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Stoneage Human: https://youtu.be/k8910CQVJ3E

First Human Evolution: https://youtu.be/qzQF9xEDo4E

Earth History: https://youtu.be/-CkfOgDy7qI

Evolution of dinosaurs: https://youtu.be/ZfWVOFLnh-c

பூமியை ஆண்ட ராட்சத பூச்சிகள்: https://youtu.be/GQqMz3epdsg

பாம்புகளின் அரசன் Titanoboa: https://youtu.be/52BTYaITaVo

மனிதனின் கடைசி நொடிகளும் மனிதன் இல்லாத பூமியும்: https://youtu.be/AI8ZHdXIKW0

செத்து பொழச்ச பூமி JUST MISS: https://youtu.be/0tD-C4ntMTo

டயனோசர் முடிவுக்கு காரணம் இது தான்: https://youtu.be/VhJKADUhKgA

பூமி மற்றும் மனிதன் உருவான வரலாறு: https://youtu.be/L1H9F_jVki0

Homo erectus lived between 1.9 million and 110,000 years ago, making it one of the longest-surviving human species.

Homo erectus was the first known species to employ complex stone tools, such as the hand axe, which is part of the Acheulean tool history. These tools were more sophisticated than those employed by their ancestors.

Control of Fire: They are thought to have been the first hominins to control and use fire for cooking, protection, and warmth, marking a key stride forward in human evolution.

Homo erectus was the first human species to migrate from Africa. They expanded over Asia (China, Indonesia) and Europe.

Homo erectus likely originated in Africa, as evidenced by the discovery of fossils there. Notably, the Turkana Boy fossil was discovered in East Africa (Kenya).

African Savannah: Homo erectus most likely evolved in savanna habitats in Africa, which were a combination of grasslands and woods, allowing access to a variety of food supplies including game animals and plants.

Homo erectus originated in Africa and gradually expanded to other regions such as Asia (Java, China) and parts of Europe.



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Vaan Veli
Santhosh

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The History of first life on our planet,
The earliest life on Earth is thought to have arisen around 3.5 to 4 billion years ago. The exact timeframe is difficult to pinpoint exactly due to the scarcity of geological and fossil data from that far period. The fossilized remnants of microbes such as bacteria and archaea provide the oldest evidence of life.

These early life forms were single-celled creatures that most likely lived in hydrothermal vents or shallow, warm oceans. The early Earth's atmosphere was significantly different from today's, with high amounts of gases such as methane, ammonia, and water vapor. Life is supposed to have originated when these basic creatures discovered the capacity to gather energy from their surroundings and reproduce.

Earth history, Human history, Earth History in tamil, History of earth, History of our life, Human evoluation

#earthhistory #historyofourearth #humanhistory #humanevolution




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Vaan Veli
Santhosh

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Top Five Extinctions
Ordovician-silurian Extinction: 440 million years ago.
Devonian Extinction: 365 million years ago.
Permian-triassic Extinction: 250 million years ago.
Triassic-jurassic Extinction: 210 million years ago.
Cretaceous-tertiary Extinction: 65 million Years Ago.

Hi,

செத்து பொழச்ச பூமி JUST MISS | Dark Side of the Earth | பூமியின் வரலாறு
நம் பூமி உருவானபோ பல பேரழிவுகளை சந்தித்துள்ளது அதே போல் உயிரினங்கள் எப்படி உருவானது மற்றும் ஏற்பட்ட பேரழிவுகளால் உயிரினங்கள் எப்படி அழிந்தது , அனைத்தையும் நாம் இந்த பதிவில் தெரிந்துகொள்ளலாம்

Approximately 485.4 million to 443.8 million years ago. Here are some key points about the Ordovician period:

Sea Life: The Ordovician is known for the diversification of marine life. It saw the proliferation of various marine organisms, including trilobites, brachiopods, cephalopods, and early fish. Some of the first jawed fish appeared during this period.

Mass Extinction: Toward the end of the Ordovician period, there was a significant mass extinction event known as the Ordovician-Silurian extinction event. It is considered one of the Big Five mass extinctions in Earth's history

Continental Drift: During the Ordovician, the continents were positioned differently than they are today due to the process of plate tectonics.

Devonian extinction:

Timing: The Late Devonian extinction occurred over several million years, spanning the later part of the Devonian period. It's not a single, sudden event like some other mass extinctions.

Affected Organisms: The Devonian extinction primarily affected marine life. It had a particularly significant impact on marine organisms like corals, trilobites, brachiopods, and various types of jawless fish. Some groups, however, such as ammonoids, bony fish, and certain types of sharks, survived the extinction relatively unscathed.

Volcanic Activity: Intense volcanic activity could have released greenhouse gases into the atmosphere, leading to global warming and changes in ocean chemistry.

The Permian-Triassic extinction event, also known as the "Great Dying," is one of the most devastating mass extinctions in Earth's history. It occurred approximately 252 million years ago, marking the boundary between the Permian and Triassic periods. Here are key details about this catastrophic event:

Extent of Extinction: The Permian-Triassic extinction event is considered the most severe mass extinction event in Earth's history. It resulted in the loss of an estimated 90-96% of marine species and around 70% of terrestrial vertebrate species. It affected life on both land and in the oceans.

Volcanic Activity: One leading hypothesis is that extensive volcanic eruptions in an area now known as the Siberian Traps released massive amounts of lava and greenhouse gases. This led to significant global warming, acid rain, and changes in ocean chemistry, contributing to the environmental stress.

The Triassic-Jurassic extinction event is one of the five major mass extinctions in Earth's history, occurring approximately 201 million years ago, at the boundary between the Triassic and Jurassic periods. Here are key details about this extinction event:

Causes: The exact causes of the Triassic-Jurassic extinction are still debated among scientists, but several contributing factors have been proposed:

Volcanic Activity: Intense volcanic activity, particularly the eruption of the Central Atlantic Magmatic Province (CAMP), released large volumes of lava and greenhouse gases into the atmosphere. This led to global warming, ocean acidification, and changes in climate patterns.

Cretaceous-tertiary Extinction:
It occurred approximately 66 million years ago at the boundary between the Cretaceous and Tertiary (now known as the Paleogene) periods. Here are key details about this extinction event:

Extent of Extinction: The K-T extinction event resulted in the extinction of an estimated 75% of Earth's species, including many marine and terrestrial organisms. It is perhaps most famously known for causing the extinction of the non-avian dinosaurs.

Effects on Marine Life: Marine ecosystems experienced significant losses during the K-T extinction. Many marine reptiles, ammonites, and other marine species went extinct. Some groups, such as mammals, crocodiles, and some types of fish, survived the event.

நன்றி

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Santhosh

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460 கோடி ஆண்டுகளுக்கு முன் நம் பூமி உருவாகி அதன் பின் தற்போதைய நிலைக்கு மாறிய விளக்கம் இந்த காட்சியில் தமிழில் கூறப்பட்டுள்ளது . உங்களுடைய கருத்துக்களை கீழ் தெரிவிக்கலாம் நன்றி.






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