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A microorganism (from the Greek: μικρός
, mikrós, "small" and ὀργανισμός, organismós, "organism"; also spelled micro organism or micro-organism) or microbe is an organism that is microscopic (usually too small to be seen by the naked human eye). The study of microorganisms is called microbiology, a subject that began with Anton van Leeuwenhoek's discovery of microorganisms in 1675, using a microscope of his own design.
Microorganisms are very diverse; they include bacteria, fungi, archaea, and protists; microscopic plants (called green algae); and animals such as plankton and the planarian. Some microbiologists also include viruses, but others consider these as non-living. Most microorganisms are unicellular (single-celled), but this is not universal, since some multicellular organisms are microscopic, while some unicellular protists and bacteria, like Thiomargarita namibiensis, are macroscopic and visible to the naked eye.
Microorganisms live in all parts of the biosphere where there is liquid water, including soil, hot springs, on the ocean floor, high in the atmosphere and deep inside rocks within the Earth's crust. Microorganisms are critical to nutrient recycling in ecosystems as they act as decomposers. As some microorganisms can fix nitrogen, they are a vital part of the nitrogen cycle, and recent studies indicate that airborne microbes may play a role in precipitation and weather.
Microbes are also exploited by people in biotechnology, both in traditional food and beverage preparation, and in modern technologies based on genetic engineering. However, pathogenic microbes are harmful, since they invade and grow within other organisms, causing diseases that kill millions of people, other animals, and plants.
- Further information: Timeline of evolution
Single-celled microorganisms were the first forms of life to develop on Earth, approximately 3–4 billion years ago. Further evolution was slow, and for about 3 billion years in the Precambrian eon, all organisms were microscopic. So, for most of the history of life on Earth the only forms of life were microorganisms. Bacteria, algae and fungi have been identified in amber that is 220 million years old, which shows that the morphology of microorganisms has changed little since the triassic period.
Most microorganisms can reproduce rapidly and microbes such as bacteria can also freely exchange genes by conjugation, transformation and transduction between widely-divergent species. This horizontal gene transfer, coupled with a high mutation rate and many other means of genetic variation, allows microorganisms to swiftly evolve (via natural selection) to survive in new environments and respond to environmental stresses. This rapid evolution is important in medicine, as it has led to the recent development of 'super-bugs' — pathogenic bacteria that are resistant to modern antibiotics.
speculative and were not based on any data or science. Microorganisms were neither proven, observed, nor correctly and accurately described until the 17th century. The reason for this was that all these early studies lacked the microscope.
= History of Classification and structure
Microorganisms can be found almost anywhere in the taxonomic organization of life on the planet. Bacteria and archaea are almost always microscopic, while a number of eukaryotes are also microscopic, including most protists, some fungi, as well as some animals and plants. Viruses are generally regarded as not living and therefore are not microbes, although the field of microbiology also encompasses the study of viruses.
- Main article: Prokaryote
Prokaryotes are organisms that lack a cell nucleus and the other membrane bound organelles. They are almost always unicellular, although some species such as myxobacteria can aggregate into complex structures as part of their life cycle.
Consisting of two domains, bacteria and archaea, the prokaryotes are the most diverse and abundant group of organisms on Earth and inhabit practically all environments where some liquid water is available and the temperature is below +140 °C. They are found in sea water, soil, air, animals' gastrointestinal tracts, hot springs and even deep beneath the Earth's crust in rocks. Practically all surfaces which have not been specially sterilized are covered by prokaryotes. The number of prokaryotes on Earth is estimated to be around five million trillion trillion, or 5 × 1030.
- Main article: Bacteria
Bacteria are practically all invisible to the naked eye, with a few extremely rare exceptions, such as Thiomargarita namibiensis. They are unicellular organisms and lack membrane-bound organelles. Their genome is usually a single loop of DNA, although they can also harbor small pieces of DNA called plasmids. These plasmids can be transferred between cells through bacterial conjugation. Bacteria are surrounded by a cell wall, which provides strength and rigidity to their cells. They reproduce by binary fission or sometimes by budding, but do not undergo sexual reproduction. Some species form extraordinarily resilient spores, but for bacteria this is a mechanism for survival, not reproduction. Under optimal conditions bacteria can grow extremely rapidly and can double as quickly as every 10 minutes.
- Main article: Archaea
Archaea are also single-celled organisms that lack nuclei. In the past, the differences between bacteria and archaea were not recognised and archaea were classified with bacteria as part of the kingdom Monera. However, in 1990 the microbiologist Carl Woese proposed the three-domain system that divided living things into bacteria, archaea and eukaryotes. Archaea differ from bacteria in both their genetics and biochemistry. For example, while bacterial cell membranes are made from phosphoglycerides with ester bonds, archaean membranes are made of ether lipids.
Archaea were originally described in extreme environments, such as hot springs, but have since been found in all types of habitats. Only now are scientists beginning to appreciate how common archaea are in the environment, with crenarchaeota being the most common form of life in the ocean, dominating ecosystems below 150 m in depth. These organisms are also common in soil and play a vital role in ammonia oxidation.
- Main article: Eukaryote
Most living things which are visible to the naked eye in their adult form are eukaryotes, including humans. However, a large number of eukaryotes are also microorganisms. Unlike bacteria and archaea, eukaryotes contain organelles such as the cell nucleus, the Golgi apparatus and mitochondria in their cells. The nucleus is an organelle which houses the DNA that makes up a cell's genome. DNA itself is arranged in complex chromosomes. Mitochondria are organelles vital in metabolism as they are the site of the citric acid cycle and oxidative phosphorylation. They evolved from symbiotic bacteria and retain a remnant genome. Like bacteria, plant cells have cell walls, and contain organelles such as chloroplasts in addition to the organelles in other eukaryotes. Chloroplasts produce energy from light by photosynthesis, and were also originally symbiotic bacteria.
Unicellular eukaryotes are those eukaryotic organisms that consist of a single cell throughout their life cycle. This qualification is significant since most multicellular eukaryotes consist of a single cell called a zygote at the beginning of their life cycles. Microbial eukaryotes can be either haploid or diploid, and some organisms have multiple cell nuclei (see coenocyte). However, not all microorganisms are unicellular as some microscopic eukaryotes are made from multiple cells.
- Main article: Protista
Of eukaryotic groups, the protists are most commonly unicellular and microscopic. This is a highly diverse group of organisms that are not easy to classify. Several algae species are multicellular protists, and slime molds have unique life cycles that involve switching between unicellular, colonial, and multicellular forms. The number of species of protozoa is uncertain, since we may have identified only a small proportion of the diversity in this group of organisms.
- Main article: Micro-animals
Mostly animals are multicellular, but some are too small to be seen by the naked eye. Microscopic arthropods include dust mites and spider mites. Microscopic crustaceans include copepods and the cladocera, while many nematodes are too small to be seen with the naked eye. Another particularly common group of microscopic animals are the rotifers, which are filter feeders that are usually found in fresh water. Micro-animals reproduce both sexually and asexually and may reach new habitats as eggs that survive harsh environments that would kill the adult animal. However, some simple animals, such as rotifers and nematodes, can dry out completely and remain dormant for long periods of time.
- Main article: Fungus
The fungi have several unicellular species, such as baker's yeast (Saccharomyces cerevisiae) and fission yeast (Schizosaccharomyces pombe). Some fungi, such as the pathogenic yeast Candida albicans, can undergo phenotypic switching and grow as single cells in some environments, and filamentous hyphae in others. Fungi reproduce both asexually, by budding or binary fission, as well by producing spores, which are called conidia when produced asexually, or basidiospores when produced sexually.
Habitats and ecology
Microorganisms are found in almost every habitat present in nature. Even in hostile environments such as the poles, deserts, geysers, rocks, and the deep sea. Some types of microorganisms have adapted to the extreme conditions and sustained colonies; these organisms are known as extremophiles. Extremophiles have been isolated from rocks as much as 7 kilometres below the Earth's surface, and it has been suggested that the amount of living organisms below the Earth's surface may be comparable with the amount of life on or above the surface. Extremophiles have been known to survive for a prolonged time in a vacuum, and can be highly resistant to radiation, which may even allow them to survive in space. Many types of microorganisms have intimate symbiotic relationships with other larger organisms; some of which are mutually beneficial (mutualism), while others can be damaging to the host organism (parasitism). If microorganisms can cause disease in a host they are known as pathogens.
- Main article: Extremophile
Extremophiles are microorganisms which have adapted so that they can survive and even thrive in conditions that are normally fatal to most life-forms. For example, some species have been found in the following extreme environments:
- Temperature: as high as Template:Convert/LoffAoffDbSoffTTemplate:Convert/test/A, as low as Template:Convert/LoffAoffDbSoffTTemplate:Convert/test/A
- Acidity/alkalinity: less than pH 0, up to pH 11.5
- Salinity: up to saturation
- Pressure: up to 1,000-2,000 atm, down to 0 atm (e.g. vacuum of space)
- Radiation: up to 5kGy
Extremophiles are significant in different ways. They extend terrestrial life into much of the Earth's hydrosphere, crust and atmosphere, their specific evolutionary adaptation mechanisms to their extreme environment can be exploited in bio-technology, and their very existence under such extreme conditions increases the potential for extraterrestrial life.
Importance in human health
- Further information: Human flora#Human bacterial flora and human health
Microorganisms can form an endosymbiotic relationship with other, larger organisms. For example, the bacteria that live within the human digestive system contribute to gut immunity, synthesise vitamins such as folic acid and biotin, and ferment complex indigestible carbohydrates.
Diseases and immunology
- Main article: Pathogenic microbes
Microorganisms are the cause of many infectious diseases. The organisms involved include pathogenic bacteria, causing diseases such as plague, tuberculosis and anthrax; protozoa, causing diseases such as malaria, sleeping sickness and toxoplasmosis; and also fungi causing diseases such as ringworm, candidiasis or histoplasmosis. However, other diseases such as influenza, yellow fever or AIDS are caused by pathogenic viruses, which are not usually classified as living organisms and are not therefore microorganisms by the strict definition. As of 2007, no clear examples of archaean pathogens are known, although a relationship has been proposed between the presence of some methanogens and human periodontal disease.
- Main article: Hygiene
Hygiene is the avoidance of infection or food spoiling by eliminating microorganisms from the surroundings. As microorganisms, particularly bacteria, are found practically everywhere, this means in most cases the reduction of harmful microorganisms to acceptable levels. However, in some cases it is required that an object or substance be completely sterile, i.e. devoid of all living entities and viruses. A good example of this is a hypodermic needle.
In food preparation microorganisms are reduced by preservation methods (such as the addition of vinegar), clean utensils used in preparation, short storage periods or by cool temperatures. If complete sterility is needed, the two most common methods are irradiation and the use of an autoclave, which resembles a pressure cooker.
There are several methods for investigating the level of hygiene in a sample of food, drinking water, equipment etc. Water samples can be filtrated through an extremely fine filter. This filter is then placed in a nutrient medium. Microorganisms on the filter then grow to form a visible colony. Harmful microorganisms can be detected in food by placing a sample in a nutrient broth designed to enrich the organisms in question. Various methods, such as selective media or PCR, can then be used for detection. The hygiene of hard surfaces, such as cooking pots, can be tested by touching them with a solid piece of nutrient medium and then allowing the microorganisms to grow on it.
There are no conditions where all microorganisms would grow, and therefore often several different methods are needed. For example, a food sample might be analyzed on three different nutrient mediums designed to indicate the presence of "total" bacteria (conditions where many, but not all, bacteria grow), molds (conditions where the growth of bacteria is prevented by e.g. antibiotics) and coliform bacteria (these indicate a sewage contamination).
- ↑ Rybicki EP (1990). The classification of organisms at the edge of life, or problems with virus systematics. S Aft J Sci 86: 182–6.
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- ↑ Max Planck Society Research News Release Accessed 21 May 2009
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- ↑ 2002 WHO mortality data Accessed 20 January 2007
- ↑ Schopf J (2006). Fossil evidence of Archaean life. Philos Trans R Soc Lond B Biol Sci 361 (1470): 869–85.
- ↑ Altermann W, Kazmierczak J (2003). Archean microfossils: a reappraisal of early life on Earth. Res Microbiol 154 (9): 611–7.
- ↑ Cavalier-Smith T (2006). Cell evolution and Earth history: stasis and revolution. Philos Trans R Soc Lond B Biol Sci 361 (1470): 969–1006.
- ↑ Schopf J (1994). Disparate rates, differing fates: tempo and mode of evolution changed from the Precambrian to the Phanerozoic. Proc Natl Acad Sci USA 91 (15): 6735–42.
- ↑ Stanley S (May 1973). An Ecological Theory for the Sudden Origin of Multicellular Life in the Late Precambrian. Proc Natl Acad Sci USA 70 (5): 1486–9.
- ↑ DeLong E, Pace N (2001). Environmental diversity of bacteria and archaea. Syst Biol 50 (4): 470–8.
- ↑ Schmidt A, Ragazzi E, Coppellotti O, Roghi G (2006). A microworld in Triassic amber. Nature 444 (7121): 835.
- ↑ Wolska K (2003). Horizontal DNA transfer between bacteria in the environment. Acta Microbiol Pol 52 (3): 233–43.
- ↑ Enright M, Robinson D, Randle G, Feil E, Grundmann H, Spratt B (May 2002). The evolutionary history of methicillin-resistant Staphylococcus aureus (MRSA). Proc Natl Acad Sci USA 99 (11): 7687–92.
- ↑ Ciccarelli FD, Doerks T, von Mering C, Creevey CJ, Snel B, Bork P (2006). Toward automatic reconstruction of a highly resolved tree of life. Science 311 (5765): 1283–7.
- ↑ 16.0 16.1 Gold T (1992). The deep, hot biosphere. Proc. Natl. Acad. Sci. U.S.A. 89 (13): 6045–9.
- ↑ Whitman W, Coleman D, Wiebe W (1998). Prokaryotes: the unseen majority. Proc Natl Acad Sci USA 95 (12): 6578–83.
- ↑ Schulz H, Jorgensen B (2001). Big bacteria. Annu Rev Microbiol 55: 105–37.
- ↑ Eagon R (1962). Pseudomonas natriegens, a marine bacterium with a generation time of less than 10 minutes. J Bacteriol 83: 736–7.
- ↑ Woese C, Kandler O, Wheelis M (1990). Towards a natural system of organisms: proposal for the domains Archaea, Bacteria, and Eucarya. Proc Natl Acad Sci USA 87 (12): 4576–9.
- ↑ De Rosa M, Gambacorta A, Gliozzi A (1 March 1986). Structure, biosynthesis, and physicochemical properties of archaebacterial lipids. Microbiol. Rev. 50 (1): 70–80.
- ↑ Robertson C, Harris J, Spear J, Pace N (2005). Phylogenetic diversity and ecology of environmental Archaea. Curr Opin Microbiol 8 (6): 638–42.
- ↑ Karner MB, DeLong EF, Karl DM (2001). Archaeal dominance in the mesopelagic zone of the Pacific Ocean. Nature 409 (6819): 507–10.
- ↑ Sinninghe Damsté JS, Rijpstra WI, Hopmans EC, Prahl FG, Wakeham SG, Schouten S (June 2002). Distribution of membrane lipids of planktonic Crenarchaeota in the Arabian Sea. Appl. Environ. Microbiol. 68 (6): 2997–3002.
- ↑ Leininger S, Urich T, Schloter M, et al. (2006). Archaea predominate among ammonia-oxidizing prokaryotes in soils. Nature 442 (7104): 806–9.
- ↑ Eukaryota: More on Morphology. (Accessed 10 October 2006)
- ↑ 27.0 27.1 Dyall S, Brown M, Johnson P (2004). Ancient invasions: from endosymbionts to organelles. Science 304 (5668): 253–7.
- ↑ Cavalier-Smith T (1 December 1993). Kingdom protozoa and its 18 phyla. Microbiol. Rev. 57 (4): 953–94.
- ↑ Corliss JO (1992). Should there be a separate code of nomenclature for the protists?. BioSystems 28 (1-3): 1–14.
- ↑ Devreotes P (1989). Dictyostelium discoideum: a model system for cell-cell interactions in development. Science 245 (4922): 1054–8.
- ↑ Slapeta J, Moreira D, López-García P (2005). The extent of protist diversity: insights from molecular ecology of freshwater eukaryotes. Proc. Biol. Sci. 272 (1576): 2073–81.
- ↑ Moreira D, López-García P (2002). The molecular ecology of microbial eukaryotes unveils a hidden world. Trends Microbiol. 10 (1): 31–8.
- ↑ Lapinski J, Tunnacliffe A (2003). Anhydrobiosis without trehalose in bdelloid rotifers. FEBS Lett. 553 (3): 387–90.
- ↑ Kumamoto CA, Vinces MD (2005). Contributions of hyphae and hypha-co-regulated genes to Candida albicans virulence. Cell. Microbiol. 7 (11): 1546–54.
- ↑ Szewzyk U, Szewzyk R, Stenström T (1994). Thermophilic, anaerobic bacteria isolated from a deep borehole in granite in Sweden. Proc Natl Acad Sci USA 91 (5): 1810–3.
- ↑ Horneck G (1981). Survival of microorganisms in space: a review. Adv Space Res 1 (14): 39–48.
- ↑ Strain 121, a hyperthermophilic archaea, has been shown to reproduce at Template:Convert/LoffAoffDbSoffTTemplate:Convert/test/A, and survive at Template:Convert/LoffAoffDbSoffTTemplate:Convert/test/A.
- ↑ Some Psychrophilic bacteria can grow at Template:Convert/LoffAoffDbSoffTTemplate:Convert/test/A, and can survive near absolute zero.
- ↑ Picrophilus can grow at pH -0.06.
- ↑ The alkaliphilic bacteria Bacillus alcalophilus can grow at up to pH 11.5.
- ↑ Dyall-Smith, Mike, HALOARCHAEA, University of Melbourne. See also Haloarchaea.
- ↑ The piezophilic bacteria Halomonas salaria requires a pressure of 1,000 atm; nanobes, a speculative organism, have been reportedly found in the earth's crust at 2,000 atm.
- ↑ See Deinococcus radiodurans
- ↑ Cavicchioli R (2002). Extremophiles and the search for extraterrestrial life. Astrobiology 2 (3): 281–92.
- ↑ O'Hara A, Shanahan F (2006). The gut flora as a forgotten organ. EMBO Rep 7 (7): 688–93.
- ↑ Eckburg P, Lepp P, Relman D (2003). Archaea and their potential role in human disease. Infect Immun 71 (2): 591–6.
- ↑ Lepp P, Brinig M, Ouverney C, Palm K, Armitage G, Relman D (2004). Methanogenic Archaea and human periodontal disease. Proc Natl Acad Sci USA 101 (16): 6176–81.
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