Results 161 to 170 of about 928 (188)
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Geochimica et Cosmochimica Acta, 2023
Uranium isotopes (238U/235U) are commonly utilised in marine carbonates to reconstruct the redox evolution of ancient oceans and the atmosphere. However, questions remain concerning U isotope fractionation during carbonate precipitation and/or early sedimentary diagenesis. Moreover, the stromatolitic nature of many Precambrian limestones and dolostones
Ashley N. Martin +3 more
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Uranium isotopes (238U/235U) are commonly utilised in marine carbonates to reconstruct the redox evolution of ancient oceans and the atmosphere. However, questions remain concerning U isotope fractionation during carbonate precipitation and/or early sedimentary diagenesis. Moreover, the stromatolitic nature of many Precambrian limestones and dolostones
Ashley N. Martin +3 more
openaire +3 more sources
Elements, 2009
Knowledge about paleoredox conditions is essential for reconstructing how the oxygenation of the Earth's surface environment has changed through time and affected the evolution of life on our planet. Some metal stable isotope systems, such as Mo isotopes, record the extent of ocean oxygenation directly.
S. Severmann, A. D. Anbar
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Knowledge about paleoredox conditions is essential for reconstructing how the oxygenation of the Earth's surface environment has changed through time and affected the evolution of life on our planet. Some metal stable isotope systems, such as Mo isotopes, record the extent of ocean oxygenation directly.
S. Severmann, A. D. Anbar
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A Multi-Basin Comparison of Paleoredox Conditions During the Mid-Silurian Mulde/Lundgreni Event
Global and Planetary ChangeAnders Lindskog +2 more
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Uranium isotope fractionation in Saanich Inlet: A modern analog study of a paleoredox tracer
Geochimica et Cosmochimica Acta, 2015Abstract Uranium isotope fractionation was studied in the sediment and water of Saanich Inlet, a seasonally anoxic fjord on the east coast of Vancouver Island. The concentration of dissolved U is the same above and below the redoxcline at ∼120 m depth, with an average δ238U value of −0.45 ± 0.06‰ (2 s.e.), which is indistinguishable from seawater ...
C. Holmden, M. Amini, R. Francois
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PALEOREDOX CONDITIONS OF THE POINT PLEASANT FORMATION IN SE OHIO
Geological Society of America Abstracts with Programs, 2022Emily Bergel +2 more
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Shark teeth: a new U isotopic archive for paleoredox reconstruction?
Goldschmidt2022 abstracts, 2022Haoyu Li +4 more
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Paleoredox Conditions of Early Carboniferous Upper Bakken Shale, Williston Basin
Proceedings of the 9th Unconventional Resources Technology Conference, 2021Dipanwita Nandy +2 more
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EXPLORING THE POTENTIAL OF THE RE ISOTOPE PALEOREDOX PROXY
Geological Society of America Abstracts with Programs, 2019Dan Louis Sullivan +2 more
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TELLURIUM ISOTOPES AS A PALEOREDOX PROXY: AN INITIAL ASSESSMENT
Geological Society of America Abstracts with Programs, 2016Naomi L. Wasserman, Thomas M. Johnson
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Tungsten (isotope) cycling in modern marine basins and implications for paleoredox reconstructions
Goldschmidt2022 abstracts, 2022Florian Kurzweil +5 more
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