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This long-lived lake provided an attractive site for animals and early humans hunting them. Artefacts be-

came embedded on the delta plain and were preserved during lake-level rise. During the Saalian glaciation

the remnant tunnel valley was completely lled with meltwater deposits and subsequently overlain by sub-

glacial till. The deposition of the Middle Pleistocene sediments within an Elsterian tunnel valley explains the

unique preservation of the sedimentary succession of Schöningen.

References:

Lang, J., Winsemann, J., Steinmetz, D., Polom, U., Pollok, L., Böhner, U., Serangeli, J., Brandes, C., Hampel,

A. & Winghart, S. (in press): The Pleistocene of Schöningen, Germany: a complex tunnel valley ll

revealed from 3D subsurface modelling and shear wave seismics. Quaternary Science Reviews.

✉ 1) Institut für Geologie, Leibniz Universität Hannover, Callinstraße 30, 30167 Hannover

2) Leibniz Institut für Angewandte Geophysik (LIAG), Stilleweg 2, 30655 Hannover

3) Niedersächsisches Landesamt für Denkmalpege, Scharnhorststraße 1, 30175 Hannover

Institut für Ur- und Frühgeschichte, Eberhardt Karls Universität Tübingen, Burgsteige 11, 72070 Tübingen

Natalia Leonova

, Sergey Nesmeyanov

, Ekaterina Vinogradova

, Olga Voeykova

Upper Paleolithic subsistence practices on the South of the Russian Plane (the reconstruction of

hilly paleolandscapes and settlement system of Kamennaya Balka sites)

Reconstructions of subsistence practice include the living sites, places of regular daily visits, frequent one-

day trips for hunting and gathering, distant hunting expeditions with using short-lived camps and must be

accompanied by series of additional reconstructions with different scales and goals.

Hilly landscapes are the most favorable territories for inhabitancy of the Upperpaleolithic people. There are

many possibilities for the choice of convenient places for base-camps and temporary camps. The region of

the Kamennaya Balka is typical for the Upper Neo-Pleistocene of the whole northern part of the Azov Sea

Area. The time of existence of the kamennobalkovskaya culture was very long – from 21-22 000 to

12-13 000 BP, that testify to the stable cultural adaptations these people to natural life of this area. The

combination of various and complete paleoecological and archeological data is the basement for construct-

ing of the models of subsistence practices in any period of the inhabitance on the sites.

The study of the spreading of the sites of Kamennaya Balka permits to suggest the following model of the

region settlement: basic-site located on the quite high board of the ravine (the height over bed-river paleo

Don were 60-70 m at 22 000 BP, 50-60 m – 15 000 BP, 40-50 m – 12-1300 BP) with several small „satellites“

not far from it – hunting and gathering camps situated on the surrounded territory.

The archaeological researches of the cultural layers permit us to say about complexity of the base-site planning

including the manufacturing zones and living places with easy ground- dwellings. At the site Kamennaya Balka

II we nd 5 simultaneous living places, so it means that there were about 50 residents. According to the rich-

ness of cultural layer, compose of planning, quantity and composition of faunal remains we may say about

rather settled and stable inhabitance in this area. This research is supported by RFBR grant 10-06-00479a.

✉

Lomonosov Moscow State University, Faculty of History, Department of Archaeology, GSP-1, Lomonosovsky

Prospekt, 27-4. Moscow, 119991, Russia. Fax: +7(495) 939-23-90

Institut of Geoecology RAS, Ulansky per., 13-2. Ab.145. Moscow, 101000, Russia. Fax: +7(495) 623-18-86

Carmen Liebermann

Virgin lands? Problems and chances of archaeology in the Upper Lusatian mining district (Saxony,

Germany)

The poster gives a short overview of archaeological investigations in the northern part of Upper Lusatia,

Germany. The area is situated at the northern part of the UNESCO biosphere reserve „Oberlausitzer

Heide- und Teichlandschaft“ and the southern part of the „Muskauer Heide“ one of the vastest areas with

inland dunes in Germany. Here, the coal-mining district is situated with currently two mines – Nochten and

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