Detecting Holocene changes in thermohaline circulation
- 15 February 2000
- journal article
- research article
- Published by Proceedings of the National Academy of Sciences in Proceedings of the National Academy of Sciences
- Vol. 97 (4) , 1343-1346
- https://doi.org/10.1073/pnas.97.4.1343
Abstract
Throughout the last glacial cycle, reorganizations of deep ocean water masses were coincident with rapid millennial-scale changes in climate. Climate changes have been less severe during the present interglacial, but evidence for concurrent deep ocean circulation change is ambiguous.Keywords
This publication has 31 references indexed in Scilit:
- Surface and deep ocean variability in the northern Sargasso Sea during marine isotope stage 3Paleoceanography and Paleoclimatology, 1999
- Influence of sea ice on the thermohaline circulation in the Arctic‐North Atlantic OceanGeophysical Research Letters, 1997
- Thermohaline instability in the North Atlantic during meltwater events: Stable isotope and ice‐rafted detritus records from Core SO75‐26KL, Portuguese MarginPaleoceanography and Paleoclimatology, 1997
- Multidecadal climate variability in the Greenland Sea and surrounding regions: A coupled model simulationGeophysical Research Letters, 1997
- Synchronous, high‐frequency oscillations in tropical sea surface temperatures and North Atlantic Deep Water production during the Last Glacial CyclePaleoceanography and Paleoclimatology, 1997
- Suborbital timescale variability of North Atlantic Deep Water during the past 200,000 yearsPaleoceanography and Paleoclimatology, 1995
- Evidence of a dissolution effect on benthic foraminiferal shell chemistry: δ13C, Cd/Ca, Ba/Ca, and Sr/Ca results from the Ontong Java PlateauPaleoceanography and Paleoclimatology, 1995
- Changes in East Atlantic Deepwater Circulation over the last 30,000 years: Eight time slice reconstructionsPaleoceanography and Paleoclimatology, 1994
- The δ13C in benthic foraminiferal tests of Fontbotia wuellerstorfi (Schwager) Relative to the δ13C of dissolved inorganic carbon in Southern Ocean Deep Water: Implications for glacial ocean circulation modelsPaleoceanography and Paleoclimatology, 1993
- Benthic foraminiferal δ13C and accumulation rates of organic carbon: Uvigerina Peregrina group and Cibicidoides WuellerstorfiPaleoceanography and Paleoclimatology, 1986