Sakai Saburo, Matsuda Shinichi, Hikida Toshihide, Shimono Akio, McManus J Barry, Zahniser Mark, Nelson David, Dettman David L, Yang Danzhou, Ohkouchi Naohiko
Institute of Biogeochemistry , Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kaganaga 237-0061, Japan.
Department of Medical Chemistry and Molecular Pharmacology, College of Pharmacy, Purdue University , West Lafayette, Indiana 47907, United States.
Anal Chem. 2017 Nov 7;89(21):11846-11852. doi: 10.1021/acs.analchem.7b03582. Epub 2017 Oct 18.
Stable isotope ratios (O/O, C/C, and O/O) in carbonates have contributed greatly to the understanding of Earth and planetary systems, climates, and history. The current method for measuring isotopologues of CO derived from CaCO is primarily gas-source isotope ratio mass spectroscopy (IRMS). However, IRMS has drawbacks, such as mass overlap by multiple CO isotopologues and contaminants, the requirement of careful sample purification, and the use of major instrumentation needing permanent installation and a high power electrical supply. Here, we report simultaneous O/O, C/C, and O/O analyses for microgram quantities of CaCO using a tunable mid-infrared laser absorption spectroscopy (TILDAS) system, which has no mass overlap problem and yields high sensitivity/precision measurements on small samples, as small as 0.02 μmol of CO (equivalent to 2 μg of CaCO) with standard errors of less than 0.08 ‰ for O/O and C/C (±0.136 ‰ and ±0.387 ‰ repeatability; n = 10). In larger samples of CO, 0.68 μmol (or 68 μg of CaCO), standard error is less than 0.04 ‰ for O/O and C/C (< ±0.1 ‰ repeatability; n = 10) and 0.03 ‰ for O/O (±0.069 ‰ repeatability; n = 10). We also show, for the first time, the relationship between O/O ratios measured using the TILDAS system and published δO values of international standard materials (NBS-18 and -19) measured by IRMS. The benchtop TILDAS system, with cryogen-free sample preparation vacuum lines for microgram quantities of carbonates, is therefore a significant advance in carbonate stable isotope ratio geochemistry and is a new alternative to conventional IRMS.
碳酸盐中的稳定同位素比率(O/O、C/C和O/O)对理解地球和行星系统、气候及历史有很大帮助。目前测量源自CaCO的CO同位素异构体的方法主要是气体源同位素比率质谱法(IRMS)。然而,IRMS存在缺点,比如多种CO同位素异构体和污染物造成的质量重叠、需要仔细的样品纯化,以及使用需要永久安装和高功率电源的大型仪器。在此,我们报告了使用可调谐中红外激光吸收光谱(TILDAS)系统对微克量的CaCO进行O/O、C/C和O/O的同步分析,该系统不存在质量重叠问题,并且对小至0.02 μmol的CO(相当于2 μg的CaCO)的小样品能进行高灵敏度/高精度测量,O/O和C/C的标准误差小于0.08‰(重复性为±0.136‰和±0.387‰;n = 10)。在CO的较大样品(0.68 μmol,或68 μg的CaCO)中,O/O和C/C的标准误差小于0.04‰(重复性<±0.1‰;n = 10),O/O的标准误差为0.03‰(重复性±0.069‰;n = 10)。我们还首次展示了使用TILDAS系统测量的O/O比率与通过IRMS测量的国际标准物质(NBS - 18和 - 19)公布的δO值之间的关系。因此,具有用于微克量碳酸盐的无低温制冷样品制备真空管路的台式TILDAS系统是碳酸盐稳定同位素比率地球化学的一项重大进展,并且是传统IRMS的一种新替代方法。