Metabolism and biomass vertical distribution of zooplankton in the Bransfield Strait during the austral summer of 2000

The vertical distribution (0–550 m) of zooplankton biomass, and indices of respiration (electron transfer system [ETS]) and structural growth (aminoacyltRNA synthetases activity [AARS]), were studied in waters off the Antarctic Peninsula during the austral summer of 2000. The dominant species were t...

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Published in:Polar Research
Main Authors: Yebra, Lidia, Hernández-León, Santiago, Almeida, Carlos, Bécognée, Pierrick
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2009
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2848
https://doi.org/10.3402/polar.v28i3.6136
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spelling ftjpolarres:oai:journals.openacademia.net:article/2848 2023-05-15T14:01:21+02:00 Metabolism and biomass vertical distribution of zooplankton in the Bransfield Strait during the austral summer of 2000 Yebra, Lidia Hernández-León, Santiago Almeida, Carlos Bécognée, Pierrick 2009-12-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2848 https://doi.org/10.3402/polar.v28i3.6136 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2848/6475 https://polarresearch.net/index.php/polar/article/view/2848 doi:10.3402/polar.v28i3.6136 Copyright (c) 2018 Polar Research Polar Research; Vol. 28 No. 3 (2009); 415-425 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2009 ftjpolarres https://doi.org/10.3402/polar.v28i3.6136 2021-11-11T19:13:21Z The vertical distribution (0–550 m) of zooplankton biomass, and indices of respiration (electron transfer system [ETS]) and structural growth (aminoacyltRNA synthetases activity [AARS]), were studied in waters off the Antarctic Peninsula during the austral summer of 2000. The dominant species were the copepod Metridia gerlachei and the euphausiid Euphausia superba. We observed a vertical krill/copepod substitution in the water column. The zooplankton biomass in the layer at a depth of 200–500 m was of the same magnitude as the biomass in the layer at a depth of 0–200 m, indicating that biomass in the mesopelagic zone is an important fraction of the total zooplankton in Antarctic waters. The metabolic rates of the zooplankton community were sustained by less than 0.5% of the primary production in the area, suggesting that microplankton or small copepods are the main food source. Neither food availability nor predation seemed to control mesozooplankton biomass. The wide time lag between the abundance peak of the dominant copepod (M. gerlachei) and the phytoplankton bloom is suggested to be the main explanation for the low summer zooplankton biomass observed in these waters. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Bransfield Strait Euphausia superba Polar Research Copepods Polar Research (E-Journal) Antarctic The Antarctic Antarctic Peninsula Austral Bransfield Strait Polar Research 28 3
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description The vertical distribution (0–550 m) of zooplankton biomass, and indices of respiration (electron transfer system [ETS]) and structural growth (aminoacyltRNA synthetases activity [AARS]), were studied in waters off the Antarctic Peninsula during the austral summer of 2000. The dominant species were the copepod Metridia gerlachei and the euphausiid Euphausia superba. We observed a vertical krill/copepod substitution in the water column. The zooplankton biomass in the layer at a depth of 200–500 m was of the same magnitude as the biomass in the layer at a depth of 0–200 m, indicating that biomass in the mesopelagic zone is an important fraction of the total zooplankton in Antarctic waters. The metabolic rates of the zooplankton community were sustained by less than 0.5% of the primary production in the area, suggesting that microplankton or small copepods are the main food source. Neither food availability nor predation seemed to control mesozooplankton biomass. The wide time lag between the abundance peak of the dominant copepod (M. gerlachei) and the phytoplankton bloom is suggested to be the main explanation for the low summer zooplankton biomass observed in these waters.
format Article in Journal/Newspaper
author Yebra, Lidia
Hernández-León, Santiago
Almeida, Carlos
Bécognée, Pierrick
spellingShingle Yebra, Lidia
Hernández-León, Santiago
Almeida, Carlos
Bécognée, Pierrick
Metabolism and biomass vertical distribution of zooplankton in the Bransfield Strait during the austral summer of 2000
author_facet Yebra, Lidia
Hernández-León, Santiago
Almeida, Carlos
Bécognée, Pierrick
author_sort Yebra, Lidia
title Metabolism and biomass vertical distribution of zooplankton in the Bransfield Strait during the austral summer of 2000
title_short Metabolism and biomass vertical distribution of zooplankton in the Bransfield Strait during the austral summer of 2000
title_full Metabolism and biomass vertical distribution of zooplankton in the Bransfield Strait during the austral summer of 2000
title_fullStr Metabolism and biomass vertical distribution of zooplankton in the Bransfield Strait during the austral summer of 2000
title_full_unstemmed Metabolism and biomass vertical distribution of zooplankton in the Bransfield Strait during the austral summer of 2000
title_sort metabolism and biomass vertical distribution of zooplankton in the bransfield strait during the austral summer of 2000
publisher Norwegian Polar Institute
publishDate 2009
url https://polarresearch.net/index.php/polar/article/view/2848
https://doi.org/10.3402/polar.v28i3.6136
geographic Antarctic
The Antarctic
Antarctic Peninsula
Austral
Bransfield Strait
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
Austral
Bransfield Strait
genre Antarc*
Antarctic
Antarctic Peninsula
Bransfield Strait
Euphausia superba
Polar Research
Copepods
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Bransfield Strait
Euphausia superba
Polar Research
Copepods
op_source Polar Research; Vol. 28 No. 3 (2009); 415-425
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2848/6475
https://polarresearch.net/index.php/polar/article/view/2848
doi:10.3402/polar.v28i3.6136
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v28i3.6136
container_title Polar Research
container_volume 28
container_issue 3
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