Deep-water carbonate dissolution in the northern South China Sea during Marine Isotope Stage 3

The production, transportation, deposition, and dissolution of carbonate profoundly form part of the global carbon cycle and affect the amount and distribution of dissolved inorganic carbon (DIC) and alkalinity (ALK), which drive atmospheric CO2 changes during glacial/interglacial cycles. These proc...

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Bibliographic Details
Main Authors: Na Wang, Bao-Qi Huang, He Li
Format: Article
Language:English
Published: SpringerOpen 2016-01-01
Series:Journal of Palaeogeography
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2095383615300493