Ead. Mitchell et al., Relationships among testate amoebae (Protozoa), vegetation and water chemistry in five Sphagnum-dominated peatlands in Europe, NEW PHYTOL, 145(1), 2000, pp. 95-106
To study the relationships between groups of organisms and the degree to wh
ich these relationships are consistent across major climatic gradients, we
analysed the testate amoeba (Protozoa) communities, vegetation and water ch
emistry of one peatland in five countries: Switzerland, The Netherlands, Gr
eat Britain, Sweden and Finland, as part of the BERI (Bog Ecosystem Researc
h Initiative) project. The relationships between the different data sets an
d subsets were investigated by means of detrended correspondence analysis,
canonical correspondence analysis and Mantel permutation tests. The compari
son of data on vegetation and testate amoebae showed that inter-site differ
ences are more pronounced for the vegetation than for the testate amoebae s
pecies assemblage. Testate amoebae are a useful tool in multi-site studies
and in environmental monitoring of peatlands because: (1) the number of spe
cies in Sphagnum-dominated peatlands is much higher than for mosses or vasc
ular plants; (2) most peatland species are cosmopolitan in their distributi
ons and therefore less affected than plants by biogeographical distribution
patterns, thus differences in testate amoeba assemblages can be interprete
d primarily in terms of ecology; (3) they are closely related to the ecolog
ical characteristics of the exact spot where they live, therefore they can
be used to analyse small-scale gradients that play a major role in the func
tioning of peatland ecosystems. This study revealed the existence of small-
scale vertical gradients within the vegetation and life-form niche separati
on in response to water chemistry. The deep-rooted plants such as Carex spp
. and Eriophorum spp. are related to the chemistry of water sampled at or n
ear the ground water table, whereas the mosses are not. Testate amoebae wer
eshown to be ecologically more closely related to the chemistry of water sa
mpled at or near the water table level and to the mosses than to the deep-r
ooted plants.