A Tree-Ring chronology from Allerød–YD transition from Koźmin (Central Poland)-Reference-Cited by-同舟云学术

A Tree-Ring chronology from Allerød–YD transition from Koźmin (Central Poland)

Published:2020-01-01 Issue:1 Volume:47 Page:101-111
ISSN:1897-1695
Container-title:Geochronometria
language:en
Short-container-title:

Author:

Krąpiec Marek¹,Szychowska-Krąpiec Elżbieta¹,Barniak Joanna¹,Goslar Tomasz²³,Kittel Piotr⁴,Michczyńska Danuta J.⁵,Michczyński Adam⁵,Piotrowska Natalia⁵,Rakowski Andrzej⁵,Wiktorowski Damian¹

Affiliation:

1. Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology , Kraków , Poland

2. Faculty of Physics, Adam Mickiewicz University , Poznań , Poland

3. Poznań Radiocarbon Laboratory, Foundation of the A. Mickiewicz University , Poznań , Poland

4. Faculty of Geographical Sciences, Department of Geomorphology and Palaeogeography, University of Lodz , Lodz , Poland

5. Institute of Physics - CSE, Silesian University of Technology , Gliwice , Poland

Abstract

Abstract Subfossil trunks of pine (Pinus sylvestris L.) from the Late Weichselian were discovered in the site Koźmin in the Koło Basin, central Poland (Dzieduszyńska et al., 2014a). Another part of organic sediments with trunks was excavated in the frame of the research project. Altogether 224 samples from Koźmin were analysed dendrochronologically; they represented generally young trees, 40 to 70 years old. Based on the most convergent sequences, the chronology 2KOL_A1 was produced, 210 years in length. With the wiggle-matching method, it was dated to ca. 13065–12855 cal BP. Dendrochronological dating of trunks buried in organic sediments, most of which occurred in situ, revealed that tree deaths occurred successively, over more than 100 years. That could have been due to unfavourable climatic conditions, as well as extreme events, e.g. strong winds.

Publisher

Walter de Gruyter GmbH

Subject

Earth and Planetary Sciences (miscellaneous)

Link

https://www.sciendo.com/pdf/10.2478/geochr-2020-0025

Reference44 articles.

1. Baillie, MGL, and Pilcher, JR. 1973. A simple crossdating program for tree-ring research. Tree-Ring Bulletin 33: 7–14.

2. Bronk Ramsey, C. 2009. Bayesian analysis of radiocarbon dates. Radiocarbon 51(1): 337–360, DOI: 10.1017/S0033822200033865.

3. Bronk Ramsey, C, van der Plicht, J, and Weninger, B. 2001. ‘Wiggle-matching’ radiocarbon dates. Radiocarbon 43(2A): 381–389, DOI: 10.1017/S0033822200038248.

4. Cook, ER, Kairiukstis, LA, eds. 1990. Methods of Dendrochronology Dordrecht: Kluwer Academic Publishers.

5. Cook, ER, and Krusic, PJ, 2005. ARSTAN v. 41d: A tree-ring standardization program based on detrending and autoregressive time series modeling, with interactive graphics. Tree-Ring Laboratory, Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York USA.

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