We
synthesize ZnS–ZnO heterostructure nanorings at ∼680
°C under carrier gases with various [CO2]/[N2] ratios simulating an anoxic and weakly reduced atmosphere on early
Earth. The synthesized nanorings consist of a ZnS–ZnO bilayered
stem, ZnO teeth, and ZnS wing-like structures between the teeth and
the ZnS layer. O atoms are supplied through the decomposition of CO2 presumably catalyzed by the ZnS surface. The respective growth
directions of ZnS and ZnO layers in the stem are [0001] and [011̅1],
and ZnO teeth are directed outward from the ring. The nanorings are
structurally different from ZnS–ZnO nanorings having inward-directed
teeth, which were grown under an oxygen-containing ambient environment.
Contrary to the assumption of sulfide dominance including ZnS and
MnS while disregarding oxygen-containing minerals such as ZnO on early
Earth, we show that ZnS–ZnO nanorings, which are more advantageous
in CO2 reduction efficiency, could be formed.