Sulfur isotope's signal of nanopyrites enclosed in 2.7 Ga stromatolitic organic remains reveal microbial sulfate reduction
2018
Microbial sulfate reduction (MSR) is thought to have operated very early on Earth and
is often invoked to explain the occurrence of sedimentary sulfides in the rock record.
Sedimentary sulfides can also form from sulfides produced abiotically during late di-
agenesis
or metamorphism.
As both biotic and abiotic processes
contribute
to the bulk
of sedimentary sulfides, tracing back the original microbial signature from the earliest
Earth record is challenging. We present in situ sulfur isotope data from nanopyrites
occurring in carbonaceous remains lining the domical shape of stromatolite knobs of
the 2.7- Gyr- old Tumbiana
Formation
(Western
Australia).
The analyzed
nanopyrites
show a large range of
δ
34
S values of about 84‰ (from −33.7‰
to +50.4‰).
The rec
-
ognition that a large
δ
34
S range of 80‰ is found in individual
carbonaceous-
rich layers
support the interpretation that the nanopyrites were formed in microbial mats through
MSR by a Rayleigh
distillation
process
during early diagenesis.
An active microbial
cy
-
cling of sulfur during formation of the stromatolite may have facilitated the mixing of
different sulfur pools (atmospheric and hydrothermal) and explain the weak mass in-
dependent signature (MIF-
S) recorded in the Tumbiana Formation. These results con-
firm that MSR participated actively to the biogeochemical cycling of sulfur during the
Neoarchean and support previous models suggesting anaerobic oxidation of methane
using sulfate in the Tumbiana environment.
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