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INTCAL 13 AND MARINE 13 RADIOCARBON AGE CALIBRATION CURVES 0 – 50 , 000 YEARS CAL BP
The IntCal09 and Marine09 radiocarbon calibration curves have been revised utilizing newly available and updated data sets from 14C measurements on tree rings, plant macrofossils, speleothems,Expand
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Intcal09 and marine09 radiocarbon age calibration curves, 0–50,000 years cal bp
Additional co-authors: TJ Heaton, AG Hogg, KA Hughen, KF Kaiser, B Kromer, SW Manning, RW Reimer, DA Richards, JR Southon, S Talamo, CSM Turney, J van der Plicht, CE Weyhenmeyer
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Persistent Solar Influence on North Atlantic Climate During the Holocene
Surface winds and surface ocean hydrography in the subpolar North Atlantic appear to have been influenced by variations in solar output through the entire Holocene. The evidence comes from a closeExpand
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INTCAL98 radiocarbon age calibration, 24,000-0 cal BP.
The focus of this paper is the conversion of radiocarbon ages to calibrated (cal) ages for the interval 24,000-0 cal BP (Before Present, 0 cal BP = AD 1950), based upon a sample set ofExpand
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IntCal04 terrestrial radiocarbon age calibration, 0-26 cal kyr BP
A new calibration curve for the conversion of radiocarbon ages to calibrated (cal) ages has been constructed and internationally ratified to replace IntCal98, which extended from 0-24 cal kyr BPExpand
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INTCAL98 radiocarbon age calibration 24
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Marine04 marine radiocarbon age calibration, 0-26 cal kyr BP
New radiocarbon calibration curves, IntCal04 and Marine04, have been constructed and internationally rati- fied to replace the terrestrial and marine components of IntCal98. The new calibration dataExpand
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Synchronized TerrestrialAtmospheric Deglacial Records Around the North Atlantic
On the basis of synchronization of three carbon-14 (14C)-dated lacustrine sequences from Sweden with tree ring and ice core records, the absolute age of the Younger Dryas-Preboreal climatic shift wasExpand
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Observations and modelling of the global distribution and long-term trend of atmospheric 14CO2
Global high-precision atmospheric Δ14CO2 records covering the last two decades are presented, and evaluated in terms of changing (radio)carbon sources and sinks, using the coarse-grid carbon cycleExpand
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Tree rings and ice cores reveal C-14 calibration uncertainties during the Younger Dryas
The Younger Dryas interval during the Last Glacial Termination was an abrupt return to glacial-like conditions punctuating the transition to a warmer, interglacial climate. Despite recent advances inExpand
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