Anaerobic respiration
Respiration without oxygen, using alternative electron acceptors.
Anaerobic respiration is a form of cellular respiration that uses electron acceptors other than molecular oxygen (O2) in its electron transport chain. It is a critical component of global biogeochemical cycles, including the nitrogen, iron, sulfur, and carbon cycles, and occurs in diverse environments such as freshwater and marine sediments, soil, subsurface aquifers, and biofilms.
- field
- Microbiology, Biochemistry, Ecology
- known_for
- Respiration using electron acceptors other than oxygen; key role in denitrification, methanogenesis, and sulfate reduction
- key_processes
- Denitrification, methanogenesis, sulfate respiration
- environments
- Freshwater and marine sediments, soil, subsurface aquifers, deep subsurface, biofilms
- applications
- Wastewater treatment, bioremediation, microbial fuel cells
Lore & Background
Anaerobic respiration differs fundamentally from fermentation. Cellular respiration (both aerobic and anaerobic) uses reduced compounds such as NADH and FADH2 to establish an electrochemical gradient across a membrane, driving ATP synthesis via ATP synthase. Fermentation, in contrast, relies solely on substrate-level phosphorylation and regenerates NAD+ by reducing organic compounds. Anaerobic respiration is less efficient than aerobic respiration because its terminal electron acceptors have smaller reduction potentials than oxygen, releasing less energy per oxidized molecule. Two important anaerobic methane formation pathways exist: carbon dioxide/bicarbonate reduction (respiration) and acetate fermentation. Anaerobic respiration is ecologically vital: denitrification returns fixed nitrogen to the atmosphere as molecular nitrogen gas; methanogenesis produces methane, a potent greenhouse gas; and sulfate respiration generates hydrogen sulfide, responsible for the 'rotten egg' smell of coastal wetlands and capable of precipitating heavy metal ions. Applications include dissimilatory denitrification for removing nitrate and nitrite from municipal wastewater, bioremediation of toxic chemicals such as arsenate, selenate, and chlorinated pollutants, and electricity generation in microbial fuel cells using bacteria that respire solid electron acceptors like oxidized iron.
Reader's Guide
Anaerobic respiration is a fundamental biological process that enables energy production in the absence of oxygen, using alternative electron acceptors such as nitrate, fumarate, sulfate, or elemental sulfur. Its ecological significance is profound: it drives key steps in the global nitrogen, sulfur, and carbon cycles, including denitrification—the main route for returning fixed nitrogen to the atmosphere—and methanogenesis, which produces biogenic methane. The process also has practical applications: denitrification is widely used in wastewater treatment to prevent eutrophication and nitrite toxicity; anaerobic bacteria can reduce toxic pollutants like arsenate and chlorinated compounds in bioremediation; and microbial fuel cells harness anaerobic respiration to generate electricity while degrading organic waste. Understanding anaerobic respiration is essential for managing greenhouse gas emissions, treating wastewater, and developing sustainable energy technologies.
Did You Know?
- Anaerobic respiration uses electron acceptors with smaller reduction potentials than oxygen, making it less efficient than aerobic respiration.
- Denitrification, a form of anaerobic respiration, is the main route by which fixed nitrogen is returned to the atmosphere as molecular nitrogen gas.
- Sulfate respiration produces hydrogen sulfide, which can precipitate heavy metal ions and lead to the deposition of sulfidic metal ores.
- Some single-cellular anaerobic ciliates use denitrifying endosymbionts to gain energy, similar to mitochondria in oxygen-respiring microorganisms.
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