Abstract
Hopanoids are lipids that are widespread in the bacterial domain and well established molecular biomarkers in modern and paleo environments. In particular, the occurrence of 13C-depleted 3-methylated hopanoids are characteristic of aerobic bacteria involved in methane oxidation. Previously the intra-aerobic methanotroph ‘Candidatus Methylomirabilis oxyfera’ (‘Ca. M. oxyfera’), which performs nitrite-dependent
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