Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean
Abstract The size partitioning of dissolved iron (dFe, <0.4 lm) into soluble (sFe, <0.02 lm) and colloidal (0.02 lm < cFe < 0.4 lm) phases was investigated at seven stations in the tropical North Atlantic Ocean, and the results are compared to the dFe size fractionation study of [sFe] =...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1048.1850 2023-05-15T13:51:35+02:00 Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean Jessica N Fitzsimmons Edward A Boyle The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.1850 http://boyle.mit.edu/%7Eed/pdfs/Fitzsimmons%282013%29GCA_125_539.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.1850 http://boyle.mit.edu/%7Eed/pdfs/Fitzsimmons%282013%29GCA_125_539.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://boyle.mit.edu/%7Eed/pdfs/Fitzsimmons%282013%29GCA_125_539.pdf text ftciteseerx 2020-04-05T00:22:31Z Abstract The size partitioning of dissolved iron (dFe, <0.4 lm) into soluble (sFe, <0.02 lm) and colloidal (0.02 lm < cFe < 0.4 lm) phases was investigated at seven stations in the tropical North Atlantic Ocean, and the results are compared to the dFe size fractionation study of [sFe] = 0.42 ± 0.03 nmol/kg) and in the oxygen minimum zone (56% sFe; [sFe] = 0.65 ± 0.03 nmol/kg). Only at remineralization depths of stations with intermediate oxygen concentrations (100-110 lmol/kg) did colloidal Fe dominate (contributing 58% of dFe) , indicating that cFe may be serving as a conduit of dFe loss during mixing of high-Fe OMZ and low-Fe gyre waters. North Atlantic Deep Water (NADW) had a typical sFe concentration of 0.34 ± 0.05 nmol/kg. In the deepest samples composed of a NADW/Antarctic Bottom Water mixture where the bottom water may have attained a $0.1 nmol/kg hydrothermal Fe input during transit past the Mid-Atlantic Ridge, sFe did not increase coincidentally with dFe, indicating that any potential hydrothermal Fe contribution was colloidal. In general, the results of this study counter the previous hypothesis of Text Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic Unknown Antarctic Mid-Atlantic Ridge |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
description |
Abstract The size partitioning of dissolved iron (dFe, <0.4 lm) into soluble (sFe, <0.02 lm) and colloidal (0.02 lm < cFe < 0.4 lm) phases was investigated at seven stations in the tropical North Atlantic Ocean, and the results are compared to the dFe size fractionation study of [sFe] = 0.42 ± 0.03 nmol/kg) and in the oxygen minimum zone (56% sFe; [sFe] = 0.65 ± 0.03 nmol/kg). Only at remineralization depths of stations with intermediate oxygen concentrations (100-110 lmol/kg) did colloidal Fe dominate (contributing 58% of dFe) , indicating that cFe may be serving as a conduit of dFe loss during mixing of high-Fe OMZ and low-Fe gyre waters. North Atlantic Deep Water (NADW) had a typical sFe concentration of 0.34 ± 0.05 nmol/kg. In the deepest samples composed of a NADW/Antarctic Bottom Water mixture where the bottom water may have attained a $0.1 nmol/kg hydrothermal Fe input during transit past the Mid-Atlantic Ridge, sFe did not increase coincidentally with dFe, indicating that any potential hydrothermal Fe contribution was colloidal. In general, the results of this study counter the previous hypothesis of |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Jessica N Fitzsimmons Edward A Boyle |
spellingShingle |
Jessica N Fitzsimmons Edward A Boyle Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean |
author_facet |
Jessica N Fitzsimmons Edward A Boyle |
author_sort |
Jessica N Fitzsimmons |
title |
Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean |
title_short |
Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean |
title_full |
Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean |
title_fullStr |
Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean |
title_full_unstemmed |
Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean |
title_sort |
both soluble and colloidal iron phases control dissolved iron variability in the tropical north atlantic ocean |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.1850 http://boyle.mit.edu/%7Eed/pdfs/Fitzsimmons%282013%29GCA_125_539.pdf |
geographic |
Antarctic Mid-Atlantic Ridge |
geographic_facet |
Antarctic Mid-Atlantic Ridge |
genre |
Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic |
genre_facet |
Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic |
op_source |
http://boyle.mit.edu/%7Eed/pdfs/Fitzsimmons%282013%29GCA_125_539.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.1850 http://boyle.mit.edu/%7Eed/pdfs/Fitzsimmons%282013%29GCA_125_539.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766255551077941248 |