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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 3 (1987), S. 75-80 
    ISSN: 1432-0789
    Keywords: Mariut region ; Correspondence analysis ; Heterogamia syriaca ; Lygos raetam ; Predators
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Soil mesofauna (sensu Ghilarov, i.e., larger than 1 mm) was sampled from under four shrub species (Lygos raetam, Thymelaea hirsuta, Lycium shawii, and Josonia candicans) growing on the littoral oolitic sand dunes at Gharbaniat, 53 km W of Alexandria, Egypt, for a period of more than 30 months, spanning 3 years. Population density (PD) was calculated in relation to area of shrub canopy. Seasons were considered, according to the prevailing climatic conditions as well as to earlier physiological studies on the animals concerned, as: four “winter” months, four “summer” months and two months for each of the transitional seasons “spring” and “autumn”. The PD values obtained for each season thus defined were combined for the 41 taxa that were sampled. The table of these data was treated by correspondence analysis (CA) and ascending hierarchic classification (AHC), by the Roux DATA-VISION programme (suitable for Apple). Results from such treatment show that fauna as related to shrub species are differentiated along the first factorial axis, while as related to seasons they are differentiated along the second axis. Taxa common to all shrubs and to all seasons are centrally placed and cause some confusion in the resolution. Summer taxa are more distantly placed than those related to the other three seasons. Fauna under Lygos is richer, more diverse, and more complementary as regards trophic levels (with predators), and could probably be the source for replenishing the fauna of the other shrubs at all seasons. The AHC method did not show a similarly clear differentiation.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2000-11-28
    Description: Vladimir Ivanovitch Vernadsky was a Russian mineralogist and crystallographer by training (St. Petersburg Univ.). He was born in St. Petersburg, on the 12th of March 1863, and died on the 6th of January 1945, in Moscow. About 1910, he became a geochemist and later on a founding father of Biogeochemistry, due to his concern with the "questions related to the importance of life on the geological history of the Earth". This new direction was the result of his field observations, of his broad mineralo-geological knowledge, and his studies, from 1917, on the phenomena of life in the biosphere, confirmed by many of his readings, like the book by Clarke (1908), "The Data of Geochemistry", and in particular the "Hydrogéologie" of J. B. Lamarck (1802). From this, and knowing the Lamarck work, and the Suess work and the definition of a biosphere he redefined and worked the biosphere concept in larger biogeochemical terms.
    Print ISSN: 2193-3081
    Electronic ISSN: 1399-1183
    Topics: Biology
    Published by Copernicus on behalf of European Ecological Federation.
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