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Tremp - Grey Garumnian, Spain
Group | Tremp |
---|---|
Formation | Grey Garumnian |
Member(s) | Middle |
Age: | 70.6 - 66.0 Ma Late/Upper Cretaceous |
Interval | Early Maastrichtian |
Tectonic Setting | Foreland basin |
Lithology | sandstone/marl, packstone/marl, mudstone, sandstone |
Number of Collections | 15 |
Number of Occurrences | 29 |
Recorded Sample Locations
Location | Region | Stratigraphic Name |
---|---|---|
Fumanya tracksite | BerguedĂ , Barcelona, Catalonia, Spain | Tremp - Grey Garumnian |
Mina Esquirol-1 | BerguedĂ , Barcelona, Catalonia, Spain | Tremp - Grey Garumnian |
Mina Esquirol-2 | BerguedĂ , Barcelona, Catalonia, Spain | Tremp - Grey Garumnian |
Mina Esquirol-3 | BerguedĂ , Barcelona, Catalonia, Spain | Tremp - Grey Garumnian |
Font de Bullidor | Pallars JussĂ , Lleida, Catalonia, Spain | Tremp - Grey Garumnian - Middle |
Les Quijoles | BerguedĂ , Barcelona, Catalonia, Spain | Tremp - Grey Garumnian |
L'Hostalet | Huesca, Aragon, Spain | Tremp - Grey Garumnian |
Lower TumĂ | BerguedĂ , Barcelona, Catalonia, Spain | Tremp - Grey Garumnian |
Els Terrers | BerguedĂ , Barcelona, Catalonia, Spain | Tremp - Grey Garumnian |
Sant JuliĂ | BerguedĂ , Barcelona, Catalonia, Spain | Tremp - Grey Garumnian |
Associated Units
Stratigraphic Name | Age | Lithology | Occurrence Records |
---|---|---|---|
Tremp - Conques | 70.6 - 66.0 Ma Late/Upper Cretaceous | sandstone, marl, conglomerate, "shale"/mudstone, conglomerate/sandstone, mudstone, sandstone/marl, conglomerate/"limestone", sandstone/mudstone | 170 |
Tremp - Grey Garumnian - Middle | 83.5 - 70.6 Ma Late/Upper Cretaceous | mudstone | 1 |
Tremp - Lower Red Garumnian | 70.6 - 66.0 Ma Late/Upper Cretaceous | sandstone/"limestone", "siliciclastic", mudstone, sandstone, sandstone/mudstone | 29 |
Recorded Fossils
References
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!