Plate Tectonics and Mass Extinctions PDF
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Utah Valley University
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Summary
This document provides an overview of plate tectonics and mass extinctions, encompassing topics such as the Earth's structure, continental plates, plate boundaries, evidence for plate tectonics including fossil distribution, continental fit, seafloor spreading, and magnetic anomalies. It also discusses mass extinction events and their potential causes, the effects of plate tectonics on evolution, and the difference between macro and microevolution, examples, and the impact of human activities on current extinction rates.
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# Plate Tectonics and Mass Extinctions ## Earth's Structure - **Crust**: The Earth's outer layer, composed of solid rock. - **Mantle**: The thickest layer, made up of hot, dense rock. - **Outer Core**: Liquid layer composed of iron and nickel. - **Inner Core**: Solid layer composed of iron and nic...
# Plate Tectonics and Mass Extinctions ## Earth's Structure - **Crust**: The Earth's outer layer, composed of solid rock. - **Mantle**: The thickest layer, made up of hot, dense rock. - **Outer Core**: Liquid layer composed of iron and nickel. - **Inner Core**: Solid layer composed of iron and nickel. ## Plate Tectonics - **Continental Plates**: Large pieces of Earth's crust that move slowly over time. - **Plate Boundaries**: The edges of the plates where they interact. - **Divergent Plate Boundaries**: Plates move apart, creating new oceanic crust at mid-ocean ridges. - **Convergent Plate Boundaries**: Plates collide, resulting in subduction zones, mountain ranges, and volcanic arcs. - **Transform Plate Boundaries**: Plates slide past each other horizontally. ## Evidence for Plate Tectonics - **Fossil Distribution**: Similar fossils found on continents now separated by oceans. - **Continental Fit**: The shapes of continents match like puzzle pieces. - **Seafloor Spreading**: New oceanic crust is formed at mid-ocean ridges, and older crust is pushed away from the ridges. - **Magnetic Anomalies**: Stripes of alternating magnetic polarity on the seafloor, indicating a pattern of crust formation and movement. ## Mass Extinctions - **Definition**: The annihilation of all individuals of a species or group of species. - **Causes**: - Climate change - Volcanic eruptions - Meteorite impacts - Sea level changes - Ocean acidification - Disease - Habitat loss - Human interaction - **Major Extinction Events**: - **Ordovician Extinction**: 445 million years ago - likely caused by rapid global cooling and falling sea levels. - **Devonian Extinction**: 340 million years ago - likely caused by asteroid impacts and rapid global cooling. - **Permian Extinction**: 250 million years ago - likely caused by volcanic activity, increased methane and CO2, and rapid global warming. - **Triassic Extinction**: 200 million years ago - likely caused by increased methane and CO2, and rapid global warming. - **Cretaceous-Paleogene Extinction**: 65 million years ago - asteroid impact, volcanic activity, and widespread fires. ## The Impact of Plate Tectonics on Evolution - **Adaptive Radiations**: Rapid diversification of species into new ecological niches. - **Example**: The Hawaiian Islands, with their diverse array of endemic species. - **Continental Drift**: - **Formation of Pangaea**: Led to a reduction in intertidal and coastal habitats and dramatic climate changes. - **Breakup of Pangaea**: Led to the isolation of continents and the development of unique species on different continents. ## Macroevolution vs. Microevolution - **Macroevolution**: Large-scale evolutionary change over vast periods of time. - **Examples**: The evolution of birds from dinosaurs, the evolution of mammals from reptiles. - **Microevolution**: Small-scale evolutionary change within a population. - **Examples**: The adaptation of house sparrows to different climates in North America, the evolution of antibiotic resistance in bacteria. ## Darwin and Wallace - **Charles Darwin and Alfred Russell Wallace**: Independently developed the theory of evolution by natural selection. - **Natural Selection**: The process by which organisms with traits better suited to their environment are more likely to survive and reproduce. ## Human Impact on Extinction - **Habitat Loss**: The primary driver of species extinction today. - **Examples**: Deforestation, agriculture, urbanization. - **Consequences**: - Loss of biodiversity - Disruption of ecosystems - Potential for cascading effects on food webs. ## Conclusion - Plate tectonics and mass extinctions are major forces shaping the history of life on Earth. - Human activities are accelerating the rate of extinction, posing a significant threat to biodiversity. - Understanding these processes is crucial for conservation efforts to protect the planet and its diverse life forms.