Phytoplankton communities of the Barents Sea frontal zone during the early spring period

Abstract In April 2018, complex studies of phytoplankton communities were carried out in the northwestern Barents Sea in the region of the Polar Front (74.8°-76.2° N) in a layer of 0-50 m. The region under study encompassed surface Arctic water and Atlantic water of the Fram branch (which conditiona...

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Published in:IOP Conference Series: Earth and Environmental Science
Main Authors: Vodopyanova, V, Larionov, V, Makarevich, P, Vashenko, P, Bulavina, A
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2020
Subjects:
Online Access:http://dx.doi.org/10.1088/1755-1315/432/1/012005
https://iopscience.iop.org/article/10.1088/1755-1315/432/1/012005/pdf
https://iopscience.iop.org/article/10.1088/1755-1315/432/1/012005
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spelling crioppubl:10.1088/1755-1315/432/1/012005 2024-06-02T07:58:06+00:00 Phytoplankton communities of the Barents Sea frontal zone during the early spring period Vodopyanova, V Larionov, V Makarevich, P Vashenko, P Bulavina, A 2020 http://dx.doi.org/10.1088/1755-1315/432/1/012005 https://iopscience.iop.org/article/10.1088/1755-1315/432/1/012005/pdf https://iopscience.iop.org/article/10.1088/1755-1315/432/1/012005 unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining IOP Conference Series: Earth and Environmental Science volume 432, issue 1, page 012005 ISSN 1755-1307 1755-1315 journal-article 2020 crioppubl https://doi.org/10.1088/1755-1315/432/1/012005 2024-05-07T14:06:30Z Abstract In April 2018, complex studies of phytoplankton communities were carried out in the northwestern Barents Sea in the region of the Polar Front (74.8°-76.2° N) in a layer of 0-50 m. The region under study encompassed surface Arctic water and Atlantic water of the Fram branch (which conditionally corresponds to the Arctic water mass) divided from the Atlantic water mass by the Polar Front. Phytoplankton community on both sides of the front were represented by early spring complex, 90% of biomass was formed by diatoms (Achnanthes taeniata, Nitzschia grunowii, Thalassiosira antarctica) . In water of Atlantic origin Phaeocystis pouchetii were found among the dominants. However, the level of development of microplankton was significantly higher in water from the Arctic Basin. The highest chlorophyll-a concentrations referred to surface Arctic water (3.13±0.43 mg/m 3 ) and Atlantic Fram water (2.04±0.29 mg/m 3 ). The concentration of chlorophyll-a at the stations performed in the Atlantic water mass was an order of magnitude lower - 0.50±0.26 mg/m 3 . Thus, during the early-spring period, the Polar Front is a powerful boundary that limits exclusively the level of development and quantitative indicators of the early spring microphytoplankton complex. The front line separates the more productive Arctic water, with average chlorophyll-a concentrations of 2-3 mg/m 3 , from the Atlantic water, in which concentrations of this pigment are an order of magnitude lower. Article in Journal/Newspaper Antarc* Antarctica Arctic Basin Arctic Barents Sea Phytoplankton IOP Publishing Arctic Barents Sea IOP Conference Series: Earth and Environmental Science 432 012005
institution Open Polar
collection IOP Publishing
op_collection_id crioppubl
language unknown
description Abstract In April 2018, complex studies of phytoplankton communities were carried out in the northwestern Barents Sea in the region of the Polar Front (74.8°-76.2° N) in a layer of 0-50 m. The region under study encompassed surface Arctic water and Atlantic water of the Fram branch (which conditionally corresponds to the Arctic water mass) divided from the Atlantic water mass by the Polar Front. Phytoplankton community on both sides of the front were represented by early spring complex, 90% of biomass was formed by diatoms (Achnanthes taeniata, Nitzschia grunowii, Thalassiosira antarctica) . In water of Atlantic origin Phaeocystis pouchetii were found among the dominants. However, the level of development of microplankton was significantly higher in water from the Arctic Basin. The highest chlorophyll-a concentrations referred to surface Arctic water (3.13±0.43 mg/m 3 ) and Atlantic Fram water (2.04±0.29 mg/m 3 ). The concentration of chlorophyll-a at the stations performed in the Atlantic water mass was an order of magnitude lower - 0.50±0.26 mg/m 3 . Thus, during the early-spring period, the Polar Front is a powerful boundary that limits exclusively the level of development and quantitative indicators of the early spring microphytoplankton complex. The front line separates the more productive Arctic water, with average chlorophyll-a concentrations of 2-3 mg/m 3 , from the Atlantic water, in which concentrations of this pigment are an order of magnitude lower.
format Article in Journal/Newspaper
author Vodopyanova, V
Larionov, V
Makarevich, P
Vashenko, P
Bulavina, A
spellingShingle Vodopyanova, V
Larionov, V
Makarevich, P
Vashenko, P
Bulavina, A
Phytoplankton communities of the Barents Sea frontal zone during the early spring period
author_facet Vodopyanova, V
Larionov, V
Makarevich, P
Vashenko, P
Bulavina, A
author_sort Vodopyanova, V
title Phytoplankton communities of the Barents Sea frontal zone during the early spring period
title_short Phytoplankton communities of the Barents Sea frontal zone during the early spring period
title_full Phytoplankton communities of the Barents Sea frontal zone during the early spring period
title_fullStr Phytoplankton communities of the Barents Sea frontal zone during the early spring period
title_full_unstemmed Phytoplankton communities of the Barents Sea frontal zone during the early spring period
title_sort phytoplankton communities of the barents sea frontal zone during the early spring period
publisher IOP Publishing
publishDate 2020
url http://dx.doi.org/10.1088/1755-1315/432/1/012005
https://iopscience.iop.org/article/10.1088/1755-1315/432/1/012005/pdf
https://iopscience.iop.org/article/10.1088/1755-1315/432/1/012005
geographic Arctic
Barents Sea
geographic_facet Arctic
Barents Sea
genre Antarc*
Antarctica
Arctic Basin
Arctic
Barents Sea
Phytoplankton
genre_facet Antarc*
Antarctica
Arctic Basin
Arctic
Barents Sea
Phytoplankton
op_source IOP Conference Series: Earth and Environmental Science
volume 432, issue 1, page 012005
ISSN 1755-1307 1755-1315
op_rights http://creativecommons.org/licenses/by/3.0/
https://iopscience.iop.org/info/page/text-and-data-mining
op_doi https://doi.org/10.1088/1755-1315/432/1/012005
container_title IOP Conference Series: Earth and Environmental Science
container_volume 432
container_start_page 012005
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