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91.
Chemically modified antisense oligonucleotides (ASOs) are widely used as a tool to functionalize microRNAs (miRNAs). Reduction of miRNA level after ASO inhibition is commonly reported to show efficacy. Whether this is the most relevant endpoint for measuring miRNA inhibition has not been adequately addressed in the field although it has important implications for evaluating miRNA targeting studies. Using a novel approach to quantitate miRNA levels in the presence of excess ASO, we have discovered that the outcome of miRNA inhibition can vary depending on the chemical modification of the ASO. Although some miRNA inhibitors cause a decrease in mature miRNA levels, we have identified a novel 2′-fluoro/2′-methoxyethyl modified ASO motif with dramatically improved in vivo potency which does not. These studies show there are multiple mechanisms of miRNA inhibition by ASOs and that evaluation of secondary endpoints is crucial for interpreting miRNA inhibition studies.  相似文献   
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The interaction of alpha-thrombin with Ala48-hirudin, Ala48-hirudin1-47, and Ala48-hirudin48-65 was analyzed. Mutations at Pro48 were found to cause only slight changes in the kon (human: 3.1 +/- 0.3 x 10(8) M-1 s-1; bovine: 1.03 +/- 0.3 x 10(8) M-1 s-1) and koff (human: 0.4 +/- 0.2 x 10(-3) s-1; bovine: 2.9 +/- 0.4 x 10(-3) s-1) rate constants for the formation of the thrombin-hirudin complex. The amino-terminal fragment Ala48-hirudin1-47 containing the three disulfide bridges and the carboxyl-terminal fragment Ala48-hirudin48-65 were derived from the Ala48 mutant by proteolysis with endoproteinase Lys-C. These fragments inhibit bovine alpha-thrombin clotting activity with IC50 values of 0.6 and 4.9 microM, respectively (2.4 nM for r-hirudin). By mapping the interaction of Ala48-hirudin-derived fragments with bovine alpha-thrombin by limited proteolysis with trypsin and pancreatic elastase distinct binding sites for each fragment were determined. The carboxyl-terminal fragment was found to bind to the proposed anion-binding exosite in the region B62-74, whereas the amino-terminal fragment binds to a region around the elastase cleavage site at residues 150-151 of the alpha-thrombin B-chain.  相似文献   
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Myotonic dystrophy (DM1) is a highly variable, multi-system disorder resulting from the expansion of an untranslated CTG tract in DMPK. In DM1 expanded CUG repeat RNAs form hairpin secondary structures that bind and aberrantly sequester the RNA splice regulator, MBNL1. RNA splice defects resulting as a consequence of MBNL1 depletion have been shown to play a key role in the development of DM1 pathology. In patient populations, both the number and severity of DM1 symptoms increase broadly as a function of CTG tract length. However significant variability in the DM1 phenotype is observed in patients encoding similar CTG repeat numbers. Here we demonstrate that a gradual decrease in MBNL1 levels results both in the expansion of the repertoire of splice defects and an increase in the severity of the splice alterations. Thus, MBNL1 loss does not have an all or none outcome but rather shows a graded effect on the number and severity of the ensuing splice defects. Our results suggest that once a critical threshold is reached, relatively small dose variations of free MBNL1 levels, which may reflect modest changes in the size of the CUG tract or the extent of hairpin secondary structure formation, can significantly alter the number and severity of splice abnormalities and thus contribute to the phenotype variability observed in DM1 patients.  相似文献   
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A sequence of paleosols in the Solo Basin, Central Java, Indonesia, documents the local and regional environments present when Homo erectus spread through Southeast Asia during the early Pleistocene. The earliest human immigrants encountered a low-relief lake-margin landscape dominated by moist grasslands with open woodlands in the driest landscape positions. By 1.5 Ma, large streams filled the lake and the landscape became more riverine in nature, with riparian forests, savanna, and open woodland. Paleosol morphology and carbon isotope values of soil organic matter and pedogenic carbonates indicate a long-term shift toward regional drying or increased duration of the annual dry season through the early Pleistocene. This suggests that an annual dry season associated with monsoon conditions was an important aspect of the paleoclimate in which early humans spread from Africa to Southeast Asia.  相似文献   
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