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Evolution__3rd_Edition

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Summary<br />

CHAPTER 21 / Rates of <strong>Evolution</strong> 611<br />

evidence can provide another sort of measurement of evolutionary rates, along with<br />

measurements of single characters.<br />

21.7 Conclusion<br />

1 <strong>Evolution</strong>ary rates of fossil characters can be<br />

measured as simple rates of change through time;<br />

logarithms are often taken of the character measurements<br />

and the rate expressed in “darwins.” <strong>Evolution</strong><br />

in horse teeth is a classic example.<br />

2 Rates of evolution measured in the fossil record are<br />

slower than those produced by artificial selection in<br />

the laboratory.<br />

3 <strong>Evolution</strong>ary rates vary between different geological<br />

times, taxa, and types of taxa. The science of evolutionary<br />

rates is mainly concerned to explain the pattern of<br />

evolutionary rates.<br />

4 Among published measurements of evolutionary<br />

rates, the rate and the time interval over which it was<br />

measured are inversely related: faster evolution is seen<br />

in shorter intervals. The reason is probably that the<br />

direction of evolution fluctuates through time.<br />

5 Eldredge and Gould stimulated a controversy about<br />

evolutionary rates by their suggestion that rates have a<br />

strict pattern (called punctuated equilibrium) where<br />

evolution is fast at times of splitting (speciation) and<br />

comes to a halt between splits. The opposite pattern, in<br />

which evolution has a constant tempo, they called<br />

phyletic gradualism.<br />

6 It is difficult to discover the pattern of evolutionary<br />

This chapter has introduced three methods of measuring rates of evolution. For single<br />

characters that show continuous variation, we can measure the metrical rate of change<br />

and express it in darwins. For characters with discrete states, we can give each state an<br />

arbitrary score and measure the rate of change of the score. A cruder measure is provided<br />

by the duration of species in the fossil record, because taxonomists will recognize<br />

a higher turnover of species in groups that evolve rapidly. All three methods have their<br />

particular uses and applications. In this chapter we have seen how paleobiologists have<br />

used all three methods to study general evolutionary questions.<br />

rates at, and between, speciation events because the<br />

fossil record is incomplete.<br />

7 There is some evidence for punctuated equilibrium,<br />

such as Cheetham’s study of Caribbean bryozoans<br />

from the Miocene and Pliocene, and some for phyletic<br />

gradualism, such as Sheldon’s study of Ordovician<br />

trilobites in Wales. No general empirical conclusion is<br />

yet possible, though punctuated equilibrium is a well<br />

confirmed phenomenon.<br />

8 <strong>Evolution</strong>ary processes and rates can be examined<br />

at all taxonomic levels from evolution within populations,<br />

through speciation, to the origin of the higher<br />

groups. <strong>Evolution</strong> may have characteristic mechanisms<br />

and rates at different levels, or the same set of rates and<br />

processes may operate equally at all levels.<br />

9 For large changes, like from a limb into a wing,<br />

evolutionary rates cannot be measured as a continuous<br />

variable. The character can instead be divided into<br />

states. The evolutionary rate can then be studied in<br />

the rate of change between states. Westoll studied the<br />

evolution of lungfish by this method.<br />

10 The number of species in a lineage per million<br />

years is a complex measure of evolutionary rate, called<br />

a taxonomic rate of evolution. Taxonomic rates can be<br />

expressed as survivorship curves.

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