CalCOFI Reports, Vol. 30, 1989 - California Cooperative Oceanic ...
CalCOFI Reports, Vol. 30, 1989 - California Cooperative Oceanic ...
CalCOFI Reports, Vol. 30, 1989 - California Cooperative Oceanic ...
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
HUNTER ET AL.: SABLEFISH REPRODUCTION<br />
CalCOFl Rep., <strong>Vol</strong>. <strong>30</strong>,<strong>1989</strong><br />
-<br />
E<br />
1.7<br />
1.6<br />
$ 1.4<br />
0<br />
0 1.3<br />
Y<br />
1.2<br />
a 1.1<br />
><br />
n<br />
a 1<br />
E 0.9<br />
L<br />
k! 0.8<br />
0.7<br />
z<br />
G o.6<br />
0.5 I 1 1 1 1 1 1 / 1 1 I 1 I I I I I<br />
0 20 40 60 80 100 120 140 160<br />
ELAPSED TIME (days)<br />
I I I I I<br />
I I I<br />
Oct Nov Dec Jan Feb<br />
'86 '87<br />
Figure 7. Mean diameter (D) of advanced<br />
oocytes in sablefish ovaries<br />
as a function of elapsed time (T) in<br />
days from October 6, 1986, to February<br />
13, 1987. Shaded area indicates<br />
oocyte diameters at which the<br />
onset of hydration occurs; total fecundity<br />
was not estimated for ovaries<br />
in which the mean diameter was<br />
~0.7 mm (dashedline).<br />
standing stock during the spawning season. By the<br />
middle of January the mean diameter of the advanced<br />
oocytes was 1.34 mm, which is close to the<br />
diameter at which hydration begins (1.5-1.6 mm)<br />
(figure 7). Thus by January, little maturation would<br />
be required to hydrate and spawn most of the advanced<br />
oocytes remaining in the ovary.<br />
We compared the mean oocyte density (mean<br />
count of advanced oocytes in two tissue samples) to<br />
one calculated from the mean diameter by regressing<br />
mean oocyte density on the computed density<br />
(% T O3)-l for fish taken in October and in<br />
January-February. In both sampling periods the intercept<br />
was very small and did not differ from zero.<br />
Assuming a zero intercept, the slope (K) was 0.94<br />
for October and 0.88 for January-February. We<br />
tested the equality of the slopes by analysis of covariance<br />
(Zar 1974), and the results indicated that<br />
the slopes were not statistically different (t = 0.253,<br />
DF = 65). We combined the data from the two<br />
cruises to obtain a common slope of 0.94 (figure 8).<br />
K was less than one because samples of ovarian tissue<br />
contain material other than advanced oocytes<br />
(tissue fragments, postovulatory follicles, immature<br />
oocytes, etc.).<br />
That K was nearly the same for fish taken in<br />
January-February as for those taken in October<br />
indicates that the fraction by weight of materials<br />
other than advanced oocytes in the tissue samples<br />
remained constant over the season, even though<br />
many of the females taken in January-February had<br />
spawned some of their oocytes. This indicates that<br />
postovulatory follicles are resorbed relatively rapidly<br />
after each spawning, and no major proliferation<br />
of vitellogenic oocytes had occurred. The relationship<br />
between observed oocyte density and the one<br />
computed from oocyte diameter was more variable<br />
for fish taken in January-February than in October:<br />
Y* = 0.55 for January-February and 0.91 for October.<br />
Ovaries containing postovulatory follicles<br />
were substantially below the 0.94 line (figure 8,<br />
insert), indicating that the higher variability in<br />
January-February was probably caused by the occurrence<br />
of ovaries in which postovulatory follicles<br />
had not been resorbed.<br />
The mean diameter of the advanced stock of oocytes<br />
was inversely correlated with total fecundity.<br />
A stepwise multiple regression of total fecundity<br />
(FT, all data, October-February) on female weight<br />
( W), oocyte diameter (D), and elapsed time (T, during<br />
the spawning season) indicated that the diameter<br />
explained more of the variation in fecundity over<br />
the spawning season than did elapsed time (table 4).<br />
The final equation was<br />
F, = 351,992 + 71.4 W - 263,462D,<br />
69