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单词 archaebacteria
释义

archaebacteria

enUK

ar·chae·bac·te·ri·um

A0403750 (är′kē-băk-tîr′ē-əm)n. pl. ar·chae·bac·te·ri·a See archaeon.
[archae(o)- + bacterium.]

archaebacteria

(ˌɑːkɪbækˈtɪərɪə) pl n, sing -rium (-rɪəm) (Microbiology) (formerly) a group of microorganisms now regarded as members of the Archaea. See archaean[from archaeo- + bacteria]

ar•chae•bac•te•ri•a

(ˌɑr ki bækˈtɪər i ə)

also ar•chae•o•bac•te•ri•a

(ˌɑr ki oʊ-)

n.pl., sing. -te•ri•um (-ˈtɪər i əm) a group of microorganisms, including methanogens and halobacteria, that are genetically and functionally different from all other living forms, thrive in oxygen-poor environments, and are sometimes classified as a separate kingdom. [1977; < New Latin, =archae-, irreg. for archaeo- archaeo- (perhaps an erroneous Latinizing of Greek arche- arche-) + bacteria bacteria]
Thesaurus
Noun1.archaebacteria - considered ancient life forms that evolved separately from bacteria and blue-green algaearchaebacteria - considered ancient life forms that evolved separately from bacteria and blue-green algaearchaebacterium, archaeobacteria, archeobacteriamoneran, moneron - organisms that typically reproduce by asexual budding or fission and whose nutritional mode is absorption or photosynthesis or chemosynthesisdivision Archaebacteria - in some classifications considered a kingdommethanogen - archaebacteria found in anaerobic environments such as animal intestinal tracts or sediments or sewage and capable of producing methane; a source of natural gashalophil, halophile - archaebacteria requiring a salt-rich environment for growth and survivalthermoacidophile - archaebacteria that thrive in strongly acidic environments at high temperatures

Archaebacteria

enUK

Archaebacteria

(är'kēbăktĭr`ēə), diverse group of bacteriabacteria
[pl. of bacterium], microscopic unicellular prokaryotic organisms characterized by the lack of a membrane-bound nucleus and membrane-bound organelles. Once considered a part of the plant kingdom, bacteria were eventually placed in a separate kingdom, Monera.
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 (prokaryotes), sometimes called the archaea and considered a major group unto themselves. Archaebacteria are contrasted with the Eubacteria, from which they differ biochemically in the arrangement of the bases in their ribosomal RNA and in the composition of their plasma membranes and cell walls. There are three major known groups of Archaebacteria: methanogens, halophiles, and thermophiles. The methanogens are anaerobic bacteria that produce methane. They are found in sewage treatment plants, bogs, and the intestinal tracts of ruminants. Ancient methanogens are the source of natural gas. Halophiles are bacteria that thrive in high salt concentrations such as those found in salt lakes or pools of sea water. Thermophiles are the heat-loving bacteria found near hydrothermal vents and hot springs. Many thermophiles are chemosynthetic (see chemosynthesischemosynthesis,
process in which carbohydrates are manufactured from carbon dioxide and water using chemical nutrients as the energy source, rather than the sunlight used for energy in photosynthesis. Much life on earth is fueled directly or indirectly by sunlight.
..... Click the link for more information.
), using dissolved sulfur or other elements as their energy source and iron as a means of respiration. Archaebacteria emerged at least 3.5 billion years ago and live in environments that resemble conditions existing when the earth was young.

Archaebacteria

A group of prokaryotic organisms that are more closely related to eukaryotes than bacteria. Based on comparative analyses of small subunit ribosomal ribonucleic acid (rRNA) sequences and selected protein sequences, the three primary lines of descent from the common ancestor are the Archaea (archaebacteria), the Bacteria, and the Eucarya (eukaryotes). Although the Archaea look like Bacteria cytologically (they are both prokaryotes), they are not closely related to them.

The Archaea can be divided into two evolutionary lineages on the basis of rRNA sequence comparisons, the Crenarchaeotae and the Euryarchaeotae. The crenarchaeotes are organisms that grow at high temperatures (thermophiles) and metabolize elemental sulfur. Most are strict anaerobes that reduce sulfur to hydrogen sulfide (sulfidogens), but a few can grow aerobically and oxidize sulfur to sulfuric acid. The euryarchaeotes have a number of different phenotypes. Thermococcus and Pyrococcus are sulfidogens like many crenarchaeotes. Archaeoglobus reduces sulfate to sulfide. Thermoplasma grows under acidic conditions aerobically or anaerobically (as a sulfidogen). Many euryarchaeotes are methane-producing anaerobes (methanogens) and some grow aerobically in the presence of very high concentrations of salt (halophiles). See Methanogenesis (bacteria)

The thermophilic archaea are found in high-temperature environments around the world. They have been isolated from soils and shallow marine sediments heated by nearby volcanoes and from deep-sea hydrothermal vents. Some are used as a source for heat-stable enzymes useful for industrial applications. The methanogenic archaea inhabit the digestive tracts of animals (especially ruminants like cows), sewage sludge digesters, swamps (where they produce marsh gas), and sediments of marine and fresh-water environments. They are of interest commercially because of their ability to produce methane from municipal garbage and some industrial wastes. Halophilic archaea live in the Great Salt Lake, the Dead Sea, alkaline salt lakes of Africa, and salt-preserved fish and animal hides. They are also commonly found in pools used to evaporate seawater to obtain salt.

The discovery of the Archaea caused a major revision in the understanding of evolutionary history. It had previously been thought that all prokaryotes belonged to one evolutionary lineage. Since their cellular organization is simpler, prokaryotes were assumed to be ancestors of eukaryotes. The discovery of the relationship of the Archaea to the Eucarya revealed that prokaryotes do not comprise a monophyletic group since they can be divided into two distinct lineages. Although the three descended from a common ancestor, modern eukaryotes may have arisen from fusions of bacterial and archaeal endosymbionts with ancestral eukaryotes. Chloroplasts and mitochondria arose from free-living bacteria which became endosymbionts. The discovery of the Archaea has also given microbiologists a better picture of the common ancestor. The deepest-branching eukaryotes (like Giardia) are strict anaerobes that lack mitochondria, and they diverged much later than the deepest-branching bacteria and archaea. The earliest archaea and bacteria (Thermotoga and Aquifex) are also anaerobes and are also extreme thermophiles. Therefore the common ancestor of these groups was probably also an extremely thermophilic anaerobe. Therefore, it is possible that life may have arisen in a relatively hot environment, perhaps like that found in deep-sea hydrothermal vents. See Bacteria, Eukaryotae, Prokaryotae

archaebacteria

[‚ar·kē·bak′tir·ē·ə] (microbiology) A group of unusual prokaryotic organisms that microscopically resemble true bacteria but differ biochemically and genetically, and form a distinct evolutionary group; some occur widely in oxygen-free environments and produce methane, while others are found in extreme salty or acidic conditions or grow at high temperatures.

Archaebacteria

enUK

Archaea

Evolutionary biology
One of the three domains of living organisms: Archaea, Bacteria and Eukaryota. While Archaea are single-celled, they are unlike bacteria given their independent evolutionary history. Archaea differ from Eukaryota in their ribosomal structure and the presence—in some—of introns in the genome, as well as other features (e.g., different membrane composition).
 
Molecular biology
Archaea are of interest in biotechnology as they have unique biochemical features (e.g., enzymes of theromophiles, such as Taq polymerase, the “workhorse” enzyme of PCR) and are extremely stable at high temperatures. Archaea include metabolic oddities (e.g., extreme halophiles, which live in extremely salty environments), methanogens (which produce methane) and sulphur-dependant extreme thermophiles (which can live in extremely hot environments).
Archaea phyla
• Crenarchaeota
• Euryarchaeota
• Korarchaeota
• Nanoarchaeota
• Thaumarchaeota (recently proposed)

ar·chae·bac·ter·i·a

(ahr'kē-bak-tēr'ē-ā) A group of microorganisms that thrive in the absence of oxygen, produce methane, and live only in bodies of highly concentrated salt water, or in the acidic waters of sulfur springs, at temperatures near 80° Celsius and pH levels as low as 2.

Archaebacteria)

one of the three primary groupings (DOMAINS) of ORGANISMS, according to some classification schemes, based on genetic structures and sequences. See CLASSIFICATION. Members of the Archaea are PROKARYOTES and include the extreme HALOPHILES, the thermoacidophiles (organisms that normally grow at high temperatures in acidic environments; see also THERMOPHILIC), and the METHANOGENS.

They differ in a number of ways from other BACTERIA, for example in the structure of their MEMBRANE LIPIDS, TRANSFER RNA molecules and CELL WALL, and in their sensitivity to ANTIBIOTICS. The Archaea is a very diverse group organized into two KINGDOMS, the CRENARCHAEOTA and the EURYARCHAEOTA. It was initially considered to represent the most ancient group of organisms still living. This is reflected in the name, from the Greek archaios, meaning ancient.

archaebacteria

enUK
  • noun

Synonyms for archaebacteria

noun considered ancient life forms that evolved separately from bacteria and blue-green algae

Synonyms

  • archaebacterium
  • archaeobacteria
  • archeobacteria

Related Words

  • moneran
  • moneron
  • division Archaebacteria
  • methanogen
  • halophil
  • halophile
  • thermoacidophile
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