Earth:Futaba Group
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Short description: Geologic formation in Japan
Futaba Group Stratigraphic range: Coniacian–Santonian | |
---|---|
Type | Geological group |
Sub-units | Ashizawa Formation, Kasamatsu Formation, Tamayama Formation |
Underlies | Unconformity with Paleogene Shiramizu Group |
Overlies | Early Cretaceous Granite, Permian shale and sandstone |
Thickness | Over 300 metres |
Lithology | |
Primary | Sandstone, siltstone, conglomerate |
Location | |
Region | northern Honshu |
Country | Japan |
The Futaba Group is a Late Cretaceous geologic group in Japan . Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.[1] It consists of both fluvial and shallow marine sediments.[2] The plesiosaur Futabasaurus was found in this unit (specifically the Tamayama Formation).
See also
- List of dinosaur-bearing rock formations
- List of stratigraphic units with indeterminate dinosaur fossils
Footnotes
- ↑ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
- ↑ Ando, Hisao; Seishi, Masao; Oshima, Mitsuharu; Matsumaru, Tetsuya (1995). "Fluvial-Shallow Marine Depositional Systems of the Futaba Group (Upper Cretaceous). Depositional facies and sequences.". Journal of Geography (Chigaku Zasshi) 104 (2): 284–303. doi:10.5026/jgeography.104.284. ISSN 0022-135X. http://joi.jlc.jst.go.jp/JST.Journalarchive/jgeography1889/104.284?from=CrossRef.
References
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN:0-520-24209-2.
Original source: https://en.wikipedia.org/wiki/Futaba Group.
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