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Crystallization and preliminary X-ray characterization of a ferritin from the hyperthermophilic archaeon and anaerobe Pyrococcus furiosus.

Crystals of the title protein have been produced and preliminary structural analysis has been carried out. The crystals belong to the orthorhombic space group C222(1), with unit-cell parameters a = 258.1, b = 340.1, c = 266.5 A. The protein forms a 24-mer of 20 kDa subunits, which assemble with 432 non-crystallographic symmetry. A total of 36 monomers are found in the asymmetric unit, corresponding to one and a half 24-mers.

Archaea↗

Metabolic channelling of carbamoyl phosphate in the hyperthermophilic archaeon Pyrococcus furiosus: dynamic enzyme-enzyme interactions involved in the formation of the channelling complex.

Protection of thermolabile metabolites and coenzymes is a somewhat neglected but essential aspect of the molecular physiology of hyperthermophiles. Detailed information about the mechanisms used by thermophiles to protect these thermolabile metabolites and coenzymes is still scarce. A case in point is CP (carbamoyl phosphate), a precursor of pyrimidines and arginine, which is an extremely labile and potentially toxic intermediate. Recently we obtained the first evidence for a physical interaction between two hyperthermophilic enzymes for which kinetic evidence had suggested that these enzymes channel a highly thermolabile and potentially toxic intermediate. By physically interacting with each other, CKase (carbamate kinase) and OTCase (ornithine carbamoyltransferase) prevent thermodenaturation of CP in the aqueous cytoplasmic environment. The CP channelling complex involving CKase and OTCase or ATCase (aspartate carbamoyltransferase), identified in hyperthermophilic archaea, provides a good model system to investigate the mechanism of metabolic channelling and the molecular basis of protein-protein interactions in the physiology of extreme thermophiles.

Arginine↗

Both nucleophile and substrate bind to the catalytic Fe(II)-center in the type-II methionyl aminopeptidase from Pyrococcus furiosus.

Metalloproteases utilize their active site divalent metal ions to generate a nucleophilic water/hydroxide. For methionine aminopeptidases (MetAPs), the exact location of this nucleophile, as well as of the substrate, with respect to the active site metal ion is unknown. In order to address this issue, we have examined the catalytically competent Fe(II)-loaded form of PfMetAP-II ([Fe(PfMetAP-II)]) in the absence and presence of both nitric oxide (NO) and the substrate-analogue inhibitor butaneboronic acid (BuBA) by kinetic and spectroscopic (EPR, UV-vis) methods. NO binds to [Fe(PfMetAP-II)] with a Kd of 200 microM forming an {FeNO}7 complex. UV-vis spectra of the resulting [Fe(PfMetAP-II)]-NO complex indicate that the Fe(II) ion is six coordinate. These data suggest that NO binding occurs without displacing the bound aquo/hydroxo moiety in [Fe(PfMetAP-II)]. On the basis of EPR spectra, the resulting Fe-NO complex is best described as NO- (S = 1) antiferromagnetically coupled to a high-spin Fe(III) ion (S = 5/2). The addition of BuBA to [Fe(PfMetAP-II)]-NO displaces the coordinated water molecule forming a six-coordinate adduct. EPR data also indicate that an interaction between the bound NO- and BuBA occurs forming a complex that mimics an intermediate step between the Michaelis complex and the tetrahedral transition-state.

Aminopeptidases↗