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Gymnogyps amplus






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Gymnogyps amplus

Temporal range: Late PleistoceneHolocene

Fossil skeleton from the La Brea Tar Pits
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Aves
Order: Cathartiformes
Family: Cathartidae
Genus: Gymnogyps
Species:
G. amplus
Binomial name
Gymnogyps amplus

L. H. Miller, 1911

Holotype Tarsometatarsus;
Samwel Cave, Shasta County, California

Gymnogyps amplus is an extinct species of large New World vulture in the family Cathartidae. The species was first described by Loye H. Miller (1911)[1]in1911 from a partial tarsometatarsus[2] recovered from Pleistocene cave deposits in Samwel Cave of northern California.[3] Harvey I. Fisher (1944) designated a set of plesiotypes from the Rancho La Brea which includes a cranium, rostrum, and mandible.[4]

The species is the only condor species found in the La Brea Tar Pits' Pit 10, which fossils date to "a Holocene radiocarbon age of 9,000 years."[4] The smaller, modern California condor may have evolved from G. amplus.[4]

References

[edit]
  1. ^ Miller, Loye Holmes (1911). "Avifauna of the Pleistocene Cave Deposits of California". Bulletin of the Department of Geology. 6 (16). University of California Publications: 390–391.
  • ^ Nadin, Elisabeth (26 October 2007). "Tracing the Roots of the California Condor". Caltech News. California Institute of Technology. Retrieved 11 October 2015.
  • ^ Fisher, H. I. (1947). "The skeletons of recent and fossil Gymnogyps". Pacific Science. 1 (4): 227–236.
  • ^ a b c Syverson, Valerie J.; Prothero, Donald R. (2010). "Evolutionary Patterns in Late Quaternary California Condors" (PDF). PalArch's Journal of Vertebrate Palaeontology. 7 (1). PalArch Foundation: 1–18. Retrieved 11 October 2015.

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  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Gymnogyps_amplus&oldid=1106745620"

    Categories: 
    Gymnogyps
    Pleistocene birds of North America
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    Taxa named by Loye H. Miller
    Prehistoric bird stubs
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    This page was last edited on 26 August 2022, at 06:43 (UTC).

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