Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/17359
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Vertical stratification of testate amoebae in the Elatia Mires, northern Greece: Palaeoecological evidence for a wetland response to recent climatic change, or autogenic processes?
Authors: Payne, Richard
Pates, Jacqueline M
Contact Email: r.j.payne@stir.ac.uk
Keywords: Mires
Peatlands
Climate change
Testate amoebae
Palaeohydrology
Issue Date: Aug-2009
Publisher: Springer
Citation: Payne R & Pates JM (2009) Vertical stratification of testate amoebae in the Elatia Mires, northern Greece: Palaeoecological evidence for a wetland response to recent climatic change, or autogenic processes?, Wetlands Ecology and Management, 17 (4), pp. 355-364.
Abstract: The Elatia Mires of northern Greece are unique ecosystems of high conservation value. The mires are climatically marginal and may be sensitive to changing hydroclimate, while northern Greece has experienced a significant increase in aridity since the late twentieth century. To investigate the impact of recent climatic change on the hydrology of the mires, the palaeoecological record was investigated from three near-surface monoliths extracted from two sites. Testate amoebae were analysed as sensitive indicators of hydrology. Results were interpreted using transfer function models to provide quantitative reconstructions of changing water table depth and pH. AMS radiocarbon dates and 210Pb suggest the peats were deposited within the last c. 50 years, but do not allow a secure chronology to be established. Results from all three profiles show a distinct shift towards a more xerophilic community particularly noted by increases in Euglypha species. Transfer function results infer a distinct lowering of water tables in this period. A hydrological response to recent climate change is a tenable hypothesis to explain this change; however other possible explanations include selective test decay, vertical zonation of living amoebae, ombrotrophication and local hydrological change. It is suggested that a peatland response to climatic change is the most probable hypothesis, showing the sensitivity of marginal peatlands to recent climatic change.
Type: Journal Article
URI: http://hdl.handle.net/1893/17359
DOI Link: http://dx.doi.org/10.1007/s11273-008-9112-8
Rights: Publisher policy allows this work to be made available in this repository. Published in Wetlands Ecology and Management, August 2009, Volume 17, Issue 4, pp 355-364 by Springer. The original publication is available at www.springerlink.com.
Affiliation: Biological and Environmental Sciences
Lancaster University

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