http://www.nwrc.usgs.gov/wdb/pub/species_profiles/82_11-085.pdf
Geographic Range: Morro Bay,
California, t o northern B r i t i s h
Columbia; Japan (Quayle 1960; Fitch
1953).
Quayle (1969a) reported
t h a t breeding occurs natural l y only
between Willapa Harbour ( l a t . 46O
N.) and Pendrell Sound ( l a t . 50°
N. ) Consistent breeding occurs
only i n Dabob and Quilcene Bays
i n Washington and Pendrell Sound
and Pipestem I n l e t i n B r i t i s h
Col umbia; breeding i s rare or
sporadic i n other locations.
Temperature plays a major r o l e i n
t h e d e v e l o,~ me n t o f t h e f e r t i l i z e d ~
oyster egg. A decrease o f 2'C
(from 24.5OC t o 22.5OC) doubled the
time required f o r the formation o f the
trochophore larvae ( G a l s t o f f 1964).
F e r t i 1 ized eggs reached the vel i g e r
stage i n 72 hours a t 14'C, and i n 28
hours at 22'C (Loosanoff and Davis
1963).
Growth of the free-swimminq l a r -
vae depends on many f a c t o r s ; the
length of the l a r v a l period i s dependent
on the water temperature. Temperatures
must be 20°C or greater f o r at
l e a s t three weeks f o r near optimal
growth (Magoon and Vining 1981).
Although larvae can survive s l i g h t l y
lower water temperatures, t h i s pro-
1 ongs t h e i r development and increases
t h e i r exposure t o pelagic predators
(Kennedy and Breisch 1981).
Growth i n oysters varies widely
w i t h t i d a l height, growing area, and
environmental conditions. Oyster
growth can be measured by increases i n
s h e l l size or body size. As a general
r u l e , growth i s f a s t e r as water temperature
increases (Loosanof f 1965).
The Pacific Northwest waters are
generally too cool for C. gigas as adult s
to spawn successfully - or their
larvae to settle in quantities apprecable for commercial use (Korringa
1976). Exceptions t o t h i s a r e Dabob
Bay and Quilcene Bay i n Washington,
where y e a r l y s p a t f a l l averages about
25 per s h e l l o f c u l t c h , w h i l e i n
P e n d r e l l Sound i n B r i t i s h Columbia,
commercial sets o f over 1,000 spat
per s h e l l are n o t uncommon (Korringa
1976; Chew, pers. comm.).
Both areas
are r e l a t i v e l y protected; summer
water temperatures r e g u l a r l y exceed
20'C and where hydrographic f e a t u r e s
f a c i l i t a t e o y s t e r l a r v a l r e t e n t i o n
(Quayle 1969a; Korringa 1976).