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Middle Ordovician cephalopods from the Valongo Formation, northern Portugal

dc.contributor.authorSá, Artur A.
dc.contributor.authorGutiérrez Marco, Juan Carlos
dc.date.accessioned2014-04-14T09:44:43Z
dc.date.available2014-04-14T09:44:43Z
dc.date.issued2009
dc.identifier.urihttp://hdl.handle.net/10272/7959
dc.description.abstractOrdovician cephalopods from the Valongo Formation are among the first Ordovician fossils described from the Iberian Peninsula. The present review shows a lower taxonomical diversity than previously reported. Large endocerids and orthocerids are abundant in beds of early Oretanian (Middle Darriwilian) age, and orthocerids and some tarphycerids occur in strata of early Dobrotivian (Late Darriwilian) age. Despite the poor preservation in shales and the absence of internal structures, five different forms of longicones were identified, remaining them in open nomenclature. Tarphycerids are better recognizable and belong to the late Darriwilian forms Trocholites fugax and T. cf. depressus, with the former species recorded over a wide area of Ibero-Armorica and Bohemia, and the second related to a Baltic form. The occurrence of the genus Trocholites among Circumpolar Gondwana cephalopod faunas is consistent with the sporadic transfer of warm to temperate water masses southwards from the vicinity of Baltica, through a period of climatic disturbances affecting the southern hemisphere during the late Darriwilianen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherMiddle Ordovicianen_US
dc.subject.otherMolluscaen_US
dc.subject.otherCephalopodaen_US
dc.subject.otherCentral-Iberian Zoneen_US
dc.subject.otherPortugalen_US
dc.titleCefalópodos del Ordovícico Medio de la Formación Valongo, norte de Portugalen_US
dc.titleMiddle Ordovician cephalopods from the Valongo Formation, northern Portugaleng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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