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Permian ammonoids Prostacheocers and Perrinites from the southern Kitakami Massif, Northeast Japan

Published online by Cambridge University Press:  20 May 2016

Masayuki Ehiro ,
Hitoshi Hasegawa  and
Akihiro Misaki
Masayuki Ehiro
Affiliation:
The Tohoku University Museum, Sendai 980-8578, Japan,
Hitoshi Hasegawa
Affiliation:
Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan
Akihiro Misaki
Affiliation:
Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan
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Extract

Permian shallow marine strata are widely distributed in the Southern Kitakami Massif, Northeast Japan. They yield many marine fossils and have been well studied both stratigraphically and biostratigraphically. However, the geological age of the upper part of the Permian in the Tassobe district, located in the northern part of the Southern Kitakami Massif (Fig. 1), is still an unsettled question. The Permian is divided into the lower Tassobe and upper Sotokawame Formations (Okuyama, 1980; Yoshida et al., 1992). Early Permian (Sakmarian–Artinskian) fusulinoideans have been known from the middle to lower-upper part of the Tassobe Formation (Hirokawa and Yoshida, 1956; Saito, 1968; Yoshida et al., 1992), whereas no age-diagnostic fossils have been found from the overlying Sotokawame Formation. In the course of the geologic survey of the Permian, we collected two ammonoid fossils from the lower part of the Sotokawame Formation, which can provide us a basis for stratigraphic correlation. This paper describes these ammonoids and discusses their stratigraphic and biogeographic significance.

Type
Paleontological Notes
Information
Journal of Paleontology , Volume 79 , Issue 6 , November 2005 , pp. 1222 - 1228
Copyright
Copyright © The Paleontological Society 

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