@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:-D40PL783-0
  skos:prefLabel "Domérien"@fr, "Domerian"@en ;
  a skos:Concept ;
  skos:broader qx8:-1PGP650C-M .

qx8: a skos:ConceptScheme .
qx8:-J39GL467-3
  skos:prefLabel "Lower Jurassic"@en, "Jurassique inférieur"@fr ;
  a skos:Concept ;
  skos:narrower qx8:-1PGP650C-M .

qx8:-1PGP650C-M
  skos:definition "Le Pliensbachien est un étage du Jurassique inférieur (Lias) succédant au Sinémurien et précédant le Toarcien, d'une durée d'environ 8 millions d'années comprise entre −190,8 ± 1,0 et −182,7 ± 0,7 millions d'années. Le Charmouthien est un synonyme du Pliensbachien. Le stratotype historique du Pliensbachien a été défini sous le nom de Pliensbach Gruppe sur des affleurements des rives du ruisseau Pliensbach près du village du même nom situé à proximité de la petite ville de Zell unter Aichelberg (commune du Bade-Wurtemberg), à 35 kilomètres au sud-ouest de Stuttgart en (Allemagne). (Adapté de : <a href=\"https://fr.wikipedia.org/wiki/Pliensbachien\">https://fr.wikipedia.org/wiki/Pliensbachien</a>)"@fr, "The Pliensbachian is an age of the geologic timescale and stage in the stratigraphic column. It is part of the Early or Lower Jurassic Epoch or Series and spans the time between 192.9 ±0.3 Ma and 184.2 ±0.3 Ma (million years ago). The Pliensbachian is preceded by the Sinemurian and followed by the Toarcian. The Pliensbachian ended with the extinction event called the Toarcian turnover. During the Pliensbachian, the middle part of the Lias was deposited in Europe. The Pliensbachian is roughly coeval with the Charmouthian regional stage of North America. The Pliensbachian takes its name from the hamlet of Pliensbach in the community of Zell unter Aichelberg in the Swabian Alb, some 30 km east of Stuttgart in Germany. The base of the Pliensbachian is at the first appearances of the ammonite species Bifericeras donovani and genera Apoderoceras and Gleviceras. The Wine Haven profile near Robin Hood's Bay (Yorkshire, England) has been appointed as global reference profile for the base (GSSP). The top of the Pliensbachian (the base of the Toarcian Stage) is at the first appearance of ammonite genus Eodactylites. (Adapted from: <a href=\"https://en.wikipedia.org/wiki/Pliensbachian\">https://en.wikipedia.org/wiki/Pliensbachian</a>)"@en ;
  skos:narrower qx8:-M9FJ9N15-8, qx8:-D40PL783-0 ;
  skos:prefLabel "Pliensbachien"@fr, "Pliensbachian"@en ;
  skos:inScheme qx8: ;
  skos:broader qx8:-J39GL467-3 ;
  skos:exactMatch <https://fr.wikipedia.org/wiki/Pliensbachien>, <https://en.wikipedia.org/wiki/Pliensbachian>, <http://data.loterre.fr/ark:/67375/26L-L6368BJ7-1> ;
  a skos:Concept ;
  dc:modified "2024-02-27T15:37:36"^^xsd:dateTime ;
  skos:altLabel "Charmouthien"@fr .

qx8:-M9FJ9N15-8
  skos:prefLabel "Carixien"@fr, "Carixian"@en ;
  a skos:Concept ;
  skos:broader qx8:-1PGP650C-M .