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basic elements of speciation
barrier to gene flow —> genetic differentiation —> reproduction isolation
the tempo of speciation
classic, gradualistic model: slow divergence of isolated populations
punctuated equilibrium: long periods of stasis followed by sudden episodes of speciation
earth’s history shows periods of slow evolution punctuated by periods of rapid evolution
cichlid fishes in lake victoria: 400 species in 12,000 years
horseshoe crabs: phenotypic stasis for 100,000,000 years
what controls the rate of speciation?
rates of mutations
rates of selection
competition among species
available habitat
generation time
rates of environmental change
specific changes leading to rapid speciation
key genetic processes change phenotype, but maintain function
polyploidy
key developmental processes change phenotype, but maintain function
alteration of genes that control organism structure
mutations in hox genes
hererochrony: changes in developmental timing or sequence
heterochrony (2 types)
sequence heterochrony: change in the time of appearance of a structure
allometric heterochrony: change in the rate of development/growth
rates of extinction
continuous process, always occurring at some background rate due to chance and natural selection
accelerated by environmental change
can occur in rapid bursts, known as mass extinction events
mass extinctions
information from geology about large-scale and/or catastrophic events
permian extinction: volcanoes? methane gas from deep sea?
cretaceous extinction: a meteor?
adaptive radiation of mammals occurred when?