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CRÔNIER, CATHERINE, MALTI, FATIMA ZOHARA, FRANÇOIS, ANGELA, BENYOUCEF, MADANI, BRICE, DENISE (2013) First occurrence of a phacopid trilobite faunule from the Upper Devonian of Saoura Valley, Algeria and biodiversity fluctuations. Geological Magazine, 150 (6) 1002-1021 doi:10.1017/s0016756813000277

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Reference TypeJournal (article/letter/editorial)
TitleFirst occurrence of a phacopid trilobite faunule from the Upper Devonian of Saoura Valley, Algeria and biodiversity fluctuations
JournalGeological Magazine
AuthorsCRÔNIER, CATHERINEAuthor
MALTI, FATIMA ZOHARAAuthor
FRANÇOIS, ANGELAAuthor
BENYOUCEF, MADANIAuthor
BRICE, DENISEAuthor
Year2013 (November)Volume150
Issue6
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756813000277Search in ResearchGate
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Mindat Ref. ID260794Long-form Identifiermindat:1:5:260794:2
GUID0
Full ReferenceCRÔNIER, CATHERINE, MALTI, FATIMA ZOHARA, FRANÇOIS, ANGELA, BENYOUCEF, MADANI, BRICE, DENISE (2013) First occurrence of a phacopid trilobite faunule from the Upper Devonian of Saoura Valley, Algeria and biodiversity fluctuations. Geological Magazine, 150 (6) 1002-1021 doi:10.1017/s0016756813000277
Plain TextCRÔNIER, CATHERINE, MALTI, FATIMA ZOHARA, FRANÇOIS, ANGELA, BENYOUCEF, MADANI, BRICE, DENISE (2013) First occurrence of a phacopid trilobite faunule from the Upper Devonian of Saoura Valley, Algeria and biodiversity fluctuations. Geological Magazine, 150 (6) 1002-1021 doi:10.1017/s0016756813000277
In(2013, November) Geological Magazine Vol. 150 (6) Cambridge University Press (CUP)
Abstract/NotesAbstractPhacopid trilobites are relatively widespread in Devonian deposits of north Gondwana and some have been collected from several sections of the Saoura Valley in SW Algeria. New occurrences of phacopids assigned to Trimerocephalus, Dianops and Phacops sensu lato are described from this area and comparisons are made with closely allied species from Morocco and Europe. The trilobite assemblages of the ‘Argiles de Marhouma’ Formation are considered to be Frasnian–Famennian in age. These new occurrences have been integrated into an analysis of Upper Devonian phacopid biodiversity. Diversity fluctuations reflect environmental changes, bioevents and stratigraphic turnovers throughout the Upper Devonian. Peak diversity was attained after the post-Kellwasser event.


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