Constraints on the ocean oxygen isotopic enrichment between the Last Glacial Maximum and the Holocene: Paleoceanographic implications
- 31 January 2002
- journal article
- Published by Elsevier in Quaternary Science Reviews
- Vol. 21 (1-3) , 315-330
- https://doi.org/10.1016/s0277-3791(01)00107-x
Abstract
No abstract availableKeywords
This publication has 78 references indexed in Scilit:
- “Implicit ice” in the global theory of glacial isostatic adjustmentGeophysical Research Letters, 1998
- Glacial‐age hydrography of the far northwest Pacific OceanPaleoceanography and Paleoclimatology, 1998
- Benthic δ18O records in the North Atlantic over the Last Glacial Period (60–10 kyr): Evidence for brine formationPaleoceanography and Paleoclimatology, 1998
- Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equationsPaleoceanography and Paleoclimatology, 1998
- Paleocean circulation during the Last Deglaciation: A bipolar seesaw?Paleoceanography and Paleoclimatology, 1998
- Rapid changes in surface and deep water conditions at the Faeroe Margin during the last 58,000 yearsPaleoceanography and Paleoclimatology, 1996
- Variations in Atlantic surface ocean paleoceanography, 50°‐80°N: A time‐slice record of the last 30,000 yearsPaleoceanography and Paleoclimatology, 1995
- Determination of δ18O of Seawater in the Deep Ocean during the Last Glacial MaximumPaleoceanography and Paleoclimatology, 1993
- Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulationPaleoceanography and Paleoclimatology, 1988
- Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the HolocenePaleoceanography and Paleoclimatology, 1988