Cusk (Brosme brosme) COSEWIC assessment and status report 2012: chapter 3

COSEWIC Executive Summary

Cusk Brosme brosme

Wildlife Species Description and Significance

The Cuskis the only member of its genus and is one of about 20 species of cod-like (Gadiforme) fishes on the east coast of Canada. The combination of a single barbel and a single dorsal fin is diagnostic and identifies this species.

A recent genetic study of population structure suggests that there is limited adult migration across deep water regions, which in combination with limited inter-site exchange of pelagic eggs and larvae because of site-specific circulatory retention and poor survival during drift phases across deep basins, is hypothesized as reducing gene flow. The Northeast and Northwest Atlantic gene pools of Cusk are different with Cusk in more southern parts of the Northwest Atlantic genetically distinct from Northeast Atlantic populations. There is a discontinuity in Cusk distribution between Canada and West Greenland that likely restricts genetic interchange. These observations support a single designatable unit for Canada.

Distribution

The Cusk is a northern species inhabiting subarctic and boreal shelf waters of the north Atlantic. Its centre of abundance in the western Atlantic is between 41-44°N latitude (Gulf of Maine and southern Scotian Shelf) where its distribution overlaps the international border of Canada and the United States in the Gulf of Maine. It also occurs in the deep waters along the edge of the continental shelf off Newfoundland and Labrador where it is rare. It has not been observed in the southern Gulf of St. Lawrence, and only four fish have been taken from the northern Gulf of St. Lawrence since the late 1970s.

Habitat

Common on hard, rough, and rocky substrates it is seldom taken on bottoms of smooth clean sand. The Cuskprefers relatively warm water of intermediate depths on the Scotian Shelf and Gulf of Maine. It is found at temperatures from 0-14°C on the Scotian Shelf with some preference for 6-10°C. Cuskare seldom found near the shore or at depths less than 20-30 m. It mostly occurs between 150-450 m depth throughout its range although recent survey work has found Cusk as deep as 1185 m along the edge of the continental shelf off Nova Scotia.

Biology

The total length (TL) of 50% maturity for Cusk in Canadian waters is 42 cm that is reached by 4-5 years of age. An aging study is currently underway; preliminary estimates suggest that these ages may be low by 100% (i.e. 50% age of maturity at age 10). The largest Cusk encountered in the commercial sampling dataset was 115 cm while the largest Cusk caught in a Halibut survey was 118 cm. Longevity, L, estimates range from 111.4-126.6 cm TL. Generation time is estimated to be 12.1 years although preliminary results from a recent aging study suggest that it could be as high as 21 years.

Spawning on the Scotian Shelf takes place from May – August with peak spawning in late June. No discrete spawning sites have yet been determined although it could occur in water deeper than 200 m. Eggs are pelagic and hatch larvae measuring 4 mm. Larvae remain in the upper water column and settle to the bottom at about 50-60 mm. The location of benthic nursery grounds is unknown but may be on rough bottom in deep water. Demersal juveniles and adults remain strongly associated with the substratum and do not swim up into the water column. They are slow-moving, sedentary and solitary and do not form large aggregations.

Cusk predators include Spiny Dogfish, Winter Skate, Atlantic Cod, Atlantic Halibut, White Hake, Atlantic Monkfish and maybe Grey Seals. Their diet consists of Crustacea, particularly crabs, shrimps and euphausiids, fish and brittlestars. Natural mortality is likely in the order of 0.14, comparable to that of other Gadoids.

Population Sizes and Trends

The trend in Fisheries and Oceans Canada (DFO) and US National Marine Fisheries Service (NMFS) bottom trawl survey indices of mature abundance over the last 3 generations is a continuous decline. These surveys may exhibit hyperdepletion where catch rates decline faster than biomass due to range contraction of the species to areas not fully covered by the survey, and the series may overestimate the rate of decline. A commercial longline catch rate series that covers the last 2 generations also shows a continuous decline. These contrast the trend in abundance of Cusk in a Halibut survey that has been stable since 1999. A model of surplus production dynamics of the population that used all the Canadian abundance indices and allowed for hyperdepletion in the trawl survey index was used to estimate the trend in mature biomass over the past 3 generations. The estimated decline was 85% and there is no indication that the decline has ceased.

Threats and Limiting Factors

Overfishing is the most important threat to Cusk. Directed fishing for Cusk has virtually ceased but the species is still taken as bycatch in fisheries for Atlantic Cod, Haddock, Pollock and Atlantic Halibut. Recent landings of Cusk from these fisheries have been in the order of 500 t annually. Cusk are also bycatch in the Lobster fishery where landings of Cusk are prohibited and all catch is discarded. Recent discards have been in the order of 250 t-300 t annually. Discarded Cusk do not likely survive given the propensity for the stomach to evert when they are brought to the surface.

Protection, Status, and Ranks

The Cusk was assessed by COSEWIC as threatened in 2003. The Governor in Council elected not to list the species under SARA (Canada Gazette July 7 2012).

In Canada, DFO Conservation Harvesting Plans are the primary regulatory tool protecting Cusk. Since 1999, directed fishing for Cusk has not been permitted and a system of quota caps was introduced to control Cusk landings. In 2010/11, quota caps for the DFO Maritimes fleets totalled 656 t. When the landings caps are met all Cusk catch must be discarded and most would not survive.

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