{"id":15402,"date":"2023-08-18T13:30:11","date_gmt":"2023-08-18T11:30:11","guid":{"rendered":"http:\/\/webwp.igme.es\/pruebaigme\/?page_id=15402"},"modified":"2024-02-07T22:23:33","modified_gmt":"2024-02-07T21:23:33","slug":"estratigrafia-y-sedimentologia","status":"publish","type":"page","link":"https:\/\/webwp.igme.es\/pruebaigme\/estacion-paleontologica-valle-del-rio-fardes\/el-centro-paleontologico-fonelas-p-1\/investigacion\/estratigrafia-y-sedimentologia\/","title":{"rendered":"Estratigraf\u00eda y Sedimentolog\u00eda"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-page\" data-elementor-id=\"15402\" class=\"elementor elementor-15402\" data-elementor-post-type=\"page\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-d4b20bc elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"d4b20bc\" data-element_type=\"section\" data-settings=\"{&quot;jet_parallax_layout_list&quot;:[]}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-4381998\" data-id=\"4381998\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-3f5c9b5 elementor-widget elementor-widget-heading\" data-id=\"3f5c9b5\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<style>\/*! elementor - v3.19.0 - 07-02-2024 *\/\n.elementor-heading-title{padding:0;margin:0;line-height:1}.elementor-widget-heading .elementor-heading-title[class*=elementor-size-]>a{color:inherit;font-size:inherit;line-height:inherit}.elementor-widget-heading .elementor-heading-title.elementor-size-small{font-size:15px}.elementor-widget-heading .elementor-heading-title.elementor-size-medium{font-size:19px}.elementor-widget-heading .elementor-heading-title.elementor-size-large{font-size:29px}.elementor-widget-heading .elementor-heading-title.elementor-size-xl{font-size:39px}.elementor-widget-heading .elementor-heading-title.elementor-size-xxl{font-size:59px}<\/style><h5 class=\"elementor-heading-title elementor-size-default\">El sector occidental de la Cuenca de Guadix alberga un gran n\u00famero de importantes yacimientos paleontol\u00f3gicos de macromam\u00edferos localizados en el marco del Proyecto Fonelas.<\/h5>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-8b82f40 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"8b82f40\" data-element_type=\"section\" data-settings=\"{&quot;background_background&quot;:&quot;classic&quot;,&quot;jet_parallax_layout_list&quot;:[]}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-bef9e70\" data-id=\"bef9e70\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-inner-section elementor-element elementor-element-b43bfa2 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"b43bfa2\" data-element_type=\"section\" data-settings=\"{&quot;jet_parallax_layout_list&quot;:[]}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-e5be7b3\" data-id=\"e5be7b3\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-fb9add5\" data-id=\"fb9add5\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-cf08c1a elementor-widget__width-auto elementor-view-default elementor-widget elementor-widget-icon\" data-id=\"cf08c1a\" data-element_type=\"widget\" data-widget_type=\"icon.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-icon-wrapper\">\n\t\t\t<div class=\"elementor-icon\">\n\t\t\t<i aria-hidden=\"true\" class=\"fas fa-file-invoice\"><\/i>\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-d3cc61c elementor-widget__width-auto elementor-widget elementor-widget-text-editor\" data-id=\"d3cc61c\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<style>\/*! elementor - v3.19.0 - 07-02-2024 *\/\n.elementor-widget-text-editor.elementor-drop-cap-view-stacked .elementor-drop-cap{background-color:#69727d;color:#fff}.elementor-widget-text-editor.elementor-drop-cap-view-framed .elementor-drop-cap{color:#69727d;border:3px solid;background-color:transparent}.elementor-widget-text-editor:not(.elementor-drop-cap-view-default) .elementor-drop-cap{margin-top:8px}.elementor-widget-text-editor:not(.elementor-drop-cap-view-default) .elementor-drop-cap-letter{width:1em;height:1em}.elementor-widget-text-editor .elementor-drop-cap{float:left;text-align:center;line-height:1;font-size:50px}.elementor-widget-text-editor .elementor-drop-cap-letter{display:inline-block}<\/style>\t\t\t\t<p>Publicaci\u00f3n<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<div data-ra-element-link=\"{&quot;url&quot;:&quot;https:\\\/\\\/journals.plos.org\\\/plosone\\\/article?id=10.1371\\\/journal.pone.0007127&quot;,&quot;is_external&quot;:&quot;&quot;,&quot;nofollow&quot;:&quot;&quot;,&quot;custom_attributes&quot;:&quot;&quot;}\" style=\"cursor: pointer\" target=\"_self\" onClick=\"window.open(&#039;https:\/\/journals.plos.org\/plosone\/article?id=10.1371\/journal.pone.0007127&#039;, &#039;_self&#039;)\" class=\"elementor-element elementor-element-4fbc52f elementor-position-left elementor-view-default elementor-mobile-position-top elementor-vertical-align-top elementor-widget elementor-widget-icon-box\" data-id=\"4fbc52f\" data-element_type=\"widget\" data-widget_type=\"icon-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<link rel=\"stylesheet\" href=\"https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/elementor\/css\/custom-widget-icon-box.min.css?ver=1707998212\">\t\t<div class=\"elementor-icon-box-wrapper\">\n\t\t\t\t\t\t<div class=\"elementor-icon-box-icon\">\n\t\t\t\t<a href=\"https:\/\/info.igme.es\/media\/EPVRF\/Docs\/FONELAS_33.pdf\" class=\"elementor-icon elementor-animation-\" tabindex=\"-1\">\n\t\t\t\t<i aria-hidden=\"true\" class=\"fas fa-file-invoice\"><\/i>\t\t\t\t<\/a>\n\t\t\t<\/div>\n\t\t\t\t\t\t<div class=\"elementor-icon-box-content\">\n\t\t\t\t<h6 class=\"elementor-icon-box-title\">\n\t\t\t\t\t<a href=\"https:\/\/info.igme.es\/media\/EPVRF\/Docs\/FONELAS_33.pdf\" >\n\t\t\t\t\t\tLa Cuenca de Guadix. Rasgos geol\u00f3gicos generales.\t\t\t\t\t<\/a>\n\t\t\t\t<\/h6>\n\t\t\t\t\t\t\t\t\t<p class=\"elementor-icon-box-description\">\n\t\t\t\t\t\tSoria, J. M. y Viseras, C. 2008. La Cuenca de Guadix. Rasgos geol\u00f3gicos generales. En: Arribas, A. (Ed). Vertebrados del Plioceno superior terminal en el suroeste de Europa: Fonelas P-1 y el Proyecto Fonelas. Instituto Geol\u00f3gico y Minero de Espa\u00f1a, serie Cuadernos del Museo Geominero, 10, 3-19.\t\t\t\t\t<\/p>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e4401ca elementor-widget elementor-widget-image\" data-id=\"e4401ca\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<style>\/*! elementor - v3.19.0 - 07-02-2024 *\/\n.elementor-widget-image{text-align:center}.elementor-widget-image a{display:inline-block}.elementor-widget-image a img[src$=\".svg\"]{width:48px}.elementor-widget-image img{vertical-align:middle;display:inline-block}<\/style>\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"1024\" height=\"687\" src=\"https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_37-1024x687.jpg\" class=\"attachment-large size-large wp-image-15222\" alt=\"Panel de correlaci\u00f3n litol\u00f3gica y magnetoestratigr\u00e1fica del relleno de la Cuenca de Guadix en la vertiente oeste del valle del r\u00edo Fardes\" srcset=\"https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_37-1024x687.jpg 1024w, https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_37-300x201.jpg 300w, https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_37-768x515.jpg 768w, https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_37-1536x1030.jpg 1536w, https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_37-scaled.webp 1920w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Panel de correlaci\u00f3n litol\u00f3gica y magnetoestratigr\u00e1fica del relleno de la Cuenca de Guadix en la vertiente oeste del valle del r\u00edo Fardes (se indica la posici\u00f3n de yacimientos relevantes de grandes mam\u00edferos, que son estudiados en el marco de este proyecto, como Fonelas P-1, Fonelas SCC-1 y Mencal-9).<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<section class=\"elementor-section elementor-inner-section elementor-element elementor-element-14c486b elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"14c486b\" data-element_type=\"section\" data-settings=\"{&quot;jet_parallax_layout_list&quot;:[]}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-a006090\" data-id=\"a006090\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-73c7038\" data-id=\"73c7038\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-51b4f90 elementor-widget__width-auto elementor-view-default elementor-widget elementor-widget-icon\" data-id=\"51b4f90\" data-element_type=\"widget\" data-widget_type=\"icon.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-icon-wrapper\">\n\t\t\t<div class=\"elementor-icon\">\n\t\t\t<i aria-hidden=\"true\" class=\"fas fa-file-invoice\"><\/i>\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-8fdf115 elementor-widget__width-auto elementor-widget elementor-widget-text-editor\" data-id=\"8fdf115\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p>Publicaci\u00f3n<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<div data-ra-element-link=\"{&quot;url&quot;:&quot;https:\\\/\\\/journals.plos.org\\\/plosone\\\/article?id=10.1371\\\/journal.pone.0007127&quot;,&quot;is_external&quot;:&quot;&quot;,&quot;nofollow&quot;:&quot;&quot;,&quot;custom_attributes&quot;:&quot;&quot;}\" style=\"cursor: pointer\" target=\"_self\" onClick=\"window.open(&#039;https:\/\/journals.plos.org\/plosone\/article?id=10.1371\/journal.pone.0007127&#039;, &#039;_self&#039;)\" class=\"elementor-element elementor-element-ee7c9ae elementor-position-left elementor-view-default elementor-mobile-position-top elementor-vertical-align-top elementor-widget elementor-widget-icon-box\" data-id=\"ee7c9ae\" data-element_type=\"widget\" data-widget_type=\"icon-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-icon-box-wrapper\">\n\t\t\t\t\t\t<div class=\"elementor-icon-box-icon\">\n\t\t\t\t<a href=\"https:\/\/info.igme.es\/media\/EPVRF\/Docs\/FONELAS_28.pdf\" class=\"elementor-icon elementor-animation-\" tabindex=\"-1\">\n\t\t\t\t<i aria-hidden=\"true\" class=\"fas fa-file-invoice\"><\/i>\t\t\t\t<\/a>\n\t\t\t<\/div>\n\t\t\t\t\t\t<div class=\"elementor-icon-box-content\">\n\t\t\t\t<h6 class=\"elementor-icon-box-title\">\n\t\t\t\t\t<a href=\"https:\/\/info.igme.es\/media\/EPVRF\/Docs\/FONELAS_28.pdf\" >\n\t\t\t\t\t\t\tCondicionantes geol\u00f3gicos para la g\u00e9nesis de un yacimiento de grandes mam\u00edferos: Fonelas P-1\t\t\t\t\t<\/a>\n\t\t\t\t<\/h6>\n\t\t\t\t\t\t\t\t\t<p class=\"elementor-icon-box-description\">\n\t\t\t\t\t\tViseras, C., Soria, J.M., Dur\u00e1n, J.J. y Arribas, A. 2004. Condicionantes geol\u00f3gicos para la g\u00e9nesis de un yacimiento de grandes mam\u00edferos: Fonelas P-1 (l\u00edmite Plio-Pleistoceno, Cuenca de Guadix-Baza, Cordillera B\u00e9tica). Bolet\u00edn Geol\u00f3gico y Minero, 115 (3), 551-565.\t\t\t\t\t<\/p>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<section class=\"elementor-section elementor-inner-section elementor-element elementor-element-2a38220 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"2a38220\" data-element_type=\"section\" data-settings=\"{&quot;jet_parallax_layout_list&quot;:[]}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-a86bb28\" data-id=\"a86bb28\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-e6b672c\" data-id=\"e6b672c\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-754b987 elementor-widget__width-auto elementor-view-default elementor-widget elementor-widget-icon\" data-id=\"754b987\" data-element_type=\"widget\" data-widget_type=\"icon.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-icon-wrapper\">\n\t\t\t<div class=\"elementor-icon\">\n\t\t\t<i aria-hidden=\"true\" class=\"fas fa-file-invoice\"><\/i>\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-046c1b2 elementor-widget__width-auto elementor-widget elementor-widget-text-editor\" data-id=\"046c1b2\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p>Publicaci\u00f3n<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<div data-ra-element-link=\"{&quot;url&quot;:&quot;https:\\\/\\\/journals.plos.org\\\/plosone\\\/article?id=10.1371\\\/journal.pone.0007127&quot;,&quot;is_external&quot;:&quot;&quot;,&quot;nofollow&quot;:&quot;&quot;,&quot;custom_attributes&quot;:&quot;&quot;}\" style=\"cursor: pointer\" target=\"_self\" onClick=\"window.open(&#039;https:\/\/journals.plos.org\/plosone\/article?id=10.1371\/journal.pone.0007127&#039;, &#039;_self&#039;)\" class=\"elementor-element elementor-element-8645233 elementor-position-left elementor-view-default elementor-mobile-position-top elementor-vertical-align-top elementor-widget elementor-widget-icon-box\" data-id=\"8645233\" data-element_type=\"widget\" data-widget_type=\"icon-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-icon-box-wrapper\">\n\t\t\t\t\t\t<div class=\"elementor-icon-box-icon\">\n\t\t\t\t<a href=\"https:\/\/info.igme.es\/media\/EPVRF\/Docs\/FONELAS_29.pdf\" class=\"elementor-icon elementor-animation-\" tabindex=\"-1\">\n\t\t\t\t<i aria-hidden=\"true\" class=\"fas fa-file-invoice\"><\/i>\t\t\t\t<\/a>\n\t\t\t<\/div>\n\t\t\t\t\t\t<div class=\"elementor-icon-box-content\">\n\t\t\t\t<h6 class=\"elementor-icon-box-title\">\n\t\t\t\t\t<a href=\"https:\/\/info.igme.es\/media\/EPVRF\/Docs\/FONELAS_29.pdf\" >\n\t\t\t\t\t\tA Large Mammals Site in a Meandering Fluvial Context (Fonelas P-1)\t\t\t\t\t<\/a>\n\t\t\t\t<\/h6>\n\t\t\t\t\t\t\t\t\t<p class=\"elementor-icon-box-description\">\n\t\t\t\t\t\tViseras, C., Soria, J.M., Dur\u00e1n, J.J., Pla, S., Garrido, G., Garc\u00eda-Garc\u00eda, F. & Arribas, A. 2006. A Large Mammals Site in a Meandering Fluvial Context (Fonelas P-1, Late Pliocene, Guadix Basin, Spain). Sedimentological keys for its palaeoenvironmental reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology, 242, 139-168.\t\t\t\t\t<\/p>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<section class=\"elementor-section elementor-inner-section elementor-element elementor-element-9c6a219 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"9c6a219\" data-element_type=\"section\" data-settings=\"{&quot;jet_parallax_layout_list&quot;:[]}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-4229eab\" data-id=\"4229eab\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-7beb314\" data-id=\"7beb314\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-086b506 elementor-widget__width-auto elementor-view-default elementor-widget elementor-widget-icon\" data-id=\"086b506\" data-element_type=\"widget\" data-widget_type=\"icon.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-icon-wrapper\">\n\t\t\t<div class=\"elementor-icon\">\n\t\t\t<i aria-hidden=\"true\" class=\"fas fa-file-invoice\"><\/i>\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-5911ca5 elementor-widget__width-auto elementor-widget elementor-widget-text-editor\" data-id=\"5911ca5\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p>Publicaci\u00f3n<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<div data-ra-element-link=\"{&quot;url&quot;:&quot;https:\\\/\\\/journals.plos.org\\\/plosone\\\/article?id=10.1371\\\/journal.pone.0007127&quot;,&quot;is_external&quot;:&quot;&quot;,&quot;nofollow&quot;:&quot;&quot;,&quot;custom_attributes&quot;:&quot;&quot;}\" style=\"cursor: pointer\" target=\"_self\" onClick=\"window.open(&#039;https:\/\/journals.plos.org\/plosone\/article?id=10.1371\/journal.pone.0007127&#039;, &#039;_self&#039;)\" class=\"elementor-element elementor-element-fb78695 elementor-position-left elementor-view-default elementor-mobile-position-top elementor-vertical-align-top elementor-widget elementor-widget-icon-box\" data-id=\"fb78695\" data-element_type=\"widget\" data-widget_type=\"icon-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-icon-box-wrapper\">\n\t\t\t\t\t\t<div class=\"elementor-icon-box-icon\">\n\t\t\t\t<a href=\"https:\/\/info.igme.es\/media\/EPVRF\/Docs\/FONELAS_30.pdf\" class=\"elementor-icon elementor-animation-\" tabindex=\"-1\">\n\t\t\t\t<i aria-hidden=\"true\" class=\"fas fa-file-invoice\"><\/i>\t\t\t\t<\/a>\n\t\t\t<\/div>\n\t\t\t\t\t\t<div class=\"elementor-icon-box-content\">\n\t\t\t\t<h6 class=\"elementor-icon-box-title\">\n\t\t\t\t\t<a href=\"https:\/\/info.igme.es\/media\/EPVRF\/Docs\/FONELAS_30.pdf\" >\n\t\t\t\t\t\tA stratigraphic framework for the Pliocene-Pleistocene continental sediments of the Guadix Basin\t\t\t\t\t<\/a>\n\t\t\t\t<\/h6>\n\t\t\t\t\t\t\t\t\t<p class=\"elementor-icon-box-description\">\n\t\t\t\t\t\tPla-Pueyo, S., Viseras, C., Soria, J.M., Tent-Mancl\u00fas, J.E. and Arribas, A. 2011. A stratigraphic framework for the Pliocene-Pleistocene continental sediments of the Guadix Basin (Betic Cordillera, S. Spain). Quaternary International, 243(1):16\u201332.\t\t\t\t\t<\/p>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<section class=\"elementor-section elementor-inner-section elementor-element elementor-element-dcc7688 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"dcc7688\" data-element_type=\"section\" data-settings=\"{&quot;jet_parallax_layout_list&quot;:[]}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-f219d04\" data-id=\"f219d04\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-6fe990f elementor-widget elementor-widget-image\" data-id=\"6fe990f\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"561\" height=\"643\" src=\"https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_38.webp\" class=\"attachment-large size-large wp-image-15223\" alt=\"Reconstrucci\u00f3n a diferentes escalas del entorno sedimentario del yacimiento Fonelas P-1\" srcset=\"https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_38.webp 561w, https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_38-262x300.jpg 262w\" sizes=\"(max-width: 561px) 100vw, 561px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Reconstrucci\u00f3n a diferentes escalas del entorno sedimentario del yacimiento Fonelas P-1. A: valle fluvial con canales meandriformes (Sistema Axial) confinado entre los abanicos aluviales de los sistemas transversales Interno y Externo. B: canal sinuoso en migraci\u00f3n lateral que es abandonado en uno de sus meandros por un proceso de chute cut off, lugar en el que se produce la ocupaci\u00f3n de grandes mam\u00edferos (representados por un hi\u00e9nido) en el meandro residual. B1 y B2: posici\u00f3n de las asociaciones de facies en dos fases consecutivas de evoluci\u00f3n del canal; una primera (B1) de canal activo y otra segunda (B2) de canal abandonado; en esta segunda los grandes mam\u00edferos bioturbaron mediante pisadas los sedimentos finos acumulados en el meandro residual.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-853ec6a\" data-id=\"853ec6a\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-9935205 elementor-widget elementor-widget-image\" data-id=\"9935205\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"451\" height=\"1024\" src=\"https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_39-451x1024.jpg\" class=\"attachment-large size-large wp-image-15224\" alt=\"Sucesi\u00f3n estratigr\u00e1fica general donde se sit\u00faa el yacimiento Fonelas P-1.\" srcset=\"https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_39-451x1024.jpg 451w, https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_39-132x300.jpg 132w, https:\/\/webwp.igme.es\/pruebaigme\/wp-content\/uploads\/2023\/08\/IMG_39.webp 567w\" sizes=\"(max-width: 451px) 100vw, 451px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Sucesi\u00f3n estratigr\u00e1fica general donde se sit\u00faa el yacimiento Fonelas P-1.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"<p>El sector occidental de la Cuenca de Guadix alberga un gran n\u00famero de importantes yacimientos paleontol\u00f3gicos de macromam\u00edferos localizados en el marco del Proyecto Fonelas. Publicaci\u00f3n La Cuenca de Guadix. Rasgos geol\u00f3gicos generales. Soria, J. M. y Viseras, C. 2008. La Cuenca de Guadix. Rasgos geol\u00f3gicos generales. En: Arribas, A. (Ed). Vertebrados del Plioceno superior&#8230;<\/p>\n","protected":false},"author":18,"featured_media":15211,"parent":15123,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_kad_post_transparent":"","_kad_post_title":"hide","_kad_post_layout":"fullwidth","_kad_post_sidebar_id":"","_kad_post_content_style":"unboxed","_kad_post_vertical_padding":"hide","_kad_post_feature":"hide","_kad_post_feature_position":"","_kad_post_header":false,"_kad_post_footer":false,"footnotes":""},"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/pages\/15402"}],"collection":[{"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/users\/18"}],"replies":[{"embeddable":true,"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/comments?post=15402"}],"version-history":[{"count":30,"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/pages\/15402\/revisions"}],"predecessor-version":[{"id":33436,"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/pages\/15402\/revisions\/33436"}],"up":[{"embeddable":true,"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/pages\/15123"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/media\/15211"}],"wp:attachment":[{"href":"https:\/\/webwp.igme.es\/pruebaigme\/wp-json\/wp\/v2\/media?parent=15402"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}