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Isotope geochemistry of sedimentary sulfates
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“The d34Ssulfate variations in 'Phanerozoic' oceans, based on evaporites (Claypool et al., 1980; Holser and Kaplan, 1966), form an overall trough-like trend similar to strontium isotopes (Figure 30).”
From Evolution of Sedimentary Rocks (2014) · cites this paper as Holser and Kaplan, 1966
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Research works printed but not linked: 89
- Adams, 1944, Upper Permian Ochoa Series of Delaware Basin, west Texas and southeastern New Mexico, Bull. Am. Assoc. Petrol. Geologists, 28, 1596
- Ancarani-Rossiello, 1963, Sul rapporto isotopico 32S34S nello zolfo elementare e nello zolfo dei solfati associati di alcuni giacimenti Italiani, Accad. Ital. Classe Sci. Fis. Mat. Nat., Rend., 34, 246
- D'Ans, 1960, Bemerkungen zur Bildung und zur Umbildungen ozeanischer Salzlagerstatten, Kali Steinsalz, 3, 69
- Applin, 1965, The Comanche Series and associated rocks in the subsurface in central and south Florida, U.S. Geol. Surv., Prof. Papers, 447
- Ault, 1959, Isotopic geochemistry of sulphur, Geochim. Cosmochim. Acta, 16, 201, 10.1016/0016-7037(59)90112-7 · DOI
- Barr, 1962, Der Werdegang der Kalisalzlagerstätten am Oberrhein, Neues Jahrb. Mineral. Abhandl., 97, 289
- Barth, 1961, Abundance of the elements, areal averages and geochemical cycles, Geochim. Cosmochim. Acta, 23, 1, 10.1016/0016-7037(61)90086-2 · DOI
- Barth, 1962, Die Menge der Kontinentalsedimente und ihre Beziehung zu den Eruptivgesteinen, Neues Jahrb. Mineral., Monatsh., 1962, 59
- Brocas, 1963, Cl, K and Na concentrations in Antarctic snow and ice, J. Geophys. Res., 68, 3999, 10.1029/JZ068i013p03999 · DOI
- Buschendorf, 1963, Schwefel-Isotopen-Untersuchungen am Pyrit-Sphalerit-Baryt-Lager Meggen/Lenne (Deutschland) und an verschiednen Devon-Evaporiten, Geochim. Cosmochim. Acta, 27, 501, 10.1016/0016-7037(63)90085-1 · DOI
- Chave, 1960, Evidence on history of sea water from chemistry of deeper subsurface waters of ancient basins, Bull. Am. Assoc. Petrol. Geologists, 44, 357
- Deevey, 1963, Fractionation of sulfur and carbon isotopes in a meromictic lake, Science, 139, 407, 10.1126/science.139.3553.407 · DOI
- Dellwig, 1955, Origin of the Salina salt of Michigan, J. Sed. Petrol., 25, 83
- Dessau, 1960, L'origine die giacimenti solfiferi Italiani alla luce delle indagini isotopiche sui carbonati della Serie Gessoso-Solfifera della Sicilia, Boll. Serv. Geol. Italia, 81, 313
- Dessau, 1962, Geology and isotopic studies of Sicilian sulfur deposits, Econ. Geol., 57, 410, 10.2113/gsecongeo.57.3.410 · DOI
- Droste, 1961, Clay minerals in sediments of Owens, China, Searles, Panamint, Bristol, Cadiz, and Danby Lake Basins, California, Bull. Geol. Soc. Am., 72, 1713, 10.1130/0016-7606(1961)72[1713:CMISOO]2.0.CO;2 · DOI
- Eriksson, 1959, The yearly circulation of chloride and sulfur in nature; meteorological, geochemical and pedological implications, Tellus, 11, 375, 10.1111/j.2153-3490.1959.tb00048.x · DOI
- Eriksson, 1960, The yearly circulation of chloride and sulfur in nature; meteorological, geochemical and pedological implications, Tellus, 12, 63, 10.1111/j.2153-3490.1960.tb01284.x · DOI
- Eriksson, 1963, The yearly circulation of sulfur in nature, J. Geophys. Res., 68, 4001, 10.1029/JZ068i013p04001 · DOI
- Feely, 1957, Gulf Coast salt-dome sulphur deposits, Bull. Am. Assoc. Petrol. Geologists, 41, 1802
- Feth, 1964, Sources of mineral constituents in water from granitic rocks of the Sierra Nevada, California and Nevada, U.S. Geol. Surv., Water Supply Papers, 1535-I, 70
- Feth, 1964, Chemical composition of snow in the northern Sierra Nevada and other areas, U.S., Geol. Surv., Water Supply Papers, 1535-J, 39
- Flint, 1958, Stratigraphy and radiocarbon dates at Searles Lake, California, Am. J. Sci., 256, 689, 10.2475/ajs.256.10.689 · DOI
- Friedrich, 1961, Identität von Wathlingenit mit Kieserit, Kali Steinsalz, 3, 221
- Füchtbauer, 1959, Die Tonminerale der Zechsteinformation, Beitr. Mineral. Petrog., 6, 320
- Gale, 1914, Owens, Searles, and Panamint Basins, southeastern California, U.S. Geol. Surv., Bull., 580-L, 251
- Goldman, 1952, Deformation, metamorphism, and mineralization in gypsumanhydrite cap rock, Sulphur-salt Dome, Louisiana, Geol. Soc. Am., Mem., 50, 163
- Gorham, 1961, Factors influencing supply of major ions to inland waters, with special reference to the atmosphere, Bull. Geol. Soc. Am., 795, 10.1130/0016-7606(1961)72[795:FISOMI]2.0.CO;2 · DOI
- Gould, 1965, Antarctica - continent of international science, Science, 150, 1775, 10.1126/science.150.3705.1775 · DOI
- Haines, 1959, Core logs from Searles Lake, San Bernardino County, California, U.S. Geol. Surv., Bull., 1045-E, 139
- Harrison, 1958, Sulphur-isotope abundances in hydrocarbons and source rocks of Uinta Basin, Utah, Bull. Am. Assoc. Petrol. Geologists, 42, 2642
- Hay, 1963, Authigenic silicate minerals in Searles Lake, California, Sedimentology, 2, 312, 10.1111/j.1365-3091.1963.tb01222.x · DOI
- Holser, 1966, Diagenetic polyhalite in Recent salt from Baja California, Am. Mineralogist, 51, 99
- Holser, 1963, Isotope geochemistry of salt rocks, Geol. Soc. Am., Spec. Papers, 76, 82
- Hoy, 1962, Structure of Winnfield Salt Dome, Winn Parish, Louisiana, Bull. Am. Assoc. Petrol. Geologists, 46, 1444
- Ivanov, 1960, Geology of halide deposits of the U.S.S.R., Tr. Vses. Nauchn. Issled. Geol. Inst., 35, 424
- Jung, 1960, Kombiniert-feinstratigraphisch-geochemische Untersuchungen der Anhydrite des Zechstein 1 in SE-Harzvorland, Geologie, 9, 58
- Junge, 1958, The concentration of chloride, sodium, potassium, calcium and sulfate in rain water over the United States, J. Meteorol., 15, 417, 10.1175/1520-0469(1958)015<0417:TCOCSP>2.0.CO;2 · DOI
- Jux, 1961, The palynologic age of diapiric and bedded salt in the Gulf Coastal province, Louisiana, Dept. Conserv., Geol. Bull., 38, 46
- Kaplan, 1960, Sulfur-isotope variations in nature. 8. Application to some biogeochemical problems, New Zealand J. Sci., 3, 338
- Kaplan, 1963, The distribution and isotopic abundance of sulphur in recent marine sediments off southern California, Geochim. Cosmochim. Acta, 27, 297, 10.1016/0016-7037(63)90074-7 · DOI
- King, 1947, Sedimentation in Permian Castile Sea, Bull. Am. Assoc. Petrol. Geologists, 31, 470
- Klaus, 1955, Über die Sporendiagnose des deutschen Zechsteinsalzes und des alpinen Salzgebirges, Z. Deut. Geol. Ges., 105, 776
- Knopf, 1918, A geologic reconnaissance of the Inyo Range and the eastern slope of the southern Sierra Nevada, Calif., U.S. Geol. Surv., Prof. Papers, 110, 130
- Kramer, 1965, History of sea water, Geochim. Cosmochim. Acta, 29, 921, 10.1016/0016-7037(65)90086-4 · DOI
- Krumbein, 1951, Occurrence and lithologic associations of evaporites in the United States, J. Sed. Petrol., 21, 63, 10.1306/D4269422-2B26-11D7-8648000102C1865D · DOI
- Kühn, 1935, Violet kainite containing hydrogen sulfide, Zentr. Mineral. Geol., 1935A, 193
- Kulp, 1961, Geologic time scale, Science, 133, 1105, 10.1126/science.133.3459.1105 · DOI
- Lang, 1942, Basal beds of Salado Formation in Fletcher potash core test, near Carlsbad, New Mexico, Bull. Am. Assoc. Petrol. Geologists, 26, 63
- Livingstone, 1963, Chemical composition of rivers and lakes, U.S. Geol. Surv., Prof. Papers, 440-G, 64
- McIntire, 1963, Trace element partition coefficients - a review of theory and applications to geology, Geochim. Cosmochim. Acta, 27, 1209, 10.1016/0016-7037(63)90049-8 · DOI
- Newell, 1957, Geological studies on the great Bahama bank, Soc. Econ. Paleontologists Mineralogists, Spec. Publ., 5, 15
- Nielsen, 1966, Schwefelisotope im marinen Kreislauf und das δ 34S der früheren Meere, Geol. Rundschau, 55, 160, 10.1007/BF01982964 · DOI
- Nielsen, 1964, Schwefel-Isotopenverhältnisse von Evaporiten aus Dentschland; ein Beitrag zur Kenntnis von S in Meerwasser-Sulfat, Geochim. Cosmochim. Acta, 28, 577, 10.1016/0016-7037(64)90078-X · DOI
- Niemann, 1960, Untersuchungen am Grauen Salzton der Grube Konigshall-Hindenburg, Reyershausen bei Göttingen, Beitr. Mineral. Petrog., 7, 137
- Ogniben, 1955, Inverse graded bedding in primary gypsum of chemical deposition, J. Sed. Petrol., 25, 273, 10.1306/74D7047F-2B21-11D7-8648000102C1865D · DOI
- Ogniben, 1957, Petrografia della Serie Solfifera Siciliana e considerazioni geologiche relative, Serv. Geol. Ital., Mem. Descrittive Carta Geol. Ital., 33, 215
- Ogniben, 1957, Secondary gypsum of the sulphur series, Sicily, and the so-called integration, J. Sed. Petrol., 27, 64
- Ogniben, 1957, Secondary gypsum of the sulphur series, Sicily, and the so-called integration, J. Sed. Petrol., 27, 469, 10.1306/74D7072C-2B21-11D7-8648000102C1865D · DOI
- Östlund, 1963, Oxidation rate of sulfide in sea water, a preliminary study, J. Geophys. Res., 68, 3995, 10.1029/JZ068i013p03995 · DOI
- Pettijohn, 1963, Chemical composition of sandstones, excluding carbonate and volcanic sands, U.S. Geol. Surv., Prof. Papers, 440S, 19
- Phleger, 1962, Sedimentology and oceanography of coastal lagoons in Baja California, Mexico, Bull. Geol. Soc. Am., 73, 145, 10.1130/0016-7606(1962)73[145:SAOOCL]2.0.CO;2 · DOI
- Rafter, 1957, Sulphur-isotopic variations in nature. 2. A quantitative study of the reduction of barium sulphate by graphite for recovery of sulphide - sulphur for sulphur-isotopic measurements, New Zealand J. Sci., B, 38, 955
- Rafter, 1957, Sulphur-isotopic variations in nature. 3. A study of the combustion characteristics of silver sulphide and lead sulphide for sulphur-isotopic measurements, New Zealand J. Sci., B, 38, 969
- Rafter, 1963, The examination of sulphur-isotope ratios in the geothermal and volcanic environment, New Zealand Dept. Sci. Ind. Res., Inst. Nucl. Studies, Rept., INS-R-25, 45
- Richter-Bernburg, 1955, Stratigraphische Gliederung des deutschen Zechsteins, Z. Deut. Geol. Ges., 105, 843
- Richter-Bernburg, 1957, Isochrone Warven im Anhydrit des Zechstein 2, Geol. Jahrb., 74, 601
- Ricke, 1960, Ein Beitrag zur Geochemie des Schwefels, Geochim. Cosmochim. Acta, 21, 35, 10.1016/S0016-7037(60)80003-8 · DOI
- Ricke, 1963, Geochemie des Schwefels und ihre Anwendung auf Fazies probleme, Fortschr. Geol. Rheinland Westfalen, 110, 271
- Roberson, 1961, Geographic distribution of major constituents in stream waters of the western conterminous United States, U.S. Geol. Surv., Prof. Papers, 424, Ddash334
- Rubey, 1951, Geologic history of sea water, Bull. Geol. Soc. Am., 62, 1111, 10.1130/0016-7606(1951)62[1111:GHOSW]2.0.CO;2 · DOI
- Sakai, 1958, Fractionation of sulphur isotopes in volcanic gases, Geochim. Cosmochim. Acta, 15, 32, 10.1016/0016-7037(58)90007-3 · DOI
- Schauberger, 1955, Zur Genese des alpinen Haselgebirges, Z. Deut. Geol. Ges., 105, 736
- Smith, 1962, Subsurface stratigraphy of Late Quaternary deposits, Searles Lake, California, a summary, U.S. Geol. Surv., Prof. Papers, 450C, 65
- Smith, 1964, Character and distribution of nonclastic minerals in the Searles Lake evaporite deposit, California, U.S. Geol. Surv., Bull., 1181-P, 58
- Stewart, 1963, Marine evaporites, U.S. Geol. Surv., Prof. Papers, 440-Y, 58
- Stuiver, 1964, Carbon-isotopic distribution and correlated chronology of Searles Lake sediments, Am. J. Sci., 262, 377, 10.2475/ajs.262.3.377 · DOI
- Thode, 1964, Stable isotopes a key to our understanding of natural processes, Bull. Can. Petrol. Geologists, 12, 242
- Thode, 1965, Sulfur-isotope geochemistry of petroleum, evaporites and ancient seas, Am. Assoc. Petrol. Geologists, Mem., 4, 367
- Thode, 1961, Sulphur-isotope geochemistry, Geochim. Cosmochim. Acta, 25, 159, 10.1016/0016-7037(61)90074-6 · DOI
- Thode, 1961, Sulphur-isotope abundances in petroleum and associated materials, Bull. Am. Assoc. Petrol. Geologists, 42, 2619
- Vinogradov, 1964, Isotopic composition and origin of volcanic sulfur, Geol. Rudn. Mestorozhd., 6, 7
- Vinogradov, 1956, Composition of sedimentary rocks of the Russian platform in relation to the history of its tectonic movements, Geokhimiya, 1956, 3
- Vinogradov, 1956, Composition of sedimentary rocks of the Russian platform in relation to the history of its tectonic movements, Geochemistry, 1956, 533
- Vinogradov, 1956, The isotopic composition of sulfur in connection with the growth of pyrites of sedimentary origin, Geokhimiya, 1956, 96
- Vinogradov, 1956, The isotopic composition of sulfur in connection with the growth of pyrites of sedimentary origin, Geochemistry, 1956, 97
- Wagner, 1953, Die tertiären Salzlagerstätten im Oberrheintal-Graben, Z. Deut. Geol. Ges., 105, 706
- White, 1963, Chemical composition of subsurface waters, U.S. Geol. Surv., Prof. Papers, 440F, 67
- Whitehead, 1961, Recent chemical analyses of waters from several closed-basin lakes and their tributaries in the western United States, Bull. Geol. Soc. Am., 72, 1421, 10.1130/0016-7606(1961)72[1421:RCAOWF]2.0.CO;2 · DOI
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Sochava, A. V. (1992) · International Geology Review · doi:10.1080/00206819209465622 · Cited by 1
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Grinenko, L. N., Zairi, N., Ponomarev, V., Ruchkin, G. V., & Tychinskii, A. A. (1980) · doi:10.1080/00206818209466992 · Cited by 1
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Shikazono, N. (2014) · Springer eBooks · doi:10.1007/978-4-431-54904-8_3 · Cited by 1
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Mauger, R. L., Kayser, R., & Gwynn, J. (2007) · doi:10.34191/ss-41 · Cited by 1
Javor, B. (1989) · doi:10.1007/978-3-642-74370-2_21 · Cited by 1
Yamamoto, M., Shibata, T., & Kusakabe, M. (1987) · doi:10.2343/geochemj.21.247 · Cited by 1
“Just one thing we are certain is that different from the Noril'sk anhydrites, evaporite sulfate is unlikely to be the main source of sulfur in the present case, because most of the 634S values of the Iratsu anhydrites are consider ably lower than +10%°, the minimum value of the evaporite sulfates (Holser and Kaplan, 1…”
BackgroundZhang, L., Zhang, H.-T., Chen, Y.-L., Liu, G.-F., Wei, L.-L., & Zhao, J. (2026) · Geological Journal · doi:10.1002/gj.70497
Ma, M., Liu, W.-H., Yuan, C., Qiu, M., Yang, Z., Wang, F., & Liu, C.-L. (2026) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2026.107470
Yeşilova, P. G., & Yeşilova, Ç. (2026) · Journal of African Earth Sciences · doi:10.1016/j.jafrearsci.2026.106266
Hou, W., Zhan, X., Zhou, Y., Liu, C.-L., Li, J., Lin, H., Yao, F., & Zhang, S. (2026) · Water · doi:10.3390/w18111284
Cheng, H.-D., Chen, Y., & Zhang, S. (2026) · Molecules · doi:10.3390/molecules31081269
Li, J., Zhang, X.-Y., Ma, Z., Zhang, Z., & Miao, W.-L. (2026) · Journal of Oceanology and Limnology · doi:10.1007/s00343-025-5206-x
Zeng, Z., Xu, Y., & Yao, W. (2026) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2026.03.023
Cheng, F.-W., Zhang, S., Wu, J., Huang, B.-F., & Zhang, D. (2025) · Minerals · doi:10.3390/min15111107
“…in the ore-forming fluids commonly have four sources: deep magmatic/mantle (generally δ 34 S ≈ − 3‰ to 3‰; [110]), seawater sulfate (generally δ 34 S ≈ 20 ± 10‰; [111]), sedimentary reduced sulfur (generally δ 34 S as low as − 40‰; [112]), and mixed sources (generally with a wide δ 34 S range).”
Elmagd, K. A., Matsumoto, R., Abioui, M., & Hazem, M. (2025) · Ore and Energy Resource Geology · doi:10.1016/j.oreoa.2025.100119
Znazen, R., Sliti, R., Khachira, A., Soussi, M., Reynaud, J.-Y., Salem, A. B., Saïdi, M., & Boukhalfa, K. (2025) · Carbonates and evaporites · doi:10.1007/s13146-025-01113-0
“This configuration led to the decrease in water salinity, favoring sulfate rather than salt precipitation in coastal sebkha settings (Holser and Kaplan 1966; Garrett 1970; Eugster 1980; Zenger 1982; Hardie 1996; Rouchy 2001; Kendall et al. 2003; Hay et al. 2006; Honor and Mclnstosh 2006; Warren…”
Tracing the Origin of Hydrogen Sulfide in the J Oilfield
Wan, L.-P., & Yuan, S. (2025) · Chemistry and technology of fuels and oils · doi:10.1007/s10553-025-01898-9
Shu, X., Meng, F., & Liang, K. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112200 · Cited by 1
Stable Isotope for Tracing the Salt Involved in the Degradation of Stone Monuments
Karalis, P., Tassi, M., Gougoura, S., Diamantopoulos, G., Kyropoulou, D., Heliades, E., Palaigeorgiou, E., & Dotsika, E. (2021) · Lecture Notes in Civil Engineering · doi:10.1007/978-3-030-90788-4_10
Spéciation et isotopie du soufre inorganique en milieu aqueux
Martinez, M. (2019) · theses.fr (ABES) · doi:10.70675/3c25f69bz194bz4e74z9ae2z55ab48f97694
“fractionnement isotopique (< 2 ‰) entre les sulfates dissous dans la solution initiale et le précipité formé peut avoir lieu (Holser and Kaplan, 1966; Raab and Spiro, 1991).”
Pasquier, V. (2017) · theses.fr (ABES) · doi:10.70675/bb19708azff44z4291z87b5zfbaa33d25c16
SULFUR ISOTOPIC EVIDENCE FOR BACTERIOGENIC SULFIDES IN BOTTOM SEDIMENTS FROM THE SEA OF JAPAN
Sasaki, A., & Kobayashi, K. (1979) · doi:10.5575/geosoc.85.595
Geochemistry of Carbon and Sulfur DSDP Leg 29
Erdman, J., Schorno, K., & Scalan, R. (1975) · doi:10.2973/dsdp.proc.31.29app4.1975
Stinn, C., & Allanore, A. (2022) · REWAS 2022: Developing Tomorrow’s Technical Cycles (Volume I) · doi:10.1007/978-3-030-92563-5_14
(2020) · Elsevier eBooks · doi:10.1016/b978-0-12-814608-8.09992-8
The effect of depositional environment and early marine diagenesis on carbonate-associated sulfate
Richardson, J. A. (2019) · Open Scholarship Institutional Repository (Washington University in St. Louis) · doi:10.7936/s80y-s604
“Due to the close agreement between modern seawater and evaporite minerals, δ34Sevap has been widely used to reconstruct δ34SSO4 since the 1960’s (Claypool et al., 1980; Holser and Kaplan, 1966; Schidlowski et al., 1977; Strauss, 1997a; Thode et al., 1974).”
BackgroundGieskes, J. (1998) · doi:10.1007/1-4020-4496-8_86
Metadata
- Authors
- Holser, W. T., & Kaplan, I. R.
- Affiliations
- University of California System (US)
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 1966
- Volume
- 1
- Pages
- 93-135
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2019135021
- Cited by
- 550
- References
- 0
- Citations by year
- 2026: 10 · 2025: 11 · 2024: 7 · 2023: 7 · 2022: 16 · 2021: 13 · 2020: 15 · 2019: 12 · 2018: 11 · 2017: 10 · 2016: 9 · 2015: 5 · 2014: 9 · 2013: 10 · 2012: 10
- FWCI
- 12.91
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- anhydrite, gypsum, sulfur isotopes, δ34S, paleoceanography, sulfur cycling, Late Paleozoic, Mesozoic, Tertiary, Late Permian, evaporites, paleogeography, tectonic change
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