Terreneuvian skeletonized microfossils from the Central Iberian Zone (Spain) and correlation of the Fortunian Stage throughout southwestern Europe

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MetadadosDescriçãoIdioma
Autor(es): dc.contributorInstituto de Geociencias (CSIC-UCM)-
Autor(es): dc.contributorUniversidad de Castilla-La Mancha-
Autor(es): dc.contributorUniversité de Lille-
Autor(es): dc.contributorUniversidade Estadual Paulista (UNESP)-
Autor(es): dc.creatorJavier Álvaro, J.-
Autor(es): dc.creatorLorenzo, Saturnino-
Autor(es): dc.creatorDevaere, Léa-
Autor(es): dc.creatorWarren, Lucas V.-
Data de aceite: dc.date.accessioned2025-08-21T17:28:52Z-
Data de disponibilização: dc.date.available2025-08-21T17:28:52Z-
Data de envio: dc.date.issued2025-04-29-
Data de envio: dc.date.issued2024-10-01-
Fonte completa do material: dc.identifierhttp://dx.doi.org/10.1016/j.palwor.2023.12.001-
Fonte completa do material: dc.identifierhttps://hdl.handle.net/11449/298979-
Fonte: dc.identifier.urihttp://educapes.capes.gov.br/handle/11449/298979-
Descrição: dc.descriptionDuring the Ediacaran–Cambrian boundary interval, the Iberian margin of West Gondwana recorded oceanic upwelling and phosphogenesis favouring the preservation of originally phosphatic and diagenetically phosphatized shells. In the Abenójar Dome and the Alcudia Anticline of the Central Iberian Zone, the Fuentepizarra Formation comprises several phosphorite and phosphatic limestone interbeds that yield a microfossil assemblage rich in the helcionellid Anabarella plana, the halkieriid Halkieria sacciformis, the hyolith Conotheca subcurvata and chancelloriid debris. The assemblage is correlatable with the Purella antiqua Zone of the Aldan-Lena region and the Purella cristata Zone of the Anabar Uplift (Siberian Platform), slightly predating the Watsonella Zone of the Siberian Platform and the Watsonella crosbyi–Oelandiella korobkovi Zone of the northern Montagne Noire (France), both close to the (not yet globally defined) base of Cambrian Age 2. Despite the intra-Terreneuvian collapse of the Cadomian Orogen, stratigraphically associated with the onset of diachronous gaps, the base and top of the Fortunian Stage is well constrained throughout southwestern Europe based on radiometric ages and the micro- and ichnofossil record.-
Descrição: dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)-
Descrição: dc.descriptionMinisterio de Ciencia e Innovación-
Descrição: dc.descriptionInstituto de Geociencias (CSIC-UCM), Dr. Severo Ochoa 7-
Descrição: dc.descriptionDepartamento de Ingeniería Geológica y Minera Universidad de Castilla-La Mancha, Manuel Meca 1-
Descrição: dc.descriptionUMR 8198 EEP CNRS Université de Lille, 1, Avenue Paul Langevin-
Descrição: dc.descriptionDepartment of Geology Institute of Geosciences and Exact Sciences São Paulo State University, Avenida 24-A, Bela Vista 178, SP-
Descrição: dc.descriptionDepartment of Geology Institute of Geosciences and Exact Sciences São Paulo State University, Avenida 24-A, Bela Vista 178, SP-
Descrição: dc.descriptionMinisterio de Ciencia e Innovación: PID2021-125585NB-I00-
Formato: dc.format1179-1194-
Idioma: dc.languageen-
Relação: dc.relationPalaeoworld-
???dc.source???: dc.sourceScopus-
Palavras-chave: dc.subjectbioaccumulation-
Palavras-chave: dc.subjectFortunian-
Palavras-chave: dc.subjectmicrofossil-
Palavras-chave: dc.subjectphosphate-
Palavras-chave: dc.subjectWest gondwana-
Título: dc.titleTerreneuvian skeletonized microfossils from the Central Iberian Zone (Spain) and correlation of the Fortunian Stage throughout southwestern Europe-
Tipo de arquivo: dc.typelivro digital-
Aparece nas coleções:Repositório Institucional - Unesp

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