Nama Group Explained

Nama Group
Period:Cambrian
Age:Ediacaran
~
Type:Group
Prilithology:Sandstone
Otherlithology:Siltstone, mudstone, limestone
Unitof:Nama Basin
Subunits:See text
Underlies:Table Mountain Sandstone
Overlies:Basement
Area:125000km2
Map:Damara-Orogen mit Damara-Gürtel, Kaoko-Gürtel und Gariep-Gürtel.png
Paleocoordinates:-41.4°N -179.2°W
Region:Omaheke, Hardap & ǁKaras Regions

The Nama Group is a 125000km2 megaregional Vendian to Cambrian group of stratigraphic sequences deposited in the Nama foreland basin in central and southern Namibia. The Nama Basin is a peripheral foreland basin, and the Nama Group was deposited in two early basins, the Zaris and Witputs, to the north, while the South African Vanrhynsdorp Group was deposited in the southern third.[1] The Nama Group is made of fluvial and shallow-water marine sediments, both siliciclastic and carbonate.[2] La Tinta Group in Argentina is considered equivalent to Nama Group.[3]

Description

The group extends from the Gariep Belt in the south to outcrops of pre-Damara basement in the north.[4] Thrombolite-stromatolite reefs in the Nama Group are best developed in the Kuibis Subgroup of the Zaris subbasin, and in the Huns platform of the Witputs subbasin.[5] The Nama Group is a series of interbedded shallow marine carbonates and siliciclastics deposited in a storm-dominated ramp setting.[6]

"Nama-type preservation" is an Ediacaran type preservation that presents sandstone castings of fossil creatures in which organisms are preserved in three dimensions, within fine-grained beds that were deposited in single storm or mudflow events: an example is Ausia fenestrata. Analysis performed in 2018 on Namacalathus and Cloudina skeletons from the Ediacaran Omkyk Member of the Nama Group demonstrates that both organisms originally produced aragonitic skeletons, which later underwent diagenetic conversion to calcite.[7]

Stratigraphy

The Nama Group is subdivided into:[8]

Subgroup Formation Member
Spitskop
Huns
Niederhagen
Urikos & Hoogland
Omkyk
Kliphoek
Kanies

Ages

The lower and upper part of the Spitskop Member of the Urusis Formation, Schwarzrand Subgroup, had originally been dated on the basis of zircons to 545.1 ± 1 Ma and 543.3 ± 1 Ma respectively. Recalibration of the Spitskop radiometric data indicates revised dates of 542.68 ± 1.25 Ma (terminal Ediacaran) and 540.61 ± 0.67 Ma (within error of the Ediacaran–Cambrian boundary), respectively. An ash bed from the Hoogland Member towards the base of the Nama Group (Zaris Formation, Kuibus Subgroup) has yielded an age of 547.4 ± 0.3 Ma, in 2018 slightly modified to 547.32 ± 0.31 Ma. The lower part of the Nomtsas Formation has yielded an age of 539.4 ± 1 Ma, in the same year recalibrated to 538.18 ± 1.11 Ma.[9]

Fossil content

Nama-type Ediacaran fossils found in the group include:

See also

References

Bibliography

Further reading

Notes and References

  1. Gresse, P. G., G. J. B. Germs. The Nama foreland basin: sedimentation, major unconformity bounded sequences and multisided active margin advance. 1993, Precambrian Research, 63(3-4):247-252, 259-272
  2. Saylor, Beverly Z., John P. Grotzinger, Gerard J. B. Germs. Sequence stratigraphy and sedimentology of the Neoproterozoic Kuibis and Schwarzrand Subgroups (Nama Group), southwestern Namibia. 1995 Precambrian Research 73:153-171.
  3. Iacumin . M. . Piccirillo . E.M. . Girardi . V.A.V. . Teixeira . W.. Bellieni . G. . Echeveste . H.. Fernández . R. . Pinese . J.P.P. . Ribot . A. . 2001 . Early proterozoic calc-alkaline and middle proterozoic tholeiitic Dyke Swarms from Central–Eastern Argentina: petrology, geochemistry, Sr–Nd isotopes and tectonic implications . . 42 . 11 . 2109–2143 . 10.1093/petrology/42.11.2109. free .
  4. Meert et al., 1997, p.639
  5. Grotzinger, 2000, p.252
  6. Wood & Curtis, 2015, p.114
  7. Pruss et al., 2018, p.763
  8. Winterleitner et al., 2015
  9. Buatois et al., 2018
  10. Hahn, G.; Pflug, H. D. (1985). "Polypenartige Organismen aus dem Jung-Präkambrium (Nama-Gruppe) von Namibia". Geologica et Palaeontologica. 19: 1–13
  11. Crimes & Germs, 1982, p.890
  12. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=51737 Reefal biostrome, Kuibis Subgroup
  13. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=51738 Thrombolite Reef, Schwarzrand Subgroup
  14. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=113370 Rietoog, Driedoornvlagte pinnacle reef complex
  15. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=89796 Aar Farm
  16. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=9881 Vendian fauna, Kuibis Formation, - Glaessner 1979
  17. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=89797 Farm Swartpunt
  18. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=10397 Niederhagen Member, Naldaus Fm., - Jenkins 1985
  19. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=6712 Kliphoek Member, Dabis Fm., - Jenkins 1985
  20. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=139601 Farm Swartpunt, Urusis Formation
  21. http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=139838 Sonntagsbrunn Farm, Nomtsas Fm., Valley Fill 2, Visionarium