Site-Resolved Observation of Vibrational Energy Transfer Using a Genetically Encoded Ultrafast Heater.

Allosteric information transfer in proteins has been linked to distinct vibrational energy transfer (VET) pathways in a number of theoretical studies. Experimental evidence for such pathways, however, is sparse because site-selective injection of vibrational energy into a protein, that is, localized heating, is required for their investigation. Here, we solved this problem by the site-specific incorporation of the non-canonical amino acid ß-(1-azulenyl)-l-alanine (AzAla) through genetic code expansion. As an exception to Kasha's rule, AzAla undergoes ultrafast internal conversion and heating after S1 excitation while upon S2 excitation, it serves as a fluorescent label. We equipped PDZ3, a protein interaction domain of postsynaptic density protein 95, with this ultrafast heater at two distinct positions. We indeed observed VET from the incorporation sites in the protein to a bound peptide ligand on the picosecond timescale by ultrafast IR spectroscopy. This approach based on genetically encoded AzAla paves the way for detailed studies of VET and its role in a wide range of proteins.

Archaeal aminoacyl-tRNA synthetases interact with the ribosome to recycle tRNAs.

Aminoacyl-tRNA synthetases (aaRS) are essential enzymes catalyzing the formation of aminoacyl-tRNAs, the immediate precursors for encoded peptides in ribosomal protein synthesis. Previous studies have suggested a link between tRNA aminoacylation and high-molecular-weight cellular complexes such as the cytoskeleton or ribosomes. However, the structural basis of these interactions and potential mechanistic implications are not well understood. To biochemically characterize these interactions we have used a system of two interacting archaeal aaRSs: an atypical methanogenic-type seryl-tRNA synthetase and an archaeal ArgRS. More specifically, we have shown by thermophoresis and surface plasmon resonance that these two aaRSs bind to the large ribosomal subunit with micromolar affinities. We have identified the L7/L12 stalk and the proteins located near the stalk base as the main sites for aaRS binding. Finally, we have performed a bioinformatics analysis of synonymous codons in the Methanothermobacter thermautotrophicus genome that supports a mechanism in which the deacylated tRNAs may be recharged by aaRSs bound to the ribosome and reused at the next occurrence of a codon encoding the same amino acid. These results suggest a mechanism of tRNA recycling in which aaRSs associate with the L7/L12 stalk region to recapture the tRNAs released from the preceding ribosome in polysomes.

An archaeal tRNA-synthetase complex that enhances aminoacylation under extreme conditions.

Aminoacyl-tRNA synthetases (aaRSs) play an integral role in protein synthesis, functioning to attach the correct amino acid with its cognate tRNA molecule. AaRSs are known to associate into higher-order multi-aminoacyl-tRNA synthetase complexes (MSC) involved in archaeal and eukaryotic translation, although the precise biological role remains largely unknown. To gain further insights into archaeal MSCs, possible protein-protein interactions with the atypical Methanothermobacter thermautotrophicus seryl-tRNA synthetase (MtSerRS) were investigated. Yeast two-hybrid analysis revealed arginyl-tRNA synthetase (MtArgRS) as an interacting partner of MtSerRS. Surface plasmon resonance confirmed stable complex formation, with a dissociation constant (K(D)) of 250 nM. Formation of the MtSerRS·MtArgRS complex was further supported by the ability of GST-MtArgRS to co-purify MtSerRS and by coelution of the two enzymes during gel filtration chromatography. The MtSerRS·MtArgRS complex also contained tRNA(Arg), consistent with the existence of a stable ribonucleoprotein complex active in aminoacylation. Steady-state kinetic analyses revealed that addition of MtArgRS to MtSerRS led to an almost 4-fold increase in the catalytic efficiency of serine attachment to tRNA, but had no effect on the activity of MtArgRS. Further, the most pronounced improvements in the aminoacylation activity of MtSerRS induced by MtArgRS were observed under conditions of elevated temperature and osmolarity. These data indicate that formation of a complex between MtSerRS and MtArgRS provides a means by which methanogenic archaea can optimize an early step in translation under a wide range of extreme environmental conditions.

Identification of amino acids in the N-terminal domain of atypical methanogenic-type Seryl-tRNA synthetase critical for tRNA recognition.

Seryl-tRNA synthetase (SerRS) from methanogenic archaeon Methanosarcina barkeri, contains an idiosyncratic N-terminal domain, composed of an antiparallel beta-sheet capped by a helical bundle, connected to the catalytic core by a short linker peptide. It is very different from the coiled-coil tRNA binding domain in bacterial-type SerRS. Because the crystal structure of the methanogenic-type SerRSxtRNA complex has not been obtained, a docking model was produced, which indicated that highly conserved helices H2 and H3 of the N-terminal domain may be important for recognition of the extra arm of tRNA(Ser). Based on structural information and the docking model, we have mutated various positions within the N-terminal region and probed their involvement in tRNA binding and serylation. Total loss of activity and inability of the R76A variant to form the complex with cognate tRNA identifies Arg(76) located in helix H2 as a crucial tRNA-interacting residue. Alteration of Lys(79) positioned in helix H2 and Arg(94) in the loop between helix H2 and beta-strand A4 have a pronounced effect on SerRSxtRNA(Ser) complex formation and dissociation constants (K(D)) determined by surface plasmon resonance. The replacement of residues Arg(38) (located in the loop between helix H1 and beta-strand A2), Lys(141) and Asn(142) (from H3), and Arg(143) (between H3 and H4) moderately affect both the serylation activity and the K(D) values. Furthermore, we have obtained a striking correlation between these results and in vivo effects of these mutations by quantifying the efficiency of suppression of bacterial amber mutations, after coexpression of the genes for M. barkeri suppressor tRNA(Ser) and a set of mMbSerRS variants in Escherichia coli.

Shuffling of discrete tRNASer regions reveals differently utilized identity elements in yeast and methanogenic archaea.

Seryl-tRNA synthetases (SerRSs) from methanogenic archaea possess distinct evolutionary origin and show minimal sequence similarity with counterparts from bacteria, eukaryotes and other archaea. Here we show that SerRS from yeast Saccharomyces cerevisiae and archaeon Methanococcus maripaludis (ScSerRS and MmSerRS, respectively) display significantly different ability to serylate heterologous tRNA(Ser). Recognition in yeast was shown to be more stringent than in archaeon. While cross-aminoacylation of M. maripaludis tRNA(Ser) (MmtRNA(Ser)) by yeast SerRS barely occurs, yeast tRNA(Ser) (SctRNA(Ser)) was shown to be a good substrate for heterologous MmSerRS. To investigate the contribution of different tRNA regions for the recognition by yeast and archaeal SerRS, chimeric tRNAs bearing separated domains of SctRNA(Ser) in MmtRNA(Ser) framework were produced by in vitro transcription and subjected to kinetic and gel mobility shift analysis with both enzymes. Generally, the recognition in M. maripaludis seems to be relatively relaxed toward tertiary elements of tRNA(Ser) structure and relies on the direct recognition of identity nucleotides. On the other hand, expression of tRNA(Ser) identity elements in yeast seems to be more sensitive toward surrounding sequence context. In both systems variable arm of tRNA was recognized as a major identity region with a strong influence on SerRS:tRNA binding. Acceptor domain of SctRNA(Ser) was also shown to be important for serylation in yeast. We propose that cognate interactions between N-terminal domain of yeast SerRS and variable region of SctRNA(Ser) place the acceptor stem into the enzyme's active site and lead to increased affinity toward serine and efficient serylation of tRNA. The same effect was not observed in M. maripaludis. Unlike its yeast counterpart, MmSerRS forms only one type of covalent complex with MmtRNA(Ser), regardless of the tRNA/SerRS molar ratio. Stoichiometry of the complex, one tRNA per dimeric SerRS, was revealed by mass spectrometry. Our studies indicate that different SerRS:tRNA recognition mode is utilized by these two systems.

Water level changes affect carbon turnover and microbial community composition in lake sediments.

Due to climate change, many lakes in Europe will be subject to higher variability of hydrological characteristics in their littoral zones. These different hydrological regimes might affect the use of allochthonous and autochthonous carbon sources. We used sandy sediment microcosms to examine the effects of different hydrological regimes (wet, desiccating, and wet-desiccation cycles) on carbon turnover. (13)C-labelled particulate organic carbon was used to trace and estimate carbon uptake into bacterial biomass (via phospholipid fatty acids) and respiration. Microbial community changes were monitored by combining DNA- and RNA-based real-time PCR quantification and terminal restriction fragment length polymorphism (T-RFLP) analysis of 16S rRNA. The shifting hydrological regimes in the sediment primarily caused two linked microbial effects: changes in the use of available organic carbon and community composition changes. Drying sediments yielded the highest CO2 emission rates, whereas hydrological shifts increased the uptake of allochthonous organic carbon for respiration. T-RFLP patterns demonstrated that only the most extreme hydrological changes induced a significant shift in the active and total bacterial communities. As current scenarios of climate change predict an increase of drought events, frequent variations of the hydrological regimes of many lake littoral zones in central Europe are anticipated. Based on the results of our study, this phenomenon may increase the intensity and amplitude in rates of allochthonous organic carbon uptake and CO2 emissions.