Global enhancement of ocean anoxia during Oceanic Anoxic Event 2: A quantitative approach using U isotopes

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Items 101–190 of 190

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17. The Sedimentary Sulfur System: Biogeochemistry and Evolution through Geologic Time
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19. Environmental controls on very high δ238U values in reducing sediments: Implications for Neoproterozoic seawater records
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21. Uranium isotope geochemistry in modern coastal sediments: Insights from Toulon Bay, France
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25. New Constraints on Global Geochemical Cycling During Oceanic Anoxic Event 2 (Late Cretaceous) From a 6‐Million‐year Long Molybdenum‐Isotope Record
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28. 98Mo/95Mo and 238U/235U in lamproites, shoshonites, and high-K calc-alkaline rocks from Western Alps: inferences on their genesis
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29. Electron flux is a key determinant of uranium isotope fractionation during bacterial reduction
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34. Carbonate uranium isotopes across Cretaceous OAE 2 in southern Mexico: New constraints on the global spread of marine anoxia and organic carbon burial
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35. Isotope Fractionation Processes of Selected Elements
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39. Redox conditions, glacio-eustasy, and the status of the Cenomanian–Turonian Anoxic Event: new evidence from the Upper Cretaceous Chalk of England
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40. Regional conditions cause contrasting behaviour in U-isotope fractionation in black shales: Constraints for global ocean palaeo-redox reconstructions
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41. Isotopic history of seawater: the stable isotope character of the global ocean at present and in the geological past
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42. Fractionation factor of 238U and 235U isotopes in the process of hydrothermal pitchblende formation: A numerical estimate
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43. Source versus weathering processes as controls on the Mackenzie river uranium isotope signature
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44. Keeping Time with Earth's Heaviest Element
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45. Incorporation and Preservation of Molybdenum and Uranium Isotope Variations in Modern Marine Sediments
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46. Assessing the Effect of Large Igneous Provinces on Global Oceanic Redox Conditions Using Non‐traditional Metal Isotopes (Molybdenum, Uranium, Thallium)
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47. The isotopic signature of UV during bacterial reduction
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48. High-Precision Determination of the 238U/235U Isotope Ratio in Rocks by Multicollector Inductively Coupled Plasma Mass Spectrometry
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50. Euxinic Systems
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57. Pentavalent U Reactivity Impacts U Isotopic Fractionation during Reduction by Magnetite
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58. Isotope Fractionation Processes of Selected Elements
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72. Geochemical Events at the Cenomanian–Turonian Boundary: Relation of Anoxia with Volcanism, Climate, and Ocean Circulation
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