Перегляд за Автор "Chepalyga, A. L."

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    Aminostratigraphy of coastal sedimentary sequences, Kerch Strait, northeastern Black Sea
    (S.n., 2008) Янко-Хомбах, Валентина Венедиктівна; Кадурін, Сергій Володимирович; Чепалига, Андрій Леонідович; Ніколас, В. А.; Мюррей-Уоллес, К. В.; Чівас, А. Р.; Янко-Хомбах, Валентина Венедиктовна; Кадурин, Сергей Владимирович; Чепалыга, Андрей Леонидович; Николас, В. А.; Мюррей-Уоллес, К. В.; Чивас, А. Р.; Yanko-Hombach, Valentyna V.; Kadurin, Serhii V.; Chepalyga, A. L.; Murray-Wallace, C. V.; Nicholas, W. A.; Chivas, A. R.
    The principal methods used to constrain the timing of sea-level and environmental changes for the Last Interglacial sedimentary sequences have been Uranium-series and luminescence dating. An alternative to these, used with success in studies on Australian coastal sedimentary sequences, is the amino acid racemization geochronological technique. Recent technological (Bruckner et al., 1991) and methodological developments (Kaufman and Manley, 1998; Hearty et al., 2006) now allow for calibrated age determinations on suitable skeletal carbonates including individual foraminifers and ostracods.
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    Документ
    Black Sea and Caspian Basins in Late Pleistocene: sea-level changes, climate and early human settlement
    (S.n, 2008) Dolukhanov, P. M.; Chepalyga, A. L.; Lavrentiev, N. V.; Kadurin, Serhii V.; Larchenkov, Yevhenii P.; Shkatova, V. K
    The climate of northern Eurasia during the Middle Wiirm/Valdai 'megainterstadial' (OIS 3), which lasted from c. 58 to 23 ka, was cool and unstable, with at least five milder oscillations (including the 'Bryansk interstadial'). The estimated summer and winter temperatures in Eastern Europe were lower than today by 4-6°C and 4-10°C, and the annual precipitation, as low as 150-250 mm (Frenzel et al.,1992).
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    Parutino
    (Astroprint, 2006) Konikov, Yevhenii G.; Chepalyga, A. L.
    The stratotype of the Bugsky horizon (Veklich, Sirenko, 1972)is located near the northern outskirts of Parutino and represents a natural outcrop on the erosional shore of Dniepero-Bugsky Liman. The slope reaches 17-20 min height.The stratigraphic section reveals the Upper Pleistocene loess-paleosol formations overlying Pliocene-Quaternary fluvio-lacustrine sediments (Fig. 6).It, in turn,is overlain by Dofinophinovskaya or Bryanskaya (Velichko, 1990)soil with a date of 26-30 ky BP.