Chemical Hydrography of the South Atlantic During the Last Glacial Maximum: Cd vs. δ13C
- 1 January 1996
- book chapter
- Published by Springer Nature
Abstract
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This publication has 41 references indexed in Scilit:
- Limits on benthic foraminiferal chemical analyses as precise measures of environmental propertiesJournal of Foraminiferal Research, 1995
- A Comparison of Carbon Isotopes and Cadmium in the Modern and Glacial Maximum Ocean: Can We Account for the Discrepancies?Published by Springer Nature ,1994
- Isotopic and Elemental Tracers in Calcium Carbonate FossilsMineralogical Magazine, 1994
- CADMIUM AND δ13C PALEOCHEMICAL OCEAN DISTRIBUTIONS DURING THE STAGE 2 GLACIAL MAXIMUMAnnual Review of Earth and Planetary Sciences, 1992
- Cadmium: Chemical tracer of deepwater paleoceanographyPaleoceanography and Paleoclimatology, 1988
- Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: changes in deep ocean circulation and chemical inventoriesEarth and Planetary Science Letters, 1985
- Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical EvidenceScience, 1982
- On the distribution of copper, nickel, and cadmium in the surface waters of the North Atlantic and North Pacific OceanJournal of Geophysical Research: Oceans, 1981
- Cadmium, zinc, copper, and barium in foraminifera testsEarth and Planetary Science Letters, 1981
- Stable isotope composition of benthic foraminifera from the equatorial PacificNature, 1981