Spatiotemporal patterns in migration timing of coho salmon (Oncorhynchus kisutch) smolts in North America

The timing of ocean entry by salmon smolts is presumed adaptive to maximize survival during this critical life transition. We analyzed the peak timing, duration, and interannual variation in timing of smolt migrations for 53 coho salmon ( Oncorhynchus kisutch ) populations from central California to...

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Published in:Canadian Journal of Fisheries and Aquatic Sciences
Main Authors: Spence, Brian C., Hall, James D.
Other Authors: Fleming, Ian
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2010
Subjects:
Online Access:http://dx.doi.org/10.1139/f10-060
http://www.nrcresearchpress.com/doi/full-xml/10.1139/F10-060
http://www.nrcresearchpress.com/doi/pdf/10.1139/F10-060
id crcansciencepubl:10.1139/f10-060
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spelling crcansciencepubl:10.1139/f10-060 2024-09-15T18:16:55+00:00 Spatiotemporal patterns in migration timing of coho salmon (Oncorhynchus kisutch) smolts in North America Spence, Brian C. Hall, James D. Fleming, Ian 2010 http://dx.doi.org/10.1139/f10-060 http://www.nrcresearchpress.com/doi/full-xml/10.1139/F10-060 http://www.nrcresearchpress.com/doi/pdf/10.1139/F10-060 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Fisheries and Aquatic Sciences volume 67, issue 8, page 1316-1334 ISSN 0706-652X 1205-7533 journal-article 2010 crcansciencepubl https://doi.org/10.1139/f10-060 2024-08-22T04:08:45Z The timing of ocean entry by salmon smolts is presumed adaptive to maximize survival during this critical life transition. We analyzed the peak timing, duration, and interannual variation in timing of smolt migrations for 53 coho salmon ( Oncorhynchus kisutch ) populations from central California to Kodiak Island, Alaska. The objective was to examine potential influences of both local watershed characteristics and larger-scale processes in the marine environment on smolt migration patterns. Multivariate analyses demonstrated a strong latitudinal gradient in migration patterns with trends toward later, shorter, and more predictable migrations with increasing latitude. Cluster analysis performed on migration descriptors indicated three major population groupings that coincide with major coastal oceanic regions in the northeast Pacific: a northern group from Kodiak Island to the Queen Charlotte Islands, British Columbia, a central group from the Queen Charlotte Islands south to the Columbia River, and a southern group from the Columbia River southward. These regional patterns transcended local variability associated with watershed characteristics and trap location, suggesting that the patterns reflect adaptation to differences in timing and relative predictability of favorable conditions in the marine environments that smolts enter. Article in Journal/Newspaper Kodiak Alaska Canadian Science Publishing Canadian Journal of Fisheries and Aquatic Sciences 67 8 1316 1334
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description The timing of ocean entry by salmon smolts is presumed adaptive to maximize survival during this critical life transition. We analyzed the peak timing, duration, and interannual variation in timing of smolt migrations for 53 coho salmon ( Oncorhynchus kisutch ) populations from central California to Kodiak Island, Alaska. The objective was to examine potential influences of both local watershed characteristics and larger-scale processes in the marine environment on smolt migration patterns. Multivariate analyses demonstrated a strong latitudinal gradient in migration patterns with trends toward later, shorter, and more predictable migrations with increasing latitude. Cluster analysis performed on migration descriptors indicated three major population groupings that coincide with major coastal oceanic regions in the northeast Pacific: a northern group from Kodiak Island to the Queen Charlotte Islands, British Columbia, a central group from the Queen Charlotte Islands south to the Columbia River, and a southern group from the Columbia River southward. These regional patterns transcended local variability associated with watershed characteristics and trap location, suggesting that the patterns reflect adaptation to differences in timing and relative predictability of favorable conditions in the marine environments that smolts enter.
author2 Fleming, Ian
format Article in Journal/Newspaper
author Spence, Brian C.
Hall, James D.
spellingShingle Spence, Brian C.
Hall, James D.
Spatiotemporal patterns in migration timing of coho salmon (Oncorhynchus kisutch) smolts in North America
author_facet Spence, Brian C.
Hall, James D.
author_sort Spence, Brian C.
title Spatiotemporal patterns in migration timing of coho salmon (Oncorhynchus kisutch) smolts in North America
title_short Spatiotemporal patterns in migration timing of coho salmon (Oncorhynchus kisutch) smolts in North America
title_full Spatiotemporal patterns in migration timing of coho salmon (Oncorhynchus kisutch) smolts in North America
title_fullStr Spatiotemporal patterns in migration timing of coho salmon (Oncorhynchus kisutch) smolts in North America
title_full_unstemmed Spatiotemporal patterns in migration timing of coho salmon (Oncorhynchus kisutch) smolts in North America
title_sort spatiotemporal patterns in migration timing of coho salmon (oncorhynchus kisutch) smolts in north america
publisher Canadian Science Publishing
publishDate 2010
url http://dx.doi.org/10.1139/f10-060
http://www.nrcresearchpress.com/doi/full-xml/10.1139/F10-060
http://www.nrcresearchpress.com/doi/pdf/10.1139/F10-060
genre Kodiak
Alaska
genre_facet Kodiak
Alaska
op_source Canadian Journal of Fisheries and Aquatic Sciences
volume 67, issue 8, page 1316-1334
ISSN 0706-652X 1205-7533
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/f10-060
container_title Canadian Journal of Fisheries and Aquatic Sciences
container_volume 67
container_issue 8
container_start_page 1316
op_container_end_page 1334
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