Předboj and Hoher Stein: Two sites of mass roveacrinid occurrence (Crinoidea, Cenomanian, Bohemian-Saxonian Cretaceous Basin)

Author:

Žítt J.,Löser C.,Nekvasilová O.,Hradecká L.,Švábenická L.

Funder

Institute of Geology of the Czech Academy of Sciences

Publisher

Elsevier BV

Subject

Paleontology

Reference102 articles.

1. Integrated Biostratigraphy (Ammonites, Roveacrinoids) at the Cenomanian-Turonian boundary in Southern Tunisia. Colloque sur le Cénomanien, Rouen, France;Abdallah;Bulletin de la Société d'etude des sciences naturelles d'Elbeuf,2001

2. Cenomanian – Coniacian zonation (foraminifers and calcareous algae) in the Guerrero-Morelos basin, southern Mexico;Aguilera-Franco;Revista Mexicana de Ciencias Geológicas,2003

3. Roveacrínidos (Crinoidea: Roveacrinida) del Cenomaniano tardío al Turoniano temprano de Cerritos, oeste de la Plataforma Valles-San Luis Potosí, México;Buitrón Sánchez;Revista de Biologia Tropical,2015

4. Upper Cretaceous;Burnett,1998

5. Roveacrinids (stemless crinoids) in the Albian carbonates of the offshore Santos Basin, southeastern Brazil: stratigraphic, palaeobiogeographic and palaeoceanographic significance;Dias-Brito;Journal of South American Earth Sciences,2001

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