His primary areas of study are Oceanography, Glacial period, Climatology, Last Glacial Maximum and Foraminifera. His Oceanography research includes themes of Subtropics and Quaternary. A large part of his Glacial period studies is devoted to Interglacial.
His research in Last Glacial Maximum intersects with topics in Climate change and Ocean gyre. His Foraminifera research is multidisciplinary, incorporating elements of Alkenone, Paleontology, Relative species abundance and Paleothermometer. The study incorporates disciplines such as Deep sea, Sediment and Plankton in addition to Sea surface temperature.
Sediment core, Oceanography, Hydrology, Foraminifera and Geochemistry are his primary areas of study. His Sediment core research includes elements of Environmental chemistry, Soil science, Mineralogy and Globigerinoides. His Oceanography study combines topics from a wide range of disciplines, such as Glacial period, Paleontology and Climatology.
His study ties his expertise on Climate change together with the subject of Glacial period. Uwe Pflaumann has researched Foraminifera in several fields, including Sediment and Plankton. His Last Glacial Maximum study deals with Ice sheet intersecting with Younger Dryas and Meltwater.
His primary areas of investigation include Sediment core, Foraminifera, Oceanography, Surface and Mineralogy. His Sediment core study integrates concerns from other disciplines, such as Hydrology, Geochemistry and Pollen. His study in the field of Plankton also crosses realms of Census.
In his research on the topic of Plankton, Sea surface temperature, Holocene, Fauna and Globigerina bulloides is strongly related with Sediment. His Sea surface temperature research incorporates themes from Glacial period, Last Glacial Maximum, Geomorphology and Climate change. His Interglacial study in the realm of Paleontology interacts with subjects such as δ18O and δ13C.
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Molecular stratigraphy: a new tool for climatic assessment
S. C. Brassell;G. Eglinton;I. T. Marlowe;U. Pflaumann.
East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the south China Sea
L. Wang;M. Sarnthein;H. Erlenkeuser;JO Grimalt.
Marine Geology (1999)
Glacial and interglacial wind regimes over the eastern subtropical Atlantic and North-West Africa
M. Sarnthein;G. Tetzlaff;B. Koopmann;K. Wolter.
Atmospheric and Oceanic Circulation Patterns off Northwest Africa During the Past 25 Million Years
Michael Sarnthein;Jörn Thiede;Uwe Pflaumann;H. Erlenkeuser.
Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum
C. Waelbroeck;A. Paul;M. Kucera;A. Rosell-Melé.
Nature Geoscience (2009)
Holocene variability of the Kuroshio Current in the Okinawa Trough, northwestern Pacific Ocean
Zhimin Jian;Zhimin Jian;Pinxian Wang;Yoshiki Saito;Jiliang Wang.
Earth and Planetary Science Letters (2000)
SIMMAX : a modern analog technique to deduce Atlantic Sea Surface Temperatures from planktonic foraminifera in deep sea sediments
Uwe Pflaumann;Josette Duprat;Claude Pujol;Laurent D. Labeyrie.
Glacial North Atlantic: Sea-surface conditions reconstructed by GLAMAP 2000
U. Pflaumann;M. Sarnthein;M. Chapman;L. d'Abreu.
Potential links between surging ice sheets, circulation changes, and the Dansgaard-Oeschger cycles in the Irminger Sea, 60-18 kyr
S van Kreveld;M Sarnthein;H Erlenkeuser;P Grootes.
Reconstruction of sea-surface temperatures from assemblages of planktonic foraminifera: multi-technique approach based on geographically constrained calibration data sets and its application to glacial Atlantic and Pacific Oceans
Michal Kucera;Mara Weinelt;Thorsten Kiefer;Uwe Pflaumann.
Quaternary Science Reviews (2005)
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