Site-directed mutagenesis reveals role of mobile arginine residue in lactate dehydrogenase catalysis

The binding of substrates to lactate dehydrogenases induces a marked rearrangement of the protein structure in which a 'loop' of polypeptide (residues 98-110) closes over the active site of the enzyme. In this rearrangement, arginine 109 (a basic residue conserved in all known lactate dehydrogenase sequences and in the homologous malate dehydrogenases) moves 0.8 nm from a position in the solvent to one in the active site where its guanidinium group resides within hydrogen bonding distance of both the reactive carbonyl of pyruvate and imidazole ring of the catalytic histidine 195 (see Fig. 1). Whilst this feature of the enzyme has been commented upon previously, the function of this mobile arginine residue during catalysis has not been tested experimentally. The advent of protein engineering has now enabled us to define the role of this basic residue by substituting it with the neutral glutamine. Transient kinetic and equilibrium studies of the mutant enzyme indicate that arginine 109 enhances the polarization of the pyruvate carbonyl group in the ground state and stabilizes the transition state. The gross active-site structure of the enzyme is not altered by the mutation since an alternative catalytic function of the enzyme (rate of addition of sulphite to NAD+), which does not require hydride transfer, is insensitive to the arginine----glutamine substitution.     

Volcanoes and climate: Krakatoa's signature persists in the ocean

We have analysed a suite of 12 state-of-the-art climate models and show that ocean warming and sea-level rise in the twentieth century were substantially reduced by the colossal eruption in 1883 of the volcano Krakatoa in the Sunda strait, Indonesia. Volcanically induced cooling of the ocean surface penetrated into deeper layers, where it persisted for decades after the event. This remarkable effect on oceanic thermal structure is longer lasting than has previously been suspected and is sufficient to offset a large fraction of ocean warming and sea-level rise caused by anthropogenic influences.     

Crystal structure of a streptococcal protein G domain bound to an Fab fragment.

Protein G is a cell-surface protein from Streptococcus which binds to IgG molecules from a wide range of species with an affinity comparable to that of antigen. The high affinity of protein G for the Fab portion of IgG poses a particular challenge in molecular recognition, given the variability of heavy chain subclass, light chain type and complementarity-determining regions. Here we report the crystal structure of a complex between a protein G domain and an immunoglobulin Fab fragment. An outer beta-strand in the protein G domain forms an antiparallel interaction with the last beta-strand in the constant heavy chain domain of the immunoglobulin, thus extending the beta-sheet into the protein G. The interaction between secondary structural elements in Fab and protein G provides an ingenious solution to the problem of maintaining a high affinity for many different IgG molecules. The structure also contrasts with Fab-antigen complexes, in which all contacts with antigen are mediated by the variable regions of the antibody, and to our knowledge provides the first details of interaction of the constant regions of Fab with another protein.     

Crystal structure of an N-terminal fragment of the DNA gyrase B protein.

The crystal structure of an N-terminal fragment of the Escherichia coli DNA gyrase B protein, complexed with a nonhydrolysable ATP analogue, has been solved at 2.5 A resolution. It consists of two domains, both containing novel protein folds. The protein fragment forms a dimer, whose N-terminal domains are responsible for ATP binding and hydrolysis. The C-terminal domains form the sides of a 20 A hole through the protein dimer which may play a role in DNA strand passage during the supercoiling reaction.     

Variations in solar luminosity and their effect on the Earth's climate

Variations in the Sun's total energy output (luminosity) are caused by changing dark (sunspot) and bright structures on the solar disk during the 11-year sunspot cycle. The variations measured from spacecraft since 1978 are too small to have contributed appreciably to accelerated global warming over the past 30 years. In this Review, we show that detailed analysis of these small output variations has greatly advanced our understanding of solar luminosity change, and this new understanding indicates that brightening of the Sun is unlikely to have had a significant influence on global warming since the seventeenth century. Additional climate forcing by changes in the Sun's output of ultraviolet light, and of magnetized plasmas, cannot be ruled out. The suggested mechanisms are, however, too complex to evaluate meaningfully at present.     

Crystal structure of RecBCD enzyme reveals a machine for processing DNA breaks

RecBCD is a multi-functional enzyme complex that processes DNA ends resulting from a double-strand break. RecBCD is a bipolar helicase that splits the duplex into its component strands and digests them until encountering a recombinational hotspot (Chi site). The nuclease activity is then attenuated and RecBCD loads RecA onto the 3' tail of the DNA. Here we present the crystal structure of RecBCD bound to a DNA substrate. In this initiation complex, the DNA duplex has been split across the RecC subunit to create a fork with the separated strands each heading towards different helicase motor subunits. The strands pass along tunnels within the complex, both emerging adjacent to the nuclease domain of RecB. Passage of the 3' tail through one of these tunnels provides a mechanism for the recognition of a Chi sequence by RecC within the context of double-stranded DNA. Gating of this tunnel suggests how nuclease activity might be regulated.