Oxidation State, Coordination, and Covalency Controls on Iron Isotopic Fractionation in Earth's Mantle and Crust

Author(s):  
Marc Blanchard ◽  
Nicolas Dauphas
2017 ◽  
pp. 24-28 ◽  
Author(s):  
N. Badullovich ◽  
F. Moynier ◽  
J. Creech ◽  
F.-Z. Teng ◽  
P.A. Sossi

Geology ◽  
2021 ◽  
Author(s):  
Michelle J. Muth ◽  
Paul J. Wallace

Whether and how subduction increases the oxidation state of Earth’s mantle are two of the most important unresolved questions in solid Earth geochemistry. Using data from the southern Cascade arc (California, USA), we show quantitatively for the first time that increases in arc magma oxidation state are fundamentally linked to mass transfer of isotopically heavy sulfate from the subducted plate into the mantle wedge. We investigate multiple hypotheses related to plate dehydration and melting and the rise and reaction of slab melts with mantle peridotite in the wedge, focusing on electron balance between redox-sensitive iron and sulfur during these processes. These results show that unless slab-derived silicic melts contain much higher dissolved sulfur than is indicated by currently available experimental data, arc magma generation by mantle wedge melting must involve multiple stages of mantle metasomatism by slab-derived oxidized and sulfur-bearing hydrous components.


2016 ◽  
Vol 177 ◽  
pp. 298-314 ◽  
Author(s):  
Rémi Belissont ◽  
Manuel Muñoz ◽  
Marie-Christine Boiron ◽  
Béatrice Luais ◽  
Olivier Mathon

Science ◽  
2019 ◽  
Vol 365 (6456) ◽  
pp. 903-906 ◽  
Author(s):  
Katherine Armstrong ◽  
Daniel J. Frost ◽  
Catherine A. McCammon ◽  
David C. Rubie ◽  
Tiziana Boffa Ballaran

The composition of Earth’s atmosphere depends on the redox state of the mantle, which became more oxidizing at some stage after Earth’s core started to form. Through high-pressure experiments, we found that Fe2+ in a deep magma ocean would disproportionate to Fe3+ plus metallic iron at high pressures. The separation of this metallic iron to the core raised the oxidation state of the upper mantle, changing the chemistry of degassing volatiles that formed the atmosphere to more oxidized species. Additionally, the resulting gradient in redox state of the magma ocean allowed dissolved CO2 from the atmosphere to precipitate as diamond at depth. This explains Earth’s carbon-rich interior and suggests that redox evolution during accretion was an important variable in determining the composition of the terrestrial atmosphere.


2016 ◽  
Vol 113 (19) ◽  
pp. 5159-5166 ◽  
Author(s):  
Rong Ye ◽  
Tyler J. Hurlburt ◽  
Kairat Sabyrov ◽  
Selim Alayoglu ◽  
Gabor A. Somorjai

Colloidal chemistry is used to control the size, shape, morphology, and composition of metal nanoparticles. Model catalysts as such are applied to catalytic transformations in the three types of catalysts: heterogeneous, homogeneous, and enzymatic. Real-time dynamics of oxidation state, coordination, and bonding of nanoparticle catalysts are put under the microscope using surface techniques such as sum-frequency generation vibrational spectroscopy and ambient pressure X-ray photoelectron spectroscopy under catalytically relevant conditions. It was demonstrated that catalytic behavior and trends are strongly tied to oxidation state, the coordination number and crystallographic orientation of metal sites, and bonding and orientation of surface adsorbates. It was also found that catalytic performance can be tuned by carefully designing and fabricating catalysts from the bottom up. Homogeneous and heterogeneous catalysts, and likely enzymes, behave similarly at the molecular level. Unifying the fields of catalysis is the key to achieving the goal of 100% selectivity in catalysis.


Nature ◽  
2020 ◽  
Vol 586 (7830) ◽  
pp. 506-507
Author(s):  
Laura Cobden
Keyword(s):  

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