Formasi Packard
| Formasi Packard Jangkauan stratigrafi: Mesozoikum | |
|---|---|
| Jenis | Formasi geologi |
| Unit | Grup Cabullona |
| Location | |
| Negara | Meksiko |
Formasi Packard adalah sebuah formasi geologi Mesozoikum.[1] Formasi ini kemungkinan berasal dari masa vertebrata darat Kirtlandian.[2] Formasi ini memiliki fauna yang serupa dengan Formasi Corral de Enmedio.[2]
Paleofauna
Sisa-sisa fragmen dari lepisosteid, trionychid, eusuchian, hadrosaurid, dan ceratopsid yang belum ditentukan telah diketahui dari Formasi Packard.
| Vertebrata dari Formasi Packard | ||||||
|---|---|---|---|---|---|---|
| Genus | Spesies | Lokasi | Posisi Stratigrafi | Kelimpahan | Catatan | Gambar |
| Albertosaurus[3] | Tidak ditentukan[3] |  | ||||
| Chamops[2] | C. segnis[2] | |||||
| Melvius[2] | Tidak ditentukan[2] | |||||
| Tototlmimus[4] | T. packardensis[4] | Grup Cabullona | ||||
Lihat juga
Catatan kaki
- ^ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
- ^ a b c d e f "Corral De Enmedio and Packard Formations, Cabollona Group, Sonora, Mexico," dalam Sullivan dan Lucas (2006). Halaman 16.
- ^ a b Terdaftar sebagai "cf. Albertosaurus sp." dalam "Corral De Enmedio and Packard Formations, Cabollona Group, Sonora, Mexico," dalam Sullivan dan Lucas (2006). Halaman 16.
- ^ a b Claudia Inés Serrano-Brañas; Esperanza Torres-Rodríguez; Paola Carolina Reyes-Luna; Ixchel González-Ramírez; Carlos González-Leóne (2016). "A new ornithomimid dinosaur from the Upper Cretaceous Packard Shale Formation (Cabullona Group) Sonora, México". Cretaceous Research. 58: 49–62. doi:10.1016/j.cretres.2015.08.013.
Referensi
- Sullivan, R.M., dan Lucas, S.G. 2006. "The Kirtlandian land-vertebrate "age" – faunal composition, temporal position and biostratigraphic correlation in the nonmarine Upper Cretaceous of western North America[pranala nonaktif permanen]." New Mexico Museum of Natural History and Science, Bulletin 35:7-29.
- Weishampel, David B.; Dodson, Peter; dan Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 hlm. ISBN 0-520-24209-2.
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