Abstract
Two species of a new Tremadocian (Early Ordovician) conodont genus from the Saint Chinian Formation of the southern Montagne Noire, France, are erected: Hammannodus sarae gen. et sp. nov. and Hammannodus juliae gen. et sp. nov. They were found within a single storm-induced limestone nodule interbedded with offshore shales belonging to the regional Shumardia (C.) pusilla (trilobite) Biozone, and to the Paltodus deltifer deltifer (conodont) Subzone. This conodont record is associated with the episodic development of carbonate productivity in temperate waters of the Montagne Noire platform, a process absent in neighbouring platforms of north-west Gondwana. The apparatus is composed of five coniform pyramidal elements occupying P and S positions and one bicostate element in the M position, having three or two sharp costae, respectively, with a subtriangular basal outline. © 2007 The Palaeontological Association.
Author supplied keywords
Cite
CITATION STYLE
Serpagli, E., Ferretti, A., Vizcaïno, D., & Álvaro, J. J. (2007). A new Early Ordovician conodont genus from the southern Montagne Noire, France. Palaeontology, 50(6), 1447–1457. https://doi.org/10.1111/j.1475-4983.2007.00714.x
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.