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Open AccessJournal ArticleDOI

Ecological significance of compatible solute accumulation by micro‐organisms: from single cells to global climate

David T. Welsh
- 01 Jul 2000 - 
- Vol. 24, Iss: 3, pp 263-290
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TLDR
The evolutionary selection for the accumulation of a specific compatible solute may not depend solely upon its function during osmoadaptation, but also upon the secondary benefits its accumulation provides, such as increased tolerance of other environmental stresses prevalent in the organism's niche.
Abstract
The osmoadaptation of most micro-organisms involves the accumulation of K+ ions and one or more of a restricted range of low molecular mass organic solutes, collectively termed ‘compatible solutes’. These solutes are accumulated to high intracellular concentrations, in order to balance the osmotic pressure of the growth medium and maintain cell turgor pressure, which provides the driving force for cell extension growth. In this review, I discuss the alternative roles which compatible solutes may also play as intracellular reserves of carbon, energy and nitrogen, and as more general stress metabolites involved in protection of cells against other environmental stresses including heat, desiccation and freezing. Thus, the evolutionary selection for the accumulation of a specific compatible solute may not depend solely upon its function during osmoadaptation, but also upon the secondary benefits its accumulation provides, such as increased tolerance of other environmental stresses prevalent in the organism’s niche or even anti-herbivory or dispersal functions in the case of dimethylsulfoniopropionate (DMSP). In the second part of the review, I discuss the ecological consequences of the release of compatible solutes to the environment, where they can provide sources of compatible solutes, carbon, nitrogen and energy for other members of the micro-flora. Finally, at the global scale the metabolism of specific compatible solutes (betaines and DMSP) in brackish water, marine and hypersaline environments may influence global climate, due to the production of the trace gases, methane and dimethylsulfide (DMS) and in the case of DMS, also couple the marine and terrestrial sulfur cycles.

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Bacterial osmoadaptation: the role of osmolytes in bacterial stress and virulence

TL;DR: The molecular mechanisms governing the accumulation of these compounds, both in Gram-positive and Gram-negative bacteria, are reviewed, focusing specifically on the regulation of their transport/synthesis systems and the ability of these systems to sense and respond to changes in the osmolarity of the extracellular environment.
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Production of atmospheric sulfur by oceanic plankton: biogeochemical, ecological and evolutionary links

TL;DR: It is not only phytoplankton biomass, taxonomy or activity, but also food-web structure and dynamics that drive the oceanic production of atmospheric sulfur, and the viewpoint on the ecological and evolutionary basis of this amazing marine biota-atmosphere link is changing.
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Osmosensing and osmoregulatory compatible solute accumulation by bacteria

TL;DR: The molecular bases for the modulation of gene expression and transport activity by temperature and medium osmolality are under intensive investigation with emphasis on the role of the membrane as an antenna for osmo- and/or thermosensors.
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Drought Stress and Root-Associated Bacterial Communities.

TL;DR: A synthesis of observed trends in recent studies is provided and possible directions for future research are discussed that are hoped will provide for more knowledgeable predictions about community responses to future drought events.
References
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Journal ArticleDOI

Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate

TL;DR: The major source of cloud-condensation nuclei (CCN) over the oceans appears to be dimethylsulphide, which is produced by planktonic algae in sea water and oxidizes in the atmosphere to form a sulphate aerosol as mentioned in this paper.
Journal ArticleDOI

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TL;DR: Osmolyte compatibility is proposed to result from the absence of osmolytes interactions with substrates and cofactors, and the nonperturbing or favorable effects of oSMolytes on macromolecular-solvent interactions.
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Iron deficiency limits phytoplankton growth in the north-east Pacific subarctic

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TL;DR: In this paper, a comparative survey of aerobic and anaerobic mineralization in the sea bed based on direct rate measurements of the two processes is presented, and the results demonstrate a surprisingly high contribution from the sulphate-reducers.
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