Punctuated equilibrium

This article is about the theory in evolutionary biology. For the theory of social change, see Punctuated equilibrium in social theory. For the album by Wino (Scott Weinrich), see Punctuated Equilibrium (album).
The punctuated equilibrium model (top) consists of morphological stability followed by rare bursts of evolutionary change via rapid cladogenesis – vertical equilibrium states separated by horizontal "jump" phases. In contrast, phyletic gradualism (below), is a more gradual, continuous model of evolution – with accumulation of small incremental changes represented by slanted bars that split at branch-points, where two separate modes of life are feasible but of which, each prospers best with divergent specializations.
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In evolutionary biology, punctuated equilibrium (also called punctuated equilibria) is a theory that proposes that once a species appears in the fossil record, the population will become stable, showing little evolutionary change for most of its geological history.[1] This state of little or no morphological change is called stasis. When significant evolutionary change occurs, the theory proposes that it is generally restricted to rare and geologically rapid events of branching speciation called cladogenesis. Cladogenesis is the process by which a species splits into two distinct species, rather than one species gradually transforming into another.

Punctuated equilibrium is commonly contrasted with phyletic gradualism, the idea that evolution generally occurs uniformly by the steady and gradual transformation of whole lineages (anagenesis).[2]

In 1972, paleontologists Niles Eldredge and Stephen Jay Gould published a landmark paper developing their theory and called it punctuated equilibria.[1] Their paper built upon Ernst Mayr's model of geographic speciation,[3] I. M. Lerner's theories of developmental and genetic homeostasis,[4] and their own empirical research.[5][6] Eldredge and Gould proposed that the degree of gradualism commonly attributed to Charles Darwin[7] is virtually nonexistent in the fossil record, and that stasis dominates the history of most fossil species.

  1. ^ a b Eldredge, Niles; Gould, S.J. (1972). "Punctuated equilibria: An alternative to phyletic gradualism". In Schopf, T.J.M. (ed.). Models in Paleobiology. San Francisco, CA: Freeman Cooper. pp. 82–115.
    Reprinted in
    Eldredge, N., ed. (1985). Time Frames (PDF). Princeton, NJ: Princeton University Press. pp. 193–223. Archived from the original (PDF) on 2020-01-13. Retrieved 2018-01-27.
  2. ^ Gould, S.J. (15 April 1982). "Punctuated equilibrium — a different way of seeing". New Scientist. Vol. 94. pp. 137–139 – via Google Books.[permanent dead link]
  3. ^ Mayr, Ernst (1954). "Change of genetic environment and evolution". In Huxley, J.; Hardy, A.C.; Ford, E.B. (eds.). Evolution as a Process. London, UK: Allen and Unwin. pp. 157–180 – via Blackwell Publishing.
  4. ^ Lerner, I.M. (1954). Genetic Homeostasis. New York, NY: John Wiley.
  5. ^ Eldredge, Niles (1971). "The allopatric model and phylogeny in Paleozoic invertebrates". Evolution. 25 (1): 156–167. doi:10.2307/2406508. hdl:2246/6568. JSTOR 2406508. PMID 28562952.
  6. ^ Gould, S.J. (1969). "An evolutionary microcosm: Pleistocene and recent history of the land snail P. (Poecilozonites) in Bermuda". Bull. Mus. Comp. Zool. 138: 407–532.
  7. ^ Rhodes, F.H.T. (1983). "Gradualism, punctuated equilibrium and the Origin of Species". Nature. 305 (5932): 269–272. Bibcode:1983Natur.305..269R. doi:10.1038/305269a0. PMID 6353241. S2CID 32953263.