{"id":10037,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1996\/01\/01\/icnologia-de-les-conques-marines-pliocenes-del-marge-nordoccidental-de-la-mediterrania\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"icnologia-de-les-conques-marines-pliocenes-del-marge-nordoccidental-de-la-mediterrania","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/icnologia-de-les-conques-marines-pliocenes-del-marge-nordoccidental-de-la-mediterrania\/","title":{"rendered":"Icnolog\u00eda de les conques marines pliocenes del marge nordoccidental de la mediterrania."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Gibert Atienza Jordi M. De <\/strong><\/h2>\n<p>Se estudia el contenido icnologico de los sedimentos marinos pliocenos del margen noroccidental del mediterraneo (catalunya y se de francia). Desde el punto de vista taxonomico, se cita la presencia de 41 icnotaxones (26 correspondientes a estructuras de bioturbacion y 15 a estructuras de bioerosion), de los cuales uno es nuevo para la ciencia. El registro icnologico de la trasgresion zancleense sobre sustratos rocosos pre-pliocenos esta constituido por la asociacion gastrochaenolites-entobia, tipicamente litoral. Se han reconocido 17 icnofabricas en los sedimentos estudiados, caracterizandose cada una por la asociacion de trazas fosiles que la componen, su indice de bioturbacion y su diversidad icnologica. La variabilidad de las icnofabricas es resultado de variaciones paleoambientales, especialmente controladas por la salinidad, la profundidad y la sedimentacion. En todas las cuencas estudiadas (excepto la del var), las asociaciones icnologicas corresponden a medios someros, con salinidad variables (a veces salobre) y marginales.  la cuenca del var presenta icnofabricas con una mayor diversidad y\/o indice de bioturbacion, indicando sus caracteristicas mas profundas y mas francamente marinas.  el uso de las icnofabricas ha resultado muy positivo para el establecimiento de condiciones ambientales del registro geologico.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Icnolog\u00eda de les conques marines pliocenes del marge nordoccidental de la mediterrania.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Icnolog\u00eda de les conques marines pliocenes del marge nordoccidental de la mediterrania. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Gibert Atienza Jordi M. De <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Jordi Martinell Callic\u00f3<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Josep Serra Kiel <\/li>\n<li>Roland Goldring (vocal)<\/li>\n<li>Richard Bromley (vocal)<\/li>\n<li>Eduardo Mayoral Alfaro (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gibert Atienza Jordi M. De Se estudia el contenido icnologico de los sedimentos marinos pliocenos del margen [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[951,27,35,953,3856,3857],"tags":[33894,33891,21695,32921,33893,33892],"class_list":["post-10037","post","type-post","status-publish","format-standard","hentry","category-barcelona","category-ciencias-de-la-tierra-y-del-espacio","category-ciencias-de-la-vida","category-geologia","category-paleontologia","category-sedimentologia","tag-eduardo-mayoral-alfaro","tag-gibert-atienza-jordi-m-de","tag-jordi-martinell-callico","tag-josep-serra-kiel","tag-richard-bromley","tag-roland-goldring"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/10037","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=10037"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/10037\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=10037"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=10037"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=10037"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}