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Updated: Jan 14, 2026

Visualizing Methane-Cycling Microbial Dynamics in Coastal Wetlands
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从一个分层的热卡斯特永久土热点释放甲的微生物和化学预测因素

Kevin S Rozmiarek1,2, Jihoon Yang3, Jenna Schambach4

  • 1Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, United States.

Frontiers in microbiology
|October 27, 2025
PubMed
概括

挥发性有机化合物 (VOC) 可以表明在永久土解过程中产生甲 (CH4). 这项研究发现,VOCs信号微生物活动,改善了来自北极土壤的CH4排放预测.

关键词:
生物地质化学建模碳循环循环的过程甲热点是甲的热点.甲同位素是甲的同位素.在这种情况下,甲醇缩会导致甲醇缩.微生物的挥发性有机化合物永久土的融化正在发生.热地土是热地土.

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