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Fig Tree Chert Stromatolite South Africa

Fig Tree Chert Stromatolite - South Africa
Fig Tree Chert Stromatolite - South Africa
Item# JPT-21873
Regular price: $220.00
Sale price: $195.00
Availability: Usually ships the next business day

Product Description

Fig Tree Chert Stromatolite - South Africa
What will we find for life on Mars? Something life stromatolites possibly, ancient microbial mats such as this. The Fig Tree Formation is a stromatolite-containing geological formation in South Africa. The rock contains fossils of microscopic life forms about three billion years old. 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.

Size: 60mm H X 60mm W X 20mm D; Ships with information tag and authenticity. Acrylic tag stand included. Stromatolite acrylic display stand base and photo cube not included. Photos of back and front. They can be interchangeable as both sides are interesting.

Additional information: The Swaziland Supergroup of the Barberton Greenstone belt, South Africa, contains some of the oldest-known, least-metamorphosed sedimentary and volcanic rocks on Earth. This early stromatolitic life represent a superbly preserved archive of life for the early earth. Chert is the most abundant sedimentary rock type within the volcanic part of this succession. The Fig Tree Group ranges to about 3.225 Ga and consists of interfingering felsic pyroclastic, orogenic terrigenous clastic, and siliceous, carbonate and baritic chemical deposits. Most Phanerozoic cherts have quartz crystals. The oceans during this time were about 40 degrees centigrade warmer than our present climate. Fossilized bacteria, including cyanobacteria, lie peacefully arranged in smooth layers within the rock. They are commonly low-relief, nearly stratiform, laterally linked domes. Rarer forms include pseudocolumns and crinkly stratiform stromatolites. The stromatolites grew on a substrate of altered komatiitic lava and sediments deposited on the lava surface, and in most places are covered by later komatiitic flows. Some fine-grained tourmaline included within the stromatolite laminae suggests that stromatolites formed in an environment dominated by boron-rich hot-spring emissions and evaporitic brines.

Some of the oldest amino acids known to exist were found in 1968 in the Fig Tree Chert, a formation of Precambrian rock located near Barberton, South Africa. The rocks were dated as being 3.1 billion years old. Older rocks containing fossils have been found since then, but this was the oldest known at the time. The rocks, studied by J. William Schopf and Elso S. Barghoorn of Harvard and Keith A. Kvenovolden of the National Aeronautics and Space Administration (NASA), were known to contain what looked like fossils of algae and bacteria, some of the earliest forms of life. Using a process called chromotography to separate chemicals, the scientists found a series of amino acids. The Fig Tree Chert contained two free and seventeen combined amino acids. There are about twenty natural amino acids, and they link together to form proteins, the essential element of living organisms. Amino acids can form without any living creature making them, and the idea of spontaneously formed life molecules was a hot research topic in the 1960s. Several labs were showing that conditions on the early Earth were just right for forming amino acids.


Click on image to enlarge. Stands and cube not included.

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