Nucleic Acids Bind to Nanoparticulate iron (II) Monosulphide in Aqueous Solutions

In the hydrothermal FeS-world origin of life scenarios nucleic acids are suggested to bind to iron (II) monosulphide precipitated from the reaction between hydrothermal sulphidic vent solutions and iron-bearing oceanic water. In lower temperature systems, the first precipitate from this process is nanoparticulate, metastable FeSm with a mackinawite structure. Although the interactions between bulk crystalline iron sulphide minerals and nucleic acids have been reported, their reaction with nanoparticulate FeSm has not previously been investigated. We investigated the binding of different nucleic acids, and their constituents, to freshly precipitated, nanoparticulate FeSm. The degree to which the organic molecules interacted with FeSm is chromosomal DNA > RNA > oligomeric DNA > deoxadenosine monophosphate approximately deoxyadenosine approximately adenine. Although we found that FeSm does not fluoresce within the visible spectrum and there is no quantum confinement effect seen in the absorption, the mechanism of linkage of the FeSm to these biomolecules appears to be primarily electrostatic and similar to that found for the attachment of ZnS quantum dots. The results of a preliminary study of similar reactions with nanoparticulate CuS further supported the suggestion that the interaction mechanism was generic for nanoparticulate transition metal sulphides. In terms of the FeS-world hypothesis, the results of this study further support the idea that sulphide minerals precipitated at hydrothermal vents interact with biomolecules and could have assisted in the formation and polymerisation of nucleic acids.     

Intercalibration of assessment methods for macrophytes in lowland streams: direct comparison and analysis of common metrics

The results of four macrophyte assessment methods (French Indice Biologique Macrophytique en Rivière, German Reference Index, British Mean Trophic Rank and Dutch Macrophyte Score) were compared, based on plant survey data of medium-sized lowland streams in Central Europe. To intercalibrate the good quality class boundaries two alternative methods were applied: direct comparison and the use of “common metrics”. While the French and British methods were highly related (R²>0.75), the German RI showed less (0.20<R²<0.55) and the Dutch DMS least correlation (R²<0.10) with other methods. Of 70 macrophyte metrics tested only Ellenberg_N was considerably related to three of the national assessment methods, thus representing a potential common metric for intercalibration. Comparison of quality class boundaries via regression analysis using both intercalibration approaches revealed major differences between classifications of the French, German and British methods, which are, in addition, related in a nonlinear way.     

Technological persistency following faunal stability during the Pleistocene: A model for reconstructing Paleolithic adaptation strategies based on mosaic evolution

Prehistoric archaeology focuses on innovations, transformations, and turnovers. We focus instead on persistency, suggesting that technological persistency in prehistoric hunter-gatherers was triggered by the stability of prey. The technological persistency-faunal stability nexus was not only crucial to human prosperity but also provided safe ground for technological and behavioral innovations, facilitating further adaptation to changing conditions. This can be viewed in the framework of mosaic evolution. We present six cases of morphological stasis enabling trophic adaptations and five archaeological cases of technological persistency following faunal stability. This model could contribute to a better understanding of technological persistency and its evolutionary role.     

Comparative Morphology of Meloidodera spp. and Verutus sp. (Heteroderidae) with Scanning Electron Microscopy

Scanning electron microscopy (SEM) of second-stage juveniles (J2), males, and females of Meloidodera floridensis, M. charis, M. belli, and Verutus volvingentis reveals detailed characteristics of the head region, lateral field, phasmid, body striae, vulva, and perineal region. In M. charis and M. belli the en face pattern conforms to a basic pattern in which the labial disc is surrounded by six lips (sectors) of the first head annulation. In J2 the head has additional annulations, whereas in males annulation is replaced by longitudinal blocks. Conversely, J2 and males of M. floridensis and V. volvingentis each have a unique derived face pattern with fusion of various lip components and with head annulation. All six lips of females of M. charis and M. belli are fused, whereas females of M. floridensis and V. volvingentis have distinct lateral lips. Lateral fields vary among species, with only slight differences at the anterior and posterior ends of the lateral lines and in the spatial relation of the lines to phasmid openings. Phasmid openings are present in adults of Meloidodera spp., but were not observed in adults of V. volvingentis; in this respect, the female perineal pattern of Verutus is different from Meloidodera spp, The very large vulva (± 48 μm long) of V. volvingentis is in sharp contrast to the minute vulva (± 6 μm long) in a population of M. charis from San Bernardino. Morphological characters revealed by SEM will be most informative when investigated throughout Heteroderidae and incorporated with additional characters for a phylogenetic analysis of the family.     

Radioactive analogs of neurotensin. II. Preparation of tritiated neurotensin from a synthetic multi-unsaturated derivative

In this second paper on the synthesis of neurotensin analogues as precursors for radiolabelling, solid phase synthesis of two polyunsaturated peptides, [Dah6, delta Pro7,10]-neurotensin and acetyl-[delta Pro10]-neurotensin-(8-13), are described. The first one contains one triple bond and two double bonds susceptible to tritiation in the same molecule, the second one contains one double bond in the shortest sequence having neurotensin activity. The C-terminal residue, Boc-Leu, was esterified on the chloromethyl-resin by its cesium salt. For the other amino acids a double coupling was carried out, the first one with dicyclohexylcarbodimide and the second one with the amino acid hydroxybenzotriazole ester. Acylation of the second amino acid, on the resin, presented some difficulties to achieve completeness and several acetylations and benzoylations had to be performed in order to block the last 4 per cent of free amines. It seems that these difficulties are related to some batches of chloromethyl-resin. Incorporation of both acetylenic lysine, N alpha-Boc-N epsilon-Z-L-2,6-diamino-4-hexynoic acid, whose synthesis is described, and N alpha-Boc-L-3,4-dehydroproline was without problems in this synthesis. After cleavage by hydrofluoric acid the crude peptides were purified by gel filtration on Bio-Gel P2 and ion exchange chromatography on carboxymethylcellulose (CM 52). [Dah6, delta Pro7,10]-neurotensin so obtained (51 per cent compared to starting Boc-Leu-resin) was in homogeneous form as characterized by amino acid analysis, thin layer chromatography in different systems and high performance liquid chromatography. The hydrogenation or tritiation product was identical with native neurotensin. Unsaturated derivative and neurotensin obtained after catalytic hydrogenation were as active as native neurotensin in inhibition of 125I-[Trp11]-neurotensin binding to rat brain synaptic membranes and in guinea pig ileum contractility test. Substitution of proline and lysine by their dehydro-derivatives did not affect the biological properties of neurotensin. The tritiated neurotensin (160-180 Ci/mmol) should be a good agent for biological characterization of neurotensin receptors and for investigation of the peptide metabolism.     

The Caune de l’Arago stone industries in their stratigraphical context

The Middle Stratigraphical Complex of the Caune de l’Arago cave site (Eastern Pyrenées, France) is dated to between 690,000 and 400,000 years old. The site contains successive, spatially distinct archaeological levels. At the base of the sequence, Unit I (OIS 14), where the P levels are among the earliest Mode 2 assemblages presently known in western Europe, contains finely shaped handaxes and a cleaver. Situated above this ensemble, Unit II (OIS 13) has revealed a series of artefact levels lacking handaxes and cleavers. Coiffing the sequence, Unit III (OIS12) has provided numerically rich faunal and lithic assemblages in association with Homo heidelbergensis remains. This paper analyses the stone industries from each artefact level taking into account raw material variability and highlights subtle technological and typological differences. This intrasite study uses a multidisciplinary approach to examine common elements and differences between levels, taking into consideration how external impact factors might have influenced global assemblage features. The Caune de l’Arago's long stratigraphical sequence provides an exceptional opportunity to observe both change and stability in Mode 2 stone-tool manufacture over a period spanning nearly 300,000 years, within the context of contrasting paleoenvironmental conditions.     

Changes in enzymic activities of UDP-D-glucuronate decarboxylase and UDP-D-xylose 4-epimerase during cell division and xylem differentiation in

The time course of the specific activities of UDP-D-glucuronate decarboxylase (E.C. 4.1.1.35) and UDP-D-xylose 4-epimerase (E.C. 5.1.3.5) have     

Spatial behaviours of Early Oldowan toolmakers in the Shungura Formation (Lower Omo Valley,Ethiopia): Proposal for an integrated approach

The spatial relationships of the Early Oldowan toolmakers with their environment have been so far addressed through raw material procurement analyses and the characterization of hominid habitat. This paper proposes to integrate these two approaches into a broader spatial analysis encompassing archaeological and environmental data (palaeontological, geological and isotopic data) from Member F and lower Member G of the Shungura Formation (Lower Omo Valley, Ethiopia). Heterogeneity in data resolution induces a multiscale approach with three levels of analysis. The level of occurrence complex allows focusing on the characterization of archaeological occurrences and on their environmental settings. The level of “study area” allows working on hominid habitats and on their raw material procurement behaviours. Finally, at the Shungura Formation scale, we can address temporal issues related to the evolution of spatial behaviours between Member F and the lower part of Member G, ca. 2.3 to 2 million years (Ma).