Tamayama Formation
| Tamayama Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Geological formation |
| Unit of | Futaba Group |
| Sub-units | Kohisagawa Member, Irimaza Member |
| Underlies | Unconformity with the Eocene Iwaki Formation |
| Overlies | Kasamatsu Formation |
| Thickness | ~ 150 metres |
| Lithology | |
| Primary | Sandstone |
| Other | Siltstone |
| Location | |
| Region | northern Honshu |
| Country |  Japan |
The Tamayama Formation is a Coniacian-Santonian geologic formation in Japan. Dinosaur remains not referrable to the genus level are among the fossils that have been recovered from the formation.[1] The lower and middle part of the formation consists of braided river sandstone, while the upper portion consists of upper shoreface to inner shelf sandstone.[2] Vertebrate taxa from the formation include Futabasaurus and Cretalamna, along with titanosauriform teeth and neosuchian remains. Seeds of the nymphaeales plant Symphaenale futabensis are also known from this formation.
Fossils
[edit]Paleofauna
[edit]- Futabasaurus suzukii
- Cretalamna appendiculata[3]
- Inoceramus
- Apiotrigonia minor[3]
- Glycymeris? sp.[3]
- Archaeromma chisatoi[5]
- Titanosauriformes indet.[4]
- Neosuchia indet.[6]
Paleoflora
[edit]See also
[edit]
Footnotes
[edit]- ^ 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.
- ^ a b c Shimada, K.; Tsuihiji, T.; Sato, T.; Hasegawa, Y. (2010). "A remarkable case of a shark-bitten elasmosaurid plesiosaur". Journal of Vertebrate Paleontology. 30 (2): 592–597. Bibcode:2010JVPal..30..592S. doi:10.1080/02724631003621920. S2CID 128760390.
- ^ a b c Saegusa, H.; Tomida, Y. (2011). "Titanosauriform teeth from the Cretaceous of Japan". Anais da Academia Brasileira de Ciências. 83 (1): 247–265. doi:10.1590/S0001-37652011000100014.
- ^ Aiba, H.; Inose, H. (2024). "A New False Fairy Wasp (Hymenoptera: Mymarommatoidea: Mymarommatidae) in Late Cretaceous Iwaki Amber from Futaba Group of Iwaki City, Fukushima Prefecture, Japan". Paleontological Research. 28 (3): 1–8. doi:10.2517/PR230020.
- ^ Yoshida, J.; Takahashi, T.; Nabana, S. (2023). "A crocodyliform osteoderm from the Tamayama Formation（Upper Cretaceous） of Fukushima, Japan". Bulletin of the Fukushima Museum. 37: 29–36.
- ^ Takahashi, Masamichi; Friis, Else Marie; Crane, Peter R. (March 2007). "Fossil Seeds of Nymphaeales from the Tamayama Formation (Futaba Group), Late Cretaceous (Early Santonian) of Northeastern Honshu, Japan". International Journal of Plant Sciences. 168 (3): 341–350. doi:10.1086/510414. ISSN 1058-5893.
- ^ Takahashi, M.; Crane, P.R.; Ando, H. (1999-06-30). "Esgueiria futabensis sp. nov., a new angiosperm flower from the Upper Cretaceous (lower Coniacian) of northeastern Honshu, Japan". Paleontological Research. 3 (2): 81–87.
- ^ Takahashi, M.; Crane, P.R.; Manchester, S.R. (2002). "Hironoia fusiformis gen. et sp. nov.; a cornalean fruit from the Kamikitaba locality (Upper Cretaceous, Lower Coniacian) in northeastern Japan". Journal of Plant Research. 115 (6): 463–473. Bibcode:2002JPlR..115..463T. doi:10.1007/s10265-002-0062-6. PMID 12579450.
References
[edit]- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.
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