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Bruggemann"]]]],["element",{"elementId":"45"},["name","Publisher"],["description","An entity responsible for making the resource available"],["elementTextContainer",["elementText",{"elementTextId":"8194"},["text","Coral Reefs\r\nJournal of the International Society for Reef Studies\r\nDOI 10.1007/s00338-012-1006-9"]]]],["element",{"elementId":"40"},["name","Date"],["description","A point or period of time associated with an event in the lifecycle of the resource"],["elementTextContainer",["elementText",{"elementTextId":"8195"},["text","2012"]]]],["element",{"elementId":"42"},["name","Format"],["description","The file format, physical medium, or dimensions of the resource"],["elementTextContainer",["elementText",{"elementTextId":"8196"},["text","pdf"]]]],["element",{"elementId":"44"},["name","Language"],["description","A language of the resource"],["elementTextContainer",["elementText",{"elementTextId":"8197"},["text","anglais"]]]],["element",{"elementId":"51"},["name","Type"],["description","The nature or genre of the resource"],["elementTextContainer",["elementText",{"elementTextId":"8198"},["text","Publication scientifique"]]]],["element",{"elementId":"38"},["name","Coverage"],["description","The spatial or temporal topic of the resource, the spatial applicability of the resource, or the jurisdiction under which the resource is relevant"],["elementTextContainer",["elementText",{"elementTextId":"8199"},["text","TAAF"]]]],["element",{"elementId":"41"},["name","Description"],["description","An account of the resource"],["elementTextContainer",["elementText",{"elementTextId":"8225"},["text","L’étude décrit quatre terrasses fossiles des Îles Glorieuses. Ces plateformes se seraient formées lors d’un épisode de haut niveau marin (+ 3m). La relative stabilité tectonique contraste avec la subsidence de l'île de Mayotte, suggérant un contexte géologique différent entre l’archipel des Comores proche, et les Glorieuses."]]]]]]],["tagContainer",["tag",{"tagId":"308"},["name","élévation du niveau de la mer"]],["tag",{"tagId":"374"},["name","paléoenvironnement"]],["tag",{"tagId":"372"},["name","pléistocène"]],["tag",{"tagId":"37"},["name","récif corallien"]],["tag",{"tagId":"375"},["name","scléractiniaires"]],["tag",{"tagId":"373"},["name","stratigraphie"]]]],["item",{"itemId":"1344","public":"1","featured":"0"},["fileContainer",["file",{"fileId":"1412"},["src","http://ifrecor-doc.fr/files/original/a5d8bc18d531b086f518d5bf2878259c.pdf"],["authentication","85c84e0b96032e10f83a30976363c9e7"]]],["collection",{"collectionId":"77"},["elementSetContainer",["elementSet",{"elementSetId":"1"},["name","Dublin Core"],["description","The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. 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