Precision and long-term stability of clumped isotope analysis of CO2by a small sector isotope ratio mass spectrometer
Precision and long-term stability of clumped isotope analysis of CO2by a small sector isotope ratio mass spectrometer
复制标题
小扇区同位素比质谱仪对 CO2 聚集同位素分析的精度和长期稳定性
DOI:
10.1002/rcm.6431
复制
发表时间:
2013
影响因子:
2
通讯作者:
Naohiro Yoshida
中科院分区:
文献类型:
--
作者:
Y. Kawamoto;M. Eto;T. Okabe;Y. Obayashi;T. Kaneko;J. Takahashi;H. Mita;K. Kanda;K. Kobayashi;Naohiro Yoshida
RATIONALEThe ratio of the measured abundance of13C–18O bonding CO2to its stochastic abundance, prescribed by the δ13C and δ18O values from a carbonate mineral, is sensitive to its growth temperature. Recently, clumped‐isotope thermometry, which uses this ratio, has been adopted as a new tool to elucidate paleotemperatures quantitatively.METHODSClumped isotopes in CO2were measured with a small‐sector isotope ratio mass spectrometer. CO2samples digested from several kinds of calcium carbonates by phosphoric acid at 25 °C were purified using both cryogenic and gas‐chromatographic separations, and their isotopic composition (δ13C, δ18O, Δ47, Δ48and Δ49values) were then determined using a dual‐inlet Delta XP mass spectrometer.RESULTSThe internal precisions of the single gas Δ47measurements were 0.005 and 0.02 ‰ (1 SE) for the optimum and the routine analytical conditions, respectively, which are comparable with those obtained using a MAT 253 mass spectrometer. The long‐term variations in the Δ47values for the in‐house working standard and the heated CO2gases since 2007 were close to the routine, single gas uncertainty while showing seasonal‐like periodicities with a decreasing trend. Unlike the MAT 253, the Delta XP did not show any significant relationship between the Δ47and δ47values.CONCLUSIONSThe Delta XP gave results that were approximately as precise as those of the MAT 253 for clumped‐isotope analysis. The temporal stability of the Delta XP seemed to be lower, although an advantage of the Delta XP was that no dependency of δ47on Δ47was found. Copyright © 2012 John Wiley & Sons, Ltd.