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Geological Quarterly
2013 Vol. 57, No. 4 637–-648
EN Malacological studies of two profiles of the Holsteinian (Mazovian) Interglacial from eastern Poland – Roskosz and Wilczyn 1/12 – are presented. They are connected with the northern part of the Wilczyn palaeolake and seems to document palaeoecological changes in the part of the climatic optimum and [...]
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 35-36
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Oceanological Studies
EN The aim of this study was to analyse fossil and subfossil diatom floras preserved in a sediment core taken from the Gulf of Gdansk, near the eastern end of the Hel Peninsula. The diatom record, supported by lithology and radiocarbon data, indicates environmental changes during the later stages of de[...]
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Oceanological and Hydrobiological Studies
EN The palaeoenvironmental changes of the south-western part of the Gulf of Gdańsk during the last 8,000 years, with reference to the stages of the Baltic Sea, were reconstructed. Diatom analyses of two cores taken from the shallower and deeper parts of the basin enabled the conclusion to be drawn that[...]
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Geochronometria
EN The early sedimentological and ecological developmental stages of a late Vistulian lake in the Żabieniec swamp near Łódź (central Poland) were analysed by radiometric dating, changes in the frequency of specimens and species composition of Cladocera and multivariate statistical analysis (DCA). The l[...]
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Studia Quaternaria
2005 Vol. 22 51-54
EN The study described in this paper is a part of a multi-proxy project, which deals with sediments originating from a former artificial water reservoir situated at the large fortified hilltop site of Vladao. The oldest sediments were deposited around 350 BC and sedimentation continues till recent time[...]
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Oceanological and Hydrobiological Studies
2005 Vol. 34, No.2 111--133
EN Four 6 m long sediment cores from the Vistula Lagoon were analyzed with respect to their content of diatoms. The aim was to detect changes of the composition of the diatom flora and to link these changes to Holocene climatic fluctuations and paleoecological stages of the Baltic Sea. The location of [...]
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Geological Quarterly
EN Foraminifera from newly exposed outcrop sections located in a Middle Miocene piggyback basin of the Outer Carpathians Nowy Sącz Basin indicate an environment of normal saline waters on the inner shelf and a temperature not lower than 18oC. The area was ideal for the proliferation of: Miliolina spp.,[...]
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Studia Geologica Polonica
2005 Vol. 124 285-296
EN In the vicinity of Kraków, Upper Cretaceous sediments rest upon the Upper Jurassic (Oxfordian) massive limestones and are developed as sands, conglomerates and marls. Foraminiferal assemblages from Upper Cretaceous sediments are dominated by calcareous benthic forms whereas planktonic foraminifers a[...]
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Acta Geologica Polonica
EN The astogeny of three species of the amural rugosan genus Scruttonia coming from the Famennian so-called main limestone cropping out in Dzikowiec (the Middle Sudetes) is described. The colonies studied reveal cyclomorphic variation usually regarded as seasonal in nature. The character and shape of t[...]
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Studia Quaternaria
2004 Vol. 21 153-165
EN Analyses of diatom assemblages were performed in sediment cores from the Szczecin Lagoon area, as a part of a multidisciplinary research including seismoacoustic profiling and different types of palaeoecological and geological analyses: palynological, macrofossil, malacological, lithological, geoche[...]
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Acta Geologica Polonica
EN Ichthyoliths, mainly shark teeth, from the Famennian of Iran and Northwest Africa are described. Evolution of shallow-water chondrichthyan assemblages on the shelves of Central Iran and the Tafilalt Platform, Morocco, related to time and environmental changes, is discussed. Four new taxa, viz. Deihi[...]
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Geological Quarterly
EN The Sarcheshmeh and Sanganeh formations are the Lower Cretaceous deep marine sequences of the Koppeh-Dagh sedimentary basin, which revealed a diverse assemblage of dinoflagellates. The paper discusses palynostratigraphy, palynofacies and palaeoenvironment of these rock units in a borehole drilled in[...]
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Annales Societatis Geologorum Poloniae
EN The Magura Nappe is the largest and southernmost tectonic unit of the Western Outer Carpathians and differ in lithofacies development from the Middle and Marginal groups of units. The age studies of the youngest deposits of the Magura Nappe play an important role in understanding the tectogenesis of[...]
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Annales Societatis Geologorum Poloniae
2013 Vol. 83, No. 3 179--200
EN While the marine molluscs from Sarmatian deposits of the Carpathian Foredeep Basin are known in general, there is a paucity of data on the terrestrial gastropods. Recently, a rich assemblage of terrestrial snails, accompanied by freshwater species, was found in Zwierzyniec, in the north-western, mar[...]
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Volumina Jurassica
EN A few distinctive bryozoan assemblages have been recognized in the Middle and Upper Jurassic sediments of the southern Poland. The Upper Callovian to Lower Oxfordian of the hardground character, epibenthic, bryozoan community at Zalas (the Kraków-Wieluf Upland) is restricted to a few cyclostomes, wh[...]
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Volumina Jurassica
EN In the Lusitanian Basin the Sinemurian corresponds to a marginal- to restricted-marine succession, representing the early stage of sea flooding in the recently formed basin, following a Late Triassic rifting event. Except for its topmost part, the Sinemurian succession belongs to the Coimbra Fm., co[...]
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Volumina Jurassica
EN At Peniche region, western Portugal, a rather continuous marly limestone succession ranging in age from the Sinemurian to the earliest Aalenian crops out. The ostracod fauna from a 74 m thick packet within this succession has been studied, encompassing deposits that range from the topmost Pliensbach[...]
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Volumina Jurassica
EN In the Middle Oxfordian (Plicatilis Zone: Patturatensis and Ouatius subzones) of the Polish Jura Chain, the present author found 12 large-sized phylloceratid specimens assigned the genus Calliphylloceras. Maximal diameter of the biggest specimen (nearly complete one coming from the Przybynów localit[...]
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Geological Quarterly
EN The depositional environment of the southern part of the Carpathian Foredeep in the Czech Republic was studied in two boreholes using sedimentological and palaeontological methods. Eight lithofacies were recognised within cores of the early Badenian deposits, comprising two facies associations, name[...]
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