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ESTIMATING SPECIES DIVERGENCE TIMES 
Tracy A. Heath 
University of Kansas 
University of California, Berkeley 
Iowa State University (in 2015) 
Tanja Stadler 
ETH Zürich 
2014 Phylogenetic Analysis in RevBayes 
NESCent Academy
A TIME-SCALE FOR EVOLUTION 
Phylogenetic trees can provide both topological information 
and temporal information 
Primates 
Artiodactyla 
Carnivora 
0.2 expected 
substitutions/site 
Cetacea 
Simiiformes 
Microcebus 
Hippo 
Homininae 
Phylogenetic Relationships Sequence 
Fossil 
Data 
Calibrations 
Did Simiiformes experience 
accelerated rates of molecular 
evolution? 
What is the age of the MRCA of 
mouse lemurs (Microcebus)? 
Equus 
Rhinoceros 
Bos 
Hippopotamus 
Balaenoptera 
Physeter 
Ursus 
Canis 
Felis 
Homo 
Pan 
Gorilla 
Pongo 
Macaca 
Callithrix 
Loris 
Galago 
Daubentonia 
Varecia 
Eulemur 
Lemur 
Hapalemur 
Propithecus 
Lepilemur 
Cheirogaleus 
Mirza 
M. murinus 
M. griseorufus 
M. myoxinus 
M. berthae 
M. rufus1 
M. tavaratra 
M. rufus2 
M. sambiranensis 
M. ravelobensis 
100 80.0 60.0 40.0 20.0 0.0 
Simiiformes 
Microcebus 
Cretaceous Paleogene Neogene Q 
Time (Millions of years) 
Understanding Evolutionary Processes (Yang & Yoder Syst. Biol. 2003)
A TIME-SCALE FOR EVOLUTION 
Phylogenetic divergence-time 
estimation 
• What was the spacial and 
climatic environment of ancient 
angiosperms? 
• Did the uplift of the Patagonian 
Andes drive the diversity of 
Peruvian lilies? 
• How has mammalian body-size 
changed over time? 
• Is diversification in Caribbean 
anoles correlated with ecological 
opportunity? 
• How has the rate of molecular 
evolution changed across the 
Tree of Life? 
Historical biogeography Molecular evolution 
(Antonelli & Sanmartin. Syst. Biol. 2011) 
(Nabholz, Glemin, Galtier. MBE 2008) 
Trait evolution 
Diversication 
Anolis fowleri (image by L. Mahler) 
(Lartillot & Delsuc. Evolution 2012) (Mahler, Revell, Glor, & Losos. Evolution 2010) 
Understanding Evolutionary Processes
THE DYNAMICS OF INFECTIOUS DISEASES 
Divergence time estimation 
of rapidly evolving 
pathogens provide 
information about spatial 
and temporal dynamics of 
infectious diseases 
Sequences sampled at 
different time horizons 
impose a temporal structure 
on the tree by providing 
ages for non-contemporaneous 
tips 
(Pybus & Rambaut. 2009. Nature Reviews Genetics.)
DIVERGENCE TIME ESTIMATION 
Goal: Estimate the ages of interior nodes to understand the 
timing and rates of evolutionary processes 
Model how rates are 
distributed across the tree 
Describe the distribution of 
speciation events over time 
External calibration 
information for estimates of 
absolute node times 
calibrated node 
Equus 
Rhinoceros 
Bos 
Hippopotamus 
Balaenoptera 
Physeter 
Ursus 
Canis 
Felis 
Homo 
Pan 
Gorilla 
Pongo 
Macaca 
Callithrix 
Loris 
Galago 
Daubentonia 
Varecia 
Eulemur 
Lemur 
Hapalemur 
Propithecus 
Lepilemur 
Cheirogaleus 
Mirza 
M. murinus 
M. griseorufus 
M. myoxinus 
M. berthae 
M. rufus1 
M. tavaratra 
M. rufus2 
M. sambiranensis 
M. ravelobensis 
100 80.0 60.0 40.0 20.0 0.0 
Simiiformes 
Microcebus 
Cretaceous Paleogene Neogene Q 
Time (Millions of years)
A TIME-SCALE FOR EVOLUTION 
Phylogenetic trees can provide both topological information 
and temporal information 
Equus 
Rhinoceros 
Bos 
Hippopotamus 
Balaenoptera 
Physeter 
Ursus 
Canis 
Felis 
Homo 
Pan 
Gorilla 
Pongo 
Macaca 
Callithrix 
Loris 
Galago 
Daubentonia 
Varecia 
Eulemur 
Lemur 
Hapalemur 
Propithecus 
Lepilemur 
Cheirogaleus 
Mirza 
M. murinus 
M. griseorufus 
M. myoxinus 
M. berthae 
M. rufus1 
M. tavaratra 
M. rufus2 
M. sambiranensis 
M. ravelobensis 
100 80.0 60.0 40.0 20.0 0.0 
Simiiformes 
Microcebus 
Cretaceous Paleogene Neogene Q 
Time (Millions of years) 
Understanding Evolutionary Processes (Yang & Yoder Syst. Biol. 2003; Heath et al. MBE 2012)
THE GLOBAL MOLECULAR CLOCK 
Assume that the rate of 
evolutionary change is 
constant over time 
A B C 
(branch lengths equal 
percent sequence 
divergence) 10% 
400 My 
200 My 
20% 
10% 
10% 
(Based on slides by Jeff Thorne; http://statgen.ncsu.edu/thorne/compmolevo.html)
THE GLOBAL MOLECULAR CLOCK 
A B C 
We can date the tree if we 
10% 
know the rate of change is 
1% divergence per 10 My 20% 
N 
10% 
10% 
200 My 
400 My 
200 My 
(Based on slides by Jeff Thorne; http://statgen.ncsu.edu/thorne/compmolevo.html)
THE GLOBAL MOLECULAR CLOCK 
If we found a fossil of the 
MRCA of B and C, we can 
use it to calculate the rate 
of change & date the root 
of the tree 
A B C 
N 
20% 
10% 
10% 
10% 
200 My 
400 My 
(Based on slides by Jeff Thorne; http://statgen.ncsu.edu/thorne/compmolevo.html)
REJECTING THE GLOBAL MOLECULAR CLOCK 
Rates of evolution vary across lineages and over time 
Mutation rate: 
Variation in 
• metabolic rate 
• generation time 
• DNA repair 
Fixation rate: 
Variation in 
• strength and targets of 
selection 
• population sizes 
A B C 
10% 
400 My 
200 My 
20% 
10% 
10%
UNCONSTRAINED ANALYSIS 
Sequence data provide 
information about branch 
lengths 
In units of the expected # of 
substitutions per site 
branch length = rate × time 
0.2 expected 
substitutions/site 
Phylogenetic Relationships Sequence 
Data
PHYLOGENETIC LIKELIHOOD 
f (D | V, θs,	) 
V Vector of branch lengths 
θs Sequence model parameters 
D Sequence data 
	 Tree topology
RATE AND TIME 
The expected # of substitutions/site occurring along a 
branch is the product of the substitution rate and time 
length = rate × time length = rate length = time 
Methods for dating species divergences estimate the 
substitution rate and time separately
RATES AND TIMES 
The sequence data 
provide information 
about branch length 
for any possible rate, 
there’s a time that fits 
the branch length 
perfectly 
5 
4 
3 
2 
1 
0 
branch length = 0.5 
time = 0.8 
rate = 0.625 
0 1 2 3 4 5 
Branch Rate 
Branch Time 
(based on Thorne & Kishino, 2005)
BAYESIAN DIVERGENCE TIME ESTIMATION 
length = rate length = time 
R = (r1, r2, r3, . . . , r2N−2) 
A = (a1, a2, a3, . . . , aN−1) 
N = number of tips
BAYESIAN DIVERGENCE TIME ESTIMATION 
length = rate length = time 
R = (r1, r2, r3, . . . , r2N−2) 
A = (a1, a2, a3, . . . , aN−1) 
N = number of tips
BAYESIAN DIVERGENCE TIME ESTIMATION 
Posterior probability 
f (R,A, θR, θA, θs | D,	) 
R Vector of rates on branches 
A Vector of internal node ages 
θR, θA, θs Model parameters 
D Sequence data 
	 Tree topology
BAYESIAN DIVERGENCE TIME ESTIMATION 
f(R,A, θR, θA, θs | D) = 
f (D | R,A, θs) f(R | θR) f(A | θA) f(θs) 
f(D) 
f(D | R,A, θR, θA, θs) Likelihood 
f(R | θR) Prior on rates 
f(A | θA) Prior on node ages 
f(θs) Prior on substitution parameters 
f(D) Marginal probability of the data
BAYESIAN DIVERGENCE TIME ESTIMATION 
Estimating divergence times relies on 2 main elements: 
• Branch-specific rates: f (R | θR) 
• Node ages: f (A | θA, C)
MODELING RATE VARIATION 
Some models describing lineage-specific substitution rate 
variation: 
• Global molecular clock (Zuckerkandl & Pauling, 1962) 
• Local molecular clocks (Hasegawa, Kishino & Yano 1989; 
Kishino & Hasegawa 1990; Yoder & Yang 2000; Yang & Yoder 
2003, Drummond and Suchard 2010) 
• Punctuated rate change model (Huelsenbeck, Larget and 
Swofford 2000) 
• Log-normally distributed autocorrelated rates (Thorne, 
Kishino & Painter 1998; Kishino, Thorne & Bruno 2001; Thorne & 
Kishino 2002) 
• Uncorrelated/independent rates models (Drummond et al. 
2006; Rannala & Yang 2007; Lepage et al. 2007) 
• Mixture models on branch rates (Heath, Holder, Huelsenbeck 
2012) 
Models of Lineage-specific Rate Variation
GLOBAL MOLECULAR CLOCK 
The substitution rate is 
constant over time 
All lineages share the same 
rate 
branch length = substitution rate 
low high 
Models of Lineage-specific Rate Variation (Zuckerkandl & Pauling, 1962)
GLOBAL MOLECULAR CLOCK 
rate prior distribution 
rate 
density 
r 
Models of Lineage-specific Rate Variation (Zuckerkandl & Pauling, 1962)
GLOBAL MOLECULAR CLOCK 
The sampled rate is applied 
to every branch in the tree 
rate prior distribution 
rate 
density 
r 
Models of Lineage-specific Rate Variation (Zuckerkandl & Pauling, 1962)
REJECTING THE GLOBAL MOLECULAR CLOCK 
Rates of evolution vary across lineages and over time 
Mutation rate: 
Variation in 
• metabolic rate 
• generation time 
• DNA repair 
Fixation rate: 
Variation in 
• strength and targets of 
selection 
• population sizes 
A B C 
10% 
400 My 
200 My 
20% 
10% 
10%
RELAXED-CLOCK MODELS 
To accommodate variation in substitution rates 
‘relaxed-clock’ models estimate lineage-specific substitution 
rates 
• Local molecular clocks 
• Punctuated rate change model 
• Log-normally distributed autocorrelated rates 
• Uncorrelated/independent rates models 
• Mixture models on branch rates
LOCAL MOLECULAR CLOCKS 
Rate shifts occur 
infrequently over the tree 
Closely related lineages 
have equivalent rates 
(clustered by sub-clades) 
branch length = substitution rate 
low high 
Models of Lineage-specific Rate Variation (Yang & Yoder 2003, Drummond and Suchard 2010)
LOCAL MOLECULAR CLOCKS 
Most methods for 
estimating local clocks 
required specifying the 
number and locations of 
rate changes a priori 
Drummond and Suchard 
(2010) introduced a 
Bayesian method that 
samples over a broad range 
of possible random local 
clocks 
branch length = substitution rate 
low high 
Models of Lineage-specific Rate Variation (Yang & Yoder 2003, Drummond and Suchard 2010)
AUTOCORRELATED RATES 
Substitution rates evolve 
gradually over time – 
closely related lineages have 
similar rates 
The rate at a node is 
drawn from a lognormal 
distribution with a mean 
equal to the parent rate 
branch length = substitution rate 
low high 
Models of Lineage-specific Rate Variation (Thorne, Kishino & Painter 1998; Kishino, Thorne & Bruno 2001)
AUTOCORRELATED RATES 
Models of Lineage-specific Rate Variation (Thorne, Kishino & Painter 1998; Kishino, Thorne & Bruno 2001)
PUNCTUATED RATE CHANGE 
Rate changes occur along 
lineages according to a 
point process 
At rate-change events, the 
new rate is a product of 
the parent’s rate and a 
-distributed multiplier 
branch length = substitution rate 
low high 
Models of Lineage-specific Rate Variation (Huelsenbeck, Larget and Swofford 2000)
INDEPENDENT/UNCORRELATED RATES 
Lineage-specific rates are 
uncorrelated when the rate 
assigned to each branch is 
independently drawn from 
an underlying distribution 
branch length = substitution rate 
low high 
Models of Lineage-specific Rate Variation (Drummond et al. 2006)
INDEPENDENT/UNCORRELATED RATES 
branch length = substitution rate 
low high 
Models of Lineage-specific Rate Variation (Drummond et al. 2006)
INFINITE MIXTURE MODEL 
Dirichlet process prior: 
Branches are partitioned 
into distinct rate categories 
branch length = substitution rate 
c 
5 
c 
4 
c 
3 
c 
2 
c 
1 
substitution rate classes 
Models of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE)
THE DIRICHLET PROCESS PRIOR (DPP) 
A stochastic process that models data as a mixture of 
distributions and can identify latent classes present in the 
data 
Branches are assumed to 
form distinct substitution 
rate clusters 
Efficient Markov chain 
Monte Carlo (MCMC) 
implementations allow for 
inference under this model 
branch length = substitution rate 
c 
5 
c 
4 
c 
3 
c 
2 
c 
1 
substitution rate classes 
DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
THE DIRICHLET PROCESS PRIOR (DPP) 
A stochastic process that models data as a mixture of 
distributions and can identify latent classes present in the 
data 
Random variables under the 
DPP informed by the data: 
• the number of rate 
classes 
• the assignment of 
branches to classes 
• the rate value for each 
class 
branch length = substitution rate 
c 
5 
c 
4 
c 
3 
c 
2 
c 
1 
substitution rate classes 
DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
THE DIRICHLET PROCESS PRIOR (DPP) 
A stochastic process that models data as a mixture of 
distributions and can identify latent classes present in the 
data 
Random variables under the 
DPP informed by the data: 
• the number of rate 
classes 
• the assignment of 
branches to classes 
• the rate value for each 
class 
DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
DPP FOR CLUSTERING PROBLEMS 
Global molecular 
clock 
branch length = substitution rate 
18 
c 
1 
rate classes 
DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
DPP FOR CLUSTERING PROBLEMS 
Independent 
rates 
branch length = substitution rate 
1 
c 
1 
1 
c 
18 
1 
c 
3 
1 
c 
2 
rate classes 
DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
DPP FOR CLUSTERING PROBLEMS 
Local molecular 
clock 
branch length = substitution rate 
5 
c 
3 
5 
c 
2 
8 
c 
1 
rate classes 
(262,142 different local molecular clocks) 
DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
DPP FOR CLUSTERING PROBLEMS 
Global molecular 
clock 
branch length = substitution rate 
4 
c 
3 
6 
c 
2 
8 
c 
1 
rate classes 
Each of the 
682,076,806,159 
configurations 
has a prior weight 
DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
MODELING RATE VARIATION 
These are only a subset of the available models for 
branch-rate variation 
• Global molecular clock 
• Local molecular clocks 
• Punctuated rate change model 
• Log-normally distributed autocorrelated rates 
• Uncorrelated/independent rates models 
• Dirchlet process prior 
Models of Lineage-specific Rate Variation
MODELING RATE VARIATION 
Are our models appropriate across all data sets? 
sloth bear 
brown bear 
polar bear 
cave bear 
Asian 
black bear 
American 
black bear 
sun bear 
American giant 
short-faced bear 
spectacled 
bear 
giant panda 
harbor seal 
100•100•100•1.00 
4.08 
5.39 
t9 
99•97•94•1.00 
5.66 
12.86 
2.75 
5.05 
19.09 
MP•MLu•MLp•Bayesian 
35.7 
0.88 
[3.11–5.27] 
4.58 
[4.26–7.34] 
[9.77–16.58] 
[3.9–6.48] 
[0.66–1.17] 
[4.2–6.86] 
[2.1–3.57] 
[14.38–24.79] 
[3.51–5.89] 
mean age (Ma) 
14.32 
[9.77–16.58] 
95% CI 
t2 
t3 
t4 
t6 
t7 
t5 
t8 
t10 
tx 
node 
100•100•100•1.00 
100•100•100•1.00 
85•93•93•1.00 
76•94•97•1.00 
100•100•100•1.00 
100•100•100•1.00 
t1 
Eocene Oligocene Miocene Plio Plei Hol 
34 23.8 5.3 1.8 0.01 
Epochs 
Ma 
Global expansion of C4 biomass 
Major temperature drop and increasing seasonality 
Faunal turnover 
Krause et al., 2008. Mitochondrial genomes reveal an 
explosive radiation of extinct and extant bears near the 
Miocene-Pliocene boundary. BMC Evol. Biol. 8. 
Taxa 
1 
5 
10 
50 
100 
500 
1000 
5000 
10000 
20000 
 
 
300 200 100 0 
MYA 
Polypteriformes 
Chondrostei 
Holostei 
Elopomorpha 
Osteoglossomorpha 
Clupeomorpha 
Denticipidae 
Gonorynchiformes 
Cypriniformes 
Gymnotiformes 
Siluriformes 
Characiformes 
Esociformes 
Salmoniformes 
Galaxiiformes 
Osmeriformes 
Stomiiformes 
Argentiniformes 
Myctophiformes 
Aulopiformes 
Percopsif. + Gadiif. 
Polymixiiformes 
Zeiforms 
Lampriformes 
Beryciformes 
Percomorpha 
Ophidiiformes 
Clade r ε ΔAIC 
1. 0.041 0.0017 25.3 
2. 0.081 * 25.5 
3. 0.067 0.37 45.1 
4. 0 * 3.1 
Bg. 0.011 0.0011 
 
 
Ostariophysi Acanthomorpha 
Teleostei 
 
 

 
Santini et al., 2009. Did genome duplication drive the origin 
of teleosts? A comparative study of diversification in 
ray-finned fishes. BMC Evol. Biol. 9.
MODELING RATE VARIATION 
These are only a subset of the available models for 
branch-rate variation 
• Global molecular clock 
• Local molecular clocks 
• Punctuated rate change model 
• Log-normally distributed autocorrelated rates 
• Uncorrelated/independent rates models 
• Dirchlet process prior 
Model selection and model uncertainty are very important 
for Bayesian divergence time analysis 
Models of Lineage-specific Rate Variation
BAYESIAN DIVERGENCE TIME ESTIMATION 
Estimating divergence times relies on 2 main elements: 
• Branch-specific rates: f (R | θR) 
• Node ages: f (A | θA, C) 
http://bayesiancook.blogspot.com/2013/12/two-sides-of-same-coin.html
PRIORS ON NODE TIMES 
Sequence data are only informative on relative rates  times 
Node-time priors cannot give precise estimates of absolute 
node ages 
We need external information (like fossils) to calibrate or 
scale the tree to absolute time 
Node Age Priors
CALIBRATING DIVERGENCE TIMES 
Fossils (or other data) are necessary to estimate absolute 
node ages 
There is no information in 
the sequence data for 
absolute time 
Uncertainty in the 
placement of fossils 
A B C 
N 
20% 
10% 
10% 
10% 
200 My 
400 My
CALIBRATION DENSITIES 
Bayesian inference is well suited to accommodating 
uncertainty in the age of the calibration node 
Divergence times are 
calibrated by placing 
parametric densities on 
internal nodes offset by age 
estimates from the fossil 
record 
A B C 
N 
200 My 
Density 
Age
FOSSIL CALIBRATION 
Fossil and geological data 
can be used to estimate the 
absolute ages of ancient 
divergences 
Time (My) 
Calibrating Divergence Times
FOSSIL CALIBRATION 
The ages of extant taxa 
are known 
Time (My) 
Calibrating Divergence Times
FOSSIL CALIBRATION 
Fossil taxa are assigned to 
monophyletic clades 
Minimum age Time (My) 
Calibrating Divergence Times Notogoneus osculus (Grande  Grande J. Paleont. 2008)
FOSSIL CALIBRATION 
Fossil taxa are assigned to 
monophyletic clades and 
constrain the age of the 
MRCA 
Minimum age Time (My) 
Calibrating Divergence Times
ASSIGNING FOSSILS TO CLADES 
Misplaced fossils can affect node age estimates throughout 
the tree – if the fossil is older than its presumed MRCA 
Calibrating the Tree (figure from Benton  Donoghue Mol. Biol. Evol. 2007)
ASSIGNING FOSSILS TO CLADES 
Crown clade: all 
living species and 
their most-recent 
common ancestor 
(MRCA) 
Calibrating the Tree (figure from Benton  Donoghue Mol. Biol. Evol. 2007)
ASSIGNING FOSSILS TO CLADES 
Stem lineages: 
purely fossil forms 
that are closer to 
their descendant 
crown clade than 
any other crown 
clade 
Calibrating the Tree (figure from Benton  Donoghue Mol. Biol. Evol. 2007)
ASSIGNING FOSSILS TO CLADES 
Fossiliferous 
horizons: the 
sources in the 
rock record for 
relevant fossils 
Calibrating the Tree (figure from Benton  Donoghue Mol. Biol. Evol. 2007)
FOSSIL CALIBRATION 
Age estimates from fossils 
can provide minimum time 
constraints for internal 
nodes 
Reliable maximum bounds 
are typically unavailable 
Minimum age Time (My) 
Calibrating Divergence Times
PRIOR DENSITIES ON CALIBRATED NODES 
Parametric distributions are 
typically off-set by the age 
of the oldest fossil assigned 
to a clade 
These prior densities do not 
(necessarily) require 
specification of maximum 
bounds 
Uniform (min, max) 
Log Normal (μ, s2) 
Gamma (a, b) 
Exponential (l) 
Minimum age Time (My) 
Calibrating Divergence Times
PRIOR DENSITIES ON CALIBRATED NODES 
Describe the waiting time 
between the divergence 
event and the age of the 
oldest fossil 
Minimum age Time (My) 
Calibrating Divergence Times
PRIOR DENSITIES ON CALIBRATED NODES 
Overly informative priors 
can bias node age 
estimates to be too young 
Minimum age 
Exponential (l) 
Time (My) 
Calibrating Divergence Times
PRIOR DENSITIES ON CALIBRATED NODES 
Uncertainty in the age of 
the MRCA of the clade 
relative to the age of the 
fossil may be better 
captured by vague prior 
densities 
Minimum age 
Exponential (l) 
Time (My) 
Calibrating Divergence Times
PUT A PRIOR ON IT 
Hyperprior: place an higher-order prior on the parameter of 
a prior distribution 
Sample the time from 
the MRCA to the 
fossil from a mixture 
of different 
exponential 
distributions 
Account for 
uncertainty in values 
of λ 
Density 
Hyperprior 
Hyperparameter 
Density 
Prior 
Parameter
CALIBRATION PRIORS IN REVBAYES 
Calibrating Divergence Times
PRIOR DENSITIES ON CALIBRATED NODES 
Common practice in Bayesian divergence-time estimation: 
Estimates of absolute node 
ages are driven primarily by 
the calibration density 
Specifying appropriate 
densities is a challenge for 
most molecular biologists 
Uniform (min, max) 
Log Normal (μ, s2) 
Gamma (a, b) 
Exponential (l) 
Minimum age Time (My) 
Calibration Density Approach
IMPROVING FOSSIL CALIBRATION 
We would prefer to 
eliminate the need for 
ad hoc calibration 
prior densities 
Calibration densities 
do not account for 
diversification of fossils 
Domestic dog 
Spotted seal 
Zaragocyon daamsi 
Ballusia elmensis 
Ursavus brevihinus 
Ursavus primaevus 
Giant panda 
Ailurarctos lufengensis 
Agriarctos spp. 
Kretzoiarctos beatrix 
Indarctos vireti 
Indarctos arctoides 
Indarctos punjabiensis 
Spectacled bear 
Giant short-faced bear 
Sloth bear 
Brown bear 
Polar bear 
Cave bear 
Sun bear 
Am. black bear 
Asian black bear 
Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
IMPROVING FOSSIL CALIBRATION 
We want to use all 
of the available fossils 
Example: Bears 
12 fossils are reduced 
to 4 calibration ages 
with calibration density 
methods 
Domestic dog 
Spotted seal 
Zaragocyon daamsi 
Ballusia elmensis 
Ursavus brevihinus 
Ursavus primaevus 
Giant panda 
Ailurarctos lufengensis 
Agriarctos spp. 
Kretzoiarctos beatrix 
Indarctos vireti 
Indarctos arctoides 
Indarctos punjabiensis 
Spectacled bear 
Giant short-faced bear 
Sloth bear 
Brown bear 
Polar bear 
Cave bear 
Sun bear 
Am. black bear 
Asian black bear 
Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
IMPROVING FOSSIL CALIBRATION 
We want to use all 
of the available fossils 
Example: Bears 
12 fossils are reduced 
to 4 calibration ages 
with calibration density 
methods 
Domestic dog 
Spotted seal 
Zaragocyon daamsi 
Ballusia elmensis 
Ursavus brevihinus 
Ursavus primaevus 
Giant panda 
Ailurarctos lufengensis 
Agriarctos spp. 
Kretzoiarctos beatrix 
Indarctos vireti 
Indarctos arctoides 
Indarctos punjabiensis 
Spectacled bear 
Giant short-faced bear 
Sloth bear 
Brown bear 
Polar bear 
Cave bear 
Sun bear 
Am. black bear 
Asian black bear 
Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
IMPROVING FOSSIL CALIBRATION 
Because fossils are 
part of the 
diversification process, 
we can combine fossil 
calibration with 
birth-death models 
Domestic dog 
Spotted seal 
Zaragocyon daamsi 
Ballusia elmensis 
Ursavus brevihinus 
Ursavus primaevus 
Giant panda 
Ailurarctos lufengensis 
Agriarctos spp. 
Kretzoiarctos beatrix 
Indarctos vireti 
Indarctos arctoides 
Indarctos punjabiensis 
Spectacled bear 
Giant short-faced bear 
Sloth bear 
Brown bear 
Polar bear 
Cave bear 
Sun bear 
Am. black bear 
Asian black bear 
Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
IMPROVING FOSSIL CALIBRATION 
This relies on a 
branching model that 
accounts for 
speciation, extinction, 
and rates of 
fossilization, 
preservation, and 
recovery 
Domestic dog 
Spotted seal 
Zaragocyon daamsi 
Ballusia elmensis 
Ursavus brevihinus 
Ursavus primaevus 
Giant panda 
Ailurarctos lufengensis 
Agriarctos spp. 
Kretzoiarctos beatrix 
Indarctos vireti 
Indarctos arctoides 
Indarctos punjabiensis 
Spectacled bear 
Giant short-faced bear 
Sloth bear 
Brown bear 
Polar bear 
Cave bear 
Sun bear 
Am. black bear 
Asian black bear 
Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Improving statistical inference of absolute node ages 
Eliminates the need to specify arbitrary 
calibration densities 
Better capture our statistical 
uncertainty in species divergence dates 
All reliable fossils associated with a 
clade are used 150 100 50 0 
Time 
Heath, Huelsenbeck,  Stadler. 2014. The fossilized birth-death process for 
coherent calibration of divergence time estimates. PNAS 111(29):E2957–E2966. 
http://www.pnas.org/content/111/29/E2957.abstract
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Recovered fossil specimens 
provide historical 
observations of the 
diversification process that 
generated the tree of 
extant species 
150 100 50 0 
Time 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
The probability of the tree 
and fossil observations 
under a birth-death model 
with rate parameters: 
λ = speciation 
μ = extinction 
ψ = fossilization/recovery 
150 100 50 0 
Time 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
We assume that the fossil 
is a descendant of a 
specified calibrated node 
The time of the fossil: A 
indicates an observation of 
the birth-death process after 
the age of the node N 
250 200 150 100 50 0 
Time (My) 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
The fossil must attach to 
the tree at some time: ⋆ 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
If it is the descendant of 
an unobserved lineage, then 
there is a speciation event 
at time ⋆ on one of the 2 
branches 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
If it is the descendant of 
an unobserved lineage, then 
there is a speciation event 
at time ⋆ on one of the 2 
branches 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
If ⋆ = A, the fossil is an 
observation of a lineage 
ancestral to the extant 
species 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
If ⋆ = A, the fossil is an 
observation of a lineage 
ancestral to the extant 
species 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
The probability of this 
realization of the 
diversification process is 
conditional on: 
λ, μ, and ψ 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Using MCMC, we can 
sample the age of the 
calibrated node • while 
conditioning on 
λ, μ, and ψ 
other node ages 
A and ⋆ 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
MCMC allows us to 
consider all possible values 
of ⋆ (marginalization) 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
MCMC allows us to 
consider all possible values 
of ⋆ (marginalization) 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
MCMC allows us to 
consider all possible values 
of ⋆ (marginalization) 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
MCMC allows us to 
consider all possible values 
of ⋆ (marginalization) 
250 200 150 100 50 0 
Time (My) 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
The posterior samples of 
the calibrated node age are 
informed by the fossil 
attachment times 
250 200 150 100 50 0 
Time (My) 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
The FBD model allows 
multiple fossils to calibrate 
a single node 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Given ⋆ and A, the new 
fossil can attach to the tree 
via speciation along either 
branch in the extant tree 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Given ⋆ and A, the new 
fossil can attach to the tree 
via speciation along either 
branch in the extant tree 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Given ⋆ and A, the new 
fossil can attach to the tree 
via speciation along either 
branch in the extant tree 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Or the unobserved branch 
leading to the other 
calibrating fossil 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
If ⋆ = A, then the new 
fossil lies directly on a 
branch in the extant tree 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
If ⋆ = A, then the new 
fossil lies directly on a 
branch in the extant tree 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Or it is an ancestor of the 
other calibrating fossil 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
The probability of this 
realization of the 
diversification process is 
conditional on: 
λ, μ, and ψ 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Using MCMC, we can 
sample the age of the 
calibrated node while 
conditioning on 
λ, μ, and ψ 
other node ages 
A and ⋆ 
A and ⋆ 
N 
250 200 150 100 50 0 
Time (My) 
N 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
MCMC allows us to 
consider all possible values 
of ⋆ (marginalization) 
250 200 150 100 50 0 
Time (My) 
Diversification of Fossil  Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
BAYESIAN INFERENCE UNDER THE FBD 
Implemented in: 
• DPPDiv: 
github.com/trayc7/FDPPDIV 
• BEAST2: 
beast2.cs.auckland.ac.nz/ 
Available soon: 
• RevBayes: 
github.com/revbayes/revbayes 
150 100 50 0 
Time 
250 200 150 100 50 0 
Time (My) 
FBD Implementation (Heath, Huelsenbeck, Stadler. PNAS 2014)
LINEAGES THROUGH TIME 
The FBD model provides an 
estimate of the number of 
lineages over time 
200 150 100 50 0 
Time (My) 
1.0 
3.0 
2.0 
1.0 
200 150 100 50 0 
Time (My) 
Number of lineages
LINEAGES THROUGH TIME 
Lineage diversity over time with fossils 
MCMC samples the 
times of lineages in 
the reconstructed tree 
and the times of the 
fossil lineages 
(for 1 simulation replicate with 10% random sample of fossils) 
Simulations: Results
LINEAGES THROUGH TIME 
Lineage diversity over time with fossils 
Visualize extant and 
sampled fossil lineage 
diversification when 
using all available 
fossils (21 total) 
(for 1 simulation replicate with 10% random sample of fossils) 
Simulations: Results
LINEAGES THROUGH TIME 
Lineage diversity over time with fossils 
Choosing only the 
oldest (calibration) 
fossils reduced the set 
of sampled fossils 
from 21 to 12, 
giving less information 
about diversification 
over time 
(for 1 simulation replicate with 10% random sample of fossils) 
Simulations: Results
BEARS: DIVERGENCE TIMES 
Sequence data for extant 
species: 
• 8 Ursidae 
• 1 Canidae (gray wolf) 
• 1 Phocidae (spotted seal) 
Fossil ages: 
• 12 Ursidae 
• 5 Canidae 
• 5 Pinnipedimorpha 
DPP relaxed clock model 
(Heath, Holder, Huelsenbeck MBE 2012) 
Fixed tree topology 
Sequence 
Data 
Fossil Data Phylogenetic Relationships 
fossil canids 
fossil pinnepeds 
stem fossil ursids 
fossil Ailuropodinae 
giant short-faced bear 
cave bear 
Empirical Analysis (Wang 1994, 1999; Krause et al. 2008; Fulton  Strobeck 2010; Abella et al. 2012)
BEARS: DIVERGENCE TIMES 
Gray wolf 
Spotted seal 
Giant panda 
Spectacled bear 
Sloth bear 
Brown bear 
Polar bear 
Sun bear 
Am. black bear 
Asian black bear 
1. fossil canids 
2. fossil pinnepeds 
2. stem fossil ursids 
3. fossil Ailuropodinae 
4. giant short-faced bear 
5. cave bear 
1 
3 
2 
4 
5 
Empirical Analysis (Heath et al. PNAS 2014; silhouette images: http://phylopic.org/)
BEARS: DIVERGENCE TIMES 
Gray wolf 
Spotted seal 
Giant panda 
Spectacled bear 
Sloth bear 
Brown bear 
Polar bear 
Sun bear 
Am. black bear 
Asian black bear 
Ursidae 
Eocene Oligocene Miocene 
60 40 20 0 
Time (My) 
Plio 
Pleis 
Paleocene 
95% CI 
Empirical Analysis (Heath et al. PNAS 2014; silhouette images: http://phylopic.org/)
BEARS: DIVERGENCE TIMES 
fossil canids 
fossil pinnipeds 
fossil Ailuropodinae 
fossil Arctodus 
fossil Ursus 
Gray wolf 
Spotted seal 
Giant panda 
Spectacled bear 
Sloth bear 
Brown bear 
Polar bear 
Sun bear 
Am. black bear 
Asian black bear 
Ursidae 
Eocene Oligocene Miocene 
60 40 20 0 
Time (My) 
Plio 
Pleis 
Paleocene 
stem fossil Ursidae 
Empirical Analysis (Heath et al. PNAS 2014; silhouette images: http://phylopic.org/)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Improved statistical inference of absolute node ages 
Biologically motivated 
models can better 
capture statistical 
uncertainty 
fossil canids 
fossil pinnipeds 
fossil Ailuropodinae 
fossil Arctodus 
fossil Ursus 
Gray wolf 
Spotted seal 
Giant panda 
Spectacled bear 
Sloth bear 
Brown bear 
Polar bear 
Sun bear 
Am. black bear 
Asian black bear 
Ursidae 
Eocene Oligocene Miocene 
60 40 20 0 
Time (My) 
Plio 
Pleis 
Paleocene 
stem fossil Ursidae 
Modeling Diversification Processes (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Improved statistical inference of absolute node ages 
Use all available fossils 
Eliminates arbitrary 
choice of calibration 
priors 
fossil canids 
fossil pinnipeds 
fossil Ailuropodinae 
fossil Arctodus 
fossil Ursus 
Gray wolf 
Spotted seal 
Giant panda 
Spectacled bear 
Sloth bear 
Brown bear 
Polar bear 
Sun bear 
Am. black bear 
Asian black bear 
Ursidae 
Eocene Oligocene Miocene 
60 40 20 0 
Time (My) 
Plio 
Pleis 
Paleocene 
stem fossil Ursidae 
Modeling Diversification Processes (Heath, Huelsenbeck, Stadler. PNAS 2014)
THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) 
Improved statistical inference of absolute node ages 
Extensions of the FBD 
can account for 
stratigraphic sampling 
of fossils and shifts in 
rates of speciation 
and extinction 
Preservation Rate 
175 150 125 100 75 50 25 0 
Time 
0.2 1.05 
Modeling Diversification Processes (Heath, Huelsenbeck, Stadler. PNAS 2014)
FOSSIL TOTAL EVIDENCE DATING 
Combining extant and fossil 
species 
Sequence 
Data 
Fossil 
Age Data 
© AntWeb.org 
Morphological 
Data 
© AntWeb.org 
Orthoptera 
Paraneoptera 
Mecoptera 
Lepidoptera 
Coleoptera Adephaga 
Coleo Polyphaga 
Raphidioptera 
Neuroptera 
Xyela 
Macroxyela 
% of morphological 
characters scored 
for each terminal 
0% 
20% 
40% 
60% 
80% 
100% 
Blasticotoma 
Runaria 
Paremphytus 
Tenthredo 
Aglaostigma 
Dolerus 
Taxonus 
Selandria 
Strongylogaster 
Monophadnoides 
Metallus 
Hoplocampa 
Nematinus 
Nematus 
Cladius 
Monoctenus 
Gilpinia 
Diprion 
Athalia 
Cimbicinae 
Abia 
Corynis 
Arge 
Sterictiphora 
Perga 
Phylacteophaga 
Lophyrotoma 
Decameria 
Acordulecera 
Neurotoma 
Acantholyda 
Cephalcia 
Pamphilius 
Onycholyda 
Megalodontes skorniakowii 
Megalodontes cephalotes 
Cephus 
Calameuta 
Hartigia 
Syntexis 
Sirex 
Xeris 
Urocerus 
Tremex 
Xiphydria 
Orussus 
Stephanidae A 
Stephanidae B 
Cynipoidea 
Megalyridae 
Evanioidea 
Trigonalidae 
Vespidae 
Apoidea C 
Apoidea B 
Apoidea A 
Chalcidoidea 
Ichneumonidae 
Abrotoxyela 
Anagaridyela 
Chaetoxyela 
Spathoxyela 
Mesoxyela mesozoica 
Liadoxyela 
Eoxyela 
Grimmaratavites 
Brigittepterus 
Xyelula 
Sogutia 
Ferganolyda 
Prosyntexis 
Thoracotrema 
Ghilarella 
Sepulca 
Onokhoius 
Karatavites 
Aulisca 
Protosirex 
Aulidontes 
Trematothorax 
Rudisiricius 
Mesolyda 
Brachysyntexis 
Kulbastavia 
Syntexyela 
Anaxyela 
Palaeathalia 
Pseudoxyelocerus 
Dahuratoma 
Undatoma 
Leioxyela 
Triassoxyela 
Nigrimonticola 
Xyelotoma 
Pamphiliidae undescribed 
Turgidontes 
Praeoryssus 
Paroryssus 
Mesorussus 
Symphytopterus 
Cleistogaster 
Leptephialtites 
Stephanogaster 
97 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 
100 100 
100 
100 
100 
100 
100 
100 
97 
68 
55 
75 
77 
91 
84 
61 
57 
62 
98 
96 
71 
71 
85 
93 
52 
95 
64 
80 
64 
99 
77 
99 
98 
97 
82 
52 
58 
94 
90 
61 83 
60 
70 
57 
70 
60 
350 300 250 200 150 100 50 0 million years before present 
(Ronquist, Klopfstein, et al. Syst. Biol. 2012.)

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Divergence-time estimation in RevBayes

  • 1. ESTIMATING SPECIES DIVERGENCE TIMES Tracy A. Heath University of Kansas University of California, Berkeley Iowa State University (in 2015) Tanja Stadler ETH Zürich 2014 Phylogenetic Analysis in RevBayes NESCent Academy
  • 2. A TIME-SCALE FOR EVOLUTION Phylogenetic trees can provide both topological information and temporal information Primates Artiodactyla Carnivora 0.2 expected substitutions/site Cetacea Simiiformes Microcebus Hippo Homininae Phylogenetic Relationships Sequence Fossil Data Calibrations Did Simiiformes experience accelerated rates of molecular evolution? What is the age of the MRCA of mouse lemurs (Microcebus)? Equus Rhinoceros Bos Hippopotamus Balaenoptera Physeter Ursus Canis Felis Homo Pan Gorilla Pongo Macaca Callithrix Loris Galago Daubentonia Varecia Eulemur Lemur Hapalemur Propithecus Lepilemur Cheirogaleus Mirza M. murinus M. griseorufus M. myoxinus M. berthae M. rufus1 M. tavaratra M. rufus2 M. sambiranensis M. ravelobensis 100 80.0 60.0 40.0 20.0 0.0 Simiiformes Microcebus Cretaceous Paleogene Neogene Q Time (Millions of years) Understanding Evolutionary Processes (Yang & Yoder Syst. Biol. 2003)
  • 3. A TIME-SCALE FOR EVOLUTION Phylogenetic divergence-time estimation • What was the spacial and climatic environment of ancient angiosperms? • Did the uplift of the Patagonian Andes drive the diversity of Peruvian lilies? • How has mammalian body-size changed over time? • Is diversification in Caribbean anoles correlated with ecological opportunity? • How has the rate of molecular evolution changed across the Tree of Life? Historical biogeography Molecular evolution (Antonelli & Sanmartin. Syst. Biol. 2011) (Nabholz, Glemin, Galtier. MBE 2008) Trait evolution Diversication Anolis fowleri (image by L. Mahler) (Lartillot & Delsuc. Evolution 2012) (Mahler, Revell, Glor, & Losos. Evolution 2010) Understanding Evolutionary Processes
  • 4. THE DYNAMICS OF INFECTIOUS DISEASES Divergence time estimation of rapidly evolving pathogens provide information about spatial and temporal dynamics of infectious diseases Sequences sampled at different time horizons impose a temporal structure on the tree by providing ages for non-contemporaneous tips (Pybus & Rambaut. 2009. Nature Reviews Genetics.)
  • 5. DIVERGENCE TIME ESTIMATION Goal: Estimate the ages of interior nodes to understand the timing and rates of evolutionary processes Model how rates are distributed across the tree Describe the distribution of speciation events over time External calibration information for estimates of absolute node times calibrated node Equus Rhinoceros Bos Hippopotamus Balaenoptera Physeter Ursus Canis Felis Homo Pan Gorilla Pongo Macaca Callithrix Loris Galago Daubentonia Varecia Eulemur Lemur Hapalemur Propithecus Lepilemur Cheirogaleus Mirza M. murinus M. griseorufus M. myoxinus M. berthae M. rufus1 M. tavaratra M. rufus2 M. sambiranensis M. ravelobensis 100 80.0 60.0 40.0 20.0 0.0 Simiiformes Microcebus Cretaceous Paleogene Neogene Q Time (Millions of years)
  • 6. A TIME-SCALE FOR EVOLUTION Phylogenetic trees can provide both topological information and temporal information Equus Rhinoceros Bos Hippopotamus Balaenoptera Physeter Ursus Canis Felis Homo Pan Gorilla Pongo Macaca Callithrix Loris Galago Daubentonia Varecia Eulemur Lemur Hapalemur Propithecus Lepilemur Cheirogaleus Mirza M. murinus M. griseorufus M. myoxinus M. berthae M. rufus1 M. tavaratra M. rufus2 M. sambiranensis M. ravelobensis 100 80.0 60.0 40.0 20.0 0.0 Simiiformes Microcebus Cretaceous Paleogene Neogene Q Time (Millions of years) Understanding Evolutionary Processes (Yang & Yoder Syst. Biol. 2003; Heath et al. MBE 2012)
  • 7. THE GLOBAL MOLECULAR CLOCK Assume that the rate of evolutionary change is constant over time A B C (branch lengths equal percent sequence divergence) 10% 400 My 200 My 20% 10% 10% (Based on slides by Jeff Thorne; http://statgen.ncsu.edu/thorne/compmolevo.html)
  • 8. THE GLOBAL MOLECULAR CLOCK A B C We can date the tree if we 10% know the rate of change is 1% divergence per 10 My 20% N 10% 10% 200 My 400 My 200 My (Based on slides by Jeff Thorne; http://statgen.ncsu.edu/thorne/compmolevo.html)
  • 9. THE GLOBAL MOLECULAR CLOCK If we found a fossil of the MRCA of B and C, we can use it to calculate the rate of change & date the root of the tree A B C N 20% 10% 10% 10% 200 My 400 My (Based on slides by Jeff Thorne; http://statgen.ncsu.edu/thorne/compmolevo.html)
  • 10. REJECTING THE GLOBAL MOLECULAR CLOCK Rates of evolution vary across lineages and over time Mutation rate: Variation in • metabolic rate • generation time • DNA repair Fixation rate: Variation in • strength and targets of selection • population sizes A B C 10% 400 My 200 My 20% 10% 10%
  • 11. UNCONSTRAINED ANALYSIS Sequence data provide information about branch lengths In units of the expected # of substitutions per site branch length = rate × time 0.2 expected substitutions/site Phylogenetic Relationships Sequence Data
  • 12. PHYLOGENETIC LIKELIHOOD f (D | V, θs, ) V Vector of branch lengths θs Sequence model parameters D Sequence data Tree topology
  • 13. RATE AND TIME The expected # of substitutions/site occurring along a branch is the product of the substitution rate and time length = rate × time length = rate length = time Methods for dating species divergences estimate the substitution rate and time separately
  • 14. RATES AND TIMES The sequence data provide information about branch length for any possible rate, there’s a time that fits the branch length perfectly 5 4 3 2 1 0 branch length = 0.5 time = 0.8 rate = 0.625 0 1 2 3 4 5 Branch Rate Branch Time (based on Thorne & Kishino, 2005)
  • 15. BAYESIAN DIVERGENCE TIME ESTIMATION length = rate length = time R = (r1, r2, r3, . . . , r2N−2) A = (a1, a2, a3, . . . , aN−1) N = number of tips
  • 16. BAYESIAN DIVERGENCE TIME ESTIMATION length = rate length = time R = (r1, r2, r3, . . . , r2N−2) A = (a1, a2, a3, . . . , aN−1) N = number of tips
  • 17. BAYESIAN DIVERGENCE TIME ESTIMATION Posterior probability f (R,A, θR, θA, θs | D, ) R Vector of rates on branches A Vector of internal node ages θR, θA, θs Model parameters D Sequence data Tree topology
  • 18. BAYESIAN DIVERGENCE TIME ESTIMATION f(R,A, θR, θA, θs | D) = f (D | R,A, θs) f(R | θR) f(A | θA) f(θs) f(D) f(D | R,A, θR, θA, θs) Likelihood f(R | θR) Prior on rates f(A | θA) Prior on node ages f(θs) Prior on substitution parameters f(D) Marginal probability of the data
  • 19. BAYESIAN DIVERGENCE TIME ESTIMATION Estimating divergence times relies on 2 main elements: • Branch-specific rates: f (R | θR) • Node ages: f (A | θA, C)
  • 20. MODELING RATE VARIATION Some models describing lineage-specific substitution rate variation: • Global molecular clock (Zuckerkandl & Pauling, 1962) • Local molecular clocks (Hasegawa, Kishino & Yano 1989; Kishino & Hasegawa 1990; Yoder & Yang 2000; Yang & Yoder 2003, Drummond and Suchard 2010) • Punctuated rate change model (Huelsenbeck, Larget and Swofford 2000) • Log-normally distributed autocorrelated rates (Thorne, Kishino & Painter 1998; Kishino, Thorne & Bruno 2001; Thorne & Kishino 2002) • Uncorrelated/independent rates models (Drummond et al. 2006; Rannala & Yang 2007; Lepage et al. 2007) • Mixture models on branch rates (Heath, Holder, Huelsenbeck 2012) Models of Lineage-specific Rate Variation
  • 21. GLOBAL MOLECULAR CLOCK The substitution rate is constant over time All lineages share the same rate branch length = substitution rate low high Models of Lineage-specific Rate Variation (Zuckerkandl & Pauling, 1962)
  • 22. GLOBAL MOLECULAR CLOCK rate prior distribution rate density r Models of Lineage-specific Rate Variation (Zuckerkandl & Pauling, 1962)
  • 23. GLOBAL MOLECULAR CLOCK The sampled rate is applied to every branch in the tree rate prior distribution rate density r Models of Lineage-specific Rate Variation (Zuckerkandl & Pauling, 1962)
  • 24. REJECTING THE GLOBAL MOLECULAR CLOCK Rates of evolution vary across lineages and over time Mutation rate: Variation in • metabolic rate • generation time • DNA repair Fixation rate: Variation in • strength and targets of selection • population sizes A B C 10% 400 My 200 My 20% 10% 10%
  • 25. RELAXED-CLOCK MODELS To accommodate variation in substitution rates ‘relaxed-clock’ models estimate lineage-specific substitution rates • Local molecular clocks • Punctuated rate change model • Log-normally distributed autocorrelated rates • Uncorrelated/independent rates models • Mixture models on branch rates
  • 26. LOCAL MOLECULAR CLOCKS Rate shifts occur infrequently over the tree Closely related lineages have equivalent rates (clustered by sub-clades) branch length = substitution rate low high Models of Lineage-specific Rate Variation (Yang & Yoder 2003, Drummond and Suchard 2010)
  • 27. LOCAL MOLECULAR CLOCKS Most methods for estimating local clocks required specifying the number and locations of rate changes a priori Drummond and Suchard (2010) introduced a Bayesian method that samples over a broad range of possible random local clocks branch length = substitution rate low high Models of Lineage-specific Rate Variation (Yang & Yoder 2003, Drummond and Suchard 2010)
  • 28. AUTOCORRELATED RATES Substitution rates evolve gradually over time – closely related lineages have similar rates The rate at a node is drawn from a lognormal distribution with a mean equal to the parent rate branch length = substitution rate low high Models of Lineage-specific Rate Variation (Thorne, Kishino & Painter 1998; Kishino, Thorne & Bruno 2001)
  • 29. AUTOCORRELATED RATES Models of Lineage-specific Rate Variation (Thorne, Kishino & Painter 1998; Kishino, Thorne & Bruno 2001)
  • 30. PUNCTUATED RATE CHANGE Rate changes occur along lineages according to a point process At rate-change events, the new rate is a product of the parent’s rate and a -distributed multiplier branch length = substitution rate low high Models of Lineage-specific Rate Variation (Huelsenbeck, Larget and Swofford 2000)
  • 31. INDEPENDENT/UNCORRELATED RATES Lineage-specific rates are uncorrelated when the rate assigned to each branch is independently drawn from an underlying distribution branch length = substitution rate low high Models of Lineage-specific Rate Variation (Drummond et al. 2006)
  • 32. INDEPENDENT/UNCORRELATED RATES branch length = substitution rate low high Models of Lineage-specific Rate Variation (Drummond et al. 2006)
  • 33. INFINITE MIXTURE MODEL Dirichlet process prior: Branches are partitioned into distinct rate categories branch length = substitution rate c 5 c 4 c 3 c 2 c 1 substitution rate classes Models of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE)
  • 34. THE DIRICHLET PROCESS PRIOR (DPP) A stochastic process that models data as a mixture of distributions and can identify latent classes present in the data Branches are assumed to form distinct substitution rate clusters Efficient Markov chain Monte Carlo (MCMC) implementations allow for inference under this model branch length = substitution rate c 5 c 4 c 3 c 2 c 1 substitution rate classes DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
  • 35. THE DIRICHLET PROCESS PRIOR (DPP) A stochastic process that models data as a mixture of distributions and can identify latent classes present in the data Random variables under the DPP informed by the data: • the number of rate classes • the assignment of branches to classes • the rate value for each class branch length = substitution rate c 5 c 4 c 3 c 2 c 1 substitution rate classes DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
  • 36. THE DIRICHLET PROCESS PRIOR (DPP) A stochastic process that models data as a mixture of distributions and can identify latent classes present in the data Random variables under the DPP informed by the data: • the number of rate classes • the assignment of branches to classes • the rate value for each class DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
  • 37. DPP FOR CLUSTERING PROBLEMS Global molecular clock branch length = substitution rate 18 c 1 rate classes DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
  • 38. DPP FOR CLUSTERING PROBLEMS Independent rates branch length = substitution rate 1 c 1 1 c 18 1 c 3 1 c 2 rate classes DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
  • 39. DPP FOR CLUSTERING PROBLEMS Local molecular clock branch length = substitution rate 5 c 3 5 c 2 8 c 1 rate classes (262,142 different local molecular clocks) DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
  • 40. DPP FOR CLUSTERING PROBLEMS Global molecular clock branch length = substitution rate 4 c 3 6 c 2 8 c 1 rate classes Each of the 682,076,806,159 configurations has a prior weight DPP Model of Lineage-specific Rate Variation (Heath, Holder, Huelsenbeck. 2012 MBE 29:939-955)
  • 41. MODELING RATE VARIATION These are only a subset of the available models for branch-rate variation • Global molecular clock • Local molecular clocks • Punctuated rate change model • Log-normally distributed autocorrelated rates • Uncorrelated/independent rates models • Dirchlet process prior Models of Lineage-specific Rate Variation
  • 42. MODELING RATE VARIATION Are our models appropriate across all data sets? sloth bear brown bear polar bear cave bear Asian black bear American black bear sun bear American giant short-faced bear spectacled bear giant panda harbor seal 100•100•100•1.00 4.08 5.39 t9 99•97•94•1.00 5.66 12.86 2.75 5.05 19.09 MP•MLu•MLp•Bayesian 35.7 0.88 [3.11–5.27] 4.58 [4.26–7.34] [9.77–16.58] [3.9–6.48] [0.66–1.17] [4.2–6.86] [2.1–3.57] [14.38–24.79] [3.51–5.89] mean age (Ma) 14.32 [9.77–16.58] 95% CI t2 t3 t4 t6 t7 t5 t8 t10 tx node 100•100•100•1.00 100•100•100•1.00 85•93•93•1.00 76•94•97•1.00 100•100•100•1.00 100•100•100•1.00 t1 Eocene Oligocene Miocene Plio Plei Hol 34 23.8 5.3 1.8 0.01 Epochs Ma Global expansion of C4 biomass Major temperature drop and increasing seasonality Faunal turnover Krause et al., 2008. Mitochondrial genomes reveal an explosive radiation of extinct and extant bears near the Miocene-Pliocene boundary. BMC Evol. Biol. 8. Taxa 1 5 10 50 100 500 1000 5000 10000 20000 300 200 100 0 MYA Polypteriformes Chondrostei Holostei Elopomorpha Osteoglossomorpha Clupeomorpha Denticipidae Gonorynchiformes Cypriniformes Gymnotiformes Siluriformes Characiformes Esociformes Salmoniformes Galaxiiformes Osmeriformes Stomiiformes Argentiniformes Myctophiformes Aulopiformes Percopsif. + Gadiif. Polymixiiformes Zeiforms Lampriformes Beryciformes Percomorpha Ophidiiformes Clade r ε ΔAIC 1. 0.041 0.0017 25.3 2. 0.081 * 25.5 3. 0.067 0.37 45.1 4. 0 * 3.1 Bg. 0.011 0.0011 Ostariophysi Acanthomorpha Teleostei Santini et al., 2009. Did genome duplication drive the origin of teleosts? A comparative study of diversification in ray-finned fishes. BMC Evol. Biol. 9.
  • 43. MODELING RATE VARIATION These are only a subset of the available models for branch-rate variation • Global molecular clock • Local molecular clocks • Punctuated rate change model • Log-normally distributed autocorrelated rates • Uncorrelated/independent rates models • Dirchlet process prior Model selection and model uncertainty are very important for Bayesian divergence time analysis Models of Lineage-specific Rate Variation
  • 44. BAYESIAN DIVERGENCE TIME ESTIMATION Estimating divergence times relies on 2 main elements: • Branch-specific rates: f (R | θR) • Node ages: f (A | θA, C) http://bayesiancook.blogspot.com/2013/12/two-sides-of-same-coin.html
  • 45. PRIORS ON NODE TIMES Sequence data are only informative on relative rates times Node-time priors cannot give precise estimates of absolute node ages We need external information (like fossils) to calibrate or scale the tree to absolute time Node Age Priors
  • 46. CALIBRATING DIVERGENCE TIMES Fossils (or other data) are necessary to estimate absolute node ages There is no information in the sequence data for absolute time Uncertainty in the placement of fossils A B C N 20% 10% 10% 10% 200 My 400 My
  • 47. CALIBRATION DENSITIES Bayesian inference is well suited to accommodating uncertainty in the age of the calibration node Divergence times are calibrated by placing parametric densities on internal nodes offset by age estimates from the fossil record A B C N 200 My Density Age
  • 48. FOSSIL CALIBRATION Fossil and geological data can be used to estimate the absolute ages of ancient divergences Time (My) Calibrating Divergence Times
  • 49. FOSSIL CALIBRATION The ages of extant taxa are known Time (My) Calibrating Divergence Times
  • 50. FOSSIL CALIBRATION Fossil taxa are assigned to monophyletic clades Minimum age Time (My) Calibrating Divergence Times Notogoneus osculus (Grande Grande J. Paleont. 2008)
  • 51. FOSSIL CALIBRATION Fossil taxa are assigned to monophyletic clades and constrain the age of the MRCA Minimum age Time (My) Calibrating Divergence Times
  • 52. ASSIGNING FOSSILS TO CLADES Misplaced fossils can affect node age estimates throughout the tree – if the fossil is older than its presumed MRCA Calibrating the Tree (figure from Benton Donoghue Mol. Biol. Evol. 2007)
  • 53. ASSIGNING FOSSILS TO CLADES Crown clade: all living species and their most-recent common ancestor (MRCA) Calibrating the Tree (figure from Benton Donoghue Mol. Biol. Evol. 2007)
  • 54. ASSIGNING FOSSILS TO CLADES Stem lineages: purely fossil forms that are closer to their descendant crown clade than any other crown clade Calibrating the Tree (figure from Benton Donoghue Mol. Biol. Evol. 2007)
  • 55. ASSIGNING FOSSILS TO CLADES Fossiliferous horizons: the sources in the rock record for relevant fossils Calibrating the Tree (figure from Benton Donoghue Mol. Biol. Evol. 2007)
  • 56. FOSSIL CALIBRATION Age estimates from fossils can provide minimum time constraints for internal nodes Reliable maximum bounds are typically unavailable Minimum age Time (My) Calibrating Divergence Times
  • 57. PRIOR DENSITIES ON CALIBRATED NODES Parametric distributions are typically off-set by the age of the oldest fossil assigned to a clade These prior densities do not (necessarily) require specification of maximum bounds Uniform (min, max) Log Normal (μ, s2) Gamma (a, b) Exponential (l) Minimum age Time (My) Calibrating Divergence Times
  • 58. PRIOR DENSITIES ON CALIBRATED NODES Describe the waiting time between the divergence event and the age of the oldest fossil Minimum age Time (My) Calibrating Divergence Times
  • 59. PRIOR DENSITIES ON CALIBRATED NODES Overly informative priors can bias node age estimates to be too young Minimum age Exponential (l) Time (My) Calibrating Divergence Times
  • 60. PRIOR DENSITIES ON CALIBRATED NODES Uncertainty in the age of the MRCA of the clade relative to the age of the fossil may be better captured by vague prior densities Minimum age Exponential (l) Time (My) Calibrating Divergence Times
  • 61. PUT A PRIOR ON IT Hyperprior: place an higher-order prior on the parameter of a prior distribution Sample the time from the MRCA to the fossil from a mixture of different exponential distributions Account for uncertainty in values of λ Density Hyperprior Hyperparameter Density Prior Parameter
  • 62. CALIBRATION PRIORS IN REVBAYES Calibrating Divergence Times
  • 63. PRIOR DENSITIES ON CALIBRATED NODES Common practice in Bayesian divergence-time estimation: Estimates of absolute node ages are driven primarily by the calibration density Specifying appropriate densities is a challenge for most molecular biologists Uniform (min, max) Log Normal (μ, s2) Gamma (a, b) Exponential (l) Minimum age Time (My) Calibration Density Approach
  • 64. IMPROVING FOSSIL CALIBRATION We would prefer to eliminate the need for ad hoc calibration prior densities Calibration densities do not account for diversification of fossils Domestic dog Spotted seal Zaragocyon daamsi Ballusia elmensis Ursavus brevihinus Ursavus primaevus Giant panda Ailurarctos lufengensis Agriarctos spp. Kretzoiarctos beatrix Indarctos vireti Indarctos arctoides Indarctos punjabiensis Spectacled bear Giant short-faced bear Sloth bear Brown bear Polar bear Cave bear Sun bear Am. black bear Asian black bear Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
  • 65. IMPROVING FOSSIL CALIBRATION We want to use all of the available fossils Example: Bears 12 fossils are reduced to 4 calibration ages with calibration density methods Domestic dog Spotted seal Zaragocyon daamsi Ballusia elmensis Ursavus brevihinus Ursavus primaevus Giant panda Ailurarctos lufengensis Agriarctos spp. Kretzoiarctos beatrix Indarctos vireti Indarctos arctoides Indarctos punjabiensis Spectacled bear Giant short-faced bear Sloth bear Brown bear Polar bear Cave bear Sun bear Am. black bear Asian black bear Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
  • 66. IMPROVING FOSSIL CALIBRATION We want to use all of the available fossils Example: Bears 12 fossils are reduced to 4 calibration ages with calibration density methods Domestic dog Spotted seal Zaragocyon daamsi Ballusia elmensis Ursavus brevihinus Ursavus primaevus Giant panda Ailurarctos lufengensis Agriarctos spp. Kretzoiarctos beatrix Indarctos vireti Indarctos arctoides Indarctos punjabiensis Spectacled bear Giant short-faced bear Sloth bear Brown bear Polar bear Cave bear Sun bear Am. black bear Asian black bear Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
  • 67. IMPROVING FOSSIL CALIBRATION Because fossils are part of the diversification process, we can combine fossil calibration with birth-death models Domestic dog Spotted seal Zaragocyon daamsi Ballusia elmensis Ursavus brevihinus Ursavus primaevus Giant panda Ailurarctos lufengensis Agriarctos spp. Kretzoiarctos beatrix Indarctos vireti Indarctos arctoides Indarctos punjabiensis Spectacled bear Giant short-faced bear Sloth bear Brown bear Polar bear Cave bear Sun bear Am. black bear Asian black bear Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
  • 68. IMPROVING FOSSIL CALIBRATION This relies on a branching model that accounts for speciation, extinction, and rates of fossilization, preservation, and recovery Domestic dog Spotted seal Zaragocyon daamsi Ballusia elmensis Ursavus brevihinus Ursavus primaevus Giant panda Ailurarctos lufengensis Agriarctos spp. Kretzoiarctos beatrix Indarctos vireti Indarctos arctoides Indarctos punjabiensis Spectacled bear Giant short-faced bear Sloth bear Brown bear Polar bear Cave bear Sun bear Am. black bear Asian black bear Fossil and Extant Bears (Krause et al. BMC Evol. Biol. 2008; Abella et al. PLoS ONE 2012)
  • 69. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Improving statistical inference of absolute node ages Eliminates the need to specify arbitrary calibration densities Better capture our statistical uncertainty in species divergence dates All reliable fossils associated with a clade are used 150 100 50 0 Time Heath, Huelsenbeck, Stadler. 2014. The fossilized birth-death process for coherent calibration of divergence time estimates. PNAS 111(29):E2957–E2966. http://www.pnas.org/content/111/29/E2957.abstract
  • 70. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Recovered fossil specimens provide historical observations of the diversification process that generated the tree of extant species 150 100 50 0 Time Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 71. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) The probability of the tree and fossil observations under a birth-death model with rate parameters: λ = speciation μ = extinction ψ = fossilization/recovery 150 100 50 0 Time Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 72. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) We assume that the fossil is a descendant of a specified calibrated node The time of the fossil: A indicates an observation of the birth-death process after the age of the node N 250 200 150 100 50 0 Time (My) Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 73. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) The fossil must attach to the tree at some time: ⋆ 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 74. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) If it is the descendant of an unobserved lineage, then there is a speciation event at time ⋆ on one of the 2 branches 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 75. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) If it is the descendant of an unobserved lineage, then there is a speciation event at time ⋆ on one of the 2 branches 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 76. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) If ⋆ = A, the fossil is an observation of a lineage ancestral to the extant species 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 77. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) If ⋆ = A, the fossil is an observation of a lineage ancestral to the extant species 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 78. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) The probability of this realization of the diversification process is conditional on: λ, μ, and ψ 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 79. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Using MCMC, we can sample the age of the calibrated node • while conditioning on λ, μ, and ψ other node ages A and ⋆ 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 80. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) MCMC allows us to consider all possible values of ⋆ (marginalization) 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 81. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) MCMC allows us to consider all possible values of ⋆ (marginalization) 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 82. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) MCMC allows us to consider all possible values of ⋆ (marginalization) 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 83. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) MCMC allows us to consider all possible values of ⋆ (marginalization) 250 200 150 100 50 0 Time (My) Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 84. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) The posterior samples of the calibrated node age are informed by the fossil attachment times 250 200 150 100 50 0 Time (My) Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 85. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) The FBD model allows multiple fossils to calibrate a single node N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 86. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Given ⋆ and A, the new fossil can attach to the tree via speciation along either branch in the extant tree N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 87. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Given ⋆ and A, the new fossil can attach to the tree via speciation along either branch in the extant tree N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 88. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Given ⋆ and A, the new fossil can attach to the tree via speciation along either branch in the extant tree N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 89. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Or the unobserved branch leading to the other calibrating fossil N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 90. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) If ⋆ = A, then the new fossil lies directly on a branch in the extant tree N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 91. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) If ⋆ = A, then the new fossil lies directly on a branch in the extant tree N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 92. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Or it is an ancestor of the other calibrating fossil N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 93. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) The probability of this realization of the diversification process is conditional on: λ, μ, and ψ N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 94. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Using MCMC, we can sample the age of the calibrated node while conditioning on λ, μ, and ψ other node ages A and ⋆ A and ⋆ N 250 200 150 100 50 0 Time (My) N Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 95. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) MCMC allows us to consider all possible values of ⋆ (marginalization) 250 200 150 100 50 0 Time (My) Diversification of Fossil Extant Lineages (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 96. BAYESIAN INFERENCE UNDER THE FBD Implemented in: • DPPDiv: github.com/trayc7/FDPPDIV • BEAST2: beast2.cs.auckland.ac.nz/ Available soon: • RevBayes: github.com/revbayes/revbayes 150 100 50 0 Time 250 200 150 100 50 0 Time (My) FBD Implementation (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 97. LINEAGES THROUGH TIME The FBD model provides an estimate of the number of lineages over time 200 150 100 50 0 Time (My) 1.0 3.0 2.0 1.0 200 150 100 50 0 Time (My) Number of lineages
  • 98. LINEAGES THROUGH TIME Lineage diversity over time with fossils MCMC samples the times of lineages in the reconstructed tree and the times of the fossil lineages (for 1 simulation replicate with 10% random sample of fossils) Simulations: Results
  • 99. LINEAGES THROUGH TIME Lineage diversity over time with fossils Visualize extant and sampled fossil lineage diversification when using all available fossils (21 total) (for 1 simulation replicate with 10% random sample of fossils) Simulations: Results
  • 100. LINEAGES THROUGH TIME Lineage diversity over time with fossils Choosing only the oldest (calibration) fossils reduced the set of sampled fossils from 21 to 12, giving less information about diversification over time (for 1 simulation replicate with 10% random sample of fossils) Simulations: Results
  • 101. BEARS: DIVERGENCE TIMES Sequence data for extant species: • 8 Ursidae • 1 Canidae (gray wolf) • 1 Phocidae (spotted seal) Fossil ages: • 12 Ursidae • 5 Canidae • 5 Pinnipedimorpha DPP relaxed clock model (Heath, Holder, Huelsenbeck MBE 2012) Fixed tree topology Sequence Data Fossil Data Phylogenetic Relationships fossil canids fossil pinnepeds stem fossil ursids fossil Ailuropodinae giant short-faced bear cave bear Empirical Analysis (Wang 1994, 1999; Krause et al. 2008; Fulton Strobeck 2010; Abella et al. 2012)
  • 102. BEARS: DIVERGENCE TIMES Gray wolf Spotted seal Giant panda Spectacled bear Sloth bear Brown bear Polar bear Sun bear Am. black bear Asian black bear 1. fossil canids 2. fossil pinnepeds 2. stem fossil ursids 3. fossil Ailuropodinae 4. giant short-faced bear 5. cave bear 1 3 2 4 5 Empirical Analysis (Heath et al. PNAS 2014; silhouette images: http://phylopic.org/)
  • 103. BEARS: DIVERGENCE TIMES Gray wolf Spotted seal Giant panda Spectacled bear Sloth bear Brown bear Polar bear Sun bear Am. black bear Asian black bear Ursidae Eocene Oligocene Miocene 60 40 20 0 Time (My) Plio Pleis Paleocene 95% CI Empirical Analysis (Heath et al. PNAS 2014; silhouette images: http://phylopic.org/)
  • 104. BEARS: DIVERGENCE TIMES fossil canids fossil pinnipeds fossil Ailuropodinae fossil Arctodus fossil Ursus Gray wolf Spotted seal Giant panda Spectacled bear Sloth bear Brown bear Polar bear Sun bear Am. black bear Asian black bear Ursidae Eocene Oligocene Miocene 60 40 20 0 Time (My) Plio Pleis Paleocene stem fossil Ursidae Empirical Analysis (Heath et al. PNAS 2014; silhouette images: http://phylopic.org/)
  • 105. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Improved statistical inference of absolute node ages Biologically motivated models can better capture statistical uncertainty fossil canids fossil pinnipeds fossil Ailuropodinae fossil Arctodus fossil Ursus Gray wolf Spotted seal Giant panda Spectacled bear Sloth bear Brown bear Polar bear Sun bear Am. black bear Asian black bear Ursidae Eocene Oligocene Miocene 60 40 20 0 Time (My) Plio Pleis Paleocene stem fossil Ursidae Modeling Diversification Processes (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 106. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Improved statistical inference of absolute node ages Use all available fossils Eliminates arbitrary choice of calibration priors fossil canids fossil pinnipeds fossil Ailuropodinae fossil Arctodus fossil Ursus Gray wolf Spotted seal Giant panda Spectacled bear Sloth bear Brown bear Polar bear Sun bear Am. black bear Asian black bear Ursidae Eocene Oligocene Miocene 60 40 20 0 Time (My) Plio Pleis Paleocene stem fossil Ursidae Modeling Diversification Processes (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 107. THE FOSSILIZED BIRTH-DEATH PROCESS (FBD) Improved statistical inference of absolute node ages Extensions of the FBD can account for stratigraphic sampling of fossils and shifts in rates of speciation and extinction Preservation Rate 175 150 125 100 75 50 25 0 Time 0.2 1.05 Modeling Diversification Processes (Heath, Huelsenbeck, Stadler. PNAS 2014)
  • 108. FOSSIL TOTAL EVIDENCE DATING Combining extant and fossil species Sequence Data Fossil Age Data © AntWeb.org Morphological Data © AntWeb.org Orthoptera Paraneoptera Mecoptera Lepidoptera Coleoptera Adephaga Coleo Polyphaga Raphidioptera Neuroptera Xyela Macroxyela % of morphological characters scored for each terminal 0% 20% 40% 60% 80% 100% Blasticotoma Runaria Paremphytus Tenthredo Aglaostigma Dolerus Taxonus Selandria Strongylogaster Monophadnoides Metallus Hoplocampa Nematinus Nematus Cladius Monoctenus Gilpinia Diprion Athalia Cimbicinae Abia Corynis Arge Sterictiphora Perga Phylacteophaga Lophyrotoma Decameria Acordulecera Neurotoma Acantholyda Cephalcia Pamphilius Onycholyda Megalodontes skorniakowii Megalodontes cephalotes Cephus Calameuta Hartigia Syntexis Sirex Xeris Urocerus Tremex Xiphydria Orussus Stephanidae A Stephanidae B Cynipoidea Megalyridae Evanioidea Trigonalidae Vespidae Apoidea C Apoidea B Apoidea A Chalcidoidea Ichneumonidae Abrotoxyela Anagaridyela Chaetoxyela Spathoxyela Mesoxyela mesozoica Liadoxyela Eoxyela Grimmaratavites Brigittepterus Xyelula Sogutia Ferganolyda Prosyntexis Thoracotrema Ghilarella Sepulca Onokhoius Karatavites Aulisca Protosirex Aulidontes Trematothorax Rudisiricius Mesolyda Brachysyntexis Kulbastavia Syntexyela Anaxyela Palaeathalia Pseudoxyelocerus Dahuratoma Undatoma Leioxyela Triassoxyela Nigrimonticola Xyelotoma Pamphiliidae undescribed Turgidontes Praeoryssus Paroryssus Mesorussus Symphytopterus Cleistogaster Leptephialtites Stephanogaster 97 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 100 97 68 55 75 77 91 84 61 57 62 98 96 71 71 85 93 52 95 64 80 64 99 77 99 98 97 82 52 58 94 90 61 83 60 70 57 70 60 350 300 250 200 150 100 50 0 million years before present (Ronquist, Klopfstein, et al. Syst. Biol. 2012.)