G
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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Journal ArticleDOI
Changes in Caribbean surface hydrography during the Pliocene shoaling of the Central American Seaway
Silke Steph,Ralf Tiedemann,Matthias Prange,Jeroen Groeneveld,Dirk Nürnberg,Lars Reuning,Michael Schulz,Gerald H. Haug +7 more
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
Lukas Glur,Stefanie B. Wirth,Ulf Büntgen,Ulf Büntgen,Adrian Gilli,Gerald H. Haug,Christoph Schär,Jürg Beer,Flavio S. Anselmetti,Flavio S. Anselmetti +9 more
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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Antarctic Zone nutrient conditions during the last two glacial cycles
Anja S Studer,Anja S Studer,Daniel M. Sigman,Alfredo Martínez-García,Verena Benz,Gisela Winckler,Gisela Winckler,Gerhard Kuhn,Oliver Esper,Frank Lamy,Samuel L Jaccard,Lukas Wacker,Sergey Oleynik,Rainer Gersonde,Gerald H. Haug +14 more
TL;DR: In a sediment core from the Pacific sector of the Antarctic Zone (AZ) of the Southern Ocean, the authors report diatom-bound N isotope (δ15Ndb) records for total recoverable diatoms and two distinct diatom assemblages (pennate and centric rich).
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Deglacial pulses of deep-ocean silicate into the subtropical North Atlantic Ocean
Anna Nele Meckler,Daniel M. Sigman,Kelly A Gibson,Roger Francois,Alfredo Martínez-García,Samuel L Jaccard,Ursula Röhl,Larry C. Peterson,Ralf Tiedemann,Gerald H. Haug +9 more
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.