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The history of cladiummariscus (l.) Pohl. In the "Klocie Ostrowieckie" reserve (Drawieński National Park). Part I

Gałka M., Tobolski K.

Studia Quaternaria

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2011

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Vol. 28

53-59

EN

The objective of the paleoecological studies undertaken in the "Klocie Ostrowieckie" reserve was mainly to reconstruct the subfossil mire vegetation at a local and regional scale. This article presents the results of palynological and plant macroremain analyses of this site, and belongs to the first published studies of such a type, made in the Drawieński National Park. Based on our studies, five phases in the history of the mire development were determined. The most pronounced feature of that history, was a decline of Cladietum marisci clearly concurrent with a strong yet puzzling expansion of pine stands occurring approximately 1000 years ago.

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The Hamburgian settlement at Mirkowice: recent results and research perspectives

Kabaciński J., Bratlund B., Kubiak L., Makowiecki D., Schild R., Tobolski K.

Folia Quaternaria

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1999

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nr 70

211-238

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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Stratigraphy, palaeoecology and radiochronology of the site of Całowanie

Schild R., Tobolski K., Kubiak-Martens L., Pazdur M. F., Pazdur A., Vogel J. C., Stafford T. W. jr

Folia Quaternaria

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1999

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nr 70

239-268

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).