Search

Emergence of the very first RNA or RNA-like oligomers from simple nucleotide precursors is one of the most intriguing questions of the origin of life research. In the current paper, we analyse the mechanism of four non-enzymatic template-free scenarios suggested for the oligomerization of chemically non-modified cyclic and acyclic nucleotides in the literature. We show that amines may have a twofold role in these syntheses: due to their high affinity to bind protons they may activate the phosphorus of the phosphate group via proton transfer reactions, or indirectly they may serve as charge compensating species and influence the self-assembling of nucleotides to supramolecular architectures compatible with the oligomerization reactions. Effect of cations and pH on the reactions is also discussed.

In the present paper, the adsorption of cysteine on hematite, magnetite and ferrihydrite was studied using FT-IR, electron paramagnetic resonance (EPR), Mössbauer spectroscopy and X-ray diffractometry. Cysteine was dissolved in artificial seawater (two different pHs) which contains the major constituents. There were two main findings described in this paper. First, after the cysteine adsorption, the FT-IR spectroscopy and X-ray diffractometry data showed the formation of cystine. Second, the Mössbauer spectroscopy did not show any increase in the amount of Fe(2+) as expected due the oxidation of cysteine to cystine. An explanation could be that Fe(2+) was oxidized by the oxygen present in the seawater or there occurred a reduction of cystine by Fe(2+) generating cysteine and Fe(3+). The specific surface area and pH at point of zero charge of the iron oxides were influenced by adsorption of cysteine. When compared to other iron oxides, ferrihydrite adsorbed significantly (p < 0.05) more cysteine. The pH has a significant (p < 0.05) effect only on cysteine adsorption on hematite. The FT-IR spectroscopy results showed that cystine remains adsorbed on the surface of the iron oxides even after being mixed with KCl and the amine and carboxylic groups are involved in this interaction. X-ray diffractometry showed no changes on iron oxides mineralogy and the following precipitated substances were found along with the iron oxides after drying the samples: cysteine, cystine and seawater salts. The EPR spectroscopy showed that cysteine interacts with iron oxides, changing the relative amounts of iron oxides and hydroxide.

We describe the one-pot synthesis of a large variety of nucleic acid bases and related compounds from formamide in the presence of zirconium minerals as catalysts. The major products observed are: purine, 2-hydroxy pyrimidine, 5-hydroxy pyrimidine, isocytosine, adenine, urea, and carbodiimide. The synthesis of low molecular weight amides and carboxylic acid derivatives (intermediates of extant metabolism) was also observed: glyoxylamide, glycolic-, lactic-, succinic-, oxalic-, fumaric-, and maleic acids. As the major problem in the origin of informational polymers is the instability of their precursors, we also investigated the effects of zirconia minerals on the stability of ribooligonucleotides in formamide and in water. The relevance of these findings with respect to the origin of informational polymers and primordial metabolism is discussed.

The present study examined the adsorption of cysteine, thiourea and thiocyanate on bentonite and montmorillonite at two different pHs (3.00, 8.00). The conditions used here are closer to those of prebiotic earth. As shown by FT-IR, Mössbauer and EPR spectroscopy and X-ray diffractometry, the most important finding of this work is that cysteine and thiourea penetrate into the interlayer of the clays and reduce Fe(3+) to Fe(2+), and as consequence, cystine and c,c'-dithiodiformamidinium ion are formed. This mechanism resembles that which occurs with aconitase. This is a very important result for prebiotic chemistry; we should think about clays not just sink of molecules, but as primitive vessels of production of biomolecules. At pH 8.00, an increasing expansion was observed in the following order for both minerals: thiourea > thiocyanate > cysteine. At pH 3.00, the same order was not observed and thiourea had an opposite behavior, being the compound producing the lowest expansion. Mössbauer spectroscopy showed that at pH 8.00, the proportion of Fe(2+) ions in bentonite increased, doubling for thiourea, or more than doubling for cysteine, in both clays. However, at pH 3.00, cysteine and thiourea did not change significantly the relative amount of Fe(2+) and Fe(3+) ions, when compared to clays without adsorption. For thiocyanate, the amount of Fe(2+) produced was independent of the pH or clay used, probably because the interlayers of clays are very acidic and HSCN formed does not reduce Fe(3+) to Fe(2+). For the interaction of thiocyanate with the clays, it was not possible to identify any potential compound formed. For the samples of bentonite and montmorillonite at pH 8.00 with cysteine, EPR spectroscopy showed that intensity of the lines due to Fe(3+) decreased because the reaction of Fe(3+)/cysteine. Intensity of EPR lines did not change when the samples of bentonite at pH 3.00 with and without cysteine were compared. These results are in accordance with those obtained using Mössbauer and FT-IR spectroscopy.

In Saccharomyces cerevisiae, imbalance of the genes coding for the heterochromatin components Sir3p and histone H4 (namely, overdosage of SIR3 and lack of one of the two genes coding for H4) causes modifications in telomere length and telomere sequence organization, favoring the insertion of Y' elements into a stably shortened (C1-3A)n repeat tract. We report here that the newly inserted Y' elements are unstable and are lost with high frequency, generating clonal subpopulations with short telomeres, as revealed by the analysis of a specific telomere (LIII) and of the overall population of telomeres. Moreover, the growth rates of the subpopulations with and without Y' elements on LIII are different, the Y'-less individuals reproducing 20% more slowly than individuals bearing Y' elements. When grown together with Y'-bearing individuals, the subpopulations with the normal LIII telomere (which are viable and genetically stable if grown alone) are rapidly competed out. Hence, genetic imbalance for the structural components of heterochromatin results in a complex and rapidly changing mixture of subpopulations in such cultures. Thus, in situations where subpopulations are allowed to compete, heterochromatin-based differential growth rates result in neo-Darwinian clonal selection.

Telomeric heterochromatin plays an essential role in telomere function, including the regulation of telomere length. We observe that in Saccharomyces cerevisiae an imbalance in the dosage of genes for two protein components of heterochromatin (namely Sir3p and histone H4) causes modifications in telomere length and telomere sequence organization. The effects of Sir3p/H4 imbalance were analyzed in yeast strains in which the wild-type SIR3 gene (normally a single-copy gene) was either absent or present in 20-30 copies, and both histone H4 genes (HHF1 and HHF2) were present or HHF1 was deleted, thus covering a wide range of viable gene-dosage combinations. Modifications of telomeres and of subtelomeric regions were identified by analyzing both the overall telomere population and by focusing on two single telomeric regions: the left telomere of chromosome III (LIII) and the right telomere of chromosome XI (RXI). The modifications induced by alteration of the Sir3p/H4 ratio consist of a reduction in the length and an increase in the instability of the terminal block of (C(1-3)A)n repeats and in susceptibility to insertion of Y' elements into this repeat element. Restoration of the wild-type gene ratio (by removal of the extra copies of SIR3 or by complementation with the missing second copy of HHF) restored the original telomere organization, both with respect to the length of the (C(1-3)A)n repeat stretch and the absence of Y' elements. This behavior shows that the stability of the wild-type sequence organization requires maintenance of the normal structure of telomeric heterochromatin.

The intergenic region of the Saccharomyces cerevisiae GAL1-GAL10 divergent promoters has been circularized in vitro in different topological states. In defined conditions, purified homologous RNA polymerase II forms two stable complexes (half-life approximately equal to 5 h) with this DNA in the presence of the four ribonucleotides, as determined by measurement (Gamper and Hearst 1983) of the amount and stability of the resulting unwinding. Each stable complex induces in the closed DNA domain a region of hypersensitivity to P1 endonuclease. The two induced hypersensitive regions are very similar: each maps on one promoter, spans over the 100 bp DNA sequence that encompasses the RNA Initiation Sites (RIS) and the TATA box, is composed by three subregions (one on the RIS, one proximal or overlapping the TATA sequence, one intermediate). We show that this promoter-localized interaction is supercoil-dependent.