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It subsequently evolved into the most powerful method of dating late Pleistocene and Holocene artifacts and geologic events up to about 50,000 years in age.The radiocarbon method is applied in many different scientific fields, including archeology, geology, oceanography, hydrology, atmospheric science, and paleoclimatology.The city of Thebes does not appear to have been of great significance before the 11th dynasty.Major construction work in the Precinct of Amun-Re took place during the 18th dynasty when Thebes became the capital of the unified ancient Egypt.

The Sheffield Dendrochronology Laboratory, Sheffield, England. The Dutch Centre for Dendrochronology (RING), Amersfoort, The Netherlands.The Climatic Research Unit, University of East Anglia, Norwich, England. Linked to: Radiocarbon dating the Dead Sea scrolls Northeastern Palaeo Indian Radiocarbon Database Debert, a palaeo Indian site in Nova Scotia Desert Research Institute Radiocarbon Laboratory (USA) Washington State University Radiocarbon Laboratory (USA) 7.11.95.Linked to: NOSAMS; the Woods Hole Oceanographic Institution's NOSAMS Facility.Much of the information presented in this section is based upon the Stuiver and Polach (1977) paper "Discussion: Reporting of C14 data". 1890 wood was chosen as the radiocarbon standard because it was growing prior to the fossil fuel effects of the industrial revolution.A copy of this paper may be found in the Radiocarbon Home Page The radiocarbon age of a sample is obtained by measurement of the residual radioactivity. T (National Institute of Standards and Technology; Gaithersburg, Maryland, USA) Oxalic Acid I (C). The activity of 1890 wood is corrected for radioactive decay to 1950. Ninety-five percent of the activity of Oxalic Acid from the year 1950 is equal to the measured activity of the absolute radiocarbon standard which is 1890 wood.