IntCal13

As 14C years is not equal to calendar years because atmospheric 14C concentration varies through time. Hence, data in AtmosphericNorth_CalC14 allows a calibration for mid-latitude Northern Hemisphere atmospher reservoir.

datasets

Bayesian analysis of luminescence data and C-14 age estimates. Bayesian models are based on the following publications: Combes, B. & Philippe, A. (2017) <doi:10.1016/j.quageo.2017.02.003> and Combes et al. (2015) <doi:10.1016/j.quageo.2015.04.001>. This includes, amongst others, data import, export, application of age models and palaeodose model.

Anne Philippe

BayLum

Chronological Bayesian Models Integrating Optically Stimulated
Luminescence and Radiocarbon Age Dating

Claire Christophe

Sebastian Kreutzer

Guillaume Guérin

Frederik Harly Baumgarten

Nicolas Frerebeau

IntCal13 function

A data frame with 3 variables.<dl>
 <dt><code>CAL.BP</code></dt>
<dd>a numeric vector correpondig to calendar years befor present</dd> <dt><code>X14C.age</code></dt>
<dd>a numeric vector correponding to 14C age</dd> <dt><code>Error</code></dt>
<dd>a numeric vector correponding to error arround 14C age measurement</dd> 
</dl>

Format

Atmospheric North data for calibration of 14C age — IntCal13

A data frame with 3 variables.<dl>
 <dt><code>CAL.BP</code></dt>
<dd>a numeric vector correpondig to calendar years befor present</dd>

 <dt><code>X14C.age</code></dt>
<dd>a numeric vector correponding to 14C age</dd>

 <dt><code>Error</code></dt>
<dd>a numeric vector correponding to error arround 14C age measurement</dd>

 
</dl>

IntCal13: Atmospheric North data for calibration of 14C age

Description

Usage

Arguments

Format

References

Examples