[S-GL39] Geochronology and Isotope Geology

[SGL39-P04] High precision and high sensitive stable isotopic analysis by using original CF/DI-IRMS system for IsoPrime100

3-min talk in an oral session

Masaharu NAKANE¹, Takashi TANAKA¹, Tomomi TETSU¹, Haruka TAKAGI², *Toyoho ISHIMURA¹ (1.National Institute of Technology, Ibaraki College, 2.Waseda University)

Keywords:High precision, stable isotopic analysis, carbon and oxygen isotope, carbonate, development

The stable carbon and oxygen isotopic compositions (δ¹³C and δ¹⁸O) of calcium carbonate, especially biogenic calcite, are used for environmental analysis (e.g. reconstruction of paleo-seawater temperature). The measurement of δ¹³C and δ¹⁸O of calcium carbonate is performed based on the comparison between the δ¹³C and δ¹⁸O of international standard calcite. Through the analysis, the isotopic values of samples should be determined precisely in order to compare and discuss with the analytical results reported in previous studies. In this study, we have developed a sample preparation system for IRMS (isotope ratio mass spectrometer) for high precision and high sensitive analysis. As a result, analytical results of NBS-19 (international standard calcite) using the developed system with dual-inlet IsoPrime100 (IRMS) showed δ¹³C= +1.95 +/-0.026‰ and δ¹⁸O= -2.20 +/-0.056‰ in long-term external analytical precision (n=36). Moreover, we found that short-term external precision (within a day) for this system have achieved around +/-0.01‰. By using the developed system with continuous-flow IsoPrime100 (IRMS), we can determine δ¹³C and δ¹⁸O of calcite and seawater (as low as 0.1 microgram of CaCO₃; 1 nmol of CO₂) with standard deviations of +/-0.1 ‰.