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Titlebook: Vegetation of the Earth and Ecological Systems of the Geo-biosphere; Heinrich Walter Book 19853rd edition Springer-Verlag Berlin Heidelber

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書目名稱Vegetation of the Earth and Ecological Systems of the Geo-biosphere
編輯Heinrich Walter
視頻videohttp://file.papertrans.cn/981/980915/980915.mp4
叢書名稱Heidelberg Science Library
圖書封面Titlebook: Vegetation of the Earth and Ecological Systems of the Geo-biosphere;  Heinrich Walter Book 19853rd edition Springer-Verlag Berlin Heidelber
描述We shall limit our observations to the conditions in natural ecosystems, since it would be beyond the scope of this book to embark upon a consideration of secondary, man-made ecosystems. 2. Classification of the Geo-biosphere into Zonobiomes The biosphere is the thin layer of the earth‘s surface to which the phenomena connected with living matter are confined. On land, this comprises the lowest layer of the atmosphere permanently inhabited by living organisms and into which plants extend, as well as the root-containing portion of the lithosphere, which we term the soil. Living organisms are also found in all bodies of water, to the very depths of the oceans. In a watery medium, however, cycling of material is achieved by means other than those on land, and the organisms (plankton) are so different that aquatic ecosystems have to be dealt with separately. The biosphere is therefore subdivided into (a) the geo-biosphere comprising terrestrial ecosystems, and (b) the hydro-biosphere, comprising aquatic ecosystems, which is the field of hydrobiologists (oceanographers and limnologists) . Our studies are confined to the geo-biosphere (Walter 1976), which constitutes the habitat of man a
出版日期Book 19853rd edition
關鍵詞Habitat; Population; Rain; Zonobiom; biome; biosphere; classification; ecology; ecosystem; environment; physio
版次3
doihttps://doi.org/10.1007/978-3-642-96859-4
isbn_softcover978-3-540-13748-1
isbn_ebook978-3-642-96859-4Series ISSN 0073-1595
issn_series 0073-1595
copyrightSpringer-Verlag Berlin Heidelberg 1985
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Zonobiome of the Temperate-Nemoral Climateicts in the southern Andes and in New Zealand, it is absent from the Southern Hemisphere. The phenomenon of facultative leaf-shedding has already been met within the tropics. There the leaves are shed only when the water balance is disturbed by a lenghty period of drought, and this leaf loss decreas
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Zonobiome of the Arid-Temperate Climateca, it occupies the entire Midwest, from southern Canada to the Gulf of Mexico. The degree of aridity varies considerably, and four subzonobiomes can be distinguished: (1) a semiarid subzonobiome having a short period of drought, with steppe and prairie vegetation (Fig. 117, Chkalov); (2) a very ari
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Zonobiome of the Arctic Tundra Climatemean temperature above 0°C, and sometimes as few as 55. The low summer temperatures are partially due to the large amount of heat required to melt the snow and thaw out the ground. Winters are rather mild in the oceanic regions but extremely cold in the continental regions (Fig. 155). However, the c
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Book 19853rd editionn of secondary, man-made ecosystems. 2. Classification of the Geo-biosphere into Zonobiomes The biosphere is the thin layer of the earth‘s surface to which the phenomena connected with living matter are confined. On land, this comprises the lowest layer of the atmosphere permanently inhabited by liv
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