USGS F-114, Ryukyu Island - Foster (1965): Late Pleistocene, Japan
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
|
Anthozoa
- Scleractinia
- Poritidae
|
|||||||
|
Porites sp.
Link 1807
|
|||||||
|
Anthozoa
- Scleractinia
- Fungiidae
|
|||||||
|
Fungia sp.
Lamarck 1801
|
|||||||
|
Gastropoda
- Neogastropoda
- Conidae
|
|||||||
|
Conus (Tuliparia) tulipa
Linnaeus 1758
|
|||||||
|
Bivalvia
- Pectinida
- Pectinidae
|
|||||||
|
Amusium sp.
(Röding 1798)
|
|||||||
|
cf. Chlamys vesiculosa
(Dunker 1877)
|
|||||||
|
Decatopecten cf. striatus
(Schumacher 1817)
|
|||||||
|
cf. Chlamys leopardus
(Reeve 1853)
|
|||||||
|
Bivalvia
- Arcida
- Glycymerididae
|
|||||||
|
Glycymeris sp.
Da Costa 1778
|
|||||||
| see common names | |||||||
Geography
| Country: | Japan | State/province: | Ryukyu |
| Coordinates: | 24.4° North, 124.2° East (view map) | ||
| Paleocoordinates: | |||
| Basis of coordinate: | estimated from map | ||
| Geographic resolution: | outcrop |
Time
| Period: | Quaternary | Epoch: | Pleistocene |
| Stage: | Late Pleistocene | 10 m.y. bin: | Cenozoic 6 |
| Key time interval: | Late Pleistocene | ||
| Age range of interval: | 0.129 - 0.0117 m.y. ago |
Stratigraphy
| Geological group: | Sakishima | Formation: | Ryukyu Limestone | ||
| Local section: | F-114 | ||||
| Regional section: | Ryukyu | ||||
| Stratigraphic resolution: | bed | ||||
| Stratigraphy comments: The Ryukyu Limestone unconformably overlies rocks of the Ishigaki Group, the Miyara Formation, the Nosoko Formation, and the Omoto Granite. Two principal lithologies are present - a stratified sandy limestone, and a massive coralliferous limestone. Conglomeratic limestone is common at th base of the formation | |||||
Lithology and environment
| Primary lithology: | planar lamination,brown,yellow poorly lithified sandy,calcareous "limestone" |
| Secondary lithology: | fine,shelly/skeletal lithified calcareous "limestone" |
| Includes fossils? | Y |
| Includes fossils? | Y |
| Lithology description: The sandy foraminiferal limestone consists of sand sized particles loosely to formly cemented together by calcium carbonate. It is white, light tan or cream. The coralliferous limestone is mostly a well lithified, bioclastic, recrystallized limestone composed of tests or fragments of forams, pieces of corals, pieces of algae, and other types of fossils in a groundmass of fine calcareous organic debris. | |
| Environment: | carbonate indet. |
Taphonomy
| Modes of preservation: | body,mold/impression |
| Size of fossils: | macrofossils |
Collection methods and comments
| Collection excludes: | all microfossils |
| Collection methods: | selective quarrying,field collection |
| Reason for describing collection: | taxonomic analysis |
| Museum repositories: | USNM |
| Collection method comments: Probably reposited in USGS and USNM collections | |
| Taxonomic list comments:Representative of corals and mollusca. Identified by J.W. Wells (corals) and F.S. MacNeil (mollusca) | |
Metadata
| Also known as: | USGS F-114 | ||
| Database number: | 41603 | ||
| Authorizer: | A. Hendy | Enterer: | A. Hendy |
| Modifier: | A. Hendy | Research group: | marine invertebrate |
| Created: | 2004-07-17 22:54:31 | Last modified: | 2025-02-22 15:12:02 |
| Access level: | the public | Released: | 2004-07-17 22:54:31 |
| Creative Commons license: | CC0 | ||
Reference information
Primary reference:
| 11144. | H. L. Foster. 1965. Geology of Ishigaki-shima Ryukyu-retto. United States Geological Survey Professional Paper 399(A):1-119 [A. Miller/A. Hendy/A. Hendy] |