@prefix qx8: <http://data.loterre.fr/ark:/67375/QX8> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .
@prefix dc: <http://purl.org/dc/terms/> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .

qx8: a skos:ConceptScheme .
qx8:-5W21L7K1-Q
  skos:prefLabel "Flandrian"@en, "Flandrien"@fr ;
  skos:exactMatch <https://fr.wikipedia.org/wiki/Flandrien_(g%C3%A9ologie)>, <https://en.wikipedia.org/wiki/Flandrian_interglacial> ;
  dc:modified "2023-11-15T14:15:35"^^xsd:dateTime ;
  skos:broader qx8:-VRSD7KHT-V ;
  a skos:Concept ;
  skos:inScheme qx8: ;
  skos:altLabel "interglaciaire flandrien"@fr, "stade flandrien"@fr, "Flandrian stage"@en, "Flandrian interglacial"@en ;
  skos:definition "The Flandrian interglacial or stage is the regional name given by geologists and archaeologists in the British Isles to the period from around 12,000 years ago, at the end of the last glacial period to the present day. As such, it is in practice identical in span to the Holocene (the present geological epoch). The Flandrian began as the relatively short-lived Younger Dryas climate downturn came to an end. This was the last phase of the Devensian glaciation, the final stage of the Pleistocene epoch. The Flandrian is traditionally seen as the latest warm interglacial in a series that has been occurring throughout the Quaternary geological period. The first part of the Flandrian, known as the Younger Atlantic, was a period of fairly rapid sea level rise, known as the Flandrian transgression. It is associated with the melting of the Fenno-Scandian, Scottish, Laurentide and Cordilleran glaciers. Fjords were formed during the Flandrian transgression when U-shaped glaciated valleys were inundated. (Adapted from: <a href=\"https://en.wikipedia.org/wiki/Flandrian_interglacial\">https://en.wikipedia.org/wiki/Flandrian_interglacial</a>)"@en, "Le Flandrien est une époque géologique informelle équivalent à l'Holocène, allant de la dernière glaciation à nos jours. Ce terme est principalement utilisé par les géologues et archéologues britanniques. La différence principale entre le Flandrien et l'Holocène est une question de nomenclature formelle : contrairement à l'Holocène, qui est désormais ratifié par la commission internationale de stratigraphie en tant que série stratigraphique à part entière, l'usage du Flandrien considère plutôt ce dernier comme un simple interglaciaire faisant partie intégrante de la série Pléistocène. (Adapté de : <a href=\"https://fr.wikipedia.org/wiki/Flandrien_(g%C3%A9ologie)\">https://fr.wikipedia.org/wiki/Flandrien_(g%C3%A9ologie)</a>)"@fr .

qx8:-VRSD7KHT-V
  skos:prefLabel "Holocène"@fr, "Holocene"@en ;
  a skos:Concept ;
  skos:narrower qx8:-5W21L7K1-Q .