{"id":4832,"date":"2023-10-29T17:25:29","date_gmt":"2023-10-29T16:25:29","guid":{"rendered":"https:\/\/www.ataunturismoa.eus\/domo-ibilaldiak\/olata-erremedio\/punto-de-informacion-8\/"},"modified":"2023-10-29T17:25:29","modified_gmt":"2023-10-29T16:25:29","slug":"punto-de-informacion-8","status":"publish","type":"domo-ibilaldiak","link":"https:\/\/www.ataunturismoa.eus\/es\/domo-ibilaldiak\/olata-erremedio\/punto-de-informacion-8\/","title":{"rendered":"Punto de informaci\u00f3n 8"},"content":{"rendered":"\n<figure class=\"wp-block-audio\"><audio controls=\"\" src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/olata_8.wav\"><\/audio><\/figure>\n\n<p>La piedra caliza del Domo se form\u00f3 principalmente a partir de la acumulaci\u00f3n de estructuras duras de animales que viv\u00edan bajo el mar, como caparazones de moluscos y fragmentos de coral. Por ello, su contenido en minerales arcillosos es muy bajo, entre el 1 y el 3%. El resto es carbonato c\u00e1lcico. La roca que tenemos enfrente es muy apropiada para observar los f\u00f3siles de aquellos seres vivos. No obstante, si observamos detenidamente las rocas que rodean el camino, se pueden encontrar m\u00e1s f\u00f3siles de las mismas caracter\u00edsticas.<\/p>\n\n<p>En esta zona se localizan principalmente los f\u00f3siles de rudistas requi\u00e9nidos. La forma de los caparazones de estos moluscos bivalvos destaca en las rocas por un llamativo color oscuro, por lo que son f\u00e1cilmente reconocibles.<\/p>\n\n<div class=\"wp-block-bod-modal-block bod-block-popup align-center modaltitlenormal\"><a href=\"javascript:void(0)\" class=\"bod-block-popup-trigger type_text\">Domoko fosilei buruzko informazio gehiago >>> Fosilak<\/a><div style=\"background-color:rgba(0, 0, 0, 0.1)\" class=\"bod-block-popup-overlay\" data-disabled-overlay-close=\"false\" data-disabled-escape-close=\"false\"><\/div><div role=\"dialog\" aria-modal=\"false\" aria-labelledby=\"\" aria-describedby=\"\" class=\"bod-block-popup-wrap modaltitlenormal\"><div style=\"background-color:#ffffff;border-radius:0px \" class=\"bod-block-popup size-xl\" data-transition=\"fade\"><div id=\"\" style=\"background-color:#ffffff;text-align:center\" class=\"bod-modal-title\"><h2 style=\"color:#000000\">Informazio orokorra: Domoko fosilak<\/h2><\/div> <div id=\"\" style=\"padding:25px \" class=\"bod-modal-content\">\n<figure class=\"wp-block-audio\"><audio controls src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/domo_fosilak.wav\"><\/audio><\/figure>\n\n\n\n<p>Domoaren ertzean gailentzen diren kareharrien sorrera Behe Kretazeoan hemen existitu zen itsaso batean gertatu zen. Zehatzagoak izateko, Aptiar garaikoak dira, orain dela 120 milioi urte ingurukoak. Itsaso hura irudikatzeko, gaur egungo itsaso tropikal bat imajinatu behar dugu: sakonera gutxiko eta ur garden eta epeleko itsaso bat.<\/p>\n\n\n\n<p>Domoko kareharria, batez ere, itsaspean bizi ziren animalien egitura gogorren pilaketatik sortu zen: moluskuen oskolak eta koral zatiak, besteak beste. Egitura horiek kaltzio karbonatoan oso aberatsak zirenez eta itsaspe hartara buztin oso gutxi iristen zenez, baldintza haietan sorturikoak, oso kareharri puruak dira: buztin proportzioa %1-3 artean dago eta gainerakoa kaltzio karbonatoa da.<\/p>\n\n\n\n<p>Arroka hauen jatorriaren aztarnak nahiko erraz aurki daitezke Domoko kareharrietan. Izan ere, bide inguruan ditugun arrokak aztertuz gero, hauen sorrerako itsaso hartan bizi ziren hainbat bizidunen fosilak aurki daitezke. Fosil hauek, bizidun mota ezberdinak identifikatzea ahalbidetzeaz gain, adituei bizidun hauen paleoekologia ulertzeko informazioa ere ematen diete. Paleoekologiak, animalia hauek bizi zireneko ingurunea nolakoa zen azaltzen digu.<\/p>\n\n\n\n<p>Ataungo Domoan bertan, kokapenaren arabera, fosil mota ezberdinak topa ditzakegu. Orokorrean, ugarienak direnak errudista izeneko molusku batzuen fosilak dira. Errudisten barruan mota ezberdinetakoak aurki daitezkeen arren, errazen identifikatzen direnak errekienido motakoak dira. Hauen oskolen forma kolore ilun deigarri batez nabarmentzen da arroketan, horregatik, nahiko erraz atzeman daitezke. Hauek forma nahiko zapala zuten eta bakarka bizi ohi ziren. Horiez gain, bertikalean hazten ziren eta kopa forma zuten monopleurido eta polikonitidoak ere bizi ziren itsaso hartan. Azken errudista mota hauek taldean hazteko joera zuten, elkarri babesa emanez. Taldekatze horietan, ertzetan zeudenek buztin eta olatuen eragin gehiago izango zuten, baina erdikoak babestuago mantenduko ziren.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"400\" src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/06\/fosil1.jpg\" alt=\"\" class=\"wp-image-4595\" srcset=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/06\/fosil1.jpg 1000w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/06\/fosil1-300x120.jpg 300w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/06\/fosil1-768x307.jpg 768w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/06\/fosil1-500x200.jpg 500w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/06\/fosil1-800x320.jpg 800w\" sizes=\"auto, (max-width: 1000px) 100vw, 1000px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"750\" src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil2.jpg\" alt=\"\" class=\"wp-image-4600\" srcset=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil2.jpg 1000w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil2-300x225.jpg 300w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil2-768x576.jpg 768w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil2-500x375.jpg 500w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil2-800x600.jpg 800w\" sizes=\"auto, (max-width: 1000px) 100vw, 1000px\" \/><\/figure>\n\n\n\n<p>Itsaso tropikal hartako koral adarkatu finak aurkitzea ere nahiko ohikoa da, nahiz eta trebatu gabeko pertsonei hauen identifikazio-lana errudistena baino zertxobait zailagoa gerta dakiguken. Koral adarkatu finen kasuan, batzuetan adarkatzeak bereizi ahal izango dira, baina beste batzuetan, koralen barne egitura erakusten duten sekzio zirkular txikiak ikus daitezke.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"750\" height=\"750\" src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil3.jpg\" alt=\"\" class=\"wp-image-4605\" srcset=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil3.jpg 750w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil3-300x300.jpg 300w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil3-150x150.jpg 150w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil3-500x500.jpg 500w\" sizes=\"auto, (max-width: 750px) 100vw, 750px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"750\" src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil4.jpg\" alt=\"\" class=\"wp-image-4610\" srcset=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil4.jpg 1000w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil4-300x225.jpg 300w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil4-768x576.jpg 768w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil4-500x375.jpg 500w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil4-800x600.jpg 800w\" sizes=\"auto, (max-width: 1000px) 100vw, 1000px\" \/><\/figure>\n\n\n\n<p>Urkilagako portutik Agautz mendira doan bidearen lehen zatian, batez ere, garai hartako ostren aztarnak aurki daitezke, batzuk bidearen ertzeko arroketan, baina baita bide zidorrean bertan azaleratzen diren zenbait harritan ere.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"750\" src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil5.jpg\" alt=\"\" class=\"wp-image-4615\" srcset=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil5.jpg 1000w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil5-300x225.jpg 300w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil5-768x576.jpg 768w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil5-500x375.jpg 500w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil5-800x600.jpg 800w\" sizes=\"auto, (max-width: 1000px) 100vw, 1000px\" \/><\/figure>\n\n\n\n<p>Hauez gain, Urkilagatik Agautza doan bidearen erdi aldean dauden kareharri harlauza batzuetan, itsaso hartako gastropodo mota baten fosil ugari ikus daitezke. Hauek nerineido motako barraskilo luzexka batzuk dira.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"768\" src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil6-1024x768.jpg\" alt=\"\" class=\"wp-image-4620\" srcset=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil6-1024x768.jpg 1024w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil6-300x225.jpg 300w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil6-768x576.jpg 768w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil6-500x375.jpg 500w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil6-800x600.jpg 800w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil6-1280x960.jpg 1280w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/09\/fosil6-rotated.jpg 1333w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n<div class=\"bod-block-close-btn align-center\"><button type=\"button\" style=\"background-color:rgba(0, 0, 0, 0.1);color:#ffffff\" class=\"type_btn bod-btn\">Itxi<\/button><\/div><\/div> <\/div> <div class=\"bod-block-popup-closer\"><\/div><\/div><\/div>\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"768\" src=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/Olata_8-1024x768.jpg\" alt=\"\" class=\"wp-image-3312\" srcset=\"https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/Olata_8-1024x768.jpg 1024w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/Olata_8-300x225.jpg 300w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/Olata_8-768x576.jpg 768w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/Olata_8-500x375.jpg 500w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/Olata_8-800x600.jpg 800w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/Olata_8-1280x960.jpg 1280w, https:\/\/www.ataunturismoa.eus\/wp-content\/uploads\/2023\/08\/Olata_8.jpg 1301w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n","protected":false},"featured_media":0,"parent":4824,"menu_order":0,"template":"","class_list":["post-4832","domo-ibilaldiak","type-domo-ibilaldiak","status-publish","hentry"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Punto de informaci\u00f3n 8 - Ataun Turismoa<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.ataunturismoa.eus\/es\/domo-ibilaldiak\/olata-erremedio\/punto-de-informacion-8\/\" \/>\n<meta property=\"og:locale\" content=\"es_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Punto de informaci\u00f3n 8 - Ataun Turismoa\" \/>\n<meta property=\"og:description\" content=\"La piedra caliza del Domo se form\u00f3 principalmente a partir de la acumulaci\u00f3n de estructuras duras de animales que viv\u00edan bajo el mar, como caparazones de moluscos y fragmentos de coral. 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