Лим Ворд - Библия Времени. Найди свое

Volcanoes gradually increase the level of carbon dioxide and methane. A new perturbation is being prepared. For a thousand years, significant areas are freed of ice, and the planet’s climate, on the whole, returns to the norm known to us.

The second option, explaining the presence of signs of ancient glaciers in the equatorial regions of the planet – a fairly rapid turn of the poles of the Earth, followed (300 million years) by their return to the site.

Somehow, sea sponges appear, that is, aquatic multicellular animals that lead an attached lifestyle, as well as mushrooms, essence, eukaryotic communities that combine the signs of plants and animals. As a result of their vital activity, soil appears.

The single continent of Rodinia splits into two parts, which diverge to the poles. The northern half is Laurasia, the southern half is Gondwana.

The sun, meanwhile, increases luminosity by 12%. The Age of Precambrian or Cryptozoic, the «Hidden Life», (sometimes called the eons of Archean and the Proterozoic together) ends.

Multicellular creatures, animals, higher plants, are 580 million years ago, thus assuming the onset of the turbulent Phanerozoic («clear life») eon – in which we live, too. His first era – Paleozoic («ancient life»). It is divided into six periods: Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. They last for 20 to 60 million years.

Galaxy the Milky Way. Reconstruction

continent of Rodinia

Laurasia and Gondwana

Trilobite

Ammonite

Stegotsefal

Meganevra (reconstruction)

Shellfish

Seismosaurus

Ankylosaurus, recognized symbol of the Mesozoic era

Pteranodone

Representative of the order Mesonihia, the ancestor of whales, according to the theory of Darwin

Evolution of the continents; from Laurasia, Gondwana and Pangea to the modern form

Mastodon

The Modern Earth. A photo from the Apollo-17, 1 hour 54 minutes after reaching the flight path to the Moon (1972)

In the Cambrian organisms, first of all, learn to build strong skeletons, according to which they are detected by paleontologists. The star of this period is trilobite, a pretty pretty arthropod, a prototype of modern cancer. There are also those that, with some stretch, can be classified as cephalopods – reminiscent of octopuses and squid. Their flowering falls on the Ordovician. The Silurian, which lasts «only» 25 million years, is marked by two mass extinctions (up to 50% of the marine life). One of them, which occurred 443 million years ago, the so-called. Ordovician-Silurian is probably due to the movement of Gondwana to the South Pole, as well as a sharp drop in the ocean level. Especially got, already was prosperous brachiopods (something like oysters), bivalve molluscs, bryozoans (colonies of small worms) and corals. The Devonian period is characterized by terrestrial vertebrates, famous brush-trotter fish, insects, as well as gymnosperms («bare» seeds hide in cones), fern-like and horsetail. Racoscorpions and fish appear. Trilobites, on the contrary, with such an abundance of predators, are rapidly dying out. However, the massive sea at the end of the Devonian, affects more than half of the entire marine life and flora; the reason for this, perhaps – the notorious comet.

A fairly long (60 million years) Carboniferous period, or carbon begins 359 million years ago, it is characterized, as the name implies, by intense coal formation. The gymnosperms are developing and thriving: coniferous, cordaite (trees resembling these very conifers), and cicadassia (a cross between palm and fern), mussels and horsetails. In warm bogs amphibians prosper (stegocephalus, they are labyrinthodontes resembling crocodile-newt), ripidity (even larger, 8-meter crocodile), in the seas – sharks reaching 13 meters in length. In the air hover mega-moves – dragonflies with a wingspan of up to 65 cm. This air itself is characterized by an elevated – up to 35%, oxygen content (now 21%).

In the Perm period (Perm, the name of the Russian city in the vicinity of which this stage is allocated) the continents unite again, somewhat differently, forming a single Pangea – washed by the unified world ocean of the Pantalassa. Later, in the Jurassic period of the next era, it will split into six continents known to us. This geological process is characterized by a decrease in the area of inland water bodies, the onset of deserts. Sandy barkhans cover almost the entire territory of present-day Siberia. Carboniferous deposits (coal) overlap with Triassic (motley sandstone, shell limestone).

The successes of the speciation of Perm are rather modest – several new species of insects. The period ends with the largest in the history of the Earth, the Permian-Triassic extinction (English The Great Dying), 252 million years ago. In less than 60 thousand years, 96% of marine species, 70% of terrestrial vertebrates and 83% of the whole class of insects perish. The main hypotheses of the causes of the event: 1 – the fall of an asteroid a few tens of kilometers in diameter. The crater near Wilkes land (Antarctica, a site with a 300 km ring anomaly opposite Australia) seems to confirm this version. 2 – the release of greenhouse gas from, until the rest at the bottom, at the earth’s poles, frozen methane hydrates. In this case, the world ocean boils, permeated with bubbles, like champagne, freed from cork, giving out about 4 trillion tons of methane to the atmosphere in less than a period of ordinary human life. The weather is going crazy, sharp (more than 6Сº per year) warming is replaced by cold snaps, and this is completely out of the question for all the inhabitants of the planet. 3 – anoxia (suffocation). The waters of the oceans, seas, lakes come into contact with hydrogen sulfide (H2S), hydrogen chloride (HCl), volcanos suddenly released into the atmosphere (including so-called Siberian traps, flooding huge areas of hot lava), acidify, lose oxygen. The remains of animals also give off the notorious H2S, which aggravates the tragedy that is taking place.