The ancient microbes that breathe sulfate and eat industrial waste

The ancient microbes that breathe sulfate and eat industrial waste
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In short: Deep in anoxic sediments and industrial sludge, a group of ancient microorganisms performs a unique metabolic feat. Instead of oxygen, these bacteria use sulfate as their primary fuel source, transforming it into hydrogen sulfide. This process powers a vast portion of the Earth's sulfur cycle and drives significant industrial corrosion.

Sulfate-reducing bacteria (SRB) are among Earth's oldest life forms, with origins dating back approximately 3.5 billion years. These microorganisms are ubiquitous in anoxic (oxygen-free) habitats, where they play a critical role in the global sulfur and carbon cycles. Unlike most life that uses oxygen for respiration, SRB perform dissimilatory sulfate reduction, using sulfate as a terminal electron acceptor to obtain energy and expelling hydrogen sulfide as a waste product.

The metabolic versatility of SRB is extensive. They can act as organotrophs, oxidizing a wide array of organic compounds including carbohydrates, alcohols, organic acids like acetate and lactate, and even complex aromatic hydrocarbons such as toluene and xylene. Some species can even degrade long-chain alkanes and short-chain hydrocarbons like ethane and propane. Additionally, some lithotrophic SRB can oxidize molecular hydrogen or even directly use metallic iron as an electron donor.

Beyond their natural roles, SRB are significant in human industry and environmental science. They are the primary agents behind microbial corrosion (MIC), where they degrade metal surfaces in marine environments and industrial systems by producing corrosive hydrogen sulfide. Conversely, their ability to break down organic matter and hydrocarbons makes them valuable in environmental biotechnology for treating wastewater and purifying industrial sludge.

Research highlights complex social behaviors among these microbes, such as syntrophy. In marine sediments, a syntrophic consortium of archaea and SRB mediates the anaerobic oxidation of methane. Other studies show that SRB can engage in interspecies electron transfer, forming partnerships to mineralize organic carbon. These interactions determine how electrons from organic matter are routed toward minerals, gases, or microbial biomass.

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