Eustatic trends in conodont diversity across the Frasnian–Famennian boundary in the stratotype area, Montagne Noire, Southern France
- 1 December 1996
- journal article
- Published by Scandinavian University Press / Universitetsforlaget AS in Lethaia
- Vol. 29 (4) , 329-337
- https://doi.org/10.1111/j.1502-3931.1996.tb01668.x
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Destabilization of the oceanic density structure and its significance to marine “extinction” eventsPublished by Elsevier ,2003
- Definition of the Frasnian/Famennian Stage boundaryEpisodes, 1993
- Anoxic events in the late Frasnian—Causes of the Frasnian-Famennian faunal crisis?Geology, 1993
- Conodont biofacies patterns in the Kellwasser Facies (upper Frasnian/lower Famennian) of the eastern Anti-Atlas, MoroccoPalaeogeography, Palaeoclimatology, Palaeoecology, 1992
- Decision on the Devonian-Carboniferous boundary stratotypeEpisodes, 1991
- The global Frasnian-Famennian »Kellwasser Event«International Journal of Earth Sciences, 1991
- Decision on the Boundary Stratotype for the Middle/Upper Devonian Series BoundaryEpisodes, 1987
- Facies patterns and depositional environments of Palaeozoic cephalopod limestonesSedimentary Geology, 1985
- Devonian eustatic fluctuations in EuramericaGSA Bulletin, 1985
- Late Devonian icriodontid biofacies models and alternate shallow-water conodont zonationPublished by Geological Society of America ,1984