Gamerabaena
| Gamerabaena Temporal range: Late Cretaceous
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Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Clade: | Pantestudines |
| Clade: | Testudinata |
| Clade: | †Paracryptodira |
| Family: | †Baenidae |
| Genus: | †Gamerabaena Lyson and Joyce, 2010 |
| Species | |
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Gamerabaena is an extinct genus of baenid turtle which existed in North Dakota during the late Cretaceous Period. It is known from a single fragmentary skull that was found in the Maastrichtian-age Hell Creek Formation. It contains the species Gamerabaena sonsalla.[1] Gamerabaena is similar to the genus Palatobaena, but it differs in its lack of a posterior expansion of the triturating (or chewing) surface, a somewhat rectangular skull, and a wide angle between the maxillae. Gamerabaena also has a lingual ridge on the inner side of the jaw that is not seen in Palatobaena.[1]
Gamerabaena is considered the sister taxon of Palatobaena and shares features with both Palatobaena and Plesiobaena. These features, which include slightly upturned eye sockets, are seen as intermediate between the two other genera. While Gamerabaena is known only from the skull, it may belong to the same species as "Baena" hayi, which is known primarily from the shell.[1]
The genus is named after Gamera, a giant flying, fire-breathing turtle from a series of Japanese tokusatsu films.[1]
Phylogeny
[edit]Cladogram after Tyler R. Lyson and Walter G. Joyce (2009).[2]
See also
[edit]- Sinemys gamera – another species of fossil turtle named after Gamera
References
[edit]- ^ a b c d Lyson, T.R.; Joyce, W.G. (2010). "A new baenid turtle from the Upper Cretaceous (Maastrichtian) Hell Creek Formation of North Dakota and a preliminary taxonomic review of Cretaceous Baenidae" (PDF). Journal of Vertebrate Paleontology. 30 (2): 394–402. doi:10.1080/02724631003618389. S2CID 89517022.
- ^ Tyler R. Lyson & Walter G. Joyce (2009). "A Revision of Plesiobaena (Testudines: Baenidae) and an Assessment of Baenid Ecology Across the K/T Boundary". Journal of Paleontology. 83 (6): 833–853. doi:10.1666/09-035.1. S2CID 85964417.
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