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Bashkirian–Moscovian (Pennsylvanian) conodonts from the pelagic atoll carbonate of the Omi Limestone, Akiyoshi Terrane, central Japan

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2020-01-01

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Article

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00262803

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2-s2.0-85089885985

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Mahidol University

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SCOPUS

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Micropaleontology. Vol.66, No.4 (2020), 351-367

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Yui Takahashi, Sachiko Agematsu, Katsuo Sashida Bashkirian–Moscovian (Pennsylvanian) conodonts from the pelagic atoll carbonate of the Omi Limestone, Akiyoshi Terrane, central Japan. Micropaleontology. Vol.66, No.4 (2020), 351-367. Retrieved from: https://repository.li.mahidol.ac.th/handle/123456789/59055

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Bashkirian–Moscovian (Pennsylvanian) conodonts from the pelagic atoll carbonate of the Omi Limestone, Akiyoshi Terrane, central Japan

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Yui Takahashi
 Sachiko Agematsu
 Katsuo Sashida

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University of Tsukuba
 Mahidol University
 Muroto Geopark Promotion Committee

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© 2020 Micropaleontology Press. All rights reserved. We discriminated Bashkirian to Moscovian (Pennsylvanian) conodont faunas including 19 species of nine genera from the Omi Limestone in the Akiyoshi Terrane and established the following four conodont zones in ascending order, the Declinognathodus noduliferus, Neognathodus symmetricus-Idiognathoides sulcatus sulcatus, “Streptognathodus” expansus, and Mesogondolella clarki Zones. These conodont zones are correlated locally and internationally. The Bashkirian/Moscovian boundary horizon is probably located at the upper part of the “S.” expansus Zone. We further systematically treated obtained conodont species, herein.

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Earth and Planetary Sciences

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https://repository.li.mahidol.ac.th/handle/123456789/59055

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Scopus 2020