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The Upper Jurassic Faïdja Formation (Northwestern Algeria): Sedimentology, biostratigraphy and ichnology

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dc.contributor.author Bouchemla I.
dc.contributor.author Bendella M.
dc.contributor.author Benyoucef M.
dc.contributor.author Lagnaoui A.
dc.contributor.author Ferré B.
dc.contributor.author Scherzinger A.
dc.contributor.author Bel Haouz W.
dc.date.accessioned 2021-02-25T20:43:12Z
dc.date.available 2021-02-25T20:43:12Z
dc.date.issued 2020
dc.identifier.issn 1464-343X
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/162307
dc.description.abstract © 2020 Elsevier Ltd The Faïdja Formation displays mixed siliciclastic-carbonate deposits distributed in three members, which are organised from bottom to top as follows: the Clayey Sandstone Faïdja Member; the Clayey Limestone Bel Aoura Member and the Sandy Claystone Douaouda Member. Sedimentological data indicate the evolution of a subsiding marine environment from the shelf edge to the lower shoreface, sporadically dominated by storms. New age based on recently collected ammonite fauna allowed us to update the age of the Faïdja Formation as Early-Late Kimmeridgian. Ichnological analysis reveals the occurrence of abundant and diverse invertebrate trace fossils, grouped in four ichnoassociations. Ichnoassociation -A- coincides with the lowermost part of the Clayey Sandstone Faïdja Member; it is distinguished by a combination of pre-graphoglyptids and post-depositional traces, ascribed to the distal Cruziana ichnofacies transitional to the Nereites ichnofacies, which indicates a lower offshore zone to shelf edge environment characterised by a low-oxygenated period (anoxic event), frequent storm events and nutrient frequency. Ichnoassociation -B- occupies the middle and upper parts of the Clayey Sandstone Faïdja Member, it is characterised by an abundance of post-depositional traces, corresponding to the archetypal Cruziana ichnofacies that indicates a lower to transitional offshore environment with short phases of low hydrodynamic energy. Ichnoassociation -C- corresponds to the Clayey Limestone Bel Aoura Member that coincides with a drastic facial change and depositional conditions; this association documents a proximal Cruziana ichnofacies, and indicates an upper to transitional offshore zone as a depositional environment. Finally, ichnoassociation -D- coincides with the Sandy Claystone Douaouda Member; it is ascribed to the proximal Cruziana ichnofacies, indicating a lower shoreface environment. The combined sedimentological and ichnological data indicates a relatively subsiding platform with shallowing upwards corresponding to distal, archetypal and proximal Cruziana ichnofacies, respectively.
dc.relation.ispartofseries Journal of African Earth Sciences
dc.subject Ammonite
dc.subject Cruziana ichnofacies
dc.subject Graphoglyptids
dc.subject Invertebrate traces
dc.subject Kimmeridgian
dc.subject Pre-atlas domain
dc.title The Upper Jurassic Faïdja Formation (Northwestern Algeria): Sedimentology, biostratigraphy and ichnology
dc.type Article
dc.relation.ispartofseries-volume 169
dc.collection Публикации сотрудников КФУ
dc.source.id SCOPUS1464343X-2020-169-SID85085506415


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  • Публикации сотрудников КФУ Scopus [24551]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

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