A Hirnantian (latest Ordovician) reefal bryozoan fauna from Anticosti Island, eastern Canada: Taxonomy and chemostratigraphy

Beitrag in einer Fachzeitschrift
(Originalarbeit)


Details zur Publikation

Autorinnen und Autoren: Ernst A, Munnecke A
Zeitschrift: Canadian Journal of Earth Sciences
Jahr der Veröffentlichung: 2009
Band: 46
Heftnummer: 3
Seitenbereich: 207-229
ISSN: 0008-4077
Sprache: Englisch


Abstract


The Natiscotec outcrop on Anticosti Island, Canada (Ellis Bay Formation, Laframboise Member, Hirnantian, Late Ordovician), exposes a patch reef some 20-30 m in diameter, 2-3 m thick, with abundant rugose corals, as well as favositids and heliolitids. Reef capping and flanking sediments include typical Hirnantian brachiopods, such as Hirnantia, Hindella, and Eospirigerina. Within the reef peloidal microbialites encrusting bryozoan colonies are common. The bryozoan fauna includes three cystoporates, seven trepostomes, and three phylloporines. Two genera and two species are new: the cystoporate Natiscotecella tenuis n. gen. and n. sp. and the phylloporine Dilaminocladia natiscotecensis n. gen. and n. sp. Three more species are also new: the cystoporates Ceramopora clara n. sp. and Acanthoceramoporella spinigera n. sp. and the trepostome Revalotrypa honguedensis n. sp. Furthermore, we identify the three trepostomes Atactoporella aff. ortoni (Nicholson, 1874), Hallopora elegantula (Hall, 1852), and Monotrypella cf. aequalis Ulrich, 1882, and a phylloporine Parachasmatopora porkunensis Lavrentjeva, 1985. Four species are identified at generic level and in open nomenclature: the three trepostomes Lioclemella sp., Calloporella sp., and Trepostomata sp. and a phylloporine ? Ralfinella sp. The bryozoan fauna shows some affinities with the Late Ordovician fauna of Scandinavia. Stable carbon isotope investigations from brachiopod shells of the same outcrop yield values for d13C of up to +6.7%, which represent the highest values reported from the Anticosti succession so far. This indicates that the stratigraphic position of the outcrop is at or close to the peak of the globally recognized Hirnantian δC excursion.



FAU-Autorinnen und Autoren / FAU-Herausgeberinnen und Herausgeber

Munnecke, Axel Prof. Dr.
Professur für Paläontologie (Schwerpunkt Faziesanalyse)


Einrichtungen weiterer Autorinnen und Autoren

Universität Hamburg


Zitierweisen

APA:
Ernst, A., & Munnecke, A. (2009). A Hirnantian (latest Ordovician) reefal bryozoan fauna from Anticosti Island, eastern Canada: Taxonomy and chemostratigraphy. Canadian Journal of Earth Sciences, 46(3), 207-229. https://dx.doi.org/10.1139/E09-017

MLA:
Ernst, Andrej, and Axel Munnecke. "A Hirnantian (latest Ordovician) reefal bryozoan fauna from Anticosti Island, eastern Canada: Taxonomy and chemostratigraphy." Canadian Journal of Earth Sciences 46.3 (2009): 207-229.

BibTeX: 

Zuletzt aktualisiert 2018-10-08 um 18:26