Chaperonins from an Antarctic archaeon are predominantly monomeric: crystal structure of an open state monomer.

Archaea are abundant in permanently cold environments. The Antarctic methanogen, Methanococcoides burtonii, has proven an excellent model for studying molecular mechanisms of cold adaptation. Methanococcoides burtonii contains three group II chaperonins that diverged prior to its closest orthologues from mesophilic Methanosarcina spp. The relative abundance of the three chaperonins shows little dependence on organism growth temperature, except at the highest temperatures, where the most thermally stable chaperonin increases in abundance. In vitro and in vivo, the M. burtonii chaperonins are predominantly monomeric, with only 23-33% oligomeric, thereby differing from other archaea where an oligomeric ring form is dominant. The crystal structure of an N-terminally truncated chaperonin reveals a monomeric protein with a fully open nucleotide binding site. When compared with closed state group II chaperonin structures, a large-scale ≈ 30° rotation between the equatorial and intermediate domains is observed resulting in an open nucleotide binding site. This is analogous to the transition observed between open and closed states of group I chaperonins but contrasts with recent archaeal group II chaperonin open state ring structures. The predominance of monomeric form and the ability to adopt a fully open nucleotide site appear to be unique features of the M. burtonii group II chaperonins.

The RNA polymerase subunits E/F from the Antarctic archaeon Methanococcoides burtonii bind to specific species of mRNA.

RNA polymerase in Archaea is composed of 11 or 12 subunits - 9 or 10 that form the core, and a heterodimer formed from subunits E and F that associates with the core and can interact with general transcription factors and facilitate transcription. While the ability of the heterodimer to bind RNA has been demonstrated, it has not been determined whether it can recognize specific RNA targets. In this study we used a recombinant archaeal MbRpoE/F to capture cellular mRNA in vitro and a microarray to determine which transcripts it specifically binds. Only transcripts for 117 genes (4% of the total) representing 48 regions of the genome were bound by MbRpoE/F. The transcripts represented important genes in a number of functional classes: methanogenesis, cofactor biosynthesis, nucleotide metabolism, transcription, translation, import/export. The arrangement and characteristics (e.g. codon and amino acid usage) of genes relative to the putative origin of replication indicate that MbRpoE/F preferentially binds to mRNA of genes whose expression may be important for cellular fitness. We also compared the biophysical properties of RpoE/F from M. burtonii and Methanocaldococcus jannaschii, demonstrating a 50°C difference in their apparent melting temperatures. By using MbRpoE/F to capture and characterize cellular RNA we have identified a previously unknown functional property of the MbRpoE/F heterodimer.

A chemically modified alpha-amylase with a molten-globule state has entropically driven enhanced thermal stability.

The thermostability properties of TAA were investigated by chemically modifying carboxyl groups on the surface of the enzyme with AMEs. The TAA(MOD) exhibited a 200% improvement in starch-hydrolyzing productivity at 60 degrees C. By studying the kinetic, thermodynamic and biophysical properties, we found that TAA(MOD) had formed a thermostable, MG state, in which the unfolding of the tertiary structure preceded that of the secondary structure by at least 20 degrees C. The X-ray crystal structure of TAA(MOD) revealed no new permanent interactions (electrostatic or other) resulting from the modification. By deriving thermodynamic activation parameters of TAA(MOD), we rationalised that thermostabilisation have been caused by a decrease in the entropy of the transition state, rather than being enthalpically driven. Far-UV CD shows that the origin of decreased entropy may have arisen from a higher helical content of TAA(MOD). This study provides new insight into the intriguing properties of an MG state resulting from the chemical modification of TAA.

Global proteomic analysis of the insoluble, soluble, and supernatant fractions of the psychrophilic archaeon Methanococcoides burtonii. Part I: the effect of growth temperature.

The response of the cold-adapted (psychrophilic) methanogenic archaeon Methanococcoides burtonii to growth temperature was investigated using differential proteomics (postincorporation isobaric labeling) and tandem liquid chromatography-mass spectrometry (LC/LC-MS/MS). This is the first proteomic study of M. burtonii to include techniques that specifically enrich for both surface and membrane proteins and to assess the effects of growth temperature (4 vs 23 degrees C) and carbon source (trimethylamine vs methanol) on cellular protein levels. Numerous surface layer proteins were more abundant at 4 degrees C, indicating an extensive remodeling of the cell envelope in response to low temperature. Many of these surface proteins contain domains associated with cell adhesion. Within the cell, small proteins each composed of a single TRAM domain were recovered as important cold adaptation proteins and might serve as RNA chaperones, in an analogous manner to Csp proteins (absent from M. burtonii). Other proteins that had higher abundances at 4 degrees C can be similarly tied to relieving or resolving the adverse affects of cold growth temperature on translational capacity and correct protein folding. The proteome of M. burtonii grown at 23 degrees C was dominated by oxidative stress proteins, as well as a large number of integral membrane proteins of unknown function. This is the first truly global proteomic study of a psychrophilic archaeon and greatly expands knowledge of the cellular mechanisms underpinning cold adaptation in the Archaea.

The genome sequence of the psychrophilic archaeon, Methanococcoides burtonii: the role of genome evolution in cold adaptation.

Psychrophilic archaea are abundant and perform critical roles throughout the Earth's expansive cold biosphere. Here we report the first complete genome sequence for a psychrophilic methanogenic archaeon, Methanococcoides burtonii. The genome sequence was manually annotated including the use of a five-tiered evidence rating (ER) system that ranked annotations from ER1 (gene product experimentally characterized from the parent organism) to ER5 (hypothetical gene product) to provide a rapid means of assessing the certainty of gene function predictions. The genome is characterized by a higher level of aberrant sequence composition (51%) than any other archaeon. In comparison to hyper/thermophilic archaea, which are subject to selection of synonymous codon usage, M. burtonii has evolved cold adaptation through a genomic capacity to accommodate highly skewed amino-acid content, while retaining codon usage in common with its mesophilic Methanosarcina cousins. Polysaccharide biosynthesis genes comprise at least 3.3% of protein coding genes in the genome, and Cell wall, membrane, envelope biogenesis COG genes are overrepresented. Likewise, signal transduction (COG category T) genes are overrepresented and M. burtonii has a high 'IQ' (a measure of adaptive potential) compared to many methanogens. Numerous genes in these two overrepresented COG categories appear to have been acquired from epsilon- and delta-Proteobacteria, as do specific genes involved in central metabolism such as a novel B form of aconitase. Transposases also distinguish M. burtonii from other archaea, and their genomic characteristics indicate they have an important role in evolving the M. burtonii genome. Our study reveals a capacity for this model psychrophile to evolve through genome plasticity (including nucleotide skew, horizontal gene transfer and transposase activity) that enables adaptation to the cold, and to the biological and physical changes that have occurred over the last several thousand years as it adapted from a marine to an Antarctic lake environment.

The crystal structure of C176A mutated [Fe]-hydrogenase suggests an acyl-iron ligation in the active site iron complex.

[Fe]-hydrogenase is one of three types of enzymes known to activate H(2). Crystal structure analysis recently revealed that its active site iron is ligated square-pyramidally by Cys176-sulfur, two CO, an "unknown" ligand and the sp(2)-hybridized nitrogen of a unique iron-guanylylpyridinol-cofactor. We report here on the structure of the C176A mutated enzyme crystallized in the presence of dithiothreitol (DTT). It suggests an iron center octahedrally coordinated by one DTT-sulfur and one DTT-oxygen, two CO, the 2-pyridinol's nitrogen and the 2-pyridinol's 6-formylmethyl group in an acyl-iron ligation. This result led to a re-interpretation of the iron ligation in the wild-type.

The crystal structure of [Fe]-hydrogenase reveals the geometry of the active site.

Biological formation and consumption of molecular hydrogen (H2) are catalyzed by hydrogenases, of which three phylogenetically unrelated types are known: [NiFe]-hydrogenases, [FeFe]-hydrogenases, and [Fe]-hydrogenase. We present a crystal structure of [Fe]-hydrogenase at 1.75 angstrom resolution, showing a mononuclear iron coordinated by the sulfur of cysteine 176, two carbon monoxide (CO) molecules, and the sp2-hybridized nitrogen of a 2-pyridinol compound with back-bonding properties similar to those of cyanide. The three-dimensional arrangement of the ligands is similar to that of thiolate, CO, and cyanide ligated to the low-spin iron in binuclear [NiFe]- and [FeFe]-hydrogenases, although the enzymes have evolved independently and the CO and cyanide ligands are not found in any other metalloenzyme. The related iron ligation pattern of hydrogenases exemplifies convergent evolution and presumably plays an essential role in H2 activation. This finding may stimulate the ongoing synthesis of catalysts that could substitute for platinum in applications such as fuel cells.

The crystal structure of the apoenzyme of the iron-sulphur cluster-free hydrogenase.

The iron-sulphur cluster-free hydrogenase (Hmd, EC 1.12.98.2) from methanogenic archaea is a novel type of hydrogenase that tightly binds an iron-containing cofactor. The iron is coordinated by two CO molecules, one sulphur and a pyridone derivative, which is linked via a phosphodiester bond to a guanosine base. We report here on the crystal structure of the Hmd apoenzyme from Methanocaldococcus jannaschii at 1.75 A and from Methanopyrus kandleri at 2.4 A resolution. Homodimeric Hmd reveals a unique architecture composed of one central and two identical peripheral globular units. The central unit is composed of the intertwined C-terminal segments of both subunits, forming a novel intersubunit fold. The two peripheral units consist of the N-terminal domain of each subunit. The Rossmann fold-like structure of the N-terminal domain contains a mononucleotide-binding site, which could harbour the GMP moiety of the cofactor. Another binding site for the iron-containing cofactor is most probably Cys176, which is located at the bottom of a deep intersubunit cleft and which has been shown to be essential for enzyme activity. Adjacent to the iron of the cofactor modelled as a ligand to Cys176, an extended U-shaped extra electron density, interpreted as a polyethyleneglycol fragment, suggests a binding site for the substrate methenyltetrahydromethanopterin.