Calibration and application of B/Ca, Cd/Ca, and δ 11 B in Neogloboquadrina pachyderma (sinistral) to constrain CO 2 uptake in the subpolar North Atlantic during the last deglaciation
The North Atlantic and Norwegian Sea are prominent sinks of atmospheric CO2 today, but their roles in the past remain poorly constrained. In this study, we attempt to use B/Ca and δ11B ratios in the planktonic foraminifera Neogloboquadrina pachyderma (si
Published in: | Paleoceanography |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/74453 https://doi.org/10.1002/palo.20024 https://openresearch-repository.anu.edu.au/bitstream/1885/74453/5/f5625xPUB4132_2013.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/74453/7/01_Yu_Calibration_and_application_of_2013.pdf.jpg |
Summary: | The North Atlantic and Norwegian Sea are prominent sinks of atmospheric CO2 today, but their roles in the past remain poorly constrained. In this study, we attempt to use B/Ca and δ11B ratios in the planktonic foraminifera Neogloboquadrina pachyderma (si |
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