200,000 BC – 12,700 BC
Collective learning is another impetus for the decrease in local entropy, at the expense of a huge increase in total entropy, of course.
250,000 BC
In Java, Indonesia, Anthropitecus erectus, later popularized as Java Man and today known as Homo Erectus, spreads
500,000 BC approx.
More recent mitochondrial DNA (mDNA) shared by Homo sapiens and Neanderthals. This is DNA passed down from generation to generation, almost identically, from mother to daughter.
900,000 – 783,000 BC
Ancient humanity was nearly wiped out around 900,000 years ago, when the global population shrank to approximately 1,280 reproducing individuals. Furthermore, the population of early human ancestors remained this small for approximately 117,000 years. The statistical method used genetic information from 3,154 living human genomes.
1,000,000 BC
Supernova RX J185635-3754 explodes, creating a neutron star 100,000 billion times denser than steel, which is traveling toward Earth at a speed of 100 km/s and will reach it in 300,000 AD, passing 170 light-years away; it is the closest neutron star ever observed (discovered
1,500,000 BC
First possible evidence of Homo erectus’s use and control of fire. This allowed them to occupy part of Europe.
1,700,000 BC
Kenya. KNM-ER 1808 is the paleonanthropological code name for a woman who lived 1.7 million years ago, whose skeleton was discovered by Kenyan anthropologist Kamoya Kimeu in 1974 at the Koobi Fora archaeological site in Kenya. She is a female Homo erectus with bone deformities
2,500,000 BC
The first stone tools were used to open the bones of animal carcasses and eat the marrow. The genus Homo is therefore low in the predatory hierarchy, able to access the carcass only after large predators, hyenas, and vultures.
2,700,000 BC
First ice in the Arctic: it is formed thanks to a change in the inclination of the Earth’s axis and a simultaneous increase in humidity (which causes intense snowfalls) due to the stratification (caused by the reduction of marine recirculation) of the waters of the
2,800,000 BC
The appearance of a supernova in the sky causes serious consequences, first of all probably a notable reduction of the ozone layer, especially at latitudes above 30 degrees.
10,000,000 BC
Following the upheaval of the Northeastern Andes, which interrupted the connection between the internal sea in the current Amazon rainforest and the Caribbean Sea, the Amazon River was born, draining the remaining lakes within.
12,000,000 BC
When the African and European continental plates collided, they not only raised new mountains in central Europe, but also created the largest lake the world has ever known. This vast body of water, the Paratethys Sea, is home to species found nowhere else, including the
15,000,000 BC
The upheaval of the Northeastern Andes severed the connection between the inland sea in the current Amazon rainforest and the Caribbean Sea; this triggered the birth of the Amazon River.
25,000,000 BC
Thirty million years ago, one of the first hominid species, Nsungwepithecus, developed in Europe. In Africa (Tanzania), the first hominid species (Rukwapithecus, which would give rise to orangutans, gorillas, chimpanzees, and humans) developed only five million years later. Hominids in Africa failed to compete with
25,000,000 BC
The first honeybees, or Apis, evolved. They are a type of vegetarian wasp.
34,000,000 BC
Europe. A dramatic change: the Great Cut. The Eocene, with its tropical climate, ends and the Oligocene, with its continental and Arctic climate, begins. The cause appears to be the detachment of South America from West Antarctica, which drastically altered ocean currents. Temperatures in England
34,000,000 BC
First whales. They evolved from what would later become dolphins, a species that (re)entered the seas about 49 million years ago.
35 – 12 million years BC
Between Greenland and Norway rises an island 500 km long north-south and 15 km wide, of marshy nature, covered with conifers and ferns. No mammals have been found, which probably never arrived here; it now lies 2 km beneath the waves in the middle of
40,000,000 BC
Rodents and monkeys arrived in South America, likely from neighboring (but not adjacent) Africa. How they got there is still unclear, but they probably migrated gradually from one island to another.
49,000,000 BC
branching off between the species that would later become dolphins, in the sea, and the one that remained on land, which would give rise to, for example, hippos. 15 million years later, whales would also branch off.
50,000,000 BC
Early Eocene. Palm trees grow in the Antarctic, crocodiles splash around in the shallows of England. The climate is significantly warmer than today. This shows that a very warm climate doesn’t necessarily mean problems for life. On the contrary, it could mean more species living
50,000,000 BC
Cava della Pesciara, Verona, Italy. An exceptional fossil deposit forms here, demonstrating how modern corals evolved in the Tethys Sea, between Europe and Africa.
55,000,000 BC
At the end of the Paleocene, Uintatherium, a huge rhinoceros-like mammal with six rounded horns, thrived.
56,000,000 BC
Paleocene-Eocene Thermal Maximum (PETM): At the North Pole, summer temperatures reached 23 degrees Celsius, and ocean levels were 70 meters higher than today. Plankton shells disappeared from the mud on the seafloor, which turned from white to red. During the PETM, a mass of carbon
56,000,000 BC
Peak greenhouse effect: This is called the Paleocene-Eocene Thermal Maximum (PETM). A mass of carbon of as yet unknown origin, equivalent to the content of all present-day coal, oil, and gas deposits, invades the atmosphere; the temperature increases by an average of 5°C.
66,036,000 BC
Deccan Traps Episode (Southern India): Massive series of eruptions in a short period of less than a million years, the episode occurs due to the outcrop of a mantle convective cell, which expels enough lava to cover the entire territory of the USA with a
66,036,000 BC
KT + 5 minutes. The tsunami, with waves 300 meters high, reaches the coast. It will cover all of present-day Texas, reaching as far as Oklahoma.
66,036,000 BC
KT + 115 seconds. The 35km-high water column from the Chicxulub meteorite triggers a tsunami with waves 300m high.
66,036,000 BC
KT Episode. The Chicxulub meteorite impact causes 20-meter waves and an earthquake measuring 11-12 on the Richter scale.
66,036,000 BC
KT Episode. Dinosaurs and 85% of species become extinct following a meteorite impact in Chicxulub, Yucatan (early Cenozoic Era); along with the dinosaurs, two-thirds of all living species on the planet become extinct; the 10km meteorite hits at 16km/s at a 30-degree angle toward the
75,000,000 BC (…)
According to Scientology doctrine, the galactic tyrant Xenu kidnaps hundreds of billions of people from other parts of the galaxy and sends them to Earth for extermination. They arrive in spaceships resembling DC-8 jets. They are exposed to thermonuclear explosions and brainwashed with a 36-day
90,000,000 BC
First plants of the Fagaceae family (oaks, chestnuts, beeches, sessile oaks, oaks, cork oaks)
90,000,000 BC
In the Pacific Rim (the ring of fire around the Pacific Ocean), most volcanoes erupt simultaneously; global warming and the resulting acid rain favor the spread of flowering plants (angiosperms).
100,000,000 BC
The Escherichia coli bacterium originates from Salmonella. It is named after the German pediatrician Theodor Escherich. For example, Escherichia coli also lives in our intestines in colonies of one hundred billion individuals.
150,000,000 BC
The oxygen level in the atmosphere drops to 21% (500 million years ago it was 31% which made any fire continuous)
214,000,000 BC
The Monicougan meteorite fell in Quebec, Canada, creating a crater 95 km in diameter.
252,000,000 BC
The Third Mass Extinction occurred at the end of the Permian, 251 million years ago, when 96% of species became extinct. The Second Extinction occurred during the Late Devonian, 375 million years ago, when 75% of living species became extinct. The First Extinction occurred 444
300,000,000 BC
Gondwana joins with North America (part of Laurasia) and forms Pangea
364,000,000 BC
Meteorite falls in Alamo, Nevada (160km crater) and another in Woodleigh, Western Australia (120km crater)
380,000,000 BC
First trees on land: the oxygen content of the atmosphere increases rapidly from 21% to 40%.
400,000,000 BC
The Earth’s year lasts 400 days due to the short length of the day; the discovery was made thanks to the 400 growth sub-rings of Devonian corals
443 – 359 million BC
Prototaxites, a colossal and mysterious life form that dominated terrestrial landscapes for millions of years, long before the advent of trees, thrive on land. From the Late Silurian to the Devonian, these gigantic structures, some reaching over 8 meters in height, formed the first “forests”
444,000,000 BC
The massive spread of plants on land causes global CO2 levels to drop, drastically reducing the greenhouse effect and thus triggering a massive planetary glaciation (snowball) that freezes the megacontinent of Gondwana. Sea levels plummet. The marine ecosystem collapses. 85% of species become completely extinct.
460,000,000 BC
The first jawless fish (Agnathan Ostracodermi). Fish gradually evolved, in the water, to develop various characteristics and behaviors that would later become typical of terrestrial animals: they were gregarious, even among different species; they developed a sense of hearing (experiments on various fish species have
500,000,000 BC
The Earth’s axial tilt decreases from over 50 degrees to 25 degrees; the reason for the sudden drop may be due to the energy released by the resonance between the rotation period of the nucleus (with axis orthogonal to the ecliptic) and the crust (22
500,000,000 BC
The Earth’s day is 22 hours long; the friction exerted by the tides against the continental shelf and the inertia employed by the Earth itself to change shape under the lunar attraction will cause the day to slowly lengthen and the Moon to recede accordingly
500 – 400 million BC
The first big fires begin (only things containing carbon can “burn” since the reaction C + O2 = CO2, so before life there were no big fires apart from lava fires); since the oxygen concentration is 30%, the fires are continuous, that is, everything that
530,000,000 BC
In the shallow waters of Burgess, now British Columbia, Canada, a variety of small animals thrive: Marrella, Yohoia, Opabinia, Burgessia, Nectocaris, Odontogriphus, Dinomischus, Amiskwia, Hallucigenia, Branchiocaris, Canadaspis, Naraoia, Aysheaia, Odaraia, Sydneia, Molaria, Habelia, Sarotrocercus, Actaeus, Alalcomenaens, Emeraldella, Leanchoilia, Sanctacaris, Wilwaxia, Anomalicaris, Peytoia, Eldonia, Banffia, Portalia,
530 – 527 million BC
Thymmothian Period. The name derives from the proto-mollusk Tommotia. The climate is mild, and there are no glaciations. Much of North America was located at tropical and temperate latitudes, which allowed the growth of massive colonies of archaeocyathids in shallow waters. Siberia, also home to
540,000,000 BC
First mollusks; they will soon diversify into gastropods (pointed shells), bivalves (two-part symmetrical shells) and cephalopods (ammonites, nautiluses, squid, octopus, cuttlefish)
635 – 540 million BC
The Ediacaran fauna (Australia) represents a completely distinct experiment in multicellular life, which will ultimately end with the Late Precambrian extinction. These are species that thrive on the seafloor, unrelated to any currently existing species. They are two-dimensional organisms, an alternative solution to the problem
640 million BC
possible “snowball earth” (Marinoan) event, a terrible ice age in which the oceans froze all the way to the tropics. Life likely survived in limited oases such as the Caribbean, the Red Sea, the Persian Gulf, the Eastern Mediterranean, the Amazon, Central Africa, Indonesia, and
680,000,000 BC
Stromatolites declined definitively; a modest recovery occurred only during the Cambrian-Ordovician transition. This decline is attributable to the appearance of the first grazing metazoans and fossa-forming organisms that biodisturbed the texture of the plates. In Italy, they are quite common in the Lower Cambrian formations
1,100,000,000 BC
The supercontinent Rodinia (Greek for “Land of Dawn”) is formed, the next mega-grouping will be Pangea after another 520 million years.
1,100,000,000 BC
The blood globin gene duplicates to form two distinct genes, one to make hemoglobin in vertebrates, and the other to make myoglobin, a protein that works in muscles.
1,200,000,000 BC – 200,000 BC
Multicellular life on Earth. Many experiments, and then dinosaurs dominated the planet for a long time. Then came mammals (a sort of rethinking of nature after the dinosaurs), and finally humans (a freak of nature?).
1,200,000,000 BC
The so-called Cambrian Outburst begins, a sudden enormous diversification of living species
1,300,000,000 BC
According to a study published August 13, 2020, in the journal Physical Review Letters, researchers have improved their estimate of the age of Earth’s solid inner core to between 1 and 1.3 billion years.
1,500,000,000 BC
Eukaryotes (Eucharia) are born, initially unicellular, like amoebas, with a nucleus and various complex organelles



