Putrefying bacteria

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Putrefying/decay bacteria are bacteria involved in putrefaction of living matter. Along with other decomposers, they play a critical role in recycling nitrogen from dead organisms. [1] Putrefying bacteria also play a role in putrefaction and fermentation of proteins in the human gastrointestinal tract. [2]

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Putrefying bacteria play a key role in the nitrogen cycle. Microbial nitrogen cycle.png
Putrefying bacteria play a key role in the nitrogen cycle.

Putrefying bacteria is a broad term used to define several species of bacteria involved in decomposition and fermentation. Putrefying bacteria play a key role in decomposing and fermenting substances within the body as well as the body itself after death. Putrefaction is defined as the final step of decomposition after death. [3] Because these bacteria play a role in decomposition after death, putrefying bacteria also play a key role in the nitrogen cycle. They deconstruct and convert substances from dead organisms so nitrifying bacteria can then convert these products into a usable form of nitrogen. [4]

Putrefying bacteria in the nitrogen cycle

The nitrogen cycle is a vital part of life, and is essential to carry out biosynthesis of nitrogen containing compounds. [5] Nitrogen is inaccessible to most organisms unless it is fixed, and this process can only be carried out by certain classes of prokaryotes. [4] Putrefying bacteria use amino acids or urea as an energy source to decompose dead organisms. In the process, they produce ammonium ions. Nitrifying bacteria then convert this ammonium into nitrate by oxidation, which can then be used by plants to create more proteins thus completing the nitrogen cycle. [6] This process is called nitrification. Energy from this oxidation reaction can also be used to synthesize organic compounds in a process called chemosynthesis. [7]

Putrefaction

Putrefaction begins soon after death. Decomposition stages.jpg
Putrefaction begins soon after death.

Putrefaction, i.e. fermentation of proteins, is considered the final step following death, and is carried out mainly by anaerobic organisms from the bowel. Putrefying bacteria produce a plethora of enzymes which aid in disintegration of the body. Because of the lack of immune function within the body, these bacteria spread through blood vessels and utilize the carbohydrates and proteins in the blood as an energy source. [3] The main bacterial species carrying out putrefaction is Cl. welchii. [8] This bacterium contributes to gas formation, breakdown of remaining blood clots, disintegration of tissue, and marked hemolysis.

This breakdown begins immediately after death, but is not noticeable to the naked eye until several hours after death. Within the following days, the body will begin to break down. The three characteristics of putrefaction are discoloration, disfiguration, and dissolution. There are many factors that could affect the rate of putrefaction in animals such as age, body composition, temperature, and if the body is located in a wet or dry area. [8] Temperature must be between 0 °C and 48 °C for putrefaction to occur. The established bacterial community also play a role in rate of putrefaction. Newborn children that have not been fed will decompose slower than a toddler's body because of the lack of an established gut microbiota. Older individuals tend to decompose slower than younger individuals. Individuals with inflammatory disease, eating disorders, sepsis, and other conditions that affect gut microbiota will all decompose at different rates.

Putrefying bacteria in gut

The gut microbiome plays a huge role in human health, and having a healthy bacterial community is essential to living a healthy life—bacteria aid in digesting nutrients that a human's gastrointestinal tract cannot process independently. Putrefying bacteria in the gut play a key role in fermenting or decomposing proteins that are not broken down by the body. [2] The process of fermentation and putrefaction mainly occurs in the distal colon. [9] These bacteria contribute to the number of metabolites in the large intestine. The gut microbial community is extremely diverse, and putrefying bacteria include diverse bacterial species. [10] Some of these bacteria include Bacillus, Clostridium, Enterobacter, Escherichia, Fusobacterium, Salmonella, etc. [2] These bacterial communities are established by diet, and the microbial modes of transmission. Today's research has not yet fully explored the implications of putrefying bacteria in the human gut microbiome, however current data suggests these bacteria could be helpful or harmful to our systems depending on the circumstances. Some products of putrefying pathways, such as Indole, have been shown to help protect against intestinal worms. Some putrefying bacteria such as Fusobacteriota (formerly Fusobacteria) contribute to harmful cancer and disease, such as colorectal carcinoma. [2]

See also

Related Research Articles

<span class="mw-page-title-main">Human microbiome</span> Microorganisms in or on human skin and biofluids

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Putrefaction is the fifth stage of death, following pallor mortis, livor mortis, algor mortis, and rigor mortis. This process references the breaking down of a body of an animal post-mortem. In broad terms, it can be viewed as the decomposition of proteins, and the eventual breakdown of the cohesiveness between tissues, and the liquefaction of most organs. This is caused by the decomposition of organic matter by bacterial or fungal digestion, which causes the release of gases that infiltrate the body's tissues, and leads to the deterioration of the tissues and organs. The approximate time it takes putrefaction to occur is dependent on various factors. Internal factors that affect the rate of putrefaction include the age at which death has occurred, the overall structure and condition of the body, the cause of death, and external injuries arising before or after death. External factors include environmental temperature, moisture and air exposure, clothing, burial factors, and light exposure. Body farms are facilities that study the way various factors affect the putrefaction process.

<span class="mw-page-title-main">Anammox</span> Anaerobic ammonium oxidation, a microbial process of the nitrogen cycle

Anammox, an abbreviation for "anaerobic ammonium oxidation", is a globally important microbial process of the nitrogen cycle that takes place in many natural environments. The bacteria mediating this process were identified in 1999, and were a great surprise for the scientific community. In the anammox reaction, nitrite and ammonium ions are converted directly into diatomic nitrogen and water.

The rumen, also known as a paunch, is the largest stomach compartment in ruminants and the larger part of the reticulorumen, which is the first chamber in the alimentary canal of ruminant animals. The rumen's microbial favoring environment allows it to serve as the primary site for microbial fermentation of ingested feed. The smaller part of the reticulorumen is the reticulum, which is fully continuous with the rumen, but differs from it with regard to the texture of its lining. It covers approximately 80% of total ruminant stomach portion

<span class="mw-page-title-main">Gut microbiota</span> Community of microorganisms in the gut

Gut microbiota, gut microbiome, or gut flora are the microorganisms, including bacteria, archaea, fungi, and viruses, that live in the digestive tracts of animals. The gastrointestinal metagenome is the aggregate of all the genomes of the gut microbiota. The gut is the main location of the human microbiome. The gut microbiota has broad impacts, including effects on colonization, resistance to pathogens, maintaining the intestinal epithelium, metabolizing dietary and pharmaceutical compounds, controlling immune function, and even behavior through the gut–brain axis.

Lithotrophs are a diverse group of organisms using an inorganic substrate to obtain reducing equivalents for use in biosynthesis or energy conservation via aerobic or anaerobic respiration. While lithotrophs in the broader sense include photolithotrophs like plants, chemolithotrophs are exclusively microorganisms; no known macrofauna possesses the ability to use inorganic compounds as electron sources. Macrofauna and lithotrophs can form symbiotic relationships, in which case the lithotrophs are called "prokaryotic symbionts". An example of this is chemolithotrophic bacteria in giant tube worms or plastids, which are organelles within plant cells that may have evolved from photolithotrophic cyanobacteria-like organisms. Chemolithotrophs belong to the domains Bacteria and Archaea. The term "lithotroph" was created from the Greek terms 'lithos' (rock) and 'troph' (consumer), meaning "eaters of rock". Many but not all lithoautotrophs are extremophiles.

<i>Bacteroides</i> Genus of bacteria

Bacteroides is a genus of Gram-negative, obligate anaerobic bacteria. Bacteroides species are non endospore-forming bacilli, and may be either motile or nonmotile, depending on the species. The DNA base composition is 40–48% GC. Unusual in bacterial organisms, Bacteroides membranes contain sphingolipids. They also contain meso-diaminopimelic acid in their peptidoglycan layer.

<span class="mw-page-title-main">Soil biology</span> Study of living things in soil

Soil biology is the study of microbial and faunal activity and ecology in soil. Soil life, soil biota, soil fauna, or edaphon is a collective term that encompasses all organisms that spend a significant portion of their life cycle within a soil profile, or at the soil-litter interface. These organisms include earthworms, nematodes, protozoa, fungi, bacteria, different arthropods, as well as some reptiles, and species of burrowing mammals like gophers, moles and prairie dogs. Soil biology plays a vital role in determining many soil characteristics. The decomposition of organic matter by soil organisms has an immense influence on soil fertility, plant growth, soil structure, and carbon storage. As a relatively new science, much remains unknown about soil biology and its effect on soil ecosystems.

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<span class="mw-page-title-main">Oral microbiology</span>

Oral microbiology is the study of the microorganisms (microbiota) of the oral cavity and their interactions between oral microorganisms or with the host. The environment present in the human mouth is suited to the growth of characteristic microorganisms found there. It provides a source of water and nutrients, as well as a moderate temperature. Resident microbes of the mouth adhere to the teeth and gums to resist mechanical flushing from the mouth to stomach where acid-sensitive microbes are destroyed by hydrochloric acid.

<span class="mw-page-title-main">Microbiota</span> Community of microorganisms

Microbiota are the range of microorganisms that may be commensal, mutualistic, or pathogenic found in and on all multicellular organisms, including plants. Microbiota include bacteria, archaea, protists, fungi, and viruses, and have been found to be crucial for immunologic, hormonal, and metabolic homeostasis of their host.

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<span class="mw-page-title-main">Microbiology of decomposition</span>

Microbiology of decomposition is the study of all microorganisms involved in decomposition, the chemical and physical processes during which organic matter is broken down and reduced to its original elements.

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<span class="mw-page-title-main">Pharmacomicrobiomics</span>

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<i>Bacteroides thetaiotaomicron</i> Species of bacterium

Bacteroides thetaiotaomicron is a gram-negative, non-motile, rod shaped obligate anaerobic bacterium that is a prominent member of the normal gut microbiome in the distal intestines. Its proteome, consisting of 4,779 members, includes a system for obtaining and breaking down dietary polysaccharides that would otherwise be difficult to digest. B. thetaiotaomicron is also an opportunistic pathogen, meaning it may become virulent in immunocompromised individuals. It is often used in research as a model organism for functional studies of the human microbiota in the gut.

Cetobacterium somerae is a microaerotolerant, Gram-negative, and rod-shaped anaerobic bacteria found in the gastrointestinal tract of fish living in freshwater ecosystems. The bacteria is also immobile and non-spore forming. C. somerae was first isolated from the feces of children with Autism spectrum disorder. Members of bacteria within the Cetobacterium genus tend to dominate the microbiota of fish in freshwater ecosystems. Cetobacterium somerae also produces vitamin B-12 within the gastrointestinal tract of fish in order to provide nutritional support for growth.

References

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