Preliminary suggestions on the Pleistocene palaeovegetation around the Biśnik Cave (Częstochowa Upland, Poland) based on studies of molecular fossils from cave sediments

• Autorzy: Krajcarz M. T. M. T. , Gola M. R. , Cyrek K. J. K. J.
• Języki publikacji: EN

Abstrakty

EN

Bisnik Cave is an important site of Middle Palaeolithic, with the longest sequence of Neanderthal settlement phases in Central Europe. In the previous studies of the Bisnik sediments, different elements of palaeoenvironment in the periods of Neanderthal occupation have been recognised, except of palaeovegetation, which could not be derived because of lack of preserved plant micro- or macrofossils. The current work is an attempt to reconstruct palaeovegetation in vicinity of the Bisnik Cave, using analysis of composition of plant-derived n-alkanes, preserved in sediments. In our study, we analyzed one sample from each of the sediment's layers 11 - 19c (early Late Pleistocene and late Middle Pleistocene). Abundant n-alkanes (mostly n-C27, n-C29 and n-C31) were found in all the sampled layers except for the layers 12, 16 and 19d, showing no alkanes at all. There is clear diversification of n-alkanes composition and cpr (carbon preference index) values between layers. Analysis of this composition, allows us to claim that the layers 11 and 14 were accumulated when the cave's vicinity was covered by dense coniferous forests, hence upon warm climate. The layers 19, 19a lower, 19b and 19c, presumably originated during cold periods when open woodlands or grasslands dominated. The other analyzed layers could be counected with intermediate vegetation in form of open woodland. However, not all of the achieved results stay in compliance with the actual stratigraphy, established basing on lithological data and palaeoecology offossil fauna, and we hope that explanation of this discrepancy would be possible after more extensive studies of molecular fossils are done.

Słowa kluczowe

EN

cave sediments; biomarkers; n-alkanes; gas chromatography; palaeoenvironment

• Wydawca: Institute of Geological Science Polish Academy of Science
• Czasopismo: Studia Quaternaria
• Rocznik: 2010
• Tom: Vol. 27
• Strony: 55--61
• Opis fizyczny: Bibliogr. 26 poz.

Twórcy

autor

Krajcarz M. T. M. T.

autor

Gola M. R.

autor

Cyrek K. J. K. J.

• Institute of Geologica I Sciences, Polish Academy of Sciences, Twarda 51/55, 00-818 Warszawa, Poland

Bibliografia

• Baker E.A. 1982. Chemistry and morphology of plant epicuticular waxes. In Cutler D.F., Alvin K.L., Price C.E. (eds), The Plant Cuticle, 139-165. Academic Press, London.
• Blyth A.J., Asrat A., Baker A., Gulliver P., Leng M.J., Genty D. 2007. A new approach to detecting vegetation and land-use change using high-resolution lipid biomarker records in stalagmites. Quaternary Research 68, 314-324.
• Cranwell P.A. 1984. Lipid geochemistry of sediments from Upton Broad, a small productive lake. Organic Geochemistry 7, 25-37.
• Cyrek K. 2006. Middle Palaeolithic Vistulian assemblages of flint artifacts from Biśnik Cave (original: Srodkowopaleolityczne vistulianskie zespoły wyrobów krzemiennych z Jaskini Biśnik). Swiatowit, Supplement series P: Prehistory and Middle Ages 11, 93-100 (in Polish).
• Cyrek K., Miroslaw-Grabowska J., Stefaniak K., Socha P. 2009. Archaeology, stratigraphy and palaeoecology of the Bisnik Cave. Studies of the Faculty of Earth Sciences, University of Silesia 56, 191-214.
• Cyrek K., Socha P., Stefaniak K., Madeyska T., Miroslaw-Grabowska J., Sudoł M., Czyżewski £. 2010. The Palaeolithic of the Biśnik Cave (Southern Poland) against the environmental background. Quaternary International 220, 5-30.
• Dinel H., Schnitzer M., Mehuys G.R. 1990. Soil Lipids: origin, nature, content, decomposition and effect on soil physical properties. In Bollag J.M., Stotzky G. (eds), Soil biochemistry, vol. 6, 397-422. Marcel Dekker, INC., New York.
• Eglinton G., Hamilton, R.J. 1967. Leaf epicuticular waxes. Science 156, 1322-1337.
• Ishiwatari R., Hirakawa, Y., Uzaki, M., Yamada, K., Yada, T. 1993. Organic geochemistry of the Japan Sea sediments - 1: Bulk organic matter and hydrocarbon analyses of core KH-79-3, C-3 from the Oki Ridge for palaeoenvironment assessments. Journal of Oceanography 50, 179-195.
• Maffei M. 1996. Chemotaxonomic significance of leaf wax n-al-kanes in the Umbelliferae, Cruciferae and Leguminosae (Subf. Papilionoideae). Biochemical Systematica and Ecology 24, 531-545.
• Marseille F., Disnar J.R., Guillet B., Noack Y. 1999. n-Alkanes and free fatty acids in humus and A1 horizons of soils under beech, spruce and grass in the Massif-Central (Monte-Lozère). France. European Journal of Soil Science 50, 433-441.
• Meyers P.A., Ishiwatari R. 1993. Lacustrine organic geochemistry - an overview of indicators of organic matter sources and diagenesis in lake sediments. Organic Geochemistry 20, 867-900.
• Mirosław-Grabowska J. 2002. Geotogtcal value of Biśnik Cave sediments (Cracow-Częstochowa Upland). Acta Geologica Polonica 52, 97-110.
• Nott C.J., Xie S., Avsejs L.A., Maddy D., Chambers F.M., Ever-shed R.P. 2000. n-Alkane distributions in ombrotrophic mires as indicators of vegetation change related to climatic variation. Organic Geochemistry 31, 231-235.
• Rao Z., Zhu Z., Wang S., Jia G., Qiang M., Wu Y. 2009. CPI values of terrestrial higher plant-derived long chain n-alkanes: a potential paleoclimatic proxy. Frontiers of Earth Science in China 3, 266-272.
• Rieley G., Collier R.J., Jones D.M., Eglinton G., Eakin P.A. 1991. Sources of sedimentary lipids deduced from stable carbon-isotope analyses of individual compounds. Nature 352,425-427.
• Schwark L., Zink K., Lechterbeck J. 2002. Reconstruction of postglacial to early Holocene vegetation history in terrestrial Central Europe via cuticular lipid biomarkers and pollen records from lake sediments. Geology 30, 463-466.
• Socha P. 2009. Small mammals (Erinaceomorpha, Soricomorpha, Chiroptera, Lagomorpha, Rodentia) from Pleistocene sedtt ments of the Biśnik Cave. Studies of the Faculty of Earth Sciences, University of Silesia 56, 215-224.
• Stefaniak K., Marciszak A. 2009. Large mammals (Carnivora, Ungulata) from Pleistocene sedtments of the Biśnik Cave. Studies of the Faculty of Earth Sciences, University of Silesia 56, 225-254.
• Uchiyama T., Ogasawara N. 1981. Constituents of Plant Leaf Wax Contained in Rice Callus Tissues. Agricultural and Biological Chemistry 45, 1261-1263.
• Van Andel T.H., Tzedakis P.C. 1996. Palaeotithic landscapes of Europe and environs, 150,000-25,000 years ago an overview. Quaternary Science Review 15, 481-500.
• Vilegas J.H.Y., Lancas F.M., Vilegas W., Pozetti G. 1997. Further triterpanes, steroids and furocoumarins from Brazilian Medicinal Plants of Dorstenia genus (Moraceae). Journal of the Brazilian Chemical Society 8, 529-535.
• Wiesenberg G. L.B., Schwarzbauer J., Schmidt W.I., Schwark L. 2004. Source and turnover of organic matter in agricultural soils derived from n-alkane/n-carboxylic acid compositions and C-isotopes signatures. Organic Geochemistry 35, 13711393.
• Wiszniowska T., Stefaniak K, Socha P. 2002. Quaternary fauna from sediments of the Biśnik Cave. In Cyrek K. (ed.) Jaskinia Biśnik. Rekonstrukcja zasiedlenia jaskini na tle zmian środowiska przyrodniczego, 193-220. Wydawnictwo UMK, Toruń (in Polish with English summary).
• Xie S., Wang Z., Wang H., Chen F., An C. 2002. The occurrence of grass vegetation over the Chinese Loess Plateau since the last interglacial: the molecular fossil record. Science ofChina, Series D: Earth Sciences 45, 53-62.
• Zhang H., Yang M., Zhang W., Lei G., Chang F., Pu Y., Fan H. 2008. Molecular fossil and paleovegetation records of paleosol S4 and adjacent loess layers in the Luochuan loess section, NW China. Science of China, Series D: Earth Sciences 51, 321-330.