Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing
Low levels of iron limit primary productivity across much of the Southern Ocean. At the basin scale, most dissolved iron issupplied to surface waters from subsurface reservoirs, because land inputs are spatially limited. Deep mixing in winter togetherwith year-round diffusion across density surfaces...
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Online Access: | https://doi.org/10.1038/ng.2554 https://doi.org/10.1038/NGEO2101 http://ecite.utas.edu.au/90755 |
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ftunivtasecite:oai:ecite.utas.edu.au:90755 2023-05-15T13:42:40+02:00 Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing Tagliabue, A Sallee, JB Bowie, AR Levy, M Swart, S Boyd, PW 2014 https://doi.org/10.1038/ng.2554 https://doi.org/10.1038/NGEO2101 http://ecite.utas.edu.au/90755 en eng Nature Publishing Group http://dx.doi.org/10.1038/NGEO2101 Tagliabue, A and Sallee, JB and Bowie, AR and Levy, M and Swart, S and Boyd, PW, Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing, Nature Geoscience, 7, (4) pp. 314-320. ISSN 1752-0894 (2014) [Refereed Article] http://ecite.utas.edu.au/90755 Earth Sciences Oceanography Chemical oceanography Refereed Article PeerReviewed 2014 ftunivtasecite https://doi.org/10.1038/ng.2554 https://doi.org/10.1038/NGEO2101 2022-09-05T22:16:43Z Low levels of iron limit primary productivity across much of the Southern Ocean. At the basin scale, most dissolved iron issupplied to surface waters from subsurface reservoirs, because land inputs are spatially limited. Deep mixing in winter togetherwith year-round diffusion across density surfaces, known as diapycnal diffusion, are the main physical processes that carryiron-laden subsurface waters to the surface. Here, we analyse data on dissolved iron concentrations in the top 1,000 m of theSouthern Ocean, taken from all known and available cruises to date, together with hydrographic data to determine the relativeimportance of deep winter mixing and diapycnal diffusion to dissolved iron fluxes at the basin scale. Using information onthe vertical distribution of iron we show that deep winter mixing supplies ten times more iron to the surface ocean eachyear, on average, than diapycnal diffusion. Biological observations from the sub-Antarctic sector suggest that following thedepletion of this wintertime iron pulse, intense iron recycling sustains productivity over the subsequent spring and summer.We conclude that winter mixing and surface-water iron recycling are important drivers of temporal variations in SouthernOcean primary production. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean eCite UTAS (University of Tasmania) Antarctic Southern Ocean Nature Genetics 45 3 314 318 |
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eCite UTAS (University of Tasmania) |
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ftunivtasecite |
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topic |
Earth Sciences Oceanography Chemical oceanography |
spellingShingle |
Earth Sciences Oceanography Chemical oceanography Tagliabue, A Sallee, JB Bowie, AR Levy, M Swart, S Boyd, PW Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing |
topic_facet |
Earth Sciences Oceanography Chemical oceanography |
description |
Low levels of iron limit primary productivity across much of the Southern Ocean. At the basin scale, most dissolved iron issupplied to surface waters from subsurface reservoirs, because land inputs are spatially limited. Deep mixing in winter togetherwith year-round diffusion across density surfaces, known as diapycnal diffusion, are the main physical processes that carryiron-laden subsurface waters to the surface. Here, we analyse data on dissolved iron concentrations in the top 1,000 m of theSouthern Ocean, taken from all known and available cruises to date, together with hydrographic data to determine the relativeimportance of deep winter mixing and diapycnal diffusion to dissolved iron fluxes at the basin scale. Using information onthe vertical distribution of iron we show that deep winter mixing supplies ten times more iron to the surface ocean eachyear, on average, than diapycnal diffusion. Biological observations from the sub-Antarctic sector suggest that following thedepletion of this wintertime iron pulse, intense iron recycling sustains productivity over the subsequent spring and summer.We conclude that winter mixing and surface-water iron recycling are important drivers of temporal variations in SouthernOcean primary production. |
format |
Article in Journal/Newspaper |
author |
Tagliabue, A Sallee, JB Bowie, AR Levy, M Swart, S Boyd, PW |
author_facet |
Tagliabue, A Sallee, JB Bowie, AR Levy, M Swart, S Boyd, PW |
author_sort |
Tagliabue, A |
title |
Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing |
title_short |
Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing |
title_full |
Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing |
title_fullStr |
Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing |
title_full_unstemmed |
Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing |
title_sort |
surface-water iron supplies in the southern ocean sustained by deep winter mixing |
publisher |
Nature Publishing Group |
publishDate |
2014 |
url |
https://doi.org/10.1038/ng.2554 https://doi.org/10.1038/NGEO2101 http://ecite.utas.edu.au/90755 |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_relation |
http://dx.doi.org/10.1038/NGEO2101 Tagliabue, A and Sallee, JB and Bowie, AR and Levy, M and Swart, S and Boyd, PW, Surface-water iron supplies in the Southern Ocean sustained by deep winter mixing, Nature Geoscience, 7, (4) pp. 314-320. ISSN 1752-0894 (2014) [Refereed Article] http://ecite.utas.edu.au/90755 |
op_doi |
https://doi.org/10.1038/ng.2554 https://doi.org/10.1038/NGEO2101 |
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Nature Genetics |
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45 |
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3 |
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314 |
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318 |
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1766171337811820544 |