Cysteine desulphurase plays an important role in environmental adaptation of the hyperthermophilic archaeon Thermococcus kodakarensis.

Abstract

The sulphur atoms of sulphur-containing cofactors that are essential for numerous cellular functions in living organisms originate from L-cysteine via cysteine desulphurase (CSD) activity. However, many (hyper)thermophilic archaea, which thrive in solfataric fields and are positioned near the root of the evolutionary tree of life, lack CSD orthologues. The existence of CSD orthologues in a subset of (hyper)thermophilic archaea is of interest with respect to the evolution of sulphur-trafficking systems for the cofactors. This study demonstrates that the disruption of the csd gene of Thermococcus kodakarensis, a facultative elemental sulphur (S(0))-reducing hyperthermophilic archaeon, encoding Tk-CSD, conferred a growth defect evident only in the absence of S(0), and that growth can be restored by the addition of S(0), but not sulphide. We show that the csd gene is not required for biosynthesis of thiamine pyrophosphate or molybdopterin, irrespective of the presence or absence of S(0), but is necessary for iron-sulphur cluster biosynthesis in the absence of S(0). Recombinant form of Tk-CSD expressed in Escherichia coli was obtained and it was found to catalyse the desulphuration of L-cysteine. The obtained data suggest that hyperthermophiles might benefit from a capacity for CSD-dependent iron-sulphur cluster biogenesis, which allows them to thrive outside solfataric environments.