Puget Group
Nowadays, Puget Group has become a topic of great interest and relevance in society. Over time, Puget Group has played a crucial role in different aspects of daily life, affecting people of all ages and lifestyles. As Puget Group continues to evolve and acquire different dimensions, it is important to thoroughly analyze its impact in various areas, from health to the economy. In this article, we will take a closer look at the many facets of Puget Group and its influence on everyday life, as well as the future perspectives it may bring.
| Puget Group | |
|---|---|
| Stratigraphic range: Paleogene | |
| Type | Group |
| Sub-units | Tiger Mountain, Tukwila, Renton |
| Lithology | |
| Primary | Deltaic |
| Other | Marine, Riverine, Volcanic |
| Location | |
| Region | King County, Washington |
| Country | United States |
The Puget Group is a geologic group in Washington (state). It preserves fossils dating back to the Paleogene period.
In the northern area of group around Renton, Washington, the Group has been divided into three formations (from oldest to youngest), the Tiger Mountain Formation, the Tukwila Formation, and Renton Formation.[1][2] Robin Burnham (1994) specifies that these formations have not been defined and extended to Puget Group outcrops to the south within the Green River gorge and all of the Tukwila formation rocks are missing. The Puget Group has been mapped across a total of six western Washington geographic quadrangles.[1]
Age
The total deposition time has been estimated to be as short as approximately 7.7 million years, from around 45 to 36 million years ago based on isotopic data reported in 1993 or as long as 51 to 34 million years ago based on the paleofloristic data of Wolfe (1968, 1977)[1]
Western North American floral stages
The Western North American floras of the Eocene were divided into four floral "stages" by Jack Wolfe (1968) based on work with the Puget Group plant fossils. The four stages, Franklinian, Fultonian, Ravenian, and Kummerian covered the Early Eocene through early Oligocene, and three of the four were given informal early/late substages. Wolfe tentatively deemed the Franklinian as Early Eocene, the Fultonian as Middle Eocene, the Ravenian as Late, and the Kummerian as Early Oligocene.[3] The beginning of the Kummerian was refined by Gregory Retallack et al (2004) as 40 mya, with a refined end at the Eocene-Oligocene boundary where the younger Angoonian floral stage starts.[4]
See also
- List of fossiliferous stratigraphic units in Washington (state)
- Paleontology in Washington (state)
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.
References
- ^ a b c Burnham, R.J. (1994). Paleoecological and Floristic Heterogeneity in the Plant-Fossil Record - An Analysis Based on the Eocene of Washington (Report). Bulletin. United States Geological Survey. pp. 1–36. doi:10.3133/b2085B. hdl:2027/mdp.39015095145341. 2085-B.
- ^ Booth, Derek; Walsh, Timothy; Troost, Kathy; Shimel, Scott. "Geologic Map of the East Half of the Bellevue South 7.5' x 15' Quadrangle, Issaquah Area, King County, Washington,U.S. Geological Survey Scientific Investigations Map 3211, scale 1:24,000" (PDF). USGS. Retrieved 27 May 2020.
- ^ Wolfe, J.A. (1968). Paleogene Biostratigraphy of nonmarine rocks in King County, Washington (Report). Professional Paper. Vol. 571. United States Geological Survey. pp. 1–29. doi:10.3133/pp571.
- ^ Retallack, G.J.; Orr, W.N.; Prothero, D.R.; Duncan, R.A.; Kester, P.R.; Ambers, C.P. (2004). "Eocene–Oligocene extinction and paleoclimatic change near Eugene, Oregon". Geological Society of America Bulletin. 116 (7–8): 817–839. Bibcode:2004GSAB..116..817R. doi:10.1130/B25281.1.
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