A fishery for snow crab, Chionoecetes opilio, began in 1979 in a shall
ow water (<200 m) area off the Avalon Peninsula of southeastern Newfou
ndland and developed rapidly with landings peaking at 8609 metric tons
(t) in 1981. Landings began to decline in 1982, and dropped to 74 t i
n 1985. This fishery collapse coincided with similar declines in catch
per unit of effort (CPUE) and abundance of newly molted male snow cra
b. In Bonavista Bay, a deep water (>200 m) fishing area north of the A
valon Peninsula, CPUE declined less and the proportion of newly molted
male snow crab remained relatively constant during the same period. C
oincident with the decline of the Avalon Peninsula fishery was a prono
unced drop in mean bottom temperature on the commercial fishing ground
s, from -0.6-degrees-C to -1.4-degrees-C, a phenomenon not observed in
Bonavista Bay. This decline in water temperature appears to have been
the cause of the fishery collapse because temperatures became low eno
ugh to interrupt the molting cycle of snow crab off the Avalon Peninsu
la. If the potential impact of the lower water temperatures and subseq
uent long-term cessation of growth and recruitment within the snow cra
b population had been recognized, the available pool of commercial-siz
ed crab could have been harvested more slowly over a period of years t
o lessen the disruption of the fishery.