Carbon and Nitrogen Substrate Utilization in the Marine Bacterium Sphingopyxis Alaskensis Strain RB2256

Carbon and Nitrogen Substrate Utilization in the Marine Bacterium Sphingopyxis Alaskensis Strain RB2256

The ISME Journal (2009) 3, 1036–1052 & 2009 International Society for Microbial Ecology All rights reserved 1751-7362/09 $32.00 www.nature.com/ismej ORIGINAL ARTICLE Carbon and nitrogen substrate utilization in the marine bacterium Sphingopyxis alaskensis strain RB2256 Timothy J Williams1, Haluk Ertan1,2, Lily Ting1 and Ricardo Cavicchioli1 1School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney, New South Wales, Australia and 2Department of Molecular Biology and Genetics, Science Faculty, Istanbul University, Vezneciler, Istanbul, Turkey Sphingopyxis alaskensis is a marine member of the Alphaproteobacteria that is adapted to heterotrophic growth under nutrient-depleted (oligotrophic) conditions. S. alaskensis strain RB2256 is an ultramicrobacterium (cell volume o0.1 lm3), and has a genome size larger than that of the ultramicrobacterium ‘Candidatus Pelagibacter ubique’ HTCC1062 (SAR11 clade of Alphaproteobac- teria): 3.35 versus 1.31 Mbp. In this study, we investigate the carbon and nitrogen metabolism of strain RB2256 using an integrated approach that combines growth and enzyme assays, proteomics and genome analysis. S. alaskensis is able to use specific amino acids and putrescine as a sole carbon and nitrogen source, and higher energy-yielding substrates such as glucose and trehalose as carbon sources. Alanine, in particular, emerges as a very important substrate in S. alaskensis metabolism. In an oligotrophic environment where competition for nutrients is intense, our data support a simplified metabolism for S. alaskensis in which the fate of certain substrates is constrained, especially at the intersections of central carbon and nitrogen metabolism, in order to ensure optimal disposition of scarce resources. This is the first investigation of central metabolism for an oligotrophic ultramicrobacterium that possesses a relatively large genome size. In contrast to the behavior so far observed for SAR11 oligotrophic bacteria, S. alaskensis shows a physiological capacity to exploit increases in ambient nutrient availability and thereby achieve high-population densities. The ISME Journal (2009) 3, 1036–1052; doi:10.1038/ismej.2009.52; published online 21 May 2009 Subject Category: integrated genomics and post-genomics approaches in microbial ecology Keywords: Sphingopyxis alaskensis; marine; oligotroph; ultramicrobacterium; amino acids; metabolism Introduction cell volume (o0.1 mm3) as the defining criterion (Schut et al., 1997a; Cavicchioli and Ostrowski, The Earth’s oceans cover the majority of the surface 2003). This is particularly useful for studies of of the planet, and have the highest cellular produc- natural communities as a variety of cell shapes is tion rate of any ecosystem on the planet (Whitman often encountered, and volume provides a measure- et al., 1998). In the open ocean, the vast majority of ment of cell size that is independent of morphology this production is carried out by bacteria, which, (Schut et al., 1997a; Cavicchioli and Ostrowski, despite the bulk nutrient-depleted (oligotrophic) 2003). Ultramicrobacteria represent a major source nature of the open ocean, can achieve densities in 5 À1 of biomass and metabolic activity in oceanic the order of 0.5–5 Â 10 cells ml (Schut et al., ecosystems, and express higher metabolic activity 1997a; Whitman et al., 1998). The majority of these per unit of volume of seawater than larger bacterial bacteria are free-living (planktonic) forms that cells (Schut et al., 1997a). As such, in marine include the smallest of all living cells, with constant 3 oligotrophic environments, these small microbial cell volumes of not more than 0.1 mm . These cells play an essential role in regulating the bacteria have been termed ‘ultramicrobacteria’, with accumulation, remineralization and transformation of the earth’s largest pool of organic carbon. Correspondence: R Cavicchioli, School of Biotechnology and However, the physiology of ultramicrobacteria has Biomolecular Sciences, The University of New South Wales, remained largely uncharacterized, in a large part Sydney, NSW, 2052, Australia. because of their resistance to cultivation. E-mail: [email protected] Received 26 March 2009; accepted 7 April 2009; published online The successful isolation and axenic cultivation of 21 May 2009 the ultramicrobacterium Sphingopyxis alaskensis C and N metabolism in Sphingopyxis alaskensis TJ Williams et al 1037 strain RB2256 (formerly Sphingomonas alaskensis) and Kjelleberg, 1998; Cavicchioli et al., 2003). has provided opportunities for studying oligo- Earlier studies on the physiology of S. alaskensis trophic growth and metabolism (Schut et al., 1993, have shown a number of properties relevant to 1995, 1997a, b; Eguchi et al., 1996; Fegatella et al., its oligotrophic ecology, including the ability to 1998; Fegatella and Cavicchioli, 2000; Ostrowski simultaneously take up mixed substrates, irrespec- et al., 2001; Cavicchioli et al., 2003). S. alaskensis tive of concentration; a constitutive broad-specifi- cells are exceptionally small (cell volume city uptake system for amino acids; and inducible o0.1 mm3), and remain essentially constant in size glucose uptake, with this substrate immediately between starvation and growth conditions (Schut converted to storage product, even during glucose- et al., 1993, 1997a, b; Cavicchioli et al., 2003). The limiting growth (Schut et al., 1995, 1997a). It reduced cell size of ultramicrobacteria provides high has also been shown earlier that the slow growth surface-to-volume ratios, which facilitates growth rate of S. alaskensis (o0.2 hÀ1) (for example, under oligotrophic conditions (Button, 1991), resis- compared with a copiotroph), even under favorable tance to grazing by predatory zooplankton (Gonza´lez growth conditions (30 1C, millimolar nutrient et al., 1990), and the ability to partition biomass levels), is not the result of insufficient ribosome among a greater number of progeny from a given synthesis, despite possessing only a single rRNA substrate pool (Fegatella et al., 1998). S. alaskensis copy per genome (Fegatella et al., 1998). Such strain RB2256 was isolated from surface experiments emphasize the physiological versatility waters (10 m depth) of Resurrection Bay, Alaska, of an ultramicrobacterium that is not confined to where it was isolated by an extinction dilution oligotrophic nutrient levels in order to grow, but also method as a numerically abundant bacterium (4105 highlight gaps in our understanding of the critical cells mlÀ1) (Schut et al., 1993). S. alaskensis aspects of S. alaskensis metabolism that may strain AF01 was also an abundant bacterial constrain growth, even under nutrient-sufficient species sampled from another North Pacific site, in conditions. oligotrophic waters (350 m deep) off the coast Earlier kinetic and metabolic data for S. alaskensis of Japan (Eguchi et al., 2001), and similar isolates are consistent with a metabolism by which certain have been obtained from the North Sea (Schut amino acids (such as alanine) represent important et al., 1993). However, in contrast to ‘Candidatus natural growth substrates, but glucose does not Pelagibacter ubique’ from the SAR11 clade (Schut et al., 1995, 1997a). Although they are (Giovannoni et al., 2005), S. alaskensis does relatively poor sources of carbon and energy, amino not seem to have been abundant in the samples acids are ubiquitous in the open ocean, with taken for the Global Ocean Survey (which, however, alanine, glutamate, glycine and serine being major does not include samples from the North Pacific) components of the DFAA reservoir (Lee and Bada, (Thomas et al., 2007). Although it is presently 1975, 1977; Andersson et al., 1985; Ishida et al., unclear how widespread this species is in ocean 1986; Eguchi and Ishida, 1990). Around 90% of the waters, its isolation over a period spanning about a nitrogen requirements of bacteria in oligotrophic decade and abundance at the time of sampling in ocean waters are believed to be served by free North Pacific locations indicates that S. alaskensis ammonia and DFAAs (Keil and Kirchman, 1991). has the capacity to proliferate in oligotrophic marine However, key aspects of the S. alaskensis metabo- waters. lism remain unknown, including the processes by The ability to grow slowly on low concentrations which ammonia and amino acids are metabolized by (nanomolar) of substrates and maintain a relatively the cell. The aim of this study was to link the constant cell size in the shift between starvation analysis of the genome sequence of S. alaskensis and growth conditions is an oligotrophic trait RB2256 to proteomic, growth and biochemical (Eguchi et al., 1996; Schut et al., 1997a, b; analyses in order to elucidate the carbon and Fegatella and Cavicchioli, 2000; Cavicchioli et al., nitrogen metabolism of this marine bacterium. One 2003). On the basis of the Michaelis–Menten outcome of this approach was the identification of constants for substrate transport (Kt), and the characteristics that helped to clarify how S. alas- available concentrations of dissolved free amino kensis could compete in oceanic environments, and acids (DFAAs) in the ocean, S. alaskensis is how this bacterium compares with model oligo- predicted to be able to grow by using DFAAs at an trophs such as ‘Cand. P. ubique’ and specialist in situ doubling time of 12 h to 3 days (Schut et al., copiotrophs. This study is the first of this kind 1995), which compares favorably with measured for a sphingomonad, a group known

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