In this paper we evaluate the utility of ergosterol as a measure of fungal
biomass in temperate soils. We summarise published findings and compare the
m with data from our own broad-scale assessment of the relationship between
ergosterol and ATP in a range of temperate soils. Two hundred and ninety f
ive plots (three cores taken from each 10 x 10 m plot) in seven ecotypes we
re sampled. Soils ranged from entirely mineral to entirely organic (0.01-46
% C-org) and sites comprised two primary successions, one on shingle ridge
on the south coast of England and one in the slack of a dune blow-out on th
e south coast of Wales, various meadow, pasture (some restored after openca
st mining) and ancient woodland soils throughout England and acid forest so
ils in Central Europe. We found a strong relationship between egosterol and
ATP (r(2) = 0.80), which was largely unaffected by the key soil properties
of C-org, C/N ratio, moisture and pH. The sources and implications of the
20% of residual variance were explored by assuming that the error was compo
unded from three sources: the inaccuracies in methods of analysis of ergost
erol and ATP, the failings of each of the variables to estimate their under
lying populations (i.e., fungal and total biomass, respectively) (e(var)),
and the non-equivalence of these populations (i.e., their incomplete overla
p) (e(pop)). By partitioning the residual variance into components correspo
nding to the levels of sampling, we estimated that the sum of the systemati
c portions of e(var) and e(pop) formed as much as three quarters of the 20%
of residual variance in the ATP-ergosterol correlation, leaving just 5% mo
stly due to random error. Despite this close relationship, the attainment o
f a universal conversion factor between ergosterol and fungal biomass, appl
icable to all temperate soils, remains elusive and problematic. Many proble
ms are caused by a lack of comparability between the various measures of fu
ngal and total biomass used and the reliability, or otherwise, of extrapola
tions based on measures of axenic cultures (in contrast to in-situ measurem
ents). The issue is further complicated by the non-linearity of the relatio
nship between fungal biomass and fungal surface area; ergosterol is more co
rrectly an index of the latter since it is a principal membrane sterol. We
conclude that ergosterol is likely to be a reliable indicator of the extent
of fungal membranes in temperate soils, if not an accurate measure of fung
al biomass. (C) 2000 Elsevier Science Ltd. All rights reserved.