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191.
Global differential gene expression in response to growth temperature alteration in group A Streptococcus 总被引:13,自引:0,他引:13 下载免费PDF全文
192.
Ehlers MR Gordon K Schwager SL Sturrock ED 《Suid-Afrikaanse tydskrif vir geneeskunde》2012,102(6):461-464
A number of membrane proteins are enzymatically cleaved or 'shed' from the cell surface, resulting in the modulation of biological events and opening novel pharmaceutical approaches to diverse diseases by targeting shedding. Our focus has been on understanding the shedding of angiotensin-converting enzyme (ACE), an enzyme that plays a pivotal role in blood pressure regulation. The identification of novel hereditary ACE mutations that result in increased ACE shedding has advanced our understanding of the role of ACE shedding in health and disease. Extensive biochemical and molecular analysis has helped to elucidate the mechanism of ACE shedding. These findings point to the potential therapeutic role of targeting shedding in regulating tissue ACE levels in cardiovascular disease. 相似文献
193.
Self-identified bisexual men report high sexual arousal to both male and female stimuli, but no study to date has compellingly
demonstrated that such men have a bisexual pattern of genital arousal. We examined sexual arousal patterns among bisexual
men recruited using stringent criteria designed to exclude those who were less likely to have sexual interest in both sexes.
Furthermore, we included a bisexual stimulus depicting a man engaged in sex simultaneously with another man and a woman. On
average, the bisexual men showed a bisexual arousal pattern, with respect to both self-reported and genital arousal. Additionally,
the bisexual men were more aroused by the bisexual stimulus compared with the homosexual and heterosexual men. Some bisexual-identified
men have bisexual genital arousal patterns, although it remains unclear how common they are. 相似文献
194.
195.
Gap junctions are composed of transmembrane proteins belonging to the connexin family. These proteins permit the exchange of mall regulatory molecules directly between cells for the control of growth, development and differentiation. Although the presence of gap junctions in teeth has been already evidenced, the involved connexins have not yet been identified in human species. Here, we examined the distribution of connexin 43 (Cx43) in embryonic and permanent intact and carious human teeth. During tooth development, Cx43 localized both in epithelial and mesenchymal dental cells, correlated with cytodifferentiation gradients. In adult intact teeth, Cx43 was distributed in odontoblast processes. While Cx43 expression was downregulated in mature intact teeth, Cx43 appeared to be upregulated in odontoblasts facing carious lesions. In cultured pulp cells, Cx43 expression was related to the formation of mineralized nodules. These results indicate that Cx43 expression is developmentally regulated in human dental tissues, and suggest that Cx43 may participate in the processes of dentin formation and pathology. 相似文献
196.
Jill M. McDermott Jeffrey S. Seewald Christopher R. German Sean P. Sylva 《Proceedings of the National Academy of Sciences of the United States of America》2015,112(25):7668-7672
Arguments for an abiotic origin of low-molecular weight organic compounds in deep-sea hot springs are compelling owing to implications for the sustenance of deep biosphere microbial communities and their potential role in the origin of life. Theory predicts that warm H2-rich fluids, like those emanating from serpentinizing hydrothermal systems, create a favorable thermodynamic drive for the abiotic generation of organic compounds from inorganic precursors. Here, we constrain two distinct reaction pathways for abiotic organic synthesis in the natural environment at the Von Damm hydrothermal field and delineate spatially where inorganic carbon is converted into bioavailable reduced carbon. We reveal that carbon transformation reactions in a single system can progress over hours, days, and up to thousands of years. Previous studies have suggested that CH4 and higher hydrocarbons in ultramafic hydrothermal systems were dependent on H2 generation during active serpentinization. Rather, our results indicate that CH4 found in vent fluids is formed in H2-rich fluid inclusions, and higher n-alkanes may likely be derived from the same source. This finding implies that, in contrast with current paradigms, these compounds may form independently of actively circulating serpentinizing fluids in ultramafic-influenced systems. Conversely, widespread production of formate by ΣCO2 reduction at Von Damm occurs rapidly during shallow subsurface mixing of the same fluids, which may support anaerobic methanogenesis. Our finding of abiogenic formate in deep-sea hot springs has significant implications for microbial life strategies in the present-day deep biosphere as well as early life on Earth and beyond.Seawater-derived hydrothermal fluids venting at oceanic spreading centers are a net source for dissolved carbon to the deep sea, with vent fluid carbon contents directly tied to the sustenance of the subseafloor biosphere (1). Highly reducing fluids rich in dissolved H2, such as those discharging from serpentinizing hydrothermal systems, are of particular interest because of the potential for abiotic reduction of dissolved inorganic carbon to organic compounds (2–6) and their potential role as precursor compounds for prebiotic chemistry associated with the origin of life (7). Although there is increasing evidence that supports an abiotic origin for CH4 and other low-molecular weight organic compounds in ultramafic-hosted hydrothermal systems (8–10), the physical conditions, reaction pathways, and timescales that control abiotic organic synthesis at oceanic spreading centers remain elusive. Working models for the formation of abiotic CH4 and other hydrocarbons observed in vent fluids involve reduction of ΣCO2 and/or CO through Fischer–Tropsch-type processes during active circulation of seawater-derived hydrothermal fluids that are highly enriched in dissolved H2 because of serpentinization of host rocks; however, this mechanism has not been conclusively shown in natural systems. Others have suggested that leaching of CH4 and low-molecular weight hydrocarbons from magmatic fluid inclusions hosted in plutonic rocks may contribute at some level to the inventory of organic compounds observed in axial hot-spring fluids (1, 11, 12). The relative influence of these processes has important implications for the total flux and real-time concentrations of aqueous organic compounds delivered to the oceans by ridge-crest hydrothermal activity. Here, we use multiple lines of evidence to preclude abiotic reduction of ΣCO2 to CH4 during active fluid circulation but show that it is reduced to the metastable intermediate species formate instead. 相似文献
197.
Georg Schett Silvia Hayer Makiyeh Tohidast‐Akrad Beatrice Jahn Schmid Susanne Lang Birgit Türk Franz Kainberger Sylva Haralambous George Kollias Andrew C. Newby Qingbo Xu Günter Steiner Josef Smolen 《Arthritis \u0026amp; Rheumatology》2001,44(12):2888-2898