Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production
In temperate, subpolar and polar marine systems, the classical perception is that diatoms initiate the spring bloom and thereby mark the beginning of the productive season. Contrary to this view, we document an active microbial food web dominated by pico- and nanoplankton prior to the diatom bloom,...
Published in: | Aquatic Microbial Ecology |
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Format: | Article in Journal/Newspaper |
Language: | English |
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2015
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Online Access: | https://orbit.dtu.dk/en/publications/82fdec73-8503-47c8-8f3e-d4c0891f5084 https://doi.org/10.3354/ame01767 https://backend.orbit.dtu.dk/ws/files/116550910/Publishers_version.pdf |
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ftdtupubl:oai:pure.atira.dk:publications/82fdec73-8503-47c8-8f3e-d4c0891f5084 2023-12-24T10:17:56+01:00 Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production Paulsen, Maria Lund Riisgaard, Karen Thingstad, T. Frede St. John, Michael Nielsen, Torkel Gissel 2015 application/pdf https://orbit.dtu.dk/en/publications/82fdec73-8503-47c8-8f3e-d4c0891f5084 https://doi.org/10.3354/ame01767 https://backend.orbit.dtu.dk/ws/files/116550910/Publishers_version.pdf eng eng info:eu-repo/grantAgreement/EC/FP7/264933 https://orbit.dtu.dk/en/publications/82fdec73-8503-47c8-8f3e-d4c0891f5084 info:eu-repo/semantics/openAccess Paulsen , M L , Riisgaard , K , Thingstad , T F , St. John , M & Nielsen , T G 2015 , ' Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production ' , Aquatic Microbial Ecology , vol. 76 , no. 1 , pp. 49-69 . https://doi.org/10.3354/ame01767 /dk/atira/pure/sustainabledevelopmentgoals/life_below_water name=SDG 14 - Life Below Water article 2015 ftdtupubl https://doi.org/10.3354/ame01767 2023-11-30T00:00:43Z In temperate, subpolar and polar marine systems, the classical perception is that diatoms initiate the spring bloom and thereby mark the beginning of the productive season. Contrary to this view, we document an active microbial food web dominated by pico- and nanoplankton prior to the diatom bloom, a period with excess nutrients and deep convection of the water column. During repeated visits to stations in the deep Iceland and Norwegian basins and the shallow Shetland Shelf (26 March to 29 April 2012), we investigated the succession and dynamics of photo - synthetic and heterotrophic microorganisms. We observed that the early phytoplankton production was followed by a decrease in the carbon:nitrogen ratio of the dissolved organic matter in the deep mixed stations, an increase in heterotrophic prokaryote (bacteria) abundance and activity (indicated by the high nucleic acid:low nucleic acid bacteria ratio), and an increase in abundance and size of heterotrophic protists. The major chl a contribution in the early winter−spring transition was found in the fraction <10 μm, i.e. dominated by pico- and small nanophytoplankton. The relative abundance of picophytoplankton decreased towards the end of the cruise at all stations despite nutrient-replete conditions and increasing day length. This decrease is hypothesised to be the result of top-down control by the fast-growing population of heterotrophic protists. As a result, the subsequent succession and nutrient depletion can be left to larger phytoplankton resistant to small grazers. Further, we observed that large phytoplankton (chl a > 50 μm) were stimulated by deep mixing later in the period, while picophytoplankton were unaffected by mixing; both physical and biological reasons for this development are discussed herein Article in Journal/Newspaper Iceland Subarctic Technical University of Denmark: DTU Orbit Aquatic Microbial Ecology 76 1 49 69 |
institution |
Open Polar |
collection |
Technical University of Denmark: DTU Orbit |
op_collection_id |
ftdtupubl |
language |
English |
topic |
/dk/atira/pure/sustainabledevelopmentgoals/life_below_water name=SDG 14 - Life Below Water |
spellingShingle |
/dk/atira/pure/sustainabledevelopmentgoals/life_below_water name=SDG 14 - Life Below Water Paulsen, Maria Lund Riisgaard, Karen Thingstad, T. Frede St. John, Michael Nielsen, Torkel Gissel Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production |
topic_facet |
/dk/atira/pure/sustainabledevelopmentgoals/life_below_water name=SDG 14 - Life Below Water |
description |
In temperate, subpolar and polar marine systems, the classical perception is that diatoms initiate the spring bloom and thereby mark the beginning of the productive season. Contrary to this view, we document an active microbial food web dominated by pico- and nanoplankton prior to the diatom bloom, a period with excess nutrients and deep convection of the water column. During repeated visits to stations in the deep Iceland and Norwegian basins and the shallow Shetland Shelf (26 March to 29 April 2012), we investigated the succession and dynamics of photo - synthetic and heterotrophic microorganisms. We observed that the early phytoplankton production was followed by a decrease in the carbon:nitrogen ratio of the dissolved organic matter in the deep mixed stations, an increase in heterotrophic prokaryote (bacteria) abundance and activity (indicated by the high nucleic acid:low nucleic acid bacteria ratio), and an increase in abundance and size of heterotrophic protists. The major chl a contribution in the early winter−spring transition was found in the fraction <10 μm, i.e. dominated by pico- and small nanophytoplankton. The relative abundance of picophytoplankton decreased towards the end of the cruise at all stations despite nutrient-replete conditions and increasing day length. This decrease is hypothesised to be the result of top-down control by the fast-growing population of heterotrophic protists. As a result, the subsequent succession and nutrient depletion can be left to larger phytoplankton resistant to small grazers. Further, we observed that large phytoplankton (chl a > 50 μm) were stimulated by deep mixing later in the period, while picophytoplankton were unaffected by mixing; both physical and biological reasons for this development are discussed herein |
format |
Article in Journal/Newspaper |
author |
Paulsen, Maria Lund Riisgaard, Karen Thingstad, T. Frede St. John, Michael Nielsen, Torkel Gissel |
author_facet |
Paulsen, Maria Lund Riisgaard, Karen Thingstad, T. Frede St. John, Michael Nielsen, Torkel Gissel |
author_sort |
Paulsen, Maria Lund |
title |
Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production |
title_short |
Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production |
title_full |
Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production |
title_fullStr |
Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production |
title_full_unstemmed |
Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production |
title_sort |
winter−spring transition in the subarctic atlantic: microbial response to deep mixing and pre-bloom production |
publishDate |
2015 |
url |
https://orbit.dtu.dk/en/publications/82fdec73-8503-47c8-8f3e-d4c0891f5084 https://doi.org/10.3354/ame01767 https://backend.orbit.dtu.dk/ws/files/116550910/Publishers_version.pdf |
genre |
Iceland Subarctic |
genre_facet |
Iceland Subarctic |
op_source |
Paulsen , M L , Riisgaard , K , Thingstad , T F , St. John , M & Nielsen , T G 2015 , ' Winter−spring transition in the subarctic Atlantic: microbial response to deep mixing and pre-bloom production ' , Aquatic Microbial Ecology , vol. 76 , no. 1 , pp. 49-69 . https://doi.org/10.3354/ame01767 |
op_relation |
info:eu-repo/grantAgreement/EC/FP7/264933 https://orbit.dtu.dk/en/publications/82fdec73-8503-47c8-8f3e-d4c0891f5084 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.3354/ame01767 |
container_title |
Aquatic Microbial Ecology |
container_volume |
76 |
container_issue |
1 |
container_start_page |
49 |
op_container_end_page |
69 |
_version_ |
1786206400960004096 |