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SCIENCE REVIEW 1987 - Bedford Institute of Oceanography

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Research<br />

weren’t always benevolent. A century ago,<br />

at the peak <strong>of</strong> the handline fishery, the<br />

fishermen on Georges and other fishing<br />

banks regularly caught shearwaters as bait<br />

- and to get a taste <strong>of</strong> fresh meat.<br />

(Discriminating gourmets preferred Sooties<br />

to Greaters.) But things are very different<br />

today. Instead, we provide a gargantuan<br />

feast <strong>of</strong> trash fish, scraps and <strong>of</strong>fal, spilling<br />

from the factory trawlers that work over<br />

the Bank. Some seabirds - Red Phalaropes,<br />

Razorbills - are too specialised in<br />

their feeding habits to exploit this bonanza.<br />

But the blizzard <strong>of</strong> Fulmars, Greater<br />

Shearwaters, Gannets, Kittiwakes and<br />

Great Black-backed Gulls behind every<br />

dragger is pro<strong>of</strong> that the specialists are in<br />

the minority.<br />

This exploitation has several long-term<br />

implications. It undoubtedly increases<br />

seabirds’ chances <strong>of</strong> surviving through the<br />

winter, when food is scarcest; this is<br />

particularly true for juvenile birds. But do<br />

we really need more large gulls? Their<br />

population explosion in the last 40 years<br />

has already turned them into a menace to<br />

the other seabirds that breed along the<br />

coasts <strong>of</strong> New England and Atlantic<br />

Canada. And what will happen if, to feed<br />

our own expanding species, we overexploit<br />

the fishery? This is becoming more and<br />

more <strong>of</strong> a possibility, as we shift our aim<br />

from traditional food species such as cod<br />

and haddock, to an industrial fishery for<br />

smelt and other small fish that can be<br />

ground down into fish-meal to feed our<br />

cattle and chickens. The next stage may<br />

well be a fishery for the larger zooplankton.<br />

The difficulty is that these small-fry are at<br />

the base <strong>of</strong> the food-web <strong>of</strong> all the higher<br />

marine predators on Georges Bank. Zooplankton<br />

feed small fish, which feed larger<br />

fish, which feed seabirds and whales. If we<br />

take away too much <strong>of</strong> the zooplankton<br />

and small-fry at the bottom, the whole<br />

marine community may collapse - and<br />

Georges Bank, now so rich, will become a<br />

desert. We had better be very careful.<br />

Further Reading.<br />

BACKUS, R.H. (ed.) <strong>1987</strong>. Georges Bank. MIT<br />

Press: Cambridge, MA, and London, U.K. 593 p.<br />

BROWN, R.G.B. 1986. Revised Atlas <strong>of</strong> eastern<br />

Canadian Seabirds. I. Shipboard Surveys. Environment<br />

Canada, Canadian Wildlife Service: Ottawa.<br />

111 p.<br />

BROWN, R.G.B. 1988. The influence <strong>of</strong> oceanographic<br />

anomalies on the distributions <strong>of</strong> storm-petrels<br />

Hydrobatidae in Nova Scotian waters. Colonial<br />

Waterbirds 11: 1-8.<br />

BROWN, R.G.B. and GASKIN, D.E. 1988. The<br />

pelagic ecology <strong>of</strong> the Grey and Red-necked<br />

Phalaropes Phalaropus fulicarius and P. lobatus in the<br />

Bay <strong>of</strong> Fundy, eastern Canada. Ibis 130. 234-250.<br />

POWERS, K.D. and BACKUS, E.H. <strong>1987</strong>. Energy<br />

transfer to seabirds. Pp. 372-373. in Backus, R.H.<br />

(ed.) Georges Bank. MIT Press: Cambridge, MA, and<br />

London, U.K.<br />

POWERS, K.D. and BROWN, R.G.B. <strong>1987</strong>.<br />

Seabirds. Pp. 359-371 in Backus, R.H. (ed.) Georges<br />

Bank. MIT Press: Cambridge, MA, and London, U.K.<br />

Georges Bank - Research behind the management <strong>of</strong> habitat<br />

and commercial resources<br />

D.C. Gordon Jr., J.D. Neilson, and G. Robert<br />

Introduction<br />

D. C. Gordon<br />

FISH stocks and their habitat are managed<br />

with the long term goal <strong>of</strong> maintaining<br />

their health and abundance. This article<br />

briefly summarizes some <strong>of</strong> the research<br />

currently underway in the Scotia-Fundy<br />

Region in support <strong>of</strong> resource and habitat<br />

management on Georges Bank. Georges<br />

Bank is a large and shallow submarine<br />

bank located on the outer continental shelf<br />

along the southern side <strong>of</strong> the Gulf <strong>of</strong><br />

Maine (Figure 1). Its rich fishery resources<br />

have long been exploited by Canadian and<br />

American fishermen. The October 1984<br />

International Court <strong>of</strong> Justice (ICJ)<br />

decision granted the northeast portion to<br />

Canada. However, while Canada won<br />

14<br />

J.D. Neilson G. Robert<br />

exclusive rights to significant fishery<br />

resources, the transboundary nature <strong>of</strong><br />

many <strong>of</strong> these stocks remain which gives<br />

rise to special problems concerning both<br />

research and management.<br />

Primary production by phytoplankton<br />

on Georges Bank is very high because <strong>of</strong><br />

near optimum conditions <strong>of</strong> light and<br />

nutrients. It is one <strong>of</strong> the most productive<br />

fishing banks in the North Atlantic<br />

(O’Reilly and Busch, 1984) and supports a<br />

diverse food web which includes both<br />

planktonic and benthic organisms and<br />

culminates in abundant finfish (cod,<br />

haddock, herring, etc.) and invertebrate<br />

(scallop, lobster, etc.) fishery resources. The<br />

landed value <strong>of</strong> Canadian fisheries from<br />

Georges Bank in 1986 was $63 million.<br />

Apart from the special circumstances<br />

surrounding the IJC decision, the environment<br />

<strong>of</strong> Georges Bank is rather unique. Its<br />

physical features are dominated by very<br />

strong currents which are generated by<br />

large volumes <strong>of</strong> water moving into and<br />

out <strong>of</strong> the Gulf <strong>of</strong> Maine and the Bay <strong>of</strong><br />

Fundy in response to the tidal forces. These<br />

currents promote vertical mixing <strong>of</strong> the<br />

water. During the winter, most <strong>of</strong> the water<br />

over the Bank is well-mixed from top to<br />

bottom, while during the summer solar<br />

heating produces stratification in water<br />

deeper than about 60 m. The boundary<br />

between the well-mixed and stratified areas<br />

is marked by a seasonal tidal front. The<br />

strong currents also help generate a<br />

clockwise rotation or gyre over the Bank

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