| one publication added to basket [231589] | The recovery of the ostracod fauna after the Late Devonian mass extinction: the Devils Gate Pass section example (Nevada, USA)
Casier, J.G.; Lethiers, F. (1998). The recovery of the ostracod fauna after the Late Devonian mass extinction: the Devils Gate Pass section example (Nevada, USA). C. r. Acad. sci., Sér. 2, Sci. terre planètes 327(7): 501-507. dx.doi.org/10.1016/S1251-8050(99)80079-2
In: Comptes Rendus de l'Académie des Sciences. Série IIA. Sciences de la Terre et des Planètes = Earth and Planetary Science. Gauthiers-Villars: Paris. ISSN 1251-8050; e-ISSN 1778-4107, more
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| Keywords |
Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Upper > Famennian
Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Upper > Frasnian
Ostracoda [WoRMS]
USA, Nevada [Marine Regions]
Marine/Coastal |
| Author keywords |
Ostracods; Frasnian-Famennian boundary; recovery; Nevada |
| Authors | | Top |
- Casier, J.G.
- Lethiers, F.
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| Abstract |
The recovery of the ostracod fauna is rapid after the Late Devonian mass extinction in the Devils Gate Pass section and fifty-nine species have been recognised in the Early Famennian. Forty-five appear for the first time, whereas fourteen others are known from the Late Frasnian (= lazarus species). The ostracod distribution in the Early Famennian at Devils Gate is greatly influenced by regional sedimentological factors principally induced by a drastic sea-level eustatic fall. |
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