JpGU-AGU Joint Meeting 2020

Presentation information

[E] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS08] Paleoclimatology and paleoceanography

convener:Yusuke Okazaki(Department of Earth and Planetary Sciences, Graduate School of Science, Kyushu University), Benoit Thibodeau(University of Hong Kong), Akitomo Yamamoto(Japan Agency for Marine-Earth Science and TechnologyAtmosphere and Ocean Research Institute), Hitoshi Hasegawa(Faculty of Science and Technology, Kochi University)

[MIS08-22] Rapid and precise carbon dioxide clumped isotope composition analysis by tunable infrared laser differential absorption spectroscopy

*David L Dettman1, Zhennan Wang1, Jay Quade1, David D Nelson2, J Barry McManus2, Katharine W Huntington3, Andrew J Schauer3, Saburo Sakai4 (1.Univ. of Arizona, Dept. of Geosciences, 2.Aerodyne Research Inc., Boston, Massachusetts, 3.Univ. of Washington, Dept. of Earth and Space Sciences, 4.Japan Agency for Marine-Earth Science and Technology, Inst. of Biogeochemistry)

Keywords:clumped isotope, isotopologue, carbonate thermometry

Carbon dioxide clumped isotope thermometry is a relatively new and important technique in carbonate isotope geochemistry. The degree of heavy isotope clumping (e.g., 16O13C18O) beyond an expected random distribution can be related to the temperature of calcite precipitation. Unlike carbonate “paleotemperature” calculations, there is no need to constrain the isotopic composition of the water in which the carbonate grew. In addition, the independent temperature estimate, when combined with carbonate δ18O values, allows us to constrain paleowater δ18O values. However, the use of isotope ratio mass spectrometry (IRMS) to do these measurements remains relatively rare because it is time-consuming and costly. We have developed an isotope ratio laser spectrometry method using tunable infrared laser differential absorption spectroscopy (TILDAS) and describe our latest results using both gaseous carbon dioxide samples and CO2 derived from carbonate minerals. The TILDAS instrument has two continuous wave lasers to directly and simultaneously measure four isotopologues involved in the 16O13C18O equilibrium calculation. Because each isotopologue is independently resolved, this approach does not have to correct for isobaric peaks, i.e. separate families of absorbance peaks exist for 16O13C18O and 17O12C18O, even though both molecules have a mass of 47 AMU. The gas samples are trapped in a low volume (~250 ml) optical multi-pass cell with a path length of 36 meters. Raw data are collected at 1.6 kHz, providing 96,000 peak-area measurements of each CO2 isotopologue per minute. With a specially designed sampling system, each sample measurement is bracketed with measurements of a working reference gas, and a precision of 0.01‰ is achieved within 20 minutes, based on four repeated measurements. The total sample size needed for a complete measurement is approximately 15 μmol of CO2, or 1.5 mg of calcite equivalent. TILDAS reported Δ16O13C18O values show a linear relationship with theoretical calculations, with a very weak dependence on bulk isotope composition. The performance of the TILDAS system demonstrated in this study is competitive with the best IRMS systems and surpasses typical IRMS measurements in several key respects, such as measurement duration and isobaric interference problems. This method can easily be applied more widely in stable isotope geochemistry by changing spectral regions and laser configurations, leading to rapid and high precision (0.01‰) measurement of conventional stable isotope ratios and δ17O in CO2 gas samples.