Abstract
Abstract The boundary between Cenomanian and Turonian (upper Cretaceous) beds in the upper basin of the Esteron river (Alpes-Maritimes, France) is defined on the basis of ammonites and pelagic foraminifera. The rich faunas of these beds are especially important because Cenomanian and Turonian beds in southeastern France are normally very poor in fossils.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
