Hydrological variability of middle European peatland during the Holocene, inferred from subfossil bog pine and bog oak dendrochronology and high-resolution peat multiproxy analysis of the Budwity peatland (northern Poland)

Author:

Margielewski Włodzimierz,Krąpiec Marek,Buczek Krzysztof,Szychowska-Krąpiec Elżbieta,Korzeń Katarzyna,Niska Monika,Stachowicz-Rybka Renata,Wojtal Agata Z.,Mroczkowska Agnieszka,Obidowicz Andrzej,Sala Dariusz,Drzewicki Wojciech,Barniak Joanna,Urban Jan

Funder

National Science Centre Poland

Publisher

Elsevier BV

Reference110 articles.

1. The Goettingen tree-ring chronologies of peat – preserved oaks and pines from Northeast Germany;Achterberg;German J. Geol.,2017

2. Dendrochronogically dated pine stumps document phase - wise bog expansion at a northwest German site between ca. 6700 BC and ca. 3400 BC;Achterberg;Clim. Past,2018

3. Dendrochronology and radiocarbon dating of subfossil conifer logs from a peat bog, Maramureş Mts;Árvai;Romania. Quat. Int.,2016

4. A simple cross-dating program for tree-ring research;Baillie;Tree-Ring Bull.,1973

5. Subfossil wood from the Rucianka raised bog (NE Poland) as an indicator of climatic changes in the first millennium BC;Barniak;Geochronometria,2014

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