Flume experiments and analytical approaches are undertaken to determin
e the stability of flat-lying Ediacaran organisms in fluid flow. Organ
isms such as Dickinsonia would not have been viable if reconstructed a
s free-living worms or syncytia. Models of flat-lying Ediacarans occup
ying a range of densities well beyond those of suggested modern analog
s were dislodged by fluid flow taken as typical of Ediacaran paleoenvi
ronments. Analytical rests suggest that parameters such as thickness o
f the organism and its coefficient of friction have little effect over
the range of flows being considered here. These results lead to four
non-exclusive interpretations of fossils of flat-lying Ediacarans: (1)
The organisms have been transported from a quieter environment (in wh
ich case their pristine preservation is similarly puzzling); (2) they
had a density approaching that of a flatfish; (3) they were secured to
the substrate in some manner; (4) they lived partially or wholly bene
ath the substrate surface.