Лим Ворд - Библия Времени. Найди свое

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    Библия Времени. Найди свое
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Лим Ворд - Библия Времени. Найди свое краткое содержание

Библия Времени. Найди свое - описание и краткое содержание, автор Лим Ворд, читайте бесплатно онлайн на сайте электронной библиотеки LibKing.Ru
История мира от сотворения Вселенной до наших живых дней на английском и русском языках. Изучаем социальный строй, денежную систему и военную технику. Создаем общее настоящее. Представляем будущее.The history of the world from the creation of the universe to our living days in English and Russian. We study the social system, the monetary system and military equipment. We create a common present. We represent the future.

Библия Времени. Найди свое - читать онлайн бесплатно ознакомительный отрывок

Библия Времени. Найди свое - читать книгу онлайн бесплатно (ознакомительный отрывок), автор Лим Ворд
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The fall (disintegration) of the USSR

The first war in the Persian Gulf 1990—1991.

The first Chechen war of 1994—1996.

The Second Chechen War of 1999—2000 (2009).

Wars of the post-Soviet period outside the Russian Federation

The Civil War in Somalia in 1988…

The war in Yugoslavia, 1991—2001

The Second Iraq War, 2003—2011.

The war in Syria in 2011…

The war in Libya in 2011…

Armed conflict in South Ossetia 2008

Armed conflict in the Donbass in 2014…

Anglo-Scottish armed conflict

Overview of some countries of interest to us

Australia, Armenia, Azerbaijan, Albania

Byelorussia, Vietnam, Germany

Georgia, Denmark, India

Israel, Ireland, Kazakhstan

Kyrgyzstan, Korea North, Korea South

Latvia, Lithuania, Estonia

Poland, RUSSIA, Saudi Arabia

Syria, Tajikistan, Turkmenistan

Turkey, Ukraine, Uzbekistan

Finland, Japan… Norway and Somalia

Book Three

Running in Paradise. The history of a possible future.

Big Bang

The Big Bang is the generally accepted theory of the origin of the universe. Of course, this is an area of scientific legends and fantasies. At first, all that is now in the world (including this light itself, and even, it seems, the very time) was in the so-called proto-Egg – a region of space, about the size of an atom, with a density of 10 to 90 degrees kg / cm³. For unknown reasons, this Egg explodes. At first, one plasma passes into the other, and back with an unthinkable speed, emitting uniformly in all directions of the so-called «plasma». relic shortwave radiation. After 380,000 years, everything is more or less calming down. The first stable hydrogen atoms appear.

After another 400 million years, gas nebulae arise. Thanks to the force of gravitational attraction, the gas concentrates in the stars and, with billions of luminaries, galaxies.

Our Galaxy (with a capital letter), otherwise – the Milky Way (Latin – via lactea) is formed 13 billion years ago, and has 200 to 400 billion stars. The age of the Solar System is 4.5 billion years. It has 8 recognized classical planets, as well as 5 so-called dwarf ones, including now also «expelled» from group «A» Pluto.

Geological Eons

Qatarhei, Archei

Our Earth, according to a widespread theory, originated from a protoplanetary disk, around this time. Strangely enough, the first, primitive forms of life, nuclear-free cells, prokaryotes, appeared almost almost immediately after the termination of the devastating asteroid bombardment (the eon of Qatarhei, 600 million years), as well as education, as a result of a terrible sliding strike on our planet, an object the size of Mars, the future companion of all lovers, the Moon. However, for another long and a half billion years, the stage of development, called Archean, life forms do not develop much. The top of this demiurgic process is unicellular eukaryotes and already relatively complex algae visible to the naked eye.

All these organisms, presumably, have a single, universal common ancestor. The genetic set of all living things on Earth is the same. Their DNA is assembled from four nucleotides (biological molecules) – adenine, guanine, cytosine and thymine.

Proterozoic

Рroterozoic – (other Greek approximately as «earlier life») – the longest geological period, 2 billion years, starts a little more than 2.5 billion years ago. For one reason or another, oxygen accumulates in the atmosphere – and it leads to the extinction of almost all anaerobic creatures. The ozone layer is formed. The next trouble for the already accustomed organisms to new conditions is the great Huronian glaciation (2.4—2.1 billion years ago). Methane combines with oxygen, forms carbon dioxide (which contributes much less to the greenhouse effect), as a result – the Earth turns into a huge «snowball». At the equator, it is almost as cold as in modern Antarctica. Life is preserved in relatively small polynyas and ponds with melt water.

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.

Phanerozoic

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 - фото 2

Galaxy the Milky Way. Reconstruction

continent of Rodinia Laurasia and Gondwana Trilobite - фото 3

continent of Rodinia

Laurasia and Gondwana Trilobite Ammonite - фото 4

Laurasia and Gondwana

Trilobite Ammonite Stegotsefal - фото 5

Trilobite

Ammonite Stegotsefal Meganevra reconstruction - фото 6

Ammonite

Stegotsefal Meganevra reconstruction Shellfish - фото 7

Stegotsefal

Meganevra reconstruction Shellfish Seismosaurus - фото 8

Meganevra (reconstruction)

Shellfish Seismosaurus Ankylosaurus recognized symbol of the Mesozoic era - фото 9

Shellfish

Seismosaurus Ankylosaurus recognized symbol of the Mesozoic era Pteranodone - фото 10

Seismosaurus

Ankylosaurus recognized symbol of the Mesozoic era Pteranodone - фото 11

Ankylosaurus, recognized symbol of the Mesozoic era

Pteranodone Representative of the order Mesonihia the ancestor of whales - фото 12

Pteranodone

Representative of the order Mesonihia the ancestor of whales according to the - фото 13

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 - фото 14

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

Mastodon The Modern Earth A photo from the Apollo17 1 hour 54 minutes after - фото 15

Mastodon

The Modern Earth A photo from the Apollo17 1 hour 54 minutes after reaching - фото 16

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.

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