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allele frequency
rate at which a specific allele appears within a population
Georges Cuvier
paleontologist that was first to formally recognize extinction
evolution
change in allele frequencies of a population across generations
fitness
individual’s ability to survive and reproduce (see also relative fitness)
fossil
the preserved remains (body fossils) or traces (trace fossils) of organisms from prehistoric time
homology
similarity between species due to inheritance from a common ancestor
James Hutton
geologist that proposed that geological change occurs gradually by accumulating small changes from processes like erosion and uplift
Jean Baptiste de Lamarck
proposed inheritance of acquired characteristics as the mechanism for evolution. Although the theory was flawed, it was an important step toward describing how evolution could occur
Law of Superposition
layers of rock are arranged in time sequence with younger layers near top
Charles Lyell
geologist that shared the gradualism view of Hutton, played role in joint publication theory of natural selection
Macroevolution
broader scale evolutionary changes that scientists see over paleontological time
malthusian catastrophe
occurs when population size exceeds resource availability, leading to intense competition and crash of population size
Gregor Mendel
geneticist that first described many characteristics of heredity
microevolution
changes in a population’s genetic structure over short time scales (as little as one generation to next)
modern synthesis
overarching evolutionary paradigm that took shape by the 1940s and scientists generally accept today
Nicholas Steno
first to formally recognize that fossils are the remains of organisms
transitional feature
trait i a fossil that is intermediate between ancestral (older) and derived (newer) species
vestigal structure
physical structure present in an organism but has no (or little) apparent function and appears to be from a functional structure in a distant ancestor
Alfred Russel Wallace
conceived and described (independently with Charles Darwin) natural selection as a mechanism for evolution
permineralization
fossilization process in which minerals enter dead organic material and forms an internal cast