2001Dicengxue zazhiRequires access

ON THE FORAMINIFERAL BIOSTRATIGRAPHY IN THE TAIYUAN FORMATION OF JINING COALFIELD (EAST AREA), SHANDONG

Jiang Han

Open publisher page 0 citations

Abstract

Based on the study on the biostratigraphy and foraminifera fauna in the Taiyuan Formation of Jining coalfield (east area) in Shandong province, 28 genera and 155 species of foraminifera have been identified. According to the distribution and vertical variation of foraminifera fossils in the strata, the foraminifera may be distinguished in descending order into 3 assemblages:Ⅲ. Tetrataxis parviconica Nodosaria longa Geinitzina spandeli , Ⅱ . Echinonodosaria echinata Glomospira regularis , Ⅰ. Bradyina sphaeroidea Palaeotextulariae assemblages. Compared with those in nearby regions and some other areas in North China, the geological age of foraminifera fauna in the Taiyuan Formation of Jining coalfield should be the early Early Permian, so the Carboniferous Permian boundary in Jining coalfield (east area) should be placed at the base of No.11 limestone in the Taiyuan Formation.

About this research paper

What this paper is about

Based on the study on the biostratigraphy and foraminifera fauna in the Taiyuan Formation of Jining coalfield (east area) in Shandong province, 28 genera and 155 species of foraminifera have been identified. According to the distribution and vertical variation of foraminifera fossils in the strata, the foraminifera may be distinguished in descending order into 3 assemblages:Ⅲ. Tetrataxis parviconica Nodosaria longa Geinitzina spandeli , Ⅱ . Echinonodosaria echinata Glomospira regularis , Ⅰ. Bradyina sphaeroidea Palaeotextulariae assemblages. Compared with those in nearby regions and some other areas in North China, the geological age of foraminifera fauna in the Taiyuan Formation of Jining coalfield should be the early Early Permian, so the Carboniferous Permian boundary in Jining coalfield (east area) should be placed at the base of No.11 limestone in the Taiyuan Formation.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Based on the study on the biostratigraphy and foraminifera fauna in the Taiyuan Formation of Jining coalfield (east area) in Shandong province, 28 genera and 155 species of foraminifera have been identified. According to the distribution and vertical variation of foraminifera fossils in the strata, the foraminifera may be distinguished in descending order into 3 assemblages:Ⅲ. Tetrataxis parviconica Nodosaria longa Geinitzina spandeli , Ⅱ . Echinonodosaria echinata Glomospira regularis , Ⅰ. Bradyina sphaeroidea Palaeotextulariae assemblages. Compared with those in nearby regions and some other areas in North China, the geological age of foraminifera fauna in the Taiyuan Formation of Jining coalfield should be the early Early Permian, so the Carboniferous Permian boundary in Jining coalfield (east area) should be placed at the base of No.11 limestone in the Taiyuan Formation.

Key concepts: Foraminifera, Biostratigraphy, Geology, Permian, Paleontology, Fauna, Carboniferous, Oceanography

Related papers

Back to paper searchBrowse research topicsOriginal source
ON THE FORAMINIFERAL BIOSTRATIGRAPHY IN THE TAIYUAN FORMATION OF JINING COALFIELD (EAST AREA), SHANDONG — Research Paper | ScholarLens