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Suva, Viti Levu, Fiji
| Formation | Suva |
|---|---|
| Age: | 23.0 - 2.6 Ma Cenozoic |
| Interval | Neogene |
| Lithology | limestone, marl |
| Number of Collections | 4 |
| Number of Occurrences | 7 |
Recorded Sample Locations
| Location | Region | Stratigraphic Name |
|---|---|---|
| Station 158 | Viti Levu, Fiji | Suva |
| Station 59 [Navosa Group] | Viti Levu, Fiji | Suva |
| Station 133 | Viti Levu, Fiji | Suva |
| Station 320 | Viti Levu, Fiji | Suva |
Associated Units
| Stratigraphic Name | Age | Lithology | Occurrence Records |
|---|---|---|---|
| Navosa | 7.25 - 5.33 Ma Miocene | 82 |
Recorded Fossils
| Accepted Name | Hierarchy | Age |
|---|---|---|
 Cycloes granulosaspecies | Animalia : Arthropoda : Malacostraca : Decapoda : Calappidae : Cycloes : Cycloes granulosa | 23.03 - 2.588 Ma Cenozoic |
| Montezumella lamiensis species | Animalia : Arthropoda : Malacostraca : Decapoda : Dairidae : Montezumella : Montezumella lamiensis | 23.03 - 2.588 Ma Cenozoic |
 Birgus latrospecies | Animalia : Arthropoda : Malacostraca : Decapoda : Diogenidae : Birgus : Birgus latro | 23.03 - 2.588 Ma Cenozoic |
| Myra fijiensis species | Animalia : Arthropoda : Malacostraca : Decapoda : Leucosiidae : Myra : Myra fijiensis | 23.03 - 2.588 Ma Cenozoic |
| Parthenope fijiensis species | Animalia : Arthropoda : Malacostraca : Decapoda : Parthenopidae : Parthenope : Parthenope fijiensis | 23.03 - 2.588 Ma Cenozoic |
| Chlorodiella junghuhni species | Animalia : Arthropoda : Malacostraca : Decapoda : Xanthidae : Chlorodiella : Chlorodiella junghuhni | 23.03 - 2.588 Ma Cenozoic |
 Maja laddispecies | Animalia : Arthropoda : Maja : Maja laddi | 23.03 - 2.588 Ma Cenozoic |
References
| Rathbun M. J. (1934) Fossil Decapod Crustaceans from Vitilevu, Fiji, Geology of Vitilevu, Fiji, 238-241 |
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!
