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Can tree rings be an indicator of
environmental impact on trees? An example from the ongoing research
in Germany
Basanta Raj Gautam*
ABSTRACT
The presented study was part of an ongoing research project named
EFORWOOD - Tools for Sustainability Impact Assessment of
Forestry-Wood Chain in Europe. It is an integrated project funded
under the European Union. Out of six complemented module of the
EFORWOOD, the study was under module two (Forest Resource
Management). Recognizing the importance of tree rings in finding
past environmental events, the study was an attempt to analyse
radial and height growth of the sample trees. The approach
illustrated in this study serves as a demonstration of the growth
dynamics analysis combining techniques for field data collection
with a scientific approach in laboratory analysis, which provides an
important input for long term dendrochronology based growth dynamic
analysis.
Key words: dendrochronology, radial increment, height increment,
environmental impact
INTRODUCTION
Forests play a major role in global environmental change (Dixon et
al. 1994). The response of forests to climatic changes emphasizes
the need for information regarding the effects of environmental
variability on forest ecosystems. Uncertainty surrounds the extent
to which tree growth can react to environmental changes, such as
rising CO2, N deposition, and increases in temperature and solar
radiation (Marco et al. 2004). Younger trees and forest stands are
generally considered more responsive than older trees and stands to
changes in environmental conditions (Ryan et al. 1997, Mund et al.
2002). Thus, a climate change-induced increase in ring width and
carbon stock is expected to be greater in younger stands than in
older ones. The increase in forest productivity could prove to be
direct evidence of the increase in photosynthetic activity of
terrestrial vegetation and the lengthening of the active growing
season, as inferred from satellite data (Myneni et al. 1997). The
general hypothesis is younger forest stands are growing faster than
older ones when they were the age of the younger ones, possibly as a
result of recent indirect human-induced effects, such as rising CO2
and temperatures and N deposition, at both global and regional
scales.
*Correspondence
Basanta Raj Gautam
University of Joensuu, Faculty of Forest Sciences,
P.O.Box 111, 80101 Joensuu, Finland
Telephone: +358 468479124
Fax: +358 132514422
E-mail:
gautam@cc.joensuu.fi
The Opinions and Views expressed in
the article are solely are those of Authors and CSSTEAP has no
responsibility on the authoriticity of its content. |