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Succession of terrestrial macrofungi along a deglaciation gradient at Glacier Blåisen, South Norway
Author(s) -
Alfredsen Gry,
Høiland Klaus
Publication year - 2001
Publication title -
nordic journal of botany
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.333
H-Index - 33
eISSN - 1756-1051
pISSN - 0107-055X
DOI - 10.1111/j.1756-1051.2001.tb01335.x
Subject(s) - deglaciation , transect , ecology , biology , abiotic component , canonical correspondence analysis , vegetation (pathology) , ecological succession , glacier , pioneer species , species richness , glacial period , medicine , paleontology , pathology
A survey of terrestrial macrofungi along a deglaciation gradient from the glacier forefront to the established vegetation has been performed. The study was accomplished along a transect from Lake Finsevann to Glacier Blåisen, South Norway. Fortysix 6 m × 6 m plots divided into 9 subplots were positioned along this transect. The frequency of fruit bodies of each species in each plot was given on a 0–9 scale reflecting their occurrence in the subplots. Biotic and abiotic environmental variables for the plots were also recorded. The numerical methods used include principal component analysis (PCA), detrended correspondence analysis (DCA), and canonical correspondence analysis (CCA). Totally 99 species of macrofungi were recorded; 80.8 % of the species belonged to the Basidiomycota and 19.2 % to the Ascomycota. About one third of the species was only found once. In general, the species richness was highest on the glacier forefront, lowest in the most established vegetation. The proportion of species of Ascomycota was highest close to the glacier front. The main gradient in the data set was shown related to the primary ecological succession following the retreat of glaciers. The second gradient was possibly related to fine scale variation due to local moisture, microtopography, and secondary distribution. Of the variation in composition of species, 3 % can be ascribed to abiotic variance, 10 % to vascular plant variance, and 16 % to the combination of the abiotic and vascular plant component of variation. The results are discussed in the light of the time since deglaciation and the influence of certain biotic and abiotic environmental factors.