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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Inc
    Journal of metamorphic geology 23 (2005), S. 0 
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Thermal models for Barrovian metamorphism driven by doubling the thickness of the radiogenic crust typically meet difficulty in accounting for the observed peak metamorphic temperature conditions. This difficulty suggests that there is an additional component in the thermal budget of many collisional orogens. Theoretical and geological considerations suggest that viscous heating is a cumulative process that may explain the heat deficit in collision orogens. The results of 2D numerical modelling of continental collision involving subduction of the lithospheric mantle demonstrate that geologically plausible stresses and strain rates may result in orogen-scale viscous heat production of 0.1 to 〉1 μW m−3, which is comparable to or even exceeds bulk radiogenic heat production within the crust. Thermally induced buoyancy is responsible for crustal upwelling in large domes with metamorphic temperatures up to 200 °C higher than regional background temperatures. Heat is mostly generated within the uppermost mantle, because of large stresses in the highly viscous rocks deforming there. This thermal energy may be transferred to the overlying crust either in the form of enhanced heat flow, or through magmatism that brings heat into the crust advectively. The amplitude of orogenic heating varies with time, with both the amplitude and time-span depending strongly on the coupling between heat production, viscosity and collision strain rate. It is argued that geologically relevant figures are applicable to metamorphic domes such as the Lepontine Dome in the Central Alps. We conclude that deformation-generated viscous dissipation is an important heat source during collisional orogeny and that high metamorphic temperatures as in Barrovian type metamorphism are inherent to deforming crustal regions.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: In trypanosomes, MRP1 and MRP2 (previously called gBPx and gBPy, in which x and y indicate the MW of these proteins in a particular species) are guide (g)RNA binding proteins that are part of a large heteromeric complex that may play a role in U-insertion/deletion editing of mitochondrial mRNAs. In order to shed more light on the function of these proteins, we generated procyclic Trypanosoma brucei cell lines in which the levels of MRP 1 and/or MRP2 mRNA were downregulated by RNA interference (RNAi). Here we report that the RNAi-mediated knockdown of MRP1 and/or MRP2 resulted in severe growth inhibition and loss of both proteins. This loss occurred even in cells in which only one of the MRPs was targeted by RNAi, indicating a mutual dependence for stability of these proteins. The elimination of the MRPs substantially reduced the levels of edited cytB and RPS12 mRNAs, but resulted in little or no reduction of edited cox2, cox3 and A6 mRNAs, as measured in poisoned primer extension analyses. Surprisingly, we found a five-fold increase in ND7 mRNA editing in MRP1+2 double knockdown cells. In addition, the knockdowns also resulted in reduction in the amounts of mRNAs that do not undergo RNA editing (cox1, ND4 and ND5 mRNAs), but little change was observed for mitoribosomal 12S rRNA. Together, the results indicate that in procyclic T. brucei, MRP1 and MRP2 play a role in transcript-specific editing and other RNA processing activities.
    Type of Medium: Electronic Resource
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