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Information on Dwarf Grasslands
Developing management options
The majority of tussock grassland research has focussed on determining the vegetation history of the mountain lands, and how pastoral management practices have influenced vegetation succession patterns. Only recently has grassland research started to look at the issue of progressive successional changes occurring on retired land (i.e. what vegetation changes will take place when tussock grasslands are retired from grazing and burning). The majority of studies have focussed on determining the impacts of pastoral use on induced montane fescue tussock grasslands (Festuca novae-zealandiae), the most widespread short tussock grassland found to the east of the Main Divide. Few studies have focussed on dryland dwarf grassland communities. There are therefore still many information gaps to be filled, some of which are currently addressed in the FRST-funded research programme "Improved Management Systems for Tussock Grasslands". For more information about this research programme and how to become involved, contact the programme leader Dr Ockie Bosch at boscho@landcare.cri.nz.
In the meantime, the suggested management options have to draw on broad principles and "best guesses" by ecologists, or observations made by people who live and work in the tussock grasslands. Such "best guesses" may be appropriate in some situations, but not others. They will be updated as and when more information becomes available.
More about...
Factors influencing the distribution and characteristics of tussock grasslands
for more information on environmental gradients that determine the distribution of tussock grassland types, or the management factors that have influenced the characteristics of tussock grasslands. |
Vegetation change since human settlement
if you want further information on a generalised model for vegetation change, east of the Main Divide. |
Dryland dwarf grasslands- a vegetation history
Practically all the vegetation of lowland intermontane basins of Central Otago would have been modified since the arrival of man approximately 1000 years ago. Evidence from buried wood, charcoal and pollen samples suggest that the Maniototo District and adjacent mountain slopes and uplands below the climatic tree line were forested ( Molloy et al. 1963) except on some large areas of saline soils. McGlone (1989) has decribed the vegetation of the very driest districts in the South Island that existed 3000 years before the present as a low conifer-broadleaf forest. Toatoa (Phyllocladus alpinus), Hall's totara (Podocarpus hallii), broadleaf (Griselinia littoralis), kowhai (Sophora microphylla), kanuka (Kunzea ericoides and Myrsine australis made up this distinctive forest type.
Buried charcoal and pollen analysis of sites in Central Otago indicate that deforestation by natural fires began at least 2500 y.b.p., with a change to a cooler and drier climate preventing regeneration. Such natural deforestation was patchy rather than extensive throughout the region, and confined to the drier valley floors and lower slopes of areas such as the Maniototo and adjacent ecological districts (McGlone 1989), where the annual rainfall was below 500mm, or on NW slopes in areas receiving up to 800mm annual rainfall (Wardle 1991). Thus the climax vegetation of the dry lowland basins, at the time when the first Polynesians arrived, would have been low scrub and grassland (short tussocks and sward grasses).
These grasslands were further modified by early pastoralists, who burnt the vegetation to improve accessibility, and grazed large numbers of sheep. The introduction of the rabbit, whose numbers reached plague proportions, further exacerbated the problem of grassland depletion, and helped to increase the extent of dwarf grasslands by preventing the revegetation of taller statured dryland short tussock grassland species.
In more recent times, other exotic plants, such as wilding pines, are establishing in dwarf grasslands, despite the severe soil mosture deficit.
Many areas which once supported dryland short tussock grasslands have been the focus of large-scale irrigation schemes. Such areas have been transformed to improved pasture and orchards. In the last decade, vineyard establishment in Central Otago has further modified areas of dwarf grasslands.
The long-term control of rabbits in some areas of dwarf grassland is resulting in an increase of taller vegetation (mainly exotic), at the expense of the low-lying plants characteristic of dwarf grasslands.
Future threats to the extent of dwarf grasslands include the establishment of lifestyle blocks, and the associated change in vegetation cover as people plant trees, lawns and pasture in an effort to make their homes more sheltered.
Management of Dwarf Grasslands
Little information is available regarding the impacts of management on dwarf grasslands. However, dwarf grasslands occur at very dry sites, as well as where excessive grazing by rabbits and/or stock has maintained a very open and low-growing vegetation cover. Patches of bare ground often accompany this community. In Central Otago, several small and rare annual herbs (e.g. Ceratocephalus pungens, Myosurus minimus, Myosotis minutiflora) grow in this habitat, and are dependant on the continued existence of an open and low-statured vegetation cover. Some level of grazing is therefore likely to be necessary to ensure that taller statured grasses and herbs do not take over (Walker et al. 1995). Such plants will compete for light, water and nutrients, and change the microclimate by increasing the surface roughness of the vegetation. Such changes are likely to occur where grazing ceases at all but the driest sites.
Vegetation succession
if you want more information on factors influencing vegetation succession (includes model for vegetation succession). |
Buffering
The relationship an area managed for conservation purposes has with it's surrounding landscape is important. Ideally, the area should be surrounded by land which will buffer it from external influences which may compromise the conservation values.
The buffer zone may:
- act as a fire break, thereby protecting neighbouring land from wild fires occurring in dense tussock grasslands, or preventing controlled fires on pastoral land inadvertently burning an area managed for conservation.
- protect the area from inadvertent AOSTD drift from neighbouring land
- protect the area in terms of the hydrological processes.
- help reduce the rate of spread of some weed species into the area e.g. intensive grazing between a forest and an ungrazed tussock grassland helps reduce the establishment of wilding trees from that forest.
Weed control
Weed spread is likely to be a problem at low to mid altitudes because these grasslands have been highly modified by pastoral activities (grazing, trampling, aerial over-sowing and top dressing, burning) and may neighbour land which has a predominantly exotic plant cover. Monitoring of the area will be necessary to determine which weed species are present and the extent of the problem. An assessment of the feasibility of controlling the weeds will then have to be made.
The need to control weed species is dependent on the characteristics of the weed (e.g. will it overtop the tussocks; does its' dispersal mechanism make it an aggressive invader?) and their impact on the indigenous ecosystem in question. Tall woody weeds are considered to be the most troublesome weed in tussock grasslands, as they have the potential to overtop and shade-out the tussocks. Wilding trees are a growing problem in Otago and inland Canterbury.
The spread of Hieracium in short tussock grasslands
Irrespective of whether managed for pastoral use, or soley for conservation purposes, many short tussock grasslands have a significant component of hawkweed.
A large number of studies have been conducted to investigate the relationship between grazing management and rate of Hieracium pilosella spread, and associated trends on vegetation composition. However, no studies have focussed specifically on tussock grasslands dominated by bristle tussock.
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