A 425 kyr record of foraminiferal shell weight variability in the western equatorial Pacific
Author:
Affiliation:
1. School of Pure and Applied Chemistry; University of Natal; Durban South Africa
2. Department of Earth Sciences; University of Cambridge; Cambridge UK
Publisher
American Geophysical Union (AGU)
Subject
Paleontology,Oceanography
Reference18 articles.
1. Foraminiferal calcification response to glacial-interglacial changes in atmospheric CO2;Barker;Science,2002
2. Foraminiferal ooze: Solution at depth;Berger;Science,1967
3. Planktonic foraminifera: Selective solution and paleoclimatic interpretation;Berger;Deep Sea Res.,1968
4. Preservation of Foraminifera
5. An evaluation of Lohmann's foraminifera-weight dissolution index;Broecker;Paleoceanography,2001
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1. Decrease in volume and density of foraminiferal shells with progressing ocean acidification;Scientific Reports;2021-10-07
2. Evidence of supra-lysoclinal dissolution of pelagic calcium carbonate in the late Quaternary in the western South Atlantic;Marine Micropaleontology;2021-06
3. Latitudinal Variation of Planktonic Foraminifera Shell Masses During Termination I;IOP Conference Series: Earth and Environmental Science;2019-03-01
4. Influence of surface ocean density on planktonic foraminifera calcification;Scientific Reports;2019-01-24
5. Perspective on the response of marine calcifiers to global warming and ocean acidification—Behavior of corals and foraminifera in a high CO2 world “hot house”;Progress in Earth and Planetary Science;2019-01-17
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