assimilatory sulfate reduction
Examples of assimilatory sulfate reduction in the following topics:
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The Sulfur Cycle
- Plants and microbes assimilate sulfate and convert it into organic forms.
- Lots of bacteria reduce small amounts of sulfates to synthesize sulfur-containing cell components; this is known as assimilatory sulfate reduction.
- By contrast, the sulfate-reducing bacteria considered here reduce sulfate in large amounts to obtain energy and expel the resulting sulfide as waste.
- This process is known as dissimilatory sulfate reduction.
- In a sense, they breathe sulfate.
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Sulfate and Sulfur Reduction
- Sulfate reduction is a type of anaerobic respiration that utilizes sulfate as a terminal electron acceptor in the electron transport chain.
- Sulfate reduction is a type of anaerobic respiration that utilizes sulfate as a terminal electron acceptor in the electron transport chain.
- The hydrogen produced during fermentation is actually what drives respiration during sulfate reduction.
- Many bacteria reduce small amounts of sulfates in order to synthesize sulfur-containing cell components; this is known as assimilatory sulfate reduction.
- Outline the process of sulfate and sulfur reduction including its various purposes
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Electron Donors and Acceptors in Anaerobic Respiration
- Instead, molecules such as sulfate (SO42-), nitrate (NO3-), or sulfur (S) are used as electron acceptors.
- Nitrate, like oxygen, has a high reduction potential.
- Sulfate reduction uses sulfate (SO2−4) as the electron acceptor, producing hydrogen sulfide (H2S) as a metabolic end product.
- Sulfate reduction is a relatively energetically poor process, and is used by many Gram negative bacteria found within the δ-Proteobacteria.
- Sulfate reduction requires the use of electron donors, such as the carbon compounds lactate and pyruvate (organotrophic reducers), or hydrogen gas (lithotrophic reducers).
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Archaeoglobus
- Archaeoglobus are sulfate-reducing archaea, coupling the reduction of sulfate to sulfide with the oxidation of many different organic carbon sources, including complex polymers.
- Archaeoglobus are lithotrophs, and can be either autotrophic or heterotrophic.The archaeoglobus strain A. lithotrophicus are lithoautotrophs, and derive their energy from hydrogen, sulfate and carbon dioxide.
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Microbial Ore Leaching
- In the process, free electrons are generated and used for the reduction of oxygen to water which produces energy in the bacterial cell.
- The net products of the reaction are soluble ferrous sulfate and sulfuric acid.
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Oxidation of Reduced Sulfur Compounds
- Biochemically, reduced sulfur compounds are converted to sulfite (SO2−3) and, subsequently, sulfate (SO2−4) by the enzyme sulfite oxidase.
- Some organisms, however, accomplish the same oxidation using a reversal of the APS reductase system used by sulfate-reducing bacteria (see above).
- Marine autotrophic Beggiatoa species are able to oxidize intracellular sulfur to sulfate.
- The reduction of elemental sulfur frequently occurs when oxygen is lacking.
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The Acetyl-CoA Pathway
- The acetyl coenzyme A (CoA) pathway, commonly referred to as the Wood-Ljungdahl pathway or the reductive acetyl-CoA pathway, is one of the major metabolic pathways utilized by bacteria.
- The acetyl-CoA pathway begins with the reduction of a carbon dioxide to carbon monoxide.
- Carbon monoxide dehydrogenase, the enzyme responsible for the reduction of a carbon dioxide to a carbonyl group, functions in numerous biochemical processes.
- These processes include metabolism of methanogens, acetogenic and sulfate-reducing bacteria.
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Wetland Soils
- Some anaerobic microbial processes include denitrification , sulfate reduction and methanogenesis and are responsible for the release of N2 (nitrogen), H2S (hydrogen sulfide) and CH4 (methane).
- Redox potential, or reduction potential , is used to express the likelihood of an environment to receive electrons and therefore become reduced.