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KEY CONCEPT The geologic time scale divides Earth ’ s history based on major past events. Index fossils are another tool to determine the relative age of rock layers. Definition: Fossils of organisms that existed only during specific spans of time over large geographic areas
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KEY CONCEPT The geologic time scale divides Earth’s history based on major past events.
Index fossils are another tool to determine the relative age of rock layers. • Definition: Fossils of organisms that existed only during specific spans of time over large geographic areas • Example: Fusulinids and trilobites. • Characteristics: Common, easy to identify, found widely around the world, only existed for a relatively brief time • Nonexample (I don’t get it either): Anything that is rare to find or that are only found in a certain region
100 250 550 1000 2000 PRECAMBRIAN TIME This time span makes up the vast majority of Earth’s history. It includes the oldest known rocks and fossils, the origin of eukaryotes, and the oldest animal fossils. Cyanobacteria Geologic Time Scale: Representation of the history of the Earth that is organized by major changes or events • Eras: Last tens to hundreds of millions of years & consist of two or more periods • Periods: Most commonly used units of time, lasting tens of millions of years • Epochs: The smallest units of time, lasting several millions of years
Eras: • Era: Cenozoic (Most recent, currently still underway) Description: Evolution of primates, diversification of mammals, flowering plants & continues today
Eras: 2. Era: Mesozoic (“Age of the Dinosaurs”) Description: Evolution & extinction of dinosaurs, evolution of ferns, cycads & mammals
Eras: 3. Era: Paleozoic (Oldest era, “Ancient life”) Description: All existing animal phyla developed, earliest land plants arose