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consist of a central area of granite and gneiss whereas most of the younger deposits have
Andrias 19
The asci in Phaeopyxis have an immature overall thickened wall (laterally †1-1.5
, W ang & N orton 1995, B ayartogtokh 2000a, 2004a) although some Belba species have
However, the significance of the species is great becau- se most have very restricted
Many cirques and gorges disturb the “general” slope morphology and have their own