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Its ichnologic study," /> <meta property="article:author" content="https://ub.academia.edu/JordiMdeGibert" /> <meta name="description" content="The Miocene marine deposits at El Camp de Tarragona basin record sedimentation in a mixed (silicilastic-carbonatic) shelf. Some of them display unusual ichnofabrics dominated almost exclusively by the ichnogenus Cylindrichnus. Its ichnologic study," /> <title>(PDF) Icnofábrica de Cylindrichnus en el Mioceno de la costa de Tarragona (Cataluña, España) | Jordi M. (de) Gibert - Academia.edu</title> <link rel="canonical" href="https://www.academia.edu/285803/Icnof%C3%A1brica_de_Cylindrichnus_en_el_Mioceno_de_la_costa_de_Tarragona_Catalu%C3%B1a_Espa%C3%B1a_" /> <script async src="https://www.googletagmanager.com/gtag/js?id=G-5VKX33P2DS"></script> <script> window.dataLayer = window.dataLayer || []; function gtag(){dataLayer.push(arguments);} gtag('js', new Date()); gtag('config', 'G-5VKX33P2DS', { cookie_domain: 'academia.edu', send_page_view: false, }); gtag('event', 'page_view', { 'controller': "single_work", 'action': "show", 'controller_action': 'single_work#show', 'logged_in': 'false', 'edge': 'unknown', // Send nil if there is no A/B test bucket, in case some records get logged // with missing data - that way we can distinguish between the two cases. // ab_test_bucket should be of the form <ab_test_name>:<bucket> 'ab_test_bucket': null, }) </script> <script> var $controller_name = 'single_work'; var $action_name = "show"; var $rails_env = 'production'; var $app_rev = '92477ec68c09d28ae4730a4143c926f074776319'; var $domain = 'academia.edu'; var $app_host = "academia.edu"; var $asset_host = "academia-assets.com"; var $start_time = new Date().getTime(); var $recaptcha_key = "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB"; var $recaptcha_invisible_key = "6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj"; var $disableClientRecordHit = false; </script> <script> window.require = { config: function() { return function() {} } } </script> <script> window.Aedu = window.Aedu || {}; window.Aedu.hit_data = null; window.Aedu.serverRenderTime = new Date(1732791993000); window.Aedu.timeDifference = new Date().getTime() - 1732791993000; </script> <script type="application/ld+json">{"@context":"https://schema.org","@type":"ScholarlyArticle","abstract":"\u0026amp;amp;amp;amp;quot;The Miocene marine deposits at El Camp de Tarragona basin record sedimentation in a mixed (silicilastic-carbonatic) shelf. Some of them display unusual ichnofabrics dominated almost exclusively by the ichnogenus Cylindrichnus. Its ichnologic study, jointly with the review of previous references, allow to observe several characteristics of this ichnogenus providing more information about their construction and functionality, as well as the potential tracemaking organisms. The trace fossils were probably produced by terebellid polychaetes under low-energy depositional conditions in a middle-distal shelf setting.\u0026amp;amp;amp;amp;quot;","author":[{"@context":"https://schema.org","@type":"Person","name":"Jordi M. (de) Gibert"}],"contributor":[],"dateCreated":"2010-08-04","dateModified":"2014-05-24","datePublished":null,"headline":"Icnofábrica de Cylindrichnus en el Mioceno de la costa de Tarragona (Cataluña, España)","inLanguage":"es","keywords":["Paleontology","Ichnology","Bioturbation","Miocene","Polychaetes","Terebellid Polychaete"],"locationCreated":null,"publication":null,"publisher":{"@context":"https://schema.org","@type":"Organization","name":null},"image":null,"thumbnailUrl":null,"url":"https://www.academia.edu/285803/Icnof%C3%A1brica_de_Cylindrichnus_en_el_Mioceno_de_la_costa_de_Tarragona_Catalu%C3%B1a_Espa%C3%B1a_","sourceOrganization":[{"@context":"https://schema.org","@type":"EducationalOrganization","name":"ub"}]}</script><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/single_work_page/loswp-102fa537001ba4d8dcd921ad9bd56c474abc201906ea4843e7e7efe9dfbf561d.css" /><link rel="stylesheet" media="all" 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Tarragona basin record sedimentation in a mixed (silicilastic-carbonatic) shelf. Some of them display unusual ichnofabrics dominated almost exclusively by the ichnogenus Cylindrichnus. Its ichnologic study, jointly with the review of previous references, allow to\r\nobserve several characteristics of this ichnogenus providing more information about their construction and functionality, as well as the potential tracemaking organisms. The trace fossils were probably produced by terebellid polychaetes under low-energy depositional conditions in a middle-distal shelf setting.","more_info":"Belaústegui, Z.; Gibert, J.M. de 2009. 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(de) Gibert" class="ds-work-card--author-avatar" src="https://0.academia-photos.com/147923/39095/35918/s65_jordi_m.._de_gibert.jpg" />Jordi M. (de) Gibert</a></div><div class="ds-work-card--detail"><div class="ds-work-card--work-metadata"><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">visibility</span><p class="ds2-5-body-sm" id="work-metadata-view-count">…</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">description</span><p class="ds2-5-body-sm">8 pages</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">link</span><p class="ds2-5-body-sm">1 file</p></div></div><script>(async () => { const workId = 285803; const worksViewsPath = "/v0/works/views?subdomain_param=api&work_ids%5B%5D=285803"; const getWorkViews = async (workId) => { const response = await fetch(worksViewsPath); if (!response.ok) { throw new Error('Failed to load work views'); } const data = await response.json(); return data.views[workId]; }; // Get the view count for the work - we send this immediately rather than waiting for // the DOM to load, so it can be available as soon as possible (but without holding up // the backend or other resource requests, because it's a bit expensive and not critical). const viewCount = await getWorkViews(workId); const updateViewCount = (viewCount) => { const viewCountNumber = Number(viewCount); if (!viewCountNumber) { throw new Error('Failed to parse view count'); } const commaizedViewCount = viewCountNumber.toLocaleString(); const viewCountBody = document.getElementById('work-metadata-view-count'); if (viewCountBody) { viewCountBody.textContent = `${commaizedViewCount} views`; } else { throw new Error('Failed to find work views element'); } }; // If the DOM is still loading, wait for it to be ready before updating the view count. if (document.readyState === "loading") { document.addEventListener('DOMContentLoaded', () => { updateViewCount(viewCount); }); // Otherwise, just update it immediately. } else { updateViewCount(viewCount); } })();</script></div><p class="ds-work-card--work-abstract ds-work-card--detail ds2-5-body-md">The Miocene marine deposits at El Camp de Tarragona basin record sedimentation in a mixed (silicilastic-carbonatic) shelf. Some of them display unusual ichnofabrics dominated almost exclusively by the ichnogenus Cylindrichnus. Its ichnologic study, jointly with the review of previous references, allow to observe several characteristics of this ichnogenus providing more information about their construction and functionality, as well as the potential tracemaking organisms. The trace fossils were probably produced by terebellid polychaetes under low-energy depositional conditions in a middle-distal shelf setting.</p><div class="ds-work-card--button-container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{"location":"continue-reading-button--work-card","attachmentId":1317385,"attachmentType":"pdf","workUrl":"https://www.academia.edu/285803/Icnof%C3%A1brica_de_Cylindrichnus_en_el_Mioceno_de_la_costa_de_Tarragona_Catalu%C3%B1a_Espa%C3%B1a_"}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{"location":"download-pdf-button--work-card","attachmentId":1317385,"attachmentType":"pdf","workUrl":"https://www.academia.edu/285803/Icnof%C3%A1brica_de_Cylindrichnus_en_el_Mioceno_de_la_costa_de_Tarragona_Catalu%C3%B1a_Espa%C3%B1a_"}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div></div></div></div><div data-auto_select="false" data-client_id="331998490334-rsn3chp12mbkiqhl6e7lu2q0mlbu0f1b" data-doc_id="1317385" data-landing_url="https://www.academia.edu/285803/Icnof%C3%A1brica_de_Cylindrichnus_en_el_Mioceno_de_la_costa_de_Tarragona_Catalu%C3%B1a_Espa%C3%B1a_" data-login_uri="https://www.academia.edu/registrations/google_one_tap" data-moment_callback="onGoogleOneTapEvent" id="g_id_onload"></div><div class="ds-top-related-works--grid-container"><div class="ds-related-content--container ds-top-related-works--container"><h2 class="ds-related-content--heading">Related papers</h2><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="0" data-entity-id="818812" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/818812/Cylindrichnus_ichnofabric_from_the_Miocene_of_theTarragona_coast_Catalonia_Spain_">Cylindrichnus ichnofabric from the Miocene of theTarragona coast (Catalonia, Spain)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="652049" href="https://ub.academia.edu/ZainBela%C3%BAstegui">Zain Belaústegui</a></div><p class="ds-related-work--abstract ds2-5-body-sm">The Miocene marine deposits at El Camp de Tarragona basin record sedimentation in a mixed (silicilastic-carbonatic) shelf. Some of them display unusual ichnofabrics dominated almost exclusively by the ichnogenus Cylindrichnus. Its ichnologic study, jointly with the review of previous references, allow to observe several characteristics of this ichnogenus providing more information about their construction and functionality, as well as the potential tracemaking organisms. The trace fossils were probably produced by terebellid polychaetes under low-energy depositional conditions in a middle-distal shelf setting.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Cylindrichnus ichnofabric from the Miocene of theTarragona coast (Catalonia, Spain)","attachmentId":4904121,"attachmentType":"pdf","work_url":"https://www.academia.edu/818812/Cylindrichnus_ichnofabric_from_the_Miocene_of_theTarragona_coast_Catalonia_Spain_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/818812/Cylindrichnus_ichnofabric_from_the_Miocene_of_theTarragona_coast_Catalonia_Spain_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="1" data-entity-id="1209420" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/1209420/Icnitas_de_aves_y_mam%C3%ADferos_del_Mioceno_temprano_de_La_Rioja_Cuenca_del_Ebro_Espa%C3%B1a_">Icnitas de aves y mamíferos del Mioceno temprano de La Rioja (Cuenca del Ebro, España).</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="517737" href="https://independent.academia.edu/IgnacioD%C3%ADazMart%C3%ADnez">Ignacio Díaz-Martínez</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="51850638" href="https://independent.academia.edu/SalvaCenicero">Salva Cenicero</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="7693055" href="https://unirioja.academia.edu/F%C3%A9lixP%C3%A9rezLorente">Félix Pérez-Lorente</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Ameghiniana, 2011</p><p class="ds-related-work--abstract ds2-5-body-sm">A new site carrying vertebrate footprints is described at Cenicero (Ebro Basin, Spain). The footprints are preserved in sandstone beds located within the “Transition Unit”, between the Agenian (early Miocene) Nájera and Haro formations. This level is placed between local biozones Y and Z. Fourteen blocks are studied; they contain 72 bird, 46 artiodactyl, and six perissodactyl footprints. Bird footprints include two ichnotaxa. The first one includes large to enormous tetradactyl footprints, with an incumbent hallux. It is identified as Gruipeda cf. maxima Panin and Avram. The second bird ichnotaxon is tridactyl with a prominent central pad, very large to enormous and with toes not joining at the proximal end. The latter feature suggests that it is probably a new bird ichnotaxon. Several ichnogeneric taxobases are proposed for bird footprints with the purpose of unifying the existing criteria between studies on extant and fossils bird ichnites. The artiodactyl footprints are small and identified as the ichnogenus Pecoripeda Vialov. The perissodactyl tracks are small and monodactyl, produced by equids, and classified as cf. Hippipeda Vialov. Key words. Miocene. Agenian. Ebro Basin. Footprints. Birds. Artiodactyls. Perissodactyls.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Icnitas de aves y mamíferos del Mioceno temprano de La Rioja (Cuenca del Ebro, España).","attachmentId":7521360,"attachmentType":"pdf","work_url":"https://www.academia.edu/1209420/Icnitas_de_aves_y_mam%C3%ADferos_del_Mioceno_temprano_de_La_Rioja_Cuenca_del_Ebro_Espa%C3%B1a_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/1209420/Icnitas_de_aves_y_mam%C3%ADferos_del_Mioceno_temprano_de_La_Rioja_Cuenca_del_Ebro_Espa%C3%B1a_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="2" data-entity-id="2279984" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/2279984/Tafonom%C3%ADa_y_contexto_paleoambiental_de_los_restos_de_un_cet%C3%A1ceo_del_Mioceno_medio_de_Tarragona_NE_Espa%C3%B1a_">Tafonomía y contexto paleoambiental de los restos de un cetáceo del Mioceno medio de Tarragona (NE España)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="2878446" href="https://barcelona.academia.edu/JordiMartinell">Jordi Martinell</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Geobios, 2011</p><p class="ds-related-work--abstract ds2-5-body-sm">Se documenta el hallazgo de un mamífero marino en el Mioceno medio de la cuenca de El Camp de Tarragona (NE España). En concreto, se trata de un esqueleto incompleto y desarticulado de un individuo juvenil de cetáceo. Los restos aparecen depositados inmediatamente por encima de una superficie de transgresión e incluidos en un nivel de calcisiltitas glauconíticas que marcan el comienzo de una secuencia somerizante y se depositaron en un ambiente de plataforma media a externa, poco energético y con una tasa de sedimentación baja. Estas condiciones favorecieron una exposición prolongada de los restos y el consecuente aumento de la duración de la fase bioestratinómica de los mismos. Ésto facilitó tanto la descomposición y desarticulación natural del cadáver, como el carroñeo por parte de diferentes tipos de organismos. La interpretación del contexto paleoambiental en el que se depositó y enterró dicho cetáceo, se basa en la combinación de la información obtenida a partir de las características tafonómicas de los propios restos óseos, de los datos obtenidos a partir de la fauna asociada a ellos y del estudio icnológico y sedimentológico del nivel donde están englobados. La integración de diferentes conjuntos de datos permite una buena caracterización del contexto paleoambiental en que se enterraron los restos estudiados.A new finding of a marine mammal is documented from the middle Miocene of El Camp basin in Tarragona (NE Spain). The incomplete and disarticulated bone remains belong to the skeleton of a juvenile cetacean. These remains appear deposited above a transgression surface and included within a glauconitic calcisiltite layer. This unit constitutes the beginning of a shallowing-upwards sequence and was deposited under low-energy conditions and low sedimentation rates in a middle-outer platform setting. This context was responsible for the long exposure of the remains and, consequently, an extension of the biostratinomic stage. These conditions favored the natural decomposition and disarticulation of the carcass, allowing the action of different types of scavenging organisms. The interpretation of the paleoenvironmental setting is based in the combination of different datasets: taphonomic data of the bone remains, paleoecologic and taphonomic information provided by the fauna associated to the bones, and ichnologic and sedimentologic interpretation of the sediments where the fossils are included. Combination of such different proxies enables a very good characterization of the paleoenvironmental context of the studied fossils.Dans ce travail, nous présentons la découverte d’un mammifère marin dans le bassin miocène moyen d’El Camp (Tarragona, Espagne). Il s’agit d’un squelette incomplet et désarticulé d’un spécimen juvénile appartenant à un cétacé. Les restes se trouvent déposés juste au-dessus d’une surface de transgression, dans un niveau de calcisiltites glauconitiques. Ces restes se sont déposés dans un environnement de plate-forme moyenne/externe, à faible énergie et faible taux de sédimentation. Ces conditions, favorables à l’exposition prolongée des restes explique la longue durée de la phase biostratinomique. Ceci à favorisé la décomposition et la désarticulation naturelle du cadavre, ainsi que le charognage produit par différents organismes. L’interprétation du contexte paléoenvironnemental proposé pour le milieu où le cadavre a été déposé et enterré s’appuie sur la combinaison de l’information obtenue à partir des caractéristiques taphonomiques des restes osseux, des données de la faune associée et de l’étude ichnologique et sédimentologique du niveau où ils sont enregistrés. L’intégration des différents ensembles de données permet une bonne caractérisation du contexte paléoenvironnemental où les restes étudiés ont été ensevelis.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Tafonomía y contexto paleoambiental de los restos de un cetáceo del Mioceno medio de Tarragona (NE España)","attachmentId":50687988,"attachmentType":"pdf","work_url":"https://www.academia.edu/2279984/Tafonom%C3%ADa_y_contexto_paleoambiental_de_los_restos_de_un_cet%C3%A1ceo_del_Mioceno_medio_de_Tarragona_NE_Espa%C3%B1a_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/2279984/Tafonom%C3%ADa_y_contexto_paleoambiental_de_los_restos_de_un_cet%C3%A1ceo_del_Mioceno_medio_de_Tarragona_NE_Espa%C3%B1a_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="3" data-entity-id="70649904" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/70649904/Presencia_del_icnog%C3%A9nero_Iguanodontipus_en_el_Cret%C3%A1cico_Inferior_de_la_provincia_de_Teruel_Espa%C3%B1a_Presence_of_the_ichnogenus_Iguanodontipus_in_the_Lower_Cretaceous_of_the_Teruel_province_Spain_">Presencia del icnogénero Iguanodontipus en el Cretácico Inferior de la provincia de Teruel (España) Presence of the ichnogenus Iguanodontipus in the Lower Cretaceous of the Teruel province (Spain)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="168838" href="https://uned.academia.edu/FranciscoGasc%C3%B3">Francisco Gascó</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2012</p><p class="ds-related-work--abstract ds2-5-body-sm">Until now, the presence of iguanodontoids in the Lower Cretaceous of the Teruel province has been restricted to fossil bones and teeth. New tracks have been found in the Areniscas de Camarillas Formation (lower Barremian) in Cabra de Mora and El Castellar (both villages located in Teruel province, Maestrazgo basin, Penagolosa Sub-basin). These new tracks are assigned to the ichnogenus Iguanodontipus, and their presence helps to complete the record of this kind of tracks in the Iberian Peninsula. Moreover, these tracks show that iguanodontoids were part of these fluvial continental ecosystems of this stratigraphic unit. It is quite remarkable the size of these ornithopods illustrated by track CPT-4399, measuring 50 cm of both length and width. This footprint has been preserved as convex epirelief.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Presencia del icnogénero Iguanodontipus en el Cretácico Inferior de la provincia de Teruel (España) Presence of the ichnogenus Iguanodontipus in the Lower Cretaceous of the Teruel province (Spain)","attachmentId":80313152,"attachmentType":"pdf","work_url":"https://www.academia.edu/70649904/Presencia_del_icnog%C3%A9nero_Iguanodontipus_en_el_Cret%C3%A1cico_Inferior_de_la_provincia_de_Teruel_Espa%C3%B1a_Presence_of_the_ichnogenus_Iguanodontipus_in_the_Lower_Cretaceous_of_the_Teruel_province_Spain_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/70649904/Presencia_del_icnog%C3%A9nero_Iguanodontipus_en_el_Cret%C3%A1cico_Inferior_de_la_provincia_de_Teruel_Espa%C3%B1a_Presence_of_the_ichnogenus_Iguanodontipus_in_the_Lower_Cretaceous_of_the_Teruel_province_Spain_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="4" data-entity-id="15365058" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/15365058/Icnofacies_de_Glossifungites_en_el_Mioceno_de_Alcoy_SE_Espa%C3%B1a_">Icnofacies de Glossifungites en el Mioceno de Alcoy (SE España)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="652049" href="https://ub.academia.edu/ZainBela%C3%BAstegui">Zain Belaústegui</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="2878446" href="https://barcelona.academia.edu/JordiMartinell">Jordi Martinell</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Icnofacies de Glossifungites en el Mioceno de Alcoy (SE España)","attachmentId":38658184,"attachmentType":"pdf","work_url":"https://www.academia.edu/15365058/Icnofacies_de_Glossifungites_en_el_Mioceno_de_Alcoy_SE_Espa%C3%B1a_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/15365058/Icnofacies_de_Glossifungites_en_el_Mioceno_de_Alcoy_SE_Espa%C3%B1a_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="5" data-entity-id="1563535" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/1563535/Los_cipr%C3%ADnidos_Pisces_del_sistema_lacustre_Oligoc%C3%A9nico_Mioc%C3%A9nico_de_los_Monegros_sector_SE_de_la_Cuenca_del_Ebro_provincias_de_Lleida_Tarragona_">Los ciprínidos (Pisces) del sistema lacustre Oligocénico-Miocénico de los Monegros (sector SE de la Cuenca del Ebro, provincias de Lleida, Tarragona, …</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="867736" href="https://ub.academia.edu/LluisCabrera">Lluis Cabrera</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Acta geológica hispánica, 1985</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Los ciprínidos (Pisces) del sistema lacustre Oligocénico-Miocénico de los Monegros (sector SE de la Cuenca del Ebro, provincias de Lleida, Tarragona, …","attachmentId":13811796,"attachmentType":"pdf","work_url":"https://www.academia.edu/1563535/Los_cipr%C3%ADnidos_Pisces_del_sistema_lacustre_Oligoc%C3%A9nico_Mioc%C3%A9nico_de_los_Monegros_sector_SE_de_la_Cuenca_del_Ebro_provincias_de_Lleida_Tarragona_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/1563535/Los_cipr%C3%ADnidos_Pisces_del_sistema_lacustre_Oligoc%C3%A9nico_Mioc%C3%A9nico_de_los_Monegros_sector_SE_de_la_Cuenca_del_Ebro_provincias_de_Lleida_Tarragona_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="6" data-entity-id="112474730" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/112474730/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Sidr%C3%B3n_Asturias_">Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1019145" href="https://uniovi.academia.edu/MarcodelaRasillaVives">Marco de la Rasilla Vives</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Estudios Geológicos, 2018</p><p class="ds-related-work--abstract ds2-5-body-sm">En el yacimiento del Pleistoceno Superior de la cueva de El Sidrón, con una datación de ~49.000 ka, conocido por sus numerosos restos fósiles de neandertales, se han recuperado restos de micromamíferos cuyo estudio detallado se realiza en este trabajo. La asociación determinada es la siguiente: Sorex araneus–Sorex coronatus, Neomys cf. fodiens, Talpa sp., Rhinolophus euryale-Rhinolophus mehelyi, Marmota cf. marmota, Eliomys quercinus, Glis glis, Arvicola terrestris, Chionomys nivalis, Microtus arvalis-Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Clethrionomys glareolus, Apodemus sylvaticus-Apodemus flavicollis y Oryctolagus cuniculus. Estos taxones están presentes en la fauna actual de Asturias y de la región cantábrica excepto Microtus oeconomus que desapareció de la península ibérica en tiempos históricos y actualmente está en regiones euroasiáticas más septentrionales. La fauna de micromamíferos en conjunto parece indicar un medio predominantemente de espacios abi...</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias)","attachmentId":109693923,"attachmentType":"pdf","work_url":"https://www.academia.edu/112474730/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Sidr%C3%B3n_Asturias_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/112474730/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Sidr%C3%B3n_Asturias_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="7" data-entity-id="308558" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/308558/Ictiofauna_De_Zonas_Someras_Del_Mar_Menor_SE_Pen%C3%ADnsula_Ib%C3%A9rica_">Ictiofauna De Zonas Someras Del Mar Menor (SE Península Ibérica)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="238486" href="https://murcia.academia.edu/DavidVerdiell">David Verdiell</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Anales de …, 2003</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Ictiofauna De Zonas Someras Del Mar Menor (SE Península Ibérica)","attachmentId":51460231,"attachmentType":"pdf","work_url":"https://www.academia.edu/308558/Ictiofauna_De_Zonas_Someras_Del_Mar_Menor_SE_Pen%C3%ADnsula_Ib%C3%A9rica_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/308558/Ictiofauna_De_Zonas_Someras_Del_Mar_Menor_SE_Pen%C3%ADnsula_Ib%C3%A9rica_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="8" data-entity-id="30716473" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/30716473/Registro_de_conodontos_delTri%C3%A1sico_Medio_en_un_nautiloideode_Espejeras_Alicante_Espa%C3%B1a_">Registro de conodontos delTriásico Medio en un nautiloideode Espejeras (Alicante, España)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="39639119" href="https://lizzysuccess.academia.edu/AnaM%C3%A1rquezAliaga">Ana Márquez Aliaga</a></div><p class="ds-related-work--metadata ds2-5-body-xs">1996</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Registro de conodontos delTriásico Medio en un nautiloideode Espejeras (Alicante, España)","attachmentId":51165003,"attachmentType":"pdf","work_url":"https://www.academia.edu/30716473/Registro_de_conodontos_delTri%C3%A1sico_Medio_en_un_nautiloideode_Espejeras_Alicante_Espa%C3%B1a_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/30716473/Registro_de_conodontos_delTri%C3%A1sico_Medio_en_un_nautiloideode_Espejeras_Alicante_Espa%C3%B1a_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="9" data-entity-id="69564224" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/69564224/Revisi%C3%B3n_bioestratigr%C3%A1fica_de_los_dep%C3%B3sitos_marinos_del_Mioceno_medio_en_la_cuenca_del_Pened%C3%A8s">Revisión bioestratigráfica de los depósitos marinos del Mioceno medio en la cuenca del Penedès</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="135954945" href="https://independent.academia.edu/ignaciomacpherson">ignacio macpherson</a></div><p class="ds-related-work--metadata ds2-5-body-xs">1994</p><p class="ds-related-work--abstract ds2-5-body-sm">Plancktonic foraminifera in middle Miocene marine sediments in the Penedes basin (NE Spain) have been examined. Using the findings of chronostratigrapbic markers in representative basin sections, identification of Langhian materials and hypothetical biostratigraphical correlations among sections have been established. Besides, the existence of Burdigalian deposits in the lower samples of the sections studied, reflecting the lower-middle Miocene transition, has been been established. The foraminifera species used are: Praeorbulina glomerosa sicana (DE STEFANI), Praeorbulina transitoria (BLOW), Globigerinoides bisphericus TODD and Globigerinoides altiaperturus (BOLLI).</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Revisión bioestratigráfica de los depósitos marinos del Mioceno medio en la cuenca del Penedès","attachmentId":79720018,"attachmentType":"pdf","work_url":"https://www.academia.edu/69564224/Revisi%C3%B3n_bioestratigr%C3%A1fica_de_los_dep%C3%B3sitos_marinos_del_Mioceno_medio_en_la_cuenca_del_Pened%C3%A8s","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/69564224/Revisi%C3%B3n_bioestratigr%C3%A1fica_de_los_dep%C3%B3sitos_marinos_del_Mioceno_medio_en_la_cuenca_del_Pened%C3%A8s"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div></div></div><div class="ds-sticky-ctas--wrapper js-loswp-sticky-ctas hidden"><div class="ds-sticky-ctas--grid-container"><div class="ds-sticky-ctas--container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{"location":"continue-reading-button--sticky-ctas","attachmentId":1317385,"attachmentType":"pdf","workUrl":null}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{"location":"download-pdf-button--sticky-ctas","attachmentId":1317385,"attachmentType":"pdf","workUrl":null}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div></div></div><div class="ds-below-fold--grid-container"><div class="ds-work--container js-loswp-embedded-document"><div class="attachment_preview" data-attachment="Attachment_1317385" style="display: none"><div class="js-scribd-document-container"><div class="scribd--document-loading js-scribd-document-loader" style="display: block;"><img alt="Loading..." src="//a.academia-assets.com/images/loaders/paper-load.gif" /><p>Loading Preview</p></div></div><div style="text-align: center;"><div class="scribd--no-preview-alert js-preview-unavailable"><p>Sorry, preview is currently unavailable. 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