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New Red Sandstone - Kingscourt Sandstone - Middle Sandstone, Meath County, Leinster, Ireland

GroupNew Red Sandstone
FormationKingscourt Sandstone
MemberMiddle Sandstone
Age:252 - 251 Ma
Phanerozoic
IntervalGriesbachian
Tectonic SettingForeland basin
Lithologysandstone/"shale"
Number of Collections2
Number of Occurrences20

Recorded Sample Locations

LocationRegionStratigraphic Name
Conglomerate Member KingscourtMeath County, Leinster, IrelandNew Red Sandstone - Kingscourt Sandstone - Middle Sandstone

Associated Units

Stratigraphic NameAgeLithologyOccurrence Records
New Red Sandstone - Kingscourt Gypsum260 - 254 Ma
Permian
shale6
New Red Sandstone - Kingscourt Gypsum - Lower Gypsum260 - 254 Ma
Permian
evaporite/"shale"56
New Red Sandstone - Kingscourt Gypsum - Lower Mudstone260 - 254 Ma
Permian
mudstone/"shale"49
New Red Sandstone - Kingscourt Gypsum - Middle Mudstone260 - 254 Ma
Permian
mudstone/claystone7
New Red Sandstone - Kingscourt Gypsum - Upper Gypsum260 - 254 Ma
Permian
evaporite/mudstone6
New Red Sandstone - Kingscourt Gypsum - Upper Mudstone260 - 254 Ma
Permian
mudstone/"shale"7
New Red Sandstone - Kingscourt Sandstone - Siltstone252 - 251 Ma
Phanerozoic
siltstone/sandstone8

Recorded Fossils

Accepted NameHierarchyAge
Acritarcha
unranked clade
99Acritarcha252.17 - 251.3 Ma
Phanerozoic
Klausipollenites sp.
genus
6Plantae : Klausipollenites252.17 - 251.3 Ma
Phanerozoic
Lundbladispora sp.
genus
6Lundbladispora252.17 - 251.3 Ma
Phanerozoic
Vitreisporites pallidus
species
7Vitreisporites : Vitreisporites pallidus252.17 - 251.3 Ma
Phanerozoic
Cycadopites sp.
genus
6Plantae : Tracheophyta : Cycadopites252.17 - 251.3 Ma
Phanerozoic

References

Visscher H. (1971) The Permian and Triassic of the Kingscourt Outlier, Ireland, Geological Survey of Ireland Special Paper 1, 1-114
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
 
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