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The Kuma formation in the Kuma massif of southern Kyushu, about 900m. thick, consists of remarkable conglomerates, sandstones, shales and subordinately intercalated limestone lenses at four horizonz. ...Fusulinids herein described and illustrated are one new species of Codonofusiella, each one species of Rauserella and Dunbarula?, one new and one previously described species of Schwagerina, one species of Parafusulina?, one new subspecies and one unnamed new form of Pseudodoliolina, one species of Verbeekina?, one new and two previously described species of Yabeina and two new species of Lepidolina. This fauna is characterized by the advanced types of Yabeina and Lepidolina, and is distinctly different from that of Yabeina globosa (=Y. inouyei) zone which has hitherto been regarded as the youngest fusulinid zone in Japan. The former is biologically more advanced than the latter. Based on this fusulinid fauna, the discussions on correlation with conglomerate-bearing late Permian formations in the Japanese Islands and with late Permian of British Columbia and Indochina are presented.続きを見る
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Ⅰ.Introduction and Acknowledgements Ⅱ.A concise account of the Kuma formation Ⅲ.Description of species Ⅳ.Stratigraphic distribution of fusulinids Ⅴ.A summary of the paleontological remarks VI.Correlation VII.Conclusive remarks Bibliography Explanation of plates Illustrations
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Mendeley出力
04_01_p001