Regulation of B-cell survival by BAFF-dependent PKCdelta-mediated nuclear signalling

Approximately 65% of B cells generated in human bone marrow are potentially harmful autoreactive B cells. Most of these cells are clonally deleted in the bone marrow, while those autoreactive B cells that escape to the periphery are anergized or perish before becoming mature B cells. Escape of self-reactive B cells from tolerance permits production of pathogenic auto-antibodies; recent studies suggest that extended B lymphocyte survival is a cause of autoimmune disease in mice and humans. Here we report a mechanism for the regulation of peripheral B-cell survival by serine/threonine protein kinase Cdelta (PKCdelta): spontaneous death of resting B cells is regulated by nuclear localization of PKCdelta that contributes to phosphorylation of histone H2B at serine 14 (S14-H2B). We show that treatment of B cells with the potent B-cell survival factor BAFF ('B-cell-activating factor belonging to the TNF family') prevents nuclear accumulation of PKCdelta. Our data suggest the existence of a previously unknown BAFF-induced and PKCdelta-mediated nuclear signalling pathway which regulates B-cell survival.     

Unborn children (protection) bill

Enoch Powell's Unborn Children (Protection) Bill passed a second reading in the British House of Commons on 22 February 1985. The authors contend that most informed scientists are dismayed because, if enacted into law, the bill would criminalize the in vitro fertilization of any human oocytes except for purposes of "embryo insertion," and many promising avenues of research would be blocked. While the pro-life lobby maintains that the development of possible methods to cure genetic diseases does not require research on human embryos, Evans and McLaren cite scientific data to argue that such research is necessary to insure that embryos chosen for implantation are chromosomally normal, to study the etiology of chromosomal disorders and eventually develop therapies for them, to improve IVF procedures, and to develop new contraceptive techniques.     

Aspartate 112 is the selectivity filter of the human voltage-gated proton channel

The ion selectivity of pumps and channels is central to their ability to perform a multitude of functions. Here we investigate the mechanism of the extraordinary selectivity of the human voltage-gated proton channel, H(V)1 (also known as HVCN1). This selectivity is essential to its ability to regulate reactive oxygen species production by leukocytes, histamine secretion by basophils, sperm capacitation, and airway pH. The most selective ion channel known, H(V)1 shows no detectable permeability to other ions. Opposing classes of selectivity mechanisms postulate that (1) a titratable amino acid residue in the permeation pathway imparts proton selectivity, or (2) water molecules 'frozen' in a narrow pore conduct protons while excluding other ions. Here we identify aspartate 112 as a crucial component of the selectivity filter of H(V)1. When a neutral amino acid replaced Asp?112, the mutant channel lost proton specificity and became anion-selective or did not conduct. Only the glutamate mutant remained proton-specific. Mutation of the nearby Asp?185 did not impair proton selectivity, indicating that Asp?112 has a unique role. Although histidine shuttles protons in other proteins, when histidine or lysine replaced Asp?112, the mutant channel was still anion-permeable. Evidently, the proton specificity of H(V)1 requires an acidic group at the selectivity filter.     

Active-site mutants altering the cooperativity of E. coli phosphofructokinase

Crystal structures of the high- and low-activity states of the allosteric enzyme phosphofructokinase implicate three arginines in substrate binding, catalysis and cooperativity. Arginines 162 and 243 reach into the active site from an adjacent subunit and interact with the cooperative substrate fructose 6-phosphate. Mutation of these arginines to serine results in mutant enzymes with reduced substrate binding and lowered cooperativity, but with little change in their catalytic ability (kcat). Arg 72 bridges the two substrates fructose 6-phosphate and ATP, and interacts with the 1-phosphate of the product fructose 1,6-biphosphate. Mutation of this residue to serine reduces the catalytic activity, cooperativity and binding of fructose 6-phosphate and fructose 1,6-bisphosphate. In the reverse reaction, the kinetics of wild-type and the Ser 72 mutant with respect to fructose 1,6-bisphosphate are hyperbolic, whereas those of the Ser 162 and Ser 243 mutants are sigmoidal. These results show that each of the three arginines contributes to cooperativity and to the transmission of allosteric signals between the four subunit of the enzyme.     

Dissolved organic carbon trends resulting from changes in atmospheric deposition chemistry

Several hypotheses have been proposed to explain recent, widespread increases in concentrations of dissolved organic carbon (DOC) in the surface waters of glaciated landscapes across eastern North America and northern and central Europe. Some invoke anthropogenic forcing through mechanisms related to climate change, nitrogen deposition or changes in land use, and by implication suggest that current concentrations and fluxes are without precedent. All of these hypotheses imply that DOC levels will continue to rise, with unpredictable consequences for the global carbon cycle. Alternatively, it has been proposed that DOC concentrations are returning toward pre-industrial levels as a result of a gradual decline in the sulphate content of atmospheric deposition. Here we show, through the assessment of time series data from 522 remote lakes and streams in North America and northern Europe, that rising trends in DOC between 1990 and 2004 can be concisely explained by a simple model based solely on changes in deposition chemistry and catchment acid-sensitivity. We demonstrate that DOC concentrations have increased in proportion to the rates at which atmospherically deposited anthropogenic sulphur and sea salt have declined. We conclude that acid deposition to these ecosystems has been partially buffered by changes in organic acidity and that the rise in DOC is integral to recovery from acidification. Over recent decades, deposition-driven increases in organic matter solubility may have increased the export of DOC to the oceans, a potentially important component of regional carbon balances. The increase in DOC concentrations in these regions appears unrelated to other climatic factors.