Palynostratigraphy of the Middle Triassic (Anisian) Eslida Formation, SE Iberian Ranges, Spain

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dc.contributor.authorJuncal Rosales, Manuel Antonio
dc.contributor.authorDiez, José B.
dc.contributor.authorHorra Del Barco, Raúl De La
dc.contributor.authorGalán Abellán, Ana Belén
dc.contributor.authorBorruel Abadía, Violeta
dc.contributor.authorFernández Barrenechea, José María
dc.date.accessioned2023-06-17T22:29:43Z
dc.date.available2023-06-17T22:29:43Z
dc.date.issued2018
dc.description.abstractThe Triassic record in the SE Iberian Ranges starts with two tecto-sedimentary units of continental origin in Buntsandstein facies: and Cañizar and Eslida Formations. The Eslida Formation always lies conformably on top of the Cañizar Formation and it grades upwards into overlying coastal mud flats, traditionally assigned to the Röt facies. In the past, accurate dating of the Eslida Formation was problematic because of its continental character, absence of datable fossil remains, and lithological similarities with Middle–Upper Permian rocks. Macroflora and fossilised vertebrate footprints in the Eslida Formation indicate an Anisian age (Middle Triassic). In this work, we date the Eslida Formation on the basis of a palynological assemblage. The precise dating of the Eslida Formation is essential in order to establish stratigraphical correlations with other units in the Iberian Ranges and to obtain palaeogeographical considerations on the rapid subsidence represented by the sedimentary record of this unit in the new NNE–SSE Middle Triassic rift developed in eastern Iberia.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Economía y Competitividad (MINECO)
dc.description.sponsorshipConsejo Superior de Investigaciones Científicas (CSIC)
dc.description.sponsorshipUniversidad Complutense de Madrid/Banco de Santander
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/47707
dc.identifier.doi10.1080/01916122.2017.1310766
dc.identifier.issnISSN: 0191-6122,online ISSN: 1558-9188
dc.identifier.officialurlhttps://www.tandfonline.com/doi/full/10.1080/01916122.2017.1310766
dc.identifier.relatedurlhttps://www.tandfonline.com/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/18564
dc.issue.number2
dc.journal.titlePalynology
dc.language.isoeng
dc.page.final157
dc.page.initial149
dc.publisherTaylor & Francis
dc.relation.projectIDCGL2014-52699P
dc.relation.projectIDCSIC (642853)
dc.relation.projectIDAnálisis de Cuencas (910429)
dc.relation.projectIDPaleoclimas (910198)
dc.rights.accessRightsrestricted access
dc.subject.cdu561"622.242"
dc.subject.keywordAnisian
dc.subject.keywordBithynian
dc.subject.keywordPelsonian
dc.subject.keywordbiostratigraphy
dc.subject.keywordpalynology
dc.subject.keywordBuntsandstein
dc.subject.keywordIberian Peninsula
dc.subject.ucmGeología estratigráfica
dc.subject.ucmPaleontología
dc.subject.unesco2506.19 Estratigrafía
dc.subject.unesco2416 Paleontología
dc.titlePalynostratigraphy of the Middle Triassic (Anisian) Eslida Formation, SE Iberian Ranges, Spain
dc.typejournal article
dc.volume.number42
dspace.entity.typePublication
relation.isAuthorOfPublication509bf5dc-e657-4052-8eca-019bb7e1350b
relation.isAuthorOfPublicationb0d179ce-eb7f-46a1-b1bf-4926c43bd780
relation.isAuthorOfPublication3c69830b-43da-40f4-8cc4-8857118becaa
relation.isAuthorOfPublication.latestForDiscoveryb0d179ce-eb7f-46a1-b1bf-4926c43bd780
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