A mixed ophiuroid—stylophoran assemblage (Echinodermata) from the Middle Ordovician (Llandeilian) of western Brittany, France

Author:

Hunter Aaron W.12,Lefebvre Bertrand1,Régnault Serge3,Roussel Philippe4,Claverie Roland5

Affiliation:

1. Centre National de la Recherche Scientifique, UMR 5561, Biogéosciences, Université de Bourgogne6 boulevard Gabriel, 21000 Dijon, France (e-mail: aaron.hunter@u-bourgogne.fr)

2. Research School of Earth Sciences, Birkbeck & University College LondonGower Street, Bloomsbury, London WC1E 6BT, UK

3. Muséum d'Histoire naturelle de Nantes12 rue Voltaire 44000 Nantes, France

4. 4 rue Arthur Lemoine de la Borderie56000 Lorient, France

5. Résidence le clos des chênes145 route de Grasse, 06600 Antibes, France

Abstract

AbstractIn the abandoned slate quarry of Guernanic, Gourin (Morbihan, France), a single horizon (Upper Member of the Schistes de Postolonnec Formation) has yielded an exquisitely preserved Llandeilian (Middle Ordovician) echinoderm assemblage composed of the ophiuroid Taeniaster armoricanus sp. nov. and the mitrate Mitrocystella incipiens. These two groups of echinoderms represent the first fossils formally described from the Middle Ordovician of the Gourin area. The brittlestar T. armoricanus sp. nov. is the third and oldest ophiuroid reported so far in the Palaeozoic of the Armorican Massif. The mitrate Mitrocystella is also described for the first time from western Brittany. Taphonomic features of this ophiuroid-stylophoran aggregation suggest that it probably corresponds to the rapid burial of a life assemblage in an otherwise quiet and moderately deep setting (shelf) below, but close to, storm wave base. This echinoderm association represents the oldest evidence for a gregarious mode of life for ophiuroids, as well as the oldest indisputable example of a mixed ophiuroid-stylophoran meadow.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

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