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Gerald H. Haug

Researcher at Max Planck Society

Publications -  198
Citations -  20379

Gerald H. Haug is an academic researcher from Max Planck Society. The author has contributed to research in topics: Glacial period & Holocene. The author has an hindex of 60, co-authored 184 publications receiving 17516 citations. Previous affiliations of Gerald H. Haug include ETH Zurich & Woods Hole Oceanographic Institution.

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Changes in Caribbean surface hydrography during the Pliocene shoaling of the Central American Seaway

TL;DR: In this paper, the authors examined pliocene d18O records of shallow and deep dwelling planktonic foraminifers from the Caribbean (Ocean Drilling Program sites 999 and 1000), the tropical east Pacific (sites 1241 and 851), and the Atlantic (site 925, Ceara Rise, and site 1006, western Great Bahama Bank) were used to examine Atlantic-Caribbean-Pacific ecosystem linkages associated with the progressive closure of the Central American Seaway.
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North Atlantic control on precipitation pattern in the eastern Mediterranean/Black Sea region during the last glacial

TL;DR: In this article, the authors present a record of relative changes in precipitation for NW Anatolia based on variations in the terrigenous supply expressed as detrital carbonate concentration.
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Frequent floods in the European Alps coincide with cooler periods of the past 2500 years

TL;DR: A 2500-year long flood reconstruction for the European Alps is presented, based on dated sedimentary flood deposits from ten lakes in Switzerland, and shows that periods with high flood frequency coincide with cool summer temperatures, which suggests enhanced flood occurrence to be triggered by latitudinal shifts of Atlantic and Mediterranean storm tracks.
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Deglacial pulses of deep-ocean silicate into the subtropical North Atlantic Ocean

TL;DR: A record of biogenic opal export from a coastal upwelling system off the coast of northwest Africa that shows pronounced opal maxima during each glacial termination over the past 550,000 years is reported, suggesting an alternative mechanism for the deglacial CO2 release.