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1,700,000,000 BC

1,700,000,000 BC

in

Oklo, Gabon. A total of 17 natural nuclear reactors are igniting. Nuclear waste of the same type and percentage as modern nuclear reactors is evident: the dreaded plutonium-239, which in its decay process generates a whole series of fission byproducts found precisely (within 1 ppm)

2,200,000,000 BC

2,200,000,000 BC

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Snowball Earth, also known as Makganyene, was an ice age of enormous proportions, probably the most extreme ever to occur on Earth. Average temperatures dropped by 45°C, and perhaps the entire planet became a vast ice sheet, reaching the equator. The oceans froze for 800

3,500,000,000 BC

3,500,000,000 BC

in

Stromatolites (Bindstone) are becoming widespread: finely laminated sedimentary structures belonging to the group of non-particulate, bioconstructed limestones, resulting from the activity of benthic photosynthetic microorganisms such as prokaryotes (e.g., cyanobacteria) and even microscopic eukaryotic algae. They form through periodic entrapment of very fine particulate sediment,

3,750,000,000 BC

3,750,000,000 BC

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Formation of sedimentary rocks in present-day western Greenland. Examined by Shidlowski in 1988 AD, they showed increased values of the isotope 12C, suggesting a probable organic origin, for example, due to photosynthesis.

3,800,000,000 BC

3,800,000,000 BC

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Bacteria are differentiated from Archaea, both single-celled organisms without a nucleus (later the Eucharia, or eukaryotes, or single- or multicellular organisms with a nucleus will differentiate from Bacteria)

3,850,000,000 BC

3,850,000,000 BC

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A meteorite the size of Rhode Island crashes into the Moon and creates Mare Imbrium, the largest crater on the Moon’s near side (NW side); the impact distributes radioactive thorium over a large area of the Moon’s near side; this area will turn out to

4.8 – 3.8 billion BC

4.8 – 3.8 billion BC

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Early Heavy Bombardment. The continuous migration of the outer giant planets of the Solar System causes an intense meteor shower on the inner planets. This phenomenon particularly affects Earth, occasionally leading to the partial or complete melting of the Earth’s crust, compromising the possible early

4,200,000,000 BC

4,200,000,000 BC

in

Latest evidence for a rotating magnetic (ferrous) core on the Moon. The experimental evidence comes from lunar samples made available by the Apollo missions, unshocked by impacts (which could also be the source of the magnetic field).

4,450,000,000 BC

4,450,000,000 BC

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After the impact, the Earth’s core reaches temperatures of 4000-7000C; the planet’s heat retention capacity is so good that it is estimated that in the following 4 billion years the core cooled by only 110C.

4,500,000,000 BC

4,500,000,000 BC

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The density of energy and other forms of matter falls below that of vacuum energy. The Universe continues to accelerate its expansion. It is 73% of its current size (4.5 billion years later).

4,700,000,000 BC

4,700,000,000 BC

in

Orion Arm, Milky Way. The supersonic wave from a supernova passes through a flattened cloud of cosmic dust, approximately 20 billion kilometers in diameter, likely the remnants of two extinct stars. The dust mixes with particles from the supernova, and the whole thing begins to