{"id":920,"date":"2023-03-14T06:53:22","date_gmt":"2023-03-14T06:53:22","guid":{"rendered":"http:\/\/uhu.es\/aula-museo-geologia\/?page_id=920"},"modified":"2023-03-15T12:04:39","modified_gmt":"2023-03-15T12:04:39","slug":"foraminiferos","status":"publish","type":"page","link":"https:\/\/www.uhu.es\/aula-museo-geologia\/coleccion-sistematica-fosiles\/foraminiferos\/","title":{"rendered":"Foramin\u00edferos"},"content":{"rendered":"\n<div class=\"wp-block-cover alignfull\"><span aria-hidden=\"true\" class=\"wp-block-cover__background has-ast-global-color-8-background-color has-background-dim\"><\/span><img decoding=\"async\" loading=\"lazy\" width=\"1600\" height=\"500\" class=\"wp-block-cover__image-background wp-image-1201\" alt=\"\" src=\"http:\/\/uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/foraminiferos.jpg\" data-object-fit=\"cover\" srcset=\"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/foraminiferos.jpg 1600w, https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/foraminiferos-300x94.jpg 300w, https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/foraminiferos-1024x320.jpg 1024w, https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/foraminiferos-768x240.jpg 768w, https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/foraminiferos-1536x480.jpg 1536w\" sizes=\"(max-width: 1600px) 100vw, 1600px\" \/><div class=\"wp-block-cover__inner-container\">\n<h1 class=\"has-text-align-center\">Foramin\u00edferos<\/h1>\n<\/div><\/div>\n\n\n\n<div style=\"height:100px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h2>Caracter\u00edsticas Generales<\/h2>\n\n\n\n<p>Son Protistas provistos de unas prolongaciones flexibles del protoplasma de la c\u00e9lula, llamados pseud\u00f3podos. Esta estructura unicelular est\u00e1 protegida normalmente por un esqueleto secretado por la propia c\u00e9lula.<\/p>\n\n\n\n<p>Las formas de la concha de los foramin\u00edferos son enormemente variadas y complejas y se utilizan para su clasificaci\u00f3n e identificaci\u00f3n.<\/p>\n\n\n\n<p>Est\u00e1 compuesta por una o m\u00e1s c\u00e1maras comunicadas entre s\u00ed por aberturas que atraviesan las paredes. Las distintas c\u00e1maras se disponen en series diversas: a lo largo de un eje (seriadas), formando una espiral (en el plano, planiespiraladas o en el espacio, trocoespiraladas), en ciclos conc\u00e9ntricos (ciclostega) o en disposiciones m\u00e1s complejas (agatistega, orbitostega,\u2026).<\/p>\n\n\n\n<p>Suelen formar grandes masas o acumulaciones, f\u00e1cilmente visibles con una lupa.<\/p>\n\n\n\n<h2>Foramin\u00edfera<\/h2>\n\n\n\n<h3>Rotaliacea<\/h3>\n\n\n<div class=\"fichas-museo\" ><article class=\"ficha-titulo\"><div><a href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/alveolina-sp\/\"><img loading=\"lazy\" src=\"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/alveolina_tn.jpg\"><\/a><h5 itemprop=\"headline\"><a class=\"ficha-enlace\" href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/alveolina-sp\/\">Alveolina sp.<\/a><\/h5><\/div><\/article><article class=\"ficha-titulo\"><div><a href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/assilina-exponens\/\"><img loading=\"lazy\" src=\"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/assilina_exponens.jpg\"><\/a><h5 itemprop=\"headline\"><a class=\"ficha-enlace\" href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/assilina-exponens\/\">Assilina exponens<\/a><\/h5><\/div><\/article><article class=\"ficha-titulo\"><div><a href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/heterostegina-sp-muestra-1\/\"><img loading=\"lazy\" src=\"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/caliza_heterostegina.jpg\"><\/a><h5 itemprop=\"headline\"><a class=\"ficha-enlace\" href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/heterostegina-sp-muestra-1\/\">Heterostegina sp. (Muestra 1)<\/a><\/h5><\/div><\/article><article class=\"ficha-titulo\"><div><a href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/heterostegina-sp-muestra-2\/\"><img loading=\"lazy\" src=\"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/heterostegina.jpg\"><\/a><h5 itemprop=\"headline\"><a class=\"ficha-enlace\" href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/heterostegina-sp-muestra-2\/\">Heterostegina sp. (Muestra 2)<\/a><\/h5><\/div><\/article><article class=\"ficha-titulo\"><div><a href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/nummulites-millecaput\/\"><img loading=\"lazy\" src=\"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/nummulites_millecaput.jpg\"><\/a><h5 itemprop=\"headline\"><a class=\"ficha-enlace\" href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/nummulites-millecaput\/\">Nummulites millecaput<\/a><\/h5><\/div><\/article><\/div>\n\n\n\n<h3>Orbitolinacea<\/h3>\n\n\n<div class=\"fichas-museo\" ><article class=\"ficha-titulo\"><div><a href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/orbitolina-sp\/\"><img loading=\"lazy\" src=\"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-content\/uploads\/2023\/03\/orbitolina.jpg\"><\/a><h5 itemprop=\"headline\"><a class=\"ficha-enlace\" href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/orbitolina-sp\/\">Orbitolina sp.<\/a><\/h5><\/div><\/article><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Caracter\u00edsticas Generales Son Protistas provistos de unas prolongaciones flexibles del protoplasma de la c\u00e9lula, llamados pseud\u00f3podos. Esta estructura unicelular est\u00e1 protegida normalmente por un esqueleto secretado por la propia c\u00e9lula. Las formas de la concha de los foramin\u00edferos son enormemente variadas y complejas y se utilizan para su clasificaci\u00f3n e identificaci\u00f3n. Est\u00e1 compuesta por una &hellip;<\/p>\n<p class=\"read-more\"> <a class=\"\" href=\"https:\/\/www.uhu.es\/aula-museo-geologia\/fosiles\/orbitolina-sp\/\"> <span class=\"screen-reader-text\">Orbitolina sp.<\/span> Read More &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":105,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","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":""},"acf":[],"_links":{"self":[{"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/pages\/920"}],"collection":[{"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/comments?post=920"}],"version-history":[{"count":19,"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/pages\/920\/revisions"}],"predecessor-version":[{"id":1319,"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/pages\/920\/revisions\/1319"}],"up":[{"embeddable":true,"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/pages\/105"}],"wp:attachment":[{"href":"https:\/\/www.uhu.es\/aula-museo-geologia\/wp-json\/wp\/v2\/media?parent=920"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}