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Lecture 18: Rates of Evolutionary Change G. G. Simpson: “Tempo & Mode in Evolution” (1944) applied principles of modern synthesis (e.g. population genetics) to fossil record macroevolution ≈ microevolution writ large Two ways to measure evolution
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1) Phylogenetic Rate Morphological Rate rate of change of character or group of characters in a lineage (anagenesis) Rate = Change/ Unit Time
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Rates of Evolution of Single Characters Haldane (1949): darwin = change in e / my (ln x 2 - ln x 1 /change in t) Transformation : % change (removes scaling effect) e.g. 34 mm to 56 mm over 12 my ln (34) = 3.526; ln (56) = 4.025 rate of change = (4.025 - 3.526) / 12 = 0.042 d
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Evolution of Equine Lineage
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Horse Teeth
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McFadden (1992): 408 specimens 26 ancestor - descendent pairs 4 characteristics of teeth In general: pointy, narrow (leaf eater) wide, flat (grazer) 26 X 4 = 104 estimates of evolutionary 0.05 - 0.1 darwins mainly positive, but also some reversals
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Comparing Rates in size of Ceratopsids = 0.06 darwins in skeletal dimensions of Passer domesticus after intro to N. Am. = 50 - 300 darwins artificial selection: 60,000 darwins! continuous fossil records show low rate masks frequent advances & reversals e.g. late Cenozoic mammals : 12 darwins for short periods
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Fluctuations in Rate Gingerich : rate of evolution 1/ time measured Short term fluctuations cancel out e.g. beaks of Darwin’s finches e.g. changes in radiolarian tests time width
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Character Types characters evolve at diff’t rates (mosaic evolution) rate of change is not constant conservative characters: canalized; general adap’ns derived characters: specialized, rapid evol’n
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Rates of change & population genetics Given: variance in character, estimate of heritability (h N 2 ), in mean over t gen’ns: can estimate strength of directional selec’n req’d i.e. proportion of pop’n that fails to reproduce in order to produce observed changes contrast: weak, stabilizing selection, but pop. size small enough that drift will produce change
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Horse Example Assume (h N 2 ) = 0.5 2 selective deaths / 10 6 individ / generation (selection) population size of < 10 4 individuals (drift)
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2) Taxonomic Rate replacement of forms origination & extinction (cladogenesis) Quantified: (# taxa originate - # taxa extinct) / unit time Or the inverse of the average duration of a species
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Cladogenesis & Anagenesis Speciation at t 1 & t 2 a & c contemporary b goes extinct
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Chronospecies Problem: Fossil record: taxonomy based on morpho characts. Hard to separate anagenesis from cladogenesis Identification of many chronospecies Chronospecies: descendent recognized as separate spp. Taxonomic Pseudoextinction
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time morphology Phylogenetic Rate = Taxonomic Rate rapid rate of morphological change leads to high rate of taxonomic replacement
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time morphology ↑ Taxonomic Rate ↑ Phylogenetic Rate high rate of turnover; little morphological change
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Relationship b/w phylogenetic rate & taxonomic rate depends on characters used to determine taxa Comparison of taxonomic rates : balance of origination & extinction e.g. Bivalvia (Pelecypoda): 17 genera appear in Ordovician 4 survive to Triassic average duration = 78 my compare to Carnivora: 8 my
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Living Fossils oldest living species: Triops cancriformis (tadpole shrimp) unchanged since Triassic! (180 mya) Coelacanth Cycad
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Recent Taxa rapid evolution poor fossil record typical of Adaptive Radiations: Elaphus PrimelaphusLoxodonta Mammuthus ~ 1 my (during Pliocene)
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Problem of stasis: Fossil Deposits: 50 - 100 my apart short term changes are lost However, observe: 1) long periods without change 2) rapid appearance of new forms 3) no transitional forms Real or Artifact?
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Quantum Evolution Problem: new taxa without fossil intermediaries Simpson: rapid, substantial evol’nary change with shift into new adaptive zones once a threshold passed in acquisition of new adaptation, strong directional selection shapes feature into new forms e.g. tarsus “pulley” in Artiodactyla: rapid evol’n & diversificat’n of deer, camels, antelopes
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Hypotheses 1) Phyletic Gradualism constant anagenetic change speciation gradual transitional forms lost in fossil record 2) Punctuated Equilibrium stasis is real evolution occurs during speciation long-term trends in morphology due to spp. sel’n
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