| Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004) | |
| Paper No. 26-5 | |
| Presentation Time: 1:00 PM-5:00 PM | ||
PLEISTOCENE CLIMATIC VARIATION IN EUROPE AND THE MEDITERRANEAN DURING NEANDERTHAL OCCUPATION | ||
|
BRADLEY, Dawn M., Department of Geology, Georgia State Univ, 24 Peachtree Center Avenue, Atlanta, GA 30302-4105, dbradley6@student.gsu.edu, CHRISTENSEN, Beth A., Geology, Georgia State Univ, 340 Kell Hall, Atlanta, GA 30303, and WILLIAMS, Frank L., Anthropology, Georgia State Univ, Atlanta, GA 30303 Environmental changes are thought to influence the physical adaptations in mammals, including hominids. We are studying the link between climate change and possible climatically induced morphological responses in a late Pleistocene hominid, the Neanderthals, by relating Neanderthal evolutionary features to coeval changes in habitat. The climate of three separate regions of known Neanderthal habitation in Western Europe, Central Europe and the East Mediterranean are examined for climatic conditions spanning 130,000 to 30,000 years BP. Paleoclimate records (pollen, planktonic foraminifera, biogenic silica, stable isotopes, and biogenic sediments) from both marine and freshwater sediments are used to determine local spatial and temporal variations in Europe (including France, Italy and Hungary) and the Mediterranean. Our study focuses on the comparison of these local changes to regional and global events. Ultimately, we will compare these paleoclimate variations with Neanderthal cranial ontogeny of the same time frame. | ||
|
Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)
General Information for this Meeting | ||
| Session No. 26--Booth# 21 Paleoclimatology/Paleoceanography (Posters) Hilton McLean Tysons Corner: Ballrooms A and B 1:00 PM-5:00 PM, Thursday, March 25, 2004 Geological Society of America Abstracts with Programs, Vol. 36, No. 2, p. 70 | ||
© Copyright 2004 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. | ||