Structure, function and stability of enzymes from the Archaea

Structural and genomic correlates of hyperthermostability

While most organisms grow at temperatures ranging between 20 and 50 degrees C, many archaea and a few bacteria have been found capable of withstanding temperatures close to 100 degrees C, or beyond, such as Pyrococcus or Aquifex. Here we report the results of two independent large scale unbiased approaches to identify global protein properties correlating with an extreme thermophile lifestyle. First, we performed a comparative proteome analyses using 30 complete genome sequences from the three kingdoms. A large difference between the proportions of charged versus polar (noncharged) amino acids was found to be a signature of all hyperthermophilic organisms. Second, we analyzed the water accessible surfaces of 189 protein structures belonging to mesophiles or hyperthermophiles. We found that the surfaces of hyperthermophilic proteins exhibited the shift already observed at the genomic level, i.e. a proportion of solvent accessible charged residues strongly increased at the expense of polar residues. The biophysical requirements for the presence of charged residues at the protein surface, allowing protein stabilization through ion bonds, is therefore clearly imprinted and detectable in all genome sequences available to date.

Primary structure determinants of the pH- and temperature-dependent aggregation of thioredoxin

Thioredoxins are small proteins found in all living organisms. We have previously reported that Chlamydomonas reinhardtii thioredoxin h exhibited differences both in its absorption spectrum and its aggregation properties compared to thioredoxin m. In this paper, we demonstrate, by site-directed mutagenesis, that the particularity of the absorption spectrum is linked to the presence of an additional tryptophan residue in the h isoform. The pH and temperature dependence of the aggregation of both thioredoxins has been investigated. Our results indicate that the aggregation of TRX is highly dependent on pH and that the differences between the two TRX isoforms are linked to distinct pH dependencies. We have also analyzed the pH and temperature dependence of 12 distinct variants of TRX engineered by site-directed mutagenesis. The results obtained indicate that the differences in the hydrophobic core of the two TRX isoforms do not account for the differences of aggregation. On the other hand, we show the importance of His-109 as well as the second active site cysteine, Cys-39 in the aggregation mechanism.

Stability and folding of the ferredoxin from the hyperthermophilic archaeon Acidianus ambivalens

The ferredoxin from the thermophilic archaeon Acidianus ambivalens is a small monomeric protein containing two iron-sulfur centres, one [3Fe-4S](1+/0) and one [4Fe-4S](2+/1+). It is an intrinsically hyperstable protein, being expressed at the organism's extreme optimal growth temperature: 80 degrees C. Using spectroscopic methods we have investigated the unfolding reaction of the Acidianus ambivalens ferredoxin. No unfolding of the oxidised ferredoxin was observed at pH 7.0, even in the presence of 8 M GuHCl. Upon increasing the pH to 10.0, the unfolding transition showed a midpoint at 6.3 M GuHCl and an unfolding-free energy of 70 kJ mol(-1) in buffer (pH 10) was estimated. Kinetic-unfolding experiments showed that the polypeptide unfolding correlated with rearrangement of the iron-sulfur centres to new ones which had strong absorption maxima at 520 and 610 nm. These new, possibly linear three-iron, clusters were coordinated to the unfolded protein but degraded slowly. From thermal experiments in the presence of GuHCl we estimated the melting temperature for the Acidianus ambivalens ferredoxin in buffer (at pH 7) to be 122 degrees C. Possible structural properties that contribute to the large thermal stability of the Acidianus ambivalens ferredoxin are discussed using a three-dimensional protein model.

Stress genes and proteins in the archaea

The field covered in this review is new; the first sequence of a gene encoding the molecular chaperone Hsp70 and the first description of a chaperonin in the archaea were reported in 1991. These findings boosted research in other areas beyond the archaea that were directly relevant to bacteria and eukaryotes, for example, stress gene regulation, the structure-function relationship of the chaperonin complex, protein-based molecular phylogeny of organisms and eukaryotic-cell organelles, molecular biology and biochemistry of life in extreme environments, and stress tolerance at the cellular and molecular levels. In the last 8 years, archaeal stress genes and proteins belonging to the families Hsp70, Hsp60 (chaperonins), Hsp40(DnaJ), and small heat-shock proteins (sHsp) have been studied. The hsp70(dnaK), hsp40(dnaJ), and grpE genes (the chaperone machine) have been sequenced in seven, four, and two species, respectively, but their expression has been examined in detail only in the mesophilic methanogen Methanosarcina mazei S-6. The proteins possess markers typical of bacterial homologs but none of the signatures distinctive of eukaryotes. In contrast, gene expression and transcription initiation signals and factors are of the eucaryal type, which suggests a hybrid archaeal-bacterial complexion for the Hsp70 system. Another remarkable feature is that several archaeal species in different phylogenetic branches do not have the gene hsp70(dnaK), an evolutionary puzzle that raises the important question of what replaces the product of this gene, Hsp70(DnaK), in protein biogenesis and refolding and for stress resistance. Although archaea are prokaryotes like bacteria, their Hsp60 (chaperonin) family is of type (group) II, similar to that of the eukaryotic cytosol; however, unlike the latter, which has several different members, the archaeal chaperonin system usually includes only two (in some species one and in others possibly three) related subunits of approximately 60 kDa. These form, in various combinations depending on the species, a large structure or chaperonin complex sometimes called the thermosome. This multimolecular assembly is similar to the bacterial chaperonin complex GroEL/S, but it is made of only the large, double-ring oligomers each with eight (or nine) subunits instead of seven as in the bacterial complex. Like Hsp70(DnaK), the archaeal chaperonin subunits are remarkable for their evolution, but for a different reason. Ubiquitous among archaea, the chaperonins show a pattern of recurrent gene duplication-hetero-oligomeric chaperonin complexes appear to have evolved several times independently. The stress response and stress tolerance in the archaea involve chaperones, chaperonins, other heat shock (stress) proteins including sHsp, thermoprotectants, the proteasome, as yet incompletely understood thermoresistant features of many molecules, and formation of multicellular structures. The latter structures include single- and mixed-species (bacterial-archaeal) types. Many questions remain unanswered, and the field offers extraordinary opportunities owing to the diversity, genetic makeup, and phylogenetic position of archaea and the variety of ecosystems they inhabit. Specific aspects that deserve investigation are elucidation of the mechanism of action of the chaperonin complex at different temperatures, identification of the partners and substitutes for the Hsp70 chaperone machine, analysis of protein folding and refolding in hyperthermophiles, and determination of the molecular mechanisms involved in stress gene regulation in archaeal species that thrive under widely different conditions (temperature, pH, osmolarity, and barometric pressure). These studies are now possible with uni- and multicellular archaeal models and are relevant to various areas of basic and applied research, including exploration and conquest of ecosystems inhospitable to humans and many mammals and plants.

Extremozymes

Extremozymes offer new opportunities for biocatalysis and biotransformations as a result of their extreme stability. From recent work, major approaches to extending the range of applications of extremozymes have emerged. Both the discovery of new extremophilic species and the determination of genome sequences provide a route to new enzymes, with the possibility that these will lead to novel applications. Of equal importance, protein engineering and directed evolution provide approaches to improve enzyme stability and modify specificity in ways that may not exist in the natural world.

Archaeal cold-adapted proteins: structural and evolutionary analysis of the elongation factor 2 proteins from psychrophilic, mesophilic and thermophilic methanogens

To identify structural features important for low temperature activity in archaeal proteins, elongation factor 2 (EF-2) genes (aef2) were sequenced from psychrophilic, mesophilic and thermophilic methanogens. Scatter plots were used to compare evolutionary distances for EF-2 amino acid sequences vs. 16S-rRNA sequences from methanogens growing at diverse temperatures. The absence of a temperature bias for the rate of protein vs. nucleic acid evolution demonstrated the importance of comparing closely related proteins in order to identify changes indicative of thermal adaptation. Three-dimensional modelling of the new EF-2 sequences enabled the identification of amino acid residues that may be important for conferring low temperature activity and included greater structural flexibility produced by fewer salt bridges, less packed hydrophobic cores and the reduction of proline residues in loop structures.