Central Shikoku (32607R): Berriasian, Japan
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
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Polycystinea
- Nassellaria
- Canoptidae
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Cinguloturris cylindra
Kemkin and Rudenko 1993
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Polycystinea
- Nassellaria
- Parvicingulidae
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Ristola aff. cretacea
(Baumgartner 1980)
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Polycystinea
- Nassellaria
- Eucyrtidiellidae
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Eucyrtidiellum pyramis
(Aita 1986)
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Polycystinea
- Nassellaria
- Archaeodictyomitridae
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| see common names | |||||||
Geography
| Country: | Japan |
| Coordinates: | 33.7° North, 133.8° East (view map) |
| Paleocoordinates: | 49.6° North, 140.0° East (Wright 2013) |
| Basis of coordinate: | stated in text |
| Geographic resolution: | outcrop |
Time
| Period: | Cretaceous | Epoch: | Early Cretaceous |
| Stage: | Berriasian | 10 m.y. bin: | Cretaceous 1 |
| Key time interval: | Berriasian | Other zone: | Pseudodictyomitra carpatica |
| Age range of interval: | 143.1 - 137.05 m.y. ago |
Lithology and environment
| Primary lithology: | lithified mudstone |
| Lithology description: Member C is composed of sandstone, mudstone, tuff and alternating beds of sandstone and mudstone. The sandstone is medium-grained, graded and ranging from 1 cm to 10 cm in thickness. Parallel and current ripple laminations are observed. The mudstone yielded radiolarians (32606R, 32607R, 32608R, 32609R). This unit is approximately 280 m thick | |
| Environment: | slope |
Taphonomy
| Modes of preservation: | body |
| Size of fossils: | mesofossils,microfossils |
Collection methods and comments
| Collection methods: | field collection |
| Reason for describing collection: | taxonomic analysis |
Metadata
| Database number: | 116557 | ||
| Authorizer: | M. Aberhan | Enterer: | D. Wellmanns | Research group: | marine invertebrate |
| Created: | 2011-09-09 00:42:21 | Last modified: | 2025-02-22 15:12:02 |
| Access level: | authorizer only | Released: | 2016-09-09 00:42:21 |
| Creative Commons license: | CC0 |
Reference information
Primary reference:
| 37488. | T. Kozai, K. Ishida, and Y. Kondo. 2006. Radiolarians, bivalves and the J/K boundary in the Birafu Formation, southern Kurosegawa Belt, Central Shikoku, SW Japan. Geosciences Journal 10(3):217-235 [M. Aberhan/D. Wellmanns] |