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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="25149251"><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/25149251/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie"><img alt="Research paper thumbnail of Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie" class="work-thumbnail" src="https://attachments.academia-assets.com/46340927/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/25149251/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie">Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie</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://beniculturali.academia.edu/IlariaMatarese">Ilaria Matarese</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PaoloPallante">Paolo Pallante</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a></span></div><div class="wp-workCard_item"><span>Archaeologia Austriaca</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The present work is the result of a geo-archaeological collaboration for the study and classifica...</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">The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. An authoptic examination allowed to identify the rock types and in some cases their probable supply area. The study of stone materials is supported by a chrono-typological examination of the objects, and a graphic and photographic documentation has also been created. The comparisons research was carried out throughout the Mediterranean area and made it possible to distinguish between groups of local beads and pendants (of local production and distribution) and groups of aegean objects. This work has made possible a chronological classification of these objects, some of which arrived in Sicily through oversease trade routes. This study has allowed to solve some issues related to the Aegean imports in Italy and the socio-economic role played by ornamental in the indigenous communities of the Bronze Age.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="184f7e40079c89de78100e97ba1df6ba" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":46340927,"asset_id":25149251,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/46340927/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="25149251"><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="25149251"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 25149251; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=25149251]").text(description); $(".js-view-count[data-work-id=25149251]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 25149251; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='25149251']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 25149251, 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: "184f7e40079c89de78100e97ba1df6ba" } } $('.js-work-strip[data-work-id=25149251]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":25149251,"title":"Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie","translated_title":"","metadata":{"abstract":"The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. 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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="25086253"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/25086253/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie"><img alt="Research paper thumbnail of Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie" 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" rel="nofollow" href="https://www.academia.edu/25086253/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie">Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie</a></div><div class="wp-workCard_item"><span>Archaeologia Austriaca</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The present work is the result of a geo-archaeological collaboration for the study and classifica...</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">The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. An authoptic examination allowed to identify the rock types and in some cases their probable supply area. The study of stone materials is supported by a chrono-typological examination of the objects, and a graphic and photographic documentation has also been created. The comparisons research was carried out throughout the Mediterranean area and made it possible to distinguish between groups of local beads and pendants (of local production and distribution) and groups of aegean objects. This work has made possible a chronological classification of these objects, some of which arrived in Sicily through oversease trade routes. This study has allowed to solve some issues related to the Aegean imports in Italy and the socio-economic role played by ornamental in the indigenous communities of the Bronze Age.</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="25086253"><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="25086253"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 25086253; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=25086253]").text(description); $(".js-view-count[data-work-id=25086253]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 25086253; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='25086253']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 25086253, 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" } } $('.js-work-strip[data-work-id=25086253]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":25086253,"title":"Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie","translated_title":"","metadata":{"abstract":"The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. An authoptic examination allowed to identify the rock types and in some cases their probable supply area. The study of stone materials is supported by a chrono-typological examination of the objects, and a graphic and photographic documentation has also been created. The comparisons research was carried out throughout the Mediterranean area and made it possible to distinguish between groups of local beads and pendants (of local production and distribution) and groups of aegean objects. This work has made possible a chronological classification of these objects, some of which arrived in Sicily through oversease trade routes. This study has allowed to solve some issues related to the Aegean imports in Italy and the socio-economic role played by ornamental in the indigenous communities of the Bronze Age.","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Archaeologia Austriaca"},"translated_abstract":"The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. An authoptic examination allowed to identify the rock types and in some cases their probable supply area. The study of stone materials is supported by a chrono-typological examination of the objects, and a graphic and photographic documentation has also been created. The comparisons research was carried out throughout the Mediterranean area and made it possible to distinguish between groups of local beads and pendants (of local production and distribution) and groups of aegean objects. This work has made possible a chronological classification of these objects, some of which arrived in Sicily through oversease trade routes. This study has allowed to solve some issues related to the Aegean imports in Italy and the socio-economic role played by ornamental in the indigenous communities of the Bronze Age.","internal_url":"https://www.academia.edu/25086253/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie","translated_internal_url":"","created_at":"2016-05-06T07:05:28.083-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3313373,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Vaghi_e_pendenti_litici_dell_età_del_bronzo_dalla_Sicilia_e_dalle_Eolie","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3313373,"first_name":"Marco","middle_initials":null,"last_name":"Pacciarelli","page_name":"MarcoPacciarelli","domain_name":"unina","created_at":"2013-02-11T06:24:48.519-08:00","display_name":"Marco Pacciarelli","url":"https://unina.academia.edu/MarcoPacciarelli"},"attachments":[],"research_interests":[{"id":399,"name":"Prehistoric Archaeology","url":"https://www.academia.edu/Documents/in/Prehistoric_Archaeology"},{"id":34817,"name":"Prehistory","url":"https://www.academia.edu/Documents/in/Prehistory"},{"id":58724,"name":"Bronze Age","url":"https://www.academia.edu/Documents/in/Bronze_Age"},{"id":80854,"name":"Sicily","url":"https://www.academia.edu/Documents/in/Sicily"},{"id":650888,"name":"Preistoria Sicilia","url":"https://www.academia.edu/Documents/in/Preistoria_Sicilia"}],"urls":[]}, dispatcherData: dispatcherData }); $(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="24993606"><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/24993606/Ilaria_Matarese_Anita_Crispino_Reinhard_Jung_Maria_Clara_Martinelli_Paolo_Pallante_Marco_Pacciarelli_Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie_Archaeologia_Austriaca_99_2015_111_153"><img alt="Research paper thumbnail of Ilaria Matarese, Anita Crispino, Reinhard Jung, Maria Clara Martinelli, Paolo Pallante, Marco Pacciarelli, Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie. Archaeologia Austriaca 99, 2015, 111-153." 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/24993606/Ilaria_Matarese_Anita_Crispino_Reinhard_Jung_Maria_Clara_Martinelli_Paolo_Pallante_Marco_Pacciarelli_Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie_Archaeologia_Austriaca_99_2015_111_153">Ilaria Matarese, Anita Crispino, Reinhard Jung, Maria Clara Martinelli, Paolo Pallante, Marco Pacciarelli, Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie. Archaeologia Austriaca 99, 2015, 111-153.</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://sicilia.academia.edu/AnitaCrispino">Anita Crispino</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://oeaw.academia.edu/ReinhardJung">Reinhard Jung</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://beniculturali.academia.edu/IlariaMatarese">Ilaria Matarese</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PaoloPallante">Paolo Pallante</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="51b45b9d14ae97765e50e37ace25c282" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":45320156,"asset_id":24993606,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/45320156/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="24993606"><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="24993606"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 24993606; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=24993606]").text(description); $(".js-view-count[data-work-id=24993606]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 24993606; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='24993606']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 24993606, 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: "51b45b9d14ae97765e50e37ace25c282" } } $('.js-work-strip[data-work-id=24993606]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":24993606,"title":"Ilaria Matarese, Anita Crispino, Reinhard Jung, Maria Clara Martinelli, Paolo Pallante, Marco Pacciarelli, Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie. Archaeologia Austriaca 99, 2015, 111-153.","translated_title":"","metadata":{"grobid_abstract":"Il presente contributo è finalizzato allo studio dei vaghi e dei pendenti in materiali litici provenienti da siti dell'età del bronzo della Sicilia e delle Isole Eolie. Attraverso una determinazione geologica autoptica è stato possibile identificare i litotipi e in alcuni casi la probabile area di provenienza. Lo studio dei materiali litici è supportato da un'analisi crono-tipologica dei reperti e da una documentazione grafica e fotografica. Nell'ambito della ricerca di confronti è stata esaminata tutta l'area del Mediterraneo ed è stato possibile individuare gruppi di ornamenti di produzione locale e reperti di produzione orientale (soprattutto in corniola) pervenuti attraverso i traffici egei. Il presente lavoro ha reso possibile realizzare un inquadramento cronologico dei reperti in esame, alcuni dei quali hanno raggiunto la Sicilia attraverso le rotte transmarine del Mediterraneo. Attraverso questo contributo è stato possibile approfondire alcuni temi relativi alle importazioni egee in Italia e al mutevole ruolo socio-economico svolto dagli oggetti d'ornamento nelle comunità indigene dell'età del bronzo.","grobid_abstract_attachment_id":45320156},"translated_abstract":null,"internal_url":"https://www.academia.edu/24993606/Ilaria_Matarese_Anita_Crispino_Reinhard_Jung_Maria_Clara_Martinelli_Paolo_Pallante_Marco_Pacciarelli_Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie_Archaeologia_Austriaca_99_2015_111_153","translated_internal_url":"","created_at":"2016-05-03T11:30:34.403-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":638877,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":19811420,"work_id":24993606,"tagging_user_id":638877,"tagged_user_id":1281295,"co_author_invite_id":null,"email":"a***o@regione.sicilia.it","affiliation":"Regione Siciliana","display_order":-1,"name":"Anita Crispino","title":"Ilaria Matarese, Anita Crispino, Reinhard Jung, Maria Clara Martinelli, Paolo Pallante, Marco Pacciarelli, Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie. 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Jung/M. Pacciarelli/G. Forstenpointner/G. Slepecki/G. E. Weissengruber/A. Galik, Funde aus dem Müllhaufen der Geschichte im Befestigungsgraben von Punta di Zambrone. In: M. Bartelheim/B. Horejs/R. Krauss (eds), Von Baden bis Troia (Festschr. E. Pernicka). OREA 3 (Rahden 2016) 175–206." 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/23570168/R_Jung_M_Pacciarelli_G_Forstenpointner_G_Slepecki_G_E_Weissengruber_A_Galik_Funde_aus_dem_M%C3%BCllhaufen_der_Geschichte_im_Befestigungsgraben_von_Punta_di_Zambrone_In_M_Bartelheim_B_Horejs_R_Krauss_eds_Von_Baden_bis_Troia_Festschr_E_Pernicka_OREA_3_Rahden_2016_175_206">R. Jung/M. Pacciarelli/G. Forstenpointner/G. Slepecki/G. E. Weissengruber/A. Galik, Funde aus dem Müllhaufen der Geschichte im Befestigungsgraben von Punta di Zambrone. In: M. Bartelheim/B. Horejs/R. Krauss (eds), Von Baden bis Troia (Festschr. E. Pernicka). OREA 3 (Rahden 2016) 175–206.</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://oeaw.academia.edu/ReinhardJung">Reinhard Jung</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ef442f2a100c44b331ee1c0874d8c8bb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":43994576,"asset_id":23570168,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/43994576/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="23570168"><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="23570168"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 23570168; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=23570168]").text(description); $(".js-view-count[data-work-id=23570168]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 23570168; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='23570168']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 23570168, 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: "ef442f2a100c44b331ee1c0874d8c8bb" } } $('.js-work-strip[data-work-id=23570168]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":23570168,"title":"R. 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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="12522215"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/12522215/Bronze_Age_vitreous_materials_from_Punta_di_Zambrone_Southern_Italy_"><img alt="Research paper thumbnail of Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)" 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" rel="nofollow" href="https://www.academia.edu/12522215/Bronze_Age_vitreous_materials_from_Punta_di_Zambrone_Southern_Italy_">Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)</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://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://unimore.academia.edu/soniaconte">Sonia Conte</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://beniculturali.academia.edu/IlariaMatarese">Ilaria Matarese</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This study presents the results of an archaeometrical investigation of Bronze Age vitreous materi...</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">This study presents the results of an archaeometrical investigation of Bronze Age vitreous materials from the archaeological<br />site of Punta di Zambrone (Calabria, southern Italy). The analyses of a set of samples (9 faience beads, 1 glassy bead) from<br />approximately 1200 BCE (Recent Bronze Age) were carried out with an environmental scanning electron microscope (ESEM) and<br />LA-ICPMS (for the glassy bead) following a non-destructive protocol. Only very small chips of faience were sampled for X-ray<br />powder diffraction (XRPD) and preparation of thin sections for ESEM analysis.<br />The glassy bead is an opaque light-blue silica-soda-lime type with an uncommon chemical composition, comparable to some<br />coeval Italian and Mycenaean glassy faience artefacts. These are called LMLK (low magnesium low potassium) glassy faience, but<br />the flux used for their production has not yet been identified. The trace-element analysis allows exclusion of a Mesopotamian or<br />Egyptian provenance for this sample, suggesting it was produced with rather impure raw materials.<br />The nine faience beads have suffered from extensive weathering. The microstructural examinations carried out with the ESEM<br />enabled definition of three different groups: (1) light beads consisting almost entirely of quartz crystals without any original<br />interparticle glass, which could be due to the heavy weathering; (2) dark beads with a high content of manganese and iron oxide<br />and scarce presence of interparticle glass in the body, suggesting the original presence of Mn/Fe-rich interparticle glass; this presence<br />indicates that a glazing mixture containing alkalis and colorants was mixed with quartz, therefore the efflorescence method could<br />have been used for glazing, in combination with either cementation or application glazing (hybrid glazing methods); and (3) one green<br />sample exhibiting an heterogeneous body rich in Mg, K, Ti, and Fe but not containing Mn. The XRPD analysis of a faience bead of<br />group 1 confirmed the exclusive presence of quartz, whereas for group 2, an additional small peak compatible with Mn oxide<br />(poosibly hausmannite) was observed. Considering the colorant used for the dark beads, the Zambrone faience beads can be compared<br />to Mesopotamian and Minoan faience beads. They belong to a type widespread in north-central Italy between the Middle and Late<br />Bronze Age, and in southern Italy between the Early and Late Bronze Age. The same type of faience is found in the Aegean from the<br />middle of the 3rd millennium BCE to the 12th century BCE.</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="12522215"><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="12522215"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 12522215; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=12522215]").text(description); $(".js-view-count[data-work-id=12522215]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 12522215; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='12522215']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 12522215, 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" } } $('.js-work-strip[data-work-id=12522215]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":12522215,"title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)","translated_title":"","metadata":{"abstract":"This study presents the results of an archaeometrical investigation of Bronze Age vitreous materials from the archaeological\nsite of Punta di Zambrone (Calabria, southern Italy). The analyses of a set of samples (9 faience beads, 1 glassy bead) from\napproximately 1200 BCE (Recent Bronze Age) were carried out with an environmental scanning electron microscope (ESEM) and\nLA-ICPMS (for the glassy bead) following a non-destructive protocol. Only very small chips of faience were sampled for X-ray\npowder diffraction (XRPD) and preparation of thin sections for ESEM analysis.\nThe glassy bead is an opaque light-blue silica-soda-lime type with an uncommon chemical composition, comparable to some\ncoeval Italian and Mycenaean glassy faience artefacts. These are called LMLK (low magnesium low potassium) glassy faience, but\nthe flux used for their production has not yet been identified. The trace-element analysis allows exclusion of a Mesopotamian or\nEgyptian provenance for this sample, suggesting it was produced with rather impure raw materials.\nThe nine faience beads have suffered from extensive weathering. The microstructural examinations carried out with the ESEM\nenabled definition of three different groups: (1) light beads consisting almost entirely of quartz crystals without any original\ninterparticle glass, which could be due to the heavy weathering; (2) dark beads with a high content of manganese and iron oxide\nand scarce presence of interparticle glass in the body, suggesting the original presence of Mn/Fe-rich interparticle glass; this presence\nindicates that a glazing mixture containing alkalis and colorants was mixed with quartz, therefore the efflorescence method could\nhave been used for glazing, in combination with either cementation or application glazing (hybrid glazing methods); and (3) one green\nsample exhibiting an heterogeneous body rich in Mg, K, Ti, and Fe but not containing Mn. The XRPD analysis of a faience bead of\ngroup 1 confirmed the exclusive presence of quartz, whereas for group 2, an additional small peak compatible with Mn oxide\n(poosibly hausmannite) was observed. Considering the colorant used for the dark beads, the Zambrone faience beads can be compared\nto Mesopotamian and Minoan faience beads. They belong to a type widespread in north-central Italy between the Middle and Late\nBronze Age, and in southern Italy between the Early and Late Bronze Age. The same type of faience is found in the Aegean from the\nmiddle of the 3rd millennium BCE to the 12th century BCE."},"translated_abstract":"This study presents the results of an archaeometrical investigation of Bronze Age vitreous materials from the archaeological\nsite of Punta di Zambrone (Calabria, southern Italy). The analyses of a set of samples (9 faience beads, 1 glassy bead) from\napproximately 1200 BCE (Recent Bronze Age) were carried out with an environmental scanning electron microscope (ESEM) and\nLA-ICPMS (for the glassy bead) following a non-destructive protocol. Only very small chips of faience were sampled for X-ray\npowder diffraction (XRPD) and preparation of thin sections for ESEM analysis.\nThe glassy bead is an opaque light-blue silica-soda-lime type with an uncommon chemical composition, comparable to some\ncoeval Italian and Mycenaean glassy faience artefacts. These are called LMLK (low magnesium low potassium) glassy faience, but\nthe flux used for their production has not yet been identified. The trace-element analysis allows exclusion of a Mesopotamian or\nEgyptian provenance for this sample, suggesting it was produced with rather impure raw materials.\nThe nine faience beads have suffered from extensive weathering. The microstructural examinations carried out with the ESEM\nenabled definition of three different groups: (1) light beads consisting almost entirely of quartz crystals without any original\ninterparticle glass, which could be due to the heavy weathering; (2) dark beads with a high content of manganese and iron oxide\nand scarce presence of interparticle glass in the body, suggesting the original presence of Mn/Fe-rich interparticle glass; this presence\nindicates that a glazing mixture containing alkalis and colorants was mixed with quartz, therefore the efflorescence method could\nhave been used for glazing, in combination with either cementation or application glazing (hybrid glazing methods); and (3) one green\nsample exhibiting an heterogeneous body rich in Mg, K, Ti, and Fe but not containing Mn. The XRPD analysis of a faience bead of\ngroup 1 confirmed the exclusive presence of quartz, whereas for group 2, an additional small peak compatible with Mn oxide\n(poosibly hausmannite) was observed. Considering the colorant used for the dark beads, the Zambrone faience beads can be compared\nto Mesopotamian and Minoan faience beads. They belong to a type widespread in north-central Italy between the Middle and Late\nBronze Age, and in southern Italy between the Early and Late Bronze Age. The same type of faience is found in the Aegean from the\nmiddle of the 3rd millennium BCE to the 12th century BCE.","internal_url":"https://www.academia.edu/12522215/Bronze_Age_vitreous_materials_from_Punta_di_Zambrone_Southern_Italy_","translated_internal_url":"","created_at":"2015-05-22T02:04:43.475-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":1087283,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":603904,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":638877,"co_author_invite_id":null,"email":"r***g@oeaw.ac.at","affiliation":"Austrian Academy of Sciences","display_order":-1533916891,"name":"Reinhard Jung","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603905,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":3313373,"co_author_invite_id":null,"email":"m***i@libero.it","affiliation":"Università degli Studi di Napoli \"Federico II\"","display_order":-920350134,"name":"Marco Pacciarelli","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603903,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":null,"co_author_invite_id":230830,"email":"r***i@unito.it","display_order":-306783377,"name":"Rossella Arletti","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603902,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":null,"co_author_invite_id":230829,"email":"s***i@unime.it","display_order":306783380,"name":"Simona Quartieri","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603901,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":1266569,"co_author_invite_id":null,"email":"i***6@gmail.com","affiliation":"Ministero della cultura","display_order":920350137,"name":"Ilaria Matarese","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603906,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":2820173,"co_author_invite_id":null,"email":"g***e@cnrs-orleans.fr","affiliation":"Centre National de la Recherche Scientifique / French National Centre for Scientific Research","display_order":1533916894,"name":"Bernard GRATUZE","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"}],"downloadable_attachments":[],"slug":"Bronze_Age_vitreous_materials_from_Punta_di_Zambrone_Southern_Italy_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":1087283,"first_name":"Sonia","middle_initials":"","last_name":"Conte","page_name":"soniaconte","domain_name":"unimore","created_at":"2012-01-02T01:54:41.213-08:00","display_name":"Sonia Conte","url":"https://unimore.academia.edu/soniaconte"},"attachments":[],"research_interests":[{"id":12523,"name":"Bronze Age Europe (Archaeology)","url":"https://www.academia.edu/Documents/in/Bronze_Age_Europe_Archaeology_"},{"id":12807,"name":"Archaeometry","url":"https://www.academia.edu/Documents/in/Archaeometry"},{"id":50115,"name":"Faience","url":"https://www.academia.edu/Documents/in/Faience"},{"id":571350,"name":"LA-ICPMS","url":"https://www.academia.edu/Documents/in/LA-ICPMS"}],"urls":[]}, dispatcherData: dispatcherData }); $(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="15207566"><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/15207566/Late_Holocene_persistence_of_Abies_alba_in_low_mid_altitude_deciduous_forests_of_central_and_southern_Italy_new_perspectives_from_charcoal_data"><img alt="Research paper thumbnail of Late Holocene persistence of Abies alba in low-mid altitude deciduous forests of central and southern Italy: new perspectives from charcoal data" class="work-thumbnail" src="https://attachments.academia-assets.com/38580009/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/15207566/Late_Holocene_persistence_of_Abies_alba_in_low_mid_altitude_deciduous_forests_of_central_and_southern_Italy_new_perspectives_from_charcoal_data">Late Holocene persistence of Abies alba in low-mid altitude deciduous forests of central and southern Italy: new perspectives from charcoal data</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://unina.academia.edu/AntonioSaracino">Antonio Saracino</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/EmiliaAllevato">Emilia Allevato</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Questions: Pollen data for Abies alba Mill., a key European tree species, show broad occurrence i...</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">Questions: Pollen data for Abies alba Mill., a key European tree species, show broad occurrence in the Italian peninsula in the early to mid-Holocene diffusion (until ca. 6000 yr ago) along the Italian peninsula and a strong decline/local extinction starting ca. 5000 yr ago. This decline has been attributed to climate <br />change. Recently, high-resolution pollen studies,mainly in northern Italian sites claim that A. alba disappearance was mainly due to human impact. We examined the presence of A. alba in archaeological sites of southern and central Italy in order to trace the late Holocene history (last 3000 yr) of this tree and enhance understanding of its role in pre-anthropic vegetation and of human involvement in its decline. <br />Location: Central and southern Italy. <br />Methods: Anthracological analysis was conducted in six archaeological layers at the archaeological site of Trebbio-Spinellina (800–600 BC, Sansepolcro, Tuscany). A critical analysis of wood/charcoal literature relevant to Abies in central <br />and southern Italy was used to corroborate the results of Trebbio-Spinellina. Charcoal records fromarchaeological sites have been compared with the current distribution of A. alba. <br />Results: At Trebbio-Spinellina, A. alba charcoal is present in all contexts examined, together with mesophilous broad-leaf taxa (Quercus deciduous, Carpinus betulus, Ostrya carpinifolia, Corylus avellana). A low charcoal percentage of Fagus sylvatica and Taxus baccata is also found; evergreen taxa are mainly represented by Quercus ilex with occasional shrubs (i.e. Viburnum, Cistus, Erica). In the literature, we identified several peninsular and insular Italian archaeological sites showing charcoal evidence of Abies, accompanied by deciduous oaks, mainly Q. cerris, and other broad-leafmesophilous trees, dating from the Iron Age to the Middle Ages. All sites, except one, lie at less than 600 m a.s.l., and far from present- day A. alba communities. <br />Conclusion: Results call for a reworking of the prevailing paradigmof A. alba as a relic mountain species. Indeed, A. alba once grew at lower altitudes than currently and was associated with deciduous oaks, mainly Q. cerris, and other mesophilous broad-leaf trees. This evidence calls into question the suitability of the Potential Natural Vegetation (PNV) concept usually applied in the floristic approach. The recent population decline is attributable to human activity rather than to climate change. Finally, the persistence of A. alba until the late Holocene calls into question the assumptions that it is a relic species with no potential to expand its spatial range.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b7d34f5e5432f63fc3ad41fed0f2b959" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":38580009,"asset_id":15207566,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/38580009/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="15207566"><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="15207566"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 15207566; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=15207566]").text(description); $(".js-view-count[data-work-id=15207566]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 15207566; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='15207566']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 15207566, 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: "b7d34f5e5432f63fc3ad41fed0f2b959" } } $('.js-work-strip[data-work-id=15207566]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":15207566,"title":"Late Holocene persistence of Abies alba in low-mid altitude deciduous forests of central and southern Italy: new perspectives from charcoal data","translated_title":"","metadata":{"abstract":"Questions: Pollen data for Abies alba Mill., a key European tree species, show broad occurrence in the Italian peninsula in the early to mid-Holocene diffusion (until ca. 6000 yr ago) along the Italian peninsula and a strong decline/local extinction starting ca. 5000 yr ago. This decline has been attributed to climate\r\nchange. Recently, high-resolution pollen studies,mainly in northern Italian sites claim that A. alba disappearance was mainly due to human impact. We examined the presence of A. alba in archaeological sites of southern and central Italy in order to trace the late Holocene history (last 3000 yr) of this tree and enhance understanding of its role in pre-anthropic vegetation and of human involvement in its decline.\r\nLocation: Central and southern Italy.\r\nMethods: Anthracological analysis was conducted in six archaeological layers at the archaeological site of Trebbio-Spinellina (800–600 BC, Sansepolcro, Tuscany). A critical analysis of wood/charcoal literature relevant to Abies in central\r\nand southern Italy was used to corroborate the results of Trebbio-Spinellina. Charcoal records fromarchaeological sites have been compared with the current distribution of A. alba.\r\nResults: At Trebbio-Spinellina, A. alba charcoal is present in all contexts examined, together with mesophilous broad-leaf taxa (Quercus deciduous, Carpinus betulus, Ostrya carpinifolia, Corylus avellana). A low charcoal percentage of Fagus sylvatica and Taxus baccata is also found; evergreen taxa are mainly represented by Quercus ilex with occasional shrubs (i.e. Viburnum, Cistus, Erica). In the literature, we identified several peninsular and insular Italian archaeological sites showing charcoal evidence of Abies, accompanied by deciduous oaks, mainly Q. cerris, and other broad-leafmesophilous trees, dating from the Iron Age to the Middle Ages. All sites, except one, lie at less than 600 m a.s.l., and far from present- day A. alba communities.\r\nConclusion: Results call for a reworking of the prevailing paradigmof A. alba as a relic mountain species. Indeed, A. alba once grew at lower altitudes than currently and was associated with deciduous oaks, mainly Q. cerris, and other mesophilous broad-leaf trees. This evidence calls into question the suitability of the Potential Natural Vegetation (PNV) concept usually applied in the floristic approach. The recent population decline is attributable to human activity rather than to climate change. Finally, the persistence of A. alba until the late Holocene calls into question the assumptions that it is a relic species with no potential to expand its spatial range.","journal_name":"Journal of Vegetation Science"},"translated_abstract":"Questions: Pollen data for Abies alba Mill., a key European tree species, show broad occurrence in the Italian peninsula in the early to mid-Holocene diffusion (until ca. 6000 yr ago) along the Italian peninsula and a strong decline/local extinction starting ca. 5000 yr ago. This decline has been attributed to climate\r\nchange. Recently, high-resolution pollen studies,mainly in northern Italian sites claim that A. alba disappearance was mainly due to human impact. We examined the presence of A. alba in archaeological sites of southern and central Italy in order to trace the late Holocene history (last 3000 yr) of this tree and enhance understanding of its role in pre-anthropic vegetation and of human involvement in its decline.\r\nLocation: Central and southern Italy.\r\nMethods: Anthracological analysis was conducted in six archaeological layers at the archaeological site of Trebbio-Spinellina (800–600 BC, Sansepolcro, Tuscany). A critical analysis of wood/charcoal literature relevant to Abies in central\r\nand southern Italy was used to corroborate the results of Trebbio-Spinellina. Charcoal records fromarchaeological sites have been compared with the current distribution of A. alba.\r\nResults: At Trebbio-Spinellina, A. alba charcoal is present in all contexts examined, together with mesophilous broad-leaf taxa (Quercus deciduous, Carpinus betulus, Ostrya carpinifolia, Corylus avellana). A low charcoal percentage of Fagus sylvatica and Taxus baccata is also found; evergreen taxa are mainly represented by Quercus ilex with occasional shrubs (i.e. Viburnum, Cistus, Erica). In the literature, we identified several peninsular and insular Italian archaeological sites showing charcoal evidence of Abies, accompanied by deciduous oaks, mainly Q. cerris, and other broad-leafmesophilous trees, dating from the Iron Age to the Middle Ages. All sites, except one, lie at less than 600 m a.s.l., and far from present- day A. alba communities.\r\nConclusion: Results call for a reworking of the prevailing paradigmof A. alba as a relic mountain species. Indeed, A. alba once grew at lower altitudes than currently and was associated with deciduous oaks, mainly Q. cerris, and other mesophilous broad-leaf trees. This evidence calls into question the suitability of the Potential Natural Vegetation (PNV) concept usually applied in the floristic approach. The recent population decline is attributable to human activity rather than to climate change. Finally, the persistence of A. alba until the late Holocene calls into question the assumptions that it is a relic species with no potential to expand its spatial range.","internal_url":"https://www.academia.edu/15207566/Late_Holocene_persistence_of_Abies_alba_in_low_mid_altitude_deciduous_forests_of_central_and_southern_Italy_new_perspectives_from_charcoal_data","translated_internal_url":"","created_at":"2015-08-26T11:16:06.897-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":31700768,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":5117631,"work_id":15207566,"tagging_user_id":31700768,"tagged_user_id":32523137,"co_author_invite_id":null,"email":"g***e@unina.it","affiliation":"Università degli Studi di Napoli \"Federico II\"","display_order":1,"name":"Gaetano Di Pasquale","title":"Late Holocene persistence of Abies alba in low-mid altitude deciduous forests of central and southern Italy: new perspectives from 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dispatcherData: dispatcherData }); $(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="8410280"><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/8410280/M_Pacciarelli_P_F_Talamo_Sull_articolazione_dell_et%C3%A0_del_Rame_nell_Italia_meridionale_tirrenica"><img alt="Research paper thumbnail of M. Pacciarelli, P.F. Talamo, Sull’articolazione dell’età del Rame nell’Italia meridionale tirrenica" class="work-thumbnail" src="https://attachments.academia-assets.com/34804170/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/8410280/M_Pacciarelli_P_F_Talamo_Sull_articolazione_dell_et%C3%A0_del_Rame_nell_Italia_meridionale_tirrenica">M. Pacciarelli, P.F. Talamo, Sull’articolazione dell’età del Rame nell’Italia meridionale tirrenica</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://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/TalamoPierfrancesco">Pierfrancesco Talamo</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In L'età del rame in Italia, Atti della XLIII riunione scientifica IIPP (Bologna 2008), Firenze 2...</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">In L'età del rame in Italia, Atti della XLIII riunione scientifica IIPP (Bologna 2008), Firenze 2011, pp. 87-94.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="0edda9a38af38eb3692d77558a5e9d7d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":34804170,"asset_id":8410280,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/34804170/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="8410280"><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="8410280"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8410280; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=8410280]").text(description); $(".js-view-count[data-work-id=8410280]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 8410280; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='8410280']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 8410280, 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: "0edda9a38af38eb3692d77558a5e9d7d" } } $('.js-work-strip[data-work-id=8410280]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":8410280,"title":"M. Pacciarelli, P.F. Talamo, Sull’articolazione dell’età del Rame nell’Italia meridionale tirrenica","translated_title":"","metadata":{"abstract":"In L'età del rame in Italia, Atti della XLIII riunione scientifica IIPP (Bologna 2008), Firenze 2011, pp. 87-94."},"translated_abstract":"In L'età del rame in Italia, Atti della XLIII riunione scientifica IIPP (Bologna 2008), Firenze 2011, pp. 87-94.","internal_url":"https://www.academia.edu/8410280/M_Pacciarelli_P_F_Talamo_Sull_articolazione_dell_et%C3%A0_del_Rame_nell_Italia_meridionale_tirrenica","translated_internal_url":"","created_at":"2014-09-20T06:43:23.332-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3313373,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":1470236,"work_id":8410280,"tagging_user_id":3313373,"tagged_user_id":32553386,"co_author_invite_id":463224,"email":"p***o@beniculturali.it","display_order":0,"name":"Pierfrancesco Talamo","title":"M. 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Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale, Rivista di Scienze Preistoriche LXII, 2012, pp. 331-362." class="work-thumbnail" src="https://attachments.academia-assets.com/34804055/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/8410168/C_Capriglione_A_De_Bonis_G_De_Tommaso_V_Guarino_M_Iuliano_D_Marino_V_Morra_M_Pacciarelli_Grandi_dolii_protostorici_d_impasto_dalla_Calabria_centromeridionale_Contributo_allo_studio_cronotipologico_tecnologico_e_funzionale_Rivista_di_Scienze_Preistoriche_LXII_2012_pp_331_362">C. Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale, Rivista di Scienze Preistoriche LXII, 2012, pp. 331-362.</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://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/CapriglioneCristina">Cristina Capriglione</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="536577c32807a699fa04af5aae6480a0" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":34804055,"asset_id":8410168,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/34804055/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="8410168"><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="8410168"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8410168; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=8410168]").text(description); $(".js-view-count[data-work-id=8410168]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 8410168; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='8410168']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 8410168, 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: "536577c32807a699fa04af5aae6480a0" } } $('.js-work-strip[data-work-id=8410168]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":8410168,"title":"C. Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale, Rivista di Scienze Preistoriche LXII, 2012, pp. 331-362.","translated_title":"","metadata":{"grobid_abstract":"Dolii di dimensioni molto grandi d'età protostorica, prodotti con forme e tecnologie paragonabili a quelle egee -denominati \"dolii a cordoni o fasce\" -furono individuati per la prima volta nel corso delle campagne di scavo effet-tuate dall'Università di Roma \"La Sapienza\" sul pianoro di Broglio di Trebisacce (CS) a partire dal Grandi dolii protostorici d'impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale SUmmaRy -large protohIstorIC Impasto dolIa from Central-southern CalabrIa. ContrIbutIon to the study of typology, Chronology, teChnology and funCtIon -a high number of fragments of large protohistoric impasto pithoi has been found in several sites in the area, and mainly in Serre di altilia (central Calabria). These fragments have been studied with other pithoi from Tropea (southern Calabria), in order to reconstruct their forms, typology, chronology, technology and function. It has been possible to define five types, with chronologies that may vary from the Final Bronze to the Early Iron age, and with parallels in several sites of Southern Italy, in Sicily and at Lipari. Petrografic analyses on fragments from Central Calabria have shown a quite variable production, locally and/or regionally made. Chemical analyses have been also performed on two residue samples, in order to identify what kind of foodstuff was originally stored in these pithoi. The results of the analyses show the presence of terpenoid resins, such as Pistacia or Pinus, which may suggest the presence of wine.","grobid_abstract_attachment_id":34804055},"translated_abstract":null,"internal_url":"https://www.academia.edu/8410168/C_Capriglione_A_De_Bonis_G_De_Tommaso_V_Guarino_M_Iuliano_D_Marino_V_Morra_M_Pacciarelli_Grandi_dolii_protostorici_d_impasto_dalla_Calabria_centromeridionale_Contributo_allo_studio_cronotipologico_tecnologico_e_funzionale_Rivista_di_Scienze_Preistoriche_LXII_2012_pp_331_362","translated_internal_url":"","created_at":"2014-09-20T06:25:08.850-07:00","section":"Papers","preview_url":null,"current_user_can_edit":{"authorship":{"id":13762973,"created_at":"2015-06-25T13:49:50.621-07:00","section_id":837803,"updated_at":"2015-06-25T13:49:50.621-07:00","user_id":1653289,"work_id":8410168,"display_order":-4194303,"is_owner":false}},"current_user_is_owner":false,"owner_id":3313373,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":1470237,"work_id":8410168,"tagging_user_id":3313373,"tagged_user_id":2772267,"co_author_invite_id":null,"email":"v***a@unina.it","affiliation":"Università degli Studi di Napoli \"Federico II\"","display_order":0,"name":"Enzo Morra","title":"C. Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale, Rivista di Scienze Preistoriche LXII, 2012, pp. 331-362."},{"id":1470239,"work_id":8410168,"tagging_user_id":3313373,"tagged_user_id":null,"co_author_invite_id":295576,"email":"s***i@archeomarche.it","display_order":4194304,"name":"Mara Silvestrini","title":"C. Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. 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Damiani, M. Pacciarelli, L'insediamento di Acquafredda e l'occupazione rurale del territorio tra Roma, Caere e Veio dal primo Ferro all’età arcaica" class="work-thumbnail" src="https://attachments.academia-assets.com/34804003/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/8410047/I_Damiani_M_Pacciarelli_Linsediamento_di_Acquafredda_e_loccupazione_rurale_del_territorio_tra_Roma_Caere_e_Veio_dal_primo_Ferro_all_et%C3%A0_arcaica">I. Damiani, M. Pacciarelli, L'insediamento di Acquafredda e l'occupazione rurale del territorio tra Roma, Caere e Veio dal primo Ferro all’età arcaica</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In La fattoria e la villa dell’Auditorium, a cura di A. Carandini con M.T. D’Alessio e H. Di Gius...</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">In La fattoria e la villa dell’Auditorium, a cura di A. Carandini con M.T. D’Alessio e H. Di Giuseppe, Bollettino della Commissione Archeologica Comunale, Supplementi XIV, Roma, L’Erma di Bretschneider, 2006, pp. 511-556.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9a0c6874c32be76391eaaabca2c531cb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":34804003,"asset_id":8410047,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/34804003/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="8410047"><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="8410047"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8410047; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=8410047]").text(description); $(".js-view-count[data-work-id=8410047]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 8410047; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='8410047']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 8410047, 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: "9a0c6874c32be76391eaaabca2c531cb" } } $('.js-work-strip[data-work-id=8410047]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":8410047,"title":"I. 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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="25149251"><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/25149251/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie"><img alt="Research paper thumbnail of Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie" class="work-thumbnail" src="https://attachments.academia-assets.com/46340927/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/25149251/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie">Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie</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://beniculturali.academia.edu/IlariaMatarese">Ilaria Matarese</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PaoloPallante">Paolo Pallante</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a></span></div><div class="wp-workCard_item"><span>Archaeologia Austriaca</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The present work is the result of a geo-archaeological collaboration for the study and classifica...</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">The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. An authoptic examination allowed to identify the rock types and in some cases their probable supply area. The study of stone materials is supported by a chrono-typological examination of the objects, and a graphic and photographic documentation has also been created. The comparisons research was carried out throughout the Mediterranean area and made it possible to distinguish between groups of local beads and pendants (of local production and distribution) and groups of aegean objects. This work has made possible a chronological classification of these objects, some of which arrived in Sicily through oversease trade routes. This study has allowed to solve some issues related to the Aegean imports in Italy and the socio-economic role played by ornamental in the indigenous communities of the Bronze Age.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="184f7e40079c89de78100e97ba1df6ba" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":46340927,"asset_id":25149251,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/46340927/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="25149251"><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="25149251"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 25149251; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=25149251]").text(description); $(".js-view-count[data-work-id=25149251]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 25149251; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='25149251']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 25149251, 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: "184f7e40079c89de78100e97ba1df6ba" } } $('.js-work-strip[data-work-id=25149251]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":25149251,"title":"Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie","translated_title":"","metadata":{"abstract":"The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. 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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="25086253"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/25086253/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie"><img alt="Research paper thumbnail of Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie" 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" rel="nofollow" href="https://www.academia.edu/25086253/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie">Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie</a></div><div class="wp-workCard_item"><span>Archaeologia Austriaca</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The present work is the result of a geo-archaeological collaboration for the study and classifica...</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">The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. An authoptic examination allowed to identify the rock types and in some cases their probable supply area. The study of stone materials is supported by a chrono-typological examination of the objects, and a graphic and photographic documentation has also been created. The comparisons research was carried out throughout the Mediterranean area and made it possible to distinguish between groups of local beads and pendants (of local production and distribution) and groups of aegean objects. This work has made possible a chronological classification of these objects, some of which arrived in Sicily through oversease trade routes. This study has allowed to solve some issues related to the Aegean imports in Italy and the socio-economic role played by ornamental in the indigenous communities of the Bronze Age.</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="25086253"><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="25086253"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 25086253; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=25086253]").text(description); $(".js-view-count[data-work-id=25086253]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 25086253; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='25086253']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 25086253, 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" } } $('.js-work-strip[data-work-id=25086253]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":25086253,"title":"Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie","translated_title":"","metadata":{"abstract":"The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. An authoptic examination allowed to identify the rock types and in some cases their probable supply area. The study of stone materials is supported by a chrono-typological examination of the objects, and a graphic and photographic documentation has also been created. The comparisons research was carried out throughout the Mediterranean area and made it possible to distinguish between groups of local beads and pendants (of local production and distribution) and groups of aegean objects. This work has made possible a chronological classification of these objects, some of which arrived in Sicily through oversease trade routes. This study has allowed to solve some issues related to the Aegean imports in Italy and the socio-economic role played by ornamental in the indigenous communities of the Bronze Age.","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Archaeologia Austriaca"},"translated_abstract":"The present work is the result of a geo-archaeological collaboration for the study and classification of beads and pendants in lithic materials from Bronze Age sites of Sicily and Aeolian Islands. An authoptic examination allowed to identify the rock types and in some cases their probable supply area. The study of stone materials is supported by a chrono-typological examination of the objects, and a graphic and photographic documentation has also been created. The comparisons research was carried out throughout the Mediterranean area and made it possible to distinguish between groups of local beads and pendants (of local production and distribution) and groups of aegean objects. This work has made possible a chronological classification of these objects, some of which arrived in Sicily through oversease trade routes. This study has allowed to solve some issues related to the Aegean imports in Italy and the socio-economic role played by ornamental in the indigenous communities of the Bronze Age.","internal_url":"https://www.academia.edu/25086253/Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie","translated_internal_url":"","created_at":"2016-05-06T07:05:28.083-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3313373,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Vaghi_e_pendenti_litici_dell_età_del_bronzo_dalla_Sicilia_e_dalle_Eolie","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3313373,"first_name":"Marco","middle_initials":null,"last_name":"Pacciarelli","page_name":"MarcoPacciarelli","domain_name":"unina","created_at":"2013-02-11T06:24:48.519-08:00","display_name":"Marco Pacciarelli","url":"https://unina.academia.edu/MarcoPacciarelli"},"attachments":[],"research_interests":[{"id":399,"name":"Prehistoric Archaeology","url":"https://www.academia.edu/Documents/in/Prehistoric_Archaeology"},{"id":34817,"name":"Prehistory","url":"https://www.academia.edu/Documents/in/Prehistory"},{"id":58724,"name":"Bronze Age","url":"https://www.academia.edu/Documents/in/Bronze_Age"},{"id":80854,"name":"Sicily","url":"https://www.academia.edu/Documents/in/Sicily"},{"id":650888,"name":"Preistoria Sicilia","url":"https://www.academia.edu/Documents/in/Preistoria_Sicilia"}],"urls":[]}, dispatcherData: dispatcherData }); $(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="24993606"><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/24993606/Ilaria_Matarese_Anita_Crispino_Reinhard_Jung_Maria_Clara_Martinelli_Paolo_Pallante_Marco_Pacciarelli_Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie_Archaeologia_Austriaca_99_2015_111_153"><img alt="Research paper thumbnail of Ilaria Matarese, Anita Crispino, Reinhard Jung, Maria Clara Martinelli, Paolo Pallante, Marco Pacciarelli, Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie. Archaeologia Austriaca 99, 2015, 111-153." 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/24993606/Ilaria_Matarese_Anita_Crispino_Reinhard_Jung_Maria_Clara_Martinelli_Paolo_Pallante_Marco_Pacciarelli_Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie_Archaeologia_Austriaca_99_2015_111_153">Ilaria Matarese, Anita Crispino, Reinhard Jung, Maria Clara Martinelli, Paolo Pallante, Marco Pacciarelli, Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie. Archaeologia Austriaca 99, 2015, 111-153.</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://sicilia.academia.edu/AnitaCrispino">Anita Crispino</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://oeaw.academia.edu/ReinhardJung">Reinhard Jung</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://beniculturali.academia.edu/IlariaMatarese">Ilaria Matarese</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PaoloPallante">Paolo Pallante</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="51b45b9d14ae97765e50e37ace25c282" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":45320156,"asset_id":24993606,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/45320156/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="24993606"><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="24993606"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 24993606; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=24993606]").text(description); $(".js-view-count[data-work-id=24993606]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 24993606; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='24993606']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 24993606, 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: "51b45b9d14ae97765e50e37ace25c282" } } $('.js-work-strip[data-work-id=24993606]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":24993606,"title":"Ilaria Matarese, Anita Crispino, Reinhard Jung, Maria Clara Martinelli, Paolo Pallante, Marco Pacciarelli, Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie. Archaeologia Austriaca 99, 2015, 111-153.","translated_title":"","metadata":{"grobid_abstract":"Il presente contributo è finalizzato allo studio dei vaghi e dei pendenti in materiali litici provenienti da siti dell'età del bronzo della Sicilia e delle Isole Eolie. Attraverso una determinazione geologica autoptica è stato possibile identificare i litotipi e in alcuni casi la probabile area di provenienza. Lo studio dei materiali litici è supportato da un'analisi crono-tipologica dei reperti e da una documentazione grafica e fotografica. Nell'ambito della ricerca di confronti è stata esaminata tutta l'area del Mediterraneo ed è stato possibile individuare gruppi di ornamenti di produzione locale e reperti di produzione orientale (soprattutto in corniola) pervenuti attraverso i traffici egei. Il presente lavoro ha reso possibile realizzare un inquadramento cronologico dei reperti in esame, alcuni dei quali hanno raggiunto la Sicilia attraverso le rotte transmarine del Mediterraneo. Attraverso questo contributo è stato possibile approfondire alcuni temi relativi alle importazioni egee in Italia e al mutevole ruolo socio-economico svolto dagli oggetti d'ornamento nelle comunità indigene dell'età del bronzo.","grobid_abstract_attachment_id":45320156},"translated_abstract":null,"internal_url":"https://www.academia.edu/24993606/Ilaria_Matarese_Anita_Crispino_Reinhard_Jung_Maria_Clara_Martinelli_Paolo_Pallante_Marco_Pacciarelli_Vaghi_e_pendenti_litici_dell_et%C3%A0_del_bronzo_dalla_Sicilia_e_dalle_Eolie_Archaeologia_Austriaca_99_2015_111_153","translated_internal_url":"","created_at":"2016-05-03T11:30:34.403-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":638877,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":19811420,"work_id":24993606,"tagging_user_id":638877,"tagged_user_id":1281295,"co_author_invite_id":null,"email":"a***o@regione.sicilia.it","affiliation":"Regione Siciliana","display_order":-1,"name":"Anita Crispino","title":"Ilaria Matarese, Anita Crispino, Reinhard Jung, Maria Clara Martinelli, Paolo Pallante, Marco Pacciarelli, Vaghi e pendenti litici dell’età del bronzo dalla Sicilia e dalle Eolie. 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Jung/M. Pacciarelli/G. Forstenpointner/G. Slepecki/G. E. Weissengruber/A. Galik, Funde aus dem Müllhaufen der Geschichte im Befestigungsgraben von Punta di Zambrone. In: M. Bartelheim/B. Horejs/R. Krauss (eds), Von Baden bis Troia (Festschr. E. Pernicka). OREA 3 (Rahden 2016) 175–206." 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/23570168/R_Jung_M_Pacciarelli_G_Forstenpointner_G_Slepecki_G_E_Weissengruber_A_Galik_Funde_aus_dem_M%C3%BCllhaufen_der_Geschichte_im_Befestigungsgraben_von_Punta_di_Zambrone_In_M_Bartelheim_B_Horejs_R_Krauss_eds_Von_Baden_bis_Troia_Festschr_E_Pernicka_OREA_3_Rahden_2016_175_206">R. Jung/M. Pacciarelli/G. Forstenpointner/G. Slepecki/G. E. Weissengruber/A. Galik, Funde aus dem Müllhaufen der Geschichte im Befestigungsgraben von Punta di Zambrone. In: M. Bartelheim/B. Horejs/R. Krauss (eds), Von Baden bis Troia (Festschr. E. Pernicka). OREA 3 (Rahden 2016) 175–206.</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://oeaw.academia.edu/ReinhardJung">Reinhard Jung</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ef442f2a100c44b331ee1c0874d8c8bb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":43994576,"asset_id":23570168,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/43994576/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="23570168"><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="23570168"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 23570168; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=23570168]").text(description); $(".js-view-count[data-work-id=23570168]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 23570168; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='23570168']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 23570168, 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: "ef442f2a100c44b331ee1c0874d8c8bb" } } $('.js-work-strip[data-work-id=23570168]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":23570168,"title":"R. 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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="12522215"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/12522215/Bronze_Age_vitreous_materials_from_Punta_di_Zambrone_Southern_Italy_"><img alt="Research paper thumbnail of Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)" 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" rel="nofollow" href="https://www.academia.edu/12522215/Bronze_Age_vitreous_materials_from_Punta_di_Zambrone_Southern_Italy_">Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)</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://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://unimore.academia.edu/soniaconte">Sonia Conte</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://beniculturali.academia.edu/IlariaMatarese">Ilaria Matarese</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This study presents the results of an archaeometrical investigation of Bronze Age vitreous materi...</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">This study presents the results of an archaeometrical investigation of Bronze Age vitreous materials from the archaeological<br />site of Punta di Zambrone (Calabria, southern Italy). The analyses of a set of samples (9 faience beads, 1 glassy bead) from<br />approximately 1200 BCE (Recent Bronze Age) were carried out with an environmental scanning electron microscope (ESEM) and<br />LA-ICPMS (for the glassy bead) following a non-destructive protocol. Only very small chips of faience were sampled for X-ray<br />powder diffraction (XRPD) and preparation of thin sections for ESEM analysis.<br />The glassy bead is an opaque light-blue silica-soda-lime type with an uncommon chemical composition, comparable to some<br />coeval Italian and Mycenaean glassy faience artefacts. These are called LMLK (low magnesium low potassium) glassy faience, but<br />the flux used for their production has not yet been identified. The trace-element analysis allows exclusion of a Mesopotamian or<br />Egyptian provenance for this sample, suggesting it was produced with rather impure raw materials.<br />The nine faience beads have suffered from extensive weathering. The microstructural examinations carried out with the ESEM<br />enabled definition of three different groups: (1) light beads consisting almost entirely of quartz crystals without any original<br />interparticle glass, which could be due to the heavy weathering; (2) dark beads with a high content of manganese and iron oxide<br />and scarce presence of interparticle glass in the body, suggesting the original presence of Mn/Fe-rich interparticle glass; this presence<br />indicates that a glazing mixture containing alkalis and colorants was mixed with quartz, therefore the efflorescence method could<br />have been used for glazing, in combination with either cementation or application glazing (hybrid glazing methods); and (3) one green<br />sample exhibiting an heterogeneous body rich in Mg, K, Ti, and Fe but not containing Mn. The XRPD analysis of a faience bead of<br />group 1 confirmed the exclusive presence of quartz, whereas for group 2, an additional small peak compatible with Mn oxide<br />(poosibly hausmannite) was observed. Considering the colorant used for the dark beads, the Zambrone faience beads can be compared<br />to Mesopotamian and Minoan faience beads. They belong to a type widespread in north-central Italy between the Middle and Late<br />Bronze Age, and in southern Italy between the Early and Late Bronze Age. The same type of faience is found in the Aegean from the<br />middle of the 3rd millennium BCE to the 12th century BCE.</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="12522215"><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="12522215"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 12522215; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=12522215]").text(description); $(".js-view-count[data-work-id=12522215]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 12522215; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='12522215']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 12522215, 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" } } $('.js-work-strip[data-work-id=12522215]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":12522215,"title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)","translated_title":"","metadata":{"abstract":"This study presents the results of an archaeometrical investigation of Bronze Age vitreous materials from the archaeological\nsite of Punta di Zambrone (Calabria, southern Italy). The analyses of a set of samples (9 faience beads, 1 glassy bead) from\napproximately 1200 BCE (Recent Bronze Age) were carried out with an environmental scanning electron microscope (ESEM) and\nLA-ICPMS (for the glassy bead) following a non-destructive protocol. Only very small chips of faience were sampled for X-ray\npowder diffraction (XRPD) and preparation of thin sections for ESEM analysis.\nThe glassy bead is an opaque light-blue silica-soda-lime type with an uncommon chemical composition, comparable to some\ncoeval Italian and Mycenaean glassy faience artefacts. These are called LMLK (low magnesium low potassium) glassy faience, but\nthe flux used for their production has not yet been identified. The trace-element analysis allows exclusion of a Mesopotamian or\nEgyptian provenance for this sample, suggesting it was produced with rather impure raw materials.\nThe nine faience beads have suffered from extensive weathering. The microstructural examinations carried out with the ESEM\nenabled definition of three different groups: (1) light beads consisting almost entirely of quartz crystals without any original\ninterparticle glass, which could be due to the heavy weathering; (2) dark beads with a high content of manganese and iron oxide\nand scarce presence of interparticle glass in the body, suggesting the original presence of Mn/Fe-rich interparticle glass; this presence\nindicates that a glazing mixture containing alkalis and colorants was mixed with quartz, therefore the efflorescence method could\nhave been used for glazing, in combination with either cementation or application glazing (hybrid glazing methods); and (3) one green\nsample exhibiting an heterogeneous body rich in Mg, K, Ti, and Fe but not containing Mn. The XRPD analysis of a faience bead of\ngroup 1 confirmed the exclusive presence of quartz, whereas for group 2, an additional small peak compatible with Mn oxide\n(poosibly hausmannite) was observed. Considering the colorant used for the dark beads, the Zambrone faience beads can be compared\nto Mesopotamian and Minoan faience beads. They belong to a type widespread in north-central Italy between the Middle and Late\nBronze Age, and in southern Italy between the Early and Late Bronze Age. The same type of faience is found in the Aegean from the\nmiddle of the 3rd millennium BCE to the 12th century BCE."},"translated_abstract":"This study presents the results of an archaeometrical investigation of Bronze Age vitreous materials from the archaeological\nsite of Punta di Zambrone (Calabria, southern Italy). The analyses of a set of samples (9 faience beads, 1 glassy bead) from\napproximately 1200 BCE (Recent Bronze Age) were carried out with an environmental scanning electron microscope (ESEM) and\nLA-ICPMS (for the glassy bead) following a non-destructive protocol. Only very small chips of faience were sampled for X-ray\npowder diffraction (XRPD) and preparation of thin sections for ESEM analysis.\nThe glassy bead is an opaque light-blue silica-soda-lime type with an uncommon chemical composition, comparable to some\ncoeval Italian and Mycenaean glassy faience artefacts. These are called LMLK (low magnesium low potassium) glassy faience, but\nthe flux used for their production has not yet been identified. The trace-element analysis allows exclusion of a Mesopotamian or\nEgyptian provenance for this sample, suggesting it was produced with rather impure raw materials.\nThe nine faience beads have suffered from extensive weathering. The microstructural examinations carried out with the ESEM\nenabled definition of three different groups: (1) light beads consisting almost entirely of quartz crystals without any original\ninterparticle glass, which could be due to the heavy weathering; (2) dark beads with a high content of manganese and iron oxide\nand scarce presence of interparticle glass in the body, suggesting the original presence of Mn/Fe-rich interparticle glass; this presence\nindicates that a glazing mixture containing alkalis and colorants was mixed with quartz, therefore the efflorescence method could\nhave been used for glazing, in combination with either cementation or application glazing (hybrid glazing methods); and (3) one green\nsample exhibiting an heterogeneous body rich in Mg, K, Ti, and Fe but not containing Mn. The XRPD analysis of a faience bead of\ngroup 1 confirmed the exclusive presence of quartz, whereas for group 2, an additional small peak compatible with Mn oxide\n(poosibly hausmannite) was observed. Considering the colorant used for the dark beads, the Zambrone faience beads can be compared\nto Mesopotamian and Minoan faience beads. They belong to a type widespread in north-central Italy between the Middle and Late\nBronze Age, and in southern Italy between the Early and Late Bronze Age. The same type of faience is found in the Aegean from the\nmiddle of the 3rd millennium BCE to the 12th century BCE.","internal_url":"https://www.academia.edu/12522215/Bronze_Age_vitreous_materials_from_Punta_di_Zambrone_Southern_Italy_","translated_internal_url":"","created_at":"2015-05-22T02:04:43.475-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":1087283,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":603904,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":638877,"co_author_invite_id":null,"email":"r***g@oeaw.ac.at","affiliation":"Austrian Academy of Sciences","display_order":-1533916891,"name":"Reinhard Jung","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603905,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":3313373,"co_author_invite_id":null,"email":"m***i@libero.it","affiliation":"Università degli Studi di Napoli \"Federico II\"","display_order":-920350134,"name":"Marco Pacciarelli","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603903,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":null,"co_author_invite_id":230830,"email":"r***i@unito.it","display_order":-306783377,"name":"Rossella Arletti","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603902,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":null,"co_author_invite_id":230829,"email":"s***i@unime.it","display_order":306783380,"name":"Simona Quartieri","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603901,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":1266569,"co_author_invite_id":null,"email":"i***6@gmail.com","affiliation":"Ministero della cultura","display_order":920350137,"name":"Ilaria Matarese","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"},{"id":603906,"work_id":12522215,"tagging_user_id":1087283,"tagged_user_id":2820173,"co_author_invite_id":null,"email":"g***e@cnrs-orleans.fr","affiliation":"Centre National de la Recherche Scientifique / French National Centre for Scientific Research","display_order":1533916894,"name":"Bernard GRATUZE","title":"Bronze Age vitreous materials from Punta di Zambrone (Southern Italy)"}],"downloadable_attachments":[],"slug":"Bronze_Age_vitreous_materials_from_Punta_di_Zambrone_Southern_Italy_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":1087283,"first_name":"Sonia","middle_initials":"","last_name":"Conte","page_name":"soniaconte","domain_name":"unimore","created_at":"2012-01-02T01:54:41.213-08:00","display_name":"Sonia Conte","url":"https://unimore.academia.edu/soniaconte"},"attachments":[],"research_interests":[{"id":12523,"name":"Bronze Age Europe (Archaeology)","url":"https://www.academia.edu/Documents/in/Bronze_Age_Europe_Archaeology_"},{"id":12807,"name":"Archaeometry","url":"https://www.academia.edu/Documents/in/Archaeometry"},{"id":50115,"name":"Faience","url":"https://www.academia.edu/Documents/in/Faience"},{"id":571350,"name":"LA-ICPMS","url":"https://www.academia.edu/Documents/in/LA-ICPMS"}],"urls":[]}, dispatcherData: dispatcherData }); $(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="15207566"><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/15207566/Late_Holocene_persistence_of_Abies_alba_in_low_mid_altitude_deciduous_forests_of_central_and_southern_Italy_new_perspectives_from_charcoal_data"><img alt="Research paper thumbnail of Late Holocene persistence of Abies alba in low-mid altitude deciduous forests of central and southern Italy: new perspectives from charcoal data" class="work-thumbnail" src="https://attachments.academia-assets.com/38580009/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/15207566/Late_Holocene_persistence_of_Abies_alba_in_low_mid_altitude_deciduous_forests_of_central_and_southern_Italy_new_perspectives_from_charcoal_data">Late Holocene persistence of Abies alba in low-mid altitude deciduous forests of central and southern Italy: new perspectives from charcoal data</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://unina.academia.edu/AntonioSaracino">Antonio Saracino</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/EmiliaAllevato">Emilia Allevato</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Questions: Pollen data for Abies alba Mill., a key European tree species, show broad occurrence i...</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">Questions: Pollen data for Abies alba Mill., a key European tree species, show broad occurrence in the Italian peninsula in the early to mid-Holocene diffusion (until ca. 6000 yr ago) along the Italian peninsula and a strong decline/local extinction starting ca. 5000 yr ago. This decline has been attributed to climate <br />change. Recently, high-resolution pollen studies,mainly in northern Italian sites claim that A. alba disappearance was mainly due to human impact. We examined the presence of A. alba in archaeological sites of southern and central Italy in order to trace the late Holocene history (last 3000 yr) of this tree and enhance understanding of its role in pre-anthropic vegetation and of human involvement in its decline. <br />Location: Central and southern Italy. <br />Methods: Anthracological analysis was conducted in six archaeological layers at the archaeological site of Trebbio-Spinellina (800–600 BC, Sansepolcro, Tuscany). A critical analysis of wood/charcoal literature relevant to Abies in central <br />and southern Italy was used to corroborate the results of Trebbio-Spinellina. Charcoal records fromarchaeological sites have been compared with the current distribution of A. alba. <br />Results: At Trebbio-Spinellina, A. alba charcoal is present in all contexts examined, together with mesophilous broad-leaf taxa (Quercus deciduous, Carpinus betulus, Ostrya carpinifolia, Corylus avellana). A low charcoal percentage of Fagus sylvatica and Taxus baccata is also found; evergreen taxa are mainly represented by Quercus ilex with occasional shrubs (i.e. Viburnum, Cistus, Erica). In the literature, we identified several peninsular and insular Italian archaeological sites showing charcoal evidence of Abies, accompanied by deciduous oaks, mainly Q. cerris, and other broad-leafmesophilous trees, dating from the Iron Age to the Middle Ages. All sites, except one, lie at less than 600 m a.s.l., and far from present- day A. alba communities. <br />Conclusion: Results call for a reworking of the prevailing paradigmof A. alba as a relic mountain species. Indeed, A. alba once grew at lower altitudes than currently and was associated with deciduous oaks, mainly Q. cerris, and other mesophilous broad-leaf trees. This evidence calls into question the suitability of the Potential Natural Vegetation (PNV) concept usually applied in the floristic approach. The recent population decline is attributable to human activity rather than to climate change. Finally, the persistence of A. alba until the late Holocene calls into question the assumptions that it is a relic species with no potential to expand its spatial range.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b7d34f5e5432f63fc3ad41fed0f2b959" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":38580009,"asset_id":15207566,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/38580009/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="15207566"><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="15207566"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 15207566; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=15207566]").text(description); $(".js-view-count[data-work-id=15207566]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 15207566; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='15207566']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 15207566, 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: "b7d34f5e5432f63fc3ad41fed0f2b959" } } $('.js-work-strip[data-work-id=15207566]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":15207566,"title":"Late Holocene persistence of Abies alba in low-mid altitude deciduous forests of central and southern Italy: new perspectives from charcoal data","translated_title":"","metadata":{"abstract":"Questions: Pollen data for Abies alba Mill., a key European tree species, show broad occurrence in the Italian peninsula in the early to mid-Holocene diffusion (until ca. 6000 yr ago) along the Italian peninsula and a strong decline/local extinction starting ca. 5000 yr ago. This decline has been attributed to climate\r\nchange. Recently, high-resolution pollen studies,mainly in northern Italian sites claim that A. alba disappearance was mainly due to human impact. We examined the presence of A. alba in archaeological sites of southern and central Italy in order to trace the late Holocene history (last 3000 yr) of this tree and enhance understanding of its role in pre-anthropic vegetation and of human involvement in its decline.\r\nLocation: Central and southern Italy.\r\nMethods: Anthracological analysis was conducted in six archaeological layers at the archaeological site of Trebbio-Spinellina (800–600 BC, Sansepolcro, Tuscany). A critical analysis of wood/charcoal literature relevant to Abies in central\r\nand southern Italy was used to corroborate the results of Trebbio-Spinellina. Charcoal records fromarchaeological sites have been compared with the current distribution of A. alba.\r\nResults: At Trebbio-Spinellina, A. alba charcoal is present in all contexts examined, together with mesophilous broad-leaf taxa (Quercus deciduous, Carpinus betulus, Ostrya carpinifolia, Corylus avellana). A low charcoal percentage of Fagus sylvatica and Taxus baccata is also found; evergreen taxa are mainly represented by Quercus ilex with occasional shrubs (i.e. Viburnum, Cistus, Erica). In the literature, we identified several peninsular and insular Italian archaeological sites showing charcoal evidence of Abies, accompanied by deciduous oaks, mainly Q. cerris, and other broad-leafmesophilous trees, dating from the Iron Age to the Middle Ages. All sites, except one, lie at less than 600 m a.s.l., and far from present- day A. alba communities.\r\nConclusion: Results call for a reworking of the prevailing paradigmof A. alba as a relic mountain species. Indeed, A. alba once grew at lower altitudes than currently and was associated with deciduous oaks, mainly Q. cerris, and other mesophilous broad-leaf trees. This evidence calls into question the suitability of the Potential Natural Vegetation (PNV) concept usually applied in the floristic approach. The recent population decline is attributable to human activity rather than to climate change. Finally, the persistence of A. alba until the late Holocene calls into question the assumptions that it is a relic species with no potential to expand its spatial range.","journal_name":"Journal of Vegetation Science"},"translated_abstract":"Questions: Pollen data for Abies alba Mill., a key European tree species, show broad occurrence in the Italian peninsula in the early to mid-Holocene diffusion (until ca. 6000 yr ago) along the Italian peninsula and a strong decline/local extinction starting ca. 5000 yr ago. This decline has been attributed to climate\r\nchange. Recently, high-resolution pollen studies,mainly in northern Italian sites claim that A. alba disappearance was mainly due to human impact. We examined the presence of A. alba in archaeological sites of southern and central Italy in order to trace the late Holocene history (last 3000 yr) of this tree and enhance understanding of its role in pre-anthropic vegetation and of human involvement in its decline.\r\nLocation: Central and southern Italy.\r\nMethods: Anthracological analysis was conducted in six archaeological layers at the archaeological site of Trebbio-Spinellina (800–600 BC, Sansepolcro, Tuscany). A critical analysis of wood/charcoal literature relevant to Abies in central\r\nand southern Italy was used to corroborate the results of Trebbio-Spinellina. Charcoal records fromarchaeological sites have been compared with the current distribution of A. alba.\r\nResults: At Trebbio-Spinellina, A. alba charcoal is present in all contexts examined, together with mesophilous broad-leaf taxa (Quercus deciduous, Carpinus betulus, Ostrya carpinifolia, Corylus avellana). A low charcoal percentage of Fagus sylvatica and Taxus baccata is also found; evergreen taxa are mainly represented by Quercus ilex with occasional shrubs (i.e. Viburnum, Cistus, Erica). In the literature, we identified several peninsular and insular Italian archaeological sites showing charcoal evidence of Abies, accompanied by deciduous oaks, mainly Q. cerris, and other broad-leafmesophilous trees, dating from the Iron Age to the Middle Ages. All sites, except one, lie at less than 600 m a.s.l., and far from present- day A. alba communities.\r\nConclusion: Results call for a reworking of the prevailing paradigmof A. alba as a relic mountain species. Indeed, A. alba once grew at lower altitudes than currently and was associated with deciduous oaks, mainly Q. cerris, and other mesophilous broad-leaf trees. This evidence calls into question the suitability of the Potential Natural Vegetation (PNV) concept usually applied in the floristic approach. The recent population decline is attributable to human activity rather than to climate change. Finally, the persistence of A. alba until the late Holocene calls into question the assumptions that it is a relic species with no potential to expand its spatial range.","internal_url":"https://www.academia.edu/15207566/Late_Holocene_persistence_of_Abies_alba_in_low_mid_altitude_deciduous_forests_of_central_and_southern_Italy_new_perspectives_from_charcoal_data","translated_internal_url":"","created_at":"2015-08-26T11:16:06.897-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":31700768,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":5117631,"work_id":15207566,"tagging_user_id":31700768,"tagged_user_id":32523137,"co_author_invite_id":null,"email":"g***e@unina.it","affiliation":"Università degli Studi di Napoli \"Federico II\"","display_order":1,"name":"Gaetano Di Pasquale","title":"Late Holocene persistence of Abies alba in low-mid altitude deciduous forests of central and southern Italy: new perspectives from 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dispatcherData: dispatcherData }); $(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="8410280"><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/8410280/M_Pacciarelli_P_F_Talamo_Sull_articolazione_dell_et%C3%A0_del_Rame_nell_Italia_meridionale_tirrenica"><img alt="Research paper thumbnail of M. Pacciarelli, P.F. Talamo, Sull’articolazione dell’età del Rame nell’Italia meridionale tirrenica" class="work-thumbnail" src="https://attachments.academia-assets.com/34804170/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/8410280/M_Pacciarelli_P_F_Talamo_Sull_articolazione_dell_et%C3%A0_del_Rame_nell_Italia_meridionale_tirrenica">M. Pacciarelli, P.F. Talamo, Sull’articolazione dell’età del Rame nell’Italia meridionale tirrenica</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://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/TalamoPierfrancesco">Pierfrancesco Talamo</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In L'età del rame in Italia, Atti della XLIII riunione scientifica IIPP (Bologna 2008), Firenze 2...</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">In L'età del rame in Italia, Atti della XLIII riunione scientifica IIPP (Bologna 2008), Firenze 2011, pp. 87-94.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="0edda9a38af38eb3692d77558a5e9d7d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":34804170,"asset_id":8410280,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/34804170/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="8410280"><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="8410280"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8410280; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=8410280]").text(description); $(".js-view-count[data-work-id=8410280]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 8410280; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='8410280']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 8410280, 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: "0edda9a38af38eb3692d77558a5e9d7d" } } $('.js-work-strip[data-work-id=8410280]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":8410280,"title":"M. 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Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale, Rivista di Scienze Preistoriche LXII, 2012, pp. 331-362." class="work-thumbnail" src="https://attachments.academia-assets.com/34804055/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/8410168/C_Capriglione_A_De_Bonis_G_De_Tommaso_V_Guarino_M_Iuliano_D_Marino_V_Morra_M_Pacciarelli_Grandi_dolii_protostorici_d_impasto_dalla_Calabria_centromeridionale_Contributo_allo_studio_cronotipologico_tecnologico_e_funzionale_Rivista_di_Scienze_Preistoriche_LXII_2012_pp_331_362">C. Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale, Rivista di Scienze Preistoriche LXII, 2012, pp. 331-362.</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://unina.academia.edu/MarcoPacciarelli">Marco Pacciarelli</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/CapriglioneCristina">Cristina Capriglione</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="536577c32807a699fa04af5aae6480a0" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":34804055,"asset_id":8410168,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/34804055/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="8410168"><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="8410168"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8410168; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=8410168]").text(description); $(".js-view-count[data-work-id=8410168]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 8410168; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='8410168']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 8410168, 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: "536577c32807a699fa04af5aae6480a0" } } $('.js-work-strip[data-work-id=8410168]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":8410168,"title":"C. Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale, Rivista di Scienze Preistoriche LXII, 2012, pp. 331-362.","translated_title":"","metadata":{"grobid_abstract":"Dolii di dimensioni molto grandi d'età protostorica, prodotti con forme e tecnologie paragonabili a quelle egee -denominati \"dolii a cordoni o fasce\" -furono individuati per la prima volta nel corso delle campagne di scavo effet-tuate dall'Università di Roma \"La Sapienza\" sul pianoro di Broglio di Trebisacce (CS) a partire dal Grandi dolii protostorici d'impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale SUmmaRy -large protohIstorIC Impasto dolIa from Central-southern CalabrIa. ContrIbutIon to the study of typology, Chronology, teChnology and funCtIon -a high number of fragments of large protohistoric impasto pithoi has been found in several sites in the area, and mainly in Serre di altilia (central Calabria). These fragments have been studied with other pithoi from Tropea (southern Calabria), in order to reconstruct their forms, typology, chronology, technology and function. It has been possible to define five types, with chronologies that may vary from the Final Bronze to the Early Iron age, and with parallels in several sites of Southern Italy, in Sicily and at Lipari. Petrografic analyses on fragments from Central Calabria have shown a quite variable production, locally and/or regionally made. Chemical analyses have been also performed on two residue samples, in order to identify what kind of foodstuff was originally stored in these pithoi. The results of the analyses show the presence of terpenoid resins, such as Pistacia or Pinus, which may suggest the presence of wine.","grobid_abstract_attachment_id":34804055},"translated_abstract":null,"internal_url":"https://www.academia.edu/8410168/C_Capriglione_A_De_Bonis_G_De_Tommaso_V_Guarino_M_Iuliano_D_Marino_V_Morra_M_Pacciarelli_Grandi_dolii_protostorici_d_impasto_dalla_Calabria_centromeridionale_Contributo_allo_studio_cronotipologico_tecnologico_e_funzionale_Rivista_di_Scienze_Preistoriche_LXII_2012_pp_331_362","translated_internal_url":"","created_at":"2014-09-20T06:25:08.850-07:00","section":"Papers","preview_url":null,"current_user_can_edit":{"authorship":{"id":13762973,"created_at":"2015-06-25T13:49:50.621-07:00","section_id":837803,"updated_at":"2015-06-25T13:49:50.621-07:00","user_id":1653289,"work_id":8410168,"display_order":-4194303,"is_owner":false}},"current_user_is_owner":false,"owner_id":3313373,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":1470237,"work_id":8410168,"tagging_user_id":3313373,"tagged_user_id":2772267,"co_author_invite_id":null,"email":"v***a@unina.it","affiliation":"Università degli Studi di Napoli \"Federico II\"","display_order":0,"name":"Enzo Morra","title":"C. Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. Contributo allo studio cronotipologico, tecnologico e funzionale, Rivista di Scienze Preistoriche LXII, 2012, pp. 331-362."},{"id":1470239,"work_id":8410168,"tagging_user_id":3313373,"tagged_user_id":null,"co_author_invite_id":295576,"email":"s***i@archeomarche.it","display_order":4194304,"name":"Mara Silvestrini","title":"C. Capriglione, A. De Bonis, G. De Tommaso, V. Guarino, M. Iuliano, D. Marino, V. Morra, M. Pacciarelli, Grandi dolii protostorici d’impasto dalla Calabria centromeridionale. 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Damiani, M. Pacciarelli, L'insediamento di Acquafredda e l'occupazione rurale del territorio tra Roma, Caere e Veio dal primo Ferro all’età arcaica" class="work-thumbnail" src="https://attachments.academia-assets.com/34804003/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/8410047/I_Damiani_M_Pacciarelli_Linsediamento_di_Acquafredda_e_loccupazione_rurale_del_territorio_tra_Roma_Caere_e_Veio_dal_primo_Ferro_all_et%C3%A0_arcaica">I. Damiani, M. Pacciarelli, L'insediamento di Acquafredda e l'occupazione rurale del territorio tra Roma, Caere e Veio dal primo Ferro all’età arcaica</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In La fattoria e la villa dell’Auditorium, a cura di A. Carandini con M.T. D’Alessio e H. Di Gius...</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">In La fattoria e la villa dell’Auditorium, a cura di A. Carandini con M.T. D’Alessio e H. Di Giuseppe, Bollettino della Commissione Archeologica Comunale, Supplementi XIV, Roma, L’Erma di Bretschneider, 2006, pp. 511-556.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9a0c6874c32be76391eaaabca2c531cb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":34804003,"asset_id":8410047,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/34804003/download_file?st=MTczMjQ3OTkzNyw4LjIyMi4yMDguMTQ2&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="8410047"><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="8410047"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8410047; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=8410047]").text(description); $(".js-view-count[data-work-id=8410047]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 8410047; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='8410047']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 8410047, 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: "9a0c6874c32be76391eaaabca2c531cb" } } $('.js-work-strip[data-work-id=8410047]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":8410047,"title":"I. Damiani, M. Pacciarelli, L'insediamento di Acquafredda e l'occupazione rurale del territorio tra Roma, Caere e Veio dal primo Ferro all’età arcaica","translated_title":"","metadata":{"abstract":"In La fattoria e la villa dell’Auditorium, a cura di A. Carandini con M.T. D’Alessio e H. Di Giuseppe, Bollettino della Commissione Archeologica Comunale, Supplementi XIV, Roma, L’Erma di Bretschneider, 2006, pp. 511-556."},"translated_abstract":"In La fattoria e la villa dell’Auditorium, a cura di A. Carandini con M.T. D’Alessio e H. 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