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Page 1
Destabilization of deep oxidized mantle drove the Great Oxidation Event.
Sci Adv. 2022 Feb 18;8(7):eabg1626. doi: 10.1126/sciadv.abg1626. Epub 2022 Feb 18.
Sci Adv. 2022.
PMID: 35179960
Free PMC article.
Evidence for oxygen-conserving diamond formation in redox-buffered subducted oceanic crust sampled as eclogite.
Aulbach S, Stachel T.
Aulbach S, et al.
Nat Commun. 2022 Apr 8;13(1):1924. doi: 10.1038/s41467-022-29567-z.
Nat Commun. 2022.
PMID: 35396553
Free PMC article.
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Cubic Fe-bearing majorite synthesized at 18-25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation.
Stagno V, Bindi L, Bonechi B, Greaux S, Aulbach S, Irifune T, Lupi S, Marras G, McCammon CA, Nazzari M, Piccirilli F, Poe B, Romano C, Scarlato P.
Stagno V, et al. Among authors: aulbach s.
Sci Rep. 2023 Sep 22;13(1):15855. doi: 10.1038/s41598-023-43037-6.
Sci Rep. 2023.
PMID: 37740075
Free PMC article.
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Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust.
Aulbach S, Woodland AB, Stern RA, Vasilyev P, Heaman LM, Viljoen KS.
Aulbach S, et al.
Sci Rep. 2019 Dec 27;9(1):20190. doi: 10.1038/s41598-019-55743-1.
Sci Rep. 2019.
PMID: 31882582
Free PMC article.
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