Abstract

Osmotic changes are common challenges for marine microorganisms. Bacteria have developed numerous ways of dealing with this stress, including reprogramming of global cellular processes. However, specific molecular adaptation mechanisms to osmotic stress have mainly been investigated in terrestrial model bacteria. In this work, we aimed to elucidate the basis of adjustment to prolonged salinity challenges at the proteome level in marine bacteria. The objects of our studies were three representatives of bacteria inhabiting various marine environments, Shewanella baltica, Vibrio harveyi and Aliivibrio fischeri. The proteomic studies were performed with bacteria cultivated in increased and decreased salinity, followed by proteolytic digestion of samples which were then subjected to liquid chromatography with tandem mass spectrometry analysis. We show that bacteria adjust at all levels of their biological processes, from DNA topology through gene expression regulation and proteasome assembly, to transport and cellular metabolism. The finding that many similar adaptation strategies were observed for both low- and high-salinity conditions is particularly striking. The results show that adaptation to salinity challenge involves the accumulation of DNA-binding proteins and increased polyamine uptake. We hypothesize that their function is to coat and protect the nucleoid to counteract adverse changes in DNA topology due to ionic shifts.

Highlights

  • Osmotic stress comprises a relatively common environmental challenge encountered by bacteria in their natural habitats

  • We investigated the effect of challenges caused by nonoptimal salinity on proteomes of S. baltica, A. fischeri and V. harveyi by growing the bacteria at low, optimal and high salt concentrations

  • Based on the calculated growth rates (Figure 1A), low, optimal and high salinity were determined as salt concentrations of 0.2, 0.7 and 2.0% for S. baltica, 2.0, 4.0 and 6.0% for A. fischeri, and 1.5, 3.0 and 4.0% for V. harveyi, respectively

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Summary

Introduction

Osmotic stress comprises a relatively common environmental challenge encountered by bacteria in their natural habitats. Microbial response to osmotic stress involves active changes in the concentration of specific osmoregulatory solutes [6,7]. These so-called compatible solutes can be accumulated up to molar concentrations without disturbing cellular processes, such as the metabolic pathways or DNA replication [1]. Glycine betaine is a common osmolyte for both bacteria and marine invertebrates [9]. In the case of bacteria, it can be synthesized in the cells from choline or transported from the environment by the ProP and ProU transport systems [5,9]

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