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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Geochemistry. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (205 pages)
    Edition: 1st ed.
    ISBN: 9783319014302
    Series Statement: Advances in Isotope Geochemistry Series
    DDC: 541.388
    Language: English
    Note: Intro -- Preface -- Acknowledgements -- Contents -- 1 Introduction -- References -- 2 Methodology of Lithium Analytical Chemistry and Isotopic Measurements -- 2.1 Historical Perspective -- 2.2 Lithium Isolation by Cation Exchange Chromatography -- 2.3 Methodology of Li Isotopic Measurements -- 2.3.1 Mass Spectrometry-Based Methods of Widest Use -- 2.3.1.1 TIMS -- 2.3.1.2 ICPMS -- 2.3.1.3 MC-ICPMS -- 2.3.1.4 SIMS -- 2.3.2 "Other" Analytical Methods -- 2.3.2.1 Atomic Absorption Spectrometry (AAS) -- 2.3.2.2 Nuclear- and Charged- Particle-Based Techniques -- 2.3.2.3 Resonance Ionization and Other Techniques -- References -- 3 Cosmochemistry of Lithium -- 3.1 Cosmology of Lithium: Big Bang Nucleosynthesis, Evolution of the Universe, and Stellar Processes -- 3.1.1 The Earliest History and Further Evolution of Lithium -- 3.1.2 The Vicinity of the Solar System -- 3.1.3 Searching for Exoplanets with Lithium -- 3.2 Cosmochemistry of Lithium in Meteorites -- 3.2.1 Lithium in Bulk Chondritic Meteorites -- 3.2.2 Lithium Distribution and Isotopic Systematics in Constituents of Chondritic Meteorites -- 3.2.3 Lithium in Other Meteorites -- 3.3 Cosmochemistry of Lithium in Planetary Bodies -- 3.3.1 Lithium in Earth's Moon -- 3.3.2 Lithium in Mars -- 3.3.3 Lithium in Vesta -- References -- 4 Li Partitioning, Diffusion and Associated Isotopic Fractionation: Theoretical and Experimental Insights -- 4.1 Introduction -- 4.2 Equilibrium Partitioning Behavior of Li -- 4.2.1 Thermodynamic Background -- 4.2.2 Lattice Strain Model for Element Partitioning -- 4.2.3 Mineral-Melt Partitioning -- 4.2.4 Mineral-Fluid Partitioning and Associated Stable Isotopic Fractionation -- 4.2.5 Inter-mineral Partitioning -- 4.3 Diffusion of Li and Associated Effects on δ7Li -- 4.3.1 Theoretical Background -- 4.3.1.1 Diffusion Coefficients -- 4.3.1.2 The Isotopic Effect. , 4.3.1.3 Diffusive Coupling -- 4.3.1.4 Diffusion, Diffusive Fractionation and Time -- 4.3.2 Experimental Diffusion Coefficients -- 4.3.3 Characteristic Time Scales of Li Diffusion in Silicates (Ol, Cpx, Pl) -- 4.3.4 Two Diffusion Mechanisms of Li in Silicates -- 4.3.4.1 Two Species Diffusion Model -- 4.3.4.2 Modeling Results-Sensitivity to fO2 -- 4.3.5 Bulk Diffusion of Li Through Rocks and Characteristic Length Scales -- 4.4 Fluid-Rock Interaction -- 4.4.1 Weathering of Igneous Rocks (Predominantly Basaltic Compositions) -- 4.4.2 Weathering of Olivine (Serpentinization) -- 4.4.3 Alteration of Sediments -- 4.4.4 Synopsis -- References -- 5 Lithium in the Deep Earth: Mantle and Crustal Systems -- 5.1 Lithium in the Mantle -- 5.1.1 Mantle Xenoliths and Related Samples -- 5.1.1.1 Pristine Peridotites and the Primitive Upper Mantle Li Budget -- 5.1.1.2 Metasomatized Peridotites and Post-magmatic Modifications -- 5.1.2 Mantle-Derived Magmas -- 5.1.2.1 Mid-Ocean Ridge Rocks -- 5.1.2.2 Intraplate Volcanic Rocks -- 5.1.2.3 Arc and Back-Arc Rocks -- 5.2 Lithium in the Continental Crust -- 5.2.1 Products of Crustal Melting -- 5.2.2 Crustal Metamorphism and Fluid Flow -- References -- 6 The Surficial Realm: Low Temperature Geochemistry of Lithium -- 6.1 Meteoric Water -- 6.2 Groundwater and Pore Waters -- 6.2.1 Shallow Groundwaters -- 6.2.2 Deep Groundwaters -- 6.2.3 Pore Waters -- 6.3 Continental Weathering -- 6.3.1 Soils and Sediments -- 6.3.2 Sedimentary Rocks -- 6.3.3 Lakes and Rivers: Dissolved Loads -- 6.4 Hydrothermal Systems -- 6.4.1 Rocks in Sea Floor Hydrothermal Systems -- 6.4.2 Fluids in Sea Floor Hydrothermal Systems -- 6.4.3 Continental Geothermal Systems -- 6.5 Marine Geochemistry of Li -- 6.5.1 The Marine Li Cycle -- 6.5.2 Secular Variation of Li in Seawater -- 6.5.2.1 Experiments and Observations -- 6.5.2.2 Interpretation and Modeling. , 6.6 Biological and Anthropogenic Li Isotopic Fractionation -- 6.6.1 Lithium in Plants and Animals -- 6.6.2 Tracer Applications in Water Treatment and Agriculture -- 6.6.3 Nuclear Forensics -- References -- 7 Summation: What Have We Learned and Where Can We Go? -- 7.1 Retrospective -- 7.2 Analytical Prospects -- 7.3 Final Words -- References.
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  • 2
    Online Resource
    Online Resource
    Cham : Springer International Publishing
    Keywords: Earth sciences ; Geochemistry ; Stabiles Isotop ; Isotopengeochemie ; Lithiumisotop ; Lithium ; Geochemie
    Description / Table of Contents: This work summarizes the historical progression of the field of lithium (Li) isotope studies and provides a comprehensive yet succinct overview of the research applications toward which they have been directed. In synthesizing the historical and current research, the volume also suggests prospective future directions of study. Not even a full decade has passed since the publication of a broadly inclusive summary of Li isotope research around the globe (Tomascak, 2004). In this short time, the use of this isotope system in the investigation of geo- and cosmochemical questions has increased dramatically, due, in part, to the advent of new analytical technology at the end of the last millennium. Lithium, as a light element that forms low-charge, moderate-sized ions, manifests a number of chemical properties that make its stable isotope system useful in a wide array of geo- and cosmochemical research fields.
    Type of Medium: Online Resource
    Pages: Online-Ressource (205 pages)
    Edition: Springer eBook Collection. Earth and Environmental Science
    ISBN: 9783319014302
    Series Statement: Advances in isotope geochemistry
    DDC: 551.9
    Language: English
    Note: Methodology of Lithium Analytical Chemistry and Isotopic MeasurementsCosmochemistry of Lithium -- Li Partitioning, Diffusion and Associated Isotopic Fractionation: Theoretical and Experimental Insights -- Lithium in the Deep Earth: Mantle and Crustal Systems -- The Surficial Realm: Low Temperature Geochemistry of Lithium.
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  • 3
    Publication Date: 2024-03-15
    Description: Lithium has proven a powerful tracer of weathering processes and chemical seawater evolution. Skeletal components of marine calcifying organisms, and in particular brachiopods, present promising archives of Li signatures. However, Li incorporation mechanisms and potential influence from biological processes or environmental conditions require a careful assessment. In order to constrain Li systematics in brachiopod shells, we present Li concentrations and isotope compositions for 11 calcitic brachiopod species collected from six different geographic regions, paralleled with data from culturing experiments where brachiopods were grown under varying environmental conditions and seawater chemistry (pH–pCO2, temperature, Mg/Ca ratio). The recent brachiopod specimens collected across different temperate and polar environments showed broadly consistent δ7Li values ranging from 25.2 to 28.1‰ (with mean δ7Li of 26.9 ± 1.5‰), irrespective of taxonomic rank, indicating that incorporation of Li isotopes into brachiopod shells is not strongly affected by vital effects related to differences among species. This results in Δ7Licalcite–seawater values (per mil difference in 7Li/6Li between brachiopod calcite shell and seawater) from −2.9‰ to −5.8‰ (with mean Δ7Licalcite–seawater value of −3.6‰), which is larger than the Δ7Licalcite–seawater values calculated based on data from planktonic foraminifera (~0‰ to ~−4‰). This range of values is further supported by results from brachiopods cultured experimentally. Under controlled culturing conditions simulating the natural marine environment, the Δ7Licalcite–seawater for Magellania venosa was −2.5‰ and not affected by an increase in temperature from 10 to 16 °C. In contrast, a decrease in Mg/Ca (or Li/Ca) ratio of seawater by addition of CaCl2 as well as elevated pCO2, and hence low-pH conditions, resulted in an increased Δ7Licalcite-seawater up to −4.6‰. Collectively, our results indicate that brachiopods represent valuable archives and provide an envelope for robust Li-based reconstruction of seawater evolution over the Phanerozoic.
    Keywords: Alkalinity, total; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate; Bicarbonate ion; Biomass/Abundance/Elemental composition; Brachiopoda; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Comau_Fjord; Containers and aquaria (20-1000 L or 〈 1 m**2); EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laboratory experiment; Lithium; Magellania venosa; OA-ICC; Ocean Acidification International Coordination Centre; Other studied parameter or process; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Registration number of species; Salinity; Sample ID; Single species; South Pacific; Species; Temperate; Temperature, water; Type; Uniform resource locator/link to reference; δ7Li; δ7Li, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 699 data points
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  • 4
    Publication Date: 2021-03-29
    Description: Chemical fingerprints of impacts are usually compromised by extreme conditions in the impact plume, and the contribution of projectile matter to impactites does not often exceed a fraction of per cent. Here we use chromium and oxygen isotopes to identify the impactor and impact-plume processes for Zhamanshin astrobleme, Kazakhstan. ε54Cr values up to 1.54 in irghizites, part of the fallback ejecta, represent the 54Cr-rich extremity of the Solar System range and suggest a CI-like chondrite impactor. Δ17O values as low as -0.22‰ in irghizites, however, are incompatible with a CI-like impactor. We suggest that the observed 17O depletion in irghizites relative to the terrestrial range is caused by partial isotope exchange with atmospheric oxygen (Δ17O = -0.47‰) following material ejection. In contrast, combined Δ17O-ε54Cr data for central European tektites (distal ejecta) fall into the terrestrial range and neither impactor fingerprint nor oxygen isotope exchange with the atmosphere are indicated.Identifying the original impactor from craters remains challenging. Here, the authors use chromium and oxygen isotopes to indicate that the Zhamanshin astrobleme impactor was a carbonaceous chrondrite by demonstrating that depleted 17O values are due to exchange with atmospheric oxygen.
    Keywords: carbonaceous chondrite; post-impact exchange; ejecta; Earth’s atmosphere ; 551
    Type: article
    Format: 8
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  • 5
    Publication Date: 2022-05-26
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Mayfield, K. K., Eisenhauer, A., Santiago Ramos, D. P., Higgins, J. A., Horner, T. J., Auro, M., Magna, T., Moosdorf, N., Charette, M. A., Gonneea, M. E., Brady, C. E., Komar, N., Peucker-Ehrenbrink, B., & Paytan, A. Groundwater discharge impacts marine isotope budgets of Li, Mg, Ca, Sr, and Ba. Nature Communications, 12(1), (2021): 148-020-20248-3, doi:10.1038/s41467-020-20248-3.
    Description: Groundwater-derived solute fluxes to the ocean have long been assumed static and subordinate to riverine fluxes, if not neglected entirely, in marine isotope budgets. Here we present concentration and isotope data for Li, Mg, Ca, Sr, and Ba in coastal groundwaters to constrain the importance of groundwater discharge in mediating the magnitude and isotopic composition of terrestrially derived solute fluxes to the ocean. Data were extrapolated globally using three independent volumetric estimates of groundwater discharge to coastal waters, from which we estimate that groundwater-derived solute fluxes represent, at a minimum, 5% of riverine fluxes for Li, Mg, Ca, Sr, and Ba. The isotopic compositions of the groundwater-derived Mg, Ca, and Sr fluxes are distinct from global riverine averages, while Li and Ba fluxes are isotopically indistinguishable from rivers. These differences reflect a strong dependence on coastal lithology that should be considered a priority for parameterization in Earth-system models.
    Description: We thank A. Beck, H. Dulai, I. Santos, C. Benitez-Nelson, W. Moore, A. Martin, and H. Windom for sample access. We also thank A. Kolevica, A. Heuser, H. Pryer, J. Middleton, R. Franks, F. Lon, N. Slater, and O. Šebek for their laboratory and analytical assistance. This material is based upon research supported by the National Science Foundation Graduate Research Fellowship Program and an internship provided through the U.S. Geological Survey Graduate Research Internship Program (GRIP). This research was also supported by grants from: the German Academic Exchange Service (DAAD), Northern California chapter of the Achievement Rewards for College Scientists Foundation, International Association of GeoChemistry, Geological Society of America, Northern California Geological Society, Myers Trust, Friends of Long Marine Lab, and UC MEXUS (to K.K.M.). We acknowledge funding from EU-ITN Horizon project 643084 (to A.E. and T.M.) and NSF grant Award Number 1259440 (to A.P.). We also acknowledge funding from NSF grant award number OCE-1736949 (to T.J.H.). Any use of trade, firm or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 6
    Publication Date: 2022-10-26
    Description: © The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nielsen, S. G., Bekaert, D., V., Magna, T., Mezger, K., & Auro, M. The vanadium isotope composition of Mars: Implications for planetary differentiation in the early solar system. Geochemical Perspectives Letters, 15, (2020): 35-39, doi:10.7185/geochemlet.2032.
    Description: The V isotope composition of martian meteorites reveals that Bulk Silicate Mars (BSM) is characterised by δ51V = −1.026 ± 0.029 ‰ (2 s.e.) and is thus ∼0.06 ‰ heavier than chondrites and ∼0.17 ‰ lighter than Bulk Silicate Earth (BSE). Based on the invariant V isotope compositions of all chondrite groups, the heavier V isotope compositions of BSE and BSM relative to chondrites are unlikely to originate from mass independent isotope effects or evaporation/condensation processes in the early Solar System. These differences are best accounted for by mass dependent fractionation during core formation. Assuming that bulk Earth and Mars both have a chondritic V isotopic compostion, mass balance considerations reveal V isotope fractionation factors Δ51Vcore-mantle as substantial as −0.6 ‰ for both planets. This suggests that V isotope systematics in terrestrial and extraterrestrial rocks potentially constitutes a powerful new tracer of planetary differentiation processes accross the Solar System.
    Description: This work was funded by NASA Emerging Worlds grant NNX16AD36G to SGN. Samples were acquired with funds from the Helmholtz Association through the research alliance HA 203 “Planetary Evolution and Life” to KM. TM contributed through the Strategic Research Plan of the Czech Geological Survey (DKRVO/ČGS 2018-2022). KM acknowledges support through NCCR PlanetS supported by the Swiss National Science Foundation. We thank Jurek Blusztajn for support in the WHOI Plasma Facility.
    Keywords: Planetary differentiation ; Vanadium isotopes ; Mars ; Stable isotope fractionation
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 7
    Publication Date: 2024-02-07
    Description: Lithium has proven a powerful tracer of weathering processes and chemical seawater evolution. Skeletal components of marine calcifying organisms, and in particular brachiopods, present promising archives of Li signatures. However, Li incorporation mechanisms and potential influence from biological processes or environmental conditions require a careful assessment. In order to constrain Li systematics in brachiopod shells, we present Li concentrations and isotope compositions for 11 calcitic brachiopod species collected from six different geographic regions, paralleled with data from culturing experiments where brachiopods were grown under varying environmental conditions and seawater chemistry (pH–pCO2, temperature, Mg/Ca ratio). The recent brachiopod specimens collected across different temperate and polar environments showed broadly consistent δ7Li values ranging from 25.2 to 28.1‰ (with mean δ7Li of 26.9 ± 1.5‰), irrespective of taxonomic rank, indicating that incorporation of Li isotopes into brachiopod shells is not strongly affected by vital effects related to differences among species. This results in Δ7Licalcite–seawater values (per mil difference in 7Li/6Li between brachiopod calcite shell and seawater) from −2.9‰ to −5.8‰ (with mean Δ7Licalcite–seawater value of −3.6‰), which is larger than the Δ7Licalcite–seawater values calculated based on data from planktonic foraminifera (~0‰ to ~−4‰). This range of values is further supported by results from brachiopods cultured experimentally. Under controlled culturing conditions simulating the natural marine environment, the Δ7Licalcite–seawater for Magellania venosa was −2.5‰ and not affected by an increase in temperature from 10 to 16 °C. In contrast, a decrease in Mg/Ca (or Li/Ca) ratio of seawater by addition of CaCl2 as well as elevated pCO2, and hence low-pH conditions, resulted in an increased Δ7Licalcite-seawater up to −4.6‰. Collectively, our results indicate that brachiopods represent valuable archives and provide an envelope for robust Li-based reconstruction of seawater evolution over the Phanerozoic.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 8
    Publication Date: 2024-02-07
    Description: Groundwater-derived solute fluxes to the ocean have long been assumed static and subordinate to riverine fluxes, if not neglected entirely, in marine isotope budgets. Here we present concentration and isotope data for Li, Mg, Ca, Sr, and Ba in coastal groundwaters to constrain the importance of groundwater discharge in mediating the magnitude and isotopic composition of terrestrially derived solute fluxes to the ocean. Data were extrapolated globally using three independent volumetric estimates of groundwater discharge to coastal waters, from which we estimate that groundwater-derived solute fluxes represent, at a minimum, 5% of riverine fluxes for Li, Mg, Ca, Sr, and Ba. The isotopic compositions of the groundwater-derived Mg, Ca, and Sr fluxes are distinct from global riverine averages, while Li and Ba fluxes are isotopically indistinguishable from rivers. These differences reflect a strong dependence on coastal lithology that should be considered a priority for parameterization in Earth-system models.
    Type: Article , PeerReviewed
    Format: text
    Format: text
    Format: text
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