Sodium-Calcium Ratios in the Planktic Foraminifera Trilobatus Sacculifer as a Proxy for Sea Surface Salinity
Recent culture and field studies have found a significant positive correlation between seawater salinity and the incorporation of sodium into foraminiferal calcite, suggesting a potential new proxy for reconstructing past changes in sea surface salinity (SSS) (Mezger et al., 2016 and Bertlich et al....
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ftdatacite:10.25777/f7xb-yg22 2023-05-15T17:34:58+02:00 Sodium-Calcium Ratios in the Planktic Foraminifera Trilobatus Sacculifer as a Proxy for Sea Surface Salinity Watkins, Colton Steele 2020 https://dx.doi.org/10.25777/f7xb-yg22 https://digitalcommons.odu.edu/oeas_etds/176/ unknown Old Dominion University Libraries Text Thesis article-journal ScholarlyArticle 2020 ftdatacite https://doi.org/10.25777/f7xb-yg22 2021-11-05T12:55:41Z Recent culture and field studies have found a significant positive correlation between seawater salinity and the incorporation of sodium into foraminiferal calcite, suggesting a potential new proxy for reconstructing past changes in sea surface salinity (SSS) (Mezger et al., 2016 and Bertlich et al., 2018). In order to test the applicability of this new proxy in an open-ocean setting, Na/Ca ratios in the planktic foraminifera Trilobatus sacculifer (T. sacculifer Na/Ca) were measured from a suite of sediment core tops spanning a natural salinity gradient from the North Atlantic subtropical gyre to the South Atlantic subtropical gyre. Initial results from nine core tops spanning a salinity range of 1.6 show a positive correlation between upper water column salinity and T. sacculifer Na/Ca (R2 = 0.81, p < 0.005). The data also suggest there is no relationship between T. sacculifer Na/Ca and shell weight, shell size, or habitat temperature, indicating that shell Na/Ca may be predominantly controlled by salinity. In addition, we generated a high-resolution downcore record of T. sacculifer Na/Ca variability over the last deglaciation from Florida Straits core JPC26. Results show good agreement between our new Na/Ca record with the previously published deglacial δ18Osw record that is also thought to reflect SSS variability from the same core (Schmidt and Lynch-Stieglitz, 2011). Both records indicate an abrupt increase in SSS during the Younger Dryas (11.7 – 12.9 kyr). Converting our new JPC26 T. sacculifer Na/Ca ratios to SSS using our Atlantic core top calibration indicates a maximum salinity change of ~2.2 across the last deglaciation. Thesis North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Lynch ENVELOPE(-57.683,-57.683,-63.783,-63.783) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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Recent culture and field studies have found a significant positive correlation between seawater salinity and the incorporation of sodium into foraminiferal calcite, suggesting a potential new proxy for reconstructing past changes in sea surface salinity (SSS) (Mezger et al., 2016 and Bertlich et al., 2018). In order to test the applicability of this new proxy in an open-ocean setting, Na/Ca ratios in the planktic foraminifera Trilobatus sacculifer (T. sacculifer Na/Ca) were measured from a suite of sediment core tops spanning a natural salinity gradient from the North Atlantic subtropical gyre to the South Atlantic subtropical gyre. Initial results from nine core tops spanning a salinity range of 1.6 show a positive correlation between upper water column salinity and T. sacculifer Na/Ca (R2 = 0.81, p < 0.005). The data also suggest there is no relationship between T. sacculifer Na/Ca and shell weight, shell size, or habitat temperature, indicating that shell Na/Ca may be predominantly controlled by salinity. In addition, we generated a high-resolution downcore record of T. sacculifer Na/Ca variability over the last deglaciation from Florida Straits core JPC26. Results show good agreement between our new Na/Ca record with the previously published deglacial δ18Osw record that is also thought to reflect SSS variability from the same core (Schmidt and Lynch-Stieglitz, 2011). Both records indicate an abrupt increase in SSS during the Younger Dryas (11.7 – 12.9 kyr). Converting our new JPC26 T. sacculifer Na/Ca ratios to SSS using our Atlantic core top calibration indicates a maximum salinity change of ~2.2 across the last deglaciation. |
format |
Thesis |
author |
Watkins, Colton Steele |
spellingShingle |
Watkins, Colton Steele Sodium-Calcium Ratios in the Planktic Foraminifera Trilobatus Sacculifer as a Proxy for Sea Surface Salinity |
author_facet |
Watkins, Colton Steele |
author_sort |
Watkins, Colton Steele |
title |
Sodium-Calcium Ratios in the Planktic Foraminifera Trilobatus Sacculifer as a Proxy for Sea Surface Salinity |
title_short |
Sodium-Calcium Ratios in the Planktic Foraminifera Trilobatus Sacculifer as a Proxy for Sea Surface Salinity |
title_full |
Sodium-Calcium Ratios in the Planktic Foraminifera Trilobatus Sacculifer as a Proxy for Sea Surface Salinity |
title_fullStr |
Sodium-Calcium Ratios in the Planktic Foraminifera Trilobatus Sacculifer as a Proxy for Sea Surface Salinity |
title_full_unstemmed |
Sodium-Calcium Ratios in the Planktic Foraminifera Trilobatus Sacculifer as a Proxy for Sea Surface Salinity |
title_sort |
sodium-calcium ratios in the planktic foraminifera trilobatus sacculifer as a proxy for sea surface salinity |
publisher |
Old Dominion University Libraries |
publishDate |
2020 |
url |
https://dx.doi.org/10.25777/f7xb-yg22 https://digitalcommons.odu.edu/oeas_etds/176/ |
long_lat |
ENVELOPE(-57.683,-57.683,-63.783,-63.783) |
geographic |
Lynch |
geographic_facet |
Lynch |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_doi |
https://doi.org/10.25777/f7xb-yg22 |
_version_ |
1766133968742121472 |