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Rainer Gersonde

Researcher at Alfred Wegener Institute for Polar and Marine Research

Publications -  139
Citations -  8102

Rainer Gersonde is an academic researcher from Alfred Wegener Institute for Polar and Marine Research. The author has contributed to research in topics: Sea ice & Glacial period. The author has an hindex of 50, co-authored 139 publications receiving 7377 citations.

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Sea-surface temperature and sea ice distribution of the Southern Ocean at the EPILOG Last Glacial Maximum—a circum-Antarctic view based on siliceous microfossil records

TL;DR: In this paper, the authors used diatoms and radiolarians to reconstruct the last glacial environment at the EPILOG (19.5 −16.0 −1.0 ǫ) or 23 −000 −19 ǔcal yr.
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Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum

Claire Waelbroeck, +51 more
- 18 Jan 2009 - 
TL;DR: This article presented an updated synthesis of sea surface temperatures during the Last Glacial Maximum, rigorously defined as the period between 23 and 19 thousand years before present, from the Multiproxy Approach for the Reconstruction of the Glacial Ocean Surface (MARGO) project.
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Links between iron supply, marine productivity, sea surface temperature, and CO2 over the last 1.1 Ma

TL;DR: In this article, the authors present a new multiproxy data set of sea surface temperatures (SST), dust and iron supply, and marine export productivity from the marine sediment core PS2489-2/ODP Site 1090 located in the subantarctic Atlantic, that allow them to evaluate various hypotheses on the role of the Southern Ocean (SO) in modulating atmospheric CO2 concentrations back to 11 Ma.
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Diatom distribution in Southern Ocean surface sediments (Atlantic sector): Implications for paleoenvironmental reconstructions

TL;DR: A study of 230 surface sediment samples collected in the Atlantic sector of the Southern Ocean between the southernmost Weddell Sea and the Subtropical Zone documents the modern distribution of diatoms revealing patterns of paleoenvironmental significance as discussed by the authors.
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The reconstruction of late Quaternary Antarctic sea-ice distribution—the use of diatoms as a proxy for sea-ice

TL;DR: In this paper, the authors used time-series sediment traps combined with the mapping of diatom assemblages from surface sediments to define a proxy for past variations of sea-ice extent.