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Metal-driven anaerobic oxidation of methane and the Sturtian deglaciation

Metal-driven anaerobic oxidation of methane and methanogenesis, mediated by a diverse microbial community, drove iron-mineral transformation and may have aided ice sheet melting, according to analysis of Sturtian iron formations from South China

Jun Hu
Sanzhong Li
Kurt O. Konhauser
ResearchOpen Access06 Aug 2025
Nature Communications

Volume: 16, P: 1-14
A HIMU-like component in Mariana Convergent Margin magma sources during initial arc rifting revealed by melt inclusions

HIMU-type seamounts may be subducted elsewhere beneath the Mariana arc, but obvious HIMU-type components appear only in the initial stages of arc rifting due to the low melting degree and being consumed during the process of back-arc spreading.

Xiaohui Li
Osamu Ishizuka
Hongxia Yu
ResearchOpen Access14 May 2024
Nature Communications

Volume: 15, P: 1-11
Assimilation of upper plate rocks at convergent margins contributes to the low δ¹⁸O isotopic signature of erupted magma

Fractionated magma in volcanic arcs assimilate upper plate hydrothermal altered oceanic crust wall rock with low oxygen isotopic signature, which contribute to the isotopic signature of erupted magma, according to geochemical and oxygen isotope data of olivine in basalt formed at the Mariana convergent margin.

Xiaohui Li
Zixuan Zhang
Qiuli Li
ResearchOpen Access02 Jul 2025
Communications Earth & Environment

Volume: 6, P: 1-9
Crystal structure and catalytic mechanism of the MbnBC holoenzyme required for methanobactin biosynthesis

Chao Dou
Zhaolin Long
Wei Cheng
ResearchOpen Access02 Feb 2022
Cell Research

Volume: 32, P: 302-314
Comparison of arterial stiffness indices measured by pulse wave velocity and pulse wave analysis for predicting cardiovascular and all-cause mortality in a Chinese population

Xin Yue
Lu Chen
Haifeng Zhang
Research09 Jan 2024
Hypertension Research

Volume: 47, P: 767-777

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Metal-driven anaerobic oxidation of methane and the Sturtian deglaciation

A HIMU-like component in Mariana Convergent Margin magma sources during initial arc rifting revealed by melt inclusions

Assimilation of upper plate rocks at convergent margins contributes to the low δ18O isotopic signature of erupted magma

Crystal structure and catalytic mechanism of the MbnBC holoenzyme required for methanobactin biosynthesis

Comparison of arterial stiffness indices measured by pulse wave velocity and pulse wave analysis for predicting cardiovascular and all-cause mortality in a Chinese population

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Assimilation of upper plate rocks at convergent margins contributes to the low δ¹⁸O isotopic signature of erupted magma