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Chapter 4: Views of Earth’s Past
Radioactivity
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What is Radioactivity? Radioactivity: the breakdown of atoms in elements from one form to another. The rate of change of a radioactive element is measured in half-lives.
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What is a Half-life? Half-life: the length of time it takes for half of the atoms in an element to change from an unstable form into another form. Elements with very long half-lives are useful in dating rocks. Igneous rocks provide the best results. Half-Life Video
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Chapter 4: Views of Earth’s Past
Geologic Time Scale
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What is Uniformitarianism?
James Hutton proposed this theory in two parts: Earth is an always-changing place. The same forces of change that are at work today were at work in the past.
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Changing the Earth Some changes are slow: mountain formation and climate change. Others are fast: volcanic eruptions, earthquakes, and floods.
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Earth’s Age Evidence has shown that:
Earth is about 4.6 billion years old Living organisms have been here for 3.8 billion years Multicellular organisms existed 1 billion years ago Humans existed 100,000 years ago
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Geologic Time Scale The geologic time scale divides Earth’s history into intervals of time. From longest to shortest Eon Era Period Epoch
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Eons There are 4 eons. The first three are the Hadean, Archaen, and Proterozoic. These are known as “Pre-Cambrian” The most recent one is the Phanerozoic.
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Phanerozoic Eon There are three eras in this eon. Paleozoic Mesozoic
Cenozoic
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Paleozoic Era Its name means “ancient life”
At the beginning, all life was oceanic (fish) By the end, life moved onto land Mostly reptiles, insects, and ferns A mass extinction occurred at the end, killing off several life forms. We don’t know what happened in detail.
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Mesozoic Era Its name means “middle life” Best known for the dinosaurs
It is when mammals, birds, and flowers first appeared Mass extinction ended this era Most likely a large asteroid that shot enough dust into the atmosphere to block the sun, which killed all plants.
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Cenozoic Era Its name means “recent life”
It is called “the age of mammals” There are two periods: Tertiary Quaternary: much of this was an ice age with mammoths, saber-toothed cats, and other giant mammals Rise of human civilization
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Our Timeline We live in the Phanerozoic Eon, the Cenozoic Era, the Quaternary Period, and the Holocene epoch.
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