Lake sediment investigations are currently concentrating on lake Chatyr-Kul in estern Kyrgyzstan, and on the Sary-Chelek Lake in the Chatkal Mountain Range (W-Kyrgyzstan), which has over 200 meter water depth and formed by a huge landslide of unknown age.
From various sub-basins of the Sary-Chelek short gravity cores were obtained with varved sediments. A thick slump found at the base of the cores is most likely caused by a major historical earthquake (Chatkal 1946 AD). As part of student qualification work, the landslide damming the Sary-Chelek, and some associated smaller lakes are currently being examined in more detail. Since 2013, various limnological and meteorological parameters have been measured in and around the Sary-Chelek. These data sets are used to understand the current dynamics of the lake and the paleoclimate proxy data obtained from lake sediments. With its seasonally stratified sediments the Sary-Chelek is a unique climate archive in the region and is to be examined in an even more intensive limnological and sedimentological manner in the future.
Partner:
Dr. Ryskul Usubaliev, Aiperi Zhumalieva (CAIAG Bishkek, Kyrgyzstan)
Prof. Oliver Korup, Katrin Langenwalter (University Potsdam)
Dr. Katja Lindhorst, Dr. Stefan Lauterbach (University Kiel)
Ecenali Ormonaliev, Toktonaly Zunusov (Sary-Chelek National Reserve Authority, Arkit, Kyrgyzstan)
Dr. Martina Stebich (Senckenberg Research Station of Quaternary Palaeontology Weimar, Germany)
Dr. Natalia Ershova (Kyrgyz-Russian Slavonian University Bishkek, Kyrgyzstan)
Gulbara Omorova (Hiking Society, Bishkek, Kyrgyzstan)
Prof. Ermek Baibagyshev (National Agrarian University, Bishkek, Kyrgyzstan)
Dr. Kanayim Teshebaeva (Vrije Universiteit Amsterdam)
Funding:
GFZ, Global Change Observatory Central Asia
Hans-Böckler-Stiftung