A switch from Si(OH) 4 to NO 3 - depletion in the glacial Southern Ocean

[1] Phytoplankton in the Antarctic deplete silicic acid (Si(OH)4) to a far greater extent than they do nitrate (NO3 ). This pattern can be reversed by the addition of iron which dramatically lowers diatom Si(OH)4:NO3 uptake ratios. Higher iron supply during glacial times would thus drive the Antarct...

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Bibliographic Details
Main Authors: Mark A. Brzezinski, Carol J. Pride, Valerie M. Franck, Daniel M. Sigman, Jorge L. Sarmiento, Katsumi Matsumoto, Nicolas Gruber, Greg H. Rau, Kenneth H. Coale
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2002
Subjects:
Paleoceanography
4215 Oceanography
General
Climate and
Antarctic
Southern Ocean
The Antarctic
Antarc*
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.5265
http://www.up.ethz.ch/people/ngruber/publications/brzezinski_grl_02.pdf
Description
Summary:[1] Phytoplankton in the Antarctic deplete silicic acid (Si(OH)4) to a far greater extent than they do nitrate (NO3 ). This pattern can be reversed by the addition of iron which dramatically lowers diatom Si(OH)4:NO3 uptake ratios. Higher iron supply during glacial times would thus drive the Antarctic towards NO3 depletion with excess Si(OH)4 remaining in surface waters. New d 30Si and d15N records from Antarctic sediments confirm diminished Si(OH)4 use and enhanced NO3 depletion during the last three glaciations. The present low-Si(OH)4 water is transported northward to at least the subtropics. We postulate that the glacial high-Si(OH)4 water similarly may have been transported to the subtropics and beyond. This input of Si(OH)4 may have caused diatoms to displace coccolithophores at low latitudes, weakening the carbonate pump and increasing the depth of organic matter remineralization. These effects may have lowered glacial atmospheric pCO2 by as

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