产甲烷
甲烷
化学
古细菌
基质(水族馆)
动力学同位素效应
甲烷厌氧氧化
环境化学
巴氏甲烷八叠球菌
还原酶
甲烷八叠球菌
生物化学
酶
无机化学
有机化学
生物
生态学
氘
物理
基因
量子力学
作者
Jonathan Gropp,Markus Bill,Max K. Lloyd,Rebekah Stein,Dipti D. Nayak,Daniel A. Stolper
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2025-08-14
卷期号:389 (6761): 711-715
被引量:6
标识
DOI:10.1126/science.adu2098
摘要
The stable isotopic composition of microbial methane varies substantially, and the underlying causes are debated. In this work, we experimentally controlled the abundance of the central enzyme in methanogenesis, methyl–coenzyme M reductase (MCR), in Methanosarcina acetivorans and tested whether its cellular concentration alters methane isotopic compositions. We found that during growth on methanol and acetate, lowering the expression of mcr increases the degree of hydrogen isotope exchange between methane and water. Using an isotope-enabled model of methanogenesis, we found that these changes result from an increase in reversibility of enzymes involved in the oxidation of the substrate methyl group. This result indicates that methane produced from organic compounds can deviate from commonly assumed pathway-specific isotope effects, with implications for the interpretation of environmentally relevant methane sources.
科研通智能强力驱动
Strongly Powered by AbleSci AI