Diplopora oregonensis is a species of algae in the genus Diplopora in the family Diploporaceae. It is a unique species of marine dasycladacean algae from the Triassic period. It was discovered by George Stanley of the University of Montana, with findings published in the 1980s. It was obtained from sands and shales of the Wallowa volcanic archipelago, more specifically the Hurwal Formation in eastern Oregon. The strata of this formation developed from geologic processing of limestone deposits. The deposits were produced along the floors of lagoons of an ancient shallow ocean.[1][2][3]
| Diplopora oregonensis Temporal range:
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|---|---|
Scientific classification 
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| Clade: | Viridiplantae |
| Division: | Chlorophyta |
| Class: | UTC clade |
| Order: | Dasycladales |
| Family: | †Diploporaceae |
| Genus: | †Diplopora |
| Species: | †D. oregonensis
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| Binomial name | |
| †Diplopora oregonensis E. Flügel et al.
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References
edit- ^ Orr, Elizabeth L.; Orr, William N. (2009). Oregon fossils (2nd ed.). Corvallis: Oregon State University Press. pp. 7–8. ISBN 9780870715730.
- ^ "The University of Montana Paleontology Center". Retrieved 23 November 2014.
- ^ Erik Flügel; Baba Senowbari-Daryan; George D. Stanley, Jr. (1989). "Late Triassic dasycladacean alga from northeastern Oregon: significance of first reported occurrence in western North America". Journal of Paleontology. 63 (3): 374–381. doi:10.1017/S0022336000019545. JSTOR 1305509. S2CID 130316730.
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