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Changes of Water Level in the Eemian Palaeolake at Imbramowice (SW Poland) Based on Isotopic and Cladoceran Data

Published online by Cambridge University Press:  20 January 2017

Joanna Mirosław-Grabowska  and
Michał Gąsiorowski
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Abstract

Isotopic and cladoceran investigations of Eemian (MIS 5e) lake sediments from Imbramowice, SW Poland, allow us to reconstruct the environmental conditions, especially changes of water level and trophic status, during the early and middle Eemian Interglaciation. We analyzed the sediments from 6.5 to 11.0 m depth in a core provided by Mamakowa (1989). The upper 6.5 m had insufficient carbonates and cladoceran contents for analyses. The analyzed section consists of sandy and organic silts at the bottom, followed by gyttja characterized by increasing CaCO3 content. Measured δ18O values oscillate from ca. -9 to -4‰ and δ13C from -3.5 to above + 6‰. Based on stable isotope analyses of carbonates, we define and characterize eight isotopic horizons (Is). We identify 26 taxa of subfossil Cladocera and seven zones (CLZ) of faunal development. Probably the greatest depth of the lake occurred with pollen zone E2; shallowing then took place. During pollen zones E2-E3, gradual warming is observed and expressed through a positive trend in both δ18O and δ13C values. Pollen zone E4 is characterized by frequent changes of water level. During the Eemian Interglaciation, excluding the initial phase of lake evolution, the lake was meso-eutrophic and eutrophic with high phytoplankton productivity.

Keywords

Stable isotopesCladoceraWater levelTrophic statusEemianSW Poland
Type
Original Articles
Information
Quaternary Research , Volume 73 , Issue 1 , January 2010 , pp. 143 - 150
Copyright
University of Washington

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References

Aalbersberg, G., Litt, T., (1998). Multiproxy climate reconstructions for the Eemian and Early Weichselian. Journal of Quaternary Science 13, 367–390.3.0.CO;2-I>CrossRefGoogle Scholar
Cheddadi, R., Mamakowa, K., Guiot, J., de Beaulieu, J.-L., Reille, M., Andrieu, V., Granoszewski, W., Peyron, O., (1998). Was the climate of the Eemian stable? A quantitative climate reconstruction from seven European pollen records. Palaeogeography, Palaeoclimatology, Palaeoecology 143, 73–85.CrossRefGoogle Scholar
Craig, H., (1953). The geochemistry of the stable carbon isotopes. Geochimica et Cosmochimica Acta 3, 53–92.Google Scholar
Fagel, N., Mackay, A.W., (2008). Weathering in the Lake Baikal watershed during the Kazantsevo (Eemian) interglacial: Evidence from the lacustrine clay record. Palaeogeography, Palaeoclimatology, Palaeoecology 259, 244–257.CrossRefGoogle Scholar
Fl"ssner, D., (2000). Die Haplopoda und Cladocera (ohne Bosminidae) Mitteleuropas. pp. 428. Backhuys Publishers, Leiden.Google Scholar
G?siorowski, M., (2002). Changes in Cladocera (Crustacea) assemblage of Kruklin Lake (Masurian Lake District) caused by artificial drop in water level. Limnological Review 2, 131–136.Google Scholar
G?siorowski, M., Hercman, H., (2005). Recent sedimentation and eutrophication of Kruklin Lake after artificial drop in water-level in the middle of 19th century. Studia Quaternaria 22, 17–25.Google Scholar
Granoszewski, W., (2003). Late Pleistocene vegetation history and climatic changes at Horoszki Du?e, eastern Poland: a palaeobotanical study. Acta Palaeobotanica Supplementum 4, 3–95.Google Scholar
Granoszewski, W., Demske, D., Nita, M., Heumann, G., Andreev, A.A., (2005). Vegetation and climate variability during the Last interglacial evidenced in the pollen record from Lake Baikal. Global and Planetary Change 46, 187–198.CrossRefGoogle Scholar
Hoefs, J., (1996). Stable Isotope Geochemistry. 1"201. Springer-Verlag, Berlin-Heidelberg.Google Scholar
Hofmann, W., (1999). Cladocerans and chironomids as indicators of lake level changes in north temperate lakes. Journal of Paleolimnology 19, 55–62.CrossRefGoogle Scholar
Hofmann, W., (2003). The long-term succession of high-altitude cladoceran assemblages: a 9000-year record from Sagistalsee (Swiss Alps). Journal of Paleolimnology 30, 291–296.CrossRefGoogle Scholar
Kaczmarska, I., (1976). Diatom analysis of Eemian profile in fresh-water deposits at Imbramowice near Wroc?aw. Acta Palaeobotanica 17, 2, 3–34.Google Scholar
Klotz, S., Guiot, J., Mosbrugger, V., (2003). Continental European Eemian and early W"rmian climate evolution: comparing signals using different quantitative reconstruction approaches based on pollen. Global and Planetary Change 36, 277–294.CrossRefGoogle Scholar
Krebs, C.J., (1994). Ecology. 4th ed HarperCollins, New York.Google Scholar
Kupryjanowicz, M., (2008). Vegetation and climate of the Eemian and Early Vistulian lakeland in northern Podlasie. Acta Palaeobotanica 48, 1, 3–130.Google Scholar
Kupryjanowicz, M., Ciszek, D., Miros?aw-Grabowska, J., Marciniak, B., Niska, M., (2005). Two climatic oscillations during the Eemian Interglacial " preliminary results of multi-proxy researches of palaeolake at Solniki, NE Poland. Polish Geological Institute Special Papers 16, 53–57.Google Scholar
Leng, M.J., Lamb, A.L., Marshall, J.D., Wolfe, B.B., Jones, M.D., Holmes, J.A., Arrowsmith, C., (2006). Isotopes in Lake Sediments. Leng, M.J. Isotopes in Palaeonvironmental Research.Springer, The Netherlands.147–184.CrossRefGoogle Scholar
Litt, T., Junge, F.W., B"ttger, T., (1996). Climate during the Eemian in north-central Europe " a critical review of the palaeobotanical and stable isotope data from central Germany. Vegetation History and Archaeobotany 5, 247–256.Google Scholar
Mamakowa, K., (1976). Vegetation of the Eemian Interglacial at Imbramowice near Wroc?aw " preliminary report. Acta Palaeobotanica 17, 1, 27–38.Google Scholar
Mamakowa, K., (1988). Pollen stratigraphy of the Eemian and adjoining glacial deposits based on continuous sequences in Poland. Bulletin of the Polish Academy of Sciences. Earth Science 36, 3"4, 299–308.Google Scholar
Mamakowa, K., (1989). Late Middle Polish Glaciation, Eemian and Early Vistulian vegetation at Imbramowice near Wroc?aw and the pollen stratigraphy of this part of the Pleistocene in Poland. Acta Palaeobotanica 29, 1, 11–176.Google Scholar
McCrea, J.M., (1950). The isotopic chemistry of carbonates and a paleotemperature scale. Journal of Chemical Physics 18, 849–857.CrossRefGoogle Scholar
Milecka, K., Szeroczy?ska, K., (2005). Changes in macrophytic flora and planktonic organisms in Lake Ostrowite, Poland, as a response to climatic and trophic fluctuations. Holocene 15, 74–84.CrossRefGoogle Scholar
Miros?aw-Grabowska, J., (2007). Isotopic records of climatic and hydrological changes during Eemian " palaeolake at Imbramowice (SW Poland). 4th International Limnogeology Congress ILIC 2007 "Limnogeology: tales of an evolving Earth", Barcelona-CosmoCaixa 11"14.07.2007. Programme and abstracts book.190.Google Scholar
Miros?aw-Grabowska, J., Niska, M., (2005). Isotopic and Cladocera records of climate changes of Early Eemian at Besiekierz (Central Poland). Geological Quarterly 49, 1, 67–74.Google Scholar
Miros?aw-Grabowska, J., Niska, M., (2007a). Reconstruction of environmental conditions of Eemian palaeolake at Studzieniec (Central Poland) on the basis of stable isotope and Cladocera analyses. Quaternary International 162"163, 195–204.CrossRefGoogle Scholar
Miros?aw-Grabowska, J., Niska, M., (2007b). Isotope and Cladocera data and interpretation from the Eemian optimum and postoptimum deposits, Kaliska palaeolake (Central Poland). Quaternary International 175, 1, 155–167.CrossRefGoogle Scholar
M"ller, W.P., (1964). The distribution of cladoceran remains in surfical sediments from three northern Indiana lakes. Investigations of Indiana Lakes and Streams 6, 1–63.Google Scholar
Niska, M., (2005). Interpretacja zmian ?rodowiska jeziornego w interglacjale eemskim na podstawie analizy subfosylnych Cladocera. PhD-thesis, Institute of Geological Science Polish Academy of Sciences, Warsaw, unpublished.Google Scholar
Nitychoruk, J., (2000). Climate reconstruction from stable-isotope composition of the Mazovian Interglacial (Holsteinian) lake sediments in eastern Poland. Acta Geologica Polonica 50, 2, 247–294.Google Scholar
R"?a?ski, K., Kuc, T., Duli?ski, M., Wachniew, P., (1998). Oxygen and carbon isotope composition of authigenic carbonates in the Holocene part of the Lake Go?ci?? sediments. Ralska-Jasiewiczowa, M., Goslar, T., Madeyska, T., Starkel, L. Lake Go?ci??. Central Poland a monographic study. Part 1.229–232.Google Scholar
Sarmaja-Korjonen, K., (2001). Correlation of fluctuations in cladoceran planktonic/littoral ratio between three cores from a small lake in S. Finland " Holocene water-level changes. Holocene 11, 53–63.CrossRefGoogle Scholar
Sarmaja-Korjonen, K., Kultti, S., Solovieva, N., Valiranta, M., (2003a). Mid-Holocene palaeoclimatic and palaeohydrological conditions in northeastern European Russia: a multi-proxy study of Lake Vankavad. Journal of Paleolimnology 30, 415–426.CrossRefGoogle Scholar
Sarmaja-Korjonen, K., Szeroczy?ska, K., G?siorowski, M., (2003b). Subfossil chydorid taxa and assemblages from lake sediments in Poland and Finland with special reference to climate. Studia Quaternaria 20, 25–34.Google Scholar
Sarmaja-Korjonen, K, Nyman, M, Kultti, S, Valiranta, M., (2006). Palaeolimnological development of Lake Njargajavri, northern Finnish Lapland, in a changing Holocene climate and environment. Journal of Paleolimnology 35, 65–81.CrossRefGoogle Scholar
Schwalb, A., (2003). D.G.Frey & E.S.Deevey Review #3; Lacustrine ostracodes as stable isotope recorders of late-glacial and Holocene environmental dynamics and climate. Journal of Paleolimnology 29, 265–351.CrossRefGoogle Scholar
Sienkiewicz, E., Gasiorowski, M., Hercman, H., (2006). Is acid rain impacting the Sudetic lakes?. Science of the Total Environment 369, 139–149.CrossRefGoogle ScholarPubMed
Szeroczy?ska, K., (1998a). Palaeolimnological investigations in Poland based on Cladocera (Crustacea). Palaeogeography, Palaeoclimatology, Palaeoecology 140, 335–345.Google Scholar
Szeroczy?ska, K., (1998b). Cladocera (Crustacea) as information source in studies of lake sediments. Studia Geologica Polonica 112, 9–28. (in Polish with English summary)Google Scholar
Szeroczy?ska, K., (2002). Human impact on lakes recorded in the remains of Cladocera (Crustacea). Quaternary International 95"6, 165–174.CrossRefGoogle Scholar
Szeroczy?ska, K., Sarmaja-Korjonen, K., (2007). Atlas of subfossil Cladocera from Central and Northern Europe. pp. 84, ?wiecie.Google Scholar
Whiteside, M.C., (1970). Danish Chydorid Cladocera: modern ecology and core studies. Ecological Monographs 40, 79–118.CrossRefGoogle Scholar
Zagwijn, W.H., (1996). An analysis of Eemian climate in Western and Central Europe. Quaternary Science Reviews 15, 451–469.CrossRefGoogle Scholar