in the NE of Iran. An outcrop of this formation in the section of Daddanlou village was studied
palynologically. The study section, 248 meters thick includs gray marl and gray shale, with
interbeded limestone. Based on study of 135 slides of 27 samples taken from this formation
showed the most of the samples contain palynomorphs (dinoflagellates). Additionally, three
forms of Chorate, Cavate, and Proximate have been abserved. In this study 37 species …