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            <title xml:lang="fr">Au fil de l’eau et de la lame. Mobilier protohistorique découvert en milieu aquatique en Midi-Pyrénées : analyses et interprétations</title>
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                <forename type="first">Lionel</forename>
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                <term xml:lang="fr">Dépôt volontaire</term>
                <term xml:lang="fr">Gué</term>
                <term xml:lang="fr">Garonne</term>
                <term xml:lang="fr">Toulouse -- Haute-Garonne -- France</term>
                <term xml:lang="fr">Toulousain</term>
                <term xml:lang="fr">Midi-pyrénées</term>
                <term xml:lang="fr">Mobilier métallique</term>
                <term xml:lang="fr">Milieu humide</term>
                <term xml:lang="fr">Cours d'eau</term>
                <term xml:lang="fr">Protohistoire méridionale</term>
                <term xml:lang="fr">Protohistoire</term>
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              <p>Recurring discoveries of protohistoric material (weapons, small metallic objects, coins, pottery, sculpture) in watercourses, especially in crossing places, or in areas of still water, is an intriguing phenomenon. The purpose of thisstudy is to produce an inventory for the Midi-Pyrénées, a vast region that runs between the Central Massif and thePyrenees, for which there is no overall study, and to ask about the modes and causes of the immersion of suchmaterial. A perspective on an inter-regional scale is proposed to cover the entire Garonne basin in the broadestsense. Many answers or hypotheses are needed to explain this complex phenomenon, characterised by a constantpresence from the middle of the 3rd millennium to the 1st century BC, and with varying evolutions over thecourse of antiquity.</p>
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              <p>La découverte récurrente de mobilier protohistorique (armes, petit mobilier métallique, monnaies, céramique, statuaire) dans les cours d’eau, notamment dans les zones de gué, ou dans les étendues d’eau stagnante est un phénomène qui intrigue. L’objet de cet article est d’en faire l’inventaire en Midi-Pyrénées, vaste région sise entre Massif central et Pyrénées, pour laquelle aucune étude d’ensemble n’existe et de s’interroger sur les modalités et causes de leur immersion. Une mise en perspective à l’échelle interrégionale s’impose afin d’embrasser l’ensemble du bassin versant garonnais lato sensu. Plusieurs réponses ou hypothèses peuvent être envisagées pour rendre compte de ce phénomène complexe caractérisé par de multiples récurrences, du milieu du 3e millénaire au 1er s. av. J.-C., et qui connaît des développements ultérieurs.</p>
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