@prefix qx8: <http://data.loterre.fr/ark:/67375/QX8> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .

qx8: a skos:ConceptScheme .
qx8:-JN3X9P45-4
  skos:altLabel "Holsteinian Stage"@en, "Holsteinian interglaciation"@en, "stade holsteinien"@fr, "interglaciaire holsteinien"@fr, "Holstein interglacial"@en, "interglaciation holsteinienne"@fr, "Holsteinian interglacial"@en ;
  skos:broader qx8:-PQ8FVKX8-3, qx8:-DBVJSC5H-W ;
  skos:inScheme qx8: ;
  skos:exactMatch <https://fr.wikipedia.org/wiki/Interglaciaire_Mindel-Riss>, <https://en.wikipedia.org/wiki/Holstein_interglacial> ;
  a skos:Concept ;
  skos:prefLabel "Holsteinian"@en, "Holsteinien"@fr ;
  skos:definition "Le Holsteinien ou Interglaciaire Mindel-Riss (dans la région alpine) désigne la période interglaciaire venant entre la glaciation de Mindel qui la précède et la glaciation de Riss qui la suit. Traditionnellement, il est considéré en tant qu'étage pollinique interglaciaire du Pléistocène moyen d'Europe du Nord, faisant suite à la glaciation de l'Elster ; d'après la région de Holstein (Allemagne). (Adapté de : <a href=\"https://fr.wikipedia.org/wiki/Interglaciaire_Mindel-Riss\">https://fr.wikipedia.org/wiki/Interglaciaire_Mindel-Riss</a> et Moureau M. & Brace G. (2000). Dictionnaire des Sciences de la Terre - Comprehensive Dictionary of Earth Science. Paris, Technip.)"@fr, "The Holstein interglacial (German: Holstein-Warmzeit or Holstein-Interglazial), also called the Mindel-Riss interglacial (Mindel-Riß-Interglazial) in the Alpine region, is the third to last major interglacial before the Holocene, the present warm period. It followed directly after the Elster glaciation and came before the Saale glaciation, during the Middle Pleistocene. The more precise timing is controversial since Holstein is commonly correlated to two different marine isotope stages, MIS 11 (424–374 thousand years ago) and MIS 9 (337–300 thousand years ago). This ambiguity is much related to the correlation problem described in more detail in the article 'Elster glaciation'. The Holstein interglacial is defined by marine sedimentation. On the stratigraphic record at the natural monument of de:Sievertsche Tongrube in Hamburg-Hummelsbüttel, its development is traced from the Elster ice age (Lauenburg clay) through the start of the warm period (freshwater depositions) to its flooding by the Holstein Sea (Cardien Sands). (Adapted from: <a href=\"https://en.wikipedia.org/wiki/Holstein_interglacial\">https://en.wikipedia.org/wiki/Holstein_interglacial</a>)"@en .

qx8:-DBVJSC5H-W
  skos:prefLabel "Pléistocène moyen"@fr, "Middle Pleistocene"@en ;
  a skos:Concept ;
  skos:narrower qx8:-JN3X9P45-4 .

qx8:-PQ8FVKX8-3
  skos:prefLabel "interglacial"@en, "interglaciaire"@fr ;
  a skos:Concept ;
  skos:narrower qx8:-JN3X9P45-4 .