extended abstracts - Geomorphic Processes and Geoarchaeology
extended abstracts - Geomorphic Processes and Geoarchaeology
extended abstracts - Geomorphic Processes and Geoarchaeology
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<strong>Geomorphic</strong> processes <strong>and</strong> geoarchaeology<br />
6. Ralska-Jasiewiczowa, M., Starkel, L. 1999. Zmiany klimatu i stosunków<br />
wodnych w holocenie. In: Geografia Polski. Środowisko przyrodnicze (Ed.) L. Starkel.<br />
PWN. Warszawa, P. 175-180 (in Polish).<br />
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Zamhöfer, S., Bork, H.R. 2005. Phases of gully erosion in The Kazimierz Dolny Area<br />
(case study: Doły Podmularskie, SE Pol<strong>and</strong>). In: Human Impact on Sensitive<br />
Geosystems. (Ed.) W. Zgłobicki <strong>and</strong> J. Rejman. Maria Curie-Skłodowska University<br />
Press, P. 121-128.<br />
PALAEOECOLOGY OF MIDDLE – LATE PALAEOLITHIC KABAZI II SITE<br />
(WESTERN CRIMEA) BY THE DATA OF SMALL MAMMALS<br />
Markova A.K.<br />
Institute of Geography, RAS, Moscow, Russia,<br />
nature@online.ru<br />
Unique multilayered open Middle – Late Palaeolithic site Kabazi II is situated on<br />
the third ridge of the Crimean Mountains. Dr. Victor Chabai investigated the archeology<br />
of the site <strong>and</strong> organized the complex study of the deposits of this monument, which<br />
includes six archeological Units with many levels [1, 2, 3]. Humans occupied the site<br />
during the long period (from Mikulino = Eemian Interglacial till the second part of Valdai<br />
Glaciation). This duration was established by archaeological materials <strong>and</strong> by the results<br />
of a number of dating methods (radiocarbon, U-series <strong>and</strong> ESR). The duration of human<br />
occupation was longed about 90 000 yr. (5-2 MIS) <strong>and</strong> covered the epochs with different<br />
climatic conditions.<br />
Material. Rich materials of small mammal remains were collected during 2000-<br />
2001 yrs. Small mammal remains were recovered from VI, V, IV, <strong>and</strong> III archaeological<br />
Units with a help of screening <strong>and</strong> washing of the deposits of these strata. All the<br />
archaeological Units include the number of levels. The saturation of the bones in the<br />
deposits is rather high. About two thous<strong>and</strong> of bones have been collected. The 911 bones<br />
were identified on the special level. According complex archeological, palynological <strong>and</strong><br />
geochronological data, all small mammal materials from Units VI-IV correspond to the<br />
different stages of Mikulino Interglacial. The materials from Unit III it seems correspond<br />
to one of early interstadials of Valdai glaciations [3, 5].<br />
Results. The analysis of rich bone materials of small mammals from Units VI, V,<br />
IV, <strong>and</strong> III of Kabazi II site indicates the following main features of environments during<br />
their deposition. The open steppe-like l<strong>and</strong>scapes prevailed during formation these<br />
archaeological units. The majority of small mammals identified from the site are the<br />
typical habitants of open environments. Some changing in nature could be fixated by the<br />
small mammal materials of Kabazi II. The mammal remains, found in Units VI <strong>and</strong> V,<br />
shows on more moderate <strong>and</strong> humid climate, than in later layers (fig. 1). Some forested or<br />
bushed areas were presented near the site during these temporal intervals, what was<br />
indicated by the finds of forest species. Later, during the deposition of Units IV-III, only<br />
steppe, semi-desert, meadow steppe, <strong>and</strong> few hydrogenous mammals inhabited the<br />
environments near the site.<br />
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