Evidence that Marine Temperatures Influence Growth and Maturation of Western Alaskan Chinook Salmon

Abstract Chinook Salmon Oncorhynchus tshawytscha from western Alaska have experienced recent declines in abundance, size, and age at maturity. Declines have led to hardships for the region's subsistence and commercial salmon harvesters, prompting calls to better understand factors affecting the...

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Published in:Marine and Coastal Fisheries
Main Authors: Siegel, Jared E., McPhee, Megan V., Adkison, Milo D.
Other Authors: Alaska Sustainable Salmon Fund
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
Subjects:
Online Access:http://dx.doi.org/10.1080/19425120.2017.1353563
https://afspubs.onlinelibrary.wiley.com/doi/pdf/10.1080/19425120.2017.1353563
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spelling crwiley:10.1080/19425120.2017.1353563 2024-06-02T08:04:20+00:00 Evidence that Marine Temperatures Influence Growth and Maturation of Western Alaskan Chinook Salmon Siegel, Jared E. McPhee, Megan V. Adkison, Milo D. Alaska Sustainable Salmon Fund Alaska Sustainable Salmon Fund 2017 http://dx.doi.org/10.1080/19425120.2017.1353563 https://afspubs.onlinelibrary.wiley.com/doi/pdf/10.1080/19425120.2017.1353563 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Marine and Coastal Fisheries volume 9, issue 1, page 441-456 ISSN 1942-5120 1942-5120 journal-article 2017 crwiley https://doi.org/10.1080/19425120.2017.1353563 2024-05-03T11:43:56Z Abstract Chinook Salmon Oncorhynchus tshawytscha from western Alaska have experienced recent declines in abundance, size, and age at maturity. Declines have led to hardships for the region's subsistence and commercial salmon harvesters, prompting calls to better understand factors affecting the life history of these populations. Western Alaskan Chinook Salmon are thought to spend their entire marine residency in the Bering Sea. The Bering Sea ecosystem demonstrates high interannual variability that is largely driven by the annual extent of sea ice. However, warming is expected to supersede interannual variability in the next several decades as a consequence of climate change. We investigated the influence of sea surface temperatures (SSTs) on the life history of western Alaskan Chinook Salmon by using information from two regional populations subject to long‐term monitoring. We found strong correlations between early marine growth and SSTs. Warmer SSTs appeared to lead to a younger age at maturity, largely through the vector of augmented growth. However, we also present evidence that warmer SSTs may additionally decrease the average age of male recruits through reduced growth thresholds for early male maturation. Our results suggest that the anticipated warming of the Bering Sea will lead to higher early marine growth and a younger average age of maturation for western Alaskan Chinook Salmon. Article in Journal/Newspaper Bering Sea Sea ice Alaska Wiley Online Library Bering Sea Marine and Coastal Fisheries 9 1 441 456
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Chinook Salmon Oncorhynchus tshawytscha from western Alaska have experienced recent declines in abundance, size, and age at maturity. Declines have led to hardships for the region's subsistence and commercial salmon harvesters, prompting calls to better understand factors affecting the life history of these populations. Western Alaskan Chinook Salmon are thought to spend their entire marine residency in the Bering Sea. The Bering Sea ecosystem demonstrates high interannual variability that is largely driven by the annual extent of sea ice. However, warming is expected to supersede interannual variability in the next several decades as a consequence of climate change. We investigated the influence of sea surface temperatures (SSTs) on the life history of western Alaskan Chinook Salmon by using information from two regional populations subject to long‐term monitoring. We found strong correlations between early marine growth and SSTs. Warmer SSTs appeared to lead to a younger age at maturity, largely through the vector of augmented growth. However, we also present evidence that warmer SSTs may additionally decrease the average age of male recruits through reduced growth thresholds for early male maturation. Our results suggest that the anticipated warming of the Bering Sea will lead to higher early marine growth and a younger average age of maturation for western Alaskan Chinook Salmon.
author2 Alaska Sustainable Salmon Fund
Alaska Sustainable Salmon Fund
format Article in Journal/Newspaper
author Siegel, Jared E.
McPhee, Megan V.
Adkison, Milo D.
spellingShingle Siegel, Jared E.
McPhee, Megan V.
Adkison, Milo D.
Evidence that Marine Temperatures Influence Growth and Maturation of Western Alaskan Chinook Salmon
author_facet Siegel, Jared E.
McPhee, Megan V.
Adkison, Milo D.
author_sort Siegel, Jared E.
title Evidence that Marine Temperatures Influence Growth and Maturation of Western Alaskan Chinook Salmon
title_short Evidence that Marine Temperatures Influence Growth and Maturation of Western Alaskan Chinook Salmon
title_full Evidence that Marine Temperatures Influence Growth and Maturation of Western Alaskan Chinook Salmon
title_fullStr Evidence that Marine Temperatures Influence Growth and Maturation of Western Alaskan Chinook Salmon
title_full_unstemmed Evidence that Marine Temperatures Influence Growth and Maturation of Western Alaskan Chinook Salmon
title_sort evidence that marine temperatures influence growth and maturation of western alaskan chinook salmon
publisher Wiley
publishDate 2017
url http://dx.doi.org/10.1080/19425120.2017.1353563
https://afspubs.onlinelibrary.wiley.com/doi/pdf/10.1080/19425120.2017.1353563
geographic Bering Sea
geographic_facet Bering Sea
genre Bering Sea
Sea ice
Alaska
genre_facet Bering Sea
Sea ice
Alaska
op_source Marine and Coastal Fisheries
volume 9, issue 1, page 441-456
ISSN 1942-5120 1942-5120
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1080/19425120.2017.1353563
container_title Marine and Coastal Fisheries
container_volume 9
container_issue 1
container_start_page 441
op_container_end_page 456
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