Electric coupling between distant nitrate reduction and sulfide oxidation in marine sediment
Ugo Marzocchi1, Daniela Trojan1, Steffen Larsen2
1Section for Microbiology, Department of Bioscience, Aarhus University, Aarhus, Denmark.
The ISME Journal
|March 1, 2014
Summary
Cable bacteria in marine sediment can now use nitrate or nitrite as electron acceptors. This couples distant sulfide oxidation to nitrate reduction, revealing a new biogeochemical process.
Area of Science:
- Microbiology
- Geochemistry
- Environmental Science
Background:
- Filamentous Desulfobulbaceae (cable bacteria) conduct electricity over long distances in marine sediments.
- They link surface oxygen reduction to deep sulfide oxidation.
- Their capacity to utilize alternative electron acceptors was previously unknown.
Purpose of the Study:
- To investigate if cable bacteria can use nitrate or nitrite as electron acceptors.
- To understand the implications for marine biogeochemical cycling.
Main Methods:
- Incubation of sulfidic marine sediment with nitrate-amended anoxic seawater.
- Monitoring for spatial separation of redox processes and pH changes.
- Microscopic identification of Desulfobulbaceae.
Main Results:
- A 4-6 mm zone formed, separating sulfide oxidation from nitrate reduction.
- pH signatures indicated proton consumption (nitrate reduction) and production (sulfide oxidation).
- Filamentous Desulfobulbaceae were detected in nitrate-amended incubations.
Conclusions:
- Cable bacteria can utilize nitrate/nitrite as electron acceptors, coupling distant sulfide oxidation.
- This represents a novel mechanism in nitrogen and sulfur cycling.
- Further research is needed to quantify the impact on elemental cycles.
Related Concept Videos
Microbes and the Sulfur Cycle
123
Sulfur is a vital element in Earth's biogeochemical systems. It transitions through various inorganic states, including sulfate (SO₄²⁻), elemental sulfur (S⁰), and sulfide (S²⁻). Abiotic and biological mechanisms across oxic and anoxic environments intricately mediate these transformations. Sulfate, the most oxidized form of sulfur, is predominantly stored in rocks, marine sediments, and oceanic waters, acting as a long-term reservoir in the global sulfur...
123
Metabolism of Chemolithotrophs
1.3K
Chemolithotrophs are microorganisms that obtain energy by oxidizing inorganic molecules such as hydrogen gas (H₂), ammonia (NH₃), reduced sulfur compounds (H₂S, S²⁻), and ferrous iron (Fe²⁺). Unlike heterotrophic organisms that rely on organic carbon, chemolithotrophs transfer electrons from these inorganic donors to the electron transport chain (ETC), generating a proton motive force (PMF) that drives ATP synthesis through oxidative phosphorylation.
1.3K
Microbes and Other Elemental Cycles
89
Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
89
Marine Microbial Ecology
66
Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
66
Microbial Mats
67
Microbial communities forming biofilms and mats represent complex, spatially structured ecosystems where metabolic processes are stratified according to light, oxygen, and nutrient gradients. Biofilms are initial colonization stages, only a few millimeters thick, while mature microbial mats can reach centimeter-scale thickness and display intricate vertical organization. Their structural and functional heterogeneity allows microorganisms to occupy distinct ecological niches within a few...
67
Deep Sea Microbial Ecology
53
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...
53


