Regulation of Algal Blooms in Antarctic Shelf Waters by the Release of Iron From Melting Sea Ice
During summer 1995-96, we measured iron in the water column and conducted iron-enrichment bottle-incubation experiments at a station in the central Ross Sea (76°30'S, 170°40'W), first, in the presence of melting sea ice, and 17 days later, in ice-free conditions. We observed a striking tem...
Published in: | Geophysical Research Letters |
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ODU Digital Commons
1997
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ftolddominionuni:oai:digitalcommons.odu.edu:oeas_fac_pubs-1102 2023-06-11T04:07:05+02:00 Regulation of Algal Blooms in Antarctic Shelf Waters by the Release of Iron From Melting Sea Ice Sedwick, Peter N. DiTullio, Giacomo R. 1997-01-01T08:00:00Z application/pdf https://digitalcommons.odu.edu/oeas_fac_pubs/93 https://doi.org/10.1029/97GL02596 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1102/viewcontent/Sedwick_1997_Regulation_of_algal_blooms_in_Ant.pdf unknown ODU Digital Commons https://digitalcommons.odu.edu/oeas_fac_pubs/93 doi:10.1029/97GL02596 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1102/viewcontent/Sedwick_1997_Regulation_of_algal_blooms_in_Ant.pdf OES Faculty Publications Iron Ross Sea Algal bloom Diatom Sea ice Phytoplankton Ice-edge blooms Antarctic Manganese Biogeochemistry Marine Biology Oceanography article 1997 ftolddominionuni https://doi.org/10.1029/97GL02596 2023-05-08T17:59:38Z During summer 1995-96, we measured iron in the water column and conducted iron-enrichment bottle-incubation experiments at a station in the central Ross Sea (76°30'S, 170°40'W), first, in the presence of melting sea ice, and 17 days later, in ice-free conditions. We observed a striking temporal change in mixed-layer dissolved iron concentrations at this station, from 0.72-2.3 nM with sea ice present, to 0.16-0.17 nM in ice-free conditions. These changes were accompanied doubling of algal (diatom) biomass. Our incubation experiments suggest that conditions were iron-replete in the presence of sea ice, and iron-deficient in the absence of sea ice. We surmise that bioavailability iron was released into seawater from the melting sea ice, stimulating phytoplankton production and the biological removal of dissolved iron from the mixed layer, until iron-limited conditions developed. These observations suggest that the episodic release of bio-available iron from melting sea ice is an important factor regulating phytoplankton production, particularly ice-edge blooms, in seasonally ice-covered Antarctic waters. Article in Journal/Newspaper Antarc* Antarctic Ross Sea Sea ice Old Dominion University: ODU Digital Commons Antarctic Ross Sea Geophysical Research Letters 24 20 2515 2518 |
institution |
Open Polar |
collection |
Old Dominion University: ODU Digital Commons |
op_collection_id |
ftolddominionuni |
language |
unknown |
topic |
Iron Ross Sea Algal bloom Diatom Sea ice Phytoplankton Ice-edge blooms Antarctic Manganese Biogeochemistry Marine Biology Oceanography |
spellingShingle |
Iron Ross Sea Algal bloom Diatom Sea ice Phytoplankton Ice-edge blooms Antarctic Manganese Biogeochemistry Marine Biology Oceanography Sedwick, Peter N. DiTullio, Giacomo R. Regulation of Algal Blooms in Antarctic Shelf Waters by the Release of Iron From Melting Sea Ice |
topic_facet |
Iron Ross Sea Algal bloom Diatom Sea ice Phytoplankton Ice-edge blooms Antarctic Manganese Biogeochemistry Marine Biology Oceanography |
description |
During summer 1995-96, we measured iron in the water column and conducted iron-enrichment bottle-incubation experiments at a station in the central Ross Sea (76°30'S, 170°40'W), first, in the presence of melting sea ice, and 17 days later, in ice-free conditions. We observed a striking temporal change in mixed-layer dissolved iron concentrations at this station, from 0.72-2.3 nM with sea ice present, to 0.16-0.17 nM in ice-free conditions. These changes were accompanied doubling of algal (diatom) biomass. Our incubation experiments suggest that conditions were iron-replete in the presence of sea ice, and iron-deficient in the absence of sea ice. We surmise that bioavailability iron was released into seawater from the melting sea ice, stimulating phytoplankton production and the biological removal of dissolved iron from the mixed layer, until iron-limited conditions developed. These observations suggest that the episodic release of bio-available iron from melting sea ice is an important factor regulating phytoplankton production, particularly ice-edge blooms, in seasonally ice-covered Antarctic waters. |
format |
Article in Journal/Newspaper |
author |
Sedwick, Peter N. DiTullio, Giacomo R. |
author_facet |
Sedwick, Peter N. DiTullio, Giacomo R. |
author_sort |
Sedwick, Peter N. |
title |
Regulation of Algal Blooms in Antarctic Shelf Waters by the Release of Iron From Melting Sea Ice |
title_short |
Regulation of Algal Blooms in Antarctic Shelf Waters by the Release of Iron From Melting Sea Ice |
title_full |
Regulation of Algal Blooms in Antarctic Shelf Waters by the Release of Iron From Melting Sea Ice |
title_fullStr |
Regulation of Algal Blooms in Antarctic Shelf Waters by the Release of Iron From Melting Sea Ice |
title_full_unstemmed |
Regulation of Algal Blooms in Antarctic Shelf Waters by the Release of Iron From Melting Sea Ice |
title_sort |
regulation of algal blooms in antarctic shelf waters by the release of iron from melting sea ice |
publisher |
ODU Digital Commons |
publishDate |
1997 |
url |
https://digitalcommons.odu.edu/oeas_fac_pubs/93 https://doi.org/10.1029/97GL02596 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1102/viewcontent/Sedwick_1997_Regulation_of_algal_blooms_in_Ant.pdf |
geographic |
Antarctic Ross Sea |
geographic_facet |
Antarctic Ross Sea |
genre |
Antarc* Antarctic Ross Sea Sea ice |
genre_facet |
Antarc* Antarctic Ross Sea Sea ice |
op_source |
OES Faculty Publications |
op_relation |
https://digitalcommons.odu.edu/oeas_fac_pubs/93 doi:10.1029/97GL02596 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1102/viewcontent/Sedwick_1997_Regulation_of_algal_blooms_in_Ant.pdf |
op_doi |
https://doi.org/10.1029/97GL02596 |
container_title |
Geophysical Research Letters |
container_volume |
24 |
container_issue |
20 |
container_start_page |
2515 |
op_container_end_page |
2518 |
_version_ |
1768379678258626560 |