Long-Term Records of Abundance and Effects of Large Scale Climate Change on Alaska Peninsula Sockeye Salmon
University of Alaska Fairbanks
Idaho State University
Idaho State University
The sustainability of Alaska’s fisheries, including the sockeye salmon fishery, is of utmost importance not only to the health of Alaska’s marine ecosystems but also to the vitality of Alaska’s coastal communities. Investigators will collect and analyze sediment cores from Sapsuk Lake, a sockeye spawning lake with traditionally large sockeye returns, to determine fluctuations in numbers of sockeye returning from the Bering Sea over the last few thousand years. This is of concern to stakeholders in the area, as historically the Sapsuk system had large runs but fish numbers have declined in recent years to the point of impacting subsistence and commercial use. The project will use sediments from Sapsuk Lake to detect relative numbers of sockeye returning to this spawning lake over the last 4000–5000 years, reconstruct changes in past productivity of the lake, and construct a model that could identify numbers of returning sockeye. Since historic data periods are too short to capture the large climatic changes the world—specifically the north—is now experiencing, long-term data sets such as this one will help determine the effects of warmer and colder climates on Bering Sea sockeye. This project will add to the knowledge of stakeholders and policymakers and may inform future management decisions and improve the chances of sustaining economic and sociocultural stability in Alaska coastal communities.
Please see Long-term records of abundance and effects of large scale climate change on Alaska peninsula sockeye salmon website for additional information.
The sustainability of Alaska’s fisheries is important not only to the health of Alaska’s ocean ecosystems but also to the health of fishing communities, both of which are being rapidly affected by global climate change. Sockeye are key to subsistence and economic well-being of communities along the Bering Sea coast, so it is important for the sustainability of these communities to understand the processes that control these fish.
Why is this an Alaska Sea Grant project?
This project addresses two Sea Grant themes: impacts on and strategies for coastal ecosystems and/or communities adapting to change, and improvements to the economic and sociocultural sustainability of Alaska coastal communities. Collecting data on long-term fluctuations (in this case thousands of years) in sockeye returns will allow researchers to determine how sockeye populations responded to environmental changes in the past. The outcomes will help predict the impacts of environmental change on sockeye stocks and help the communities that rely on them build strategies to cope with changes.
How will researchers conduct their study?
Investigators will reconstruct long-term sockeye escapement history in Sapsuk Lake, western Alaska Peninsula, using stable isotope analysis of lake core sediments as an indicator of marine-derived nutrients (i.e., relative numbers of salmon carcasses decaying into surrounding sediments) and numerous markers of climate, ocean, and lake conditions. The past 4000–5000 years include several periods of climatic variability, and can provide valuable information on the relationship between climate change and sockeye salmon systems.
- Get a sedimentary sequence from Sapsuk Lake that shows the latter half of the Holocene (last 5000 years).
- Collect and analyze water and zooplankton from stations that ADFG sampled in the 1990s.
- Conserve half of sediment core for future research in cold storage at ISU.
- Reconstruct records of salmon abundance at decadal resolution using δ15N, radiocarbon dating of recovered core material, and an isotope-based model.
- Use biogenic opal, organic carbon, and δ13C to reconstruct past changes in terrestrial and aquatic carbon cycles and lake primary production.
- Compare the results to paleoclimatic and paleoceanographic data from the literature.
- Compare results to previously cored lakes in the Bristol Bay area.
- Compare salmon abundance trends and climatic history to other Bristol Bay and Alaska Peninsula paleoenvironmental records.
- Evaluate a lake-system 15N isotope-balance model against modern Sapsuk fisheries data and sediment analyses, and apply this model to estimates of the number of fish that are permitted to spawn (escapement) over the 5000 year record.
- Provide data to policy makers and stakeholders through informal meetings in villages, web-based data and reports, and formal conference settings and journal articles.
Nelson Lagoon Tribal Council
ADF&G Kodiak Limnology Laboratory
Idaho State University
Nicholas Sagalkin, Regional Finfish Research Supervisor, ADFG
Katherine Reedy, Associate Professor, Idaho State University
What researchers learned
The Sapsuk Lake data appears to follow the broad scale trends found in other sockeye spawning lakes that drain both in the North Pacific and the southern Bering Sea. This is in direct contrast to a previously published report which concluded that each spawning lake is unique in its trends over the last 500 years (Rogers et al 2013). Although fine scale change may be more localized and occur on short time-scales, changes in numbers of returning salmon show similar patterns across larger areas over centennial time-scales. Many of these changes appear to be related to broad scale climate and productivity fluctuations, such as the climatic shift associated with initiation of the Little Ice Age, which began in Alaska ca. 700 yr BP. If the connections between ocean-climate conditions and salmon are valid, then this research could potentially point to bottom-up drivers of fluctuations in sockeye salmon stock sizes. This in turn, could direct a new set of research, based on linkages between these particular drivers and sockeye survival rates. These linkages would be a very useful tool to management and stakeholders as they plan for the future of sockeye harvesting in a rapidly changing system.