The DOI matches its Crossref record; the references it cites are not checked yet.
Siderite acid fractionation factors for sealed and open vessel digestions at 70 °C and 100 °C
Open accessOverview
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Specific acid fractionation factors for different analytical methods and reaction temperatures have been derived empirically.
“but specific acid fractionation factors for different analytical methods and reaction temperatures have also been derived empirically. 18 , 32 , 33”
From Improving the routine analysis of siderite for δ 13 C and δ 18 O in environmental change research (2023) · cites this paper as [33]
The interlaboratory comparison of ETH test siderites was undertaken on a retrospective basis and the BGS and UoL measurements were completed approximately 12 months after the original ETH data had been published.
“The interlaboratory comparison of ETH test siderites was undertaken on a retrospective basis and the BGS and UoL measurements were completed approximately 12 months after the original ETH data had been published. 33”
From Improving the routine analysis of siderite for δ 13 C and δ 18 O in environmental change research (2023) · cites this paper as [33]
Three published studies report estimates for the temperature‐dependent fractionation of oxygen isotopes during the production of CO2 by reaction of siderite with anhydrous phosphoric acid between 25°C and 150°C.
“Three published studies report estimates for the temperature‐dependent fractionation of oxygen isotopes during the production of CO2 by reaction of siderite with anhydrous phosphoric acid between 25°C and 150°C. 18 , 29 , 33”
From Improving the routine analysis of siderite for δ 13 C and δ 18 O in environmental change research (2023) · cites this paper as [33]
Changes in the δ18O value of CO2 with reaction progress have been reported for calcite, dolomite, and siderite.
“Changes in the δ18O value of CO2 with reaction progress have been reported for calcite, dolomite, and siderite. 26 , 33 , 39 , 58”
From Improving the routine analysis of siderite for δ 13 C and δ 18 O in environmental change research (2023) · cites this paper as [33]
Citations
The citation lists haven’t been fetched yet
References 30 · Cited by 17
Research works printed but not linked: 15
- Boschetti, 2005, Continuous-flow δ18O measurements: new approach to standardization, high-temperature thermodynamic and sulfate analysis, Rapid Commun. Mass Spectrom., 19, 3007, 10.1002/rcm.2161 · DOI
- Bottinga, 1968, Oxygen isotope fractionation between CO2 and water, and the isotopic composition of marine atmospheric CO2, Earth Planet. Sci. Lett., 5, 285, 10.1016/S0012-821X(68)80054-8 · DOI
- Kele, 2015, Temperature dependence of oxygen- and clumped isotope fractionation in carbonates: a study of travertines and tufas in the 6–95°C temperature range, Geochim. Cosmochim. Acta, 168, 172, 10.1016/j.gca.2015.06.032 · DOI · Paper page
- Kim, 2015, Normalization of stable isotope data for carbonate minerals: implementation of IUPAC guidelines, Geochim. Cosmochim. Acta, 158, 276, 10.1016/j.gca.2015.02.011 · DOI · Paper page
- Ludvigson, 1998, Meteoric sphaerosiderite lines and their use for paleohydrology and paleoclimatology, Geology, 26, 1039, 10.1130/0091-7613(1998)026<1039:MSLATU>2.3.CO;2 · DOI
- McCrea, 1950, On the isotope chemistry of carbonates and a paleotemperature scale, J. Chem. Phys., 18, 849, 10.1063/1.1747785 · DOI · Paper page
- Müller, 2016, Clumped isotope fractionation during phosphoric acid digestion of carbonates at 70°C, Chem. Geol.
- Poulsen, 2007, General circulation model simulation of the δ18O content of continental precipitation in the middle Cretaceous: a model-proxy comparison, Geology, 35, 199, 10.1130/G23343A.1 · DOI
- Suarez, 2009, Isotopic composition of low-latitude paleoprecipitation during the early Cretaceous, Bull. Geol. Soc. Am., 121, 1584, 10.1130/B26453.1 · DOI
- Suarez, 2011, Quantification of a greenhouse hydrologic cycle from equatorial to polar latitudes: the mid-Cretaceous water bearer revisited, Palaeogeogr. Palaeoclimatol. Palaeoecol., 307, 301, 10.1016/j.palaeo.2011.05.027 · DOI
- Ufnar, 2002, The mid-Cretaceous water bearer: isotope mass balance quantification of the Albian hydrologic cycle, Palaeogeogr. Palaeoclimatol. Palaeoecol., 188, 51, 10.1016/S0031-0182(02)00530-8 · DOI
- Wachter, 1985, Exchange of oxygen isotopes in carbon dioxide-phosphoric [correction of phosphoric] acid systems, Isot. Geosci., 52, 365, 10.1016/0168-9622(85)90046-6 · DOI · Paper page
- Wacker, 2013, Clumped isotope analysis of carbonates: comparison of two different acid digestion techniques, Rapid Commun. Mass Spectrom., 27, 1631, 10.1002/rcm.6609 · DOI · Paper page
- White, 2001, Middle K greenhouse hydrologic cycle of North America, Geology, 29, 363, 10.1130/0091-7613(2001)029<0363:MCGHCO>2.0.CO;2 · DOI · Paper page
- Wiesli, 2004, Experimental determination of Fe isotope fractionation between aqueous Fe(II), siderite and green rust in abiotic systems, Chem. Geol., 211, 343, 10.1016/j.chemgeo.2004.07.002 · DOI
Metadata
- Authors
- Fernandez, A., van Dijk, J., Müller, I. A., & Bernasconi, S. M.
- Affiliations
- ETH Zurich (CH)
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2016-12
- Volume
- 444
- Pages
- 180-186
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2531278255
- Cited by
- 17
- References
- 30
- Citations by year
- 2026: 1 · 2025: 2 · 2024: 2 · 2022: 5 · 2021: 1 · 2020: 1 · 2019: 2 · 2017: 2 · 2016: 1
- FWCI
- 1.39
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Licence
- Locations
- Chemical Geology (acceptedVersion)
- DIGITAL.CSIC (Spanish National Research Council (CSIC)) (acceptedVersion)
- Funders
- Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung (160046, 156408)
- Topics
- 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
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- siderite, oxygen isotope fractionation, fractionation factor, acid digestion, temperature dependence, clumped isotopes, carbonate minerals, paleoenvironmental reconstruction
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
