{"id":33937,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/nannoplancton-calcareo-del-mioceno-de-la-cordillera-betica-sector-oriental\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"nannoplancton-calcareo-del-mioceno-de-la-cordillera-betica-sector-oriental","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/nannoplancton-calcareo-del-mioceno-de-la-cordillera-betica-sector-oriental\/","title":{"rendered":"Nannoplancton calcareo del mioceno de la cordillera betica (sector oriental)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jos\u00e9 Antonio Martin Perez <\/strong><\/h2>\n<p>Tras el estudio de numerosas secciones en sedimentos marinos del mioceno de la cordillera b\u00e9tica, norte de marruecos y sureste de italia, se establece la biozonaci\u00f3n de estos materiales mediante nanoplancton calc\u00e1reo, en la que se han diferenciado 13 zonas y 12 subzonas. Igualmente el esquema bioestratigr\u00e1fico propuesto ha sido correlacionado con los existentes de foramin\u00edferos planct\u00f3nicos. La integraci\u00f3n de este esquema bioestratigr\u00e1fico en el cronoestratigr\u00e1fico, permite caracterizar los l\u00edmites de los pisos del mioceno mediante una serie de bioeventos. As\u00ed mismo, se han realizado en cinco secciones, an\u00e1lisis multivariantes con el f\u00edn de discriminar cambios en las condiciones paleoambientales que puedan ser utilizadas desde el punto de vista estratigr\u00e1fico y paleoecol\u00f3gico, e incluso detectar diferencias entre secciones localizadas en \u00e1reas diferentes dentro del mismo intervalo de tiempo.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Nannoplancton calcareo del mioceno de la cordillera betica (sector oriental).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Nannoplancton calcareo del mioceno de la cordillera betica (sector oriental). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jos\u00e9 Antonio Martin Perez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/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>Jorge Martinez Gallego<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Antonio Vera Torres <\/li>\n<li>Jos\u00e9 Abel Flores Villarejo (vocal)<\/li>\n<li>Jos\u00e9 Mar\u00eda Gonzalez Donoso (vocal)<\/li>\n<li>Roque Aguado Merlo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jos\u00e9 Antonio Martin Perez Tras el estudio de numerosas secciones en sedimentos marinos del mioceno de la [&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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