Wikipedia

Black Crow Limestone

The Black Crow Limestone is an Early Eocene (Late Ypresian to Early Lutetian) geologic formation in the Sperrgebiet, ǁKaras Region of southwestern Namibia. The limestones of the approximately 10 metres (33 ft) thin formation were deposited in a lacustrine to paludal environment. The formation provides many fossil mammals and amphibians, reptiles, fresh water snails and fish.

Black Crow Limestone
Stratigraphic range: Late Ypresian-Early Lutetian
~48–43 Ma
↓
TypeGeological formation
UnderliesBlaubok Conglomerate
OverliesGariep Group
Thickness10 m (33 ft)
Lithology
PrimaryLimestone
Location
LocationNamib Desert
Coordinates27°22′40″S 15°27′46″E / 27.3778°S 15.4629°E / -27.3778; 15.4629
Approximate paleocoordinates33°42′S 6°12′E / 33.7°S 6.2°E / -33.7; 6.2
RegionǁKaras Region
Country Namibia
ExtentSperrgebiet
Type section
Locationnear Bogenfels

The formation crops out near Bogenfels in Namibia

Description edit

The type locality of Black Crow lies a few km north-east of Bogenfels Ghost Town, in the central part of the Tsau//Khaeb National Park (old name – Sperrgebiet) in Namibia.[1] The Black Crow Limestone with a total thickness of about 10 metres (33 ft),[2] is an Early Eocene stratigraphic unit of the Sperrgebiet that was formed in a small basin cutting into the dolomites of the Proterozoic Gariep Group.[1] The top of the formation is formed by an erosional unconformity at the base of the Late Oligocene to Early Miocene Blaubok Conglomerate. The fauna from the Black Crow Limestone, especially the arsinoithere Namatherium blackcrowense and the reithroparamyid rodent Namaparamys inexpectatus indicate a Late Ypresian or Early Lutetian age for the deposits. The limestones are likely to be older than 42.5 Ma on the basis of radio-isotopic dates obtained from phonolite cobbles reworked from lavas considered to have erupted later than the limestone deposition. The carbonates could be as old as 47 ± 1 Ma, i.e. Late Ypresian to Early Lutetian.[3]

Abundant pedotubules in the formation suggest accumulation in a swampy setting. There is a 20 centimetres (7.9 in) thick bed of carbonatite breccia intercalated in the fossiliferous limestone which indicates that carbonate deposition occurred contemporaneously with volcanic activity at the Ystervark Carbonatite Centre 15 kilometres (9.3 mi) to the east of Black Crow,[4] and other volcanoes in the region, which periodically injected vast quantities of carbonate into the sub-aerial terrestrial ecosystem.[5]

Fossil content edit

Various fossils have been recovered from the formation. The fossil land snails from the Black Crow Limestone, even though they are not very diverse, show biogeographic affinities with present-day southwestern Africa (Western Cape in South Africa and Western Namibia) and they suggest that at the time of deposition, the region lay within a zone of summer rainfall rather than winter rainfall.[6] The paleoclimate has been interpreted as hot and humid, contrasting with the arid desert of today.[7]

The following fossils are reported from the formation:[8][9]

Mammals
Amphibians
Reptiles
Birds - indeterminate post-cranial elements
Fish
Snails

See also edit

References edit

  1. ^ a b Pickford, 2018e, p.81
  2. ^ Pickford, 2015, p.107
  3. ^ Pickford, 2018d, p.64
  4. ^ Pickford, 2015, p.105
  5. ^ a b c d e f Morales & Pickford, 2018, p.72
  6. ^ Pickford, 2018a, p.19
  7. ^ Dauteuil et al., 2018, p.6
  8. ^ Mein & Pickford, 2018, p.39
  9. ^ Black Crow at Fossilworks.org
  10. ^ Pickford, 2015, p.109
  11. ^ Pickford, 2018e, p.83
  12. ^ Morales & Pickford, 2018, p.75
  13. ^ Mein & Pickford, 2018, p.41
  14. ^ Pickford, 2018d, p.66
  15. ^ a b Pickford, 2018b, p.32
  16. ^ Pickford, 2018b, p.30
  17. ^ Pickford, 2018b, p.28
  18. ^ Pickford, 2018a, p.21
  19. ^ Pickford, 2018a, p.20

Bibliography edit

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