Abstract
The Sainte-Anne Formation (Châteaupanne Unit, Armorican Massif) consists of immature sandstones conformably deposited upon reefal limestones. Plant debris are abundant in the Saint-Anne sandstones (hence their older name of Schistes et gres a Psilophytes), but only rare crinoids and brachiopods have been found. The faunal content is analyzed in detail, consisting of a few columnals of crinoids and brachiopods (Ambocoelia and Plectodonta minor, the most common species). The distribution in space and time of the genus Plectodonta in Europe is analyzed, and allows proposing an Emsian to early Eifelian age for the Sainte-Anne Fm. Consequently, the Sainte-Anne Fm (Armorican Massif) could be the earliest record of the relief created at the beginning of the Variscan orogeny.
Sign-in/Register to access full text options 
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 callMore From: Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen
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.
