Articles | Volume 69, issue 2
E&G Quaternary Sci. J., 69, 247–260, 2020
https://doi.org/10.5194/egqsj-69-247-2020
E&G Quaternary Sci. J., 69, 247–260, 2020
https://doi.org/10.5194/egqsj-69-247-2020
Research article
14 Dec 2020
Research article | 14 Dec 2020

Snail assemblages in Holocene floodplain research – an example from the southern Caucasus

Hans von Suchodoletz et al.

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Cited articles

Adamia, S., Alania, V., Chabukiani, A., Chichua, G., Enukidze, O., and Sadradze, N.: Evolution of the late Cenozoic basins of Georgia (SW Caucasus): a review, in: Sedimentary basin tectonics from the Black Sea and Caucasus to the Arabian Platform, edited by: Sosson, M., Kaymkci, N., Stephenson, R. A., Bergerat, F., and Starostenko, V., Geological Society London Special Publications, London, UK, 239–259, 2010. 
Akhundov, T.: South Caucasus in the Neolithic and Early Bronze Age: The question of epochs and periods, in: A view from the highlands: Archeological studies in honour of Charles Burney, edited by: Sagona, A., Peeters Publishers, Leuven, Belgium, 421–436, 2004. 
Alexandrowicz, W. P.: Molluscan communities in Late Holocene fluvial deposits as an indicator of human activity: A study in Podhale basin in South Poland, Ekologia Bratislava, 32, 111–125, https://doi.org/10.2478/eko-2013-0010, 2013. 
Avsin, N., Vandenberghe, J., van Balen, R., Kiyak, N. G., and Öztürk, T.: Tectonic and climatic controls on Quaternary fluvial processes and river terrace formation in a Mediterranean setting, the Göksu River, southern Turkey, Quat. Res., 91, 533–547, https://doi.org/10.1017/qua.2018.129, 2019. 
Babek, O., Sedlacek, J., Novak, A., and Letal, A.: Electrical resistivity imaging of anastomosing river subsurface stratigraphy and possible controls of fluvial style change in a graben-like basin, Czech Republic, Geomorphology, 317, 139–156, https://doi.org/10.1016/j.geomorph.2018.05.012, 2018. 
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We studied snails from Holocene river sediments of the upper Alazani River in the southeastern Caucasus. Since no natural floodplain forests existed in the river valley until ca. 4500 years ago, our snail data confirm a formerly suggested regional settlement center from the ca. 8000 years unknown thus far. Furthermore, increasing proportions of water-related snails for ca. 4000 years indicate a shift of the river course possibly linked with the formation of the Greater Caucasus.