Microorganisms that can grow at and above 100-degrees-C were discovere
d a decade ago, and about 20 different genera are now known. These so-
called hyperthermophiles are the most ancient of all extant life; all
but two genera are classified as Archaea. All have been isolated from
geothermal heated environments including deep-sea hydrothermal vents.
This group includes some methanogenic and sulfate-reducing species, bu
t the majority are strictly anaerobic heterotrophs that utilize comple
x peptide mixtures as sources of energy, carbon, and nitrogen. Only a
few species are saccharolytic. Most of the hyperthermophiles absolutel
y depend on the reduction of elemental sulfur (S0) to H2S for signific
ant growth, a property that severely limits their large-scale culture
in conventional fermentation systems. Consequently, most physiological
and metabolic studies have focused on those that can also grow in the
absence of S0, including species of the Archaea, Pyrococcus and Therm
ococcus, and the bacterium Thermotoga. The fermentative pathways for t
he metabolism of both peptides and carbohydrates in the Archaea appear
to depend upon enzymes that contain tungsten, an element seldom used
in biological systems. The mechanisms of S0 reduction and energy conse
rvation remain unclear. Enzymes purified from the S0-reducing hyperthe
rmophiles include proteases, amylolytic-type enzymes, hydrogenases, re
dox proteins, various ferredoxin-linked oxidoreductases, dehydrogenase
s, and DNA polymerases, some of which are active up to 140-degrees-C.
However, complete amino acid sequences are known for only a handful of
these proteins, and the three-dimensional structure of only one hyper
thermophilic protein has been determined. Potential mechanisms by whic
h proteins and various biological cofactors and organic intermediates
are stabilized at extreme temperatures are only now beginning to emerg
e.