... hydrogen-poor bitumen 贫氢沥青 hydrogen-sulfide-forming bacteria 生成硫化氢的细菌 hydrogen-to-carbon ratio 氢碳原子比 ...
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同时，地表下渗的大气降水携带了细菌类微生物，对原生有机质进行生物降解，并生成硫化氢类还原物质。
Moreover, the microorganism which was brought by permeable surface water degraded the primary kerogen in sedimantary rocks and could produce reducing matters. The precipitation and th…
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