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EARTH Unit 9.1 1 UNIQUE EARTH Earth has a long and complex history. Time and again, the splitting and collision of continents has resulted in the formation of new ocean basins and the creation of great mountain ranges. Furthermore, the nature of life on our planet has experienced dramatic changes through time. 2 UNIQUE EARTH There is only one place in the universe, as far as we know, that support life – a modest-sized planet called Earth that orbits an average-sized star, the Sun. Life on Earth appears to be all around us; it is found in boiling mudpots and hot springs, in the deep abyss of the ocean, and even under the Antarctic Ice Sheet. 3 UNIQUE EARTH Living space on our planet, however, is significantly limited when we consider the needs of individual organisms, particularly humans. The global ocean covers 71% of Earth’s surface, but only a few hundred meters below the water’s surface, pressures are so intense that humans cannot survive without an atmospheric diving suit. 4 UNIQUE EARTH In addition, many continental areas are too steep, too high, or too cold for us to inhabit. Nevertheless, based on what we know about bodies in the solar system – and the hundreds of planets recently discovered orbiting around other stars – Earth is still by far the most accommodating. 5 UNIQUE EARTH What fortuitous events produced a planet so hospitable to life? Earth was not always as we find it today. During its formative years, our planet became hot enough to support a magma ocean. 6 UNIQUE EARTH Earth also survived a several hundred million year period of extreme bombardment by asteroids, to which the heavily cratered surfaces of Mars and Moon testify. The oxygen rich atmosphere that makes higher life forms possible developed relatively recently. 7 UNIQUE EARTH Serendipitously, Earth seems to be the right planet, in the right location, at the right time. 8 THE RIGHT PLANET If the Earth was more massive, gravity would be stronger, resulting in the retention of high levels of ammonia and methane. If the Earth was smaller, oxygen, water vapor, and other gases would have escaped. 9 THE RIGHT PLANET If the Earth did not have a lithosphere and asthenosphere, it wouldn’t have motion from tectonic plates – this tectonic activity creates landmasses. Also, the molten outer core is the reason why we have a magnetic field that protects Earth’s life forms. 10 THE RIGHT LOCATION If the Earth were 10% closer, our atmosphere would be like the one on Venus – too hot. If the Earth were 10% farther, it would be too cold. Earth’s proximity to an average sized star has allowed enough time for the evolution of humans. 11 THE RIGHT TIME Last, but not least, timing is a critical factor. The first organisms to live on Earth were extremely primitive and came into existence roughly 3.8 billion years ago. From that point, innumerable changes occurred. Let’s look at 2 major Earth-altering events. 12 THE RIGHT TIME The first event is the development of the Earth’s atmosphere. Earth’s primitive atmosphere consisted of mostly methane, water vapor, ammonia, and carbon dioxide. Due to photosynthesis, free oxygen came into existence, resulting in the flourishing of various life forms. 13 THE RIGHT TIME The second event occurred about 65 million years ago, our planet was struck by an asteroid 10 km wide. We learned of this as the cause of the Cretaceous Extinction, which led to the demise of nearly ¾ of all plant and animals species, including the dinosaurs. Eventually, mammals that survived flourished to become the dominant species. 14 THE RIGHT TIME 15 https://www.youtube.com/watch?v=tzAx7d2Dqz w 16 JUST RIGHT As various observers have noted, Earth developed under “just right” conditions to support life. Astronomers refer to this as the Goldilocks scenario: Venus is too hot, Mars is too cold, Earth is just right. 17 VIEWING EARTH’S HISTORY We will be focusing on the origin and the evolution of Earth. Researchers utilize many tools to interpret clues about Earth’s past. Using tools as well as clues contained in the rock record, scientists continue to unravel many complex events of the geologic past. 18