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Conversely, nuclear testing increased the amount of 14 C in the atmosphere, which attained a maximum in of almost twice what it had been before the testing began. Measurement of radiocarbon was originally done by beta-counting devices, which counted the amount of beta radiation emitted by decaying 14 C atoms in a sample.
More recently, accelerator mass spectrometry has become the method of choice; it counts all the 14 C atoms in the sample and not just the few that happen to decay during the measurements; it can therefore be used with much smaller samples as small as individual plant seedsand gives results much more quickly. The development of radiocarbon dating has had a profound impact on archaeology. In addition to permitting more accurate dating within archaeological sites than previous methods, it allows comparison of dates of events across great distances.
Histories of archaeology often refer to its impact as the ""radiocarbon revolution"". Radiocarbon dating has allowed key transitions in prehistory to be dated, such as the end of the last ice ageand the beginning of the Neolithic and Bronze Age in different regions.
InMartin Kamen and Samuel Ruben of the Radiation Laboratory at Berkeley began experiments to determine if martha stewart dating results of the elements common in organic matter had isotopes with half-lives long enough to be of value in biomedical research. They synthesized 14 C using the laboratory's cyclotron accelerator and soon discovered that the atom's half-life was far longer than had been previously thought. Korffthen employed at the Franklin Institute in Philadelphiathat the interaction of slow neutrons with 14 N in the upper atmosphere would create 14 C.
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