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(PDF) Holocene Vegetation and Human Impact, Central Alps
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true; window.loswp.showSignupCaptcha = false window.loswp.willEdgeCache = false; window.loswp.work = {"work":{"id":46964219,"created_at":"2021-04-20T03:07:25.702-07:00","from_world_paper_id":168285386,"updated_at":"2025-01-31T11:31:55.239-08:00","_data":{"ai_title_tag":"Holocene Vegetation and Human Impact, Central Alps","grobid_abstract":"AIASSUNTO -Evotuzione della veqetezione e impeito entropico durante I'Olocene nelle Alpi Centrali. La successione paleobotanica del/a torbiera di Pian Venezia (Trento, Italia) -II Quaternario Italian Journal of QuaternarySciences, 9(2), 1996, 737-744 -In questa artico-10 vengono presentati i risultati preliminari delle anallsl palsobotanlche condotte sulla torbiera di Pian Venezia (2270 m s.l.rn., Val di Peio,Alpi italiane orlentall), Lo soopo della ricerca e la ricostruzione dell'evoluzione olocenlca della vegetazione in un arnbiente ad elevate altltudlne, presso i1limite del bosco, Sulla successione di torba sono state ottenute 6 date 14C. La sedimentazione orqanica e lnlzlata in una fase avanzata del Preboreale ed econtinuata fino al presente. La successione polllnlca di Pian Venezia ha registrato numerosi eventi vegetazionali chs hanno caratterizzato la storia della vegetazione nell'Olocene. Nel tarde Preboreale una prateria alplna con arbusti (Salix e Alnus) e presente nelle vicinanze della torbiera, mentre psrslstono aree con vegetazione discontinua picnlera, come indicata dalla presenza di granuli di Androsace ed Oxyria. Picea compare con curva continua circa 8.900 anni BP e sublsee un brusco aumento circa 8.700 anni BP, allorche I'abete rosso raggiunge I'alta Val di Peio. Durante l'Atlantico medio e superlors, la presenza nella torba di aghi e stomi di cambro e di larice nonche di semi di cembro indicano che iI bosco circondava la torblera, Fagus e di Abies cornpalono rispettivamente circa 6.500 e 6.000-5.500 anni BP. Due lmportantl fasi di impatto antropico sono evidentl: ta prima (4.000 -3.000 annl BP) pub essere attribuita al tardo Neolitico, la seconda (che inizia circa 2.200 anni BP) al perlodo romano. Nei livelli datati a quest'ultirna fase compaiono spore di Podospore e Sporormielte, funghi coprofili, il che suggerisce I'estenslone del pascolo nel Pian Venezia.","grobid_abstract_attachment_id":"66311497"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"high","language":"en","title":"Holocene vegetation development and human impact in the Central Alps: The 'Pian Venezia' palaeobotanical record (Trento, Italy)","broadcastable":true,"draft":null,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [64762434]; window.loswp.locale = "en"; window.loswp.countryCode = "SG"; window.loswp.cwvAbTestBucket = ""; window.loswp.designVariant = "ds_vanilla"; window.loswp.fullPageMobileSutdModalVariant = "full_page_mobile_sutd_modal"; window.loswp.useOptimizedScribd4genScript = false; window.loginModal = {}; window.loginModal.appleClientId = 'edu.academia.applesignon'; window.userInChina = "false";</script><script defer="" src="https://accounts.google.com/gsi/client"></script><div class="ds-loswp-container"><div class="ds-work-card--grid-container"><div class="ds-work-card--container js-loswp-work-card"><div class="ds-work-card--cover"><div class="ds-work-cover--wrapper"><div class="ds-work-cover--container"><button class="ds-work-cover--clickable js-swp-download-button" data-signup-modal="{"location":"swp-splash-paper-cover","attachmentId":66311497,"attachmentType":"pdf"}"><img alt="First page of “Holocene vegetation development and human impact in the Central Alps: The 'Pian Venezia' palaeobotanical record (Trento, Italy)”" class="ds-work-cover--cover-thumbnail" src="https://0.academia-photos.com/attachment_thumbnails/66311497/mini_magick20210420-13722-kemfnm.png?1618920773" /><img alt="PDF Icon" class="ds-work-cover--file-icon" src="//a.academia-assets.com/images/single_work_splash/adobe_icon.svg" /><div class="ds-work-cover--hover-container"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span><p>Download Free PDF</p></div><div class="ds-work-cover--ribbon-container">Download Free PDF</div><div class="ds-work-cover--ribbon-triangle"></div></button></div></div></div><div class="ds-work-card--work-information"><h1 class="ds-work-card--work-title">Holocene vegetation development and human impact in the Central Alps: The 'Pian Venezia' palaeobotanical record (Trento, Italy)</h1><div class="ds-work-card--work-authors ds-work-card--detail"><a class="ds-work-card--author js-wsj-grid-card-author ds2-5-body-md ds2-5-body-link" data-author-id="64762434" href="https://independent.academia.edu/CesareRavazzi"><img alt="Profile image of Cesare Ravazzi" class="ds-work-card--author-avatar" src="//a.academia-assets.com/images/s65_no_pic.png" />Cesare Ravazzi</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 = 46964219; 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La successione paleobotanica del/a torbiera di Pian Venezia (Trento, Italia) -II Quaternario Italian Journal of QuaternarySciences, 9(2), 1996, 737-744 -In questa artico-10 vengono presentati i risultati preliminari delle anallsl palsobotanlche condotte sulla torbiera di Pian Venezia (2270 m s.l.rn., Val di Peio,Alpi italiane orlentall), Lo soopo della ricerca e la ricostruzione dell'evoluzione olocenlca della vegetazione in un arnbiente ad elevate altltudlne, presso i1limite del bosco, Sulla successione di torba sono state ottenute 6 date 14C. La sedimentazione orqanica e lnlzlata in una fase avanzata del Preboreale ed econtinuata fino al presente. La successione polllnlca di Pian Venezia ha registrato numerosi eventi vegetazionali chs hanno caratterizzato la storia della vegetazione nell'Olocene. Nel tarde Preboreale una prateria alplna con arbusti (Salix e Alnus) e presente nelle vicinanze della torbiera, mentre psrslstono aree con vegetazione discontinua picnlera, come indicata dalla presenza di granuli di Androsace ed Oxyria. Picea compare con curva continua circa 8.900 anni BP e sublsee un brusco aumento circa 8.700 anni BP, allorche I'abete rosso raggiunge I'alta Val di Peio. Durante l'Atlantico medio e superlors, la presenza nella torba di aghi e stomi di cambro e di larice nonche di semi di cembro indicano che iI bosco circondava la torblera, Fagus e di Abies cornpalono rispettivamente circa 6.500 e 6.000-5.500 anni BP. Due lmportantl fasi di impatto antropico sono evidentl: ta prima (4.000 -3.000 annl BP) pub essere attribuita al tardo Neolitico, la seconda (che inizia circa 2.200 anni BP) al perlodo romano. Nei livelli datati a quest'ultirna fase compaiono spore di Podospore e Sporormielte, funghi coprofili, il che suggerisce I'estenslone del pascolo nel Pian Venezia.</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":66311497,"attachmentType":"pdf","workUrl":"https://www.academia.edu/46964219/Holocene_vegetation_development_and_human_impact_in_the_Central_Alps_The_Pian_Venezia_palaeobotanical_record_Trento_Italy_"}">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":66311497,"attachmentType":"pdf","workUrl":"https://www.academia.edu/46964219/Holocene_vegetation_development_and_human_impact_in_the_Central_Alps_The_Pian_Venezia_palaeobotanical_record_Trento_Italy_"}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div><div class="ds-signup-banner-trigger-container"><div class="ds-signup-banner-trigger ds-signup-banner-trigger-control"></div></div><div class="ds-signup-banner ds-signup-banner-control"><div id="ds-signup-banner-close-button"><button class="ds2-5-button ds2-5-button--secondary ds2-5-button--inverse"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">close</span></button></div><div class="ds-signup-banner-ctas"><img src="//a.academia-assets.com/images/academia-logo-capital-white.svg" /><h4 class="ds2-5-heading-serif-sm">Sign up for access to the world's latest research</h4><button class="ds2-5-button ds2-5-button--inverse ds2-5-button--full-width js-swp-download-button" data-signup-modal="{"location":"signup-banner"}">Sign up for free<span class="material-symbols-outlined" style="font-size: 20px" translate="no">arrow_forward</span></button></div><div class="ds-signup-banner-divider"></div><div class="ds-signup-banner-reasons"><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Get notified about relevant papers</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Save papers to use in your research</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Join the discussion with peers</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Track your impact</span></div></div></div><script>(() => { // Set up signup banner show/hide behavior: // 1. 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Ravazzi on``Paleoclimatic record of the past 22,000 yr in Venice (Northern Italy): Biostratigraphic evidence and chronology''[Quaternary …</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="157777" href="https://ita-professional.academia.edu/AlbertoLezziero">Alberto Lezziero</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Quaternary …, 2007</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":"Reply to the comment by C. Ravazzi on``Paleoclimatic record of the past 22,000 yr in Venice (Northern Italy): Biostratigraphic evidence and chronology''[Quaternary …","attachmentId":51315255,"attachmentType":"pdf","work_url":"https://www.academia.edu/644945/Reply_to_the_comment_by_C_Ravazzi_onPaleoclimatic_record_of_the_past_22_000_yr_in_Venice_Northern_Italy_Biostratigraphic_evidence_and_chronology_Quaternary_","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/644945/Reply_to_the_comment_by_C_Ravazzi_onPaleoclimatic_record_of_the_past_22_000_yr_in_Venice_Northern_Italy_Biostratigraphic_evidence_and_chronology_Quaternary_"><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="16663431" 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/16663431/PINI_R_BERTINI_A_MARTINETTO_E_VASSIO_E_2014_The_Pleistocene_flora_of_northern_Italy_In_Kustatscher_E_Roghi_G_Bertini_A_Miola_A_eds_Palaeobotany_of_Italy_Naturmuseum_Sudtirol_pp_290_307_ISBN_978_88_87108_06_4">PINI, R., BERTINI, A., MARTINETTO, E., VASSIO, E., 2014. The Pleistocene flora of northern Italy. In Kustatscher, E., Roghi, G., Bertini, A., Miola, A (eds.), Palaeobotany of Italy. Naturmuseum Sudtirol, pp. 290-307. ISBN 978-88-87108-06-4</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="5714420" href="https://unito.academia.edu/EdoardoMartinetto">Edoardo Martinetto</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":"PINI, R., BERTINI, A., MARTINETTO, E., VASSIO, E., 2014. The Pleistocene flora of northern Italy. In Kustatscher, E., Roghi, G., Bertini, A., Miola, A (eds.), Palaeobotany of Italy. Naturmuseum Sudtirol, pp. 290-307. ISBN 978-88-87108-06-4","attachmentId":39106736,"attachmentType":"pdf","work_url":"https://www.academia.edu/16663431/PINI_R_BERTINI_A_MARTINETTO_E_VASSIO_E_2014_The_Pleistocene_flora_of_northern_Italy_In_Kustatscher_E_Roghi_G_Bertini_A_Miola_A_eds_Palaeobotany_of_Italy_Naturmuseum_Sudtirol_pp_290_307_ISBN_978_88_87108_06_4","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/16663431/PINI_R_BERTINI_A_MARTINETTO_E_VASSIO_E_2014_The_Pleistocene_flora_of_northern_Italy_In_Kustatscher_E_Roghi_G_Bertini_A_Miola_A_eds_Palaeobotany_of_Italy_Naturmuseum_Sudtirol_pp_290_307_ISBN_978_88_87108_06_4"><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="30907879" 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/30907879/The_Lateglacial_and_early_Holocene_sequence_of_Grotta_di_Pozzo_L_Aquila_in_the_mountains_of_central_Italy">The Lateglacial and early Holocene sequence of Grotta di Pozzo (L’Aquila), in the mountains of central Italy</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="909683" href="https://unican.academia.edu/ElianaCatelli">Eliana Catelli</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="3972111" href="https://uni-tuebingen.academia.edu/EleonoraGargani">Eleonora Gargani</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="2370845" href="https://uniroma1.academia.edu/GiuseppeDeAngelis">Giuseppe De Angelis</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="6143674" href="https://urv.academia.edu/GiancarloRuta">Giancarlo Ruta</a></div><p class="ds-related-work--abstract ds2-5-body-sm">a cura di / eds.:</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":"The Lateglacial and early Holocene sequence of Grotta di Pozzo (L’Aquila), in the mountains of central Italy","attachmentId":51332611,"attachmentType":"pdf","work_url":"https://www.academia.edu/30907879/The_Lateglacial_and_early_Holocene_sequence_of_Grotta_di_Pozzo_L_Aquila_in_the_mountains_of_central_Italy","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/30907879/The_Lateglacial_and_early_Holocene_sequence_of_Grotta_di_Pozzo_L_Aquila_in_the_mountains_of_central_Italy"><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="12608502" 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/12608502/Biochronology_and_palaeoenvironmental_changes_from_the_Middle_Pliocene_to_the_Late_Pleistocene_in_Central_Italy">Biochronology and palaeoenvironmental changes from the Middle Pliocene to the Late Pleistocene in Central Italy</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="31552565" href="https://independent.academia.edu/LeonardoSalari">Leonardo Salari</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="5714420" href="https://unito.academia.edu/EdoardoMartinetto">Edoardo Martinetto</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Geodiversitas, 2011</p><p class="ds-related-work--abstract ds2-5-body-sm">Biochronologie et variations paléo-environnementales en Italie centrale du Pliocène moyen à la fi n du Pléistocène. Les variations paléo-environnementales qui ont eu lieu en Italie du Pliocène moyen au Pléistocène supérieur sont décrites. Il semblerait que le nombre des espèces de mammifères de grande taille ait peu augmenté, surtout pour les unités biochronologiques du Galérien à l’Aurélien supérieur. Au contraire, les données paléobotaniques montrent une diminution progressive des espèces arborées depuis le Pliocène moyen jusqu’au début du Pléistocène inférieur et une augmentation des surfaces occupées par les prairies et les steppes. Ces derniers évènements sont attestés par l’apparition des espèces hypsodontes parmi les mammifères. La répartition des faunes de mammifères entre les côtes adriatique et tyrrhénienne de l’Italie centrale, pendant le Pléistocène moyen et supérieur, semble ne pas avoir été infl uencée par des diff érences climatiques et environnementales. Quand les données sur l’Adriatique sont plus complètes, il est en fait alors possible d’observer une tendance qui est similaire à celles de la Tyrrhénienne. La plupart des mégaherbivores ont une origine asiatique, et on peut émettre l’hypothèse que dans les phases interglaciaires, l’Appennin toscan-émilien a permis aux taxons qui venaient du Nord-Est de l’Europe, de rentrer et se diff user sur la côte de la mer Tyrrhénienne, plus diversifi ée, alors que durant les périodes glacières, ils ont suivi l’étroit couloir de la Ligurie. Cette recherche confi rme encore le rôle de la péninsule italienne comme aire de refuge de l’Europe continentale ; cette condition particulière a permis aux faunes de mammifères italiennes de développer des lignées endémiques (comme Elephas antiquus italicus Osborn, 1931, Cervus elaphus rianensis Leonardi & Petronio, 1974, C. e. aretinus Azzaroli, 1947, etc.). Pour terminer, la biodiversité a subi une forte chute dans les derniers 30 000 ans, très probablement provoquée par les activités anthropiques et le refroidissement climatique du dernier périglaciaire.</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":"Biochronology and palaeoenvironmental changes from the Middle Pliocene to the Late Pleistocene in Central Italy","attachmentId":46053222,"attachmentType":"pdf","work_url":"https://www.academia.edu/12608502/Biochronology_and_palaeoenvironmental_changes_from_the_Middle_Pliocene_to_the_Late_Pleistocene_in_Central_Italy","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/12608502/Biochronology_and_palaeoenvironmental_changes_from_the_Middle_Pliocene_to_the_Late_Pleistocene_in_Central_Italy"><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="9635632" 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/9635632/4_3_La_flora_del_Carbonifero_della_Sardegna_The_Carboniferous_flora_of_Sardinia">4.3 La flora del Carbonifero della Sardegna - The Carboniferous flora of Sardinia</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="2763431" href="https://unica-it.academia.edu/GiovanniGScanu">Giovanni G. Scanu</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="2706756" href="https://unica.academia.edu/CarlaBuosi">Carla Buosi</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":"4.3 La flora del Carbonifero della Sardegna - The Carboniferous flora of Sardinia","attachmentId":35837632,"attachmentType":"pdf","work_url":"https://www.academia.edu/9635632/4_3_La_flora_del_Carbonifero_della_Sardegna_The_Carboniferous_flora_of_Sardinia","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/9635632/4_3_La_flora_del_Carbonifero_della_Sardegna_The_Carboniferous_flora_of_Sardinia"><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="4909181" 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/4909181/New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_">New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)</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="2530541" href="https://uib-es.academia.edu/Lloren%C3%A7PicornellGelabert">Llorenç Picornell-Gelabert</a></div><p class="ds-related-work--abstract ds2-5-body-sm">Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. 14 C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. Environmental data, obtained from microvertebrate and archaeobotanical remains, show the aridification and opening of the landscape from the base to the top of the sequence as a consequence of the human impact.</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":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)","attachmentId":32173547,"attachmentType":"pdf","work_url":"https://www.academia.edu/4909181/New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_","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/4909181/New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_"><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="23034282" 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/23034282/Elements_to_correlate_marine_and_continental_sedimentary_successions_in_the_context_of_the_neotectonic_evolution_of_the_central_Apennines">Elements to correlate marine and continental sedimentary successions in the context of the neotectonic evolution of the central Apennines</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="44681563" href="https://romatre.academia.edu/PaolaMolin">Paola Molin</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Il Quaternario, 2003</p><p class="ds-related-work--abstract ds2-5-body-sm">E Er rn ne es st to o C Ce en nt ta am mo or re e 1 1 , , F Fr ra an nc ce es sc co o D Dr ra am mi is s 2 2 , , G Gi ia an nd do om me en ni ic co o F Fu ub be el ll li i 2 2 , , P Pa ao ol la a M Mo ol li in n 2 2 & & S St te ef fa an ni ia a N Ni is si io o 3 3 ABSTRACT The central Apennines show geologic and geomorphic features that report the strong influence of extensional tectonics and regional uplift on their recent evolution. The goal of this paper is to find out the time constraints of the chain uplift, focusing on the elements of correlation between marine and continental successions on both the Adriatic and Tyrrhenian sides. All along the range, the most ancient landforms are gently rolling or flat summit surfaces. On the Tyrrhenian side, the interaction between the chain uplift and the extensional tectonics related to the opening of the Tyrrhenian basin, generated several neoautoctonous basins that are older in Tuscany (since the Tortonian) and younger in the Latium-Abruzzo area (since the Pliocene). On the Adriatic side, the combined action of uplift and climatic changes, produced several depositional sequences, separated by angular unconformities. In the western basins, progressively coarsening upward sediments, corresponding to the Globorotalia crassaformis biozone, are found. At Valle Ricca, in the upper section of these deposits, a 2.1 Myr old volcanic layer, corresponding to the base of the Globorotalia inflata biozone, is present. The Valle Ricca succession is truncated by an erosion surface over which marine and brackish sandy clay (Argille Sabbiose del Chiani-Tevere) lay down. Similarly, in the periadriatic basin, a volcanic layer, dated 2.1 Myr, has been found at Bellante, in the upper part of a pelitic sequence. An angular unconformity separates this sequence from overlaying conglomerate and sand, recording a progressively eastward shifting of the coastline as a consequence of the uplift. Contemporaneously, extensional tectonics progressively affected the Apennine chain giving rise to a number of intermontane depressions, within which coarse breccia and lacustrine-alluvial deposits were deposited. In the Rieti and L'Aquila basins, the finding of Equus stenonis and Mammuthus meridionalis refer the basal part of these deposits to an age not older than the lower Pleistocene. Around 0.8 Myr B.P., in correspondence with a base level drop induced by a sudden increase of uplift rate, the coastline rapidily shifted seawards and littoral sandy-pebbly sediments were deposited along both sides of the Apennines. Contemporaneously, increased stream erosion rates gave rise to the present valley network, within which the interaction of river incision and climate changes generated several orders of alluvial terraces. In this contest, a hunched backward river erosion breached most of intramontane depressions, draining off the lakes and causing the erosion of the basin sedimentary sequence. In conclusion, according to all these considerations, we hypothesize that the topographic growth of the range was slow until the end of the lower Pleistocene, when a strong increase of the uplift rate affected the chain and the surrounding coastal belts. RIASSUNTO L'Appennino centrale presenta caratteri geologici e geomorfologici che documentano l'intensa influenza della tettonica estensionale e del sollevamento regionale sulla sua evoluzione recente. In questo lavoro si intendono evidenziare gli elementi di correlazione tra le successioni marine e continentali della fascia periadriatica abruzzese e peritirrenica laziale, al fine di proporre dei vincoli temporali all'evoluzione recente dell'Appennino. Gli elementi geomorfologici più antichi, riscontrabili lungo tutta la catena appenninica, sono rappresentati da superfici sommitali gentilmente ondulate o pianeggianti. Sul versante occidentale la tettonica distensiva legata all'apertura del Tirreno ha generato una complessa serie di bacini neoautoctoni più antichi in Toscana (dal Tortoniano) e più recenti nell'area laziale (dal Pliocene). Sul versante adriatico il sollevamento della catena ha dato origine a discordanze angolari che individuano numerose sequenze sedimentarie in assetto monoclinalico. Sul versante tirrenico della catena, si depositano sedimenti progressivamente più grossolani riferibili alla fine della biozona a Globorotalia crassaformis. In particolare, a Valle Ricca, al tetto di questi depositi e alla base della biozona a Globorotalia inflata, è stato trovato un livello vulcanico datato 2.1 Ma. Su tale successione si appoggiano in discordanza le "Argille Sabbiose del Chiani-Tevere" di ambiente marino e salmastro. Similmente, sul versante adriatico, presso Bellante, è stato rinvenuto un livello vulcanico datato 2.1 Ma nella parte superiore di una sequenza di depositi pelitici. Questa è troncata al tetto da una discordanza angolare che la separa da sedimenti conglomeratici e sabbiosi. Contemporaneamente, la tettonica estensionale interessa progressivamente la catena generando una serie di bacini intermontani, delimitati da faglie normali. I materiali di riempimento sono costituiti alla base da sedimenti grossolani che passano verso l'alto a depositi alluvionali e fluvio-lacustri. Nelle conche di Rieti e de L'Aquila il ritrovamento di Equus stenonis e Mammuthus meridionalis consente di riferire la parte basale di questi sedimenti ad un'età non più giovane del Pleistocene inferiore. Intorno a 0.8 Ma B.P., in concomitanza con un forte abbassamento relativo del livello di base, legato ad un subitaneo incremento del tasso di sollevamento, si verifica un più marcato avanzamento delle linee di costa, accompagnato dalla messa in posto di depositi sabbioso-ciottolosi di ambiente litorale lungo i margini occidentale e orientale dell'Appennino. Contemporaneamente, un aumento del tasso di incisione fluviale dà origine all'attuale sistema di valli, all'interno delle quali, per effetto dell'interazione tra l'aumento dell'erosione fluviale e le variazioni climatiche, si sono formati più ordini di terrazzi alluvionali. In tale contesto, l'erosione regressiva dei corsi d'acqua ha profondamente inciso le soglie della maggior parte dei bacini intermontani, prosciugando i laghi ed erodendo gran parte dei depositi presenti. In conclusione, in base a queste considerazioni si può ipotizzare che la crescita topografica della catena appenninica è stata lenta fino alla fine del Pleistocene inferiore, quando si è verificato un forte incremento del tasso di sollevamento.</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":"Elements to correlate marine and continental sedimentary successions in the context of the neotectonic evolution of the central Apennines","attachmentId":43543184,"attachmentType":"pdf","work_url":"https://www.academia.edu/23034282/Elements_to_correlate_marine_and_continental_sedimentary_successions_in_the_context_of_the_neotectonic_evolution_of_the_central_Apennines","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/23034282/Elements_to_correlate_marine_and_continental_sedimentary_successions_in_the_context_of_the_neotectonic_evolution_of_the_central_Apennines"><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":66311497,"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":66311497,"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_66311497" 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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Italian Journal of Quaternary Science”, 22 (2), 2009</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":"Geoarcheological evidences of Late Holocene discontinuous progradation of the Versilia coastal plain between Camaiore and Viareggio (Tuscany, Italy)","attachmentId":30314974,"attachmentType":"pdf","work_url":"https://www.academia.edu/2262842/Geoarcheological_evidences_of_Late_Holocene_discontinuous_progradation_of_the_Versilia_coastal_plain_between_Camaiore_and_Viareggio_Tuscany_Italy_","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-related-work-grid-card-view-pdf" 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record of the past 22,000 years in Venice (Northern Italy): Biostratigraphic evidence and chronology” by Serandrei Barbero et al. [Quaternary International 140–141, 37–52]. “Interstadials” or phases of accumulation of reworked pollen?</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1273542" href="https://unimib.academia.edu/CesareRavazzi">Cesare Ravazzi</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Quaternary International, 2006</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":"Comment on “Paleoclimatic record of the past 22,000 years in Venice (Northern Italy): Biostratigraphic evidence and chronology” by Serandrei Barbero et al. 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href="https://www.academia.edu/17080433/Comment_on_Paleoclimatic_record_of_the_past_22_000_years_in_Venice_Northern_Italy_Biostratigraphic_evidence_and_chronology_by_Serandrei_Barbero_et_al_Quaternary_International_140_141_37_52_Interstadials_or_phases_of_accumulation_of_reworked_pollen"><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-related-work-sidebar-card" data-collection-position="16" data-entity-id="38475632" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/38475632/Holt_et_al_2018_Middle_Upper_Paleolithic_transition_Riparo_Bombrini_Balzi_Rossi_Liguria_Italy_pdf">Holt et al 2018 - Middle-Upper Paleolithic transition Riparo Bombrini (Balzi Rossi, Liguria, Italy).pdf</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1849892" href="https://lingue.academia.edu/FabioNegrino">Fabio Negrino</a><span>, </span><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="547136" href="https://museoarcheofinale.academia.edu/DanieleArobba">Daniele Arobba</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Quaternary International, 2018</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":"Holt et al 2018 - Middle-Upper Paleolithic transition Riparo Bombrini (Balzi Rossi, Liguria, Italy).pdf","attachmentId":59028391,"attachmentType":"pdf","work_url":"https://www.academia.edu/38475632/Holt_et_al_2018_Middle_Upper_Paleolithic_transition_Riparo_Bombrini_Balzi_Rossi_Liguria_Italy_pdf","alternativeTracking":true}"><span 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northern Apennines, Italy”, Il Capitale Culturale 12: 537-563 [2015]</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="304354" href="https://unipi.academia.edu/LionelloMorandi">Lionello Morandi</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Il Capitale Culturale 12 (2015), pp. 537-563 (ISSN 2039-2362)</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":"“Late Würm and Early-Middle Holocene environmental change and human activities in the northern Apennines, Italy”, Il Capitale Culturale 12: 537-563 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In the upper Volturno basin, central Italy: first report</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="300602" href="https://unisi.academia.edu/MauroColtorti">Mauro Coltorti</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":"Isernia La Pineta: lower paleolithic with fauna before 0,7 M.Y. 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data-entity-id="11466228" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/11466228/Anthropic_land_use_and_vegetation_dynamics_in_mountain_areas_of_Cavargna_Valley_Lepontine_Alps_Lombardy_N_Italy_during_the_Holocene_Lanfredo_Castelletti">Anthropic land use and vegetation dynamics in mountain areas of Cavargna Valley (Lepontine Alps, Lombardy, N-Italy) during the Holocene Lanfredo Castelletti</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="3205611" href="https://google.academia.edu/LanfredoCastelletti">Lanfredo Castelletti</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":"Anthropic land use and vegetation dynamics in mountain areas of Cavargna Valley 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The peopling of northern and central Italy at the LGM. In: Antonioli F., Vai G.B. (eds.) Litho-Palaeoenvironmental Maps of Italy during the last two Climatic Extremes, Explanatory Notes, pp. 59-60. Museo Geologico Giovanni Capellini: Bologna</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="8738704" href="https://uniroma1.academia.edu/MargheritaMussi">Margherita Mussi</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":"MUSSI M., PERESANI M. 2004. The peopling of northern and central Italy at the LGM. In: Antonioli F., Vai G.B. (eds.) Litho-Palaeoenvironmental Maps of Italy during the last two Climatic Extremes, Explanatory Notes, pp. 59-60. 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