Phosphorus dynamics in the Barents Sea
The Barents Sea is considered a warming hotspot in the Arctic; elevated sea surface temperatures have been accompanied with increased inflow of Atlantic water onto the shelf sea. Such hydrodynamic changes and a concomitant reduction of sea ice coverage enables a prolonged phytoplankton growing season...
Published in: | Limnology and Oceanography |
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Wiley Periodicals LLC
2020
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Online Access: | http://plymsea.ac.uk/id/eprint/9064/ http://plymsea.ac.uk/id/eprint/9064/1/lno.11602.pdf https://doi.org/10.1002/lno.11602 |
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ftplymouthml:oai:plymsea.ac.uk:9064 2023-05-15T14:26:48+02:00 Phosphorus dynamics in the Barents Sea Downes, P Goult, S Woodward, EMS Widdicombe, CE Tait, K Dixon, JL 2020-09-23 text http://plymsea.ac.uk/id/eprint/9064/ http://plymsea.ac.uk/id/eprint/9064/1/lno.11602.pdf https://doi.org/10.1002/lno.11602 en eng Wiley Periodicals LLC http://plymsea.ac.uk/id/eprint/9064/1/lno.11602.pdf Downes, P; Goult, S; Woodward, EMS; Widdicombe, CE; Tait, K; Dixon, JL. 2020 Phosphorus dynamics in the Barents Sea [in special issue: Biogeochemistry and Ecology across Arctic Aquatic Ecosystems in the Face of Change] Limnology and Oceanography, lno.11602. 1-17. https://doi.org/10.1002/lno.11602 <https://doi.org/10.1002/lno.11602> cc_by_4 CC-BY Biology Chemistry Earth Observation - Remote Sensing Ecology and Environment Marine Sciences Oceanography Publication - Article PeerReviewed 2020 ftplymouthml https://doi.org/10.1002/lno.11602 2022-09-13T05:49:48Z The Barents Sea is considered a warming hotspot in the Arctic; elevated sea surface temperatures have been accompanied with increased inflow of Atlantic water onto the shelf sea. Such hydrodynamic changes and a concomitant reduction of sea ice coverage enables a prolonged phytoplankton growing season, which will inevitably affect nutrient stoichiometry and the controls on primary production. During the summer of 2018, we investigated the role of phosphorus in mediating primary production in the Barents Sea. Dissolved inorganic phosphorus (DIP), its most bioavailable form, had an average net turnover time of 9.4�4.8 d. The most southern Atlantic influenced station accounted for both the highest rates of primary production (655 mg C m2 d−1) and shortest net DIP turnover (2.8�0.5 d). The fraction of assimilated DIP released as dissolved organic phosphorus (DOP) at this station was < 4% compared to an average of 21% at all other stations. We observed significant differences between phytoplankton communities in Arctic and Atlantic waters within the Barents Sea. Slower DIP turnover and greater release of DOP was associated with Phaeocystis pouchetii dominated communities in Arctic waters. Faster turnover rates and greater phosphorus retention occurred among the Atlantic phytoplankton communities dominated by Emiliania huxleyi. Thesefindings provide baseline measurements of P utilization in the Barents Sea, and suggest increased Atlantic intrusion of this region could be accompanied by more rapid DIP turnover, possibly leading to future P limitation (rather than N limitation) on primary production Article in Journal/Newspaper Arctic Arctic Barents Sea Phytoplankton Sea ice Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) Arctic Barents Sea Limnology and Oceanography 66 S1 |
institution |
Open Polar |
collection |
Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) |
op_collection_id |
ftplymouthml |
language |
English |
topic |
Biology Chemistry Earth Observation - Remote Sensing Ecology and Environment Marine Sciences Oceanography |
spellingShingle |
Biology Chemistry Earth Observation - Remote Sensing Ecology and Environment Marine Sciences Oceanography Downes, P Goult, S Woodward, EMS Widdicombe, CE Tait, K Dixon, JL Phosphorus dynamics in the Barents Sea |
topic_facet |
Biology Chemistry Earth Observation - Remote Sensing Ecology and Environment Marine Sciences Oceanography |
description |
The Barents Sea is considered a warming hotspot in the Arctic; elevated sea surface temperatures have been accompanied with increased inflow of Atlantic water onto the shelf sea. Such hydrodynamic changes and a concomitant reduction of sea ice coverage enables a prolonged phytoplankton growing season, which will inevitably affect nutrient stoichiometry and the controls on primary production. During the summer of 2018, we investigated the role of phosphorus in mediating primary production in the Barents Sea. Dissolved inorganic phosphorus (DIP), its most bioavailable form, had an average net turnover time of 9.4�4.8 d. The most southern Atlantic influenced station accounted for both the highest rates of primary production (655 mg C m2 d−1) and shortest net DIP turnover (2.8�0.5 d). The fraction of assimilated DIP released as dissolved organic phosphorus (DOP) at this station was < 4% compared to an average of 21% at all other stations. We observed significant differences between phytoplankton communities in Arctic and Atlantic waters within the Barents Sea. Slower DIP turnover and greater release of DOP was associated with Phaeocystis pouchetii dominated communities in Arctic waters. Faster turnover rates and greater phosphorus retention occurred among the Atlantic phytoplankton communities dominated by Emiliania huxleyi. Thesefindings provide baseline measurements of P utilization in the Barents Sea, and suggest increased Atlantic intrusion of this region could be accompanied by more rapid DIP turnover, possibly leading to future P limitation (rather than N limitation) on primary production |
format |
Article in Journal/Newspaper |
author |
Downes, P Goult, S Woodward, EMS Widdicombe, CE Tait, K Dixon, JL |
author_facet |
Downes, P Goult, S Woodward, EMS Widdicombe, CE Tait, K Dixon, JL |
author_sort |
Downes, P |
title |
Phosphorus dynamics in the Barents Sea |
title_short |
Phosphorus dynamics in the Barents Sea |
title_full |
Phosphorus dynamics in the Barents Sea |
title_fullStr |
Phosphorus dynamics in the Barents Sea |
title_full_unstemmed |
Phosphorus dynamics in the Barents Sea |
title_sort |
phosphorus dynamics in the barents sea |
publisher |
Wiley Periodicals LLC |
publishDate |
2020 |
url |
http://plymsea.ac.uk/id/eprint/9064/ http://plymsea.ac.uk/id/eprint/9064/1/lno.11602.pdf https://doi.org/10.1002/lno.11602 |
geographic |
Arctic Barents Sea |
geographic_facet |
Arctic Barents Sea |
genre |
Arctic Arctic Barents Sea Phytoplankton Sea ice |
genre_facet |
Arctic Arctic Barents Sea Phytoplankton Sea ice |
op_relation |
http://plymsea.ac.uk/id/eprint/9064/1/lno.11602.pdf Downes, P; Goult, S; Woodward, EMS; Widdicombe, CE; Tait, K; Dixon, JL. 2020 Phosphorus dynamics in the Barents Sea [in special issue: Biogeochemistry and Ecology across Arctic Aquatic Ecosystems in the Face of Change] Limnology and Oceanography, lno.11602. 1-17. https://doi.org/10.1002/lno.11602 <https://doi.org/10.1002/lno.11602> |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1002/lno.11602 |
container_title |
Limnology and Oceanography |
container_volume |
66 |
container_issue |
S1 |
_version_ |
1766300231374209024 |