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CHRONOLOGY OF WORLD HISTORY |
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CHRONOLOGY OF WORLD HISTORY |
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This work is dedicated to the laborers, artisans, agricultural workers, and craftsmen, as well as the countless unnamed innovators and inventors, whose tireless efforts and sacrifices have shaped civilizations, even if their names are not recorded in history books.
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-Rabi Roy
Jawaharlal Nehru's significant book 'Glimpses of World History' has motivated me to create this comprehensive record of world events, spanning from ancient times to the present day, based on insights collected from the works of various authors. -The Blogger
Difference between Earth and World in the English language: The terms "earth" and "world" have
distinct meanings in the English language. "Earth" refers to the physical planet we inhabit, while "world" can denote a broader range of concepts, including other planets, human society, and even the universe. The distinction is important as it affects how the terms are used in various contexts, from geography to philosophy and literature. In this document, we have used the word ‘WORLD’ in a broader range of concepts.
Volume 1 π° Chapter 1
Let us start from universe.
Γ
Q. What is the Big Bang Theory?
A. The Big Bang Theory is the leading scientific explanation for the origin of the universe, proposing that it began as an extremely hot and dense point approximately 13.8 billion years ago and has been expanding ever since.
The Big Bang Theory
The most prominent scientific theory about the origin of the Earth involves a spinning cloud of dust called a solar nebula. This nebula is a product of the Big Bang. Philosophers, religious scholars and scientists have lots of ideas about where the universe came from (those thoughts may be discussed separately later on), but the most widely held scientific theory is the Big Bang Theory. According to this theory, the universe originated in an enormous explosion.
Before the Big Bang, all of the matter and energy now in the universe was contained in a singularity. A singularity is a point with an extremely high temperature and infinite density. It's also what's found at the center of a black hole. This singularity floated in a complete vacuum until it exploded, flinging gas and energy in all directions. Imagine a bomb going off inside an egg -- matter moved in all directions at high speeds.
As the gas from the explosion cooled, various physical forces caused particles to stick together. As they continued to cool, they slowed down and became more organized, eventually growing into stars. This process took about a billion years.
About five billion years ago, some of this gas and matter became our sun. At first, it was a hot, spinning cloud of gas that also included heavier elements. As the cloud spun, it collected into a disc called a solar nebula. Our planet and others probably formed inside this disc. The center of the cloud continued to condense, eventually igniting and becoming a sun.
There's no concrete evidence for exactly how the Earth formed within this nebula. Scientists have two main theories. Both involve accretion, or the sticking together of molecules and particles. They have the same basic idea -- about 4.6 billion years ago, the Earth formed as particles collected within a giant disc of gas orbiting what would become our sun. Once the sun ignited, it blew all of the extra particles away, leaving the solar system as we know it. Our moon formed in the solar nebula as well -- read "Where Did the Moon Come From?" to learn more.
At first, the Earth was very hot and volcanic. A solid crust formed as the planet cooled, and impacts from asteroids and other debris caused lots of craters. As the planet continued to cool, water filled the basins that had formed in the surface, creating oceans.
Through earthquakes, volcanic eruptions and other factors, the Earth's surface eventually reached the shape that we know today. Its mass provides the gravity that holds everything together and its surface provides a place for us to live. But the whole process would not have started without the sun.
Read it: https://en.wikipedia.org/wiki/Big_Bang
π c. 6,000,000,000: The estimated age of the Solar
System (variously
estimated as 4,700,000,000 to
6,500,000,000)[3]
Details of the Planets' names in our Solar System:
1. Mercury
1.
Planet Mercury is the closest planet to the Sun in our Solar
system. Its size is also the smallest among all other planets.
2. Venus
3. Earth
Read in detail: When Earth evolved, it did not have the life-supporting oxygen that we breathe today. Researchers have now identified the conditions on the planet before the evolution of oxygen by using rock fossils.
"Fossils are like time capsules, preserving life's story in stone," said Richard Fortey, a British palaeontologist, geologist, and writer.
Researchers analysed stromatolites, layered rock-like formations made by Cyanobacteria (one of the oldest bacteria). They hold ancient records from two-and-a-half billion years ago.
HOW NITROGEN HELPED EARTH
The team analyzed nitrogen cycling patterns within ancient stromatolites, preserved in southern Zimbabwe.
Nitrogen, which is vital for life on Earth, must be converted into usable, bio-available, forms as it passes through the atmosphere, soil, plants, and animals in the nitrogen cycle.
Nitrogen cycling patterns were chosen as they can help in finding the Earth's condition before the evolution of oxygen and the beginning of photosynthesis. This method of research is also less explored when compared to oxygen evolution and its impact.
Dr. Ashley Martin from the Department of Geography and Environmental Sciences at Northumbria University said that nitrogen and phosphorus are the two key nutrients that control productivity in the oceans over periods.
Dr. Martin added a note on the importance of ammonium for the biological process, and mentioned the presence of a high amount of nitrogen deep inside the ocean in the form of ammonium.
This ammonium reservoir would have been very beneficial for early life, providing the nitrogen source needed for biological processes to occur.
As early oceans had very little oxygen, they were influenced by volcanic activities. This in turn helped in the growth of microbes which acted as pioneers in the evolution of oxygen.
"We have long been puzzled by the unusual nitrogen isotope values in these rocks. "Our new findings suggest a strong linkage to hydrothermal nutrient recycling, meaning that early life may in part have been fuelled by volcanic activity," Dr Eva Stueken from the University of St Andrews explained.
The study published in Nature Communications highlights the role of the volcano, which had a lasting impact on the evolution of life at that time.
4. Mars
5. Jupiter
6. Saturn
7.
Uranus
8.
Neptune
Source: https://onlymyenglish.com/planets-name-in-english/
§ Pluto is a
dwarf planet[4]
located in the Kuiper Belt, a region of icy bodies beyond Neptune's orbit.
Discovered in 1930, Pluto was initially classified as the ninth planet in our
solar system but was redefined as a dwarf planet by the International
Astronomical Union in 2006. It is characterized by its small size, irregular
orbit, and diverse geological features, including mountains, valleys, and
glaciers.
π c. 440,000,000: Silurian Age: vertebrate
animals developed; large sea scorpions; first land plants (leafless) appeared.
π c. 395,000,000: Devonian
Age: active volcanoes formed mountains; osteichthyes[8],
bony fishes existed; leafy land plants and trees developed; wingless creatures
left the sea and came ashore; period of old red sandstone.
π c. 340,000,000: Carboniferous
Age: giant trees yielding our coal; development of amphibian reptiles;
legs first appeared.
c. 225,000,000: First evolution of the dinosaurs c. 65,000,000: Disappearance of dinosaurs |
π 275,000,000: Permian Age: rapid development of land life gradually dominated life in the sea, but still mainly reptilian.
π c. 225,000,000: Triassic
Age: development of ichthyosaurus and crustacean ancestors; first
evolution of the dinosaurs, two
distinct orders (Saurischia and Ornithischia); originally these creatures were
bipedal, but later often became quadrupedal. Winged insects and small
mammals were present; palm ferns were also visible.
π c. 195,000,000: Jurassic
Age[9]: a
period of limestone formation; great increase in size of dinosaurs---principal
age of the great reptiles; first bird, archaeopteryx having teeth and reptilian
characteristics; ammonites in the sea.
π c. 140,000,000: Australia
severed from land-mass Asia: cause of continued existence of primitive
animal life on the continent.
A. According to the Cambridge dictionary, a continent is defined as “one of the seven large land masses on the earth's surface, surrounded, or mainly surrounded, by sea, and usually consisting of various countries”.
π c. 136,000,000: Cretaceous
Age: chalk foundations laid; great areas of swamp bordered the seas;
terrible and fantastic lizards developed, including pterodactyls; earliest
beginnings of warm-blooded mammals.
π c. 65,000,000: Eocene
Age: the disappearance of dinosaurs and marine reptiles; rapid
development of mammals; early on, dinotherium, mastodon and saber-toothed
tiger.
Q. When did man first find out about dinosaurs?
A. No human being has ever met a dinosaur alive. Dinosaurs were animals that inhabited most parts of the world, but they died everywhere about 6,500,000 years ago. Dinosaurs were extinct when humans came into the world.
Dinosaurs are known to us because of their remains. These are bones, found in skeletons or separately; footprints in the rock; skin-prints, also in the rock; and eggs.
There is some doubt as to when the first recognizable dinosaur bones were discovered. Footprints have been known for many years. A dinosaur skeleton may have been seen at Haddonfield, New Jersey, toward the end of the 1770s.
The first bones that are still available for examination and identification are some that were discovered in England. One set was found in 1822 and is now in the British Museum of Natural History in London.
Another set of dinosaur bones found about the same time was the basis for the first scientific description of any dinosaur. This was done in 1824 by a professor at Oxford University.
So it appears that human knowledge of dinosaurs is quite recent.
Dinosaur specimens have been found in great numbers in the United States, Canada, Argentina, Brazil, India, Africa, Australia, Mongolia, China, France, Germany, Portugal and the Soviet Union (which no longer exists in the 20th century). This indicates that dinosaurs really lived all over the world. - 16/11/2022
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π c. 38,000,000: Oligocene
Age: extension of land masses; monkeys and apes existed.
Q. What is the difference between monkeys and apes?
By Alison Eldridge
Monkeys and apes are both primates, which mean they’re both parts of the human family tree. As distinguished relatives, we should probably be able to tell them apart. But when you look at a gibbon or a marmoset, how do you know which is a monkey and which is an ape?
The quickest way to tell the difference between a monkey and an ape is by the presence or absence of a tail. Almost all monkeys have tails; apes do not. Their bodies are different in other ways too: monkeys are generally smaller and narrow-chested, while apes are larger and have broad chests and shoulder joints that allow them to swing through trees (while some monkeys also have this ability, most of them are built for running across branches rather than swinging). Although you can’t recognize this difference on sight, apes have an appendix and monkeys do not. Apes are generally more intelligent than monkeys, and most species of apes exhibit some use of tools. While both monkeys and apes can use sounds and gestures to communicate, apes have demonstrated higher ability with language, and some individual apes have been trained to learn human sign languages.
However, perhaps the best way to remember, like with so many things, is rote memorization. There are only a handful of ape species, while there are hundreds of species of monkeys. If the primate you’re trying to place is not a human, gibbon, chimpanzee, bonobo, orangutan, or gorilla (or a lemur, loris, or tarsier), then it’s a monkey.
***
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The compiler of this documentation, Rabi Roy,
is grateful to his friend Late Swapan Chakraborty, a footpath bookseller
in Kolkata, India, and a thinker as well, for his contribution to this part of
the book.
[1]Pre-history means literally “before
history”, from the Latin word for “before,” prΓ¦,
and Greek ΞΉΟΟΞΏΟΞ―Ξ±.
[2] The Neolithic Revolution, also known as the Agricultural Revolution,
refers to the significant transition in human history from nomadic
hunter-gatherer societies to settled agricultural communities. This period
marked the development of farming, the domestication of animals, and the
establishment of permanent settlements, which allowed for larger populations
and the rise of early civilizations. It is considered a pivotal moment in human
history, occurring around 12,000 years ago.
[3] The
Solar System: The collection of eight planets and their moons in orbit
round the sun, together with smaller bodies in the form of asteroids,
meteoroids, and comets. The major
planets of the solar system are (in order of distance from the sun) Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune. Pluto, which is very much known as ninth planet, is a
dwarf planet.
[6] Trilobites
are extinct fossil arthropods that first appeared around 521 million years ago
during the Cambrian Period. They are easily recognized by their distinctive
three-lobed, three-segmented form. Trilobites were exclusively marine animals
and are known from more than 10,000 fossil species. They were arthropods,
divided into three parts from head to tail and from side to side. Trilobites
were abundant during the Cambrian and Ordovician periods but eventually went
extinct. -Britannica
[7] Sponges
are primitive multicellular aquatic animals that constitute the phylum
Porifera. They are permanently affixed (sessile), mostly marine, solitary or
colonial invertebrates. Sponges have bodies full of pores and channels allowing
water to circulate through them. They consist of jelly-like mesohyl sandwiched
between two thin layers of cells. The mesohyl contains embedded amoeboid cells
that secrete tiny needles called spicules or protein fibers that help give the
sponge its structural strength. -Britannica
[8] Osteichthyes
refers to a class of vertebrates known as bony fish, characterized by an
endoskeleton primarily composed of bone tissue. This class includes over 30,000
species, making it the largest class of vertebrates. Key features of
Osteichthyes include a skeletal endoskeleton, gill covers (operculum), and, in
most cases, paired fins.
[9] The Jurassic Age, spanning
from approximately 201.3 million to 145
million years ago, was a significant period in Earth's history marked by
the dominance of dinosaurs and major geological changes. The Jurassic Period is
part of the Mesozoic Era and is divided into three epochs: Early Jurassic
(201.3 to 174.1 million years ago), Middle Jurassic (174.1 to 163.5 million
years ago), and Late Jurassic (163.5 to 145 million years ago). -Britannica