Mayday - integrative analytics for expression data

Background  

DNA Microarrays have become the standard method for large scale analyses of gene expression and epigenomics. The increasing complexity and inherent noisiness of the generated data makes visual data exploration ever more important. Fast deployment of new methods as well as a combination of predefined, easy to apply methods with programmer's access to the data are important requirements for any analysis framework. Mayday is an open source platform with emphasis on visual data exploration and analysis. Many built-in methods for clustering, machine learning and classification are provided for dissecting complex datasets. Plugins can easily be written to extend Mayday's functionality in a large number of ways. As Java program, Mayday is platform-independent and can be used as Java WebStart application without any installation. Mayday can import data from several file formats, database connectivity is included for efficient data organization. Numerous interactive visualization tools, including box plots, profile plots, principal component plots and a heatmap are available, can be enhanced with metadata and exported as publication quality vector files.     

The Hemagglutinin of Bat-Associated Influenza Viruses Is Activated by TMPRSS2 for pH-Dependent Entry into Bat but Not Human Cells

New World bats have recently been discovered to harbor influenza A virus (FLUAV)-related viruses, termed bat-associated influenza A-like viruses (batFLUAV). The internal proteins of batFLUAV are functional in mammalian cells. In contrast, no biological functionality could be demonstrated for the surface proteins, hemagglutinin (HA)-like (HAL) and neuraminidase (NA)-like (NAL), and these proteins need to be replaced by their human counterparts to allow spread of batFLUAV in human cells. Here, we employed rhabdoviral vectors to study the role of HAL and NAL in viral entry. Vectors pseudotyped with batFLUAV-HAL and -NAL were able to enter bat cells but not cells from other mammalian species. Host cell entry was mediated by HAL and was dependent on prior proteolytic activation of HAL and endosomal low pH. In contrast, sialic acids were dispensable for HAL-driven entry. Finally, the type II transmembrane serine protease TMPRSS2 was able to activate HAL for cell entry indicating that batFLUAV can utilize human proteases for HAL activation. Collectively, these results identify viral and cellular factors governing host cell entry driven by batFLUAV surface proteins. They suggest that the absence of a functional receptor precludes entry of batFLUAV into human cells while other prerequisites for entry, HAL activation and protonation, are met in target cells of human origin.     

Climate‐driven rampant speciation of the Cape flora

Aim To test whether the radiation of the extremely rich Cape flora is correlated with marine‐driven climate change. Location Middle to Late Miocene in the south‐east Atlantic and the Benguela Upwelling System (BUS) off the west coast of South Africa. Methods We studied the palynology of the thoroughly dated Middle to Late Miocene sediments of Ocean Drilling Program (ODP) Site 1085 retrieved from the Atlantic off the mouth of the Orange River. Both marine upwelling and terrestrial input are recorded at this site, which allows a direct correlation between changes in the terrestrial flora and the marine BUS in the south‐east Atlantic. Results Pollen types from plants of tropical affinity disappeared, and those from the Cape flora gradually increased, between 10 and 6 Ma. Our data corroborate the inferred dating of the diversification in Aizoaceae c. 8 Ma. Main conclusions Inferred vegetation changes for the Late Miocene south‐western African coast are the disappearance of Podocarpus‐dominated Afromontane forests, and a change in the vegetation of the coastal plain from tropical grassland and thicket to semi‐arid succulent vegetation. These changes are indicative of an increased summer drought, and are in step with the development of the southern BUS. They pre‐date the Pliocene uplift of the East African escarpment, suggesting that this did not play a role in stimulating vegetation change. Some Fynbos elements were present throughout the recorded period (from 11 Ma), suggesting that at least some elements of this vegetation were already in place during the onset of the BUS. This is consistent with a marine‐driven climate change in south‐western Africa triggering substantial radiation in the terrestrial flora, especially in the Aizoaceae.     

Morphological and histological changes of dermal scales during the fish‐to‐tetrapod transition

Witzmann F. (2011). Morphological and histological changes of dermal scales during the fish‐to‐tetrapod transition. —Acta Zoologica (Stockholm) 92 : 281–302. The gastral scales of limbed tetrapodomorphs evolved from the ‘elpistostegid’‐type of scale by an enlargement and differentiation of the articulation facets and a shortening and broadening of the keel. These changes caused a tighter connection between gastral scales within a scale row and a greater overlap between the rows. Dorsal round scales of limbed tetrapodomorphs developed from a gastral scale‐type by an alteration of the ontogenetic pathway. The posterolateral direction of scale rows in ‘elpistostegids’ was retained in the gastral scalation of most limbed tetrapodomorphs, whereas the arrangement of round dorsal scales is modified to a transverse orientation. Both gastral and dorsal scales of limbed tetrapodomorphs consist solely of parallel‐fibred bone with circumferential growth marks. The proportionally larger overlap surfaces of gastral scales and their mode of articulation in the ventral midline indicate that the body of limbed tetrapodomorphs might have been more flexible than that of their finned relatives. The alteration of dermal scales was one of the most rapid morphological changes during the fish‐to‐tetrapod transition. Once established, gastral and dorsal scales were retained as a conservative character in different lineages of basal tetrapods, in both the amphibian and the amniote lineages.     

Isomeric equilibria in complexes of adenosine 5'-triphosphate with divalent metal ions. Solution structures of M(ATP)2- complexes

Solution structures of M(ATP)2- complexes are reviewed. First the self-stacking properties of ATP4- and M(ATP)2- are shortly described. It is emphasized that for an evaluation of solution structures of M(ATP)2- complexes only results from diluted solutions (below 1 mM) should be used. Next, a comprehensive set of stability data obtained under such conditions from potentiometric pH titrations is summarized for the complexes of Mg2+, Ca2+, Mn2+, Co2+, Ni2+, Cu2+, Zn2+ and Cd2+ with ATP, and for comparison also with pyrimidine nucleoside 5'-triphosphates (YTPs), i.e. CTP, UTP and TTP. The stabilities for the M(ATP)2- complexes are mostly larger than those for the corresponding M(YTP)2- species; this increased stability results from the metal ion back-binding to the base residue in M(ATP)2-, i.e. macrochelates are formed. Detailed analysis of the stability data allows calculation of the percentage of the closed form for the several M(ATP)2- complexes: back-binding is most pronounced in Cu(ATP)2- (67 +/- 2%), remarkable in Zn(ATP)2- (28 +/- 7%), and not observable for Ca(ATP)2- (2 +/- 6%). Comparison of these results with those from 1H-NMR and ultraviolet spectrophotometric studies allows the conclusion that two types of base back-bound macrochelates are formed: one with a direct, i.e. innersphere, M2+/N-7 coordination, and one with a water molecule between the metal ion and N-7, i.e. an outersphere interaction occurs [e.g. to about 10% in Mg(ATP)2-] through hydrogen bonding of a coordinated water to N-7. The formation degree of both forms of these closed isomers is quantified. The biological implications of these results are indicated and the versatility of ATP as a ligand is discussed by summarizing pertinent examples.     

Self-association of nucleotides

The self-association of nucleosides decreases within the series adenosine>guanosine>inosine>cytidine ≈uridine. The same trend is observed for the corresponding nucleotides, though less pronounced, as the charge effect governs series like adenosine ? AMP^2?>ADP^3??ATP^4?. Protonation of adenosine considerably reduces its self-stacking tendency: this is different with ATP^4?, where a maximum is reached for H₂(ATP)^2? caused by additional ionic interactions in the [H₂(ATP)]₂ ^4? dimer. Metal ion coordination may promote self-association, e.g., of ATP^4? via (mainly) charge neutralization (Mg²⁺) and the formation of intermolecular bridges in dimeric stacks (Zn²⁺, Cd²⁺). These results allow definition of conditions with negligible self-association and thus the determination of the stability and structure of monomeric nucleotide complexes in aqueous solution, e.g., quantification of macrochelate formation in M(ATP)^2? complexes. Some biological implications of the results are indicated.     

Evaluation of the metal-ion-coordinating differences between the 2'-, 3'- and 5'-monophosphates of adenosine

The stability constants of the 1:1 complexes formed between Mg2+, Ca2+, Sr2+, Ba2+, Mn2+, Co2+, Ni2+, Cu2+, Zn2+ or Cd2+ and 2'AMP2-, 3'AMP2- or 5'AMP2- were determined by potentiometric pH titration in aqueous solution (I = 0.1 M, NaNO3; 25 degrees C). The experimental conditions were carefully selected such that self-association of the nucleotides and their complexes is negligibly small; i.e. it was made certain that the properties of the monomeric divalent-metal-ion--AMP [M(AMP)] complexes were studied. Based on recent measurements with simple phosphate monoesters, R-MP2- where R is a non-coordinating residue [Massoud, S. S. & Sigel, H. (1988) Inorg. Chem. 27, 1447-1453], it is shown that all the M(AMP) complexes of the alkaline earth ions, with the possible exception of Mg(5'AMP), have exactly the stability expected for a sole-phosphate coordination of the metal ion. The same property is revealed for the complexes with Mn2+, Co2+, Zn2+ or Cd2+ and 3'AMP2-; in case of Ni(3'AMP) and Cu(3'AMP) a slight stability increase just at the edge of the experimental-error limits is indicated. This slight stability increase is attributed to the formation of a macrochelate (possibly with N-3); in fact, additional information confirms macrochelation for Cu(3'AMP). About 45% of Cu(2'AMP) exists in aqueous solution as a macrochelate (probably involving N-3); the other M(2'AMP) complexes (M2+ = Mn2+, Co2+, Ni2+, Zn2+, Cd2+) form (if at all) only traces of a base-backbound species. Most pronounced is macrochelate formation with 5'AMP2-: all mentioned 3d ions and Zn2+ or Cd2+ form to some extent macrochelates via N-7 (the structures of these closed species are indicated). In case of M(5'AMP) the base-binding site is certain: replacement of N-7 by a CH unit (tubercidin 5'-monophosphate) eliminates any increased complex stability, whereas formation of the 1,N6-etheno bridge to form 1,N6-ethenoadenosine 5'-monophosphate results in the phenanthroline-like N-6,N-7 site which facilitates macrochelation significantly.