Description Usage Arguments Value References Examples
Quantile function that computes the age corresponding to a particular probability for the upper bound of a distribution of ages (Strauss & Sadler 1989, Gingerich & Uhen 1998, Solow 2003). The method of Strauss & Sadler (1989) assumes that the distribution of fossil ages is uniform and their formula depends on the fossil ages range and the number of fossil ages. The method of Solow (2003) is a general method for non-uniform distributions and depends on the temporal gap between the oldest and the second oldest fossil ages. Both methods assume that fossil ages are independent samples from the same distribution (only relevant for the two oldest ages for Solow's method), therefore, fossils should be as independent as possible (ideally from different geological formations and different regions).
In the particular case where there are only two fossil ages and no baseline age specified, Strauss & Sadler's and Solow's methods converge to the same result; the quantile functions are simply Xn/(1-P), and the likelihood function is 1/X.
1 |
p |
The desired probability level |
ages |
A vector of fossil ages. These do not need to be sorted |
baseline |
Youngest bound of the distribution that could be the present (=0) or some other geological age of reference. If a baseline is not provided, the minimum value of ages is used as baseline and n-1 is used for the sample size instead of n for calculations (Solow 2003). |
method |
Either |
A numeric value (or vector of numeric values, if multiple p values are provided) representing the age estimate of the clade origin given the method a p value provided
Claramunt2015cladeage
\insertRefGingerich1998cladeage
\insertRefNorris2015cladeage
\insertRefSolow2003cladeage
\insertRefStrauss1989cladeage
\insertRefWang2007cladeage
\insertRefWang2009cladeage
\insertRefWang2010cladeage
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