to the conclusion that most Cepheids
lie within a range of one magnitude at any
one period, which implies that most of the
observed dispersion is intrinsic. Sandage
(18) contemplates the even larger range of
1.2 magnitudes at a given period.
Hitherto I have spoken in terms of ob-
served quantities only. Further progress
cannot be made without some very ele-
mentary theoretical assumptions: first, that
the relationship P-/p = C is accurately ful-
filled; second, that Cepheids conform to the
mass-luminosity relationship. Granted these
premises, then if there is a dispersion in
magnitude at a given period, three con-
clusions follow:
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 10
1. At a given period there is:
(a) a dispersion in color, the bluest stars be-
ing of highest luminosity
(b) a dispersion in luminosity, the brightest
stars being the bluest
2. At a given luminosity, there is:
(a) a dispersion in period, stars of longest
period being the reddest
(b) a dispersion in color, the reddest stars
being of longest period
3. At a given color, there is:
(a) a dispersion in period, stars of longest
period being brightest
(b) a dispersion in luminosity, the brightest
stars being of longest period
These three conclusions are shown graphi-
cally in Figs. 3, 4, and 5, which have been
drawn for a range of magnitude of 1.0 at a
given period, and for a range of color of 0.2
at a given magnitude.
The relation between mean color and ab-
solute magnitude is not implicit in the as-
sumptions, but can be shown to be plausible.
The existence of a mean period-spectrum
relation for Cepheids has long been recog-
nized, and the data given by Code (19) de-
fine it accurately. If all Cepheids were of
the same color, they would all have the
same surface temperature. But the more
luminous Cepheids would then have some-
what earlier spectral classes cn account of
lower surface gravity. Since the opposite is
observed, we can infer that bright Cepheids
are somewhat redder than fainter Cepheids
and that the difference of color between two
Cepheids is greater than the difference
found between two stars of comparable
luminosities and identical spectral class.
Data on the accurate colors of Cepheids
in other galaxies are needed, both to test
the qualitative statements just made and to
provide quantitative material from which
consistent period-magnitude-color arrays
may be constructed. However, the effect of
obscuration also enters into such colors, and
even if all Cepheids in a system were of the
same true color at a given period, obscura-
tion and extinction would conspire to make
the most reddened stars the faintest. The
size of the effect in our own system may be
judged from the diagram of maximal color
index against logarithm of period repro-
duced by Walraven, Muller and Oosterhoff
(20). The diagram contains a few points
for the two Magellanic Clouds, from meas-
ures by Gascoigne; these, and the few colors
DECEMBER 1959
M log P
ne
0
PAYNE-GAPOSCHKIN: CEPHEID VARIABLES
B30
Fig. 3.—Relation between period and absolute magnitude (schematic); light lines show equal col-
ors; broken lines separate the domains of different curve types. The arrow shows the possible course of
Cepheid development.
0.2
Fic. 4—Relation between period and color (schematic). Light lines show equal absolute mag-
nitudes; broken lines separate the domains of the different curve types. Arrows show the possible
course of Cepheid development.
published or discussed by Gascoigne and
Kron (21), Gascoigne (22), and Gascoigne
and Eggen (23) are not inconsistent with
the view here expressed. Gascoigne and
Eggen act on the belief that the evidence
for identity in color between galactic and
Magellanic Cepheids, though not conclusive,
is encouraging. Opinion has long been di-
vided on this matter, and I will state my
own view—that the colors of the galactic
and the Magellanic Cepheids are essentially
similar, and that the dispersion of color is
as decribed above in simplified terms.
The Hertzsprung relationship.—The rela-
tion between the period, luminosity, and
light curve of a Cepheid must next be con-
JOURNAL OF
THE
Fic. 5—Relation between color and absolute
magnitude (schematic). Light lines show equal pe-
riods; broken lines separate the domains of the
different curve types. The arrow shows the possi-
ble course of Cepheid development.
sidered. The fact that averaged hght curves
for several stars with a small range of
period display the Hertzsprung relation
shows clearly that form of light curve is
closely related to period. If the period-
luminosity curve has a dispersion, then, 1f
stars of a given period should have identical
light curves, stars of a given absolute mag-
nitude should have light curves that differ
systematically with period.
The Cepheids in the Small Magellanic
Cloud furnish information on this point. In
order to present the data something must
be said about the classification of hght
curves. The Bailey types a and ec for the
variables in globular clusters are excellent
criteria, unambiguous and mutually ex-
clusive. Type b, however, grades into type
a and today is usually combined with it. In
the classification of light curves, as in other
matters (period frequencies, absolute lumi-
nosities of RR Lyrae stars) a globular
cluster appears, so to speak, to lack a di-
mension in comparison to a system like the
Small Cloud. This dimension is very likely
mass: stars on the horizontal branch of a
globular cluster must all be of almost the
same mass. The Cepheids in a large system
WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 10
also differ in the time dimension. Methods
of analysis and classification that give
clear-cut results for globular clusters will
not necessarily do so when applied to more
complex groups. This statement, obvious in
regard to color-magnitude arrays, is no less
true of the classification of light curves.
Methods that suffice for RR Lyrae stars
are not flexible enough for Cepheids.
The first photoelectric light curves of
Cepheids confirmed the variety and com-
plexity of the hght curves and color changes.
Eggen (24) first defined groups A, B, C to
represent the hght curves, on the basis of
relationships between period and amplitudes
of light and color. Whether or not is was
intended, the names suggested a parallel
with the Bailey types, which has no physi-
cal justification. In a later paper, the defini-
tions for types A, B, and C have been modi-
fied: a star is of type C if the light curve is
symmetrical (M — m = 0.37 P), of type B
if a hump is present, of type A if no hump
is observed (25).
To me it has always seemed that the
Hertzsprung relationship is fundamental in
describing the light curves of Cepheids, and
that three classes are not enough to cover
its complexities. My own classes have been
defined as follows (26)
u: smooth, asymmetrical (6 Cephei)
v: smooth rise, hump on decline (yj Aquilae)
w: saddle-shaped curve (S X Velorum)
x: central peak, shoulder on each side (Z La-
certae )
y: sharp rise, preceded by small rise (S Z
Aquilae)
z: smooth, asymmetrical (U Carinae)
: sine curve (G H Carinae)
Eggen’s type C covers types s and x, his
B covers v and w, and his A covers u, y,
and 2.
The period-luminosity curve for minimal
photographic brightness in the Small Mag-
ellanic Cloud is shown in Fig. 6, which em-
bodies a great deal of unpublished material
kindly made available by Dr. Shapley, for
over 600 stars. The magnitudes are on the
uncorrected Harvard scale; Arp’s photo-
electric work has shown that the range of
magnitudes should be increased.
The points corresponding to stars with
different curve types have been plotted with
distinctive symbols, and I have indicated by
O39
PAYNE-GAPOSCHKIN: CEPHEID VARIABLES
DECEMBER 1959
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340
broken lines the approximate domains oc-
cupied by hght curves of different types.
An earlier diagram of the same kind (26)
made with about a hundred stars from both
clouds shows the effect more clearly. This
is in part because the light curves were
better determined, in part because the stars
were selected for freedom from obvious
obscuration. The reality of the dependence
of curve type on luminosity as well as on
period was verified by means of the x? test.
Points for curve type u could not be in-
eluded in the discussion on account of in-
completeness at faint magnitudes.
A feature of Fig. 6 that does not run
parallel to the other curve types is the
group of symmetrical curves for stars of
short period. These small-range curves seem
to follow a period-luminosity spread par-
allel to the main one, and overlapping it
slightly. These stars are of such interest
that they must be examined critically to
see whether their small range, and compara-
tively high luminosity for their period, could
result from the presence of unresolved com-
panions. They seem to be too numerous for
this to be a likely interpretation. Moreover,
they have counterparts in our galaxy (GH
Carinae, FF Aquilae, DT Cyegni).
Cepheids of similar curve type, there-
fore, are not aligned precisely with Cephe-
ids of similar period. In Figs. 3, 4, and 5,
the domains of similar curve type are sepa-
rated vy broken lines. These domains cut
lines of equal period (mean density), equal
luminosity, and equal color, at various
angles, so curve type is not primarily de-
termined by any of these properties of the
star.
Development of RR Lyrae stars—The
place of the RR Lyrae stars in stellar de-
velopment has been deduced from their
well-defined position in the H-R diagrams
of globular clusters. They are evidently
members of the horizontal branch; the con-
tinuity of star counts through the variable
star domain, in variable-rich clusters, sug-
gest that they move along the horizontal
branch (27). The correlation of period and
color found in Messier 3 by Roberts and
Sandage implies that an RR Lyrae star
changes its period as it crosses the gap, and
makes an abrupt transition to or from
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 10
“overtone” pulsation as it crosses the inter-
face between the type a and c¢ curves.
Changes of period are not (and are unlikely
to be) large enough to indicate which way
the RR Lyrae star travels in the H-R plane
although one can infer that many writers
think in terms of progress from long to
short period, from fundamental to over-
tone, from right to left in the HR plane.
If the method of mapping empirical evo-
lutionary tracks employed by Sandage (28)
is valid, the distribution of stars along the
horizontal branch might give a clue to the
rate at which a star crosses the variable
gap, or at least the relative rate at which
different parts of the path are traversed.
As Arp (29) has pointed out, a strongly
populated horizontal branch goes with a
large variable star population, but there
are variable-poor clusters such as Messier
2 in which only one side of the variable star
gap 1s well populated. Within the gap itself,
however, the variable stars are not distrib-
uted uniformly with period. In » Centauri,
for example, numbers of stars within equal
limits of log P are as follows:
0.4to 0.5 to 0.6to 0.7 to 0.8to 0.9 to
log P 0.5 0.6 0.7 0.8 0.9 1.0
Number of stars 6 Bill 15 38 25 10
These numbers do not change uniformly, as
might be expected for steady progress across
the gap; rather they suggest acceleration-
deceleration-acceleration as the gap is
crossed. For classical Cepheids the situa-
tion is even more complex. In any one
globular cluster there is a very small dis-
persion of absolute magnitude at any one
period, but in a large stellar system such as
the Magellanic Clouds and Messier 31, the
dispersion in magnitude at one period adds
at least one dimension to the problem.
Development of Cepheids—It has long
been recognized that the Cepheid variables
lie within the Hertzsprung gap in the HR
plane. Although the true colors of galactic
Cepheids, and their dispersion, are ex-
tremely difficult to determine, as has al-
ready been mentioned, it seems very likely
that all Cepheids with a given luminosity
lie within a restricted range of color (about
0.2 magnitude), and that no other stars lie
within this range. The Population II Ceph-
elds seem to occupy a similar domain,
DECEMBER 1959
probably somewhat to the blue of the do-
main for classical Cepheids. The situation
as I see it is shown in Fig. 7. The variable
supergiants appear to lie on either side of
the Cepheid domain (30).
The picture has been refined by the dis-
covery of a few Cepheid variables in galac-
tic clusters (31). The well-established mem-
bers are tabulated below.
Light curve
Cluster Cepheid Boucd
econ This
paper
NGC 6664 EV Sct 3.09 C s
NGC 7788 CE Cas a (82) 4.45
CF Cas 4,87 AB u
CE Cas b 183
Messier 25 U Sgr 6.74 AB Vv
NGC 129 DL Cas 8.00 CP s?
NGC 6087 S Nor 9.75 (e x
The suggestion of Bidelman that UX Persei
(oan Une Perse: (5737), VX Persei
(104.90) and SZ Cassiopeiae (134.60) are
members of the Perseus I association should
be mentioned (33). The Burbidges regard
SZ Cassiopeiae as “probably a member of
the cluster.” The apparent magnitudes of
all four stars are correlated with their pe-
riods.
The stars in the table are all as bright as,
or brighter than, the brightest main se-
quence stars in the clusters (34); the four
possible members of the Perseus cluster are
fainter than the bright B stars and M stars
in the Perseus double cluster. These data
suggest that the age of a Cepheid in a ga-
lactic cluster can be determined:
Age of
Age of 2
Star Cluster cluster ees Ref.
years SOAS
EV Sct NGC 6664 2X 108 (33)
CE Cas a
CF Cas NGC 7778
CE Cas b
108 (33)
U Ser Messier 25
DL Cas NGC 129
S Nor NGC 6087
SZ Cas h, x Persei 108 (35)
Perseus I 4 X 106 (36)
The Cepheids in galactic clusters evi-
PAYNE-GAPOSCHKIN:
CEPHEID VARIABLES 341
dently lie within the Hertzsprung gap, and
it is rather clearly indicated that a star be-
comes a Cepheid as it reaches a certain
critical color as it crosses the gap. Analogy
with globular clusters, where nonvariable
stars are found on both side of the gap,
might suggest that it emerges on the other
side of the gap and becomes a red giant,
and at least in NGC 6664 there is clear evi-
dence of red giants (31). If SZ Cassiopeiae
is a member of the Perseus Association, it
again is associated wtih red giants, and ER
Carinae has been suggested as a possible
(though unverified) member of NGC 3582,
which is very rich in red giants. We note
also that the lower limit of the classical
Cepheids is not far from the place (between
NGC 752 and Messier 67) where the Hertz-
sprung gap has narrowed and disappeared.
The general picture is shown in Fig. 8,
which amplifies Sandage’s well-known dia-
gram by the addition of material for the
Orion I association (37) and the Magellanic
Clouds (38).
The three Cepheids in NGC 7778 display
a rather small range of periods and magni-
tudes. The bright “galactic” cluster NGC
1866 in the Large Magellanic Cloud is an
example of a cluster that contains many
Cepheids, most of them in a restricted range
of period (39). The following table gives
the names, periods, and approximate mean
magnitudes; stars within 10’ of the center
of the cluster are marked with asterisks.
HV Period Mean HV Period Mean
d Mpg d Mpg
12206* 2.506 16.1 12194* 3.205 16.0
12208 2.604 16.2 12205* 3.210 15.9
12199* 2.639 16.51 12189 3.246 16.4
12200* 2.725 16.4 12187 3.287 15.8
12209 2.930 16.21 12204* 3.439 15.6
12188 2.9384 16.31 12201* 3.444 15.8
12211 2.940 16.21 12193 3.465 16.3
12203* 2.954 16.4 12198* 3.523 16.2
12202* 3.101 16.2 12207 4.566 15.8
12196* 3.113 16.4 12211 5.083 15.9
12197* 3.144 16.01 12186 12.24 15.0
12195 3.190
Most of the Cepheids in NGC 1866 lie
within the limits 0.40 and 0.55 in log P, and
there is a trend toward brighter magni-
tudes for longer periods. The picture is like
that presented by nearby galactic clusters,
except that NGC 1866 is much richer in
we)
=
bo
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. 10
Long
\ Period
\ Variavles
Maximum
\ Range
Variable ped supergiants
Magellanic Cepheids
Classical Cepheids (mean)
W Virginis stars
Dwarf Cepheids
Beta Canis Majoris Stars
Variable Supergiants
Mf RR Lyrae domain
Oe0e00e0
Fic. 7.—Domains of the several types of variable stars in the color-magnitude array. The original
main sequence is sketched as a light line.
Cepheids. Details of its color-magnitude
array will be of extreme interest. If there is
a detailed analogy with galactic clusters, we
can infer an age comparable with that of
EV Scuti from the average period of the
Cepheids. With the anticipated discovery of
more Cepheids in Magellanic clusters, we
can look forward to verification and exten-
sion of the dating procedure.
Galactic clusters provide suggestive quali-
tative information about the course of de-
velopment of a Cepheid; among other things
they suggest that the Cepheids follow a
route like that of stars of mass over 2.5
suns, and move more or less horizontally
across the HR plane, rather than rising
sharply after leaving the main sequence,
like stars of solar mass and less. This is the
justification for the earlier assumption that
Cepheids conform to the mass-luminosity
relation.
In a globular cluster, there is a strong
correlation between the amplitudes and pe-
riods of the RR Lyrae stars, which we have
mentioned as probably traversing the hori-
zontal branch across the variable gap: as
we go from long to shorter period, the ampli-
tude rises to a maximum, and then falls
abruptly at the transition between curves of
type a and type c. In NGC 1866 we note
that four stars of amplitude 1.2 magnitudes
and more lie between log P = 0.5 and 0.54,
but there are also two stars of large ampli-
tude with log P = 0.41, one of them within
10’ of the center of the cluster. The numbers
of stars within equal limits of log P are:
DECEMBER 1959 PAYNE-GAPOSCHKIN: CEPHEID VARIABLES 343
=—o (0) ah 8 1le2 1.6 2 O
ae 1 i] } | ] | ]
=10)— S52—_ —- 2x10
a r) Fe
a oe 7 ec
B 8 6» o1 e
-8 Bf of PI = & se i
KR
mY © ~ aes
Pee,
6 J a LMC
Nese O 6231 “ee
*e
| &
{00 = ®@4 Pi | - 5x10
= th Na |
| Ee 1o?
Pl ~ M3
\S.
ee “ld | ae
A,
a Ml Mfl1 7
% & - 5x10
ey = p% e ee
> } SS 108
Oa Bor M 67 2% %,
, 2 %
é im 8
a a= § (8)
/be 4 xl
s* 52 Bi Ss Ae
ae 752 f
nee g IiCe Large Magellanic Cloud
O I : Orion I
Fy PI: Perseus I -5x10
+h — 6231: NGC 6231
P II: Perseus II Sw alolTe.
RO Sun Pls: Pleiades
\ H : Hyades
Pr: Praesepe
C3 Coma
+6 — 752: NGC 752
+8 =
Fre. 8.—The Cepheid variable domain as related to the color-luminosity
arrays of galactic clusters and associations.
0.5 to 0.65 0.7 to over 1.0
0.4to 0.45
o 0.5 OSS tol0s7 0e75
log P 0.45 t
Number of stars 4 7 9 1 1 1
Thus the greatest concentration of periods
coincides with a maximum of amplitude.
Here again there is no indication of steady
progress through the gap, but of a slowing-
up in the neighborhood of log P = 0.525.
A single cluster presents a simpler pic-
ture than the Cepheids in a larger system;
its stars may be regarded as having disper-
sion in mass, but do not differ appreciably
in age. It is not surprising that the Small
Cloud displays no simple relation between
period, luminosity and mean amplitude.
Fig. 9 shows a contour map of mean ampli-
tudes in the period-luminosity plane. Small
amplitudes are characteristic of periods be-
tween 8 and 10 days and apparent magni-
tude 15.4 (about absolute magnitude —3.6),
and also of the strip to the short-period
edge of the diagram for apparent magni-
tudes less than 16.0. These latter small
amplitudes correspond to the type s light
curves of Fig. 6. The fact that they are as-
sociated with the shorter periods speaks
against the possibility that they are caused
by unresolved companions, for there is no
reason why unresolved companions should
have a preference for particular periods;
they should be equally common at all
periods for a given apparent magnitude.
Large amplitudes show an even more strik-
ing distribution. They occur, as is well
344 JOURNAL OF THE WASHINGTON
Dots:
Lieht cross-hatching:
Vertical shading:
Horizontal shadine:
Heavy cross-hatching:
ACADEMY OF SCIENCES’ VOL. 49, No. 10
Amplitude
less than 0.7
O5'/ 80) WA
OSS tole!
ileil Yee) ila ss!
over 1.3
Cloud (schematic contour diagram).
known, for the more luminous stars, but
they also occur at the low-luminosity, long-
period edge of the period-luminosity array.
The occurrence of large amplitudes among
the fainter Magellanic Cepheids has been
noted by Arp and is undoubtedly a real
phenomenon.
If the path of any one Cepheid is a hori-
zontal track across the period-luminosity
plane, we might be able to trace the changes
that a star undergoes by examining the
changes in light curve at any one apparent
(and therefore absolute) magnitude with
changing period. Figs. 10, 11, and 12 show
such series of light curves at seven different
apparent magnitudes, and are typical for
the whole available material. At brighter
magnitudes, the light curve shows system-
atic changes and shifts of one prevalent
pattern, which recall the Hertzsprung rela-
tionship, and illustrate the angle at which
light curves of different types cross the
average period-luminosity relation. For
fainter magnitudes, however, the stars of
shortest period tend to have small-ampli-
tude, symmetrical light curves (type s),
which recall the type ¢ light curves for RR
Lyrae stars in globular clusters.
If it is accepted that a Cepheid travels
from left to right in the HR plane, and if
DECEMBER 1959
14,9 to 15.0
2017
11.407
PAYNE-GAPOSCHKIN:
CEPHEID VARIABLES
- Z lacertae
10,886
TT Anuilae
UG Yee:
VY Carinae
18,937
Fig. 10.—Light curves of Cepheids in the Small Magellanic Cloud, mean apparent photographic
magnitude 14.9. Harvard Variable number and period are indicated for each. On the right, for com-
parison, several galactic Cepheids (photoelectric light curves by Eggen, except, for UU Muscae, Har-
vard photographic light curve).
the type s light curves represent overtone
pulsations (as Sandage has suggested for
the very similar Eggen type c¢ curves),
must we suppose that the developing Ceph-
eid proceeds in the direction overtone to
fundamental, short to long period?
With this possibility in mind we can re-
examine the amplitudes of the Magellanic
Cepheids. Instead of drawing a contour dia-
gram of mean amplitudes, we draw contour
diagrams of the frequencies of amplitudes
less than O™.7 and greater than 1™.0 (Fig.
13). The picture is now greatly simplified,
and suggests that the complexities of Fig.
9 are a consequence of two overlapping
distributions. This possibility cannot be
profitably explored further until accurate
photoelectric amplitudes are available.
Finally, let us compare the frequency of
periods of stars in different parts of the
period-luminosity plane. The results de-
rived from over 600 Cepheids in the Small
Cloud are shown as a contour diagram in
Fig. 14. The division into two groups is
very evident. If, again, we suppose that a
Cepheid moves from left to right across the
diagram, then we can infer that its progress
is not uniform.
The rate of development might be ex-
pected to be a function of the mass (ie.,
the luminosity), faster for more luminous
stars. It should also be a function of the
time: for constant mass, log P should in-
crease as 3/2 log R, where R is the star’s
radius. Thus, if the radius increased in
proportion to the time, log P should in-
346
15.4 to 15.5
1402
5 o)G UGS)
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
15.9 to 16.0
VOL. 49, No. 10
pO BEV aaN
1,301
»26.1 to 16.2
Fie. 11.—Light curves of Cepheids in the Small Magellanic Cloud, mean apparent photographic
magnitudes 15.4, 15.9, and 16.1. Arrangement as in Fig. 10.
crease at an accelerated rate, and the great-
est number of Cepheids at any one lumi-
nosity should occur for the shortest periods.
However, it seems probable from analogy
with the earlier development of massive
stars, that Rf itself increases at an acceler-
ated rate with time, so the concentration of
Cepheids at the shortest periods would be
enhanced even more. Fig. 14 is not con-
sistent with these expectations. There are
two maxima of period-frequency for all
stars at and below magnitude 16. A similar
situation has already been noted for the
RR Lyrae stars in » Centauri. The observa-
tions indicate that if a Cepheid moves
across the period-luminosity plane, its de-
velopment slows down in the neighborhood
of two periods, different for each magni-
tude level.
If the two sets of contours refer respec-
tively to the overtone and the fundamental,
however, they also refer to different values
of R at a given period. In this case, in order
to convert Fig. 14 into a contour diagram
representing frequency of mean. density,
we must shift the lower-period distribu-
tion to the right by an appropriate amount.
If the two frequency distributions are thus
combined, we obtain Fig. 15, which strongly
suggests a single distribution, and also
raises the question whether a given star
passes through the Cepheid domain with
overtone pulsation, or fundamental pulsa-
tion, or both successively. Here again we
DECEMBER 1959
16.2 to 16.3
2110
1,763
PAYNE-GAPOSCHKIN: CEPHEID VARIABLES
16.4 to 16.5
1.438
Oo
347
16.6 to 16,7
2197
1769
te 127)
1.630
Fig. 12.—Light curves of Cepheids in the Small Magellanic Cloud, mean apparent photographic
magnitudes 16.2, 16.4, and 16.6. Arrangement as in Fig. 10.
need accurate light curves and colors in
order to clarify the picture. A diagram hke
Fig. 15 might prove to be the most funda-
mental representation of the relation be-
tween luminosity and mean density, and we
note that its slope in the lower part is
greater than that of the period-luminosity
relation.
The question of the rate at which an indi-
vidual Cepheid traverses the HR plane
leads immediately into the wider question
of the significance of the frequency of pe-
riods. The large number of Cepheids of
short period in the Small Cloud, as com-
pared with our own galaxy, has been dis-
cused by Shapley and McKibben (40), who
regard the difference as real. Indeed, it is
difficult to suppose that selection and ob-
scuration could have cut down the numbers
of galactic Cepheids with periods less than
three days by a factor of ten; down to a
given apparent magnitude, the Cepheids of
longer period are at a greater disadvantage.
If all stars that leave the main sequence
and move to the right in the HR diagram
become Cepheids at some stage, we might
(if their progress was uniform or followed
a known law) predict the number of Ceph-
elds per cubic parsec by means of the Sal-
peter “creation function.” However, as we
have argued above, a uniform progression
does not seem to fit the known facts. We
348 JOURNAL OF THE WASHINGTON
ACADEMY OF SCIENCES VOL. 49, No. 10
Fig. 13.—Distributions of amplitudes for Cepheids of average photographic magnitude 16.0 and
fainter in the Small Magellanic Cloud. Left side: ight shading, over 4 stars between limits of 0.1 in log
P and in my, ; heavy shading, over 6 stars. Horizontal shading: amplitude over 1.0; vertical shading:
amplitude less than 0”.7. Right side: light shading: over 6 per cent of Cepheids in given magnitude
interval; heavy shading: over 10 per cent of Cepheids in given magnitude interval. Horizontal and
vertical shading have the same meaning as on the left.
could invert the argument, and, assuming
that Cepheids follow the period-luminosity
law exactly, use the number of observed
Cepheids at each period to calculate the
duration of the Cepheid stage at that period.
This procedure is so uncertain that I shall
not presume to make a numerical applica-
tion of it; it predicts an increasing number
of Cepheids per cubic parsee down to peri-
ods of about a day, since all stars down to
this luminosity presumably rate as massive
stars, and may be thought to move nearly
horizontally across the HR diagram.
However, the data can be used in another
way, to examine the source of the difference
between the period distribution in the Small
Cloud and in our own galaxy. If the Ceph-
eids are strictly comparable in the two sys-
tems, their rate of progress at a given ab-
solute magnitude should be the same, and
if the distribution of periods is as different
as it appears to be, the only conclusion that
can be drawn is that the “birth function”
in the Small Cloud differs from that in our
galaxy, and increases more steeply with
decreasing luminosity, at least down to ab-
solute magnitude —1.5. Information on the
observed luminosity function in the Small
Cloud is very indefinite, but this is an ob-
servational datum that could readily be
obtained. It is possible, as Arp has sug-
gested, that Cepheids in the Small Cloud
(and, by inference, the Small Cloud itself)
may differ from their galactic counterparts
in chemical composition. A difference in
chemical composition would, if large
enough, have a noticeable effect on the
mass-luminosity relation (417), and perhaps
on the luminosity function itself.
In conclusion, I can summarize my opin-
ion concerning the present status of the
period-luminosity relation. The preliminary
task of determining its average course has
been completed, and we are nearing a con-
sensus concerning the colors of Cepheids,
and the relation of mean color to period.
Future work must be concerned with the
dispersions of the period-luminosity rela-
i
;
7
DECEMBER 1959
PAYNE-GAPOSCHKIN: CEPHEID VARIABLES
o49
Frequency of logP
(interval in log P = 0.1
interval in Me " 0.1)
Dots: less than 5
Horizontal shading:
Cross hatching H
Filled area:
Fia. 14.—Contour diagram showing frequency of log P in the period-luminosity plane.
tion, the period-luminosity-color relation,
and the period-luminosity-light curve rela-
tion. The part played by the Cepheid stage
in stellar development will stimulate studies
of the relation of period-frequency to the
local birth function and to the rate of
progress of a star through the variable stage.
These last problems are intimately tied up
with the study of stellar interiors, and
the machine computation of evolutionary
tracks. In this area, speculation is worse
than valueless, and the greatest service that
can be rendered by the student of variable
stars 1s the provision of data that are ac-
curate and complete—in other words, the
systematic discovery of variable stars in
carefully selected systems, accurate studies
of brightness, light curve and color, and de-
termination of luminosity functions.
REFERENCES
(1) Pickertne, E.C. Cire. Astr. Observ. Harvard
Coll. 173. 1912:
(2) Baitzy, S. I. Ann. Astr. Observ. Harvard
Coll. 38. 1902.
(3) SHaptey, H. Star clusters: 125. 1930.
(4) Hussite, E. P. Astrophys. Journ. 62: 409.
1925; 63: 17. 1926; 69: 145. 1929.
(5) Baapg, W. Trans. Int. Astr. Union 8: 397.
1954; Publ. Astr. Soc. Pacific 68: 1. 1956.
(6) Roserts, M., and Sanpace, A. R. Astr. Journ.
59: 190. 1954.
(7) SanpacE, A. R. Steilar populations: 52. Vati-
ean Observatory, 1958.
350 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
Frequency of log P
(adjusted periods)
(interval in log P = 0.
interval in Mh, * 0.1
Dots: less than 5
Horizontal shading: 5 , 6
Cross-hatching: 7 to 9
Filled area: 10 to 15
Fic. 15—Contour diagram showing frequency
of logarithm of adjusted period (see text) for the
material of Fig. 14.
(8) Arp, H.C. Handb. der Phys. 51: 118. 1958.
(9) Hertzsprune, E. Bull. Astr. Inst. Nether-
lands 96. 1926.
(10) Payne-GaposcHKIN, C. Ann. Astr. Obsery.
Harvard Coll. 113: 173. 1954.
(11) SHapney, H., and Nam, V. McK. Proc.
Amer. Phil. Soc. 92: 310. 1948.
(12) Payne-GaposcHKIN, C. Variable stars and
galactic structure: 42. 1954.
(13) Paynn-GaposcHKIN, C. Astr. Journ. 52: 218.
1947.
(14) Paynn-GaposcHKIN, C.
1142. 1956.
(15) Paynne-GaposcHKIN, C. Variable stars and
galactic structure: 13. 1954.
Vistas in astronomy:
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(16) SHapLey, H. Star clusters: 132. 1930.
(17) Arp, H.C. Astr. Journ. 63: 45. 1958.
(18) SanpacE, A. R. Astrophys. Journ. 127: 513.
1958.
(19) Copr, A. Astrophys. Journ. 106: 309. 1947.
(20) Watraven, TH., Mutier, A. B., and OosTEr-
Horr, P. Tu. Bull. Astr. Inst. Netherlands
484. 1958.
(21) Gascorene, S. C. B., and Kron, G. E. Publ.
Astr. Soc. Pacific 64: 196. 1952.
(22) Gascoticne, S. C. B. Australian Journ. Sci.
Suppl. 1957.
(23) Gascoreng, S. C. B., and Eaecen, O. J.
Monthly Notices Roy. Astr. Soc. 117:
423. 1957.
(24) Eccen, O. J. Astrophys. Journ. 113: 367.
1951.
(25) Eacen, O. J., Gascoicne, 8S. C. B., and Burr,
E. J. Monthly Notices Roy. Astr. Soc.
117: 423. 1957.
(26) Payne-GaposcHkKIN, C. Variable stars and
galactic structure: 34. 1952.
(27) Burpipcr, G. R., and BursincE,
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(28) Sanpace, A. R. Astrophys. Journ. 126: 326.
1957.
(29) Arp, H. C. Handb. der Phys. 51: 110. 1958.
(30) Ast, H. A. Astrophys. Journ. 126: 138. 1957.
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Krart, R. P. Astrophys. Journ. 126: 225.
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Arp, H. C. Handb. der Phys. 51: 99. 1958;
Astrophys. Journ. 128: 166. 1958.
SanpaceE, A. R. Astrophys. Journ. 128: 150.
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(32) Srartkova, G. A. Variable Stars (U.S.S.R.)
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(33) BursipceE, G. R., and Bursmcs,
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(34) Irwin, J. B. Proc. Nat. Sci. Found., Char-
lottesville. 1956.
Sanpace, A. R. Stellar populations: 41. Vati-
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(36) Horrner, S. von. Zeitschr. fiir Astrophys.
42: 273. 1957.
(37) Jounson, H. L.
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(39) SHaptey, H., and Nam, V. McK. Asitr.
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EK. M.
i pmo ts
(35
a
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DECEMBER 1959 NICOL ET AL: DIFFERENTIATION IN SOME INVERTEBRATES
dol
PALEONTOLOGY —Paleontologic record of the primary differentiation in some
major invertebrate groups. Davip Nico, GEORGE A. DEsBoROUGH, and JAMES
R. Sotiipay, Southern Illinois University, Carbondale, Ill.
(Received July 9, 1959)
A table of the geologic ranges of the prin-
cipal animal phyla, prepared by Shrock and
Twenhofel (1953, p. 11), should be of inter-
est to all students of evolution. According
to their data, the animal phyla with a good
fossil record, those having hard parts that
are readily preserved, all appeared by about
450 million years ago, and most of them are
still older. In other words, according to
present knowledge of the fossil record, the
major differentiation of the animal king-
dom was completed by about the end of the
Cambrian period. Probable exceptions to
this, which would now appear to be few in
number, would be of two kinds—animal
phyla with poor or no fossil records and ex-
tinct phyla which are not recognized as such
now. At the present state of knowledge it
can be said that only many lesser groups—
classes, orders, families, and genera—first
appeared in time less than 450 million years
ago.
This would seem to support the assertion
of Willis (1940, p. 186):
It is clear that the tests give a very strong evi-
dence indeed in favour of the theory of differen-
tiation or divergent mutation, according to which
the course of evolution is in the opposite direction
to what has hitherto been supposed, and by muta-
tions which tend to diminish as time goes on, but
go in the direction family-genus-species. The or-
ganism that first represents the family is, of course,
at the same time its first genus and species, but
these are of different rank from genera and species
in a larger family. By further mutations this will
then give rise to further genera and species. The
first new genus formed will usually be widely di-
vergent from the parent genus of the family, even
if the family be quite small, e.g. of two genera
only. Later formations will be less and less diver-
gent on the whole, but will show some of the char-
acters of divergence of their first parents. The
main lines of divergence are therefore given by
the latter, and later genera fill them in, as shown
by a good dichotomous key.
This is the main theme in Willis’s book,
and he repeats it many times in various
ways. In another place Willis (p. 191)
states: “Evolution goes on in what one may
call the downward direction from family
to variety, not in the upward, required by
the theory of natural selection.” Willis at-
tributes the idea of divergent mutation to
H. B. Guppy and claims that it was adum-
brated by St. Hilaire. More recently James
Small (1951, p. 181) has stated the same
idea: ‘““The general factual picture of evolu-
tion 1s now one of progressive evolution by
apparently large steps for the phyla, com-
bined with diversification of genetic pat-
terns downwards from phyla to families,
genera, species and lower categories.” Schin-
dewolf (1951, p. 139) has stressed divergent
mutation, too, as shown by this paragraph:
Palaeontological evidence suggests that the be-
ginning of each phylogenetic cycle, irrespective of
the systematic category concerned, is marked by
an intensification of evolution. In the later phases,
the rate of evolution is much smaller and the
ability to change decreases. An instructive example
is the evolution of the placental mammals in the
early Tertiary. In the upper Cretaceous the In-
sectivora appear, initiating the evolutionary cycle
of the Eutheria. At the boundary of Cretaceous
and Tertiary, and in the early Paleocene all other
known placental orders become differentiated from
the original group. Twenty-five orders, represent-
ing the entire morphological range of the subclass,
appear 1n the relatively short period of 10-15 mil-
lon years, whilst during the subsequent, post-
Paleocene, period of 60 million years not a single
new order is added.
Other workers who have favored the the-
ory of early primary divergence could be
cited, but the ones either mentioned or
quoted herein should suffice to show that
this is not a new idea nor is it without its
adherents today. The thesis of these work-
ers is that the major subdivisions of a group
(e.g., classes of a phylum or orders of a
class) generally originate early in its his-
tory, whereas new subdivisions of lesser
rank (e.g., genera and species) may arise at
any time throughout the group’s geologic
history.
For this paper the writers have taken 13
major invertebrate groups with a good pa-
leontologic record and have recorded the
oo2 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
eeologic ranges of their primary subgroups.
In the case of a phylum, the geologic ranges
of its classes were plotted; in the case of a
class, the geologic ranges of its orders were
recorded; and so on. With these data we
hope to show whether the basic pattern of
evolution is like that described by Willis
and others who claim that primary diver-
vent mutation occurs early in the history of
a major group or is like that deseribed by
other workers who contend that primary d1-
vergences occur as a gradual and steady
process throughout the geologic history of
each group. The latter idea is convention-
ally considered the more logical pattern In
evolution. Except for some work by Schin-
dewolf almost no analyses of this sort have
been attempted by invertebrate paleontolo-
ists.
COMPILATION AND PRESENTATION OF DATA
Thirteen examples are presented, all
taken from invertebrate groups with a good
fossil record. The writers have purposely
avoided groups like the Trilobita and the
Porifera because so much of the history of
their divergence ranges back to the base of
the Cambrian that a long pre-Cambrian
history might be postulated for both of them
even though the direct evidence of the fos-
sil record is scanty or absent. We have
avoided groups where the basic classifica-
tion is not well understood or where the fos-
sil record is rather poor. Our examples are
drawn from the following phyla: Protozoa
(1), Coelenterata (3), Bryozoa (1), Bra-
chiopoda (1), Mollusca (2), Arthropoda
(1), Echinodermata (3), and Protochordata
(1). These, we believe, give us a reasonably
large sample of the invertebrate phyla, al-
though additional examples could have been
obtained.
Another way by which we have attempted
to avoid a bias of the data is to exclude the
declining phase of a group’s evolution—1.e.,
the phase in which it approaches extinction.
For example, we have used only the Paleo-
zoic history of the orders of nautiloids and
the superfamilies of articulate brachiopods
because the possibility of the occurrence of
a primary divergence in a group approach-
vou. 49, No. 10
ing extinction is remote. However, in the
case of the graptolites we have included
data on the final stage of the group’s exist-
ence because the complete geologic history,
from inception to extinction, illustrates a
typical pattern of rapid evolution.
The first appearance of a particular group
is the most important part of the data pre-
sented here. No attempt was made to show
the phylogenetic relationships of the vari-
ous groups to each other, for two reasons.
The first is that this information is unim-
portant for our purposes in this paper. Sec-
ondly, many of these relationships are not
well understood and are a matter of conjec-
ture. The writers do not claim to be experts
on the phylogeny of the groups used as ex-
amples.
In the presentation of the data concern-
ing the time of origin, only the primary di-
vergences or largest subdivisions of a par-
ticular group have been used. In other
words, for the phylum Mollusca we have
considered only the classes; for the subclass
Nautiloidea we have used only the orders.
We are well aware that scientists differ
in their opinions concerning the classes
which should be included in a particular
phylum, the orders which should be in-
cluded in a particular class, and, in some
cases, the question of whether a certain
eroup should be ranked as a class or an
order or whether another group should be
ranked as an order or a family. For this
paper we have excluded aberrant groups for
which the allocation is questionable and
have sought to avoid excesses of classifica-
tional splitting and lumping. In deciding
which primary subdivisions to include in
each of our major groups we have relied on
either the consensus or the latest authority.
We have also done this for the data regard-
ing the time of the first appearance of each
primary subdivision, in some cases taking
the majority opinion from standard text-
books on paleontology and zoology and in
others using the most recent authoritative
work. Only in the latter cases have we spe-
cifically cited the references from which our
data were taken.
There is no exact agreement on the time
DECEMBER 1959 NICOL ET AL.: DIFFERENTIATION IN SOME INVERTEBRATES
span, in millions of years, of the various
periods of geologic history. We have used
the same time scale as was used by Knight
(1952, p. 7) with the exception of dividing
the Carboniferous into Mississippian and
Pennsylvanian periods and combining the
Tertiary and Quaternary periods by using
the Cenozoic era. Knight stated that his
data were taken from Report of the meas-
urement of geologic time of the Division of
Geology and Geography, National Research
Council, for 1949-1950, p. 18. The writers
have not seen this latter reference. The
chart used by Knight is here reproduced,
with few modifications:
Era or period ered maior Vasieaee a
Cenozoic 60 0-60
Cretaceous 70 60-130
Jurassic 25 130-155
Triassic 30 155-185
Permian 25 185-210
Pennsylvanian 25 210-235
Mississippian 30 235-265
Devonian 55 265-320
Silurian 40 320-360
Ordovician 80 360-440
Cambrian 80 440-520
DISCUSSION OF COMPILED DATA
The sequence in which the examples are
presented is from the groups of organisms
that are structurally simpler to the more
complex ones. The first example (Fig. 1),
therefore, comprises four families of plank-
tonic Foraminifera as compiled by Loeb-
lich and collaborators (1957). These fam-
ilies are generally considered by most
micropaleontologists to be phylogenetically
related, although there are a few planktonic
Foraminifera not included in these four
families. In preparing this figure the writers
arbitrarily assigned the same amount of
time to each of the Cretaceous stages, there
being 12 of them if the Danian is excluded
as was done by Loeblich and his collabo-
rators. The first family, the Orbulinidae,
appeared at the beginning of the Hau-
terivian stage, approximately 120 million
years ago, and continues to the present. At
the beginning of the Aptian stage, approxi-
mately 12 million years later, two more
families emerged—the Globorotalidae and
300
CENOZOTIC
GLOBOR|IOTALIIDAE
GLOBOTIRUNCANIDAE
ics}
<
a 4
H
a
H
a
ica)
x
&
Zz
<
x=
ORBULINI|DAE
CRETACEOUS
__ Fic. 1—Periods of existence of four related fam-
ilies of planktonic Foraminifera. Data taken from
Loeblich and collaborators, 1957. Horizontal stubs
demark 10-million-year intervals.
the Hantkeninidae. These two families also
have living representatives. Finally, at the
beginning of the Turonian stage, the last
of the families arose, the Globotruncanidae,
only 30 million years after the first-appear-
ing of these four families. The Globo-
truncanidae were a relatively short-lived
family that became extinct at the end of
the Cretaceous. To summarize: within 12
milion years three of the four families
made their appearance, and within ap-
proximately 30 million years all of them
had emerged. Thus, all the basic differentia-
tion took place within a time span of 30
milion years and no new families have
appeared in the last 90 million years.
The next example (Fig. 2) comprises the
families of tabulate corals (data taken from
Hill and Stumm in Moore, 1956). The first
two families of the Tabulata, the Chaeteti-
dae and Syringophyllidae, appeared almost
simultaneously at the beginning of the mid-
dle Ordovician. Two more families, the
Heliolitidae and Halysitidae, made their
appearance during the upper part of the
middle Ordovician no more than 20 million
years later. At the beginning of the late
Ordovician the Auloporidae and Favositi-
dae arose; this was no more than 30 million
years after the first two families of tabulate
corals began their existence. Thus, in ap-
proximately 30 million years the basic di-
AY
Or
TS
JOURNAL OF THE
PENNSYLVANWIABS
MISSISSIPPIANS
DEVONIAN
SILURIAN o
ORDOVICIAN
ETID
WASHINGTON ACADEMY OF SCIENCES
_SYRIWGOPH
VOL. 49, No. 10
WARTUNA
AUILOPORIDAE
FAIVOSITIDAE
WHALIYSITIDAE
Gay S| Peter Hiv Len Nop
COLUM
Fie. 2.—Paleozoic history of the families of tabulate corals. Data taken from Hill and Stumm in Moore,
1956. Horizontal stubs demark 20-million-year intervals.
Fic. 3.—Periods of existence of the suborders of rugose corals. Data taken from Hill zn Moore, 1956.
Horizontal stubs demark 20-million-year intervals.
vergence of the Tabulata was completed,
and no new families appeared throughout
the remaining 200 million years of the Pa-
leozoic era.
Many of the major groups studied have
included subgroups which existed only
briefly, usually early in the history of the
major group. For example, the Syringophyl-
lidae, Heliolitidae, and Halysitidae ap-
peared within the first 20 million years of
tabulate existence. The Syringophyllidae
were extant for about 70 million years, the
Heliolitidae for less than 120 million years,
and the Halysitidae for about 80 million
years. The occurrence of short-lived sub-
groups is common enough that it should be
considered an important phenomenon, al-
though it has been left unexplained in the-
ories on the basic causes of evolution.
The suborders of the rugose corals (Fig.
3) (data taken from Hill in Moore, 1956)
provide another illustrative example of
rapid primary divergence. All three subor-
ders of the Rugosa emerged within about
the first 10 million years of the order’s be-
ginning in the middle Ordovician. No new
suborders appeared during the remainder of
the Paleozoic, a span of 220 million years,
although many families and groups of lesser
rank did arise after all of the suborders had
been established.
Another interesting example (Fig. 4) is
that of the primary divergence in the scle-
ractinian corals (data taken from Wells an
Moore, 1956). Three of the five suborders
appeared almost simultaneously in the mid-
dle Triassic. About 25 million years later
the fourth suborder arose in the early Juras-
sic. Some 80 million years after that, or
about 105 million years after the sclerac-
tinians began, the last suborder originated
in the late Cretaceous. No new suborders
have appeared during the 70 million years
since. Most of the basic divergence in the
scleractinian corals took place within the
first 25 million years, and only one new
suborder appeared in the last 150 million
years of scleractinian history.
Many scientists, particularly in the field
of genetics, would expect evolution to be a
DECEMBER 1959 NICOL ET AL.: DIFFERENTIATION IN SOME INVERTEBRATES
CENOZOTIC
t{
CRETACEOUS
JURASSIC
tenet eA So LC
FUNGIINA
1 <
| 2
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, ial
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wi
300
CAIRYOPHY ELINA
DEINDROPHYLLIINA_
ASE CACO Na
SI CPAUR Ya OsPeHaVeLeLplalaNen
Fic. 4.—Periods of existence of suborders of scleractinian corals. Data taken from Wells zn Moore,
1956. Horizontal stubs demark 10-million-year intervals.
Fie. 5.—Hypothetical periods of existence of suborders of scleractinian corals. If evolution were a
slow, gradual, and steady process, with primary divergences occurring at regular intervals throughout
geologic history, new suborders of scleractinian corals would have arisen at 35-million-year intervals.
Cf. Fig. 4.
relatively steady and gradual process, with
primary divergences occurring one by one
at regular intervals throughout the history
of a major group. We digress here in order
to compare the actual paleontologic record
of the suborders of the scleractinian corals
with the theoretical record which would
have been established if this hypothesis
were true (cf. Figs. 4 and 5). Assuming that
the scleractinian corals have existed for
175 million years, the first suborder having
originated at the beginning of the middle
Triassic, one might expect the other four
suborders to appear thereafter one at a time
at 35-million-year intervals (and a new
suborder would be due to arise soon). Thus,
according to the “regular interval” theory,
one suborder would have originated at the
base of the middle Triassic, one in the mid-
dle Jurassic, one in the early middle Creta-
ceous, one in the late Cretaceous, and one
near the middle Cenozoic. In actual fact,
however, the record is remarkably different.
It should be pointed out that the forego-
ing comparative example is based on a
group that evinces little or no indication of
decline in evolutionary vigor at the present
time. Similar comparisons between actual
and theoretical evolution are presented in
CENOZOIC
CRETACEOUS
JURASSIC
TRIASSIC
PERMIAN
PENNSYLVANIAN
MISSISSIPPIAN
DEVONIAN
SILURIAN -:
ORDOVICIAN
CAMBRIAN
Fic. 6—Periods of existence of classes of Bryo-
zoa. Horizontal stubs demark 20-million-year in-
tervals.
CRYPTOSTIOMAT
CTENOSTOMATA
CYCLOSTOM
Figs. 8 and 9, the classes of the Mollusca,
and Figs. 12 and 13, the classes of the Echi-
nodermata. These phyla also show no tend-
ency toward extinction at the present time.
In all three examples it is clear that major
divergences have not occurred gradually or
at regular intervals throughout the history
of each group.
Returning to the presentation of the basic
data, we cite another good case of early
rapid divergence: the five classes of the
phylum Bryozoa (Fig. 6). Within prob-
ably 10 million years during late Cambrian
and early Ordovician times, four of the five
classes appeared. Not until 310 million
years later did the fifth class, the Cheilo-
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
vou. 49, No. 10
stomata, make its debut during the late
Jurassic. No new classes of the Bryozoa
have appeared within the past 140 million
years. In other words, most of the basic di-
vergence in the Bryozoa occurred during a
brief span of 10 million years; for the past
450 million years, little primary divergence
has occurred within the phylum.
The superfamilies of the Paleozoic articu-
late brachiopods (Fig. 7) also provide a
good example of rapid primary divergence.
The data were taken from Cooper and Wil-
liams (1952, part of fig. 6, p. 332). At the
beginning of the Cambrian the Orthacea
emerged. No more than 20 million years
later, still in the early Cambrian, three more
superfamilies began their existence. Two of
these, the Rustellacea and the Kutorgina-
cea, were short-lived and became extinct
within about 35 million years. Then there
was a lag of nearly 80 million years, or 100
million years after the beginning of the
Cambrian, before more divergent mutation
took place. The Triplesiacea and the Atry-
pacea appeared almost simultaneously in
the middle of early Ordovician time. About
10 million years later two more superfami-
lies emerged in the late early Ordovician.
Some 15 million years after that, five more
superfamilies appeared; this was accom-
plished by middle Ordovician time. During
the late Ordovician one more superfamily
arrived on the scene, the Productacea. Thus,
within a part of the Ordovician period span-
ning less than 60 million years, 10 new su-
perfamilies appeared. By the middle part of
the early Silurian the last two superfamilies
began their existence. It took more than 170
million years for all 16 of the superfamilies
to emerge. In the remaining 165 million
years of the Paleozoic era, no new super-
families of articulate brachiopods appeared,
and, with one possible exception, none arose
during the articulate brachiopods’ period of
decline in evolutionary vigor, the 185 mil-
lion years represented by the Mesozoic and
Cenozoic eras.
The time lag of 80 to 100 million years
between the appearance of the first articu-
late brachiopod superfamilies and the time
of rapid divergence which began in the early
Ordovician is analogous to the time lag be-
tween the inception and the period of rapid
DECEMBER 1959
sary
PENNSYLVANIAN
ME SSESSIPPIAN
SELURIAN
ORDOVICIAN
CAMBRIAN
KUTORGI|NACEA
—SYNTROPIHIACEA
RUSTELLIACEA
NICOL ET AL.: DIFFERENTIATION IN SOME INVERTEBRATES
a mall:
E
ATRYPACE|A
TERE BOR ATU A Ce A cere)
EAR uO zDAURC!
BN
PENTAM|IERACHA_
BAC BO m Ta eC Roma ele OSCE.
DALMANHLLAC |
RHYNCHIONELY
STROPHO
Fic. 7.—Paleozoic history of superfamilies of articulate brachiopods. Data taken from Cooper and
Williams, 1952, part of fig. 6, p. 332. Horizontal stubs demark 20-million-year intervals.
emergence of the mammalian orders. As in
the case of the mammals, the postponement
of rapid divergence of the articulate brachi-
opods may have been due in part to compe-
tition from another group—in this instance
the inarticulate brachiopods which flour-
ished first. Another possibility is that the
Cambrian seas may have been more suit-
able for animals with chitinophosphatic
shells (e.g., most, but not all, of the inar-
ticulate brachiopods), whereas a favorable
environment for animals with calcareous
shells (e.g., the articulate brachiopods) did
not develop until later. This possibility
seems to be confirmed by the fact that many
calcareous-shelled animals originated in
the early and middle Ordovician (Ray-
mond, 1939, p. 42) ; examples are the pelecy-
pods, the rugose and tabulate corals, and
the bryozoans. Possibly these two factors
together may have caused the postpone-
ment of rapid primary divergence of the
articulate brachiopods.
The classes of the Mollusca (Fig. 8) orig-
inated early in the history of the phylum.
The gastropods began at the base of the
Cambrian. About 60 million years later, in
the late Cambrian, the Cephalopoda and
the Amphineura appeared. Twenty million
years after this latter event, at the begin-
ning of the Ordovician, the Pelecypoda be-
gan their existence. Finally, the Scaphopoda
emerged at the base of the Silurian, 160 mil-
lion years after the beginning of the Cam-
brian, or 80 million years after the appear-
ance of the Pelecypoda. No new classes of
Mollusca have emerged during the 360 mil-
lion years since the beginning of the Silu-
rian. In other words, most of the primary
divergence within the Mollusca was accom-
plished in no more than 80 million years,
and it all occurred within a span of 160 mil-
lion years. All the known classes of the Mol-
lusca are long-lived.
Once again the authors digress, this time
to compare the actual history of the ap-
358 JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
CENOZOTIC
VOL. 49, No. 10
CRETACEOUS lie
JUULReACSISELG in
TER IAPS SelG
CAPIHOPODA
Tee
PEWUECYPODA casita
er
FERMIAN
PENNSYLVANIAN
Mol Sesh siSel PP AUN
DEVONIAN
SILURIAN
ORDOVICIAN
CEPHALOP
AMPHINEU
CAMBRIAN
Se ee ce ee ees
CEPH|ALOPOD
GAISTROFODA
Eo isG
Fig. 8.—Periods of existence of classes of Mollusca. Horizontal stubs demark 20-million-year intervals.
Fig. 9.—Hypothetical periods of existence of classes of Mollusca. If evolution were a slow, gradual,
and steady process, with primary divergences occurring at regular intervals throughout geologic his-
tory, new classes of Mollusca would have arisen at 104-million-year intervals. Cf. Fig. 8.
pearance of the molluscan classes, based on
the paleontologiec record, with a hypotheti-
cal sequence of divergences based on the
idea that the classes should appear at ap-
proximately regular intervals throughout
the entire history of the phylum. If the time
from Cambrian to Recent is taken as 520
million years and the first class originated
at the base of the Cambrian, then the next
four classes should have emerged one by
one at approximately 104-million-year in-
tervals and a new, or sixth, class could be
expected to appear soon. Accordingly, one
class should have arisen at the beginning of
the Cambrian, the next one in the early
middle Ordovician, the third near the be-
ginning of the Devonian, another at about
the base of the Permian, and the last known
one in the middle Cretaceous. That the ac-
tual record is sharply different from the
hypothetical is illustrated by a comparison
of Figs. 8 and 9.
Another case of early rapid divergence
(Fig. 10) is seen in the orders of the nauti-
loids (data taken from Flower and Kummel,
1950, with slight modifications). During the
late Cambrian the first order of nautiloids,
the Ellesmeroceratida, appeared. Beginning
at the base of the Ordovician and extending
to the middle Ordovician, a tremendous
DECEMBER 1959 NICOL ET AL.: DIFFERENTIATION IN SOME INVERTEBRATES
PERMIAN
Mook om LPPIAN
DEVONIAN
SrLUR IAN
ORDOVICIAN
CAMBRIAN
ENDOCERAI|TIDA
TPAUR EDS HUYaCu sa | ReAG Te TITA
ELILESMEROCEMRATIOA
TIDEA
TeTsO PAC | x
MICHELIN|OCERA
309
A
RUDOCE
DEOCKRATIDA4&
DEtESECrO)SVOReiaD
ACTINOCE
AUSEOLORCUEDRUR
ONCOCERA
BARRAN
Fig. 10.—Paleozoic history of orders of nautiloid cephalopods. Data taken from Flower and Kummel,
1950, with slight modifications. Horizontal stubs demark 20-million-year intervals.
burst of divergent mutation occurred:
within a span of no more than 40 million
years, and within about 60 million years of
the first appearance of the nautiloids, nine
new orders emerged. Several of these were
relatively short-lived, having existed for
about 100 million years and in a few cases
even less. Between 80 and 90 million years
later, in the early Devonian, two more or-
ders appeared. Finally, the last two orders
arose in the early Mississippian about 195
million years after the beginning of nauti-
loid history. No new orders of nautiloids
emerged during the final 80 million years
of the Paleozoic, nor did any appear during
the Mesozoic and Cenozoic eras when the
general trend of the nautiloids was toward
extinction. It is noteworthy that five-sev-
enths of the nautiloid orders originated
within the first one-seventh of the nauti-
loids’ period of existence. In other words,
most of the major groups (10 of 14) ap-
peared between the late Cambrian and mid-
dle Ordovician. This corresponds well with
the time of rapid divergence of many other
organisms that had calcareous shells. In the
last 400 million years of nautiloid history
only four new orders emerged, and even
they all began within the first 135 million
years of that span of time.
The first superfamily of Paleozoic ostra-
codes (Fig. 11) emerged at the beginning
of the Ordovician period. In the early Ordo-
vician, also, and about 15 million years
later, two more superfamilies appeared.
About 190 million years after that, the
fourth and last superfamily originated; this
was at the base of the Pennsylvanian period.
During the remainder of the Paleozoic era,
50 million years, no new superfamilies of
360
PERMIAN
PENNSYLVANIAN
M i7S)5 LS'S'L Peper aN
DEVONIAN
SVGe LE Ve BE IN
ORDOVICIAN
LEPERDI
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
BEYRIC
VOL. 49, No. 10
CYPRID
CAMERAT
hh ENE at
Fia. 11.—Paleozoic history of four superfamilies of ostracodes.
Horizontal stubs demark 20-million-year intervals.
Fig. 14.—Paleozoic history of three subclasses of crinoids.
Horizontal stubs demark 20-million-year intervals.
ostracodes emerged. Thus, three of the four
major groups of ostracodes arose within a
span of 15 million years during the early
Ordovician, and only one new superfamily
appeared during the remaining 240 million
years of the Paleozoic era.
In regard to early divergent mutation,
perhaps the most illustrative and interest-
ing group studied comprises the classes of
the pkylum Echinodermata (Fig. 12). The
data, collated from several different sources,
represent a concensus of authorities. A few
questionable groups were not included, as
for instance the Bothriocidaroida, which is
considered a separate class by Moore
(Moore, Lalicker, and Fischer, 1952, p. 577)
but not by others, and the classes Cya-
moidea and Cycloidea, which are aberrant
short-lived middle Cambrian groups and
are discussed only by Shrock and Twen-
hofel (1953, pp. 694-696). If these groups
had been included in the present study, the
depiction of early divergent mutation
among the echinoderms would have been
even more striking.
Near the beginning of the Cambrian the
Edrioasteroidea appeared, and about 25
million years later, in the middle Cambrian,
the Eocrinoidea made their debut. Also in
the middle Cambrian, and about 10 million
years after the appearance of the Eoeri-
noidea, the Carpoidea emerged. For the re-
mainder of the Cambrian, about 40 million
years, no new classes of echinoderms ap-
peared. At the beginning of the Ordovician,
however, three more classes arose. Within
the next 40 million years, and no later than
middle Ordovician, the Paracrinoidea, Cys-
toidea, Echinoidea, and Blastoidea made
their debut. The Holothuroidea originated
in the middle Devonian, no more than 110
million years later than the middle Ordovi-
cian. No new classes appeared after the
middle Devonian, or for the past 290 mil-
lion years. Except for the holothuroids, all
the classes of echinoderms emerged within
the first 120 million years (roughly the
first quarter) of the history of the phylum.
The most rapid divergence took place within
the first 40 million years of the Ordovician
period, coinciding again with the time of
rapid divergent mutation of many major
groups of animals with calcareous skeletons.
It is interesting to note here that several
of the echinoderm classes were short-lived,
having originated and expired early in the
history of the phylum.
The writers have chosen the classes of the
DECEMBER 1959 NICOL ET AL.: DIFFERENTIATION IN SOME INVERTEBRATES
CENOZOTIC
CRETACEOUS |
JURASSIC
Dekel WANS) 3) 15 (C
PERMIAN
361
|
iMpIeSs’S S'S IP PIAN
DEVONIAN
SILURIAN
ORDOVICIAN
CAMBRIAN
EOCRIN|OIDEA
CRINOIDE
Snfeidenoomlles ool 3. | se eee en a
CARPIOIDEA
aa are sr ee ee
CYSTOI|DEA
-ECHINIOIDEA
BLAS
PARACRI
Fia. 12.—Periods of existence of classes of Echinodermata.
Horizontal stubs demark 20-million-year intervals.
phylum Echinodermata, a group that shows
no evidence of becoming extinct, for presen-
tation of another example of the difference
between the actual and hypothetical records
of primary differentiation. If we assume
that the phylum’s history from early Cam-
brian to Recent spans 520 million years
and if we theorize that evolution is a rela-
tively steady and gradual process, the 11
classes of echinoderms should have origi-
nated one by one at about 47-million-year
intervals. Hence, their individual emer-
gences should have occurred in the (1) base
of the Cambrian, (2) middle Cambrian, (3)
early Ordovician, (4) late Ordovician, (5)
late Silurian, (6) late middle Devonian, (7)
latest Mississippian, (8) late Permian, (9)
middle Jurassic, (10) middle Cretaceous,
and (11) early Cenozoic. The theory ap-
pears fallacious, however, when one ex-
amines the actual record, which shows that
three classes originated before the Ordovi-
362 JOURNAL OF THE
CENOZOIC
CRETACEOUS
JURASSIC
TORS Ay SSG
PERMIAN
PENNSYLVANIAN
MISSISSIPPIAN
DEVONTAN
SILURIAN
ORDOVICIAN
CAMBRIAWN
ie
CRIINOIO
CARPOIDE
EOCRIINOIDEA
EDRIOAST|IEROIDEA _ Be eee
WASHINGTON
ACADEMY OF SCIENCES VOL, 49, No. 10
UROIDEA
BLAS|TOIDEA
pod dng [ee
el INOYDEJA
See | ow es
HOLOTH
a
'
TELLER
Fie. 13.—Hypothetical periods of existence of classes of Echinodermata. If evolution were a slow,
gradual, and steady process, with primary divergences occurring at regular intervals throughout geo-
logic history, new classes of Echinodermata would have arisen at 47-million-year intervals. Horizontal
stubs demark 20-million-year intervals. Cf. Fig. 12.
clan, seven during the Ordovician, and only
one thereafter. To facilitate comparison we
present the actual and theoretical records
in Figs. 12 and 13.
The first subclass of Paleozoic crinoids
(Fig. 14), the Camerata, appeared at or
near the beginning of the Ordovician. No
more than 30 million years later, in the
early middle Ordovician, the other two sub-
classes made their debut. Once again we see
the early and middle Ordovician as a period
of rapid emergence of animals having cal-
careous shells. For the remainder of Paleo-
zoic time, about 225 million years, no new
subclasses of crinoids arose.
The orders of the irregular echinoids are
an excellent case of adaptive radiation and
rapid divergent mutation (Fig. 15). As soon
as the echinoids developed the ability to
thrive on a sandy or muddy substrate, they
DECEMBER 1959 NICOL ET AL.: DIFFERENTIATION IN SOME INVERTEBRATES
CENOZOIC
PEASTROIDA
CRETACEOUS
ASSIDULOIDA
C
<
[=)
H
oO
o
=z
<
&
<
Qe
n
<
a
Ln
(e)
Qe
al
&
oO
[2]
=)
o
x
JURASSIC
Fic. 15—Periods of existence of orders of ir-
regular echinoids. Horizontal stubs demark 10-mil-
lion-year intervals.
evolved quickly. The first order, Holecty-
poida, appeared in the early Jurassic. Two
more orders sprang into existence almost si-
multaneously in the early Jurassic, prob-
ably no more than two million years later.
The last order, the Clypeastroida, did not
emerge until the late Cretaceous, about 70
million years later. For the past 80 million
years no new orders of irregular echinoids
have arisen. Most of the primary divergent
mutation occurred within the first two mil-
lion years of the existence of the irregular
echinoids; only one new order arose during
the subsequent 150 million years.
The five orders of graptolites (Fig. 16)
give an excellent and typical picture of the
entire history, from inception to extinction,
of a rapidly evolving group of organisms.
The Dendroidea appeared first in the mid-
dle Cambrian. About 25 million years later,
in the late Cambrian, the Graptoloidea
arose; and approximately 10 million years
after that, at the beginning of the Ordovi-
cian period, the other three orders began
their existence. Two of the latter three or-
ders were short-lived, existing for less than
30 million years. All of the basic divergence
within the graptolites was accomplished in
about 35 million years. In the remaining
363
185 million years of graptolite existence, no
new orders appeared.
The history of the graptolites can be di-
vided into three phases such as Schindewolf
(1951, p. 139) has depicted for other groups
of animals. The first phase of rapid diver-
gent evolution (typogenesis) occurred in
the graptolites from middle Cambrian to
the beginning of the Ordovician—approxi-
mately 35 million years—and was charac-
terized by the origin of all of the orders.
The second phase (typostasis), or the acme
of development of graptolites from the
standpoint of numbers of families, genera,
and species, occurred during the Ordovician
and Silurian periods, or in about 120 mil-
lion years. This second phase was marked
not only by the origins of new families, gen-
EARLY
BMISSISSIPPIAW
oe eae
SILURIAN
ORDOVICIAN
TUBOIDEA ae
+
GRIAPTOLOIDEA
CAMAROIDEA
STOLOWOIDEA
DENDROIDIEA
CAMBRIAN
Fic. 16.—Periods of existence of orders of grap-
tolites. Horizontal stubs demark 10-million-year
intervals.
364 JOURNAL OF THE
era, and species but by the extinction of
others. Finally, in the third phase (typoly-
sis) the numbers of lesser subgroups de-
clined and the graptolites became extinct.
This last phase occurred during the Devo-
nian and early Mississippian and spanned
65 million years. The senior author (1954, p.
24) has shown that a similar cycle of de-
velopment, on a much smaller scale, oc-
curred in the long-lived pelecypod species
Glycymeris americana with regard to its
populations and variations.
INFERENCES AND CONCLUSIONS
Believing that the 13 examples used in
this study are representative of major inver-
tebrate groups, the authors observe that
primary divergent mutation typically oc-
curs early in a group’s history, as dia-
erammed by Schindewolf (1950, p. 239).
Thus, the origin of a phylum is closely fol-
lowed by the origin of all its classes; the in-
ception of a class is soon followed by the
inception of all its orders; and a new order
is quickly completed in terms of its families.
An occasional major divergence may occur
much later than the others, but this is rather
exceptional. These observations are at vari-
ance with the theory that primary differen-
tiation occurs gradually and at regular in-
tervals throughout the history of a given
group. That the latter contention is fallaci-
ous 1s graphically demonstrated by a com-
parison of Fig. 4 with 5, 8 with 9, and 12
with 13, depicting the actual and theoreti-
cal histories of the suborders of the sclerac-
tinian corals and the classes of the Mollusca
and Echinodermata.
One possible explanation for early pri-
mary divergent mutation within a major
eroup of animals is alluded to in a somewhat
different aspect by Simpson, Pittendrigh,
and Tiffany (1957, p. 588). In discussing the
appearance of the amphibians they have
this to say:
It is characteristic of evolution that the am-
phibians did not evolve from late, specialized, pro-
gressive or perfected osteichthyans, such as the
teleosts, but from primitive forms that lived near
the beginning of osteichthyan history. It has usu-
ally been true that when a radical adaptive change
occurs and a new major group arises, it originates
from primitive and not from advanced members
WASHINGTON ACADEMY OF SCIENCES
VoL. 49, no. 10
of the ancestral group. With progressive adapta-
tion to any one way of life, there often comes a
time when the adaptation seems to become irre-
vocable—a special aspect of the irrevocability of
evolution in general. Then change to a radically
different way of life becomes, if not impossible, at
least extremely improbable.
For example, suppose that the Cephalo-
poda arose from the Gastropoda: this must
have occurred, if at all, early in gastropod
history, while the gastropods were still
primitive and relatively unspecialized, be-
cause later representatives of a major group
are generally too specialized to give rise to
another group of equal rank. The actual
case is that the Cephalopoda did emerge in
the first one-eighth of gastropod history,
during the time that the gastropods still had
primitive or unspecialized representatives.
A fairly common phenomenon is the oc-
currence of aberrant short-lived subgroups
such as two orders of graptolites, several
classes of echinoderms, three families of
tabulate corals, several superfamilies of
articulate brachiopods, and several orders
of nautiloids. In most, but not all, cases
these short-lived subgroups were among the
earlier divergences of their respective
groups. If the taxonomic rank assigned to
these subgroups is correct on the basis of
morphology, then several interesting infer-
ences can be drawn. First: knowing that
extinction of families, orders, and classes is
not uncommon, one might reasonably as-
sume that extinction of phyla is also not
uncommon. The type of geologic history
could be the same, in which case extinct
phyla may well be more numerous than pa-
leontologists have heretofore acknowledged.
Thus, when dealing with aberrant groups
which can be only doubtfully allocated to
extant phyla, perhaps taxonomists would be
more accurate in assuming that they repre-
sent extinct phyla. With little confidence
and less evidence, paleontologists have al-
located aberrant groups such as the conu-
lariids, stromatoporoids, labechiids, recep-
taculitids, and pleosponges to phyla which
still have living representatives; but the
fossil groups are sufficiently different from
modern groups that such allocations may
be erroneous and the extinct groups may ac-
tually represent, extinct phvla.
DECEMBER 1959 NICOL ET AL.: DIFFERENTIATION IN SOME INVERTEBRATES
It should be stressed, however, that not
all extinct groups do represent extinct
phyla, no matter how difficult their proper
allocations to extant phyla may be. A class
of fossil animals having structurally simple
hard parts may be so lacking in distinctive-
ness that its phyletic assignment is dubious;
and yet, if the soft parts were available for
examination, all doubt would be removed.
Moore (Moore, Lalicker, and Fischer, 1952)
makes an excellent point when he states
(pp. 273-274): “The scaphopods hold un-
questioned status as members of the Mol-
lusca in good standing, but if they were
known only as fossils, it is certain that they
would be put on an incertae sedis (uncer-
tain classification) list.”
Let us further explore the possibility that
extinct phyla may be fairly numerous. The
extinction of a phylum of course implies the
extinction of all its classes. Conversely, the
survival of other phyla implies the survival
of at least some of their classes and occa-
sionally the inception of new classes. Con-
sidering extinctions, survivals, and new in-
ceptions, one is led to wonder whether there
were more phyla and classes of living inver-
tebrates at any one time in the past than
there are today. In the case of the echino-
derm and bryozoan classes, to cite but two
examples, there is no doubt. One has only to
look at Figs. 6 and 12 to see that these
phyla had more classes of living representa-
tives in the Paleozoic era than in the pres-
ent. Yet these phyla do not appear to be
approaching extinction. That is to say, de-
spite a net reduction in the number of
classes, the echinoderms and bryozoans are
still flourishing and may actually have more
genera and species today than at any other
moment of history.
Although they may represent fewer
classes and phyla, we would be inclined to
believe that there are as many species, gen-
era, families, and possibly orders of animals
and plants living on the earth today as at
any specific time in the geological past.
When one considers the ecological relation-
ships among plants and animals, one real-
izes that the appearance of a new species
generally provides another ecological niche
or habitat for one or more additional species
369
as commensals, symbionts, or parasites. The
development of grasses provided impetus to
the evolution of mammals; the origin of
flowering plants promoted the development
of insects; more fundamentally, the emer-
gence of land plants was followed by rapid
evolution of terrestrial animals. Further-
more, most non-parasitic animals have par-
asites living inside or outside their bodies,
and many of the parasites are peculiar to
one or, at most, a few species of host; and
so the origin of a new host species encour-
ages the origin of new parasites. Of course,
it follows that the extinction of a species
may lead to the extinction of some or all of
its commensals, symbionts, and parasites;
but we strongly suspect that in the general
trend of geologic history the proliferation
of some genera has fully offset the decline
of others. Accordingly, while there may
have been a net decline in the number of
major living groups (phyla and classes),
there has probably been no net decline in
the number of minor living groups (genera
and species).
Commenting on extinctions, survivals,
and new inceptions of major and minor
groups, Simpson, Pittendrigh, and Tiffany
(1957, p. 754) state:
Since the Ordovician innumerable groups have
died out, but as they disappeared their places were
simply taken over by other groups, generally of
more recent origin. Among animals and animal-like
protists that are at all likely to leave a fossil record,
there are only 12 phyla and 31 classes in the pres-
ent seas. That actually represents a slight decrease
from the 13 phyla and 33 classes known for late
Ordovician seas. The recent phyla are the same as
those of the Ordovician. Several of the classes are
of later origin and have replaced extinct classes
present in the Ordovician. Replacement has been
more and more complete at lower levels of the
hierarchy of classification.
Why have some of the major groups be-
come extinct? In assembling the data for
this paper we have observed the following
facts. It seems that several different basic
patterns of morphology arose among the
groups which, early in their history, had a
number of short-lived primary subgroups,
as for example the classes of the Echinoder-
mata and the orders of the Nautiloidea. In
each case, the “successful” pattern of mor-
366
phology was exhibited only by the long-
lived subgroups and was characterized by
the development of numerous genera and
species flourishing over a wide geographic
area for a long period of time. Once the
basic pattern had been established, subse-
quent modifications were relatively minor
but numerous. In contrast, the basic mor-
phologic patterns adopted by the _ short-
lived subgroups (and a few of the long-lived
ones) exhibited very few minor modifica-
tions and never became ‘“‘successful” in the
sense of being characterized by large num-
bers of genera and species and broad geo-
eraphie range.
Completing our summary, we call atten-
tion to the fact that many groups of ani-
mals with calcareous skeletons show pri-
mary divergence most rapidly during the
latest Cambrian and early and middle Or-
dovician. Exemplifying this phenomenon
are the echinoderms, the tabulate and ru-
gose corals, the bryozoans, the articulate
brachiopods, the mollusks, the nautiloids,
and the Paleozoic crinoids. Raymond (1939,
pp. 34, 38-40, 42) noted that the Ordovician
was a period of rapid development and
evolution of caleareous-shelled animals, and
our data confirm his assertions.
LITERATURE CITED
Cooper, G. ArTHUR, and WiLiiaAms, ALwyn. Sig-
nificance of the stratigraphic distribution of
brachiopods. Journ. Pal. 26 (3): 326-337, 12
figs. 1952.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 10
FLower, R. H., and Kummet, B., Jr. A classification
of the Nautiloidea. Journ. Pal. 24 (5): 604—
616, 1 fig. 1950.
Knicut, J. Brookes. Primitive fossil gastropods
and their bearing on gastropod classification.
Smithsonian Misc. Coll. 117 (13): 56 pp., 2
pls., 10 figs. 1952.
LorBLicH, ALFRED R., Jr., and CoLLABorators. Stud-
zes in Foraminifera. U.S. Nat. Mus. Bull. 215:
323 pp., 74 pls., 30 text figs. 1957.
Moorrt, Raymonp C. Treatise on imvertebrate pa-
leontology: Part F, Coelenterata: 498 pp.
University of Kansas Press and Geological So-
ciety of America, 1956.
Moorrt, Raymonp C., Lavicker, Ceci G., and
FiscuHer, ALFRED G. Invertebrate fossils: 766
pp. McGraw-Hill, New York, 1952.
Nicot, Davin. Growth and decline of populations
and the distribution of marine pelecypods.
Journ. Pal. 28 (1): 22-25, 2 fies) 1954,
Raymonn, Percy E. Prehistoric life: 324 pp. Har-
vard University Press, 1939.
ScHINDEWOLF, Otto H. Grundfragen der Paldon-
tologie: 506 pp. E. Schweizerbart, Stuttgart,
1950.
. Geologische Zeit und organische Entwick-
lung. Proc. Linn. Soc. London 162 (2): 134—
140, 2 figs. 1951.
SuHrock, R. R., and TwENHOFEL, W. H. Principles
of wvertebrate paleontology: 816 pp. Mc-
Graw-Hill, New York, 1953.
Simpson, G. G., PirTenpRIGH, C. S., and TIFFANY,
L. H. Life: an introduction to biology: 845 pp.
Harcourt, Brace, New York, 1957.
SMALL, JAMES. Discussion on time-rates in evolu-
tion. Proc. Linn. Soc. London 162 (2): 130-
134. 1951.
Wutls, J. C. The course of evolution by differen-
tration or divergent mutation rather than by
selection: 207 pp. Cambridge University Press,
1940.
DECEMBER 1959 VAN DENACK & HANSON: DANTHONIA-LICHEN-MOSS COMMUNITY
367
BOTANY .—The Danthonia-Lichen-Moss community in Washington, D.C., and
vicinity. Sister JuLIA Marin VAN DmNACK and HmrBert C. Hanson, Catholic
University of America.
(Received May 25, 1959)
The purpose of this paper is to describe a
Danthonia-Lichen-Moss community as it
exists in Washington, D.C., and vicinity and
to discuss its possible role in ecological suc-
cession. This community, heretofore unde-
scribed, is ecologically interesting as it
seems to be confined to disturbed places and
is found in woodland clearings, along the
periphery of woods, and on eroding areas.
It consists chiefly of the poverty oat-grass,
Danthonia spicata,! the lichens, Cladonia
cristatella and C. subtenuis, and a variety
of mosses.
PROCEDURE
Six stands of the Danthonia-Lichen-Moss
community in different locations in and
near Washington, D.C., were analyzed dur-
ing March and April 1959. The greatest dis-
stance between stands was 7 miles.
The vegetation was analyzed by means
of 2-decimeter-square quadrats placed at
regular intervals through the center of each
stand (except in stand 3 where intense ero-
sion and degradation of the community ne-
cessitated selection of quadrat areas for
study). Ten quadrat samples were studied
in each of the six stands. Cover estimates of
the vegetation were made using the Hult-
Sernander scale modified by Hanson (1953)
where a cover of 6 is assigned a species with
vertical projection of its living parts cover-
ing 3/4 to 4/4 of the quadrat, 5—1/2 to
3/4, 4-1/4 to 1/2, 3—1/8 to 1/4, 2—1/8
to 1/16, 1—less than 1/16, x—rare, vitality
low. From tabulated data on each stand the
average cover and per cent constancy of
each species were computed (see Table 1).
Soil samples from 0 to 1 inch and 1 inch
to 3 inch depths were taken and analyzed
for texture by the Bouyoucos (1951) hy-
drometer method, pH according to the col-
orometric system using bromecresol green
indicator, and color designation with the
Munsell color charts (Soil Survey Staff,
1951).
1 Nomenclature follows Gleason (1952).
The first study area was located on the
west side of U.S. Highway No. 1 on top of
a hill south of the business section in Uni-
versity Park, Md. (Fig. 1). It consisted of
a small irregular area (106 by 30 feet at its
ereatest dimensions) in a gravelly clearing
among pines (Pinus virginiana). The degree
of slope and other pertinent data for this
and each of the other stands are listed in
Table 1.
The second stand of this study was lo-
cated at the edge of an open white oak
woods near St. Paul’s College, Fourth Street,
NE., Washington, D.C. The woods here ap-
pears to have been artificially cleared, as
there were no tall shrubs and only a few
scattered forbs near the Danthonia, lichen,
and moss vegetation which grew on a slight
north-facing slope just above a three foot
bank bordering the street sidewalk. A rec-
tangular area 24 by 13 feet was chosen as
representative of the Danthonia-Lichen-
Moss community here.
The third and most poorly developed
community considered in this study was at
3900 Harewood Road, Washington, D.C.,
situated on a northern slope in an open
stand of oak, pine, and tulip trees. The com-
munity components occurred in irregular
patches along the hillside which showed evi-
dence of severe frost action and erosion.
A fourth stand 65 by 20 feet was studied
near Sisters’ College on the Catholic Uni-
versity campus, Washington, D.C. This
community covered an open, nearly level
area adjoining a pine (Pinus virginiana)
stand and was subject to occasional mow-
ing.
The fifth and most thriving community
was located on the north side of Edgewood
Road just off U.S. Highway No. 1, half a
mile south of the Plant Industry Station,
Beltsville, Md. The stand 60 by 12 feet was
on a level area from northwest to southeast
between a pine (Pinus virginiana) woods
and an old field invaded by the bluestem
broomsedge, Andropogon virginicus. Across
the road from stand 5 north of a pine woods,
368
stand 6 comprised a rectangular area 75
by 12 it.
OBSERVATIONS
The soils supporting these communities
in the various areas of study ranged in tex-
ture from sandy loam to loam with a clay
loam “B” layer in stands 3 and 6. They
varied greatly in the percentage of gravel
present with some soils showing a 40 to 60
percent gravel content, while others con-
tained little or no gravel. Variation was also
noted in color. The “A” soil layers ranged
from dark gray through dark red-brown to
yellowish brown. The “B” layers exhibited
more uniformity, most of them being yel-
lowish brown. A striking similarity in pH
was observed among the various soil sam-
ples all of which were acid with about a pH
4.5 reaction except for one pH 5.4 reading
in the top soil of stand 3.
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VoL. 49, No. 10
Regardless of the differing conditions in
which the community was found (difference
in intensity of erosion, frost action, degree
and exposure of slope, etc.), the three chief
components of this community, Danthona,
lichens, and mosses, show a high degree of
constancy (see Table 1). No single species
of moss, however, is regularly associated
with the Danthonia spicata-Cladoma cris-
tatella-Cladonia subtenuis communities ob-
served in this study. In stands 1 and 4
Ceratodon purpureus was the chief moss
while Pohlia nutans and Dicranella hetero-
malla were most frequent in stand 2. The
former moss was again frequent in stand 4
with scattered cushions of Leucobryum al-
bidum. Dicranella heteromalla appeared in-
frequently again in stands 3 and 4 and fre-
quently in stand 6. Polytrichum commune
was found in part of stand 5. Generally
where lichen cover was high, moss cover
TABLE 1.—ASSOCIATION OF DANTHONIA-LICHEN-Moss COMMUNITIES
Analysismumben.tecsc hoc. ee oe lean oie eer tae
Dates(o5oe. eee ee SPE tas) sete an a A
INambenotezdmaisamip lessee eeeerneee ere errr
Slope, degrees
Cover, percent
Stones or bare ground
Debris
Total number of species
DANTHONIA SPICATA
LIcHENS*
MosseEs
Agrostis hyemalis
Andropogon virginicus
Anthozanthum odoratum
Aristida dichotoma
Digitaria sanguinalis
Juncus tenuis
Luzula campestris
Panicum albomarginatum
Triodia flava
Antennaria plantaginifolia...........
Aster sp
Cassia chamaechrista
IDUCHeSTCOMENG ICG eae a a ee
Liatris graminifolia
Lonicera japonica
Potentilla canadensis
Solidago nemoralis
Pinus virginiana
OQuercusiSced VN ee ae
CeCe cf at Gu 6. SP o8o Coo. pwn
4-10 Average | Average
cover fre-
10 10 10 10 quency
N, 20 Nw, 5 NE, 0 W,5 (percent)
34.5 84.5 93.5 88.5
223 1.1 A 8 1.6 75
S37, 2.4 3.6 3.0 2.9 100
5 14 11 13
PAS 72) Salli 2.9 2 97
one 3.0 3.9 2.4 od 97
ileal 9 eS 2.8 1.9 80
ao; .03 2
120 all 3 2 17
6 al 8
aD X ae 07 8
x x
x x 2
.02 2
SD .07 7
2 .03 3
.03 3
x 2
A 07 i)
XK x 2
a, .03 - 3
-o .08 8
2 a et .07 10
.O ‘2 pa 15
a7 aL .05 5
ai .02 2
* Lichens: Cladonia cristatella Tuck. (common), Cladonia subtenuis (des Abb.) Evans (frequent),
Baeomyces roseus Pers. (rare). Mosses: Ceratodon purpureus (Hedw.) Brid. (common), Dicranella hetero-
malla (Hedw.) Schimp. (frequent), Pohlia nutans (Hedw.) Lindb. (frequent), Hurhynchium hians
(Hedw.) Jaeg. (infrequent), Leucobryum albidum (Brid.) Lindb. (infrequent), Polytrichum commune
Hedw. (infrequent), Dicranella heteromalla var. orthocarpa (Hedw.) Par. (sparse), Ditrichum pallidum
(Hedw.) Hampe (sparse).
DECEMBER 1959 VAN DENACK & HANSON: DANTHONIA-LICHEN-MOSS COMMUNITY
369
Fig. 1.—Stand No. 1. A Danthonia-Lichen-Moss community in a scrub pine opening. Goldenrod is
scattered. University Park, Md. April 26, 1959.
was low. In two such instances the Dan-
thonia cover was also low.
In stand 5 the pink-earth lichen Baeomy-
ces roseus mingled with the Cladonia sub-
tenuis and rated about equal in cover. It is
interesting to note that this pink-earth
lichen is a soil stabilizer of wide distribution
in eastern United States and is most often
found on new road cuts (Hale, 1959, per-
sonal communication). The level terrain of
stand 5 and the presence of this lichen along
a poorly defined footpath through the center
of the community may account for the high
cover (93.5 percent) observed here.
The 17 percent degree of constancy noted
for the broomsedge grass indicates that
where it occurs adjacent to Danthonia com-
munities it readily invades when a certain
degree of stability is maintained by the
Danthonia, lichens, and mosses. The other
species listed in Table 1 are of such infre-
quent occurrence and low cover that they
appear to be accidental and do not essen-
tially belong to this community-type.
DISCUSSION AND CONCLUSIONS
It appears that disturbance such as clear-
ing a forest, scraping off the top soil, tram-
pling, and erosion favor the establishment
of this community of Danthonia, lichens,
and mosses. Danthonia spicata has a high
tolerance for the infertile “raw” soil in such
sites. It not only propagates by seeds in
panicles, but also by large basally borne
seeds called ‘“cleistogenes” (Hitchcock,
1950). Some species of Cladonia and mosses
are likewise hardy pioneers in these bare
areas. The Danthonia seeds germinate in
the soil, especially where some deposition is
occurring in cracks of the lichen mat and in
moss cushions. The mosses grow mostly
during late winter and early spring and pro-
duce sporangia before the end of April if
moisture is available for a sufficiently long
time. Moisture and shade also apparently
favor the continuance of this community,
but dry weather causes cracking and break-
ing up of the lichen mat, thus accelerating
erosion. Freezing in cold weather in a num-
ber of places causes heaving, loosening of
the soil, severing the attachment of plants
to the soil and increases erosion. When ero-
sion has started, parts of the stand disinte-
erate rapidly, usually leaving a gravelly sur-
face on which invasion takes place again.
In some spots it appears that a cycle of in-
vasion, growth, and degradation may be re-
peated several times before other species
such as Andropogon virginicus or Pinus vir-
giniana invade and cause the disappearance
of most of the lichens. Similar cracking of
lichen mats, especially those formed by
Diplochistes scrwposus (Schreb.) Norm.,
followed by erosion has been noted by the
junior author in Colorado. Churchill and
Hanson (1958) mention the drying and
breaking of the hehen mat in the initiating
of the downgrade series of cyclic changes
in vegetation in the Arctic (cf. Watt, 1947).
Reduced light intensity, such as is found
in openings and along edges of woods, and
soil that remains wet for a considerable
time after rains, is favorable for the best
expression of this community. Danthonia
does occur in open sunlight, but the lichen
and moss components are poorly developed
or lacking in such areas. Danthonia can
also survive in areas where deposition is ac-
tively occurring, but mosses and lichens
cannot.
As in other communities an excessive or
deficient supply of plant requirements may
prove limiting to the establishment and con-
tinuance of the vegetation. Too severe frost
action and erosion in stand 3 may account
for the poor condition of the community
here. Schramm (1958) points out that soil
heaving by frost action can easily occur in
soil with a clay component as high as that
found in this stand. The lichen mats and
moss cushions are lifted by this action and
offer little resistance to rain and runoff. The
undermined Danthonia clumps soon erode
away also. The most flourishing community
was found in loam soil in stand 5 where the
ground was level. The winds and high tem-
perature of a Washington summer may fur-
ther limit this community by causing drying
of the moss and early disintegration of the
lichen mats. An excessive amount of litter
and debris in the form of pine needles, twigs,
branches, and leaves also interferes with the
JOURNAL OF THE WASHINGTON ACADEMY OF SCIENCES
VOL. 49, No. 10
erowth of the plants, particularly the l-
chens and mosses.
The soil type in general did not seem to
limit the community except where clay soils
favored frost action and eliminated the
pink-earth lichen, a sand-adapted species
according to Nearing (1947). The Cladonia
species and Danthonia appear to have a
wide tolerance for different kinds of sub-
strates. The mosses, however, seem to flour-
ish best in the loam of the oak woods in
stand 2.
From the study of these six communities
it appears that the Danthonia-Lichen-Moss
community is characteristic of disturbed
areas in the vicinity of Washington, D.C.
It occurs on a variety of soils as a pioneer
in the revegetation of waste places. It is
not known at present how widespread this
community is. It appears important as a
transitional stage in succession by stabiliz-
ing the soil and is followed by invasion and
establishment of less tolerant grasses, par-
ticularly Andropogon virginicus, shrubs,
and tree seedlings. If this invasion does not
occur, the lichen mat breaks up, erosion and
frost action may occur and the community
is likely to deteriorate even to the bare
ground stage. Thus a cyclic series of down-
grade and upgrade vegetational changes
may be initiated. As invasion of other spe-
cies, however, does occur in time, this com-
munity performs a useful soil-stabilizing
service in nature’s economy in the revegeta-
tion of disturbed areas.
ACKNOWLEDGMENTS
The authors are indebted to Dr. Howard
Crum of the National Museum of Canada,
Ottawa, for the identification of the mosses
and to Dr. Mason E. Hale of the U.S. Na-
tional Museum for the identification of the
lichens.
LITERATURE CITED
Bovuyoucos, G. J. A recalibration of the hydrome-
ter method for making mechanical analysis of
souls. Agron. Journ. 43: 434-488. 1951.
CuurcHILL, EtuHan D., and Hanson, Herpert C.
The concept of climax in arctic and alpine
vegetation. Bot. Rev. 24: 127-191. 1958.
Gueason, H. A. The new Britton and Brown il-
lustrated flora of the northeastern United
States and adjacent Canada: 3 vols. New
York Botanical Garden, New York, 1952.
DECEMBER 1959
Hanson, Hersert C. Vegetation types in north-
western Alaska and comparisons with com-
munities in other Arctic regions. Ecology 34:
111-140. 1953.
Hitcucock, A. §. Manual of the grasses of the
United States: 1051 pp., Washington, 1950.
Nearine, G. G. The lichen book: 648 pp. Ridge-
wood, N. J., 1947.
ACADEMY NEWS
3/1
ScuramM, J. R. Mechanism of frost heaving of
seedlings. Proc. Amer. Phil. Soc. 102 (4): 333-
350. 1958.
Sort Survey Starr. Sozl survey manual. US. Dept.
Agr. Handb. 18: 503 pp. Washington, 1951.
Watt, A. S. Pattern and process in the plant com-
munity. Journ. Ecol. 35: 1-22. 1947.
ACADEMY NEWS
Dr. Jacos RaBINow, president of the Rabinow
Engineering Co., Inc., of Washington, D.C., has
been awarded a Longstreth Medal of the Frank-
lin Institute for his work on the magnetic fluid
clutch.
Dr. Wautter RaAmpBerc, president of the
ACADEMY in 1952 and head of the Mechanics
Division at the National Bureau of Standards
until this year, is now scientific attache at the
American Embassy in Rome, Italy.
Dr. Francis B. SiusBee, president of the
ACADEMY in 1951, retired as head of the Elec-
tricity and Electronics Division, NBS, this year.
The successful career and pleasant associations
in this country of Dr. SHaN-Fu SHEN of the
University of Maryland were featured this sum-
mer in U.S. Information Office releases to the
Far East. He was the recipient of the AcADEMY’s
Engineering Sciences Award at the Annual Din-
ner this year.
Dr. Hersert P. Brorpa, of the Free Radicals
Research Section, National Bureau of Standards,
left in September to spend a year in Cambridge,
England.
INDEX TO VOLUME 49
An asterisk (*) denotes the abstract of a paper before the Academy or an affliated society
PROCEEDINGS OF THE ACADEMY AND AFFILIATED SOCIETIES
Geological Society of Washington. 90.
AUTHOR
AssoTT, IrA H. Extramural science and research
activities of the National Aeronautics and
Space Administration. 87.
ANDREASEN, G. i. See ZietTz, Ismore. 90.
Back, Wiu1am. Emergence of geology as a pub-
lic function, 1800-1879. 205.
Bayer, FreperickK M. A review of the gorgona-
cean genus Placogorgia Studer, with a descrip-
tion of Placogorgia tribuloides, a new species
from the Straits of Florida. 54.
Bsornsson, Ina P. Responses of certain fungi,
particularly Trichoderma sp., to light. 317.
BuakeE, Doris H. Seven new galerucid beetles
from the West Indies. 178.
Brope, Ropert B. Extramural science programs of
the National Science Foundation. 66.
BUELL, CRAWFoRD R. Pay plans and people. 1.
CAMPBELL, FRANK L. Science and education in the
Washington area. 97.
CraBiLL, R. E., Jk. A new Floridan Pectiniunguis,
with reappraisal of its type species and com-
ments on the status of Adenoschendyla and
LIitoschendyla (Chilopoda: Geophilomorpha:
Schendylidae). 324.
Notes on Mecistocephalus in the Ameri-
cas, with a redescription of Mecistocephalus
guildingu Newport. (Chilopoda: Geophilomor-
pha: Mecistocephalidae). 188.
CuatTrecasas, Jose. New chiropterophilous Solana-
ceae from Colombia. 269.
Dane, Carte H. *The New Mexico geologic map
—a summary of 30 years of geologic progress.
O5:
Davis, Norman T. See Drake, Caru J. 19.
Dermen, Hatc. Adventitious bud and stem rela-
tionship in apple. 261.
DesporoucH, GrorceE A. Sulphide mineralization
and associated structure in northern Union
County, Illinois. 172.
See also Nicot, Davin. 351.
Drake, Cart J.. and Davis, Norman T. A new
subfamily, genus, and species of Lygaeidae
(Hemiptera—Heteroptera) from Australia. 19.
DRESCHLER, CHARLES. Two new species of Harpo-
sportum parasitic on nematodes. 106.
Drypen, HueH L. The exploration of space. 165.
DunuHamM, CHartes L. Extramural science pro-
grams of the Atomic Energy Commission. 84.
Dupree, A. Hunter. Asa Gray and American ge-
ology. 227.
FRIEDMAN, IRVING.
tic sea ice. 94.
FRIEDMAN, JuLeS. Development of geologic
thought concerning Ulster County, New York.
252.
*Deuterium and the age of Arc-
Washington Academy of Sciences. 37.
INDEX
Goopine, R. U. Taxonomy of the copepod genera
Pherma and Pestvfer. 122.
Grantz, ArtTHUR. See Zietz, Istpore. 90.
Grice, Georce D. A new species of Haloptilus
(Copepoda: Calonoida) from equatorial and
subtropical waters of the east-central Pacific
Ocean. 193.
GurnNEY, ASHLEY B. A new grasshopper of the
genus Achurwm from eastern Texas (Orthop-
tera: Acrididae). 117.
Hack, J. T. *The relation of manganese to sur-
ficial deposits in the Shenandoah Valley, Vir-
ginia. 93.
Hanson, Herpert C. See Van Denack, Sister
JuLIA Marte. 367.
Hewett, D. F. *Deposits of the manganese ox-
ides. 95.
HorrMan, RicHarp L. Antrogonodesmus, a new
chelodesmoid genus from Cuba, and a rede-
scription of Amphelictogon dolius Chamberlin
(Polydesmida, Chelodesmidae). 284.
Howetit, J. V. Geology plus adventure:
story of the Hayden Survey. 220.
Incram, S. B. Education for the Age of Tech-
nology. 293.
Iwal, Tamotsu. See Matsupara, Kityomatsvu. 27.
KELLEY, VINCENT C. *Structure and fracture sys-
tems of the Colorado Plateau. 94.
LANDEN, Davin. Impact of the development of
photogrammetry upon geology. 234.
*New developments in photogrammetric
measurements for geologists. 93.
Loomis, H. F. Miullipeds collected enroute from
Florida to San Antonio, Texas, and vicinity.
157.
Luxes, GeorceE D. Extramural science programs
of the Department of Defense. 70.
Marton, L. Men and electrons. 98.
Martsupara, Kryomatsu, and Iwai, Tamotsu. De-
scription of a new sandfish, Kraemeria sexra-
diata, from Japan, with special reference to its
osteology. 27.
Mayer-Oakes, WitiiAM J. Relationship between
Plains Early Hunter and Eastern Archaic. 146.
McPuerson, A. T. Introductory remarks to sym-
posium on “Extramural Science Programs of
the Federal Government.” 65.
Meap, Gites W. Bathypterois pectinatus, a new
bathyal iniomous fish from the eastern Pacific.
290.
MisscH, A. T. See Newman, W. L. 90.
Newman, W. L.; Miescu, A. T.; and SHoEMAKER,
E. M. *Chemical composition as a guide to
the size of sandstone-type uranium deposits,
Colorado Plateau. 90.
The
373
ov
Nicot, Davin; DrsporoucH, Grorce A.; and Soiur-
pAY, JAMES R. Paleontologic record of the pri-
mary differentiation in some major inverte-
brate groups. 351.
Notan, THomas B. The United States Geological
Survey and the advancement of geology in the
public service. 209.
OruseR, Paut H. The role of the Smithsonian
Institution in early American geology. 215.
Owen, Epcar W. Remarks on the history of
American petroleum geology. 256.
PancBporN, Mark W., Jr. A history of the popu-
larization of geology in America: A_ biblio-
graphical survey. 224.
PAyNE-GAPOSCHKIN, C. Cepheid variables and the
period-luminosity relation. 333.
Ravup, Davy M. *The effect of environment on
echinoid morphology. 91.
Reep, JOHN C., Jr. *Crystalline rocks of the Po-
tomac River Gorge near Washington, D. C. 92.
Ross, CuHartes A. The Wolfcamp Series (Per-
mian) and new species of fusulinids, Glass
Mountains, Texas. 299.
Rupp, VetvA E. Supplementary studies in Aeschy-
nomene, I: Series Viscidulae, including a new
species and five new varieties. 45.
JOURNAL OF THE ACADEMY OF SCIENCES
VoL. 49, No. 10
SeecerR, RaymMonp J. Franklin as a physicist. 129.
Moon bound. 42.
Serry, L. R. Muscles of the hip and thigh of the
emperor penguin. 183.
Suaw, Byron T. Extramural science programs of
the United States Department of Agriculture.
81.
SHOEMAKER, CLARENCE R. Three new cave amphi-
pods from the West Indies. 273.
SHOEMAKER, E. M. See Newman, W. L. 90.
Sottipay, JAMES R. See Nicot, Davin. 351.
Van Denack, Sister JutiA Marte, and Hanson,
Herspert C. The Danthonia-Lichen-Moss
community in Washington, D. C., and vicinity.
367.
Van Stryke, C. J. Extramural science programs of
the National Institutes of Health. 75.
WELLS, JoHN W. Notes on the earliest geological
maps of the United States, 1756-1832. 198.
Wixson, JoHN A. Darwinian natural selection and
vertebrate paleontology. 231.
ZieETzZ, IstpoRE; ANDREASEN, G. E.; and Grantz,
ArtHurR. *An aeromagnetic study of the Cook
Inlet area, Alaska. 90.
SUBJECT INDEX
Archeology. Relationship between Plains Early
Hunter and Eastern Archaic. Witiiam J.
Mayer-Oakes. 146.
Astronautics. The exploration of space. Hucu L.
Drypen. 165.
Astronomy. Cepheid variables and the period-
luminosity relation. C. PAyNne-GAPoscHKIN.
333.
Botany. Adventitious bud and stem relationship
in apple. Haig Derrmen. 261.
New chiropterophilous Solanaceae from Co-
lombia. Josk CuATRECASAS. 269.
Supplementary studies in Aeschynomene, I:
Series Viscidulae, including a new species
and five new varieties. VatvA EK. Rupp. 45.
The Danthonia-Lichen-Moss community in
Washington, D. C., and vicinity. Sister JULIA
Marig VAN Denack and Hersert C. HaAn-
SON. 367.
Education. Education for the Age of Technology.
S. B. Ineram. 293.
Science and education in the Washington area.
Frank L. CAMPBELL. 97.
Entomology. A new grasshopper of the genus
Achurum from eastern Texas (Orthoptera:
Acrididae). ASHLEY B. Gurney. 117.
A new subfamily, genus, and species of Lygaei-
dae (Hemiptera-Heteroptera) from Aus-
tralia. Cart J. DRAKE and Norman T. Davis.
19.
Seven new galerucid beetles from the West
Indies. Doris H. Buaxke. 178.
General science. Extramural science and research
activities of the National Aeronautics and
Space Administration. IrA H. Assort. 87.
Extramural science programs of the Atomic
Energy Commission. CHARLES L. DUNHAM.
Extramural science programs of the Depart-
ment of Defense. Grorce D. Luxss. 70.
Extramural science programs of the National
Institutes of Health. C. J. VAN Suyke. 75.
Extramural science programs of the National
Science Foundation. Rosert B. Brope. 66.
Extramural science programs of the United
States Department of Agriculture. Byron T.
SHAw. 81.
Introductory remarks [to symposium on “Ex-
tramural Science Programs of the Federal
Government”]. A. T. McPuerson. 65.
Moon bound. Raymonp J. Srrcer. 42.
Geology. *An aeromagnetic study of the Cook
Inlet area, Alaska. Istpore ZieTz, G. E.
ANDREASEN, and ARTHUR GRANTZ. 90.
*Chemical composition as a guide to the size
of sandstone-type uranium deposits, Colo-
rado Plateau. W. L. Newman, A. T. Miescu,
and EK. M. SHormaker. 90.
“Crystalline rocks of the Potomac River Gorge
near Washington, D. C. JoHn C. Regn, Jr.
92.
“Deposits of the manganese oxides. D. F. Hnw-
ETT. 95.
*Deuterium and the age of Arctic sea ice.
IrvING FRIEDMAN. 94.
*New developments in photogrammetric meas-
urements for geologists. DAvip LANDEN. 93.
*Structure and fracture systems of the Colo-
rado Plateau. Vincent C. KeLuey. 94.
Sulphide mineralization and associated struc-
ture in northern Union County, Illinois.
Grorce A. DresporoucH. 172.
Symposium on the history of American ge-
ology. VARIOUS AUTHORS. 197.
*“The New Mexico geologic map—a summary
of 30 years of geologic progress. CaRLE H.
Dane. 95.
*The relation of manganese to surficial deposits
in the Shenandoah Valley, Virginia. J. T.
Hack. 93.
The Wolfcamp Series (Permian) and new spe-
cies of fusulinids, Glass Mountains, Texas.
Cuarues A. Ross. 299.
See also History of science.
History of science. A history of the populariza-
tion of geology in America: A bibliographical
survey. Mark W. PAnaporn, JR. 224.
Asa Gray and American geology. A. HUNTER
DUPREE. 227.
Darwinian natural selection and vertebrate
paleontology. JoHN A. WIxLson. 231.
Development of geologic thought concerning
Ulster County, New York. Jutes Friepman.
252.
Emergence of geology as a public function,
1800-1879. Witiu1am Back. 205.
Franklin as a physicist. RAyMonp J. SEEGER. 129.
Geology plus adventure: The story of the
Hayden Survey. J. V. Howe tu. 220.
Impact of the development of photogrammetry
upon geology. Davip LANDEN. 234.
Notes on the earliest geological maps of the
United States, 1756-1832. JouN W. WELLS.
198.
Remarks on the history of American petroleum
geology. Epcar W. Owen. 256.
The role of the Smithsonian Institution in
early American geology. Paut H. OrHsmr.
215.
The United States Geological Survey and the
advancement of geology in the public serv-
ice. THomas B. Nowan. 209.
Ichthyology. Bathypterois pectinatus, a new bath-
yal iniomous fish from the eastern Pacific.
Gites W. Meap. 290.
Description of a new sandfish, Kraemeria sex-
radiata, from Japan, with special reference to
its osteology. Kryomatsu. Matsuspara and
Tamotsu Iwat. 27.
Mycology. Two new species of Harposporium
parasitic on nematodes. CHARLES DRESCHLER.
106.
News of members. 53, 272, 371.
Notes and news. “Night-gowned” fishes, 33; Com-
pressive properties of human enamel and
dentin, 34; Experimental map papers con-
375
taining synthetic fibers, 35; “De-lousing”
shrimp, 40; Insects as flyers, 52; Archeology
salvage program in Chattahoochee Valley,
62; Grass primer reprinted, 62; Graphical
diagnosis of interlaboratory tests, 112; Bird
migration studies, 120; Excavations at La
Venta, 121; Dr. Friedmann awarded Elhot
Medal, 128; National Science Foundation
makes educational grant to Washington
Academy of Sciences, 164; Tracking camera
photographs Vanguard I in orbit, 171; Amer-
ican Institute of Chemists honor award, 182;
Fisher award in analytical chemistry, 196;
Former Academy president (Hrdlicka) me-
morialized, 272; R. E. Snodgrass honored,
331; Katmai area described, 332.
Obituaries. Clarence R. Shoemaker, 63; James
Herbert Hibben, 196.
Paleontology. Paleontologic record of the primary
differentiation 1m some major invertebrate
groups. Davin Nico, Grorce A. DEsBorouGH,
and JAMES R. Soniipay. 351.
*The effect of envionment on echinoid mor-
phology. Davin M. Ravp. 91.
Physics. Men and electrons. L. Marton. 98.
Plant physiology. Responses of certain fungi, par-
ticularly Trichoderma sp., to light. Ina P.
Bsornsson. 317.
Science administration.
CrawForp R. BusELu. 1.
JOURNAL OF THE ACADEMY OF SCIENCES
Pay plans and _ people.
vou. 49, no. 10
Zoology. A new Floridan Pectiniunguis, with re-
appraisal of its type species and comments
on the status of Adenoschendyla and Lito-
schendyla (Chilopoda: Geophilomorpha:
Schendylidae). R. E. Crasinu, Jr. 324.
A new species of Haloptilus (Copepoda: Ca-
lanoida) from equatorial and subtropical
waters of the east-central Pacific Ocean.
GerorGE D. Grice. 193.
Antrogonodesmus, a new chelodesmoid genus
from Cuba, and a redescription of Amphe-
lictogon doliuus Chamberlin (Polydesmida,
Chelodesmidae). Ricuarp L. HorrmMan. 284.
A review of the gorgonaean genus Placogorgia
Studer, with a description of Placogorgia
tribuloides, a new species from the Straits
of Florida. Frepertck M. Bayer. 54.
Millipeds collected enroute from Florida to
San Antonio, Texas, and vicinity. H. F.
Loomis. 157.
Muscles of the hip and thigh of the emperor
penguin. L. R. Serry. 183.
Notes on Mecistocephalus in the Americas,
with a redescription of Mecistocephalus
guildingu Newport (Chilopoda: Geophilo-
morpha: Mecistocephalidae). R. E. Crastr1u,
JR. 188.
Taxonomy of the copepod genera Pherma and
Pestifer. R. U. Gooprne. 122.
Three new cave amphipods from the West In-
dies. CLARENCE R. SHOEMAKER. 273.
Officers of the Washington Academy of Sciences
JOURS NECE 1 FRANK L. CAMPBELL, National Research Council
WTESCGERE-CIECL...........5..6- LawRENcE A. Woop, National Bureau of Standards
OES LTTE). woe) Heinz Sprecut, National Institutes of Health
OPE SUOE". Oh 0 W. G. BrompacHer, National Bureau of Standards
PMRENUMISE oa... ss.» Morris C. Lerxinp, Armed Forces Institute of Pathology
Custeazan of Publications............... Haratp A. ReHpER, U.S. National Museum
OIA ooh l6 OC CHESTER H. Paaes, National Bureau of Standards
MREACTSMEOU UO ic ok oe ee ecb eae eenes H. A. Bortruwicx, T. D. Stewart
| EEC OL Bourpon F. ScriBNeR, KeitH C. JOHNSON
TST 0) Puitip H. ABELSON, Howarp S. RaAapPLlEYE
Board of Managers....All the above officers plus the vice-presidents representing the
affiliated societies
CHAIRMEN OF COMMITTEES
Standing Committees
TIN Eo ee Frank L. CaMpBELL, National Research Council
RR RI ce cis a cis sk eo ic ev ae enss RautpH B. KENNARD, American University
Membership............ LawRENcCE M. KusuHner, National Bureau of Standards
WEGMOGTADAS.................. Dean B. Cowlsz, Carnegie Institution of Washington
Awards for Scientific Achievement....... FrAaNK A. BIBERSTEIN, Catholic University
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Encouragement of Science Talent.............. Leo ScuusBert, American University
Science Education............ RaYyMoOND J. SEEGER, National Science Foundation
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PENG PVGIAGIONS. .0....... 0000. c ecco ee Joun K. Tartor, National Bureau of Standards
Special Committees
2 7 age eee Harotp H. SHeparp, U. S. Department of Agriculture
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Space Administration
CONTENTS
Page
AstronoMy—Cepheid variables and the period-luminosity relation.
C. PAYNE-GAPOSCHEIN....... 22 5. 02 dss. op aba te Oe 333
PALEONTOLOGY.—Paleontologic record of the primary differentiation in
some major invertebrate groups. Davip NicoL, GEoRGE A. DESBOR-
oucH, and James R. SOLLMAY....-.:........- ee 301
Botany.—The Danthonia-Lichen-Moss community in Washington,
D.C., and vicinity. Sister JuLIA Marie Van DENACK and HER-
BERT WU, HANSON... 20)... 0.05 Dias ee oe 367
AGADEMY INEWS) (0.25). oe ee ae ns Ce ee ee 371
Inne ro Vouume 49. 2... one. oc st Re oe eee 373
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