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Stéphanie Desprat

Researcher at University of Bordeaux

Publications -  53
Citations -  3401

Stéphanie Desprat is an academic researcher from University of Bordeaux. The author has contributed to research in topics: Interglacial & Glacial period. The author has an hindex of 26, co-authored 52 publications receiving 2912 citations. Previous affiliations of Stéphanie Desprat include PSL Research University & Woods Hole Oceanographic Institution.

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Consistently dated Atlantic sediment cores over the last 40 thousand years

Claire Waelbroeck, +67 more
- 02 Sep 2019 - 
TL;DR: This is the first set of consistently dated marine sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation and climate changes over vast regions of the Atlantic Ocean.
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Contrasting impacts of Dansgaard-Oeschger events over a western European latitudinal transect modulated by orbital parameters

TL;DR: In this article, the authors focused on latitudinal variability in the forest cover extent and composition of western Europe during the succession of Dansgaard-Oeschger (D-O) and Heinrich (H) events, showing new pollen records for core MD04-2845.
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Present-day and past (last 25000 years) marine pollen signal off western Iberia

TL;DR: In this article, a comparison between modern terrestrial and marine pollen signals in and off western Iberia shows that marine pollen assemblages give an integrated image of the regional vegetation colonising the adjacent continent.
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North-south palaeohydrological contrasts in the central Mediterranean during the Holocene: tentative synthesis and working hypotheses

TL;DR: In this paper, a multi-proxy approach and a strategy combining lacustrine and marine records along a north-south transect were used to reconstruct high-resolution and well-dated palaeohydrological records and to assess their spatial and temporal coherency.
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Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data

TL;DR: In this paper, high-resolution analyses of the ODP Site 976 pollen record show a cooling trend during the Bolling/Allerod period, and two warm episodes bracketing a cooling event that represent a Bolling-Older Dryas- Allerod succession.