Thermoproteota

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Thermoproteota
RT8-4.jpg
Archaea Sulfolobus infected with specific virus STSV-1.
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Archaea
Kingdom: Proteoarchaeota
Superphylum: TACK group
Phylum: Thermoproteota
Garrity & Holt 2021 [1]
Class
Synonyms
  • "Eocyta" Lake et al. 1984
    This also applies to TACK group
  • "Crenarchaeota" Garrity and Holt 2001
  • "Gearchaeota" corrig. Kozubal et al. 2013
  • "Marsarchaeota" Jay et al. 2018
  • "Nezhaarchaeota" Wang et al. 2019
  • "Thermoproteaeota" Oren et al. 2015
  • "Thermoproteota" Whitman et al. 2018
  • "Verstraetearchaeota" Vanwonterghem et al. 2016

The Thermoproteota are prokaryotes that have been classified as a phylum of the domain Archaea. [2] [3] [4] Initially, the Thermoproteota were thought to be sulfur-dependent extremophiles but recent studies have identified characteristic Thermoproteota environmental rRNA indicating the organisms may be the most abundant archaea in the marine environment. [5] Originally, they were separated from the other archaea based on rRNA sequences; other physiological features, such as lack of histones, have supported this division, although some crenarchaea were found to have histones. [6] Until 2005 all cultured Thermoproteota had been thermophilic or hyperthermophilic organisms, some of which have the ability to grow at up to 113 °C. [7] These organisms stain Gram negative and are morphologically diverse, having rod, cocci, filamentous and oddly-shaped cells. [8] Recent evidence shows that some members of the Thermoproteota are methanogens.

Contents

Thermoproteota were initially classified as a part of Regnum Eocyta in 1984, [9] but this classification has been discarded. The term "eocyte" now applies to either TACK (formerly Crenarchaeota) or to Thermoproteota.

Sulfolobus

One of the best characterized members of the Crenarchaeota is Sulfolobus solfataricus . This organism was originally isolated from geothermally heated sulfuric springs in Italy, and grows at 80 °C and pH of 2–4. [10] Since its initial characterization by Wolfram Zillig, a pioneer in thermophile and archaean research, similar species in the same genus have been found around the world. Unlike the vast majority of cultured thermophiles, Sulfolobus grows aerobically and chemoorganotrophically (gaining its energy from organic sources such as sugars). These factors allow a much easier growth under laboratory conditions than anaerobic organisms and have led to Sulfolobus becoming a model organism for the study of hyperthermophiles and a large group of diverse viruses that replicate within them.

16S rRNA based LTP_06_2022 [11] [12] [13] 53 marker proteins based GTDB 09-RS220 (24 April 2024) [14] [15] [16]
"TACK"
"TACK"
"JANJXX01"

"Panguiarchaeales"

"Korarchaeia"

"Korarchaeales"

"BAT"
"Bathyarchaeia"

"Bifangarchaeales" [B24]

"Hecatellales" [B25]

"Xuanwuarculales" [RBG-16-48-13]

"Houtuarculales" [40CM-2-53-6]

"Wuzhiqiibiales" [TCS64]

"Zhuquarculales" [EX4484-135]

"Bathyarchaeales" [B26-1]

(MCG)
Nitrososphaeria_A

"Caldarchaeales"

Nitrososphaeria

"Geothermarchaeales"

Conexivisphaerales

Nitrososphaerales

"Sulfobacteria"
"Methanomethylicia"
("Verstraetearchaeota")
"Thermoproteia"

"Gearchaeales"

Thermofilales

Thermoproteales

Thermoproteota

Recombinational repair of DNA damage

Irradiation of S. solfataricus cells with ultraviolet light strongly induces formation of type IV pili that can then promote cellular aggregation. [17] Ultraviolet light-induced cellular aggregation was shown by Ajon et al. [18] to mediate high frequency inter-cellular chromosome marker exchange. Cultures that were ultraviolet light-induced had recombination rates exceeding those of uninduced cultures by as much as three orders of magnitude. S. solfataricus cells are only able to aggregate with other members of their own species. [18] Frols et al. [17] [19] and Ajon et al. [18] considered that the ultraviolet light-inducible DNA transfer process, followed by homologous recombinational repair of damaged DNA, is an important mechanism for promoting chromosome integrity.

This DNA transfer process can be regarded as a primitive form of sexual interaction.

Marine species

Beginning in 1992, data were published that reported sequences of genes belonging to the Thermoproteota in marine environments. [20] , [21] Since then, analysis of the abundant lipids from the membranes of Thermoproteota taken from the open ocean have been used to determine the concentration of these “low temperature Crenarchaea” (See TEX-86). Based on these measurements of their signature lipids, Thermoproteota are thought to be very abundant and one of the main contributors to the fixation of carbon .[ citation needed ] DNA sequences from Thermoproteota have also been found in soil and freshwater environments, suggesting that this phylum is ubiquitous to most environments. [22]

In 2005, evidence of the first cultured “low temperature Crenarchaea” was published. Named Nitrosopumilus maritimus , it is an ammonia-oxidizing organism isolated from a marine aquarium tank and grown at 28 °C. [23]

Possible connections with eukaryotes

The research about two-domain system of classification has paved the possibilities of connections between crenarchaea and eukaryotes. [24]

DNA analysis from 2008 (and later, 2017) has shown that eukaryotes possible evolved from thermoproteota-like organisms. Other candidates for the ancestor of eukaryotes include closely related asgards. This could suggest that eukaryotic organisms possibly evolved from prokaryotes.

These results are similar to the eocyte hypothesis of 1984, proposed by James A. Lake. [9] The classification according to Lake, states that both crenarchaea and asgards belong to Kingdom Eocyta. Though this has been discarded by scientists, the main concept remains. The term "Eocyta" now either refers to the TACK group or to Phylum Thermoproteota itself.

However, the topic is highly debated and research is still going on.

See also

Related Research Articles

<span class="mw-page-title-main">Nanoarchaeota</span> Phylum of archaea

Nanoarchaeota is a proposed phylum in the domain Archaea that currently has only one representative, Nanoarchaeum equitans, which was discovered in a submarine hydrothermal vent and first described in 2002.

<span class="mw-page-title-main">Korarchaeota</span> Proposed phylum within the Archaea

The Korarchaeota is a proposed phylum within the Archaea. The name is derived from the Greek noun koros or kore, meaning young man or young woman, and the Greek adjective archaios which means ancient. They are also known as Xenarchaeota. The name is equivalent to Candidatus Korarchaeota, and they go by the name Xenarchaeota or Xenarchaea as well.

The Thermoprotei is a class of the Thermoproteota.

Mollicutes is a class of bacteria distinguished by the absence of a cell wall. The word "Mollicutes" is derived from the Latin mollis, and cutis. Individuals are very small, typically only 0.2–0.3 μm in size and have a very small genome size. They vary in form, although most have sterols that make the cell membrane somewhat more rigid. Many are able to move about through gliding, but members of the genus Spiroplasma are helical and move by twisting. The best-known genus in the Mollicutes is Mycoplasma. Colonies show the typical "fried-egg" appearance.

<i>Sulfolobus</i> Genus of archaea

Sulfolobus is a genus of microorganism in the family Sulfolobaceae. It belongs to the archaea domain.

Halobacteriaceae is a family in the order Halobacteriales and the domain Archaea. Halobacteriaceae represent a large part of halophilic Archaea, along with members in two other methanogenic families, Methanosarcinaceae and Methanocalculaceae. The family consists of many diverse genera that can survive extreme environmental niches. Most commonly, Halobacteriaceae are found in hypersaline lakes and can even tolerate sites polluted by heavy metals. They include neutrophiles, acidophiles, alkaliphiles, and there have even been psychrotolerant species discovered. Some members have been known to live aerobically, as well as anaerobically, and they come in many different morphologies. These diverse morphologies include rods in genus Halobacterium, cocci in Halococcus, flattened discs or cups in Haloferax, and other shapes ranging from flattened triangles in Haloarcula to squares in Haloquadratum, and Natronorubrum. Most species of Halobacteriaceae are best known for their high salt tolerance and red-pink pigmented members, but there are also non-pigmented species and those that require moderate salt conditions. Some species of Halobacteriaceae have been shown to exhibit phosphorus solubilizing activities that contribute to phosphorus cycling in hypersaline environments. Techniques such as 16S rRNA analysis and DNA–DNA hybridization have been major contributors to taxonomic classification in Halobacteriaceae, partly due to the difficulty in culturing halophilic Archaea.

Methanococcus is a genus of coccoid methanogens of the family Methanococcaceae. They are all mesophiles, except the thermophilic M. thermolithotrophicus and the hyperthermophilic M. jannaschii. The latter was discovered at the base of a “white smoker” chimney at 21°N on the East Pacific Rise and it was the first archaeal genome to be completely sequenced, revealing many novel and eukaryote-like elements.

<span class="mw-page-title-main">Thermococci</span> Class of archaea

In taxonomy, the Thermococci are a class of microbes within the Euryarchaeota.

<span class="mw-page-title-main">Methanomicrobia</span> Class of archaea

In the taxonomy of microorganisms, the Methanomicrobia are a class of the Euryarchaeota.

In the taxonomy of microorganisms, the Methanomicrobiales are an order of the Methanomicrobia. Methanomicrobiales are strictly carbon dioxide reducing methanogens, using hydrogen or formate as the reducing agent. As seen from the phylogenetic tree based on 'The All-Species Living Tree' Project the family Methanomicrobiaceae is highly polyphyletic within the Methanomicrobiales.

<span class="mw-page-title-main">Sulfolobales</span> Order of archaea

Sulfolobales is an order of archaeans in the class Thermoprotei.

<span class="mw-page-title-main">Thermococcales</span> Order of archaea

In taxonomy, the Thermococcales are an order of microbes within the Thermococci. The species within the Thermococcales are used in laboratories as model organisms. All these species are strict anaerobes and can ferment sugars as sources of carbon, but they also need elemental sulfur.

Thermoproteales are an order of archaeans in the class Thermoprotei. They are the only organisms known to lack the SSB proteins, instead possessing the protein ThermoDBP that has displaced them. The rRNA genes of these organisms contain multiple introns, which can be homing endonuclease encoding genes, and their presence can impact the binding of "universal" 16S rRNA primers often used in environmental sequencing surveys.

In taxonomy, the Methanocorpusculaceae are a family of microbes within the order Methanomicrobiales. It contains exactly one genus, Methanocorpusculum. The species within Methanocorpusculum were first isolated from anaerobic digesters and anaerobic wastewater treatment plants. In the wild, they prefer freshwater environments. Unlike many other methanogenic archaea, they do not require high temperatures or extreme salt concentrations to live and grow.

Methanomicrobiaceae are a family of archaea in the order the Methanomicrobiales.

<span class="mw-page-title-main">Methanosarcinaceae</span> Family of archaea

In taxonomy, the Methanosarcinaceae are a family of the Methanosarcinales.

Methanospirillaceae are a family of microbes within Methanomicrobiales.

Methanocalculus is a genus of the Methanomicrobiales, and is known to include methanogens.

In the taxonomy of microorganisms, Candidatus Methanoregula is a genus of the Methanomicrobiales. It was isolated from an acidic peat bog. It produces methane at the lowest pH of any known organism.

Saccharolobus solfataricus is a species of thermophilic archaeon. It was transferred from the genus Sulfolobus to the new genus Saccharolobus with the description of Saccharolobus caldissimus in 2018.

References

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