Paleolimnological evidence for the onset and termination of glacial aridity from Lake Tanganyika, Tropical East Africa

Geochemical and sedimentological data in a continuous 60,000-year sediment core record from the Kalya horst region of central Lake Tanganyika provide a detailed history of paleoclimate-mediated weathering and overflow events from upstream Lake Kivu. Univariate (elemental profiles), bivariate (elemen...

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Veröffentlicht in:	Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2007-09, Vol.252 (3), p.405-423
Hauptverfasser:	Felton, Anna A., Russell, James M., Cohen, Andrew S., Baker, Mark E., Chesley, John T., Lezzar, Kiram E., McGlue, Michael M., Pigati, Jeffrey S., Quade, Jay, Curt Stager, J., Tiercelin, Jean Jacques
Format:	Artikel
Sprache:	eng
Schlagworte:	Africa Earth Sciences Freshwater Geochemistry Lake Tanganyika Last Glacial Maximum Late Pleistocene paleoclimate Paleolimnology Rift lakes Sciences of the Universe Stratigraphy
Online-Zugang:	Volltext
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