983 resultados para Escape peaks


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Cell cycle withdrawal in postmitotic cells involves cyclin-dependent kinase (Cdk) inhibitors that repress cell cycle Cdk activity. During mouse neurogenesis, cortical postmitotic neurons are shown here to accumulate high levels of the p27 Cdk inhibitor compared with their progenitor neuroblasts. Elevated p27 levels in staged embryo brain extracts correlate with p27 binding to Cdk2, and Cdk inactivation. Yet, Cdk5, which is associated with the noncyclin activator p35 in neurons, remains active in the presence of high p27 levels. Both in vitro and in vivo, p27 and related inhibitors can recognize a cyclin D-Cdk5 complex but not a p35-Cdk5 complex. The results indicate that the choice of activator determines the susceptibility of Cdk5 to p27 and related Cdk inhibitors, and thus its ability to act in postmitotic cells.

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The process of RNA chain initiation by RNA polymerases plays a central role in the regulation of transcription. In this complex phase of transcription, short oligomers are synthesized and released from the enzyme-promoter complex in a reaction termed abortive initiation. The polymerase undergoes many cycles of abortive initiation prior to completion of the initiation process, which is signaled by the translocation of the enzyme away from the promoter, release of sigma factor, and formation of an elongation complex in which the RNA is stably bound. We have studied the parameters that affect escape from the promoter by Escherichia coli RNA polymerase for the phage T7 A1 promoter, the phage T5 N25 promoter, and the chimeric promoter T5 N25antiDSR. The latter site contains a synthetic initial transcribed region that reduces its ability to synthesize RNA both in vivo and in vitro. Clearance from T5 N25antiDSR can be stimulated up to 10-fold in vitro by addition of the E. coli transcript cleavage factor GreA or GreB, but these factors have little effect on transcription from the normal T7 A1 or T5 N25 promoters. Using an E. coli strain lacking GreA and GreB, we were also able to show stimulation of transcription by the Gre factors from the T5 N25antiDSR promotor in vivo. The stimulation of RNA chain initiation by Gre factors, together with their known biochemical properties in the transcription elongation reaction, suggests some specific models for steps in the transcription initiation reaction.

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Learning is widely thought to result from altered potency of synapses within the neural pathways that mediate the learned behavior. Support for this belief, which pervades current physiological and computational thinking, comes especially from the analysis of cases of simple learning in invertebrates. Here, evidence is presented that in one such case, habituation of crayfish escape, the learning is more due to onset of tonic descending inhibition than to the intrinsic depression of circuit synapses to which it was previously attributed. Thus, the altered performance seems to depend at least as much on events in higher centers as on local plasticity.

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A sequel to another novel can be written as its own stand-alone book. Several authors have accomplished this, most notably J.K. Rowling in the early Harry Potter books. Other writers have failed in their attempts. Following Gameland: Warriors and Wizards, the sequel Escape from Pirate Isle is an attempt at writing a stand-alone book. Similar to the first story, Charles and Cindy, who are brother and sister, are magically transported into a board game to rescue their father. While the story was initially intended to stand on its own, in the end it does not, but not because the first novel needs to be read in order to understand it. Instead, it needs a sequel to be a complete story.

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Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014

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DSDP cores from areas of low (Site 505) and high heat flow (Site 504 B) near the Costa Rica Rift, together with seismic profiles from the Panama Basin, have been studied to determine the relationship between: (1) carbonate content and physical and acoustic properties; and (2) carbonate content, carbonate diagenesis and acoustic stratigraphy. Except for ash and chert layers, bulk density correlates strongly and linearly with carbonate content. Velocity is uniform downcore and only small variations at a small scale are measured. Thus an abrupt change in carbonate content will cause abrupt changes in acoustic impedance and should cause reflectors that can be detected acoustically. A comparison of seismic profiler reflection records with physical properties, carbonate content and reflection coefficients indicates that the main reflectors can be identified with ash layers, diagenetic boundaries, and carbonate content variations. Diagenesis of carbonate sediments is present at Site 504B in a 260 m-thick ooze-chalk-limestone/chert sequence. These diagenetic sequences occur in areas of higher heat flow (200 mW/m**2). Seismic profiler records can be used to map the extent and depth of these diagenetic boundaries.

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The first well logs collected below the Antarctic circle were obtained during Leg 113 at Site 693 on the Dronning Maud Land Margin (Antarctica) in the Weddell Sea. Gamma-ray, resistivity, and sonic logs were collected between 108.0 and 439.0 mbsf. The downhole logs show good agreement with the data collected from cores and provide a continuous measurement of the sedimentary record. These continuous log records show that the rather uniform Tertiary lithology seen in cores is characterized by high-frequency variability in the log data. Several thin hard streaks are identified, the largest of which coincides with a major Miocene hiatus. Associated with this hiatus is a change to lower illite content (and correspondingly lower gamma-ray counts) and to a significant increase in diatom content. Spectral analysis of the logs was performed on the lower Pliocene through upper Oligocene interval (108.0-343.0 mbsf). Between 108.0 and 245.0 mbsf, average sedimentation rates (50 and 26 m/m.y.) are high enough to show that variance is present in the orbital eccentricity (~95 k.y.) and obliquity (~41 k.y.) bands. Between 253.0 and 343.0 mbsf, the sedimentation rate (8 m/m.y.) is too low to resolve high frequency variations. The Milankovitch frequencies are best developed in the resistivity logs. Resistivity is responding to changes in porosity, which in these sediments is controlled by the abundance of biosiliceous sediments, particularly diatoms. The orbital forcing suggested by the Milankovitch frequencies may be influencing diatom productivity by inducing oscillations in upwelling, ice coverage, pack ice, and/or polynya. Although variations in diatom abundance were observed in the cores, they were not attributed to a Milankovitch signal, and therefore in this environment, downhole logs are an important contribution to the detection and understanding of orbitally influenced changes in sedimentation.

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