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USNM9269, Ratchaburi Province, Thailand
| Lat/Long (Decimal) | 13.402,99.759 |
|---|---|
| Co-ordinates Derivation | based on nearby landmark |
| Given Location | Ratchaburi, Thailand |
| Mindat.org Region (for given coordinates) | Ratchaburi Province, Thailand |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| USNM9269, Block 1, Khao Chang Hill, Rat Buri | Grant R. E. (1976) | Rat Buri | Blocks sampled were either "in place" in the limestone mass; others were from float. But because the jungle terrain makes measurement of stratigraphic sections difficult, the stratigraphy is unknown. The age of the Rat Buri fauna is problematic. "Rat Buri" limestones likely range in age from Kungurian through Capitanian to perhaps Wuchiapingian. Wordian fusulinids appear most common in other collections, but are not found in association with the brachiopod localities. The brachopod fauna is most | "limestone" | 272.3 - 268.8 Ma Permian |
| USNM9269, Block 2, Khao Chang Hill, Rat Buri | Grant R. E. (1976) | Rat Buri | Blocks sampled were either "in place" in the limestone mass; others were from float. But because the jungle terrain makes measurement of stratigraphic sections difficult, the stratigraphy is unknown. The age of the Rat Buri fauna is problematic. "Rat Buri" limestones likely range in age from Kungurian through Capitanian to perhaps Wuchiapingian. Wordian fusulinids appear most common in other collections, but are not found in association with the brachiopod localities. The brachopod fauna is most | "limestone" | 272.3 - 268.8 Ma Permian |
| USNM9269, Block 3, Khao Chang Hill, Rat Buri | Grant R. E. (1976) | Rat Buri | Blocks sampled were either "in place" in the limestone mass; others were from float. But because the jungle terrain makes measurement of stratigraphic sections difficult, the stratigraphy is unknown. The age of the Rat Buri fauna is problematic. "Rat Buri" limestones likely range in age from Kungurian through Capitanian to perhaps Wuchiapingian. Wordian fusulinids appear most common in other collections, but are not found in association with the brachiopod localities. The brachopod fauna is most | "limestone" | 272.3 - 268.8 Ma Permian |
| USNM9269, Block 4, Khao Chang Hill, Rat Buri | Grant R. E. (1976) | Rat Buri | Blocks sampled were either "in place" in the limestone mass; others were from float. But because the jungle terrain makes measurement of stratigraphic sections difficult, the stratigraphy is unknown. The age of the Rat Buri fauna is problematic. "Rat Buri" limestones likely range in age from Kungurian through Capitanian to perhaps Wuchiapingian. Wordian fusulinids appear most common in other collections, but are not found in association with the brachiopod localities. The brachopod fauna is most | "limestone" | 272.3 - 268.8 Ma Permian |
Recorded Fossils
References
| Grant R. E. (1976) Permian brachiopods from southern Thailand, Paleontological Society Memoir 9, 1-269 |
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!
