The alpine subnival
belt (4300-5000 m a.s.l.) of Himalaya-Hengduan Mountains (HHM) experiences a
summer monsoonal climate, with heavy rain fall interrupted by short periods of
intense solar radiance in the growing period. Low temperature caused by rain
(or cloud) slows the development of flowers and seeds; there has been an
extensive interest in study how low temperature drives the evolution ofhighly-specialized morphological features in alpine plants. For example, the
densely pubescent inflorescences of Saussurea medusa (known as ‘Himalayan
woolly plant’) have a key role in temperature control and water repellence in
cool and humid summer. On the other hand, the overlapping large
semi-translucent bracts covering racemes of Rheum nobile (known as ‘Himalayan
glasshouse plant’) function to warm floral tissues and have protective effects
against UV-B radiation and rain.
However, none of the research has ever focused
on the selective pressure of high temperature caused by transient strong solar
radiation (particularly in the midday) in alpine plant. High temperaturereduces pollen viability and some species have evolved cooling mechanisms(evaporation and self-shading) in tropical environments. In a recent study, we
used Eriophyton wallichii Bentham (Lamiaceae), an alpine perennial herb with
woolly structures (particularly in leaves, corolla and calyxes) and overlapping
leaves covering reproductive organs, to explore the specialized morphology of
an alpine plant adapted to growth and reproduce in sites characterized by
transient heavy rainfall and strong solar radiation.
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