“…Higher altitude areas tend to be dominated by typically Antarctic fellÞeld, or wind desert areas, while the lowlands have closed, tundra-like vegetation (Gremmen 1981, Bergstrom and. On the basis of their histories, and lack of vascular vegetation, Chown (1989) grouped these fellÞeld habitats and the rocky shoreline areas characteristic of most of these islands (e.g., de Villiers 1976, Knox 1994) into a single, Ôepi-lithicÕ biotope. The habitats constituting this biotope are thought to have been continually present, even during the Neogene glacial maxima, when many of the islands had a substantial ice cover (Hall 1990, Chown 1994, Bergstrom and Chown 1999.…”