zooplankton taxonomy and sorting programs University … · I -rlil - -, -- I I , AD-756 661 Drift...

47
-rlil I - -, -- I I , AD-756 661 Drift Station Biclogy zooplankton taxonomy and sorting programs University of Southern California prepared for Office of Naval Research JANUARY 1973 Distributed By: NuBs National Technical Information Service U. S. DEPARTMENT OF COMMERCE

Transcript of zooplankton taxonomy and sorting programs University … · I -rlil - -, -- I I , AD-756 661 Drift...

-rlil I - - , -- I I ,

AD-756 661

Drift Station Biclogyzooplankton taxonomy andsorting programs

University of Southern California

prepared for

Office of Naval Research

JANUARY 1973

Distributed By:

NuBsNational Technical Information ServiceU. S. DEPARTMENT OF COMMERCE

UNIVERSITY OF SOUTHERN CALIFORNIA

Department of Biological Sciences

FINAL REPORT

on

DRIFT STATION BIOLOGY:

Zooplankton Taxonomy and Sorting Programs

September, 1969-October, 1972

Prepared under contract with theOffice of Naval ResearchN00014-67-A-02 69-0013 i RTT? _. gNR 307-270 A): Approvfd fo: pu ici

NATIONAL TECHNICALINFORMATION SERVICE

U S Department of CommerceSpringfield VA 22151

Reproduction in whole or in part Principal Investigator:is permitted for any purpose of Dr. H. Re Fernandezthe United States Government. Assistant Professor of Biology

University of Southern CaliforniaLos Angeles, California 900"17

UnclassifiedSecurity Classification

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I ORIGINATING ACTIVITY (Corporate outhe) 2|. REPORT SECURITY CLASSIFICATION

University of Southern California UnclassifiedDepartment of Biological Sciences 26. GROUP

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Final Report on Drift Station Biology: Zooplankton Taxonomy andSorting Programs.

4. OESCRIPTIVt NOTES (Type o1 teport and inclusive date*)

Final Regort Set. 1969-October 19725, AU THORIS) (First name, middle initial, 14t name)

Hector R. Fernandez

SREPORT DATE 0?e. TOTAL NO. OF PAGES 76. No. OF NEPSJanuary, 1973

CONTRACT OR GRANT NO. e. ORIGINATOR-$ REPORT NUM@ERIS)

N00014-67-A-0269-0013b. PROJECT NO.

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this report)

d.

10. OlSTRIUTION %TATEMENT

Dintribution of this document is unlimited.

11, SUPPLEMENTARY N'JTES l12. SPONSORING MILITARY ACTIVITY

Office of Naval Research

13. AUSTRACT

The taxonomic studies of the USC Arctic Project are briefly summar-ized. This report includes a description of the practical taxonomicguides, the sorting program and studies which were derived from thesorting program. This work has two main objectives, first the iden-tification of Arctic zooplankton, and second a more detailed studyof the biology of some of the organisms, to form the basis forbiochemical and physiological investigations. The report alsoincludes a list of stations and of the organisms identified.

FORM (PAGE !)0102.014.6600 Security Classification

UnclassifiedSecurity Classification

14. K LINK A LINK 8 I.INK CKErY WONOS

ROLE WT ROLE WY ROLE WT

V -Final Report, Drift Station Biology

Zooplankton Taxonomy and SortingPrograms, USC.

4

DD Novo*1473 Unclassified(PAGE 2) Security Classification

UNIVERSITY OF SOUTHERN CALIFORNIA

Department of Biological Sciences

FINAL REPORT

on

DRIFT STATION BIOLOGY

Zooplankton Taxonomy and Sorting Programs

September, 1969-October, 1972

Prepared under contract with theOffice of Naval ResearchN00014-67-A-0269-0013NR 307-270

Reproduction in whole or ii. part Principal Investigator:is permitted for any purpose of Dr. H. R. Fernandezthe United States Government. Assistant Professor of Biology

University of Southern CaliforniaLos Angeles, California 90007

N" Iel

Table of Cortents

Intrng nction. .* * o * . . * 0 * * 0 * 0 0 0 * * * 0 * * . 1

Taxonomic Guides. . . . . 2 * . . . . . 0 * * 0 * * * * * * . 2

Zooplankton Sorting ProgramSampling method . . . ... . . . .. . . . . ...... 6Sampling processing. . . . . . . . . . . . . . . . . . . . . 6Results of sorting program ........ .. .. .. . 8

Vertical Distribution and Life Historl, of theAnnelid Pelogobia longicirrata. . . . . . ... . . . e

The Growth Cycle and Related VerticalDistribution of the Pteropod, sii-tellahelicina, in the Central Arctic Ocean ...... . 9

Taxonomy and Distribution of the ArcticSpecies of Lucicutia (Copepoda:Calanoida) . . . . .10

On the Ostracod Fauna of the Arctic Bas..n . . . . . 0Annual Vertical Distribuion of Calanuihvperboreus in the Central Arctic Ocean. . . . . . .11

Contributions, 1969-1972 ....... . ........ .13

Tables I-XIII: Zooplankton Collections from T-3between February 27, 1970 and February 2, 1973 ....... . .15

rn~m

II

Introduction

The current activities of the USC Arctic Project range from

taxonomic descriptions of Arctic zooplankton to physiological and

biochemical investigations of the adaptations of selected species.

In this report we summarize only those activities and findings

which are immediately related to the taxonomic contributions of

the project.

It is clear to all students of Arctic biology, that much

remains to be done. When a present day biologist directs his

j attention to the Arctic, he is immediately faced with the problems

of the identification of the organ'-'.-ms which are found there as

well as with the small amount of background information on the

biology of the animals which is usually necessary in order to

design appropriate ecAperimeits. With these two problems in mind,

the main thrust of our taxonomic effort has been directed towards

tie identification of the marine fauna and producing taxonomic

guxides which will enable any biologist to readily identify Arctic

zooplankton. Furthermore, through systematic collections in terms

of tirae and deptho we have been able to carry out additional studies

on -he biology of selected species which in our estimation contri-

bute sign:ificantly to ecology of the Arctic Ocean.

This report covers the period from September 1969 until

October 1972

2

Taxonomic Guides

To assist o-her members of thi3 project as well as other

scientists interested in Arctic biology, we have prepared a series

c practical taxonomic gmides to aid in the identification of Arctic

zooplankton. Of great help in the production of these guides was

the fact tt,.t the University of Southern California had been en-

gaged in surveys of the Arctic fauna for almost two decddes.

A large amount of taxonomic information was thus already on hand.

The guides have beer prepared in such a manner that even the non-

specialist can use them readily. They have been published as

technical reports entitled "Taxonomic Guides to Arctic Zooplankton",

in six separate issues:

Zooplankton (I): Amphipods of the Central ArcticEuphausiids of the Arctic Basinand Peripheral Seas

Zooplankton (II): Medusne of the Central ArcticSiphonophores of the Central ArcticCtenophores of the Central Arctic

Zooplankton (III):Species of the Arctic Ocean ChaetognathsPteropods of the Central ArcticDecapods of the Central Arctic

Zooplankton (IV): Key to the Calanoid Copepods of theCentral Arctic Ocean

Zooplankton (V): Pelagic Polychaetes of the CentralArctic Basin

Zooplankton (VI): Appendicularians of the Central ArcticMysids of the Arctic Ocean and

Confluent SeasField Guide to Arctic Zooplanktonic

CrustaceansOstracods of the Central Arctic

Complete reference to these guides is available in the list of

........... -11 -7

3

contributions (pp. 13-14).

Preparation of these guides required identification of organ-

isms collected earlier in the central Arctic from the ice stations

(ARLIS I, II, and T-3) and the nuclear submarines, Sea Dragon and

Sea Skate. Scattered collections from peripheral seas made from

drifting ice stations and coast guard cutters, Northwind (Sept.

1963), Burton Island (Sept. 1960), and Eastwind (July-August 1967)

were also examined. Because material collected from peripheral

seas was relatively small, the generalized guides to species in

most cases, could only be constructed for central Arctic zooplank-

ton. The guides, however, provide enough information of general

nature which is applicable to the principal taxonomic groups and

can be useful to scientists who work on zooplankton from the

peripheral seas as well.

Each guide Consists of dichotomous keys and illustrations of

adult zooplankton anatomy. All have been constructed so that very

little or no dissection of the specimen is necessary for identifi-

cation. Pertinent references to the literature dealing specifically

with the individual species as well as the taxonomic group have

been included in each guide to provide additional information fUr

anyone requiring more detailed information. Furthermore, discus-

sions of taxonomic methods, terminology and discussions in depth

on individual species are provided whenever possible.

During the preparation of these guides, established interna-

tional specialists in the different taxonomic groups have been

4

called upon for comment and advice whenever it was required. We

would like to express our gratitude to the following colleagues

for their helpful advice.

Dr. A. Buchmann AppendiculariansHamburg, Germany

Dr. B. Frost CopepodsDepartment of OceanographyUniversity of WashingtoL

Dr. J. C. Vaupel von Klein CopepodsRijks Museum of Natural HistoryWest Germany

Dr. Cadet Hand MedusaeBodega Marine Laboratory

Dr. G. 0. Mackie MedusaeUniversity of British Columbia

Dr. 0. S. Tatersall MysidsGreat Britain

Dr. M. V. Angel OstracodsNational Institute of OceanographyGreat Britain

Dr. G. B. Deevey OstracodsFlorida State Museum

Dr. C. W. Hart, Jr. OstracodsAcademy of Natural SciencesPennsylvania

Dr. E. I. Schornikov OstracodsAcademy of SciencesUSSR

Dr. K. Fauchald PolychaetesHancock FoundationUniversity of Southern California

Dr. Olga Hartman PolychaetesHancock FoundationUniversity of Southern California

m • •I =. - •. = =

Dr. John GarthHancock FoundationUniversity of Southern California

The guides were subjected to rigorous evaluation tests in

which the principal criteria were accuracy and degree of ease in

establishing the identification of the organism. This work has

required, not only the examination of hundreth of samples taken

throughout the years, but also comprehensive review of the liter-

ature of the Arctic fauna as far back as the late 18th century.

The responsibility for coordination and editorial work in

the production of the guides was given to Ms. Hester Kobayashi.

6

Zooplankton Sorting Program

Sampling Method

Sorted under this program were samples collected from Ice

Island, T-3, with 1 meter diameter, 215 micrometer mesh, closing

nets towed vertically at a uniform rate of 20 meters per minute.

Samples were collected from March 1970 to September 1970 by

Mr. John Dawson and Mr. Lloyd Ellis, of USC, and from December

1970 to January 1972 by members of the University of Washington

T-3 Program under Dr. T. S. English.

The following sampling protocol was used:

tiarch-Sept. 1970 December 1970-Jan. 1972

Depth (m) Increments (m) Depth (m) Increments (m)0 to 300 50 0 to 400 25300 to 900 200 400 to 500 100900 to 1500 300 500 to 900 2001500 to 2000 500 900 to 1500 300

1500 to 2000 500

Sample Processing

The preliminary processing of the collected samples was done

under the direction of Mr. John Dawson. Undergraduates were

trained to recognize the major groups of zooplankton prominent in

the Arctic water column. This function has involved eight under-

graduates partially supported under the Federal College Work Study

Program.

With the help of these student assistants, samples were com-

pletely separated into the following general taxonomic groups and

and the numbers of the specimens recorded'

7

Taxonomic groupschaetognathaappendicularia ( larvaceans)nemertinapolychaetactenophorahydrozoascyphozoasiphonophorapteropodaamphipodaIopepoda

The identification of animals to genera and species, only a

small portion of which is complete, has been handled by specialists

in the USC group. The data have been recorded in special tabulation

sheets and arranged for easy retrieval for computer treatment in the

future. -All samples and data are stored in the Hancock Foundation

of the University of Southern California. Ta',les I-XIII summarize

the e.-tent of the sorting work to the present.

.4)

%i

8

Results of the Sorting Program

The sorting program had two principal objectives. First, it

was designed to provide additional information of the faunal

content of the central Arctic Basin and thereby enable'us to

produce more complete and accurate taxonomic guides. Second,

through the systematic collection at discrete depths with closing

nets over a two year period, it was possible to accumulate a

wealth of synoptic information on the distribution of zooplankton

in time and space over a long period of time. Analysis of this

information has now yielded a large amount of information on ver-

tical migrations and life cycles. This information in turn allow-

ed us to select those key species which can serve as models in

studying vertical migrations of zooplankton populations as well as

those interactjins between organisms and the environment which

play an important role in the formation and behavior of sonar

scattering layers of biological origin. The studies which already

have been completed are summarized below.

Vertical Distribution and Life History of the AnnelidPelogobia longicirrata

Pelagobia longicirrata is the most common pelagic polychaetein the central Arctic Basin. It is a cosmopolitan species whichis found not only in the Arctic but in deep waters of other oceansas well. Since very little is known about the biology of pelagicpolychaetes it was decided to analyse the presence of Pelagobiain our plankton samples in order to study its vertical distribu-tion and life cycle.

The results indicate that the majority of the animals arelocated between 300 and 500 meters throughout most of the year.The specimens found in this depth range are primarily breedingadults over 13 segments in size. In the spring and summer, the

9

percentage of animals which are found below 500 meters increases.Ho-." er, most animals found below 500 meters tend to be less than13 segments in size with the smallest specimens usually associatedwith the greatest depths. It was also found that 'he period ofthe year during which the percentage of animals increases below500 meters is closely correlated with the breeding season. Ourobservations suggest that adults spawn between 300 and 500 metersin the spring and that the eggs or larvae, or both descend todepths below 1000 meters. Then as the larvae develop they ascendgradually.

This study was carried out by Mr. Douglas Yingst.

The Growth Cycle and Related Vertical Distributionof the Pteropod, Spiratella helicina,

in the Central Arctic Ocean-- The mechanisms which give rise to aggregations of plankton

communities in the water column are not well understood. However,it is known that a number of factors both of environmental andbiological origins can influence the formation and behavior ofthese aggregations. As an approach to this problem the pteropodS. helicina was selected as a model organism because of itspresence in the 50 meter scattering layer in the Arctic, its re-lative abundance, dependence upon particulate material for food,and ease in recognition. Here we report on a study of its growthcycle and verticAl distribution.

The growth and reproductive cycle of S. helicina in the cen-tral Arctic Ocean was studied by examining samples collected fromalong the drift paths of ice stations ARLIS I, II, and T-3. Shelldiameters were measured, and gonadal development examined by his-tological means. Vertical distribution in the water column wasalso investigated.

S. helicina has an annual life cycle; spawning occurs mainlyduring the spring and summer months and the oldest animals dieby March. Maturation of young into males occurs as the animalsreach about 0.7 mm diamete2 (February-April) and to hermaphroditesby the time they reach about 0.8 mm (May). The young double their

size during the months of October to January. This growth rateslows down at the time of sexual maturation and through the majorspawning period but picks up again during the fall and winter.Growth and maturation during the winter months suggests that somefood must be available to S. helicina during the dark period ofthe year when phytoplankton is least available.

The analysis of the vertical distribution indicates thatthe youngest juvenile forms tend to remain predominantly in the first

f

10

50 meters interval of the water column (0.2 mm to 0.4 mm), there-after remaining within the first 100 meters until maturation.Animals larger than 0.9 mm seem to be dispersed in the water columnduring the peak period of primary productivity and concentratedin the top 100 m when food is less abundant.

This study was carried out by Ms. Hester Kobayashi.

Taxonomy and Distribution of the Arctic Speciesof Lucicutia (Copepoda: Calanoida)

Analysis of approximately 400 plankton hauls from the ArcticOcean revealed the presence of Lucicutia polaris Brodsky, L.pseudopolaris Heptner, and L. anomala Brodsky in samples collec-ted in deep waters. The two former species are closely relatedbut differ in morphological and biolegical characteristics of theadults and juvenile stages. The male of L. anomala is describedfor the first time. These species have a wide geographical dis-tribution in the Arctic Ocean. They inhabit the Arctic bottomwater and show different but overlapping ranges of vertical dis-tribution. L. pseudopolaris is most abundant at a deptb of about1500 m; L. polaris preferentially lives at a depth of about 2000m; and L. anomala is found in waters deeper than 2000 m but ismost abundant at depths exceeding 3000 m.

This study was performed by Mr. Julio Vidal and recentlyappeared in the Bull. So. Calif. Academy of Sciences. 70(l):23-30,1971.

On the Ostracod Fauna of the Arctic Basin

This study involved the analysis of plankton and undericecollections from drift stations ARLIS I, ARLIS II and T-3. Fivespecies of ostracods have been identified, among which, one isnew to science and one is a new record in the Arctic Ocean.

Conchoecia borealis maxima is the predominant species in theBasin and is found in collections from the first 1500 meters ofthe water column.

Conchoecia elegans is found together with C. borealis maximain collections from the first 750 meters. The Arctic specimensappear larger than those collected at lower latitudes in theAtlantic. On the basis of the variation in sizes, it appears thata taxonomic revision should be considered.

Conchoecia skogsbergi, the 'long form' of the C. rotundagroup, is very common in the Antarctic and north Atlantic, but isa new record in the Arctic. This species is similar to the speciesdescribed by Angel (1968) but the present form is larger. Recent

investigation shows that this species also varies considerably insize at different latitudes, thus requires taxonomic revision too.

A female of a new species of Bathyconchoecia has been collec-ted and is still under study.

Acetabulastoma arcticum, earlier described by Baker and Wong(1968) as Paradoxostoma rostratum, is a paras..tic form which in-fests the amphipods, Gammarus wilkitzkii and Gammaracanthusloricatua. Although other species of Sammarids have been examined,these are the only two species infested by Acetabulastoma.

I Mr. Yuk maan Leung was assigned to study the ostr;ods.

Annual Vertical Distribution of Calanus hyperbgreusin the Central Arctic Ocean

Calanus hyperboreus is the largest and one of the most abun-dant copepods in the central Arctic Basin. We have carried outa study of the biology of this copepod with special emphasis onvertical distribution of copepodite stages II through V and ofthe adult males and females over a two year period.

During the molting sequence from copepodite stage II to adultform, the most rapid growth occurs during July, presumably coin-ciding with the phytoplankton bloom. Our study of the verticaldistribution patterns of the different stages suggest that thereare three different types. Copepodite stages II to V show onetype which is characterized by an undulating annual vertical mi-gration. For example the maximum concentration of stages II-Vcopepodites occurs at depths between 300 and 500 meters in winter.During the spring there is a gradual migration towards the surface.At the end of the summer they descend once again gradually to re-main at depths of 300 to 500 meters during winter.

Adult females are mainly found at depths of 100 meters in thespring, and as the season progresses they appear to descend at a.rate of 50 meters per month. However during the summer they arefound everywhere from the surface to a depth of 300 meters. Itis thought that the females which migrate downwards in the springremained there and that those found at the surface are newly moltedfemales. In the fall the population centered at 150 meters. ByDecember, however, they are distributed from near the surface to450 meters. It is possible that those adult females which wereconcentrated in the fall at 150 meters remained near the surfaceduring December, and those females found at greater depths arethe result of molting from stage V coppoc.ites which are found indeep water in December.

12

The vertical distribution of adult males centers between 400_and 800 meters and therefore is generally deeper than that of thefemales. They also differ in that they are only present duringthe spring and early summer. It is at this time when we foundup. tO 30% of the females gravid.

Careful analysis of the life span of the various stagessuggests that in the Arctic Basin C. -hperboreus has a generationlength of about three years.

This work was carried out by Mr. John Dawson.

.rc

g

13 --

Contributions1969-1972

Published:

Vidal, J. 1971. Taxonomy and Distribution of the Arctic Speciesof Lucicutia (Copepoda: Calanoida). Bull. So. Calif. Acad.Sciences. 70(l):23-30.

In preparation:

Dawson, J. Annual Vertical Distribution of Calanus hyperboreusin the Central Arctic Basin.

Kobayashi, H. The Growth Cycle and Related Vertical DistributionSpiratella helicina in thM Central Arctic Ocean.

Leung, Y. M. On the Ostracod Fana of the Arctic Basin.

Yingst, D. Vertical Distribution and Life History of the AnnelidPelogobia lonqicirrata.

Technical Reports:

Zooplankton (I): Arphipods of the Central Arctic...J.R. TencatiEuphausiids of the Arctic

Basin and Peripheral Seas ...... Y.M. Leung

USC Technical Report 2 (1970)H. Kobayashi, ed.

Zooplankton (II): Medusae of the Central Arctic ..... W.D. Shirleyand Y.M. Leung

Siphonophores of the CentralArctic ................. . . .... Y.M, Leung

Ctenophores of the CentralArctic

USC Techinical Report 3 (1970)H. Kobayashi, ed.

Zooplankton (IV): Key to the Calanoid Copepods of

j the Central Arctic Ocean ........ J. Vidal JUSC Technical Report 5 (1971)H. Kobayashi, ed.

iA

14

2zqoplanktn,,-AV):- Pelagic Polychaetes -of the

-~-- -Central Arctic Baain#..........D.R. YinqstUSC Technical Report 1(1972)-

ZooplAnkton- (VI): Appdfndicularians of the Central

l~yidsof the Arctic Ocean andCdonf-luent Seas

Field Guide to Arctic Zooplank-=W -~toniicF-CrustaceanO

Ostracods of the Central Arctic

USC Technical Report 2 (11972)-I. Kobayashi, ed.

'4vT V!-

Tables I.-XIII*: Zooplankton Collections fromT-3 between Irebruary 27, 1970and February 2, 1972

*code used in Tables1=sorted to species2=partially sorted tospecies

3=not sorted to species

1. 2~ 3. 1 22-27-7 -1 ,

3D '3 041 .4l "I41 09/ " -77 I., :4 '4.: 2* .. u-.]~,

S D 1330 S-0 X4, 1342 3 127D 1471 50 xC10 150-130 x'D 1S45 200-150 x X70 1.4,2S-.3* 0£D 1510 300-250 X

110 1920 5O0-O £ X10 20:0 500-300 X X13 3-2-70 1ON) 84' 23' 112' 401 700-500 1537 x X140 1133 900-7JO X15D 3-3-70 O33 S4 23' 113' 0' 1200-900 1580 x1 D 11:5 1S00-1200I'D 3-6-70 1340 84* 22' 113' 28' 50-0 1730I 'D 135S

19D 1420 100-50NoI17 150-100 x x100 15 200-150 X x211) 1750 2S-200 x x1925 300-250 x230 3-9-70 105 84 21' 113' 28' 500-300 1715 X K240 11%0 700-500 x x3-10-70 3039 00 22' 13' 26' 900-700 1683 x20 1154 1200-1000 I270 3-11-70 1107 84' 23' 112' 370 1200-900 1S6S280 3-12-70 1121 84' 21' 112* 350 1500-1200 168029D 3-13-70 0651 84' 22' 112* 35' 100-50 1660 x x300 0912 50-0-p31b 0935 I32D 1005 150-100 x

2SO-200330 1040 150-00 X x34D 1S 300-250 xS - S7 Surface x33-1-70 0 64* 111 113* 40' S-0 161037D 1320 100-50 x x39D 1345 00S39D 341S 150-100 x x x43D 1445

15.-20041D 150 300-250 x x420 165 500-300 X x430 3705 700-500 K44 1935 64' 1' 113' 400 900-700 X$1305

1200-900 X4%0 3-16-70 i135 84- 14' 114' 10' 1500-1200 2087 X41D 3-1.7-70 0910 I4' 13) 114* 42' 100-0 2197 X48D MS 00-04 1105 2000-1500 190.13D 3-17-1O 1410 500-490 Xsit, 1455 400-300 X1530 200-100 X),20-70 1435 84* 08' 114' 2S0 50-0 207S X1Al0 150-100 X(L 1525 100..50 KIss 1200-150

0 1705 2S0-200177300-250 X3-22-70 G43 84* 09 13o 56 SO-0 97 xOAS 6 ,SO-O

f1o 102 100-504110 1027 100-50 x x'A4D 13 150-100 x xSO 11A I05-10061230 200-150 x441) 5300 250-200

4 325 200-IS0 x xCV40 1315% 250-200 K X119D 1425 300-250 x701) 11 O'IOD 1'4 30f*',Sn x

500-300 x720 1,- *,!-.00 x'131 ?,60 "71/0-WO

-a 40 04 R Rd U I.3

- ~ ~ ~ ~ ~ ~ s -- -

- - - - - - - - -

xx x.x x

X X X

X x xx

x xx xx

xxx

x x

x x x x

x x x x x xx x x xx xx x

xx x X xx x x

,. x XXxx x x x:

x .xx x x

x x x xx x x x

x xxx x xx x x

x x X %

- x x x I11

x x x xxx x X x

x x .1

x x

I lx

L

U13;T1 I t il lu

W. 1 2 3 1231

2210 70- -.,

7bbD 2330 !900)-700 X

710 3-30-70 135# 16'III 1132, 12 00-00 1763 X

79 1535 510-u x

970 14-55-70 05 S13 113* O74 1500-1200 X80 1500-1200 x

SID 3-29-70 9905 SO I 112* 20105 X

1000 1636 10-0x

03 12 ISO-lO0

940D 1750 20IOx

10 2950 250-2001030 2025 300-2S0 x x10D 2100 500-300 x x

105 3-3000 800G 18' 112* 394 900-700 1 X107 235 1200-90010 3-31-70 120 84* 18 i2' 38' 1500-1200 176 X90 4-5-70 130 84* 17' 112* 41' 50-0 1770 X

0 115 100-70so 6 X95" 12 100-50 X

110 4--0 iO 4 1' 11'3 O 20-90 o6

96D 4-07 ISO-100 x1176' 4' 150-100 1 X

. 1S3 100-15 x

110 4-1670 026 250-200 x x170D 040 50-0010 10001 300-250 x10 120 300-250 X x

104D 2100500-303 x

100 210 500-300, x x10 1255 700-500 x10 220 700-500 x10 4-6-70 1340 5 O17 112" 36 900-72) x10 4-7-70 84 17' 1123 41 900-72b 7 x.270 4-6-70 Il G 15' 112" 53 3 900-700 1 X12l0 1 900-700 x1300 4-1-70 1430 84 261 112* 36' 1200-900 1762 x111 10 1200-900 x1340 4-10-70 1 83 84 16 112* 40' 100-1200 1609 x13's0 1405 1500-1175 x116D 4-14-70 1420 84' 24' 112* 06' SO-O0 13 X

117D 0940 50-0IND 1000100-S0

1370 10.20 1~00-50 K1320 1045 150-100 K143D 1101US-100 x14410 1'i4s e200-150 . x

123D 122020SOx124D 13S 250-200

2 1450a) I ~300-25 0 X127D 1525 300-250 X128D 1610 00-300 x

12D11 500-300 xx

I I

13D 4-15-0o 43 84" 22 12 4 0if 4. 700-SOO 151 I3 7OSO0

13DtI 900-700134 4-16-70 1230 40 22* 111].* 5s* 12CL-900 159o

13e.D1400'200-9Ano13D 4-17-70 145 84* 220 112* 04' M0(0-12i00 12 X

1o7D 1420500-1200

1301502o0.G.100140D 17o rao-4010

140 4-241-70 1215 440 21, In1" set1 .0-0 I7

1430 VXJ'.al-lo0

14',D 2',.0-200o

,14I _

,4-21-7 14'.0 10 0l1 " 0')' 300_111-0

, IX

2 ~ta

1 2 3 123 1 2 1 23 1 23 1 23 1 23 1 2 32 331 24 12 31 2 1 2iL21

xx x x x xx x X xX

x x x xx x x x x

x x x x x x x.x x x x xX

x x x

x x x

xx xIx x x xxx ~ ~ x X X X x .xy

x xx x x xX x x xX

XXx x x xx x x X X X x

x x x x xxXX X X X x x

x x x x x xxxx x x x x

x x x x

x x X x

x x x x x

x x K 'x x

x~ x XK X S

xx x x x xx x x x

x x xx x x x z

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