Paleontology & Geology

Radiocarbon Dating (Carbon-14) Equation

Calculates the radiocarbon age of organic archaeological and fossil specimens up to ~50,000 years old based on remaining ¹⁴C activity relative to pre-industrial modern carbon.

\[ t = -\frac{T_{1/2}}{\ln(2)} \cdot \ln\left( \frac{A}{A_0} \right) = -8267 \cdot \ln\left( \frac{A}{A_0} \right) \]
Plain Text Formula: t = -(5730 / ln(2)) * ln(A / A0) = -8267 * ln(A / A0)

📐 Variable Definitions & Parameters

Symbol Variable Name Standard Unit Physical Definition
\[ t \] Radiocarbon Age years Before Present (BP) Time elapsed since specimen ceased carbon assimilation
\[ A / A_0 \] Activity Fraction percent or ratio Current ¹⁴C specific activity divided by modern standard (13.56 dpm/g C)
\[ T_{1/2} \] C-14 Half-Life 5,730 years Cambridge standard physical half-life of Carbon-14

💡 Worked Engineering Example

Problem Statement:

A fossil bone displays 25% of modern ¹⁴C activity (A/A0 = 0.25). Calculate its age.

Step-by-Step Solution:

  1. ln(0.25) = -1.38629
  2. t = -8,267 * (-1.38629) = 11,460 years BP
  3. Alternatively: 2 half-lives elapsed = 2 * 5,730 = 11,460 years
🎯 Result: The specimen dates to 11,460 years BP (Younger Dryas / end of the Pleistocene epoch).
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