["itemContainer",{"xmlns:xsi":"http://www.w3.org/2001/XMLSchema-instance","xsi:schemaLocation":"http://omeka.org/schemas/omeka-xml/v5 http://omeka.org/schemas/omeka-xml/v5/omeka-xml-5-0.xsd","uri":"http://ifrecor-doc.fr/items/browse?output=omeka-json&tag=pal%C3%A9oenvironnement","accessDate":"2026-04-14T23:03:35+02:00"},["miscellaneousContainer",["pagination",["pageNumber","1"],["perPage","15"],["totalResults","1"]]],["item",{"itemId":"1572","public":"1","featured":"0"},["fileContainer",["file",{"fileId":"1661"},["src","http://ifrecor-doc.fr/files/original/b5ecc982932789d87b4ef3c8c474ef83.pdf"],["authentication","7c1f4b68ca40814359e4cbc2774a22c0"]]],["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. For more information see, http://dublincore.org/documents/dces/."],["elementContainer",["element",{"elementId":"50"},["name","Title"],["description","A name given to the resource"],["elementTextContainer",["elementText",{"elementTextId":"8192"},["text","Tectonic stability since the last interglacial offsets the Glorieuses Islands from the nearby Comoros archipelago"]]]],["element",{"elementId":"39"},["name","Creator"],["description","An entity primarily responsible for making the resource"],["elementTextContainer",["elementText",{"elementTextId":"8193"},["text","M. M. M. Guillaume • J.-L. Reyss • P. A. Pirazzoli • J. H. 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"]]]]]