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Did the Benue Trough connect the Gulf of Guinea with the Tethys Ocean in the Cenomanian? : New evidence from the Palynostratigraphy of the Yola Sub-basin

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dc.contributor.authorUsman, Musa B
dc.contributor.authorBrasier, Alexander T
dc.contributor.authorJolley, David W
dc.contributor.authorAbubakar, Usman
dc.contributor.authorMukkafa, Shehu
dc.contributor.institutionUniversity of Aberdeen.Geosciencesen
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.contributor.institutionUniversity of Aberdeen.Centre for Energy Transitionen
dc.date.accessioned2021-10-23T23:04:28Z
dc.date.available2021-10-23T23:04:28Z
dc.date.embargoedUntil2021-10-24
dc.date.issued2021-03
dc.descriptionAcknowledgements: M.B. Usman gratefully acknowledges the Petroleum Technology Development Fund (PTDF) for the award of a scholarship to study at the University of Aberdeen. The anonymous reviewers and the editor Eduardo Koutsoukos are thanked for their suggestions and corrections of the manuscript. We also acknowledge Roger David Burgess and Kelly Rebecca Snow for their technical assistance at the palynological laboratory of the University of Aberdeen.en
dc.description.statusPeer revieweden
dc.format.extent16
dc.format.extent4334272
dc.identifier178120765
dc.identifier621993fa-7463-430b-a1e4-bcfcb0dfaca7
dc.identifier85097471614
dc.identifier000607216800003
dc.identifier.citationUsman, M B, Brasier, A T, Jolley, D W, Abubakar, U & Mukkafa, S 2021, 'Did the Benue Trough connect the Gulf of Guinea with the Tethys Ocean in the Cenomanian? New evidence from the Palynostratigraphy of the Yola Sub-basin', Cretaceous Research, vol. 119, 104683. https://doi.org/10.1016/j.cretres.2020.104683en
dc.identifier.doi10.1016/j.cretres.2020.104683
dc.identifier.issn0195-6671
dc.identifier.otherORCID: /0000-0001-6103-2848/work/86450033
dc.identifier.otherORCID: /0000-0003-0909-2952/work/169078613
dc.identifier.urihttps://hdl.handle.net/2164/17384
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=85097471614&partnerID=8YFLogxKen
dc.identifier.vol119en
dc.language.isoeng
dc.relation.ispartofCretaceous Researchen
dc.subjectTrans-Saharaen
dc.subjectLate Cretaceousen
dc.subjectPalynomorphsen
dc.subjectbiostratigraphyen
dc.subjectBenue Troughen
dc.subjectNigeriaen
dc.subjectFailed riften
dc.subjectBiostratigraphyen
dc.subjectBIMA FORMATIONen
dc.subjectSTRATIGRAPHYen
dc.subjectNIGERIAen
dc.subjectEVOLUTIONen
dc.subjectFACIES ANALYSISen
dc.subjectCRETACEOUS SEDIMENTSen
dc.subjectBASINen
dc.subjectPALYNOLOGYen
dc.subjectAGEen
dc.subjectQE Geologyen
dc.subjectQ Scienceen
dc.subjectPalaeontologyen
dc.subjectSupplementary Dataen
dc.subject.lccQEen
dc.subject.lccQen
dc.titleDid the Benue Trough connect the Gulf of Guinea with the Tethys Ocean in the Cenomanian? : New evidence from the Palynostratigraphy of the Yola Sub-basinen
dc.typeJournal articleen

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