Mid- to late Holocene climate-driven regime shifts inferred from diatom, ostracod and stable isotope records from Lake Son Kol (Central Tian Shan, Kyrgyzstan)

Anja Schwarz, Falko Turner, Stefan Lauterbach, Birgit Plessen, Kim J. Krahn, Sven Glodniok, Steffen Mischke, Martina Stebich, Roman Witt, Jens Mingram, Antje Schwalb

Rannsóknarafurð: Framlag til fræðitímaritsGreinritrýni

21 Tilvitnanir (Scopus)

Útdráttur

Arid Central Asia represents a key region for understanding climate variability and interactions in the Northern Hemisphere. Patterns and mechanisms of Holocene climate change in arid Central Asia are, however, only partially understood. Multi-proxy data combining diatom, ostracod, sedimentological, geochemical and stable isotope analyses from a ca. 6000-year-old lake sediment core from Son Kol (Central Kyrgyzstan) show distinct and repeated changes in species assemblages. Diatom- and ostracod-inferred conductivity shifts between meso-euhaline and freshwater conditions suggest water balance and regime shifts. Organism-derived data are corroborated by stable isotope, mineralogical and geochemical records, underlining that Son Kol was affected by strong lake level fluctuations of several meters. The δ13Ccarb18Ocarb correlation shows repeated switchovers from a closed to an open lake system. From 6000 to 3800 and 3250 to 1950 cal. yr BP, Son Kol was a closed basin lake with higher conductivities, increased nutrient availability and a water level located below the modern outflow. Son Kol became again a hydrologically open lake at 3800 and 1950 cal. yr BP. Comparisons to other local and regional paleoclimate records indicate that these regime shifts were largely controlled by changing intensity and position of the Westerlies and the Siberian Anticyclone that triggered changes in the amount of winter precipitation. A strong influence of the Westerlies ca. 5000–4400, 3800–3250 and since 1950 cal. yr BP enhanced the amount of precipitation during spring, autumn and winter, whereas cold and dry winters prevailed during phases with a strong Siberian Anticyclone and southward shifted Westerlies at ca. 6000–5000, 4400–3800 and 3250–1950 cal. yr BP. Similarities between variations in winter precipitation at Son Kol and records of the predominant NAO-mode further suggest a teleconnection between wet (dry) winter climate in Central Asia and a positive (negative) NAO-mode. Thus, this study identifies climate fluctuations as the main driver for hydrological regime shifts in Son Kol controlling physicochemical conditions and consequently causing abrupt species assemblage changes. This emphasizes the importance of multi-proxy approaches to identify triggers, thresholds and cascades of aquatic ecosystem transformations.

Upprunalegt tungumálEnska
Síður (frá-til)340-356
Síðufjöldi17
FræðitímaritQuaternary Science Reviews
Bindi177
DOI
ÚtgáfustaðaÚtgefið - 1 des. 2017

Athugasemd

Funding Information:
This study was financially supported by the German Federal Ministry of Education and Research (BMBF) within the joint research project CADY (Central Asian Climate Dynamics, grant no. 03G0813 ). We thank Dieter Berger (GFZ Potsdam), Sagynbek Orunbaev and Kalia Jusupova (both CAIAG Bishkek) for their help during field work, Daniela Misch (TU Braunschweig) for technical assistance in the laboratory, Katharina Ptach and Cornelia Fischer (both TU Braunschweig) for their help with the ostracod preparation and analyses and Sylvia Pinkerneil, Ted Moldenhawer and Yvonne Beutlich (all GFZ Potsdam) for their help with the geochemical analyses. The Karatal-Japyryk State Nature Reserve in Naryn (Kyrgyzstan) kindly provided permission to access Son Kol.

Publisher Copyright:
© 2017 Elsevier Ltd

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