Sphenopsalis Nobilis
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Sphenopsalis Nobilis
''Sphenopsalis'' is a genus of extinct mammal from the Paleocene of what is now Central Asia. It was a member of the extinct Order (biology), order Multituberculata, and lies within the suborder Cimolodonta and the superfamily Taeniolabidoidea. The genus was named by William Diller Matthew, W. Granger and George Gaylord Simpson in 1928. Many workers believe that members of the Taeniolabidoidea, such as ''Sphenopsalis'', are all quite similar. For example, they all share a short wide snout and a blocky head so it is probably instructive to look at a close and more commonly occurring relative, ''Lambdopsalis bulla'', a likely burrower. This organism is found in the fossil record from 59-55 million years ago, during the Thanetian age. One distinguishing feature of this genus is a single rooted 4th premolar (P4). Based on the structure of their teeth, ''Sphenopsalis'' appears to have been a leaf eater (foliovore). They and/or their close relatives may have been partially adapted ...
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Thanetian
The Thanetian is, in the International Commission on Stratigraphy, ICS Geologic timescale, the latest age (geology), age or uppermost stage (stratigraphy), stratigraphic stage of the Paleocene epoch (geology), Epoch or series (stratigraphy), Series. It spans the time between . The Thanetian is preceded by the Selandian Age and followed by the Ypresian Age (part of the Eocene). The Thanetian is sometimes referred to as the Late Paleocene. Stratigraphic definition The Thanetian was established by Switzerland, Swiss geologist Eugène Renevier in 1873. The Thanetian is named after the Thanet Formation, the oldest Cenozoic deposit of the London Basin, which was first identified in the area of Kent (southern England) known as the Isle of Thanet. The base of the Thanetian Stage is laid at the base of magnetic chronozone C26n. The references profile (Global Boundary Stratotype Section and Point) is in the Zumaia section (43° 18'N, 2° 16'W) at the beach of Itzurun, Pais Vasco, northern ...
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