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  • 1
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Analytical Biochemistry 185 (1990), S. 206-212 
    ISSN: 0003-2697
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Biology , Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-1912
    Keywords: α1-Adrenoceptors ; α2-Adrenoceptors ; Endogenous noradrenaline ; Exogenous noradrenaline ; Proximal saphenous vein ; Distal saphenous vein
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Summary In the present study the relationship between adrenergic nerve terminals and postjunctional α-adrenoceptors mediating the responses to the endogenous transmitter was compared at proximal and distal levels of the canine saphenous vein. Concentration-response curves to noradrenaline and to tyramine as well as frequency-response curves to electrical stimulation were compared at both levels of the vessel, in the absence and presence of either prazosin (100nmol·l−1) or yohimbine (100nmol·l−1) The influence of inhibition of neuronal uptake by cocaine (12 µmol·l−1) on the responses to noradrenaline in the presence of prazosin (56 nmol·l−1) or yohimbine (20 nmol·l−1) was compared at the proximal level. The results show that, at the proximal level, the maximal responses to electrical stimulation and tyramine reached 80.1±2.2 (n = 18) and 74.2±1.9 (n = 18)%, respectively, of the maximal responses to noradrenaline, and 70.3±0.8 (n = 15) and 53.1 ± 1.2 (n = 14) %, respectively, at the distal level. Furthermore, the proximal strips were more sensitive to electrical stimulation than the distal ones. Prazosin had a much greater inhibitory effect on the contractile responses to noradrenaline than on those to electrical stimulation, at both levels. At proximal level, the shifts (to the right) of the concentration (frequency)-response curves (at EC50) amounted to 0.58±0.02 (n = 16) and 0.18±0.02 (n = 8) log units, respectively (P〈0.05), but, at the distal level, to 1.12±0.03 (n = 16) and 0.28±0.08 (n = 8) log units, respectively (P〈 0.05). At the proximal level, yohimbine antagonizes about equally the responses to noradrenaline and the responses to electrical stimulation. However, at the distal level, the shift of the concentration-response curve to noradrenaline was much larger than that of the frequency-response curve to electrical stimulation [1.12±0.07 and 0.80±0.10 (n = 6) log units at EC50, respectively (P〈0.05)]. The leftward shift of the concentration-response curve to noradrenaline caused by cocaine was more pronounced in the presence of prazosin than in the presence of yohimbine: 0.95±0.15 and 0.69±0.12 (n = 12) log units, respectively (P〈0.05). We conclude that, in the canine saphenous vein: 1) noradrenaline released from the adrenergic nerve terminals by electrical stimulation and by tyramine preferentially activates α2-adrenoceptors at both proximal and distal levels; 2) the effectiveness of α2-adrenoceptor stimulation is greater at the proximal than at the distal level; 3) α1-adrenoceptors at the distal level seem to be different from those at the proximal one.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Earth, moon and planets 14 (1975), S. 463-471 
    ISSN: 1573-0794
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Nine U-Th-Pb whole-rock analyses of selected brecciated materials from sample 72215 and one analysis of a pigeonite basalt clast from 72275 are presented. Both samples are from Boulder 1, Apollo 17. These data supplement previous Boulder 1 U-Th-Pb analyses of samples 72275 and 72255. U and Th concentrations indicate that most of the samples contain a moderate to large KREEP component. Samples containing the least KREEP are a noritic clast (72255,49; Civet Cat clast) and an anorthositic clast (72275,117). Evidence for the migration of Pb from Pb-rich matrix material into relatively Pb-poor clasts is presented for two clasts. Most of the Boulder 1 data define a linear trend that intersects concordia at ∼ 3.9 and 4.4 b.y. when plotted on a U-Pb concordia diagram. The presence of one anorthositic clast distinctly off this trend indicates that a simple two-stage U-Pb evolution history is inadequate to explain all the data. Accordingly physical significance is only attached to the lower concordia intercept age of 3.9–4.0 b.y. The older concordia intercept age of ∼ 4.4 b.y. is interpreted to reflect an averaging of events both older and younger than 4.4 b.y. The data suggest that significant differentiation and/or metamorphism occurred ∼ 4.2 b.y. ago. The age of this event, however, is not accurately defined by these data.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 47 (1974), S. 255-280 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract U-Pb analyses of zircons from the southern paragneiss zone of the Gotthard massif in the central Alps indicate these rocks were derived from one or more source areas ≧ 1400 m.y. old and were strongly affected by both the Caledonian and Hercynian orogenies. Rb-Sr whole-rock analyses also appear to reflect the Hercynian event while Rb-Sr analyses of a metamorphic inclusion and a boudin indicate that these small-scale samples were affected by the Alpine orogeny. U-Pb whole rock data appear to reflect only the Hercynian event; these data, when corrected for primordial lead, furthermore yield an upper concordia intercept of 4500 m.y., possibly resulting from a U-Pb fractionation very early in the history of the earth. A more refined three-stage U-Pb evolution model yields an age of about 4480 m.y. rather than 4500 m.y. for this hypothesized early terrestrial differentiation. Geologically these data emphasize that: 1) the southern paragneiss zone of the Gotthard massif contains metasediments which have experienced the Caledonian orogeny and are at least 400 m.y. old; 2) the Hercynian episode in this region was pervasive indeed; and 3) the Alpine orogeny affected the Rb-Sr and U-Pb whole rock systems to a far lesser degree than the preceding orogenic episodes and apparently did not affect the U-Pb zircon systems investigated at all.
    Type of Medium: Electronic Resource
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