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
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
2015
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/65375 |
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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