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Zhegallo, E.A., Rozanov, A.Yu., Ushatinskaya, G.T., Hoover, R.B., Gerasimenko, L.M. and Ragozina, A.L. (2000) Atlas of Microorganisms from Ancient Phosphorites of Khubsugul (Mongolia). Huntsville, Alabama, 167.

has been cited by the following article:

  • TITLE: Concerning the Original Viewpoint of Biogeologic Accumulation of the Old Bedded Phosphorites in the Khubsugul and Zavkhan Basins of Mongolia

    AUTHORS: Dorj Dorjnamjaa, Gundsambuu Altanshagai

    KEYWORDS: Khubsugul, Zavkhan, Basin, Phosphorite, Fossils, Biota, Accumulation

    JOURNAL NAME: Open Journal of Geology, Vol.5 No.9, September 29, 2015

    ABSTRACT: This paper concerns deals withbiogeologicaccumulation and their peculiarities, lithological unites of the phosphorite-bearing formations of these basins and an evolution of the old biota. Old bedded phosphorites are believed to be connected with specific biogeological events happening in the Neoproterozoic glaciation, which was followed by rapid deglaciation,Ediacaran bioradiation and the “great” postglacial transgression bearing phosphorites at its initial phase. The Mongolian phosphate basins give evidence of this phenomenon. Khubsugul basin is located in the northern Mongolia. The Neoproterozoic-Cambrian phosphorite-bearing khubsugul group is subdivided into 3 formations as ongolik, kheseen and erkhelnuur which are rich in organic fossils (a group of cyanobacterial mats, archaeocyaths, trilobites) in the ascending order. The Zavkhan basin lies in the western Mongolia. The Ediacaran-lower Cambrian sediments are divided into five formations: Maikhanuul (diamictites), Tsagaanolom (phosphorite-bearing carbonate), Bayangol, Salaanygol and Khairkhan. All the formations contain the paleontological fossils (algae, sponges, cyanobacterial mats, ichnocoenosis, soft-bodied fauna, archaeocyaths, etc.). Bedded phosphorites are the object for comprehensive research of bacterial paleontology. It is shown at example of the Mongolian Khubsugul and Zavkhan sea shelf phosphate basins. The expounded actual material clearly shows that the heterogeneous biologic activity, suitable geologic (transgressive systems tracts) and paleogeographic (glaciations, warm climate, etc.) conditions played an important role in the formation and accumulation of the biogenic bedded phosphorites.