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            <title xml:lang="en">Environments and Palacolithic occupations of Central Italy : the long middle Pleistocene sequence of Valle Giumentina</title>
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            <idno type="halRefHtml">Géographie. Université Panthéon-Sorbonne - Paris I; Università degli studi (Pise, Italie), 2017. Français. &lt;a target="_blank" href="https://www.theses.fr/2017PA01H107"&gt;&amp;#x27E8;NNT : 2017PA01H107&amp;#x27E9;&lt;/a&gt;</idno>
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                <title xml:lang="en">Environments and Palacolithic occupations of Central Italy : the long middle Pleistocene sequence of Valle Giumentina</title>
                <title xml:lang="fr">Environnements et occupations paléolithiques d'Italie centrale : la longue séquence pléistocène moyen de Valle Giumentina</title>
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                <authority type="school">École doctorale de Géographie de Paris. Espace, sociétés, aménagement (Paris ; 2000-....)</authority>
                <authority type="supervisor">Catherine Kuzucuoğlu</authority>
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                <authority type="jury">Jean-Jacques Bahain [Président]</authority>
                <authority type="jury">Damase Mouralis [Rapporteur]</authority>
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                <authority type="jury">Giorgio Manzi</authority>
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                <term xml:lang="en">Palaeoenvironment</term>
                <term xml:lang="en">Lower Palaeolithic</term>
                <term xml:lang="en">Central Italy</term>
                <term xml:lang="en">Tephra</term>
                <term xml:lang="en">Micromorphology</term>
                <term xml:lang="en">Sedimentology</term>
                <term xml:lang="en">Middle Pleistocene</term>
                <term xml:lang="fr">Paléoenvironnement</term>
                <term xml:lang="fr">Pléistocène moyen</term>
                <term xml:lang="fr">Sédimentologie</term>
                <term xml:lang="fr">Micomorphologie</term>
                <term xml:lang="fr">Téphra</term>
                <term xml:lang="fr">Italie centrale</term>
                <term xml:lang="fr">Paléolithique inférieur</term>
                <term xml:lang="it">Pleistocene medio</term>
                <term xml:lang="it">Sedimentologia</term>
                <term xml:lang="it">Micromorfologia</term>
                <term xml:lang="it">Tefra</term>
                <term xml:lang="it">Paleoambiente</term>
                <term xml:lang="it">Palaeolitico inferiore</term>
                <term xml:lang="it">Italia centrale</term>
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              <p>An integrated multidisciplinary study (sedimentology, geochemistry, micromorphology, biomarker analysis, geochronology and tephrochronology) was undertaken on the sedimentary infill of the Valle Giumentina basin (Abruzzo, Italy). In the 1950s an outstanding archaeological sequence, composed of nine human occupation levels ascribed to Acheulean eand Clactonian, was discovered inside this continental succession, 45m deep. Since then, the site is a reference for the definition of the Italian and European Lower Palaeolithic. This study depicts an evolution of the Valle Giumentina basin in four phases during the Middle Pleistocene, on a time span comprised between 600 and 400 ka, corresponding to MIS15-MIS12. The comparison with the contemporaneous palaeoenvironmental archives highlights that Valle Giumentina is a high-precision record and that its evolution is close to the East-Mediterranean sites. The new chronostratigraphic framework built by our results allows to precise the chronology of each archaeological level and to reconstruct the environmental context of the Palaeolithic human occupations.</p>
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              <p>Cette thèse présente l’étude pluridisciplinaire (sédimentologie, géochimie, micromorphologie, étude des biomarqueurs, géochronologie et téphrostratigraphie) réalisée sur le remplissage sédimentaire du bassin de Valle Giumentina (Abruzzes, Italie). La longue séquence continentale conservée dans le bassin, épaisse de 45 m, a livré dans les années 1950 neuf niveaux d’occupation préhistoriques attribués à l’Acheuléen et au Clactonien. Depuis, le site constitue une référence pour la définition du Paléolithique inférieur d’Italie et d’Europe. Les données issues de cette étude ont permis de produire une reconstitution détaillée de l’évolution du bassin de Valle Giumentina, qui s’articule en quatre phases principales au cours du Pléistocène moyen et qui documente deux cycles climatiques glaciaire-interglaciaire complets entre 600 et 400 ka, corrélés avec les stades isotopiques (MIS) 15 à 12. La comparaison de Valle Giumentina avec les principales archives paléoclimatiques contemporaines révèle qu’il s’agit d’un enregistrement extrêmement détaillé, dont l’évolution se rapproche de celles reconnues en Méditerranée orientale. Le nouveau cadre chronostratigraphique établi dans notre étude permet en outre de préciser la chronologie de chacun des niveaux archéologiques et de reconstruire les contextes environnementaux contemporains des occupations paléolithiques.</p>
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              <p>Questa tesi presenta lo studio pluridisciplinare (sedimentologia, geochimica, micromorfologia, studi dei bioindicatori, geocronologia e tefrostratigrafia) realizzato sul riempimento sedimentario del bacino di Valle Giumentina (Abruzzo, Italia). La lunga sequenza continentale conservata all'interno del bacino, profonda 45 metri, ha restituito negli anni 1950 nove livelli di occupazione preistorici, attributi all'Acheuleano e al Clactoniano. Da allora il sito rappresenta un riferi-mento per la definizione del Paleolitico inferiore d'Italia e d'Europa. I risultati del nostro studio hanno permesso di elabo-rare una ricostruzione dettagliata dell'evoluzione del bacino di Valle Giumentina, che si articola in quattro fasi principali durante il Pleistocene medio e che documenta due cicli interglaciale-glaciale completi, tra 600 e 400 ka, correlati con gli stadi isotopici (MIS) 15-12. Il confronto tra Valle Giumentina e i siti paleoclimatici contemporanei di riferimento, rivela che la sua successione stratigrafica rappresenta un archivio estremamente dettagliato, la cui evoluzione é simile a quella delle lunghe sequenze del Mediterraneo orientale. Il quadro cronostratigrafico definito nell'ambito del presente lavoro di tesi permette inoltre di precisare la cronologia di ciascuno dei livelli archeologici e di ricostruire il contesto ambientale delle occupazioni paleolitiche.</p>
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