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Mejía Luz María
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(2018)
Unraveling the Potential for Sea Surface Temperature Reconstructions Using Coccolith Clumped Isotope
Mejía LM, Fernández Á, Guitián J, Zhang H, Bernasconi S & Stoll H
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(2017)
Modelling the Mechanisms Controlling d88/86Sr Variations in Coccolithophores
Mejía LM, Paytan A, Eisenhauer A, Böhm F, Kolevica A, Bolton C, Méndez-Vicente A, Abrevaya L, Isensee K & Stoll H
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(2017)
Phytoplankton CO2 Estimates and the Carbon Concentrating Mechanism over Quaternary Glacial Cycles
Stoll H, Hermandez-Almeida I, Guitian J, Mejia LM, Phelps S & Polissar P
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(2014)
δ13C of Opal-Bound Organic Matter and Opal B Content in Fossil Diatoms of Different Sizes and Geometries
Mejía LM, Abrevaya L, Méndez-Vicente A, Bolton C & Stoll H
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(2013)
B Content and δ11B from Cultured Diatoms (Thalassiosira weissflogii & T. pseudonana): Relationship to pH<sub>seawater</sub> And Diatom C Acquisition
Mejía LM, Fietzke J, Isensee K, Méndez-Vicente A, Pisonero J, Shimizu N, González C, Monteleone B & Stoll H
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Mejia Luz Maria
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(2019)
The Impact of Growth Rate and pCO2 on Coccolithophore Carbon Isotopes in the Past: Do Model Results fit with Ocean Proxies Records?
Zhang H, Stoll H, Hokinson B, Jenny D, Mejia LM & Liu C
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(2016)
New Perspectives on the Evolution of CO2 in the Late Cenozoic
Stoll H, Mejia LM, Bolton C, Guitian J, Hernandez Sanchez MT, Abrevaya L, Mendez-Vicente A & Gonzalez-Lemos S
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(2015)
Optimizing pCO2 Reconstructions from Marine Phytoplankton
Stoll H, Bolton C, Hernandez Sanches MT, Mejia LM, Mendez-Vicente A, Abrevaya L & Anderson R
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(2015)
Constraining the Mechanisms Driving δ44/40Ca Variations in Coccolithophores: A Mixed Culture and Fossil Study Approach
Mejía LM, Paytan A, Eisenhauer A, Kolevica A, Abrevaya L, Bolton C, Méndez-Vicente A, Isensee K, González-Lemos S & Stoll H
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Mejía Ramírez Luz
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(2018)
Coccolith Based Clumped Isotope Sea Surface Temperatures during the Cretaceous Thermal Maximum
Fernandez A, Mejía Ramírez L, Guitian Bermejo J, Zhang H, Stoll H & Bernasconi S
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Mejía Ramírez Luz María
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(2019)
Calcification Temperature of Surface Oceans: A Coccolith Clumped Isotope Approach
Mejía Ramírez LM, Fernández A, Zhang H, Guitián J, Pérez-Huerta A, Bernasconi S & Stoll H
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Mejia Ramirez Luz Maria
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(2023)
Clumped Isotopes Applied to Coccolith Calcite: A New Way of Reconstructing Temperatures from Euphotic Oceans
Mejia Ramirez LM, Stoll H, Bernasconi SM, Fernandez A, Zhang H, Guitián J, Sadatzki H, Hernández-Almeida I & Pälike H
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Mejia-Ramirez L.M.
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(2014)
Threshold Adaptations of Marine Algae to CO2 in the Late Cenozoic
Stoll H, Bolton C, Mejia-Ramirez LM, Mendez-Vicente A, Hernandez-Sanchez MT & Abrevaya L
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(2012)
Biomineralization in Diatoms and Coccoliths Recording Carbon Acquisition Strategies
Bolton C, Isensee K, Mejia-Ramirez LM, Mendez-Vicente A, Pisonero J, Shimizu N & Stoll H
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Mejías M.
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(2007)
Radium Isotopes as Tracers of Submarine Groundwater and Nitrogen Discharge in a Karstic Area
Garcia-Solsona E, Garcia-Orellana J, Masqué P, Mejías M & Ballesteros B
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Mejias O.
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(2023)
Exploration for Critical Metals in Australia’s Mine Waste to Support the Energy Transition
Parbhakar-Fox A, Jackson LM, Bhowany K, Guerin K, Han Z, Blannin R, Moyo A, Nicholls L & Mejias O
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Mejorada A.
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(2003)
Isotope Signatures of Microbial Processes in Sulfidic Hot Springs
Abrajano T, Manson R, Mejorada A & Yan B
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Meka S.
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(2020)
Planetary Geochronology Using Machine Learning
Benedix G, Lagain A, Chai K, Meka S, Servis K, Bland P, Norman C, Towner M, Sansom E & Anderson S
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Mekala R.M.
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(2016)
Diversity in the Granites of Nalgonda Region of EDC: Evidence for the Neoarchean Crustal Growth Processes
Shukla S & Mekala RM
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(2008)
Origin of High µ Isotope Signature in Late Archean Granitoids
Ulrich T, Kamber B, Mekala RM & Whitehouse M
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(2005)
Geochemistry of High Fe- Tholeiites from the Ramagiri-Hungund Greenstone Belt of Eastern Dharwar Craton, India
Mekala RM, Drona SS & Thota GR
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Mekhonoshin A.
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(2010)
Traces of Melting in Mantle Spinel Peridotite Xenolith from Khorog Volcano (Northern Mongolia)
Mekhonoshin A, Kolotitlina T & Pavlova L
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(2008)
Thermochronologic “Hearing” of the Roots of Caledonian Mountains of the Central Asian Fold Belt: Are They Parts of a Single Orogen?
Travin A, Yudin D, Vladimirov A, Volkova N, Khromykh S, Mekhonoshin A & Kolotilina T
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(2005)
TECTONOTHERMAL EVOLUTION OF OLKHONSKAYA COLLISION SYSTEM: CONSTRAINTS FROM <+>40<$>Ar/<+>39<$>Ar DATA ON GRANITE VEINS SEALED INSIDE ULTRAMAFIC BODIES
Yudin D, Travin A, Khromyh S, Vladimirov A, Mekhonoshin A & Volkova N
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Meki M.
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(2020)
Carbon Flow Through Energycane Agroecosystems Established Post-Intensive Agriculture
Crow S, Wells J, Sierra C, Youkhana A, Ogoshi R, Richardson D, Glazer C, Meki M & Kiniry J
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Mekic M.
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(2019)
Stable Carbon Isotope Fractionation during Photodegradation of Triclosan in the Aqueous Phase
Jin B, Liu Y, Mekic M, Carena L, Vione D, Gligorovski S & Zhang G
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Mekik F.
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(2008)
In Search of the Deglacial Carbonate Preservation Maximum: Why is it Missing?
Mekik F, Anderson R & Ridgwell A
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Mel M.
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(2022)
In-Tandem Microcalorimetry-2D Perturbation Correlation Spectroscopy for Resolving Catalytic and non-CAtalytic Reactions at the Oxide-Water Interface
Manzie A, Mel M & Harvey OR
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Mel'gunov M.
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(2002)
REE Geochemistry of the Fluorite from Yucca Mountain, USA: Fingerprinting Multiple Sources of Matter in Hydrothermal Fluids
Smirnov S, Dublyansky Y, Mel'gunov M & Mel'gunova E
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Mel'gunova E.
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(2002)
REE Geochemistry of the Fluorite from Yucca Mountain, USA: Fingerprinting Multiple Sources of Matter in Hydrothermal Fluids
Smirnov S, Dublyansky Y, Mel'gunov M & Mel'gunova E
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Melacci P.
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(2004)
MARSIS: Subsurface Sounding Performances
Picardi G, Cartacci M, Masdea A, Seu R & Melacci P
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Melai C.
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(2022)
The Ferric Iron Contents of Lower Mantle Minerals and their Use in the Determination of Deep Diamond Formation Conditions
Frost D, Melai C, McCammon C, Boffa Ballaran T, Miyajima N & Huang R
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(2021)
The Oxygen Fugacity of Sublithospheric Diamond Formation and the Conditions Encountered during their Ascent to the Surface
Melai C, Frost D, Boffa Ballaran T & McCammon C
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(2020)
Nitrogen Contents and Nitrogen Isotope Fractionation in Subduction Zones
Melai C, Frost D, Furukawa Y, Ishida A & Suzuki A
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(2020)
The Redox State of Subduction Zones and the Implications for the Speciation of Volatiles
Frost D, Eberhard L, Melai C, Boffa Ballaran T & McCammon C
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Melankholina E.
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(2019)
Geochemical Evolution
of the Jurassic Plume
Magmatism in The
e. Antarctica
Sushchevskaya N, Belyatsky B, Sobolev A, Letchenkov G & Melankholina E
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Melánová K.
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(2016)
Molecular Simulations of Layered Materials Intercalated with Organic Species
Psenicka M, Pospíšil M & Melánová K
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Melby K.
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(2022)
Fayda: A Data Processing, Visualization, and Predictive Platform for Atomic ICP-MS/MS
Richardson R, French AD, Melby K, Arnquist I & Harouaka K
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(2022)
Characterization of Gas Phase Atomic Cation Reactivity with Selected Reagent Gases in Collision Cell ICP-MS/MS Analyses
Melby K, French AD, Eiden G, Hoppe E, Arnquist I & Harouaka K
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(2021)
Reaction Roulette: Utilizing Elemental MS/MS for the Characterization of Gas Phase Ion-Molecule Interactions
Harouaka K, Allen C, Melby K, Bylaska E, Eiden G, Cox R, di Vacri ML, Hoppe E & Arnquist I
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Melchakova L.
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(2010)
Allophane and Palagonite as the Product of Volcanic Glass Alteration of Different Ages
Kuznetsova E, Motenko R, Vigasina M & Melchakova L
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Melcher Frank
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(2013)
Analysis of Fluid Inclusions with fs-LA-ICP-MS
Albrecht M, Derrey IT, Horn I, Schuth S, Melcher F & Weyer S
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(2012)
Development of (U-Th)/He Geochronology of Columbite Ores
Dunkl I, Melcher F, Henjes-Kunst F & von Eynatten H
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(2007)
Driekop Platinum Pipe, Bushveld Complex, South Africa: New Insights
Oberthür T, Rudashevsky NS, Rudashevsky VN, Cabri L, Melcher F, Kocks H, Lodziak J & Klosa D
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(2007)
"Blood Coltan": Fingerprinting of Columbite-Tantalite Ores
Sitnikova M, Melcher F, Oberthür T, Henjes-Kunst F, Gerdes A, Brätz H & Davis D
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(2005)
Characterising and U-Series Dating (TIMS) of Travertine from Hungary
Sierralta M, Melcher F & Frechen M
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(2004)
Detailed EDXRF Mapping of Pt-Ore – A Fast and Cheap Analytical Tool
Rammlmair D, Wittenberg A, Melcher F, Lodziak J & Merkle R
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