Cited by 11Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisGeological formations and processes

The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.

Redox conditions through the Permian-Triassic transition in the upper Khuff formation, Saudi Arabia

Eltom, Hassan A., Abdullatif, Osman M., Babalola, Lamidi O.·2017·Palaeogeography, Palaeoclimatology, Palaeoecology

Overview

Integrity signals

Registry

Crossref · 10.1016/j.palaeo.2017.01.046

Cites

2 of 2 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Verification

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

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?

Citations

Cites

Show all 2 references

Research works printed but not linked: 76

  1. Abu-Ali, 1999, Paleozoic petroleum system of central Saudi Arabia, GeoArabia, 4, 321, 10.2113/geoarabia0403321 · DOI
  2. Adams, 1958, Thorium-to-uranium ratios as indicators of sedimentary processes: example of concept of geochemical facies, AAPG Bull., 42, 387
  3. Al-Aswad, 1997, Stratigraphy, sedimentary environment and depositional evolution of the Khuff formation in south-central Saudi Arabia, J. Pet. Geol., 20, 307, 10.1111/j.1747-5457.1997.tb00638.x · DOI
  4. Algeo, 2004, Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclothems, Chem. Geol., 206, 289, 10.1016/j.chemgeo.2003.12.009 · DOI
  5. Algeo, 2007, Sequencing events across the Permian–Triassic boundary, Guryul Ravine (Kashmir, India), Palaeogeogr. Palaeoclimatol. Palaeoecol., 252, 328, 10.1016/j.palaeo.2006.11.050 · DOI
  6. Algeo, 2007, The Permian–Triassic boundary at Nhi Tao, Vietnam: evidence for recurrent influx of sulfidic watermasses to a shallow-marine carbonate platform, Palaeogeogr. Palaeoclimatol. Palaeoecol., 252, 304, 10.1016/j.palaeo.2006.11.055 · DOI
  7. Algeo, 2010, Changes in productivity and redox conditions in the Panthalassic Ocean during the latest Permian, Geology, 38, 187, 10.1130/G30483.1 · DOI
  8. Bau, 1996, Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, South Africa, Precambrian Res., 79, 37, 10.1016/0301-9268(95)00087-9 · DOI
  9. Baud, 1997, Biotic response to mass extinction: the lowermost Triassic microbialites, Facies, 36, 238
  10. Baud, 2013, Permian‐Triassic Transition and the Saiq/Mahil Boundary in the Oman Mountains: Proposed correction for lithostratigraphic nomenclature, GeoArabia, J. Middle East Pet. Geosci., 18, 87
  11. Berthelin, 2006, Mixed Late Permian floras and related paleoenvironments in the upper Khuff formation of central Saudi Arabia, GeoArabia, 11, 56, 10.2113/geoarabia110365 · DOI
  12. Bowring, 1998, U/Pb zircon geochronology and tempo of the end-Permian mass extinction, Science, 280, 1039, 10.1126/science.280.5366.1039 · DOI
  13. Campbell, 1992, Synchronism of the Siberian traps and the Permian-Triassic boundary, Science, 258, 1760, 10.1126/science.258.5089.1760 · DOI
  14. Cantrell, 2014, Tethyan petroleum systems of Saudi Arabia, Vol. 106, 613
  15. Cao, 2009, Biogeochemical evidence for euxinic oceans and ecological disturbance presaging the end-Permian mass extinction event, Earth Planet. Sci. Lett., 281, 188, 10.1016/j.epsl.2009.02.012 · DOI
  16. Chen, 2015, Diagenetic uptake of rare earth elements by bioapatite, with an example from the Lower Triassic of South China, Earth Sci. Rev., 149, 177, 10.1016/j.earscirev.2015.01.013 · DOI
  17. Clarkson, 2015, Ocean acidification and the Permo-Triassic mass extinction, Science, 348, 229, 10.1126/science.aaa0193 · DOI
  18. Cole, 1994, Organic geochemistry of the Paleozoic petroleum system of Saudi Arabia, Energy Fuel, 8, 1425, 10.1021/ef00048a034 · DOI
  19. Collin, 2015, Geochemistry of post-extinction microbialites as a powerful tool to assess the oxygenation of shallow marine water in the immediate aftermath of the end-Permian mass extinction, Int. J. Earth Sci., 104, 1025, 10.1007/s00531-014-1125-3 · DOI
  20. Crasquin-Soleau, 2006, Ostracods of the Permian-Triassic Khuff formation, Saudi Arabia: palaeoecology and palaeobiogeography, GeoArabia, 11, 55, 10.2113/geoarabia110155 · DOI
  21. Ehrenberg, 2008, Uranium depletion across the Permian–Triassic boundary in Middle East carbonates: signature of oceanic anoxia, AAPG Bull., 92, 691, 10.1306/02140807095 · DOI
  22. Eltom, 2016, Geochemical characterization of the Permian–Triassic transition at outcrop, central Saudi Arabia, J. Pet. Geol., 39, 95, 10.1111/jpg.12630 · DOI
  23. Eltom, 2016, Integration of facies architecture, ooid granulometry and morphology for prediction of reservoir quality, Lower Triassic Khuff formation, Saudi Arabia, Pet. Geosci.
  24. Eltom, 2016, Three-dimensional outcrop reservoir analog model: A case study of the Upper Khuff Formation oolitic carbonates, central Saudi Arabia, J. Pet. Sci. Eng.
  25. Erwin, 1994, The Permo-Triassic extinction, Nature, 367, 231, 10.1038/367231a0 · DOI
  26. Erwin, 2002, End-Permian mass extinctions: a review, Vol. 356, 353
  27. Feng, 2014, Evolution of oceanic redox conditions during the Permo-Triassic transition: evidence from deepwater radiolarian facies, Earth Sci. Rev., 137, 34, 10.1016/j.earscirev.2013.12.003 · DOI
  28. Fischer, 2001, Jurassic gastropod faunas of central Saudi Arabia, GEOARABIA-MANAMA-, 6, 63, 10.2113/geoarabia060163 · DOI
  29. Forel, 2009, Ostracods (Crustacea) and water oxygenation in the earliest Triassic of South China: implications for oceanic events at the end­Permian mass extinction, Aust. J. Earth Sci., 815, 10.1080/08120090903002631 · DOI
  30. Forel, 2013, In the aftermath of the end-Permian extinction: the microbialite refuge, Terra Nova, 25, 137, 10.1111/ter.12017 · DOI
  31. Grice, 2005, Photic zone euxinia during the Permian­Triassic superanoxic event, Science, 307, 705, 10.1126/science.1104323 · DOI
  32. Groves, 2005, Extinction, survival, and recovery of lagenide foraminifers in the Permian-Triassic boundary interval, central Taurides, Turkey, J. Paleontol., 79, 1, 10.1666/0022-3360(2005)79[1:ESAROL]2.0.CO;2 · DOI
  33. Heydari, 2003, Permian–Triassic boundary interval in the Abadeh section of Iran with implications for mass extinction: part 1. Sedimentology, Palaeogeogr. Palaeoclimatol. Palaeoecol., 193, 405, 10.1016/S0031-0182(03)00258-X · DOI
  34. Hotinski, 2001, Ocean stagnation and end-Permian anoxia, Geology, 29, 7, 10.1130/0091-7613(2001)029<0007:OSAEPA>2.0.CO;2 · DOI · Paper page
  35. Insalaco, 2006, Upper Dalan Member and Kangan Formation between the Zagros Mountains and offshore Fars, Iran: depositional system, biostratigraphy and stratigraphic architecture, GEOARABIA-MANAMA-, 11, 75, 10.2113/geoarabia110275 · DOI
  36. Isozaki, 1997, Permo-Triassic boundary superanoxia and stratified superocean: records from lost deep sea, Science, 276, 235, 10.1126/science.276.5310.235 · DOI · Paper page
  37. Kakuwa, 2006, Cerium negative anomaly just before the Permian and Triassic boundary event—the upward expansion of anoxia in the water column, Palaeogeogr. Palaeoclimatol. Palaeoecol., 229, 335, 10.1016/j.palaeo.2005.07.005 · DOI
  38. Knoll, 1996, Comparative earth history and Late Permian mass extinction, Science, 273, 452, 10.1126/science.273.5274.452 · DOI
  39. Koehrer, 2010, Facies and stratigraphic framework of a Khuff outcrop equivalent: Saiq and Mahil formations, Al Jabal al-Akhdar, Sultanate of Oman, GeoArabia, 15, 91, 10.2113/geoarabia150291 · DOI
  40. Krull, 2000, Delta 613C depth profiles from paleosols across the Permian-Triassic boundary: evidence for methane release, Geol. Soc. Am. Bull., 112, 1459, 10.1130/0016-7606(2000)112<1459:CDPFPA>2.0.CO;2 · DOI
  41. Krystyn, 2003, A unique Permian–Triassic boundary section from Oman, Palaeogeogr. Palaeoclimatol. Palaeoecol., 191, 329, 10.1016/S0031-0182(02)00670-3 · DOI
  42. Kump, 2005, Massive release of hydrogen sulfide to the surface ocean and atmosphere during intervals of oceanic anoxia, Geology, 33, 397, 10.1130/G21295.1 · DOI
  43. Land, 1973, Sodium in carbonate sediments and rocks: a possible index to the salinity of diagenetic solutions, J. Sediment. Res., 43, 614
  44. Lawrence, 2006, Rare earth element and yttrium variability in South East Queensland waterways, Aquat. Geochem., 12, 39, 10.1007/s10498-005-4471-8 · DOI
  45. Lehrmann, 2003, Permian-Triassic boundary sections from shallow-marine carbonate platforms of the Nanpanjia ng Basin, South China: implications for oceanic conditions associated with the end-Permian extinction and its aftermath, PALAIOS, 18, 138, 10.1669/0883-1351(2003)18<138:PBSFSC>2.0.CO;2 · DOI
  46. Loope, 2013, Shallow water redox conditions from the Permian–Triassic boundary microbialite: the rare earth element and iodine geochemistry of carbonates from Turkey and South China, Chem. Geol., 351, 195, 10.1016/j.chemgeo.2013.05.014 · DOI
  47. Maurer, 2009, The geology of Khuff outcrop analogues in the Musandam Peninsula, United Arab Emirates and Oman, GeoArabia, 14, 125, 10.2113/geoarabia1403125 · DOI
  48. McLennan, 1989, Rare earth elements in sedimentary rocks; influence of provenance and sedimentary processes, Rev. Mineral. Geochem., 21, 169
  49. Morgan, 2004, Contemporaneous mass extinction, continental flood basalts, and “impact signals”: are mantle plume-induced lithospheric gas explosions the cause link?, Earth Planet. Sci. Lett., 217, 263, 10.1016/S0012-821X(03)00602-2 · DOI
  50. Mundil, 2004, Age and timing of the Permian mass extinctions: U/Pb dating of closed-system zircons, Science, 305, 1760, 10.1126/science.1101012 · DOI
  51. Nielsen, 2004, Evidence for sulfidic deep water during the Late Permian in the East Greenland Basin, Geology, 32, 1037, 10.1130/G20987.1 · DOI
  52. Powers, 1966, Geology of the Arabian peninsula, Geol. Surv. Prof. Pap., 560, 1
  53. Pruss, 2004, Late early Triassicmicrobial reefs of the western United States: a description and model for their deposition in the aftermath of the end-Permian mass extinction, Palaeogeogr. Palaeoclimatol. Palaeoecol., 211, 127, 10.1016/j.palaeo.2004.05.002 · DOI
  54. Rampino, 1998, Evidence for abrupt latest Permian mass extinction of foraminifera; results of tests for the Signor–Lipps effect, Geology, 26, 415, 10.1130/0091-7613(1998)026<0415:EFALPM>2.3.CO;2 · DOI
  55. Renne, 1995, Synchronology and causal relations between Permian-Triassic boundary crises and Siberian flood volcanism, Science, 269, 1413, 10.1126/science.269.5229.1413 · DOI
  56. Retallack, 1999, Postapocalyptic greenhouse paleoclimate revealed by earliest Triassic Paleosols in the Sydney Basin, Australia, Geol. Soc. Am. Bull., 111, 52, 10.1130/0016-7606(1999)111<0052:PGPRBE>2.3.CO;2 · DOI
  57. Riccardi, 2006, Sulfur isotopic evidence for chemocline upward excursions during the end-Permian mass extinction, Geochim. Cosmochim. Acta, 70, 5740, 10.1016/j.gca.2006.08.005 · DOI
  58. Richoz, 2006, Stratigraphie et variations isotopiques ducarbone dans le Permien supérieur et le Trias inférieur de quelques localités de la Néotéthys (Turquiee, Oman et Iran), Institut de Géologie et Paléontologie. Mémoire de Géologie de Lausanne, 46
  59. Richoz, 2010, Permian–Triassic boundary interval in the Middle East (Iran and N. Oman): progressive environmental change from detailed carbonate carbon isotope marine curve and sedimentary evolution, J. Asian Earth Sci., 39, 236, 10.1016/j.jseaes.2009.12.014 · DOI
  60. Schubert, 1992, Early Triassic stromatolites as post-mass extinction disaster forms, Geology, 20, 883, 10.1130/0091-7613(1992)020<0883:ETSAPM>2.3.CO;2 · DOI
  61. Sharland, 2004, Arabian plate sequence stratigraphy, GeoArabia, 9, 199, 10.2113/geoarabia0901199 · DOI
  62. Song, 2012, Geochemical evidence from bio-apatite for multiple oceanic anoxic events during Permian–Triassic transition and the link with end-Permian extinction and recovery, Earth Planet. Sci. Lett., 353, 2
  63. Stanley, 1994, A double mass extinction at the end of the Paleozoic Era, Science, 266, 1340, 10.1126/science.266.5189.1340 · DOI
  64. Thackeray, 1990, Carbon isotopic evidence from Late Permian Therapsids teeth, for a progressive change in atmospheric CO2 composition, Nature, 347, 751, 10.1038/347751a0 · DOI
  65. Tribovillard, 2006, Trace metals as paleoredox and paleoproductivity proxies: an update, Chem. Geol., 232, 12, 10.1016/j.chemgeo.2006.02.012 · DOI · Paper page
  66. Twitchett, 2004, Rapid marine recovery after the end-Permian extinction event, Geology, 32, 805, 10.1130/G20585.1 · DOI
  67. Vaslet, 2005, The Permian-Triassic Khuff Formation of central Saudi Arabia, GEOARABIA-MANAMA-, 10, 77, 10.2113/geoarabia100477 · DOI
  68. Wang, 2009, Ecological evolution across the Permian/Triassic boundary at the Kangjiaping section in Cili County, Hunan Province, China, Sci. China Ser. D Earth Sci., 52, 797, 10.1007/s11430-009-0077-0 · DOI
  69. Webb, 2000, Rare earth elements in Holocene reefal microbialites: a new shallow seawater proxy, Geochim. Cosmochim. Acta, 64, 1557, 10.1016/S0016-7037(99)00400-7 · DOI · Paper page
  70. Wender, 1998, Paleozoic (Pre-Khuff) hydrocarbon geology of the Ghawar area, eastern Saudi Arabia, GeoArabia, 3, 273, 10.2113/geoarabia0302273 · DOI
  71. Wignall, 1992, Anoxia as a cause of the Permian–Triassic mass extinction: facies evidence from Northern Italy, Palaeogeogr. Palaeoclimatol. Palaeoecol., 93, 21, 10.1016/0031-0182(92)90182-5 · DOI · Paper page
  72. Wignall, 1988, Interpreting benthic oxygen levels in mudrocks: a new approach, Geology, 16, 452, 10.1130/0091-7613(1988)016<0452:IBOLIM>2.3.CO;2 · DOI · Paper page
  73. Wignall, 1996, Oceanic anoxia and the end-Permian mass extinction, Science, 272, 1155, 10.1126/science.272.5265.1155 · DOI
  74. Wignall, 2005, Pyrite framboid evidence for oxygen­ poor deposition during the Permian- Triassic crisis in Kashmir, Palaeogeogr. Palaeoclimatol. Palaeoecol., 216, 183, 10.1016/j.palaeo.2004.10.009 · DOI
  75. Wilkin, 1996, The size distribution of framboidal pyrite in modern sediments: an indicator of redox conditions, Geochim. Cosmochim. Acta, 60, 3897, 10.1016/0016-7037(96)00209-8 · DOI
  76. Ziegler, 2001, Late Permian to Holocene paleofacies evolution of the Arabian plate and its hydrocarbon occurrences, GeoArabia, 6, 445, 10.2113/geoarabia0603445 · DOI

Cited by

Sorted by citations

Metadata

Authors
Eltom, H. A., Abdullatif, O. M., & Babalola, L. O.
Affiliations
King Fahd University of Petroleum and Minerals (SA)
Corresponding author
Eltom, Hassan A.
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
2017-04
Volume
472
Pages
203-215
ISSN
0031-0182 (ISSN-L)
OpenAlex
W2588317326
Cited by
11
References
2
Citations by year
2026: 1 · 2025: 2 · 2024: 1 · 2023: 1 · 2021: 1 · 2020: 1 · 2019: 3 · 2017: 1
FWCI
0.93
Type
journal article
Language
en
Open access
closed
Locations
Palaeogeography Palaeoclimatology Palaeoecology (publishedVersion)
Funders
King Abdulaziz City for Science and Technology (NSTIP-10-OIL1379-04)
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 › Earth-Surface Processes › Geological formations and processes
Keywords
Permian-Triassic boundary, redox conditions, Khuff Formation, rare earth elements, trace elements, Th/U ratio, uranium, vanadium, cerium anomaly, shallow marine environment, Tethys, end-Permian mass extinction, oxic conditions, Saudi Arabia

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