Radiocarbon age offsets of foraminifera resulting from differential dissolution and fragmentation within the sedimentary bioturbated zone
Author:
Affiliation:
1. School of Earth, Ocean and Planetary Sciences; Cardiff University; Cardiff UK
2. Lamont-Doherty Earth Observatory of Columbia University; Palisades New York USA
3. AMS 14C Laboratory; IPP ETH Hoenggerberg; Zurich Switzerland
Publisher
American Geophysical Union (AGU)
Subject
Paleontology,Oceanography
Reference29 articles.
1. Changing atmospheric Δ14C and the record of deep water paleoventilation ages;Adkins;Paleoceanography,1997
2. Glacial-interglacial stability of ocean pH inferred from foraminifer dissolution rates;Anderson;Nature,2002
3. The impact of bioturbation on AMS 14C dates on handpicked foraminifera: A statistical model;Andrée;Radiocarbon,1987
4. Reconstruction of the last deglaciation: Deconvolved records of δ18O profiles, micropaleontological variations and accelerator mass spectrometric 14C dating;Bard;Clim. Dyn.,1987
5. Foraminiferal calcification response to glacial-interglacial changes in atmospheric CO2;Barker;Science,2002
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