LEADER 01048nam--2200361---4500 001 990000798060203316 005 20091103174619.0 035 $a0079806 035 $aUSA010079806 035 $a(ALEPH)000079806USA01 035 $a0079806 100 $a20011210d19611969km-y0ENGy0103----ba 101 $aeng 102 $aUS 200 1 $aSecurities regulation$fby Louis Loss 205 $a2 ed. 210 $aBoston$cLittle Brown$d1961-1969 215 $a6 v.$d24 cm 410 $12001 606 $aTitoli$yStati Uniti d'America$xRegolamentazione 676 $a346.73092 700 1$aLOSS,$bLouis$0227220 801 0$aIT$bsalbc$gISBD 912 $a990000798060203316 951 $aXXV.3.N. 202 1 (IG VIII 18 524 1)$b65268 EC$cXXV.3.N. 202 1 (IG VIII)$d00251481 959 $aBK 969 $aGIU 979 $aPATTY$b90$c20011210$lUSA01$h1052 979 $c20020403$lUSA01$h1726 979 $aPATRY$b90$c20040406$lUSA01$h1655 979 $aRSIAV4$b90$c20091103$lUSA01$h1746 996 $aSecurities Regulation$9582727 997 $aUNISA LEADER 05298 am 2200649 n 450 001 9910674059803321 005 20210709 010 $a2-7351-2623-4 024 7 $a10.4000/books.editionsmsh.45168 035 $a(CKB)5670000000617115 035 $a(FrMaCLE)OB-editionsmsh-45168 035 $a(PPN)268465649 035 $a(EXLCZ)995670000000617115 100 $a20230227j|||||||| ||| 0 101 0 $afre 135 $auu||||||m|||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aArchéologie d?un paysage $eLes étangs de Saint-Blaise (Bouches-du-Rhône) /$fFrédéric Trément 210 $aParis $cÉditions de la Maison des sciences de l?homme$d2021 210 31$aParis :$cMaison des sciences de l'homme,$d1999. 215 $a1 online resource (314 pages) $cillustrations, maps ;$ddigital file (PDF) 225 1 $aDocuments d'arche?ologie franc?aise,$x0769-010X ;$v74 311 $a2-7351-0797-3 (OCoLC)41755217 327 $aThis work presents the findings of research conducted from 1988 to 1993 near the étang de Berre.On the basis of systematic surveying, soundings and the excavation of a Gallo - Roman establishment, F Trément situates the major sites of Saint-Blaise and the Fossæ Marianæ in a globally and dynamically perceived space.Using earth and life sciences (geomorphology, sedimentology, palynology?). and with recourse to texts and iconography, the archaeologist broadens his focus, to encompass the landscape in its entirety. This microregion is characterised by numerous closed depressions, which explain the high population density during the Neolithic, the Iron Age and in Antiquity, and constitute sedimentary records of the evolution of the surroundings.The author seeks to understand how the successive waterside communities adapted to this shifting and harsh environment, how they appropriated the space and set about exploiting it, more or less consciously, leaving their mark, more or less enduring. 330 $aCet ouvrage présente les résultats de recherches conduites de 1988 h 1993 près de l?étang de Berre. Des prospections systématiques, des sondages et la fouille d?un établissement gallo-romain ont permis a F. Trément de replacer les sites majeurs de Saint-Blaise et des Fossæ Marianæ dans un espace appréhendé de façon globale et dynamique. Le recours aux sciences de la Terre et de la Vie (géomorphologie, sédimentologie, palynologie .), aux textes et a l?iconographie autorise l?archéologue à élargir le champ de ses préoccupations à l?ensemble du paysage. Les nombreuses dépressions fermées qui caractérisent cette microrégion et expliquent son peuplement très dense au Néolithique, à l?âge du Fer et dans l?Antiquité constituent de véritables enregistreurs sédimentaires de l?évolution du milieu. L?auteur s?attache à examiner comment les communautés riveraines successives se sont adaptées à ce milieu changeant et contraignant, se sont approprié l?espace, l?ont organisé pour l?exploiter, y ont laissé leur marque, plus ou moins consciente, plus ou moins durable This work presents the findings of research conducted from 1988 to 1993 near the étang de Berre. On the basis of systematic surveying, soundings and the excavation of a Gallo - Roman establishment,F Trément situates the major sites of Saint-Blaise and the Fossæ Marianæ in a globally and dynamically perceived space. Using earth and life sciences (geomorphology, sedimentology, palynology?). and with recourse to texts and iconography, the archaeologist broadens his focus, to encompass the landscape in its entirety. This microregion is characterised by numerous closed depressions, which explain the high population density during the Neolithic, the Iron Age and in Antiquity, and constitute sedimentary records of the evolution of the surroundings. 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