{"id":32681,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-de-la-deglaciacion-finicuaternaria-en-el-nw-de-la-peninsula-iberica-datos-paleobotanicos-y-geomorfologicos\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"estudio-de-la-deglaciacion-finicuaternaria-en-el-nw-de-la-peninsula-iberica-datos-paleobotanicos-y-geomorfologicos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-de-la-deglaciacion-finicuaternaria-en-el-nw-de-la-peninsula-iberica-datos-paleobotanicos-y-geomorfologicos\/","title":{"rendered":"Estudio de la deglaciacion finicuaternaria en el nw de la peninsula iberica: datos paleobotanicos y geomorfologicos."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Luisa Santos Fidalgo <\/strong><\/h2>\n<p>Este trabajo es el estudio paleobotanico de dos sierras del nw peninsular (sierra del courel y sierra de queixa-invernadoiro), afectadas por procesos glaciares durante el pleistoceno superior, y contribuye al conocimiento de la evolucion de la vegetacion del noroeste de la peninsula iberica en la etapa final glaciar y en el postglaciar holoceno.Se han estudiado cinco secuencias polinicas: cuatro en la sierra de queixa y una en la sierra del courel, obteniendose 15 dataciones 14c de los sedimentos. Los resultados nos han permitido la elaboracion de diagramas polinicos que cubren el intervalo de tiempo entre el final del tardiglaciar y la actualidad.  el periodo cubierto por el registro palinologico corresponde solo a la parte final del representado por los datos geologico-geomorfologicos, si bien de estos ultimos no existen mas que dataciones relativas, hasta el momento. La evolucion de la vegetacion esta representada desde el tardiglaciar, y presenta rasgos generales similares en ambas sierras, aunque existen peque\u00f1as diferencias en su evolucion.  un analisis comparativo entre estos resultados y los de las regiones proximas permite conocer y explicar los diferentes comportamientos locales de la vegetacion.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio de la deglaciacion finicuaternaria en el nw de la peninsula iberica: datos paleobotanicos y geomorfologicos.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio de la deglaciacion finicuaternaria en el nw de la peninsula iberica: datos paleobotanicos y geomorfologicos. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Luisa Santos Fidalgo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 A coru\u00f1a<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/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>Juan  Ram\u00f3n Vidal Roman\u00ed<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: LLuis Pall\u00ed Bux\u00f3 <\/li>\n<li>Luis Salas Gomez (vocal)<\/li>\n<li>Angela Alonso Millan (vocal)<\/li>\n<li> Saa Otero M. Pilar (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Luisa Santos Fidalgo Este trabajo es el estudio paleobotanico de dos sierras del nw peninsular (sierra del [&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":[18576,27,35,953,75,3856,7419],"tags":[22731,16164,87234,84989,89814,89815],"class_list":["post-32681","post","type-post","status-publish","format-standard","hentry","category-a-coruna","category-ciencias-de-la-tierra-y-del-espacio","category-ciencias-de-la-vida","category-geologia","category-geomorfologia","category-paleontologia","category-palinologia","tag-angela-alonso-millan","tag-juan-ramon-vidal-romani","tag-lluis-palli-buxo","tag-luis-salas-gomez","tag-luisa-santos-fidalgo","tag-saa-otero-m-pilar"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/32681","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=32681"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/32681\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=32681"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=32681"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=32681"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}