{"id":11306,"date":"2018-03-09T08:56:34","date_gmt":"2018-03-09T08:56:34","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-post-glaciar-del-nivel-del-mar-en-el-n-o-de-la-peninsula-iberica-el-caso-del-golfo-artabro\/"},"modified":"2018-03-09T08:56:34","modified_gmt":"2018-03-09T08:56:34","slug":"evolucion-post-glaciar-del-nivel-del-mar-en-el-n-o-de-la-peninsula-iberica-el-caso-del-golfo-artabro","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evolucion-post-glaciar-del-nivel-del-mar-en-el-n-o-de-la-peninsula-iberica-el-caso-del-golfo-artabro\/","title":{"rendered":"Evolucion post-glaciar del nivel del mar en el n.o. de la peninsula iberica: el caso del golfo artabro"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Mar\u00eda  Jose Mosquera Sante <\/strong><\/h2>\n<p>En esta tesis doctoral se estudia la evolucion de las condiciones marinas, durante el holoceno, deducidas a partir de las asociaciones de foraminiferos bentonicos. El area estudiada comprende el tramo de costa definido entre las islas sisargas y el cabo prior (golfo artabro) donde se situan las llamadas rias intermedias, entre las poblaciones de a coru\u00f1a y ferrol.  las diferentes muestras, todas marinas a excepcion de porta real (que es una superficie de afloramiento) fueron recogidas con sonda vibrocorer por lo que son marinas y de car\u00e1cter arenoso, de entre todas se seleccionaron las siguientes: cinco de do\u00f1inos, una en ferrol, una en ares, dos en a coru\u00f1a, uno en orzan y una en sabon-punta langosteira.  para el analisis microfaunistico, se dividio cada sondeo en diferentes niveles, de los que se extrajeron siempre que fue posible, entre 250-300 caparazones o la totalidad de los mismos en el caso de no alcanzar dicho numero, lo que aunque ecologicamente carece de significado, solo su presencia nos permite definir un ambiente marino.  en su mayoria se trata de poblaciones oligoespecificas, con dominio de lobatula lobatula, acompa\u00f1ada de especies tipicamente eurihalina (amonia beccari, quinqueloculina seminula) o especies de caparazones peque\u00f1os y poco ornamentados, en lo que se refiere al muro de los diferentes sondeos, mientras hacia el techo de las poblaciones se hacen mas variadas, con la aparicion de elementos de plataforma (lobatula refulgens) y plactonicos (globigerna bulloides) asi como especies tipicamente marinas (rosalina globularis, planorbulina mediterranensis), indicativas de aguas mas profundas y de condiciones ecologicas mas estables. En todos los sondeos aparecen unos intervalos en los que los foraminiferos son escasos en numero y que siempre se acompa\u00f1an de espiculas de esponjas, protoconchas, restos de conchas de bivalvos y gasteropodos, por lo que corresponden siempre a facies sedimentarias marinas con grandes<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evolucion post-glaciar del nivel del mar en el n.o. de la peninsula iberica: el caso del golfo artabro<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evolucion post-glaciar del nivel del mar en el n.o. de la peninsula iberica: el caso del golfo artabro <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Mar\u00eda  Jose Mosquera Sante <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 A coru\u00f1a<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 14\/06\/2001<\/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: Guillermo Mateu Mateu <\/li>\n<li> Gracia Prieto Francisco Javier (vocal)<\/li>\n<li>Helena Pato Granja (vocal)<\/li>\n<li>Francisco Javier Rodriguez Vidal (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Mar\u00eda Jose Mosquera Sante En esta tesis doctoral se estudia la evolucion de las condiciones marinas, durante 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