甲烷
化学合成
基因组
化学
波罗的海
生物合成
古细菌
环境化学
生物
生物化学
生态学
基因
海洋学
地质学
古生物学
热液循环
深海热液喷口
作者
William W. Metcalf,Benjamin M. Griffin,Robert M. Cicchillo,Jiangtao Gao,Sarath Chandra Janga,Heather A. Cooke,Benjamin T. Circello,Bradley S. Evans,Willm Martens‐Habbena,David A. Stahl,Wilfred A. van der Donk
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2012-08-30
卷期号:337 (6098): 1104-1107
被引量:307
标识
DOI:10.1126/science.1219875
摘要
Relative to the atmosphere, much of the aerobic ocean is supersaturated with methane; however, the source of this important greenhouse gas remains enigmatic. Catabolism of methylphosphonic acid by phosphorus-starved marine microbes, with concomitant release of methane, has been suggested to explain this phenomenon, yet methylphosphonate is not a known natural product, nor has it been detected in natural systems. Further, its synthesis from known natural products would require unknown biochemistry. Here we show that the marine archaeon Nitrosopumilus maritimus encodes a pathway for methylphosphonate biosynthesis and that it produces cell-associated methylphosphonate esters. The abundance of a key gene in this pathway in metagenomic data sets suggests that methylphosphonate biosynthesis is relatively common in marine microbes, providing a plausible explanation for the methane paradox.
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