Isotope studies of dolomite formation under sedimentary conditions
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This prediction is in good agreement with the observation of Clayton et al. (1968) for a natural fractionation of 35.05%o between sedimentary dolomite and its interstitial water.
“being in good agreement with the observation of Clayton et al. (1968) for a natural fractionation of 35.05%o between sedimentary dolomite and its interstitial water.”
From Oxygen isotope fractionation in carbonate and sulfate minerals. (1999) · cites this paper as Clayton et al. (1968)
Oxygen isotope studies of some metamorphic assemblages containing dolomite and calcite pointed to an 18O-enrichment, by an extrapolation to sedimentary conditions, of 5 to 9%o in dolomite relative to coexisting calcite.
“Oxygen isotope studies of some metamorphic assemblages containing dolomite and calcite pointed to an18O-enrichment, by an extrapolation to sedimentary conditions, of 5 to 9%o in dolomite relative to coexisting calcite (e.g., Clayton and Epstein, 1958; Engel et al., 1958; Clayton et al., 1968; Sheppard and Schwarcz, 1970).”
From Oxygen isotope fractionation in carbonate and sulfate minerals. (1999) · cites this paper as Clayton et al., 1968
Dolomite that possibly formed in isotopic equilibrium with the surrounding water has been found only in a few localities.
“Dolomite which possibly formed in isotopic equilibrium with the surrounding water has been found only in a few localities.”
From The isotopic composition of secondary dolomites (1970) · cites this paper as CLAYTON et al. (1968)
The fractionation factor calculated by Clayton et al. for the sedimentary dolomite of Deep Spring Lake and the associated interstitial water fits very closely the extrapolation of the high-temperature experiments.
“Here it is interesting to note that the fractionation factor calculated by CLAYTON et al. (1968) for the sedimentary dolomite of the Deep Spring Lake (Calif.) and the associated interstitial water fits very closely the extrapolation of the high tempera- ture experiments (Fig. 3).”
From The isotopic composition of secondary dolomites (1970) · cites this paper as CLAYTON et al. (1968)
Cites
On the Isotopic Chemistry of Carbonates and a Paleotemperature Scale
McCrea, J. M. (1950) · The Journal of Chemical Physics · doi:10.1063/1.1747785 · Cited by 3,742 · see citing works
Measurement of ratios of total oxygen of carbonates
Sharma, T., & Clayton, R. N. (1965) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(65)90011-6 · Cited by 433 · see citing works
Self-citationOxygen-Isotope Fractionations in Systems Containing Dolomite
Northrop, D. A., & Clayton, R. N. (1966) · The Journal of Geology · doi:10.1086/627153 · Cited by 405 · see citing works
Self-citationOxygen Isotope Fractionation in the System Dolomite-Calcite-Carbon Dioxide
O'Neil, J. R., & Epstein, S. (1966) · Science · doi:10.1126/science.152.3719.198 · Cited by 160 · see citing works
Weber, J. N. (1964) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(64)90125-5 · Cited by 17 · see citing works
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Oxygen isotope fractionation in carbonate and sulfate minerals.
Zheng, Y.-F. (1999) · GEOCHEMICAL JOURNAL · doi:10.2343/geochemj.33.109 · Cited by 468 · see citing works
“pointed to an '8O-enrichment, by an extrapolation to sedimentary conditions, of 5 to 9%o in dolo mite relative to coexisting calcite (e.g., Clayton and Epstein, 1958; Engel et al., 1958; Clayton et al., 1968; Sheppard and Schwarcz, 1970).”
BackgroundSheppard, S. M. F., & Schwarcz, H. P. (1970) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00373200 · Cited by 446 · see citing works
McKenzie, J. A. (1981) · The Journal of Geology · doi:10.1086/628579 · Cited by 345 · see citing works
Oxygen and carbon isotope fractionation in the system dolomite–water–CO2 to elevated temperatures
Horita, J. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2013.12.027 · Cited by 298 · see citing works
Oxygen isotope fractionation during the dolomitization of calcium carbonate
Matthews, A., & Katz, A. (1977) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(77)90249-6 · Cited by 260 · see citing works
The isotopic composition of secondary dolomites
Fritz, P., & Smith, D. G. W. (1970) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(70)90056-6 · Cited by 247 · see citing works
Lacustrine dolomite—an overview of modern, Holocene, and Pleistocene occurrences
Last, W. M. (1990) · Earth-Science Reviews · doi:10.1016/0012-8252(90)90004-f · Cited by 211 · see citing works
Theoretical calculation of oxygen isotope fractionation factors in carbonate systems
Chacko, T., & Deines, P. (2008) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2008.06.001 · Cited by 164 · see citing works
Reaction rates and δO18 variation for the carbonate-phosphoric acid preparation method
Walters, L. J., Claypool, G. E., & Choquette, P. W. (1972) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(72)90002-6 · Cited by 110 · see citing works
García Del Cura, M. A., Calvo, J. P., Ordóñez, S., Jones, B. F., & Cañaveras, J. C. (2001) · Sedimentology · doi:10.1046/j.1365-3091.2001.00388.x · Cited by 81 · see citing works
Self-citationCalcium and magnesium-limited dolomite precipitation at Deep Springs Lake, California
MEISTER, P., REYES, C., BEAUMONT, W., RINCON, M., COLLINS, L., BERELSON, W., STOTT, L., CORSETTI, F., & NEALSON, K. H. (2011) · Sedimentology · doi:10.1111/j.1365-3091.2011.01240.x · Cited by 81 · see citing works
NIELSEN, P., SWENNEN, R., & KEPPENS, E. (1994) · Sedimentology · doi:10.1111/j.1365-3091.1994.tb02011.x · Cited by 77 · see citing works
An Early Holocene Primary Dolomite Layer of Abiotic Origin in Lake Sayram, Central Asia
Cheng, J., Meng, X., Zhang, E., Jiang, Q., Ni, Z., & Ji, J. (2021) · Geophysical Research Letters · doi:10.1029/2021gl096309 · Cited by 20 · see citing works
Liu, X., Deng, W., & Wei, G. (2019) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8365 · Cited by 11 · see citing works
Zhang, J. (2024) · Molecules · doi:10.3390/molecules29030698 · Cited by 6 · see citing works
“Therefore, in the natural water body (seawater, surface water, or groundwater), there will also be an H 2 CO 3 aqueous solution in the form of H 2 CO 3 molecules.”
Background
- Authors
- Clayton, R. N., & Jones, B. F.
- Affiliations
- University of Chicago (US)
- United States Geological Survey (US)
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1968-04
- Volume
- 32
- Issue
- 4
- Pages
- 415-432
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2066458246
- Cited by
- 132
- References
- 5
- Citations by year
- 2025: 2 · 2024: 3 · 2023: 3 · 2022: 3 · 2021: 4 · 2020: 1 · 2019: 3 · 2018: 4 · 2016: 2 · 2015: 2 · 2014: 4 · 2012: 2
- FWCI
- 19.56
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- dolomite formation, stable carbon isotopes, magnesian calcite, isotope fractionation, lake sediments
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