Extending the Calibrated Radiocarbon Record

The radiocarbon record is an important tool for accurate dating of climatic records, archaeological artifacts, and other records of past events. A calibrated record exists up to 24,000 years ago, but as [Bard][1] explains in his Perspective, extending the record beyond this time has been difficult. He highlights the record by [ Beck et al .][2], which covers 24,000 to 45,000 years before present. The record shows large fluctuations in the radiocarbon ratio and is an important step toward an extended calibrated record. [1]: http://www.sciencemag.org/cgi/content/full/292/5526/2443 [2]: http://www.sciencemag.org/cgi/content/short/292/5526/2453

[1]  G. Wasserburg,et al.  238U234U230Th232Th systematics and the precise measurement of time over the past 500,000 years , 1987 .

[2]  E. Bard,et al.  Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados corals , 1990, Nature.

[3]  J. Beck,et al.  A Large Drop in Atmospheric 14C/12C and Reduced Melting in the Younger Dryas, Documented with 230Th Ages of Corals , 1993, Science.

[4]  W. Broecker,et al.  Correlations between climate records from North Atlantic sediments and Greenland ice , 1993, Nature.

[5]  E. Bard,et al.  High concentration of atmospheric 14C during the Younger Dryas cold episode , 1995, Nature.

[6]  AMS 14C Dating of Varved Sediments from Lake Suigetsu, Central Japan and Atmospheric 14C Change During the Late Pleistocene , 1995 .

[7]  E. Bard,et al.  Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge , 1996, Nature.

[8]  C. Laj,et al.  Correlation of Marine 14C Ages from the Nordic Seas with the GISP2 Isotope Record: Implications for 14C Calibration Beyond 25 ka BP , 1997, Radiocarbon.

[9]  J. Overpeck,et al.  Deglacial changes in ocean circulation from an extended radiocarbon calibration , 1998, Nature.

[10]  Kitagawa,et al.  Atmospheric radiocarbon calibration to 45,000 yr B.P.: late glacial fluctuations and cosmogenic isotope production , 1998, Science.

[11]  E. Bard,et al.  Radiocarbon Calibration by Means of Mass Spectrometric 230Th/234U and 14C Ages of Corals: An Updated Database Including Samples from Barbados, Mururoa and Tahiti , 1998, Radiocarbon.

[12]  Revision and tentative extension of the tree-ring based 14C calibration, 9200-11,855 cal BP , 1998 .

[13]  J. W. Beck,et al.  INTCAL98 Radiocarbon Age Calibration, 24,000–0 cal BP , 1998, Radiocarbon.

[14]  P. Mellars The Neanderthal Problem Continued , 1999, Current Anthropology.

[15]  F. d’Errico,et al.  The Chronology and Taphonomy of the Earliest Aurignacian and Its Implications for the Understanding of Neandertal Extinction , 1999 .

[16]  Alexandra Schramm,et al.  Calibration of the 14C time scale to > 40 ka by 234U-230Th dating of Lake Lisan sediments (last glacial Dead Sea) , 2000 .

[17]  A. Kirkland,et al.  Hydrological impact of heinrich events in the subtropical northeast atlantic , 2000, Science.

[18]  K. Lambeck,et al.  Last Ice Age Millennial Scale Climate Changes Recorded in Huon Peninsula Corals , 2000, Radiocarbon.

[19]  Edwards,et al.  Extremely Large Variations of Atmospheric 14C Concentration During the Last Glacial Period , 2001, Science.

[20]  Humans on the Move , 2001, Science.