Titlebook: Ecological Systems of the Geobiosphere; 2 Tropical and Subtr Heinrich Walter,Siegmar-W. Breckle Textbook 1986 Springer-Verlag Berlin Heidel

ACRO

書目名稱Ecological Systems of the Geobiosphere影響因子(影響力)




書目名稱Ecological Systems of the Geobiosphere影響因子(影響力)學(xué)科排名




書目名稱Ecological Systems of the Geobiosphere網(wǎng)絡(luò)公開度




書目名稱Ecological Systems of the Geobiosphere網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Ecological Systems of the Geobiosphere被引頻次




書目名稱Ecological Systems of the Geobiosphere被引頻次學(xué)科排名




書目名稱Ecological Systems of the Geobiosphere年度引用




書目名稱Ecological Systems of the Geobiosphere年度引用學(xué)科排名




書目名稱Ecological Systems of the Geobiosphere讀者反饋




書目名稱Ecological Systems of the Geobiosphere讀者反饋學(xué)科排名

Eeg332

The Soilsrs innumerable heterotrophic fungi, and everywhere a great diversity of bacteria. Many vertebrates live partly in the soil; a few, such as the mole, live entirely below ground. Amongst the invertebrates, there is a very large number of phytophagous, saprophagous and zoophagous forms, from large spec

Intrepid

GIBE

Consumerscycle” of organic matter (Vol. I, p.41). Mere descriptions of the fauna and the habits of individual animal groups or species is not enough. Today we are still only at the stage of preliminary investigations necessary to achieve this goal. In his . Tischler (1976) describes the characteristic featur

tolerance

是限制

是限制

The Pedobiome of Zonobiome Ier rock is primarily poor in nutrients. The other pedobiomes, such as dry lithobiomes on limestone, psammobiomes, helobiomes and halobiomes are almost as well-developed as in ZB II, and will thus be dealt with in the discussion of the latter, although certain differences will also be indicated.

橫截,橫斷

The Zonoecotonesthe equator, in the region of the zenith rains. These always fall where the sun is precisely at the zenith at midday. Thus, the rainfall belt shifts with the position of the sun — during the northern summer, as far as the northern tropic; during the southern summer, as far as the southern tropic: th

Countermand

Climatic Conditions in east Africa around 8° N; it does not cover the Ethiopian highlands or the dry Horn of Africa. South of the equator this zonobiome covers an even larger area, extending far to the south; it does not include that part of the west coast affected by the Benguela current, nor the equatorial east coas

努力趕上

Soil Conditionst become stone hard when the soil dries out, forming lateritic crusts or “hardpan” (ZB I, p. 18). In the perhumid climate of ZB I this seldom occurs, but is frequently the case in the humid-arid climate of ZB II. Zonobiome I is mainly limited to the large equatorial basins, whereas in Africa south o