@prefix qx8: . @prefix skos: . qx8: a skos:ConceptScheme . qx8:-LSZ379CH-1 skos:definition "À l'échelle des temps géologiques, le Capitanien est un étage du Permien. C'est la dernière ou plus récente des trois subdivisions de l'époque du Guadalupien. Le Capitanien est daté entre -265,1 ± 0,4 et -259,1 ± 0,5 millions d'années (Ma). Il est précédé par le Wordien et suivi par le Wuchiapingien. L'étage Capitanien doit son nom au Capitan Reef dans les montagnes Guadalupe au Texas. Le début de l'étage est défini comme le moment de l'apparition stratigraphique de fossiles de l'espèce de conodonte Jinogondolella postserrata. Le point stratotypique mondial est situé à Nipple Hill dans le sud des montagnes Guadalupe, dans un affleurement de la Formation de Bell Canyon. La fin du Capitanien (et le début du Wuchiapingien) est défini comme le moment de l'apparition stratigraphique de fossiles de l'espèce de conodonte Clarkina postbitteri. (Adapté de : https://fr.wikipedia.org/wiki/Capitanien)"@fr, "In the geologic timescale, the Capitanian is an age or stage of the Permian. It is also the uppermost or latest of three subdivisions of the Guadalupian Epoch or Series. The Capitanian lasted between 264.28 and 259.51 million years ago. It was preceded by the Wordian and followed by the Wuchiapingian. A significant mass extinction event occurred at the end of this stage, which was associated with anoxia and acidification in the oceans and possibly caused by the volcanic eruptions that produced the Emeishan Traps. This extinction event may be related to the much larger Permian–Triassic extinction event that followed about 10 million years later. The name comes from the Capitan Reef in the Guadalupe Mountains (Texas, United States). The base of the Capitanian Stage is defined as the place in the stratigraphic record where fossils of conodont species Jinogondolella postserrata first appear. The global reference profile for this stratigraphic boundary is located at Nipple Hill in the southern Guadalupe Mountains of Texas. The top of the Capitanian (the base of the Wuchiapingian and Lopingian series) is defined as the place in the stratigraphic record where the conodont species Clarkina postbitteri postbitteri first appears. Carbon isotopes in marine limestone from the Capitanian age show an increase in δ13C values. The change in carbon isotopes in the sea water reflects cooling of global climates. This climatic cooling may have caused the end-Capitanian extinction event among species that lived in warm water, like larger fusulinids (Verbeekninidae), large bivalves (Alatoconchidae) and rugose corals, and Waagenophyllidae. (Adapted from: https://en.wikipedia.org/wiki/Capitanian)"@en ; a skos:Concept ; skos:inScheme qx8: ; skos:broader qx8:-L6WRLWZS-B ; skos:prefLabel "Roadian"@en, "Roadien"@fr ; skos:exactMatch , . qx8:-L6WRLWZS-B skos:prefLabel "Guadalupian"@en, "Guadalupien"@fr ; a skos:Concept ; skos:narrower qx8:-LSZ379CH-1 .