Fig Tree Formation

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.[1] Identified organisms include the bacterium Eobacterium isolatus 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.[2]

Fig Tree Formation Stratigraphic range: Paleoarchean ~3260 Ma Pha. Proterozoic Archean Had'n ↓
Type	Geological formation
Unit of	Barberton Supergroup
Underlies	Moodies Group
Overlies	Onverwacht Group
Lithology
Primary	Sandstone
Other	Shale
Location
Location	Kaapvaal Craton
Coordinates	25.8°S 31.0°E
Region	Barberton Greenstone Belt, Mpumalanga
Country	South Africa
Location of the Barberton Greenstone Belt

See also

• Archean life in the Barberton Greenstone Belt
• Warrawoona Group

References

1. 2015 - Brown - Exploring the Evolution of Oxygen on the Early Earth: Constraining the Evolution of Oxidative Phosphorylation Through the Utilization of Uranium Isotopes
2. Barberton geological field mapping report 2012

Further reading

• "Fig Tree microfossils". Encyclopædia Britannica Online. Encyclopædia Britannica Inc. 2016. Retrieved Oct 9, 2016.
• 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.