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LATE PERMIAN DEEP WATER STRATIGRAPHY IN SHAIWA OF ZIYUN, GUIZHOU

Gao Yong

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Abstract

The Late Permian strata of Shaiwa section can be divided into four parts according to lithostratigraphy and biostratigraphy. One bivalve zone ( Claraia primitiva Hunanopecten exilis zone) and two brachiopod zones ( Neochonetes substrophomenoides Orthothetina ruber zone, Acosarina dorsisulcata Crurithyris speciosa zone) were set up; Wuchiapingian and Changhsingian were separated for the first time from this section based on conodonts, bivalves and brachiopods.

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What this paper is about

The Late Permian strata of Shaiwa section can be divided into four parts according to lithostratigraphy and biostratigraphy. One bivalve zone ( Claraia primitiva Hunanopecten exilis zone) and two brachiopod zones ( Neochonetes substrophomenoides Orthothetina ruber zone, Acosarina dorsisulcata Crurithyris speciosa zone) were set up; Wuchiapingian and Changhsingian were separated for the first time from this section based on conodonts, bivalves and brachiopods.

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Available abstract

The Late Permian strata of Shaiwa section can be divided into four parts according to lithostratigraphy and biostratigraphy. One bivalve zone ( Claraia primitiva Hunanopecten exilis zone) and two brachiopod zones ( Neochonetes substrophomenoides Orthothetina ruber zone, Acosarina dorsisulcata Crurithyris speciosa zone) were set up; Wuchiapingian and Changhsingian were separated for the first time from this section based on conodonts, bivalves and brachiopods.

Key concepts: Biostratigraphy, Paleontology, Geology, Permian, Lithostratigraphy, Stratigraphy, Chronostratigraphy, Sedimentary rock

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