Abstract
Magnesite (MgCO3) is an important phase for the carbon cycle in and out of the Earth’s mantle. Its comparably large P-T stability has been inferred for several years based on the absence of its decomposition in experiments. Here we report the first experimental evidence for synthesis of magnesite out of its oxide components (MgO and CO2) at P-T conditions relevant to the Earth’s mantle.
Magnesite formation was observed in situ using synchrotron X-ray diffraction, coupled with laserheated diamond-anvil cells (DACs), at pressures and temperatures of Earth’s mantle. Despite the existence of multiple high-pressure CO2 polymorphs, the magnesite-forming reaction was observed to proceed at pressures ranging from 5 to 40 GPa and temperatures between 1400 and 1800 K. No other pressure-quenchable materials were observed to form via the MgO + CO2 = MgCO3 reaction. This work further strengthens the notion that magnesite may indeed be the primary host phase for oxidized carbon in the deep Earth
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Highlights and Breakthroughs. A step closer to predicting the bonding geometry of crystals
- Minerals in the Human. Body Crystal chemistry of cement-asbestos
- Versatile monazite: Resolving geological records and solving challenges in materials science. Microprobe analysis and dating of monazite from the Potsdam Formation, New York: A progressive record of chemical reaction and fluid interaction
- A study of ruby (corundum) compositions from the Mogok Belt, Myanmar: Searching for chemical fingerprints
- The dehydroxylation of chrysotile: A combined in situ micro-Raman and micro-FTIR study
- Synchrotron Mössbauer study of Fe-bearing pyrope at high pressures and temperatures
- In situ Raman spectroscopic study of transient polyhedral distortions during cesium ion exchange into sitinakite
- A micro-reflectance IR spectroscopy method for analyzing volatile species in basaltic, andesitic, phonolitic, and rhyolitic glasses
- Fundamental Mössbauer parameters of synthetic Ca-Mg-Fe pyroxenes
- Iron oxidation state in phyllosilicate single crystals using Fe-K pre-edge and XANES spectroscopy: Effects of the linear polarization of the synchrotron X-ray beam
- Effect of particle size on phase transitions in metastable alumina nanoparticles: A view from high-resolution solid-state 27Al NMR study
- Magnesite formation from MgO and CO2 at the pressures and temperatures of Earth’s mantle
- Investigation of the hydrozincite structure by infrared and solid-state NMR spectroscopy
- Local structure in C2/c clinopyroxenes on the hedenbergite (CaFeSi2O6)-ferrosilite (Fe2Si2O6) join: A new interpretation for the Mössbauer spectra of Ca-rich C2/c clinopyroxenes and implications for pyroxene exsolution
- On the effect of carbonate on barite growth at elevated temperatures
- The structure of (Ca,Co)CoSi2O6 pyroxenes and the Ca-M2+ substitution in (Ca,M2+)M2+Si2O6 pyroxenes (M2+ = Co, Fe, Mg)
- Structure of mixed-layer corrensite-chlorite revealed by high-resolution transmission electron microcopy (HRTEM)
- In situ dehydration behavior of veszelyite (Cu,Zn)2Zn(PO4)(OH)3-2H2O: A single-crystal X-ray study
- Ab-initio determination of high-pressure and high-temperature thermoelastic and thermodynamic properties of low-spin (Mg1–xFex)O ferropericlase with x in the range [0.06, 0.59]
- The composite modulated structure of cupropearceite and cupropolybasite and its behavior toward low temperature
- Oxidation in CSPV experiments involving H2O-bearing mafic magmas: Quantification and mitigation
- Coexisting hydroxyl groups and H2O molecules in minerals: A single-crystal neutron diffraction study of eosphorite, MnAlPO4(OH)2·H2O
- Rapidcreekite in the sulfuric acid weathering environment of Diana Cave, Romania
- Terrywallaceite, AgPb(Sb,Bi)3S6, isotypic with gustavite, a new mineral from Mina Herminia, Julcani Mining District, Huancavelica, Peru
- Lead-tellurium oxysalts from Otto Mountain near Baker, California: X. Bairdite, Pb2Cu42+Te26+O10(OH)2(SO4)(H2O), a new mineral with thick HCP layers
- Lusernaite-(Y), Y4Al(CO3)2(OH,F)11·6H2O, a new mineral species from Luserna Valley, Piedmont, Italy: Description and crystal structure
- Fe-rich and As-bearing vesuvianite and wiluite from Kozlov, Czech Republic
- WinPyrox: A Windows program for pyroxene calculation classification and thermobarometry
- Further work on experimental plagioclase equilibria and the Skaergaard liquidus temperature
- Leter. Discovery of dmisteinbergite (hexagonal CaAl2Si2O8) in the Allende meteorite: A new member of refractory silicates formed in the solar nebula