Distribution and factors influencing the characteristics of tussock grasslandsEnvironmental Gradients (from Scott, 1969) The distribution of tussock grassland types is related to two environmental gradients. The first is a moisture gradient of rainfall, soil water holding capacity, etc., and in New Zealand is probably best approximated by a soil moisture or soil type classification. The second is a temperature gradient, which in the native grasslands is largely dictated by the combined effects of altitude and aspect. In particular localities, the temperature gradient also corresponds to a sequence of topographic landforms e.g. slopes, moraine, flood plains etc. The relationship between the grasslands and associated vegetation types according to these two gradients is given below.
Grasslands are bounded by Celmisia herbfields at higher altitudes and where low temeperatures
prevail; and by beech forest, occassionally by podocarp forest and by associated shrubs on
wettest sites; and by pastures comprising mainly exotic species on low altitude warm sites.
Tall tussocks occur at higher altitudes, ranging from Chionohcloa rigida on drier sites, through to
other species at moist sites. Remnants of copper tussock occur on intermediate temperature and
moisture sites.
At lower altitudes are the short tussock grasslands in which Festuca novae-zelandiae is generally
the dominant species, together with a large area of modified tussock grassland derived from
Festuca grasslands or in which Rytidosperma species are prominent.
Disturbance and stress factors which shape the characteristics of tussock grasslands (from
McKendry & O'Connor, 1990)
Tussock grasslands to the east of the Main Divide have been used for pastoral activities for the
past 150 years. The characteristics of a tussock grassland type are therefore not only a reflection
of these environmental factors, but also the disturbance and stress factors associated with pastoral
activities. These are outlined in the table below.
Ecological interpretation of pastoral activity (from McKendry and O'Connor, 1990)
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