Fig Tree Formation

Fig Tree Formation
Stratigraphic range: Paleoarchean ~
Type	Geological formation
Unit of	Barberton Supergroup
Underlies	Moodies Group
Overlies	Onverwacht Group
Lithology
Primary	Sandstone
Other	Shale
Location
Location	Kaapvaal craton
Coordinates
Region	Barberton Greenstone Belt, Mpumalanga
Country	South Africa
Location of the Barberton Greenstone Belt

The Fig Tree Formation, also called Fig Tree Group, is a stromatolite-containing geological formation in South Africa. The rock contains fossils of microscopic life forms of about 3.26 billion years old. Identified organisms include the bacterium Eobacterium isolatum and the algae-like Archaeosphaeroides barbertonensis. The fossils in the Fig Tree Formation are considered some of the oldest known organisms on Earth, and provide evidence that life may have existed much earlier than previously thought. The formation is composed of shales, turbiditic greywackes, volcaniclastic sandstones, chert, turbiditic siltstone, conglomerate, breccias, mudstones, and iron-rich shales.

Meteorite Impact

This formation also contains evidence of the biggest known meteorite impact on earth [1].

See also

• Archean life in the Barberton Greenstone Belt
• Warrawoona Group

Further reading

• Byerly G.R., Lower D.R. & Walsh M.M. (1986). Stromatolites from the 3300–3500-Myr Swaziland Supergroup, Barberton Mountain Land, South Africa. Nature, 319: 489–491.