Cambrian microfossils from the High Atlas, Morocco: Taxonomic, biostratigraphic, palaeobiogeographic, and depositional significance of the Brèche à Micmacca limestone beds

TitleCambrian microfossils from the High Atlas, Morocco: Taxonomic, biostratigraphic, palaeobiogeographic, and depositional significance of the Brèche à Micmacca limestone beds
Publication TypeJournal Article
Year of Publication2023
AuthorsMghazli, K, Lazreq, N, Geyer, G, Landing, E, Boumehdi, MA, Youbi, N
JournalJournal of African Earth Sciences
Volume197
Pagination104751
ISSN1464343X
Abstract

Diverse helcionelloid molluscs (link is external), probable polychaetes, and sclerites (link is external) of other metazoan (link is external) groups are described from the Brèche à Micmacca Member at section Le IX in the Lemdad syncline (link is external) in the High Atlas, southern Morocco. The collections include more than 3,000 specimens and complement earlier described faunal assemblages from this interval. The new material includes 21 species of 13 genera, with 15 helcionelloid species (or forms), one supposed orthothecid hyolith, and 5 pseudopelagielliform species. They record a relatively limited amount of biotic change through the Morocconus notabilis and Ornamentaspis frequens trilobite (link is external) biozones in the Souss Basin. Eotebenna cf. papilio Runnegar and Jell1976, is the first record of the genus in Africa and West Gondwana (link is external). Dorispira? lemdadensis n. sp., Yochelcionella longituba n. sp., and Yochelcionella gracilituba n. sp. are proposed. The Le XI associations are compared with those from other localities of the Brèche à Micmacca Member in terms of their biostratigraphic and palaeoecological implications. The assemblages include forms that are similar to those from coeval faunas from the Siberian Platform, North China, Australia, and Laurentia (link is external) (SNAL) and assist in interregional and continental biostratigraphic correlation and the understanding of palaeogeographic connections. This study concludes that Lower–Middle Cambrian boundary interval trilobites and small shelly fossils comprise a West Gondwanan assemblage (i.e., Morocco, Iberia, Saxo-Thuringia) that differs from palaeogeographically distant coeval faunas from tropical SNAL regions.

URLhttps://www.sciencedirect.com/science/article/abs/pii/S1464343X2200303X (link is external)
DOI10.1016/j.jafrearsci.2022.104751 (link is external)
Short TitleJournal of African Earth Sciences