Younger Dryas climatic reconstructions in central Poland

Pawłowski, D.

doi:10.1515/agp-2017-0026

Artykuł - szczegóły

Tytuł artykułu

Younger Dryas climatic reconstructions in central Poland

Autorzy

Pawłowski D.

Treść / Zawartość

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DOI

10.1515/agp-2017-0026

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Abstrakty

Cladoceran-based paleotemperature estimates for the Younger Dryas for ten sections of paleo-oxbow lakes, valley mires, and lacustrine sediments from central Poland are presented, and their potential usefulness to climatostratigraphy is described. Most of the changes observed in the cladoceran assemblages are responses to climate changes. The cladoceran-based temperature reconstructions reflect cold conditions during the Younger Dryas (YD) and allow a division of this period into two phases: an older colder phase, between 12,800 and 12,000 cal yrs BP, and a younger, warmer phase, between ca. 12,000 and 11,500 cal yrs BP. The geomorphological features of the study sites and local environmental forces are also taken into consideration. The cladoceran-inferred summer temperature estimates from all of the study sites correspond closely with the available climate reconstruction for the YD in central Europe.

Słowa kluczowe

Younger Dryas cladocera temperature oxbow lake climate

młodszy dryas Cladocera temperatura starorzecze klimat

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2017

Tom

Vol. 67, no. 4

Strony

567--584

Opis fizyczny

Bibliogr. 92 poz., rys., tab., wykr.

Twórcy

autor

Pawłowski D.

dominikp@amu.edu.pl

Institute of Geology, Adam Mickiewicz University, ul. B. Krygowskiego 12, 61-680 Poznań, Poland

Bibliografia

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Uwagi

Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).

Typ dokumentu

Bibliografia

Identyfikator YADDA

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