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Carboniferous conodont biostratigraphy

dc.contributor.authorBarrick, James E.
dc.contributor.authorAlekseev, Alexander S.
dc.contributor.authorBlanco Ferrera, Silvia 
dc.contributor.authorGoreva, Natalia
dc.contributor.authorHu, Key
dc.contributor.authorLambert, Lance L.
dc.contributor.authorNemyrovska, Tamara I.
dc.contributor.authorQi, Yuping
dc.contributor.authorRitter, Scott
dc.contributor.authorSanz López, Javier 
dc.contributor.editorLucas, S. G.
dc.contributor.editorSchneider, J. W.
dc.contributor.editorWang, X.
dc.contributor.editorNikolaeva, S.
dc.date.accessioned2024-02-06T07:55:15Z
dc.date.available2024-02-06T07:55:15Z
dc.date.issued2022
dc.identifier.citationGeological Society, London, Special Publications 512 (2022); doi:10.1144/SP512-2020-38
dc.identifier.isbn978-1-78620-542-1
dc.identifier.issn0305-8719
dc.identifier.urihttps://hdl.handle.net/10651/71184
dc.descriptionEl Serpukhoviense en el Palaeotethys Occidental: variaciones climáticas y sus consecuencias sobre las biotas, aspectos paleoambientales, paleogeográficos y bioestratigráficosspa
dc.description.abstractCarboniferous conodont biostratigraphy comprises regional zonations that reflect the palaeogeographical distribution of taxa and distinct shallow-water and deep-water conodont biofacies. Some species have a global distribution and can effect high quality correlations. These taxa are incorporated into definitions of global Carboniferous chronostratigraphic units. A standard global Carboniferous zonation has not been developed. The lowermost Mississippian is zoned by Siphonodella species, excepet in shallow-water facies, where other polygnathids are used. Gnathodus species radiated during the Tournaisian and are used to define many Mississippian zones. A late Tournaisian maximum in diversity, characterized by short-lived genera, was followed by lower diversity faunas of Gnathodus species and carminate genera through the Visean and Serpukhovian. By the late Visean and Serpukhovian, Lochriea provides better biostratigraphic resolution. Shallow-water zonations based on Cavusgnathus and Mestognathus are difficult to correlate. An extinction event near the base of the Pennsylvanian was followed by the appearance of new gnathodid genera: Rhachistognathus, Declinognathodus, Neognathodus, Idiognathoides and Idiognathodus. By the middle of the Moscovian, few genera remained: Idiognathodus, Neognathodus and Swadelina. During the middle Kasimovian and Gzhelian, only Idiognathodus and Streptognathodus species were common. Near the end of the Gzhelian, a rediversification of Streptognathodus species extended into the Cisuralian.spa
dc.description.sponsorshipS B-F and J S-L would like to thank the support provided by the project CGL2016–78738-P of the Spanish Government.spa
dc.format.extentp. 695-768spa
dc.language.isoengspa
dc.publisherThe geological Society Londonspa
dc.relation.ispartofThe Carboniferous Timescale, Geological Society, London, Special Publications 512spa
dc.rightsCC Reconocimiento – No Comercial – Sin Obra Derivada 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectConodontspa
dc.subjectCarboniferous chronostratigraphyspa
dc.subjectstandard zonationspa
dc.subjectregional zonationspa
dc.subjectpalaeogeographyspa
dc.titleCarboniferous conodont biostratigraphyspa
dc.typearticle journalspa
dc.identifier.doi10.1144/SP512-2020-38
dc.relation.projectIDCGL2016–78738-Pspa
dc.rights.accessRightsopen accessspa
dc.type.hasVersionAM


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