Abstract

Molecular sequence data provide information about relative times only, and fossil-based age constraints are the ultimate source of information about absolute times in molecular clock dating analyses. Thus, fossil calibrations are critical to molecular clock dating, but competing methods are difficult to evaluate empirically because the true evolutionary time scale is never known. Here, we combine mechanistic models of fossil preservation and sequence evolution in simulations to evaluate different approaches to constructing fossil calibrations and their impact on Bayesian molecular clock dating, and the relative impact of fossil versus molecular sampling. We show that divergence time estimation is impacted by the model of fossil preservation, sampling intensity and tree shape. The addition of sequence data may improve molecular clock estimates, but accuracy and precision is dominated by the quality of the fossil calibrations. Posterior means and medians are poor representatives of true divergence times; posterior intervals provide a much more accurate estimate of divergence times, though they may be wide and often do not have high coverage probability. Our results highlight the importance of increased fossil sampling and improved statistical approaches to generating calibrations, which should incorporate the non-uniform nature of ecological and temporal fossil species distributions.

Highlights

  • The fossil record formerly provided the only time scale for evolutionary history, despite the combined phylogenetic, ecological and stratigraphic processes that have resulted in a highly incomplete and non-uniform record of life [1]

  • Fossil calibrations are critical to molecular clock dating, but competing methods are difficult to evaluate empirically because the true evolutionary time scale is never known

  • We explored the impact of competing variables on prior and posterior estimates of divergence times using coverage, relative interval width and relative root mean square error (RMSE), which is a combined measure of accuracy and precision

Read more

Summary

Introduction

The fossil record formerly provided the only time scale for evolutionary history, despite the combined phylogenetic, ecological and stratigraphic processes that have resulted in a highly incomplete and non-uniform record of life [1]. A major challenge to constructing reliable clade age constraints is that the stratigraphic distribution of fossils is highly uneven, influenced by factors that lead to variation in sedimentary rock volume during different intervals We incorporate such variation into our simulations using a model that relates the probability of fossil recovery (the combined effects of preservation and sampling) to cyclic changes in sea level [22]. The results of our simulation study suggest that controls on the stratigraphic distribution of fossil taxa, and their sampling, should inform the development of models for divergence time analysis. The simulated fossil occurrence data were used to establish minimum and maximum constraints on node ages, which were used to construct calibration densities in the Bayesian estimation of divergence times (electronic supplementary material, figure S1).

Results
Discussion
Conclusion
Findings
16. Parham JF et al 2012 Best practices for justifying
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call