Related Experiment Video
Updated: Jan 23, 2026

07:26
Visualizing Methane-Cycling Microbial Dynamics in Coastal Wetlands
Published on: January 31, 2025
810
Microbial Cycling of Methanethiol.
1School of Life Sciences, University of Warwick, Coventry, UK.
Current Issues in Molecular Biology
|June 6, 2019
Summary
Methanethiol (MT), a malodorous sulfur compound, plays a key role in the global sulfur cycle. Microorganisms drive its production and degradation across diverse environments, impacting various biological and environmental processes.
Area of Science:
- Biogeochemistry
- Environmental Microbiology
- Organic Chemistry
Background:
- Methanethiol (MT) is a volatile organic sulfur compound recognized for its potent, unpleasant odor.
- It functions as a crucial reactive intermediate in the global sulfur cycle, linking major sulfur compounds like dimethylsulfoniopropionate, dimethylsulfide, and methionine.
- MT contributes significantly to malodor in various settings, including animal husbandry, waste management, and biological processes such as halitosis.
Purpose of the Study:
- To elucidate the biogeochemical significance of methanethiol (MT) within the global sulfur cycle.
- To review and synthesize current knowledge on microbial pathways involved in MT production and degradation.
- To highlight the environmental and biological relevance of MT due to its malodorous properties.
Main Methods:
- Literature review and synthesis of existing research on methanethiol (MT).
- Analysis of microbial pathways for MT synthesis and degradation.
- Examination of MT's role in various terrestrial, aquatic, and host-associated environments.
Main Results:
- Methanethiol (MT) is a central intermediate in microbial sulfur metabolism, connecting diverse sulfur compounds.
- A wide array of microorganisms, under both aerobic and anaerobic conditions, are responsible for MT production and consumption.
- MT-producing and degrading microbes are ubiquitous in various ecosystems, including soil, water, and associated with plants and animals.
Conclusions:
- Methanethiol (MT) is a critical link in microbial sulfur cycling with broad environmental and biological implications.
- Understanding the microbial pathways of MT is essential for managing malodor and comprehending sulfur biogeochemistry.
- The diverse roles of MT underscore the importance of microbial activity in sulfur transformations and ecosystem function.
Related Concept Videos
What are Biogeochemical Cycles?
39.2K
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
39.2K
The Water Cycle
28.2K
The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
28.2K
The Phosphorus Cycle
43.8K
Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
43.8K
The Nitrogen Cycle
59.7K
Nitrogen atoms, present in all proteins and DNA, are recycled between abiotic and biotic components of the ecosystem. However, the primary form of nitrogen on Earth is nitrogen gas, which cannot be used by most animals and plants. Thus, nitrogen gas must first be converted into a usable form by nitrogen-fixing bacteria before it can be cycled through other living organisms. The use of nitrogen-containing fertilizers and animal waste products in human agriculture has greatly influenced the...
59.7K
The Carbon Cycle
43.3K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
43.3K
The Sulfur Cycle
51.8K
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
51.8K

