Sinking phytoplankton associated with carbon flux in the Atlantic Ocean

Author:

Durkin Colleen A.1,Van Mooy Benjamin A. S.1,Dyhrman Sonya T.2,Buesseler Ken O.1

Affiliation:

1. Marine Chemistry and Geochemistry; Woods Hole Oceanographic Institution; Woods Hole Massachusetts

2. Department of Earth and Environmental Science; Lamont-Doherty Earth Observatory, Columbia University; Palisades New York

Publisher

Wiley

Subject

Aquatic Science,Oceanography

Reference62 articles.

1. Role of slowly settling particles in the ocean carbon cycle;Alonso-González;Geophys. Res. Lett.,2010

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

3. Sinking rate response to depletion of nitrate, phosphate and silicate in four marine diatoms;Bienfang;Mar. Biol.,1982

4. Does planktonic community structure determine downward particulate organic carbon flux in different oceanic provinces? Deep-Sea Res. Part Oceanogr;Boyd;Res. Pap.,1999

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