TY - JOUR
T1 - Atmospheric 14C/12C changes during the last glacial period from hulu cave
AU - Cheng, Hai
AU - Lawrence Edwards, R.
AU - Southon, John
AU - Matsumoto, Katsumi
AU - Feinberg, Joshua M.
AU - Sinha, Ashish
AU - Zhou, Weijian
AU - Li, Hanying
AU - Li, Xianglei
AU - Xu, Yao
AU - Chen, Shitao
AU - Tan, Ming
AU - Wang, Quan
AU - Wang, Yongjin
AU - Ning, Youfeng
N1 - Publisher Copyright:
© 2017 The Authors.
PY - 2018/12/14
Y1 - 2018/12/14
N2 - Paired measurements of 14C/12C and 230Th ages from two Hulu Cave stalagmites complete a precise record of atmospheric 14C covering the full range of the 14C dating method (~54,000 years). Over the last glacial period, atmospheric 14C/12C ranges from values similar to modern values to values 1.70 times higher (42,000 to 39,000 years ago). The latter correspond to 14C ages 5200 years less than calibrated ages and correlate with the Laschamp geomagnetic excursion followed by Heinrich Stadial 4. Millennial-scale variations are largely attributable to Earth’s magnetic field changes and in part to climate-related changes in the oceanic carbon cycle. A progressive shift to lower 14C/12C values between 25,000 and 11,000 years ago is likely related, in part, to progressively increasing ocean ventilation rates.
AB - Paired measurements of 14C/12C and 230Th ages from two Hulu Cave stalagmites complete a precise record of atmospheric 14C covering the full range of the 14C dating method (~54,000 years). Over the last glacial period, atmospheric 14C/12C ranges from values similar to modern values to values 1.70 times higher (42,000 to 39,000 years ago). The latter correspond to 14C ages 5200 years less than calibrated ages and correlate with the Laschamp geomagnetic excursion followed by Heinrich Stadial 4. Millennial-scale variations are largely attributable to Earth’s magnetic field changes and in part to climate-related changes in the oceanic carbon cycle. A progressive shift to lower 14C/12C values between 25,000 and 11,000 years ago is likely related, in part, to progressively increasing ocean ventilation rates.
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U2 - 10.1126/science.aau0747
DO - 10.1126/science.aau0747
M3 - Article
C2 - 30545886
AN - SCOPUS:85058446427
SN - 0036-8075
VL - 362
SP - 1293
EP - 1297
JO - Science
JF - Science
IS - 6420
ER -