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A new approach to palynostratigraphy of the middle–late Famennian Gafo Formation, southern sector of the Pulo do Lobo Domain, SW Iberia (Portugal and Spain)

dc.contributor.authorMendes, Márcia
dc.contributor.authorPereira, Zélia
dc.contributor.authorVaz, Nuno
dc.contributor.authorDíez-Montes, Alejandro
dc.contributor.authorMatos, João X.
dc.contributor.authorAlbardeiro, Luis
dc.contributor.authorManuel Carvalho Fernandes, Paulo
dc.contributor.authorJorge, Raul
dc.contributor.authorChew, David
dc.date.accessioned2023-03-30T09:16:20Z
dc.date.available2023-03-30T09:16:20Z
dc.date.issued2022-04
dc.description.abstractNew palynological results from the Gafo Formation (southern sector of the Pulo do Lobo Domain, South Portuguese Zone) are integrated with recently studied sections and drillholes from the Portuguese and Spanish sectors. A total of 44 samples were studied, 27 of which were positive for palynomorph taxonomy. This research revealed well preserved palynological assemblages, including 73 spore species allocated to 28 genera, four acritarch genera, three prasinophyte algae genera plus common chitinozoan remains. Some additional forms were retained under open nomenclature. From this, the first complete age determination for the Gafo Formation in Portugal and Spain was achieved, indicating a middle Famennian (Grandispora gracilis–Grandispora famenensis, GF Biozone) to a late Famennian (Grandispora echinata, VH Biozone) age. A greywacke sample from the same Gafo Formation was dated by U–Pb zircon geochronology and a maximum depositional age of 369 ± 2.5 Ma was obtained. A correlation between these palynological and U–Pb zircon data and the palynoflora assemblages of previous authors was made, as well as with the ages of felsic volcanic rocks found intercalated in the Gafo Formation, confirming the complex stratigraphy of Pulo do Lobo Domain. The results are consistent with stratigraphic mapping and structural interpretations, allowing a middle–late Famennian age (GF and VH Biozone) to be assigned to the Gafo Formation sedimentary rocks. This work has also contributed to a reinterpretation of Gafo Formation depositional facies correlatives (e.g. the Santa Barbara Group in Spain) as being the same lithological unit.pt_PT
dc.description.sponsorshipEU/Interreg-VA/Poctep/ 0052_GEO_FPI_5_E Project, Science Foundation Ireland (grant no. 13/RC/2092_P2)pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.1017/S0016756822000346pt_PT
dc.identifier.eissn1469-5081
dc.identifier.urihttp://hdl.handle.net/10400.1/19353
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherCambridgept_PT
dc.subjectPalynologypt_PT
dc.subjectFamennianpt_PT
dc.subjectBiostratigraphypt_PT
dc.subjectGafo Formationpt_PT
dc.subjectPulo do Lobo Domainpt_PT
dc.subjectSouth Portuguese Zonept_PT
dc.titleA new approach to palynostratigraphy of the middle–late Famennian Gafo Formation, southern sector of the Pulo do Lobo Domain, SW Iberia (Portugal and Spain)pt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage1470pt_PT
oaire.citation.issue8pt_PT
oaire.citation.startPage1454pt_PT
oaire.citation.titleGeological Magazinept_PT
oaire.citation.volume159pt_PT
person.familyNameFernandes
person.givenNamePaulo
person.identifier422469
person.identifier.ciencia-id051D-A133-65D9
person.identifier.orcid0000-0003-4888-0230
person.identifier.ridJ-6577-2014
person.identifier.scopus-author-id57197129025
rcaap.rightsrestrictedAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationa2d98df3-a9c2-4364-a737-25b4e89df80b
relation.isAuthorOfPublication.latestForDiscoverya2d98df3-a9c2-4364-a737-25b4e89df80b

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