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Published byBrian Chase Modified over 9 years ago
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The Fossil Record – made up of all the fossils ever discovered on Earth provides evidence that species have changed over time Fossil – the remains or evidence of once-living organisms
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Mineralization minerals in water replace the organism’s original material and harden into rock Carbonization extreme pressure drives off the organism’s liquids and gases leaving only the carbon outline
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Molds and Casts Mold – impression of an organism in hardened mud or sand Cast – a fossil copy of an organism in a rock created by sediment filling in the mold
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Trace Fossils preserved evidence of the organism’s activity, like footprints Original Material original tissues of an organism, like insects in amber (tree sap)
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Relative-Age – scientists determine the relative order in which rock layers were deposited( Most Accurate when the rock layers are undisturbed.) Absolute-Age (Radioactive Dating)– scientists use the ratio of unstable isotopes to stable isotopes to find the age of rocks; more precise ex. carbon-14 dating
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a chart that divides Earth’s history into different time units
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Extinction – occurs when last individual organism of a species dies Mass Extinction when many species become extinct within a few million years or less there have been 5 mass extinctions in the Phanerozoic eon Causes of Extinction Sudden change – like meteor impact or volcanic eruption Gradual change – like tectonic plates or sea level changes
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the change over time in populations of related organisms
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