Elisabeth Bay Formation

Elisabeth Bay Formation
Stratigraphic range: Aquitanian-Burdigalian
~21 Ma
Type Geological formation
Overlies Blaubok Conglomerate
Lithology
Primary Siltstone
Other Sandstone, claystone, conglomerate
Location
Coordinates 27°00′S 15°18′E / 27.0°S 15.3°E / -27.0; 15.3Coordinates: 27°00′S 15°18′E / 27.0°S 15.3°E / -27.0; 15.3
Approximate paleocoordinates 27°54′S 12°48′E / 27.9°S 12.8°E / -27.9; 12.8
Region ǁKaras Region
Country  Namibia
Extent Sperrgebiet
Type section
Named for Elizabeth Bay

The Elisabeth Bay Formation, alternatively spelled as Elizabeth Bay Formation, is an Early Miocene (Aquitanian to Burdigalian, around 21 Ma)[1] geologic formation in the Sperrgebiet, ǁKaras Region of southwestern Namibia, overlying the Blaubok Conglomerate.[2] The freshwater green and red siltstones, sandstones, intercalations of conglomerates and claystones of the formation were deposited in a fluvial environment,[3] infilling a paleovalley incised during the Oligocene low sea stand, which backfilled during the Burdigalian marine transgression.[1] The Elisabeth Bay Formation provides many fossil mammals, snakes and other reptiles.

Fossil content

The following fossils are reported from the formation:[4][5][6]

Mammals
Reptiles

See also

References

  1. 1 2 3 4 5 6 7 Pickford, 2018, p.88
  2. Dauteuil et al., 2018, p.6
  3. Elisabeth Bay Formation at Fossilworks.org
  4. Elisabethfeld at Fossilworks.org
  5. Grillental 6 at Fossilworks.org
  6. Grillental at Fossilworks.org
  7. Pickford, 2018, p.89

Bibliography

Further reading

  • J.-C. Rage. 2008. Squamate reptiles from the Lower Miocene of the Sperrgebiet, Namibia. In M. Pickford and B. Senut (eds.), Geology and palaeobiology of the northern Sperrgebiet, Namibia. Memoir of the Geological Survey of Namibia (Ministry of Mines and Energy, Windhoek) 20:93-103
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