THE VEGETATION OF SUB-ANTARCTIC CAMPBELL ISLAND

Citation
Cd. Meurk et al., THE VEGETATION OF SUB-ANTARCTIC CAMPBELL ISLAND, New Zealand journal of ecology, 18(2), 1994, pp. 123-168
Citations number
62
Categorie Soggetti
Ecology
ISSN journal
01106465
Volume
18
Issue
2
Year of publication
1994
Pages
123 - 168
Database
ISI
SICI code
0110-6465(1994)18:2<123:TVOSCI>2.0.ZU;2-I
Abstract
The vegetation of Campbell Island and its offshore islets was sampled quantitatively at 140 sites. Data from the 134 sites with more than on e vascular plant species were subjected to multivariate analysis. Out of a total of 140 indigenous and widespread adventive species known fr om the island group, 124 vascular species were recorded; 85 non-vascul ar cryptogams or species aggregates play a major role in the vegetatio n. Up to 19 factors of the physical environment were recorded or deriv ed for each site. Agglomerative cluster analysis of the vegetation dat a was used to identify 21 plant communities. These (together with cryp togam associations) include: maritime crusts, turfs, megaherbfields, t ussock grasslands, and shrublands; mid-elevation swamps, flushes, bogs , tussock grasslands, shrublands, dwarf forests, and induced meadows; and upland tundra-like tussock grasslands, tall and short turf-herbfie lds, bogs, flushes, rock-ledge herbfields, and fellfields. Axis 1 of t he DCA ordination is largely a soil gradient related to the eutrophyin g impact of marine spray, sea mammals and birds, and nutrient flushing . Axis 2 is an altitudinal (or thermal) gradient. Axis 3 is related to soil reaction and to different kinds of animal influence on vegetatio n stature and species richness, and Axis 4 also appears to have fertil ity and animal associations. Autecological interpretation of the data demonstrates clear niche segregation of congeneric species and ;specie s with similar growth forms. The notable megaherbs and giant tussocks may be an adaptation to harvesting nutrients from the aerosol precipit ate. Heat harvesting in the cool, cloudy, wet, and windy climate may a lso be implicated. The history of farming and natural disturbances has resulted in a complex mosaic of vegetation-soil systems of varying ma turity. Their putative dynamic interrelationships are depicted in term s of impacts of burning, grazing, marine animals and climate change an d subsequent recovery or primary and secondary succession.