Temblor Formation Explained
Temblor Formation |
Type: | Geologic formation |
Age: | Late Oligocene-Mid Miocene ~ |
Period: | Miocene |
Prilithology: | Shale, sandstone |
Namedfor: | Temblor Ranch, McKittrick district, Kern County |
Namedby: | Anderson |
Year Ts: | 1905 |
Region: | Western San Joaquin Valley, Kern County, California |
Country: | United States |
Subunits: | Agua Sandstone Member, Buttonbed Sandstone Member, Carneros Sandstone Member, Cymric Shale Member, Devilwater Siltstone, Gould Shale, Media Shale Member, Round Mountain Silt, Santos Shale Member, Wygal Sandstone Member |
Underlies: | Monterey Formation |
The Temblor Formation is a geologic formation in California. It preserves fossils dating back from the Late Oligocene to the Middle Miocene of the Neogene period. It is notable for the famous Sharktooth Hill deposit (otherwise known as Ernst Quarry).[1]
Fossils
Vertebrates
Cartilagenous fishes
Sharks
Rays and skates
Reptiles
Birds
- †Diomedea californica
- †Fulmarus miocaenus
- †Hadrogyps aigialerus
- †Megalodytes morejohni[4]
- †Morus vagabundus[4]
- †Osteodontornis orri[4]
- †Pandion homalopteron[4]
- †Presbychen abavus[4]
- †Puffinus inceptor[4]
Mammals
See also
External links
Notes and References
- Web site: Vast Bed of Ancient Bones and Shark Teeth Explained . LiveScience . By Charles Q. Choi.
- Boessenecker, Ehret, D, Long, D, Churchill, M, Martin, E, Boessenecker, S. The Early Pliocene extinction of the mega-toothed shark Otodus megalodon: a view from the eastern north Pacific. PeerJ. 2019 Feb 13;7:e6088. doi: 10.7717/peerj.6088. eCollection 2019.
- Malchow, A. 2009. MIOCENE SHARK TOOTH HILL LOCALITY, KERN COUNTY, CALIFORNIA. Geological Society of America North-Central Section - 43rd Annual Meeting (2-3 April 2009)
- Stegall, J. 2016. Fossil Birds of the Mojave Desert & Environs. Murturango Press, Ridgecrest, California.
- L. G. Barnes. 1988. A new fossil pinniped (Mammalia: Otariidae) from the middle Miocene Sharktooth Hill Bonebed, California. Contributions in Science 396:1-11