Аннотация:Abstract Molar‐tooth carbonate refers to a sort of rock that has ptygmatical folded structure comparable to the ivory. This kind of carbonate exists in a special time range (from Middle to Neoproterozoic). Its origin and the possibility to use it in stratigraphic correlation of the paleocontinent is the key task of the IGCP447, a project on Proterozoic molar tooth carbonates and the evolution of the earth (2001–2005). The importance lies in that the molar‐tooth structure is the key to solving problems related to Precambrian biological and global geochemical events. The molar‐tooth structure is associated with microorganisms. Development and recession of such carbonates have relations with the evolution process of early lives and abrupt changes in sea carbonate geochemistry. In recent years, based on researches on petrology, geochemistry and Sr isotope of molar‐tooth carbonate in the Jilin‐Liaoning and Xuzhou‐Huaiyang area, the authors hold that it can be used as a marker for stratigraphic sequence and sedimentary facies analyses.
