Palaeoenvironmental and climatic changes during the early pleistocene recorded in the lacustrine-boggy-fluvial sediments at Komorniki, NE Poland

• Autorzy: Khursevich G. , Nita M. , Ber A. , Sanko A. , Fedenya S.
• Języki publikacji: EN

Abstrakty

EN

The lacustrine-boggy-fluvial sequence at Komorniki, NE Poland was subject to complex (geological, palynological, diatomological and malacological) investigations. These sediments occur between the Narevian and Nidanian glaciations tills and belong to the Augustovian Interglacial of Poland correlated with the Cromerian 1 Interglacial of the Netherlands. Two cold stages of a glacial rank and one warm stage of interglacial rank (with dominant pollen of Quercus, Ulmus, Carpinus, Alnus, Tilia and Corylus in sediments corresponding to the climatic optimum) have been distinguished in the pollen succession. The latter is similar to that known from the Augustovian Interglacial profiles at Szczebra, Kalejty and Czarnucha. Diatom succession from the Komorniki section includes certain unidentified, apparently new small species of Stephanodiscus, Staurosirella and Pseudostaurosira side be side with the Pleistocene extinct taxon of Stephanodiscus niagarae var. insuetus and a relatively widespread species of S. rotula characterizing by some morphological peculiarities. In the composition of the malacofauna the fluvial extinct species of Fagotia wuesti and Sphaerium cf. rivicola are the most important molluscs for the biostratigraphy. Among them, Sphaerium cf. rivicola is known from the late Tiglian in the Netherlands. Fagotia wuesti is characteristic of the Bavel Interglacial in the Netherlands, as well as of the Borntal and Artern interglacials in Germany.

Słowa kluczowe

EN

lithology; pollen analysis; diatoms; malacofauna; palaeoenvironment; Lower Pleistocene; NE Poland

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Polish Geological Institute Special Papers
• Rocznik: 2005
• Tom: Vol. 16
• Strony: 35--44
• Opis fizyczny: Bibliogr. 31 poz., wykr.

Twórcy

autor

Khursevich G.

• Institute of Geological Sciences, National Academy of Sciences of Belarus, Kuprevich 7, 220141 Minsk, Belarus

autor

Nita M.

• Faculty of Earth Sciences, University of Silesia, Będzińska 60, 41-200 Sosnowiec, Poland

autor

Ber A.

• Polish Geological Institute, Rakowiecka 4, 00-975 Warszawa, Poland

autor

Sanko A.

• Institute of Geological Sciences, National Academy of Sciences of Belarus, Kuprevich 7, 220141 Minsk, Belarus

autor

Fedenya S.

• Institute of Geological Sciences, National Academy of Sciences of Belarus, Kuprevich 7, 220141 Minsk, Belarus

Bibliografia

• 1. ANTSIFEROVA G.A., 1991 -The diatom flora of the Lower Pleistocene interglacial (Muchkapian) deposits (in Russian with English summ.). Algologia, 1, 1: 104-108.
• 2. BER A., 2000 - Pleistocene of north-eastern Poland and neighbouring areas against crystalline and sedimentary basement (in Polish with English summ.). Pr. Państw. Inst. Geol., 170.
• 3. BUKHTIYAROVA L., 1999 - Diatoms of Ukraine Inland waters. M.G. Kholodny Institute of Botany, Kyiv.
• 4. DIATOMOVYE vodorosli SSSR (iskopayemye i sovremennye). Tom II, vypusk 2, 1992. Nauka, St. Petersburg.
• 5. JANCZYK-KOPIKOWA Z., 1975 - Flora of the Mazovian Interglacial at Ferdynandów (in Polish with English summ.). Biul. Inst. Geol, 290: 5-94.
• 6. JANCZYK-KOPIKOVA Z., 1996-Temperate stages of the Mesopleistocene in the NE Poland (in Polish with English summ.). Biul. Państw. Inst. Geol., 373: 49-66.
• 7. KACPRZAK L., LISICKI S., WINTER H., 2002 - Stratigraphical position of the Czarnucha, the Cisów and the Domuraty sections in the Middle and Lower Pleistocene, NE Poland. Field Symp. on Quaternary geology and geodynamics in Belarus. Abstracts: 19-21. Inst. of Geol. Sc., Minsk.
• 8. KHURSEVICH G.K., FEDENYA S.A., 1998 - Microstratigraphy of the Alexandrian Interglacial deposits on the data of diatom analysis (in Russian with English summ.). Doklady NANBelarusi, 42, 5: 107-112.
• 9. KHURSEVICH G.K., LOGINOVA L.P., 1986 - Vozrast i paleogeographicheskiye usloviya phormirovaniya drevneozernykh otlozheniy Rechitskogo Pridneproviya (po dannym diatomovykh issledovanij). In: Pleistotsen Rechitskogo Pridneproviya Byelorussii (ed. R.A. Zinova): 76-142. Nauka i tekhnika, Minsk.
• 10. KHURSEVICH G.K., PRZYBYŁOWSKA-LANGE W., LOGINOVA L.P., 1990 - Coeval diatom floras from the Pleistocene profiles of Krasnaya Dubrova (Belarus) and Ferdynandów (Poland) (in Russian with English summ.). Doklady AN BSSR, 34,2: 179-183.
• 11. KRAMMER K., LANGE-BERTALOT H., 1986 - Bacillariophyceae. 1: Naviculaceae. Fischer, Stuttgart.
• 12. KRAMMER K., LANGE-BERTALOT H., 1988 - Bacillariophyceae. 2: Bacillariaceae, Epithemiaceae, Surirellaceae. VEB Gustav Fischer Verlag, Jena.
• 13. KRAMMER K., LANGE-BERTALOT H., 1991a - Bacillariophyceae. 3: Centrales, Fragilariaceae, Eunotiaceae. VEB Gustav Fischer Verlag, Jena.
• 14. KRAMMER K., LANGE-BERTALOT H., 1991b - Bacillariophyceae. 4: Achnanthaceae, Kritische Erganzungen zu Navicula (Lineolatae) und Gomphonema Gesamtliteraturverreichnis. VEB Gustav Fischer Verlag, Jena.
• 15. LANGE-BERTALOT H., 2001 - Navicula sensu stricto. 10 genera separated from Navicula sensu lato. Frustulia. A. R. G. Gantner Verlag K. G.
• 16. LANGE-BERTALOT H., METZELTIN D., 1996 - Oligotrophie-Indicatoren 800 taxa repräsentativ rei diverse Seen-Typen / Iconographia Diatomologica. Vol. 2. Koeltz Scientific Book, Konigstein.
• 17. MANIA D., 1973 - Paläookologie, Faunenentwicklung und Stratigraphie des Eiszeitalters im mittleren Elbe-Saalegebiet auf Grund von Molluskengesellschaften. Geologie, 21, Beiheft 76/79: 1-175.
• 18. MARCINIAK B., 2004 - Diatoms from Lower Pleistocene lacustrine sediments of Poland. 18th Intern. Diatom Symp. (eds. A. Witkowski et al): p. 150. University of Szczecin, Szczecin.
• 19. MARCINIAK B., LINDNER L., 2003 - Diatoms and geology of the Ferdynandovian Interglacial lake sediments in Poland (in Polish with English summ.). Botanical Guidebooks, 26: 199-215.
• 20. MEIJER T., 1989 - Notes on Quaternary freshwater mollusks of the Netherlands, with descriptions of some new species. Mededelingen van de Werkgroep voor Tertiaire en Kwartaire Geologie, 26,4: 145-181.
• 21. MEIJER T., PREECE R.C., 1996 - Malacological evidence relating to the stratigraphical position of the Cromerian. In: The early Middle Pleistocene in Europe (ed. C. Turner): 53-82. Brookfield, Rotterdam.
• 22. MENNING M., WIEGANK F., 1982 - Magnetostratigraphische Korrelation - Moglichkeiten und Ergebnisse. Zeitschriftfur der Geologischen Wissenschaften, 10: 1307-1322.
• 23. PIDEK I.A. 2003 - Mesopleistocene vegetation history in the northern foreland of the Lublin Upland based of palaeobotanical studies of the profiles from Zdany and Brus sites. Maria Curie-Skłodowska Press. Lublin.
• 24. ROUND F.E., CRAWFORD R.M., MANN D.G., 1990 - The diatoms. Biology and morphology of genera. Cambridge University, Cambridge.
• 25. SANKO A.F., 1999 - Fauna molluskov Glatsiopleistotsena i Golotsena Belarusi. Nauka i Tekhnika, Minsk.
• 26. SKOMPSKI S., 1982 - Correlation of the Mazovian Interglacial of western Poland with the Holstein Interglacial of the eastern part of German Democratic Republic. Biul. Inst. Geol., 343: 51-58.
• 27. VELICHKEVICH F.Ju., KHURSEVICH G.K., RYLOVA T.B., LITVINYUK G.I., 1997 - Stratigraphy of the Middle Pleistocene of Belarus (in Russian). Strat. Geol. Correl., 5, 4: 68-84.
• 28. WIEGANK F., 1987 - Untersuchungen zur Chronostratigraphie des Mittel- und Jungquartärs der DDR. Zeitschrift fur der Geologischen Wissenschaften, 15: 263-279.
• 29. WINTER H., 1999 - Opracowanie dotyczące wyników analizy palinologicznej próbek z wiercenia Czarnucha, Domuraty i Cisów, arkusz Sztabin. Centr. Arch. Geol. Państw. Inst. Geol., Warszawa (unpubl.).
• 30. WINTER H., 2001 - New profile of Augustowski Interglacial in north-eastern Poland (in Polish with English summ.). Geneza, litologia i stratygrafia utworów czwartorzędowych, t. 3, Seria Geografia, nr 64: 439-449. Wyd. Nauk. UAM, Poznań.
• 31. ZEISSLER H., 1971 - On Fagotia acicularis (Férussac) from the Quaternary deposits in the valleys of Helme and Unstrut. J. Conch. Lond., 27: 257-265.