Related Experiment Video
Updated: Jul 17, 2026

15:19
Development of Sulfidogenic Sludge from Marine Sediments and Trichloroethylene Reduction in an Upflow Anaerobic Sludge Blanket Reactor
Published on: October 15, 2015
Methane-consuming archaebacteria in marine sediments
K U Hinrichs1, J M Hayes, S P Sylva
1Woods Hole Oceanographic Institution, Massachusetts 02543, USA.
Nature
|May 11, 1999
Summary
Marine sediments consume methane anaerobically via archaea distinct from known methanogens. This discovery reveals novel microbial pathways for methane cycling in seafloor environments.
Area of Science:
- Marine microbiology
- Geochemistry
- Molecular biology
Background:
- Methane is abundant in marine sediments but is consumed before reaching oxygenated waters.
- Anaerobic methane oxidation is crucial for regulating atmospheric methane but the responsible organisms remain largely uncharacterized.
- Biogeochemical data suggest a multi-organism process involving methanogens and sulfate-reducers.
Purpose of the Study:
- To investigate the microbial communities responsible for anaerobic methane consumption in marine sediments.
- To identify novel microorganisms involved in methane cycling.
- To provide direct evidence for the biological source of specific lipid biomarkers.
Main Methods:
- Analysis of lipid biomarkers in sediments associated with a decomposing methane hydrate.
- Stable isotope analysis (carbon-13 depletion) to trace methane as a carbon source.
- Gene surveys using small-subunit ribosomal RNA (16S rRNA) to identify microbial populations.
Main Results:
- Lipid biomarkers strongly depleted in carbon-13 indicate methane as the primary carbon source for archaea.
- These archaea are phylogenetically distinct from previously known methanogens.
- 16S rRNA gene surveys revealed a dominant, novel archaeal group related to methanogenic orders.
Conclusions:
- Evidence suggests a new group of archaea, unrelated to known methanogens, are responsible for anaerobic methane consumption.
- This finding expands our understanding of methane cycling in marine environments.
- The study identifies novel archaeal lineages involved in the anaerobic oxidation of methane.
Related Concept Videos
Overview of Archaea
Archaea, named after the Archaean eon, represent a unique domain of life, distinct from bacteria and eukaryotes, with remarkable traits. Their cellular and molecular features, ecological adaptability, and industrial relevance highlight their importance in understanding life processes and leveraging biotechnology.Cellular and Molecular CharacteristicsA defining feature of archaea is their unique membrane composition. Archaeal membranes contain ether-linked isoprenoid lipids, which confer...
Diversity of Archaea I
Archaea, a domain of single-celled microorganisms, are classified into five major phyla based on genetic and biochemical characteristics: Euryarchaeota, Crenarchaeota, Thaumarchaeota, Korarchaeota, and Nanoarchaeota. Among these, the phylum Euryarchaeota is notable for its remarkable diversity in morphology, metabolism, and ecological adaptations.Morphological and Metabolic DiversityMembers of Euryarchaeota exhibit a variety of cellular shapes, including rods and cocci. Their metabolic pathways...
Diversity of Archaea II
Archaea, one of the three domains of life, exhibit remarkable diversity and adaptability, thriving in both extreme and moderate environments. Historically, most identified archaea have been classified into two major phyla: Euryarchaeota and Crenarchaeota. However, recent molecular studies have expanded this classification to include three additional phyla: Thaumarchaeota, Nanoarchaeota, and Korarchaeota, each exhibiting unique characteristics and ecological roles.Thaumarchaeota: Mesophiles...
Diversity of Archaea III
Crenarchaeota, a prominent phylum of Archaea, is remarkable for its ability to thrive in extreme environments characterized by high temperatures and acidity. These microorganisms inhabit sulfuric hot springs, volcanic systems, and submarine hydrothermal vents, where temperatures often exceed 100°C. The unique adaptations of Crenarchaeota not only allow survival under such extreme conditions but also provide insights into the mechanisms of life in primordial Earth-like environments.Morphological...
Microbes and Methanogenesis
Methanogenesis is a critical microbial process in anaerobic ecosystems responsible for the biological production of methane, a potent greenhouse gas and valuable biofuel. This metabolic pathway is primarily facilitated by methanogenic archaea, which thrive in anoxic environments such as wetlands, sediments, and animal gastrointestinal tracts. The absence of oxygen in these habitats prevents aerobic respiration, thereby favoring alternative biochemical pathways for organic matter degradation.In...
Deep Sea Microbial Ecology
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...

