Tethys. Specimens have been recovered from carbonate, siliciclastic, volcanoclastic or
mixed carbonate/siliciclastic successions dated from the late Santonian or early Campanian
to the latest Maastrichtian, but often only fragmented shells have been collected and
described. Many species have been established but the constructional morphology of
individuals and, in particular, the characters of the outer shell layer were seldom adequately …
M TENTOR - deu.edu.tr
The genus Pseudopolyconites is distributed in Upper Cretaceous successions of the Central
Tethys. Specimens have been recovered from carbonate, siliciclastic, volcanoclastic or
mixed carbonate/siliciclastic successions dated from the late Santonian or early Campanian
to the latest Maastrichtian, but often only fragmented shells have been collected and
described. Many species have been established but the constructional morphology of
individuals and, in particular, the characters of the outer shell layer were seldom adequately …