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The Black Sea experienced fundamental environmental changes during the last glacial-interglacial transitions. During the last 670,000 years, the Black Sea was at least twelve times connected to Mediterranean Sea, received saltwater via the Bosporus strait, and evolved to a brackish anoxic water body. A lowered global sea level during glacials caused isolation of the basin from the open ocean, and the Black Sea became limnic and well-oxygenated. The last glacial-interglacial history of the Black Sea is relatively well understood and demonstrates the high sensitivity of this basin to global climate and environmental changes. Previous studies particularly focussed on the evolution during the last glacial with meltwater pulses, warming during the glacial-interglacial transition, and the development from a ventilated lake to the present euxinic/brackish water body. Apart from the interglacial warming, the Black Sea sediments clearly recorded short-term abrupt temperature changes associated with cooling during Heinrich events and the Younger Dryas as well the Bølling-Allerød warming, which occurred over the northern hemisphere. However, our knowledge about the Black Sea history before 40,000 BP is comparatively poor even though crucial for understanding hemisphere-wide atmospheric teleconnection patterns and climate mechanisms during older glacials and interglacials. A multiproxy approach has been applied on three gravity cores and surface sediment from the southeastern Black Sea comprising ostracod geochemistry (Mg/Ca, Sr/Ca, U/Ca, 87Sr/86Sr), major and trace elements (Al, Ca, Fe, K, Ti, Mo, Re, Sr, W, Zr) and organic biomarkers (n-alkanes, alkenones, UK’37-palaeotemperatures, glycerol dialkyl glycerol tetraethers, TEX86-palaeotemperatures, BIT-index). The cores cover the last 134,000 a and provide new findings concerning the last and penultimate glacial-interglacial transitions (12,000- 0 a BP; 134,000-120,000 a BP) as well as the abrupt climate changes during the last glacial period (64,000-20,000 a BP). The major topics of this work are i) the penultimate glacial-interglacial transition (Saalian-Eemian), ii) the environmental conditions in the Black Sea “Lake” during abrupt climate oscillations of the last glacial period, iii) and the comparison of the redox evolution during Eemian and Holocene sapropel formation. Two meltwater pulses caused a pronounced freshening of the Black Sea “Lake” during the ending penultimate glacial, which originated from the melting Fennoscandian Ice Sheet. Due to unusually high radiogenic Sr-isotope signatures of benthic ostracods, a potential Himalayan source communicated via the Caspian Sea is also likely. During the glacial-interglacial transition the temperatures in the Black Sea increased from 9°C to 17°C and the associated global sea-level rise allowed the reconnection between the Mediterranean and Black Seas around 128,000 a BP. Eemian sapropel formation started shortly after the intrusion of saltwater and the water body became gradually euxinic. In comparison with the Holocene sapropel, the Eemian proxy records imply warmer and stronger euxinic conditions and distinctly higher enrichments of redox-sensitive trace elements like e.g. Mo, Re, and W. Because the seawater forms the ultimate source for several trace metals, these enrichments were most likely favoured by the higher salinity due to a ca. 10 m higher sea level and enhanced Mediterranean Sea - Black Sea water exchange. Based on biomarker analyses, lake surface temperatures could be calculated for the first time for the period between 64,000 and 20,000 a BP, which includes the Marine Isotope Stage (MIS) 3. Abrupt stadial/interstadial temperature changes with amplitudes of up to 4°C in the Black Sea “Lake” clearly resemble the Greenland Dansgaard-Oeschger pattern. However, an exceptional cooling during the so-called Heinrich events is not evident from our cores. This finding agrees with modelling results proposing a deeper penetration of regular Dansgaard-Oeschger cycles into the Eurasian continent when compared with the Heinrich events. During the warm and more humid interstadials, the Black Sea “Lake” became fresher and more productive and the water level probably increased. During the colder and more arid stadials the freshwater supply was decreased and productivity was low. Aridity and stronger westerly winds favoured the input of aeolian transported detritus. The long-term pattern from 64,000 to 20,000 a BP demonstrates a strong influence of orbital-driven changes in the Eurasian ice volume and associated atmospheric circulation patterns over the Black Sea region. The present multi-proxy study demonstrates that the sediments from the SE Black Sea clearly record not only orbital- but also millennial-scale climate and environmental changes and thus represent an important continental archive for climate change bridging the North Atlantic-Eurasian corridor.
The focus of this study is on the geochronological and paleo-climatic characterization of late Pleistocene glaciations in Turgen and the Khangai Mountains located in central and western Mongolia. These two mountain ranges form a 700 km long NW-SE transect through Mongolia and allow assumptions of the temporal and causal dynamics of the regional late Quaternary glaciations and their correlation to other mountain glacier records from Central and High Asia. In order to evaluate extent and timing of the Pleistocene glaciations in Mongolia, geomorphological mapping and cosmogenic radionuclide (CRN) surface exposure dating (10Be) were carried out in four valley systems located in the Khangai and Turgen Mountains. Additionally, a coupled 2-D surface energy balance and ice flow model was used to determine steady-state conditions for glaciers under various climatic scenarios. With this model it is possible to test combinations of temperature and precipitation settings, which would produce glacier configurations that fit the field-mapped ice extent. In total, 47 glacial boulders and roche moutonnées were sampled, prepared and AMS measured to determine the absolute timing of moraine formation and ice retreat based on 10Be surface exposure dating. Of these, 27 samples were obtained from the Khangai Mountains (three separate moraine sequences) and 20 samples were taken from the Turgen Mountains (two moraine sequences). The dating results (presented as minimum ages) give evidence for a late Pleistocene maximum ice expansion during late MIS 5 (81−78 ka) and major ice advances during MIS 2 (26−20 ka) in both mountain ranges. Only in the Khangai Mountains (central Mongolia) very significant glacier advances also occurred during mid-MIS 3 (49−35 ka), which exceeded the ice limits set during the MIS 2 glaciation. A final ice position, constructed shortly before the onset of full ice retreat was formed between 19-16 ka, and is likely to represent a recessional ice stillstand, or alternatively a final ice readvance during the early part of the last-glacial-interglacial-transition (LGIT) in both mountain ranges. Energy/mass balance and ice flow modeling results suggest that climatic conditions during the MIS 5 and MIS 3 maximum advances in the Khangai Mountains were depressed between a ∆T of -6.0 to -5.2 °C with a precipitation factor of 1.25-1.75 (P = 125-175 %, compared to modern conditions), and a ∆T of -5.3 to -4.4 °C (P = 75-125 %), respectively. For the MIS 2 ice advances modeling results from the Turgen and Khangai Mountains suggest a temperature depression ∆T of -5.7 to -4.6 °C (at 22 ka; P = 25-50 %) in the East-Turgen, and a ∆T of -7.5 to -6.6 °C (at 20 ka; P = 25-50 %) in the Chulut area (Khangai Mountains). These results document a 1.8 - 2 °C difference of the modeled temperatures required to expand the studied paleo-glaciers in the Turgen and Khangai mountains to their field-mapped MIS 2 ice limits, highlighting a spatially differentiated pattern of paleo-temperature lowering across the studied 700 km NW-SE transect. Taken together, the presented record indicates that the largest ice advance in both investigated mountain ranges occurred during the MIS 5 / MIS 4 transition, despite earlier suggestions by previous studies that the local glacial maximum would be associated with the coldest periods of the last glacial cycle (i.e. MIS 4 or MIS 2). Glacier systems in the Khangai Mountains also increased substantially during MIS 3 (local LGM) in response to cool but comparable wet conditions, probably with a greater-than-today input from winter precipitation and an additional input of recycled moisture from expanded paleo-lakes in the Valley of the Great Lakes. The lack of a severe cooling during the MIS 3 ice advances, and probably also during the late MIS 5 ice expansion, suggests that variations in atmospheric circulation patterns, with its significance for controlling the regional precipitation/moisture supply, was a key driver for these late Pleistocene ice advances in Mongolia. This notwithstanding, there is also clear evidence for the development of an extensive glaciation during MIS 2, coinciding with a period of severe cooling and hyperarid conditions. This highlights that glacier systems in Mongolia responded sensitively, both, to variations in moisture supply and its seasonal distribution, and to the marked insolation minima during the last glacial cycle.