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Marine vertebrate remains from the Toarcian – Aalenian succession of Southern Beaujolais, Rhône, France

By: Vincent, Peggy.
Contributor(s): Martin, Jeremy E | Fischer, Valentin | Suan, Guillaume | Khalloufi, Bouziane | Sucheras-Marx, Baptiste | Lena, Alex | Janneau, Kevin | Rousselle, Bruno | Rulleau, Louis.
Material type: ArticleArticleDescription: 822-834pp ; maps; ; Illustration.Subject(s): Diversity | France | Jurassic | Marine vertebrates In: Geological magazine : Vol. 150 Iss. 1-6 Year. 2013Summary: A previously undocumented marine vertebrate fauna comprising ichthyosaur, plesiosaur, marine crocodilian and fish remains from the Toarcian–Aalenian succession at Lafarge quarry, southern Beaujolais (Rhône, France) is described on the basis of both historical collections and new discoveries. The taxonomic composition of the Lafarge quarry marine vertebrate assemblage highlights its cosmopolitan nature and strong relationships with taxa known from elsewhere in Europe. Several groups are recorded for the first time in the Toarcian–Aalenian succession of France, implying new palaeobiogeographic interpretations and prompting discussion of marine amniote diversity during this interval.
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Article Article Library and Information Centre
Periodical Section
Bound Journal Collection Not for loan 002531_54
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002531

A previously undocumented marine vertebrate fauna comprising ichthyosaur, plesiosaur, marine crocodilian and fish remains from the Toarcian–Aalenian succession at Lafarge quarry, southern Beaujolais (Rhône, France) is described on the basis of both historical collections and new discoveries. The taxonomic composition of the Lafarge quarry marine vertebrate assemblage highlights its cosmopolitan nature and strong relationships with taxa known from elsewhere in Europe. Several groups are recorded for the first time in the Toarcian–Aalenian succession of France, implying new palaeobiogeographic interpretations and prompting discussion of marine amniote diversity during this interval.

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