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Morphology of Molar-Tooth Structures in Neoproterozoic and Its Indication Significance for the Depositional Environment of Jinshitan Area in Dalian, Eastern Liaoning Province

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摘要

Exemplified by “molar tooth” (MT) from Neoproterozoic Xingmincun Formation of Jinshitan in Dalian, this paper studied its morphological characteristics and analyzed its indication significance for sedimentary environment. A series of MT with complicated morphologies are developed in limestone of Upper Xingmingcun Formation. On the basis of a detailed observation, molar teeth are divided into ribbon, short-straight bar, worm, filamentous, dotted and detritus forms, with the ribbon form being dominant. Some sedimentary rhythms composed of silt-carbonates, micrite-carbonates, laminated carbonates and mud-carbonates were identified. Molar teeth were formed in the lower part of shallow subtidal-intertidal microfacies. It is thus concluded that different sets of morphology represent different lithofacies or rhythmic units, showing the indication significance for the morphology of MT.

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