{"id":71020,"date":"2018-03-09T23:15:32","date_gmt":"2018-03-09T23:15:32","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-paleontologico-del-yacimiento-del-eoceno-superior-de-zambrana-alava-region-vasco-cantabrica-tafonoma%c2%ada-paleobiologa%c2%ada-de-mama%c2%adferos-e-implicaciones-biocronologicas\/"},"modified":"2018-03-09T23:15:32","modified_gmt":"2018-03-09T23:15:32","slug":"estudio-paleontologico-del-yacimiento-del-eoceno-superior-de-zambrana-alava-region-vasco-cantabrica-tafonoma%c2%ada-paleobiologa%c2%ada-de-mama%c2%adferos-e-implicaciones-biocronologicas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-vida\/estudio-paleontologico-del-yacimiento-del-eoceno-superior-de-zambrana-alava-region-vasco-cantabrica-tafonoma%c2%ada-paleobiologa%c2%ada-de-mama%c2%adferos-e-implicaciones-biocronologicas\/","title":{"rendered":"Estudio paleontol\u00f3gico del yacimiento del eoceno superior de zambrana (\u00e1lava, regi\u00f3n vasco-cant\u00e1brica). tafonom\u00eda, paleobiolog\u00eda de mam\u00edferos e implicaciones biocronol\u00f3gicas)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Ainara Badiola Kortabitarte <\/strong><\/h2>\n<p>El yacimiento paleontol\u00f3gico del eoceno superior de zambrana forma parte de uno de los sistemas lacustres m\u00e1s antiguos del flanco sur del sinclinal de miranda-trevi\u00f1o (regi\u00f3n vasco-cant\u00e1brica). El estudio sedimentol\u00f3gico indica condiciones palustres t\u00edpicas de zonas de margen lacustre, en un ambiente c enagoso. Las caracter\u00edsticas tafon\u00f3micas de la asociaci\u00f3n sugieren que los f\u00f3siles son aut\u00f3ctonos y descartan la existencia de reelaboraci\u00f3n.  los niveles excavados en zambrana han proporcionado f\u00f3siles de 25 taxones de vertebrados, correspondientes a anfibios (anuros), reptiles (escamosos, qulonios, cocodrilos) y mam\u00edferos. El estudios sistem\u00e1tico se ha centrado fundamentalmente en el registro de estos \u00faltimos (marsupiales, roedores, carn\u00edvoros, artiod\u00e1ctilos y perisod\u00e1ctilos), proponi\u00e9ndose cino nuevos taxones de perisod\u00e1ctilos ecuoideos, incluyendo dos nuevos g\u00e9neros de plagiolophinae y tres nuevas especies, \u00e9stas \u00faltimas pertenecientes a los g\u00e9neros palaeotherium (palaeotheriidae), leptolophus y pachynolophus (pachynolophidae). El yacimiento tambi\u00e9n ha proporcionado f\u00f3siles de invertebrados, carof\u00edtas y semillas de plantas.  el estudio paleoecol\u00f3gico sugiere  un medio con masas arboladas, quiz\u00e1s alrededor del lago, y h\u00e1bitats m\u00e1s abiertos y\/o \u00e1ridos en el resto de la zona. Desde un punto de vista paleobiogeogr\u00e1fico, en zambrna se observan ecuoideos de car\u00e1cter end\u00e9mico ib\u00e9rico, emparentados con los de mazater\u00f3n (cuenca del duero, mp 15-16) y llamaquique (cuenca de oviedo, mp 16-17). no obstante, la asociaci\u00f3n de artiod\u00e1ctilos de zambrana es t\u00edpicamente europea, lo que hace pensar en la existencia de contactos con el resto de europa occidental durante el headoniense superior.  zambrana es hasta la fecha el \u00fanico enclave de la pen\u00ednsula ib\u00e9rica que ha proporcionado una asociaci\u00f3n f\u00edsol de mam\u00edferos del nivel de referencia mp 18. Su estudio contribuye a un mejor conocimiento paleobiol\u00f3gico<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio paleontol\u00f3gico del yacimiento del eoceno superior de zambrana (\u00e1lava, regi\u00f3n vasco-cant\u00e1brica). tafonom\u00eda, paleobiolog\u00eda de mam\u00edferos e implicaciones biocronol\u00f3gicas)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio paleontol\u00f3gico del yacimiento del eoceno superior de zambrana (\u00e1lava, regi\u00f3n vasco-cant\u00e1brica). tafonom\u00eda, paleobiolog\u00eda de mam\u00edferos e implicaciones biocronol\u00f3gicas) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Ainara Badiola Kortabitarte <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Pa\u00eds vasco\/euskal herriko unibertsitatea<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 29\/10\/2004<\/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>Humberto Astibia Ayerra<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Cuesta ru\u00edz-colmenares Miguel \u00e1ngel <\/li>\n<li>carmen Ses\u00e9 benito (vocal)<\/li>\n<li>Mar\u00eda nieves L\u00f3pez mart\u00ednez (vocal)<\/li>\n<li>Jorge Morales romero (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Ainara Badiola Kortabitarte El yacimiento paleontol\u00f3gico del eoceno superior de zambrana forma parte de uno de los 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