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dc.contributor.authorPaz, Maximiliano-
dc.contributor.authorMángano, Gabriela-
dc.contributor.authorBuatois, Luis-
dc.contributor.authorCarmona, Noelia Beatriz-
dc.contributor.authorDesjardins, Patricio-
dc.contributor.authorReijenstein, H.-
dc.contributor.authorGonzalez Tomassini, Federico-
dc.date.accessioned2022-09-08T15:17:09Z-
dc.date.available2022-09-08T15:17:09Z-
dc.date.issued2018-
dc.identifier.urihttp://rid.unrn.edu.ar/handle/20.500.12049/9069-
dc.language.isoenes_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/-
dc.titleBottom currents in the jurassic-cretaceous vaca muerta formation black shales (argentina): an example of benthos response to oxygen delivery in oxygendeficient environmentses_ES
dc.typeObjeto de conferenciaes_ES
dc.rights.licenseCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-ND 4.0)-
dc.description.filiationPaz, Maximiliano. University of Saskatchewan, Department of Geological Sciences, 114 Science Place, S7N 5E2 Saskatoon, Canadaes_ES
dc.description.filiationMángano, Gabriela. Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada,es_ES
dc.description.filiationBuatois, Luis. Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada,es_ES
dc.description.filiationCarmona, Noelia Beatriz. Universidad Nacional de Río Negro, Instituto de Investigación en Paleobiología y Geología, Río Negro, Argentina.es_ES
dc.description.filiationDesjardins, Patricio. Shell Exploration and Production Company, 150N Dairy Ashford St, TX, 77019, Houston, USAes_ES
dc.description.filiationReijenstein, H. Chevron, 1400 Smith, Houston, USAes_ES
dc.description.filiationGonzalez Tomassini, Federico. Phoenix Global Resources, Alem 855, C1001AAQ, Buenos Aires, Argentinaes_ES
dc.subject.keywordVaca Muertaes_ES
dc.subject.keywordbottom currentses_ES
dc.type.versioninfo:eu-repo/semantics/publishedVersiones_ES
dc.subject.materiaCiencias Exactas y Naturaleses_ES
dc.origin.lugarDesarrolloUniversidad Nacional de Río Negroes_ES
dc.description.resumenThe Vaca Muerta Formation represents marine bottomset and foreset facies of a mixed carbonatesiliciclastic ramp developed during Late Jurassic-Early Cretaceous in the Neuquén Basin, Argentina. Mudstone, marl and limestone deposited in low-energy, oxygen-deficient settings constitute the main lithologies of this formation. The present contribution describes mudstone and minor very fine-grained sandstone lithofacies showing variable intensities of bioturbation in cores from two wells (239 m thick in total) from the central Neuquén Basin area. Nine cycles of oxygenation events occur within outer to mid ramp settings and are subdivided in low- and highenergy. Low-energy cycles (30-50 cm thick) are characterized by very thin-bedded, parallel- to ripple cross-laminated, coarse to medium mudstone couplets. Intervals grade from highly bioturbated to sparsely bioturbated, showing Teichichnus and biodeformational structures. Highenergy cycles (1-10 m thick) show typical coarsening-upward trends in the lower part to finingupward patterns in the upper part. Their bases consist of a mottled mudstone and minor sandstone, grading towards sharp-based, thin-bedded, current-ripple cross-laminated mudstone. The cycles end with a mottled interval capped by cryptobioturbated mudstone. Bioturbation index displays a distinctive decrease to increase pattern, showing particularly small occurrences of Asterosoma, Bergaueria, Conichnus, Cylindrichnus, Palaeophycus, Planolites, Phycosiphon, Skolithos and escape trace fossils. Equilibrium behavior is inferred for Bergaueria and Conichnus. The cycles record bottom current activity at the upper slope, with hydrodynamic energy and oxygenation being limiting factors for the benthos and, therefore, controlling bioturbation. The cycles display increasing to decreasing energy conditions that show an inverse correlation with bioturbation index driven by shorter colonization windows in the higher energy settings (middle parts of the cycles). Bottom currents delivered oxygen to bottom waters, supporting a moderately diverse ichnofauna. Waning of bottom currents towards the end of the cycles generated progressive deoxygenation of the seafloor. Cryptobioturbation on top indicates that smaller organisms were able to thrive in lower oxygen conditions, documenting the last stage of the oxygenation event.es_ES
dc.relation.journalTitleISC2018, Québec Cityes_ES
dc.type.subtypeResumenes_ES
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