2007 POINTS OF VIEW trees are binary, split fit is co-Pareto on components (Wilkinson et al., 2005a). When input trees have polytomies, an optimal splitfitsupertree could include arbitrary resolutions that do not contradict any displayed splits. In that case, split fit can fail to be co-Pareto (but not sub-Pareto) on components. In contrast, the corresponding strict consensus, the split fit* supertree, suppresses all arbitrary resolutions and must be co-Pareto on components. A method that is co-Pareto on components must also be co-Pareto (and sub-Pareto) on triplets and on nestings. Our example confirms that triplet fit is not co-Pareto on components. For example, of the 1677 triplet MRP supertrees, 339 include the component (DE). This is not present in either input tree but all the triplets that it entails are present in at least one of the input trees. It also confirms that that the MinCut methods are not co-Pareto on components 337 (Semple and Steel, 2000). For example, D and K are grouped together in the MinCut supertree (Fig. lc) and D and K nest within A-P in both input trees but they are not a component in either input tree (Fig. 1). Co-Pareto on triplets.—The triplet fit method is analogous to split fit, and by analogy we might expect that triplet fit* is co-Pareto and thus sub-Pareto on triplets, and that triplet fit is sub-Pareto on triplets and co-Pareto on triplets when input trees are binary (in which case there are no arbitrary resolutions). However, unlike full splits, combinations of displayed triplets can entail triplets that are not displayed. Thus, the analogy breaks down and there are, as yet, no proofs for any of these conjectures, which remain open problems. Similarly, quartet fit' is conjectured but has not been shown to be co-Pareto and sub-Pareto on quartets. Syst. Biol. 56(2):337-345,2007 Copyright © Society of Systematic Biologists ISSN: 1063-5157 print / 1076-836X online DOI: 10.1080/10635150701258795 Alarm Bells for the Molecular Clock? No Support for Ho et al.'s Model of Time-Dependent Molecular Rate Estimates BRENT C. EMERSON Centre for Ecology, Evolution and Conservation, School of Biological Sciences, University of East Anglia, Norwich NR4 7TJ, UK; E-mail: [email protected] In a recent paper, Ho etal. (2005) appear to have provided startling evidence for a relationship between the rate of molecular evolution and sampling time that they then describe with the fitting of vertically translated exponential decay curves. If correct, their results carry major implications for molecular evolutionary biology (Penny, 2005), and their work follows from the observed disparity between mitochondrial DNA (mtDNA) rate estimates directly measured from pedigree studies and those inferred from intraspecific and interspecific phylogenetic studies. A number of recent studies of control region mtDNA from detailed human pedigrees have reported exceptionally high estimates of mutation rate, summarized in Howell et al. (2003). Pooling data from two comparable Leber hereditary optic neuropathy studies (Howell et al., 1996,2003), Howell et al. (2003) obtained a pedigree divergence rate of 1.0 mutations/bp/Myr (mutations per base pair per million years) for the control region. Building on these data, Howell et al. (2003) also combined data from a number of unrelated pedigree studies (Bendall et al., 1996; Cavelier et al., 2000; Heyer et al., 2001; Howell et al., 1996, 2003; Mumm et al., 1997; Parsons and Holland, 1998; Parsons etal., 1997; Sigurdardottir etal., 2000; Soodyall etal., 1997) and obtained a broadly similar control-region pedigree divergence rate of 0.95 mutations/bp/Myr. Ho et al. (2005) point out that this value is vastly greater (approximately 50 x) than the phylogenetically derived divergence rate of approximately 0.02 mutations/bp/Myr for protein-coding mitochondrial DNA. However, it should be acknowledged that, as deduced from comparative phylogenetic studies, the control region evolves much faster than the protein-coding regions within human mitochondrial DNA. Thus, in real terms, pedigree mutation rates for the human mitochondrial control region appear to be approximately 5- to 10-fold higher than phylogenetically derived divergence rates of 0.087 to 0.236 mutations/bp/Myr (Hasegawa et al., 1993; Stoneking et al., 1992; Tamura and Nei, 1993). Although there are insufficient data to provide robust estimates on pedigree divergence rates for proteincoding regions of human mitochondrial DNA, Howell etal. (2003) have presented some suggestive data by pooling data from three studies (Cavelier et al., 2000; Howell etal., 1996, 2003), arriving at a divergence rate of 0.06 mutations/bp/Myr, approximately three times higher than the phylogenetic rate of 0.02 mutations/bp/Myr for protein-coding mitochondrial DNA (but note that Howell et al., 2003, incorrectly assert that the pedigree-derived estimate is approximately 30 times higher than the phylogenetic rate). Thus, bearing in mind the paucity of protein-coding pedigree data, current estimates place the mitochondrial DNA pedigree control region and protein-coding rates to be approximately 5 to 10 times and 3 times higher than their respective phylogenetic rates. To investigate further the transition between pedigree mutation rates and long-term mutation rates, Ho et al. (2005) have estimated rates of change (c.f. rate of divergence) from mitochondrial sequences of primate (protein-coding and control region) and avian (proteincoding) taxa and compared these rates in the context of 338 VOL. 56 SYSTEMATIC BIOLOGY the time points from which they were calibrated. In all three cases it was found that there was a measurable transition between the high, short-term (<2 Myr) and the low, long-term (>2 Myr) mutation rate. Furthermore, it was found that the relationship between the age of the calibration and the rate of change can be described by a vertically translated exponential decay curve. On the basis of their results, Ho et al. (2005) advocate that rate curves may be used for correcting divergence date estimates by taking the proposed rate decay into account. The results of Ho et al. (2005) have far-reaching implications for any study involving the use of intra- or interspecific sequence data on a timescale less than 2 Myr, so it is pertinent to assess their results critically. The robust nature of a study such as theirs relies primarily on four elements: (1) the reliability of the DNA sequence data, (2) the ability of the methodology to accurately estimate genetic divergence values, (3) the representative nature of the sampling, and (4) the accuracy and validity of the calibration points. If we accept at face value the sequence data obtained by Ho et al. (2005) from the published literature, we are left with distance estimation, representative sampling, and calibration as potential sources of error within the analyses of Ho et al. (2005). Here I provide a critical reanalysis of the data of Ho et al. (2005) in the context of these potential sources of error and demonstrate that, beyond the pedigree data summarized by Howell et al. (2003), there is no evidence for time dependency of molecular rate estimates. Similar to Ho et al. (2005), rates were estimated using Bayesian analysis as implemented in the program BEAST vl.3 (Drummond etal., 2002; Drummond and Rambaut, 2003) with a relaxed molecular clock. Analyses by Ho et al. (2005) were performed with an unreleased version of BEAST (Ho, personal communication) that allowed rates to vary throughout the tree in an autocorrelated manner, with the rate in each 0.20 TT branch being drawn from an exponential distribution whose mean was equal to the rate in its parent branch. BEAST vl.3 uses an uncorrelated model of rate change, and rates have been sampled from a lognormal distribution. Following a burn-in of 1,000,000 cycles, rates were sampled once every 500 cycles from 10,000,000 Markov chain Monte Carlo (MCMC) steps. I used the computer program Tracer vl.2.1 (Rambaut and Drummond, 2005) to ensure that (1) chains had converged to a stationary distribution and (2) effective sample sizes were greater than 100, as recommended (Drummond and Rambaut, 2003). ESTIMATION OF GENETIC DIVERGENCE The most extreme rate estimate Ho et al. (2005) obtained for primate protein-coding mtDNA comes from their reanalysis of cytochrome b (cytb) sequence data obtained for Mandrillus sphinx by Telfer etal. (2003) (Fig. 1). Using a calibration date of 0.8 Mya (million years ago) and applying Bayesian analysis with a relaxed clock model as implemented by the program BEAST, they obtained a mean mutation rate estimate of 0.116 mutations/bp/Myr. This is in fact a rather curious result. Ho et al. (2005) assert that, with three exceptions (chimpanzee-bonobo split, chimpanzee-human split, and Neandertals), calibration dates used in their study are based on either paleontological or biogeographical data. However, in the case of the mandrill data set, the calibration date of 0.8 Mya is not of paleontological or biogeographical origin. Rather, it is derived from Telfer et al. (2003) applying a phylogenetic nucleotide substitution rate estimate (0.035 mutations/bp/Myr) for silent sites within the primate cytb gene (Pesole et al., 1999) to their six haplotypes to obtain an age estimate for the most recent common ancestor (mrca) of M. sphinx. Ignoring the circularity in using a date derived from the 0.20 (a) 0.15 0.15 •0, o.io o O) c 0.10 0.05 0.05 (b) (0 o o a: o 10 15 20 25 30 35 40 o 10 o 15 20 o 25 o 30 35 40 Age of calibration (Myr) FIGURE 1. Estimated rate of change (in average nucleotide changes per site per million years) plotted against the date used to calibrate the estimate for mtDNA protein-coding genes of primate taxa for (a) Ho et al. (2005) and (b) this study. Data points represent the mean value, and error bars denote 95% credibility intervals. The open triangle represents cytb data for Mandrillus sphinx (Telfer et al., 2003). Open circles represent cytb data compiled by Ho et al. (2005) for the following divergences (from left to right): chimpanzee-bonobo, chimpanzee-human, gorilla-human, gibbon-hominidae, anthropoid-cercopithecoid, platyrrhine-catarrhine. Closed circles represent ND4 data compiled by Ho et al. (2005) for the following divergences (from left to right): chimpanzee-human, gorilla-human, orangutan-human, gibbon-hominidae, anthropoid-cercopithecoid, platyrrhine-catarrhine. The closed triangle represents the gorilla-human split (Horai et al., 1995). 2007 339 POINTS OF VIEW same molecular data, simply through applying Bayesian analysis with a relaxed clock model, Ho et al. (2005) have obtained a mutation rate estimate among M. sphinx sequences substantially higher than the rate estimate of Pesole et al. (1999). Given that all but one of the mandrill substitutions occur at silent sites, one would expect the rate estimate of Ho et al. (2005), estimated across all sites, to be lower than that of Pesole et al. (1999), which is estimated across only silent sites. That the rate estimate of Ho et al. (2005) is approximately three times higher than that of Pesole et al. (1999) suggests that this is an artefact of the Bayesian analysis. This discrepancy between rate estimates may be due to problems of parameter identifiability in the analysis of Ho et al. (2005) that used an autocorrelated relaxed clock. Unlike the uncorrelated model, the autocorrelated model requires a prior probability distribution (prior) on the rate at the root as well as a model of autocorrelated rate change. It is thus possible that there were simply too many parameters in the analysis, given the relatively low information content of the sequences (Ho, personal communication). Parameter nonidentifiability has the potential to confound rate estimates, and Sullivan et al. (1999) have previously demonstrated problems for parameter estimation related to the limited information content of sequences. For the mandrill analysis, as for all of their analyses, Ho et al. (2005) estimated rates using the HKY+F+I model (Hasegawa et al., 1985; Yang, 1994). Analysis of MCMC parameter estimates for kappa (transition/transversion bias), pinv (proportion of invariable sites), and alpha (the gamma-distribution shape parameter) reveal these to be distributed uniformly throughout the sampling interval, particularly for kappa and alpha, irrespective of the bounds placed upon the sampling interval. Although this may be largely inconsequential for rate estimates with regard to alpha and pinv, increased upper bounds for kappa can lead to increased rate estimates (personal observation). To avoid this problem, I used maximum likelihood estimates using PAUP* as initial values for parameters with lower and upper bounds of 80% and 120%, respectively, of their value. Within their original analysis, Telfer et al. (2003) used the simpler HKY model of sequence evolution (Hasegawa et al., 1985), and this is in fact the model of sequence evolution selected by the Akaike information criterion (AIC) for the mandrill sequence data using PAUP* v4.0bl0 (Swofford, 1988) in conjunction with Modeltest v3.7 (Posada and Crandall, 1998). The simpler but more appropriate HKY model of sequence evolution, with appropriate parameterization of kappa, yields a mutation rate estimate of 0.023 mutations/bp/Myr, a value not at odds with the traditional phylogenetic estimate. For all subsequent analyses I have used the model with the best AIC score for each data set as determined with ModelTest, with each parameter given lower and upper bounds of 80% and 120%, repectively, of the ML estimate of the initial value. One of the two extreme rate estimates Ho et al. (2005) obtained for primate noncoding mtDNA (0.37 mutations/bp/Myr) comes from their estimated mutation rate for the control region in an analysis comprising four contemporary human control region sequences and four Neandertal ancient DNA sequences, with the rate estimate calibrated using the radiocarbon dates of the Neandertal sequences. Repeating the analysis of Ho et al. (2005) highlights an error in tree estimation that compromises the estimation of substitution rate from this data set. Trees sampled from the post-burn-in chain are not rooted with Neandertals and humans as sister groups; instead a monophyletic group of human sequences is nested within paraphyletic Neandertal sequences. Neither constraining both clades to be monophyletic nor enforcing a strict clock resolved the problem. It would appear that the sampling dates from the Neandertal sequences are confounding the tree construction as the removal of these dates does result in reciprocal monophyly for both groups. Here I have undertaken a two-stage analysis of the same sequence data set as Ho et al. (2005) to obtain a control region mutation rate specific for Neandertals. In a first analysis I have derived an estimate for the age of the mrca of the four Neandertals. In a second analysis I have used this age to estimate the mutation rate for the control region within Neandertals. Age Estimate for the Neandertal Mrca To estimate the age of the mrca of Neandertals, I have included the four Neandertal sequences and sequences from human, chimpanzee, and gorilla, with the appropriate sampling dates applied for each of the sequences, and using the HKY mutation model. Inspection of tree files from an initial analysis revealed that the majority of topologies were incorrect, often to an alarming degree (e.g., Neandertals branching off basally, resulting in greatly inflated estimates of mutation rate). Thus, for a subsequent analysis, I imposed monophyly constraints for (1) the four Neandertal sequences; (2) Neandertals and humans; and (3) Neandertals, humans, and chimps. Age constraints from the fossil record were also incorporated. The calibration age used by Ho et al. (2005) for the split between the gorilla lineage and the lineage giving rise to the other three taxa is 7.5 Myr, so I have constrained the root to be no older than 8 Myr. The calibration age used by Ho et al. (2005) for the split between the chimpanzee lineage and the human lineage is 5 Myr, so I have constrained the age of this node to be between 4 and 6 Myr. Additionally I have constrained the age of the human-Neandertal split to be no older than the 620 kya (thousand years ago) age estimate of Krings et al. (1997). Other age estimates exist (Krings et al., 1999; Ovchinnikov et al., 2000), but that of Krings et al. (1997) is the oldest, and thus most conservative for a Neandertal control region rate estimate. No minimum age constraint was imposed for this node, and a starting tree compatible with the constraints was used. The age estimate for the Neandertal mrca from this analysis is 295 kya. Estimated Mutation Rate for Neandertal Control Region I performed two analyses to estimate the mutation rate for a data set comprising the four Neandertal control 340 SYSTEMATIC BIOLOGY VOL. 56 data as it incorporates all calibration points, including the more important 1.5 Mya. Pan paniscus-Pan troglodytes data point not included in the ND4 data set. I have parameterized the analysis using the best-fit model for the primate cytb data set (GTR+F+I model) and constrained the analysis so that for each of the calibration points, the group of taxa associated with the calibration point is monophyletic. It is clear from Figure 1 that, with a more rigorous analytical approach, the trend described by Ho et al. (2005) no longer exists for primate protein-coding mitochondrial DNA. The curvilinear relationship described by Ho et al. (2005) for avian protein-coding mtDNA sequence data is essentially driven by nine data points with calibrations of 1 Myr or less. Among these nine data points there are four phylogenetically independent divergence events for three geologically independent calibration points. Eight of the nine data points come from a study of Indian Ocean sunbirds by Warren et al. (2003) where data from three mitochondrial gene regions (ATPase6, cytb, and ND4) were analyzed using a combined data approach to construct phylogenetic relationships. Warren et al. (2003) identify three nodes from their phylogeny that can be used as calibration points, and these are used in the reanalysis of Ho et al. (2005). However, Ho et al. (2005) have converted these three nodes into eight data points by analyzing the three mitochondrial regions individually. Given the obvious linkage between these three mitochondrial genes, and the fact that the same individual birds were sequenced for each region, phylogenetic independence is compromised. Here, I have analyzed these three divergence events using a combined data approach (Fig. 2). The remaining data point of 1 Myr or less comes from Krajewski and King's (1996) phylogenetic analysis of cranes. Krajewski and King (1996) identify four calibration points encompassing nine phylogenetically independent diversification events. Ho et al. (2005) have sampled only four of these nine calibration points, but here I include all nine, which includes an additional data point of 1 Myr or less. Additional calibration points of 1 Myr or less exist within the data set of Fleischer et al. (1998) but were not analyzed by Ho et al. (2005).. Fleischer et al. (1998) present molecular phylogenetic data for the drepanidines of the Hawaiian Islands and illustrate an apparent relationship between separation time and molecular divergence for three calibration points derived from the geological ages REPRESENTATIVE SAMPLING of the Hawaiian Islands. Ho et al. (2005) incorporate only In addition to the Mandrillus sphinx data set, Ho et al. two of these calibration points when in fact a total of (2005) have used seven hominid calibrations for their pri- five can be identified using the criteria of Fleischer et al. mate protein-coding analyses. Some of these are from the (1998). The additional two are (1) the Kauai and Hawaii fossil record, whereas others are derived from molecu- akepa split and (2) the Kauai and Oahu/Maui/Hawaii lar data combined with paleontological estimates. Most amakihi split. Here I include all five calibration points, of these calibration points are represented by two mi- which include two additional data points of 1 Myr or tochondrial genes, cytb and ND4, for the same lineage less. Additional avian mtDNA data calibration points, divergence event, but given the linkage of these genes all greater than 10 Myr, come from Randi's (1996) phythere is an inherent lack of phylogenetic independence. logenetic analysis of Alectoris partridges and Nunn and Thus, a more appropriate strategy is for either the analy- Stanley's (1998) study of tube-nosed seabirds. As with sis of a single region, or the combination of both mtDNA the other analyses, I have parameterized with the approprotein-coding regions. Here, I have analyzed the cytb priate mutation model and the necessary monophyly region sequences and using the HKY model. For the first analysis I circumvented using the sampling ages associated with the sequences by reducing the age of the mrca to 253 kya. This treats the Neandertal sequences as if they had been sampled contemporaneously by reducing the age of the mrca by the maximum sampling age of the sequences. This will, if anything, provide an overestimate of the mutation rate because whereas two of the sequences have sampling dates of 42 kya, the other two sequences have sampling dates of 40 kya and 29 kya. This analysis gave an estimated mutation rate of 0.05 mutations/bp/Myr, a value compatible with traditional phylogenetic estimates. For the second analysis, I incorporated the sampling ages for each of the sequences and obtained a mutation rate estimate of 0.79 mutations/bp/Myr, a value more than 10 times higher than the previous estimate. The only sensible explanation for the much higher rate estimate when sampling dates are incorporated is that, rather than reflecting the time dependency of the control-region mutation rate, it is an artefact resulting from a limitation with incorporating noncontemporaneous sequence samples for BEAST analyses. Repeating the analysis of the human-Neandertal sequence data set with the mutation parameters of Ho et al. (2005), I arrived at an even higher rate estimate (1.98 mutations/bp/Myr) and could only obtain a value close to the published estimate (0.37 mutations/bp/Myr) by placing an upper bound on the mutation rate so that it did not exceed the pedigree rate estimate of Howell et al. (2003; 0.475 mutations/bp/Myr). It would appear that the rate estimate obtained by Ho et al. (2005) is flawed, due primarily to a problem associated with the BEAST software for the analysis of non-contemporaneous sequence samples. For all subsequent analyses, I have enforced monophyly constraints such that a group of taxa associated with the calibration point is monophyletic. This appears to be a critical constraint, as BEAST does not require a user-specified tree topology (Drummond and Rambaut, 2003), and if trees are sampled where the group of interest is not monophyletic, this will result in exaggerated rate estimates. This problem was particularly apparent for the primate control region data, where sampled trees in the absence of monophyly constraints were often topologically incorrect. 2007 POINTS OF VIEW 20 Age of calibration (Myr) FIGURE 2. Estimated rate of change (in average nucleotide changes per site per million years) plotted against the date used to calibrate the estimate for mtDNA protein-coding genes of avian taxa for (a) Ho et al. (2005) and (b) this study. Data points represent the mean value, and error bars denote 95% credibility intervals, (a) Open circles, grey filled circles, and filled circles represent cytb, ATPase6, and ND4 divergences, respectively, among sunbirds of the Indian Ocean (Warren et al., 2003). In (b) these data have been combined and are represented by open circles. Open diamonds represent cytb divergences among Hawaiian drepanidines (Fleischer et al., 1998). Filled triangles represent cytb divergences among cranes (Krajewski and King, 1996). The open triangle represents the divergence between chickens and partridges (Randi, 1996). Filled diamonds represent divergences within the Procellariiformes (Nunn and Stanley, 1998). constraints have been applied. Although two out of seven rate reestimates generated from recent time points are notably higher than the rest (Fig. 2), both can be adequately explained without recourse to arguments of time dependency. Assumption 3: Divergence Events Do Not Predate Island Ages Two phenomena can lead to the violation of this assumption, and thus the overestimation of mutation rate estimates. The first involves population genetic variation within the ancestral island population (Fig. 3). If CALIBRATION ACCURACY haplotype and nucleotide diversity are appreciable in The two high avian rate estimates come from the In- the ancestral population, then the greater is the probdian Ocean island archipelago-based analysis of Warren ability that the gene coalescent time between descenet al. (2003), who expand on the work of Fleischer et al. dent lineages on different islands predates the island (1998) to identify eight assumptions, which when vio- age. This may be controlled for by using contemporary lated will lead to incorrect rate estimates when dating intra-specific levels of variation as a proxy (Wilson et al., nodes from island ages. Excluding assumptions regard- 1985), but sampling in the sunbird and drepanidine studing lineage rate variation and branch length estimation, ies is not adequate to do this. Importantly, the inflation two of these assumptions, and an additional assumption of the rate estimate due to ancestral population variation (Emerson, 2002), will lead to elevated rate estimates if will be greater for more recent time points. The second they are violated. phenomenon that can lead to overestimation of mutation rate estimates is lineage extinction (Fig. 4), and island archipelagos are perhaps the one system where the Assumption 1: K-Ar Dates of Earliest Subaerial Lavas and pervasive role of extinction has been best documented Island Ages Are Correctly Estimated (e.g., Emerson, 2003; Emerson and Kolm, 2005; Emerson Clearly, if island ages are underestimated, this will lead and Oromi, 2005; Gillespie, 2004; MacArthur and Wilson, to an overestimation of mutation rate estimates. 1967; Ricklefs and Bermingham, 2001). Given these assumptions, it seems unlikely that the Assumption 2: Subaerial Lavas Representing the First two high rate estimates reflect a general trend of time Emergence of the Island above Sea Level Are Accessible to dependency for molecular rate estimates, particularly so Geologists and Have Not Been Deeply Buried by More when five other rate estimates for time points of 1 Myr Recent Strata or less do not deviate from rate estimates generated from Similar to assumption 1, if the earliest lavas are buried, older time points. The final extreme rate estimate presented by Ho et al. then island ages will be underestimated, leading to an overestimation of mutation rate estimates. Recent arthro- (2005) comes from an analysis of Amerindian control repod analyses on the Canary Islands have demonstrated gion sequences from the Nuu-Chah-Nulth tribe (Kolman the use of molecular phylogenetic data to corroborate et al., 1995; Ward et al., 1991). For their analysis, Ho geological speculation of older lavas lying hidden be- et al. (2005) have calibrated the mrca of this sequence data set with a date of 24,000 years, representing the neath younger terrain (Emerson et al., 2006). 342 SYSTEMATIC BIOLOGY Divergence predates colonisation VOL. 56 Simultaneous colonisation and divergence ' divergence • colonisation colonisation < time divergence < source island colonised island source island colonised island FIGURE 3. Ancestral population genetic variation, island colonization, speciation, and genetic divergence. In the first diagram, the two contemporary taxa carry alleles that diverged prior to island colonization, and this would lead to the overestimation of mutation rate by calibrating with the age of the colonized island. In the second diagram, genetic divergence is coincident with island colonization. The potential effect of ancestral population genetic variation on the overestimation of mutation rate is greater for more recent colonization events. Moheli Moheli Moheli 1 t (a) I Grande Comore 1 Grande Comore Madagascar Madagascar Africa •Africa Africa •Africa Grande Comore Grande Comore (b) I Madagascar • Madagascar Africa Africa Africa Africa j Moheli 1 Moheli Moheli I Anjouan J* I Anjouan (c) I Grande Comore • Grande Comore Madagascar Madagascar Africa Africa Africa -Africa FIGURE 4. Lineage extinction and incomplete sampling of extant taxa are important considerations when estimating the ages of colonization events from a molecular phylogeny. (a) Phylogenetic relationships among island subspecies oiNectarinia notata and mainland species of Nectarinia (modified from Warren et al., 2003). The filled circle denotes the node assigned an age of 0.5 Myr for calibrating the divergence between the Moheli and Grande Comore subspecies, under the assumption that the youngest island of Grande Comore (maximum age 0.5 Myr) is the most recently colonized, (b) In the event of the extinction of the subspecies on Moheli, the same calibration strategy would result in an overestimate of the substitution rate, (c) An extinct sister taxa of the Gran Comore subspecies (in this case a hypothetical species on Anjouan) would lead to an overestimate of the substitution in (a). 2007 POINTS OF VIEW 30 0 5 10 15 20 25 Age of calibration (Myr) FIGURE 5. Estimated rate of change (in average nucleotide changes per site per million years) plotted against the date used to calibrate the estimate for mtDNA control region sequences of primate taxa for (a) Ho et al. (2005) and (b) this study. Data points represent the mean value, and error bars denote 95% credibility intervals. Open circles represent data compiled by Ho et al. (2005) for the following divergences (from left to right): Neandertals, chimpanzee-bonobo (represented twice), chimpanzee-human, orangutan-human, anthropoid-cercopithecoid. The closed circle represents data for Amerindians (Ward et al., 1991). The filled triangle represents an additional estimate for the chimpanzee-human divergence (Vigilant et al., 1991). The open triangle represents the gorilla-human divergence taken from the data of Ho et al. (2005). The pedigree estimate of Howell et al. (2003) has been excluded. 2003) compared with the more moderate mutation rates typically inferred from phylogenetic studies. This begs the question of when the apparent high rate estimate derived from pedigree data falls to a level compatible with traditional phylogenetic estimates, and this is a fundamentally important question for molecular evolutionary biologists. Ho et al. (2005) have presented data suggesting that for time points up to 2 Mya, rate estimates may be inflated above traditionally held values, but analyses presented here leave little, if any, cause for concern. That is not to say that the phenomenon that Ho et al. (2005) have attempted to address is neither an important nor interesting one. However, it would seem likely that the time-scale upon which the pedigree rate converges to the evolutionary rate is very much shorter than the timescale Ho et al. (2005) have focused on, and it is debatable whether this convergence would follow an exponential distribution, or if such a pattern existed, whether it could not be equally explained by coalescent effects. The present study does highlight some concerns with the use of Metropolis-Hastings Markov chain Monte Carlo (MCMC) integration to estimate both mutation rates and divergence dates. Several factors can lead to the exaggeration of mutation rate and divergence date estimates. Adequate parameterization is clearly needed, particularly when divergences between sequences are low (personal observation), and care must be taken to ensure that sampled trees are not at odds with the specific hypotheses being tested. Finally, the incorporation of noncontemporaneously sampled sequences in the analyses conducted here has also led to erroneous results. The findings presented here carry implications for recent studies, many of which incorporate ancient DNA sequences, where MCMC integration has been carCONCLUSIONS ried out for the estimation of divergence dates (e.g., Studies based on pedigree data have produced re- Bunce et al., 2003; Weinstock et al., 2005), mutation rates markably high estimates of mutation rate (Howell et al., (e.g., Lambert et al., 2002; Ritchie et al., 2004; Shapiro midpoint between the estimates of 15,000 (Morrell, 1990) and 33,000 (Dillehay and Collins, 1988) years for the entrance of humans into the Americas. The flaw in the analysis of this data point is that it assumes that NuuChah-Nulth tribe mtDNA diversity is derived from a single founding mitochondrial lineage. This is clearly not the case, as Nuu-Chah-Nulth haplotypes are not monophyletic when placed in reference to other mtDNA sequences from outside the Americas. In their original paper, Ward et al. (1991) pointed out that the magnitude of sequence divergence within the Nuu-Chah-Nulth suggests that the origin of this diversity predates the entry of humans into the Americas. The Nuu-Chah-Nulth are genetically quite diverse, representing much of the genetic diversity present across both Amerind and Na-Dene tribes (Kolman et al., 1995), which belongs to four founding haplotypes groups (Schurr, 2004). As such, there is no reliable date for calibrating the mrca of this data set and it must be removed from the analysis. For the remaining control region rate estimates (Fig. 5), I have used the same sequence data as Ho et al. (2005) and the same calibration points, with one exception. The deep time point of 25.85 Myr representing the anthropoidcercopithecoid split has been removed (the age of this event is clearly outside of the time frame for which the control region can be considered phylogenetically useful) and the more recent time point of 7.5 Myr representing the split between the gorilla lineage and the chimpanzee/human lineage has been added. It is clear from Figure 5 that with a more rigorous analytical approach the trend described by Ho et al. (2005) no longer exists for primate noncoding mitochondrial DNA. 344 SYSTEMATIC BIOLOGY VOL. 56 Horai, S., K. Hayasaka, R. Kondo, K. Tsugane, and N. Takahata. 1995. Recent african of modern humans revealed by complete sequences of hominid mitochondrial DNAs. Proc. Natl. Acad. Sci. USA 92:532536. Howell, N., I. Kubacka, and D. A. Mackey. 1996. How rapidly does the ACKNO WLEDG EMENTS human mitochondrial genome evolve? Am. J. Hum. Genet. 59:501509. I would like to thank Tammy Steeves, Melanie Pierson, and Neil Gemmell for stimulating discussion and helpful comments on an ear- Howell, N., C. B. Smejkal, D. A. Mackey, P. F. Chinnery, D. M. Turnball, and C. Herrnstadt. 2003. The pedigree rate of sequence divergence lier version of the manuscript, and two anonymous referees and Simon in the human mitochondrial genome: There is a difference between Ho for helpful comments and suggestions. Particular thanks to Simon phylogenetic and pedigree rates. Am. J. Hum. Genet. 72:659-670. Ho for providing additional detail not contained within the original manuscript. Thank you also to Neil Gemmell and the University of Kolman, C. J., E. Bermingham, R. Cooke, R. H. Ward, T. D. Arias, and F. Guionneau-Sinclair. 1995. Reduced mtDNA diversity in the Ngobe Canterbury for providing office space and facilities during a sabbatical Amerinds of Panama. Genetics 140:275-283. visit. Krajewski, C, and D. G. King. 1996. Molecular divergence and phylogeny: Rates and patterns of cytochrome b evolution in cranes. Mol. REFERENCES Biol. Evol. 13:21-30. Bendall, K. E., V. A. Macaulay, J. R. Baker, and B. C. Sykes. 1996. Hetero- Krings, M., H. Geisert, R. W. Schmitz, H. Krainitzki, and S. Paabo. 1999. DNA sequence of the mitochondrial hypervariable region II from thje plasmic point mutations in the human mtDNA control region. Am. et al., 2004), and demography (e.g., Biek et al., 2006; Drummond et al., 2005), and these may need to be reevaluated. J. Hum. Genet. 59:1276-1287. neandertal type specimen. Proc. Natl. Acad. Sci. USA 96:5581-5585. Biek, R., A. J. Drummond, and M. Poss. 2006. A virus reveals popula- Krings, M., A. C. Stone, R. W. Schmitz, H. Krainitzki, M. Stoneking, tion structure and recent demographic history of its carnivore host. and S. Paabo. 1997. Neandertal DNA sequences and the origin of Science 311:538-541. modern humans. Cell 90:19-30. Bunce, M., T. H. Worthy, T. Ford, W. Hoppitt, E. Willerslev, A. J. Drum- Lambert, D. M., P. A. Ritchie, C. D. Millar, B. Holland, A. J. Drummond, mond, and A. Cooper. 2003. Extreme reversed sexual size dimorand C. Baroni. 2002. Rates of evolution in ancient DNA from Adelie phism in the extinct New Zealand moa Dinornis. Nature 425:172-175. penguins. Science 295:2270-2273. Cavelier, L., E. Jazin, P. Jalonen, and U. Gyllensten. 2000. MtDNA sub- MacArthur, R. H., and E. O. Wilson. 1967. The theory of island biogeogstitution rate and segregation of heteroplasmy in coding and nonraphy. Princeton University Press, Princeton, New Jersey. coding regions. Hum. Genet. 107:45-50. Morrell, V. 1990. Confusion in earliest America. Science 248:439-441. Dillehay, T. D., and M. B. Collins. 1988. Early cultural evidence from Mumm, S., M. P. Whyte, R. V. Thakker, K. H. Buetow, and D. Schlessinger. 1997. MtDNA analysis shows common ancestry in two Monte-Verde in Chile. Nature 332:150-152. kindreds with X-linked recessive hypoparathyroidism and reveals a Drummond, A. J., G. K. Nicholls, A. G. Rodrigo, and W. Solomon. 2002. Estimating mutation parameters, population history and geheteroplasmic silent mutation. Am. J. Hum. Genet. 60:153-159. nealogy simultaneously from temporally spaced sequence data. Ge- Nunn, G. B., and S. E. Stanley. 1998. Body size effects and rates of netics 161:1307-1320. cytochrome b evolution in tube-nosed seabirds. Mol. Biol. Evol. 15:1360-1371. Drummond, A. J., and A. Rambaut. 2003. BEAST, version 1.3. Oxford Ovchinnikov, I. V, A. Gotherstrom, G. P. Romanova, V. M. Kharitonov, University Press, Oxford, UK. K. Liden, and W. Goodwin. 2000. Molecular analysis of Neanderthal Drummond, A. J., A. Rambaut, B. Shapiro, and O. G. Pybus. 2005. DNA from the northern Caucasus. Nature 404:490-493. Bayesian coalescent inference of past population dynamics from Parsons, T. J., and M. M. Holland. 1998. Mitochondrial mutation rate molecular sequences. Mol. Biol. Evol. 22:1185-1192. revisited: Hotspots and polymorphism. Nat. Genet. 18:110. Emerson, B. C. 2002. Evolution on oceanic islands: Molecular phylogeneric approaches to understanding pattern and process. Mol. Ecol. Parsons, T. J., D. S. Muniec, K. Sullivan, N. Woodyatt, R. Alliston11:951-966. Grenier, M. R. Wilson, D. L. Berry, K. A. Holland, V. W. Weedn, P. Emerson, B. C. 2003. Genes, geology and biodiversity: Faunal and floral Gill, and M. M. Holland. 1997. A high observed substitution rate in diversity on the island of Gran Canada. Anim. Biodivers. Conserv. the human mitochondrial DNA control region. Nat. Genet. 15:363368. 26:9-20. Emerson, B. C, S. Forgie, S. L. Goodacre, and P. Oromi. 2006. Testing Penny, D. 2005. Evolutionary biology—Relativity for molecular clocks. phylogeographic predictions on an active volcanic island: BrachyNature 436:183-184. deres rugatus (Coleoptera: Curculionidae) on La Palma (Canary Is- Pesole, G., C. Gissi, A. De Chirico, and C. S. Saccone. 1999. Nucleotide lands). Mol. Ecol. 15:449^58. substitution rate of mammalian mitochondrial genomes. J. Mol. Evol. 48:427-343. Emerson, B. C, and N. Kolm. 2005. Species diversity can drive speciaPosada, D., and K. A. Crandall. 1998. ModelTest: Testing the model of tion. Nature 434:1015-1017. DNA substitution. Bioinformatics 14:817-818. Emerson, B. C, and P. Oromi. 2005. Diversification of the forest beetle genus Tarphius on the Canary Islands, and the evolutionary origins Rambaut, A., and A. J. Drummond. 2005. Tracer, version 1.2.1. of island endemics. Evolution 59:586-598. Randi, E. 1996. A mitochondrial cytochrome b phylogeny of the alecFleischer, R. C, C. E. Mclntosh, and C. L. Tarr. 1998. Evolution on a toris partridges. Mol. Phylogenet. Evol. 6:214-227. volcanic conveyor belt: using phylogenetic reconstructions and K- Ricklefs, R. E., and E. Bermingham. 2001. Nonequilibrium diversity Ar-based ages of the Hawaiian Islands to estimate molecular evoludynamics of the Lesser Antillean avifauna. Science 294:1522-1524. tionary rates. Mol. Ecol. 7:533-545. Ritchie, P. A., C. D. Millar, G. C. Gibb, C. Baroni, and D. M. Lambert. Gillespie, R. G. 2004. Community assembly through adaptive radiation 2004. Ancient DNA enables timing of the Pleistocene origin and in Hawaiian spiders. Science 303:356-359. Holocene expansion of two Adelie penguin lineages in Antarctica. Hasegawa, M., A. DiRenzo, T. D. Kocher, and A. C. Wilson. 1993. ToMol. Biol. Evol. 21:240-248. ward a more accurate estimate for the human mitochondrial DNA Schurr, T. G. 2004. The peopling of the New World: Perspectives from tree. J. Mol. Evol. 37:347-354. molecular anthropology. Annu. Rev. Anthropol. 33:551-583. Hasegawa, M., H. Kishino, and T. Yano. 1985. Daring of the human-ape Shapiro, B., A. J. Drummond, A. Rambaut, M. C. Wilson, P. E. Matheus, splitting by a molecular clock of mitochondrial DNA. J. Mol. Evol. A. V. Sher, O. G. Pybus, M. T. P. Gilbert, I. Barnes, J. Binladen, E. 22:160-174. Willerslev, A. J. Hansen, G. F. Baryshnikov, J. A. Burns, S. Davydov, Heyer, E., E. Zietkiewicz, A. Rochowski, V. Yotova, J. Puymirat, and D. J. C. Driver, D. G. Froese, C. R. Harington, G. Keddie, P. Kosintev, Labuda. 2001. Phylogenetic and familial estimates of mitochondrial M. L. Kunz, L. D. Martin, R. O. Stephenson, J. Storer, R. Tedford, S. substitution rates: Study of control region mutations in deep-rooting Zimov, and A. Cooper. 2004. Rise and fall of the Beringian steppe pedigrees. Am. J. Hum. Genet. 69:1113-1126. bison. Science 306:1561-1565. Ho, S. Y. W., M. J. Phillips, A. Cooper, and A. J. Drummond. 2005. Time Sigurdardottir, S., A. Helgason, J. R. Gulcher, K. Stefansson, and P. dependency of molecular rate estimates and systematic overestimaDonnelly. 2000. The mutation rate in the human mtDNA control tion of recent divergence times. Mol. Biol. Evol. 22:1561-1568. region. Am. J. Hum. Genet. 66:1599-1609. 2007 POINTS OF VIEW 345 Soodyall, H., T. Jenkins, A. Mukherjee, E. Du Toit, D. F. Roberts, and Ward, R. H., B. L. Frazier, K. Dew-Jager, and S. Paabo. 1991. Extensive M. Stoneking. 1997. The founding mitochondrial DNA lineages of mitochondrial diversity within a single Amerindian tribe. Proc. Natl. Tristan da Cunha. Am. J. Phys. Anthropol. 104:167-175. Acad. Sci. USA 88:8720-8724. Stoneking, M., S. T. Sherry, A. J. Redd, and L. Vigilant. 1992. New ap- Warren, B. H., E. Bermingham, R. C. J. Bowie, R. P. Prys-Jones, and C. proaches to dating suggest a recent age for the human mtDNA anThebaud. 2003. Molecular phylogeography reveals island colonizacestor. Philos. Trans. R. Soc. Lond. Ser. B Biol. Sci. 337:167-175. tion history and diversification of western Indian Ocean sunbirds Sullivan, J., D. L. Swofford, and G. J. P. Naylor. 1999. The effect of taxon (Nectarinia: Nectariniidae). Mol. Phylogenet. Evol. 29:67-85. sampling on estimating rate heterogeneity parameters of maximum- Weinstock, J., E. Willerslev, A. Sher, W. Tong, S. Y. W. Ho, D. Rubenstein, likelihood models. J. Mol. Evol. 16:1347-1356. J. Storer, J. Burns, L. Martin, C. Bravi, A. Prieto, D. Froese, E. Scott, L. Xulong, and A. Cooper. 2005. Evolution, systematics, and phySwofford, D. 1988. PAUP*. Phylogenetic analysis using parsimony logeography of Pleistocene horses in the new world: A molecular (*and other methods). Version 4. Sinauer Associates, Sunderland, perspective. PLoS Biol. 3:e241. Massachussetts. Tamura, K., and M. Nei. 1993. Estimation of the number of nucleotide Wilson, A. C, R. L. Cann, S. M. Carr, M. George, U. Gyllensten, et al. substitutions in the control region of mitochondrial DNA in humans 1985. Mitochondrial DNA and two perspectives on evolutionary geand chimpanzees. Mol. Biol. Evol. 10:512-526. netics. Biol. J. Linn. Soc. 26:375-400. Telfer, P. T., S. Souquiere, S. L. Clifford, K. A. Abernethy, M. W. Bruford, Yang, Z. 1994. Maximum likelihood phylogenetic estimation from T. R. Disotell, K. N. Sterner, P. Roques, P. A. Marx, and E. J. Wickings. DNA sequences with variable rates over sites: Approximate meth2003. Molecular evidence for deep phylogenetic divergence in Manods. J. Mol. Evol. 39:306-314. drillus sphinx. Mol. Ecol. 12:2019-2024. Vigilant, L., M. Stoneking, H. Herpending, K. Hawkes, and A. C. First submitted 6 March 2006; reviews returned 6 June 2006; final acceptance 28 September 2006 Wilson. 1991. African populations and the evolution of human mitochondrial DNA. Science 253:1503-1507. Associate Editor: Jack Sullivan Syst. Biol. 56(2):345-355,2007 Copyright © Society of Systematic Biologists ISSN: 1063-5157 print / 1076-836X online DOi: 10.1080/10635150701286549 Seeing the Trees for the Network: Consensus, Information Content, and Superphylogenies OLIVIER GAUTHIER AND FRANCOIS-JOSEPH LAPOINTE Departement de sciences biologiques, Universite de Montreal, C.P. 6128, Succursale Centre-Ville, Montreal (Quebec) H3C 3J7, Canada; E-mail: [email protected];[email protected] Phylogenetic inference often leads to solutions made up of multiple trees on a given set of leaves or taxa. These competing hypotheses might be the equally optimal trees obtained from the analysis of a single matrix using maximum parsimony (Hennig, 1979) or maximum likelihood (Felsenstein, 1981) or the set of most probable trees produced by Bayesian analysis (Rannala and Yang, 1996; Larget and Simon, 1999; Mau et al., 1999). They might also have been inferred independently from different data sets or even be the result of resampling methods such as the bootstrap or the jackknife (Felsenstein, 1985; Penny and Hendy, 1985, 1986). Consensus methods are commonly used to identify areas of conflict and agreement among such multiple trees; they can represent the relationships that are supported either unanimously or by a majority of trees while discarding other, less supported relationships (Bryant, 2003). Thus, a consensus method is usually defined as a function that takes as input a set, or profile, of trees on the same set of taxa and returns a single tree on the same set of taxa (Leclerc and Cucumel, 1987; Steel et al., 2000; Bryant, 2003). This function can take different forms, and many consensus methods have been proposed (see Swofford, 1991; Bryant, 2003, for reviews), amongst which the strict consensus (Sokal and Rohlf, 1981) and majority-rule consensus (Margush and McMorris, 1981) are perhaps the most widely used and understood. These various functions differ in two major respects: (1) the kind of information they preserve and (2) the way they deal with conflict among input trees. Indeed, the information contained in a tree can be considered in terms of nesting, three- or four-taxon statements, components, and branch lengths, while conflict can be left unresolved or dealt with using different criteria (Bryant, 2003). Notwithstanding these differences, most methods abide to the prevailing phylogenetic model: that of a tree embedding a hierarchy of descent. This model puts forward a fully resolved, or binary, tree as the ideal representation of evolution. In practice, consensus trees are seldom binary and they embed—i.e., are compatible with—multiple binary trees. Indeed, because it is often impossible to distinguish between hard and soft polytomies (Nelson and Platnick, 1980; Maddison, 1989) and because the latter can be resolved in a number of different ways, an unresolved tree can be refined by a set of binary trees
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