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Landform Analysis
2015 Vol. 29 49--61
EN Loess-soil sequences provide one of the most continuous and detailed records of the climate changes on land areas in the Quaternary. The Late Pleistocene loess section in Dankowice (Niemcza-Strzelin Hills) is one of the best recognized in SW Poland. For the investigation of the chemical composition [...]
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Geochronometria
2000 Vol. 19 7-12
EN Otically stimulated luminescence (OSL) studies on the 14C dated section of the Middle Nemunas (Middle Vistulian) limno-alluvial deposits of the Jiesia river were made. The most deposits from palaeolake with broad, low-gradient floors of Middle Nemunas interstadial in Central Lithuania are inferred t[...]
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Annales Societatis Geologorum Poloniae
2012 Vol. 82, No. 2 177–-191
EN The paper deals with the morphometric analysis of remains of the reindeer Rangifer tarandus Linnaeus, 1758 from 20 Late Pleistocene cave localities in Poland. In most of the localities, the species was the most abundant component of the large mammal fauna; the remains came from individuals, killed b[...]
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Geological Quarterly
EN Successions of loess and other deposits in the Kolodiiv profile, formed during the Eemian Inter glacial and Vistulian Glacial (OIS 5-2), are characterized using the results of heavy mineral analysis. Weathered local carbonate rocks and fluvial deposits (Wartanian Glacial, OIS 6) are used for compari[...]
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Geological Quarterly
EN Detailed geological and palaeobotanical study of about 400 boreholes through Quaternary deposits in eastern Belarus has enabled the recognition of a number of Middle and Late Pleistocene interglacial sites and demonstrated the stratigraphical position of Alexandrian (Holsteinian) and Muravian (Eemia[...]
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Geochronometria
2002 Vol. 21 1-16
EN Optically stimulated luminescence (OSL) dating of light-exposed sediments is used increasingly as a mean of establishing a sediment deposition chronology in a wide variety of late Quaternary studies. There has been considerable technological development in the last few years . in instrumentation, in[...]
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Geochronometria
2015 Vol. 42, no.1 172--181
EN The interglacial deposits in the South Lithuanian Snaigupėlė outcrop and borehole Snaigupėlė-705 are marked for different bedding conditions though the sections are in proximity of each other. In the borehole section, the interglacial deposits are thicker and bedding at a greater depth than the anal[...]
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Studia Quaternaria
2019 Vol. 36, Nr 2 137--145
EN The Vistulian decline was a period of rapid environmental events. The authors correlated ages of the last Scandinavian Ice Sheet limits in northern Poland with ages of prominent events adapting the conditions of periglacial environment of Central Poland in response to the Late Vistulian climate warm[...]
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Geochronometria
2007 Vol. 28 55-59
EN The River Rega valley near Łobez was formed by a rapid icesheet degradation. Evolution of valleys of rivers (including the Rega) discharging into the Baltic Sea began in late Plenivistulian; it was then that glacifluvial outwash levels and kame terraces were formed. At that time, the water was flowi[...]
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Geological Quarterly
EN This paper summarizes geochemical and palaeopedological investigations of the Upper Pleistocene loess-palaeosol sequences at the Kolodiiv site. The Kolodiiv 2, 3 and 5 profiles were selected for this study. The Kolodiiv 2 profile contains loesses, interglacial (Eemian) and interstadial (Vistulian) p[...]
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Geochronometria
2015 Vol. 42, no.1 126--138
EN Luminescence dating was applied on coarse-grained monomineralic potassium-rich feldspar and polymineralic fine-grained minerals of five samples derived from fluvial deposits of the River Weser in northwestern Germany. We used a pulsed infrared stimulated luminescence (IRSL) single aliquot regenerati[...]
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Polish Geological Institute Special Papers
2008 Vol. 23 117-138
EN The aim of this study was the reinterpretation of the published and unpublished Late-Pleistocene and Holocene pollen and diatom diagrams of deposits from the sedimentary basins of the Southern Baltic Sea and the correlation of the distinguished biostratigraphic units with lithological parameters, se[...]
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Annales Societatis Geologorum Poloniae
EN This paper presents the results of absolute dating and biostratigraphical analysis carried out for alluvial sediments of an abandoned Starunia ozokerite mine located in the Velyky Lukavets River valley, in which large mammal remains were discovered in the first half of the 20th century. The sediment[...]
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Polish Geological Institute Special Papers
2004 Vol. 13 167-174
PL Geostanowiska położone w białoruskiej części środkowego Niemna zawierają obszerną informację o środowiskach sedymentacyjnych oraz rozwoju sieci hydrograficznej w obrębie zlewni Niemna - jednej z wielkich rzek Europy centralnej. Badania sukcesji sedymentacyjnych w stanowiskach z jednoznaczną pozycją [...]
EN Geosites in the Belarussian part of the Middle Neman area contain a rich information on sedimentary environments and development of hydrographical network within the drainage basin of Neman – one of the largest rivers of central Europe. A study of sediment successions of the best stratigraphically d[...]
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Kwartalnik Geologiczny
PL Odkrywka Koźmin KWB Adamów znajduje się na rozległej równinie aluwialnej w zachodniej części basenu uniejowskiego. Powierzchnię równiny pokrywają osady tarasowe vistulianu pocięte wąskimi strefami aluwiów holoceńskich. W zachodniej części obszaru A. Mańkowska (1980) wyróżniła piaski glacifluwialne z[...]
EN Several alternating organic-mineral and mineral beds of the Vistulian, accumulated by a braided river, are recorded from outcrops of the Adamów open-cast mine. They have considerable lateral extension and are underlain by the Wartanian till. Sedimentary structures and lithologic analyses prove varyi[...]
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Geochronometria
2001 Vol. 20 75-80
EN The stratotype of Merkine (Eemian) interglacial in Lithuania is the Jonionys section near Merkine town in south Lithuania. The lacustrine sediments containing rich fossil flora in this section were formed under the conditions of Merkine interglacial and Nemunas (Vistulian) glacial. The fossil-bearin[...]
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Polish Geological Institute Special Papers
2003 Vol. 10 5-79
PL Krzywą względnych zmian poziomu morza skonstruowano na podstawie 314 dat radiowęglowych osadów pochodzących z różnych środowisk lądowych i morskich. Próbki do datowań pobrano z 163 stanowisk zlokalizowanych na obszarze polskiej części południowego Bałtyku i przyległej strefy brzegowej. Przy konstruo[...]
EN The relative sea level curve was developed for the southern Baltic area, based on a set of 314 radiocarbon datings of different terrestrial and marine sediments, collected at 163 sites located in the Polish part of the Southern Baltic and in the adjacent coastal land area. When developing the curve,[...]
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Kwartalnik Geologiczny
PL Przedstawiono niektóre wyniki badań geologicznych i geomorfologicznych z obszaru największego basenu zastoiskowego Białorusi, tj. zbiornika połockiego położonego na obszarze ostatniego zlodowacenia pomiędzy strefami marginalnymi fazy święciańskiej (frankfurckiej) i stadium brasławskiego (pomorskiego[...]
EN Evidence of glacioisostatic rebound within the ice marginal zone of the last glaciation is presented. The largest glacial lake of Belarus, i.e. the Polotsk lake situated at a short distance from the maximum limit of the Poozerie (Weichselian) Glaciation, was chosen as an object. Spectrum of glaciola[...]
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Przegląd Geologiczny
2012 Vol. 60, nr 11 605–-614
EN The most representative and long Late Pleistocene pollen sequences covering the late glacial of the penultimate glaciation (Warta/Pripiat), the last interglacial (Eemian/Muravian) and the early glacial of the Last Glaciation (Vistulian/Poozerie) from the territory of Poland and Belarus have been cor[...]
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Acta Geologica Polonica
2015 Vol. 65, no. 2 245--261
EN Slope deposits developed on calcareous sandstone and limestone formations in the eastern part of the Podhale Basin (Carpathians) were studied. In total, the analysis included fifteen profiles of such sediments, which revealed the presence of abundant malacofaunas comprising 39 mollusc species. Five [...]
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