Chemical separation and MC-ICPMS analysis of U, Th, Pa and Ra isotope ratios of carbonates. Issue 8 (11th July 2018)

• Record Type: Journal Article
• Authors: Obert, J. Christina; Scholz, Denis; Lippold, Jörg; Felis, Thomas; Jochum, Klaus Peter; Andreae, Meinrat O.
• Is Part Of: Journal of analytical atomic spectrometry. Volume 33:Issue 8(2018)
• Page Start: 1372
• Page End: 1383
• Publication Date: 2018-07-11
• Subjects: Atomic spectra -- Periodicals; Atomic absorption spectroscopy -- Periodicals; 543.0858
• DOI: 10.1039/c7ja00431a
• Languages: English
• ISSNs: 0267-9477

Abstract

Abstract : Ion exchange chemistry and MC-ICPMS measurements of U, Th, Pa and Ra isotope ratios from the same carbonate sample. Abstract : Diagenetic alteration of fossil reef corals may have severe effects on the reliability of 230 Th/U-ages. The widely applied criteria introduced to test for the reliability of coral 230 Th/U-ages are often not sufficient to identify all altered ages. The combination of 230 Th/U- with 231 Pa/U-dating has been suggested as a promising method to identify altered ages. Furthermore, 226 Ra/ 230 Th ratios can provide information about the diagenetic history during the last 10 000 years. Here we present a method to chemically separate U, Th, Pa and Ra from the same aliquot of a carbonate sample. The isotope ratios of our mixed U–Th–Pa–Ra spike are calibrated using a secular equilibrium material treated in the same way as the samples during chemical separation and mass spectrometric analysis. This approach does not only circumvent corrections for the radioactive decay of the short-lived 233 Pa spike, but also enables us to estimate the reproducibility of the spike calibration. The relative standard deviation (RSD) of the spike ratios is 0.27% for 229 Th/ 236 U, 4.2% for 228 Ra/ 236 U and between 0.6 and 4.0% for 233 Pa/ 236 U. The RSDs of the final ratios are 1.2% for 231 Pa/ 235 U and 3.4% for 226 Ra/ 230 Th. We assess the individual sources of uncertainty ( e.g., mass spectrometric corrections, counting statistics, and spike calibration) in detail and quantify their contribution to the total uncertainties of the final isotope ratios. Most corrections contribute only moderately to the final uncertainties. However, in the case of a large abundance of natural isotopes in the spike, this correction can have a large influence on both the ratios and their uncertainties. Another parameter affecting the final uncertainties and the reproducibility of the method is the sample size and, thus, the concentration of the natural isotopes. This discussion provides useful guidelines for future applications and can be adjusted to the individual requirements of a specific user.