The influence of salinity on Mg/Ca in planktic foraminifers - Evidence from cultures, core-top sediments and complementary δ 18 O
The Mg/Ca ratio in foraminiferal calcite is one of the principal proxies used for paleoceanographic temperature reconstructions, but recent core-top sediment observations suggest that salinity may exert a significant secondary control on planktic foramini
Published in: | Geochimica et Cosmochimica Acta |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Pergamon-Elsevier Ltd
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/74153 https://doi.org/10.1016/j.gca.2013.07.028 https://openresearch-repository.anu.edu.au/bitstream/1885/74153/5/f5625xPUB3990_2013.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/74153/7/01_H%C3%B6nisch_The_influence_of_salinity_on_2013.pdf.jpg |
Summary: | The Mg/Ca ratio in foraminiferal calcite is one of the principal proxies used for paleoceanographic temperature reconstructions, but recent core-top sediment observations suggest that salinity may exert a significant secondary control on planktic foramini |
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