Deep-Sea Research I 46 (1999) 1391}1415 Mesozooplankton in the Arctic Ocean in summer

The biomass, species and chemical composition of the mesozooplankton and their impact on lower food levels were estimated along a transect across the Arctic Ocean. Mesozooplankton biomass in the upper 200 m of the water column was signi"cantly higher (19}42 mg DW m~3) than has previously been r...

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Main Authors: Delphine Thibault, Erica J. H. Head, Patricia A. Wheeler
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1997
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.3784
http://www.com.univ-mrs.fr/~botha/thibault et al, AOS94.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.582.3784 2023-05-15T13:22:45+02:00 Deep-Sea Research I 46 (1999) 1391}1415 Mesozooplankton in the Arctic Ocean in summer Delphine Thibault Erica J. H. Head Patricia A. Wheeler The Pennsylvania State University CiteSeerX Archives 1997 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.3784 http://www.com.univ-mrs.fr/~botha/thibault et al, AOS94.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.3784 http://www.com.univ-mrs.fr/~botha/thibault et al, AOS94.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.com.univ-mrs.fr/~botha/thibault et al, AOS94.pdf text 1997 ftciteseerx 2016-08-28T00:02:51Z The biomass, species and chemical composition of the mesozooplankton and their impact on lower food levels were estimated along a transect across the Arctic Ocean. Mesozooplankton biomass in the upper 200 m of the water column was signi"cantly higher (19}42 mg DW m~3) than has previously been reported for the Arctic Ocean, and it reached a maximum at ca. 873N in the Amundsen Basin. The lowest values were recorded in the Chukchi Sea and Nansen Basin, where ice cover was lower (50}80%) than in the central Arctic Ocean. In the deeper strata (200}500 m) of the Canadian and Eurasian Basins, the biomass was always much lower (4.35}16.44 mg DW m~3). The C/N (g/g) ratio for the mesozooplankton population was high (6.5}8.5) but within the documented range. These high values (when compared to 4.5 at lower latitudes) may be explained by the high lipid content. Mesozooplankton accounted for approx-imately 40 % of the total particulate organic carbon in the upper 100 m of the water column. Mesozooplankton species composition was homogeneous along the transect, consisting mainly of copepods (70}90 % of the total number). It was dominated by four large copepod species (Calanus hyperboreus, C. glacialis, C.,nmarchicus and Metridia longa), which together ac-counted for more than 80 % of the total biomass. According to measurements of gut pigment and gut turnover rates, the mesozooplankton on average ingested between 6 and 30 % of their body carbon per day as phytoplankton. Microzooplankton may have provided an additional source of energy for the mesozooplankton community. These data emphasize the importance of mesozooplankton in the arctic food web and reinforce the idea that the Arctic Ocean should Text amundsen basin Arctic Arctic Ocean Calanus hyperboreus Chukchi Chukchi Sea Nansen Basin Phytoplankton Copepods Unknown Amundsen Basin ENVELOPE(74.000,74.000,87.000,87.000) Arctic Arctic Ocean Chukchi Sea
institution Open Polar
collection Unknown
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language English
description The biomass, species and chemical composition of the mesozooplankton and their impact on lower food levels were estimated along a transect across the Arctic Ocean. Mesozooplankton biomass in the upper 200 m of the water column was signi"cantly higher (19}42 mg DW m~3) than has previously been reported for the Arctic Ocean, and it reached a maximum at ca. 873N in the Amundsen Basin. The lowest values were recorded in the Chukchi Sea and Nansen Basin, where ice cover was lower (50}80%) than in the central Arctic Ocean. In the deeper strata (200}500 m) of the Canadian and Eurasian Basins, the biomass was always much lower (4.35}16.44 mg DW m~3). The C/N (g/g) ratio for the mesozooplankton population was high (6.5}8.5) but within the documented range. These high values (when compared to 4.5 at lower latitudes) may be explained by the high lipid content. Mesozooplankton accounted for approx-imately 40 % of the total particulate organic carbon in the upper 100 m of the water column. Mesozooplankton species composition was homogeneous along the transect, consisting mainly of copepods (70}90 % of the total number). It was dominated by four large copepod species (Calanus hyperboreus, C. glacialis, C.,nmarchicus and Metridia longa), which together ac-counted for more than 80 % of the total biomass. According to measurements of gut pigment and gut turnover rates, the mesozooplankton on average ingested between 6 and 30 % of their body carbon per day as phytoplankton. Microzooplankton may have provided an additional source of energy for the mesozooplankton community. These data emphasize the importance of mesozooplankton in the arctic food web and reinforce the idea that the Arctic Ocean should
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Delphine Thibault
Erica J. H. Head
Patricia A. Wheeler
spellingShingle Delphine Thibault
Erica J. H. Head
Patricia A. Wheeler
Deep-Sea Research I 46 (1999) 1391}1415 Mesozooplankton in the Arctic Ocean in summer
author_facet Delphine Thibault
Erica J. H. Head
Patricia A. Wheeler
author_sort Delphine Thibault
title Deep-Sea Research I 46 (1999) 1391}1415 Mesozooplankton in the Arctic Ocean in summer
title_short Deep-Sea Research I 46 (1999) 1391}1415 Mesozooplankton in the Arctic Ocean in summer
title_full Deep-Sea Research I 46 (1999) 1391}1415 Mesozooplankton in the Arctic Ocean in summer
title_fullStr Deep-Sea Research I 46 (1999) 1391}1415 Mesozooplankton in the Arctic Ocean in summer
title_full_unstemmed Deep-Sea Research I 46 (1999) 1391}1415 Mesozooplankton in the Arctic Ocean in summer
title_sort deep-sea research i 46 (1999) 1391}1415 mesozooplankton in the arctic ocean in summer
publishDate 1997
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.3784
http://www.com.univ-mrs.fr/~botha/thibault et al, AOS94.pdf
long_lat ENVELOPE(74.000,74.000,87.000,87.000)
geographic Amundsen Basin
Arctic
Arctic Ocean
Chukchi Sea
geographic_facet Amundsen Basin
Arctic
Arctic Ocean
Chukchi Sea
genre amundsen basin
Arctic
Arctic Ocean
Calanus hyperboreus
Chukchi
Chukchi Sea
Nansen Basin
Phytoplankton
Copepods
genre_facet amundsen basin
Arctic
Arctic Ocean
Calanus hyperboreus
Chukchi
Chukchi Sea
Nansen Basin
Phytoplankton
Copepods
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http://www.com.univ-mrs.fr/~botha/thibault et al, AOS94.pdf
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