Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica
Elemental and carbon isotopic analyses of suspended and sea ice particulate organic matter (POC) from Antarctica show enrichments in $\sp{13}$C unrelated to atmospheric CO$\sb2$ variations. Phytoplankton bloom-related POC from the southwestern Ross Sea during 1992 had a range in $\delta\sp{13}$C of...
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ftriceuniv:oai:scholarship.rice.edu:1911/13991 2023-05-15T13:51:03+02:00 Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica Rogers, Jennifer Carol Dunbar, Robert B. 1995 95 p. application/pdf https://hdl.handle.net/1911/13991 eng eng Rogers, Jennifer Carol. "Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica." (1995) Master’s Thesis, Rice University. https://hdl.handle.net/1911/13991 . https://hdl.handle.net/1911/13991 THESIS GEOL. 1995 ROGERS Biochemistry Thesis Text 1995 ftriceuniv 2022-08-09T20:39:12Z Elemental and carbon isotopic analyses of suspended and sea ice particulate organic matter (POC) from Antarctica show enrichments in $\sp{13}$C unrelated to atmospheric CO$\sb2$ variations. Phytoplankton bloom-related POC from the southwestern Ross Sea during 1992 had a range in $\delta\sp{13}$C of 7$\rm\perthous.\ \delta\sp{13}C\sb{POC}$ collected from pack ice had an 11$\rm\perthous$ range, with highest values found in the Bellingshausen and Amundsen Seas and lower values found in Ross Sea pack ice. Organic matter $\delta\sp{13}$C from phytoplankton blooms in the southwestern Ross Sea is strongly correlated with POC concentration, suggesting high rates of bloom-related CO$\sb2$(aqueous) drawdown that may cause disequilibrium as a result of stable stratification of the upper water column and partial isolation of the surface water CO$\sb2$ pool. Isotopic and organic carbon composition of surface sediments is similar to the upper water column, thus primary isotopic signals are preserved. Surface sediment $\delta\sp{13}$C values are 1 to 3$\rm\perthous$ enriched in $\sp{13}$C relative to surface water POC $\delta\sp{13}$C. Highest isotopic values were found in areas that receive large amounts of phytoplankton bloom detritus. Future downcore carbon isotopic analyses may prove useful as tracers of bloom dynamics and sea ice production. Thesis Antarc* Antarctica Ross Sea Sea ice Rice University: Digital Scholarship Archive Ross Sea |
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Rice University: Digital Scholarship Archive |
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Biochemistry Rogers, Jennifer Carol Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica |
topic_facet |
Biochemistry |
description |
Elemental and carbon isotopic analyses of suspended and sea ice particulate organic matter (POC) from Antarctica show enrichments in $\sp{13}$C unrelated to atmospheric CO$\sb2$ variations. Phytoplankton bloom-related POC from the southwestern Ross Sea during 1992 had a range in $\delta\sp{13}$C of 7$\rm\perthous.\ \delta\sp{13}C\sb{POC}$ collected from pack ice had an 11$\rm\perthous$ range, with highest values found in the Bellingshausen and Amundsen Seas and lower values found in Ross Sea pack ice. Organic matter $\delta\sp{13}$C from phytoplankton blooms in the southwestern Ross Sea is strongly correlated with POC concentration, suggesting high rates of bloom-related CO$\sb2$(aqueous) drawdown that may cause disequilibrium as a result of stable stratification of the upper water column and partial isolation of the surface water CO$\sb2$ pool. Isotopic and organic carbon composition of surface sediments is similar to the upper water column, thus primary isotopic signals are preserved. Surface sediment $\delta\sp{13}$C values are 1 to 3$\rm\perthous$ enriched in $\sp{13}$C relative to surface water POC $\delta\sp{13}$C. Highest isotopic values were found in areas that receive large amounts of phytoplankton bloom detritus. Future downcore carbon isotopic analyses may prove useful as tracers of bloom dynamics and sea ice production. |
author2 |
Dunbar, Robert B. |
format |
Thesis |
author |
Rogers, Jennifer Carol |
author_facet |
Rogers, Jennifer Carol |
author_sort |
Rogers, Jennifer Carol |
title |
Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica |
title_short |
Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica |
title_full |
Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica |
title_fullStr |
Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica |
title_full_unstemmed |
Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica |
title_sort |
carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the ross sea, antarctica |
publishDate |
1995 |
url |
https://hdl.handle.net/1911/13991 |
geographic |
Ross Sea |
geographic_facet |
Ross Sea |
genre |
Antarc* Antarctica Ross Sea Sea ice |
genre_facet |
Antarc* Antarctica Ross Sea Sea ice |
op_relation |
Rogers, Jennifer Carol. "Carbon-13/carbon-12 ratios in surface water and sea ice organic matter-variability and contributions to the sediments of the Ross Sea, Antarctica." (1995) Master’s Thesis, Rice University. https://hdl.handle.net/1911/13991 . https://hdl.handle.net/1911/13991 THESIS GEOL. 1995 ROGERS |
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1766254622584864768 |