
Abstract: "Although it is not known when or where life on Earth began, some of the 
earliest habitable environments may have been submarine-hydrothermal 
vents. Here we describe putative fossilized microorganisms that are at 
least 3,770 million and possibly 4,280 million years old in ferruginous 
sedimentary rocks, interpreted as seafloor-hydrothermal vent-related 
precipitates, from the Nuvvuagittuq belt in Quebec, Canada. These 
structures occur as micrometre-scale haematite tubes and filaments with 
morphologies and mineral assemblages similar to those of filamentous 
microorganisms from modern hydrothermal vent precipitates and analogous 
microfossils in younger rocks. The Nuvvuagittuq rocks contain 
isotopically light carbon in carbonate and carbonaceous material, which 
occurs as graphitic inclusions in diagenetic carbonate rosettes, apatite
 blades intergrown among carbonate rosettes and magnetite–haematite 
granules, and is associated with carbonate in direct contact with the 
putative microfossils. Collectively, these observations are consistent 
with an oxidized biomass and provide evidence for biological activity in
 submarine-hydrothermal environments more than 3,770 million years ago."
Read More:
http://www.bbc.com/news/science-environment-39117523
http://www.nature.com/nature/journal/v543/n7643/full/nature21377.html