Global Geology    2020 23 (4): 199-213   ISSN: 1673-9736  CN: 22-1371/P   New palaeoclimatic insights on the Late Cretaceous environments of Mongolia based on the isotope data (δ13C, δ18O) of dinosaur eggshells and pedogenic carbonates from Bayn Dzak section S. V. Naugolnykh, V. N. Kuleshov Geological Institute of Russian Academy of Sciences, Moscow 101135, Russia 收稿日期 2020-08-02  修回日期 2020-09-03  网络版发布日期 null 参考文献  Andrews R C. 1932. The new conquest of Central Asia, natural history of Central Asia. Part I. New York:American Museum of Natural History, 1-687. Barsbold R, Khand Y. 2008. The non-marine Cretaceous of Mongolia//Paleoclimates in Asia during the Cretaceous:their variations, causes, and biotic and environmental responses. Ulaanbaatar:Paleontological Center of Mongolian Academy of Sciences, 13-16. Barsbold R, Khand Y, Tsogtbaatar K, et al. 2012. Geology and mineral resources of Mongolia. Volume II. Paleontology. Ulan-Bator:Soembo, 1-529. 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Chinese Journal of Geochemistry, 19(1):29-34. 通讯作者: S. V. Naugolnykh