Seawater carbonate ion-d13C systematics and application to glacial-interglacial North Atlantic ocean circulation
Seawater carbonate ion and δ13C are affected by many processes including biology, air-sea exchange, alkalinity change, and mixing between different water masses. Study of modern ocean data shows that deep ocean carbonate ion and δ13C of dissolved inorga
Published in: | Earth and Planetary Science Letters |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/65375 https://doi.org/10.1016/j.epsl.2008.04.010 https://openresearch-repository.anu.edu.au/bitstream/1885/65375/5/Yu_J_2008_Seawater_carbonate.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/65375/7/01_Yu_Seawater_carbonate_ion-d13C_2008.pdf.jpg |
Summary: | Seawater carbonate ion and δ13C are affected by many processes including biology, air-sea exchange, alkalinity change, and mixing between different water masses. Study of modern ocean data shows that deep ocean carbonate ion and δ13C of dissolved inorga |
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