Fisher (2004a), Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX), Limnol

During the Southern Ocean Iron Experiment (SOFeX), we analyzed Si, P, S, Mn, Ni, and Zn in individual diatoms, autotrophic flagellates, and heterotrophic flagellates with synchrotron-based X-ray fluorescence (SXRF) and calcu-lated cellular C from measurements of cell size. Element stoichiometries fo...

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Main Authors: Benjamin S. Twining, Stephen B. Baines, Nicholas S. Fisher
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.4262
http://www.aslo.org/lo/toc/vol_49/issue_6/2115.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.532.4262 2023-05-15T18:25:08+02:00 Fisher (2004a), Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX), Limnol Benjamin S. Twining Stephen B. Baines Nicholas S. Fisher The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.4262 http://www.aslo.org/lo/toc/vol_49/issue_6/2115.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.4262 http://www.aslo.org/lo/toc/vol_49/issue_6/2115.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aslo.org/lo/toc/vol_49/issue_6/2115.pdf text ftciteseerx 2016-01-08T10:40:15Z During the Southern Ocean Iron Experiment (SOFeX), we analyzed Si, P, S, Mn, Ni, and Zn in individual diatoms, autotrophic flagellates, and heterotrophic flagellates with synchrotron-based X-ray fluorescence (SXRF) and calcu-lated cellular C from measurements of cell size. Element stoichiometries for the different types of protists (nor-malized to either C, S, or P) were generally in good agreement with prior bulk analyses of natural assemblages but also revealed previously undocumented differences in elemental composition among cell types. Flagellated cells contained 39 % more P than diatoms, which in turn contained 79 % more Mn, 3-fold more Ni, and 2.6-fold more Zn than flagellates. Heterotroph cells contained approximately 40 % more P and twice as much Zn as autotrophs. Manganese and Ni stoichiometries were negatively related to cell volume, while larger cells contained more Zn per mole C. Iron fertilization resulted in an approximate doubling of Mn, Ni, and Zn quotas and smaller increases in cellular P, but the timing of the stoichiometric changes varied between the two patches. Silicon contents of diatoms dropped approximately 40 % after the first Fe addition but returned to prefertilization levels as cellular P doubled following the second addition, resulting in 40 % lower Si: P ratios in the fertilized waters. The mean elemental stoichiometries calculated for all cells analyzed were comparable with previously published extended Redfield ratios for mixed plankton assemblages, but the observed differences between diatoms and flagellates and between auto- Text Southern Ocean Unknown Southern Ocean
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language English
description During the Southern Ocean Iron Experiment (SOFeX), we analyzed Si, P, S, Mn, Ni, and Zn in individual diatoms, autotrophic flagellates, and heterotrophic flagellates with synchrotron-based X-ray fluorescence (SXRF) and calcu-lated cellular C from measurements of cell size. Element stoichiometries for the different types of protists (nor-malized to either C, S, or P) were generally in good agreement with prior bulk analyses of natural assemblages but also revealed previously undocumented differences in elemental composition among cell types. Flagellated cells contained 39 % more P than diatoms, which in turn contained 79 % more Mn, 3-fold more Ni, and 2.6-fold more Zn than flagellates. Heterotroph cells contained approximately 40 % more P and twice as much Zn as autotrophs. Manganese and Ni stoichiometries were negatively related to cell volume, while larger cells contained more Zn per mole C. Iron fertilization resulted in an approximate doubling of Mn, Ni, and Zn quotas and smaller increases in cellular P, but the timing of the stoichiometric changes varied between the two patches. Silicon contents of diatoms dropped approximately 40 % after the first Fe addition but returned to prefertilization levels as cellular P doubled following the second addition, resulting in 40 % lower Si: P ratios in the fertilized waters. The mean elemental stoichiometries calculated for all cells analyzed were comparable with previously published extended Redfield ratios for mixed plankton assemblages, but the observed differences between diatoms and flagellates and between auto-
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Benjamin S. Twining
Stephen B. Baines
Nicholas S. Fisher
spellingShingle Benjamin S. Twining
Stephen B. Baines
Nicholas S. Fisher
Fisher (2004a), Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX), Limnol
author_facet Benjamin S. Twining
Stephen B. Baines
Nicholas S. Fisher
author_sort Benjamin S. Twining
title Fisher (2004a), Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX), Limnol
title_short Fisher (2004a), Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX), Limnol
title_full Fisher (2004a), Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX), Limnol
title_fullStr Fisher (2004a), Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX), Limnol
title_full_unstemmed Fisher (2004a), Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX), Limnol
title_sort fisher (2004a), element stoichiometries of individual plankton cells collected during the southern ocean iron experiment (sofex), limnol
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.4262
http://www.aslo.org/lo/toc/vol_49/issue_6/2115.pdf
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source http://www.aslo.org/lo/toc/vol_49/issue_6/2115.pdf
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http://www.aslo.org/lo/toc/vol_49/issue_6/2115.pdf
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