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Translation Series No.1211

Translation Series No.1211

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- 143 -<br />

•<br />

U7,) tdL<br />

comparablenece of the yields of cruises that had been selected as eapteee<br />

per unit effort.<br />

Let us examine once more the age composition of the Catches in<br />

Table 33 in order to discover the cause of the fluctuations in the catches<br />

yelw-at,s<br />

of the sea year classes A.1+ and Ae2+. In 1958 the average yeeke-la-eet of<br />

• yewgmolt<br />

of 1955 as A.1+ contrasts with the good y arls-set of smolt of 1955<br />

as A.2+. For this reason the share of the sea year class A.1+ WaA onky 54 per<br />

cent. A year later appear together the good yeaele act of smolt of 1957<br />

as A.1+ and the average of 1956 as A.2+. A.1+ accounts therefore for 72<br />

per cent of the catches. In 1960 the sea year class A.1+ is represented<br />

ye,v-éless yeew-<br />

by the poor yearic-cet of smolt of 1958. In comparison with the good yecela<br />

CA.45<br />

Set of 1957 (A.2+) it yields a share of only 49 per cent. In 1961 the av-<br />

erage ycartc7 act of smolt of 1959 as A.1+ in comparison with the poor one<br />

of the year 1958 made up 77 per cent of the catches. In the yeax 1962 the<br />

[P. 314]<br />

good yearls-cet of smolt of 1960 furnished even 90 per cent of the catches,<br />

de,ss<br />

whereas the sea year class A.2+ is represented by the average yeario sot<br />

of 1959. The percentage of the sea year classes in the catches is thus<br />

y eev<br />

alwgys dependent on the relative strength of the yecTlezzeefs of smolt.<br />

5.3.1.3. The salmon with spawning marks<br />

During their spawning migration, the salmon probablycease to<br />

feed already before they enter the rivers. It has, already been stated that<br />

the development of the gonads is accelerated during this period. Since the<br />

fish also have to supply the energy for the spawning migration and for the<br />

spawning, all body reserves are being mobilized. Among other things, there<br />

is a degradation of Substance on the scales (T. H. Jgxvi and W. J. M.<br />

Menzies 1936): This involves a more or less complete resorption along the

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