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Seasonal Fluctuations in Ionic Concentrations Drive Microbial Succession in a Hypersaline Lake Community

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Seasonal Fluctuations in Ionic Concentrations Drive Microbial Succession in a Hypersaline Lake Community UC San Diego UC San Diego Previously Published Works Title Seasonal fluctuations in ionic concentrations drive microbial succession in a hypersaline lake community. Permalink https://escholarship.org/uc/item/7k55w6d9 Journal The ISME journal, 8(5) ISSN 1751-7362 Authors Podell, Sheila Emerson, Joanne B Jones, Claudia M et al. Publication Date 2014-05-01 DOI 10.1038/ismej.2013.221 Peer reviewed eScholarship.org Powered by the California Digital Library University of California The ISME Journal (2014) 8, 979–990 & 2014 International Society for Microbial Ecology All rights reserved 1751-7362/14 www.nature.com/ismej ORIGINAL ARTICLE Seasonal fluctuations in ionic concentrations drive microbial succession in a hypersaline lake community Sheila Podell1, Joanne B Emerson2,3, Claudia M Jones2, Juan A Ugalde1, Sue Welch4, Karla B Heidelberg5, Jillian F Banfield2,6 and Eric E Allen1,7 1Marine Biology Research Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA; 2Department of Earth and Planetary Sciences, University of California, Berkeley, CA, USA; 3Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA; 4School of Earth Sciences, Byrd Polar Research Center, Ohio State University, Columbus, OH, USA; 5Department of Biological Sciences, University of Southern California, Los Angeles, CA, USA; 6Department of Environmental Science, Policy, and Management, University of California, Berkeley, CA, USA and 7Division of Biological Sciences, University of California, San Diego, La Jolla, CA, USA Microbial community succession was examined over a two-year period using spatially and temporally coordinated water chemistry measurements, metagenomic sequencing, phylogenetic binning and de novo metagenomic assembly in the extreme hypersaline habitat of Lake Tyrrell, Victoria, Australia. Relative abundances of Haloquadratum-related sequences were positively correlated with co-varying concentrations of potassium, magnesium and sulfate, but not sodium, chloride or calcium ions, while relative abundances of Halorubrum, Haloarcula, Halonotius, Halobaculum and Salinibacter-related sequences correlated negatively with Haloquadratum and these same ionic factors. Nanohaloarchaea and Halorhabdus-related sequence abundances were inversely correlated with each other, but not other taxonomic groups. These data, along with predicted gene functions from nearly-complete assembled population metagenomes, suggest different ecological phenotypes for Nanohaloarchaea and Halorhabdus-related strains versus other community members. Nucleotide percent G þ C compositions were consistently lower in community metagenomic reads from summer versus winter samples. The same seasonal G þ C trends were observed within taxonomically binned read subsets from each of seven different genus-level archaeal groups. Relative seasonal abundances were also linked to percent G þ C for assembled population genomes. Together, these data suggest that extreme ionic conditions may exert selective pressure on archaeal populations at the level of genomic nucleotide composition, thus contributing to seasonal successional processes. Despite the unavailability of cultured representatives for most of the organisms identified in this study, effective coordination of physical and biological measurements has enabled discovery and quantification of unexpected taxon-specific, environ- mentally mediated factors influencing microbial community structure. The ISME Journal (2014) 8, 979–990; doi:10.1038/ismej.2013.221; published online 12 December 2013 Subject Category: Microbial population and community ecology Keywords: archaea; halophile; hypersaline; metagenome; microbial succession Introduction measurements of both physical and biological factors, but obtaining this information over temporal Microbial studies in extreme environments seek to and spatial scales relevant to natural microbial understand how extraordinary physicochemical communities is challenging. Extreme hypersaline stresses shape adaptive responses in both individual aqueous environments harboring limited phylo- organisms and entire communities. Achieving this genetic diversity provide tractable model ecosystems goal requires coordinated, detailed, accurate to confront these challenges (Demergasso et al., 2008; Bodaker et al., 2009; Pagaling et al., 2009; Correspondence: EE Allen, Marine Biology Research Division, Oh et al., 2010; Boujelben et al., 2012; Makhdoumi- University of California, San Diego, Scripps Institution of Kakhki et al., 2012; Oren, 2013). Although overall Oceanography, 9500 Gilman Drive MC0202, La Jolla, CA 92093- salt concentrations in these habitats are, by defini- 0202, USA. E-mail: [email protected] tion, at or exceeding the limits of ionic solubility, Received 20 September 2013; revised 5 November 2013; accepted geochemical variation in water sources as well as 10 November 2013; published online 12 December 2013 minerals dissolved from surrounding rocks and Seasonal ion concs drive microbial succession S Podell et al 980 sediments contribute to variable ratios of different Microorganisms able to survive the most extreme ionic species over space and time (Javor, 1989; Oren, hypersaline environments employ a ‘salt-in’ strategy 2013). Evaporative concentration and mineral pre- to achieve osmotic stability, balancing high extra- cipitation, accelerated at higher temperatures, selec- cellular sodium with high intracellular potassium tively deplete some ionic species while enriching (Oren et al., 2002). Direct measurements in both the others (Javor, 1989). Intermittent rainfall, agricul- archaeaon Halorubrum sodomense and the bacterium tural runoff and intrusion from groundwater aqui- Salinibacter ruber confirm this pattern, demonstrating fers provide additional sources of geochemical intracellular potassium levels exceeding 3.0 M variability (Macumber, 1992; Ionescu et al., 2012). (Oren, 1998; Oren et al., 2002). Extreme halophiles The biological effects of dissolved ionic species also contain much higher intracellular magnesium are mediated not only by absolute concentrations levels than non-halophiles. Cultured Halobacterium but also by ionic ratios (Park, 2012), which affect the salinarum cells, for example, were found to have efficiency of cellular ion pumps and antiporters total intracellular magnesium concentrations exceeding used for balancing intracellular osmolarity and 100 mM, more than three-fold higher than Escherichia establishing electrochemical gradients for energy coli cells (30 mM) measured using the same technique production and nutrient transport (Oren, 2013). (de Me´dicis et al., 1986). However, work in this Ionic concentrations also affect the aqueous solubi- area is not sufficiently complete to determine lity of oxygen, which is vanishingly low in extreme whether intracellular concentrations of some ions hypersaline waters (Sherwood et al., 1991). Para- might be better controlled than others under doxically, the dominant microorganisms in these naturally occurring conditions, or whether particular habitats are aerobic, heterotrophic Archaea, along combinations or ratios of ion concentrations might with bacteria from the genus Salinibacter. Although have synergistic effects that are not apparent when most cultivated microbial strains isolated from varying ionic species one at a time (Park, 2012). extreme hypersaline environments are capable of Extensive changes to protein amino acid composi- facultative anaerobic fermentation, they grow opti- tion have been observed in microorganisms using a mally in the laboratory under aerobic conditions salt-in strategy, presumably to counter potential (Dyall-Smith, 2009; Andrei et al., 2012). The adverse effects of high salt concentrations on protein surprising abundance of oxygen-loving organisms structure (Fukuchi et al., 2003; Bolhuis et al., 2008). in environments with such low oxygen solubility Specifically, proteins of salt-in halophiles are may be explained by the occurrence of non- enriched in amino acids with negatively charged equilibrium conditions at the air-water interface, side chains, enhancing solubility and depleted in providing locally higher oxygen availability. The residues with bulky hydrophobic groups, increasing extent to which temporal differences in mixing structural flexibility. Little is known about whether efficiency from wind or other factors might affect nucleic acid sequences undergoing replication, oxygen distribution through the water column in transcription and/or translation might also need natural hypersaline environments is largely special adaptations to function in organisms using a unknown, but may vary greatly, especially over salt-in strategy for osmotic balance. Nucleic acid small distances relevant to microbial localization. structure and stability are known to be exquisitely One the most successful microbes in extreme sensitive to ionic concentrations in vitro, especially hypersaline waters, the square archaeaon Halo- magnesium, which is orders of magnitude more quadratum walsbyi, has a specialized cell morphology active than sodium or potassium in increasing utilizing large intracellular gas vesicles to facilitate double-stranded DNA melting temperature (Hartwig, energy-efficient flotation of tightly packed, nearly two- 2001; Owczarzy et al., 2008) and stabilizing RNA dimensional flat colonies (Walsby, 1980; Bolhuis et al., hairpin structures (Bizarro et al., 2012). 2004). This unique morphology may be an adaptation Cultured
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