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Effects of Improved 17 O Correction on Interlaboratory Agreement in Clumped Isotope Calibrations, Estimates of Mineral‐Specific Offsets, and Temperature Dependence of Acid Digestion Fractionation
Open accessAbstract
The clumped isotopic composition of carbonate‐derived CO 2 (denoted Δ 47 ) is a function of carbonate formation temperature and in natural samples can act as a recorder of paleoclimate, burial, or diagenetic conditions. The absolute abundance of heavy isotopes in the universal standards VPDB and VSMOW (defined by four parameters: R 13 VPDB , R 17 VSMOW , R 18 VSMOW , and λ ) impact calculated Δ 47 values. Here, we investigate whether use of updated and more accurate values for these parameters can remove observed interlaboratory differences in the measured T‐Δ 47 relationship. Using the updated parameters, we reprocess 14 published calibration data sets measured in 11 different laboratories, representing many mineralogies, bulk compositions, sample types, reaction temperatures, and sample preparation and analysis methods. Exploiting this large composite data set ( n = 1,253 sample replicates), we investigate the possibility for a “universal” clumped isotope calibration. We find that applying updated parameters improves the T‐Δ 47 relationship (reduces residuals) within most labs and improves overall agreement but does not eliminate all interlaboratory differences. We reaffirm earlier findings that different mineralogies do not require different calibration equations and that cleaning procedures, method of pressure baseline correction, and mass spectrometer type do not affect interlaboratory agreement. We also present new estimates of the temperature dependence of the acid digestion fractionation for Δ 47 (Δ* 25‐X ), based on combining reprocessed data from four studies, and new theoretical equilibrium values to be used in calculation of the empirical transfer function. Overall, we have ruled out a number of possible causes of interlaboratory disagreement in the T‐Δ 47 relationship, but many more remain to be investigated.
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“The CDES-referenced calibration of Petersen et al. (2019) is a compilation and recalculation of existing data [n = 132 samples (>1,200 replicate analyses) from 11 laboratories] spanning 4-800°C generated prior to the establishment of I-CDES.”
From Frontiers of Carbonate Clumped Isotope Thermometry (2023) · cites this paper as Petersen et al. 2019
Experimental — accuracy not yet measuredThe source backs part of the claim, not all of it — or backs it for a different population, condition or comparison.
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“The contribution from Ti calibration uncertainty is small compared to the contribution from sample and reference frame measurements (e.g., Petersen et al. 2019, figure 8).”
From Frontiers of Carbonate Clumped Isotope Thermometry (2023) · cites this paper as Petersen et al. 2019
Experimental — accuracy not yet measuredThe source backs part of the claim, not all of it — or backs it for a different population, condition or comparison.
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“Up to 1-2°C external precision (2 standard error of the mean) can be achieved with extensive replication (e.g., Petersen et al. 2019).”
From Frontiers of Carbonate Clumped Isotope Thermometry (2023) · cites this paper as Petersen et al. 2019
Experimental — accuracy not yet measuredThe source backs part of the claim, not all of it — or backs it for a different population, condition or comparison.
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“Theoretical equilibrium i values of clumped molecules increase with decreasing temperature (T ).”
From Frontiers of Carbonate Clumped Isotope Thermometry (2023) · cites this paper as Petersen et al. (2019)
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“These two calibrations are offset from each other by 3°C near 25°C and 7°C near 100°C and show a similar temperature dependence as the 47 theoretical equilibrium calculations of Schauble et al. (2006) and Hill et al. (2014) (difference of ∼2°C at Earth surface temperatures).”
From Frontiers of Carbonate Clumped Isotope Thermometry (2023) · cites this paper as Petersen et al. (2019)
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“However, the results of InterCarb, and the discussions in the literature (e.g., Petersen et al., 2019) show that with the HG/EG approach there are still poorly understood interlaboratory discrepancies (as suggested by Figure 6) which are absent in the carbonate‐based normalization (see Figure 5).”
From InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards (2021) · cites this paper as Petersen et al., 2019
Experimental — accuracy not yet measuredThe source backs part of the claim, not all of it — or backs it for a different population, condition or comparison.
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“The comparison of calibrations established in different laboratories, however, remains challenging, because of many factors: the lack of carbonate standards to compare across laboratories, the fact that clumped isotope data pre-2016 are not calculated using the”
From Calibration of the oxygen and clumped isotope thermometers for (proto-)dolomite based on synthetic and natural carbonates (2019) · cites this paper as Petersen et al., 2019
Experimental — accuracy not yet measuredThe source backs part of the claim, not all of it — or backs it for a different population, condition or comparison.
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“the statistical evaluation of the Winkelstern et al. (2016) dataset reevaluated in Petersen et al. (2019) for 75 °C acid digestion is significantly different in slope (p value of 0.0395) and intercept to the re-evaluated ETH calcite calibration dataset.”
From Calibration of the oxygen and clumped isotope thermometers for (proto-)dolomite based on synthetic and natural carbonates (2019) · cites this paper as Petersen et al., 2019
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“Numerous studies have produced empirical T-47 calibrations that relate i values measured in natural, synthetic, biogenic, and abiogenic carbonates of different mineralogies to their known growth temperatures (e.g., Petersen et al. 2019, and references therein) (Figure 3).”
From Frontiers of Carbonate Clumped Isotope Thermometry (2023) · cites this paper as Petersen et al. 2019
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“The result of this study was that differences among calibrations were reduced but not eliminated by the recalculation, implying that other factors must be responsible for the remaining discrepancies.”
From InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards (2021) · cites this paper as Petersen et al. (2019)
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“The theoretical values linking measurements to theory were calculated by Wang et al. (2004) and revised by Petersen et al. (2019).”
From InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards (2021) · cites this paper as Petersen et al. (2019)
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“Among the factors responsible for discrepant calibrations and laboratory comparability, two important ones cannot be tested with a gas‐based standardization: (1) the absolute value and temperature dependence of the phosphoric acid fractionation factor (see Petersen et al., 2019 for a recent compilation) and (2) possible CO2 equilibration effects during acid digestion of the sample.”
From InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards (2021) · cites this paper as Petersen et al., 2019
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“The weighted averages of the four standards (projected to 90 °C for the reactions at 25 and 70 °C using the acid temperature correction suggested by Petersen et al., 2019), comprising 873 analyses of the carbonate standards and 946 heated and equilibrated gases from 10 different laboratories, are reported in Table 1 and Figure 2.”
From InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards (2021) · cites this paper as Petersen et al., 2019
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“The phosphoric acid reaction of the carbonate to CO 2 produces a temperature-dependent isotopic fractionation whose temperature dependence is relatively well constrained for calcite (e.g.Defliese et al., 2015;Murray et al., 2016;Petersen et al., 2019) but not for dolomite.”
From Calibration of the oxygen and clumped isotope thermometers for (proto-)dolomite based on synthetic and natural carbonates (2019) · cites this paper as Petersen et al., 2019
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“The effect on the recalculated temperatures in older publications is difficult to predict without a full recalculation that includes all heated and equilibrated gases measured with the samples (Petersen et al., 2019).”
From Calibration of the oxygen and clumped isotope thermometers for (proto-)dolomite based on synthetic and natural carbonates (2019) · cites this paper as Petersen et al., 2019
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(2021) · doi:10.1029/2020gc009592 · Cited by 131
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BackgroundMethodInfluentialSelf-citationA proxy for all seasons? A synthesis of clumped isotope data from Holocene soil carbonates
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De Vleeschouwer, D., Peral, M., Marchegiano, M., Füllberg, A., Meinicke, N., Pälike, H., Auer, G., Petrick, B., Snoeck, C., Goderis, S., et al. (2022) · Climate of the Past · doi:10.5194/cp-18-1231-2022 · Cited by 24
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
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
A Decrease to Low Carbonate Clumped Isotope Temperatures in Cryogenian Strata
Mackey, T., Jost, A., Creveling, J., & Bergmann, K. (2020) · AGU Advances · doi:10.1029/2019av000159 · Cited by 22
“…of 13C and 18O into multiply substituted carbonate isotopologues (Δ47; Eiler, 2007), and multiple carbonate mineralogies generally have similar temperature dependencies (Bonifacie et al., 2017; Bergmann, Finnegan, et al., 2018; see Bonifacie et al., 2017; Petersen et al., 2019; MACKEY ET AL.”
BackgroundMatera, 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
Self-citationClumped isotope acid fractionation factors for dolomite and calcite revisited: Should we care?
Lu, C., Murray, S. T., Koeshidayatullah, A., & Swart, P. K. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120637 · Cited by 25
A robust methodology for triple (∆47, ∆48, ∆49) clumped isotope analysis of carbonates
Bernecker, M., Hofmann, S., Staudigel, P., Davies, A., Tagliavento, M., Meijer, N., Ballian, A., & Fiebig, J. (2023) · Chemical Geology · doi:10.1016/j.chemgeo.2023.121803 · Cited by 22
Self-citationLi, 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 23
Self-citationTechnical Note: Developments and Applications in Triple Oxygen Isotope Analysis of Carbonates
Fosu, B., Subba, R., Peethambaran, R., Bhattacharya, S., & Ghosh, P. (2020) · ACS Earth and Space Chemistry · doi:10.1021/acsearthspacechem.9b00330 · Cited by 23
Pourret, O., Anand, P., Arndt, S., Bots, P., Dosseto, A., Li, Z., Marin‐Carbonne, J., Middleton, J. L., Ngwenya, B. T., & Riches, A. J. V. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2021.05.054 · Cited by 22
Kelson, J. R., Petersen, S., Niemi, N. A., Passey, B. H., & Curley, A. N. (2022) · Geology · doi:10.1130/g49634.1 · Cited by 23
Self-citationAbsolute age and temperature of belemnite rostra: Constraints on the Early Cretaceous cooling event
Wang, T., Yang, P., He, S., Hoffmann, R., Zhang, Q., Farnsworth, A., Feng, Y., Randrianaly, H. N., Xie, J., Yue, Y., et al. (2024) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104353 · Cited by 21
Central Asian modulation of Northern Hemisphere moisture transfer over the Late Cenozoic
Prud'homme, C., Scardia, G., Vonhof, H., Guinoiseau, D., Nigmatova, S., Fiebig, J., Gerdes, A., Janssen, R., & Fitzsimmons, K. (2020) · Communications Earth & Environment · doi:10.1038/s43247-021-00173-z · Cited by 24
Self-citationZamanian, K., Lechler, A. R., Schauer, A. J., Kuzyakov, Y. V., & Huntington, K. W. (2021) · Quaternary Research · doi:10.1017/qua.2020.109 · Cited by 21
“T(Δ47) was calculated for mean Δ47 using the calibration of Petersen et al. (2019), which is based on data produced using the same or similar analytical methods and the same 17O correction as our samples. δ13C and δ18O values were placed on the VPDB scale using C64 and C2 for δ13C, and C64 and…”
MethodSelf-citationReassessment of ocean paleotemperatures during the Late Ordovician
Barney, B. B., & Grossman, E. L. (2022) · Geology · doi:10.1130/g49422.1 · Cited by 22
Wang, R., Xiao, Y., Yu, K., Jones, B., Wu, L., Liang, F., Yang, Y., & Chang, B. (2022) · Sedimentary Geology · doi:10.1016/j.sedgeo.2021.106079 · Cited by 19
O'Hora, H., Petersen, S., Vellekoop, J., Jones, M. M., & Scholz, S. R. (2022) · Climate of the past · doi:10.5194/cp-18-1963-2022 · Cited by 20
Self-citationLi, L., Garzione, C. N., Lu, H., & Quade, J. (2024) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2024.118961 · Cited by 19
Li, P., Zou, H., Hao, F., Yu, X., Wang, G., & Eiler, J. M. (2020) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2020.104660 · Cited by 19
Davies, A., Davis, S., & John, C. M. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120317 · Cited by 19
Self-citationZhang, J. Z., Petersen, S., Winkelstern, I. Z., & Lohmann, K. C. (2021) · Paleoceanography and Paleoclimatology · doi:10.1029/2020pa004145 · Cited by 19
Self-citationBajnai, D., Coplen, T. B., Methner, K., Löffler, N., Krsnik, E., & Fiebig, J. (2021) · Geophysical Research Letters · doi:10.1029/2021gl093257 · Cited by 19
“(b) Differences in the ∆47-derived calcite precipitation temperatures (Petersen et al., 2019) between DHC2-8 (33.”
BackgroundMethodInfluentialSelf-citationEffects of oxygen plasma ashing treatment on carbonate clumped isotopes
Adlan, Q., Davies, A. J., & John, C. M. (2020) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8802 · Cited by 17
“088‰ to obtain a final Δ47(CDES) value.(57) The bulk δ(18)O value was corrected for acid digestion at 90 C”
MethodSelf-citationHarper, D., Suarez, M., Uglesich, J., You, H., Li, D.-Q., & Dodson, P. (2021) · Climate of the Past · doi:10.5194/cp-17-1607-2021 · Cited by 15
Chang, B., Defliese, W. F., Li, C., Huang, J., Tripati, A., & Algeo, T. J. (2019) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8678 · Cited by 17
Self-citationThermochemical oxidation of methane by manganese oxides in hydrothermal sediments
Huang, Q., Jiang, S., Pi, D.-H., Konhauser, K. O., Wen, X., Lu, L., & Yan, H. (2023) · Communications Earth & Environment · doi:10.1038/s43247-023-00891-6 · Cited by 16
Wang, T., Hoffmann, R., He, S., Zhang, Q., Li, G., Randrianaly, H. N., Xie, J., Yue, Y., & Ding, L. (2023) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104220 · Cited by 16
Quandt, D., Micheuz, P., Kurz, W., Kluge, T., Boch, R., Hippler, D., Krenn, K., & Hauzenberger, C. A. (2019) · Geochemistry Geophysics Geosystems · doi:10.1029/2019gc008369 · Cited by 16
“We choose the four calibrations as they are related to inorganic carbonate, mostly calcite, cover a wide range of temperatures, and are consistent with the extensive Δ47 calibration assessment of Petersen et al. (2019).”
ResultSelf-citationKim, S. L., Zeichner, S. S., Colman, A. S., Scher, H. D., Kriwet, J., Mörs, T., & Huber, M. S. (2020) · Paleoceanography and Paleoclimatology · doi:10.1029/2020pa003997 · Cited by 16
“…(2017) are an approximation as we do not account for internal carbonate standard differences, acid digestion fractionation (Δ*25−X), or 17O corrections, which are important factors in clumped isotope paleothermometer applications (Olack & Colman, 2019; Petersen et al., 2019; Schauer et al., 2016).”
BackgroundSelf-citationFosu, B. R., Ghosh, P., Weisenberger, T. B., Spürgin, S., & Viladkar, S. G. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2021.01.037 · Cited by 15
Clumped isotopic compositions of cultured and natural land-snail shells and their implications
Dong, J., Eiler, J. M., An, Z., Li, X., Liu, W., & Hu, J. (2021) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2021.110530 · Cited by 16
Wierzbowski, H. (2021) · Geosciences · doi:10.3390/geosciences11100419 · Cited by 15
Li, L., DeCelles, P. G., Kapp, P., Garzione, C. N., Quade, J., & Yanay, N. (2024) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2024.04.007 · Cited by 15
Re‐determination of R ( 13 C/ 12 C) for Vienna Peedee belemnite (VPDB)
Dunn, P. J. H., Malinovsky, D., Ogrinc, N., Potočnik, D., Flierl, L., Rienitz, O., Paul, D., & Meijer, H. A. J. (2024) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.9773 · Cited by 15
“28 Other methods to determine carbon isotopic composition such as nuclear magnetic resonance (NMR) 29 – 32 and optical spectroscopy 33,34 may also use R VPDB ( 13 C/ 12 C) during data processing to ensure carbon isotope delta values are consistent with those obtained by IRMS, unless calibration is…”
Kele, S., Sallam, E., Capezzuoli, E., Rogerson, M., Wanas, H., Shen, C.-C., Lone, M., Yu, T.-L., Schauer, A., & Huntington, K. (2020) · Journal of the Geological Society · doi:10.1144/jgs2020-147 · Cited by 12
“Δ47 values of 10 selected samples from Gebel Kalabsha, Kurkur, Dungul and Dineigil oases and Gebel El Digm range between 0.658 ± 0.017 and 0.715 ± 0.012‰ (Table 1), corresponding to a temperature range between 36 and 16°C, using the calibration of Petersen et al. (2019).”
MethodInfluentialSelf-citationLake level controls the recurrence of giant stromatolite facies
Ingalls, M., Fetrow, A. C., Snell, K. E., Frantz, C. M., & Trower, E. J. (2021) · Sedimentology · doi:10.1111/sed.12967 · Cited by 15
Cao, B., Luo, X., Wang, X., Zhang, L., & Shi, H. (2022) · Sedimentology · doi:10.1111/sed.13071 · Cited by 15
“These Δ47 values were projected to 90°C for the reactions at 25°C using an acid fractionation factor of −0.088‰ (Petersen et al., 2019).”
BackgroundMethodInfluentialWang, Y., Passey, B., Roy, R., Deng, T., Jiang, S., Hannold, C., Wang, X., Lochner, E., & Tripati, A. (2021) · GSA Bulletin · doi:10.1130/b35784.1 · Cited by 16
Self-citationHow Hot Is Too Hot? Disentangling Mid‐Cretaceous Hothouse Paleoclimate From Diagenesis
Fetrow, A. C., Snell, K. E., Di Fiori, R. V., Long, S. P., & Bonde, J. W. (2022) · Paleoceanography and Paleoclimatology · doi:10.1029/2022pa004517 · Cited by 15
Detecting hydrologic distinctions among Andean lakes using clumped and triple oxygen isotopes
Katz, S. A., Levin, N. E., Rodbell, D. T., Gillikin, D. P., Aron, P. G., Passey, B. H., Tapia, P. M., Serrepe, A. R., & Abbott, M. B. (2022) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2022.117927 · Cited by 14
Self-citationDietzel, M., & Boch, R. (2024) · Geochemistry · doi:10.1016/j.chemer.2024.126206 · Cited by 14
Sun, F., Wang, Y., Jablonski, N. G., Hou, S., Ji, X., Wolff, B., Tripati, A., Cao, J., & Yang, X. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120123 · Cited by 14
Self-citationPeaple, M. D., Beverly, E. J., Garza, B., Baker, S., Levin, N. E., Tierney, J. E., Häggi, C., & Feakins, S. J. (2022) · Organic Geochemistry · doi:10.1016/j.orggeochem.2022.104433 · Cited by 14
Anderson, N. T., Bonifacie, M., Jost, A. B., Siebert, J., Bontognali, T., Horita, J., Müller, I. A., Bernasconi, S. M., & Bergmann, K. D. (2024) · Geochemistry, Geophysics, Geosystems · doi:10.1029/2023gc011049 · Cited by 13
“This is similar to the method used by Petersen et al. (2019).”
BackgroundMethodInfluentialSelf-citationNehmé, C., Todisco, D., Breitenbach, S. F. M., Couchoud, I., Marchegiano, M., Peral, M., Vonhof, H., Hellström, J., Tjallingii, R., Claeys, P., et al. (2022) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104050 · Cited by 14
Self-citationRyan, B. H., Petersen, S., Rivers, J. M., & Kaczmarek, S. E. (2023) · Journal of Sedimentary Research · doi:10.2110/jsr.2022.117 · Cited by 13
Self-citationMarchegiano, M., Peral, M., Venderickx, J., Martens, K., García‐Alix, A., Snoeck, C., Goderis, S., & Claeys, P. (2024) · Geophysical Research Letters · doi:10.1029/2023gl107426 · Cited by 14
“The raw measured Δ 47 values are processed using the IUPAC Brand's isotopic parameters (Brand et al., 2010; Daëron et al., 2016; Petersen et al., 2019) and converted to the ICDES 90° C scale, using the most recent values for the ETH‐1, ETH‐2, and ETH‐3 carbonate reference materials (Ber-nasconi et…”
MethodSelf-citationClumped and oxygen isotope sclerochronology methods tested in the bivalve Lucina pensylvanica
Zhang, J. Z., & Petersen, S. (2023) · Chemical Geology · doi:10.1016/j.chemgeo.2023.121346 · Cited by 12
Self-citationQuandt, D., Micheuz, P., Kurz, W., Bernasconi, S. M., Hippler, D., Krenn, K., & Hauzenberger, C. A. (2020) · Geochemistry Geophysics Geosystems · doi:10.1029/2019gc008745 · Cited by 13
“We use this calibration because it has been produced with the same instrumentation and data reduction schemes as the data presented in this study and thus guarantees robust temperature estimates avoiding uncertainties related to poor interlaboratory comparability (Petersen et al., 2019).”
MethodSelf-citationDuan, W., Wang, X., Tan, M., Cui, L., Wang, X., & Xiao, Z. (2022) · Geophysical Research Letters · doi:10.1029/2022gl098296 · Cited by 11
“Updated bulk solution precipitation (BSP) mode, typically for Δ47-temperature calibration (Petersen et al., 2019):”
MethodInfluentialCurley, A. N., Petersen, S. V., Edie, S. M., & Guo, W. (2023) · Biological Reviews · doi:10.1111/brv.12940 · Cited by 11
Self-citationZhang, S., Liu, Q., Tang, M., & Liu, Y. (2020) · ACS Earth and Space Chemistry · doi:10.1021/acsearthspacechem.9b00307 · Cited by 11
Saenger, C. P., Schauer, A. J., Heitmann, E. O., Huntington, K. W., & Steig, E. J. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120059 · Cited by 11
Self-citationSuarez, M., Knight, J. A., Godet, A., Ludvigson, G., Snell, K., Murphy, L., & Kirkland, J. (2020) · Special Publications · doi:10.1144/sp507-2020-85 · Cited by 10
Isotopic measurements of carbon dioxide: the role of measurement science and standards
Meija, J. (2023) · Analytical and Bioanalytical Chemistry · doi:10.1007/s00216-023-05000-2 · Cited by 11
Synthetic Witherite for Standardisation of Clumped Isotope ( Δ47 ) Measurements
Kong, K., Guo, Y., Deng, W., & Wei, G. (2023) · Geostandards and Geoanalytical Research · doi:10.1111/ggr.12520 · Cited by 10
Metadata
- Authors
- 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., Olack, G. A., Schauer, A. J., Bajnai, D., Bonifacie, M., Breitenbach, S. F. M., Fiebig, J., Fernandez, A. B., Henkes, G. A., Hodell, D., Katz, A., Kele, S., Lohmann, K. C., Passey, B. H., Peral, M. Y., Petrizzo, D. A., Rosenheim, B. E., Tripati, A., Venturelli, R., Young, E. D., & Winkelstern, I. Z.
- Affiliations
- University of Michigan (US)
- University of California, Los Angeles (US)
- University of Washington (US)
- Laboratoire des Sciences du Climat et de l'Environnement (FR)
- Imperial College London (GB)
- ETH Zurich (CH)
- University of Chicago (US)
- Heidelberg University (DE)
- Goethe University Frankfurt (DE)
- Institut de physique du globe de Paris (FR)
- University of Cambridge (GB)
- Department of Earth Sciences ETH‐Zurich Zurich Switzerland
- Stony Brook University (US)
- Institute for Geological and Geochemical Research (HU)
- Jet Propulsion Laboratory (US)
- University of South Florida St. Petersburg (US)
- Grand Valley State University (US)
- Corresponding author
- Petersen, S. V.
- ORCID
- 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.
- Olack, G. A.
- Schauer, A. J.
- Bajnai, D.
- Bonifacie, M.
- Breitenbach, S. F. M.
- Fiebig, J.
- Fernandez, A. B.
- Henkes, G. A.
- Hodell, D.
- Katz, A.
- Kele, S.
- Lohmann, K. C.
- Passey, B. H.
- Peral, M. Y.
- Petrizzo, D. A.
- Rosenheim, B. E.
- Tripati, A.
- Venturelli, R.
- Young, E. D.
- Winkelstern, I. Z.
- Venue
- Geochemistry, Geophysics, Geosystems
- Publisher
- American Geophysical Union (AGU)
- Published
- 2019-07
- Volume
- 20
- Issue
- 7
- Pages
- 3495-3519
- ISSN
- 1525-2027 (ISSN-L)
- OpenAlex
- W2947366632
- Semantic Scholar
- ead0cf9b337105657195db631c449c24e051275e
- Cited by
- 209
- References
- 89
- Citations by year
- 2026: 16 · 2025: 14 · 2024: 32 · 2023: 28 · 2022: 35 · 2021: 45 · 2020: 23 · 2019: 16
- FWCI
- 11.89
- Type
- journal article
- Language
- en
- Open access
- hybrid
- doi.org
- Licence
- Locations
- Geochemistry Geophysics Geosystems (publishedVersion, other-oa)
- Northumbria Research Link (Northumbria University) (acceptedVersion, other-oa)
- Repository of the Academy's Library (Library of the Hungarian Academy of Sciences) (acceptedVersion)
- Digital Commons - University of South Florida (University of South Florida) (submittedVersion, other-oa)
- HAL (submittedVersion, other-oa)
- Deep Blue (University of Michigan) (submittedVersion, other-oa)
- OSTI OAI (U.S. Department of Energy Office of Scientific and Technical Information) (submittedVersion, other-oa)
- HAL Portal Artxiker (Hindustan Aeronautics Limited (India)) (submittedVersion)
- OSTI OAI (U.S. Department of Energy Office of Scientific and Technical Information) (submittedVersion)
- VUBIR (Vrije Universiteit Brussel) (submittedVersion)
- Funders
- National Science Foundation (1156134, 1713275, 0923831)
- U.S. Department of Energy (DE‐SC0010288)
- Nemzeti Kutatási Fejlesztési és Innovációs Hivatal (KH 125584)
- Natural Environment Research Council (NE/M003752/1)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- clumped isotopes, interlaboratory agreement, empirical transfer functions, carbonate diagenesis
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