Rapid and precise measurement of carbonate clumped isotopes using laser spectroscopy

Author:

Yanay Nitzan1ORCID,Wang Zhennan1ORCID,Dettman David L.12ORCID,Quade Jay1ORCID,Huntington Katharine W.3ORCID,Schauer Andrew J.3ORCID,Nelson David D.4ORCID,McManus J. Barry4,Thirumalai Kaustubh1ORCID,Sakai Saburo5,Rebaza Morillo Anna1ORCID,Mallik Ananya1ORCID

Affiliation:

1. Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA.

2. Estuary Research Center, Shimane University, Shimane, Japan.

3. Department of Earth and Space Sciences and IsoLab, University of Washington, Seattle, WA 98195, USA.

4. Aerodyne Research Inc., Billerica, MA 01821, USA.

5. Institute of Biogeochemistry, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa 237-0061, Japan.

Abstract

Carbonate clumped isotope abundance is an important paleothermometer, but measurement is difficult, slow, and subject to cardinal mass ( m/z ) interferences using isotope ratio mass spectrometry (IRMS). Here, we describe an optical spectroscopic measurement of carbonate clumped isotopes. We have adapted a tunable infrared laser differential absorption spectrometer (TILDAS) system to measure the abundances of four CO 2 isotopologues used for clumped isotope thermometry. TILDAS achieves the same precision (0.01‰ SE) as IRMS measurements rapidly (∼50 min per carbonate analysis) and using small samples (<2 mg of calcite), without making assumptions about 17 O abundance in the sample. A temperature calibration based on 406 analyses of CO 2 produced by digestion of 51 synthetic carbonates equilibrated at 6° to 1100°C is consistent with results for natural carbonates and previous calibrations. Our system results were indistinguishable from IRMS systems after replicating the InterCarb interlaboratory calibration. Measurement by TILDAS could change the landscape for clumped isotope analysis.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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