Geochronometria

, Volume 41, Issue 1, pp 104–110 | Cite as

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

Research Article

Abstract

The dendrochronological studies were carried out on very well preserved sub-fossil pine wood found in the biogenic deposits of the Rucianka raised bog (NE Poland). Local floating chronologies, covering the period 990-460 cal BC, were dated on the basis of radiocarbon analyses. Growth depressions in annual treering widths indicated periodical deterioration of the environmental conditions, which affected tree growth. Identified germination and dying-off phases (GDO) should be related to the wetter climatic periods. The extinction of trees took place during periods of higher groundwater level which, in turn, caused favourable conditions for growth of young pines.

Keywords

dendrochronology subfossil wood Pinus sylvestris Holocene NE Poland 

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Copyright information

© Versita Warsaw and Springer-Verlag Wien 2013

Authors and Affiliations

  1. 1.Faculty of Geology, Geophysics and Environmental ProtectionAGH-University of Science and TechnologyCracowPoland
  2. 2.Marine Geology Branch in Gdańsk-OliwaPolish Geological Institute — National Research InstituteGdańskPoland

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