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Formation of Earth
Earth formed approximately 4.6 billion years ago, initially characterized by volcanic activity and an atmosphere rich in gases like ammonia, methane, and carbon dioxide.
Fossil
A fossil is preserved remains of a once-living organism, showing evidence of evolution and providing insight into the past.
Cyanobacteria
Organisms that produced oxygen in the early Earth's atmosphere.
Early Earth atmosphere composition
Early Earth consisted of ammonia, methane, water vapor, carbon dioxide, and only trace amounts of oxygen.
Endosymbiotic Theory
Eukaryotic cells originated when prokaryotic organisms were engulfed by a host cell.
Natural Selection
A process where organisms with favorable traits survive and reproduce more successfully than those without these traits.
The significance of the fossil record
The fossil record shows evidence of evolution, extinction events, and how organisms have changed over time.
Charles Darwin
The scientist who wrote 'On the Origin of Species' and used fossils to provide evidence for evolution.
Support for evolution
Evidence includes homologous structures, vestigial structures, analogous structures, the fossil record, DNA and molecular evidence, and embryology.
Survival of the fittest
The concept that organisms with favorable traits are more likely to survive and reproduce than those with less favorable traits.
Stanley Miller and Harold Urey's Experiment
Demonstrated that organic molecules, specifically amino acids, could form spontaneously from inorganic precursors under conditions simulating the early Earth atmosphere.
First organisms on Earth
The first organisms were aerobic prokaryotes.
Influences on Charles Darwin
Geologist Charles Lyell's theory of gradualism, Thomas Malthus's work on population growth, and Jean-Baptiste Lamarck's early evolutionary ideas.