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    Volume 43 Issue 8
    Aug.  2018
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    Luo Liang, Wang Dongbing, Chu Daoliang, Wu Qingjie, Li kaicheng, 2018. Biostratigraphy and Geometric Morphometrics of Conchostracans from the Middle Triassic in Southern Lancangjiang Zone. Earth Science, 43(8): 2833-2847. doi: 10.3799/dqkx.2018.158
    Citation: Luo Liang, Wang Dongbing, Chu Daoliang, Wu Qingjie, Li kaicheng, 2018. Biostratigraphy and Geometric Morphometrics of Conchostracans from the Middle Triassic in Southern Lancangjiang Zone. Earth Science, 43(8): 2833-2847. doi: 10.3799/dqkx.2018.158

    Biostratigraphy and Geometric Morphometrics of Conchostracans from the Middle Triassic in Southern Lancangjiang Zone

    doi: 10.3799/dqkx.2018.158
    • Received Date: 2018-03-08
    • Publish Date: 2018-08-15
    • The Triassic volcanic and sedimentary rocks are the important components in the geological records of the southern Lancangjiang zone.However, little is known about the biostratigraphic correlation in this area.In this study, three species and one indeterminate species in one genera of conchostracans were recognized for the first time from the Manghuai Formation of the study area, including Euestheria minuta, Euestheria yipinglangensis, Euestheria dazuensis and Euestheria sp..For the purpose of the comparison, quantitative and semi-quantitative descriptions of the specimens, we took eight standard linear measurements from each well-preserved specimen.A reduced major axis (RMA) regression line has been fitted to the scatter of carapace length versus carapace height, showing a significant linear correlation between them.In addition, the principal component analysis of the linear measurements and fourier coefficients for the outlines of the conchostracan specimens indicates a great deal of intraspecific variations among these four species.Finally, it is suggested that the upper part of the Manghuai Formation in the southern Lancangjiang zone is the Middle Triassic (Ladinian) depositions according to the fossils assemblage and isotopic dating evidences.

       

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