Spring phytoplankton onset after the ice break-up and sea-ice signature (Adélie Land, East Antarctica)

The phytoplankton onset following the spring ice break-up in Adélie Land, East Antarctica, was studied along a short transect, from 400 m off the continent to 5 km offshore, during the austral summer of 2002. Eight days after the ice break-up, some large colonial and solitary diatom cells, known to...

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Published in:Polar Research
Main Authors: Riaux-Gobin, Catherine, Poulin, Michel, Dieckmann, Gerhard, Labrune, Céline, Vétion, Gilles
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2011
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/3048
https://doi.org/10.3402/polar.v30i0.5910
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spelling ftjpolarres:oai:journals.openacademia.net:article/3048 2023-05-15T14:01:21+02:00 Spring phytoplankton onset after the ice break-up and sea-ice signature (Adélie Land, East Antarctica) Riaux-Gobin, Catherine Poulin, Michel Dieckmann, Gerhard Labrune, Céline Vétion, Gilles 2011-01-09 application/pdf text/html application/epub+zip text/xml https://polarresearch.net/index.php/polar/article/view/3048 https://doi.org/10.3402/polar.v30i0.5910 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/3048/pdf_58 https://polarresearch.net/index.php/polar/article/view/3048/html_67 https://polarresearch.net/index.php/polar/article/view/3048/6900 https://polarresearch.net/index.php/polar/article/view/3048/xml_67 https://polarresearch.net/index.php/polar/article/view/3048 doi:10.3402/polar.v30i0.5910 Copyright (c) 2018 Polar Research Polar Research; Vol 30 (2011) 1751-8369 Ice break-up phytoplankton sea-ice signature East Antarctica info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2011 ftjpolarres https://doi.org/10.3402/polar.v30i0.5910 2021-11-11T19:13:37Z The phytoplankton onset following the spring ice break-up in Adélie Land, East Antarctica, was studied along a short transect, from 400 m off the continent to 5 km offshore, during the austral summer of 2002. Eight days after the ice break-up, some large colonial and solitary diatom cells, known to be associated with land-fast ice and present in downward fluxes, were unable to adapt in ice-free waters, while some other solitary and short-colony forming taxa (e.g., Fragilariopsis curta, F. cylindrus) did develop. Pelagic species were becoming more abundant offshore, replacing the typical sympagic (ice-associated) taxa. Archaeomonad cysts, usually associated with sea ice, were recorded in the surface waters nearshore. Rough weather restricted the data set, but we were able to confirm that some microalgae may be reliable sea-ice indicators and that seeding by sea ice only concerns a few taxa in this coastal area of East Antarctica. Keywords: Ice break-up; phytoplankton; sea-ice signature; East Antarctica (Published: 10 January 2011) Citation: Polar Research 2011, 30, 5910, doi:10.3402/polar.v30i0.5910 Article in Journal/Newspaper Antarc* Antarctica East Antarctica Polar Research Sea ice Polar Research (E-Journal) Austral East Antarctica Polar Research 30 1 5910
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
topic Ice break-up
phytoplankton
sea-ice signature
East Antarctica
spellingShingle Ice break-up
phytoplankton
sea-ice signature
East Antarctica
Riaux-Gobin, Catherine
Poulin, Michel
Dieckmann, Gerhard
Labrune, Céline
Vétion, Gilles
Spring phytoplankton onset after the ice break-up and sea-ice signature (Adélie Land, East Antarctica)
topic_facet Ice break-up
phytoplankton
sea-ice signature
East Antarctica
description The phytoplankton onset following the spring ice break-up in Adélie Land, East Antarctica, was studied along a short transect, from 400 m off the continent to 5 km offshore, during the austral summer of 2002. Eight days after the ice break-up, some large colonial and solitary diatom cells, known to be associated with land-fast ice and present in downward fluxes, were unable to adapt in ice-free waters, while some other solitary and short-colony forming taxa (e.g., Fragilariopsis curta, F. cylindrus) did develop. Pelagic species were becoming more abundant offshore, replacing the typical sympagic (ice-associated) taxa. Archaeomonad cysts, usually associated with sea ice, were recorded in the surface waters nearshore. Rough weather restricted the data set, but we were able to confirm that some microalgae may be reliable sea-ice indicators and that seeding by sea ice only concerns a few taxa in this coastal area of East Antarctica. Keywords: Ice break-up; phytoplankton; sea-ice signature; East Antarctica (Published: 10 January 2011) Citation: Polar Research 2011, 30, 5910, doi:10.3402/polar.v30i0.5910
format Article in Journal/Newspaper
author Riaux-Gobin, Catherine
Poulin, Michel
Dieckmann, Gerhard
Labrune, Céline
Vétion, Gilles
author_facet Riaux-Gobin, Catherine
Poulin, Michel
Dieckmann, Gerhard
Labrune, Céline
Vétion, Gilles
author_sort Riaux-Gobin, Catherine
title Spring phytoplankton onset after the ice break-up and sea-ice signature (Adélie Land, East Antarctica)
title_short Spring phytoplankton onset after the ice break-up and sea-ice signature (Adélie Land, East Antarctica)
title_full Spring phytoplankton onset after the ice break-up and sea-ice signature (Adélie Land, East Antarctica)
title_fullStr Spring phytoplankton onset after the ice break-up and sea-ice signature (Adélie Land, East Antarctica)
title_full_unstemmed Spring phytoplankton onset after the ice break-up and sea-ice signature (Adélie Land, East Antarctica)
title_sort spring phytoplankton onset after the ice break-up and sea-ice signature (adélie land, east antarctica)
publisher Norwegian Polar Institute
publishDate 2011
url https://polarresearch.net/index.php/polar/article/view/3048
https://doi.org/10.3402/polar.v30i0.5910
geographic Austral
East Antarctica
geographic_facet Austral
East Antarctica
genre Antarc*
Antarctica
East Antarctica
Polar Research
Sea ice
genre_facet Antarc*
Antarctica
East Antarctica
Polar Research
Sea ice
op_source Polar Research; Vol 30 (2011)
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/3048/pdf_58
https://polarresearch.net/index.php/polar/article/view/3048/html_67
https://polarresearch.net/index.php/polar/article/view/3048/6900
https://polarresearch.net/index.php/polar/article/view/3048/xml_67
https://polarresearch.net/index.php/polar/article/view/3048
doi:10.3402/polar.v30i0.5910
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v30i0.5910
container_title Polar Research
container_volume 30
container_issue 1
container_start_page 5910
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