Examination of fracture surfaces near the fusion crust of the martian meteo
rite Allan Hills (ALH) 84001 have been conducted using scanning electron mi
croscopy (SEM) and atomic force microscopy (AFM) and has revealed structure
s strongly resembling mycelium. These structures were compared with similar
structures found in Antarctic cryptoendolithic communities. On morphology
alone, we conclude that these features are not only terrestrial in origin b
ut probably belong to a member of the Actinomycetales, which we consider wa
s introduced during the Antarctic residency of this meteorite. If true, thi
s is the first documented account of terrestrial microbial activity within
a meteorite from the Antarctic blue ice fields. These structures, however,
do not bear any resemblance to those postulated to be martian biota, althou
gh they are a probable source of the organic contaminants previously report
ed in this meteorite.