Teresa Madeyska-Niklewska
Articles
Geographia Polonica (2011) vol. 84, Special Issue Part 1, pp. 81-94 | Full text
doi: https://doi.org/GPol.2011.S1.6
Abstract
The actual state of research on natural aspects of history of prehistoric settlement inthe peri- and meta-Carpathian zones based on investigations of important multilayer Palaeolithicsites is presented. Traces of Palaeolithic people stay, in the form of cultural layers, arefound at sites representing three types of sedimentary environment, i.e. cave (Biśnik cave in theCzęstochowa Upland, Obłazowa cave in the Podhale region), loess (Galich and Yezupil in theGalich Prydnistrov’ia region, Velykyj Glybochok in the Podil’ia region), and travertine (Hôrka-Ondrej and other sites in the Spiš region).Different geological methods were used in investigations of separate site types, and the obtainedresults are complementary and verify one another. Their comparison enables us to obtain multilevelpicture of palaeoenvironmental changes. Correlation of deposit sections in these differenttypes of sites is based on climatically controlled sequences of environmental changes. Chronostratigraphicextents of individual cultural units from selected sites and their correlation arebased on oxygen-isotope stratigraphy. The extents are presented as continuous despite the factthat cultural layers represent mostly traces of short-lasting settlement.Investigations of Palaeolithic sites in the Podil’ia and Prydnistrov’ia regions proved that settlementexisted from the penultimate interglacial to the end of the last glacial (MOIS 7-2). Materialsfrom the Biśnik cave represent similar period but there are premises that Middle Palaeolithicsettlement started earlier.
Keywords: Palaeolithic chronology, cave sites, loess sites, travertine sites, palaeoenvironment, Poland, Ukraine
, Laboratoire de Géologie du Quaternaire de l'Institut de Géologie de l'Académie Polonaise des Sciences
Situation stratigraphique des ensembles micoquo-prondnikiens
Geographia Polonica (1969) vol. 17, pp. 387-393 | Full text
, Laboratoire de Géologie du Quaternaire de l'Institut de Géologie de l'Académie Polonaise des Sciences