New sub-micrometre analyses of the famous Apex chert ‘microfossils’ are presented.
Candidate filamentous ‘microfossils’ comprise stacks of phyllosilicate grains.
The distribution of carbon is inconsistent with fossilised prokaryote cells.
Carbon also occurs throughout the quartz matrix and in late stage fractures.
‘Microfossils’ are thus reinterpreted as hydrothermally mediated mineral artefacts.