inverseSurv | R Documentation |
This function replicates the model-fitting procedure for forward and reverse survivorship curve data, described by Michael Foote in a series of papers (2001, 2003a, 2003b, 2005). These methods are discrete interval taxon ranges, as are used in many other functions in paleotree (see function arguments). This function can implement the continuous time, pulsed interval and mixed models described in Foote (2003a and 2005).
make_inverseSurv( timeList, groups = NULL, p_cont = TRUE, q_cont = TRUE, PA_n = "fixed", PB_1 = 0, Nb = 1, drop.extant = TRUE )
timeList |
A two column matrix, with the first and last occurrences of taxa
given in relative time intervals (i.e. ordered from first to last). If a list
of |
groups |
Either NULL (the default) or matrix with the number of rows equal
to the number of taxa and the number of columns equal to the number of 'systems'
of categories for taxa. Taxonomic membership in different groups is indicated
by numeric values.
For example, a dataset could have a 'groups' matrix composed of a column representing
thin and thick shelled taxa, coded |
p_cont |
If |
q_cont |
If |
PA_n |
The probability of sampling a taxon after the last interval
included in a survivorship study. Usually zero for extinct groups,
although more logically has the value of 1 when there are still extant
taxa (i.e., if the last interval is the Holocene and the group is
still alive, the probability of sampling them later is probably 1...).
Should be either be (a) a numeric value between |
PB_1 |
The probability of sampling a taxon before the first interval
included in a survivorship study. Should be a value of 0 to 1, or |
Nb |
The number of taxa that enter an interval (the |
drop.extant |
Drops all extant taxa from a dataset before preceding. |
The design of this function to handle mixed continuous and discrete time models means that parameters can mean very different things, dependent on how a model is defined. Users should carefully evaluate their function arguments and the discussion of parameter values as described in the Value section.
A function of class paleotreeFunc
, which takes a vector equal to the number
of parameters and returns the *negative* log likelihood
(for use with optim
and
similar optimizing functions, which attempt to minimize support values).
See the functions listed at modelMethods
for manipulating and examining
such functions and constrainParPaleo
for constraining parameters.
The function output will take the largest number of parameters possible with respect to groupings and time-intervals, which means the number of parameters may number in the hundreds. Constraining the function for optimization is recommended except when datasets are very large.
Parameters in the output functions are named p
, q
and r
, which are
respectively the origination, extinction and sampling parameters. If the
respective arguments p_cont
and q_cont
are TRUE
, then p
and q
will
represent the instantaneous per-capita origination and extinction rates
(in units of per lineage time-units). When one of these arguments is given as FALSE
,
the respective parameter (p
or q
) will represent per-lineage-interval rates.
For p
, this will be the per lineage-interval rate of a lineage producing
another lineage (which can exceed 1 because diversity can more than double) and
for q
, this will be the per lineage-interval 'rate' of a lineage going extinct,
which cannot be observed to exceed 1
(because the proportion of diversity that goes extinct cannot exceed 1).
To obtain the per lineage-interval rates from a
set of per lineage-time unit rates, simply multiply the per lineage-time-unit
rate by the duration of an interval (or divide, to do the reverse; see Foote,
2003 and 2005). r
is always the instantaneous per-capita sampling rate, in
units per lineage-time units.
If PA_n
or PB_1
were given as NULL
in the arguments, two additional parameters
will be added, named respectively PA_n
and PB_1
, and listed separately for every
additional grouping. These are the probability of a taxon occurring before the first
interval in the dataset (PB_1
) and the probability of a taxon occurring after
the last interval in a dataset (PA_n
). Theses will be listed as PA_n.0
and PB_1.0
to indicate that they are not related to any particular time-interval included
in the analysis, unlike the p
, q
, and r
parameters (see below).
Groupings follow the parameter names, separated by periods; by default, the
parameters will be placed in groups corresponding to the discrete intervals
in the input timeList
, such that make_inverseSurv
will create a function with
parameters p.1
, q.1
and r.1
for interval 1; p.2
, q.2
and r.2
for
interval 2 and so on. Additional groupings given by the user are listed after
this first set (e.g. 'p.1.2.2
').
Because of the complicated grouping and time interval scheme, combined with the probable preference of users to use constrained models rather that the full models, it may be difficult to infer what the rates for particular intervals and groups actually are in the final model, given the parameters that were found in the final optimization.
To account for this, the function output by inverseSurv
also contains
an alternative mode which takes input rates and returns the final values along with
a rudimentary plotting function. This allows users to output per-interval and per-group
parameter estimates. To select these feature, the argument altMode
must
be TRUE
. This function will invisibly return the rate values for each
group and interval as a list of matrices, with each matrix composed of the
p
, q
and r
rates for each interval, for a specific grouping.
This plotting is extremely primitive, and most users will probably find the
invisibly returned rates to be of more interest. The function layout
is
used to play plots for different groupings in sequence, and this may lead to
plots which are either hard to read or even cause errors (because of too many
groupings, producing impossible plots). To repress this, the argument plotPar
can be set to FALSE
.
This capability means the function has more arguments that just the
usual par
argument that accepts the vector of parameters for running an
optimization. The first of these additional arguments, altMode
enables
this alternative mode, instead of trying to estimate the negative log-likelihood
from the given parameters. The other arguments augment the calculation and plotting
of rates.
To summarize, a function output by inverseSurv
has the following arguments:
A vector of parameters, the same length as the number of parameters needed. For plotting, can be obtained with optimization
If FALSE
(the default) the function will work like ordinary model-fitting functions,
returning a negative log-likelihood value for the input parameter values in par
. If TRUE
,
however, the input parameters will instead be translated into the by-interval, by-group rates
used for calculating the log-likelihoods, plotted (if plotPar
is TRUE
) and these final
interval-specific rates will be returned invisibly as described above.
If TRUE
(the default) the calculated rates will be plotted, with each
grouping given a separate plot. This can be repressed by setting plotPar
to FALSE
. As the only
conceivable purpose for setting plotPar
to FALSE
is to get the calculated rates, these will not
be returned invisibly if plotPar
is FALSE
.
If FALSE
, the default option, the rates plotted and returned will
be in units per lineage-time units, if those rates were being treated as rates for a
continuous-time process (i.e. p_cont = TRUE
and q_cont = TRUE
for p
and q
, respectively,
while r is always per lineage-time units). Otherwise, the respective rate will be in
units per lineage-interval. If ratesPerInt
is TRUE
instead, then all rates, even
rates modeled as continuous-time process, will be returned as per lineage-interval rates,
even the sampling rate r
.
If FALSE
(the default) rates are plotted on a linear scale. If TRUE
,
rates are plotted on a vertical log axis.
If TRUE
(default) the sampling rate and extinction rate will be plotted slightly
ahead of the origination rate on the time axis, so the three rates can be easily differentiated.
If FALSE
, this is repressed.
The position of a legend indicating which line is
which of the three rates on the resulting plot. This
is given as the possible positions for argument x
of the function
legend
, and by default is "topleft"
, which will be generally
useful if origination and extinction rates are initially low. If
legendPosition = NA
, then a legend will not be plotted.
This function is an entirely new rewrite of the methodology derived and presented by Foote in his studies. Thus, whether it would give identical results cannot be assumed nor is it easy to test given differences in the way data is handled between our coded functions. Furthermore, there may be differences in the math due to mistakes in the derivations caught while this function was programmed. I have tested the function by applying it to the same Sepkoski genus-level dataset that Foote used in his 2003 and 2005 papers. Users can feel free to contact me for detailed figures from this analysis. Overall, it seems my function captured the overall pattern of origination and sampling rates, at least under a model where both origination and extinction are modeled as continuous-time processes. Extinction showed considerably more variability relative to the published figures in Foote (2005). Additional analyses are being run to identify the sources of this discrepancy, and the function is being released here in paleotree on a trial basis, so that it can be more easily loaded onto remote servers. Users should be thus forewarned of this essentially 'beta' status of this function.
David W. Bapst, with some advice from Michael Foote.
Foote, M. 2001. Inferring temporal patterns of preservation, origination, and extinction from taxonomic survivorship analysis. Paleobiology 27(4):602-630.
Foote, M. 2003a. Origination and Extinction through the Phanerozoic: A New Approach. The Journal of Geology 111(2):125-148.
Foote, M. 2003b. Erratum: Origination and Extinction through the Phanerozoic: a New Approach. The Journal of Geology 111(6):752-753.
Foote, M. 2005. Pulsed origination and extinction in the marine realm. Paleobiology 31(1):6-20.
This function extensively relies on footeValues
.
A similar format for likelihood models can be seen in durationFreq
.
Also see freqRat
, sRate2sProb
,
qsRate2Comp
sProb2sRate
and qsProb2Comp
.
For translating between sampling probabilities and sampling rates, see
SamplingConv
.
# let's simulate some taxon ranges from an imperfectly sampled fossil record set.seed(444) record <- simFossilRecord( p = 0.1, q = 0.1, nruns = 1, nTotalTaxa = c(30,40), nExtant = 0 ) taxa <- fossilRecord2fossilTaxa(record) rangesCont <- sampleRanges(taxa, r = 0.5) #bin the ranges into discrete time intervals rangesDisc <- binTimeData(rangesCont, int.length = 5) #apply make_inverseSurv likFun <- make_inverseSurv(rangesDisc) #use constrainParPaleo to make the model time-homogeneous # match.all ~ match.all will match parameters # so only 2 parameters: p (= q) and r constrFun <- constrainParPaleo(likFun, match.all~match.all) results <- optim(parInit(constrFun), constrFun, lower = parLower(constrFun), upper = parUpper(constrFun), method = "L-BFGS-B", control = list(maxit = 1000000) ) results #plot the results constrFun(results$par, altMode = TRUE) ## Not run: #unconstrained function with ALL of the 225 possible parameters!!! # this will take forever to converge optim(parInit(likFun), likFun, lower = parLower(likFun), upper = parUpper(likFun), method = "L-BFGS-B", control = list(maxit = 1000000) ) ## End(Not run)
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