Coherent Sign Switching in Multiyear Trends of Microbial Plankton

Since the 1990s, phytoplankton biomass on the continental shelf of Nova Scotia and in the Labrador Sea has undergone sustained changes in the spring and fall, which are accompanied by changes in bacterioplankton that are dampened in amplitude but coherent in the direction of change. A reversal of tr...

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Published in:Science
Main Authors: Li, William K. W., Harrison, W. Glen, Head, Erica J. H.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2006
Subjects:
Online Access:http://dx.doi.org/10.1126/science.1122748
https://www.science.org/doi/pdf/10.1126/science.1122748
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spelling craaas:10.1126/science.1122748 2024-09-09T19:50:38+00:00 Coherent Sign Switching in Multiyear Trends of Microbial Plankton Li, William K. W. Harrison, W. Glen Head, Erica J. H. 2006 http://dx.doi.org/10.1126/science.1122748 https://www.science.org/doi/pdf/10.1126/science.1122748 en eng American Association for the Advancement of Science (AAAS) Science volume 311, issue 5764, page 1157-1160 ISSN 0036-8075 1095-9203 journal-article 2006 craaas https://doi.org/10.1126/science.1122748 2024-06-20T04:01:55Z Since the 1990s, phytoplankton biomass on the continental shelf of Nova Scotia and in the Labrador Sea has undergone sustained changes in the spring and fall, which are accompanied by changes in bacterioplankton that are dampened in amplitude but coherent in the direction of change. A reversal of trend in biomass change, so-called sign switching, occurs both in time and in space. Thus, whenever (spring or fall) and wherever (Scotian Shelf or Labrador Sea) phytoplankton increase or decrease, so also does bacterioplankton. This tandem sign switch indicates coupling of the trophic levels at a multiyear time scale and contributes to an ecological fingerprint of systemwide forcing. Article in Journal/Newspaper Labrador Sea AAAS Resource Center (American Association for the Advancement of Science) Science 311 5764 1157 1160
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Since the 1990s, phytoplankton biomass on the continental shelf of Nova Scotia and in the Labrador Sea has undergone sustained changes in the spring and fall, which are accompanied by changes in bacterioplankton that are dampened in amplitude but coherent in the direction of change. A reversal of trend in biomass change, so-called sign switching, occurs both in time and in space. Thus, whenever (spring or fall) and wherever (Scotian Shelf or Labrador Sea) phytoplankton increase or decrease, so also does bacterioplankton. This tandem sign switch indicates coupling of the trophic levels at a multiyear time scale and contributes to an ecological fingerprint of systemwide forcing.
format Article in Journal/Newspaper
author Li, William K. W.
Harrison, W. Glen
Head, Erica J. H.
spellingShingle Li, William K. W.
Harrison, W. Glen
Head, Erica J. H.
Coherent Sign Switching in Multiyear Trends of Microbial Plankton
author_facet Li, William K. W.
Harrison, W. Glen
Head, Erica J. H.
author_sort Li, William K. W.
title Coherent Sign Switching in Multiyear Trends of Microbial Plankton
title_short Coherent Sign Switching in Multiyear Trends of Microbial Plankton
title_full Coherent Sign Switching in Multiyear Trends of Microbial Plankton
title_fullStr Coherent Sign Switching in Multiyear Trends of Microbial Plankton
title_full_unstemmed Coherent Sign Switching in Multiyear Trends of Microbial Plankton
title_sort coherent sign switching in multiyear trends of microbial plankton
publisher American Association for the Advancement of Science (AAAS)
publishDate 2006
url http://dx.doi.org/10.1126/science.1122748
https://www.science.org/doi/pdf/10.1126/science.1122748
genre Labrador Sea
genre_facet Labrador Sea
op_source Science
volume 311, issue 5764, page 1157-1160
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.1122748
container_title Science
container_volume 311
container_issue 5764
container_start_page 1157
op_container_end_page 1160
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