Grade Level(s):
- 9-12
- 13-16
- Advanced
- General
Source:
- UC Museum of Paleontology
Resource type:
- Tutorial
Time: 30 minutes
Overview
Usually, extinction operates at a fairly constant rate, culling some species while speciation generates new ones. However, at a few points in life's history the humdrum of regular extinction has been interrupted by mass extinctions. Learn more about these biodiversity crises.
- [History of life: Grades 9-12] During the course of evolution, only a small percentage of species have survived until today.
- [History of life: Grades 9-12] Background extinctions are a normal occurrence.
- [History of life: Grades 9-12] Rates of extinction vary.
- [History of life: Grades 9-12] Mass extinctions occur.
- [History of life: Grades 9-12] Extinction can result from environmental change.
- [History of life: Grades 9-12] Extinctions may create opportunities for further evolution in other lineages to occur.
- [History of life: Grades 13-16] During the course of evolution, only a small percentage of species have survived until today.
- [History of life: Grades 13-16] Background extinctions are a normal occurrence.
- [History of life: Grades 13-16] Rates of extinction vary.
- [History of life: Grades 13-16] Mass extinctions occur.
- [History of life: Grades 13-16] Extinction can result from environmental change.
- [History of life: Grades 13-16] Human influence may be causing a modern mass extinction.
- [History of life: Grades 13-16] Extinctions may create opportunities for further evolution in other lineages to occur.
- [Studying evolution: Grades 9-12] Scientists use fossils (including sequences of fossils showing gradual change over time) to learn about past life.
- [Studying evolution: Grades 9-12] Scientists use physical, chemical, and geological evidence to establish the age of fossils.
- [Studying evolution: Grades 13-16] Scientists use fossils (including sequences of fossils showing gradual change over time) to learn about past life.
- [Studying evolution: Grades 13-16] Scientists use physical, chemical, and geological evidence and comparative anatomy to establish the age of fossils.
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