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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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“The IUPAC parameter set (Brand et al. 2010) was used to correct for 17O interferences (Daëron et al. 2016; Schauer et al. 2016).”
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Xia, L.-J., Zhou, L.-X., van der Schoot, M. V., Rella, C., Liu, L.-X., Zhang, G., & Wang, H.-Y. (2016) · Science China. Earth Sciences · doi:10.1007/s11430-016-5294-8 · Cited by 5
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“There are a number of so-called (17)O algorithms which have been formulated to overcome this [27, 30, 31].”
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“Clumped isotope values for all samples and standards were corrected following the methods of Huntington et al. (2011) with revised absolute isotopic abundances reported following the Brand et al. (2010) parameters recommended by Da€eron et al. (2016).”
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“∙1000=‰ (1) In this work, the reported δ13C values of the investigated samples are given relatively to the internationally accepted reference standard, Vienna Peedee belemnite (VPDB) [Brand et al., 2010].”
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“Isotope ratio calculations use the IUPAC 17O parameters (Brand et al., 2010) and apply the 90°C acid fractionation factor of Kim et al. (2007).”
MethodPhysical model for multi-point normalization of dual-inlet isotope ratio mass spectrometry data
Srivastava, A. (2022) · Analytical and Bioanalytical Chemistry · doi:10.1007/s00216-022-04137-w · Cited by 4
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“Both methodologies used the International Union of Applied Chemistry (IUPAC) parameters for 17 O correction and isotopic ratios for Vienna Pee Dee Belemnite (VPDB) and Vienna Standard Mean Ocean Water (VSMOW) (Bernasconi et al., 2018; Brand et al., 2010; Daëron et al., 2016).”
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Understanding the relationship between foraminiferal Mg/Ca and clumped isotope thermometers
Peral, M., Caley, T., Malaizé, B., Extier, T., Rossignol, L., Barathieu, H., Dassié, É. P., Bassinot, F., Blamart, D., & Daëron, M. (2025) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2025.08.011 · Cited by 1
OCEAN—An EXCEL add-in for 17O correction using a novel approximation
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Herlambang, A., John, C., & Drake, H. (2023) · Geofluids · doi:10.1155/2023/8445328 · Cited by 1
“This equation includes a range of calcite precipitated between 25 and 250°C [35] reprocessed using our internal values for the standards and the ‘IUPAC-recommended (17)O correction’ parameters [36] which assume the values for ratios of C, O, O in VPDB standard, and a mass-dependent slope λ that relates δ(17)O and δ(18…”
MethodJiménez‐Rodríguez, S., Quade, J., Dettinger, M. P., Huntington, K. W., & Kelson, J. R. (2022) · Chemical Geology · doi:10.1016/j.chemgeo.2022.120798 · Cited by 2
Final report on pilot study CCQM-P211: carbon isotope delta measurements of vanillin
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Firewood residential heating – local versus remote influence on the aerosol burden
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“Therefore, carbon isotope ratios 13R = 13C 12C are given using the delta value: δ13C= (13C/12C)sample− (13C/12C)VPDB (13C/12C)VPDB × 1000‰, (3) where (13C/12C)VPDB is the internationally accepted Vienna Pee Dee Belemnite (VPDB) value of 0.0111828 (Brand et al., 2010; Craig, 1957).”
MethodInfluentialCarbon Isotopic Measurements of Nanotubes to Differentiate Carbon Sources
Chartrand, M. M. G., Kingston, C. T., Simard, B., & Mester, Z. (2019) · ACS Omega · doi:10.1021/acsomega.9b03254 · Cited by 1
Stable Isotope Techniques for Gas Source Mass Spectrometry
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Supplemental Material: A tropically hot mid-Cretaceous North American Western Interior Seaway
Jones, M. M., & al., E. (2022) · doi:10.1130/geol.s.19633128.v1
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Internal water and organic matter increase calcite clumped isotope reactivity
Sun, Z., Cheng, J., Banerjee, S., & Grossman, E. L. (2026) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2026.07.038
Bitault, H., Hollis, C., Tonetto, A., Deschamps, P., Léonide, P., & Fournier, F. (2026) · Sedimentology · doi:10.1111/sed.70136
Jet-induced rainfall seasonality and C4 migration over East Asia
Da, J., Sun, C.-R., Serach, L., Gallagher, T., Lu, H.-Y., Huntington, K., Feng, R., Zhang, H.-Z., Wang, H., Ji, S., et al. (2026) · Nature Communications · doi:10.1038/s41467-026-74312-5
“Δ 47 values were calculated using established methods 63 , with the exceptionthat weusedupdated 17 Ocorrectionparameters 64 , following recommendations of ref.”
Peharda, M., de Winter, N. D., Schöne, B., Uvanović, H., van der Lubbe, J. V. D., Verdegaal-Warmerdam, S., Bujas, N., Stanić, R., & Janeković, I. (2026) · Regional Studies in Marine Science · doi:10.1016/j.rsma.2026.105143
Zheng, H.-D., Xiong, Q., Zhou, X., Chang, B., Dai, H., Cai, H.-Z., Wang, L. X., Li, Y.-C., Xue, L.-F., Chen, M., et al. (2026) · Chemical Geology · doi:10.1016/j.chemgeo.2026.123529 · Cited by 1
Chartrand, M., Yang, L., Methven, B., Mihai, O., Hélie, J.-F., Adamowicz-Walczak, A., Middlestead, P., Mester, Z., & Meija, J. (2026) · Analytical and Bioanalytical Chemistry · doi:10.1007/s00216-026-06428-y
“…an internal spread-sheet to apply the recommended IUPAC linear approximation algorithm 17 O correction [10]; UO used the Santrock, Studley, and Hayes (SSH) algorithm [11], and Geotop used the SSH algorithm in the software, but used the IUPAC recommended K , λ , R 13 , R 17 , and R 18 values [10].”
Middle Eocene hyperthermal seasonality from Paris Basin marine mollusks
Marlot, L., Huyghe, D., Briais, J., Daëron, M., Fléhoc, C., Emmanuel, L., Merle, D., Aguerre-Chariol, O., & Lartaud, F. (2026) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2026.113547
Rinyu, L., Czébely, A., Kiss, D., Kele, S., Czellár, S., Molnár, J., & Túri, M. (2025) · International Journal of Mass Spectrometry · doi:10.1016/j.ijms.2025.117565 · Cited by 1
Müller, I. A., Rijkes, D., Judd, E. J., Hamers, M., Plümper, O., Jagt, J. W. M., & Ziegler, M. (2025) · Cretaceous Research · doi:10.1016/j.cretres.2025.106258
Braniecki, G. F. N., Surge, D. M., & Hyland, E. G. (2025) · Geosciences · doi:10.3390/geosciences15080295
Koltai, G., Spötl, C., Rinyu, L., Honiat, C., Racine, T. M. F., Zhang, H., Krüger, Y. S., & Dublyansky, Y. V. (2024) · Chemical Geology · doi:10.1016/j.chemgeo.2024.122454
Pederson, C. L., Klaus, J. S., McNeill, D., & Swart, P. K. (2024) · Sedimentology · doi:10.1111/sed.13196
“Homogenized sediments were also measured for their inorganic δ 13 C carb and δ 18 O carb values by dissolution in phosphoric acid using the common acid bath method (Swart et al ., 1991) Craig, 1957; Brand et al ., 2010) and modified for a triple collector mass spectrometer.”
Ping, H., Deng, W., Chen, H., Guo, Y., Kong, K., Yang, X., & Liu, J. (2024) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2024.106773
Padgett, A. B., Hyland, E. G., West, C. K., Burgener, L., Greenwood, D. R., & Basinger, J. F. (2023) · Paleoceanography and Paleoclimatology · doi:10.1029/2023pa004609 · Cited by 1
“Data were processed using Easotope software (John & Bowen, 2016), using the Brand et al. (2010) 17 O correction parameters (Daëron et al., 2016; Schauer et al., 2016) and corrected with a 70°C calcite acid fractionation of 0.066 (Petersen et al., 2019).”
MethodInfluentialLange, L., Diório, G. R., Bahniuk, A. M., & Cury, L. F. (2023) · Journal of South American Earth Sciences · doi:10.1016/j.jsames.2023.104459
Xi, L., & Beaupré, S. (2021) · Limnology and Oceanography : Methods · doi:10.1002/lom3.10450
“4; Supporting Information), where 13Rstd = 0.01118 is the 13C/12C ratio in the isotope reference standard of carbon (Pee Dee Belemnite [PDB]; Brand et al. 2010; Brand et al. 2014; Chang and Li 1990; Craig 1957; Meija et al. 2016; Rosman and Taylor 1998).”
BackgroundInfluentialLinol, B., Montañez, I., Lombardo, A., Kuta, D., Upadhyay, D., Arnold, A. J., Tripati, A., Bauer, A., & Musa, S. (2021) · South African Journal of Geology · doi:10.25131/sajg.124.0045
Betancourt, C., Küppers, C., Sager, U., Hoyer, A., Kaminski, H., Rapp, G., John, A., Küpper, M., Quass, U., Kuhlbusch, T., et al. (2020) · doi:10.5194/acp-2020-1133
“…13 𝐶 12 are given using the delta value: 125 𝛿13𝐶 = ( 𝐶 13 / 𝐶 12 )𝑠𝑎𝑚𝑝𝑙𝑒−( 𝐶 13 / 𝐶 12 )𝑉𝑃𝐷𝐵 ( 𝐶 13 / 𝐶 12 )𝑉𝑃𝐷𝐵 × 1000 ‰ (3) where ( 𝐶 13 / 𝐶 12 )𝑉𝑃𝐷𝐵 is the internationally accepted Vienna Peedee Belemnite (VPDB) value of 0.0111828 (Brand et al., 2010;Craig, 1957).”
InfluentialAbsolute isotope ratios of carbon dioxide – a feasibility study
Flierl, L., Rienitz, O., Brewer, P. J., Meijer, H. A. J., & Steur, F. (2020) · Journal of Analytical Atomic Spectrometry · doi:10.1039/d0ja00318b · Cited by 3
Veillard, C. (2019) · doi:10.25560/76532
“The minimum amount of CO2 required for analysis is of the order of 20 mbar (Brand et al., 2010).”
BackgroundMethodInfluentialAssonov, S., Brenninkmeijer, C., Schuck, T., & Taylor, P. (2010) · doi:10.5194/acpd-10-5999-2010
“All isotope data are on the VPDB-CO2 scale (linked to NBS-19-CO2) by using the (17)O correction after Assonov and Brenninkmeijer (2003) which is currently being officially recommended (13th WMO/IAEA Meeting; Brand et al., 2009).”
MethodSelf-citationMAJOR CONTROLS ON DIAGENESIS IN THE MARTIN BRIDGE FORMATION: WALLOWA MOUNTAINS, OREGON
Eisenberg, J. L., & Bershaw, J. (2021) · Abstracts with programs - Geological Society of America · doi:10.1130/abs/2021am-370334
“Δ47 values are calculated using established methods (Santrock et al., 1985; Eiler and Schauble, 2004; Huntington et al., 2009; Brand et al., 2010; Schauer et al., 2016; Daëron et al., 2016) and are corrected to the carbon dioxide equilibrium scale (CDES) of (Dennis et al., 2011) using CO2…”
Method
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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