Upper Pleistocene palaeoenvironmental changes at the Zwierzyniec site, Central Poland

Kalińska-Nartiša, E.; Dzierżek, J.; Bińka, K.; Borkowski, A.; Rydelek, P.; Zawrzykraj, P.

doi:10.7306/gq.1280

Artykuł - szczegóły

Tytuł artykułu

Upper Pleistocene palaeoenvironmental changes at the Zwierzyniec site, Central Poland

Autorzy

Kalińska-Nartiša E. , Dzierżek J. , Bińka K. , Borkowski A. , Rydelek P. , Zawrzykraj P.

Treść / Zawartość

Pełne teksty:

Kalińska-Nartisa_Upper_Geol. Quart._Vol. 60_No 3_2016.pdf

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Identyfikatory

DOI

10.7306/gq.1280

Warianty tytułu

Języki publikacji

Abstrakty

The paper presents the data on an Eemian–Late Glacial sedimentary sequence from the Zwierzyniec site, central Poland. A number of boreholes document one or two organic layers that occur beneath one or two horizons of clayey and silty deposits of ice-dammed lakes. This study demonstrates to which extent the Zwierzyniec site can contribute to a better understanding of the palaeoenvironmental changes during the Eemian–Vistulian time-frame in central Poland. To study it, a multi-proxy approach was applied, involving: palynological and plant macrofossil analysis, study of rounding of quartz grains and morphology of their surface, and investigations of sand mineralogy and till petrography. The results show that a till bed is overlain by a sandy series corresponding to the glacial-interglacial transition. Either one or two distinct peaks of organic accumulation are evidenced by peat horizons. The lower horizon records spectra with hazel and hornbeam, and did, therefore, accumulate in the Eemian. Observed only in some boreholes, the upper peat horizon marks the Brørup (or the lower part of the Rederstall stadial) represented by forest-steppe conditions with patchy mosaics of larch and further transition into sedges and herbaceous taxa. Localized in between the two peat sequences, the sandy horizon marks a long-lasting aeolian transformation with weathering by frost in the Early Vistulian. Again, significant changes of the palaeoenvironmental regime occurred, and are manifested in the one or two horizons of the glaciolacustrine sediments. This corresponded to the last glaciation in the region, when the ice-dammed lakes formed during the Main Stadial.

Słowa kluczowe

pollen plant macrofossils glaciolacustrine Eemian–Vistulian sequence palaeoenvironment Central Poland

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2016

Tom

Vol. 60, No. 3

Strony

610--623

Opis fizyczny

Bibliogr. 98 poz., rys., tab., wykr.

Twórcy

autor

Kalińska-Nartiša E.

Lund University, Department of Geology, Sölvegatan 12, Lund 223 62, Sweden

autor

Dzierżek J.

University of Warsaw, Faculty of Geology, Żwirki i Wigury 93, 02-089 Warszawa, Poland

autor

Bińka K.

University of Warsaw, Faculty of Geology, Żwirki i Wigury 93, 02-089 Warszawa, Poland

autor

Borkowski A.

University of Warsaw, Faculty of Geology, Żwirki i Wigury 93, 02-089 Warszawa, Poland

autor

Rydelek P.

University of Warsaw, Faculty of Geology, Żwirki i Wigury 93, 02-089 Warszawa, Poland

autor

Zawrzykraj P.

University of Warsaw, Faculty of Geology, Żwirki i Wigury 93, 02-089 Warszawa, Poland

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Uwagi

Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.

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Bibliografia

Identyfikator YADDA

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