The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean
The distribution of dissolved zinc (Zn) was investigated in the Atlantic sector of the Southern Ocean in the austral autumn of 2008 as part of the IPY GEOTRACES expedition ZERO & DRAKE. Research focused on transects across the major frontal systems along the Zero Meridian and across the Drake Pa...
Published in: | Deep Sea Research Part II: Topical Studies in Oceanography |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2011
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Subjects: | |
Online Access: | https://oceanrep.geomar.de/id/eprint/12444/ https://oceanrep.geomar.de/id/eprint/12444/1/Distribution.pdf https://oceanrep.geomar.de/id/eprint/12444/2/tables.csv https://doi.org/10.1016/j.dsr2.2010.10.041 |
_version_ | 1821748436910735360 |
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author | Croot, Peter Baars, Oliver Streu, Peter |
author_facet | Croot, Peter Baars, Oliver Streu, Peter |
author_sort | Croot, Peter |
collection | OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
container_issue | 25-26 |
container_start_page | 2707 |
container_title | Deep Sea Research Part II: Topical Studies in Oceanography |
container_volume | 58 |
description | The distribution of dissolved zinc (Zn) was investigated in the Atlantic sector of the Southern Ocean in the austral autumn of 2008 as part of the IPY GEOTRACES expedition ZERO & DRAKE. Research focused on transects across the major frontal systems along the Zero Meridian and across the Drake Passage. There was a strong gradient in surface zinc concentrations observed across the Antarctic Polar Front along both transects and high zinc levels were found in surface waters throughout the Southern Ocean. Vertical profiles for dissolved Zinc showed the presence of local minima and maxima in the upper 200 m consistent with significant uptake by phytoplankton and release by zooplankton grazing, respectively. Highest deep water zinc concentrations were found in the centre of the Weddell Gyre associated with Central Intermediate Water (CIW), a water mass which is depleted in O2, elevated in CO2 and is regionally a CFC minimum. Our data suggests that the remineralization of sinking particles is a key control on the distribution of Zn in the Southern Ocean. Disappearance ratios of zinc to phosphate (Zn:P) in the upper water column increased southwards along both transects and based on laboratory studies they suggest slower growth rates of phytoplankton due to iron or light limitation. Zinc and silicate were strongly correlated throughout the study region but the disappearance ratio (Zn:Si) was relatively uniform overall except for the region close to the ice edge on the Zero Meridian. |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Drake Passage IPY Southern Ocean |
genre_facet | Antarc* Antarctic Drake Passage IPY Southern Ocean |
geographic | Antarctic Southern Ocean The Antarctic Austral Drake Passage Weddell |
geographic_facet | Antarctic Southern Ocean The Antarctic Austral Drake Passage Weddell |
id | ftoceanrep:oai:oceanrep.geomar.de:12444 |
institution | Open Polar |
language | English |
op_collection_id | ftoceanrep |
op_container_end_page | 2719 |
op_doi | https://doi.org/10.1016/j.dsr2.2010.10.041 |
op_relation | https://oceanrep.geomar.de/id/eprint/12444/1/Distribution.pdf https://oceanrep.geomar.de/id/eprint/12444/2/tables.csv Croot, P., Baars, O. and Streu, P. (2011) The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean. Deep Sea Research Part II: Topical Studies in Oceanography, 58 (25-26). pp. 2707-2719. DOI 10.1016/j.dsr2.2010.10.041 <https://doi.org/10.1016/j.dsr2.2010.10.041>. doi:10.1016/j.dsr2.2010.10.041 |
op_rights | info:eu-repo/semantics/restrictedAccess |
publishDate | 2011 |
publisher | Elsevier |
record_format | openpolar |
spelling | ftoceanrep:oai:oceanrep.geomar.de:12444 2025-01-16T19:19:55+00:00 The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean Croot, Peter Baars, Oliver Streu, Peter 2011 text https://oceanrep.geomar.de/id/eprint/12444/ https://oceanrep.geomar.de/id/eprint/12444/1/Distribution.pdf https://oceanrep.geomar.de/id/eprint/12444/2/tables.csv https://doi.org/10.1016/j.dsr2.2010.10.041 en eng Elsevier https://oceanrep.geomar.de/id/eprint/12444/1/Distribution.pdf https://oceanrep.geomar.de/id/eprint/12444/2/tables.csv Croot, P., Baars, O. and Streu, P. (2011) The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean. Deep Sea Research Part II: Topical Studies in Oceanography, 58 (25-26). pp. 2707-2719. DOI 10.1016/j.dsr2.2010.10.041 <https://doi.org/10.1016/j.dsr2.2010.10.041>. doi:10.1016/j.dsr2.2010.10.041 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2011 ftoceanrep https://doi.org/10.1016/j.dsr2.2010.10.041 2023-04-07T15:00:48Z The distribution of dissolved zinc (Zn) was investigated in the Atlantic sector of the Southern Ocean in the austral autumn of 2008 as part of the IPY GEOTRACES expedition ZERO & DRAKE. Research focused on transects across the major frontal systems along the Zero Meridian and across the Drake Passage. There was a strong gradient in surface zinc concentrations observed across the Antarctic Polar Front along both transects and high zinc levels were found in surface waters throughout the Southern Ocean. Vertical profiles for dissolved Zinc showed the presence of local minima and maxima in the upper 200 m consistent with significant uptake by phytoplankton and release by zooplankton grazing, respectively. Highest deep water zinc concentrations were found in the centre of the Weddell Gyre associated with Central Intermediate Water (CIW), a water mass which is depleted in O2, elevated in CO2 and is regionally a CFC minimum. Our data suggests that the remineralization of sinking particles is a key control on the distribution of Zn in the Southern Ocean. Disappearance ratios of zinc to phosphate (Zn:P) in the upper water column increased southwards along both transects and based on laboratory studies they suggest slower growth rates of phytoplankton due to iron or light limitation. Zinc and silicate were strongly correlated throughout the study region but the disappearance ratio (Zn:Si) was relatively uniform overall except for the region close to the ice edge on the Zero Meridian. Article in Journal/Newspaper Antarc* Antarctic Drake Passage IPY Southern Ocean OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Antarctic Southern Ocean The Antarctic Austral Drake Passage Weddell Deep Sea Research Part II: Topical Studies in Oceanography 58 25-26 2707 2719 |
spellingShingle | Croot, Peter Baars, Oliver Streu, Peter The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean |
title | The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean |
title_full | The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean |
title_fullStr | The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean |
title_full_unstemmed | The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean |
title_short | The distribution of dissolved zinc in the Atlantic sector of the Southern Ocean |
title_sort | distribution of dissolved zinc in the atlantic sector of the southern ocean |
url | https://oceanrep.geomar.de/id/eprint/12444/ https://oceanrep.geomar.de/id/eprint/12444/1/Distribution.pdf https://oceanrep.geomar.de/id/eprint/12444/2/tables.csv https://doi.org/10.1016/j.dsr2.2010.10.041 |