Celery top pine, Adventure Bay pine.
Synonymy (Farjon 1998):
Shrubs, or trees to 20 m tall and 50 cm DBH, typically with a single round bole. Branches spreading or ascending to form a pyramidal crown. Bark dark brown with large lenticels, with age becoming scaly and furrowed, with a red or pink inner bark. Twigs straight, round, stiff, smooth, the newest shoots reddish, maturing green. True leaves occur on seedlings and are 10-15 × 1 mm, linear, acute, with a midvein; stomata on the lower surface. Deciduous filiform leaves to 3 mm long appear on new shoots and on margins of phylloclades. Phylloclades are deciduous, mostly simple, flattened, 2.5-5 cm long, mostly cuneate or rhombic in outline, with crenate or lobed margins, with ± parallel venation; color varies from reddish at emergence through bright green, darkening with age. Stomata on the underside, numerous. Pollen cones on short stems branching from a terminal bud, in clusters of 1-5, 5-8 × 2-2.5 mm, pink, maturing yellow, soon deciduous. Seed cones axillary to filiform leaves, or terminal, in clusters of 1-4, each with 2-5 fertile bracts emerging from a red or purple structure 3-5 mm long. Seeds each in a white aril covering 2/3 of the seed, ca. 5 mm long, greenish black (Farjon 2010).
From sea level to timberline in the temperate rain forests of Tasmania at elevations of up to 1200 m. Climate is cool wet maritime with no seasonal drought. The largest and tallest trees occur at low elevations in Eucalyptus forest, typically as an understory tree (some of these eucalypts approach 100 m in height). Above 700-800 m elevation it occurs in woodland with subalpine species such as Eucalyptus coccifera, Nothofagus cunninghamii, N. gunnii, Athrotaxis cupressoides, A. selaginoides, and a rich diversity of shrubs. In alpine settings it occurs in acidic, well-drained soils (typically the parent material is dolerite) as a shrub with a highly diverse woody plant association that often includes the conifers Diselma archeri, Phaerosphera hookeriana, and Podocarpus lawrencei (Farjon 2010 and pers. obs. 2015). You can create a highly detailed map, and access specimen data, using the "search" function at the Australia Virtual Herbarium.
Based on data from 53 collection localities, its climate preferences include a mean annual temperature of 9.0°C, with an average minimum in the coldest month of 1.7°C, and a mean annual precipitation of 1700 mm (Biffin et al. 2011, Table S5). Hardy to Zone 9 (cold hardiness limit between -6.6°C and -1.1°C) (Bannister and Neuner 2001).
A study of the lowland Eucalyptus regnans forest in the Styx Valley found that the stand originated following catastrophic wildfire ca. 1490-1510 A.D., with Eucalyptus and Phyllocladus both establishing in the initial regeneration cohort. Both species established widely in the initial cohort and have seen relatively little regeneration since that time; it follows that both have lifespans exceeding 500 years, and also that Phyllocladus, as well as Eucalyptus, is adapted to stand-replacing fire (Wood et al. 2010).
A plausible estimate is 800 years (Victorian Woodworkers Association [no date]). A ring count of 604 rings in 10 cm is reported from a tree on Mount Read, central Tasmania (IDS 1996). One tree-ring chronology, presumably based on living tree material, covers 665 years (Ogden and Dunwiddie 1982).
Twelve tree-ring chronologies were collected in about 1971 by the Americans Valmore C. LaMarche Jr. and Peter W. Dunwiddie in what were evidently the first explorations of the dendrochronological characteristics of the species (NOAA, Ogden and Dunwiddie 1982). Shortly thereafter, the Australians and New Zealanders began work in the area, assembling chronologies for a variety of native gymnosperms and successfully applying them to a variety of problems in work summarized by D.A. Norton, John Ogden and J.G. Palmer (Palmer and Ogden 1992, Norton and Palmer 1992, Ogden and Dunwiddie 1982). P. aspleniifolius has not been employed as extensively as some other Australasian species, but has been useful in some studies of past climate variation and in estimation of variations in atmospheric carbon-14 production in the southern hemisphere (Barbetti et al. 1995). The earliest tree-ring chronology based on live trees begins in 1450 AD.
Celery top pine has an attractive wood, is commercially harvested, and has been used for boatbuilding, woodturning, flooring, and cabinetry (Tasmanian Timber 2007).
This species presents a classic example of timber mining. The species is currently being exploited as a commercial crop and timber remains available. However, the trees take several centuries to mature. Such a course seems likely to lead to the commercial extinction of the species. Some conservation measures exist: "The conservation of the craftwood resource is related to the conservation of special species timbers as a whole. Large tracts of rainforest (34 per cent of the 565,000 ha total in the State) are reserved in Tasmania's National Parks and World Heritage areas. Of the 40 recognised rainforest plant communities, three are poorly reserved and three are not known in reserves" (Commonwealth of Australia 1999).
This species is quite common within its range in Tasmania. I found it at the Tahune Airwalk, Mount Field National Park, and Lake St. Clair National Park, and Cradle Mountain National Park.
The epithet compares this species to the foliage of a maidenhair fern, specifically, Asplenium ruta-muraria, a European species (Farjon 2010).
Commonwealth of Australia. 1999. Tasmania. http://www.rfa.gov.au/rfa/tas/raa/soceco/ch6_4.html, accessed 2000.04.24, now defunct.
International Dendrology Society. Year Book 1996.
Tasmanian Timber. 2007. Celery Top. http://www.tastimber.tas.gov.au/species/pdfs/Celery.pdf, accessed 2017.12.29.
Wood, S. W., Q. Hua, K. J. Allen, and D. M. J. S. Bowman. 2010. Age and growth of a fire prone Tasmanian temperate old-growth forest stand dominated by Eucalyptus regnans, the world’s tallest angiosperm. Forest Ecology and Management 260:438-447.
Allen, K. J. 2002. The temperature response in the ring widths of Phyllocladus aspleniifolius (celery–top pine) along an altitudinal gradient in the Warra LTER Area, Tasmania. Geographical Research 40(3):287-299.
Allen, K.J. 1998. A dendroclimatological investigation of Phyllocladus aspleniifolius (Labill.) Hook.f. Ph.D. dissertation, The University of Tasmania. 344 pp.
Barbetti, M., T. Bird, G. Dolezal, G. Taylor, R. Francey, E. Cook, and M. Peterson. 1992. Radiocarbon variations from Tasmanian conifers: first results from late Pleistocene and Holocene logs. Radiocarbon 34(3): 806-817.
Barker, P.C.J. 1995. Phyllocladus aspleniifolius: Phenology, germination, and seedling survival. New Zealand Journal of Botany.
Barker, P.C.J. and J.B. Kirkpatrick. 1994. Phyllocladus aspleniifolius: variability in the population structure, the regeneration niche and dispersion patterns in Tasmanian forests. Australian Journal of Botany 42(2):163-190.
Native Conifers of Tasmania, a short but interesting and well illustrated site maintained by the Department of Environment and Land Management, Parks and Wildlife Service, Tasmania. Accessed 2009.03.23.
Last Modified 2018-01-21