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东昆仑南带加嗡门地区碳酸盐岩地层中发现的中元古代晚期-新元古代早期叠层石组合以大型锥叠层石及其相关的分子Conophytongarganicusvar.inkeni,C.cf.ressotiMenchikov,Jacutophytonf.和Conicodomeniaf.等最丰富,并与Baicalia共生,故可视之为Conophyton—Baicalia组合。该叠层石组合可以与天山和华北等地蓟县系中部—青白口系中部叠层石组合对比,尤其酷似于天山地区蓟县系的爱尔基干组合和华北蓟县系的闪坡岭叠层石组合,而显著有别于华南地块。它还可以与南乌拉尔、西伯利亚、北美、北非和阿拉斯加半岛等地区的中里菲界上部—上里菲界下部层位中的叠层石组合对比。加嗡门叠层石组合的时限为距今1300~850Ma,大致为蓟县纪中期—青白口纪中期或中里菲晚期—晚里菲早期。东昆仑南带存在前寒武纪微地块,当时此微地块的古地理和古环境与天山、华北、西伯利亚和阿拉斯加半岛等地区的前寒武纪地块相似,均位于低纬度区,其上均广泛发育适宜叠层石繁育的温暖陆表海,它们可能共同处于罗迪尼亚超大陆的低纬度大陆边缘部位,与华南地块的不同。这对本区和东昆仑地层和大地构造研究,以及对罗迪尼亚超大陆重建提供了新的古生物约束。
The Late Mesoproterozoic-Early Neoproterozoic monoliths found in the carbonate rock formations in the area of Hummun region in the southern East Kunlun area are dominated by the large conoid strata and their related molecules, Conophytongarganicus var. Ineni, C. cf. Pressot, Menchikov, Jacutophytonf. And Conicodomeniaf. And other most abundant, and Baicalia symbiotic, it can be regarded as the Conophyton-Baicalia combination. The stratigraphic assemblage can be compared with the stratigraphic assemblage of central Jixian-Qingbaikou System in Tianshan and North China, especially resembling the combination of the Aierkegan Formation in Jixian, Tianshan and the Sheupingling stratigraphic assemblage in Jixian, North China , But significantly different from the South China block. It can also be compared with the stratigraphic assemblages in the upper part of the Upper-Middle Philippine-Upper-Felfec, in the Southern Urals, Siberia, North America, North Africa and the Alaskan Peninsula. Plus Hum door laminated stone combination of time interval 1300 ~ 850Ma ago, roughly Jixian Ji Middle - Qingbaikou middle or mid-Philippine late - late Philippine early. Precambrian microfacies exist in the eastern Kunlun area. At that time, the paleogeography and paleoenvironment of the microtitrapies were similar to the Precambrian blocks in the Tianshan, North China, Siberia and Alaskan Peninsula, all located in the lower latitudes Both of them are well-developed for the warm land surface sea of stratigraphic propagation. They may all co-exist in low-latitude continental margins of the Rodinian supercontinent, different from the South China block. This provides new paleontological constraints on the study of stratigraphy and geotectonics in the area and the East Kunlun Mountains and the reconstruction of the Supercontinent of the Rodinia.