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Depositional environment and redox conditions of the Moncorvo Ironstone: Unveiling the evolution of ironstones under Rheic Ocean influence

datacite.subject.fosCiências Naturais::Ciências da Terra e do Ambiente
datacite.subject.sdg13:Ação Climática
datacite.subject.sdg14:Proteger a Vida Marinha
dc.contributor.authorUrbano, Emilio Evo Magro Correa
dc.contributor.authorPreto Gomes, Maria Elisa
dc.contributor.authorPinto de Meireles, Carlos Augusto
dc.contributor.authorBrandão, Paulo Roberto Gomes
dc.contributor.authorHippertt, Joa Pedro T.M.
dc.contributor.authorScholz, Ricardo
dc.contributor.authorLana, Cristiano
dc.date.accessioned2025-07-25T16:22:03Z
dc.date.available2025-07-25T16:22:03Z
dc.date.issued2025-06
dc.description.abstractABSTRACT: Ironstones, as key archives of past marine environments, provide invaluable insights into Paleozoic history. Their mineralogy may reflect the physical-chemical conditions of the environment and the nature of available sediments. This study focuses on the Moncorvo Ironstone, a Lower-Middle Ordovician deposit formed during the opening of the Rheic Ocean. Here, we use an integrated approach combining sedimentology, petrology, and geochemistry to constrain the depositional settings and the redox landscape associated with the ironstone deposition. The Moncorvo Ironstone present some unusual characteristics, such as the lack of ooids, an uncommon mineralogy, and a stratigraphic thickness that can reach over >45 m, a remarkable feature for an ironstone. Our investigation reveals that this iron-rich sequence is distributed in two distinct marine environments: an inner shelf and a middle to distal shelf. Each environment has a unique mineral assemblage. Despite the influence of metamorphism and deformation, evidence suggests that much of the mineralogy and texture of this deposit still preserve characteristics of the original sediments. Finally, our findings, alongside a careful assessment of the mineralogy of other ironstones of similar age, suggest a strong stratification of the Rheic Ocean throughout the Early and Middle Ordovician.eng
dc.identifier.citationUrbano, E., Gomes, M.E.P., Meireles, C.A.P., Brandão, P.R.G., Hippertt, J.P.T.M., Scholz, R. & Lana, C. (2025). Depositional environment and redox conditions of the Moncorvo Ironstone: Unveiling the evolution of ironstones under Rheic Ocean influence. In: Sedimentary Geology, 2025, vol. 482, article 106885. https://doi.org/10.1016/j.sedgeo.2025.106885
dc.identifier.doi10.1016/j.sedgeo.2025.106885
dc.identifier.eissn1879-0968
dc.identifier.issn0037-0738
dc.identifier.urihttp://hdl.handle.net/10400.9/6007
dc.language.isoeng
dc.peerreviewedyes
dc.publisherElsevier
dc.relation.hasversionhttps://www.sciencedirect.com/science/article/pii/S0037073825000806?via%3Dihub
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectGeochemistry
dc.subjectIronstone
dc.subjectIron oxides
dc.subjectOrdovician
dc.subjectRheic ocean
dc.subjectMoncorvo (Portugal)
dc.titleDepositional environment and redox conditions of the Moncorvo Ironstone: Unveiling the evolution of ironstones under Rheic Ocean influenceeng
dc.typejournal article
dspace.entity.typePublication
oaire.citation.titleSedimentary Geology
oaire.citation.volume482
oaire.versionhttp://purl.org/coar/version/c_970fb48d4fbd8a85
person.familyNamePreto Gomes
person.familyNamePinto de Meireles
person.givenNameMaria Elisa
person.givenNameCarlos Augusto
person.identifier.ciencia-id8F18-7134-14DB
person.identifier.ciencia-id1A14-BFCF-0DEA
person.identifier.orcid0000-0003-3105-8435
person.identifier.orcid0000-0002-5130-224X
relation.isAuthorOfPublication3a2c44cf-4f0b-4a06-b9c7-04cc0b0c488d
relation.isAuthorOfPublicationae541720-a10b-454b-9c20-c4af131b9b8d
relation.isAuthorOfPublication.latestForDiscovery3a2c44cf-4f0b-4a06-b9c7-04cc0b0c488d

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