Mantle data imply a decline of oxidizable volcanic gases could have triggered the Great Oxidation
地幔数据表明，可氧化火山气体的减少可能引发了大氧化事件。
期刊:Nature Communications
影响因子:15.7
doi:10.1038/s41467-020-16493-1
Kadoya, Shintaro; Catling, David C; Nicklas, Robert W; Puchtel, Igor S; Anbar, Ariel D
