Radiocarbon-age differences among coexisting planktic foraminifera shells: The Barker Effect
Author:
Affiliation:
1. Lamont-Doherty Earth Observatory; Columbia University; Palisades New York USA
Publisher
American Geophysical Union (AGU)
Subject
Paleontology,Oceanography
Link
http://www.agu.org/journals/pa/pa1102/2011PA002116/2011PA002116.pdf
Reference15 articles.
1. Radiocarbon age offsets of foraminifera resulting from differential dissolution and fragmentation within the sedimentary bioturbated zone;Barker;Paleoceanography,2007
2. Planktonic foraminifera: Selective solution and paleoclimatic interpretation;Berger;Deep Sea Res. Oceanogr. Abstr.,1968
3. CaCO3 size distribution: A paleocarbonate ion proxy?;Broecker;Paleoceanography,1999
4. Search for a glacial-age 14C-depleted ocean reservoir;Broecker;Geophys. Res. Lett.,2010
5. Accelerator mass spectrometric radiocarbon measurements on foraminifera shells from deep sea cores;Broecker;Radiocarbon,1990
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