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class="ds2-5-body-sm-bold">Talks</span></a></li></ul></div><div class="divider ds-divider-16" style="margin: 0px;"></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Marcello Schiattarella</h3></div><div class="js-work-strip profile--work_container" data-work-id="98257760"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/98257760/Carta_Geologica_dItalia_alla_scala_1_50000_F_504_Sala_Consilina"><img alt="Research paper thumbnail of Carta Geologica d'Italia alla scala 1:50000 - F.504 Sala Consilina" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/98257760/Carta_Geologica_dItalia_alla_scala_1_50000_F_504_Sala_Consilina">Carta Geologica d'Italia alla scala 1:50000 - F.504 Sala Consilina</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/EVAPESCATORE">Eva Pescatore</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://unibas-it.academia.edu/MarcelloSchiattarella">Marcello Schiattarella</a></span></div><div class="wp-workCard_item"><span>A.T.I., SystemCart srl, L.A.C. srl. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="109660046"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/109660046/In_situ_and_satellite_long_term_monitoring_of_the_Latronico_landslide_Italy_displacement_evolution_damage_to_buildings_and_effectiveness_of_remedial_works"><img alt="Research paper thumbnail of In situ and satellite long-term monitoring of the Latronico landslide, Italy: displacement evolution, damage to buildings, and effectiveness of remedial works" class="work-thumbnail" src="https://attachments.academia-assets.com/107718478/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/109660046/In_situ_and_satellite_long_term_monitoring_of_the_Latronico_landslide_Italy_displacement_evolution_damage_to_buildings_and_effectiveness_of_remedial_works">In situ and satellite long-term monitoring of the Latronico landslide, Italy: displacement evolution, damage to buildings, and effectiveness of remedial works</a></div><div class="wp-workCard_item"><span>Engineering Geology</span><span>, Nov 1, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a764130565f29220d9ef0cb1d75de710" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":107718478,"asset_id":109660046,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/107718478/download_file?st=MTczMjgzMjI0OCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="109660046"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="109660046"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 109660046; 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The spatial and temporal evolution of a multi-stage complex landslide located in a catchment of the frontal sector of the southern Apennine chain was reconstructed by multitemporal geomorphological analysis, near-surface seismic survey, and DEM comparison. The Tolve landslide shows a multi-decadal evolution characterized by intermittent periods of activity and dormancy. Geomorphological evidences suggest that the initial failure of the large-scale landslide has a multi-millennial age and can be related to a rototranslational movement that evolved in an earth ow. Recent evolution is associated with a major reactivation event in the middle and lower sectors of the larger complex landslide, which probably is related to a heavy rainfall event occurred in January 1972. Recent evolution is mainly associated with minor movements in the source area, toe advancements, and widespread shallow landslides along the ank of the earth ow. 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geodatabase of Late Pleistocene - Holocene palaeo sea-level markers in the Gulf of Naples" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/109660039/A_geodatabase_of_Late_Pleistocene_Holocene_palaeo_sea_level_markers_in_the_Gulf_of_Naples">A geodatabase of Late Pleistocene - Holocene palaeo sea-level markers in the Gulf of Naples</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">During the Late Pleistocene and Holocene periods, the Italian coasts have undergone a very articu...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">During the Late Pleistocene and Holocene periods, the Italian coasts have undergone a very articulated geological and geomorphological evolution, due to the complex and differentiated interaction of endogenous and exogenous dynamics. Aim of this study is to implement a geodatabase concerning the geomorphological, stratigraphic, biological and archaeological palaeo sea-level proxies located in the Gulf of Naples, in order to provide a catalogue of the most representative markers and an overall picture of ancient shorelines positions since the Late Pleistocene.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="109660039"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="109660039"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 109660039; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=109660039]").text(description); $(".js-view-count[data-work-id=109660039]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 109660039; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='109660039']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 109660039, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=109660039]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":109660039,"title":"A geodatabase of Late Pleistocene - Holocene palaeo sea-level markers in the Gulf of Naples","translated_title":"","metadata":{"abstract":"During the Late Pleistocene and Holocene periods, the Italian coasts have undergone a very articulated geological and geomorphological evolution, due to the complex and differentiated interaction of endogenous and exogenous dynamics. 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Landforms analysis completed the frame of the recent evolution of the plain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="115151978"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="115151978"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 115151978; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=115151978]").text(description); $(".js-view-count[data-work-id=115151978]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 115151978; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='115151978']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 115151978, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=115151978]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":115151978,"title":"Late Quaternary geology and morphoevolution of the Volturno coastal plain, southern Italy","translated_title":"","metadata":{"abstract":"The Volturno alluvial-coastal plain is a relevant feature of the Tyrrhenian side of southern Italy. 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Responsabile del Progetto CARG per la Regione Camp...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Dirigente Settore Difesa del Suolo: Giulivo I. Responsabile del Progetto CARG per la Regione Campania: Monti L. Aree emerse Isola di Procida Coordinatore scientifico: D&#39;Argenio B. Redazione scientifica: Putignano M.L. Direttore del rilevamento: Morra V. Rilevatori: Perrotta A., Scarpati C. Analisi petrochimiche: Fedele L. Analisi geocronologiche 40Ar/39Ar: Calvert A.T., Insinga D., Lepore S. Isola di Vivara Coordinatore scientifico e Direttore del rilevamento: Sbrana A. Rilevatori: Marianelli P., Sbrana A. Aree marine Coordinatori scientifici: D&#39;Argenio B., Marsella E. Redazione scientifica: Putignano M.L. 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In order to obtain a deeper insight in the phenomenon, its kinematic features have been investigated by means of both ground based displacement measurements (by mobile and fixed-in-place inclinometers) and by the processing of images acquired by synthetic aperture radar sensors (ERS, Envisat, COSMO-SkyMed satellites). The results of the analyses show that the landslide system includes different phenomena at different scales and of different age, from old and huge landslides (early stage of last post-glacial) to young shallower reactivations. Secondary creep and rain-induced displacements coexist, occurring at different depths. The reconstruction of the kinematic history of the system inhabited area-subsoil shows that the yearly average displacement rates have been almost constant over the last 25 years (several cm/year). The depth of the slip surfaces and the volumes of the instable soils explain why the numerous and expensive remedial measures and stabilization interventions have had very limited effects, if any, on the displacement rate field.","publication_date":{"day":1,"month":11,"year":2018,"errors":{}},"publication_name":"Engineering Geology","grobid_abstract_attachment_id":107718478},"translated_abstract":null,"internal_url":"https://www.academia.edu/109660046/In_situ_and_satellite_long_term_monitoring_of_the_Latronico_landslide_Italy_displacement_evolution_damage_to_buildings_and_effectiveness_of_remedial_works","translated_internal_url":"","created_at":"2023-11-23T05:06:25.203-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":30759451,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":107718478,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/107718478/thumbnails/1.jpg","file_name":"j.enggeo.2018.08.01720231123-1-fazqib.pdf","download_url":"https://www.academia.edu/attachments/107718478/download_file?st=MTczMjgzMjI0OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"In_situ_and_satellite_long_term_monitori.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/107718478/j.enggeo.2018.08.01720231123-1-fazqib-libre.pdf?1700745517=\u0026response-content-disposition=attachment%3B+filename%3DIn_situ_and_satellite_long_term_monitori.pdf\u0026Expires=1732835746\u0026Signature=OW3fvL6rzNqPtxqQF0L~IxXwahlFgqQKNb59xKpvSgNGNULHQNJ72JafSuKf3i0TcgmIXe6F3rjh7Ar-Gs0x4ZQVTarFHSAwFyYAvF0ZaD1NtpQnHEAu2l8IamEOxkS6hLAdd63l4wBU5LdIz-YZAUqumOj8If~INvkzsjHk5tthK1cBWMDVkt0zEWP-EnCuTHhpFdngM5CNh117Ym7iI-JPBmqzHncdWojNXqZl6ZRwRoWcl5sxnjqLhgOWVOnYYCPr914Tr3efkq8s6FA-q3j1J-tMVNN8AkEz98AorIVnVRuunMgTBQdzRXEPccqbf8S1yoVZrDzZ75Bp5dEsCQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"In_situ_and_satellite_long_term_monitoring_of_the_Latronico_landslide_Italy_displacement_evolution_damage_to_buildings_and_effectiveness_of_remedial_works","translated_slug":"","page_count":41,"language":"en","content_type":"Work","owner":{"id":30759451,"first_name":"Marcello","middle_initials":"","last_name":"Schiattarella","page_name":"MarcelloSchiattarella","domain_name":"unibas-it","created_at":"2015-05-05T03:02:43.265-07:00","display_name":"Marcello Schiattarella","url":"https://unibas-it.academia.edu/MarcelloSchiattarella"},"attachments":[{"id":107718478,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/107718478/thumbnails/1.jpg","file_name":"j.enggeo.2018.08.01720231123-1-fazqib.pdf","download_url":"https://www.academia.edu/attachments/107718478/download_file?st=MTczMjgzMjI0OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"In_situ_and_satellite_long_term_monitori.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/107718478/j.enggeo.2018.08.01720231123-1-fazqib-libre.pdf?1700745517=\u0026response-content-disposition=attachment%3B+filename%3DIn_situ_and_satellite_long_term_monitori.pdf\u0026Expires=1732835746\u0026Signature=OW3fvL6rzNqPtxqQF0L~IxXwahlFgqQKNb59xKpvSgNGNULHQNJ72JafSuKf3i0TcgmIXe6F3rjh7Ar-Gs0x4ZQVTarFHSAwFyYAvF0ZaD1NtpQnHEAu2l8IamEOxkS6hLAdd63l4wBU5LdIz-YZAUqumOj8If~INvkzsjHk5tthK1cBWMDVkt0zEWP-EnCuTHhpFdngM5CNh117Ym7iI-JPBmqzHncdWojNXqZl6ZRwRoWcl5sxnjqLhgOWVOnYYCPr914Tr3efkq8s6FA-q3j1J-tMVNN8AkEz98AorIVnVRuunMgTBQdzRXEPccqbf8S1yoVZrDzZ75Bp5dEsCQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":73,"name":"Civil Engineering","url":"https://www.academia.edu/Documents/in/Civil_Engineering"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":20564,"name":"Engineering Geology","url":"https://www.academia.edu/Documents/in/Engineering_Geology"},{"id":182316,"name":"Remedial Education","url":"https://www.academia.edu/Documents/in/Remedial_Education"},{"id":199886,"name":"Landslide","url":"https://www.academia.edu/Documents/in/Landslide"},{"id":215106,"name":"Satellite","url":"https://www.academia.edu/Documents/in/Satellite"}],"urls":[{"id":35747062,"url":"https://doi.org/10.1016/j.enggeo.2018.08.017"}]}, dispatcherData: dispatcherData }); 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The spatial and temporal evolution of a multi-stage complex landslide located in a catchment of the frontal sector of the southern Apennine chain was reconstructed by multitemporal geomorphological analysis, near-surface seismic survey, and DEM comparison. The Tolve landslide shows a multi-decadal evolution characterized by intermittent periods of activity and dormancy. Geomorphological evidences suggest that the initial failure of the large-scale landslide has a multi-millennial age and can be related to a rototranslational movement that evolved in an earth ow. Recent evolution is associated with a major reactivation event in the middle and lower sectors of the larger complex landslide, which probably is related to a heavy rainfall event occurred in January 1972. Recent evolution is mainly associated with minor movements in the source area, toe advancements, and widespread shallow landslides along the ank of the earth ow. 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geodatabase of Late Pleistocene - Holocene palaeo sea-level markers in the Gulf of Naples" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/109660039/A_geodatabase_of_Late_Pleistocene_Holocene_palaeo_sea_level_markers_in_the_Gulf_of_Naples">A geodatabase of Late Pleistocene - Holocene palaeo sea-level markers in the Gulf of Naples</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">During the Late Pleistocene and Holocene periods, the Italian coasts have undergone a very articu...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">During the Late Pleistocene and Holocene periods, the Italian coasts have undergone a very articulated geological and geomorphological evolution, due to the complex and differentiated interaction of endogenous and exogenous dynamics. Aim of this study is to implement a geodatabase concerning the geomorphological, stratigraphic, biological and archaeological palaeo sea-level proxies located in the Gulf of Naples, in order to provide a catalogue of the most representative markers and an overall picture of ancient shorelines positions since the Late Pleistocene.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="109660039"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="109660039"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 109660039; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=109660039]").text(description); $(".js-view-count[data-work-id=109660039]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 109660039; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='109660039']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 109660039, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=109660039]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":109660039,"title":"A geodatabase of Late Pleistocene - Holocene palaeo sea-level markers in the Gulf of Naples","translated_title":"","metadata":{"abstract":"During the Late Pleistocene and Holocene periods, the Italian coasts have undergone a very articulated geological and geomorphological evolution, due to the complex and differentiated interaction of endogenous and exogenous dynamics. Aim of this study is to implement a geodatabase concerning the geomorphological, stratigraphic, biological and archaeological palaeo sea-level proxies located in the Gulf of Naples, in order to provide a catalogue of the most representative markers and an overall picture of ancient shorelines positions since the Late Pleistocene.","publication_date":{"day":null,"month":null,"year":2018,"errors":{}}},"translated_abstract":"During the Late Pleistocene and Holocene periods, the Italian coasts have undergone a very articulated geological and geomorphological evolution, due to the complex and differentiated interaction of endogenous and exogenous dynamics. Aim of this study is to implement a geodatabase concerning the geomorphological, stratigraphic, biological and archaeological palaeo sea-level proxies located in the Gulf of Naples, in order to provide a catalogue of the most representative markers and an overall picture of ancient shorelines positions since the Late Pleistocene.","internal_url":"https://www.academia.edu/109660039/A_geodatabase_of_Late_Pleistocene_Holocene_palaeo_sea_level_markers_in_the_Gulf_of_Naples","translated_internal_url":"","created_at":"2023-11-23T05:06:23.496-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":30759451,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"A_geodatabase_of_Late_Pleistocene_Holocene_palaeo_sea_level_markers_in_the_Gulf_of_Naples","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":30759451,"first_name":"Marcello","middle_initials":"","last_name":"Schiattarella","page_name":"MarcelloSchiattarella","domain_name":"unibas-it","created_at":"2015-05-05T03:02:43.265-07:00","display_name":"Marcello Schiattarella","url":"https://unibas-it.academia.edu/MarcelloSchiattarella"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":30254,"name":"Pleistocene","url":"https://www.academia.edu/Documents/in/Pleistocene"},{"id":32163,"name":"Holocene sea level change","url":"https://www.academia.edu/Documents/in/Holocene_sea_level_change"},{"id":35587,"name":"Quaternary","url":"https://www.academia.edu/Documents/in/Quaternary"},{"id":78965,"name":"Holocene","url":"https://www.academia.edu/Documents/in/Holocene"},{"id":1013900,"name":"Cartographic Geodatabase","url":"https://www.academia.edu/Documents/in/Cartographic_Geodatabase"},{"id":2979514,"name":"Gulf of Naples","url":"https://www.academia.edu/Documents/in/Gulf_of_Naples"}],"urls":[{"id":35747055,"url":"https://iris.unibas.it/handle/11563/138785"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="5722340" id="talks"><div class="js-work-strip profile--work_container" data-work-id="28090791"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/28090791/Nuovo_progetto_di_ricerca_pluridisciplinare_sul_sito_del_Paleolitico_inferiore_del_Cimitero_di_Atella_Potenza_Basilicata_New_multidisciplinary_research_project_on_the_Lower_Palaeolithic_site_of_Cimitero_di_Atella_Potenza_Basilicata_"><img alt="Research paper thumbnail of Nuovo progetto di ricerca pluridisciplinare sul sito del Paleolitico inferiore del Cimitero di Atella (Potenza, Basilicata)/New multidisciplinary research project on the Lower Palaeolithic site of Cimitero di Atella (Potenza - Basilicata)." class="work-thumbnail" src="https://attachments.academia-assets.com/48407943/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/28090791/Nuovo_progetto_di_ricerca_pluridisciplinare_sul_sito_del_Paleolitico_inferiore_del_Cimitero_di_Atella_Potenza_Basilicata_New_multidisciplinary_research_project_on_the_Lower_Palaeolithic_site_of_Cimitero_di_Atella_Potenza_Basilicata_">Nuovo progetto di ricerca pluridisciplinare sul sito del Paleolitico inferiore del Cimitero di Atella (Potenza, Basilicata)/New multidisciplinary research project on the Lower Palaeolithic site of Cimitero di Atella (Potenza - Basilicata).</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://iuo.academia.edu/ClaudiaAbruzzese">Claudia Abruzzese</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://univ-paris1.academia.edu/RoxaneRocca">Roxane Rocca</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://mae.academia.edu/DanieleAureli">Daniele Aureli</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/LeoPaolaDi">Paola Di Leo</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PaoloGiannandrea">Paolo Giannandrea</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://unibas-it.academia.edu/MarcelloSchiattarella">Marcello Schiattarella</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Il sito del Cimitero di Atella, localizzato ai margini dell’attuale abitato, è ubicato circa 10 k...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Il sito del Cimitero di Atella, localizzato ai margini dell’attuale abitato, è ubicato circa 10 km a  sud del Monte Vulture (Basilicata, Italia meridionale). Lo scavo, condotto per più di vent’anni dal Prof. E. Borzatti von Löwenstern, ha riportato alla luce un’importante sequenza stratigrafica contenente due principali livelli archeologici attributi all’Acheuleano antico (Borzatti et al. 1990, 1997). Il materiale litico e faunistico, allo stato attuale delle ricerche, è datato a circa 0.63 Ma, sulla base di correlazioni stratigrafiche, vulcanologiche e biocronologiche (Borzatti et al. 1990; Ciolli 1997; Di Muro 1999; Zucchelli 2002). Un nuovo progetto multidisciplinare, avviato nel 2015, si propone di riattivare le ricerche su quest’importante sito, cercando di apportare un contributo alla problematica scientifica relativa al primo Acheuleano in Europa. L’obiettivo di questo programma è di rivalutare il contesto crono-stratigrafico, i processi di formazione del sito e le caratteristiche dell’associazione faunistica e dell’industria litica.  La presenza di depositi lacustri, probabilmente in relazione con il bacino endoreico di Atella-Vitalba, e di diversi livelli vulcanici, attribuibili verosimilmente ad episodi eruttivi del centro vulcanico del Vulture, permetteranno sicuramente di collocare la sequenza nel suo preciso contesto crono-stratigrafico. Un nuovo riesame dell’industria litica (Abruzzese 2014, Abruzzese et al. 2016) ha individuato nell’insieme una grande variabilità di catene operative (grandi strumenti, piccoli strumenti, produzione di schegge). Questa diversità, al centro delle problematiche attuali sul Paleolitico inferiore, fa del Cimitero di Atella un sito rilevante che permetterà di fornire nuovi e inediti dati al dibattito scientifico sull’evoluzione dei sistemi tecnici durante il Pleistocene medio in Italia. <br /><br />The site of Cimitero di Atella is located in the village of Atella (Basilicata, Southern Italy), at about 10 km of the Vulture Mt. The 20 years excavation of Prof. E. Borzatti von Löwenstern, brought to light an important sequence containing two archaeological levels attributed to the Lower Acheulean (Borzatti et al. 1990, 1997). The lithic implements and faunal remains are at the moment dated to 0.63 Ma on the base of stratigraphical, volcanological and biochronological correlations (Borzatti et al. 1990; Ciolli 1997; Di Muro 1999; Zucchelli 2002). A new multidisciplinary project, started in 2015, proposes to reactivate the research on this important site. The aim of this program is to re-assess the chrono-stratigraphical context, as well as the site formation and the features of fauna and lithic industry. The presence of lacustrine deposits at the bottom of the stratigraphic succession, related to the Atella paleo-lake, and of several volcanic layers in the uppermost part of the sequence, probably belonging to the Vulture Mt. eruptive events, will certainly allow us to re-collocate the sequence in a more precise chronological context. The new study of lithic industry (Abruzzese 2014, Abruzzese et al. 2016) shows that the assemblage contains in fact a great variability of reduction sequences (large cutting-tools, small tools, flakes production). This diversity, at the centre of the current research on Lower Palaeolithic, make of Cimitero di Atella an important site, which will add new and unpublished data to the debate on the evolution of technical systems in Italy during the Middle Pleistocene. <br /><br />References<br />Abruzzese, C., 2014. Il sito paleolitico di Atella (Pz) nel quadro del primo popolamento europeo: studio tecnologico dell’industria litica. Tesi di Laurea. Uni-versità degli Studi Di Napoli « L’Orientale ». <br />Abruzzese, C., Aureli, D., Rocca, R., 2016. Assessment of the Acheulean in Southern Italy: new study on the Cimitero di Atella site (Basilicata, Italy). Quaternary International 393, 158-168. <br />Borzatti von Löwenstern, E., Sozzi, M., Vannucci, S., Vianello, F., 1990. L’acheuleano antico del cimitero di Atella. Prime indagini sulla stratigrafia del sedimento e sulle industrie litiche. Studi per l’ecologia del quaternario 12.<br />Borzatti von Löwenstern, E., Palchetti, A., Sozzi, M. 1997. Témoignages de l’Acheuléen inferieur en Italie Méridionale: Le gisement du Cimitero di Atella (Basilicata). L’Anthropologie, 101(4): 617-638.<br />Ciolli  N. 1997. Elephas antiquus Falconer & Cautley del Cimitero di Atella (PZ). Studi per l’Ecologia del Quaternario, 19: 25-33.<br />Di Muro,  A. 1999. Inquadramento tefrostratigrafico del sito acheuleano del Cimitero di Atella (Basilicata, Italia). Studi per l’Ecologia del Quaternario, 21: 7-14. <br />Zucchelli,  M. 2002. I cervidi dell’Acheuleano antico nel Cimitero di Atella (Potenza). Studi per l’Ecologia del Quaternario,  24: 13-17.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="280f75c08fa1b883ed9f690bd87cdd88" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":48407943,"asset_id":28090791,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/48407943/download_file?st=MTczMjgzMjI0OCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="28090791"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="28090791"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 28090791; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=28090791]").text(description); $(".js-view-count[data-work-id=28090791]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 28090791; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='28090791']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 28090791, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "280f75c08fa1b883ed9f690bd87cdd88" } } $('.js-work-strip[data-work-id=28090791]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":28090791,"title":"Nuovo progetto di ricerca pluridisciplinare sul sito del Paleolitico inferiore del Cimitero di Atella (Potenza, Basilicata)/New multidisciplinary research project on the Lower Palaeolithic site of Cimitero di Atella (Potenza - Basilicata).","translated_title":"","metadata":{"abstract":"Il sito del Cimitero di Atella, localizzato ai margini dell’attuale abitato, è ubicato circa 10 km a sud del Monte Vulture (Basilicata, Italia meridionale). Lo scavo, condotto per più di vent’anni dal Prof. E. Borzatti von Löwenstern, ha riportato alla luce un’importante sequenza stratigrafica contenente due principali livelli archeologici attributi all’Acheuleano antico (Borzatti et al. 1990, 1997). Il materiale litico e faunistico, allo stato attuale delle ricerche, è datato a circa 0.63 Ma, sulla base di correlazioni stratigrafiche, vulcanologiche e biocronologiche (Borzatti et al. 1990; Ciolli 1997; Di Muro 1999; Zucchelli 2002). Un nuovo progetto multidisciplinare, avviato nel 2015, si propone di riattivare le ricerche su quest’importante sito, cercando di apportare un contributo alla problematica scientifica relativa al primo Acheuleano in Europa. L’obiettivo di questo programma è di rivalutare il contesto crono-stratigrafico, i processi di formazione del sito e le caratteristiche dell’associazione faunistica e dell’industria litica. La presenza di depositi lacustri, probabilmente in relazione con il bacino endoreico di Atella-Vitalba, e di diversi livelli vulcanici, attribuibili verosimilmente ad episodi eruttivi del centro vulcanico del Vulture, permetteranno sicuramente di collocare la sequenza nel suo preciso contesto crono-stratigrafico. Un nuovo riesame dell’industria litica (Abruzzese 2014, Abruzzese et al. 2016) ha individuato nell’insieme una grande variabilità di catene operative (grandi strumenti, piccoli strumenti, produzione di schegge). Questa diversità, al centro delle problematiche attuali sul Paleolitico inferiore, fa del Cimitero di Atella un sito rilevante che permetterà di fornire nuovi e inediti dati al dibattito scientifico sull’evoluzione dei sistemi tecnici durante il Pleistocene medio in Italia. \n\nThe site of Cimitero di Atella is located in the village of Atella (Basilicata, Southern Italy), at about 10 km of the Vulture Mt. The 20 years excavation of Prof. E. Borzatti von Löwenstern, brought to light an important sequence containing two archaeological levels attributed to the Lower Acheulean (Borzatti et al. 1990, 1997). The lithic implements and faunal remains are at the moment dated to 0.63 Ma on the base of stratigraphical, volcanological and biochronological correlations (Borzatti et al. 1990; Ciolli 1997; Di Muro 1999; Zucchelli 2002). A new multidisciplinary project, started in 2015, proposes to reactivate the research on this important site. The aim of this program is to re-assess the chrono-stratigraphical context, as well as the site formation and the features of fauna and lithic industry. The presence of lacustrine deposits at the bottom of the stratigraphic succession, related to the Atella paleo-lake, and of several volcanic layers in the uppermost part of the sequence, probably belonging to the Vulture Mt. eruptive events, will certainly allow us to re-collocate the sequence in a more precise chronological context. The new study of lithic industry (Abruzzese 2014, Abruzzese et al. 2016) shows that the assemblage contains in fact a great variability of reduction sequences (large cutting-tools, small tools, flakes production). This diversity, at the centre of the current research on Lower Palaeolithic, make of Cimitero di Atella an important site, which will add new and unpublished data to the debate on the evolution of technical systems in Italy during the Middle Pleistocene. \n\nReferences\nAbruzzese, C., 2014. Il sito paleolitico di Atella (Pz) nel quadro del primo popolamento europeo: studio tecnologico dell’industria litica. Tesi di Laurea. Uni-versità degli Studi Di Napoli « L’Orientale ». \nAbruzzese, C., Aureli, D., Rocca, R., 2016. Assessment of the Acheulean in Southern Italy: new study on the Cimitero di Atella site (Basilicata, Italy). Quaternary International 393, 158-168. \nBorzatti von Löwenstern, E., Sozzi, M., Vannucci, S., Vianello, F., 1990. L’acheuleano antico del cimitero di Atella. Prime indagini sulla stratigrafia del sedimento e sulle industrie litiche. Studi per l’ecologia del quaternario 12.\nBorzatti von Löwenstern, E., Palchetti, A., Sozzi, M. 1997. Témoignages de l’Acheuléen inferieur en Italie Méridionale: Le gisement du Cimitero di Atella (Basilicata). L’Anthropologie, 101(4): 617-638.\nCiolli \u2028N. 1997. Elephas antiquus Falconer \u0026 Cautley del Cimitero di Atella (PZ). Studi per l’Ecologia del Quaternario, 19: 25-33.\nDi Muro, \u2028A. 1999. Inquadramento tefrostratigrafico del sito acheuleano del Cimitero di Atella (Basilicata, Italia). Studi per l’Ecologia del Quaternario, 21: 7-14. \nZucchelli, \u2028M. 2002. I cervidi dell’Acheuleano antico nel Cimitero di Atella (Potenza). Studi per l’Ecologia del Quaternario, 24: 13-17.","location":"Genova, Italy","event_date":{"day":null,"month":2,"year":2016,"errors":{}},"organization":"Istituto Italiano di Preistoria e Protostoria"},"translated_abstract":"Il sito del Cimitero di Atella, localizzato ai margini dell’attuale abitato, è ubicato circa 10 km a sud del Monte Vulture (Basilicata, Italia meridionale). Lo scavo, condotto per più di vent’anni dal Prof. E. Borzatti von Löwenstern, ha riportato alla luce un’importante sequenza stratigrafica contenente due principali livelli archeologici attributi all’Acheuleano antico (Borzatti et al. 1990, 1997). Il materiale litico e faunistico, allo stato attuale delle ricerche, è datato a circa 0.63 Ma, sulla base di correlazioni stratigrafiche, vulcanologiche e biocronologiche (Borzatti et al. 1990; Ciolli 1997; Di Muro 1999; Zucchelli 2002). Un nuovo progetto multidisciplinare, avviato nel 2015, si propone di riattivare le ricerche su quest’importante sito, cercando di apportare un contributo alla problematica scientifica relativa al primo Acheuleano in Europa. L’obiettivo di questo programma è di rivalutare il contesto crono-stratigrafico, i processi di formazione del sito e le caratteristiche dell’associazione faunistica e dell’industria litica. La presenza di depositi lacustri, probabilmente in relazione con il bacino endoreico di Atella-Vitalba, e di diversi livelli vulcanici, attribuibili verosimilmente ad episodi eruttivi del centro vulcanico del Vulture, permetteranno sicuramente di collocare la sequenza nel suo preciso contesto crono-stratigrafico. Un nuovo riesame dell’industria litica (Abruzzese 2014, Abruzzese et al. 2016) ha individuato nell’insieme una grande variabilità di catene operative (grandi strumenti, piccoli strumenti, produzione di schegge). Questa diversità, al centro delle problematiche attuali sul Paleolitico inferiore, fa del Cimitero di Atella un sito rilevante che permetterà di fornire nuovi e inediti dati al dibattito scientifico sull’evoluzione dei sistemi tecnici durante il Pleistocene medio in Italia. \n\nThe site of Cimitero di Atella is located in the village of Atella (Basilicata, Southern Italy), at about 10 km of the Vulture Mt. The 20 years excavation of Prof. E. Borzatti von Löwenstern, brought to light an important sequence containing two archaeological levels attributed to the Lower Acheulean (Borzatti et al. 1990, 1997). The lithic implements and faunal remains are at the moment dated to 0.63 Ma on the base of stratigraphical, volcanological and biochronological correlations (Borzatti et al. 1990; Ciolli 1997; Di Muro 1999; Zucchelli 2002). A new multidisciplinary project, started in 2015, proposes to reactivate the research on this important site. The aim of this program is to re-assess the chrono-stratigraphical context, as well as the site formation and the features of fauna and lithic industry. The presence of lacustrine deposits at the bottom of the stratigraphic succession, related to the Atella paleo-lake, and of several volcanic layers in the uppermost part of the sequence, probably belonging to the Vulture Mt. eruptive events, will certainly allow us to re-collocate the sequence in a more precise chronological context. The new study of lithic industry (Abruzzese 2014, Abruzzese et al. 2016) shows that the assemblage contains in fact a great variability of reduction sequences (large cutting-tools, small tools, flakes production). This diversity, at the centre of the current research on Lower Palaeolithic, make of Cimitero di Atella an important site, which will add new and unpublished data to the debate on the evolution of technical systems in Italy during the Middle Pleistocene. \n\nReferences\nAbruzzese, C., 2014. Il sito paleolitico di Atella (Pz) nel quadro del primo popolamento europeo: studio tecnologico dell’industria litica. Tesi di Laurea. Uni-versità degli Studi Di Napoli « L’Orientale ». \nAbruzzese, C., Aureli, D., Rocca, R., 2016. Assessment of the Acheulean in Southern Italy: new study on the Cimitero di Atella site (Basilicata, Italy). Quaternary International 393, 158-168. \nBorzatti von Löwenstern, E., Sozzi, M., Vannucci, S., Vianello, F., 1990. L’acheuleano antico del cimitero di Atella. Prime indagini sulla stratigrafia del sedimento e sulle industrie litiche. Studi per l’ecologia del quaternario 12.\nBorzatti von Löwenstern, E., Palchetti, A., Sozzi, M. 1997. Témoignages de l’Acheuléen inferieur en Italie Méridionale: Le gisement du Cimitero di Atella (Basilicata). L’Anthropologie, 101(4): 617-638.\nCiolli \u2028N. 1997. Elephas antiquus Falconer \u0026 Cautley del Cimitero di Atella (PZ). Studi per l’Ecologia del Quaternario, 19: 25-33.\nDi Muro, \u2028A. 1999. Inquadramento tefrostratigrafico del sito acheuleano del Cimitero di Atella (Basilicata, Italia). Studi per l’Ecologia del Quaternario, 21: 7-14. \nZucchelli, \u2028M. 2002. I cervidi dell’Acheuleano antico nel Cimitero di Atella (Potenza). 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