{"title":"Schindewolfoceras y otras formas de ammonoideos en el Devónico Superior de la Cordillera Ibérica","authors":"J. R. Montesinos, R. Gozalo","doi":"10.7203/sjp.25212","DOIUrl":null,"url":null,"abstract":"Las capas Frasnienses de la Cordillera Ibérica han suministrado representantes de Schindewolfoceras Miller, hecho importante, dado que este género se consideró hasta fechas recientes como distribuido exclusivamente en Norteamérica. El conjunto de faunas encontradas soporta cierto grado de afinidad faunística entre el Dominio Palentino de la Cordillera Cantábrica y la Unidad de Herrera de la Cordillera Ibérica. ","PeriodicalId":37953,"journal":{"name":"Spanish Journal of Paleontology","volume":" ","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-09-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Spanish Journal of Paleontology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.7203/sjp.25212","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 0
Abstract
Las capas Frasnienses de la Cordillera Ibérica han suministrado representantes de Schindewolfoceras Miller, hecho importante, dado que este género se consideró hasta fechas recientes como distribuido exclusivamente en Norteamérica. El conjunto de faunas encontradas soporta cierto grado de afinidad faunística entre el Dominio Palentino de la Cordillera Cantábrica y la Unidad de Herrera de la Cordillera Ibérica.
期刊介绍:
The journal is international and publishes original manuscripts in Spanish and, preferentially, British spelling English on all aspects of broad interest in palaeontology. Particularly, the SJP aims to communicate and promote palaeontological research to the global scientific community. Moreover, articles on new discoveries and approaches are especially welcome. Finally, studies of present-day material can be included if they have significant palaeontological relevance.