Ammonite biostratigraphy and bioevents in the Jurassic e Cretaceous boundary of central Chile

dc.contributor.authorSalazar, Christian
dc.contributor.authorStinnesbeck, Wolfgang
dc.contributor.authorAlvarez, Miguel
dc.date.accessioned2020-09-02T21:07:13Z
dc.date.available2020-09-02T21:07:13Z
dc.date.issued2019
dc.description.abstractAmmonites are abundant and well preserved in the Tithonian-Valanginian (Upper Jurassic eLowerCretaceous) sedimentary successions of the central Chilean Andes, known as the Lo Valdes and Ba~nos delFlaco Formations. A total of 1429 ammonites were collected from these stratigraphic units and thefollowing index zones based on ammonites are here proposed, from base to top: Virgatosphinctes mex-icanus/Pseudolissoceras cf. zitteli,Windhauseniceras internispinosum,Micracanthoceras microcanthum/Corongoceras alternans,Substeueroceras koeneni (Berriasella fraudans and Groebericeras rocardi sub-zones)and Thurmanniceras thurmanni/Argentiniceras fasciculatum.Our analyses indicate that “Ammonite Richness”is high in the middle and upper Tithonian and intothe lower Berriasian part of the succession, but decreases towards the lower Valanginian. Highest sim-ilarity values are established for the upper Tithonian, coincident with a high diversity; similarity declinesin the lower Berriasian. The main faunal turnover occurred between the early and late Berriasian fol-lowed by a secondary bioevent between the late Berriasian and early Valanginianes
dc.format.extent16 p.es
dc.identifier.citationCretaceous Research 107 (2020)es
dc.identifier.uriDOI: 10.1016/j.cretres.2019.104282es
dc.identifier.urihttp://hdl.handle.net/11447/3393
dc.language.isoenes
dc.subjectAmmonite biostratigraphyes
dc.subjectBioevent analysises
dc.subjectLo Valdés Formationes
dc.subjectFormation South Americaes
dc.subjectBaños del Flaco Formationes
dc.subjectSouth Americaes
dc.titleAmmonite biostratigraphy and bioevents in the Jurassic e Cretaceous boundary of central Chilees
dc.typeArticlees

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