| Literature DB >> 28449025 |
Jesus Lozano-Fernandez1,2, Mario Dos Reis3, Philip C J Donoghue1, Davide Pisani1,2.
Abstract
Establishing an accurate timescale for the history of life is crucial to understand evolutionary processes. For this purpose, relaxed molecular clock models implemented in a Bayesian MCMC framework are generally used. However, these methods are time consuming. RelTime, a non-Bayesian method implementing a fast, ad hoc, algorithm for relative dating, was developed to overcome the computational inefficiencies of Bayesian software. RelTime was recently used to investigate the timing of origin of animals, yielding results consistent with early strict clock studies from the 1980s and 1990s, estimating metazoans to have a Mesoproterozoic origin-over a billion years ago. RelTime results are unexpected and disagree with the largest majority of modern, relaxed, Bayesian molecular clock analyses, which suggest animals originated in the Tonian-Cryogenian (less that 850 million years ago). Here, we demonstrate that RelTime-inferred divergence times for the origin of animals are spurious, a consequence of the inability of RelTime to relax the clock along the internal branches of the animal phylogeny. RelTime-inferred divergence times are comparable to strict-clock estimates because they are essentially inferred under a strict clock. Our results warn us of the danger of using ad hoc algorithms making implicit assumptions about rate changes along a tree. Our study roundly rejects a Mesoproterozoic origin of animals; metazoans emerged in the Tonian-Cryogenian, and diversified in the Ediacaran, in the immediate prelude to the routine fossilization of animals in the Cambrian associated with the emergence of readily preserved skeletons.Entities:
Keywords: Bayesian relaxed-clock methods; RelTime; animal evolution; fossil calibrations; molecular clocks
Mesh:
Year: 2017 PMID: 28449025 PMCID: PMC5447329 DOI: 10.1093/gbe/evx079
Source DB: PubMed Journal: Genome Biol Evol ISSN: 1759-6653 Impact factor: 3.416
F—(a) RelTime-inferred relative divergence times versus Bayesian relative divergence times estimated in this study under the autocorrelated, relaxed, CIR clock model. (b) Relative divergence times estimated in this study under the autocorrelated, relaxed, CIR clock model versus absolute divergence times re-estimated under the 24 fossil calibrations and root age prior of (Erwin et al. 2011). The red line connects the maximum and minimum values on the scatter plot. (c) Relative node ages versus the corresponding relative branch rates estimated using RelTime. The red line indicates the relative depth in the animal phylogeny after which all Reltime-inferred relative rates are assigned the same, constant rate. The rates assigned to branches deeper than the red line in Panel C are equal to one, which is the median rate for the dataset. (d) Relative node ages versus corresponding relative branch rates estimated using Bayesian inference under the autocorrelated, relaxed, CIR clock model. Under the CIR model branch rates vary along the entire tree. (e) Node ages versus SE for RelTime-inferred relative rates of evolution. (f) Relative nodes ages versus SE for Bayesian relative divergence times inferred using the CIR clock. SE, standard error. Scatter plots have been generated in R. In all panels (a–f), the values of R2 (the square of the linear correlation coefficient) are given. RelTime values have been normalised to one.
F—A graphical representation of how RelTime-inferred relative rates change along the phylogeny. This figure illustrates that all rate changes inferred by RelTime for nonterminal branches but one are rate accelerations that happened towards the tips of the tree. Reltime effectively assumes clock-like evolution across the deep branches of the Opisthokonta.
Summary of the Bayesian Analyses Carried Out Using Two Sets of Fossil Calibrations
| Calibration Set | Substitution Model | Clock Model | Number of Calibrations | Root age Calibration | Soft Bound |
|---|---|---|---|---|---|
| Erwin | CAT-GTR+G | CIR | 24 | Gamma with mean=1,000 Ma and SD = 100 Myr | 5% |
| Battistuzzi | CAT-GTR+G | CIR | 22 | Exponential* with mean=1,000 Ma | 5% |
Note.—Legend: 24 = The original 24 calibration set of Erwin et al. (2011). These calibrations are available, with their palaeontological justifications, in table S4 of the original study of Erwin et al. (2011). 22 = The calibration set used by Battistuzzi et al. (2015) and composed of all the calibrations of Erwin et al. (2011) with the exclusion of two that Battistuzzi et al. (2015) deemed to be flawed following their RelTime analysis. Excluded calibrations are: (1) The soft maximum on the crown Demospongiae, set by Erwin et al. (2011) to 713 Ma based on molecular biomarker evidence (Love et al. 2009; Sperling et al. 2010; Love and Summons 2015). (2) The soft maximum on the origin of Ambulacraria, set to 565 Ma based on arguments presented in Peterson et al. (2008). Note that this soft maximum has recently been reevaluated by Benton et al. (2015), but for the scope of our study this is not relevant as the absolute divergence time estimated by Erwin et al. (2011) for this clade is fully compatible with the Benton et al. (2015) constraint. *Note: Battistuzzi et al. (2015) described their root calibration as a gamma density with mean = 1,000 Ma and SD = 1,000 Myr. This gamma density has shape parameter = 1, and it is thus an exponential distribution of mean = 1,000 Ma.
Divergence Times for Key Nodes as Estimated Under the 22-Fossil Calibration Set and Root Prior of Battistuzzi et al. (2015) and the 24-Fossil Calibration Set and Root Prior of Erwin et al. (2011) (see table 1 for details)
| Calibration Set | MCMC Run | Root Age (Ma) | Crown-Metazoa (Ma) | Crown-Eumetazoa (Ma) | Crown-Bilateria (Ma) |
|---|---|---|---|---|---|
| Battistuzzi | Marginal priors | 2,810 (6,046–1,091) | 2,354 (4,611–1,045) | 2,075 (4,102–1015) | 1,846 (3,724–898) |
| Battistuzzi | Posterior | 1,604 (2,096–1171) | 1,126 (1,349–922) | 964 (1,126–825) | 862 (988–757) |
| Erwin | Marginal priors | 1,026 (1,235–841) | 960 (1,178–732) | 875 (1,130–629) | 852 (1,118–615) |
| Erwin | Posterior | 986 (1,134–858) | 778 (853–721) | 701 (765–659) | 672 (716–637) |
Note.—Legend: Battistuzzi = Mean node ages (and 95% HPDs) inferred using the reduced set of 22 fossil calibrations and the diffuse root age calibration of Battistuzzi et al. (2015) (see “Materials and Methods” section and table 1). Erwin = Mean node ages (and 95% HPDs) inferred using the same set of 24 fossil calibrations and root age calibration used in the in the original Bayesian analysis of Erwin et al. (2011) (see “Materials and Methods” section and table 1). Marginal Priors are calculated by running the MCMC chain with no data according to the calibration set used (table 1). Posteriors are calculated by running the MCMC chain with the molecular data and the calibration set used (table 1). Whereas the prior mean age of the crown Metazoa in Battistuzzi et al. (2015) study was deep in the Neoarchaean 2,354 Ma before the Neoproterozoic-Mesoproterozoic boundary, the mean prior crown age for the same node in the study of Erwin et al. (2011) is 960 Ma at all effect centered on the Neoproterozoic-Mesoproterozoic boundary. It follows that while the calibrations and root prior of Erwin et al. (2011) allowed a fair test of whether the age of animals happened in the Mesoproterozoic or in the Neoproterozoic, those of Battistuzzi et al. (2015) did not, biasing the results towards a Mesoproterozoic origin of animals.
F—Time trees showing marginal priors and posterior divergence time estimated for the metazoan tree of life under the CIR clock model. (a) Marginal priors of divergence times using the 22 fossil-calibration set (table 1). (b) Posterior divergence times using the 22 fossil-calibrations set (table 1). (c) Marginal priors of divergence times using the 24 fossil-calibration set (table 1). (d) Posterior divergence times estimates using the 24 fossil-calibration set (table 1). In (a) and (b), the calibration density on the root age is exponential with mean = 1,000 Myr. In (c) and (d), the calibration density on the root age is gamma with mean = 1,000 Ma and SD = 100 Ma. Nodes are drawn at the posterior means and horizontal thick bars represent the 95% highest posterior density (HPD) intervals. The HPD interval bar for the crown-metazoan node age is highlighted in green. Images on the bottom x axis depicts relevant geological and biological events. It is noticeable that irrespective of the fossil calibrations and node age prior used, posterior divergence times always tend to sit at the right end (i.e. young ages) of the prior distribution. The results presented here represent strong evidence rejecting the Battistuzzi et al. (2015) hypothesis that animals had a long cryptic history that went unrecorded in the fossil record.