The relationships between dissolved zinc and major nutrients phosphate and silicate along the GEOTRACES GA02 transect in the west Atlantic Ocean
Dissolved zinc (Zn) has a nutrient‐type distribution in the ocean that more closely resembles the distribution of silicate (Si) than phosphate (PO 4 ). However, Zn is a trace‐nutrient and mostly present in the organic fraction of phytoplankton rather than the siliceous frustule. It has been suggeste...
Published in: | Global Biogeochemical Cycles |
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Language: | English |
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ftnioz:oai:imis.nioz.nl:306545 2023-05-15T13:47:57+02:00 The relationships between dissolved zinc and major nutrients phosphate and silicate along the GEOTRACES GA02 transect in the west Atlantic Ocean Middag, R. de Baar, H.J.W. Bruland, K.W. 2019 application/pdf https://www.vliz.be/imisdocs/publications/75/324675.pdf en eng info:eu-repo/semantics/altIdentifier/wos/000458243500005 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1029/2018gb006034 https://www.vliz.be/imisdocs/publications/75/324675.pdf info:eu-repo/semantics/openAccess %3Ci%3EGlobal+Biogeochem.+Cycles+33%281%29%3C%2Fi%3E%3A+63-84.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1029%2F2018gb006034%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1029%2F2018gb006034%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2019 ftnioz https://doi.org/10.1029/2018gb006034 2022-05-01T14:09:00Z Dissolved zinc (Zn) has a nutrient‐type distribution in the ocean that more closely resembles the distribution of silicate (Si) than phosphate (PO 4 ). However, Zn is a trace‐nutrient and mostly present in the organic fraction of phytoplankton rather than the siliceous frustule. It has been suggested the coupling of Zn and Si is caused by the strong depletion of nutrients in the Southern Ocean, possibly combined with scavenging of Zn. Here we assess the distribution of Zn and nutrients along the conduit of southward traveling waters of northern origin and northward traveling waters of Antarctic origin to unravel the influence of various water masses and local biogeochemical processes in the Atlantic Ocean. The distribution of Zn and Si is governed by mixing such that influence of remineralization is barely distinguishable, whereas the distribution of PO 4 is influenced by both processes. The subsurface water masses that supply nutrients to the surface ocean are depleted in Zn. Indeed, the Southern Ocean water masses play a driving role, but remarkably, also subsurface water masses from northern high‐latitude origin are depleted in Zn. Both northern and southern high‐latitude waters have a relatively high Zn:PO 4 uptake and remineralization ratio, implying it is Zn availability and not only chronic iron limitation that leads to increased Zn uptake in the high‐latitude regions. The limited supply of Zn to the surface Atlantic Ocean can explain the lack of an Atlantic Zn remineralization signal and indicates Zn might play a role in phytoplankton community composition and productivity. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean NIOZ Repository (Royal Netherlands Institute for Sea Research) Antarctic Southern Ocean Global Biogeochemical Cycles 33 1 63 84 |
institution |
Open Polar |
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NIOZ Repository (Royal Netherlands Institute for Sea Research) |
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ftnioz |
language |
English |
description |
Dissolved zinc (Zn) has a nutrient‐type distribution in the ocean that more closely resembles the distribution of silicate (Si) than phosphate (PO 4 ). However, Zn is a trace‐nutrient and mostly present in the organic fraction of phytoplankton rather than the siliceous frustule. It has been suggested the coupling of Zn and Si is caused by the strong depletion of nutrients in the Southern Ocean, possibly combined with scavenging of Zn. Here we assess the distribution of Zn and nutrients along the conduit of southward traveling waters of northern origin and northward traveling waters of Antarctic origin to unravel the influence of various water masses and local biogeochemical processes in the Atlantic Ocean. The distribution of Zn and Si is governed by mixing such that influence of remineralization is barely distinguishable, whereas the distribution of PO 4 is influenced by both processes. The subsurface water masses that supply nutrients to the surface ocean are depleted in Zn. Indeed, the Southern Ocean water masses play a driving role, but remarkably, also subsurface water masses from northern high‐latitude origin are depleted in Zn. Both northern and southern high‐latitude waters have a relatively high Zn:PO 4 uptake and remineralization ratio, implying it is Zn availability and not only chronic iron limitation that leads to increased Zn uptake in the high‐latitude regions. The limited supply of Zn to the surface Atlantic Ocean can explain the lack of an Atlantic Zn remineralization signal and indicates Zn might play a role in phytoplankton community composition and productivity. |
format |
Article in Journal/Newspaper |
author |
Middag, R. de Baar, H.J.W. Bruland, K.W. |
spellingShingle |
Middag, R. de Baar, H.J.W. Bruland, K.W. The relationships between dissolved zinc and major nutrients phosphate and silicate along the GEOTRACES GA02 transect in the west Atlantic Ocean |
author_facet |
Middag, R. de Baar, H.J.W. Bruland, K.W. |
author_sort |
Middag, R. |
title |
The relationships between dissolved zinc and major nutrients phosphate and silicate along the GEOTRACES GA02 transect in the west Atlantic Ocean |
title_short |
The relationships between dissolved zinc and major nutrients phosphate and silicate along the GEOTRACES GA02 transect in the west Atlantic Ocean |
title_full |
The relationships between dissolved zinc and major nutrients phosphate and silicate along the GEOTRACES GA02 transect in the west Atlantic Ocean |
title_fullStr |
The relationships between dissolved zinc and major nutrients phosphate and silicate along the GEOTRACES GA02 transect in the west Atlantic Ocean |
title_full_unstemmed |
The relationships between dissolved zinc and major nutrients phosphate and silicate along the GEOTRACES GA02 transect in the west Atlantic Ocean |
title_sort |
relationships between dissolved zinc and major nutrients phosphate and silicate along the geotraces ga02 transect in the west atlantic ocean |
publishDate |
2019 |
url |
https://www.vliz.be/imisdocs/publications/75/324675.pdf |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_source |
%3Ci%3EGlobal+Biogeochem.+Cycles+33%281%29%3C%2Fi%3E%3A+63-84.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1029%2F2018gb006034%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1029%2F2018gb006034%3C%2Fa%3E |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/000458243500005 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1029/2018gb006034 https://www.vliz.be/imisdocs/publications/75/324675.pdf |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2018gb006034 |
container_title |
Global Biogeochemical Cycles |
container_volume |
33 |
container_issue |
1 |
container_start_page |
63 |
op_container_end_page |
84 |
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1766248053267759104 |