Microbial eukaryotic distribution in a dynamic Beaufort Sea and the Arctic Ocean

When Pacific Waters enter the Arctic Ocean, there is an abrupt change from temperature to salinity stratification of the upper water column. This change coincides with a faunal change as Pacific and Bering Sea zooplankton and fish species are replaced by Arctic species. The clear changes in distribu...

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Published in:Journal of Plankton Research
Main Authors: Lovejoy, Connie, Potvin, Marianne
Format: Text
Language:English
Published: Oxford University Press 2010
Subjects:
Online Access:http://plankt.oxfordjournals.org/cgi/content/short/fbq124v1
https://doi.org/10.1093/plankt/fbq124
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spelling fthighwire:oai:open-archive.highwire.org:plankt:fbq124v1 2023-05-15T14:32:22+02:00 Microbial eukaryotic distribution in a dynamic Beaufort Sea and the Arctic Ocean Lovejoy, Connie Potvin, Marianne 2010-09-29 06:35:35.0 text/html http://plankt.oxfordjournals.org/cgi/content/short/fbq124v1 https://doi.org/10.1093/plankt/fbq124 en eng Oxford University Press http://plankt.oxfordjournals.org/cgi/content/short/fbq124v1 http://dx.doi.org/10.1093/plankt/fbq124 Copyright (C) 2010, Oxford University Press Article TEXT 2010 fthighwire https://doi.org/10.1093/plankt/fbq124 2016-11-16T18:35:49Z When Pacific Waters enter the Arctic Ocean, there is an abrupt change from temperature to salinity stratification of the upper water column. This change coincides with a faunal change as Pacific and Bering Sea zooplankton and fish species are replaced by Arctic species. The clear changes in distributions of larger organisms suggest that the Arctic is an ideal environment to test hypothesis of endemism in single-celled planktonic groups. Here, we investigate the distribution of phylotypes of small protists identified by their 18S rRNA gene. We constructed nine new clone libraries from three different water masses from samples collected along the continental shelf and offshore of Beaufort Sea, Western Canadian Arctic. The new data combined with all other available sequences from the Arctic were used to identify possible phylotypes with restricted Arctic distributions. Among those only reported to date from the Arctic were an oligotrichous ciliate, a chlorarachniophyte and a rhizarian. In the near-surface shelf sample, we also retrieved sequences from Pacific species that had not been previously reported in the Arctic. The occurrences of those phylotypes were best explained by incursions of Pacific Water as coastal currents in combination with elevated temperatures in 2005 that would have been favourable to the non-Arctic phylotypes. Overall, we found support for the notion of microbial biogeography and our results suggest that the Arctic may be vulnerable to microbial community changes. Text Arctic Arctic Ocean Beaufort Sea Bering Sea Zooplankton HighWire Press (Stanford University) Arctic Arctic Ocean Bering Sea Pacific Journal of Plankton Research 33 3 431 444
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Article
spellingShingle Article
Lovejoy, Connie
Potvin, Marianne
Microbial eukaryotic distribution in a dynamic Beaufort Sea and the Arctic Ocean
topic_facet Article
description When Pacific Waters enter the Arctic Ocean, there is an abrupt change from temperature to salinity stratification of the upper water column. This change coincides with a faunal change as Pacific and Bering Sea zooplankton and fish species are replaced by Arctic species. The clear changes in distributions of larger organisms suggest that the Arctic is an ideal environment to test hypothesis of endemism in single-celled planktonic groups. Here, we investigate the distribution of phylotypes of small protists identified by their 18S rRNA gene. We constructed nine new clone libraries from three different water masses from samples collected along the continental shelf and offshore of Beaufort Sea, Western Canadian Arctic. The new data combined with all other available sequences from the Arctic were used to identify possible phylotypes with restricted Arctic distributions. Among those only reported to date from the Arctic were an oligotrichous ciliate, a chlorarachniophyte and a rhizarian. In the near-surface shelf sample, we also retrieved sequences from Pacific species that had not been previously reported in the Arctic. The occurrences of those phylotypes were best explained by incursions of Pacific Water as coastal currents in combination with elevated temperatures in 2005 that would have been favourable to the non-Arctic phylotypes. Overall, we found support for the notion of microbial biogeography and our results suggest that the Arctic may be vulnerable to microbial community changes.
format Text
author Lovejoy, Connie
Potvin, Marianne
author_facet Lovejoy, Connie
Potvin, Marianne
author_sort Lovejoy, Connie
title Microbial eukaryotic distribution in a dynamic Beaufort Sea and the Arctic Ocean
title_short Microbial eukaryotic distribution in a dynamic Beaufort Sea and the Arctic Ocean
title_full Microbial eukaryotic distribution in a dynamic Beaufort Sea and the Arctic Ocean
title_fullStr Microbial eukaryotic distribution in a dynamic Beaufort Sea and the Arctic Ocean
title_full_unstemmed Microbial eukaryotic distribution in a dynamic Beaufort Sea and the Arctic Ocean
title_sort microbial eukaryotic distribution in a dynamic beaufort sea and the arctic ocean
publisher Oxford University Press
publishDate 2010
url http://plankt.oxfordjournals.org/cgi/content/short/fbq124v1
https://doi.org/10.1093/plankt/fbq124
geographic Arctic
Arctic Ocean
Bering Sea
Pacific
geographic_facet Arctic
Arctic Ocean
Bering Sea
Pacific
genre Arctic
Arctic Ocean
Beaufort Sea
Bering Sea
Zooplankton
genre_facet Arctic
Arctic Ocean
Beaufort Sea
Bering Sea
Zooplankton
op_relation http://plankt.oxfordjournals.org/cgi/content/short/fbq124v1
http://dx.doi.org/10.1093/plankt/fbq124
op_rights Copyright (C) 2010, Oxford University Press
op_doi https://doi.org/10.1093/plankt/fbq124
container_title Journal of Plankton Research
container_volume 33
container_issue 3
container_start_page 431
op_container_end_page 444
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