Causes and biogeochemical implications of regional differences in silicification of marine diatoms

Author:

Baines Stephen B.1,Twining Benjamin S.2,Brzezinski Mark A.3,Nelson David M.4,Fisher Nicholas S.5

Affiliation:

1. Department of Ecology and Evolution; Stony Brook University; Stony Brook; New York; USA

2. Bigelow Laboratory for Ocean Sciences; West Boothbay Harbor; Maine; USA

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

4. Institut Universitaire Européen de la Mer; Technopôle Brest-Iroise; Plouzané; France

5. School of Marine and Atmospheric Sciences; Stony Brook University; Stony Brook; New York; USA

Publisher

American Geophysical Union (AGU)

Subject

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

Reference68 articles.

1. A new, mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals;Armstrong;Deep Sea Res., Part II,2002

2. Export flux of carbon at the equator during the EqPac time-series cruises estimated from Th-234 measurements;Bacon;Deep Sea Res., Part II,1996

3. Silicification of eastern equatorial Pacific diatoms exposed to additions of silicic acid and iron;Baines;Deep Sea Res.,2010

4. Regulation of oceanic silicon and carbon preservation by temperature control on bacteria;Bidle;Science,2002

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