An open-ocean assessment of alkenone δD as a paleo-salinity proxy

Author:

Gould JessicaORCID,Kienast MarkusORCID,Dowd Michael,Schefuß Enno

Funder

National Sciences and Engineering Research Council of Canada

Government Nova Scotia's Research and Innovation Graduate Scholarship. ES acknowledges funding through

DFG Research Center/Cluster of Excellence “The Ocean in the Earth System”

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference64 articles.

1. Alkenone δ13C as a proxy for past PCO2 in surface waters: results from the late quaternary angola current;Andersen,1999

2. Organic carbon isotopic composition of phytoplankton and sea surface pCO2 reconstructions in the Southern Indian Ocean during the last 50,000 yr;Bentaleb;Org. Geochem.,1996

3. Long-chain alkenones and UK′37 variability along a south-north transect in the Western Pacific Ocean;Bentaleb;Global Planet Change,2002

4. Carbon isotopic composition of the C37:2 alkenone in core top sediments of the South Atlantic Ocean: effects of CO2 and nutrient concentrations;Benthien;Global Biogeochem. Cycl.,2002

5. Consistent fractionation of 13C in nature and in the laboratory: growth-rate effects in some haptophyte algae;Bidigare;Global Biogeochem. Cycl.,1997

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