Origins and Ecology of the Sierran Alpine Flora and Vegetation
Chabot BF and Billings WD. 1972. Origins and Ecology of the Sierran Alpine Flora and Vegetation. Ecological Monographs. 42(2):163-199
The alpine flora of the Sierra Nevada has developed relatively recently and largely in situ from western American sources. The Sierra thus provides a good site for an attempt to answer the question "How does an alpine flora originate?". The primary study area was a transect from the desert near Bishop, CA (1400 m) to Piute Pass in the Sierra Nevada (3540 m). Upward along the transect the vegetational gradient is Ephedra nevadensis-Tetradymia spinosa desert shrub, Pinus monophylla-Artemesia tridentata open woodland, Pinus jeffreyi open forest, Pinus murrayana forest, Pinus albicaulis-subalpine herbaceous vegetation, and scattered alpine communities. Environmental monitoring stations were maintained at several locations along the transect during two summers. Laboratory experiments showed several physiological responses to be characteristic of Sierran alpine populations. These may be important in plant evolution and migration into an alpine habitat. 1. Germination of seeds from alpine plants occurred maximally between 20 and 30 degrees C. Constitutive dormancy is a minor factor; the low winter temperatures of the alpine zone appear to operate as an exogeneous dormancy control. Desert and low elevation species of this area are predominantly winter-germinators and have maximum germination at low temperatures. 2. Mature alpine plants have strong dormancy control by short photoperiod; dormancy of lower elevation populations may be induced by either short or long photoperiods. 3. Temperatures of the upper photosynthetic compensation point and maximum net photosynthesis are lower in plants of alpine species. 4. Low temperature regimes cause plants to shift dark respiration to higher rates when compared with plants of the same species from high temperature regimes; this change appears to have both genotypic and phenotypic causes. 5. Considerable acclimation of dark respiration to a change in temperature can occur in as little as 8-10 hours, beginning 1-2 hours after the change. The speed of acclimation increases with increasing temperature and is genetically based. Populations from higher elevations have faster acclimation rates than plants from lower elevations. This characteristic could allow alpine plants to adapt rapidly to changing weather conditions. 6. Acclimation of dark respiration does not appear to be related to changes in leaf water potential, diffusion resistance, or isozymes of three dehydrogenases. It is related to changes in the rate of mitochondrial oxidation. 7. Translocation of starch from chloroplasts at low temperatures was impaired in desert species, but was maintained in an alpine species. Although a number of physiological processes in alpine plants are adapted to low temperatures, there is no indication that any single process, or adaptation to temperature alone, is responsible for the evolution and success of an alpine species. Efficient utilization of a short, cold growing season may be the most important selective characteristic in the origin of an alpine flora. Some genera of lower elevations near the Sierra are already pre-adapted, in their winter and spring growth patterns, to such a low-temperature regime and may have provided a part of the present Sierran alpine gene pool.
- Type
- Journal Article
- Authors
- Chabot, Brian; Billings, W.
- Units
- SIEN
- Keywords
- Alpine Plants, Desert, Eastern Sierra Nevada, Vascular Plants, vegetational gradient