Hydrological (in)stability in Southern Siberia during the Younger Dryas and early Holocene

被引:6
作者
Harding, P. [1 ,2 ]
Bezrukova, E., V [3 ,4 ]
Kostrova, S. S. [3 ,5 ]
Lacey, J. H. [6 ]
Leng, M. J. [6 ,7 ]
Meyer, H. [5 ]
Pavlova, L. A. [3 ]
Shchetnikov, A. [8 ,9 ,10 ]
Shtenberg, M., V [11 ]
Tarasov, P. E. [12 ]
Mackay, A. W. [1 ]
机构
[1] UCL, Environm Change Res Ctr, Dept Geog, London WC1E 6BT, England
[2] Royal Holloway Univ London, Dept Geog, Ctr Quaternary Res, Egham TW20 0EX, Surrey, England
[3] SB RAS, Vinogradov Inst Geochem, Irkutsk 664033, Russia
[4] SB RAS, Irkutsk Sci Ctr, Irkutsk 664033, Russia
[5] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Res Unit Potsdam, D-14473 Potsdam, Germany
[6] British Geol Survey, Natl Environm Isotope Facil, Keyworth NG12 5GG, Notts, England
[7] Univ Nottingham, Ctr Environm Geochem, Sch Biosci, Loughborough LE12 5RD, Leics, England
[8] SB RAS, Inst Earths Crust, Irkutsk 664033, Russia
[9] Irkutsk State Univ, 2 Chkalov St, Irkutsk 664003, Russia
[10] Russian Acad Sci, Geol Inst, Pyzhevsky Lane 7, Moscow 119017, Russia
[11] UB RAS, Inst Mineral, Miass 456317, Russia
[12] Free Univ Berlin, Inst Geol Sci, Palaeontol, D-12249 Berlin, Germany
关键词
LGIT; Siberia; Paleoclimate; Paleohydrology; Stable-isotopes; Diatoms; OXYGEN-ISOTOPE RECORD; ABRUPT CLIMATE-CHANGE; LAST GLACIAL MAXIMUM; LAKE BAIKAL REGION; HIGH-RESOLUTION; CENTRAL-ASIA; CONTAMINATION SIGNALS; DIATOM DISSOLUTION; BOTTOM SEDIMENTS; LATE PLEISTOCENE;
D O I
10.1016/j.gloplacha.2020.103333
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Southern Siberia is currently undergoing rapid warming, inducing changes in vegetation, loss of permafrost, and impacts on the hydrodynamics of lakes and rivers. Lake sediments are key archives of environmental change and contain a record of ecosystem variability, as well as providing proxy indicators of wider environmental and climatic change. Investigating how hydrological systems have responded to past shifts in climate can provide essential context for better understanding future ecosystem changes in Siberia. Oxygen isotope ratios within lacustrine records provide fundamental information on past variability in hydrological systems. Here we present a new oxygen isotope record from diatom silica (delta O-18(diatom)) at Lake Baunt (55 degrees 11'15 '' N, 113 degrees 01,45 '' E), in the southern part of eastern Siberia, and consider how the site has responded to climate changes between the Younger Dryas and Early to Mid Holocene (ca. 12.4 to 6.2 ka cal BP). Excursions in delta O-18(diatom) are influenced by air temperature and the seasonality, quantity, and source of atmospheric precipitation. These variables are a function of the strength of the Siberian High, which controls temperature, the proportion and quantity of winter versus summer precipitation, and the relative dominance of Atlantic versus Pacific air masses. A regional comparison with other Siberian delta O-18(diatom) records, from lakes Baikal and Kotokel, suggests that delta O-18(diatom) variations in southern Siberia reflect increased continentality during the Younger Dryas, delayed Early Holocene warming in the region, and substantial climate instability between similar to 10.5 to similar to 8.2 ka cal BP. Unstable conditions during the Early Holocene thermal optimum most likely reflect localised changes from glacial melting. Taking the profiles from three very different lakes together, highlight the influence of site specific factors on the indi-vidual records, and how one site is not indicative of the region as a whole. Overall, the study documents how sensitive this important region is to both internal and external forcing.
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页数:15
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