@phdthesis{Wegwerth2016,
  author    = {Antje Wegwerth},
  title     = {The glacial and interglacial history of the Black Sea during the last 134 ka: About meltwater events, abrupt temperature changes, and sapropels},
  journal    = {Die glaziale und interglaziale Entwicklung des Schwarzen Meeres w{\"a}hrend der letzten 134.000 Jahre: {\"U}ber Schmelzwasserereignisse, abrupte Temperaturschwankungen und Sapropele},
  url       = {https://nbn-resolving.org/urn:nbn:de:gbv:9-002442-6},
  year      = {2016},
  abstract  = {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 B{\o}lling-Aller{\o}d 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.},
  language  = {en}
}