Vertical Distribution of Age-0 Walleye Pollock During Late Summer: Environment or Ontogeny?

Variability in the late-summer vertical distribution of age-0 Walleye Pollock Gadus chalcogrammus in the southeastern Bering Sea has been attributed to a range of physical and biological factors. Using acoustic data (38 and 120 kHz) collected during the 2010 Bering Aleutian Salmon International Surv...

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Published in:Marine and Coastal Fisheries
Main Authors: Sandra L. Parker-Stetter, John K. Horne, Samuel S. Urmy
Format: Text
Language:English
Published: American Fisheries Society 2015
Subjects:
Online Access:https://doi.org/10.1080/19425120.2015.1057307
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spelling ftbioone:10.1080/19425120.2015.1057307 2024-06-02T08:04:23+00:00 Vertical Distribution of Age-0 Walleye Pollock During Late Summer: Environment or Ontogeny? Sandra L. Parker-Stetter John K. Horne Samuel S. Urmy Sandra L. Parker-Stetter John K. Horne Samuel S. Urmy world 2015-01-01 text/HTML https://doi.org/10.1080/19425120.2015.1057307 en eng American Fisheries Society doi:10.1080/19425120.2015.1057307 All rights reserved. https://doi.org/10.1080/19425120.2015.1057307 Text 2015 ftbioone https://doi.org/10.1080/19425120.2015.1057307 2024-05-07T00:51:43Z Variability in the late-summer vertical distribution of age-0 Walleye Pollock Gadus chalcogrammus in the southeastern Bering Sea has been attributed to a range of physical and biological factors. Using acoustic data (38 and 120 kHz) collected during the 2010 Bering Aleutian Salmon International Survey (BASIS) and dedicated high-resolution surveys (HR1 and HR2), we evaluated whether late-summer distributions could be explained by water column properties (environment) or whether sampling was likely occurring during the ontogenetic shift of age-0 Walleye Pollock from near-surface habitat to demersal habitat (ontogeny). Neither water column attributes (temperature, relative temperature, salinity, dissolved oxygen, and density gradient) nor the acoustic density of zooplankton prey strongly predicted the acoustic estimates of age-0 Walleye Pollock vertical presence or density. At 6 of 10 paired BASIS—HR1 stations, age-0 Walleye Pollock shifted deeper in the water column between BASIS sampling and the HR1 sampling conducted 8–34 d later. There were no consistent differences in FL (P > 0.05 for 2 of 4 station pairs) or energy density (P > 0.05 for 3 station pairs) between age-0 Walleye Pollock caught in near-surface trawls and those caught in midwater trawls. Our data suggest that the observation of both near-surface and midwater age-0 Walleye Pollock during late summer is likely due to an ontogenetic habitat shift; however, the causative factor was not clear given the limited sample sizes and explanatory variables. The timing of the ontogenetic shift, which appears to have begun before August 18, 2010, can ultimately affect survey strategies, and knowledge of this timing can provide additional insight into factors affecting the overwinter survival of age-0 Walleye Pollock. Text Bering Sea BioOne Online Journals Bering Sea Marine and Coastal Fisheries 7 1 349 369
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description Variability in the late-summer vertical distribution of age-0 Walleye Pollock Gadus chalcogrammus in the southeastern Bering Sea has been attributed to a range of physical and biological factors. Using acoustic data (38 and 120 kHz) collected during the 2010 Bering Aleutian Salmon International Survey (BASIS) and dedicated high-resolution surveys (HR1 and HR2), we evaluated whether late-summer distributions could be explained by water column properties (environment) or whether sampling was likely occurring during the ontogenetic shift of age-0 Walleye Pollock from near-surface habitat to demersal habitat (ontogeny). Neither water column attributes (temperature, relative temperature, salinity, dissolved oxygen, and density gradient) nor the acoustic density of zooplankton prey strongly predicted the acoustic estimates of age-0 Walleye Pollock vertical presence or density. At 6 of 10 paired BASIS—HR1 stations, age-0 Walleye Pollock shifted deeper in the water column between BASIS sampling and the HR1 sampling conducted 8–34 d later. There were no consistent differences in FL (P > 0.05 for 2 of 4 station pairs) or energy density (P > 0.05 for 3 station pairs) between age-0 Walleye Pollock caught in near-surface trawls and those caught in midwater trawls. Our data suggest that the observation of both near-surface and midwater age-0 Walleye Pollock during late summer is likely due to an ontogenetic habitat shift; however, the causative factor was not clear given the limited sample sizes and explanatory variables. The timing of the ontogenetic shift, which appears to have begun before August 18, 2010, can ultimately affect survey strategies, and knowledge of this timing can provide additional insight into factors affecting the overwinter survival of age-0 Walleye Pollock.
author2 Sandra L. Parker-Stetter
John K. Horne
Samuel S. Urmy
format Text
author Sandra L. Parker-Stetter
John K. Horne
Samuel S. Urmy
spellingShingle Sandra L. Parker-Stetter
John K. Horne
Samuel S. Urmy
Vertical Distribution of Age-0 Walleye Pollock During Late Summer: Environment or Ontogeny?
author_facet Sandra L. Parker-Stetter
John K. Horne
Samuel S. Urmy
author_sort Sandra L. Parker-Stetter
title Vertical Distribution of Age-0 Walleye Pollock During Late Summer: Environment or Ontogeny?
title_short Vertical Distribution of Age-0 Walleye Pollock During Late Summer: Environment or Ontogeny?
title_full Vertical Distribution of Age-0 Walleye Pollock During Late Summer: Environment or Ontogeny?
title_fullStr Vertical Distribution of Age-0 Walleye Pollock During Late Summer: Environment or Ontogeny?
title_full_unstemmed Vertical Distribution of Age-0 Walleye Pollock During Late Summer: Environment or Ontogeny?
title_sort vertical distribution of age-0 walleye pollock during late summer: environment or ontogeny?
publisher American Fisheries Society
publishDate 2015
url https://doi.org/10.1080/19425120.2015.1057307
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geographic Bering Sea
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op_source https://doi.org/10.1080/19425120.2015.1057307
op_relation doi:10.1080/19425120.2015.1057307
op_rights All rights reserved.
op_doi https://doi.org/10.1080/19425120.2015.1057307
container_title Marine and Coastal Fisheries
container_volume 7
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container_start_page 349
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