Silicic acid dynamics in the glacial sub-Antarctic: Implications for the silicic acid leakage hypothesis-Reference-Cited by-同舟云学术

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Silicic acid dynamics in the glacial sub-Antarctic: Implications for the silicic acid leakage hypothesis

Published:2007-08-29 Issue:3 Volume:21 Page:n/a-n/a
ISSN:0886-6236
Container-title:Global Biogeochemical Cycles
language:en
Short-container-title:Global Biogeochem. Cycles

Author:

Beucher Charlotte P.¹,Brzezinski Mark A.²,Crosta Xavier³

Affiliation:

1. Marine Science Institute; University of California; Santa Barbara; California; USA

2. Department of Ecology Evolution and Marine Biology and Marine Science Institute; University of California; Santa Barbara; California; USA

3. UMR-CNRS 5805 EPOC; Université Bordeaux I; Talence; France

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Reference54 articles.

1. Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilization;Altabet;Global Biogeochem. Cycles,1994

2. Atmospheric dust under glacial and interglacial conditions;Andersen;Geophys. Res. Lett.,1998

3. The Southern Ocean's biological pump during the Last Glacial Maximum;Anderson;Deep Sea Res., Part II,2002

4. Southern Ocean fronts from the Greenwich meridian to Tasmania;Belkin;J. Geophys. Res.,1996

5. Control of phytoplankton growth by iron supply and irradiance in the subantarctic Southern Ocean: Experimental results from the SAZ project;Boyd;J. Geophys. Res.,2001

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