Shell weights from the South Atlantic

Geochemistry, Geophysics, Geosystems

Volumn 5, Issue 3, 2004, Pages

  Broecker, W S ^a   Clark, Elizabeth ^a  

^a Doherty Earth Observatory of Columbia University   (United States)

Author keywords

Foraminifera; Shell weights

Indexed keywords

EID: 71749087876     PISSN: 15252027     EISSN: 15252027     Source Type: Journal    
DOI: 10.1029/2003GC000625     Document Type: Article

References (9)

1. 2, Science, 297, 833-836.
2. Broecker, W. S., E. Clark, D. C. McCorkle, T.-H. Peng, I. Hajdas, and G. Bonani (1999), Evidence for a reduction in the carbonate ion content of the deep sea during the course of the Holocene, Paleoceanography, 14, 744-752.
3. Broecker, W. S., and E. Clark (2001), An evaluation of Lohmann's foraminifera-weight dissolution index, Paleoceanography, 16, 531-534.
4. Charles, C. D., and J. J. Morley (1988), The paleoceanographic significance of the radiolarian Didymocyrtis Tetrathalamus in Eastern Cape Basin sediments, Palaeogeo. Palaeoclim. Palaeoeco., 66, 113-126.
5. 2 and pH, Global Biogeochem. Cycles, 10, 527-541.
6. 2(aq), Geochim. Cosmochim. Acta, 61, 501-514.
7. Lohmann, G. P. (1995), A model for variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolution, Paleoceanography, 10, 445-457.
8. Schulte, S., and E. Bard (2003), Past changes in biologically mediated dissolution of calcite above the chemical lysocline recorded in Indian Ocean sediments, Quaternary Sci. Rev., 22, 1757-1770.
9. Wenzhöfer, F., M. Adler, O. Kohls, C. Hensen, B. Strotmann, S. Boehme, and H. D. Schulz (2001), Calcite dissolution driven by benthic mineralization in the deep-sea: In situ measurements, Geochim. Cosmochim. Acta, 65, 2677-2690.