Anaerobic oxidation of methane (AOM) exerts an important control on the release of methane (CH4) from marine sediments. The highest rates of oceanic AOM occur at cold seeps, where subsurface fluid flow drives rapid vertical migration of CH4…
Source: Proceedings of the National Academy of Sciences (PNAS) | Earth, Atmospheric and Planetary Sciences
Proceedings of the National Academy of Sciences (PNAS)
Topics: Earth, Atmospheric and Planetary Sciences- Fine and ultrafine Martian dust presents additional risks for future crewed missions to Mars
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- In-cloud motions shape warm-rain production in marine clouds: Evidence from multiyear observations
- Thermodynamic origin of atmospheric new particle formation: Theory for stable nucleating pairs
- Improved assessment of Alaskan Arctic coastal wave exposure accounting for landfast ice
- Multiyear dual-isotope fingerprinting at South Asian receptor sites constrains carbon monoxide sources and enhanced oxidation
- Extensive glacier loss in the coterminous United States
- Multiple-oxygen isotope constraints on aerobic respiration and gross primary productivity
