Molteno Formation

From Wikipedia, the free encyclopedia
Stratigraphy of the Karoo Supergroup in the Karoo Basin
Period Group Formation west of 24°E Formation east of 24°E Assemblage Zone
Jurassic Drakensberg Hiatus Drakensberg
Stormberg Clarens
Triassic Elliot
Molteno
Beaufort
Burgersdorp Cynognathus
Katberg Lystrosaurus
Balfour
Permian Dicynodon
Teekloof
Cistecephalus
Middleton
Tropidostoma
Pristerognathus
Abrahams-Kraal Koonap
Tapinocephalus
Eodicynodon
Ecca Waterford Waterford
Tierberg / Fort Brown Fort Brown
Laingsburg / Ripon Ripon
Collingham Collingham
White Hill White Hill
Prince Albert Prince Albert
Carboniferous Dwyka Elandsvlei Elandsvlei
References: Rubidge (2005),[1] Selden and Nudds (2011).[2]

The Molteno Formation is a palaeontological formation of the Stormberg Group, located in the main Karoo (Gondwana) Basin, South Africa.

It dates to the Upper Triassic (Carnian) period and is rich in fossils.

Formation

Formed from river sands when the region's climate was still wet, this layer represents the first stage of the gradual desertification that is recorded in the sediments of the Stormberg Group - from the Triassic period, through the Jurassic, as the Gondwana supercontinent moved slowly northwards.

This sandstone is now exposed as cliffs in the Drakensberg and can be easily recognised by its sparkling appearance (this is due to tiny quartz crystals that bind the sand grains together). Dolorite intrusives are also common. Rocks of this formation provide a unique window into the time of the origin of the dinosaurs, mammals, and possibly also of flowering plants.

Flora and Fauna

Reconstruction of the vegetation of Molteno formation. Kirstenbosch Botanical Gardens.

The Molteno Biome, as the reconstructed community of flora and fauna is known, showed an unusually large biodiversity at class and order level, especially in insects and gymnosperms (which reached their heyday during this period). Other especially common flora were species of fern, horsetail and cycad.

Much of the region, at the time, fell within an enormous network of inland river deltas. To date, seven primary habitat types (or ecozones) have been identified, each with their own large assemblage of species:

  • Dicroidium riparian forest (types 1 & 2)
  • Dicroidium woodland
  • Sphernobaiera woodland
  • Heidiphyllum thicket
  • Equisetum marsh
  • Fern & Gingkophytopsis meadow[3]

Location

The rock formation stretches in a broad band, from the Eastern Cape, through Lesotho and the Orange Free-State in South Africa. It is named after the town of Molteno in the Stormberg Mountains of the Eastern Cape.

Due to the lush vegetation of the Triassic river deltas, this is today the coal-bearing horizon of the Eastern Cape, with four main coal seams: Indwe, Guba, Molteno and Gubenxa.


See also

Wikimedia Commons has media related to Molteno formation.

References

  1. ↑ Rubidge, B.S. (2005). "Re-uniting lost continents – Fossil reptiles from the ancient Karoo and their wanderlust". South African Journal of Geology 108 (1): 135–172. doi:10.2113/108.1.135. 
  2. ↑ Selden, P.; and Nudds, J. (2011). "Karoo". Evolution of Fossil Ecosystems (2 ed.). Manson Publishing. pp. 104–122. ISBN 9781840761603. 
  3. ↑ JM Anderson: Gondwana Alive. National Botanical Institute. Pretoria: 2001. p.74.
  • Vickers-Rich, Patricia & Rich, Thomas Hewett (1993); Wildlife of Gondwana. Reed. ISBN 0-7301-0315-3


This article is issued from Wikipedia. The text is available under the Creative Commons Attribution/Share Alike; additional terms may apply for the media files.