Drupal-Biblio17<style face="normal" font="default" size="100%">Controls on uranium isotopic fractionation in the Late Paleoproterozoic ocean</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Evaluating manganese removal in groundwater using pilot scale biofilters: the role of filter media characteristics during startup</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Late-orogenic retrograde zircon growth</style>Drupal-Biblio5<style face="normal" font="default" size="100%">Oxygenating Earth [current title on website reads &quot;Archean Atmosphere, Hydrosphere and Biosphere Evolution: Insights from The Isotopic Record&quot;</style>Drupal-Biblio5<style face="normal" font="default" size="100%">Oxygenation of the Proterozoic Earth&rsquo;s surface: An evolving story</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Reel-to-reel Re-Os records: Earth system transactions preserved in sediments</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Transient marine bottom water oxygenation on continental shelves by ~2.65 billion years ago</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Effects of lithium isotopes on sodium/lithium co-transport and calcium efflux through the sodium/calcium/lithium exchanger in mitochondria</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Uranium isotopes in non-euxinic shale and carbonate reveal dynamic Katian marine redox conditions accompanying a decrease in biodiversity prior to the Late Ordovician mass extinction</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Butterfly effect of shallow ocean deoxygenation on past marine biodiversity</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Cascade electrocatalysis via AgCu single-atom alloy and Ag nanoparticles in CO<sub>2</sub> electroreduction toward multi-carbon products</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Evaluation of the molybdenum isotope system as a petroleum tracer: the Phosphoria petroleum system, western U.S.A.</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Global ocean redox changes before and during the Toarcian Oceanic Anoxic Event</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Lithium isotopes differentially modify mitochondrial amorphous calcium phosphate cluster size distribution and calcium capacity</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Molybdenum isotope evidence from restricted-basin mudstones for an intermediate extent of oxygenation in the late Ediacaran ocean</style>Drupal-Biblio17<style face="normal" font="default" size="100%">No evidence for expansion of global ocean euxinia during the base Stairsian mass extinction event (Tremadocian, Early Ordovician)</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Selectively reducing nitrate into NH<sub>3</sub> in neutral media by PdCu single-atom alloy electrocatalysis</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Technical comment on &ldquo;Reexamination of 2.5-Ga &#39;whiff&#39; of oxygen interval points to anoxic ocean before GOE&rdquo;</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Uranium and molybdenum isotope evidence for globally extensive marine euxinia on continental margins and in epicontinental seas during the Devonian-Carboniferous Hangenberg Crisis</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Insights from modern diffuse flow hydrothermal systems into the origin of post-GOE deep-water Fe-Si precipitates</style>Drupal-Biblio17<style face="normal" font="default" size="100%">The Mo- and U-isotope signatures in alternating shales and carbonate beds of rhythmites: a comparison and implications for redox conditions across the Cambrian-Ordovician boundary</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Molybdenum isotope-based redox deviation driven by continental margin euxinia during the early Cambrian</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Shale heavy metal isotope records of low environmental O<sub>2</sub> between two Archean oxidation events</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Significance of <sup>56</sup>Fe depletions in late-Archean shales and pyrite</style>Drupal-Biblio5<style face="normal" font="default" size="100%">Assessing the effect of large igneous provinces on global oceanic redox conditions using non-traditional metal isotopes (molybdenum, uranium, thallium)</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Consective Fe redox cycles decrease bioreducible Fe(III) and Fe isotope fractionations by eliminating small clay particles</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Long-lived anatexis in the exhumed middle crust of the Torngat Orogen: constraints from phase equilibria modeling and garnet, zircon, and monazite chronology</style>Drupal-Biblio17<style face="normal" font="default" size="100%">New constraints on mid-Proterozoic ocean redox from stable thallium isotope systematics of black shales</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Recent advances in geochemical paleo-oxybarometers</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Estimating ancient seawater isotope compositions and global ocean redox conditions by coupling the molybdenum and uranium isotope systems of euxinic organic-rich mudrocks</style>Drupal-Biblio17<style face="normal" font="default" size="100%">An expanded shale d98Mo record permits recurrent shallow marine oxygenation during the Neoarchean</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Inverse correlation between the molybdenum and uranium isotope compositions of Upper Devonian black shales caused by changes in local depositional conditions rather than global ocean redox variations</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Molybdenum isotope constraints on the origin of vanadium hyper-enrichments in Ediacaran-Phanerozoic marine mudrocks</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Fully oxygenated water columns over continental shelves before the Great Oxidation Event</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Multiple negative molybdenum isotope excursions in the Doushantuo Formation (South China) fingerprint complex redox-related processes in the Ediacaran Nanhua Basin</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Extensive marine anoxia during the terminal Ediacaran Period</style>Drupal-Biblio17<style face="normal" font="default" size="100%">A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Good golly, why moly? The stable isotope geochemistry of molybdenum</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Marine redox conditions during deposition of Late Ordovician and Early Silurian organic-rich mudrocks in the Siljan ring district, central Sweden</style>Drupal-Biblio17<style face="normal" font="default" size="100%">A multi-isotope approach towards constraining the origin of large-scale Paleoproterozoic B-(Fe) mineralization in NE China</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Temporal record of osmium concentrations and <sup>187</sup>Os/<sup>188</sup>Os in organic-rich mudrocks: implications for the osmium geochemical cycle and the use of osmium as a paleoceanographic tracer</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Uranium isotope compositions of mid-Proterozoic black shales: evidence for an episode of increased ocean oxygenation at 1.36 Ga and evaluation of the effect of post-depositional hydrothermal fluid flow</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Genesis of a giant Paleoproterozoic strata-bound magnesite deposit: Constraints from Mg isotopes</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Oceanic oxygenation events in the anoxic Ediacaran ocean</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Trace elements at the intersection of marine biological and geochemical evolution</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Oxygenation of a Cryogenian ocean (Nanhua Basin, South China) revealed by pyrite Fe isotope compositions</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Redox conditions across the Cambrian-Ordovician boundary: elemental and isotopic signatures retained in the GSSP carbonates</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Transient episodes of mild environmental oxygenation and oxidative continental weathering during the late Archean</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Uranium and molybdenum isotope evidence for an episode of widespread ocean oxygenation during the late Ediacaran Period</style>Drupal-Biblio5<style face="normal" font="default" size="100%">Chapter 8.21 - The geologic history of seawater</style>Drupal-Biblio17<style face="normal" font="default" size="100%">An osmium-based method for assessing the source of dissolved rhenium and molybdenum to Archean seawater</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Bioavailability of zinc in marine systems through time</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Depositional age of the early Paleoproterozoic Klipputs Member, Nelani Formation (Ghaap Group, Transvaal Supergroup, South Africa) and implications for low-level Re-Os geochronology and Paleoproterozoic global correlations</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Re-Os age constraints and new observations of Proterozoic glacial deposits in the Vazante Group, Brazil</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Uranium isotope fractionation suggests oxidative uranium mobilization at 2.50 Ga</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Anomalous molybdenum isotope trends in Upper Pennsylvanian euxinic facies: Significance for use of d<sup>98</sup>Mo as a global marine redox proxy</style>Drupal-Biblio5<style face="normal" font="default" size="100%">Chapter 6 - The global iron cycle</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Ocean oxygenation in the wake of the Marinoan glaciation</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Molybdenum isotope constraints on the extent of late Paleoproterozoic ocean euxinia</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Molybdenum isotope evidence for mild environmental oxygenation before the Great Oxidation Event</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Pervasive oxygenation along late Archaean ocean margins</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Correlation of Sturtian diamictite successions in southern Australia and northwestern Tasmania by Re-Os black shale geochronology and the ambiguity of &ldquo;Sturtian&rdquo;-type diamictite &ndash; cap carbonate pairs as chronostratigraphic marker horizon</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Re-Os and Mo isotope systematics of black shales from the Middle Proterozoic Velkerri and Wollogorang Formations, McArthur Basin, northern Australia</style>Drupal-Biblio5<style face="normal" font="default" size="100%"><sup>187</sup>Re-<sup>187</sup>Os geochronology of Precambrian organic-rich sedimentary rocks</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Global correlation of the Vazante Group, São Francisco Basin, Brazil: Re-Os and U-Pb radiometric age constraints</style>Drupal-Biblio17<style face="normal" font="default" size="100%">A whiff of oxygen before the Great Oxidation Event?</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Re-Os geochronology of post-glacial black shales in Australia: Constraints on the timing of &ldquo;Sturtian&rdquo; glaciation</style>Drupal-Biblio17<style face="normal" font="default" size="100%">Constraints on the timing of Marinoan &ldquo;Snowball Earth&rdquo; glaciation by <sup>187</sup>Re-<sup>187</sup>Os dating of a Neoproterozoic, post-glacial black shale in western Canada</style>