TY - JOUR
T1 - High-precision and high-resolution carbonate 230Th dating by MC-ICP-MS with SEM protocols
AU - Shen, Chuan Chou
AU - Wu, Chung Che
AU - Cheng, Hai
AU - Lawrence Edwards, R.
AU - Hsieh, Yu Te
AU - Gallet, Sylvain
AU - Chang, Ching Chih
AU - Li, Ting Yong
AU - Lam, Doan Dinh
AU - Kano, Akihiro
AU - Hori, Masako
AU - Spötl, Christoph
N1 - Funding Information:
We thank J. Schwieters, X. Wang, and B. Claudia for providing advice about instrumental techniques. We also thank H.-W. Chiang and N.D. Ngai for help with field work in Vietnam. Discussion with G.S. Burr of the University of Arizona was helpful. Constructive and comprehensive reviews by three anonymous reviewers significantly improved this paper. Funding for this research is provided by National Science Council Grants ( 98-2116-M-002-012 , 99-2628-M-002-012 , 100-2116-M-002-009 , and 101-2116-M-002-009 to C.C.S.) and NSF Grants ( 1103403 , 1103320 , 0908792 , and 0902867 to R.L.E.).
Publisher Copyright:
© 2012 Elsevier Ltd.
PY - 2012/12/15
Y1 - 2012/12/15
N2 - To facilitate the measurement of U-Th isotopic compositions suitable for high-precision and high-resolution 230Th dating of coral and speleothem carbonates, secondary electron multiplier (SEM) protocol techniques for multicollector inductively coupled plasma mass spectrometry (MC-ICP-MS) have been developed. The instrumental sensitivities are 1-2%, with a precision of ±1-2‰ (2σ) for abundance determination of 50-200fg 234U (1-4ng 238U) or 230Th. This method features chemistry refinements, improvements to procedural and instrumental blanks, spectral inference reductions, and careful consideration of non-linear SEM behavior. Measurement consistency of this MC-ICP-MS combined with previous mass spectrometric results on U-Th standards and a variety of carbonates demonstrates the validity of the SEM protocol method. For fossil corals, a routine U-Th isotopic determination at permil-level precision requires only 10-50mg of carbonate. As little as 200mg of young coral with an age of less than 20yr can be dated with a precision of ±0.3-0.8yr. About 20-200mg speleothem samples with sub-ppm-to-ppm U are required to earn a 5‰ precision on ages from 5 to 100kyr. Requirement of small sample size, 10-100s mg carbonate, can permit high temporal resolution to date speleothems with slow growth rates, i.e., 1-10mm/kyr. This high-precision 230Th chronology is critical to accurately establish age models, date events and splice geochemical proxy time series records from multiple samples in the fields of paleoclimatology and paleoceanography. The U-Th isotopic determination techniques described here can also be applied to different environmental samples, such as waters, rocks, and sediments.
AB - To facilitate the measurement of U-Th isotopic compositions suitable for high-precision and high-resolution 230Th dating of coral and speleothem carbonates, secondary electron multiplier (SEM) protocol techniques for multicollector inductively coupled plasma mass spectrometry (MC-ICP-MS) have been developed. The instrumental sensitivities are 1-2%, with a precision of ±1-2‰ (2σ) for abundance determination of 50-200fg 234U (1-4ng 238U) or 230Th. This method features chemistry refinements, improvements to procedural and instrumental blanks, spectral inference reductions, and careful consideration of non-linear SEM behavior. Measurement consistency of this MC-ICP-MS combined with previous mass spectrometric results on U-Th standards and a variety of carbonates demonstrates the validity of the SEM protocol method. For fossil corals, a routine U-Th isotopic determination at permil-level precision requires only 10-50mg of carbonate. As little as 200mg of young coral with an age of less than 20yr can be dated with a precision of ±0.3-0.8yr. About 20-200mg speleothem samples with sub-ppm-to-ppm U are required to earn a 5‰ precision on ages from 5 to 100kyr. Requirement of small sample size, 10-100s mg carbonate, can permit high temporal resolution to date speleothems with slow growth rates, i.e., 1-10mm/kyr. This high-precision 230Th chronology is critical to accurately establish age models, date events and splice geochemical proxy time series records from multiple samples in the fields of paleoclimatology and paleoceanography. The U-Th isotopic determination techniques described here can also be applied to different environmental samples, such as waters, rocks, and sediments.
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U2 - 10.1016/j.gca.2012.09.018
DO - 10.1016/j.gca.2012.09.018
M3 - Article
AN - SCOPUS:84867641348
SN - 0016-7037
VL - 99
SP - 71
EP - 86
JO - Geochmica et Cosmochimica Acta
JF - Geochmica et Cosmochimica Acta
ER -