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Fishery bulletin of the Fish and Wildlife Service - NOAA

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176 FISHERY BULLETIN OF THE FISH AND WILDLIFE SERVICE<br />

TABLÉ 6.—Deviations <strong>of</strong> individual cruise frequencies <strong>of</strong> lengths <strong>of</strong> larvae <strong>and</strong> postlarvae from <strong>the</strong> average<br />

frequency l <strong>of</strong> <strong>the</strong> 9 cruises <strong>of</strong> <strong>the</strong> season <strong>of</strong> 193%<br />

Aim, 34A<br />

Length<br />

6<br />

7<br />

8<br />

9<br />

10<br />

U<br />

12<br />

13<br />

14<br />

16<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

22<br />

аз<br />

24<br />

25<br />

26<br />

27<br />

23<br />

29<br />

30<br />

37<br />

51<br />

Loa<br />

0.477<br />

.602<br />

.699<br />

.778<br />

.845<br />

.903<br />

.964<br />

1.000<br />

1.041<br />

1.079<br />

1.114<br />

1.148<br />

1.176<br />

1.204<br />

1.230<br />

1.255<br />

1.279<br />

1.301<br />

1.322<br />

1.342<br />

1.362<br />

1.380<br />

1.398<br />

1.415<br />

1.481<br />

1.447<br />

1.462<br />

1.477<br />

1.668<br />

1.708<br />

Average number per cruise<br />

Observed values «<br />

Number<br />

8,470<br />

2,773<br />

1,045<br />

421<br />

225<br />

112<br />

43<br />

10 4.29<br />

2.14<br />

1.44<br />

1.49<br />

.77<br />

.36<br />

.37<br />

.67<br />

.37<br />

.17<br />

.17<br />

.16<br />

.14<br />

.03<br />

.09<br />

.11<br />

.14<br />

.14<br />

.03<br />

.03<br />

.01<br />

Loa number »<br />

13.93<br />

13.44<br />

13.02<br />

12.62<br />

12.35<br />

12.05<br />

11.63<br />

11.00<br />

10.63<br />

10.33<br />

10.16<br />

10.17<br />

9.89<br />

9.66<br />

9.67<br />

9.76<br />

9.57<br />

9.23<br />

9.23<br />

9.20<br />

9.16<br />

8.48<br />

8.95<br />

9.04<br />

9.15<br />

9.15<br />

8.48<br />

8.48<br />

8.00<br />

Theoretical<br />

values '<br />

Loo number ><br />

•14.00<br />

13.41<br />

12.98<br />

12.63<br />

12.36<br />

12.05<br />

11.56<br />

11.10<br />

10.72<br />

10.33<br />

10.15<br />

10.00<br />

9.82<br />

9.72<br />

9.61<br />

9.48<br />

9.36<br />

9.27<br />

9.16<br />

9.08<br />

9.00<br />

8.90<br />

8.83<br />

8.76<br />

8.67<br />

8.60<br />

8.60<br />

8.45<br />

8.00<br />

7.36<br />

I<br />

Der.<br />

-0.40<br />

-.18<br />

-.60<br />

-1.05<br />

-1.28<br />

-1.45<br />

-1.65<br />

II<br />

Dee.<br />

-0.20<br />

-.49<br />

-.10<br />

-.14<br />

-1.04<br />

-1.75<br />

-1.55<br />

III<br />

Dev.<br />

-0.13<br />

-.07<br />

+.23<br />

+.11<br />

-.18<br />

-.45<br />

-.29<br />

-.25<br />

-.02<br />

Cruises<br />

IV<br />

Deo.<br />

+0.26<br />

+.24<br />

-.10<br />

-.33<br />

-.96<br />

-.37<br />

-.10<br />

-.62<br />

-.42<br />

V<br />

Dec.<br />

-0.28<br />

-.32<br />

+.04<br />

+.42<br />

+.80<br />

+.25<br />

+.18<br />

-.25<br />

+.06<br />

-.03<br />

-.16<br />

+.30<br />

VI<br />

See.<br />

-0.04<br />

+.61<br />

+.39<br />

+.07<br />

+.24<br />

+.62<br />

+.72<br />

+.51<br />

+.36<br />

+.27<br />

+.46<br />

+.30<br />

+.18<br />

VII<br />

Dm.<br />

-0.06<br />

-.64<br />

-.24<br />

-.31<br />

-.62<br />

-.77<br />

-.44<br />

-.02<br />

-.02<br />

+.62<br />

+.70<br />

+.90<br />

+.88<br />

+.58<br />

+.87<br />

+1.22<br />

+1.13<br />

+.73<br />

+.84<br />

+.92<br />

VIII<br />

Da>.<br />

-Ô. 80<br />

-.67<br />

-.33<br />

. -.12<br />

+.04<br />

+.25<br />

-.24<br />

+.03<br />

-.01<br />

-.06<br />

-.31<br />

-.53<br />

+.01<br />

+.15<br />

+.07<br />

IX<br />

Dee.<br />

-Ï.4Î<br />

-.81<br />

-.64<br />

-.56<br />

-.44<br />

-.26<br />

-1.11<br />

-.43<br />

-.40<br />

+.18<br />

-.53<br />

-.31<br />

+.15<br />

+.55<br />

+.34<br />

+1.11<br />

+.62<br />

+1.06<br />

+1.23<br />

+1.44<br />

+1.51<br />

+.97<br />

+1.42<br />

+1.85<br />

1 Deviations were taken from <strong>the</strong> <strong>the</strong>oretical ra<strong>the</strong>r than observed values. The <strong>the</strong>oretical values were derived from <strong>the</strong> observed<br />

values by fitting straight lines to <strong>the</strong> points resulting from <strong>the</strong> plot <strong>of</strong> logarithm <strong>of</strong> numbers against logarithm <strong>of</strong> lengths in<br />

fig. 6.<br />

ï From 3 to 12 mm., inclusive, <strong>the</strong> average was <strong>of</strong> <strong>the</strong> first 7 cruises; from 13 to 51 mm., inclusive, it was <strong>of</strong> 9 cruises.<br />

'10 was added to <strong>the</strong> logarithm <strong>of</strong> each number in order to simplify notation in <strong>the</strong> case <strong>of</strong> decimal numbers.<br />

There is, in addition, external evidence that <strong>the</strong> chosen series <strong>of</strong> homologies is<br />

correct <strong>and</strong> <strong>the</strong> alternate series incorrect.<br />

The geographic distribution <strong>of</strong> successive stages needed to fit <strong>the</strong> alternate<br />

series would not be in harmony with any possible system <strong>of</strong> drifts. The 3- <strong>and</strong> 4-mm.<br />

larvae <strong>of</strong> cruise IV were <strong>of</strong>f Long Isl<strong>and</strong> <strong>and</strong> <strong>the</strong> 6- to 8-mm. larvae <strong>of</strong> cruise V were<br />

mainly in <strong>the</strong> <strong>of</strong>fing <strong>of</strong> <strong>the</strong> sou<strong>the</strong>rn coast <strong>of</strong> New Jersey by <strong>the</strong> next cruise. To<br />

assume that <strong>the</strong>se were homologous would require drifting at an average rate <strong>of</strong> 25<br />

miles per day, which is far too fast for non-tidal currents in this area, comparing<br />

ra<strong>the</strong>r to such swift ocean currents as <strong>the</strong> Gulf Stream (Iselin, 1936, p. 43). On <strong>the</strong><br />

o<strong>the</strong>r h<strong>and</strong>, <strong>the</strong> system <strong>of</strong> homologies indicated by <strong>the</strong> letters in figure 7 requires no<br />

fantastic assumptions as to drift. In fact, it will be shown below (p. 183) that <strong>the</strong><br />

movements <strong>of</strong> larvae designated by this system <strong>of</strong> homologies follow a pattern closely<br />

aiid definitely related to wind-impelled .drifts.<br />

Fur<strong>the</strong>rmore, <strong>the</strong> growth rate <strong>of</strong> <strong>the</strong> larvae that would be indicated by <strong>the</strong><br />

alternate series is not consistent with <strong>the</strong> lengths <strong>of</strong> <strong>the</strong> smallest post-planktonic<br />

stages. The range hi size <strong>and</strong> <strong>the</strong> modal lengths <strong>of</strong> small post-planktonic mackerel<br />

taken in July <strong>and</strong> August <strong>of</strong> certain years have been indicated in figure 8. Unfortunately,<br />

<strong>the</strong> earliest available sample <strong>of</strong> such material in <strong>the</strong> 1932 measurements was<br />

drawn August 30, nearly 50 days after <strong>the</strong> latest tow net material. It lies close to<br />

<strong>the</strong> projected S-S <strong>and</strong> T-T lines <strong>of</strong> <strong>the</strong> chosen homologies <strong>and</strong> far from <strong>the</strong> projected<br />

line that would result from <strong>the</strong> alternative homologies. That this does not result by<br />

coincidence from altered growth rates intervening between cruise material <strong>and</strong> postplanktonic<br />

material is shown by <strong>the</strong> range <strong>and</strong> modal sizes from earlier dates in 1926

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