A 9000 year record of cyclic vegetation changes identified in a montane peatland deposit located in the Eastern Carpathians (Central-Eastern Europe): Autogenic succession or regional climatic influences?
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- 作者：Mariusz Gałkaa ; galka@amu.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Ioan Tanţăub ; ioan.tantau@ubbcluj.ro" class="auth_mail" title="E-mail the corresponding author ; Vasile Ersekc ; vasile.ersek@northumbria.ac.uk" class="auth_mail" title="E-mail the corresponding author ; Angelica Feurdeanb ; d ; afeurdean@senckenberg.de" class="auth_mail" title="E-mail the corresponding author ; angelica.feurdean@gmail.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Sphagnum succession ; Plant macrofossil remains ; Holocene ; Climate change ; Sphagnum magellanicum ; Eriophorum vaginatum
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：1 May 2016
- 年：2016
- 卷：449
- 期：Complete
- 页码：52-61
- 全文大小：2230 K
文摘
The scientific merit of this paper resides from:
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It is the very first study concerning the development of a bog in Central-Eastern Europe.
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The use of high-quality data set i.e., high-temporal resolution, continuous plant macrofossil record.
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Hypothesis testing of a hotly debated subject regarding the driving factors for peatland development and functioning, that is regional climate changes versus autogenic succession from an area where nothing is known about the subject.
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Implication of the use of ombrothrophic mountains bog as a palaeoclimatic archive.
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Consolidates the geographical coverage of proxy reconstruction of past climate variability in a poorly studied region.