Yui Takahashi, Yuichi Fukushima, G. Tanaka, Yukio Miyake
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引用次数: 0
摘要
在日本中部福井县Kuzuryu地区的Hida Gaien带Ō tani (=Ohtani或Otani)组的石灰岩块(以前称为Ō boradani组)中发现了以链齿虫为特征的牙形石动物群。区系包括波纹链齿菌、优雅链齿菌、卓越链齿菌、细纹链齿菌、特有链齿菌、贝拉贡多拉菌、G。参:雅草和G。Cf. pohli这些streptognathodid具有广泛的地理分布,表明kasasimovian(晚宾夕法尼亚)时代中晚期,比以往研究中根据fusulinid化石推断的Gzhelian(晚宾夕法尼亚)时代稍早。
Kasimovian (Late Pennsylvanian) conodont fauna from a limestone block in the Ōtani Formation, Kuzuryu area of the Hida Gaien belt, Fukui Prefecture, central Japan
: A conodont fauna characterized by Streptognathodus species was recovered from a limestone block (previously called Ō boradani Formation) of the Ō tani (=Ohtani or Otani) Formation belonging to the Hida Gaien belt distributed in the Kuzuryu area, Fukui Prefecture, central Japan. The fauna consists of Streptognathodus corrugatus , S. elegantulus , S. excelsus , S. gracilis , Idiognathodus sp., Gondolella bella , G . cf. elegantula and G . cf. pohli . These streptognathodids have a wide geographic distribution and indicate a middle–late Kasimovian (Late Pennsylvanian) age, which is slightly older than the Gzhelian (latest Pennsylvanian) age infferred from fusulinid fossils in previ ous studies.