Sl. Stephenson et al., A COMPARATIVE BIOGEOGRAPHICAL STUDY OF MYXOMYCETES IN THE MID-APPALACHIANS OF EASTERN NORTH-AMERICA AND 2 REGIONS OF INDIA, Journal of biogeography, 20(6), 1993, pp. 645-657
Although species lists for particular localities have been compiled by
numerous workers, relatively few biogeographical studies of myxomycet
es (plasmodial slime moulds) have been carried out. In the present stu
dy, the data represented by a total of 3788 collections of myxomycetes
made during the period of 1954-90 from two study areas in the mid-App
alachians of eastern North America and study areas in northwestern and
southern India were analysed to obtain information on the biogeograph
ical relationships and patterns of occurrence of these organisms. The
climate of the study area in southern India is tropical/subtropical, w
hereas both study areas in eastern North America and the one in north
western India have a temperate climate. Based on coefficient of commun
ity indices calculated for all possible combinations of the four diffe
rent data sets, southern India had the lowest overall similarity (mean
index = 0.322) to the other study areas. Members of the Physarales ma
de up a much greater proportion (63%) of the collections from southern
India than elsewhere, whereas members of the Liceales were conspicuou
sly under-represented when compared to the other study areas. The majo
rity of collections ( > 63%) from southern India occurred on leaf litt
er and other types of non-woody plant debris, whereas > 80% of all col
lections from eastern North America and north western India were made
from woody substrates. These results suggest that myxomycetes show rec
ognizable patterns of latitudinal variation not unlike those described
for many other groups of organisms. Not only is the assemblage of spe
cies found in tropical/subtropical regions of the world distinctly dif
ferent from that of temperate regions, but the species present also ex
hibit quite different patterns of distribution with respect to the typ
es of substrates upon which they typically occur.