Field emission scanning electron microscopy was used to characterize m
ycobiont wall surfaces in Umbilicaria hyperborea from Greenland. To de
termine the precise intrathalline distribution of phenolics, compariso
ns were made of hyphal surface features and dimensions before and afte
r acetone extraction. Stratification was evident within the medulla, a
s extracellular phenolics were observed only on hyphae near or within
the algal zone. The outside diameter of hyphae in this region was thus
significantly greater than in the remainder of the medulla. Surface d
eposits were also examined in 1350-year-old subfossil thalli and hypha
l diameters were compared statistically to those in extant thalli. The
mean hyphal diameter in the upper medulla was nor significantly less
in subfossil specimens than in recent thalli, suggesting that phenolic
cover was maintained in spite of glaciation. However, after ice buria
l phenolic masses tended to be flatter than in recent specimens and fi
nely tuberculate. The appearance of mycobiont hyphae in the cortex of
subfossil thalli seemed to be the same as in extant thalli, except tha
t there tended to be more compressible, smaller and less conglutinated
filaments near the algal layer. (C) 1997 The British Lichen Society.