Microbial anhydrobiosis.

Jason Bosch, Gilda Varliero, John E Hallsworth, Tiffany D Dallas, David Hopkins, Beat Frey, Weidong Kong, Pedro Lebre, Thulani P Makhalanyane, Don A Cowan

Journal: Environmental microbiology 2022;23(11):6377-6390

PMID: 34347349

Abstract

The loss of cellular water (desiccation) and the resulting low cytosolic water activity are major stress factors for life. Numerous prokaryotic and eukaryotic taxa have evolved molecular and physiological adaptions to periods of low water availability or water-limited environments that occur across the terrestrial Earth. The changes within cells during the processes of desiccation and rehydration, from the activation (and inactivation) of biosynthetic pathways to the accumulation of compatible solutes, have been studied in considerable detail. However, relatively little is known on the metabolic status of organisms in the desiccated state; that is, in the sometimes extended periods between the drying and rewetting phases. During these periods, which can extend beyond decades and which we term 'anhydrobiosis', organismal survival could be dependent on a continued supply of energy to maintain the basal metabolic processes necessary for critical functions such as macromolecular repair. Here, we review the state of knowledge relating to the function of microorganisms during the anhydrobiotic state, highlighting substantial gaps in our understanding of qualitative and quantitative aspects of molecular and biochemical processes in desiccated cells.

© 2021 Society for Applied Microbiology and John Wiley & Sons Ltd.

Address: Centre for Microbial Ecology and Genomics, Department of Biochemistry, Genetics and Microbiology, University of Pretoria, Pretoria, 0002, South Africa.; Institute for Global Food Security, School of Biological Sciences, Queen's University Belfast, 19 Chlorine Gardens, Belfast, Northern Ireland, BT9 5DL, UK.; Scotland's Rural College, Edinburgh, EH9 3JG, UK.; Rhizosphere Processes Group, Swiss Federal Research Institute WSL, Birmensdorf, 8903, Switzerland.; State Key Laboratory of Tibetan Plateau Earth System Science (LATPES), Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS), Beijing, 100101, China.
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