Ribosome: an Ancient Cellular Nano-Machine for Genetic Code Translation

The energy landscape of the ribosome

The ribosome is a prototypical assembly that can be used to establish general principles and techniques for the study of biological molecular machines. Motivated by the fact that the dynamics of every biomolecule is governed by an underlying energy landscape, there has been great interest to understand and quantify ribosome energetics. In the present review, we will focus on theoretical and computational strategies for probing the interactions that shape the energy landscape of the ribosome, with an emphasis on more recent studies of the elongation cycle. These efforts include the application of quantum mechanical methods for describing chemical kinetics, as well as classical descriptions to characterize slower (microsecond to millisecond) large-scale (10-100 Å) rearrangements, where motion is described in terms of diffusion across an energy landscape. Together, these studies provide broad insights into the factors that control a diverse range of dynamical processes in this assembly.

Investigation of Allosteric Effect of 2,8-Dimethylation of A2503 in E. coli 23S rRNA by Molecular-Dynamics Simulations

Ribosome is a molecular machine that synthesizes all cellular proteins. It also is a target of about half of the clinically used antibiotics. Adaptive chemical modification of ribosomal RNAs residues is one of the ways to provide resistance to certain antibiotics. A curious example of such modification is 2,8-dimethylation of A2503 in 23S rRNA, which induces resistance to phenols, linkosamides, oxazolidinones, pleuromutilins, and certain macrolides. In this article the effect of 2,8-dimethylation of A2503 on conformation and mobility of RNA residues of the 70S E. coli ribosome was investigated employing molecular dynamics simulations method. Significant alterations were detected both in the immediate environment of the 2503 23S rRNA residue and in the nucleotides located deeper in the nascent peptide exit tunnel (NPET), which are known to be involved in signal transmission from the antibiotics bound in the NPET to the peptidyl transferase center. These alterations shift the ribosome towards the A/A, P/P-state from the conformationally different state - P/P, E/E one in our case. The obtained results allow us to conclude that the effect of m²m⁸A2503 modification involves additional stabilization of the A/A, P/P-state favoring the peptidyl transferase reaction (PTR) contrary to antibiotics that inhibit PTR.

Geological and Geochemical Constraints on the Origin and Evolution of Life

The traditional tree of life from molecular biology with last universal common ancestor (LUCA) branching into bacteria and archaea (though fuzzy) is likely formally valid enough to be a basis for discussion of geological processes on the early Earth. Biologists infer likely properties of nodal organisms within the tree and, hence, the environment they inhabited. Geologists both vet tenuous trees and putative origin of life scenarios for geological and ecological reasonability and conversely infer geological information from trees. The latter approach is valuable as geologists have only weakly constrained the time when the Earth became habitable and the later time when life actually existed to the long interval between ∼4.5 and ∼3.85 Ga where no intact surface rocks are known. With regard to vetting, origin and early evolution hypotheses from molecular biology have recently centered on serpentinite settings in marine and alternatively land settings that are exposed to ultraviolet sunlight. The existence of these niches on the Hadean Earth is virtually certain. With regard to inferring geological environment from genomics, nodes on the tree of life can arise from true bottlenecks implied by the marine serpentinite origin scenario and by asteroid impact. Innovation of a very useful trait through a threshold allows the successful organism to quickly become very abundant and later root a large clade. The origin of life itself, that is, the initial Darwinian ancestor, the bacterial and archaeal roots as free-living cellular organisms that independently escaped hydrothermal chimneys above marine serpentinite or alternatively from shallow pore-water environments on land, the Selabacteria root with anoxygenic photosynthesis, and the Terrabacteria root colonizing land are attractive examples that predate the geological record. Conversely, geological reasoning presents likely events for appraisal by biologists. Asteroid impacts may have produced bottlenecks by decimating life. Thermophile roots of bacteria and archaea as well as a thermophile LUCA are attractive.