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From the present investigation and analysis, there are two Jurassic black rock series in Qiangtang Basin, Tibet. One is in the Shuanghu-Sewa where the different lithological types develop such as mudstones, marls, oil shales and etc. The other is in the Bailongbinghe-Amdo as limestones, marls, shales and so on. In the Shuanghu-Sewa area, many geologists have worked and got achievements. For example, Sun et al. found Harpoceratacea ammonites in the Zamunaqu profile in 1979, which showed the marine Jurassic strata crop out.

1986; van der Merwen and Medina, 1989), and have heavier carbon isotope values when hot and dry (Ehleringer, 1993). Therefore, it is concluded that at the beginning of the Early Jurassic the climate is warmer and more humid than before and afterward. The sudden creasing of fern spores and the distinct negative excursion of organic carbon isotope in the 24 lowest member of Jurassic of the Haojiagou section are similar with some other sections. It may reflect a globally climatic change. , et al.

On the basis of our study, we suggest these strata are of the same age in spite of Quse Formation, or Zesong Formation, or Bilong Formation. In other words, there are transition strata of deep water continental shelf, to slope, and to the deep water basin different from the Yanshiping Group of platform or Mugagangri Group of deep water flysch facies. Above-mentioned results showed it is wrong of only shallow water deposits in the Qiangtang basin. , which are the index fossils of Hettangian stage in the southern Tibet; (2) Arietites-Suiciferites assemblage: mainly includes Arnioceras, Arietites, Baucaulticeras, Geviceras and so on, which compares to the Arnioceras seruicostatum zone and A.

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Short papers for the 8th International Congress on the Jurassic System―Marine and non-marine Jurassic

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