a. Zonation (parallel bands of vegetation) occurs due to changing abiotic/climatic conditions (e.g. temperature, oxygen levels, carbon dioxide levels, soil depth, wind speed, aspect, water availability, nutrient availability);
b. Plants which can survive in colder conditions are found higher in the mountains (such as conifers, which begin photosynthesizing as soon as temperatures rise above 0∘C ) / colder temperatures means that not all types of vegetation/species can grow there/changes the types of vegetation;
c. Plants (e.g. deciduous trees) which require longer growing seasons are found lower in the mountains (as the snow melts more quickly in spring) / water availability reduces with altitude which restricts the type of plant species that can grow there;
d. Soils become thinner with altitude, limiting (tree) root development, (creating alpine meadows);
e. Plants that can tolerate thin/nutrient-poor soils dominate higher elevations (leading to alpine meadows rather than dense forests);
f. South-facing slopes are warmer and snow melts more quickly, resulting in higher upper limits for each zone / north-facing slopes are cooler/retain snow longer providing shorter growing seasons and different vegetation zones compared to similar altitudes on south-facing slopes;
g. At higher altitudes, increased exposure to wind reduces tree growth/limits plant height/favours low-growing/wind-resistant species;
h. Increased UV radiation at high altitudes favours plants with protective adaptations (such as waxy leaves or compact growth);
i. With increase in altitude there is a reduction in oxygen levels which results in a change in the types of vegetation;
Note to examiners: Accept the converse where appropriate. For credit response must link to either zonation or change in vegetation type. Do not accept 'less vegetation' instead of 'changes to the type of vegetation'.
Marking guidance: