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  • 1
    Electronic Resource
    Electronic Resource
    Fluid inclusions in rocks from the amphibolite-facies gneiss to charnockite progression in southern Karnataka, India: direct evidence concerning the fluids of granulite metamorphism (1984)
    Oxford, UK : Blackwell Publishing Ltd
    Journal of metamorphic geology 2 (1984), S. 0 
    Details
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract Fluid inclusion studies of rocks from the late Archaean amphibolite-facies to granulite-facies transition zone of southern India provide support for the hypothesis that CO2,-rich H2O-poor fluids were a major factor in the origin of the high-grade terrain. Charnockites, closely associated leucogranites and quartzo-feldspathic veins contain vast numbers of large CO2-rich inclusions in planar arrays in quartz and feldspar, whereas amphibole-bearing gray gneisses of essentially the same compositions as adjacent charnockites in mixed-facies quarries contain no large fluid inclusions. Inclusions in the northernmost incipient charnockites, as at Kabbal, Karnataka, occasionally contain about 25 mol. % of immiscible H2O lining cavity walls, whereas inclusions from the charnockite massif terrane farther south do not have visibile H2OMicrothermometry of CO2 inclusions shows that miscible CH4 and N2 must be small, probably less than 10mol.%combined. Densities of CO2 increase steadily from north to south across the transitional terrane. Entrapment pressures calculated from the CO2 equation of state range from 5 kbar in the north to 7.5 kbar in the south at the mineralogically inferred average metamorphic temperature of 750°C, in quantitative agreement with mineralogic geobarometry. This agreement leads to the inference that the fluid inclusions were trapped at or near peak metamorphic conditions.Calculations on the stability of the charnockite assemblage biotite-orthopyroxene-K-feldspar-quartz show that an associated fluid phase must have less than 0.35 H2O activity at the inferred P and T conditions, which agrees with the petrographic observations. High TiO2 content of biotite stabilizes it to lower H2O activities, and the steady increase of biotite TiO2 southward in the area suggests progressive decrease of aH2O with increasing grade. Oxygen fugacities calculated from orthopyroxene-magnetite-quartz are considerably higher than the graphite CO2-O2 buffer, which explains the absence of graphite in the charnockites.The present study quantifies the nature of the vapours in the southern India granulite metamorphism. It remains to be determined whether CO2-flushing of the crust can, by itself, create large terranes of largeion lithophile-depleted granulites, or whether removal of H2O-bearing anatectic melts is essential.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1525-1314.1984.tb00299.x
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  • 2
    Electronic Resource
    Electronic Resource
    Orthopyroxene-bearing, mafic migmatites at Cone Peak, California: evidence for the formation of migmatitic granulites by anatexis in an open system (1993)
    Oxford, UK : Blackwell Publishing Ltd
    Journal of metamorphic geology 11 (1993), S. 0 
    Details
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract Orthopyroxene-bearing migmatites, exposed at the summit of Cone Peak in the Santa Lucia Range, California, offer an opportunity to explore potential links between granulite facies metamorphism and migmatite formation. Geothermobarometry indicates that the metamorphic temperatures and pressures were in the approximate ranges of 700–750° C and 7.0–7.5 kbar. The rocks at the summit comprise three domains: relatively coarse-grained, leucocratic veins; relatively fine-grained, biotite-enriched zones at the margins of the veins; and a biotite–hornblende-bearing host rock. Orthopyroxene is concentrated in the veins, which have also the highest ratio of anhydrous to hydrous minerals of the three rock types. The composition of the veins, together with their textures and modes, suggest that they formed through anatexis involving a dehydration-melting reaction which consumed hornblende and produced orthopyroxene. Variability in mineralogy and composition indicates that there was some local migration of magma along the veins before their final solidification. The biotite-enriched zones formed either by the concentration of residual biotite at the margins of the vein, or through the metasomatic conversion of hornblende (and/or pyroxene) to biotite, or by a combination of the two processes. Significant differences in the chemistry of the neosome (vein + biotite-enriched zone) and the host rock rule out simple dehydration melting in a local closed system. The model that explains best the mineralogical and chemical patterns involves triggering of melting by an influx of a low-aH2O mixed fluid which added K and Si to and removed Ca from the neosome.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1525-1314.1993.tb00148.x
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  • 3
    Electronic Resource
    Electronic Resource
    Tree vigour and the susceptibility of Douglas fir to Armillaria root disease (1998)
    Oxford, UK : Blackwell Publishing Ltd
    Forest pathology 28 (1998), S. 0 
    Details
    ISSN: 1439-0329
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: In this study the effects of thinning, fertilization and pruning on the vigour of Douglas fir (Pseudotsuga menziesii) and its susceptibility to Armillaria root disease were explored. Tree vigour was defined as the relative capacity for tree growth, expressed as the above-ground biomass increment per unit of photosynthetic tissue, or growth efficiency (GE). It has been hypothesized that trees with higher GE can better resist pathogen attack, and that GE can be used as a predictor of tree susceptibility to disease. In a previous study, four Douglas fir plantations were thinned, fertilized and pruned in all combinations, and the effects of these treatments on tree vigour were measured after 10 years. Root disease was not a factor in the initial study design, and mortality was ignored until 8 years after the treatments were applied. The results of an earlier study were utilized and the correlation between Armillaria root disease incidence and the effects of earlier stand treatments on tree growth was tested. Armillaria ostoyae was the primary mortality agent in the study area. Disease incidence on infested subplots ranged from 2 to 20%. Armillaria ostoyae incidence was the highest at medium tree density (6.1%), slightly lower on the low density (5.6%), and lowest on the unthinned plots (3.8%). There were no significant correlations between disease incidence and previous tree growth. The vigour of trees that became symptomatic or died by 1993 was not significantly different in 1983–85 from the vigour of trees that remained asymptomatic. On these sites, in areas of infestation, A. ostoyae is killing the largest, fastest growing trees, as well as less vigorous trees. Armillaria continues to cause mortality, regardless of the growth efficiency or growth rate of the host.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1439-0329.1998.tb01164.x
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  • 4
    Electronic Resource
    Electronic Resource
    Molecular cloning, partial purification, and characterization of a haemin-binding lipoprotein from Haemophilus influenzae type b (1991)
    Oxford, UK : Blackwell Publishing Ltd
    Molecular microbiology 5 (1991), S. 0 
    Details
    ISSN: 1365-2958
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Medicine
    Notes: A library of genomic DNA fragments from Haemophilus influenzae type b (Hib) DL42 was constructed in plasmid pBR322, transformed into Escherichia coli strain RR1, and screened for recombinant clones with haemin-binding activity by plating onto haemin-containing agar. Expression of haemin-binding activity by clones correlated with the expression of a protein with an apparent molecular weight of 51000 (51K) that was also recognized by anti-Hib strain DL42 serum in immunoblots. One recombinant clone, designated pHM2, with the smallest DNA insert (3.62kb) was characterized further. Ethanol inhibition of expression of pHM2 in minicells revealed that the 51K protein was the result of a processing event involving a larger precursor. E. coli RR1(pHM2) adsorbed haemin in liquid suspensions as well as from solid media. Subcloning of a 2.6 kb fragment of pHM2 into a shuttle vector permitted the construction of a recombinant Hib clone, DL42(pHM1002), which overexpressed the 51K haemin-binding protein. This 51K protein appears to be peripherally associated with the inner, and possibly outer, membranes of Hib. Affinity chromatography on haemin-agarose was utilized to purify the haemin-binding protein from both E. coli RR1(pHM2) and Hib DL42(pHM1002) to near homogeneity. The use of the antibiotic globomycin in a minicell expression system and radioimmunoprecipitation analysis of Hib proteins intrinsically radiolabelled with [3H]-palmitate indicated that the 51K haemin-binding protein is a lipoprotein.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-2958.1991.tb02107.x
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  • 5
    Electronic Resource
    Electronic Resource
    Molecular cloning of a gene involved in lipooligosaccharide biosynthesis and virulence expression by Haemophilus influenzae type B (1991)
    Oxford, UK : Blackwell Publishing Ltd
    Molecular microbiology 5 (1991), S. 0 
    Details
    ISSN: 1365-2958
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Medicine
    Notes: A wild-type Haemophilus influenzae type b (Hib) genomic DNA library was constructed in the plasmid shuttle vector pGJB103. A virulence-deficient lipooligosaccharide (LOS) mutant of Hib was used as a recipient for genetic transformation to screen this Hib genomic DNA library for genes involved in LOS expression. A recombinant plasmid containing a 7.8 kb Pstl fragment of Hib DNA was shown to transform this LOS mutant to reactivity with a monoclonal antibody (mAb) specific for a wild-type LOS epitope. Transformation of two different virulence-deficient LOS mutants with a 4.4kb BglII fragment of this recombinant plasmid yielded transformants which expressed LOS that bound the wild-type LOS-specific mAb and yielded profiles in sodium dodecyl sulphate/polyacrylamide gradient gel electrophoresis different from those of the original LOS mutants. These transformants with structurally altered LOS molecules also exhibited increased virulence in an animal model for invasive Hib disease. The virulence-transforming ability was further localized to a 1.8kb BglII-AlwNI fragment of the Hib DNA insert. Nucleotide sequence analysis indicated the presence of a single large open reading frame within this fragment. This open reading frame contained 19 consecutive repeats of the tetramer CAAT near the 5’end. Linker insertion mutagenesis was used to demonstrate directly the involvement of this open reading frame in both LOS biosynthesis and virulence expression by Hib.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-2958.1991.tb01884.x
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