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
Main Authors: Yu, Jimin, Elderfield, H, Piotrowski, Alexander
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2015
Subjects:
ion
Online Access:http://hdl.handle.net/1885/65375
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