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E. Michel

Researcher at Centre national de la recherche scientifique

Publications -  24
Citations -  1351

E. Michel is an academic researcher from Centre national de la recherche scientifique. The author has contributed to research in topics: Glacial period & Thermohaline circulation. The author has an hindex of 16, co-authored 24 publications receiving 1239 citations.

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Evidence for changes in the North Atlantic Deep Water linked to meltwater surges during the Heinrich events

TL;DR: In this paper, high resolution benthic δ 18 O and δ 13 C records from North Atlantic sediment cores were used to monitor the impact of Heinrich events on thermohaline circulation and to estimate the sensitivity of deep oceanic circulation to changes in freshwater input to the North Atlantic surface waters.
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Changes in the vertical structure of the North Atlantic Ocean between glacial and modern times

TL;DR: In this paper, temperature/salinity/density diagrams of the water column have been constructed using plancktic and benthic foraminifera δ18O values together with sea surface temperature estimates obtained by using micropaleontological transfer functions.
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Hydrographic changes of the Southern Ocean (southeast Indian Sector) Over the last 230 kyr

TL;DR: In this article, the oxygen and carbon isotopic composition of planktonic (N. pachyderma sinistra and G. bulloides) and benthic (Cibicidoides wuellerstorfi, Epistominella exigua, and Melonis barleeanum) foraminifera have been analysed.
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Quantifying the roles of ocean circulation and biogeochemistry in governing ocean carbon-13 and atmospheric carbon dioxide at the last glacial maximum

TL;DR: The authors examined the impact of changes in ocean circulation and biogeochemistry in governing the change in ocean carbon-13 and atmospheric CO2 at the last glacial maximum (LGM).
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Climate variability across the last deglaciation in NW Iberia and its margin

TL;DR: In this paper, a comparison between marine and terrestrial data from the NW Iberian margin, core MD03-2697, allows us to accurately evaluate, without chronological ambiguity, the vegetation response to North Atlantic climate events across the last deglaciation.