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The lab also provides δ13C measurements NOT in conjunction with C14 analysis except for water samples.

The following is a list of links to pages that might share the same title.Please follow one of the disambiguation links below or search to find the page you were looking for if it is not listed.Variations as such are unrelated to time and natural radioactive decay.It is common practice in radiocarbon laboratories to correct radiocarbon activities for sample fractionation.Fractionation during the geochemical transfer of carbon in nature produces variation in the equilibrium distribution of the isotopes of carbon (12C, 13C and 14C).

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Craig (1953) first identified that certain biochemical processes alter the equilibrium between the carbon isotopes.

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