Articles | Volume 69, issue 2
https://doi.org/10.5194/egqsj-69-165-2020
© 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-69-165-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Reconstruction of palaeoenvironmental variability based on an inter-comparison of four lacustrine archives on the Peloponnese (Greece) for the last 5000 years
Institute for Ecosystem Research, Kiel University, Olshausenstraße 75, 24118 Kiel, Germany
Pavlos Avramidis
Department of Geology, University of Patras, Rio 26504 Patras, Greece
Annette Haug
Institute for Classical Archaeology, Kiel University,
Johanna-Mestorf-Str. 5, 24118 Kiel, Germany
Torben Kessler
Institute for Classical Archaeology, Kiel University,
Johanna-Mestorf-Str. 5, 24118 Kiel, Germany
Arndt Schimmelmann
Department of Earth and Atmospheric Sciences, Indiana University, 1001 E 10th Street, Bloomington, IN 47405-1405, USA
Ingmar Unkel
Institute for Ecosystem Research, Kiel University, Olshausenstraße 75, 24118 Kiel, Germany
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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.
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This article is the preface of the special issue "Quaternary research in times of change – inspired by INQUA Roma 2023". It is a result of the XXI INQUA Congress held in Rome in July 2023. It briefly presents the nine contributions published in this volume.
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E&G Quaternary Sci. J., 69, 139–160, https://doi.org/10.5194/egqsj-69-139-2020, https://doi.org/10.5194/egqsj-69-139-2020, 2020
Short summary
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.
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Short summary
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.
We present two new palaeolake archives of Pheneos and Kaisari, Peloponnese, and compare them...