Elisabeth Bay Formation

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.

Elisabeth Bay Formation
Stratigraphic range: Aquitanian-Burdigalian
~
TypeGeological formation
OverliesBlaubok Conglomerate
Lithology
PrimarySiltstone
OtherSandstone, claystone, conglomerate
Location
Coordinates27.0°S 15.3°E / -27.0; 15.3
Approximate paleocoordinates27.9°S 12.8°E / -27.9; 12.8
RegionǁKaras Region
Country Namibia
ExtentSperrgebiet
Type section
Named forElizabeth Bay
Elisabeth Bay Formation is located in Namibia
Elisabeth Bay Formation
Elisabeth Bay Formation (Namibia)

Fossil content

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

Mammals
Reptiles

See also

References

  1. 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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