Stromatolites are biologically produced structures
formed by colonies of photosynthesizing cyanobacteria. Their building
communities include oldest known fossils, dating back some 3.5 billion
years-old. Stromatolites are unique trace fossils that record both the effect
of microbes in the local environment and the effect of environmental influences
on microbial ecosystems.
Stromatolite is derived from Greek word means “Stony
Carpet”. Today stromatolites are nearly extinct in marine environments, living
a precarious existence in only few localities worldwide.
Formation:
They can form inorganically when seawaters are
oversaturated with chemical precipitates. The four most widely cites paths are
as follows for the formation of stromatolites.
- · Trapping model
- · Precipitating model
- · Stabilizing model
- · Calcifying model
In short process of formation can described as:
During Precambrian times, bacterial mats formed
extensive platforms for trapping and cementing sediments. For photosynthetic
bacteria depletion of CO2 in surrounding water could cause
precipitation of Calcium Carbonate. This Calcium Carbonate precipitation adding
to grains of sediments together formed stromatolitec layers that grow one upon
another with the living bacterial colonies occupying the upper most layers.
Below is the layered stromatolite formed from the activity of ancient
cyanobacteria.
Conclusion:
Stromatolites are fossil evidence of prokaryotic
life that remains today. They maintain and recycle the atomic ingredients upon
which proteins that “are” all life are made, including oxygen, nitrogen and
carbon.
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