Cal bp radiocarbon dating
From 14,000 to 26,000 years BP, 80% of the data in the Int Cal04 were provided by our laboratory and we have subsequently doubled the amount of data in the 14,000 to 26,000 year BP time interval (Cao et al., 2006; Fairbanks et al., 2005; 2006). Our calibration extends to the limits of radiocarbon age dating to 50,000 cal yrs B. using the same coral sample and data quality control measures and dating techniques as applied to our younger samples and those we provided to Int Cal04.Another difference between the selections of Int Cal04 versus our calibration program is philosophical.View the entire radiocarbon calibration curve here.The tree ring atmospheric radiocarbon calibration data set spanning 0 to 12,410 years BP is superior to all other atmospheric radiocarbon calibration data due to the number and quality of the radiocarbon measurements and the accuracy and precision of the tree dendrochronology (Stuiver et al., 1998; Reimer et al., 2004).
There are presently two choices for calibration curves beyond 12,410 years BP: Int Cal04 (Hughen et al., 2004) to 26,000 years or our calibration curve (Fairbanks et al., 2005) from 0 to 55,000 years BP.
In addition, we have reanalyzed the radiocarbon and U age dates from our earlier radiocarbon calibration work using new pretreatment and analytical techniques and state-of-the-art instrumentation at higher precision; we report these new results in this WEB site and in Fairbanks et al., (2005).
In our radiocarbon calibration paper (Fairbanks et al., 2005), we present paired C age determinations (Lawrence Livermore National Lab and Leibniz-Labor for Radiometric Dating and Isotope Research Christian-Albrechts University Kiel) that span the entire range of the radiocarbon dating technique and present a radiocarbon calibration curve based on a Bayesian statistical model with rigorous error estimations.
The papers describing the use of these curves are published in Radiocarbon: SHCal13 - Hogg et al 2013a and Int Cal13 – Reimer et al 2013.
Of practical importance to a wide range of scientific disciplines is the radiocarbon calibration, which is used for converting radiocarbon ages to calendar years; essential for measuring time and rates of change for numerous scientific fields.Due to the importance of an accurate and precise radiocarbon calibration curve, we have measured many samples in duplicate and validated the quality of the samples by dating the older samples with redundant U dates.