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    中国百强科技报刊

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    Volume 32 Issue 5
    Sep.  2007
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    CHEN Fen-ning, ZHANG Ke-xin, KOU Xiao-hu, LIN Qi-xiang, ZHENG Zhi-min, XU Ya-dong, 2007. Middle Permian Foramninfera Fauna of the Daguanshan Formation in Xiahe and Tongren Area, West Qinling, China. Earth Science, 32(5): 691-702.
    Citation: CHEN Fen-ning, ZHANG Ke-xin, KOU Xiao-hu, LIN Qi-xiang, ZHENG Zhi-min, XU Ya-dong, 2007. Middle Permian Foramninfera Fauna of the Daguanshan Formation in Xiahe and Tongren Area, West Qinling, China. Earth Science, 32(5): 691-702.

    Middle Permian Foramninfera Fauna of the Daguanshan Formation in Xiahe and Tongren Area, West Qinling, China

    • Received Date: 2007-06-16
    • Publish Date: 2007-09-25
    • The middle Permian Daguanshan Fm., consisting of reef limestone, is well developed in Xiahe County, Gansu Province and Tongren County, Qinghai Province, China. There exist abundant fossils, such as fibrous sponges, calcisponges, bryozoans, foraminiferas, fusulinidas, calcareous algae and corals. Our research is based on 39 species of foramninfera that belong to 27 generas, which include 16 species of fusulinida pertaining to 11 generas. The foraminifera fauna in this area may be divided into two Non-fusulinida assembldges, two fusulinida assembldges and one fusulinida zone respectively in ascending order as follows: Non-fusulinida assembldges: Pachyphloia-Cribrogenerina-Nodosaria and Cribrogenerina-Hemigordius; two fusulinida assembldges: Parafusulina-Pseudofusuluna assembldge, Cancellina cf. houchangensis Zone Afghanella-Sphaerulina assembldge. We compared the Fusulinida assembldges of Daguanshan Formation with the Fusulinida zones worldwide at the same stratum, and concluded that the age of Daguanshan Formation is Luodian-Lengwu stage, Middle Permian.

       

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