Posted on:
August 6, 2021
Last updated on:
August 3, 2022
Authors: Veerle Rots, Justin Coppe, Nicholas J. Conard
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string(2383) "The MGfU is an internationally recognized, peer-review, open-access journal for Early Prehistory, Quaternary Ecology and Human Evolution that has served the research community and the 500 members of the Society for Prehistory (GfU: Gesellschaft für Urgeschichte ) since 1994. The MGfU is a leading European journal for Paleolithic Archaeology and presents studies in Global Prehistory, while highlighting ongoing research in Central Europe and supporting the work of the Museum of Prehistory in Blaubeuren . The journal is a cooperative project of the University of Tübingen and Kerns Verlag | Kerns Publishing.
Older issues: MGfU Reports #1-28 are available via the GFU website.
Please direct any questions to N.J. Conard, M. Bolus or a member of the editorial board.
Editor-in-Chief
Nicholas J. Conard
Editor
Michael Bolus
Editorial Board
Shara Bailey (New York)
François Bon (Toulouse)
Ariane Burke (Montreal)
Katja Douze (Geneva)
Clive Gamble (London)
Sabine GaudzinskiWindheuser (Mainz)
Katerina Harvati (Tübingen)
JeanJacques Hublin (Leipzig)
Robert L. Kelly (Laramie, Wyoming)
Johannes Krause (Leipzig/Tübingen)
Steven L. Kuhn (Tucson)
Foni Le BrunRicalens (Luxemburg)
Feng Li (Beijing)
Christopher E. Miller (Tübingen)
Philip Nigst (Vienna)
Akira Ono (Tokyo)
Marco Peresani (Ferrara)
Guillaume Porraz (AixenProvence)
Jürgen Richter (Köln)
Simone Riehl (Tübingen)
Florent Rivals (Tarragona)
Wil Roebroeks (Leiden)
Veerle Rots (Liège)
Britt M. Starkovich (Tübingen)
Thorsten Uthmeier (Erlangen)
Pawel ValdeNowak (Krakow)
Lyn Wadley (Johannesburg)"
["post_title"]=>
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with contributions in English and German "
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Published in: Mitteilungen der Gesellschaft für Urgeschichte, Vol. 30
During the 2020 season at Hohle Fels Cave in the Ach Valley of southwestern Germany the excavation team from the University of Tübingen recovered a bifacial leaf point in archaeological horizon (AH) X. This horizon is the fifth deepest of the Middle Paleolithic horizons at the site and is located roughly 120 cm beneath the base of the rich Aurignacian layers of the cave.