XVI INQUA Congress
Paper No. 83-8
Presentation Time: 10:50 AM-11:10 AM


ZIELHOFER, Christoph1, FAUST, Dominik1, MOLDENHAUER, Klaus-Martin2, and BAENA ESCUDERO, Rafael3, (1) Dresden, Germany, christoph.zielhofer@mailbox.tu-dresden.de, (2) Eichstätt, Germany, (3) Sevilla, Spain

In the course of the latest Pleistocene to mid-Holocene, the Medjerda river system in Mediterranean Tunisia shows events of increased flooding and aggradation of relatively coarse overbank deposits. Active geomorphodynamics in river systems do correlate with an aridification of the climate, but not with temperature. The centennial scale latest Pleistocene to mid-Holocene standard profile of the Ghardimaou floodplain (mid-Medjerda river) indicates active fluvial dynamics during 12.4 to 11.8, 6.6 to 6.0 and as of 4.8 ka cal BP. Correlations with secondary palaeoclimatical findings imply global and regional causes of the latest Pleistocene to mid-Holocene climatic development as there are North Atlantic Deep Water formation, fluctuations in Saharan humidity (monsoonal systems) and autochthonous impacts of Mediterranean weather phenomena. Medjerda sediment-archives show a short activity (12.4 to 11.8 ka cal BP) during the Younger Dryas in comparison to other archives of the mid-latitudes.


We would like to thank the Deutsche Forschungsgemeinschaft (DFG) for the financing of this project (FA 239/2-2).


Zielhofer, C., Faust, D., Diaz del Olmo, D. and Baena, R. (2002): Sedimentation and soil formation phases in the Ghardimaou basin (northern Tunisia) during the Holocene. Quaternary International 93-94, 109-125.

Zielhofer, C., Faust, D., Baena Escudero, R., Diaz del Olmo, F., Kadereit, A., Moldenhauer, K.-M. and Porras, A. (submitted): The centennial scale Holocene standard profile of the mid-Medjerda valley (Northern Tunisia). The Holocene

XVI INQUA Congress
General Information for this Meeting
Session No. 83
Were Abrupt Climate Changes at the Last Glacial Termination Globally Synchronous?
Reno Hilton Resort and Conference Center: Reno Ballroom
8:00 AM-12:00 PM, Wednesday, July 30, 2003

Geological Society of America Abstracts with Programs, , p. 222

© Copyright The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.