Geochimica et Cosmochimica Acta

Papers
(The TQCC of Geochimica et Cosmochimica Acta is 12. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-12-01 to 2025-12-01.)
ArticleCitations
Re-evaluating the diffusivity of phosphorus in olivine: Implications of low diffusive mobility for thermochronology117
Anomalous 234U/238U isotopic composition in Southern Ocean sediments111
The multicomponent exchange of metals between magmatic fluids and silicate melts94
Citation for the 2022 Science Innovation Award to Lenny Winkel81
An internal energy-dependent model for the Grüneisen parameter of silicate liquids73
Impacts of sulfonic acids on fungal manganese oxide production72
Origin of moderately volatile element depletion on differentiated bodies: Insights from the evaporation of indium from silicate melts67
Path-integral molecular dynamics predictions of equilibrium H and O isotope fractionations between brucite and water66
Zircons underestimate mantle depletion of early Earth65
Abiotic iron oxidation controlled the deposition of Neoproterozoic iron formations63
Geochemical characterization of scoriaceous and unmelted micrometeorites from the Sør Rondane Mountains, East Antarctica: Links to chondritic parent bodies and the effects of alteration62
Helium isotope evidence for mixing of mantle-derived fluids and deeply penetrating surface waters in an obducted peridotite massif62
Iron isotope fractionation in magnetite produced by the marine magnetotactic bacterium Magnetovibrio blakemorei59
Near-congruent Li isotope signature from weathering and erosion of a tectonically active mountain range56
Helium, neon and argon in alkaline basalt-related corundum megacrysts: Implications for their origin and forming process52
Foraminiferal denitrification and deep bioirrigation influence benthic biogeochemical cycling in a seasonally hypoxic fjord50
Experiments revealing the formation of refractory methylmercury pools in natural sediments and soils50
Temporal relationships among lunar crustal rocks49
Petrology and Geochemistry of Poikilitic Shergottite Northwest Africa 1950: bridging the gap between depleted and intermediate sources in Martian Mantle49
Experimental constraints on Mg isotope fractionation during the aragonite–calcite transition and implications for seawater δ26Mg reconstruction49
Exploring the affinity and selectivity of sedimentary mackinawite (FeS) towards natural organic matter48
Chromium stable isotope distributions in the southwest Pacific Ocean and constraints on hydrothermal input from the Kermadec Arc48
Beyond anoxia: Exploring sedimentary thallium isotopes in paleo-redox reconstructions from a new core top collection48
Boron in wildfires: New insights into boron isotope fractionation during volatilisation, leaching and adsorption after combustion48
Phytase-mediated hydrolysis of different soil phytate species: Kinetics and mineral interfacial mechanisms46
Manganese oxidation states and availability in forest weathering profiles of contrasting climate45
Iron biogeochemistry in sediments on the western continental shelf of the Antarctic Peninsula45
Nanoscale mechanisms of carboxyl carbon preservation during Fe(II)-induced ferrihydrite transformation45
Soil iGDGTs temperature dependence: From the Tibetan Plateau to the global scale and its implications for the Holocene temperature conundrum45
The geochemical evolution of basalt Enhanced Rock Weathering systems quantified from a natural analogue44
Using 224Ra/228Th disequilibrium to quantify carbon transformation and export from intertidal sandy and muddy sediments44
Juvenile continental crust evolution in a modern oceanic arc setting: Petrogenesis of Cenozoic felsic plutons in Fiji, SW Pacific42
The overlooked role of denitrifying bacteria in mediating vanadate reduction42
A non-classical crystallization mechanism of microbially-induced disordered dolomite42
Experimental chondrite–water reactions under reducing and low-temperature hydrothermal conditions: Implications for incipient aqueous alteration in planetesimals41
Widespread lithogenic control of marine authigenic neodymium isotope records? Implications for paleoceanographic reconstructions41
Citation for the 2023 Alfred E. Treibs award to Shucheng Xie39
Survivability and pathways of amino acids in oceanic hydrothermal systems: A mechanistic study of phenylalanine39
Geochemical evolution of a sublacustrine hydrothermal vent system: Temporal constraints imposed by reactive transport modeling39
Archaeal tetraether lipids and their biphytane carbon isotope composition in sediments along an estuarine biogeochemical gradient38
Acceptance of the 2022 Clair C. Patterson Medal to Xiangdong Li38
Sequestration of carbon in the forearc mantle wedge37
Acceptance of the 2022 F.W. Clarke Award to Yige Zhang37
Clumped and conventional isotopes of natural gas reveal basin burial, denudation, and biodegradation history36
Diffusion of H-bearing species in anorthite-diopside glass below and across the glass transition36
Age, genetics, and crystallization sequence of the group IIIE iron meteorites36
Uniform initial 10Be/9Be inferred from refractory inclusions in CV3, CO3, CR2, and CH/CB chondrites35
Molybdenum isotopes record dehydrated slab components input to arc magmatism in subduction zones35
Combined Ca, Sr isotope and trace element analyses of Late Cretaceous dinosaur teeth: assessing diet versus diagenesis35
Activity model for 36 elements in Fe-Ni-Si-S-C liquids with application to terrestrial planet accretion and mantle geochemistry: New data for Ru, Re, Pt, Os, Ti, Nb, and Ta35
Hydrothermal mobilization and molecular transformations of dissolved organic matter from deep subsurface sediments35
The importance of carbon to the formation and composition of silicates during mantle metasomatism34
Evaporation kinetics of silicon carbide in a low-pressure H2-H2O gas mixture: Implications for the survivability of presolar silicon carbide grains in the protosolar disk34
Distinct dynamics of plant- and microbial-derived soil organic matter in relation to varying climate and soil properties in temperate agroecosystems34
Potassium isotopic equilibrium fractionation induced by clay adsorption and incorporation: A density functional theory study34
Near-equilibrium kinetics in the Fe(II)-silicate system and the significance of nanoparticle greenalite in Archaean Iron Formations34
Surface energetics of wurtzite and sphalerite polymorphs of zinc sulfide and implications for their formation in nature34
Fluid systems captured by giant amethyst-hosted fluid inclusions from continental flood basalts34
Anaerobic oxidation of methane from abandoned oil and gas wells leaking into aquifers33
Fe-Mg in olivine: simultaneous experimental determination of the diffusion-driven isotope fractionation along with tracer- and inter-diffusion coefficients33
Substrate chemistry trumps mineral protection in governing temperature sensitivity of organic carbon mineralization in saline lake sediments33
The oxygen fugacity of intermediate shergottite NWA 11043: implications for Martian mantle evolution33
Schreibersite oxidation under varied oxygen buffers33
Copper mobilization in the lower continental crust beneath cratonic margins, a Cu isotope perspective32
Constraining the mass-dependent Ti isotope composition of the chondritic reservoir – An inter-laboratory comparison study32
Surface ocean biogeochemistry and deep ocean circulation control relationships between nutrient-type trace metals (Cd, Ni, Cu, and Zn) and nutrients in the South Atlantic Ocean near the subtropical fr32
Position-specific carbon isotopes of Murchison amino acids elucidate extraterrestrial abiotic organic synthesis networks32
Kinetic zinc isotope fractionation in olivine phenocrysts records magma evolution history of intra-plate basalts32
Thermodynamic constants of formation of disulfide anion in aqueous solutions32
Whole-rock Mg isotopes distinguishing high- and low-temperature S-type granites31
Deep carbon recycling via the Tianshan basalt province and its contribution to Cenozoic elevated atmospheric CO2 concentration31
Effects of sulfate reduction processes on the trace element geochemistry of sedimentary pyrite in modern seep environments31
Size-dependent dynamics of the internal carbon pool drive isotopic vital effects in calcifying phytoplankton31
Influence of structural Fe content in clay minerals on selenite redox reactions: Kinetics and structural transformations31
Noble gas (He, Ne, and Ar) solubilities in high-pressure silicate melts calculated based on deep-potential modeling31
High manganese redox variability and manganate predominance in temperate soil profiles as determined by X-ray absorption spectroscopy30
Light stable Cr isotope compositions of mid-ocean ridge basalts: Implications for mantle source composition30
Processes controlling nickel and its isotopes in anoxic sediments of a seasonally hypoxic bay30
Isotopic and trace element data of Tissint indicate a homogeneous strewn field, mobilization of Sr, REE, and Pb during shock metamorphism, and limits on the incorporation of martian surficial material30
Average major element composition of the upper continental crust derived from an integrated study of sedimentary and igneous rocks30
Geochemistry of impact glasses in the Chang’e-5 regolith: Constraints on impact melting and the petrogenesis of local basalt30
Nature of slab-mantle interactions recorded by coupled δ13C–δ15N–δ18O signatures and elemental compositions of Koidu diamonds and their inclusions30
Persistent organic alkalinity in the ocean29
Iron biogeochemical redox cycling dominantly controls cadmium availability in acidic paddy soils29
Insights into the response of coral biomineralisation to environmental change from aragonite precipitations in vitro29
No ion is an island: Multiple ions influence boron incorporation into CaCO329
Controls on Li partitioning and isotopic fractionation in inorganic calcite29
Chlorine and NaCl in hydrous basaltic melts28
Accretion of warm chondrules in weakly metamorphosed ordinary chondrites and their subsequent reprocessing28
Biogenic iron minerals as a potential survival mechanism for nitrate-reducing iron-oxidizing bacteria28
Citation for the 2021 H.C. Urey Award to Sachiko Amari28
Dating martian mafic crust; microstructurally constrained baddeleyite geochronology of enriched shergottites Northwest Africa (NWA) 7257, NWA 8679 and Zagami28
Planktic foraminifera record the succession of anaerobic metabolisms in particle microenvironments across a pelagic oxygen gradient28
Symplectite formation in ultramafic achondrites by impact percolation of a sulfide melt28
Corrigendum to “Genetics, age, and crystallization history of group IC iron meteorites” [Geochim. Cosmochim. Acta 340 (2023) 108–119]28
Complex zoning in the nakhlite and chassignite martian meteorites reveals multi-stage petrogenesis and undercooling during crystallization28
Antimony(V) reaction with particulate natural organic matter: Sorption behavior, binding mechanism, and environmental implications28
Diffusion timescale conundrum in contact metamorphism: Oxygen isotope and trace element profiles in dolomite28
Initial 244Pu/238U ratios and search for presolar SiC in Ca-Al-rich inclusions from CV3 chondrites using noble gas and trace element abundances28
Observed seasonal trends of diatom-derived C20 highly branched isoprenoids (HBIs): implications for paleoclimate studies27
The chondritic impactor origin of the Ni-rich component in Australasian tektites and microtektites27
Significant Mg isotope disequilibrium during crustal anatexis: Implications for heterogeneous Mg isotopic compositions in the continental crust27
Thermodynamics of NaCl in dense water vapor via cross virial coefficients27
Tourmaline composition probes serpentinite-derived fluid mobility in subduction zones27
The Re/Mo redox proxy reconsidered27
Hf–W isotope systematics of bulk chondrites: Implications for early Solar System evolution27
Indigenous carbon-rich matter associated with unusual aqueous alteration features in Nakhla: Complex formation and preservation history27
Climate warming and strengthened hydrologic cycle accelerate CO2 release from rock weathering27
Kinetic factors control trace element and isotope zoning in Archean pyrite corona nodules27
Nickel isotopic variations in Ni–Cu sulfide deposits: from theoretical predictions to natural observations27
Three-dimensional observation of GEMS grains: Their high-temperature condensation origin27
Unravelling chondrule formation processes: Clues from the potassium isotopic composition of chondrules from unequilibrated ordinary chondrites26
Chemical weathering signatures at Mt. Achernar, Central Transantarctic Mountains II: Surface exposed sediments26
Inter-method differences (SIMS vs. IRMS) in oxygen isotope fractionation: insights from Chinook salmon otoliths26
Tracing short-lived hydrothermal circulation systems and water–rock interactions around small-scale intrusions26
Continental evaporites as brine sources for formation of SEDEX and MVT deposits: Implications from boron isotope compositions of tourmaline26
Deciphering the origin(s) of H and Cl in Apollo 15 quartz monzodiorites: Evidence for multiple processes and reservoirs26
Contrasting photochemical behaviors between biogenic-sourced and combustion-sourced dissolved organic nitrogen26
Phosphorus hotspots in pedogenic carbonate coatings determined by zoned microscale arrangement and organo-mineral interactions26
An exploration of whether Earth can be built from chondritic components, not bulk chondrites26
Diffusion of halogens (F, Cl, Br, I) in silicic melt26
Sulfur cycling at two Mars-relevant saline lakes underscores the importance of dynamic metabolic substrate concentrations for isotopic biosignatures26
Slab dehydration and potassium-lithium recycling in the forearc indicated by potassium and lithium isotope compositions of exhumed metabasites25
Triple oxygen isotope compositions of globally distributed soil carbonates record widespread evaporation of soil waters25
Nitrogen in the Orgueil meteorite: Abundant ammonium among other reservoirs of variable isotopic compositions25
Corrigendum to “Multiple fluid-rock interactions in the subduction channel evidenced by magnesium isotope”. [Geochim. et Cosmochim. Acta 403 (2025) 67–78]25
Rare earth elements and yttrium in suspension-feeding bivalves (dog cockle, Glycymeris glycymeris L.): Accumulation, vital effects and pollution25
Reading the climate signals hidden in bauxite25
Evaluating isoprenoidal hydroxylated GDGT-based temperature proxies in surface sediments from the global ocean25
Quantitative in situ Raman spectroscopy investigation on HSO4− dissociation at high pressures (up to 420 MPa) and its geological implication25
Effect of sulfate on the kinetic and equilibrium Magnesium isotope fractionation between low Mg-calcite and fluid25
Ferro-chloro-winchite in Northwest Africa (NWA) 998 apatite-hosted melt inclusion: New insights into the nakhlite parent melt25
Pyrrhotites in asteroid 162173 Ryugu: Records of the initial changes on their surfaces with aqueous alteration25
Calcium isotope evidence for the formation of early condensates in the Solar System from unmixed reservoirs with distinct nucleosynthetic origins25
Reduction and transformation of Cr(VI)-associated ferrihydrite by Shewanella oneidensis MR-1: Kinetics and secondary minerals25
Sources and fate of particulate organic matter along the river-estuary-coastal ocean continuum: Constraints from amino acid and amino sugar carbon isotopes24
Origin of the Ca-phosphate inclusions in Ivory Coast and Australasian Muong-Nong-type tektites24
Pulsating dissolution of crystalline matter: A surface-controlled process24
Fluid-mediated Zr transfer in subduction zones: constraints from extreme Zr isotope fractionation in an ultrahigh-pressure eclogite–vein system in the Dabie orogen24
Zinc isotope fractionation during mid-ocean ridge basalt differentiation: Evidence from lavas on the East Pacific Rise at 10°30′N24
Effective reduction of refractory selenate by natural granite and claystone under gamma irradiation24
Effect of temperature on 2H/1H fractionation in semi-continuous cultures of a marine diatom, coccolithophore, and dinoflagellate24
Aggregation reduces the release of bioavailable silicon from allophane and phytolith24
Improved kinetics for mineral dissolution reactions in pore-scale reactive transport modeling24
Impact of aerobic reworking of biomass on steroid and hopanoid biomarker parameters recording ecological conditions and thermal maturity24
Tracing the source and transport of Hg during pedogenesis in strongly weathered tropical soil using Hg isotopes24
Detection of incipient aqueous alteration in carbonaceous chondrites24
Non-alkali metals titrate silica out of carbonatite melts into insoluble silicate minerals24
Accessory minerals constrain anatexis and melt extraction in deep crust and implications for granite genesis24
The absence of an effect of nickel on iron isotope fractionation during core formation23
Impact of CO2 on sulfur concentration at sulfide saturation in silicate melts: implication for deep Earth sulfur cycling23
Geochemical conditions regulating chromium preservation in marine sediments23
Zircon (U-Th)/He impact crater thermochronometry and the effects of shock microstructures on He diffusion kinetics23
Nickel isotope fractionation factors between silicate minerals and melt23
Citation for the 2021 Clair C. Patterson Award to Michael F. Hochella23
Silica polymerization and nanocolloid nucleation and growth kinetics in aqueous solutions23
Calcium isotope fractionation during tropical weathering of granites23
Alteration enrichment of nitrogen in the gabbroic oceanic crust: Implications for global subducting nitrogen budget and subduction-zone nitrogen recycling23
Contemporaneously growing speleothems and their value to decipher in-cave processes – A modelling approach23
Species and biosynthetic effects cause uncorrelated variation in oxygen and hydrogen isotope compositions of plant organic compounds23
Rare earth elements and yttrium (REY) in fjord waters: Comparison between seawater in the Trondheimfjord (Norway), its local riverine REY sources and the North Atlantic23
Layer-to-tunnel manganese oxides transformation triggered by pyrogenic carbon and trace metals: Key role of reducing and oxidizing components cooperation23
Thermodynamics of ultrarefractory condensates: Implications for the high-temperature limit of the inner dust rim of the early solar protoplanetary disk23
High precipitation rates characterize biomineralization in the benthic foraminifer Ammonia beccarii23
Mechanism of arsenic release from realgar oxidation in the presence of dissolved oxygen: Effect of reactive oxygen species and light-induced transformation23
Asteroids accretion, differentiation, and break-up in the Vesta source region: Evidence from cosmochemistry of mesosiderites23
The viscosity of aqueous solutions as analogs to cryovolcanic liquids22
Productivity and organic carbon loading control uranium isotope behavior in ancient reducing settings: Implications for the paleoredox proxy22
Zinc isotopic evidence for enhanced oceanic primary productivity during termination of the late Ediacaran Shuram Excursion22
Time scales and mechanisms of uranium uptake in altered ocean crust; observations from the ∼15 million year-old site 1256 in the eastern equatorial Pacific22
Evolution of rare earth element and εNd compositions of Gulf of Mexico seawater during interaction with Mississippi River sediment22
Chromium isotopes in an acidic fluvial system: Implications for modern and ancient Cr isotope records22
Discrepant mass accumulation rates of sediments in the South Pacific Ocean from 230Th and 3He measurements22
Iodine cycling in the subarctic Pacific Ocean: Insights from 129I22
Decoupling of Fe isotope and Fe3+/ΣFe in arc igneous rocks: Implications for crustal metasomatism and its contribution to mantle redox22
An empirical calibration of the serpentine-water oxygen isotope fractionation at T = 25–100 °C22
Tungsten (VI) speciation in hydrothermal solutions up to 400°C as revealed by in-situ Raman spectroscopy22
The ikaite to calcite transformation: Implications for palaeoclimate studies22
Aluminium substitution affects jarosite transformation to iron oxyhydroxides in the presence of aqueous Fe(II)22
On the provenance of GEMS, a quarter century post discovery22
Coupled reduction of structural Fe(III) in nontronite and oxidation of petroleum hydrocarbons22
Extreme lithium isotope fractionation in quartz from the Stewart pegmatite22
High methylation potential of mercury complexed with mixed thiolate ligands by Geobacter sulfurreducens PCA21
FROG: A global machine-learning temperature calibration for branched GDGTs in soils and peats21
Interactions of manganese oxides with natural dissolved organic matter: Implications for soil organic carbon cycling21
Oxidizing fluids associated with detachment hosted hydrothermal systems: Example from the Suye hydrothermal field on the ultraslow-spreading Southwest Indian Ridge21
Tracing DUPAL anomaly evolution in the Tethyan-Indian oceanic mantle21
Noble gas evolution of the martian atmosphere in the last 4 Gyr recorded by regolith breccia NWA 811421
Iron cycling and isotopic fractionation in a ferruginous, seasonally ice-covered lake21
Speciation and thermodynamic properties of La(III)-Cl complexes in hydrothermal fluids: A combined molecular dynamics and in situ X-ray absorption spectroscopy study21
Magnesium isotopic evidence for staged enhancement of the East Asian Summer Monsoon precipitation since the Miocene21
Micropore sites in ferrihydrite are responsible for its higher affinity towards As(III) relative to As(V)21
Drivers of inorganic and organic carbon removal in aged oceanic crust21
Rates of dehydration in hydrous, high-Fo, magmatic olivines21
Towards building a unified adsorption model for goethite based on direct measurements of crystal face compositions: I. Acidity behavior and As(V) adsorption21
Zn isotopic variations in ore-related granite and ore minerals in a magmatic-hydrothermal deposit21
Uranium-series and strontium isotope systematics in soil carbonates from dryland Critical Zones: Implications for soil inorganic carbon storage and transformation21
Spatial evolution and temporal stability of hydrothermal processes at sediment-covered spreading centers: Constraints from Guaymas Basin, Gulf of California21
The mineralogy and alteration history of the Yamato-type (CY) carbonaceous chondrites21
The role of calcium phosphates and silicates in the storage and transport of phosphorus at the upper-to-lower mantle transition: An experimental study to 25 GPa in a model peridotitic bulk composition21
Age and genetic relationships among CB, CH and CR chondrites21
Evolution of the preserved European continental crust, constrained by U-Pb, O and Hf isotopic analyses of river detrital zircons21
40Ar/39Ar dating of basaltic rocks and the pitfalls of plagioclase alteration21
A process-based geochemical framework for carbonate sediments during marine diagenesis20
Magmatic crystallization drives zircon Zr isotopic variations in a large granite batholith20
An oxygen fugacity-temperature-pressure-composition model for sulfide speciation in Mercurian magmas20
Equilibrium indium isotope fractionation between indium-bearing minerals: Insights from first-principles calculations20
Systematics of helium diffusion sinks in apatite demonstrated by 4He/3He degassing experiments and modeling20
Vivianite oxidation is not photocatalyzed20
Titanium isotope heterogeneity in the Earth’s mantle: A case study of the Horoman peridotite massif20
Marine barite morphology as an indicator of biogeochemical conditions within organic matter aggregates20
Refining the signature of thallium isotopes in low oxygen marine environments20
The partitioning behavior of Mo during magmatic fluid exsolution and its implications for Mo mineralization20
The dynamic influence of subsurface geological processes on the assembly and diversification of thermophilic microbial communities in continental hydrothermal systems20
Zinc isotopic fractionation during magmatic differentiation and hydrothermal processes: implications for Li mineralization in the Jiajika granitic pegmatites, Sichuan, China20
Effects of particle size and AQDS on the flow of electron equivalents between magnetite and aqueous Fe2+20
Site-specific interactions enhanced dissolution of natural aragonite (110) surfaces in succinic acid (SUC) solutions: Implications for the oceanic aragonite dissolution fluxes20
The mechanism and kinetics of the replacement of chalcopyrite by covellite under mild-hydrothermal conditions (120–200 °C)20
Potassium-39-derived 36Ar production during fission-neutron irradiation and its effect on 40Ar/39Ar ages20
Tungsten in the mantle constrained by continental lithospheric peridotites: Less incompatible and more abundant20
High-C content and CO2/Ba ratio of the Earth’s enriched upper mantle20
Extreme Mo isotope variations recorded in high-SiO2 granites: Insights into magmatic differentiation and melt–fluid interaction20
Kinetic constraints for the formation of microniches for microaerophilic Fe(II) oxidation20
Mapping the redox state of the young Solar System using ytterbium valence state20
Experimental metasomatic incorporation of sulfur into fluorapatite as a function of coupled substitutions involving sodium, silicon, iron, and cerium20
The influence of secondary weathering processes on dissolved nickel isotope compositions under cold climatic conditions – Observations from the Mackenzie Basin20
Dissolved organic matter and nutrient processing in organic-rich subterranean estuaries: Implications for future land use and climate scenarios20
Partitioning of noble gases (He, Ne, Ar, Kr, Xe) during Earth’s core segregation: A possible core reservoir for primordial noble gases20
Rhenium-platinum group elements reveal seawater incursion induced massive lacustrine organic carbon burial19
Reactive transport experiments of coupled carbonation and serpentinization in a natural serpentinite. Implication for hydrogen production and carbon geological storage19
Sulfate-driven anaerobic oxidation of methane inferred from trace-element chemistry and nickel isotopes of pyrite19
Triple oxygen isotope variability of precipitation in a tropical mountainous region19
Carbon and hydrogen isotope fractionation during aqueous diffusion of benzene19
Acceptance of the 2022 Science Innovation Award to Lenny Winkel19
53Mn-53Cr chronometry of ureilites: Implications for the timing of parent body accretion, differentiation and secondary reduction19
Iron and silicon isotope fractionation in silicate melts using first-principles molecular dynamics19
Si isotope composition of Earth’s mantle and oceanic basalts19
Uranium(VI) hydrolysis up to 250 °C and its geological implications19
Molecular evidence for the export of terrigenous organic matter to the north Gulf of Mexico by solid-state 13C NMR and Fourier transform ion cyclotron resonance mass spectrometry of humic acids19
Symbiont regulation of nitrogen metabolism and excretion in tropical planktonic foraminifera19
Molybdenum isotopic constraints on the origin of EM1-type continental intraplate basalts19
Partitioning of nickel and cobalt between metal and silicate melts: Expanding the oxy-barometer to reducing conditions19
Germanium speciation in experimental and natural sphalerite: Implications for critical metal enrichment in hydrothermal Zn-Pb ores19
Sedimentary cycling of zinc and nickel and their isotopes on an upwelling margin: Implications for oceanic budgets and paleoenvironment proxies19
Redox heterogeneity of picritic lavas with respect to their mantle sources in the Emeishan large igneous province19
Corrigendum to “Different metal coordination in sub- and super-critical fluids: Do molybdenum(VI) chloride complexes contribute to mass transfer in magmatic systems?” [Geochim. Cosmochim. Acta 354 (2019
Elemental sulfur, hydrogen sulfide, and carbon monoxide-driven dimerization of glycine at sub-millimolar concentrations: Implications for the origin of life19
Assessing the validity and limits of linear density models for predicting dissociation–association equilibria in supercritical water18
Mobilization and fractionation of Ti-Nb-Ta during exhumation of deeply subducted continental crust18
Tracing the provenance of mineral dust over the northern and southern Indian Oceans during the GEOTRACES-India (GI-01, GI-02) expeditions18
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