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Correction for the 17O interference in δ(13C) measurements when analyzing CO2 with stable isotope mass spectrometry (IUPAC Technical Report)
Open accessAbstract
Measurements of δ( 13 C) determined on CO 2 with an isotope-ratio mass spectrometer (IRMS) must be corrected for the amount of 17 O in the CO 2 . For data consistency, this must be done using identical methods by different laboratories. This report aims at unifying data treatment for CO 2 IRMS by proposing (i) a unified set of numerical values, and (ii) a unified correction algorithm, based on a simple, linear approximation formula. Because the oxygen of natural CO 2 is derived mostly from the global water pool, it is recommended that a value of 0.528 be employed for the factor λ, which relates differences in 17 O and 18 O abundances. With the currently accepted N ( 13 C)/ N ( 12 C) of 0.011 180(28) in VPDB (Vienna Peedee belemnite) reevaluation of data yields a value of 0.000 393(1) for the oxygen isotope ratio N ( 17 O)/ N ( 16 O) of the evolved CO 2 . The ratio of these quantities, a ratio of isotope ratios, is essential for the 17 O abundance correction: [ N ( 17 O)/ N ( 16 O)]/[ N ( 13 C)/ N ( 12 C)] = 0.035 16(8). The equation [δ( 13 C) ≍ 45 δ VPDB-CO2 + 2 17 R / 13 R ( 45 δ VPDB-CO2 – λ 46 δ VPDB-CO2 )] closely approximates δ( 13 C) values with less than 0.010 ‰ deviation for normal oxygen-bearing materials and no more than 0.026 ‰ in extreme cases. Other materials containing oxygen of non-mass-dependent isotope composition require a more specific data treatment. A similar linear approximation is also suggested for δ( 18 O). The linear approximations are easy to implement in a data spreadsheet, and also help in generating a simplified uncertainty budget.
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“Due to the possible large uncertainties related to Assonov 17 O calibration parameters (50-53), we calculated raw Δ 47 values using the 17 O calibration parameters reported in ref. 53, which have been shown to improve interlaboratory data consistency (54).”
From Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the "dolomite problem" (2020) · cites this paper as [53]
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“The preceding interlaboratory bias correction of the temperature calibration for dolomites based on a single standard may not be optimal, but it is still better for Δ 47 temperature calculations than direct use of the original calibration in ref. 50, which was not given in the Brand parametric framework nor calibrated to the ETH standard values reported in ref. 53.”
From Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the "dolomite problem" (2020) · cites this paper as [53]
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Bernasconi, S. M., Daëron, M., Bergmann, K. D., Bonifacie, M., Meckler, A. N., Affek, H. P., Anderson, N., Bajnai, D., Barkan, E., Beverly, E., et al. (2021) · Geochemistry Geophysics Geosystems · doi:10.1029/2020gc009588 · Cited by 340
Anderson, N. T., Kelson, J. R., Kele, S., Daëron, M., Bonifacie, M., Horita, J., Mackey, T. J., John, C. M., Kluge, T., Petschnig, P., et al. (2021) · Geophysical Research Letters · doi:10.1029/2020gl092069 · Cited by 323
Bernasconi, S. M., Müller, I. A., Bergmann, K. D., Breitenbach, S. F. M., Fernandez, A., Hodell, D. A., Jaggi, M., Meckler, A. N., Millan, I., & Ziegler, M. (2018) · Geochemistry, Geophysics, Geosystems · doi:10.1029/2017gc007385 · Cited by 301
“Because a detailed discussion of the derivation and choice of these parameters was published by Brand et al. (2010), the above authors refer to these parameters as the Brand parameters.”
BackgroundAbsolute isotopic abundance ratios and the accuracy of Δ47 measurements
Daëron, M., Blamart, D., Peral, M., & Affek, H. P. (2016) · Chemical Geology · doi:10.1016/j.chemgeo.2016.08.014 · Cited by 310
Stable isotope deltas: tiny, yet robust signatures in nature
Brand, W. A., & Coplen, T. B. (2012) · Isotopes in Environmental and Health Studies · doi:10.1080/10256016.2012.666977 · Cited by 289
“with i denoting the mass number of the heavy isotope of element E (the mostly more abundant lighter isotope is omitted in this short-hand form of δ, for extended versions, see, for instance, [15]),4 Rsa is the respective isotope number ratio of a sample, and Rref is that of the reference material.”
BackgroundSelf-citationMost Earth-surface calcites precipitate out of isotopic equilibrium
Daëron, M., Drysdale, R. N., Peral, M., Huyghe, D., Blamart, D., Coplen, T. B., Lartaud, F., & Zanchetta, G. (2019) · Nature Communications · doi:10.1038/s41467-019-08336-5 · Cited by 236
Self-citationA revised 1000 year atmospheric δ13C‐CO2 record from Law Dome and South Pole, Antarctica
Rubino, M., Etheridge, D. M., Trudinger, C. M., Allison, C. E., Battle, M. O., Langenfelds, R. L., Steele, L. P., Curran, M., Bender, M., White, J. W. C., et al. (2013) · Journal of Geophysical Research Atmospheres · doi:10.1002/jgrd.50668 · Cited by 238
“A new 17O-correction algorithm [Brand et al., 2010] has been used to derive ı13C and ı18O from the measured ı45CO2 and ı46CO2 allowing improved external comparisons (with other data sets).”
MethodInfluentialBonifacie, M., Calmels, D., Eiler, J. M., Horita, J., Chaduteau, C., Vasconcelos, C., Agrinier, P., Katz, A., Passey, B. H., Ferry, J. M., et al. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2016.11.028 · Cited by 233
Compiled records of carbon isotopes in atmospheric CO 2 for historical simulations in CMIP6
Graven, H., Allison, C. E., Etheridge, D. M., Hammer, S., Keeling, R. F., Levin, I., Meijer, H. A. J., Rubino, M., Tans, P. P., Trudinger, C. M., et al. (2017) · Geoscientific model development · doi:10.5194/gmd-10-4405-2017 · Cited by 270
Petersen, S. V., Defliese, W. F., Saenger, C., Daëron, M., Huntington, K. W., John, C. M., Kelson, J. R., Bernasconi, S. M., Colman, A. S., Kluge, T., et al. (2019) · Geochemistry, Geophysics, Geosystems · doi:10.1029/2018gc008127 · Cited by 209
“Beginning from either raw voltages or sample mean δ 45 to δ 49 values, data was reprocessed two ways, using the SG parameters de fi ned by Huntington et al. (2009) or the updated “ IUPAC ” parameters de fi ned by Brand et al. (2010).”
InfluentialNormalization of stable isotope data for carbonate minerals: Implementation of IUPAC guidelines
Kim, S.-T., Coplen, T. B., & Horita, J. (2015) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2015.02.011 · Cited by 207
Self-citationHigh‐precision measurements of 17 O/ 16 O and 18 O/ 16 O ratios in CO 2
Barkan, E., & Luz, B. (2012) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.6400 · Cited by 255
Kelson, J. R., Huntington, K. W., Schauer, A. J., Saenger, C., & Lechler, A. R. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2016.10.010 · Cited by 177
A revised calibration of the clumped isotope thermometer
Zaarur, S., Affek, H. P., & Brandon, M. T. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.07.026 · Cited by 163
“Note that (4c) is an empirical relationship that is calibrated for mass-dependent fractionation in terrestrial environments (Brand et al., 2010).”
BackgroundChang, B., Li, C., Liu, D., Foster, I., Tripati, A., Lloyd, M. K., Maradiaga, I., Luo, G., An, Z., She, Z., et al. (2020) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1916673117 · Cited by 159
Schauer, A. J., Kelson, J., Saenger, C., & Huntington, K. W. (2016) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.7743 · Cited by 157
Dual clumped isotope thermometry resolves kinetic biases in carbonate formation temperatures
Bajnai, D., Guo, W., Spötl, C., Coplen, T. B., Methner, K., Löffler, N., Krsnik, E., Gischler, E., Hansen, M., Henkel, D., et al. (2020) · Nature Communications · doi:10.1038/s41467-020-17501-0 · Cited by 147
Self-citationMüller, I. A., Fernández, Á., Radke, J., van Dijk, J., Bowen, D., Schwieters, J. B., & Bernasconi, S. M. (2017) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.7878 · Cited by 141
“All data have been processed using the parameters from([33]) for the (17)O abundance correction, as recently recommended([34]).”
MethodA robust calibration of the clumped isotopes to temperature relationship for foraminifers
Meinicke, N., Ho, S. L., Hannisdal, B., Nürnberg, D., Tripati, A., Schiebel, R., & Meckler, A. N. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.11.022 · Cited by 121
“For example, the intercept of the travertine calibration of Kele et al. (2015) decreased by 0.038‰ with the updated 17O abundance correction of Brand et al. (2010) (Bernasconi et al., 2018).”
InfluentialUpdated calibration of the clumped isotope thermometer in planktonic and benthic foraminifera
Peral, M., Daëron, M., Blamart, D., Bassinot, F., Dewilde, F., Smialkowski, N., Isguder, G., Bonnin, J., Jorissen, F., Kissel, C., et al. (2018) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.07.016 · Cited by 113
A proxy for all seasons? A synthesis of clumped isotope data from Holocene soil carbonates
Kelson, J. R., Huntington, K. W., Breecker, D. O., Burgener, L. K., Gallagher, T. M., Hoke, G. D., & Petersen, S. V. (2020) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2020.106259 · Cited by 113
Experimental calibration of clumped isotope reordering in dolomite
Lloyd, M. K., Ryb, U., & Eiler, J. M. (2018) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.08.036 · Cited by 100
“…available and regularly updated (www.github.com/maxmansaxman/clumpy). δ13C and δ18O values (and by extension, raw ∆47 values) were calculated using the Brand et al. (2010) reference parameters recommended by Daëron et al. (2016) and Schauer et al. (2016) and the Taylor polynomial method…”
MethodPagel, M., Bonifacie, M., Schneider, D., Gautheron, C., Brigaud, B., Calmels, D., Cros, A., Saint-Bézar, B., Landrein, P., Sutcliffe, C. N., et al. (2017) · Chemical Geology · doi:10.1016/j.chemgeo.2017.12.026 · Cited by 120
Ostrom, N. E., & Ostrom, P. H. (2011) · Advances in isotope geochemistry · doi:10.1007/978-3-642-10637-8_23 · Cited by 84
“was initially developed by Harmon Craig and has been followed with more recent improvements (Craig 1957; Santrock et al. 1985; Kaiser 2008; Kaiser and Ro¨ckmann 2008; Brand et al. 2010 ).”
MethodBergmann, K., Finnegan, S., Creel, R. C., Eiler, J. M., Hughes, N. C., Popov, L. E., & Fischer, W. W. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2017.11.015 · Cited by 100
“Following Schauer et al. (2016) and Daëron et al. (2016), we used 17O correction parameters outlined in Brand et al. (2010).”
MethodInfluentialA guide for proper utilisation of stable isotope reference materials
Meier-Augenstein, W., & Schimmelmann, A. (2019) · Isotopes in Environmental and Health Studies · doi:10.1080/10256016.2018.1538137 · Cited by 77
“‰ symbol) being confused with an SI unit, particularly in graphs and tables, one can present relative abundance data as 10(3) × δ values [9,10].”
BackgroundAssonov, S., Groening, M., Fajgelj, A., Hélie, J., & Hillaire‐Marcel, C. (2020) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8867 · Cited by 75
Self-citationEnsuring the reliability of stable isotope ratio data—beyond the principle of identical treatment
Carter, J. F., & Fry, B. (2013) · Analytical and Bioanalytical Chemistry · doi:10.1007/s00216-012-6551-0 · Cited by 71
“53 [29], the “Craig” algorithm is retained to maintain comparability with published data, especially δ (13)C determination of carbonates.”
Clumped isotope fractionation during phosphoric acid digestion of carbonates at 70 °C
Müller, I. A., Violay, M. E. S., Storck, J.-C., Fernandez, A., van Dijk, J., Madonna, C., & Bernasconi, S. M. (2017) · Chemical Geology · doi:10.1016/j.chemgeo.2016.11.030 · Cited by 64
Rates of dark CO2 fixation are driven by microbial biomass in a temperate forest soil
Akinyede, R., Taubert, M., Schrumpf, M., Trumbore, S. E., & Küsel, K. (2020) · Soil Biology and Biochemistry · doi:10.1016/j.soilbio.2020.107950 · Cited by 86
Resetting Southern Tibet: The serious challenge of obtaining primary records of Paleoaltimetry
Quade, J., Leary, R., Dettinger, M., Orme, D., Krupa, A., DeCelles, P., Kano, A., Kato, H., Waldrip, R., Huang, W.-T., et al. (2020) · Global and Planetary Change · doi:10.1016/j.gloplacha.2020.103194 · Cited by 63
Mangenot, X., Gasparrini, M., Rouchon, V., & Bonifacie, M. (2017) · Sedimentology · doi:10.1111/sed.12427 · Cited by 78
“Noticeably, the recent work of Da€eron et al. (2016) and Schauer et al. (2016) underlines that when the 17O parameters from Brand et al. (2010) are used to process isotopic data [instead of the 17O parameters from Santrock et al. (1985) commonly used in the clumped isotope community to date], small…”
BackgroundSwart, P. K., Murray, S. T., Staudigel, P. T., & Hodell, D. A. (2019) · Geochemistry, Geophysics, Geosystems · doi:10.1029/2019gc008209 · Cited by 60
“The δ13C and δ18O values of the CO2 were calculated from the ratios of masses 45/44 and 46/44 measured using a Thermo 253 and corrected for the typical isobaric interferences using the methods of Brand et al. (2010).”
MethodLi, L., Fan, M., Davila, N., Jesmok, G., Mitsunaga, B., Tripati, A., & Orme, D. (2018) · Geological Society of America Bulletin · doi:10.1130/b32060.1 · Cited by 65
Optimizing the Use of Carbonate Standards to Minimize Uncertainties in Clumped Isotope Data
Kocken, I. J., Müller, I. A., & Ziegler, M. (2019) · Geochemistry, Geophysics, Geosystems · doi:10.1029/2019gc008545 · Cited by 57
Lawson, M. J., Shenton, B. J., Stolper, D. A., Eiler, J. M., Rasbury, E. T., Becker, T. P., Phillips-Lander, C. M., Buono, A., Becker, S. P., Pottorf, R., et al. (2017) · Geological Society of America Bulletin · doi:10.1130/b31656.1 · Cited by 62
“…Schauer et al. (2016)demonstrated that when the difference between the δ13C of the reference gas and sample is less than 10‰, as is the case for all samples in this study, the difference between the Santrock et al. (1985) and the more recent Brand et al. (2010) correction scheme is negligible.”
BackgroundModestou, S. E., Leutert, T. J., Fernandez, A., Lear, C. H., & Meckler, A. N. (2020) · Paleoceanography and Paleoclimatology · doi:10.1029/2020pa003927 · Cited by 57
“All data were processed using the software package Easotope (John & Bowen, 2016) employing IUPAC correction parameters (Brand et al., 2010; Daëron et al., 2016).”
MethodChen, S., Ryb, U., Piasecki, A. M., Lloyd, M. K., Baker, M. B., & Eiler, J. M. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.05.018 · Cited by 55
“…of bulk and clumped isotope 268 compositions, we used the 17O/16O, 18O/16O ratios for VSMOW and the 13C/12C ratio for VPDB 269 suggested by Brand et al. (2010), which were found to minimize inter- and intra-laboratory 270 discrepancies in reported Δ47 values (Schauer et al., 2016; Daëron…”
MethodMurray, S. T., Higgins, J. A., Holmden, C. E., Lu, C., & Swart, P. K. (2020) · Sedimentology · doi:10.1111/sed.12775 · Cited by 62
“These parameters have been used despite the fact that when using equilibrated gases herein only minimal differences were found using the Brand et al. (2010) values compared to the values based on Craig (1957).”
MethodDavies, A., & John, C. M. (2018) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.07.038 · Cited by 64
Veillard, C., John, C. M., Krevor, S. C. M., & Najorka, J. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.02.012 · Cited by 63
“We used the 17O correction factors reported in Brand et al. (2010) and recommended by Daëron et al. (2016).”
MethodMurray, S. T., & Swart, P. K. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2017.02.021 · Cited by 52
Temperature Dependence of Clumped Isotopes (∆ 47 ) in Aragonite
de Winter, N. J., Witbaard, R., Kocken, I. J., Müller, I. A., Guo, J., Goudsmit, B., & Ziegler, M. (2022) · Geophysical Research Letters · doi:10.1029/2022gl099479 · Cited by 52
“Isotopic values were calculated using the latest International Union of Pure and Applied Chemistry values (Brand et al., 2010; Daëron et al., 2016).”
Coupled Mg/Ca and clumped isotope analyses of foraminifera provide consistent water temperatures
Breitenbach, S. F. M., Mleneck-Vautravers, M. J., Grauel, A.-L., Lo, L., Bernasconi, S. M., Müller, I. A., Rolfe, J., Gázquez, F., Greaves, M., & Hodell, D. A. (2018) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.03.010 · Cited by 51
Near Equilibrium 13C18O Bonding During Inorganic Calcite Precipitation Under Chemo‐Stat Conditions
Levitt, N. P., Eiler, J. M., Romanek, C. S., Beard, B. L., Xu, H., & Johnson, C. M. (2018) · Geochemistry, Geophysics, Geosystems · doi:10.1002/2017gc007089 · Cited by 48
Hermoso, M., Horner, T. J., Minoletti, F., & Rickaby, R. E. M. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2014.05.002 · Cited by 56
“Carbon isotope composition 13 The co-addition of 17O in the medium also has an effect on the determination of the 45CO2/44CO2 and 46CO2/44CO2, and hence on δ13CDIC and δ13Cc (Santrock et al., 1985; Brand et al., 2010).”
Mangenot, X., Bonifacie, M., Gasparrini, M., Götz, A., Chaduteau, C., Ader, M., & Rouchon, V. (2017) · Chemical Geology · doi:10.1016/j.chemgeo.2017.10.011 · Cited by 54
“Note that using the 17 O parameters from Brand et al. (2010) would only lead to small differences in 47 values of both of our standards and samples (ie. less than ±0.010‰), well within the analytical uncertainty on Δ47 measurements.”
InfluentialA 600-Million-Year Carbonate Clumped-Isotope Record from the Sultanate of Oman
Bergmann, K. D., Al Balushi, S. A. K., Mackey, T. J., Grotzinger, J. P., & Eiler, J. M. (2018) · Journal of Sedimentary Research · doi:10.2110/jsr.2018.51 · Cited by 46
“%) using the correction parameters from Huntington et al. (2009) compared to those from Brand et al. (2010) (Table 4).”
MethodFleisher, A. J., Yi, H., Srivastava, A., B, O. L. P. A., Zobov, N. F., & Hodges, J. T. (2021) · Nature Physics · doi:10.1038/s41567-021-01226-y · Cited by 76
Katz, A., Bonifacie, M., Hermoso, M., Cartigny, P., & Calmels, D. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2017.02.025 · Cited by 44
“…the choice of appropriate parameters accounting for the 17O interferences in d13C determination (e.g., parameters from Santrock et al., 1985 or Brand et al., 2010), and/or the stability/accuracy of the frames constructed to correct raw ∆47 values from the effects of non-linearity and…”
BackgroundClumped-isotope palaeothermometry and LA-ICP-MS U–Pb dating of lava-pile hydrothermal calcite veins
MacDonald, J., Faithfull, J., Roberts, N. M. W., Davies, A., Holdsworth, C., Newton, M., Williamson, S., Boyce, A. J., & John, C. M. (2019) · Contributions to Mineralogy and Petrology · doi:10.1007/s00410-019-1599-x · Cited by 61
Andreu-Hayles, L., Lévesque, M., Martin‐Benito, D., Huang, W., Harris, R. A., Oelkers, R., Leland, C., Fernández, J. M., Anchukaitis, K., & Helle, G. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2018.09.007 · Cited by 45
“(6)) in a more complex way that also includes an automatic correction of 17O (Brand et al., 2010).”
BackgroundMethodHigh-precision measurements of δ(17)O and (17) Oexcess of NBS19 and NBS18.
Barkan, E., Musan, I., & Luz, B. (2015) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.7378 · Cited by 45
Abundances of isotopologues and calibration of CO 2 greenhouse gas measurements
Tans, P., Crotwell, A., & Thoning, K. (2017) · Atmospheric measurement techniques · doi:10.5194/amt-10-2669-2017 · Cited by 44
“For more detailed descriptions of this relationship see Santrock et al. (1985), Assonov and Brenninkmeijer (2003), Brand et al. (2010) and references therein.”
BackgroundSang, X.-F., Gensch, I., Laumer, W., Kammer, B., Chan, C., Engling, G., Wahner, A., Wissel, H., & Kiendler-Scharr, A. (2012) · Environmental Science and Technology · doi:10.1021/es204094v · Cited by 44
A stable isotope toolbox for water and inorganic carbon cycle studies
Hillaire-Marcel, C., Kim, S.-T., Landais, A., Ghosh, P., Assonov, S., Lécuyer, C., Blanchard, M., Meijer, H. A. J., & Steen-Larsen, H. C. (2021) · Nature Reviews Earth & Environment · doi:10.1038/s43017-021-00209-0 · Cited by 43
Self-citationJena Reference Air Set (JRAS): a multi-point scale anchor for isotope measurements of CO 2 in air
Wendeberg, M., Richter, J. M., Rothe, M., & Brand, W. A. (2013) · Atmospheric measurement techniques · doi:10.5194/amt-6-817-2013 · Cited by 48
“Factors contributing to the uncertainty are the correction for N2O present in the analyzed gas (Sirignano et al., 2004; Ghosh and Brand, 2004), the δ18O value used for digesting the calcite during standardization (Wendeberg et al., 2011) and the 17O correction (Brand et al., 2010).”
BackgroundMethodSelf-citationHyland, E., Huntington, K., Sheldon, N., & Reichgelt, T. (2018) · Climate of the Past · doi:10.5194/cp-14-1391-2018 · Cited by 42
“Following recent work (Daëron et al., 2016; Schauer et al., 2016), mass spectrometer data are corrected using the 17O correction values recommended by Brand et al. (2010).”
MethodBurgener, L., Hyland, E., Huntington, K. W., Kelson, J. R., & Sewall, J. O. (2019) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2018.12.004 · Cited by 52
Chimiak, L. M., Elsila, J. E., Dallas, B., Dworkin, J. P., Aponte, J. C., Sessions, A. L., & Eiler, J. M. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.09.026 · Cited by 47
Brogi, A., Liotta, D., Capezzuoli, E., Matera, P. F., Kele, S., Soligo, M., Tuccimei, P., Ruggieri, G., Yu, T.-L., Shen, C.-C., et al. (2020) · Geothermics · doi:10.1016/j.geothermics.2019.101763 · Cited by 38
“(2016), IUPAC parameters were used to correct for 17O interference (Brand et al., 2010).”
MethodAdnew, G. A., Hofmann, M. E. G., Paul, D., Laskar, A. H., Surma, J., Albrecht, N., Pack, A., Schwieters, J. B., Koren, G., Peters, W., et al. (2019) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8478 · Cited by 47
“In this study we used a λ value of 0.528 to calculate the Δ17O of CO2 following Barkan and co‐workers6,7 and the 17O‐correction algorithm by Brand et al.8 Δ17O ¼ ln δ17Oþ 1 − λ ln δ18Oþ 1 (4) Since the discovery of mass‐independent fractionation,9 the Δ17O value has been used to study sources/sinks of atmospheric trac…”
MethodInfluentialMatthews, A., Affek, H. P., Ayalon, A., Vonhof, H., & Bar‐Matthews, M. (2021) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2021.107223 · Cited by 48
Flores, E., Viallon, J., Moussay, P., Griffith, D., & Wielgosz, R. (2017) · Analytical Chemistry · doi:10.1021/acs.analchem.6b05063 · Cited by 35
Why Measure 17O? Historical Perspective, Triple-Isotope Systematics and Selected Applications
Miller, M. F., & Pack, A. (2021) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2021.86.01 · Cited by 44
Upadhyay, D., Lucarelli, J., Arnold, A., Flores, R., Bricker, H., Ulrich, R. N., Jesmok, G., Santi, L., Defliese, W., Eagle, R. A., et al. (2021) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.9143 · Cited by 33
A calibration equation between Δ 48 values of carbonate and temperature
Swart, P. K., Lu, C., Moore, E. W., Smith, M. E., Murray, S. T., & Staudigel, P. T. (2021) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.9147 · Cited by 43
Reconsidering the uplift history and peneplanation of the northern Lhasa terrane, Tibet
Ingalls, M., Rowley, D. B., Currie, B. S., & Colman, A. S. (2020) · American Journal of Science · doi:10.2475/06.2020.01 · Cited by 38
Ingalls, M. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.02.005 · Cited by 30
Hudson, A. M., Quade, J., Ali, G., Boyle, D., Bassett, S., Huntington, K. W., De los Santos, M. G., Cohen, A. S., Lin, K., & Wang, X. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2017.06.024 · Cited by 32
“Insufficient data are available to recalculate previously published calibration samples using the Brand et al. (2010) correction at this time.”
MethodResultInfluentialPrehistoric cooking versus accurate palaeotemperature records in shell midden constituents
Müller, P., Staudigel, P., Murray, S., Vernet, R., Barusseau, J., Westphal, H., & Swart, P. (2017) · Scientific Reports · doi:10.1038/s41598-017-03715-8 · Cited by 32
Rapid and precise measurement of carbonate clumped isotopes using laser spectroscopy
Yanay, N., Wang, Z., Dettman, D. L., Quade, J., Huntington, K. W., Schauer, A. J., Nelson, D. D., McManus, J. B., Thirumalai, K., Sakai, S., et al. (2022) · Science Advances · doi:10.1126/sciadv.abq0611 · Cited by 31
Thiagarajan, N., Crémière, A., Blättler, C. L., Lepland, A., Kirsimäe, K., Higgins, J. A., Brunstad, H., & Eiler, J. M. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.03.015 · Cited by 41
Davies, A. J., & John, C. M. (2017) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.7902 · Cited by 30
Kelson, J. R., Huth, T. E., Passey, B. H., Levin, N. E., Petersen, S., Ballato, P., Beverly, E. J., Breecker, D. O., Hoke, G. D., Hudson, A. M., et al. (2023) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2023.06.034 · Cited by 43
Clumped isotope thermometry in bivalve shells: A tool for reconstructing seasonal upwelling
Caldarescu, D. E., Sadatzki, H., Andersson, C., Schäfer, P., Fortunato, H., & Meckler, A. N. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.11.019 · Cited by 41
Carbonate clumped isotope values compromised by nitrate-derived NO2 interferent
Fiebig, J., Bernecker, M., Meijer, N., Methner, K., Staudigel, P. T., Davies, A., Bayarjargal, L., Spahr, D., Winkler, B., Hofmann, S., et al. (2024) · Chemical Geology · doi:10.1016/j.chemgeo.2024.122382 · Cited by 29
Weger, R. J., Murray, S. T., McNeill, D. F., Swart, P. K., Eberli, G. P., Blanco, L. R., Tenaglia, M., & Sánchez, L. E. R. (2019) · AAPG Bulletin · doi:10.1306/10021817384 · Cited by 39
Calibration of δ17O and 17Oexcess values of three international standards: IAEA‐603, NBS19 and NBS18
Barkan, E., Affek, H., Luz, B., Bergel, S., Voarintsoa, N. R., & Musan, I. (2019) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8391 · Cited by 29
McCormick, C. A., Corlett, H., Clog, M., Boyce, A. J., Tartèse, R., Steele‐MacInnis, M., & Hollis, C. (2023) · Basin Research · doi:10.1111/bre.12789 · Cited by 33
USGS44, a new high‐purity calcium carbonate reference material for δ 13 C measurements
Qi, H., Moossen, H., Meijer, H. A. J., Coplen, T. B., Bijma, A. T., Reid, L. T., Geilmann, H., Richter, J. M., Rothe, M., Brand, W. A., et al. (2020) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.9006 · Cited by 34
Self-citationSpatial pattern of super-greenhouse warmth controlled by elevated specific humidity
van Dijk, J., Fernandez, A., Bernasconi, S., Rugenstein, J. C. C., Passey, S. R., & White, T. (2020) · Nature Geoscience · doi:10.1038/s41561-020-00648-2 · Cited by 27
Equilibrated Gas and Carbonate Standard‐Derived Dual (Δ 47 and Δ 48 ) Clumped Isotope Values
Lucarelli, J. K., Carroll, H. M., Ulrich, R. N., Elliott, B. M., Coplen, T. B., Eagle, R. A., & Tripati, A. (2023) · Geochemistry, Geophysics, Geosystems · doi:10.1029/2022gc010458 · Cited by 27
“All data used the IUPAC parameter set (Brand et al., 2010; Daëron et al., 2016).”
Self-citationBilau, A., Bienveignant, D., Rolland, Y., Schwartz, S., Godeau, N., Guihou, A., Deschamps, P., Mangenot, X., Brigaud, B., Boschetti, L., et al. (2022) · Earth-Science Reviews · doi:10.1016/j.earscirev.2022.104270 · Cited by 33
Dunn, P., Lu, H., Malinovsky, D., & Goenaga-Infante, H. (2015) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.7376 · Cited by 26
Crivellari, S., Viana, P. J., Campos, M. D. C., Kuhnert, H., Lopes, A. B. M., Cruz, F. W., & Chiessi, C. M. (2021) · Journal of Analytical Atomic Spectrometry · doi:10.1039/d1ja00030f · Cited by 29
Internal Water Facilitates Thermal Resetting of Clumped Isotopes in Biogenic Aragonite
Nooitgedacht, C. W., van der Lubbe, J. J. L., Ziegler, M., & Staudigel, P. T. (2021) · Geochemistry Geophysics Geosystems · doi:10.1029/2021gc009730 · Cited by 41
Nooitgedacht, C. W., van der Lubbe, J. J. L., de Graaf, S., Ziegler, M., Staudigel, P. T., & Reijmer, J. J. G. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.12.008 · Cited by 28
Saenger, C., Gabitov, R. I., Farmer, J. R., Watkins, J. M., & Stone, R. P. (2017) · Chemical Geology · doi:10.1016/j.chemgeo.2017.02.014 · Cited by 25
Guo, Y., Deng, W., Liu, X., Kong, K., Yan, W., & Wei, G. (2021) · Marine Geology · doi:10.1016/j.margeo.2021.106513 · Cited by 30
Briard, J., Pucéat, E., Vennin, E., Daëron, M., Chavagnac, V., Jaillet, R., Merle, D., & de Rafélis, M. (2020) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2019.109582 · Cited by 24
Dong, J., Eiler, J. M., An, Z., Wu, N., Liu, W., Li, X., Kitchen, N., & Lu, F. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.119414 · Cited by 26
Staudigel, P. T., & Swart, P. K. (2018) · Geochemistry Geophysics Geosystems · doi:10.1029/2018gc007500 · Cited by 25
“The Δ47 values for CO2 gas derived from barium carbonate are calculated using the methods outlined by Huntington et al. (2011), using the Brand et al. (2010) revised absolute composition for Pee Dee belemnite R13 (Chang & Li, 1990), R18 (Baertschi, 1976), R17 (Assonov & Brenninkmeijer, 2003), and…”
MethodAssonov, S., Brenninkmeijer, C., Schuck, T., & Taylor, P. (2010) · Atmospheric chemistry and physics · doi:10.5194/acp-10-8575-2010 · Cited by 23
Self-citationClog, M., Lindgren, P., Modestou, S., McDonald, A., Tait, A., Donnelly, T., Mark, D. F., & Lee, M. (2024) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2024.01.023 · Cited by 26
Li, H., Liu, X., Arnold, A., Elliott, B. M., Flores, R., Kelley, A. M., & Tripati, A. (2021) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2021.116840 · Cited by 24
Matera, P. F., Ventruti, G., Zucchi, M., Brogi, A., Capezzuoli, E., Liotta, D., Yu, T., Shen, C., Huntington, K. W., Rinyu, L., et al. (2021) · Geofluids · doi:10.1155/2021/8817487 · Cited by 25
Zhang, N., Lin, M., Snyder, G. T., Kakizaki, Y., Yamada, K., Yoshida, N., & Matsumoto, R. (2019) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2019.02.005 · Cited by 29
Burgener, L., Huntington, K. W., Sletten, R. S., Watkins, J. M., Quade, J., & Hallet, B. (2018) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.06.006 · Cited by 28
Amplified seasonality in western Europe in a warmer world
de Winter, N. J., Tindall, J. C., Johnson, A. L. A., Goudsmit, B., Wichern, N., Kaskes, P., Claeys, P., Huygen, F., van Leeuwen, S. M., Metcalfe, B., et al. (2024) · Science Advances · doi:10.1126/sciadv.adl6717 · Cited by 23
Metadata
- Authors
- Brand, W. A., Assonov, S. S., & Coplen, T. B.
- Affiliations
- Max Planck Society (DE)
- European Commission (BE)
- United States Geological Survey (US)
- Venue
- Pure and Applied Chemistry
- Publisher
- Walter de Gruyter GmbH
- Published
- 2010-05-26
- Volume
- 82
- Issue
- 8
- Pages
- 1719-1733
- ISSN
- 0033-4545 (ISSN-L)
- 1365-3075
- OpenAlex
- W2129805855
- Cited by
- 385
- References
- 27
- Citations by year
- 2026: 20 · 2025: 27 · 2024: 38 · 2023: 45 · 2022: 48 · 2021: 52 · 2020: 36 · 2019: 36 · 2018: 36 · 2017: 20 · 2016: 6 · 2015: 4 · 2014: 3 · 2013: 5 · 2012: 6
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Pure and Applied Chemistry (publishedVersion)
- Joint Research Centre (European Commission) (submittedVersion)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric and Environmental Gas Dynamics
- Physical Sciences › Physics and Astronomy › Instrumentation › Scientific Measurement and Uncertainty Evaluation
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Keywords
- carbon-13 stable isotopes, carbon dioxide, isotope ratio mass spectrometry, oxygen isotope ratios, uncertainty budget
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