Abstract
Two occurrences of Visean ammonoids in the Ural Mountains form the basis for this paper. In the Kzyl-Shin Gorge on the Kiya river, Aktiubinsk province, a bed of gray fragmental limestone, 1 m thick, has yielded the following genera: *Prolecanites, *Pronorites, Beyrichoceras, *Nomismoceras, *Girtyoceras, Trizonoceras, Arcanoceras, and *Goniatites. Also, east of the village of Novosamarskaya on the Sakmara river, Orenburg province, a black limestone block contains the genera marked with an asterisk (*) in the list above, together with Kazalchoceras. The Kzyl-Shin assemblage is of particular interest because it includes Beyrichoceras, generally not found with Goniatites this high in the Carboniferous section. Based on the Goniatites, assignable to the group of G. crenistria Phillips, and other components, the assemblage is dated as very late Visean. It probably is equivalent to the bottom part of the Caney Shale of Oklahoma that contains Girtyoceras meslerianum (Girty) and Goniatitesmultiliratus Gordon. The ...
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.