Mediterranee最新文献

{"title":"Médiation géoarchéologique et paysagère","authors":"Camille Provendier, Benoît Devillers","doi":"10.4000/mediterranee.13730","DOIUrl":"https://doi.org/10.4000/mediterranee.13730","url":null,"abstract":"","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-10-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42155824","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Les agressions au patrimoine littoral de la province d’Alicante","authors":"Gabino Ponce Herrero, Juan Antonio Marco Molina, J. Mira","doi":"10.4000/mediterranee.13285","DOIUrl":"https://doi.org/10.4000/mediterranee.13285","url":null,"abstract":"","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-10-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43702536","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Foreword","authors":"Benoît Devillers, Pau Olmos Benlloch, Père Castanyer","doi":"10.4000/mediterranee.12859","DOIUrl":"https://doi.org/10.4000/mediterranee.12859","url":null,"abstract":"","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-10-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"49163172","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"L’île de Carabane","authors":"Mamadou Thior, A. Sy, Issa Mballo, El hadj Balla Dieye, Dramane Cissokho, D. Sow, L. Descroix","doi":"10.4000/mediterranee.13660","DOIUrl":"https://doi.org/10.4000/mediterranee.13660","url":null,"abstract":"","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-10-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45382862","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"L’érosion côtière et ses implications archéologiques","authors":"L. Ménanteau","doi":"10.4000/mediterranee.13430","DOIUrl":"https://doi.org/10.4000/mediterranee.13430","url":null,"abstract":"","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-10-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46655596","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Galileo’s revolution and the infancy of meteorology in Padua, Florence and Bologna","authors":"Dario Camuffo","doi":"10.4000/mediterranee.12565","DOIUrl":"https://doi.org/10.4000/mediterranee.12565","url":null,"abstract":"","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-06-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41472997","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Palaeogeography of Ancient Lasaia (SE Crete, Greece)","authors":"N. Mourtzas, Eleni Kolaiti","doi":"10.4000/mediterranee.12549","DOIUrl":"https://doi.org/10.4000/mediterranee.12549","url":null,"abstract":"","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-05-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42726881","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"La morphogenèse holocène dans le Haut-Tell tunisien entre nature et société","authors":"Abdelhamid Ben Ghazi","doi":"10.4000/mediterranee.11762","DOIUrl":"https://doi.org/10.4000/mediterranee.11762","url":null,"abstract":"","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-02-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47192161","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Géoarchéologie de Port‑la‑Nautique (étangs narbonnais)","authors":"Clément Flaux, Nicolas Carayon, Camille Faisse, M. Guy, Tiphaine Salel, C. Sanchez","doi":"10.4000/mediterranee.11732","DOIUrl":"https://doi.org/10.4000/mediterranee.11732","url":null,"abstract":"Les routes fluviales, lagunaires et maritimes de l’histoire du port de Narbonne se croisent au cœur des etangs narbonnais et s’inscrivent dans un cadre geographique mouvant qui impose a son etude une approche geoarcheologique. Nous presentons ici l’etude du cas de Port la Nautique, situe vers l’extremite nord des etangs narbonnais et dont l’archeologie a revele l’intense activite portuaire qui s’y est deroulee entre le 1er siecle avant et le 1er siecle de notre ere. La compilation de 83 colonnes sedimentaires extraites au sein et autour de ce port antique permet de mieux apprehender l'evolution de ce rivage lagunaire occupe depuis l'Antiquite et d’apporter des indications paleo‑hydrologiques sur le fonctionnement des etangs a cette periode. Nos principales conclusions sont les suivantes :1 - le toit du substrat marneux miocene decrit d'ouest en est correspond a une morphologie de vallon qui explique l'accessibilite du site depuis le plateau du Quatourze et a promu un secteur lagunaire profond a proximite d’un rivage rocheux egalement dote de sources d’eaux douces ;2 - le niveau des etangs narbonnais est enregistre entre – 5 et – 5,6 m NGF vers 5500 avant notre ere et entre – 0,6 et – 0,3 NGF autour du changement d’ere ;3 - les assemblages faunistiques traduisent un environnement lagunaire tres ouvert aux influences marines durant l’antiquite. L’âge reservoir antique de la lagune est mesure entre 400 et 550 ans, en coherence avec celui du golfe du Lion actuel ;4 - apres l’antiquite, une phase de confinement du secteur par rapport au domaine marin correspond au compartimentage tardif des etangs narbonnais ;5 - les periodes antiques et contemporaines sont caracterisees par un taux de sedimentation apparent moyen de 9 ± 5 mm.an-1 et 33 ± 6 mm.an-1, respectivement. La periode intermediaire est caracterisee par un taux moyen de 0,5 ± 0,2 mm.an-1, similaire au taux de sedimentation moyen apparent mesure sur l'ensemble de la sequence lagunaire deposee depuis 7 500 ans (autour de 0,6 mm.an‑1). Ces deux phases de rapide exhaussement des fonds lagunaires sont mises en relation avec la presence de structures portuaires, dont le role protecteur face aux houles induit un role de piege a sediments ;- 6) durant l'occupation portuaire antique, la bathymetrie evolue entre 2,7 et 1 m a l'ouest et au centre et entre 3,2 et 2 m a l'est du site. La diminution de la hauteur d’eau disponible ferme l’acces de Port–la–Nautique aux navires de moyenne capacite et induit peut-etre le declin de son activite portuaire ;","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-05-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45236698","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Mobilité du trait de côte et destruction des vestiges archéologiques de la façade nord‑occidentale du Cap Bon (Tunisie)","authors":"M. Kouka, S. Trabelsi","doi":"10.4000/mediterranee.11676","DOIUrl":"https://doi.org/10.4000/mediterranee.11676","url":null,"abstract":"Le lineaire cotier situe entre Sidi Daoud et Sidi Errais (Cap Bon, Tunisie) a connu un recul modere a l’origine de la destruction d’une partie importante des vestiges archeologiques. Cette etude vise a fournir une base de donnees sur l’evolution recente et actuelle du rivage le long de la facade nord-occidentale du Cap Bon. Pour ce faire, l’approche SIG a consiste en une comparaison de photographies aeriennes de trois missions de 1962, 1989 et 2000 avec l’image Google Earth de 2018. La mesure de la dynamique du trait de cote s’est faite par le biais du l’extension Digital Shoreline Analysis System (DSAS) sous ARCGIS. Les resultats des analyses diachroniques montrent clairement qu’il n’existe presque aucun espace epargne par le recul des rivages et qu’un important patrimoine archeologique est en cours de destruction.","PeriodicalId":38417,"journal":{"name":"Mediterranee","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-03-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42249887","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}