Stromatolites
What are Stromatolites?
Stromatolites are between the world’s most former fossils, approximately of which are above 3.5 billion years old. Stromatolites are structures organized by huge colonies of cyanobacteria, once called blue green algae, which added directly to the formation of the Earth’s atmosphere and its currently livable state. Stromatolites are organized by prokaryotic cyanobacteria, which have cells inadequate a definite nucleus. The photosynthesizing powerhouses can be determined in fossilized form all over the world, indicating that they played a tremendous role in making the Earth a hospitable situation for other forms of life.
Stromatolites were called “living rocks” by individuals before their demand makeup was understood, and they do correspond rocks, growing to well over three feet (one meter) high and being almost as wide. From a distance, a colony of stromatolites can look like a series of boulders scattered across the beach. The cyanobacteria which dominate stromatolites process many of the piece of life, including oxygen, carbon, and nitrogen.
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