Silicic acid leakage from the Southern Ocean as a possible mechanism for explaining glacial atmospheric pCO 2, Global Biogeochem

[1] Using a simple box model, we investigate the effects of a reduced Si:N uptake ratio by Antarctic phytoplankton on the marine silica cycle and atmospheric pCO2. Recent incubation experiments demonstrate such a phenomenon in diatoms when iron is added [Hutchins and Bruland, 1998; Takeda, 1998; Fra...

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Bibliographic Details
Main Authors: Katsumi Matsumoto, Jorge L. Sarmiento, Mark A. Brzezinski
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.144.3413
http://www.gfdl.noaa.gov/reference/bibliography/2002/knm0201.pdf