TR-150

TECHNICAL REPORT

SUBMARINE SEDIMENT DATA COLLECTION
AND MANAGEMENT AT THE
U.S. NAVAL OCEANOGRAPHIC OFFICE

JOHN K. DUNCAN
Environment Branch

Oceanographic Analysis Division
Marine Sciences Department

AUGUST 1964

roe

; MoE U.S. NAVAL OCEANOGRAPHIC OFFICE
ho. 12-150 WASHINGTON, D. C. 20390
Price 75 cents

ABSTRACT

This report has been prepared for the use of persons studying
the composition of the sea bottom. It describes the source,
type, quantity, and geographic distribution of bottom sediment
information available at the U.S. Naval Oceanographic Office
and lists the principal types of charts which can be prepared
from such information. It also describes the forms in which
bottom sediment data appear and discusses their relative re-
liability in terms of the sampling device employed, the type of
analysis made, and the classification or description of the
sediment. Furthermore, this report describes the filing system
used to organize, control, maintain, and retrieve the data.

FOREWORD

This technical report discusses the collection, use, relative

reliability, and control of submarine sediment data at the U. S. Naval

Oceanographic Office. Data sources are listed and their geographic

distribution charted by one-degree quadrangles.

DENYS W. KNOLL
Rear Admiral, U. S. Navy

Commander
U. S. Naval Oceanographic Office

AYO

iil
O 0301 OO44498 5

i

MA

iii

TABLE OF CONTENTS

Page
RG TOW OT Cluvnsriet Wap halite itey fe Yeo fo! te) Nay, ta. Mo, fo te) Mo) Mey ts Melo SPeR Tel Mal hes: eats iii
JLRS OR IMYEAESCS 6 G6 GhiG dui Gu sonoma c Cai lath Parra Mich le ae vi
Mal CMe eiys, Wales io MOVCRE cetera Stometay mar vialca! aly! geen amore, Meo a) alr nmralt famine. vii
Teintroductiony seen. te FSA SUMS OOS Lee A IY, ERS 1
II. Major Sources of Submarine Sediment Data ..... 5 0 1
Mnanpublished Survey, Data: yo. sea el cee sia te See 1
B. Published Survey or Laboratory Data. ....... . 2
CreNauticaleG arts: 5... ) she) tsi w te) eel) ss ce ce 3
III. Bottom Sediment Chart Compilation ....... 5 O-comd 4
IV. Relative Reliability of Data ....... a lo Olko sake Oo 5
V. Collection, Filing, and Control of Bottom
Sechlenoints IDE! Vee ea ory: Gk Gabo bun: 6) Or Cad GO MORO 7
em GOllkection: Ofebataly oc) cps) sen) syne sein ene cen er a O60 q
ByOnganization ofsDatay ballet mmr. Meet tar eitoh sire he eae 14
Go GomGsell Oe IDEN Ap ob 6 ovo) 6 avo Gol eGo a5 0 0 20
ViteiGomposition of Data Collection™ 3. 2795 32 4 5 6 = « 21
Will, Jebiorpeeyynte INNS G4 G65 5 6 oo OOo OOO oo OOO 22

LIST OF FIGURES

Figure

i

10.

Ib 2s

W

13's

14,

Wisye

LO

U. S. Naval Oceanographic Office Sediment
Analysis Summary

Sample Analysis Emphasizing Water Content.

. Sample Classification Reported by an Italian Source .

. Biological and Mineral Composition of a Sample

Reported by British Source. ......

. Description and Grain Size Distribution of a Sample

Reported by a Swedish Source

. Description, Grain Size, and Organic Composition of a

Sample Translated from a Russian Source .

. Example of a Detailed Description of a Surface

Sediment Sample Reported in a Portuguese
IPWISICAEO “5 oo 5 6504600 560000060

. Example of Field Classification and Chemical Analysis

of a Core Reported in a Russian Publication .

. Example of Biological or Micropaleontologic Analysis of

a Sediment Sample...

Description and Phi Grain Size Distribution
OH 6, GOpe Serle 5 6 656 5615 6 0

Sample Description Reported in French.

‘Brief Field Classification of a Core Sample

Example of Graphic Representation of Core Analysis

Ten-degree Divisions of Marsden Squares

Five. and One-degree Divisions of Marsden Squares,

Eastern North Atlantic Ocean - Distribution of

Submarine Sediment Sample Analyses ......... oa

vi

Page

10
Wl

WL
11
M7

12

13
15
15

16
16
16
I 2
18

19

63

Wile

18,

Ge

20,

(adhe

ZZ.

43.

24,

(Ala,

Western North Atlantic Ocean - Distribution of Submarine
Sediment Sample Analyses

South Atlantic Ocean - Distribution of Submarine
Sediment Sample Analyses
Eastern North Pacific Ocean — Distribution

of Submarine Sediment Sample Analyses.

Western North Pacific Ocean - Distribution
of Submarine Sediment Sample Analyses .

Eastern South Pacific Ocean - Distribution
of Submarine Sediment Sample Analyses.....

Western South Pacific Ocean ~ Distribution
of Submarine Sediment Sample Analyses .

Indian Ocean - Distributuon of Submarine Sediment
Sample Analyses.

Arctic Ocean ~ Distribution of Submarine Sediment
Sample Analyses.

Seas around Antarctica - Distribution of Submarine
Sediment Sample Analyses

TABLE

Variation of Area of 1° Quadrangles with Latitude

vii

Page

65

67

69

val

73

UD)

CU

vy

81

62

a>\
vatuiye
ey

SUBMARINE SEDIMENT DATA COLLECTION AND MANAGEMENT AT
THE U. S. NAVAL OCEANOGRAPHIC OFFICE

I. Introduction

The primary purpose of establishing a bottom sediment data file
is to collect in one place all pertinent data in a form suitable for rapid
sorting and retrieval. It also unites on one card or series of cards all
of the information describing a particular sample or locations, since
the data may be scattered widely through many publications.

II. Major Sources of Submarine Sediment Data

There are three principal sources of bottom sediment information;
unpublished survey data; published survey or laboratory data reports
and data reported in the scientific literature, or in research reports;
and nautical charts.

A. Unpublished Survey Data

Unpublished survey data are the most difficult tolocate, acquire,
or use, Their existence is discovered, often by hearsay, by personal
contact with researchers in the field, and by conscientious and constant
perusal of the scientific literature for clues. Careful search for the
location of unpublished data and lengthy correspondence with the
Owners are usually required before they can be borrowed or copied.
Finally, since such data often are incompletely analyzed, unchecked,
handwritten and often illegible, and unsummarized, considerable labor
and expense are required to put them in intelligible and usable form.
The information about a single sample often is scattered through a
large number of laboratory analysis sheets, each reporting a single
operation or type of analysis such as organic carbon analysis; pipette
division of the fine fractions; sieve separation of the coarse grains;
mineral separation and identification; indentification of foraminifera;
measurements of wet density, plasticity, shear strength, chemical
composition, and radioactivity; and many- others. The field description,
geographic location, water depth, andtype of sampler often are recorded
on separate forms. The great difficulty of acquiring and processing
such unpublished data, except those available from Oceanographic
Office surveys, has caused effort to be concentrated primarily on
published data.

B. Published Survey or Laboratory Data

Descriptions and analyses of large numbers of sediment
samples appear in scientific journals, cruise reports, progress reports
of research contracts, and published data reports. Data are reported
in an infinite variety of tables, lists, graphs, histograms, profiles,
sections, summaries, and descriptions. The reported data often are
incompatible because they have been derived through many different
methods of analysis and are described in terms of different systems of
classification and units of weights and measurement. One example is
the basic classification of sediments in terms of mud, sand, gravel,
and rock which is subject to the following difficulties:

1. These terms may describe quantitatively measured and
computed grain size composition,or the observer’s opinion based upon
the appearance of the sample (wet or dry) or the feel of the sample,or
both. If the classification is based upon appearance and feel, its
accuracy depends upon many varying and indefinable factors such as
the observer’s bias, knowledge, and experience; the type and amount of
organic material; and the homogeneity of the sample. Experiments have
shown that even experienced geologists permit a small (less than 10
percent) proportion of clay, dark color, or stickiness to obscure the
dominant coarseness of a sand sample and will classify it as mud or
mud-sand.,

2. If the grain size of the sediment is measured in the labora-
tory, classification of the sample still is complicated by determination
of the range of grain sizes which defines a mud, sand, or gravel. Such
definitions are arbitrary, and no single system of classification has
become widely accepted. Attempts to equate English, metric, and
logarithmic (phi) scales of measurement cause additional complications.

3. A third source of disagreement in sediment classification
is in selection of the statistical parameters (mean, median, or mode
of the frequency distribution of grain sizes) used to classify a sample,
and the effect of the type and amount of deviation of the grain size
distribution from the normal (sorting, skewness, kurtosis). Some
geologists describe a sample composed of 70 percent sand sized
grains and 30 percent or more silt as a silty sand, while others would
classify the same sample as only a sand. Others adopt 20 or 10 percent
as the minimum proportion of silt to be classified as silty sand.
Some geologists use an elaborate descriptive system,using and often
mixing English terms with others of Latin and Greek derivation such

as pSammitic pellite (sandy clay), arenaceous lutaceous argillite (sandy
silty clay), or psephitic argillaceous calcarenite (gravelly clayey
calcareous sand), each denoting fairly specific proportions of each
particle size class.

4. Confusion also arises in combining particle size classifica-
tions with ones which denote chemical or mineral composition or
origin of the sediment. It is extremely difficult to determine exactly
what is meant by‘‘coral sand,’’i.e., whether it is coral (size of particle
may range from clay size to massive reefs) and sand, or sand sized
calcium carbonate grains of coral origin. Shell may describe mollusks
as large as giant clams or microscopic skeletal remains of pelagic
foraminifera. Rockand stone are very indefinite terms used to describe
a wide range of particle sizes, as well as solid bedrock outcrops or
reefs, Detritus, alluvium, and diluvium are terms which indicate
origin or mode of deposition, but they are used by many authors to
imply various particle size ranges. Volcanic ash and pumice indicate
origin and composition with unspecific grain size implications. The
terms mud and ooze are used in many different ways to indicate or
only to imply fine grain size, or to indicate plasticity, origin, or
composition.

5. Determination of exact English equivalents of foreignlanguage
terms is difficult and often impossible. The term “wadden” often is
used in European journals to describe tidal flat sediments, but some
authors restrict it to mud or silts and clays, others include sand
sized grains, and many use it without defining it. Russian scientists
are not consisteut in their use of terms such as mud, as the same
author (M. V. Klenova) equates it with silt on one page, equates it with
silt and clay on another, and uses it on a third page in a very general
sense of a “muddy” sediment which may include large proportions of
sand, gravel, pebbles, and shell. Thus, the lack of consistency in
analysis, definition, and reporting of bottom sediment data makes it
very difficult to adapt machine methods economically to their storage,
retrieval, and analysis.

C. Nautical Charts

Abbreviated designations of bottom type appear on nearly all
U. S. and foreign nautical charts. The notations of bottom material are
made from field descriptions of samples obtained in the course of
hydrographic surveys. Few of them are based upon laboratory analysis
of samples. They are subject to all of the inconsistencies listed above.
However, they are the only type of sediment information existent in

sufficient quantities to permit drawing boundaries between different
sediment types. U. S. nautical chart notations of bottom material have
been defined by W. H. Berninghausen* and his definitions are used as
the basis for geologic interpretation of these data in the Naval
Oceanographic Office.

The number of sediment notations on nautical charts varies
geographically with water depth, Since hydrographic surveys are made
primarily to locate dangers to navigation and to chart areas of shoal
water having depths less than the draft of ships, most soundings and
consequently bottom sediment notations are in shoal nearshore waters
of 25 fathoms or less. The number of nautical chart notations also
depends on the country which produces the chart. Japanese and
Portuguese charts are remarkable for printing a notation of the bottom
type for almost every sounding. On some Japanese and Portuguese
large scale nearshore charts, notations exceed 50,000 per one-degree
quadrangle. Such density of information permits highly exact and
detailed delineation of sediment types.

The use of bottom notations on foreign nautical charts is complicated
by the language barrier. Nautical chart notations appear in 16 major
foreign languages (not including national variations such as between
Spanish and Argentinian) and pose the dual problem of translation to
English and of determining if the definition of the foreign term is
fully equivalent to the definition of the English term. An example of
this problem is “st.” which is “stein” on German charts and “stone”
on British Admiralty charts. It is difficult to determine whether the
British use “stone” as synonymous with “rock” to denote a specific

range of grain size, or generally to include material ranging from fine

gravel through boulders to bedrock reefs, or possibly to indicate lack
of specific knowledge of the bottom except that it is hard. It is even
more difficult to determine if the German use of the term corresponds
to the British use, and to equate both to some term in the U. S. classi-
fication of bottom materials, which does not include “stone” as a
separate category.

III, Bottom Sediment Chart Compilation

Several types of bottom sediment charts can be prepared showing
the geographic distribution of various properties of submarine surface
sediments. However, only four major types of sediment charts can be

SN a NP ee aD ise
*BERNINGHAUSEN, W. H. The Quality of the Bottom, a Glossary of

Terms, U. S, Navy Hydrographic Office, SP-56, 11 p., November 1961.
Washington, D.C.

prepared from nautical chart notations of bottom type. One
type shows bottom material classified descriptively as mud, sand,
gravel, rock, coral, shell, and various combinations of these, Another
can show the quality of the bottom in terms of hard, soft, sticky, rough,
etc. The third can show sediments classed according to origin and
composition, i.e., shell, coral, volcanic material, oozes (globigerina,
radiolarian, diatom, pteropod), blue mud,and red clay. The fourth
type of chart can show sediment color,

Charts can be prepared for limited areas showing the surface
distribution of other properties of submarine sediments suchas mineral
composition, chemical composition, statistical grain size parameters,
radioactivity, engineering properties, organic content, species of
planktonic foraminifera, paleomagnetism, and many others, Other
charts can show the vertical variations of these properties in the
bottom. However, such charts require information from cores and
carefully collected and analyzed sediment samples which are available
in sufficient quantities only for small areas. For most of the oceans
and seas such data can be presented only for widely scattered specific
locations, and no meaningful boundaries can be drawn showing the
extent of or change in any parameter except on very large scale charts
of small areas.

IV. Relative Reliability of Data

The value of bottom sediment data depends upon how reliably the
samples represent the population (sea floor) from which they are
drawn. Sediment data reliability varies according to sampling design,
type of sample, sampling instrument, accuracy of the ship’s position,
handling, movement and storage of sample, type of analysis, and
initial purpose of collecting the sample. Rarely can the effect of all of
these be evaluated for a particular sample or suite of samples. Usually
only an estimate of how representative a sample is can be made.

Sediment data can be divided into three major reliability groups,
which are relative and often overlap:

A. The best data are those obtained from laboratory analysis of
core samples. These are usually less distorted inthe sampling process
than other types of samples and therefore more representative of the
sediment as it exists on the sea floor. Core samples are usually more
carefully handled and analyzed than other types because of the longer
time requirements and greater expense of obtaining them. Considerable
differences in reliability exist between different types of coring devices
(gravity, piston, vibro-piston, hydrostatic) and the type of material
sampled, Coarse grained and hard sediments such as coarse sand,

gravel, and rock are difficult to core, andoften poor samples or none at
all are obtained. For hard coarse materials (gravel, sand) a scoopfish
or bucket dredge may obtain the most representative sample.

B. Generally less representative than cores are dredge, trawl,
grab or snapper, and scoopfish samples, even when carefully analyzed
by conscientious and competent persons, The grab and snapper samples
usually destroy the structure of the sediment and often bias the grain
size distribution toward coarser sizes by winnowing or washing in the
sampling process. Trawls and dredges also may bias the size distri-
bution by preferential selection of certain sizes. However, they provide
composite samples of the submarine bottom material over an area
or along a track. While such a composite sample is not representative
of the material at any specific spot, it probably is more representative
of the range of material in a region than one or even several cores,
Therefore, one composite sample might better describe the bottom
materials of a given area than one core sample, but ten core samples
would describe more accurately the materials of the same area than
would ten composite samples.

C. The poorest data and the most numerous are abbreviated nota-
tions of types and consistency of bottom materials which appear on
boat sheets, compilation sheets, and printed nautical charts. Most
of them are cursory identifications of small samples, often only a few
grains, brought up on sounding leads in the course of hydrographic
surveys. The identifications of these inadequate samples are made
routinely by enlisted naval personnel who usually have little or no
scientific training insedimentary petrology or mineralogy. Navigational
positioning errors are compounded by cartographic compilation and
printing errors, Although some of the notations are highly reliable
and accurate abbreviations of field descriptions of samples from the
other two groups, they usually cannot be distinguished from the
majority of less reliable data and must be classed with them. The total
effect of all of these possible sources of errors significantly reduces
the reliability of bottom sediment charts based solely upon nautical
chart notations. The charts become much more reliable when chart
notations are substantiated by numerous and well-distributed core and
grab samples.

The bottom sediment data collection maintained by the U. S. Naval
Oceanographic Office (apart from chart compilations) consists almost
entirely of data of the first two classes. Data in the third class are
included only when reported in professional journals (such as Annalen
der Hydrographie, Deutsches Hydrographisches Zeitschrift, and Annales

Hydrographiques) or in the scientific literature, where exact positions
are given and some evaluation can be made of their validity (Figures
Zp, Only) and) 12).

Nautical chart notations are compiled region by region from foreign
and domestic charts of all scales from 1:5,000 harbor charts to
1:10,000,000 charts covering large ocean areas, The compilation bases
are acetate or tissue overlays placed on large or medium scale
nautical charts on which the notations are assembled from all available
charts which cover portions of the area of the base chart, The numbers
and nationality of the chart sources are listed on each overlay, and
notes indicate overlaps on other compilation bases. When completed,
photostatic reductions of the overlays are made. These are filed
together with other miscellaneous geologic data numerically in folders,
each of which corresponds to a single sheet of the worldwide strategic
plotting chart series,

V. Collection, Filing, and Control of Bottom Sediment Data

Bottom sediment data are analyzed and published in such a great
variety of forms that coding or conversion of data to machine punch
cards is impractical until some international agreement is reached
on uniformity in reporting geologic data. for this and other reasons,
manual filing of data on 5" x 8" index cards was adopted.

A. Collection of data -= Bottom sediment data are assembled
through systematic search of the published scientific literature and by
acquisition, whenever possible, of unpublished data reports, field
notes, laboratory analysis summary sheets, survey data records,
intelligence reports, and ship logs. Progress in the search is recorded
on a 3" x 5" card, one for each journal or series of reports examined
which contains bottom sediment data. On the cards are listed the
volumes, years, and issue numbers which have been searched and
from which all data have been abstracted, The following journals
often contain submarine geologic information and have been partially
or completely searched to date. This is far from a complete list,
and new ones are added when found. It does not include the many
sources of data which are not published serially.

American Association of Petroleum Geologists, Bulletin
American Journal of Science

Antarctic Record (Japan)

Archiv der Deutschen Seewarte

Australian Journal of Marine and Freshwater Research

Centre de Recherches et d’Etudes Oceanographiques, Cahiers du

Commercial Fisheries Review

Consejo Oceanografico Ibero Americano, Memorias del

Deep Sea Research

Deutsche Hydrographische Zeitschrift

Geographical Review

Geographical Journal

Geological Society of America, Bulletin of

Geology, Journal of

Geophysics

Geophysical Research, Journal’ of

Gosudarstvennogo Okeanograficheskogo Instituta, Trudy

Grdnland, Meddelelser om

Hydrographie und Maritimen Meteorologie, Annalen der

Hydrographiques, Annales

Instituta Okeanologii, Trudy

Institute Oceanographique (Monaco), Annales

Institute Oceanographique (Monaco), Bulletin

Instituto Espanol de Oceanografia, Boletin del

Instituto Espanol de Oceanografia, Trabajos

Japanese Journal of Geology and Geography

Limnology and Oceanography

Marine Biological Association (UK), Journal of

Marine Research, Journal of

New Zealand Oceanographic Committee, Publications

Okeanologiya

Oceanografiska Institutet i G¢teborg, Meddelander fran

Oceanographical Society of Japan, Journal (Nippon Kaiyo Gakkaisi)

Oceanologia et Limnologia Sinica

Ozeanographie (Deutsches Hydrographische Institute)

Records of Oceanographic Works in Japan

Science

Scottish Geographical Magazine

Scripps Institution of Oceanography, Bulletins

Scripps Institution of Oceanography, Contributions

Sedimentary Petrology, Journal of

Sedimentology

Station Marine d’EndOume, Recueil de Travaux

Vsesoyuz Nauchno-Issledovatel'skiy Instituta Morskogo
Rybnogo Khozyaistva i Okeanografia, Trudy

Woods Hole Oceanographic Institute (MIT) Papers in
Physical Oceanography

Woods Hole Oceanographic Institute, Technical Reports

Data from these sources are abstracted and recorded on the 5%
x 8" data cards, or negative photostats are made of relevant tables,
figures, or pages of text and stapled or glued to the cards. Usually only
one sample is recorded on each card, front and rear; however, very
detailed analyses sometimes require several cards which are clipped
or stapled together. Where two or more samples are taken at a single
location by the same ship, they may be recorded on a single card
even if they are different types of samples (Figure 5), Occasionally,
when a very close sampling design is followed ona survey, several
samples are recorded on a single card, but only if they are located
within a single degree of latitude and longitude (Figures 2,3, and 4).

Several representative examples of the types of data and forms in
which bottom samples are recorded on data cards are shown in Figures
1 through 12, The U. S. Naval Oceanographic Office summarizes most
of its sediment data as shown in Figure |. Only the results of engineer-
ing tests (Atterberg limits, unconfined compression strength, vane
shear strength, and consolidation rate), which are made ona few
samples, are reported on a different form. A photostatic reduction of
the summary sheet is made to mount it onthe 5" x 8" data card,

Figure 2 presents an example of a core analysis (Code 47) which
gives the representative median grain size and sorting coefficients;
however, the water content is the only sediment property for which
the vertical variation is given. In Figure 3 data from an Italian source
(Code 276) shows field classifications of eight shallow water samples
of the surface sediment which were obtained within the one-degree
quadrangle 44°-45°N, 12°-13°E. Such data are more reliable than
nautical chart notations only because the source is identified anda
scientist (Mario Picotti) has classified the sediment samples. A
third sample (Code 20, Murray and Chumley, 1924-1926) in Figure 4
classifies a pelagic sediment sample and reports its mineral composi-
tion and the relative proportions of various types of organic remains.

In Figurel0a shallow water core sample obtained during ATLANTIS
Cruise 21 (Code 172) gives a field description of the core, the median
and mean grain size, the size sorting coefficient, and the percentage
distribution of grain sizes using the phi notation for three representa-
tive subsamples. A summary description of a deepwater core (Figurel1)
is reported from a French source (Code 138). A qualitative classification
of a deepwater sample obtained by the ATLANTIS Cruise 151 is of
limited value because of the paucity of information and no indication
as to type of sample (Figure 12).

1. SAMPLE HUMBER 10 7.N. Gill 5. SAMPLER TYPE Orange Peel

2. LATITUDE 29° 40 00 6. WATER DEPTH (fm.) 15.
3. Loncitune O80 45 00 7. CORE LENGTH (in.)
4. DATE (Day, month, year) 26 April 1953 « CORE PENETRATION (in.)

11. COLOR Pale Olive
10 Y 6/2

12. ODOR

15. MAXIMUM POROSITY (%) 45

16. MINIMUM POROSITY (%) 35

17. WATER CONTENT (%)

18. ORGANIC CARBON CONTENT (%)

19. SIZE ANALYSIS AND STATISTICAL MEASURES

a (%)
b. -24 to -1, (%)
c to 04 (%)

h. 4, to 6, (%)
i. 6, to By (%)
j. > 8, (4)

. SUBSAMPLE DRY WEIGHT (am)

. SPHERICITY (avg. )

. ROUNDNESS (avg. )

23. SURFACE TEXTURE (ava. )

. DOMIKANT MINERAL (%)

. SECONDARY MINERAL (%) Shell 20

. OTHER MINERALS (%)

27. REMARKS:

Gill Il, Station No. 20—Regular
Large shell framents up to 5 cm.

FIGURE 1 U.S. NAVAL OCEANOGRAPHIC OFFICE SEDIMENT ANALYSIS SUMMARY

10

CODE 47 MS 152

LATITUDE LONGITUDE BOTTOM SEDIMENTS OFF
43°05’N 70° 42°W PORTSMOUTH, NEW HAMPSHIRE
(APPROX) 1947

WATER CONTENT AND LIQUID LIMIT RESULTS

WATER CONT. WATER CONT. WATER CONT. WATER CONT. MED. SORT.
STA. TOP MIDSEC. BOTTOM OF LIQ. LIMIT DIAM. COEFF.SO LOG SO
83 127.0 143.0 160.0 117.9 0.00295 29) 0.46

FIGURE 2 SAMPLE ANALYSIS EMPHASIZING WATER CONTENT

CODE 276 PICOTTI, MARIO MS 179

DATE: (9, 13) 16/8/55 (10) 17/8/55 (12, 14) 20/8/55 (10B, 12B, 12-15) 9/9/55

STA. NO. LAT. N. LONG. E. DEPTH (M) TYPE OF BOTTOM
9 Ave e58°! 100 1. S55 Co 24.5 FANGO
10 44. 58 00 12, 4554) Gioe 3 SABBIA FANGOSA CON ARGILLA
12 44 48 DA 12) 248° 1336 34.5 FANGO GRIGIO
13 Ab— ghd AS 12038) SO 30 FANGO GRIGIO
14 “ay G3 24 12 frr4it = 100 33 FANGO GRIGIO
10B 44. 58 00 12 1 €54, 00 33 SABBIA FINE
128 44. 4824 1:2" > hee/AB wn hs36 32 ARGILLA
12-15 AAD e489, 654 126 ihe 55eae 00 37 FANGO POCA SABBIA

FIGURE 3 SAMPLE CLASSIFICATION REPORTED BY AN ITALIAN SOURCE

CODE 20 MS 146

1107 S. S. “BRITANNIA”’
SOUNDING 396, JULY 18, 1899, LAT. 46°22'35”N., LONG. 18°51'56”W., 2522 FATHOMS.

GLOBIGERINA OOZE, LIGHT BROWN, SLIGHTLY COHERENT.
CALCIUM CARBONATE (82-65%), PELAGIC FORAMINIFERA (78%), BOTTOM FORAMINIFERA
(2%), OTHER REMAINS (2-65%), INCLUDING OSTRACODS, ECHINOID SPINES,
COCCOLITHS, RHABDOLITHS, COCCOSPHERES, FRAGMENTS OF LIMESTONE.

RESIDUE (17-35%), BROWN—
MINERALS (5%), M. DI. O-O8 MM., ROUNDED AND ANGULAR; PRINCIPALLY QUARTZ
GRAINS, WITH ROCK FRAGMENTS, PUMICE, VOLCANIC GLASS ETC.
SILICEOUS REMAINS (2%), RADIOLARIA, SPONGE SPICULES, DIATOMS, IMPERFECT

CASTS.
FINE WASHINGS (10-35%), AMORPHOUS CLAYEY MATTER WITH FINE MINERAL

PARTICLES.

FIGURE 4 BIOLOGICAL AND MINERAL COMPOSITION OF A SAMPLE REPORTED
BY A BRITISH SOURCE

ili]

CODE 214

ALBATROSS 1947-48

MS 024

04°45’N., 128°08’E. WATER DEPTH 7710 METERS (MINDANAO TROUGH)

CORE NO. 108 CORE LENGTH—390 CM.

DEPTH IN
CORE CM.
0-3.5 GREY-BROWN SAND. DEEPEST PART OF CORE PROBABLY A MUD
3.5-285.5 GREYISH GREEN CLAY AND SILT WITH | FLOW. NEXT ABOVE ARE GRADED SAND LAYERS
SEVERAL DARK LAYERS. (TURBIDITY CURRENTS—KUENEN). THESE BEDS
285.5-360 SEVERAL LAYERS OF DARK SAND CON- COVERED BY 3 METERS OF FINE-GRAINED TER-
TAINING SILT AND CLAY. SOME RESTRIAL MUD WITH MINOR AMOUNTS OF
LAYERS BECOME COARSER WITH DEPTH. | VOLCANIC GLASS AND ORGANIC SILICA. A
EretiomenuNere SM Sane LAYER IS ABOVE ALL. COARSE
360-389.5 IRREGULARLY MIXED SAND, SILT AND oe Pua NERS ES ergs
CLAY—LIGHT PARTS ARE FINER THAN 7c
THE DARK ONES.
PARTICLE SAMPLE DEPTH (CM.) WT. % OF DRY, SALT FREE SEDIMENT
SIZE MM.
<.006 2 pep 5iuies 63 uuerl545gur52 5m 207 OO REG OGRENES 24034200 CMO
006-.02 5.7 49.2 56.2 36.0 3.9 IAA FAA 166
02-06 19 19.0 16.5 15.2 2.2 a5 a1 E28 20a) 72
06-.125 85 950 TOO 11 SIO 650 92 240 15.9
Wee AS NO, Al Gd) 150 BO son 70 SR On 201 236
25-.5 539 Cheeses Om eo m0/6 ADVE 2 508163 16:4 27-77 Alias
5-1.0 ise) = S02 = Ol ax Shi GENS 124 102
1.0-2.0 O05 = = = = an OS Wl Or Ts 3.2
72.0 - - - — - ex - 20 98 — —
Be ee x Be yg a =) AON BO = =
FIGURE 5 DESCRIPTION AND GRAIN SIZE DISTRIBUTION OF A SAMPLE REPORTED
BY A SWEDISH SOURCE
CODE 262 PERSEY MS 283
78°37.3'N. STA. DEPTH ORG. MAT. % PETERSEN DREDGE
55° 20'E. NO. (M) c NIw C/NI™="co2 BROWN SANDY MUD
1927-31 1261 207 79.4. Ally aye Za gh O5 CORE 0-4 CM BROWN SANDY MUD
4-16 CM. GREENISH-GREY MUD
16-25 MM. DARK GREY CLAYEY MUD
SURFACE SAMPLE
% GRAIN SIZE %
M.M. M.M.
>I 27 <0.01 16
0.1 1 <0.01 30
0.05 26

FIGURE 6 DESCRIPTION, GRAIN SIZE, AND ORGANIC COMPOSITION OF A
SAMPLE TRANSLATED FROM A RUSSIAN SOURCE

12

CODE 163 MS 005

02°59’N. 49°20'W

ae ae
A um Ne ae ar
<t °
ZL ZL —
= 809 OS) ©) 08 Zo
a = Om~- <& z Ze, z
pie retro ae Oat" "B78 Q Q3-Q)
¢ = Of Bs 9% 2 Zz O = 1 Q3 MEDIANA SORTING
5 9 a Ew <2
PR ES, 19.0,) |. 210, ue z
Sl A GY 166 “16 ODO OOS is Oi Ores “ORI 12 — O05

A
311—AREIAS CONCHIFERAS DE COR CINZA E BEIGE, COM 84% DE AREIA E 16% DE
CALCARIO.

NATUREZA MINERALOGICA DOS GRAOS:

NA MAIORIA QUARTZO CRISTALIZADO OU TRANSPARENTE, COM POUCAS MICAS BRANCAS
E ALGUMAS BIOTITAS MARRON MAIS OU MENOS ALTERADAS.

GRAOS DE ARENITO PARECENDO ANTIGO.

GRANDE ABUNDANCIA DE MINERAIS PESADOS.

MORFOLOGIA DOS GRAOS:
OS GRAOS SAO TODOS UM POUCO DESGASTADOS, TENDO A FRAGAO GROSSA 20 ATE
30% DE ‘‘ARREDONDADOS BRILHANTES”, SENDO ALGUNS FOSCOS.

ORGANISMOS:

GRANDE QUANTIDADE DE ORGANISMOS PLANETONICOS E BENTICOS.

CONCHAS DE LAMELIBRANQUIOS, GASTEROPODES E LARVAS.

ECHINODERMOS-FRAGMENTOS DE ESPINAS E UM PEQUENO TIPO DE ECHINODERMO
INTEIRO, DE 8 MM. DE DIAMETRO.

ALGUNS COPROLITOS.

OSTRACODES—ESPICULAS SILICOSAS DE ESPONJAS, FORAMINIFEROS, ARENACEOS E
PLANCTONICOS.

GLOBIGERINAS, ORBULINAS, ETC., SENDO ALGUMAS CHEIAS DE MATERIAL FERRUGINOSO
OU PRETO.

NOTA:

OBSERVA-SE UMA CONCHA ANTIGA, CHEIA DE UM ARENITO CALCARIO ANTIGO, COM
GRAOS BEM ARRENDONDADOS. SEM DUVIDA O REVOLVIMENTO DE UMA FORMACAO MAIS
ANTIGO.

2— —FRACAO FINA:

ENCONTRA-SE SILTES, ARGILAS E MICAS EM FOLHETOS FINOS, ALGUMAS ESPICULAS
SILICOSAS, COM CANAL CHEIO DE TERRA FERRUGINOSA. ALGUMAS VEZES OBSERVA-SE O
INICIO DE RECRISTALIZACAO DA SILICA AMORFA QUE COMEGA A SE POLARIZAR. NOTA-SE
TAMBEM ALGUNS “‘COCOLITOS'’ SENDO UM PERFEITAMENTE CONSERVADO, ENQUANTO
MUITOS OUTROS APRESENTAM-SE FRAGMENTADOS NA LAMINA ESTUDADA.

FIGURE 7 EXAMPLE OF A DETAILED DESCRIPTION OF A SURFACE SEDIMENT
SAMPLE REPORTED IN A PORTUGUESE PUBLICATION

13

An example of a sediment analysis that is primarily biological and
consists of a listing of the species whose skeletal remains have been
identified in the sample is provided by Figure 9.

Figure 6 provides examples of samples reported in Swedish and
Russian publications, A long core from one of the deepest ocean trenches
is reported by the Swedish Deep Sea Expedition (Code 214) and gives
a field description of the color and grain size classification, a descrip-
tion of the origin of the material, and the percentage of grains in
various size classes at different levels in the core. The Russian
publication (Code 262) reports both a core and a dredge sample taken
at the same location in the Barents Sea.In this example the information
was abstracted from several widely separated pages in the publication,
translated, and assembled on one card, a very laborious task.

Another example of treatment of Soviet data is shown in Figure 8.
Here the Russian has been transliterated and translatedfor this report;
however, on most of the data cards the information appears in the
Cyrillic form and has been neither transliterated nor translated.
The widespread ignorance of Russian among Americans greatly limits
the use of such data except where translation facilities are available.

Figure 7 is an example of a long description of a sample in Portu-
guese. Here the language is less of a barrier to English speaking
researchersthan in Figure 8 but still may cause some difficulty for
those unfamiliar with Romance languages.

Another problem in handling sediment data is the reproduction of
graphic portrayals of samples(Figure 13). Placing such information on
individual sample data cards is complicated further when the original
is in color, which cannot be reproduced photostatically.

B. Organization of data file -- The datacards are filed geographic-
ally by using the Marsden square system (Figures 14 and 15), The
first order division is by 10-degree squares, the second by 5-degree
squares, and the third by l-degree squares, Five-degree square divi-
sions have been used to date in only a few 10-degree squares in which
there are too many cards for convenient manual sorting. It has not
been necessary as yet to use the l-degree square breakdown. The
Marsden square number is entered on the upper right-hand corner of
the data card.

14

CODE 94 MS 176

CORE NO. 10, DEPTH 1708 M. 42°30'N., 40°25/E.

Or
= Mm 25
28 OL SEtO
20 CHARACTERISTICS OF THE b3Zeu
= w SEDIMENT el OS ee
& 6 Eaabz oO cy ¥
a0 TOO CGE a|o < rt
20-30 IL GLINISTII, SERII S PROSLOYAMI. SOVRE- 0.87 0.445 0.038 17.86 8.2
MENNIYE OTLOZHENIYA. (CLAYEY MUD,
GREY, WITH LAYERS. CONTEMPORARY
SEDIMENTS.)
90-100 IL GLINISTII, SERII, S PROSLOYAMI, DREV- 1.39 0.285 0.025 18.33 8.6
NECHERNOMORSKIYE OTLOZHENIYA.
(CLAYEY MUD, GREY WITH LAYERS. EARLY
BLACK SEA SEDIMENTS.)
220-230 i 0.91 0.244 0.023 18.4] 8.1
310-320 : 1.03 0.223 0.022 17.31 8.1
480-490 z 0.75 0.325 0.036 12.75 8.1
595-605 IL GLINISTII, SERII, S PRIMEC'YU ALEVRITA. 0.79 0.184 0.021 10.17 8.0

NOVOYEVSKINSKIYE OTLOZHENIYA.
(CLAYEY MUD, GREY, WITH A MIXTURE
OF SILT. NOVOYEVSKINSK SEDIMENTS.)

710-721 IL GLINISTH, SERII, ODNORODNII. NOVOY- 0.45 0.222 0.028 9.39 7.9
EVSKINSKIYE OTLOZHENIYA. (CLAYEY MUD,
GREY, HOMOGENOUS. NOVOYEVSKINSK
SEDIMENTS.)

FIGURE 8 EXAMPLE OF FIELD CLASSIFICATION AND CHEMICAL ANALYSIS OF A
CORE REPORTED IN A RUSSIAN PUBLICATION

CODE 125 MS 465

DATE—12TH DECEMBER, 1912

POSITION—LAT. 42°381/2’S. LONG. 148°41 1/2’E.

DEPTH—1,320 FATHOMS

DESCRIPTION—GREEN TERRIGENOUS MUD, WITH SPONGE-SPICULES AND FORAMINIFERA;
MUCH DECOMPOSING MATTER.

COMPOSITION:—
CARBONATE OF LIME
PERCENTAGE FORAMINIFERA OTHER ORGANISMS
72-85 BILOCULINA, MILIOLINA, SIGMOILINA, PLANISPIRINA, A FEW LARGE COCCOLITHS, NUMEROUS
BULIMINA, VIRGULINA, BOLIVINA, CASSIDULINA, ECHINOID SPINES. OSTRACODA ABUN-
EHRENBERGINA, LAGENA, NODOSARIA, TRIPLASIA, DANT (AGLARIA, PONTOCYPRIS, ARGIL-
CRISTELLARIA, POLYMORPHINA, UVIGERINA, SAGRAINA, LAECIA, MACROCYPRIS, BYTHOCYPRIS,
GLOBIGERINA, ORBULINA, PULLENIA, SPIRILLINA, BAIRDIA, CYTHERE, KRITHE, LOXOCON-
DISCORBINA, ANOMALINA, TRUNCATULINA, PULVINU- CHA, XESTOLEBERIS, CYTHERURA, CY-
LINA, ROTALIA, NONIONINA, POLYSTOMELLA, AND THEROPTERON, BYTHOCYTHERE, PSEU-
HETEROSTEGINA. DOCYTHERE, CYTHERIDEIS, XIPHICHILUS
AND CYTHERELLA.
RESIDUE -
PERCENTAGE SILICEOUS ORGANISMS FINE WASHINGS
27-15 ARENACEOUS FORAMINIFERA (PELOSINA, RHIZAMMINA, SPONGE-SPICULES AND TERRIGENOUS

NOURIA, REOPHAX, HAPLOPHRAGMIUM, TEXTULARIA, SAND.
GAUDRYINA, TROCHAMMINA AND CLAVULINA).
SPONGE-SPICULES AND A FEW RADIOLARIA.

FIGURE 9 EXAMPLE OF BIOLOGICAL OR MICROPALEONTOLOGIC ANALYSIS OF
A SEDIMENT SAMPLE

15

CODE 172 ATLANTIS 21
CRUISE &
STATION DATE LATITUDE LONGITUDE
NUMBER (N) (W)
21 6-20-56 28°57’ 89°07’

PHI @ CLASSES (%)
0 1 2 3 4 5 6 7 8

21 +1 CUMULATIVE TO 5.24 1.28 10.03 19.12 15.37
+42 0.06 0.42 0.46 8.88 30.55 12.80 9.45 8.52
+3 0.09 0.24 0.55 8.91 24.74 15.47 9.82 9.76

CORE 56-14-21—PREDOMINANTLY TAN-GRAY CLAYEY SILT. TOP SEVEN
ERED.

WATER
DEPTH
(FT)

60

9

11.61
10.80
12.50

BOTTOM
SEDIMENT
SAMPLE
G(31)
10 MD®@ MS
37.33) 80 7.7
2.16 5.7 7.2
0.77 +6.0 7.3

INCHES THINLY LAY-
REMAINDER OF CORE OF HOMOGENOUS SILT EXCEPT FOR THIN LAYER OF SILTY

CLAY AND ORGANIC MATERIAL AT 20 INCHES. VERY FINE SAND 5% TO 10% IN SAMPLES.

SAMPLES AT SURFACE, 13, AND 25 INCHES. LENGTH, 27 INCHES.

FIGURE 10 DESCRIPTION AND PHI GRAIN SIZE DISTRIBUTION OF A CORE SAMPLE

CODE 138
CAROTTE 251 PROVENANCE: ATLANTIQUE EQUATORIAL
STATION 356 POSITION 00°33/N.; 37°06.5’W.

PROFONDEUR: 4,540 M.
LONGUEUR: 940 CM.

MS 004

ARGILE ROUGE CALCAIRE (DE 0% A 60% CO3CA) AVEC, A CERTAINS
NIVEAUX, DES QUANTITES PLUS OU MOINS IMPORTANTES DE BOUE BLEUE.
LA TENEUR EN FER (FE 203 RAPPORTE AU SEDIMENT SANS CALCAIRE) VARIE

DE 4% A 8% AVEC UNE VALEUR MOYENNE DE 7%.

MS 110-2

ATLANTIC OCEAN 7/12/47— 6/ 18/48

FIGURE 11 SAMPLE DESCRIPTION REPORTED IN FRENCH
CODE 51 ATLANTIS 151
LATITUDE LONGITUDE ATLANTIS CRUISE 151
30°07’N. = -17°27'W.
DEPTH (FM) SEDIMENT DESCRIPTION
2387 SOFT BROWN MUD

FIGURE 12 BRIEF FIELD CLASSIFICATION OF A CORE SAMPLE

16

MS 081

SO@

1.7
2.9
2.9

CM.

100

200

300

400

500

600

700

CODE

\
IN

SSX

DSSS)

5

PROBE
NO.

=

wOonNnaunh WO —

220

PROBE
NO. 1

NO.2 g00

900

1100

1400

<0.2

15
17
12
13
19
21
24
25

WJ

V)VDW\

—_

0.2-0.63

13
12
15
29
22
15
11
17

ALBATROSS 1947-48 MS 005
06°17'N., 43°20'W. WATER DEPTH—4490 METERS

FORAMINIFEROUS RED CLAY

RED CLAY

BLUE MUD

SAND

PROBE
NO. SEDIMENTTIEFE SEDIMENTART
LOTKERN NR. 255
1 20.6- 25.8 CM. FORAMINIFERENREICHER
ROTER TON
2 90.0- 95.2 CM. ROTER TON
3 D372 39=2) CMs SANDIGER BLAUSCHLICK
4 297.2- 298.2 CM. SAND
5 504.1- 511.5 CM. ROTER TON MIT FORAMINI-
FEREN
6 575.9- 583.2 CM. ROTER TON
7 583.2- 586.8 CM. TUFF IN ROTEM TON
9 833.9- 840.7 CM. ROTER TON
12 1255.4-1261.7 CM. ROTER TON MIT AGGREGA-
TEN
13 1295.2-1304.9 CM. BLAUSCHLICK
KORNGROSSENKLASSEN IN ©
0.63-2 2-6.32 6.32-20 20-63.2 63.2-200 > 200
23 17 13 10 4 5
13 15 19 23 1
14 52 Za
22 19 10 3 1 3
22 24 10 2 1
26 24 12 1 1
26 22 12 5)
27 24 6 1

FIGURE 13 EXAMPLE OF GRAPHIC REPRESENTATION OF CORE ANALYSIS

aly/

SIYVNOS NAGSYVW JO SNOISIAIG 3349I3G-NaL vl JYNO!d

01 02

18

(o)

NORTH LATITUDE

SOUTH LATITUDE

WEST LONGITUDE EAST LONGITUDE

WEST LONGITUDE EAST LONGITUDE

FIGURE 15 FIVE-AND ONE-DEGREE DIVISIONS OF MARSDEN SQUARES

19

SOUTH LATITUDE © NORTH LATITUDE

°

10

C. Control of data -- Control of the data is accomplished by use
of a card file of bibliographic sources, a tally card file, and a log
book of sources coded and keyed to bibliographic and data cards.

The bibliographic file is a complete record ofall sources, published
and unpublished, from which data have been obtained. Each biblio-
graphic card contains the complete bibliographic citation including the
library which owns the reference; the ship, expedition, or operation
which collected the samples; the date of the survey; the bibliographic
code number; alistof cross references; andcertain pertinent comments.
The comments usually indicate the number and types of samples
reported in the source and the numbers of the 10-degree Marsden
squares in which the data are filed. The cross references are kept toa
minimum and key the geographic area (sea, gulf, bay, etc.) of the survey
(unless it is worldwide or oceanwide), the ship or ships, expedition,
operation code names, and author(s) of the report to the bibliographic
card, When small station location or sediment distribution charts
appear in the sources, reduced copies are made and fastened to the
bibliographic card,

The library from which the source publication was obtained is
indicated on the card (preceding the call number)as follows: NAV
OCEANO - Naval Oceanographic Office, USCGS - U. S. Coast and
Geodetic Survey, LC - Library of Congress, USGS - U. S. Geological
Survey, DI - Department of the Interior, SI - Smithsonian Institution
(National Oceanographic Data Center, WB - Weather Bureau, DA -
Department of Agriculture, and WHOI (Woods Hole Oceanographic
Institute),

The bibliographic cards are filed alphabetically by name of the
survey ship and cruise number; e.g., VEMA-6 follows VEMA-5., If
the ship is not given, then the expedition, cruise, or operation name is
used, e.g., Capricorn Expedition, DEEP FREEZE (operation), AMOS
(project). If none of theseis given, thenthe cards are filed alphabetically
by senior author or occasionally by geographic area name if the source
deals with a limited area such as the Sea of Azov.

The purposes of the bibliographic file are:

1. To direct users of data to the original source for information
not supplied by the data card.

2. To prevent duplication of data by indicating if recently acquired
data or sources already have been filed.

20

3. To provide bibliographic listings of marine geologic sources of
information (not only bottom sediment samples) for specific areas
through area cross references, and to provide lists of reports dealing
with projects, operations, cruises, or expeditions.

4, To relate reports and analyses which come from several sources
or authors but deal with the same samples. The ship, expedition, or
project name with the date is most useful for this purpose.

5. To be able to enter on the cards additional information about
the samples from new sources by using the list of Marsden squares
given under comments on the bibliographic card.

The tally file is maintained to provide current listings of the num-
bers and geographic distributions of bottom sediment samples contained
in the data collection, Eventually, it ishoped, the tally file will indicate
the worldwide distribution of all published and muchunpublished bottom
sediment data. This file is used as a guide in planning oceanographic
surveys by indicating regions for which data are lacking and where
survey efforts should be concentrated. Charts prepared periodically
from this file will indicate progress in the collection of submarine
sediment information.

The tally cards also show the number of core samples and the
number of samples of other types (designated surface samples) in
each one-degree square. The code number of the source of each sample
or the ship’s name and date of collection are recorded on the tally
card,

A log book is maintained in which all bibliographic sources of
bottom sediment data are entered and numbered (code number) in the
chronological order in which their data are added to the data file. Its
major purpose is to serve as an additional record of sources and as a
key to sources which may be indicated on data and tally cards only by
code number

VI. Composition of Data Collection

The data file now contains analyses or descriptions of approximately
20,000 samples, of which about 17,000 are surface samples and 3,000
are core samples. Data for several thousand of the samples were ob-
tained from foreign language sources, many of which have been partially
translated. However, translation time and cost remain a restriction
on full use of foreign sources. Russian, Japanese, Chinese, German,
French, Spanish, Greek, Italian, Portuguese, Dutch, Finnish, Turkish,

21

Israeli, and Scandinavian as well as English language sources have
supplied data for the collection,

The worldwide distribution of bottom sediment data in the Naval
Oceanographic Office collection as of 1 January 1963 is shown in
Figures 16 through 25. Two categories of data are shown for each one-
degree quadrangle (note exception in North Pole Chart,Figure 24),
namely the number of core samples and the number of surface samples
of all other types (trawls, dredges, snappers, etc.).

To aid in adequate evaluation of relative density of data per unit
area, the table on page 62 is included to show the latitudinal variation
in area of 1° quadrangles.

VII. Bibliographic File

The bibliographic file on which this report is based consists of the
following sources, Following each citation is a list of the ships and
expeditions or project names involved, where appropriate. The library

from which the referenced publication was obtained is indicated by
abbreviations (identified on page 20) preceding the call number. Where

no library is given the publication is in the Naval Oceanographic Office
Library.

ANON. Dredging results from the oceanographic cruise “Tithys.”
Research Proceedings, Marine Laboratory, Greece, vol. l,no. 2,
pp. 7-11, 1962. WHOI

TITHYS 1961

- - - Lothungen im Chinesischen Meere und bei Japan. Annalen der
Hydrographie und Martimen Meteorologie, jahrgang III, no. 23 and
24, p. 470, 1875. VK 588 Ao 1875
ERZHERZOG FRIEDRICH 1875

- -- Tiefseelotungen S. M. S. “PLANET” 1910 unter dem kommando
von Korvettenkapitan Dominik, Annalen der Hydrographie und
Maritimen Meteorologie, jahrgang 39, heft I, pp. 16-20, 1911.
VK 588 Ao 1911

PLANET 1910

--- Kleinere Mitteilungen - 3, Lotungen in dem Bosporus und dem
Schwarzen Meere. Annalen der Hydrographie und Maritimen
Meteorologie, jahrgang 34, p. 135, March 1906. VK 588 A6é 1906

VON PODBIELSKI 1905

22

AGASSIZ, A. Reports on the scientific results of the expedition to
the tropical Pacific in charge of Alexander Agassiz by the U. S.
Fish Commission Steamer ALBATROSS from August 1899 to
March 1900, Commander Jefferson F. Moser, U. S. N., Com-
manding. I. Preliminary Report and list of stations with remarks
on the deep-sea deposits by Sir John Murray. Memoirs of the
Museum of Comparative Zoology at Harvard College, vol. XXVI,
no. 1, pp. 1-114, Cambridge, January 1902. (USGS) S(214)qH 3l

ALBATROSS 1899-1900, 1904-1905

AKSENOV, A. A. O zanosimosti podkhednykh portovykh kanalov v
Azovskom More (Deposition in the port approaches and channels
of the Azov Sea). Glavnoye Upravleniye Gidrometeorologicheskoi
Sluzhby pri Sovete Ministrov SSSR, Trudy Gosudarstvennogo Okeano-
graficheskogo Insituta, vypusk 31 (43) pp. 58-71, ed. A.A. Aksenov,
Leningrad, 1956. Serial File

ALCOCK, A. A _ naturalist in Indian seas, or four years with the
Royal Indian Marine Survey Ship “Investigator.” John Murray,
London, 328 p. 1902. QL 137 A35

INVESTIGATOR 1888-1892

ALVERSON, D. L. Deep-water trawling survey off the coast of
Washington (Aug. 27-Oct 19, 1951), U. S. Fishand Wildlife Service,
Commercial Fisheries Review, vol. 13, no. 11, pp. 1-16, November
1951. Serial File

JOHN N. COBB 1951

- - - Deep-water trawling survey off the Oregonand Washington coasts
(August 25-October 3, 1952), U. S. Fish and Wildlife Service,
Commercial Fisheries Review, vol. 15, no. 10, pp. 5-15, October
1953. Serial File

JOHN N. COBB 1952

ANDERSON, A. W. Oceanographic data report, Project Chiper, March-
April 1960. U.S. Navy Hydrographic Office, Informal Manuscript
Reports No. 0-38-62, pp. Bl-11, September 1962. Unpublished
Manuscript.

CHIPER (Project)
BURTON ISLAND 1960

ATHEARN, W. D. Bottom sediments and Foraminiferafrom Labrador,
BLUE DOLPHIN 1951 and 1952. Woods Hole Oceanographic
Institution, Reference No. 54-42. 16 p., June 1954. Unpublished
Manuscript. GC 491 W8A8 54-42

BLUE DOLPHIN 1951-1952

23

BADER, R. G., and HENRY, V. J. Marine sediments of Prince of
Wales Strait and Amundsen Gulf, West Canadian Arctic. Texas
A & M College, Department of Oceanography and Meteorology,
Series No. 130, also University of Washington, Department of
Oceanography, Contribution No. 231, Journal of Marine Research,
vOlwuli/noO wl, spp els>—2, 1 JDO moe rich ere
BEAUFORT SEA EXPEDITION 1953

BERRIT, G. R. Etude des teneurs en manganese et en carbonates de
quelques carottes sedimentaires Atlantiques et Pacifiques.
Meddelanden fran Oceanografiska [Institutet 1 Goteborg, 23, Sjatte
Foljden, ser. B, band 6, no, 12, 61 p., GoOteborgs Kungl. Vetens-
kapsoch Vitterhets-Samhalle, 1955. AS 284 G7 No. 23

ALBATROSS 1947-1948
SWEDISH DEEP SEA EXPEDITION 1947-1948

BERTHOIS, L. I. Contribution a l’étude litholigique ges galets du fond
de la Manche in “Missions du navire cablier “Emile-Baudot” sur
le plateau continental Breton (Juillet- Aut- Septembre 1 ey a ee
Cahiers du Centre de Récherches et d'Etudes OceAnographiques,
Travaux de la Station Océanographiques de la Rochelle-Pallice,

, Cahier No, 3, pp. 1-10, February 1950. GC7 F8Al No, 3
EMILE-BAUDOT 1949
(Cable Ship)

BEZRUKOV, P.L., MURDMAA,I.O., SAIDOVA, Kh. M. and FILATOVA,
Z. A. Ob osadkakh i donnoi faune severnoi chasti, Vostochno-
Kitaiskogo Morya. (Sediments and bottom fauna of the northern
part of the East China Sea). Oceanologia et Limnogie Sinica,
vol. 1, no. 3, pp. 293-315, November 1958. Serial File

VITYAZ 1955

BLACK, M. Fossil coccospheres from a Tertiary outcrop onthe
continental slope. Geological Magazine, vol. XCIX, no. 2, pp.
123-127, March-April 1962. (USGS)

SARSIA (R/V) 1959

BLANC-VERNET, L. Etude de quelques sediments dragues au nord du
Cap Corse, Marseille. Station Marine d’Endoume. Recueil de
Travaux, Fascicule 34, Bulletin No. 21, pp. 103-120, 1961.
uncatalogued

CALYPSO 1957 (Sept.)
GYF 1956

BOGGILD, O. B. Sediments sous-marins recuellis dans la mer du
Gronland., Geologie. Louis Philippe Robert, Duc d’Orleans,
Croisiére océanographique accomplié a bord de la Belgica dans
la mer du Gronland 1905, pp. 85-98, C. Bulens, ed. Bruxelles,
1907. (USGS)530.1 qL93

24

--- Samples of the sea-floor along the coast of East Greenland
741/2-70 N. L. Carlsbergfondet Expedition til @st Grdnland,
udfort i Aarene 1898-1900 under Ledelse af G. Amdrup, II,
Meddelelser om Grgnland, Med 16, vol. 28, pp. 95. Kjfbenhavn,
1909. Serial File

CARLSBERGFONDETS EXPEDITION TO EAST GREENLAND
1898-1900

BORDOVSKIY, O. K. K khimii osadkov tsentral’noi chasti Tikhogo
Okeana (The chemistry of sediments of the Central Pacific Ocean),
Akademiya Nauk, SSSR, Trudy Instituta Okeanologii, tom XLII,
pp. 107-116, 1960. Serial File

VITYAZ 1953-1955

BOURCART, J. Les sediments precontinentaux profonds dans le Golfe
de Génes. Deep Sea Research, vol. 5, no. 3, pp. 215-221, March
1959. Serial File

CALYPSO 1958

BOURNE, G. C. Report of a trawling cruise in HMS RESEARCH off
the southwest coast of Ireland. Journal of the Marine Biological
Association of the United Kingdom, vol. 1 (N. S.), pp. 306-323,
1889-1890. Serial File

RESEARCH (HMS) 1889

BRAMLETTE, M. N. and BRADLEY, W. H. Geology and biology of
North Atlantic deep-sea cores between Newfoundland and Ireland.
Part 1, Lithology and geologic interpretations. U.S. Department
of the Interior, Geological Survey Professional Paper 196, pp.
1-33, Government Printing Office. 1942. GC 380 B8

LORD KELVIN 1936

BRENNECKE, W. Ozeanographische arbeiten der Deutschen Antark-
tisches Expedition. Annalen der Hydrographie und Maritimes
Meteorologie, jahrgang 39, heft VII, pp. 350-353, heft IX, pp. 464-
471, heft XII, pp. 642-647, 1911. VK 588 A6 1911

DEUTSCHLAND 1911
DEUTSCHEN ANTARKTISCHEN EXPEDITION 1911

--- Die forschungsreise SMS “Planet” Annalen der Hydrographie
und Maritimen Meteorologie, jahrgang 34, pp. 353-361, 414,
457-462, and 556-558, 1906. VK 588 A6é 1906

PLANET 1906

BRODIE, J. W. Features of the sea-floor west of New Zealand.
New Zealand Oceanographic Committee, Publication No. 7, New
Zealand Journal of Science and Technology, sect. B, vol. 33,
no. 5, pp. 373-384, March 1952. GCl N45 No. 7

RECORDER (cable ship) 1932
725)

BROTSKAYA, V. and ZENKEVICH, L. Materialy po kolichestvennomy
uchetu donnoi fauny Barentsova, Belogo i Karskogo morti (Materi-
als for the quantitative evaluation of the bottom fauna of the
Barents, White and Kara seas) vol. 6--Kolichestvenniy uchet
donnoi faun Cheshskoi guby (A qualitative evaluation of the bottom
fauna of the Cheshskayo Bay). Gidro-meteorologicheskii Komitet
SSSR, Trudy, Gosudarstvennogo Okeanograficheskogo Instituta
Moskva, tom II, vyp. 2, pp. 41-56, 1932. Serial File

PERSEY X

BRUUN, A. ATLANTIDE-Report No. 1. Scientific results of the
Danish Expedition to the coasts of tropical West Africa 1945-1946.
The University of Copenhagen and the British Museum (Natural
History) London, Danish Science Press Ltd., pp. 1-47, 1950.
Q115 Atlantide 1945-1946 No. 1

ATLANTIDE 1945-1946
DANISH EXPEDITION TO TROPICAL WEST AFRICA 1945-1946

---, LANGER, E., and PAULY, H. Magnetic particles found by
raking the deep sea bottom. Deep Sea Research, vol. 2, no. 3,
pp.230-246, April 1955. Serial File

GALATHEA
DANISH DEEP SEA EXPEDITION 1950-1952

BRUYEVICH, S. V. and ZAITSEVA, E. D. K khimii osadkov severo-
zapadnoi chasti Tikhogo Okeana (The chemistry of sediments of
of the northwestern part of the Pacific Ocean). Akademiya Nauk
SSSR, Trudy Instituta Okeanologii, tom XLII, pp. 1-88, 1960.
Serial File

VITYAZ 1949-1955

BUCHANAN, J. Y. On the composition of some deep-sea deposits from
the Mediterranean. Proceedings, Royal Society of Edinburgh,
vol. 18, 1892. GC 387 BY

DACIA, S. S. Sept. 1879

CARSOLA, A. J. Marine geology of the Beaufort and eastern Chukchi
Seas. U.S. Navy Electronics Laboratory, San Diego, California
NE 12-221-3 (NEL 2A5) Report 392, 49 p., 6 August 1953,
Gerais u5
BURTON ISLAND (US AGB-1) 1950-1952
BAREX RESUPPLY EXPEDITION

26

CEBULSKI, DONALD E. Distribution of Foraminifera in the barrier
reef and lagoon of British Honduras. The Agriculture and Mechan-
ical College of Texas, Department of Oceanography and Meteorology,
Project 24, Ref. 61-13T, May 1961.

CHAPMAN, F. Sea floor deposits from soundings. Australasian
Antarctic Expedition 1911-1914 under the leadership of Sir Douglas
Mawson, Part 1, Scientific Reports. Series A., vol 11, Oceanog-
raphy, pp. 1-60, J. Spence Actg. Gov't Printer, Sydney, 1922.
Q115 AAE 1911-1914 Series A II-III

AURORA 1911-1914
AUSTRALASIAN ANTARCTIC EXPEDITION 1911-1914

CHUMLEY, J. Report on the deposit samples collected during the
‘*Michael Sars’’ North Atlantic Deep-Sea Expedition 1910in‘‘ Report
on the scientific results of the MICHAEL SARS North Atlantic
Deep Sea Expedition 1910.’’ vol. 1, pp. 1-10, Bergen Museum,
John Grieg, Bergen (1929-1933). Z115 M 6 v.1

MICHAEL SARS
NORTH ATLANTIC DEEP SEA EXPEDITION 1910

CLARKE, A. H., JR. Abyssal mollusks from the South Atlantic Ocean.
Contribution No. 503. Lamont Geological Observatory Bulletin,
Museum of Comparative Zoology Harvard College, vol. 125,no. 12,
pp. 345-387, October 1961.

VEMA CRUISES 12 and 14 1957, 1958

- - - HUNTSMAN, A. G. Results of the Hudson Bay Expedition,
1920. III. The Echinoderms, IV. The Ascidiacea. Contributions to
Canadian Biology, New Series, vol. 1, nos, 2 and 3, pp. 21-38,
1922. Serial File

HUDSON BAY EXPEDITION 1920

COHEE, G. F. Sediments of the submarine canyons off the California

coast. Journal of Sedimentary Petrology, vol. 8, no. 1, pp. 19-33,
April 1938. Serial File

27

COLOM, G. Foraminiferos de los costas de Galiciea (Campanas del
‘*Xauen’’ en 1949-1950). Boletin del Instituto Espanol de Oceanograf-
ia No. 52, 58 p.,7 June 1952 Serial File

XAUEN 1949-1950

CREAGER, J. S. and McMANUS, D.C. Preliminary investigations of
the marine geology of the southeastern Chukchi Sea. BROWN
BEAR Cruise No. 236, 1 August to 2 September 1959. University
of Washington, Department of Oceanography, Technical Report
No. 68. Reference 61-15. 46 p. May 1961, GC 856 W2A4 No. 68

BROWN BEAR CRUISE 236 Aug.-Sept. 1959
PLOWSHARE (OPERATION) -
CHARIOT (PROJECT)

CUSHMAN, J. A. Foraminifera, Part M, Volume IX: Annelids,
parasitic worms, protozoans, etc. Report of the Canadian Arctic
Expedition 1913-1918, Southern Party 1913-1916, J. de Labro-
querie Tache, Ottawa. 13 p., February 6, 1920.(USGS)502(980)C
165 v.9, pt. M

CANADIAN ARCTIC EXPEDTION 1913-1918

DANGEARD, L. Observations de geologie sous-marine et d’oceano-
graphie relatives ‘a la Manche. Annales de 1’Institut Océanographique
(Foundation Albert 1 Prince de Monaco) New series, tome VI,
fasc. 1, pp. 1-295, 1928. GC 1 Monaco Serie II

POURQUOI-PAS ? 1922-1927

DAVIS, J. K. Soundings. Australasian Antarctic Expedition 1911-1914
under the leadership of Sir Douglas Mawson. Part 3, Scientific
Reports, series A, vol. II, Oceanography, pp. 91-102. T.H.
Tennant, Actg. Gov’s Printer, Sydney NSW, Australia, 1940.
Q115 AAE 1911-1914 Series A II-III.

AURORA 1911-1914
AUSTRALASIAN ANTARCTIC EXPEDITION 1911-1914

DAY, A. A. The continental margin between Brittany and Ireland. Deep
Sea Research, vol. 5, no. 4, pp. 249-265, May 1959. (NOO) Serial
File

DALRYMPLE (HMS)
SARSIA (RN)

28

DEMEL, J. and MULICKI, Z. Quantitative investigations onthe biologic-
al bottom productivity of the south Baltic. Reports of the south
Baltic. Reports of the Sea Fisheries Institute (Morski Instytut
Rybacki) in Gdynia, Nr. 7, pp. 75-126. Warsaw, Poland, 1954,
(D. I.) QH 301 G27, No. 7

DI NAPOLI ATTATA, E. Btude delacarotte No. 19 campagne du “Vema”
dans la Méditerranée (Mer Tyrrhénienne) in “La topographie et la
geologie des profondeurs océaniques. ” Collogues Internationaux du
Centre National de la Recherche Scientifique, vol. LXXXIII, Nice-
Walllefranche s5=l2) Mar. 1958, pp. -6l=71, “Publ, Parisml959:
(LC) GC 83 F7

VEMA Cruise 10 1956

DORAN, E. JR. Land forms of the southeast Bahamas. The University
of Texas Publication No. 5509, 38 p. May1, 1955. (NOO) GB 429 D6
LADY LEONA (Sloop) 1953-1954

DRYGALSKI, E. von. I. Lothungen, Zweiter Theil-Sonderberichte
uber die fahrt von Kapstadt bis Kerguelen in Deutsche Sudpolar-
Expedition auf dem Schiff “Gauss,” Bericht uber die wissenschaft-
lichen arbeiten auf der fahrt von Kapstadt bis zu den Kerguelen
27 November 1901 bis 2 Januar 1902. Veroffentlichungen des
Instituts fur Meereskunde und des Geographischen Instituts und
der Universitat Berlin, heft 2, August 1902. E. S. Mittler u.
Sohn, Berlin. GCl B5 No. 2.5

GAUSS 1901-1903
DEUTSCHE SUDPOLAR EXPEDITION 1901-1903

EMERY, K.O., Geology of Johnston Island and its surrounding shal-
lows, central Pacific Ocean. Bulletin of the Geological Society
CtmeAmenicaiiviols 67, no, Ll), pps. 1505-1520; (November 1956,
Serial File

DVO wm On bULGHER,. Wi oS. GOULD Ho Ro and Sib PAR y Rib.
Submarine geology off San Diego, California. Scripps Institution
of Oceanography, New Series, no, 588, Allan Hancock Foundation
Contribution no. 85, The Journal of Geology, vol. 60, no. 6,
pp. 511-548, November 1952. Serial File

29

EMERY, K. O. and HULSEMAN, J. The relationship of sediments, life
and water in a marine basin. Deep Sea Research, vol. 8, no. 5,
pp. 165-180, 1962. Serial File

VELERO IV

ERICSON, D. B., EWING, M. and HEEZEN, B.C. Turbidity currents
and sediments in North Atlantic. Lamont Geological Observatory
Contribution No. 47. Woods Hole Oceanographic Institution Con-
tribution No. 604, Bulletin of the American Association of Petro-
leum Geologists, vol. 36, no. 3, pp. 489-511, March 1952. Serial
File

ATLANTIS CRUISE 152 1947-1951

ERICSON, D. B., EWING, M., WOLLIN, G. and HEEZEN, B.C. Atlantic
deep-sea sediment cores. Geological Society of America Bulletin,
vol, 72, no, 2, pp. 193-286, February 1961. Serial File

ATLANTIS REHOBOTH
CARYN SAN PABLO
VEMA

ERICSON, D. B. and WOLLIN, G. Micropaleontology and lithology of
Arctic sediment cores. Lamont Geological Observatory Contribu-
tion No. 346, in “Scientific studies at Fletcher's Ice Island, T-3
(1952-1955),” vol. I, Geophysical Research Papers No. 63, Geo-
physics Research Directorate, Air Force Cambridge Research
Center, USAF, Air Force Research and Development Command
AFLRC-TR-59-232(1) ASTIA Document No. AD-216813, pp. 51-58,
September 1959. QC 801 U5G3 No. 63 v. 1

Fletcher’S ICE ISLAND (T-3)

EWING, M. and HEEZEN, B. C. Puerto Rico Trench topographic and
geophysical data. Lamont Geological Observatory Contribution
No. 135, in Poldervaart, A. Crust of the Earth (A Symposium),
Geological Society of America Special Paper 62, pp. 255-263,
1955.

ATLANTIS 1949-1954
CHALLENGER
SAN PABLO

FELL, H. B. The fauna of the Rose Sea, Part 1, Ophiuroidea. New
Zealand Oceanographic Institute Memoir No. 18, New Zealand
Department of Scientific and Industrial Research, Bulletin 142,
79 p., 1961. GCl N452 M5 No. 18

ENDEAVOUR Cruise I 1958
(HMNZS) Cruise II 1959

30

FLEMING, R. H. and Staff. Physical and chemical data, North Pacific
Ocean Brown Bear Cruise 199, July-Aug. 1958 for the International
Geophysical Year of 1957-1958. University of Washington, Depart-
ment of Oceanography, Special Report 30, pp. 12-13, March 1959.
GC 856 W2A3 No, 30

BROWN BEAR Cruise 199 July-Aug. 1958

FORD, E. Animal communities of the level sea-bottom in the waters
adjacent to Plymouth. Journal of the Marine Biological Associa-
tion of the United Kingdom, vol. XIII (NS), no. 1, pp. 164-224,
December 1923. Serial File

FREDRIKSSON, K. A sediment core from the Mindanao Trough. Re-
ports of the Swedish Deep-Sea Expedition 1947-1948. Sediment
cores from the West Pacific, vol. VI, fasc. IV, pp. 97-134, Gote-
borgs Kungl. Vetenskaps Och Vitterhets-Samhalle, July 1959.
Q115 S 8 v. 6-7

ALBATROSS 1947-1948
SWEDISH DEEP SEA EXPEDITION 1947-1948

GAUTIER, Y. V. Sur quelques Bryozoaires de la “Zone a coraux
profonds” du Golfe de Génes (Campagne de la “Calypso” de
Novembre 1957). Bulletin de 1’Institut Océanographique, Monaco,
no, 1123, 10 p. 25 July 1958. (DI) GC1 1 45

CALYPSO 1957
ELIE-~MONNIER 1952

GOETHEM, C. VON Etude physique et chimique du milieu marin.
Institut Royal des Sciences Naturelle de Belgique. “Expédition
Océanographique Belge dans les eaux Cotiéres Africaines del
‘Atlantique Sud (1948-1949),” Resultats Scientifiques, vol. II,
fasc. 1, 152 p., Bruxelles, 1951. Z115 EY vy. 2, fasc. 1,

NOORDENDE 1948-1949

GOLDBERG, E. P. and KOIDE, M. Ionium-thorium chronology in deep
sea sediments ofthe Pacific. Science, vol, 128, no. 3330, pp. 1003,
October 24, 1958. Serial File.

CAPRICORN
CHINOOK

CHUBASCO

CUSP

NORTHERN HOLIDAY

Sh

GOMEZ DE LLARENA, J. Observaciones sobre los sedimentos recogidos
entre los Cabos Juby y Bojador. Exploracion Oceanografica del
Africa Occidential, Boletin del Instituto Espanol de Oceanografia,
no, 29, 23 p., 20 March 1950. Serial File

MALASPINA May-June 1947

4
GONZALEZ PENA, J. M. Estadio mineralégico comparativeo de la
fraccion ‘‘arcilla’’ de algunos sedimentos del litoral espanol,
Po S62 the Boletin del Instituto Espanal de Oceanografia, no. 90,

Madrid, 15 February 1958, Serial File
XAUEN 55-7 & 56-1

GORSHKOVA, T. I. Organicheskiye veshchestvo i karbonaty v osadkakh
Barenstova Morya (Organic matter and carbonates in the sedi-
ments of the Barents Sea). Kolebaniya chislennosti i usloviya
promysla donnykh ryb v Bareustovom More (Variations in the
number and trade conditions of bottom fish in the Barents Sea).
Trudy Polyarnogo Nauchno-Issledovatel’skogo Instituta Morskogo
Rybnogo Khozyaistva i Okeanografiy Imeni N. M. Knipovicha
(PINRO) uypusk X, pp. 260-280, 1957. (LC) SH1.M8

PERSEY 1927-1931
NICOLAI KNIPOVICH 1930-1931

GORSLINE, DONN S. and STEWART, R. A. Benthic marine exploration
of Bahia de San Quintin, Baja, California, 1960-1961. Marine and
Quaternary Geology. Pacific Naturalist, vol. 3, no. 8, Oct. 16,
1962.

Serial File

GOULD, H. R. and BUDINGER, T. F. Control of sedimentation and
bottom configuration by convection currents, Lake Washington,
Washington. University of Washington, Department of Oceanography
Contribution No, 221, Journal of Marine Research, vol.17, pp. 183-
NOS algo Sr

Serial File

GRIEG, J. A. Brachiopoda, Scaphopoda, Gastropoda, and Lamelli-
branchiata from the “Michael Sars” North Atlantic Deep-Sea
Expedition 1910. Report of the Scientific Results of the “Michael
Sars” North Atlantic Deep-Sea Expedition 1910, vol. III, pt. I,
DM Nelo, WOE, Bergen Museum, John Grieg, Bergen 1933.
Q115 Mé v.3

MICHAEL SAR 1910
NORTH ATLANTIC DEEP-SEA EXPEDITION 1910

32

GRIPENBERG, S. A _ study of the sediments of the North Baltic and
adjoining seas. Vth Hydrological Conference of the Baltic States.
Communication 12A. Helsinki-Helsingfors, 23lp., 1934.

GB 660 Baltic 1936 Commun,
NAUTILUS (FINLAND) 1924-1930

HABE, T. Pelecypod shell remains in Tanabe Bay, Wakayama Pre-
fecture, Records of Oceanographic Works in Japan, Special Number
4, pp. 39-51, March 1960. Serial File

HAMILTON, E. L. Upper Cretaceous, Tertiary, and Recent planktonic
foraminifera from Mid-Pacific flat-topped seamounts. Jounal of
Paleontology, vol. 27, no. 2, pp. 204-237, March 1953. (USGS) also
Contribution No. 615, 1953, Scripps Institution of Oceanography
G@ 1S535953

MID-PAC 1950

HANZAWA, S. Diatom (Ethmodiscus) ooze obtained from the tropical
southwestern North Pacific Ocean. Records of Oceanographic
Works in Japan, vol. VII, no. 1, pp. 37-43, May 1953. Serial File

KOSYU
MANSYU
OD ©

HEEZEN, B. C., ERICSON, D. B. and EWING, M. Further evidence
for a turbidity current following the 1929 Grand Banks earthquake.
Deep Sea Research, vol. 1, no. 4, pp. 193-202, July 1954.
Serial File

ATLANTIS CRUISE 180 1952

HERAS, A, R. et al. Analisis de fondos de la Bahia de Cadiz, Boletin
del Instituto Espanol de Oceanografia, no. 75, 30 p., Madrid,
15 April 1956, Serial File
XAUEN 1953

HILL, M. N. and KING, W. B. R. Seismic prospecting in the English
Channel and its geological interpretation. Quarterly Journal of
the Geological Society of London, vol. CIX, no. 1, pp. 1-19, 1953.
(LC) QE 1 G4

33

HOHNK, W. Ein beitrag zur ozeanischen Mykologie in-Bohnecke,
Buckmann, A. Die expeditionen von F. F. S. “Anton Dohrn” und
V.F.S. “Gauss” in Internationalen Geophysikalischen Jahr 1957/
1958. Deutsches Hydrographisches Institut-Hamburg, Deutschen
Hydrographischen Zeitschrift, Erganzungsheft Reihe B (4°), nr.
3p eo Ula, NOH), Seresieul ime

ANTON DOHRN_ 1958

HOLME, N. A. The bottom fauna of Great West Bay, Journal of the
Marine Biological Association of the United Kingdom, vol. 29,
pp. 163-183, 1950-1951. Serial File

HOLTEDAHL, H. On the Norwegian continental terrace, primarily
outside Mdre-Romsdal: its geomorphology and sediments. With
contribution on the Quaternary geology of the adjacent land on
the bottom deposits of the Norwegian Sea. Universitet i Bergen,
Arbok 1955, Naturvitenskapelig rekke nr. 14, 209 p. A.S. John
Griegs Boktrykkeri, Bergen 1957. GB 457.3 H7

ARMAUER HANSEN 1950-1953
G. ©. SARS #954

- - - Geology and paleontology of Norwegian Sea bottom cores,
Journal of Sedimentary Petrology, vol. 29, no. 1, pp. 16-29,
March, 1959. Serial File

ARMAUER HANSEN 1950-1953
GG. OaSARS eelg54

HOLZMAN, J. E. Submarine geology of Cortes and Tanner Banks.
Journal of Sedimentary Petrology, vol. 22, no. 2, pp. 97-118,
June 1952. Serial File

VELEROIV 1949

HOSOKAWA,.I., OKOBE, S., and HAMODA, S. Oceanographical studies
on the sediments in the East China Sea, (1) On the contents of
organic carbon and total nitrogen. Journal of the Oceanographical
Society of Japan, vol. 15, no. 2, pp. 43-47, June 1959. Serial File

HOSHINO, M. and ICHIHARA, Y. Submarine topography and bottom
sediments off Kumano-nada and Enshu Nada. Journal of the

Oceanographical Society of Japan, vol. 16, no. 2, pp. 41-46,
June 1960. Serial File

34

HOUGH, J. L. Sediments of Cape Cod Bay, Massachusetts. Woods
Hole Oceanographic Institution Contribution No. 184, Journal of
Sedimientanyin Petrology, vol ili2) now) pp. el0=305, April942.
Serial File

ASTERIAS 1935

HOUGH, J. L. Sediments of Buzzards Bay, Massachusetts. Woods Hole
Oceanographic Institution Contribution No. 187, Journal of Sedi-
mentary Petrology, vol. 10, no. 1, pp. 19-32, April 1940.

Serial File
ASTERIAS 1934

HUNKINS, K. L., EWING, M., HEEZEN, B. C. and MENZIES, R. J.
Biological and geological observations on the first photographs of
the Arctic Ocean deep-sea floor. Lamont Geological Observatory
Contribution No. 411. Limnology and Oceanography, vol. 5, no. 2,
pp. 154-161, April 1960. Serial File

ARCTIC DRIFT STATION “A” DECEMBER 1957

HURLEY, R. J. Expedition Chinook I lowering log June-August 1956.
Scripps Institution of Oceanography. 23 P. 1956. GC 781 S4E9
also GC771 S4S5

CHINOOK I EXPEDITION 1956
SPENCER F. BAIRD 1956

IJAMA, A. The bottom sediments of the Japan and Kuril trenches
collected by the Ryofu Maru during the Japanese Deep Sea Expedi-
tion in 1959. JEDS Contribution No. 8. Geological Institute,
University of Tokyo, The Oceanographical Magazine, vol. ll, no. 2,
pp. 225-231, May 1960. Serial File

RYOFU MARU 1959

JARKE, J. Beitrag zur kenntnis der foraminiferen-fauna der mittleren
und westlicken Barents-See. Reprint - Int. Revue ges. Hydrobiol.,
vol. 45, no. 4, pp. 581-654, 1960. Deutsches Hydrographisches
Institut, Oceanographie 1960, nr. 8, Hamburg, 1961. GC 1H 1 1960

CORDILLERA 1939 FRANKEN 1939
HEINRICH BAUMGARTEN 1938 STUTTGART 1938

KAGAMI, H. and IJIMA, A. On the bottom sediments off Onagawa and
Kushiro, the adjacent continental slope of Japan Trench. JEDS
Contribution No. 9, Geological Institute, University of Tokyo,
The Oceanographical Magazine, vol. 11, no. 2, pp. 233-242, March
1960. Serial File

RYOFU MARU 1959

35

KAGAMI, H. Submarine sediments off Sakata, Yamagata, Japan.
Geological Institute University of Tokyo Contribution, Japanese
Journal of Geology and Geography, vol. XXXII, nos. 3-4, pp. 397-
410, November 25, 1961. Serial File

MEIYO
TENKAI
TORII

KLENOVA, M. V. Geologiya Barentsova Morya (Geology ofthe Barents
Sea). Akademiya Nauk SSSR, Komissiya po Problemam Severa,
pri Prezidiume AN SSSR, 367 p., Moskva, 1960.

ISSLEDOVATEL’ NICOLAI KNIPOVICH
POLYARNAYA ZVEZDA PERSEY

SADKO KASHALOT
PERSEY-2 SRT-440

KNOX, G. A. General account of the Chatham Islands 1954 Expedition.
New Zealand Department of Scientific and Industrial Research
Bulletin 122, New Zealand Oceanographic Institute Memoirs No.
2. 37 p., 1957. GCl N452 M5 (WB Library) M06.5/931 K74ge

CHATHAM ISLANDS EXPEDITION 1954
NORA NIVEN 1907
ALERT 1954

KOBAYASHI, K., OINUMA, K., and SAIDO, T. Clay mineralogical
study on recent sediments (I) Samples JEDS-iR'’, JEDS-1R®".
JEDS Contribution No. 15, Geological Institute, University of
Tokyo, The Oceanographical Magazine, vol. 11, no, 2, pp. 215-223,
March 1960. Serial File

RYOFU MARU 1959

KOMUKAI, R. On the bottom topography and sediments in the western
passage of Tsugaru Strait. The Report of the Hydrographic Office,
Maritime Safety Office, Tokyo, Japan. Various pages. 1956.
GC 821 K8

IIOMMAMT, . Go eich COON, de E. Preliminary results of recent
deep drilling on Cape Code, Massachusetts. Science, vol. 137,
no. 3523, p. 34, July 1962. Serial File

36

KROG, H. Post-glacial submergence of the Great Belt dated by pollen-
analysis and radio carbon, International Geological Congress,
Report of the Twenty-First Session Norden, Part IV, Proceedings,
Section 4 ~ Chronology and Climatology of the Quaternary, pp. 127-
13s, UNOO.

KRUMBEIN, W. C. and ABERDEEN, E. The sediments of Barataria
Bay amounnalmotisedimentarye Petrology, vole a1,) now len pps s— lil,
Aprilligs ia serial bale

KUENEN, P. H. Two problems of marine geology: atolls and canyons.
Verhndelingen der Koninklijke Nederlandsche Akadamie van
Wetenschappen, Afd. Natuurkunde, Tweede Sectie, Deel XLIII,
no. 3, pp. 1-69, 1947,N. V. Nood-Hollandsche Uitgevers Maats-~
schappij, Amsterdam, 1947. QE 33 K9

KUENEN, P. H. Geological results, vol. V, Bottom samples, pt. 3,
Collecting of the samples and some general aspects, section I. also
NEEB, I. G. A. The composition and distribution of the samples in “The
Snellius Expedition in the eastern part of the Netherlands East-
Indies 1929-1930. 265p., E. T. Brill-Leiden, 1943. Q115 SNELLIUS
Vo Dp je &
SNELLIUS EXPEDITION 1929-1930

KULP, O. Beitrag zur entwicklungsgeschichte der Mecklenburger
Bucht, Petermanns Geographische Mitteilungen, heft 4, 105
jahrgang, pp. 249-256, VEB. Hermann Haack, Geographische
Kartographische, Anstalt Gotha, Dresden, DDR, 1961. Translation.

KULP, J. L. and CARR, D. R. Surface area of deep-sea sediments.
Lamont Geological Observatory Contribution 14, Journal of Geology,
vol. 60, no. 2, March 1952. Serial File

URC wiG we HOnaminiferes jet Ostracodesy ide 1*Etang de Thau. Revue
des Travaux de l'Institut des Péches Maritimes, tome XX\, fasc.
A. GELS JD, esse, Wo SSl AOS INS) s75 45 ie, Z
OSTREA 1956-1958

37

LAEVASTU, T. The occurrence of pigments in marine sediments.
Department of Oceanography, University of Washington Contribution
No. 228, Journal of Marine Research, vol. 17, no. 4, pp. 325-334,
November 1958. Serial File

DAROND; E. Cy, DIETZ, RS.) PRETCHARD, D> We Oceanographic
measurements from the USS NEREUS on a cruise to the Bering
and Chukchi Seas, 1947, Report 91 Problem 2A5, U.S. Navy
Electronics Laboratory, San Diego, California. 96 p., February
1949. GL 841 U5 B4l

NEREUS 1947

LAUGHTON, A. S. Sound propagation in compacted ocean sediments.
Geophysics, vol. XXII, no. 2, pp. 233-260, April 1957. Serial File
DISCOVERY II 1952

LIVINGSTONE, R. Preliminary investigation of the southeastern
Alaska abalone (Haliotis Kamtschatkova). Part I--Exploratory
diving. U. S. Fish and Wildlife Service, Commercial Fisheries
Review, vol. 14, no. 9, pp. 8-16, September 1952. Serial Pile

LADY BESS Sept.-Oct. 1951.

LLARENA, J. G. de Observaciones sobre los sedimentos de las
costas de Galicia (Campanas del “Xauen” en 1949-1950). Boletin
del Instituto Espanol de Oceanografia, no. 52., 24 p., November
LOS Zao e Tia lable

XAUEN 1949-1950

LOCHER, F. W. Sedimentpetrographische untersuchung der lotkerne
255 und 257. Reports of the Swedish Deep-Sea Expedition.
Sediment cores from the North Atlantic Ocean, vol. VII, no. 4,
pp. 187-208. Goteborgs Kungl. Vetenskaps- och Vitterhets-Samhalle
IES, ON GS SS 5% On7/

ALBATROSS 1947-1948
SWEDISH DEEP SEA EXPEDITION 1947-1948

MATTHEWS, L. H. The marine deposits of the Patagonian continental
shelf. Discovery Reports, vol. IX, pp. 175-206, University Press,
Cambridge, 1934. Q115 Discovery v. 9

WILLIAM SCORESBY (RRS) 1927-1932

38

MENARD, H. W. Pleistocene and Recent sediment from the floor of
the northeastern Pacific Ocean. Geological Society of America,
Bulletin, vol. 64, no. 11, pp. 1279-1294, November 1953. Serial
Bales

NORTHERN HOLIDAY 1951

MENARD, H. W., ALLISON, E. C. and DURHAM, J. W. A drowned
Miocene terrace in the Hawaiian Islands, Science, vol. 138,
no. 3543, pp. 896-897, 23 November 1962 Serial File

ARGO 1961

MOLENGRAFF, G. A. F. Geologie-Hoofdstruk (Chapter) VI in “De
zeeén van Nederlandsch Oost-Indie,” Koninklyk Nederlandsch
Aardrijkskundig Genootschap, pp. 272-357. E. J. Brill, Leiden,
1922. (USGS) 503(910) qN28

CACHALOT 1858 GAZELLE 1875
CHALLENGER 1874-1875 SIBOGA 1899-1900
VALDIVIA 1899

MOORE, H. B. The muds of the Clyde Sea area. 1. Phosphate and
nitrogen contents. Journal of the Marine Biological Association
(United Kingdom), vol. 16, pp. 595-607, 1930. Serial File

MOORE, DAVID G. and SHUMWAY, GEORGE. Sediment thickness and
physical properties; Pigeon Point Shelf, California. Journal of
Geophysical Research, vol. 64, no. 3, March 1959. Serial File

MULLER, G. Die rezenten sedimente im Golf von Neapel. Pubblicazioni
della Stazione Zoologica di Napoli, vol. 31, fasc. 1, pp. 1-27,
September 1959. (also in Geol. Rundsch. vol. 47, 1958). (SI)

CAVOLINI 1957

MUNTHE, H. Den Svenska Hydrografiska Expeditionen Ar 1877 under
ledving af F. L. Ekman, Afdelningen II, Kongliga Svenska
Vetenskaps-Akademiens Handlingar, Ny Fjold, bandet 27, no. 2.
35 p. Stockholm, 1894. (USDA) 502 St6 H27, 1894.

SVENSKA HYDROGRAFISKA EXPEDITIONEN AR 1877
MURRAY, J. Balfour Shoal: a submarine elevation in the Coral Sea.
The Scottish Geographical Magazine, vol. 13, no. 3, March 1897.

Serial File
PENGUIN (HMS) 1894-1895

39

- = - Onthe depth and marine deposits of the Indian Ocean, with
descriptions of the deposit-samples collected by Mr. J. Stanley
Gardiner in 1905. Report No. 13 of the Percy Sladen Trust
Expedition to the Indian Ocean in 1905, under the leadership of
Mr. J. Stanley Gardiner. The Transactions of the Linnean Society
of Hendon, end) Ser, Zoolosy,n voles lionmpt mon 10-8 54.) pp >> =o9 oF
June 1910. WS 1SS7tiT WOOD, Wo Zp iIN@s 3

PERCY SLADEN TRUST EXPEDITION 1905

- -- On marine deposits inthe Indian, Southern, and Antarctic Oceans.
The Scottish Geographical Magazine, vol. 5, no. 8, pp. 405-435,
August 1889. (WB) No. 13328, S43 1lgv.5. 1889

EGERIA (HMS) 1887
FLYING FISH (HMS) 1887
INVESTIGATOR (HMS) 1887

MURRAY, J. and CHUMLEY, J. The deep-sea deposits of the Atlantic
Ocean. Transactions of the Royal Society of Edinburgh, vol. LIV,
pt. I. - Session 1923-1924, pp. 1-252, R. Grant & Son, Edinburgh,
1924. (USGS) S(512) qEd. 52 v. 54, 1924-1926.

ATLANTIC DEEP SEA DEPOSITS 1857-1911

ARGUS (HMS) 1879 MINIA (SS) 1903
BRITANNIA (SS) 1897-99 MUTINE (HMS) 1907-08
BUCCANEER (SS) 1886 PORCUPINE (HMS) 1869
CHALLENGER (HMS) 1872-76 RAMBLER (HMS) 1895-99
CYCLOPS (HMS) 1857 SCOTIA (SS) 1883
DACA (SS) 1883293 SEINE (SS) 1889
DOLPHIN (USS) 1889 SERPENT (HMS) 1872-76
EGERIA (HMS) 1897 SIEMENS (SS) 1875
ENTERPRISE (USS) 1883 SILVERTOWN (SS) 1884
FARADAY (SS) 1903 STEPHAN (SS) 1911
GAZELLE (SS) 1875 SYLVIA (HMS) 1886
GETTYSBURG (USS) 1876 TALISMAN (SS) 1883
GOLDFINCH (HMS) 1902-05 TRITON (HMS) 1882
KNIGHT ERRANT (HMS) 1880 VALDIVIA (SS) 1898
MICHAEL SARS (SS) 1910 VALOROUS (HMS) 1875

MURRAY, J. and LEE, G. V. The depth and marine deposits of the
Pacific. Reports on the scientific results of the Expedition to the
Tropical Pacific on USS Steamship ALBATROSS, August 1899 -
March 1900, no. XVII. Memoirs of the Museum of Comparative
ANNA TS WS Bp MO, No UO ios Iwme I9OO, EGO tl Az

ALBATROSS EXPEDITION TO THE TROPICAL PACIFIC 1899-1900

40

MURRAY, J. and RENARD, A. F. Report on deep-sea deposits based
on the specimens collected in the years 1872 to 1876. In “Report
on the scientific results of the voyage of HMS Challenger during
the years 1873-1876", 523 p., London: Longmans & Co., 1891.
Q115 CHALLENGER 1873-1876 vol. 2

CHALLENGER 1873-1876

NANSEN, F. The Norwegian North Polar Expedition 1893-1896.
Scientific Results, vol. IV-1904, vol. V-1906, Jacob Dydwad,
Christiania, Q115 N8 v.4, v. 5

NORWEGIAN NORTH POLAR EXPEDITION 1893-1896

- - - The bathymetrical features of the North Polar Seas with the
discussion of the continental shelves and previous oscillations of
Chiemms hone —linespr VOl nus, spt.celSs cole prea sune a JO Zr—ehebel 904.
Q115 N8 v.4
NORWEGIAN NORTH POLAR EXPEDITION 1893-1896

NASU, N. Particle size distribution in the vicinity off Sagami River
mouth, (The processes forming beach and dune sands), Journal
of the Faculty of Science, University of Tokyo, Section II--Geology,
Mineralogy, Geography, Geophysics, vol. X, pt. 1, pp. 65-103,
NOS O= NO Sine (USGS) G(620) T62

ASASHIO R/V 1950

- - - Oceanographic investigation in the Chukchi Sea during the summer
of 1958. The Scientific Reports of the Whales Research Institute,
no. 15, pp. 143-157, Tokyo, November, 1960. (LC) Serial Division

FUMI MARU No. 16 1958

NASU, N., IJIMA, A. and KAGAMI, H. Geological results in the Japanese
Deep Sea Expedition in 1959 -- Exploration of the Ramapo Deep
in the Japan Trench and the southernmost part of the Kurile
Trench by the RYOFU MARU. JEDS Contribution No. 6, Geological
Institute, University of Tokyo, The Oceanographical Magazine,
VOlnMlleEnonIey) pps 201214. March l960— 5s Serialeniles
RY COMM) MUNRO! ay)

NAVARRO, F. de P. Exploracion oceanografica del Africa Occidental
desde el Cabo Ghir al Cabo Juby -- Resultados de las campanas
del “Malaspina” y del “XKauen” en Mayo de 1946. Ministerio de
Marina, Instituto Espanol de Oceanografia, Trabajos, no. 20.
39 p. Madrid, 1947. GC 1 S7 No.20

XAUEN 1946
MALASPINA 1946

41

NEAVERSON, E. The sea-floor deposits I. General characters and
distribution. Discovery Reports, vol. IX, pp. 295-350, University
Press, Cambridge, 1934. Q115 Discovery v. 9

DISCOVERY (RRS.) 1925-1933
WILLIAM SCORESBY 1927-1932

NEUMANN, A. C. The configuration and sediments of Stetson Bank,
northwestern Gulf of Mexico. The Agricultural and Mechanical
College of Texas, A& M, Project 24, Reference 58-5T, Technical
Report No. 26., 124 p., February 1958. G52) f35No. Ze

DNS IN UNO IDN BYE, BISA, SID, LYST

NIINO, H. On the soundings from the sea bottom at the offing of Cape
Cook, Prince Harald Coast, Antarctic continent. Report of the
Japanese Antarctic Research Expeditions, no. Ile) appease —2 i,
January 1961, also in Journal of Tokyo University Fisheries
(Special ed.), vol. 1, no. 3, 1958. Serial File

SECOND JAPANESE ANTARCTIC RESEARCH EXPEDITION 1957-58
UMITAKA MARU 1957

- -- Study on the natural radioactivity of bottom deposits (II). Bottom
deposits in the vicinity of Takamatsu City, SetoInland Sea. Records
of ,Oceanographic Works in Japan, Special No. 4 (New Series),
Japanese National Commission for UNESCO, pp. 165-170, March
1960. Serial File under “Records of”

SHINYO MARU 1958

_-- Sediments of Oki Bankinthe Japanese Sea, Journal of Sedimentary
Petrology, vol. 18, no. 2, pp. 79-85, August 1948. Serial File
SOYO MARU 1941
SUIROBU MARU

NORIN, E. The sediments of the central Tyrrhenian Sea. Reports
of the Swedish Deep-Sea Expedition 1947-1948. Sediment cores
from the Mediterranean Sea and the Red Sea, vol. VII, Fasc. 1,
pp. 1-136, Géteborgs Kungl. Vetenskaps-Och Vitterhets-Samhalle,
1958, Q115 S8 v. 8-10

ALBATROSS 1947-1948
SWEDISH DEEP SEA EXPEDITION 1947-1948

NYBELIN, O. Introduction and station list. Report of the Swedish
Deep-Sea Expedition 1947-1948. Zoology, vol. I, fasc. 1, pp. 1-28.
GOteborgs Kungl. Vetenskaps-Och Vitterhets-Samhalle, 1958.
Q 115 S8 1947/48 v. 2 fasc. 1

ALBATROSS 1947-1948
SWEDISH DEEP SEA EXPEDITION 1947-1948

42

--- Zoological results of the “Skagerrak” expedition 1946. Introduc-
tion and station list. Goteborgs Kungl, Vetenskaps=och Vitterhets=
Samhalles Handlingar fj. 6, ser. B, band 5, no. ll. 12 p., 1947.
(Meddelanden Fran Géteborgs Musei Zoologiska Avdelning 118).
(DA) P50 Z5Gal\ EH

ALBATROSS 1947-1948
SKAGERRAK 1946

OFFICER, C. B. and WEBER, J. H. Useof continuous seismic profiles
in offshore explorations and engineering. Offshore, vol. 10, no. 6,
pp. 36-37, July 1959. Serial File

OLIVER, M. Carta pesca de los Baleares I. Este y Sur de Menorca.
Instituto Espanol de Oceanografia, Trabajos, no. 26, pp. 7-20,
Madrid, 1959. GCal Sv

XAUEN 1958

ORTH, Beitrage zur meereskunde, Annalen der Hydrographie und
Meritimen Meteorologie, Jahrgang der Hydrographischen Mitteil-
Uncen liwno. 15 sund.= lo) @pp. 302=310, N87 55 VIG SSSeAowlsi7,5

DRACHE 1874 INEZ MUS
METEOR 1873 POMMERANIA 1873

OSTROUMOV, E. A. and FOMINA, L. C. O formakh soyedinenii seri v
donnykh otlozheniyakh severo-zapadnoi chasti Tikhogo Okeana
(Types of sulfur compounds in the bottom sediments of the north-
western portions cf the Pacific Ocean) in Geologicheskiye
issledovaniya v dalnevostochnikh moryakh (Geologic studies in the
Far Eastern Seas), Akademiya Nauk SSSR, Trudy Instituta
Okeanologii, tom XXXII, pp. 206-214, 1960. Serial File

VITYAZ

OSTROUMOV, E. A. and VOLKOV, I. I. O formakh soyedinenii sery
vy donnykh otlozheniyakh Tikhogo Okeana u Novoi Zelandii (Forms
of sulfur compounds in the bottom sediments of the Pacific Ocean
near New Zealand), Akademiya Nauk, SSSR, Trudy Instituta Okeano-
logii, tom XLII, pp. 117-124, 1960. Serial File

VITYAZ

OTTMANN, F. Estudo das amostras do fundo recolhidas pelo N. E.
“Almirante Saldanha na regidao da embocadura do Rio Amazonas.
Missao da Diretoria de Hidrografia e Navegacao por ocasiao do
Ano Geofisico Internacional (Dezembro de 1958). Trabalhos do
Instituto de Biologia Maritima e Oceanografia, Universidade do
Riecitemeole le) no. 1, pp. (v-106, December) 1959 (IE) R52558599
R649 UIYSY

ALMIRANTE SALDANHA 1958

43

OTTMANN, F. and OTTMANN, J. M. Les sediments de l’embouchure
du Capibaribe, Recife, Bresil. Trabalhos do Instituto de Biologia
Maritima e Oceanografia, Universidade de Recife, vol. 1, no. 1,
pp. 51-69, December 1959. (LC) 525.7.99 R.29 1959

OWEN, D. M. ATLANTIS Cruise 151 to Mediterranean area, Scientific
Reporte NOnece Bottom samples and underwater photography.
Woods Hole Oceanographic Institution, Reference No, 49-8. 38 p.
January 1949. Q115 A88 No. 2

ATLANTIS CRUISE 151 1947-1948

PARR, W. J. Foraminifera. Reports-Series B (Zoology and Botany)
B.A.N.Z. Antarctic Research Expedition 1929-1931, vol. V, pt. 6,
pp. 235-392, B.A.N.Z.A.R. Expedition Committee, University of
Adelaide, The Hassell Press, Adelaide, May 1950. Q115 BANZ
SOI, 135 We B PEO

BRITISH-AUSTRALIAN-NEW ZEALAND ANTARCTIC RESEARCH
EXPEDITION (BANZ) 1929-1931

PEREZ MATEOS, J. Mineralogia de la fraccion ‘‘arena’’ de los
sedimentos marinos que se estudian. pp. 29-35, Boletin del
Instituto Espanol de Oceanografia, no. 90, Madrid, 15 February
1958. Serial File

XAUEN 55-7 & 56-1 1955-56

PERRY, R. B. A study of the marine sediments of the Canadian
Eastern Arctic Archipelago. Fisheries Research Board of Canada,
Atlantic Oceanographic Group, Manuscript Report Series (Ocean-
ographic and Limnological) no. 89., 80p., April1961. GC 854 C2M2
No. 89

LABRADOR July-October 1957

PETTERSSON, H. Three sediment cores from the Tyrrhenian Sea.
Meddelanden fran Oceanografiska Institutet i Goteborg, 15, Gote-
borgs Kungl. Vetenskaps-och Vittershets-Samhalles Handlingar,
Sjatte Foljden, ser. B band 5, no. 13, 94p., 1948. AS 284 G7
No, 11-20

SKAGERRAK 1946

44

- -- Teneur en radium des depots de mer profonde (PRINCESS-ALICE
II et CHALLENGER). Résultats des compagnes scientifiques
accomplies sur son yacht par Albert Ier Prince Souverain de
Monaco, fasc LXXXI, pp. 3-50, 1930. (LC) QL5 A3

CHALLENGER
PRINC ESSE-ALICE II

PHILIPPI, E. Die Grundproben der Deutschen Sudpolar-Expedition
1901-1903 in -- Drygalski, E. von, Deutsche Sudpolar Expedition
1901-1903 im Auftrage des Reicksamtes des Innern, band II.
Geographie und Geologie, heft VI, pp. 415-616. Berlin. 1910.
(LC) Q115 D49

DEUTSCHES SUDPOLAR EXPEDITION 1901-1903
GAUSS 1901-1903

PE GR eee SearandaRICSON, eDrss: Hydrography the western
Atlantic, bottom sediments off Portsmouth, New Hampshire. Woods
Hole Oceanographic Institution, Technical Report No. 6., 15.,
August 1947. GC 501 W8 No. 6-10

ANTON DOHRN R/V_ 1946
PHYSALIA R/V 1946

PICOTTI, M. Crociera talassografica Adriatica 1955, III. Tabelle
delle osservazioni fisiche, chimiche, biologiche e psammografiche,
Instituto Sperimentale Talassografico Trieste, Pubbl. N. 361,
Estratto dell’Archive di Oceanografia e Limnologia, vol. XI,
fasc. 3, pp. 371-377 and tables. 1960. GCl T80 No. 361

ADRIATIC THALASSOGRAPHIC CRUISE 1955

PIRIE, J. H. H. Scottish National Antarctic Expedition 1902-1904:
Deep sea deposits. Transactions of the Royal Society of Edinburgh,
VOlwexduDerpts 3, Session 1912-1913, pp. 645-086) 193.

(USGS) S (512) q E 52
SCOTIA 1902-1904
SCOTTISH NATIONAL ANTARCTIC EXPEDITION 1902-1904

PORTER, URQUHART, McCREARY and O’BRIEN CONSULTING EN-

GINEERS. Feasibility study for harbor development, San Clemente
Island, California. U. S. Navy, Bureau of Yards and Docks,
Eleventh Naval District, Public Works Office, San Diego, Californ-
ia. 74 p. December 1956. Uncatalogued.

45

PRATJE, O. Die bodenbedeckung der sudlichen und mittleren Ostsee
und ihre bedeutung fur die ausdeutung fossiler sedimente (43.
Beitrag zur geologie der meere). Deutsches Hydrographisches
Institut, Hamburg, Deutsches Hydrographische Zeitschrift, band
1, heft 2/3, pp. 45-61, June 1948. Serial File

PRVAV EE ©} Die sedimente des Stdatlantischen Ozeans. Erste
Lieferung-Correns, C. gewinnung und bearbeitung der boden proben,
A. Die verfahren der gewinnung und untersuchung der sedimente.
B. Schott, W. Die foraminiferen in dem aquatorialen teil des
Atlantischen Ozeans. 2. Lieferung - C. Zusammenstellung der
untersuchungsergebnisse nach stationen geordnet. D. Auswertung
der ergebnisse, Wissenschaftliche Ergebnisse der Deutschen At-
lantischen Expedition auf dem Forschungs und Vermessungsschiff
“Meteor” 1925-1927. Herausgegeben in auftrage der Notgemein-
schaft der Deutschen Wissenschaft von A. Defant, band III, Verlag
von Wi, des Gruytersiand Coy, berlin wand) eipzipey 29Sipaselo sie
Q115 Meteor bd. 3, Teil 2 and 3

METEOR 1925-1927
DEUTSCHEN ATLANTISCHEN EXPEDITION 1925-1927

RAO, M.S. Distribution of calcium carbonateinthe shelf sediments off
East coast of India. Journal of Sedimentary Petrology, vol. 28,
no. 3, pp. 274-285, September 1958, Serial File

INDIAN MINESWEEPERS 1952-1957

REED, J. J. and LEOPARD, A. E. Sediments of Cook Strait, New
Zealand Oceanographic Committee Publication No. 17, New Zealand
Journal of Science and Technology, Section B, ‘vol. 30, ime, I,
pp. 14-22, July 1954. GCl N45 No. 17

LACHLAN (HMNZS)

REVELLE, R. R. I. Marine bottom samples collected in the Pacific
Ocean by the CARNEGIE on its seventh cruise.

PIGGOT, C. S. Il. Radium content of ocean-bottom sediments. Scientific
results of cruise VII of the CARNEGIE during 1928-1929 under
command of Captain J. P. Ault. Oceanography II, Dept. of
Terrestrial Magnetism, Carnegie Institute of Washington. Pub.
556, 196 p., 1944. Q115 CARNEGIE 0-1-IV

CARNEGIE VII 1928-1929:

46

RICHARDS, H. C€. and HILL, D. Great Barrier Reef bores, 1926
and 1937 —~ descriptions, analysis and interpretations. Reports
ole thewGreat barrienmReet eGommittee, volves plblepss0RApril
MOA 2 USGS) i Sa(890) G32) vee5

GREAT BARRIER REEF 1926 - 1927

RICHTER, E. VON Liste der grundproben von der studienfahrt der
‘‘Minseroog’’ 1923 Senckenbergiana, Wissenschaftliche Mitteill-
ungen, Senckenbergischen Naturforschenden Gesselschaft in
Frankfurt a. M., band 10, heft 5, pp. 195-203, September 1928.
(USGS) S (530) F 884

MINSEROOG 1923

RICKETTS, N. G. and TRASK, P. D. The bathymetry and sediments,
Part 1, Scientific Results (of) The ‘‘Marion’’ Expedition to Davis
Strait and Baffin Bay under the direction of the U. S. Coast Guard,
1928, U. &. Treasury Department, Coast Guard, Bulletin No. 19,
Sik jos CGolPsOsy Wiveslatoyertonig IDS (Ge WO sz. ONS: WSCC IPs Ib; UO28~

MARION (USCG) 1928

RIEDEL, W. R. Siliceous organic remains in pelagic sediments, In-
SILICA IN SEDIMENTS, a publication of the Society of Economic
Paleontologists and Mineralogists, pp. 80-91, May 1959.

GC 771 S485
GUIDE (USCGS) 1923
PIONEER (USCGS) 1922
MID-PAC EXPEDITION 1953

RIIS-CARSTENSEN, E. The Godthaab Expedition 1928. Report on the
expedition. Kommissionen for Videnskabelige Undersdgelser i
Gronland, band 78, nr. 1, pp. 3-105, 1931. (USGS) (980) Mbd. 78
1931-1939

GODTHAAB 1928

ROSENBERG, L. A. Mikrobiologischeskaya kharakteristika gruntov i
vody Sredizemnogo Morya (Microbiological characteristics of the
bottom and water of the Mediterranean Sea). Akademiya Nauk SSSR,
Okeanolgiya, vol. 2, no. 1, pp. 109-117, Moskva, 1962. Serial File

AKADEMIK S. VAVILOV June-August 1960

47

SCHAEFERS, E. A. and SMITH, K. A. Shellfish explorations in the
Yakutat Bay area, Alaska, by the JOHN N. COBB, Spring 1953.
U. S. Fish and Wildlife Service, Commercial Fisheries Review,
vol. 16, no. 3, pp. l=lly Marzch eliG54eaSexialerpilie
JOHN N. COBB 1953

SCHAEFERS, E. S., SMITH, J. A. and GREENWOOD, M. R. Bottom fish
and shellfish explorations in the Prince William Sound area,
Alaska, 1954. U. S. Fish and Wildlife Service, Commercial Fish-
eries Review, vol. 17, no. 4, pp. 6-28, April 1955. Serial File

JOHN N. COBB 1954

SCHMIDT, J. Report on the Danish Oceanographical Expeditions
1908-1910 to the Mediterranean and adjacent seas, vol. I: I.
Introduction, pp. 1-48. III. Béggild, O. B. The deposits of the sea
bottom, pp. 255-269. Andr. Fred. Hést & Son, Copenhagen, 1912.
OH5eDs3eNor!

THOR 1908-1910

SCHULER, F. Untersuchungen tiber die machtigkeit von schlickschichten
mit hilfe des echographen. Deutsche Hydrographischen Zeit-
schrifts band 5,ehett.5/O,mpparccOaZeoleelo>2euse rialwrilie

GAUSS (VFS) May 1952

SKISHKINA, O. V. Khimicheskii sostav ilovikh vod Tikhogo Okeana
(Chemical composition of the interstital water of the Pacific
Ocean), Akademiya Nauk SSSR, Trudy Instituta Okeanologii, tom
XXXIII, pp. 146-164, 1959. Serial File

VITYAZ 1953-1955

- - - Sulfaty v ilovykh vodakh Chernogo Morya (Sulfates in the muds
of waters of the Black Sea), Problemy Khimii Morya, Akademiya
Nauk SSSR, Trudy Instituta Okeanologii, tom XXXIII, pp. 178-193,
1:95 9). eSenialebple

AKADEMIK VAVILOV 1956

SHUKRI, N. M. and HIGAZY, R. A. Mechnical analysis of some bottom
deposits of the northern Red Sea. Journal of Sedimentary Petrology,
vol. 14, no. 2, pp. 43-69, August 1944. Serial File

MAHABITH (RRS)
EGYPTIAN PRELIMINARY EXPEDITION TO THE NORTHERN RED
SEA 1934-1935

48

STEPHEN, A. C. The Sipunculids of Haifa Bay and neighbourhood,
The Bulletin of the Research Council of Israel, vol 7B, No. 3-4,
pp. 129-136, Oct. 1958. Records File EN3/EF40, RS 05788, 19
Jul. 62

STETSON, H. C. The sediments of the continental shelf off the eastern
coast of the United States. WHOI Contribution No. 178, Papers in
Physical Oceanography and Meteorology, Massachusetts Institute
of Technology and Woods Hole Oceanographic Institution, vol. V.,
no. 4; 47 p.. July) 1938. @€ 851 P15, v. 5 No. 4

STETSON, H. C. The sediments and stratigraphy of the East coast
continental margin; Georges Bank to Norfolk Canyon. WHOI.Con-
tribution No. 487,Papers in Physical Oceanography and Meteorology,
Massachusetts Institute of Technology and Woods Hole Oceano-
graphice Institution, vol. XI, no. 2; 52 p., August 1949. QC 851
IPI) Wo LL INOS Z

STETSON, H. C. -Part I. The Continental terrace of the western Gulf
of Mexico; its surface sediments, origin and development.

TRASK, P. D. -Part II. Chemical studies of sediments of the western
Gulf of Mexico. Papers in Physical Oceanography and Meteorology,
Massachusetts Institute of Technology and Woods Hole Oceano-
graphic Institution, vol. XII, no. 4, pp. 3-119, May 1953. QC851
P15 v. 12 No. 4

ATLANTIS 1947

STETSON, H. C. Bottom deposits. Contribution No. 5, Woods Hole
‘Oceanographic Institution, Part V. in ‘‘Scientific Results of the
Nautilus Expedition 1931.’’ Papers in Physical Oceanography and
Meteorology, Massachusetts Institute of Technology and Woods
Hole Oceanographic Institution, vol. II, no. 3, pp. 17-37, June 1933.
@OCESSIFP Srv. 2, No. 3

NAVA TEWSy (URS)! 1931
WILKINS-ELLSWORTH EXPEDITION 1931

STETSON, H. C. and SCHALK, M. Marine erosion of glacial deposits
in Massachusetts Bay. Woods Hole Oceanographic Institution
Contribution No. 52, Journal of Sedimentary Petrology, vol. 5,
no. 1, pp. 40-51, April 1935. Serial File

49

SMITH, R. J. and CRILLY, J. B. Application of X-ray diffraction to
oceanic soil analysis. U. S. Naval Civil Engineering Laboratory,
Port Hueneme, California, Technical Report R-213, Y-5015-01-001
(g)) 2Zepe 26) Octobermlgio2e

SMITH, W. D. Recent underwater surveys using low frequency sound
to locate shallow bedrock. Bulletin of the Geological Society of
America, vol. 69, no. 1. pp. 79-90, January 1958, Serial File

PASSAMAQUODDY BAY SURVEY 1951

SPETHMANN, H. Studien Uber die bodenzusammen-setzung der
Baltischen depression vom Kattegat bis zur Insel Gottland.
Laboratorium fur Internationale Meeresforschung in Kiel, Hydro-
grafische Abteilung nr.8,Wissenschaftliche Meeresuntersuchungen
Kommission zur Wissenschaftlichen Untersuchung der Deutschen
Meere in Kiel und der Biologischen Anstalt auf Helgoland, Neue
folge, 12th band, pp. 303-314, Scan Kiel, 1911 (USGS) 530qW 1
aiwel Neh Bde Sz

POSEIDON 1909

STARIKOVA, N. D. Nekotoriye danniye po organischeskomy veshchestvu
zhidkoi fazi osadkov Chernogo i Azovskogo morei (Some data on
the organic composition of the liquid phase of sediments of the
Black and Azov Seas) in Khimiya Morya (Marine Chemistry)
Akademiya Nauk SSSR, Trudy Okeanograficheskoi Komissii, tom X,
vyp. 2, pp. 30-48, 1960. (LC) T168.25, Tom X, vyp 2. 1960

VAVILOV 1956-1957

STARIKOVA, N. D. Organicheskii veshchesti zhidkoi fazi osadkov
severozapadnoi chasti Tikhogo okeano (Organic matter of the
liquid phase of the sediments of the northwestern Pacific Ocean).
Akademiya Nauk SSSR, Trudy Instituta Okeanologii, tom XXXII,
a5 WORN NOB

VASRNPAZ lO 5355

STARK, J. T. and DAPPLES, E. C. Nearshore lagoon sediments from

Raiatea, Society Islands. Journal of Sedimentary Petrology, vol.
11, no. 1, pp. 21-27, April 1941 Serial File

50

STETSON, H. C. and UPSON, J. E. Bottom deposits of the Ross Sea,
Woods Hole Oceanographic Institution Contribution No. 130.
Journal of Sedimentary Petrology, vol. 7, no. 2, pp. 55-66, August
(9SU6 Sercteul ks

BEAR 1934
Second Byrd Antarctic Expedition 1934-35

STETSON, T. R. Report on Atlantis Cruise No. 266 June-July 1961,
Woods Hole Oceanographic Institution, Reference No. 61-35, 24 p.
October 1961. Uncatalogued

ATLANTIS 1961 Cruise 266

STEWART, H. B. Oceanographic cruise report USC&GSS EXPLORER
1960. Seattle, Wash. to Norfolk, Virginia, 2 Feb. - 27 Apr. 1960.
Coast and Geodetic Survey, U. S. Department of Commerce. GPO,
Wash. D. C., pp. 100-120, 1960. GC 57 S8

EXPLORER (USCGS) 2 Feb. - 27 Apr. 1960

STRIDE, A. H. A linear pattern on the sea floor and its interpretation
Journal of the Marine Biological Association ofthe United Kingdom,
vol. 38, no. 2, pp. 313-318, June 1959. Serial File

SARSIA (RV) Sept. 1958

STUBBINGS, H. G. The marine deposits of the Arabian Sea. An in-
vestigation into their distribution and biology. The John Murray
Expedition 1933-34, Scientific Reports, vol. III, no. 2, pp. 32-158,
British Museum (Natural History), 1939. Q115 Murray 1933-34
v. 2 and 3

THE JOHN MURRAY EXPEDITION 1933-34
MAHABISS 1933-34

SUGIMURA, Y. and NOGUCHI, J. Content of organic matter in the
bottom sediments off Lutzow-Holm Bay collected: by the 2nd
Japanese Antarctic Research Expedition. Antarctic Record, vol.
12, no. 3, March 1961. Serial File or HO Route Sheet No. 936

Second Japanese Antarctic Research Expedition 1957-58
SOYA 1957-58

SUSSBACH, S. and BRECKNER, A. Die _ seeigel, seesterne und
schlangensterne der Nord-und Ostsee. Wissenshaftliche Meere-
suntersuchungen, Kommission zur Wissenschaftlichen Unter-
suchungen der Deutschen Meere in Kiel und der Biologischen
Anstalt auf Helgoland. Neue folge, 12th band, Abteilung Kiel, pp.
169-299, 1911. (USGS) 530q W76 wil ‘‘Kiel’’ N. F. Bd. 1112

POSEIDON 1902-07
51

SUTTON, G. Hy, BERCKHEMBER,) Hi) vand! SNAG, J, H-Physicall
analysis of deep sea sediments. Lamont Geological Observatory
Contribution No. 260, Geophysics, vol. XXII, no. 4, pp. 779-812,
October 1957. Serial File

VEMA 4 July-Sept 1954

SVIRENKO, I. P. Granulometricheskiy i mineralogicheskiy sostavy
donnykh otlozheniy morya Deyvisa (Granulometric and mineralogic
composition of the bottom sediments of the Davis Sea).
Arkticheskiy i Antarktischeskiy Nauchno-Is sledovatel’skiy Institut,
Glavnogo Upravleniya Severnogo Morskogo Puti, Ministerstva Mor-
skogo Flota SSSR, Informatsionnyi Byulleten Sovietskoi Ant-
arkticheskoi Ekspeditsii, no. 22, pp. 17-31, Morskoi Transport,
Leningrad, 1960. G 860 S581 No. 22

Oss UC e 2) 2) 1/

THOMAS, C. W., Commander - Bering Sea Patrol, 1948, Report, U.
S. Coast Guard, various pages and annexes, 1948. Q115 B51 1948
NORTHWIND (USCG) 1948

THORP, E. M. The sediments of Pearl and Hermes Reef. Journal of
Sedimentary Petrology, vol. 6, no. 2, pp. 109-118, August 1936
Serial File

THORP, E. M. Descriptions of deep-sea bottom samples from the
western North Atlantic and the Caribbean Sea. Scripps Institution
of Oceanography, Bulletin, Technical Series, vol. 3, no. 1, pp. 1-31,
IDSG Gist YS G3 Wicd

BACHE SIALIA
DISCOVERER SURVEYOR
GUIDE
LYDONIA
PIONEER
AMEONWEIDA, Ne meade lithologique de fonds recueilles dans les

parages de la Nouvelle-Zemble. Duc D'Orleans - Campagne Arctique
de 1907, 28 p., Charles Bulens, ed. Bruxelles, 1910. Q115Belgica
1907, Vol I Large.

BELGICA 1907

DUC D'ORLEANS CAMPAGNE ARCTIQUE DE 1907

52

THOULET, M. J. Relations entre la composition des sediments sous-
marins et les conditions des eaux superficielles. Bulletin de

l'Institut Oceanographique (Monaco) no, 470, 28 p., 1 February
1926. GCI Monaco 469-486

TODD, J. P. Shoal water deposits of the Bermuda Banks. Woods
Hole Oceanographic Institution, Contribution No. 191, Journal of
Sedimentary Petrology, vol. 9, no. 1, pp. 8-13, April 1939. Serial
File

TODD, R. Foraminifera from western Mediterranean deep-sea cores.
Reports of the Swedish Deep-Sea Expedition 1947-48. Sediment
cores from the Mediterranean Sea and the Red Sea, vol VII,
fasc, II, pp. 169-215, Gdteborges Kungl. Vetenskaps-Och Vitterhets-
Samhalle, 1958 Q115 S8 v. 8-10

ALBATROSS 1946-48
SWEDISH DEEP SEA EXPEDITION 1947-48

TOLBERT, W. H. and AUSTIN, G. B. On the nearshore marine
environment of the Gulf of Mexico at Panama City, Florida.
U. S. Navy Mine Defense Laboratory Tehnical Paper No. TP 161,
104 p., May 1959. GC 521 U505
SEASITE (Project) 1955-58

TOOMBS, R. B. Some characteristics of Bute Inlet sediments.
Canadian Committee on Oceanography, Transactions of the Royal
SocietyavotiiGanadas volt... ssieries lnm pp m59 05 mune mh9 50.
GC-83 C2

TRASK, P.D. Originand environment of source sediments of petroleum.
American Petroleum Institute Project 4, 1926-31, Gulf Publishing
Co., Houston, Texas, 323 p., 1932. (USGS) 467 T 69

API Project 4 1926-31

TYLER, S. A. A study of sediments from the North Carolina and
Florida coasts. Journal of Sedimentary Petrology, vol. 4, no. l,
PpasllywApril 1934. Serial eile

LYDONIA (USCGS)

URRY, W. D. Radioactivity of ocean sediments, VI. Concentrations of
the radio-elements in marine sediments of the southern hemisphere
American Journal of Science, vol. 247, no. 4, pp. 257-275, April
1949. Serial File

NORTHWIND 1946-47

53

VASNETSOV, V. A. K gidrologii Karskogo morya (Hydrology of the
Kara Sea). Trudy Gosundarstvennogo Okeanograficheskogo Instituta,
tom. I, ivypusk. 2=3,)spp.5 5-46, Sle (OG Cle do eaelemoS 1y/is2

PERSEY-14 Sept 1927

VAYSSIERE, A. J. Resultats des campagnes scientifiques accomplies
sur son yacht par Albert I-er, Prince Souverain de Monaco.
Mollusques, Heteropodes et Eupteropodes provenant des campagnes
des yachts Princesse-Alice I et II et Hirondelle II. fascicule
LXXI, 383 p. 4, June 1927. Imprimerie de Monaco. 1927. (LC)
QL 5.A3

HIRONDELLE 1886-1915
PRINCESSE-ALICE I & II 1886-1915

VERNON, J. H. and BADER, R. G. Recent sedimentation and related
oceanographic factors in the west Mississippi delta area. The
Agricultural and Mechanical College of Texas, Department of
Oceanography and Meteorology, Texas A and M Research
Foundation, A and M Project 142 and 197, Reference 61-6T and
61-10F, 187 pp., May 1961.

VINOGRADOVA, P. S. Issledovaniye rel'efa dna i gruntov raiona
Korytova (Investigation of the bottom relief and sediments in the
Korytov region), Kolebaniy chislennostii usloviya promysla donnykh
ryb v Barentsevom More. (Variations in the number and trade con-
ditions of bottom fish in the Barents Sea). Trudy Polyarnogo
Nauchno-Issledovatel'skogo Instituta Morskogo Rybnogo Khozyaistva
i Okeanografiy Imeni N. M. Knipovicha (PINRO), Vypusk X, pp.
1862197, 1957. (EG) SH lo M's

KASHALOT 1935-54 PERSEY-2 1954
PERSE 21935

WALTON, W. R. Ecology of living benthonic Foraminifera, Todos
Santos Bay, Baja California. Scripps Institution of Oceanography
Contribution No. 814, Marine Foraminifera Laboratory Contribution
No. 23, Journal of Paleontology, vol. 29, no. 6, pp. 952-1018,
November 1955. (USGS) G (200) J83p

WANGERSKY, P. J. Sedimentation in three carbonate cores. Journal
of Geology, vol. 70, no. 3; pp. 364-374, May 1962. Serial) mile

54

WEIBULL, W. The thickness of ocean sediments measured by a re-
flection method. Meddelanden fran Oceanografiska Institutet i Gote-
borg. 12. Goteborgs Kungl. Vetenskaps-och Vittershets-Samh§@lles
Handlingar, Sjatte FOljden, ser. B., band 5, no. 4, 17 p., 1947.
AS284 G7 No. 11-20

SKAGERRAK 1944-45

WISEVEAN, iJ De HH. and BENNE DT, oH: the distributionjof organic
carbon and nitrogen in sediments from the Arabian Sea. vol. III,
no. 4, pp. 194-221, 1940. Q115 Murray 1933-34 v. 2 and 3
MAHABISS 1933-34
THE JOHN MURRAY EXPEDITION 1933-34

WIG III, RG | Ig Bottom sediments of Georges Bank, Journal of
Sedimentary Petrology, vol. 31, no. 2, pp. 165-188, June 1961.
Serial File

ALBATROSS III (USFWS) 1957

WISEMAN, J. D. The relation between paleotemperature and carbonate
in an equatorial Atlantic pilot core. Journal of Geology, vol. 67,
no. 6, pp. 685-690, November 1959. Serial File

ALBATROSS 1947-48
SWEDISH DEEP SEA EXPEDITION 1947-48

WOLFENDEN, R. N. Scientific and biological researches in the North
Atlantic conducted by the author on his yachts ‘‘The Walwin”’
and the ‘‘Silver Belle.’’ Memoirs of the Challenger Society, no. 1,
234 p.,Rebman Ltd. London, 1907. Q115 Wolf
SILVER BELLE 1904-07
WALWIN 1904-07

ZAITSEVA, E. D. Yemkost! obmena kationov osadkov Tikhogo Okeana
(Exchange capacity of cations of Pacific Ocean sediments), Trudy
Instituta Okeanologii, Akademii Nauk, SSSR, tom XXXII, pp. 128-
136, 1959. Serial File

VITYAZ 1953-55

ZIEGLER, J., HOFFMEISTER, W., GIESE,G., and TASHA, H. Discovery
of Eocene sediments in subsurface of Cape Cod. Science, vol. 132,
no. 2437, pp. 1397-98, 11 November 1960, Serial File

CAPE COD 1960

55

HUMBOLDT STATE COLLEGE. An oceanographic study between the
points of Trinidad Head and Eel River. Humboldt State College,
Arcata, California, Annual Report-1959 for the California Water
Pollution Control Board, 1959. TD 425 C2

INSTITUTO ESPANOL DE OCEANOGRAFIA Exploracion oceanografica
del Africa Occidental Campanas del ‘‘Malaspina’’ en 1947 y 1948
en aguas del Sahara, desde Cabo Juby aPunta Durnford-Registro
de operaciones, Boletin del Instituto Espanol de Oceanografia no.
23, 28 p. 26 January 1950. Serial File

MALASPINA 1947-58 Cruise 475 and 485

INSTITUTO ESPANOL DE OCEANOGRAFIA Exploracion oceanografica
del Africa Occidental Campana del ‘‘Malaspina’’ en enero de 1950
en aguas del Sahara, desde Punta Durnforda Cabo Barbas, Registro
de operaciones, Ministerio de Marina, Boletin del Instituto Espanol
de Oceanografia, no. 38, 12 p., Madrid 15 July 1950. Serial File

MALASPINA Cruise 501 January 1950

INSTITUTO ESPANOL DE OCEANOGRAFIA Campana del ‘‘Tofino’’
‘**T,.5212°’ (13 a 20 Diciembre de 1952). Registro de operaciones:
sondeos con cable. Cuadro 1. Instituto Espanol de Oceanografia,
Trabajos,, no.) 922, opp. lash Maldridt elo 53 eG Gi aleSimNonecilayZ9

TOFINO T-5212

INSTITUTO ESPANOL DE OCEANOGRAFIA Campanas del ‘‘Xauen’’
en 1947 y 1948 en el Mar de Albor4n y en el Estrecho de Gibraltar,
Boletin del Instituto Espanol de Oceanografia, no. 18, 53p.,
30 June 1949. GCl Spain 1949 Nos. 13-24 or Serial File

XAUEN Cruise X-474, 481, 482, 488 Sept. 1948

INSTITUTO ESPANOL DE OCEANOGRAFIA Campanas biologicas del
‘*Xauen’’ en las costas del Mediterraneo marroqui, Mar de Alboran,
Baleares Noroeste y Cantabrico espanoles en los anos 1952, 1953
y 1954, Registro de operaciones, Boletin del Instituto Espanol de
Oceanografia, now 103,)) pp. 3=150,) mebruarny, e961) (Sexialaerilie

XAUEN 1952-54

INSTITUT OKEANOLOGII, ADADAMIYA NAUK, SSSR. Bottom sediment
tables ‘‘Ekvator’’ Atlantic Ocean, 3-31 October 1958. (NODC)
137.5 A-2

HKVEATIORT Octs ig 58

56

INSTITUT OKEANOLOGII, AKADEMIYA NAUK, SSSR. Bottom sediment
tables ‘‘Ekvator’’ Atlantic Ocean, 3-31 October 1958. (NODC)
W355) AeA

BKVATOR Oct) 1958

INSTITUT OKEANOLOGII, AKADEMIYA NAUK, SSSR. Bottom sediment
tables) *“bkKvator”” Atlantic Ocean, 28 March = 25 )April/1958.
(NODC) 137.5 A-1

EKVATOR 1958

INSTITUT OKEANOLOGII, AKADEMIYA NAUK, SSSR. Bottom sediment
tables lst cruise ‘‘M. Lomonosov’’ Atlantic Ocean, November 1957.
(NODC) 137.4 A-2

MIKHAIL LOMONOSOV 1 November 1957

INSTITUT OKEANOLOGII, AKADEMIYA NAUK, SSSR. Bottom sediment
tables Second Cruise ‘‘Mikhail Lomonosov”’ Atlantic Ocean, 2 Mar.-
5 June 1958, 30 p. (NODC) 137.4A2
MIKHAIL LOMONOSOV Cruise 2 Mar-Jun 1958

KOBE MARINE OBSERVATORY. The report of the oceanographical
observations on board the R. M.S. ‘‘Syunpu Maru’’ in the Maizuru
Bay (Oct. 15-18, 1947). The Kobe Marine Observatory, The Data
of the Oceanographical Observation, no. 7, 10 p., 1947. GC 821
Kobe No. 7

SYUNPU MARU (RMS) 1947

SCRIPPS INSTITUTION OF OCEANOGRAPHY. List of cores collected
on CAPRICORN (1952-53), CUSP (1954) and ACAPULCO TRENCH
(1954) Expeditions, University of California, LaJolla, pp. Ss
1 May 1958, GC 380 S4L7

CAPRICORN EXPEDITION 1952-53
HORIZON 1952-53
SPENCER F. BAIRD 1952-53

SCRIPPS INSTITUTION OF OCEANOGRAPHY. List of cores collected
on CAPRICORN (1952-53), CUSP (1954) and ACAPULCO TRENCH
(1954) Expeditions. University of California, LaJolla, 30 p., 1 May
1958. GC 380 S4L7

CHUBASCO (ACAPULCO TRENCH) 1954
CUSP 1954
CAPRICORN 1952-53

57

SCRIPPS INSTITUTION OF OCEANOGRAPHY DOWNWIND Expedition
1957-58. List of cores and dredge samples copied from shipboard
logs. University of California, LaJolla, 28 p., May 1958. GC771
S4 D7

DOWNWIND EXPEDITION 1957-58
SPENCER F. BAIRD
HORIZON

SCRIPPS INSTITUTION OF OCEANOGRAPHY. List of cores and dredge
samples copied from shipboard logs on the Fanfare Expedition
O59.

FANFARE EXPEDITION 1959

SCRIPPS INSTITUTION OF OCEANOGRAPHY. Pacific bottom samples.
MUKLUK Expedition, July-August 1957. Core and dredge samples.
Information from shipboard coring log. 6 p.,1957. GC 851 S4 M9

MUKLUK EXPEDITION 1957

SCRIPPS INSTITUTION OF OCEANOGRAPHY. Northern Holiday core
log August-September 1951, Scripps Institution of Oceanography
7 p., 1951. GC 781 S4 N87 also GC 771 S4 S5
NORTHERN HOLIDAY 1951

U. S. COAST AND GEODETIC SURVEY. Bottom sediment Analysis
Work Sheets (for USC and GS Ship Hydrographer) vol 2, May to
Junesi955 .Or TS SlsUSZavy. 2 ;

HYDROGRAPHER (USCGS) May-June 1955

U. S. NAVY HYDROGRAPHIC OFFICE. Bottom Sediments, North Atlantic
Ocean and Adjacent Seas 1949-53. 246 p., May 1958. H. O. TR-36
(unpublished)

AMOS 1949-53

U. S. NAVY HYDROGRAPHIC OFFICE. Survey results of BuShips-
Hydrographic Office anchor testing - bottom sediment sampling
conducted in Norfolk-Little Creek area, York River mouth and Key
West harbor approaches 2 October through 7 November 1956,
U. S. Navy Hydrographic Office, H. O. Misc. 16547, 10 p.,March
1957. H. O. Misc. 16547

Anchor Test 1956

58

U. S. NAVY HYDROGRAPHIC OFFICE. Operation Deep Freeze 60,
1959-60, Oceanographic survey results. Technical Report TR-82,
ZS Do, Swine WNoils ists (O); ase ti
DEEP FREEZE 60 Expedition 1960
BURTON ISLAND (AGB-1)
EASTWIND (WAGB-279)
GLACIER (AGB-4)

U. S. NAVY HYDROGRAPHIC OFFICE. Operation Deep Freeze II

1956-57 oceanographic survey results. Technical Report TR-29.
155 p., October 1957. H. O. TR-29

ATKA (USS)

DEEPFREEZE II 1956-57

GLACIER (AGB-4)

NORTHWIND (USCGS)

STATEN ISLAND (USS)

U. S. NAVY HYDROGRAPHIC OFFICE. Oceanographic survey results
Project 572, July - Sept. 1955 USS REQUISITE (AGS-18) Beaufort
Sea, Amundsen Gulf, Dolphin and Union Strait, Shepherd Bay.
U. S. Navy Hydrographic Office, Wash. D. C. 170 p., April 1957.
HO Misc. No. 16366

REQUISITE (AGS 18) USS 1955

U. S. NAVY HYDROGRAPHIC OFFICE. Oceanographic survey results
Task Force Five 26-August - 20 Sept. 1955, USS STATEN ISLAND
(AGB-5) Beaufort Sea, Chukchi Sea, Bering Strait, Bering Sea.
Hes@s) Mise. No: 15047236; 6 ps, March: 1956..HO! Misict! 15047236

STATEN ISLAND (USS - AGB-5) 1955

U.S. NAVY HYDROGRAPHIC OFFICE. Oceanographic observations in
Arctic waters, Task Force Five and Six, Summer-Autumn 1956,
USS REQUISITE (AGS-18), USS ELDORADO (AGC-11), USS ATKA
(AGB-3) USCGC EASTWIND (WAGB-279) Technical Report TR-58,
89 p. October 1960. HC TR-58

ATKA (USS-AGB- 3)

Task Force 5 and 6
EASTWIND (USCGC-WAGB-279)
REQUISITE (USS-AGS-18)
ELDORADO (USS-AGS-11)

59

U. S. NAVY HYDROGRAPHIC OFFICE. Oceanographic observations,
Arctic waters, Task Force Five and Six, Summer - Autumn 1957.
Technical Report TR-59, 45 p., November 1959. HO TR-59

ATKA (USS-AGB-3) EASTWIND (USCGC-WAGB-279)
Task Force 5 and 6 WESTWIND (USCGC-WAGB-281)
SPAR (USCGC-WAGL-403)

U. S. NAVY HYDROGRAPHIC OFFICE. Bottom sediment analyses.
Supplement No. 1 to oceanographic observations U.S.F. & W.S.
M/V Theodore N, Gill Cruises I-IX 1953-54, U. S. Navy Hydro-
graphic Office, Wash. D. CeH.nOy Mise.) 1560) 0;el 9s ps) June Mg 5e.
HO Misc, 15610

THEODORE N. GILL (M/V) Cruise I-IX 1953-54

U. S. NAVY HYDROGRAPHIC OFFICE. Oceanographic survey results
Bering Sea area Winter and Spring 1955. Technical Report TR-46,
oi py Aprile 95 oso Ouwlin=4 OM lO 5s

BURTON ISLAND (AGB-1)
NORTHWIND (USCGC-WAGB-282) 1955

U. S. NAVY HYDROGRAPHIC OFFICE. Unpublished bottom sediment
analysis summary and work sheets - Bottom samples taken aboard
CYRUS FIELD during cable laying operations south and east of
Newfoundland and Georges Bank, 1953-55, vol. 1. QE581 U52
Wo whe

CYRUS FIELD (Cable Layer) 1953-55

USS WHIPPOORWILL. Hydrographic-oceanographic-meteorological
data collected by USS WHIPPOORWILL (MSC 207) during the period
27-31 July 1959 while operating at Karatsu, Japan. Ltr. to Hydro-
grapher MSC-207/01: an/3160 Ser: 292, 17 August 1959. (NAV-
OCEANO Records) File Hl, RS 12654, 31 August 1959

WHIPPOORWILL (USS) 1959

U. S. NAVY HYDROGRAPHIC OFFICE. Unpublished summary sheets
of samples taken by various U. S. Navy ships in the Mediterranean
Sea by Ocean Survey Division - James Underwood in charge.
Sept.) Olf=janwoZ

SWERVE FLOOD (project)

60

U.S. NAVY HYDROGRAPHIC OFFICE. Samples taken along submarine
cable routes by Bell Telephone Laboratories, and analyzed by the
U.S. Navy Hydrographic Office.

U. S. NAVY HYDROGRAPHIC OFFICE. Unpublished data of bottom
samples taken during June 1962 by Naval Oceanographic Office
for Naval Ordnance Laboratory off Ft. Lauderdale, Florida

AKL-43

U.S. NAVY HYDROGRAPHIC OFFICE. Unpublished summary sheets of
sediment samples taken by the USS ATKA and USCGC WESTWIND
dummp@eroject, Arctic 1958. 1U., S. Hydrographic j@ftice Cruise
00602

ARCTIC 1958
ATKA (USS) 1958
WESTWIND (USCGC) 1958

U. S. NAVY HYDROGRAPHIC OFFICE. Unpublished summary sheets
of sediment samples taken by U. S. Hydrographic Office Cruises
in the Arctic region in 1959.
ING IGM ILS)

61

Variation of Area of 1° Quadrangles with Latitude

Latitude (°) Approximate
Area of 1°
Quadrangle
(nautical miles )

0 3,768
10 3,534
20 3,307
30 3,118
40 2,763
45 2,555
50 2,324
55 2,079
60 1,813
65 1,533
70 1,241
75 941
80 631
85 317
89 63
90 0

62

LEGEND

-CORE SAMPLE

-SURFACE SEDIMENT SAMPLE

IN U.S. NAVAL OCEANOGRAPHIC

a

QUADRANGLE THE NUMBER OF ANALYSES

FIGURES INDICATE FOR EACH ONE-DEGREE
FILED

OFFICE ON 1 JANUARY 1963.

+t

iRvert4

4

7

5{_ 13] 11 40 \og~77 Sis)

3} 12)G0 4 24

-

2|_ 3} 17) 15) 19) 271

;

2

J

/2

Tishaa!

1

|
1

a ae -

1
|

FIGURE 16 EASTERN NORTH ATLANTIC OCEAN—DISTRIBUTION OF SUBMARINE SEDIMENT SAMPLE ANALYSES
a

LEGEND 2
——CORE SAMPLE Zz

33—SURFACE SEDIMENT SAMPLE

FIGURES INDICATE FOR EACH ONE-DEGREE
QUADRANGLE THE NUMBER OF ANALYSES
FILED IN U.S. NAVAL OCEANOGRAPHIC
OFFICE ON 1 JANUARY 1963,

FIGURE 17 WESTERN NORTH ATLANTIC OCEAN—DISTRIBUTION OF SUBMARINE SEDIMENT SAMPLE ANALYSES
65

if

va 7
oa

ey

2. gle level lini yr Sega
ry : keine

senna aceon

dscenips

SASAIVNY 31dWVS LNaWIG3S INIAYWANS JO NOLLNSIISIQ—NV390 JUNVILY HINOS 81 38NdId

€96L AYVNNVE |

NO 331430 SIHdVYDONVIDO IVAYN 'S Ni
31d S3SAIWNV JO Y38WNN 3JHL JIONVEGVNO
33YD3G-INO HDVI YO4 FLVDIGNI S3YNDI4

Ddwvs LN3WIGAS 3JDV4INS —zi |

JdWvs JWOD ——f
N3931

LEGEND
f34—CORE SAMPLE
LIZ—SURFACE SEDIMENT SAMPLE

FIGURES INDICATE FOR EACH ONE-DEGREE
QUADRANGLE THE NUMBER OF ANALYSES FILED
IN U.S. NAVAL OCEANOGRAPHIC OFFICE ON

1 JANUARY 1963,

FIGURE 19 EASTERN NORTH PACIFIC OCEAN—DISTRIBUTION OF SUBMARINE SEDIMENT SAMPLE ANALYSES:
69

LEGEND

Ale SAMPLE
3 —SURFACE SEDIMENT SAMPLE

FIGURES INDICATE FOR EACH ONE-DEGREE
QUADRANGLE THE NUMBER OF ANALYSES FILED
IN U.S. NAVAL OCEANOGRAPHIC OFFICE ON
1 JANUARY 1963.

FIGURE 20 WESTERN NORTH PACIFIC OCEAN—DISTRIBUTION OF SUBMARINE SEDIMENT SAMPLE ANALYSES
7

es
peakeetee ert slept
(eee

she e bietci ita A CPAReee AERA ENAT MY 8 SH

SISATVNYV J1dWVS LN3WIGIS INIYVWENS JO NOUNBIISIO~NVIDO DisIOVd HLNOS NYBLS¥9 LZ IWNDId

20El

Ov

COO Lee

“£96 AYWANYE L
NO 331dJO DIHAVYDONVIDO IVAYN 'S 1 NI
Galld SASAIVNVY 4O 438WNN 3HL JIONVYaYNO
3WIOIGINO HDVA YO ALVDIGNI S3¥NdI4

JdWvS LNIWIGaS pK
Wdwvs 3OI—z
N3931

‘ia
§

thi f

Ag
:
i

popes re,

oT

eet \

SISAIVNY 31dW¥S LN3WIG3S INIYVYWENS JO NOILNBIMISIO—N¥390 JIsID¥d HINOS N¥31SIM ZZ INO

“E96L AYVANYE |

NO 3314JO DIHAVYDONVIDO IVAYN SN NI
3d S3SAIVNY 4O Y38WNN 3JHL JIONVYGVNO
334¥930-3NO HDVF YOI FLVDIGNI SIYNSI4

Wdwvs LN3awid3as eal
JdWVS JOD -——£
QN3931

i

EB
feist
ug

ee

ODES eee
CORES ERReeeee

2091

v
ie

ican tet

24

zl}
REEnE

lo}
ys: +
4

NEL

FIGURE 23 INDIAN OCEAN—DISTRIBUTION OF SUBMARINE SEDIMENT SAMPLE ANALYSES
7

CORE SAMPLE
L12— SURFACE SEDIMENT SAMPLE

FIGURES INDICATE FOR EACH ONE-DEGREE

——

FILED IN U.S. NAVAL OCEANOGRAPHIC

QUADRANGLE THE NUMBER OF ANALYSES
OFFICE ON 1 JANUARY 1963.

LEGEND
pipes, SAMPLE
1 —SURFACE SEDIMENT SAMPLE

FIGURES INDICATE FOR EACH ONE-DEGREE
QUADRANGLE THE NUMBER OF ANALYSES FILED
IN U.S. NAVAL OCEANOGRAPHIC OFFICE ON
1 JANUARY 1963.

FIGURES SHOWN FOR 5° QUADRANGLES
NORTH OF 85°N.

FIGURE 24 ARCTIC OCEAN—DISTRIBUTION OF SUBMARINE SEDIMENT SAMPLE ANALYSES
79

aiid

i
\S

Lp

LEGEND

CORE SAMPLE
SURFACE SEDIMENT SAMPLE

FIGURES INDICATE FOR EACH ONE-DEGREE

2.

iz

QUADRANGLE THE NUMBER OF ANALYSES FILED
IN U.S. NAVAL OCEANOGRAPHIC OFFICE ON

1 JANUARY 1963.

Y
Wi
\ \y

<

S

S

myer,
ai

=
a
at SS
(ae, =
=== S|
a
SoSsssSss=s5
ey ee
SSS
SEER EES

Ps
iit
ee

FIGURE 25 SEAS AROUND ANTARCTICA—DISTRIBUTION OF SUBMARINE SEDIMENT SAMPLE ANALYSES

OSI-UL “TEE
ugoung “3 uyof :1oynE “TT

*ao1jJO o1ydeidoues20
TEAEN ‘S'f au} Je JUSMIaSeUEW pue
uoTdaTIOD ye WauUlIpes ouTieUIgnsS :31}h *

AZo[Oa aut IeyA *

T

e

syuauntpag auyreuqns *¢

uo}eJUeMAIpag *

4

sjuew{pag WOH “T

OST-U.L “TTT
WW

weoung “Mf wyof :royyne

“2010 o1ydesrdouea00

TeEARN “S'f au} 3 JUeMIAZeULW pue
uopdaTI[OD e}eC JUsMIpag suyAeMIgNS ‘apy °

AZo[Oa) auyIeyA *
sjuatipag euyreuigns *
UO}FEWUSTATPES *
syuem}pes WoRO" ~

ANOS

‘uMoUs S} Say[Zuerpenb aaidep-auo Aq uoIyNqT1}SIp

aPlA P[IOM pue pajs}] ole Sadmmos eyed *9d1HJO
otyderdoues00 [eAeN ‘S'N eu} 3e eyep JUSUTIpas
aulrewmigns Suy10}s pue Zutssaooad ‘Suyanoes jo
gpoyjeul ay} Saq{iosap }10dar TeopuYysa} SIUL

*soanSty pue arty opydessoryqiq

Sutpnyout ‘dgg * 961 ISHBny “ueoung "YH
uyof 4q ¥O1dAO OIHAVUDONV HOO TVAVN
‘$° FHL LV LNSWaDVNVW CNV NOLL

-OATIOO VLVC LNAWIGaS ANIUVWANS
ao1JO s1ydesrdoueed0 [BABN “SN

*uMoUsS S] Se[Zuerpenb aaidap-auo Aq uoTNgTIySIp

aplA plIOA pue pajs}] ere sevInos eyed “3010

aqydesZoueas0 [eAEN “S’N oy} 3e eyep JUSUITpes
auyrewmgns Juy10}s pue Jujsseooid ‘Zuyanoas jo
gpoyjew ay} Seq{1osap y10der [eoyuyse} STYL

*saan31y pue at} oyydessoq[q1q

Suypnyouy “dgg * P96 sNBny ‘weoungd "H
uyof 4q AO1AA0 OIHAVUDONV HOO TVAVN
“$°N AHL LV LNAANSDVNVW CNV NOLL

-OFTI00 VLVG LNAWIGdS ANIUVINENS
ad1JJO d1yde1d0ueeI0 [BAEN “S “N

OSI-UL “TET
uvoung ‘3M uyof :1oyyNe “TT
‘ao1YJO o1yde1s0uea09
JRAEN ‘SN ay} Je JUOMaZeULW pue
uoT}DaT[ND Vyeq JUsUTIpag sulsvUgngS +9131} *

cal

AZojOa) autre *
syuemIpag auyreuqns *
uoTJeUSMATpas *
sjuemIpas woyog °

ANH

OGI-UL “TEE
veoung “a uyof :royyne “TT
*ao1JO olydeisouea00
TRARN "S'f. OU} Je JUSMTAaSeUey pue
wO}}daTT0D eye WeuUlypas supseMgnsS :a1}1 “t

AZ0[0a) JULIE “Ff
syuatapag auyreuqns “¢
UO}JEJUSTA TPIS “Z
sjuaul{peas WOYVC_ “T

‘uMoUsS ST Seysueapenb aaidap-auo Aq uopynq}1}SIp

APIA P[IOM pue pajs}] are saoinos e}eq *3d1}JO
otyderdouea00 [TeAeN “S'f) ay} ye Byep Juattpas
aulreugns Suy10}s pue Butssaooad ‘dutanoas jo
Spoyjeul oy} Saql1osap y10da1 [eoyUYyIe} STL

*saandty pue opty o1ydesrdoryqiq

Sutpnyout “dgg * P961 ISNBny ‘uvoung "y

uyof Aq AOIAAO OIHAVUDONV AOO TVAVN

‘SN GHL LV LNANGADVNVW GNV NOIL
-OATIOO VLVC LNAWIGES ANIUVINGNS

ao1JO o1ydes1d0ue|00 [VAEN *S ‘ND

‘uous Ss} se[Zuerpenb aerdep-auo Aq uoFNqI13STp

aplA plo pue pays}] ore saoanos eyed * 201330
atydeardouea20 [VAN “S'N 9y} ye Eyep JUSUIpas
aulrewgns Juy10}s pue Zuysseooid ‘dupanoes jo
spoyjau ay} Saq{1osep }10der TeoTUYyse} STYL

“samy pue ayy ofydesdoqTqiq

Surpnyouy “dgg * 7961 ISNSNy ‘ueounq "A

uyof 4q AD1dAO DIHAVUDONV OO TVAVN

‘SO FHL LV LNSNADVNVW GNV NOLL
-O3TIOO VLVG LNAWIGAS ANIUVINENS

Ei) 89) otyde.120ue8200 TeAeN "SN

=
‘ i :
ni
i
-

oy
‘
ce
4)
%
fs

‘pais