In this section
Inland & alpine
- Basic cliffs, scarps and tors
- Boulderfields of acidic rocks (non-volcanic)
- Boulderfields of calcareous rocks
- Braided riverbeds
- Calcareous cliffs, scarps and tors
- Calcareous screes
- Cliffs, scarps and tors of acidic rocks
- Cliffs, scarps and tors of quartzose rocks
- Cloud forests
- Frost hollows
- Granitic gravel fields
- Granitic sand plains
- Inland outwash gravels
- Inland saline (salt pans)
- Inland sand dunes
- Limestone erosion pavements
- Old tephra (>500 years) plains (= frost flats)
- Recent lava flows
- Sandstone erosion pavements
- Screes of acidic rocks
- Strongly leached terraces and plains
- Ultrabasic boulderfields
- Ultrabasic cliffs, scarps and tors
- Ultrabasic hills
- Ultrabasic screes
- Volcanic boulderfields
- Volcanic debris flows or lahars
- Volcanic dunes
- Young tephra plains and hillslopes
Ultrabasic rocks contain very little quartz or feldspar and are composed essentially of ferromagnesium silicates, metal oxides, and native metals (Anon 1962). They produce soils with low concentrations of major plant nutrients and high concentrations of toxic metals such as nickel, chromium, and cobalt. Screes are the accumulation of course debris, ranging from gravel (2-64 mm) and cobbles (64-256 mm) to patches of boulders (> 256 mm) mantling slopes (often in association with protruding in situ bedrock). Screes have also been referred to as 'shingle slides' (Fisher 1969). Slopes are generally somewhat below the natural angle of repose of about 32 degrees. Screes are often armoured on the surface with large fragments overlying finer particles that provide a rooting medium for plants. Screes can form under a forest canopy in some situations but this ecosystem comprises mostly openland above treeline. These conditions result in vegetation that is often characterised by stunted, slow growing, small-leaved trees and shrubs. Plants characteristic of fertile soils can be present, but these sites also support ultrabasic endemics and ecotypes of widespread species e.g., sun orchids (Thelymitra pauciflora).
Ultramafic screes, serpentine screes
Notable flora and fauna
There is little information pertaining specifically to ultrabasic screes and the following list is derived from those present on ultrabasic sites generally. Threatened plants include the nationally critical Red Hills forget-me-not (Myosotis laeta), spiral sun orchid (Thelymitra matthewsii) and Notothlaspi (a) (CHR 363071: Red hills), the nationally endangered Pittosporum serpentinum, the naturally uncommon Berggren's sedge (Carex berggrenii), Carex devia, Travers' sedge (Carex traversii), Speden's mountain daisy (Celmisia spedenii), Red Hills snow tussock (Chionochloa defracta), Surville Cliffs haloragis (Haloragis erecta subsp. cartilaginea), Veronica urvilleana, Red Hills button daisy (Leptinella pyrethrifolia var. linearifolia), Monro’s forget-me-not (Myosotis monroi), Pimelea suteri, Pittosporum pimeleoides subsp. majus, ultramafic cushion poa (Poa acicularifolia subsp. ophitalis).
Not threatened (Holdaway et al. 2012)
Ultrabasic screes exclude the majority of species, including exotic weeds, but invasion by pines (Pinus spp.) and Douglas fir (Pseudotsuga menziesii) is of concern on the Red Hills Ridge in Marlborough. They offer no potential for agriculture and are too remote to be influenced by development on adjacent land other than forestry plantations in Marlborough. Historically, some areas of ultrabasic rocks were mined and they are still potentially threatened by this activity. Shrubland on the scree margins is susceptible to fire especially in drier interior sites (Red Hills/Richmond Range).
Where do they occur?
There are very limited areas of screes on ultrabasic rocks in Nelson-Marlborough on Red Hills Ridge, and in South Westland on Little Red Hill at the head of the Barrier River and on the western side of the Olivine Range. It is worth noting that some references in the literature to screes on ultrabasic rock do not fit our definition where the substrate is merely loose rock or stones over consolidated bedrock (e.g. Dun Mt., Nelson).
Dawson JW 1988. Scree Plants in Forest Vines to Snow Tussocks: The Story of New Zealand Plants. Victoria University Press, Wellington.
Dawson JW 1988. Serpentine Vegetation in Forest Vines to Snow Tussocks: The Story of New Zealand Plants. Victoria University Press, Wellington.
Fisher FJF 1969. Rock, shingle-slide and riverbed. In: Knox GA ed. The natural history of Canterbury. Wellington, AH and AW Reed. Pp. 106-116.
Lee WG 1992. New Zealand ultramafics. In: Roberts BA, Proctor J eds The ecology of areas with serpentinized rocks. A world view. The Netherlands, Kluwer. Pp. 375-418.
Lee WG, Hewitt AE 1982. Soil changes associated with development of vegetation on an ultramafic scree, northwest Otago, New Zealand. Journal of the Royal Society of New Zealand 12 : 229-242.
McIntosh PD, Lee WG 1986. Soil-vegetation relationships on the Dun Mountain Ophiolite Belt at West Dome, Southland, New Zealand. Journal of the Royal Society of New Zealand 16: 363-379.
Wardle P 1991. Vegetation of New Zealand. Cambridge University Press. 672 p.
Wilson JB, Lee WG, Mark AF 1990. Species diversity in relation to ultramafic substrate and to altitude in southwestern New Zealand. Vegetatio 86: 15-20.