The Middle to Upper Devonian Kuh-e-Bande-Abdol-Hossein section in eastern Central Iran is an overall shallow marine, nearshore to open marine facies setting that contains a highly variable conodont record generally characterised by an Icriodid-Polygnathid biofacies. The lithology and the palaeoenvironmental setting is similar to other localities in Central Iran and exhibits numerous hiatuses. A continuous biostratigraphic record could not be established, but the section preserves the Givetian/Frasnian boundary. Based on the conodont record, major gaps also occur in the Famennian which confirms earlier results reported from other sections of similar palaeoenvironments in Central Iran.

中文翻译：

---

浅水Kuh-e-Bande-Abdol-Hossein段（伊朗中部SE Anarak）的牙形质地层学和牙形质生物相

伊朗中部东部的中上泥盆统Kuh-e-Bande-Abdol-Hossein断面是一个整体浅海，近岸至开放海相环境，其中包含高度可变的牙形石记录，通常以Icriodid - Polygnathid生物相为特征。岩性和古环境与伊朗中部其他地区相似，并表现出许多裂变。无法建立连续的生物地层记录，但该断面保留了纪维天/弗拉西尼亚边界。根据牙形石的记录，在法门尼盆地也存在重大差距，这证实了伊朗中部类似古环境其他部分的早期报道。