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  • 1
    Electronic Resource
    Electronic Resource
    The Equatorial Atlantic Mid-Ocean Channel: An Ultra High-Resolution Image of Its Burial History Based on TOPAS Profiles (1997)
    Springer
    Marine geophysical researches 19 (1997), S. 115-135 
    Details
    ISSN: 1573-0581
    Keywords: Mid-ocean channels ; Equatorial Atlantic ; Parametric echosounder sedimentary infilling
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Multibeam bathymetric and ultra high-resolution seismic data reveal that the distal course of the Equatorial Atlantic Mid-Ocean Channel (EAMOC) extends further east and south than was previously known, and is controlled by the presence of morphologic highs related to the Fernando de Noronha Fracture Zone. Distal course of the EAMOC is buried by sediments, and does not have bathymetric expression on the seafloor. The channel fill consists of three seismic sequences, suggesting that the recent geological evolution of the channel is composed of successive phases of decreasing sedimentary activity that finally resulted in its complete burial. Tectonic and volcanic activity related to the Fernando de Noronha Fracture Zone and Ridge, together with the effect of strong pulses of the Antarctic bottom water current during the upper Pliocene are suggested to have contributed to the progressive burial and the final abandonment of the EAMOC.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1004273902719
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    Sedimentary evolution of the northwestern Alboran Sea during the Quaternary (1992)
    Springer
    Geo-marine letters 12 (1992), S. 144-149 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Five depositional bodies occur within the Quaternary deposits of the northwestern Alboran Sea: Guadalmedina-Guadalhorce prodelta, shelf-edge wedges, progradational packages, Guadiaro channel-levee complex, and debris flow deposits. The sedimentary structure reflects two styles of margin growth characterized: 1) by an essentially sediment-starved outer, shelf and upper slope and by divergent slope seismic facies; 2) by a prograding sediment outer shelf, and parallel slope seismic facies. Eustatic oscillations, sediment supply, and tectonic tilting have controlled the type of growth pattern, and the occurrence of the depositional bodies. Debris flows were also controlled locally by diapirism.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02084925
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    Paper (German National Licenses)
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  • 3
    Electronic Resource
    Electronic Resource
    Pleistocene progradational growth pattern of the northern Catalonia continental shelf (northwestern Mediterranean) (1994)
    Springer
    Geo-marine letters 14 (1994), S. 264-271 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Pleistocene sedimentary growth pattern of the northern Catalonia continental shelf is characterized by the vertical stacking of seaward downlapping regressive deposits. These deposits are characterized by a progradational development, with oblique clinoforms of low angle in the middle continental shelf, that become more inclined seaward in the outer continental shelf and shelfbreak. Eustatic sea level fluctuations controlled the development of this sedimentary pattern, whereas sediment supply conditioned the nonuniform progradation along the continental shelf and subsidence due to both sediment loading and tectonics controlled its preservation through and along the continental shelf.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01274062
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    Paper (German National Licenses)
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  • 4
    Electronic Resource
    Electronic Resource
    Geotechnical properties and preliminary assessment of sediment stability on the continental slope of the northwestern Alboran Sea (1992)
    Springer
    Geo-marine letters 12 (1992), S. 150-156 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Laboratory analysis of core samples from the western Alboran Sea slope reveal a large variability in texture and geotechnical properties. Stability analysis suggests that the sediment is stable under static gravitational loading but potentially unstable under seismic loading. Slope failures may occur if horizontal ground accelerations greater than 0.16g are seismically induced. The, Alboran Sea is an active region, on which earthquakes inducing accelerations big enough to exceed the shear strength of the soft soil may occur. Test results contrast with the apparent stability deduced from seismic profiles.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02084926
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  • 5
    Electronic Resource
    Electronic Resource
    Association study of proposed candidate genes/regions in a population of Spanish asthmatics (2000)
    Springer
    European journal of epidemiology 16 (2000), S. 745-750 
    Details
    ISSN: 1573-7284
    Keywords: Association ; Asthma ; Atopy ; Bronchial hyperresponsiveness ; Candidate genes ; Linkage disequilibrium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract A number of genes/regions have recently been reported to be linked to asthma or its related phenotypes (i.e. atopy and bronchial hyperresponsiveness), by genetic linkage and allele-sharing methods. We have performed a case–control study comparing the allelic distribution of nine microsatellite markers and two genetic variants in a group of patients attended at emergency room departments because of an acute attack of asthma with respect to an external healthy population of controls. A total of 146 asthmatic subjects and 50 population controls from Barcelona, Spain, were genotyped for nine microsatellite markers from some asthma/atopy candidate genes/regions: the β-subunit of the high-affinity IgE receptor (FcεRI-β) located on chromosome 11; the 5q31–32 candidate region; the T-cell receptor genes, TCR-α on chromosome 14 and TCR-β on chromosome 7. Two genetic variants of the β-subunit of the high-affinity IgE receptor (FcεRI-β) gene were also analyzed. None of the asthmatic or control individuals carried the Ile181Leu variant. There were no significant differences between asthmatic and control subjects neither for the polymorphic markers nor for the other variant of the β-subunit of the high-affinity IgE receptor (FcεRI-β) gene. No association could be observed in this sample of Spanish asthmatics with the genes/regions studied.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1026758319621
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  • 6
    Electronic Resource
    Electronic Resource
    Influence on survival of p24 antigen levels in patients with AIDS or advanced AIDS related complex treated with zidovudine (1992)
    Springer
    European journal of clinical microbiology & infectious diseases 11 (1992), S. 1181-1185 
    Details
    ISSN: 1435-4373
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract In a prospective study sixty-eight patients consecutively diagnosed as having AIDS or advanced ARC who were started on zidovudine therapy were followed up for a median period of 725 days. In the 20 patients who had a baseline p24 antigen level above 20 pg/ml, there was a statistically significant trend towards reduction of the p24 antigen levels after the first month of treatment. The median time of survival of the 68 patients was 702 days and the median symptom-free period was 510 days. Treatment with zidovudine significantly reduced the p24 antigen levels. However, the life expectancy and the symptom-free period were not statistically different in the patients with p24 antigen levels always below or with levels always above two arbitrarily chosen cut-off points of 20 pg/ml and 50 pg/ml, respectively.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01961142
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