{"id":116965,"date":"2018-03-11T10:46:17","date_gmt":"2018-03-11T10:46:17","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-aptiense-del-pagasarri-ganekogorta-sur-de-bilbao-estratigrafa%c2%ada-y-geoqua%c2%admica\/"},"modified":"2018-03-11T10:46:17","modified_gmt":"2018-03-11T10:46:17","slug":"el-aptiense-del-pagasarri-ganekogorta-sur-de-bilbao-estratigrafa%c2%ada-y-geoqua%c2%admica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/paleontologia-de-los-invertebrados\/el-aptiense-del-pagasarri-ganekogorta-sur-de-bilbao-estratigrafa%c2%ada-y-geoqua%c2%admica\/","title":{"rendered":"El aptiense del pagasarri-ganekogorta (sur de bilbao): estratigraf\u00eday geoqu\u00edmica"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jone Mendicoa Larrauri <\/strong><\/h2>\n<p>El aptiense es un periodo al que tradicionalmente se ha atribuido un clima c\u00e1lido,aunque con importantes fluctuaciones. Las intensas erupciones volc\u00e1nicas y lasubsiguiente liberaci\u00f3n de co2 provocaron perturbaciones en el ciclo del carbono quese reflejan como acumulaciones de materia org\u00e1nica globales asociadas a eventosan\u00f3xicos (v. G. Oae1a), perturbaciones en el ciclo del carbono o cambios en elcrecimiento y desaparici\u00f3n de las plataformas carbonatadas. El \u00e1rea al sur de bilbao,en la cuenca vasco-cant\u00e1brica se caracteriza por presentar uno de los registro m\u00e1spotentes para este periodo a nivel mundial. La presente tesis doctoral aborda elestudio detallado de estos materiales desde un punto de vista sedimentol\u00f3gico,bioestratigr\u00e1fico y geoqu\u00edmico. El an\u00e1lisis de las caracter\u00edsticas de estos materiales hapermitido reconstruir los paleoambientes de sedimentaci\u00f3n y su evoluci\u00f3n durante esteperiodo. Los datos obtenidos de los an\u00e1lisis de is\u00f3topos del carbono y el contenido demateria org\u00e1nica han permitido reconocer eventos oceanogr\u00e1ficos de edad aptiense.Las dataciones mediante ammonites han llevado a asignar una edad precisa a lasformaciones descritas y a los principales eventos aptienses identificados en lassecciones. Todos estos datos, nos han permitido comparar las secciones del sur debilbao con otras dentro de la cuenca vasco-cant\u00e1brica y\/o otras cuencas, mediante lacorrelaci\u00f3n de niveles clave (v. G. Oae1a, niveles de acumulaci\u00f3n de materia<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El aptiense del pagasarri-ganekogorta (sur de bilbao): estratigraf\u00eday geoqu\u00edmica<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El aptiense del pagasarri-ganekogorta (sur de bilbao): estratigraf\u00eday geoqu\u00edmica <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jone Mendicoa Larrauri <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Pa\u00eds vasco\/euskal herriko unibertsitatea<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 19\/12\/2014<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Pedro Angel Fernandez Mendiola<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: victoriano Pujalte navarro <\/li>\n<li>beatriz Badenas lago (vocal)<\/li>\n<li>marcos Aurell cardona (vocal)<\/li>\n<li>Mar\u00eda nieves Mel\u00e9ndez hevia (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jone Mendicoa Larrauri El aptiense es un periodo al que tradicionalmente se ha atribuido un clima c\u00e1lido,aunque [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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