0000000000384732

AUTHOR

A. Joshua West

showing 3 related works from this author

Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum.

2021

Description

MultidisciplinaryEarth Environmental Ecological and Space Sciences010504 meteorology & atmospheric sciencesIsotopes of lithiumGeochemistrychemistry.chemical_elementSciAdv r-articlesGeology15. Life on land010502 geochemistry & geophysics01 natural sciencesGeochemistrychemistry13. Climate actionCarbon isotope excursionErosionEnhanced weatheringPeriod (geology)Environmental scienceWater cycleCarbon0105 earth and related environmental sciencesResearch ArticleScience advances
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Mercury contents and isotope ratios from diverse depositional environments across the Triassic–Jurassic Boundary: Towards a more robust mercury proxy…

2021

Abstract Mercury is gaining prominence as a proxy for large igneous province (LIP) volcanism in the sedimentary record. Despite temporal overlap between some mass extinctions and LIPs, the precise timing of magmatism relative to major ecological and environmental change is difficult to untangle, especially in marine settings. Changes in the relative contents of Hg in sedimentary rocks through time, or ‘Hg anomalies’, can help resolve the timing of LIP activity and marine extinctions. However, major questions remain unanswered about the fidelity of Hg as a proxy for LIP magmatism. In particular, depositional (e.g., redox) and post-depositional (e.g., oxidative weathering) processes can affec…

Extinction eventCarbonate platformLithologyStable isotope ratioLarge igneous provinceGeochemistryMercuryEnd–Triassic extinction Mercury isotope Triassic–Jurassic boundary MercuryEnd–Triassic extinction; Mercury; Mercury isotope; Triassic–Jurassic boundaryMercury isotopeSedimentary depositional environmentEnd–Triassic extinctionMagmatismGeneral Earth and Planetary SciencesSedimentary rockTriassic–Jurassic boundaryGeologyEarth-Science Reviews
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The lithium and magnesium isotope signature of olivine dissolution in soil experiments

2021

Abstract This study presents lithium and magnesium isotope ratios of soils and their drainage waters from a well-characterised weathering experiment with two soil cores, one with olivine added to the surface layer, and the other a control core. The experimental design mimics olivine addition to soils for CO2 sequestration and/or crop fertilisation, as well as natural surface addition of reactive minerals such as during volcanic deposition. More generally, this study presents an opportunity to better understand how isotopic fractionation records weathering processes. At the start of the experiment, waters draining both cores have similar Mg isotope composition to the soil exchangeable pool. …

OlivineStable isotope ratioGeologyWeathering010501 environmental sciencesengineering.material010502 geochemistry & geophysics01 natural sciences6. Clean waterchemistry.chemical_compoundchemistry13. Climate actionGeochemistry and PetrologyEnvironmental chemistrySoil waterEnhanced weatheringengineeringCarbonateDissolutionDeposition (chemistry)Geology0105 earth and related environmental sciencesChemical Geology
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