{"id":45298,"date":"2019-04-26T19:11:15","date_gmt":"2019-04-26T19:11:15","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/oligoceno-mioceno-inferior-por-medio-de-foraminiferos-planctonicos-en-el-sector-central-de-las-cordilleras-beticas\/"},"modified":"2019-04-26T19:11:15","modified_gmt":"2019-04-26T19:11:15","slug":"oligoceno-mioceno-inferior-por-medio-de-foraminiferos-planctonicos-en-el-sector-central-de-las-cordilleras-beticas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/oligoceno-mioceno-inferior-por-medio-de-foraminiferos-planctonicos-en-el-sector-central-de-las-cordilleras-beticas\/","title":{"rendered":"Oligoceno-mioceno inferior por medio de foraminiferos planctonicos en el sector central de las cordilleras beticas"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Eustoquio Martinez Molina <\/strong><\/h2>\n<p>Se estudia el oligoceno-mioceno inferior (del sector central de las cordilleras beticas) por medio de foraminiferos planctonicos  estableciendo una biozonacion basada en los mismos que se correlaciona con la escala cronoestratigrafica. Se data una importante fase orogenica que alcanzo su maximo apogeo en la parte superior de la zona de g. Altiaperturus (burdigaliense inferior). Se aborda el estudio paleontologico en detalle de los distintos taxones  que ha servido de base para el establecimiento de la filogenia  lo cual da pie para esbozar una nueva sistematica. Se deduce la existencia de una serie de tendencias evolutivas que intervinieron en la filogenia de los foraminiferos planctonicos. Se define una nueva especie denominada protentella navazuelensis que constituye un eslabon en la linea filogenetica de g-(t-) obesa &#8211; p. Prolixa.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Oligoceno-mioceno inferior por medio de foraminiferos planctonicos en el sector central de las cordilleras beticas<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Oligoceno-mioceno inferior por medio de foraminiferos planctonicos en el sector central de las cordilleras beticas <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Eustoquio Martinez Molina <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1979<\/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>Jos\u00e9 Mar\u00eda Gonzalez Donoso<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Mar\u00eda Gonzalez Donoso <\/li>\n<li>Jaime Trujols Santoja (vocal)<\/li>\n<li>Asuncion Linares Rodriguez (vocal)<\/li>\n<li> De Porta Vernet Jaime (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Eustoquio Martinez Molina Se estudia el oligoceno-mioceno inferior (del sector central de las cordilleras beticas) por medio [&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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