Fernando Formation
Fernando Formation Stratigraphic range: Pliocene epoch, Neogene period | |
---|---|
Type | Geologic formation |
Underlies | Pico Formation |
Location | |
Region |
Los Angeles Basin, Santa Monica Mountains Los Angeles County, California |
Country | United States |
The Fernando Formation is a Pliocene stratigraphic unit and geologic formation in the greater Los Angeles Basin and Santa Monica Mountains, in Los Angeles County of Southern California.
Geology
Outcrops of the formation in Santa Monica Mountains National Recreation Area have produced fossil shark teeth.[1][2]
Classification
The underlying Repetto Formation is equivalent in age to the Fernando Formation, and some researchers consider it as well as the overlying Pico Formation to be a junior synonym based on benthic foraminifera stages.[3] Other researchers maintain that the Repetto and Pico Formations are distinct stratigraphic units, and that the use of the name "Fernando Formation" should be stopped due to several issues with stratigraphic correlation and access to the type section.[4]
See also
- Geology of Los Angeles County, California
References
- ↑ Hunt, Santucci, and Kenworthy (2006). "Santa Monica Mountains National Recreation Area", page 67.
- ↑ Hunt, ReBecca K.; Santucci, Vincent L.; and Kenworthy, Jason (2006). "A preliminary inventory of fossil fish from National Park Service units." in S.G. Lucas, J.A. Spielmann, P.M. Hester, J.P. Kenworthy, and V.L. Santucci (ed.s), Fossils from Federal Lands. New Mexico Museum of Natural History and Science Bulletin 34, pp. 63–69.
- ↑ Sorlien, Christopher C.; Seeber, Leonardo; Broderick, Kris G.; Luyendyk, Bruce P.; Sliter, Ray W.; Normark, William R. "The Palos Verdes anticlinorium along the Los Angeles, California coast: implications for underlying thrust faulting." Geochemistry, Geophysics, Geosystems. Volume 14, Number 6, pp. 1866-1890. doi:10.102/ggge.20112
- ↑ Blake, Gregg H. 1991. "Review of the Neogene biostratigraphy and stratigraphy of the Los Angeles Basin and implications for basin evolution," In: Biddle, Kevin T. (ed), "Active Margin Basins", AAPG Memoir 52, 319pp.
Neogene Period | |||
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Miocene | Pliocene | ||
Aquitanian | Burdigalian Langhian | Serravallian Tortonian | Messinian |
Zanclean | Piacenzian |