Sub-fossil wood from the Rucianka raised bog (NE Poland) as an indicator of climatic changes in the first millennium BC Cover

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Sub-fossil wood from the Rucianka raised bog (NE Poland) as an indicator of climatic changes in the first millennium BC

Geochronometria

Volume 41 (2014): Issue 1 (March 2014)

By: Joanna Barniak, Marek Krąpiec and Leszek Jurys

Open Access

|Dec 2013

Authors

Joanna Barniak

barniak@geol.agh.edu.pl

Faculty of Geology, Geophysics and Environmental Protection, AGH-University of Science and Technology, A. Mickiewicza 30, 30-059, Cracow, Poland

Marek Krąpiec

Faculty of Geology, Geophysics and Environmental Protection, AGH-University of Science and Technology, A. Mickiewicza 30, 30-059, Cracow, Poland

Leszek Jurys

Marine Geology Branch in Gdańsk-Oliwa, Polish Geological Institute — National Research Institute, Kościerska 5, 80-328, Gdańsk, Poland

DOI: https://doi.org/10.2478/s13386-013-0126-5 | Journal eISSN: 1897-1695

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Language: English

Page range: 104 - 110

Published on: Dec 20, 2013

Published by: Sciendo

In partnership with: Paradigm Publishing Services

Publication frequency: 1 issue per year

Keywords:

dendrochronology,

subfossil wood,

Pinus sylvestris,

Related subjects:

Geosciences, other

© 2013 Joanna Barniak, Marek Krąpiec, Leszek Jurys, published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

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