Crossed hydrophobic interaction immunoelectrophoresis: An analytical method for detection of amphiphilic proteins in crude mixtures and for prediction of the result of hydrophobic interaction chromatography

Crossed hydrophobic interaction immunoelectrophoresis is an analytical technique in which the principles of quantitative immunoelectrophoresis and hydrophobic interaction are directly combined. Using phenyl-Sepharose as hydrophobic (amphiphilic) matrix we have shown how the method permits detection of amphiphilic proteins in three model systems: native- and trypsinated intestinal brush border aminopeptidase, serum proteins, and detergent-solubilized erythrocyte proteins. In the case of first system the relative amounts of the two forms of the enzyme have been determined using immunochemical quantification. Comparison of the present method with column hydrophobic interaction chromatography reveals concordant results for both serum and erythrocyte proteins. Tests of some alkyl-substituted agaroses show that they work in a manner similar to phenyl-Sepharose.     

Early anaerobic metabolisms

Before the advent of oxygenic photosynthesis, the biosphere was driven by anaerobic metabolisms. We catalogue and quantify the source strengths of the most probable electron donors and electron acceptors that would have been available to fuel early-Earth ecosystems. The most active ecosystems were probably driven by the cycling of H2 and Fe2+ through primary production conducted by anoxygenic phototrophs. Interesting and dynamic ecosystems would have also been driven by the microbial cycling of sulphur and nitrogen species, but their activity levels were probably not so great. Despite the diversity of potential early ecosystems, rates of primary production in the early-Earth anaerobic biosphere were probably well below those rates observed in the marine environment. We shift our attention to the Earth environment at 3.8Gyr ago, where the earliest marine sediments are preserved. We calculate, consistent with the carbon isotope record and other considerations of the carbon cycle, that marine rates of primary production at this time were probably an order of magnitude (or more) less than today. We conclude that the flux of reduced species to the Earth surface at this time may have been sufficient to drive anaerobic ecosystems of sufficient activity to be consistent with the carbon isotope record. Conversely, an ecosystem based on oxygenic photosynthesis was also possible with complete removal of the oxygen by reaction with reduced species from the mantle.     

Irreversible inactivation of red cell chloride exchange with phenylglyoxal, and arginine-specific reagent

Chloride exchange in resealed human erythrocyte ghosts can be irreversibly inhibited with phenylglyoxal, a reagent specific for the modification of arginyl residues in proteins. Phenylglyoxal inhibits anion transport in two distinct ways. At 0 degrees C, inhibition is instantaneous and fully reversible, whereas at higher temperature in an alkaline extracellular medium, covalent binding of phenylglyoxal leads to an irreversible inhibition of the transport membranes system. Indiscriminate modification of membrane arginyl residues was prevented by reacting the with phenylglyoxal in an alkaline extracellular medium while maintaining intracellular pH near neutrality. The rate of modification of anion transport depends on phenylglyoxal concentration, pH, temperature, and the presence of anions and reversible inhibitors of the anion transport system in fashions that are fully compatible with the conclusion that phenylglyoxal modifies arginyl residues that are essential for anion binding and translocation. Phenylglyoxal reacts rapidly with the deprotonated form of the reactive groups. It is proposed that the effects of anions and of negatively charged transport inhibitors on the rate of irreversible binding of phenylglyoxal are related to the effects of the anions on a positive interfacial potential. This potential determines the local pH, and thereby the concentration of deprotonated groups, in an exofacial region of the anion transport protein.     

Transcriptional Profiling of Whole Blood Identifies a Unique 5-Gene Signature for Myelofibrosis and Imminent Myelofibrosis Transformation

Identifying a distinct gene signature for myelofibrosis may yield novel information of the genes, which are responsible for progression of essential thrombocythemia and polycythemia vera towards myelofibrosis. We aimed at identifying a simple gene signature – composed of a few genes - which were selectively and highly deregulated in myelofibrosis patients. Gene expression microarray studies have been performed on whole blood from 69 patients with myeloproliferative neoplasms. Amongst the top-20 of the most upregulated genes in PMF compared to controls, we identified 5 genes (DEFA4, ELA2, OLFM4, CTSG, and AZU1), which were highly significantly deregulated in PMF only. None of these genes were significantly regulated in ET and PV patients. However, hierarchical cluster analysis showed that these genes were also highly expressed in a subset of patients with ET (n = 1) and PV (n = 4) transforming towards myelofibrosis and/or being featured by an aggressive phenotype. We have identified a simple 5-gene signature, which is uniquely and highly significantly deregulated in patients in transitional stages of ET and PV towards myelofibrosis and in patients with PMF only. Some of these genes are considered to be responsible for the derangement of bone marrow stroma in myelofibrosis. Accordingly, this gene-signature may reflect key processes in the pathogenesis and pathophysiology of myelofibrosis development.