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tom Vol. 30, Nr 2
125--133
EN
In the field seasons of 1990 to 2008 the Combined Prehistoric Expedition conducted an extensive archaeological, archaeozoological, archaeobotanical and geomorphological field work at more than a hundred sites in the Nabta, Kiseiba, El Kortain, Gebal El Beid, Gebel Ramlah and Berget El Sheb Areas, South Western Desert of Egypt. The research has helped to develop a long chronological sequence of Late Glacial and Holocene climatic changes in the region. The climatic sequence has been supported by more than 300 14C and OSL assays that permitted to place most of the climatic events in a firm chronological frame.
3
Content available remote Stratigraphy, palaeoecology and radiochronology of the site of Całowanie
61%
EN
The site of Całowanie is one of the most important, if not the most important, late Lateglacial and early Holocene sites of the North European Plain. It is a multi-level cultural complex composed of over twenty occupational entities, most of which are sealed by mineral and biogenic deposition. The cultural deposits of the site cover a time span from an early Allerod to a late Boreal or from ca. 11,900 to 8,300 years BP (uncalibrated).
4
Content available remote The Hamburgian settlement at Mirkowice: recent results and research perspectives
61%
EN
In the early 1990s another Hamburgian settlement was discovered in the northern part of the Polish Plain - the most eastern and northern settlement known up to now. The paper discusses initial results of the international research program that was built up around this discovery: (1) stratigraphy and geomorphology of the site; (2) general characteristic of the lithic industry, and (3) faunal remains. The site at Mirkowice creates an exceptional situation for modern environmental studies of the Late Glacial, including reconstruction of plant and animal assemblages of that times and proper correlation of geological and geomorphological processes of the area with the human occupation. Altogether, the Mirkowice project has a research potential to be a benchmark for a modern chronostratigraphy of the Late Glacial in the Lowland.
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