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De Wever, Patrick, O’dogherty, Luis, Caridroit, Martial, Dumitrica, Paulian, Guex, Jean, Nigrini, Catherine, Caulet, Jean-Pierre (2003) Diversity of radiolarian families through time. Bulletin de la Société géologique de France, 174 (5) 453-469 doi:10.2113/174.5.453

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Reference TypeJournal (article/letter/editorial)
TitleDiversity of radiolarian families through time
JournalBulletin de la Société géologique de France
AuthorsDe Wever, PatrickAuthor
O’dogherty, LuisAuthor
Caridroit, MartialAuthor
Dumitrica, PaulianAuthor
Guex, JeanAuthor
Nigrini, CatherineAuthor
Caulet, Jean-PierreAuthor
Year2003 (September 1)Volume174
Issue5
PublisherEDP Sciences
DOIdoi:10.2113/174.5.453Search in ResearchGate
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Mindat Ref. ID530217Long-form Identifiermindat:1:5:530217:2
GUID0
Full ReferenceDe Wever, Patrick, O’dogherty, Luis, Caridroit, Martial, Dumitrica, Paulian, Guex, Jean, Nigrini, Catherine, Caulet, Jean-Pierre (2003) Diversity of radiolarian families through time. Bulletin de la Société géologique de France, 174 (5) 453-469 doi:10.2113/174.5.453
Plain TextDe Wever, Patrick, O’dogherty, Luis, Caridroit, Martial, Dumitrica, Paulian, Guex, Jean, Nigrini, Catherine, Caulet, Jean-Pierre (2003) Diversity of radiolarian families through time. Bulletin de la Société géologique de France, 174 (5) 453-469 doi:10.2113/174.5.453
In(2003, September) Bulletin de la Société géologique de France Vol. 174 (5) EDP Sciences
Abstract/NotesAbstract
The examination of radiolarian biodiversity at the family level through Phanerozoic time reveals some general trends known in other groups of organisms, especially among plankton, while some other trends seem to be quite peculiar. The Permian /Triassic crisis that is one of the most important in the evolution of marine organisms, is marked in radiolarian assemblages by the extinction of two orders (Albaillellaria and Latentifistularia) towards the end of the Permian, and mostly by the tremendous diversification of Spumellaria and Nassellaria in the early-mid Triassic. Radiolarian diversity increased from Cambrian to Jurassic, remained quite stable during the Cretaceous and has decreased slightly since then.


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