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SHURAM EXCURSION

  • Shuram excursion
  • The Shuram excursion, or Shuram-Wonoka excursion, is a change in δ13C, or in the ratio of carbon-13 to carbon-12, taking place during the Ediacaran period

    Shuram excursion

    Shuram_excursion

  • Ediacaran
  • Third and last period of the Neoproterozoic Era

    glaciation events, such as the Gaskiers and Baykonurian glaciations. The Shuram excursion also occurred during this period, but its glacial origin is unlikely

    Ediacaran

    Ediacaran

    Ediacaran

  • Gametrail Formation
  • Geologic formation in Canada

    carbonate ramp. Found recorded within the Gametrail Formation is a Shuram excursion, where there is a sudden negative δ13C anomaly, with Carbon-13 levels

    Gametrail Formation

    Gametrail_Formation

  • Ediacaran biota
  • Life of the Ediacaran period

    evidence for transient marine-shelf oxidation during the Ediacaran Shuram Excursion". Geology. 46 (3): 267–270. doi:10.1130/G39663.1. Benus (May 1988)

    Ediacaran biota

    Ediacaran biota

    Ediacaran_biota

  • White Sea assemblage
  • Ediacaran biotic assemblage

    evidence for transient marine-shelf oxidation during the Ediacaran Shuram Excursion". Geology. 46 (3): 267–270. doi:10.1130/G39663.1. Evans, Scott D.;

    White Sea assemblage

    White Sea assemblage

    White_Sea_assemblage

  • Nama assemblage
  • Ediacaran biotic assemblage

    evidence for transient marine-shelf oxidation during the Ediacaran Shuram Excursion". Geology. 46 (3): 267–270. doi:10.1130/G39663.1. Wood, Rachel; Bowyer

    Nama assemblage

    Nama assemblage

    Nama_assemblage

  • Δ13C
  • Measure of relative carbon-13 concentration in a sample

    Paleoproterozoic - Positive excursion Shunga-Francevillian event (2,080 Ma) Paleoproterozoic - Negative excursion Shuram-Wonoka excursion (570–551 Ma) Neoproterozoic

    Δ13C

    Δ13C

  • End-Ediacaran extinction
  • Mass extinction event at the end of the Ediacaran period, 539 million years ago

    Negative δ13C excursions—geochemical signals often associated with mass extinctions—are observed during the Late Ediacaran. The Shuram excursion occurred around

    End-Ediacaran extinction

    End-Ediacaran_extinction

  • Lantian Formation
  • Geologic formation in Anhui Province, China

    "Ediacaran Negative excursion 3", which itself is correlated to the Shuram excursion. Meanwhile, the δ34S pyrite isotopes present a spatial pattern, and

    Lantian Formation

    Lantian Formation

    Lantian_Formation

  • Avalon assemblage
  • Ediacaran biotic assemblage

    evidence for transient marine-shelf oxidation during the Ediacaran Shuram Excursion". Geology. 46 (3): 267–270. doi:10.1130/G39663.1. Liu, Alexander G

    Avalon assemblage

    Avalon assemblage

    Avalon_assemblage

  • John P. Grotzinger
  • largest carbon isotope excursion in Earth history, suggesting dramatic reorganization of Earth's carbon cycle. The Shuram Excursion closely precedes impressive

    John P. Grotzinger

    John P. Grotzinger

    John_P._Grotzinger

  • Kheseen Formation
  • Geologic formation in Mongolia

    has been inferred to either be the late Ediacaran Shuram excursion, or the Basal Cambrian δ13C excursion (BACE) in previous studies, with both of these being

    Kheseen Formation

    Kheseen_Formation

  • Clemente Formation
  • Ediacaran geologic formation found in Sonora, Mexico

    Death Valley, California, and preserves an isotopic record of the Shuram excursion. At its type section, the Clemente Formation consists of 210.3 m (690 ft)

    Clemente Formation

    Clemente_Formation

  • Neoproterozoic oxygenation event
  • Neoproterozoic surge in atmospheric oxygen

    December 2013). "The stratigraphic relationship between the Shuram carbon isotope excursion, the oxygenation of Neoproterozoic oceans, and the first appearance

    Neoproterozoic oxygenation event

    Neoproterozoic oxygenation event

    Neoproterozoic_oxygenation_event

  • Sheepbed Formation
  • Geologic formation in Canada

    "Deep‐water first occurrences of Ediacara biota prior to the Shuram carbon isotope excursion in the Wernecke Mountains, Yukon, Canada". Geobiology. 22 (3)

    Sheepbed Formation

    Sheepbed_Formation

  • Nadaleen Formation
  • Geologic formation in Canada

    Nadaleen and Drook Formations had established themselves before the Shuram excursion anomaly seen in the overlying Gametrail Formation. The Nadaleen Formation

    Nadaleen Formation

    Nadaleen_Formation

  • 2026 in paleontology
  • acritarchs (otherwise predominantly known from pre-Shuram strata) in the horizon recording the Shuram excursion. Yang et al. (2026) study the composition of

    2026 in paleontology

    2026_in_paleontology

  • Stirling Quartzite
  • Geologic formation in the Mojave Desert

    Wernicke, B. P.; Bowring, S. A. (1 July 2011). "The Shuram and subsequent Ediacaran carbon isotope excursions from southwest Laurentia, and implications for

    Stirling Quartzite

    Stirling Quartzite

    Stirling_Quartzite

  • Blueflower Formation
  • Geologic formation in the Northwest Territories, Canada

    "Deep‐water first occurrences of Ediacara biota prior to the Shuram carbon isotope excursion in the Wernecke Mountains, Yukon, Canada". Geobiology. 22 (3)

    Blueflower Formation

    Blueflower_Formation

  • 2020 in paleontology
  • onset and termination of the Shuram carbon isotope excursion is published by Rooney et al. (2020), who argue that this excursion was divorced from the rise

    2020 in paleontology

    2020_in_paleontology

  • 2019 in paleontology
  • (2019). A study on ocean oxygen levels during the Ediacaran Shuram negative C-isotope Excursion and the middle Ediacaran, and on their implications for the

    2019 in paleontology

    2019_in_paleontology

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