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Reflection of climatic changes during interpleniglacial in the geoecosystems of South-Eastern Poland

contemporaneous central Asian mountains with the upper tree line controlled by temperature (July temp. +10°C), and the lower tree-line controlled by humidity ( Grichuk, 1973 ; Bottema, 1979 ; Starkel, 1977 ; Kowalkowski and Starkel, 1984 ). For most of the last cold stage Central Europe was occupied by discontinuous permafrost, so a summer active layer was dependent on local conditions, like a type of soil, exposition of slopes and mezorelief. The authors decided to review the earlier studies, including the sites surveyed in the years 1960–1980. The interpretation of the

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New exposure of loess deposits in Boyanychi (Ukraine) — Results of thermoluminescence analyses

northern France. Review of Palaeobota-ny and Palynology 85: 231–242. http://dx.doi.org/10.1016/0034-6667(94)00128-7 [32] Fedorowicz S, 2006. Metodyczne aspekty luminescencyjnego oznaczania wieku osadów neoplejstoceńskich Europy Środkowej (Methodological aspects of luminescence dating of Central Europe’s Neopleistocene deposits). Wydawnictwo Uniwersytetu Gdańskiego: 156 pp (in Polish). [33] Fedorowicz S, Prylypko S, Bogucki A and Łanczont M, 2008. Międzylaboratoryjne porównanie dat termoluminescencyjnych (TL) próbek z

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The 443-Year Tree-Ring Chronology for the Scots Pine from Upper Silesia (Poland) as A Dating Tool and Climate Proxy

radial increment of the Scots pine (Pinus syl- vestris L.) from the area of Dolny Slask. Folia Forestalia Polonica ser. A, 42: 55-66. Friedrich MS, Remmele B, Kromer J, Hofmann M, Spurk KF, Kaiser CO and Kuppers M, 2004. The 12,460-year Hohenheim oak and pine tree-ring chronology from Central Europe - a unique annual record for radiocarbon calibration and paleoenvironment recon¬structions. Radiocarbon 46(3): 1111-1122. Fritts H, 1976. Tree Rings and Climate London. Academic Press: 1¬280. Gil E, 1976. Muzeum Wsi Opolskiej

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The early Miocene flora of Güvem (Central Anatolia, Turkey): a window into early Neogene vegetation and environments in the Eastern Mediterranean

Greece: a comment to Merceron et al., 2016 (Geobios, doi:10.1016/j.geobios.2016.01.004). Geobios, 49: 135–146. DENK T. & GRIMM G.W. 2009. The biogeographic history of beech trees. Rev. Palaeobot. Palynol., 158: 83–100. DENK T. & GRIMM G.W. 2010. The oaks of western Eurasia: traditional classifications and evidence from two nuclear markers. Taxon, 59: 351–366. DENK T., GRÍMSSON F. & ZETTER R. 2012. Fagaceae from the Early Oligocene of Central Europe: persisting New World and emerging Old World biogeographic links. Rev. Palaeobot. Palynol., 169: 7

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Phenological Analysis of the Last Glacial Vertebrates from the Territory of Moravia (the Czech Republic) – Continuity and Change in Faunistic Communities

) Musil, R. (1999a): The Environment in Moravia during the Stage 3. - In: Central and Eastern Europe from 50.000-30.000 BP. International Workshop in the Neanderthal Museum, March18-21, 1999, Abstracts, pp. 23-27. Musil, R. (1999b): Životní prostředí v posledním glaciálu na území Moravy [The environment in the Last Glacial on the territory of Moravia]. - Acta Musei Moraviae, Scientiae geologicae, 84: 161-186. (in Czech) Musil, R. (1999c): The environment in Moravia during the Stage 3. - In: State of the Stage Project at the Start of its

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Low to middle Pleistocene paleoclimatic record from the Kraków-Częstochowa Upland (Poland) based on isotopic and calcite fabrics analyses

studied chronology. High resolution and precise chronologies are relatively easy to complete for young speleothems. In speleothem science, the 230 Th/U method is usually the best way to obtain precise chronologies. For older periods ( i . e ., older than 0.5 Ma), dating becomes a serious challenge. Theoretically, older material could be dated with the U-Pb method. However, this method requires relatively high uranium content (minimum of a few ppm), whereas typical speleothems from Poland (and all of Central Europe) have uranium concentrations below 0.1 ppm. Another

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Morphometric analysis of metacarpal and metatarsal bones of cave bears (Carnivora, Ursidae)

scaling and its applications. – Applied Psychological Measurement, 7: 373–514. https://doi.org/10.1177/014662168300700401 Dempster, A. P., Laird, N. M., Rubin, D. B. (1977): Maximum likelihood from incomplete data via the EM algorithm. – Journal of the Royal Statistical Society, Series B, 39: 1–38. Döppes, D., Kempe, S., Rosendahl, W. (2008): Dated paleontological cave sites of Central Europe from late Middle Pleistocene to early Upper Pleistocene (OIS 5 to OIS 8). – Quaternary International, 187: 97–104. https://doi.org/10.1016/j.quaint.2007

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The fossil record of tadpoles

): Cinq nouveaux gisements de Pelobatidae (Amphibiens, Anoures) dans l’Oligocène d’Europe central. – Neues Jahrbuch für Geologie und Paläontologie, Monatshefte, 1997(7): 434–446. Gaudant, J., Vatsev, M. (2012): Palaeobatrachids (Amphibia, Anura) in the Oligocene sediments of the “Pirin” Mine (Brezhani Graben, southwestern Bulgaria). – Geologica Balcanica, 41(1-3): 97–103. Giebel, C. (1850): Über eine neue Art von Palaeophrynos Tsch. aus dem Braunkohlengebilde des Siebengebirges. – Jahresbericht des Naturwissenschaftlichen Vereins in Halle, 3: 44

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Representatives of the family Actinostromatidae (Stromatoporoidea) in the Devonian of southern Poland and their ecological significance

. Sedymentacja utworów węglanowych dewonu środkowego rejonu Dębnika [Sedimentation of the Middle Devonian carbonates of the Dębnik area]. Studia Geologica Polonica 75, 59-100. Łuczyński, P., 1998. Stromatoporoid morphology in the Devonian of the Holy Cross Mountains, Poland. Acta Palaeontologica Polonica 43, 653-663. Łuczyński, P., 2008. Growth forms and distribution patterns of stromatoporoids exposed on Devonian palaeobottom surfaces; Holy Cross Mountains, central Poland. Acta Geologica Polonica 58, 303-320. May, A., 2005. Die

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Integration of numerical models and geoinformatic techniques in the delimitation of a protection zone for the MGB 319 complex multi-aquifer system in southwest Poland

Abstract

The study area, situated near the city of Wrocław in southwest Poland, is part of the hydrogeological system of the Quaternary/Neogene MGB 319, inclusive of a buried valley of high water potential, named the Bogdaszowice structure. This structure is an alternative source of water supply for the Wrocław city area. Numerical modelling is the most effective tool in establishing a groundwater protection strategy for Major Groundwater Basins (MGBs) in complex aquifer systems. In the present study, the first step was to assess the hydrodynamic conditions of the Radakowice groundwater intake by analyses of head contours, pathlines, average flow times and capture zones of particular wells. Subsequently, these results were used in combination with other data and compiled as GIS layers. The spatial distribution of hydraulic conductivity was based on the lithology of surface sediments. Other data sets such as the thickness of the unsaturated zone, average soil moisture and infiltration rate were taken either directly from the model or were calculated. Based on the input data obtained, vertical flow time calculations for every model cell were made. The final outcome is a map of the protection zone for the aquifer system of the MGB 319.

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