| dbo:abstract
|
- The Bajo de Véliz Formation is stratigraphic formation of the Paleozoic located in the , Argentina. This formation lies in the northwestern sector of San Luis, about 25 km west of Santa Rosa de Conlara. Containing a slice of the Carboniferous-Permian transition, it is one of the key upper Paleozoic successions characterizing that era in westernmost Gondwana, which South America was a part of in the Paleozoic. It consists of Cautana (Upper Carboniferous), Pallero (end-Pennsylvanian to Cisuralian), and Lomas (Permian) units. Based on the paleoflora found in the middle upper Pallero unit, it was suggested to be of earliest Cisuralian age of the early Permian, though there is still ambiguity as insects associated with that layer have been assigned to the late Pennsylvanian of the Carboniferous. It is one of the key windows into the fossil life of the Gzhelian to Asselian, and is known as the formation where the thought-to-be giant spider Megarachne, actually a eurypterid, was discovered. (en)
- El Parque provincial Bajo de Véliz es un área protegida ubicada en cercanías de la localidad de Santa Rosa de Conlara, en el departamento Junín, al noreste de la provincia de San Luis, en la región central de la Argentina. El parque protege un importante yacimiento paleontológico del período carbónico superior. (es)
|
| dbo:thumbnail
| |
| dbo:wikiPageID
| |
| dbo:wikiPageLength
|
- 12889 (xsd:nonNegativeInteger)
|
| dbo:wikiPageRevisionID
| |
| dbo:wikiPageWikiLink
| |
| dbp:age
| |
| dbp:country
| |
| dbp:extent
| |
| dbp:name
|
- Bajo de Véliz Formation (en)
|
| dbp:namedby
| |
| dbp:otherlithology
| |
| dbp:overlies
| |
| dbp:period
| |
| dbp:prilithology
| |
| dbp:region
| |
| dbp:subunits
|
- Cautana, Pallero & Lomas members (en)
|
| dbp:type
| |
| dbp:unitof
| |
| dbp:wikiPageUsesTemplate
| |
| dbp:yearTs
| |
| dcterms:subject
| |
| georss:point
|
- -32.31138888888889 -65.41333333333333
|
| rdf:type
| |
| rdfs:comment
|
- El Parque provincial Bajo de Véliz es un área protegida ubicada en cercanías de la localidad de Santa Rosa de Conlara, en el departamento Junín, al noreste de la provincia de San Luis, en la región central de la Argentina. El parque protege un importante yacimiento paleontológico del período carbónico superior. (es)
- The Bajo de Véliz Formation is stratigraphic formation of the Paleozoic located in the , Argentina. This formation lies in the northwestern sector of San Luis, about 25 km west of Santa Rosa de Conlara. Containing a slice of the Carboniferous-Permian transition, it is one of the key upper Paleozoic successions characterizing that era in westernmost Gondwana, which South America was a part of in the Paleozoic. (en)
|
| rdfs:label
|
- Bajo de Véliz Formation (en)
- Parque provincial Bajo de Véliz (es)
|
| rdfs:seeAlso
| |
| owl:sameAs
| |
| geo:geometry
|
- POINT(-65.413330078125 -32.311389923096)
|
| geo:lat
| |
| geo:long
| |
| prov:wasDerivedFrom
| |
| foaf:depiction
| |
| foaf:isPrimaryTopicOf
| |
| is dbo:wikiPageRedirects
of | |
| is dbo:wikiPageWikiLink
of | |
| is foaf:primaryTopic
of | |
