Costras ferromanganesíferas pelágicas inducidas por comunidades bentónicas microbianas en el límite Jurásico Medio-Superior (Subbético Externo, provincia de Córdoba)

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dc.contributor.authorMolina, José Miguel
dc.contributor.authorReolid, Matías
dc.date.accessioned2014-03-11T10:09:32Z
dc.date.available2014-03-11T10:09:32Z
dc.date.issued2010
dc.description.abstractA hardground with Fe-Mn crusts of an important Middle-Upper Jurassic stratigraphic discontinuity in the External Subbetic has been analysed. These are mainly hydrogenetic-biogenic crusts induced by the activity of benthic microbial communities. The main organisms related with the Fe-Mn mineralization are probably fungi. The pelagic swells of the External Subbetic were a favourable environment for the development ofauthigenic mineralizations mainly by a very low rate of sedimentation and the existence of submarine volcanic processes in the neighboring Median Subbeticen_US
dc.identifier.urihttp://hdl.handle.net/10272/7851
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherHardgrounden_US
dc.subject.otherMicrobial communitiesen_US
dc.subject.otherFe-Mn crustsen_US
dc.subject.otherStratigraphic discontinuitiesen_US
dc.subject.otherJurassicen_US
dc.titleCostras ferromanganesíferas pelágicas inducidas por comunidades bentónicas microbianas en el límite Jurásico Medio-Superior (Subbético Externo, provincia de Córdoba)en_US
dc.titlePelagic Fe-Mn crusts induced by benthic microbial communities in the Middle-Upper Jurassic boundary (External Subbetic, Cordoba province)eg
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 48, (2010)