Serpentinized troctolites exposed near the Kairei Hydrothermal Field, Central Indian Ridge: Insights into the origin of the Kairei hydrothermal fluid supporting a unique microbial ecosystem

Abstract

The vent fluids of the Kairei Hydrothermal Field (KHF) on the Central Indian Ridge near the Rodriguez Triple Junction are atypical. They have a very high H 2 concentration, a relatively high Si concentration, and a remarkably low CH 4/H 2 ratio. Recently, particular attention has been paid to the KHF, because the hydrothermal fluids are suggested to support a hydrogen-based hyperthermophilic subsurface lithoautotrophic microbial ecosystem (HyperSLiME), which is considered to be a likely modern analogue for the early Earth ecosystems prior to photosynthesis. Despite the increasing interest in the fluid chemistry and associated biota, the origin of the unusual chemistry of the hydrothermal fluids is still uncertain. Here we suggest interaction of seawater with troctolite recently discovered from small hills near the KHF, provide a possible explanation for the composition of the KHF fluids. Dives with the manned submersible Shinkai 6500 recovered plagioclase dunite, troctolites, and olivine gabbros, which generally constitute the lower oceanic crust. Microscopic observations revealed that olivine crystals in the samples were partly to completely replaced by serpentine and magnetite, indicating the generation of H 2 by serpentinization reactions between olivine and hydrothermal fluids. Theoretical model calculations predict that the high H 2 and high Si concentrations of the hydrothermal fluids can be attributed to serpentinization of the troctolites and subsequent hydrothermal reactions with basaltic wall rocks under the KHF. The unique geological setting of the Kairei hydrothermal system, where deep crustal rocks are emplaced in the shallower part of oceanic crust, is considered to be responsible for the unusual chemistry of the Kairei hydrothermal fluids driving the occurrence of the HyperSLiME.