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Richards Spur is a Permian fossil locality located at the Dolese Brothers Limestone Quarry north of Lawton, Oklahoma. The locality preserves clay and mudstone fissure fills of a karst system eroded out of Ordovician limestone and dolomite, with the infilling dating to the Artinskian stage of the early Permian (Cisuralian), around 289 to 286 million years ago. Fossils of terrestrial animals are abundant and well-preserved, representing one of the most diverse Paleozoic tetrapod communities known. A common historical name for the site is Fort Sill, in reference to the nearby military base. Fossils were first reported at the quarry by workers in 1932, spurring a wave of collecting by local and international geologists. Early taxa of interest included the abundant reptile Captorhinus and micro

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  • Richards Spur (nl)
  • Richards Spur (en)
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  • Richards Spur is a Permian fossil locality located at the Dolese Brothers Limestone Quarry north of Lawton, Oklahoma. The locality preserves clay and mudstone fissure fills of a karst system eroded out of Ordovician limestone and dolomite, with the infilling dating to the Artinskian stage of the early Permian (Cisuralian), around 289 to 286 million years ago. Fossils of terrestrial animals are abundant and well-preserved, representing one of the most diverse Paleozoic tetrapod communities known. A common historical name for the site is Fort Sill, in reference to the nearby military base. Fossils were first reported at the quarry by workers in 1932, spurring a wave of collecting by local and international geologists. Early taxa of interest included the abundant reptile Captorhinus and micro (en)
  • Richards Spur is een fossielenvindplaats uit het Perm, gelegen in de Dolese Brothers Limestone Quarry, ten noorden van Lawton in de Amerikaanse staat Oklahoma. De vindplaats bewaart spleetvullingen van klei en moddersteen van een karstsysteem dat is geërodeerd uit het Ordovicium-kalksteen en dolomiet, waarbij de opvulling dateert uit de Artinskien-periode van het Vroeg-Perm (Cisuralien), ongeveer 289 tot 286 miljoen jaar geleden. Fossielen van landdieren zijn overvloedig en goed bewaard gebleven, wat neerkomt op een van de meest diverse en bekende Paleozoïsche tetrapode gemeenschappen. Een veel voorkomende historische naam voor de vindplaats is Fort Sill, in verwijzing naar de nabijgelegen militaire basis. In 1932 werden voor het eerst fossielen gemeld in de steengroeve door deskundigen, w (nl)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Captorhinus_aguti_p.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Delorhynchus_cifellii_skulls.png
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