Luminescence chronostratigraphy for the loess deposits in Złota, Poland

Moska, P.; Adamiec, G.; Jary, Z.; Bluszcz, A.; Poręba, G.; Piotrowska, N.; Krawczyk, M.; Skurzyński, J.

doi:10.1515/geochr-2015-0073

Artykuł - szczegóły

Tytuł artykułu

Luminescence chronostratigraphy for the loess deposits in Złota, Poland

Autorzy

Moska P. , Adamiec G. , Jary Z. , Bluszcz A. , Poręba G. , Piotrowska N. , Krawczyk M. , Skurzyński J.

Wybrane pełne teksty z tego czasopisma

Identyfikatory

DOI

10.1515/geochr-2015-0073

Warianty tytułu

Konferencja

Conference Proceedings of the 12th International Conference “Methods of Absolute Chronology” May 11-13th, 2016, Gliwice-Paniówki, Poland

Języki publikacji

Abstrakty

Loess formations in Poland display a close relationship with cooling and warming trends of the Northern Hemisphere during the Pleistocene. Loess sequences sensitively record regional palaeoclimatic and palaeoecological changes. The Złota loess profile (21°39’E, 50°39’N) provides a unique opportunity to reconstruct climate conditions in the past in this part of Poland. This continuous sequence of loess and palaeosol deposits allows to distinguish between warmer and more humid climate which is favourable for soil development and much colder and dry periods which are conducive to loess accumulation. The silty and sandy aeolian material originates mainly from weathered rock surfaces affected by frost shattering or from glaciofluvial/fluvial deposits of river flood plains. In Poland, loess and loess-like formations occur in the southern part of the country, mostly in the south polish uplands, i.e. in the Lublin, Sandomierz, and Cracow Uplands. We used different techniques to establish a chronological framework for this site. 21 samples for luminescence dating were collected from the investigated loess profile in Złota. Infrared post-IR IRSL dating method was applied to the polymineral fine grains (4–11µm). The dating results are accompanied by detailed analyses of the geochemical composition, organic carbon and carbonate. Also, analysis of magnetic susceptibility and grain-size distribution were investigated. Based on such a large stratigraphic dataset an age-depth model using OxCal has also been constructed for this site.

Słowa kluczowe

luminescence dating post-IR IRSL loess stratigraphy

Wydawca

De Gruyter

Czasopismo

Geochronometria

Rocznik

2018

Tom

Vol. 45, no. 1

Strony

44--55

Opis fizyczny

Bibliogr. 56 poz., rys.

Twórcy

autor

Moska P.

Piotr.Moska@polsl.pl

Silesian University of Technology, Institute of Physics – Center for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland

autor

Adamiec G.

Silesian University of Technology, Institute of Physics – Center for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland

autor

Jary Z.

Institute of Geography and Regional Development, University of Wroclaw, 50-137 Wroclaw, Poland

autor

Bluszcz A.

Silesian University of Technology, Institute of Physics – Center for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland

autor

Poręba G.

Silesian University of Technology, Institute of Physics – Center for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland

autor

Piotrowska N.

Silesian University of Technology, Institute of Physics – Center for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland

autor

Krawczyk M.

Institute of Geography and Regional Development, University of Wroclaw, 50-137 Wroclaw, Poland

autor

Skurzyński J.

Institute of Geography and Regional Development, University of Wroclaw, 50-137 Wroclaw, Poland

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-2c9989b1-164e-4d65-949c-8931d256f987