“…For many centuries after glaciation, plants of open country would have had the opportunity to evolve at lower altitudes before they were confined to alpine and subalpine belts by the expansion of closed forests. High productivity is not characteristic of New Zealand mountain flora but there are many examples of adaptation to particular features of island mountain climate (Scott, 1961(Scott, , 1970Wardle, 1963;Mark, 1969Mark, , 1975Hadley and Rosen, 1974;Payton and Brasch, 1978;Sakai and Wardle, 1978;Benecke and Havranek, 1980). As presented by Cockayne (1928), the mountain vegetation of New Zealand is characterized by tussock grasslands and evergreen forests as well as shrublands, herbfields, and dwarf vegetation, often of cushion form.…”