Microfossil assemblages are described from the early Neoproterozoic Ma
dley and Browne Formations, western Officer Basin. One chert and eleve
n siliciclastic samples yielded microfossils. Myxococcoides cantabrigi
ensis occurs as pustular mats in the chert sample and Eomicrocystis ma
lgica, Pterospermopsimorpha granulata, Skiagia sp. cf. S. pusilla, and
undetermined species of Obruchevella, Heliconema, and Trachystrichosp
haera are present in acid macerated samples. Leiosphaeridia spp. and S
iphonophycus spp. are also found in fine-grained siliciclastic samples
, with clusters of Synsphaeridium sp. in some samples. These findings
enable a more substantial reconstruction of the palaeoenvironment of S
upersequence 1 in the western Centralian Superbasin. The acanthomorph
acritarchs are considered to be planktonic eucaryotes washed into envi
ronments which ranged from coastal sabkha through to tidal flats, whic
h may be the source of the prokaryotic, benthic, matforming cyanobacte
ria.