| Literature DB >> 20515493 |
Abstract
BACKGROUND: A positive relationship between diversification (i.e., speciation) and nucleotide substitution rates is commonly reported for angiosperm clades. However, the underlying cause of this relationship is often unknown because multiple intrinsic and extrinsic factors can affect the relationship, and these have confounded previous attempts infer causation. Determining which factor drives this oft-reported correlation can lend insight into the macroevolutionary process.Entities:
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Year: 2010 PMID: 20515493 PMCID: PMC2901258 DOI: 10.1186/1471-2148-10-162
Source DB: PubMed Journal: BMC Evol Biol ISSN: 1471-2148 Impact factor: 3.260
Currently published hypotheses supported by a positive correlation between diversification and nucleotide substitution rates.
| Extrinsic (Ecological) explanations: | 1) Evolutionary rates are causally unrelated to the process of speciation, but are linked to traits or habitats that promote diversification. | 1a) Life history. Increased generation time can cause mutations to accumulate faster over absolute time than they do in organisms with a slower life history [ |
|---|---|---|
| 1b) Environmental energy. High levels of environmental energy such as UV radiation and temperature are mutagenic and tend to speed up development, resulting in increased rates of nucleotide substitution. Environmental energy is linked to both species richness and to rates of molecular evolution, but environmental energy does not appear to affect speciation rates via its effect on mutation rates. Instead, environmental energy directly affects both species-richness and faster evolution [ | ||
| Intrinsic explanations: | 2) Faster rates of molecular evolution in speciose clades are caused by rapid bursts of evolution during speciation events. | 2a) Rapid evolution due to drift during speciation: If speciation commonly occurs in small, peripheral populations [e.g., founder event speciation, [ |
| 2b) Rapid evolution due to increased selection pressure during speciation: Speciation involving adaptation to a new niche or geographic range will involve strong selection favoring traits adaptive in the new environment. In this process of adaptation, average population fitness may decline, reducing population sizes [ | ||
| 3) Faster rates of molecular evolution may cause speciation, by: | 3a) Increasing the rate at which reproductive isolation develops between isolated populations [ | |
| 3b) Increasing the rate of production of new adaptations via increased mutational genetic variation [ | ||
| Statistical artifact explanation: | 4) Finally, the relationship between diversification and molecular evolution may be a statistical artifact. | When multiple substitutions have occurred at the same nucleotide position, this is undetectable on unbranched clades. However, if branching events have occurred between these 'multiple hits', then multiple substitutions at the same site are detectable. It will therefore appear as though the more speciose clade has undergone more substitutions (i.e., evolved faster) than its species-poor counterpart. This artifact is known as the node density effect [ |
Evolutionary rates estimates.
| Antirrhineae | 1.070 | (0.716, 1.588) | 0.989 | (0.602, 1.533) | 0.924 | 8.10E-03 | (6.24E-03, 1.02E-02) | 0.547 | (0.367, 0.737) |
| 0.379 | (0.275, 0.516) | 0.239 | (0.106, 0.401) | 0.631 | 1.69E-03 | (1.24E-03, 2.20E-03) | 0.921 | (0.697, 1.180) | |
| Chironiinae | 0.456 | (0.292, 0.702) | 0.350 | (0.133, 0.637) | 0.769 | 6.32E-03 | (4.45E-03, 8.45E-03) | 0.422 | (0.245, 0.601) |
| 0.234 | (0.170, 0.342) | 0 | (0, 0.166) | 0 | 2.17E-03 | (1.01E-03, 3.82E-03) | 0.809 | (0.422, 1.214) | |
| 0.956 | (0.670, 1.350) | 0.589 | (0.175, 1.086) | 0.617 | 8.26E-03 | (5.25E-03, 1.18E-02) | 0.753 | (0.512, 1.016) | |
| 0.366 | (0.259, 0.515) | 0.330 | (0.205, 0.492) | 0.902 | 2.78E-03 | (1.93E-03, 3.69E-03) | 0.722 | (0.514, 0.944) | |
| 1.547 | (1.112, 2.139) | 1.388 | (0.900, 2.023) | 0.898 | 2.18E-03 | (1.26E-03, 3.28E-03) | 1.060 | (0.554, 1.631) | |
| Lycieae | 0.177 | (0.136, 0.292) | 0 | (0, 0.163) | 0 | 2.80E-03 | (1.97E-03, 3.70E-03) | 0.497 | (0.246, 0.758) |
| Phrymoideae | 0.265 | (0.185, 0.375) | 0.188 | (0.079, 0.320) | 0.709 | 6.22E-03 | (4.79E-03, 7.72E-03) | 0.632 | (0.487, 0.790) |
| Polemoniaceae | 0.318 | (0.254, 0.396) | 0.227 | (0.145, 0.321) | 0.715 | 5.15E-03 | (4.25E-03, 6.11E-03) | 0.551 | (0.450, 0.656) |
| 1.649 | (1.181, 2.282) | 1.466 | (0.957, 2.134) | 0.889 | 6.56E-03 | (5.13E-03, 8.04E-03) | 0.614 | (0.477, 0.760) | |
| Saniculoideae | 0.259 | (0.194, 0.345) | 0.164 | (0.073, 0.269) | 0.631 | 1.78E-03 | (1.30E-03, 2.27E-03) | 0.611 | (0.442, 0.794) |
| 0.053 | (0.039, 0.095) | 0 | (0, 0.061) | 0 | 1.21E-03 | (9.34E-04, 1.52E-03) | 0.667 | (0.419, 0.959) |
Estimates for speciation rate (λ), extinction rate (μ), relative extinction rate (∑), mean rate of nucleotide substitution at the ITS1 and ITS2 loci (mean rate = number of substitutions per site/age in millions of years. It is calculated for each branch, then summed over all branches), and the coefficient of variation (c.v.) in mean substitution rate (c.v. rate = among-branch variance in ITS rate, scaled by the mean. I.e., for a tree with a c.v. of 0.50, the rate of ITS evolution varies across lineages by 50% of the mean). Confidence intervals (C.I.) for diversification rates were calculated from their likelihood profiles. 95% HPD (Highest Posterior Density) intervals for ITS rates are from BEAST (Tracer) analysis of MCMC output.
Figure 1Effects of the mean and among-branch variation in ITS substitution rate on speciation and extinction rates across temperate angiosperm clades. a,b: The mean rate of ITS substitution predicts speciation (log[lambda]) and extinction (ε2), suggesting that elevated background mutation rates facilitate both of these processes. c,d: The coefficient of variation in substitution rate does not predict either speciation or extinction, suggesting that a punctuated evolution model is inappropriate to describe the relationship between rates of molecular evolution and speciation.
Nucleotide substitution models and calibration dates for each of the 13 clades under consideration.
| Clade | Substitution model | Calibration Priors | ||||
|---|---|---|---|---|---|---|
| Node | age (mya) | source | citation | distribution * | ||
| Antirrhineae | GTR+I+Γ | Ingroup | 38-48 | previous estimate | [ | Normal, 43, 3 |
| 21.49 ± 4.27 | previous estimate | [ | Normal, 21.49, 6 | |||
| GTR+Γ | Ingroup | 34 - 45 | fossil and previous estimate | [ | Uniform, 34, 45 | |
| 17.1 | vicariance event | [ | Uniform, 0, 17.1 | |||
| Chironiinae | GTR+Γ | Ingroup | 54.8 | fossil - earliest Gentianaceae | [ | Uniform, 0, 54.8 |
| Mexican species of | 5 | vicariance event | [ | Normal, 5, 0.2 | ||
| 2 | vicariance event | [ | Normal, 2, 0.2 | |||
| GTR+Γ | Ingroup | 5-26 | previous estimate | [ | Uniform, 5, 26 | |
| 5 | vicariance event | [ | Normal, 5, 1.0 | |||
| GTR+Γ | ITS rate for Brassicaceae | [ | Uniform, 4.5E-3, 8.3E-3 subst/site/my | |||
| GTR+Γ | Ingroup | 65 | fossil | [ | Lognormal, 65, 0, 1 | |
| Canary Island clade | 0-21 | vicariance event | [ | Normal, 12, 3 | ||
| GTR+I+Γ | Ingroup | 18 | previous estimate | [ | Normal, 18, 2.5 | |
| Lycieae | GTR+I+Γ | Ingroup | 86-20 | previous estimate | [ | Uniform, 20, 86 |
| 29.4 ± 9.7 | previous estimate | [ | Normal, 29.5, 5.9 | |||
| Australian-Eurasian split | 14.1 ± 3.2 | previous estimate | [ | Normal, 14.1, 1.945 | ||
| Phrymoideae | GTR+I+Γ | Ingroup + | 49.4 | previous estimate - minimum | [ | Lognormal, 49.4, 0, 1 |
| 3.93 | previous estimate | [ | Normal, 3.93, 2.46 | |||
| Polemoniaceae | GTR+I+Γ | Ingroup | 41.3 - 91.2 | previous estimate | [ | Normal, 50, 5 |
| Giliae | 41.3 | fossil | [ | Lognormal, 41.3, 0, 1 | ||
| GTR+I+Γ | Ingroup | 25 | fossil | [ | Lognormal, 25, 0, 1 | |
| 11.61 - 3.6 | fossil | [ | Lognormal, 3.6, 2, 1 | |||
| 3.6 - 2.59 | fossil | [ | Lognormal, 2.69, 2, 1 | |||
| Saniculoideae | GTR+Γ | Ingroup | 33.7 - 69 | fossil and previous estimate | [ | Lognormal, 33.7, 2, 1 |
| 33.7 | fossil | [ | Lognormal, 33.7, 0, 1 | |||
| GTR+Γ | Ingroup | 34 - 69.7 | fossil and previous estimate | [ | Uniform, 34, 70 | |
| 34 | fossil | [ | Lognormal, 0, 1 | |||
*Values separated by commas represent the following parameters: Normal, mean, standard deviation (s.d.); Uniform, lower bound, upper bound; or Lognormal, zero offset, mean, s.d.
Units are in m.y. (millions of years) unless otherwise indicated.