The camerate crinoid Scyphocrinites Zenker in the Upper Silurian or Lower Devonian of New Brunswick, Canada

Auteurs-es

  • Stephen K. Donovan Naturalis Biodiversity Center, Leiden, the Netherlands
  • Randall F. Miller

DOI :

https://doi.org/10.4138/atlgeol.2014.014

Mots-clés :

Paleontology, Crinoidea, Stratigraphy, Preservation

Résumé

The mid-Paleozoic Scyphocrinites Zenker has a distal attachment modified into a globular flotation structure and, uniquely for a crinoid, joined the obligate plankton. Such a flotation structure has been found in the Indian Point Formation (Pridolian to Lochkovian) of Flatlands, northern New Brunswick. It is most likely Pridolian (Upper Silurian) based on the primitive morphology. This identification is confirmed by the globular gross morphology, multi-plated calcite structure, age and similarity to coeval fossils from Cornwall, southwestern England.

Biographie de l'auteur-e

Stephen K. Donovan, Naturalis Biodiversity Center, Leiden, the Netherlands

Researcher with 34 years experience of Lower Paleozoic crinoids

Téléchargements

Publié-e

2014-12-02

Comment citer

Donovan, S. K., & Miller, R. F. (2014). The camerate crinoid Scyphocrinites Zenker in the Upper Silurian or Lower Devonian of New Brunswick, Canada. Atlantic Geoscience, 50, 290–296. https://doi.org/10.4138/atlgeol.2014.014

Numéro

Vol. 50 (2014)

Rubrique

Articles

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