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The two-domain system is a biological classification by which all organisms in the tree of life are classified into two domains, Bacteria and Archaea. [ 1 ] [ 2 ] [ 3 ] It emerged from development of knowledge of archaea diversity and challenges the widely accepted three-domain system that classifies life into Bacteria, Archaea, and Eukarya . [ 4 ]
Traditionally, Archaea only included its prokaryotic members, but since this has been found to be paraphyletic, as eukaryotes are now known to have evolved from archaea. Even though the domain Archaea cladistically includes eukaryotes, the term "archaea" (sg.: archaeon / ɑːr ˈ k iː ɒ n / ar-KEE-on, from the Greek "ἀρχαῖον", which ...
Two kingdoms, Archaebacteria (archaea) and Eubacteria (for bacteria) were established. [22] Based on further studies, Woese, Otto Kandler and Mark Wheelis introduced the concept of "domain" in 1990 as the highest level of biological classification, and proposed the three-domain system consisting of Eucarya, Bacteria and Archaea. [23]
According to the domain system, the tree of life consists of either three domains, Archaea, Bacteria, and Eukarya, [1] or two domains, Archaea and Bacteria, with Eukarya included in Archaea. [3] [4] In the three-domain model, the first two are prokaryotes, single-celled microorganisms without a membrane-bound nucleus.
Archaea – a domain of single-celled microorganisms, morphologically similar to bacteria, but they possess genes and several metabolic pathways that are more closely related to those of eukaryotes, notably the enzymes involved in transcription and translation. Many archaea are extremophiles, which means living in harsh environments, such as ...
In 1990 Carl Woese et al. introduced the three-domain system. [35] [36] The prokaryotes were split into two domains, the archaea and the bacteria, while the eukaryotes become a domain in their own right. The key difference from earlier classifications is the splitting of archaea from bacteria.
Starting in 1985, researchers proposed that life arose at hydrothermal vents, [234] [235] that spontaneous chemistry in the Earth's crust driven by rock–water interactions at disequilibrium thermodynamically underpinned life's origin [236] [237] and that the founding lineages of the archaea and bacteria were H 2-dependent autotrophs that used ...
Pyrococcus furiosus is a strictly anaerobic, heterotrophic, sulfur-reducing archaea originally isolated from heated sediments in Vulcano, Italy by Fiala and Stetter. It is noted for its rapid doubling time of 37 minutes under optimal conditions, meaning that every 37 minutes the number of individual organisms is multiplied by two, yielding an exponential growth curve.