Research Results

3 What is IntCal?

Radiocarbon (14C) dating is the most widely used method in the world for dating time to about 50,000 years ago. However, dating based on the amount of 14C remaining is not always accurate and requires a 'conversion table', called a calibration model, to convert the measurements into true values.

 

The "conversion table" should not vary from one researcher to another, but should be standardized according to a global agreement among the scientific communities. The most widely used calibration model in the world today is called IntCal, which was first proposed in 1998 and has been updated in 2004, 2009, 2013 and 2020.

 

IntCal is the international standard "measure" that gives definition to geological time, functioning in the same way as the prototype metre or the Greenwich Observatory. Because of its outstanding quali-ty, the data from the Lake Suigetsu Varves was adopted in its entirety for the 2013 edition of IntCal (IntCal13), regarded as a major turning point in the history of IntCal.

 

Because of IntCal's principle of avoiding over-reliance on data from only one location, IntCal13 also combines data from not only Lake Suigetsu but also other locations. However, it is clear that the Lake Suigetsu Varves provides by far the most reliable data in the IntCal13 components in terms of the number of data used, the "determinacy" of the calibrated ages, and the "purity" of the data in that it did not have to take into account old carbon from deep sea water or limestone.

 

In August 2020, IntCal was updated for the first time in seven years (IntCal20).

 

The updated IntCal 20 includes about 250 new stalactite (stalagmite) data from China's Hulu Cave as well as about 500 pieces data from Lake Suigetsu, carried over from IntCal 13, making Lake Suigetsu and the Hulu Cave the two greatest sources of data.

 

 

Instructional video of IntCal20 (YouTube)