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作 者:YANGXiangning JINXiaochi JIZhansheng WANGYizhao YAOJianxin YANGHailin
机构地区:[1]DepartmentofEarthSciences,NanjingUniversity,Nanjing,Jiangsu210093 [2]InstituteofGeology,ChineseAcademyofGeologicalSciences,26BaiwanzhuangRoad,Beijing100037 [3]GeologicalSurveyofYunnan,YujiangRoad,Yuxi,Yunnan653100
出 处:《Acta Geologica Sinica(English Edition)》2004年第1期15-21,共7页地质学报(英文版)
基 金:a grant(No.40232024)from National Science Foundation of China(NSFC).
摘 要:Fossil materials of Shanita and Hemigordius from a section northeast of the Woniusi (the Woniu Temple) of Baoshan, western Yunnan are described and figured in this paper. Field investigation indicates that fossils of these two foraminifer genera are extremely abundant and form a typical Shanita-Hemigordius assemblage in the so-called 'Cracked Limestone' in the Baoshan area. Preliminary study has revealed that the features of this assemblage, which includes Shanita amosi, S. chagouensis, Hemigordius renzi and H. biconcavus, are similar not only to the Shanita fauna previously reported from the Shazipo Formation in the Zhengkang area, west Yunnan, but also to those from the Permian of Burma, Thailand, Iran and Turkey.Fossil materials of Shanita and Hemigordius from a section northeast of the Woniusi (the Woniu Temple) of Baoshan, western Yunnan are described and figured in this paper. Field investigation indicates that fossils of these two foraminifer genera are extremely abundant and form a typical Shanita-Hemigordius assemblage in the so-called 'Cracked Limestone' in the Baoshan area. Preliminary study has revealed that the features of this assemblage, which includes Shanita amosi, S. chagouensis, Hemigordius renzi and H. biconcavus, are similar not only to the Shanita fauna previously reported from the Shazipo Formation in the Zhengkang area, west Yunnan, but also to those from the Permian of Burma, Thailand, Iran and Turkey.
关 键 词:Shanita Hemigordius PERMIAN Baoshan YUNNAN
分 类 号:Q911.7[天文地球—古生物学与地层学] P534.46[生物学—古生物学]
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