Benthic foraminiferal B/Ca ratios reflect deep water carbonate saturation state
Top Cited Papers
- 15 June 2007
- journal article
- research article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 258 (1-2) , 73-86
- https://doi.org/10.1016/j.epsl.2007.03.025
Abstract
No abstract availableKeywords
This publication has 73 references indexed in Scilit:
- Lack of a significant temperature influence on the incorporation of Cd into benthic foraminiferal testsGeochemistry, Geophysics, Geosystems, 2004
- Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time seriesPaleoceanography and Paleoclimatology, 2003
- Paired benthic foraminiferal Cd/Ca and Zn/Ca evidence for a greatly increased presence of Southern Ocean Water in the glacial North AtlanticPaleoceanography and Paleoclimatology, 2002
- A dramatic Atlantic dissolution event at the onset of the last glaciationGeochemistry, Geophysics, Geosystems, 2001
- What caused the glacial/interglacial atmospheric pCO2 cycles?Reviews of Geophysics, 2000
- Oceanic pH control on the boron isotopic composition of foraminifera: Evidence from culture experimentsPaleoceanography and Paleoclimatology, 1996
- Variations in Mg/Ca and Sr/Ca ratios of planktonic foraminifera caused by postdepositional dissolution: Evidence of shallow Mg‐dependent dissolutionPaleoceanography and Paleoclimatology, 1996
- Suborbital timescale variability of North Atlantic Deep Water during the past 200,000 yearsPaleoceanography and Paleoclimatology, 1995
- Coordination of Adsorbed Boron: A FTIR Spectroscopic StudyEnvironmental Science & Technology, 1995
- Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the HolocenePaleoceanography and Paleoclimatology, 1988