estimate of its age (a raw radiocarbon age).[4] However, over time there are small fluctuations in the ratio of 14 C to 12 C in the atmosphere, fluctuations that have been noted in natural records of the past, such as sequences of tree rings and cave deposits. These C12/C14 ratio records allow fine-tuning, or "calibration", of the raw radiocarbon age, to give a more accurate estimate of the calendar date of the material. One of the most frequent uses of radiocarbon dating is to estimate the age…
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