Our solar system formed approximately 4.5 billion years ago.
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Earth's moon was formed when the earth was still a young molten planet.
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Earth has cooled off enough to have a crust over its molten core. For millions of years asteroids pelted our planet and brought microscopic crystals of ice to Earth.
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Microscopic life existed on earth. Cyanobacteria were creating oxygen through photosynthesis.
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For billions of years Earth's climate had been changing due to plate tectonics and microscopic life. Then we entered an ice age nicknamed Snowball Earth.
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When Snowball Earth melted there was an explosion of evolution. A wide diversity of life developed in the oceans.
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Animal life in the ocean continued to diversify, while plant and fungal life on land started to get established.
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During this warm period many plants and animals thrived.
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Each animal was developing specialized features for hunting and avoiding being eaten.
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Tetrapods started to live on land.
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Fish, tetrapods, and invertebrates continue to evolve interesting features.
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Swamps with lush plants from this time period turned into the coal and oil reserves we are using today.
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Complex plant life created high oxygen levels. This allowed for giant insects to rule the air.
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The giant supercontinent of Pangea has formed with both deserts and ice caps. Plants and animals have to adapt to drier environment and a wider range of temperatures.
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On land both herbivores and carnivores have developed large bodies as they live in complex ecosystems.
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Volcanic activity and a depletion of oxygen in the oceans lead to the extinction of 75% of all life on the planet. (81% marine life and 70% of terrestrial)
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After the Permian Extinction, reptiles quickly evolved to take over the land, oceans, and air. This is the age of the dinosaurs.
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During this period Pangea pulled apart and our current continents started to form, and alongside the dinosaurs are first mammals and many other species that still exist today.
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This was a wam period for our planet. Flowering plants and pollinators evolved during this time.
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Due to the warm climate sea levels were high. Shallow seas covered what is dry land today.
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Dinosaurs were the dominant animal life on all seven continents.
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When a giant asteroid hit Earth it created a world-wide extinction that took place in a matter of hours. The impact sent rock vapor into space. The vapor cooled and returned to the planet as tiny shards of glass. The friction of these shards reentering the atmosphere caused temperatures to spike dangerously hot.
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Life evolved in the niches left open by the K-T extinction.
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As the continents separated, each ecosystem became distinct.
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Many interesting animals of this time period are no longer alive today, but we can see similarities to modern animals in their body structures.
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Evolution was also spurred on by a climate that cycled between global warming and ice ages.
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Ocean life was also interesting during this time period.
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There are many branches of our family tree.
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Many of our earliest hominin ancestors lived in the Great Rift Valley of Africa.
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This is the time period when our ancestors became bipedal.
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As the last ice age impacted the planet our ancestors in the genus Homo continued to evolve in Africa.
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Some of our evolutionary cousins evolved alongside our ancestors, but their lineage did not survive. "Paranthropus" means "alongside humans"
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As our ancestors left Africa, they interacted with a variety of other animals.
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Many hominins were established throughout the Europe and Asia before our species, Homo sapiens, even existed.
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Our species Homo sapiens has been on our planet for only a tiny portion of our planet's history. Yet our impact on our planet is so great we call today's time period Anthropocene -- or the epoch where human activity is having the greatest influence on climate and environment.
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