anaerobic
respiration used by some Halobacterium species with
nitrate, sulfur, thiosulfate as terminal electron
acceptors
ATP synthesized by other Halobacterium species
using a light-mediated bacteriorhodopsin/retinal system
Hypersaline aquatic environments with alkaline pH
such as Great Salt Lake, Dead Sea, solar salt evaporating ponds
(salterns) and salted fish, are the normal habitat for these
Archaea
Methanogens
Gram-negative or Gram-positive - some have
pseudopeptidoglycan, some have protein, some have
polysaccharide cell walls; coenzyme F420 fluorescence used for
identification of methanogens; 3 orders and 13 genera based on
16S rRNA structure
long (Methanobacterium,
Methanothrix) or short (Methanobrevibacter)
rods (0.5-1 µm wide) that occur as very long
filaments
cocci (1.5-2.5 µm) that occur in singlets
(Methanococcus), aggregates (Methanolobus),
packets (Methanosarcina), or chains
(Methanopyrus)
spirals (Methanospirillum)
plate-shaped (Methanoplanus)
Strictlyanaerobic, fastidious (require
vitamins, amino acids, nickel {part of coenzyme F430,
hydrogenase, carbon monoxide dehydrogenase}, iron, cobalt);
Methanopyrus is an extreme thermophile; no known
methanogens have a complete TCA cycle; some can fix nitrogen
lithotrophs
- generate methane using hydrogen and carbon dioxide that is
fixed via a reductive acetyl-CoA pathway
(Methanobacterium, Methanothermus,
Methanococcus, Methanogenium,
Methanoplanus)
organotrophs - generate methane from methyl
groups of formate, methanol (Methanosphaera,
Methanosarcina, Methanococcoides) or acetate
(Methanothrix, Methanosaeta)
Environments rich in organic matter such as
anaerobic sewage digestors, anoxic freshwater sediments and the
rumen of cattle are normal habitats for these Archaea; they are
very important as sources of methane (natural gas)
Extreme Thermophiles
Gram-negative
rods (Methanopyrus, Thermoproteus)
disc-shapes (Thermodiscus)
filaments (Thermofilum)
irregular (lobate) spheres 0.8-1 µm in diameter
(Sulfolobus)
spheres that are motile via lophotrichous flagella
(Thermococcus, Pyrococcus,
Staphylothermus)
Obligateanaerobes that require
temperatures above 50C for growth (sometimes higher than
70C) and use sulfur as electron acceptor (except Sulfolobus,
which uses oxygen or ferric iron)
organotrophs - use a modified Entner-Duodoroff
pathway to oxidize organic compounds for energy (oxygen or
sulfur serves as final electron acceptor)
organic compound + S
H2S + CO2 (Thermococcus,
Thermoproteus, Desulfurococcus,
Thermofilum, Pyrococcus)
organic compound + O2
H2O + CO2 (Sulfolobus)
organic compound
CO2 + fatty acids
(Staphylothermus)
organic compound
CO2 + H2 (Pyrococcus)
lithotrophs - can also grow organotrophically
using sulfur as an electron acceptor (see above)
Methanopyrus - oxidizes hydrogen for energy (4
H2 + carbon dioxide yields methane + 2 water)
and fixes carbon dioxide at the same time (thermophilic
methanogen)
Pyrodictium - optimum temperature, 105C; uses
hydrogen as energy source, sulfur as electron acceptor
(H2 + S
H2S) and carbon dioxide as carbon source (via
a reverse (reductive) acetyl-CoA pathway)
Sulfolobus - optimum temperature for growth,
70-80C; requires a pH of 2-3; aerobically oxidizes sulfur
(2 S + 3 O2 + 2 H2O
2 H2SO4) and ferrous iron (4 FeS +
15 oxygen + 2 water
2 Fe2(SO4)3 + 2
H2SO4) for energy; fixes carbon
dioxide via a reverse (reductive) TCA cycle much like
that seen in green sulfur bacteria
Thermoproteus - grows at 78-96C, pH 1.7-6.5;
uses hydrogen as energy source, sulfur as electron
acceptor (H2 + S
H2S) and carbon dioxide as carbon source
Geothermally heated, acidic soils or waters which
contain sulfur (solfatara), such as those in Yellowstone
National Park and near marine hydrothermal vents are the usual
habitats for these Archaea
Sulfate Reducers
(Archaeoglobus)
Irregular, motile spheres
Thermophilic (83C is optimum), methanogenic,
anaerobes which extract electrons from hydrogen,
lactate, glucose, etc. and reduce sulfate, sulfite, or
thiosulfate to sulfide
High-temperature, sulfate-containing environments
such as marine hydrothermal vents are the usual habitats for
these Archaea
Wall-Less Archaea
(Thermoplasma)
No cell wall (resemble Mycoplasmas)
single triple-layered membrane that contains
glycoproteins plus lipopolysaccharide consisting of
tetraether lipid with mannose and glucose
irregular filamentous shape at or above 59C, spherical
(0.3-2 µm) below 59C
very small genome, with DNA surrounded by histone-like
DNA-binding proteins
budding is mode of reproduction
Acidophilic thermophilic aerobic organotroph
Coal refuse piles which are heated and made acidic
by (other) lithotrophic bacteria which oxidize iron pyrite
(FeS) to sulfuric acid are the only habitats in which these
Archaea are found in nature
Crenarchaeota
most are extreme
thermophiles with growth optima at temperatures greater
than 80C and many of these are anaerobic lithotrophs
(Pyrodictium), organolithotrophs or
organotrophs (Thermococcus, Thermoproteus) that
require elemental sulfur for optimal growth
(Desulfurococcus)
Sulfolobus is an aerobic organolithotroph
there are also a number of as yet unidentified marine
crenarchaeotes, including some cryophiles
Korarchaeota
newly discovered extreme thermophiles
these are the most primitive life forms discovered to
date