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Fossil Evidence of Change Part 2 Chapter 14 Section 1
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Dating Fossils Relative dating is a method used to determine the age of rocks by comparing them with those in other layers.
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Law of superposition states that younger layers of rock are deposited on top of older layers
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Radiometric dating uses the decay of radioactive isotopes to measure the age of a rock
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This method requires that the half-life of the isotope, which is the amount of time it takes for half of the original isotope to decay, is known.
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Uranium 238 decays to Lead 206 with a half-life of 4510 million years.
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Geologic Time Scale (GTS) GTS is a record of Earth’s history Epochs are the smallest unit of geologic time lasting several million years
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Periods are divisions of geologic time lasting tens of millions are years
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Era is a unit of geologic time consisting of 2 or more periods that lasts hundreds of millions of years
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Precambrian First 4 billion years Life 1 st appeared cyanobacteria and eukaryotic cells also emerged
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The Paleozoic Era In just a few million years, the ancestors of most major animal groups diversified in what scientists call the Cambrian explosion.
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1 st life on land emerged during this era Mass extinctions have occurred every 26-30 million years on average
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Between 60-75% of the species alive went extinct in each of these events The cause of these extinctions include geological forces and increased volcanic activity disrupting ecosystems and changing climate
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The Mesozoic Era Mammals and dinosaurs fist appeared Flowering plants evolved from non-flower plants
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Birds evolved from a group of predatory dinosaurs 65 million years ago, a meteorite struck Earth
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Paleontologists have evidence of this due to the large amounts of iridium which is rare on Earth, but common on meteorites
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The meteor probably did not wipe out all the species, but debris from the impact probably stayed in the atmosphere for months or even years affecting global climate
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The Cenozoic Era Is the most recent era Mammals became the dominant land animals Humans appeared near the end in the Neogene period
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