Mountain toatoa (Silba 1986).
Syn: P. aspleniifolius var. alpinus (Silba 1986), P. trichomanoides var. alpina Parlatore 1868. Type locality: Nelson. P. alpinus is polymorphic and possibly several varieties with different geographical ranges are included in the present description. Adequate comparison of New Zealand forms with those of the Tasmanian P. aspleniifolius have not been made (Allan 1961).
Monoecious, strongly aromatic shrub or tree up to 9 m tall, trunk short, up to 40 cm in diameter. True leaves occur only on seedlings and occasionally on young plants. They are narrow-linear, acute, deciduous, up to 1.5 cm long, on older plants shorter. Phylloclades alternate to subopposite, rhachis short. Phylloclades of juvenile plants up to 2 cm long, deeply divided, thin, with narrow-linear segments, glaucous below; of adults thick, coriaceous, 1-2.5 cm, occasionally up to 6 cm long, 2 cm wide. Phylloclade shape various; narrow-rhomboid or spathulate, sparingly or much lobed, often elliptic to obovate, cuneate at base, apex subacute to broad-obtuse, margins crenate, leaf-denticles small. Pollen cones 5-6 mm long in fascicles of 2-5, rarely solitary, apical, with pedicels 1-2 mm long; sporophylls with small variously shaped apiculi, stems erose. Female cones arise along the margins or on the stalks of the phylloclades; receptacle of red, fleshy scales; mature heads ca. 6-7 mm diameter. Seeds nutlike, black, exserted, ovoid, compressed, ca. 2.5 mm long, obtuse; cupule white, irregularly lobed, up to 2/3 length of seed (Allan 1961, Salmon 1996).
New Zealand: N and S Islands from latitude 36° 50' southwards. It is found on the Coromandel Peninsula between Cape Colville and Te Aroha and from the volcanic plateau southwards between 900 m and 1,600 m to Mt Cargill, Fiordland and Southland. In South Westland and Southland it occurs down to sea level (Allan 1961, Salmon 1996). Based on data from 1119 collection localities, its climate preferences include a mean annual temperature of 8.7°C, with an average minimum in the coldest month of -0.7°C, and a mean annual precipitation of 2705 mm (Biffin et al. 2011, Table S5). Hardy to Zone 8 (cold hardiness limit between -12.1°C and -6.7°C) (Bannister and Neuner 2001).
One tree-ring chronology, presumably based on living tree material, covers 259 years (data on file with ITRDB).
Development of tree-ring chronologies apparently began a collection in the 1970s at Pegleg Creek (S Island: 42°S, 171°E; 279 years) by Dunwiddie (1979). P. alpinus tree ring data have been used in a study of climate change in New Zealand over the last thousand years (Burrows and Greenland 1979). The most recent survey of dendrochronological work with the species is provided by Norton and Palmer (1992).
This species is very common in the alpine and subalpine shrublands and adjacent montane forests of Tongariro National Park. It can be seen from the north trailhead up to Ketetahi Hut on the Tongariro Crossing, and on all of the walks along the Bruce Road and around Whakapapa Village on Mount Ruapehu. It is probably found on most other subalpine scrub trails in the Ruapehu area as well. The walk up to Ketetahi Hut is particularly interesting because the mountain toatoa grows as a forest tree up to about 9 m tall beneath taller trees (including Podocarpus cunninghamii) near the start of the walk, and diminishes in stature as the track climbs upward until it is only a battered shrub growing in the company of Podocarpus nivalis and Lepidothamnus laxifolius.
Wardle, P. 2001. Distribution of native forest in the upper Clutha district, Otago, New Zealand. New Zealand Journal of Botany 39:435-446. Available: http://www.royalsociety.org.nz/Site/publish/Journals/nzjb/2001/34.aspx, accessed 2009.03.22, now defunct.
Wardle, P. 2001. Holocene forest fires in the upper Clutha district, Otago, New Zealand. New Zealand Journal of Botany 39:523-542. Available: http://www.royalsociety.org.nz/Site/publish/Journals/nzjb/2001/42.aspx, accessed 2009.03.22, now defunct.
The New Zealand Plant Conservation Network, accessed 2010.10.03.
Last Modified 2013-03-28