作者: H.-P. Blume , D. M. White , L. Beyer , M. Bölter , D. Kuhn
DOI: 10.1007/978-3-642-56318-8_9
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摘要: Soil formation in the Antarctic is a recognised process. The occurrence of accumulations organic matter despite hostile climate, and soils by debris mosses, lichens algae widespread (Campbell Claridge 1987; Beyer et al. 1999). This leads to mineral which may contain large amounts soil maritime (Blume 1996). In contrast, patches are associated locally with shallow coastal regions East Antarctica (Beyer