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

Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Yu, Jimin, Elderfield, H, Piotrowski, Alexander
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Keywords: Carbonate ions
Charged particles
Seawater
Electrons
benthic foraminifera
calcite
carbon dioxide
carbon sequestration
carbonate system
glacial-interglacial cycle
inorganic carbon
ion
Last Glacial
oceanic circulation
tracer
water co d13C
benthic foraminiferal B/Ca
carbonate ion concentration
North Atlantic
ocean circulation
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
Description
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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