Mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off South Georgia, Southern Ocean
<jats:p>Abstract. The island of South Georgia is situated in the iron (Fe)-depleted Antarctic Circumpolar Current of the Southern Ocean. Iron emanating from its shelf system fuels large phytoplankton blooms downstream of the island, but the actual supply mechanisms are unclear. To address this...
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Copernicus GmbH
2018
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Online Access: | http://hdl.handle.net/10026.1/15842 https://doi.org/10.5194/bg-15-4973-2018 |
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ftunivplympearl:oai:pearl.plymouth.ac.uk:10026.1/15842 2024-06-09T07:40:06+00:00 Mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off South Georgia, Southern Ocean Schlosser, C Schmidt, K Aquilina, A Homoky, WB Castrillejo, M Mills, RA Patey, MD Fielding, S Atkinson, A Achterberg, EP 2018-08-22 4973-4993 application/pdf http://hdl.handle.net/10026.1/15842 https://doi.org/10.5194/bg-15-4973-2018 en eng Copernicus GmbH ISSN:1726-4170 ISSN:1726-4189 E-ISSN:1726-4189 1726-4170 1726-4189 http://hdl.handle.net/10026.1/15842 doi:10.5194/bg-15-4973-2018 2020-7-18 Not known 3708 Oceanography 37 Earth Sciences 3701 Atmospheric Sciences 3703 Geochemistry 3705 Geology journal-article 2018 ftunivplympearl https://doi.org/10.5194/bg-15-4973-2018 2024-05-14T23:46:24Z <jats:p>Abstract. The island of South Georgia is situated in the iron (Fe)-depleted Antarctic Circumpolar Current of the Southern Ocean. Iron emanating from its shelf system fuels large phytoplankton blooms downstream of the island, but the actual supply mechanisms are unclear. To address this, we present an inventory of Fe, manganese (Mn), and aluminium (Al) in shelf sediments, pore waters, and the water column in the vicinity of South Georgia, alongside data on zooplankton-mediated Fe cycling processes, and provide estimates of the relative dissolved Fe (DFe) fluxes from these sources. Seafloor sediments, modified by authigenic Fe precipitation, were the main particulate Fe source to shelf bottom waters as indicated by the similar Fe ∕ Mn and Fe ∕ Al ratios for shelf sediments and suspended particles in the water column. Less than 1 % of the total particulate Fe pool was leachable surface-adsorbed (labile) Fe and therefore potentially available to organisms. Pore waters formed the primary DFe source to shelf bottom waters, supplying 0.1–44 µmol DFe m−2 d−1. However, we estimate that only 0.41±0.26 µmol DFe m−2 d−1 was transferred to the surface mixed layer by vertical diffusive and advective mixing. Other trace metal sources to surface waters included glacial flour released by melting glaciers and via zooplankton egestion and excretion processes. On average 6.5±8.2 µmol m−2 d−1 of labile particulate Fe was supplied to the surface mixed layer via faecal pellets formed by Antarctic krill (Euphausia superba), with a further 1.1±2.2 µmol DFe m−2 d−1 released directly by the krill. The faecal pellets released by krill included seafloor-derived lithogenic and authigenic material and settled algal debris, in addition to freshly ingested suspended phytoplankton cells. The Fe requirement of the phytoplankton blooms ∼ 1250 km downstream of South Georgia was estimated as 0.33±0.11 µmol m−2 d−1, with the DFe supply by horizontal/vertical mixing, deep winter mixing, and aeolian dust estimated as ∼0.12 µmol m−2 d−1. ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Krill Euphausia superba Southern Ocean PEARL (Plymouth Electronic Archiv & ResearchLibrary, Plymouth University) Antarctic Southern Ocean Biogeosciences 15 16 4973 4993 |
institution |
Open Polar |
collection |
PEARL (Plymouth Electronic Archiv & ResearchLibrary, Plymouth University) |
op_collection_id |
ftunivplympearl |
language |
English |
topic |
3708 Oceanography 37 Earth Sciences 3701 Atmospheric Sciences 3703 Geochemistry 3705 Geology |
spellingShingle |
3708 Oceanography 37 Earth Sciences 3701 Atmospheric Sciences 3703 Geochemistry 3705 Geology Schlosser, C Schmidt, K Aquilina, A Homoky, WB Castrillejo, M Mills, RA Patey, MD Fielding, S Atkinson, A Achterberg, EP Mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off South Georgia, Southern Ocean |
topic_facet |
3708 Oceanography 37 Earth Sciences 3701 Atmospheric Sciences 3703 Geochemistry 3705 Geology |
description |
<jats:p>Abstract. The island of South Georgia is situated in the iron (Fe)-depleted Antarctic Circumpolar Current of the Southern Ocean. Iron emanating from its shelf system fuels large phytoplankton blooms downstream of the island, but the actual supply mechanisms are unclear. To address this, we present an inventory of Fe, manganese (Mn), and aluminium (Al) in shelf sediments, pore waters, and the water column in the vicinity of South Georgia, alongside data on zooplankton-mediated Fe cycling processes, and provide estimates of the relative dissolved Fe (DFe) fluxes from these sources. Seafloor sediments, modified by authigenic Fe precipitation, were the main particulate Fe source to shelf bottom waters as indicated by the similar Fe ∕ Mn and Fe ∕ Al ratios for shelf sediments and suspended particles in the water column. Less than 1 % of the total particulate Fe pool was leachable surface-adsorbed (labile) Fe and therefore potentially available to organisms. Pore waters formed the primary DFe source to shelf bottom waters, supplying 0.1–44 µmol DFe m−2 d−1. However, we estimate that only 0.41±0.26 µmol DFe m−2 d−1 was transferred to the surface mixed layer by vertical diffusive and advective mixing. Other trace metal sources to surface waters included glacial flour released by melting glaciers and via zooplankton egestion and excretion processes. On average 6.5±8.2 µmol m−2 d−1 of labile particulate Fe was supplied to the surface mixed layer via faecal pellets formed by Antarctic krill (Euphausia superba), with a further 1.1±2.2 µmol DFe m−2 d−1 released directly by the krill. The faecal pellets released by krill included seafloor-derived lithogenic and authigenic material and settled algal debris, in addition to freshly ingested suspended phytoplankton cells. The Fe requirement of the phytoplankton blooms ∼ 1250 km downstream of South Georgia was estimated as 0.33±0.11 µmol m−2 d−1, with the DFe supply by horizontal/vertical mixing, deep winter mixing, and aeolian dust estimated as ∼0.12 µmol m−2 d−1. ... |
format |
Article in Journal/Newspaper |
author |
Schlosser, C Schmidt, K Aquilina, A Homoky, WB Castrillejo, M Mills, RA Patey, MD Fielding, S Atkinson, A Achterberg, EP |
author_facet |
Schlosser, C Schmidt, K Aquilina, A Homoky, WB Castrillejo, M Mills, RA Patey, MD Fielding, S Atkinson, A Achterberg, EP |
author_sort |
Schlosser, C |
title |
Mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off South Georgia, Southern Ocean |
title_short |
Mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off South Georgia, Southern Ocean |
title_full |
Mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off South Georgia, Southern Ocean |
title_fullStr |
Mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off South Georgia, Southern Ocean |
title_full_unstemmed |
Mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off South Georgia, Southern Ocean |
title_sort |
mechanisms of dissolved and labile particulate iron supply to shelf waters and phytoplankton blooms off south georgia, southern ocean |
publisher |
Copernicus GmbH |
publishDate |
2018 |
url |
http://hdl.handle.net/10026.1/15842 https://doi.org/10.5194/bg-15-4973-2018 |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic Antarctic Krill Euphausia superba Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctic Krill Euphausia superba Southern Ocean |
op_relation |
ISSN:1726-4170 ISSN:1726-4189 E-ISSN:1726-4189 1726-4170 1726-4189 http://hdl.handle.net/10026.1/15842 doi:10.5194/bg-15-4973-2018 |
op_rights |
2020-7-18 Not known |
op_doi |
https://doi.org/10.5194/bg-15-4973-2018 |
container_title |
Biogeosciences |
container_volume |
15 |
container_issue |
16 |
container_start_page |
4973 |
op_container_end_page |
4993 |
_version_ |
1801383598062829568 |