1. The fossil record shows several patterns of evolution over geological time, including stasis, gradual morphological changes, and speciation.
2. Speciation can occur through either phyletic gradualism of small incremental changes over long periods, or through punctuated equilibrium of stasis with sudden changes following geographic isolation.
3. Complex structures evolved through incremental modifications of existing structures driven by genetic changes over generations in response to environmental pressures, rather than appearing abruptly, as seen in the evolution of limbs, jaws, wings, and other anatomical features.