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Strange isotopes: Scientists explain a methane isotope paradox of the seafloor


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IMAGE: The Guaymas Basin hydrothermal vents - the home of the studied methane-oxidizing microorganisms. The heat loving microorganisms thrive under the orange microbial mat in the background. The high temperatures of.
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Credit: Woods Hole Oceanographic Institution
Methane, a chemical compound with the molecular formula CH4, is not only a powerful greenhouse gas, but also an important energy source. It heats our homes, and even seafloor microbes make a living of it. The microbes use a process called anaerobic oxidation of methane (AOM), which happens commonly in the seafloor in so-called sulfate-methane transition zones - layers in the seafloor where sulfate from the seawater meets methane from the deeper sediment. Here, specialized microorganisms, the ANaerobically MEthane-oxidizing (ANME) archaea, consume the methane. They live in close association with bacteria, which use electrons released during methane oxidation for sulfate reduc ....

Itay Halevy , Marcus Elvert , Jonathan Gropp , Gunter Wegener , Marine Environmental Sciences , Max Planck Institute For Marine Microbiology , Weizmann Institute Of Science , Max Planck Institute , Marine Microbiology , Weizmann Institute , குண்டர் வெஜனர் , கடல் சுற்றுச்சூழல் அறிவியல் , வெய்ஸ்மேன் நிறுவனம் ஆஃப் அறிவியல் , கடல் நுண்ணுயிரியல் , வெய்ஸ்மேன் நிறுவனம் ,

Strange isotopes: Scientists explain a methane isotope paradox of the seafloor


 E-Mail
IMAGE: The Guaymas Basin hydrothermal vents - the home of the studied methane-oxidizing microorganisms. The heat loving microorganisms thrive under the orange microbial mat in the background. The high temperatures of.
view more 
Credit: Woods Hole Oceanographic Institution
Methane, a chemical compound with the molecular formula CH4, is not only a powerful greenhouse gas, but also an important energy source. It heats our homes, and even seafloor microbes make a living of it. The microbes use a process called anaerobic oxidation of methane (AOM), which happens commonly in the seafloor in so-called sulfate-methane transition zones - layers in the seafloor where sulfate from the seawater meets methane from the deeper sediment. Here, specialized microorganisms, the ANaerobically MEthane-oxidizing (ANME) archaea, consume the methane. They live in close association with bacteria, which use electrons released during methane oxidation for sulfate reduc ....

Itay Halevy , Marcus Elvert , Jonathan Gropp , Gunter Wegener , Marine Environmental Sciences , Max Planck Institute For Marine Microbiology , Weizmann Institute Of Science , Max Planck Institute , Marine Microbiology , Weizmann Institute , குண்டர் வெஜனர் , கடல் சுற்றுச்சூழல் அறிவியல் , வெய்ஸ்மேன் நிறுவனம் ஆஃப் அறிவியல் , கடல் நுண்ணுயிரியல் , வெய்ஸ்மேன் நிறுவனம் ,