An exceptional storm accumulation of nautilids in the Lower Cretaceous of the Neuquén Basin, Argentina

dc.creatorCichowolski, Marcela
dc.creatorPazos, Pablo J.
dc.creatorTunik, Maisa A.
dc.creatorAguirre Urreta, Beatriz
dc.date2011
dc.date.accessioned2023-08-30T16:28:21Z
dc.date.available2023-08-30T16:28:21Z
dc.identifierCichowolski, Marcela., Pazos, Pablo J., Tunik, Maisa A. y Aguirre Urreta, Beatriz. (2011). An exceptional storm accumulation of nautilids in the Lower Cretaceous of the Neuquén Basin, Argentina. Wiley; Lethaia; 45 (1); 1-18
dc.identifier0024-1164
dc.identifier1502-3931
dc.identifierhttps://onlinelibrary.wiley.com/doi/abs/10.1111/j.1502-3931.2011.00271.x
dc.identifierhttps://rid.unrn.edu.ar/jspui/handle/20.500.12049/5340
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8529736
dc.descriptionFil: Cichowolski, Marcela. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. IDEAN. Buenos Aires, Argentina.
dc.descriptionFil: Pazos, Pablo J. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. IDEAN. Buenos Aires, Argentina.
dc.descriptionFil: Tunik, Maisa A. Universidad Nacional de Río Negro. Instituto de Investigaciones en Paleobiología y Geología. Río Negro, Argentina.
dc.descriptionFil: Aguirre Urreta, Beatriz. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas. Instituto de Estudios Andinos “Don Pablo Groeber". Buenos Aires, Argentina.
dc.descriptiontrue
dc.descriptionAn exceptional accumulation of nautilid shells of the species Cymatoceras perstriatum (Steuer) is reported and described in the Lower Cretaceous Agrio Formation of the Neuque´n Basin (west-central Argentina). The bed represents a storm deposit in a shallowwater environment within the mid-ramp. The evidences of a storm-related origin of the bed come from the petrographic analysis and taphonomic features of the shells, specially the sedimentary infill pattern. The shells are dispersed in patches within the stratum, without any orientation relative to the bedding plane. It is proposed that the shells were floating after the death of the animals, although most of them have an almost complete living chamber. The presence of some heavily encrusted shells suggests that there is a mixing of specimens with different drift times. A variety of factors related to the origin of such high number of nautilid shells are discussed, including a transgressive stand system tract, the possible existence of a gregarious behaviour, changes in salinity and wind directions. h Lower Cretaceous, Nautilids, Neuque´n Basin, shell accumulation, storm deposit.
dc.formatapplication/pdf
dc.languageen
dc.publisherWiley
dc.relation45 (1)
dc.relationLethaia
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/4.0/
dc.subjectCretaceous
dc.subjectNeuquén Basin
dc.subjectStorm
dc.titleAn exceptional storm accumulation of nautilids in the Lower Cretaceous of the Neuquén Basin, Argentina


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