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Question
ees unit 3: study guide
objective 1: geologic time and fossils
- how is geologic time organized?
- what is the oldest and longest era? what life existed then?
- what is the most recent era? what life is dominant?
- in which eras were there extinctions and what were the accepted causes of those extinctions?
- when(in geologic time) did pangaea form and start breaking up?
- explain how pangaea broke up.
- how do fossils help explain climates that may have once existed on continents?
- list the four types of fossils and give examples of each.
- what are the conditions that favor fossil formation?
- what does the principle of fossil succession state and how does it help to establish geologic history?
- what are the three characteristics of an index fossil?
Brief Explanations
- Geologic time is organized into eons, eras, periods, epochs, and ages based on major geological and biological events.
- The Hadean is the oldest and the Precambrian is the longest era. Early simple life - forms like bacteria and archaea existed then.
- The Cenozoic is the most recent era. Mammals are the dominant life - form.
- Extinctions occurred in eras like the Permian (massive volcanic activity and climate change) and the Cretaceous (asteroid impact).
- Pangaea formed around 335 million years ago and started breaking up around 175 million years ago.
- Pangaea broke up due to tectonic plate movements driven by convection currents in the mantle.
- Fossils can indicate past climates as certain organisms thrive in specific climates. For example, coal deposits suggest a warm, wet climate.
- The four types of fossils are body fossils (e.g., dinosaur bones), mold fossils (e.g., impression of a shell in rock), cast fossils (e.g., a rock filling a mold), and trace fossils (e.g., dinosaur footprints).
- Conditions favoring fossil formation include rapid burial, low oxygen environments, and hard body parts.
- The principle of fossil succession states that fossils occur in a definite, recognizable order. It helps in dating rocks and establishing geologic history.
- Index fossils are widespread, abundant, and existed for a short geologic time.
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- Organized into eons, eras, periods, epochs, ages.
- Oldest - Hadean, Longest - Precambrian; Bacteria, archaea.
- Cenozoic; Mammals.
- Permian (volcanic activity, climate change), Cretaceous (asteroid impact).
- Formed ~335 million years ago, started breaking up ~175 million years ago.
- Due to tectonic plate movements.
- Indicate past climates as organisms have climate preferences.
- Body (dinosaur bones), Mold (shell impression), Cast (rock - filled mold), Trace (dinosaur footprints).
- Rapid burial, low oxygen, hard body parts.
- Fossils occur in a definite order; helps in dating rocks and history.
- Widespread, abundant, short - lived geologically.