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Lower Lukuga - Schistes noirs, Tanganyika, DR Congo
| Group | Lower Lukuga |
|---|---|
| Formation | Schistes noirs |
| Age: | 296 - 290 Ma Permian |
| Interval | Sakmarian |
| Number of Collections | 2 |
| Number of Occurrences | 6 |
Recorded Sample Locations
| Location | Region | Stratigraphic Name |
|---|---|---|
| Kongolo | Tanganyika, DR Congo | Lower Lukuga - Schistes noirs |
| Lukuga | Tanganyika, DR Congo | Lower Lukuga - Schistes noirs |
Associated Units
| Stratigraphic Name | Age | Lithology | Occurrence Records |
|---|---|---|---|
| Upper Lukuga - Transition | 279 - 272 Ma Permian | 8 |
Recorded Fossils
| Accepted Name | Hierarchy | Age |
|---|
References
| Hoeg O. A., Bose M.N. (1960) The Glossopteris flora of the Belgian Congo, with a note on some fossil plants from the Zambesi Basin (Mozambique), Annales du Musee Royal du Congo Belge 32, 1-99 |
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!
