Articles | Volume 69, issue 2
https://doi.org/10.5194/egqsj-69-139-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/egqsj-69-139-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A 2600-year high-resolution climate record from Lake Trichonida (SW Greece)
Institute for Ecosystem Research, Christian-Albrechts-Universität,
Olshausenstraße 75, 24118 Kiel, Germany
Pavlos Avramidis
Department of Geology, University of Patras, Rio, 26504 Patras, Greece
Walter Dörfler
Institute of Pre- and Protohistoric Archaeology,
Christian-Albrechts-Universität, Johanna-Mestorf-Straße 2–6, 24118 Kiel,
Germany
Alexandros Emmanouilidis
Department of Geology, University of Patras, Rio, 26504 Patras, Greece
Ingmar Unkel
Institute for Ecosystem Research, Christian-Albrechts-Universität,
Olshausenstraße 75, 24118 Kiel, Germany
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We present two new palaeolake archives of Pheneos and Kaisari, Peloponnese, and compare them with records from Stymphalia and Asea by applying the same set of analyses to all sites. We focus on different spatial scales to estimate the validity range of the proxy signals. Geochemical ratios depict hydrological variation and environmental changes over the last 5000 years. They indicate drier phases, but timing and duration vary, which may be explained by site-specific ecosystem responses.
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We present two new palaeolake archives of Pheneos and Kaisari, Peloponnese, and compare them with records from Stymphalia and Asea by applying the same set of analyses to all sites. We focus on different spatial scales to estimate the validity range of the proxy signals. Geochemical ratios depict hydrological variation and environmental changes over the last 5000 years. They indicate drier phases, but timing and duration vary, which may be explained by site-specific ecosystem responses.
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Short summary
This paper reconstructs climatic changes during the last 2600 years in southern Greece based on a sediment core from Lake Trichonida. We provide an age-depth model and continuous geochemical data. Carbonate-rich material is linked to drier/warmer conditions, while terrigenous sediment input was stronger during wetter/colder conditions. Wetter phases coincide with a more negative North Atlantic Oscillation index, suggesting that this is a major driver for precipitation variability in the region.
This paper reconstructs climatic changes during the last 2600 years in southern Greece based on...