Did You Know?
Walleye pollock live to 15 years old or more.
Walleye pollock (Gadus chalcogrammus) are distributed broadly in the North Pacific Ocean and eastern and western Bering Sea. In the Gulf of Alaska, pollock are considered as a single stock separate from those in the Bering Sea and Aleutian Islands. They are semidemersal (i.e., semi-bottom dwelling) distributed from near the surface to depths of 500 m. In the BSAI region, three areas are identified for pollock management purposes. These include the eastern Bering Sea shelf, the Aleutian Islands Region and the Central Bering Sea—Bogoslof Island area. In late winter/early spring pollock form huge spawning aggregations, including those found in Shelikof Strait and the eastern Bering Sea northwest of Unimak Island. Smaller aggregations in the Gulf of Alaska include those at the Shumagin Islands, the entrance to Prince William Sound, and near Middleton Island. In summer, large aggregations have been found on the east side of Kodiak Island, nearshore along the southern Alaska Peninsula, and other areas. Pollock migrate seasonally between spawning and feeding areas. They feed on copepods, euphausiids, and fish, and are preyed on by other fish, marine mammals, and seabirds. Pollock enter the fishery around age 3 and live to 15 years or more.
Growth and Reproduction
Pollock spawn in shallow (90 to 200 m) waters of the outer continental shelf. There is also evidence that pollock spawn in oceanic areas off the continental shelf. Oceanic spawning has been reported over waters 640 m deep south of Seward, Alaska, and in the Aleutian basin. Some spawning may also occur under the sea ice. Spawning in the Bering Sea occurs at temperatures of 1 to 3°C. Temperature at time of spawning is, however, apparently not as important for the Shelikof Strait spawning population. Pollock consistently return to Shelikof Strait to spawn, though the temperature varies from 3.5 to 6.5°C. In the Bering Sea, spawning begins in late February. Fish in the southeastern Bering Sea spawn first. Most spawning occurs from late March to mid June, with a peak in May. In the western Gulf of Alaska, it was found that more than 85% of pollock adults had spawned prior to their earliest sampling in May, indicating that most spawning occurred in March and April. Spawning and pre-spawning fish move high in the water column, forming dense schools. Eggs are Planktonic and are found primarily within 30 m of the surface. Pollock begin to recruit to the spawning population at age two, but age classes four and five contribute most to potential reproduction of the population. Estimates of individual female fecundity are difficult to achieve because ovaries of female pollock contain oocyte populations composed of two or three size classes. The percent of each size class released during spawning is uncertain. Pollock breed yearly. Length of incubation is dependent upon temperature. Incubation time from fertilization to 50% hatching is 10 days at 10°C but up to 27.4 days at 2°C. Newly hatched larvae are 3.5 to 4.4 mm in length and apparently float upside-down at the water surface. The yolk sac is absorbed at about 7.0 to 7.5 mm (22 days at 2°C).
In the Bering Sea, euphausiids are the most important food for pollock under 400 mm. Fish make an important contribution to the diet of adult Bering Sea pollock, making up 70% of stomach contents by volume in a study done by the department in 1978. Pollock larvae (4.8 to 17.7 mm standard length) from the Bering Sea consume mainly copepod nauplii and eggs and adult copepods (especially Oithona similis). Copepods are, however, consumed only by small (less than 200 mm) pollock. Studies in the Bering Sea have shown that small (young of the year and one-year-old) pollock comprise at least 44% by weight of the total stomach contents of adult pollock. In the Southeastern Gulf of Alaska, it was found that small (less than 250 mm) walleye pollock ate mostly planktonic crustaceans, particularly euphausiids, mysids, and copepods, while large pollock (larger than 349 mm) generally ate larger prey, such as shrimp and fish. Cannibalism was observed in only 1% of the stomachs; however, few pollock greater than 450 mm have been examined. Pollock feed mainly in the shallow (90 to 140 m) waters of the outer continental shelf, where tidal mixing occurs in the spring. Juveniles follow a diel vertical movement, rising to feed on zooplankton near the surface at night. In the Bering Sea, pollock feeding activity is concentrated in the summer months (June - August). Pollock feed very little or not at all during the spawning period (April - mid May).
In the Bering Sea, pollock follow a circular pattern of migration, moving inshore to the shallow (90 to 140 m) waters of the continental shelf to breed and feed in the spring (March), and moving to warmer, deeper areas of the shelf (160 to 300 m) in the winter months (December-February). Similar movement has also been noted In the Gulf of Alaska.
Range and Habitat
Walleye pollock are schooling fish, found on or near the sea bottom as well as at mid water and near-surface depths, although most catches are found between 50 and 300 m. Juvenile (age 0) pollock in their first months of life are found above the thermocline (depth at which temperature rapidly decreases) in the Bering Sea. It’s also been observed that age 0 pollock avoid depths where water temperature is less than approximately 2.5 to 3.0°C. Age 0 pollock begin to settle to the bottom in the fall months, after which they mainly occupy semi demersal waters Concentrations of adult walleye pollock in the Bering Sea are usually found in water temperatures between 2 and 4°C.
Status, Trends, and Threats
The biomass of pollock in the eastern Bering Sea is currently at a medium level relative to recent (post-1978) levels and appears to be decreasing. Pollock biomass in the Gulf of Alaska is relatively low but increasing. Populations in neither area are considered neither overfished nor approaching overfished conditions.
Although localized depletion of pollock in the eastern Bering Sea may occur as a result of commercial exploitation, pollock apparently have the ability to rapidly repopulate areas where localized depletion may have occurred. In Prince William Sound, where a relatively small, state-managed fishery occurs, pollock survey biomass estimates from the biennial bottom trawl survey have declined recently, and fishery harvest levels have been reduced as a result. Recent genetic studies provided evidence suggesting that spawning aggregations in some areas in or adjacent to the Gulf of Alaska, such as Prince William Sound, may be sufficiently different to merit management as distinct stocks.
Concerns about habitat degradation of the ocean bottom resulting from bottom trawling for pollock have largely been addressed by conversion of the fishery in the eastern Bering Sea to pelagic trawl gear. Similar concerns about habitat degradation in the Gulf of Alaska led to a prohibition on trawling east of 140° W longitude. Pollock is considered essential prey for Steller sea lions and management measures, such as fishery time and area closures around critical sea lion habitat, as well as reductions in seasonal proportions of pollock TAC that can be taken from critical habitat, have been implemented to mitigate possible negative impacts of pollock fisheries on Steller sea lions.
Bering Sea Aleutian Islands, Gulf of Alaska
Euphausiids, fish copepod nauplii and eggs and adult copepods
Marine mammals, fish and seabirds
Managed by both state and federal agencies
Did You Know?
- Walleye pollock live to 15 years old or more.
- Walleye pollock spawn annually.
- Alaska pollock is the largest fishery by volume in the United States.
- Walleye pollock is a member of the cod family.
Primary products from the commercial pollock fishery include surimi, minced product, fillets, meal, oil and roe.
Federal fisheries for walleye pollock occur in the Gulf of Alaska and Bering Sea Aleutian Islands. In the Gulf of Alaska, winter fishing has traditionally targeted pre-spawning aggregations in Shelikof Strait and the Shumagin Islands. Summer fishing has often occurred on the east side of Kodiak Island and along the Alaska Peninsula. Beginning in 1992, the Gulf of Alaska pollock Total Allowable Catch has been apportioned temporally and spatially to try to reduce negative impacts on Steller sea lions. The entire Gulf of Alaska pollock quota is allocated to the inshore sector. Winter fishing in the Bering Sea Aleutian Islands is concentrated on spawning aggregations on the continental shelf of the eastern Bering Sea, mainly north and west of Unimak Island. Fall fishing has recently concentrated near Unimak Island and along the 100 m contour northwest of the Pribilof Islands. Measures have been taken to try to reduce potential negative impacts of the pollock fishery on endangered Steller sea lions. These measures have included fishery exclusion zones around sea lion rookeries and haulouts and changes in seasonal apportionments to reduce catch near critical habitat and temporally disperse the fishery. Former fishing grounds in the Aleutian Islands were closed to pollock fishing in 2000. Limitations have been placed on the number of vessels participating in the Bering Sea Aleutian Islands pollock fisheries. The Bering Sea Aleutian Islands quota has been allocated among the western Alaska Community Development Quota program and the inshore, offshore and mothership sectors of the industry.
Parallel fisheries for pollock take place in state waters around Kodiak Island, in the Chignik Area, and along the South Alaska Peninsula. An open access state-waters fishery takes place in Prince William Sound (PWS); the guideline harvest level (GHL) for this fishery is deducted from the combined federal Western, Central, and West Yakutat Gulf of Alaska Regulatory Area (W/C/WYAK) acceptable biological catch (ABC), and has ranged from a low of 2.0 million lb in 2004 and 2005 to a high of 8.5 million lb in 2014. The management plan (5 AAC 28.263) specifies that fishery occurs in three section located within the Inside District; no more than 60 percent of the GHL may be taken from any one section in order to reduce potential impacts on the endangered population of Steller sea lions by geographically apportioning the catch. The management plan also restricts bycatch to no more than 5 percent of the total round weight of pollock harvested, and the Alaska Department of Fish and Game (ADF&G) further manages bycatch by apportioning the percentage among the following species groups: rockfish (0.5%), salmon (0.04%), shark (0.96%), squid (3.0%), and other species (0.5%). The directed fishery for pollock in PWS has typically experienced low bycatch rates relative to many other groundfish fisheries. Currently, the GHL is determined as 2.5 percent of the combined W/C/WYAK ABC based on the GHL historical percent average from 2001 to 2010. ADF&G has and may reserve a percentage of the calculated GHL for a test fishery. Revenues from these test fisheries are used to fund PWS commercial fishery management, including groundfish stock assessment and inseason pollock catch sampling.
Over 95% of the pollock catch in the Bering Sea Aleutian Islands is taken with pelagic trawls. In the Gulf of Alaska,90% of the catch is also taken using pelagic rawls. In both the Gulf of Alaska and Bering Sea Aleutian Islands there is a small incidental catch with hook and line and pot gear. Since 1995, a pelagic trawl fishery in Prince William Sound has targeted pollock. In the 5-year period ending 2002 pollock harvests have averaged almost 2.9 billion pounds (1.3 million tons (mt)) in the federal fishery and have varied from a high of almost 118 million pounds (53,000 mt) in the state fishery in 1998 to a recent low of about 2.5 million pounds (1,200 mt) in 2002. The federal fishery had an average of 196 permitted vessels and the catch yielded an average exvessel value of almost $267 million. Counterpart values for the state fishery were six permits and almost $215 thousand.
- National Marine Fishieres Service Atka mackerel migration
- Commercial Fishing Regulations
- Alaska Fishery Exvessel Prices
- Groundfish and Shellfish Statistical Area Maps
- Gulf of Alaska Rationalization
- North Pacific Fisheries Management Council (NPFMC)
- National Oceanic and Atmospheric Administration
- Fishing Vessels in Alaska (PDF 182 kB)
- Commercial Fishing Seasons in Alaska (PDF 273 kB)
- Commercial Fishing Reporting Requirements (PDF 173 kB)
- An Assessment of Age Determination Needs and Samples Sizes for Groundfish Managed by the State of Alaska (PDF 237 kB)