Supplementary document Trehalose/2

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Supplementary document
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Trehalose/2-sulfotrehalose biosynthesis and glycine-betaine uptake are widely
spread mechanisms for osmoadaptation in the Halobacteriales
Authors: Noha H. Youssef, Kristen N. Savage-Ashlock, Alexandra L. McCully, Brandon
Luedtke, Edward I. Shaw, Wouter D. Hoff, and Mostafa S. Elshahed
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Detailed Materials and Methods
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Archaeal strains. Haladaptatus paucihalophilus strain DX253T (DSM18195) was
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isolated from Zodletone spring, a sulfide- and sulfur-rich spring in southwestern
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Oklahoma (Savage et al 2007), and maintained in our laboratory. Natrialba magadii
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DSM3394, Natrinema pellirubrum DSM15624, Natronobacterium gregorii DSM3393,
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Natronococcus occultus DSM3396, Halalkalicoccus jeotgali DSM18796, and
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Haloterrigena turkmenica DSM5511 were kindly provided by Drs. Jonathan A. Eisen
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and Marc T. Facciotti (University of California Davis). All other strains were purchased
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from the German Collection of Microorganisms (DSMZ, Braunschweig, Germany). All
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cultures were maintained in DSMZ-recommended media (Table S1) on sealed agar plates
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or agar slants and stored at 4ºC.
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Genome of Haladaptatus paucihalophilus strain DX253T. DNA was extracted from
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100 mls of a late exponential phase culture using MoBio Powersoil DNA Extraction kit
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(MO BIO Laboratories, Carlsbad, California). The high-quality extracted DNA was
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sequenced using the service of a commercial sequencing provider (Engencore, now Selah
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Genomics, Columbia, South Carolina) using 454 FLX technology. The genome was
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assembled using Newbler assembler into 32 Contigs (N50 = 267, 250 bp, N90 = 100,497
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bp). Gene calling, annotation, and metabolic construction was conducted using the
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Department of Energy Integrated Microbial Genomes (IMG) platform (Markowitz et al
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2012).
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Growth media and Experimental setup. Haladaptatus paucihalophilus was grown in a
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defined media containing (g.l-1): MgCl2.6H2O (20), K2SO4 (5), CaCl2.2H2O (0.1), NH4Cl
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(0.5), KH2PO4 (0.05), and sodium pyruvate (0.5). The medium was buffered to a pH of
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6.8 using 25mM HEPES. After autoclaving, 1 ml of modified Wolin’s metal solution
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containing (g.l-1): EDTA, 0.5; MnSO4·H2O, 3; NaCl, 1; CaCl2·2H2O, 0.1; ZnSO4·7H2O,
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0.1; FeSO4·7H2O, 0.1; CuSO4·5H2O, 0.01; AlK(SO4)2, 0.01; Na2MoO4·2H2O, 0.01; boric
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acid, 0.01; Na2SeO4, 0.005;NiCl2·6H2O, 0.003, and 10 ml of vitamin solution (Widdel
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and Pfennig 1981) were added to 1 l of the above medium. This medium has a similar
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composition to DSMZ 1125, but with no yeast extract and with pyruvate rather than
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sucrose as a carbon source. This was done to ensure that any compatible solutes detected
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in cell extracts are synthesized de novo. NaCl concentrations were varied between 75-275
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g.l-1 in different experiments. All other strains were cultured in their DSMZ media at
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three different salt concentrations (Table S1) that are close to their lower, optimum, and
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higher NaCl growth range. In experiments assessing glycine betaine uptake in
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Haladaptatus paucihalophilus, glycine betaine (10 g.l-1, Sigma-Aldrich, St. Louis, MO)
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was added to the growth medium described above. For all other microorganisms, no
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glycine betaine was added since they were grown in complex media containing yeast
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extract, where glycine betaine is one of its components (estimated at 110 μg/g yeast
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extract (Dulaney et al 1968)). Approximately, 1.5x108 cells in the exponential phase were
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used as an inoculum for 250 ml cultures in all experiments. Cultures were grown to late
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exponential phase (O.D. ~0.5), harvested, and used for the quantification of various
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intracellular solutes as described below.
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Analytical methods.
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Identification of compatible solutes in cell-free ethanol extracts. The presence and
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identity of compatible solutes in cell-free extracts were initially screened using 1H-
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nuclear magnetic resonance spectroscopy (1H-NMR), and high performance liquid
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chromatography (HPLC). Cell pellets were extracted using a modified ethanol extraction
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method (Falicia Goh et al 2011). Cell pellets were washed three times in a sterile isotonic
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NaCl solution, followed by lyophilization. The lyophilized cell pellets were extracted
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with 70% ethanol, vortexed for 5 min, then centrifuged at 10,000 xg for 10 min. Ethanol
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extraction was repeated 2 more times and the combined ethanol extracts were evaporated
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overnight at 37ºC. For HPLC analysis, dried ethanol extracts were re-dissolved in water
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and 20 µl were analyzed on an Agilent 1100 Series (Santa Clara, CA) HPLC with a
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refractive index detector and an Aminex HPX-87P column. Analysis was conducted at
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85°C using a mobile phase of deionized water pumped at 0.6 mL/min for 30 min (Sluiter
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et al 2008). Trehalose was identified in the cell-free extracts by comparison to a trehalose
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standard (Sigma-Aldrich). For 1H-NMR analysis, dried ethanol extracts were dissolved in
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0.5 ml of D2O and 0.09 mM solution of 2,2-Dimethyl-2-Silapentane-5-Sulfonate-d6
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sodium salt (DSS) in D2O. Spectra were taken at 25oC with a one-pulse sequence with
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water pre-saturation on a Varian Inova 600 NMR spectrometer with a 5 mm indirect
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detection probe, using a 1.5 second pre-saturation delay between pulses and 6.6
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microsecond 90 degree pulse. The spectra were referenced to DSS at 0 ppm, with error in
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ppm values of +/- 0.05 ppm. Spectra were transformed with MNova software (Masterlab
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research, Santiago de Compostela, Spain), using solvent signal suppression to remove the
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residual water resonance. Reference trehalose was used for comparison.
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Quantification of ions and compatible solutes. Cell pellets were washed in sterile
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isotonic NaCl solution. After removal of all traces of medium, the pellet was frozen at -
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20ºC overnight followed by thawing in 10 ml solution of 10% perchloric acid (PCA).
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Thawed pellets were vortexed for 5 min, followed by incubation at room temperature for
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2 hours during which cells lysed and proteins precipitated. Extracts were then centrifuged
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at 10,000 xg for 15 min. The pellet containing the precipitated proteins was suspended in
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0.85% saline solution and used for protein quantification using total protein kit (Micro
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Lowry kit, Onishi and Barr Modification by Sigma Aldrich). The supernatant, containing
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the cell-free, protein-free, extract was used for quantification of intracellular solutes and
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ions as described below.
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Quantification of trehalose in cell-free extracts. The concentration of trehalose in cell-
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free PCA extracts was determined enzymatically (Neves et al 1994) using a trehalase
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assay kit (Megazyme®, Wicklow, Ireland). In addition to trehalose, this enzymatic assay
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is suitable for the quantification of 2-sulfotrehalose, a putative compatible solute
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previously identified in a few alkaliphilic Halobacteriales genera (Natrialba magadii,
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Natronobacterium gregorii, and Natronococcus occultus (Desmarais et al 1997)). This is
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due to the fact that trehalase enzyme requires only one free hydroxyl group at the 2′
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position for hydrolytic activity (Mori et al 2009, Ocon et al 2007), and hence the presence
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of a sulfonate group at one of the 2′ positions should not hinder its activity.
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Therefore, to differentiate trehalose from 2-sulfotrehalose, we devised a fast
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method to detect the presence of a 2′-O-sulfonate group based on the action of abalone
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snail sulfatase (Sigma-Aldrich), shown to be specific for cleaving the 2′-O-sulfonate
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group of trehalose (Uzawa et al 2004), followed by quantification of the released
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inorganic sulfate turbidimetrically (Lundquist et al 1980). PCA extracts positive for
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trehalose were assayed for the presence of free inorganic sulfate before and after
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treatment with abalone snail sulfatase (1 U per 1.5 µmole trehalose for 75 hours at 37ºC).
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Differences in inorganic sulfate content were converted to µmole sulfate and compared to
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the total amount of trehalose (µmoles) in the extracts. The sulfate:trehalose ratio obtained
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for Natronococcus occultus, previously shown to produce 2-sulfotrehalose (Desmarais et
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al 1997), was 0.44±0.26. This value is in accordance with the previously reported yield of
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abalone snail sulfatase of 28% on p-nitrophenyl-2-O-sulfo-glycoside (Uzawa et al 2004).
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Sulfate:trehalose ratios > 0.1 were deemed indicative of 2-sulfotrehalose production. By
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comparison, the sulfate:trehelose ratio for Haladaptatus paucihalophilus, shown by 1H-
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NMR to produce trehalose rather than 2-sulfotrehalose, never exceeded 0.01.
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Quantification of glycine betaine in cell-free extracts. Glycine betaine was quantified in
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PCA extracts using a colorimetric assay for quaternary ammonium compounds (QACs)
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as described before (Grieve and Grattan 1983). The assay is based on the precipitation of
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QACs as their periodide salts. Under acidic conditions (pH 0-1) and at low temperatures
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(0-4ºC), betaine precipitates, when reacted with a KI-I2 reagent, as glycine betaine-
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periodide complex, which has a characteristic absorbance at 365 nm when dissolved in
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1,2-dichloroethane. Concentrations of glycine betaine in PCA extracts were calculated
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using a glycine betaine standard curve (0-200 µg/ml).
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Quantification of intracellular potassium in cell-free extracts. Intracellular K+ levels
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were quantified in cell free extracts of various Halobacteriales species
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spectophotmetrically using an approach based on the formation of K+-K+-specific
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ionophore complex in the presence of a dye anion followed by the extraction of the K+-
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K+-specific ionophore complex using an organic solvent and measuring the increase in
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the absorbance of the organic layer (Takagi et al 1981). PCA extracts were mixed with
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the K+-specific ionophore, Kryptofix 221 (Sigma Aldrich) in the presence of the anionic
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dye picrate. The K+-Kryptofix 221 complex was then extracted by vortexing with
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toluene. The increase in the absorbance of the organic layer, proportional to the K+
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concentration in the PCA extracts, was measured at 360 nm against toluene.
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Quantification of intracellular free amino acids in cell-free extracts. PCA extracts were
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assayed for free amino acids using the services of the Protein Chemistry Lab of Texas
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A&M University. Free Amino acids are derivatized with o-phthalaldehyde (OPA) and 9-
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fluoromethyl-chloroformate (FMOC). OPA reacts with all amino acids except proline,
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while FMOC reacts with proline. The derivatized amino acids are separated by reverse
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phase HPLC on an Agilent 1260 liquid chromatograph using a 5 µm reverse phase
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column and a gradient elution using 100% solvent A (20mM Na acetate buffer with
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0.018% v/v triethylamine, 0.05mM EDTA, and 0.3% tetrahydrofuran, pH 7.2) at 0 min,
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going to 60% Solvent B (100 mM Na acetate buffer: acetonitrile: methanol (1:2:2 v/v))
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over 17 min with flow rate of 0.45 ml/min. Amino acids tagged with OPA are detected at
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338/390 nm by the Variable Wavelength (UV) detector (G1365D), while proline (tagged
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with FMOC) is detected at 266/324 nm.
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RNA extraction and gene expression. Total RNA was extracted from triplicate
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Haladaptatus paucihalophilus cultures grown in defined medium described above in
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presence of multiple salt concentrations (75, 125, 175, 225, and 275 g.l-1) using Tri
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Reagent (Ambion®, Austin, TX) (Morgan et al 2010). Cell pellets from late exponential
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phase cultures were solubilized in TRI Reagent® Solution (Ambion®), and processed
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according to the manufacturer’s instruction. Contaminating DNA was removed from all
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RNA preparations using RQ1 DNase (Promega®), followed by phenol/chloroform
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extraction, and ethanol precipitation. To check for the complete removal of DNA, the
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RNA preparation was used as a template in a PCR reaction conducted in a 50-μl volume
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mixture containing the following (final concentrations are given): 2 μl of extracted RNA,
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1× PCR buffer (Promega), 2.5 mM MgSO4, 0.2 mM dNTPs mixture, 2.5 U of GoTaq
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Flexi DNA polymerase (Promega), and 0.5 µM each of H. paucihalophilus-specific 16S
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rRNA gene primers F: 5′-GCTTTTGAGAGGAGGTGCAT-3′, and R: 5′-
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TAATGTACCCAGCCACCACA-3′, corresponding to bases 974-993, and 1078-1097,
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respectively of H. paucihalophilus 16S rRNA gene (GenBank accession number
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NR_043744). PCR amplification was carried out according to the following protocol:
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initial denaturation for 5 min at 95°C, followed by 30 cycles of denaturation at 95°C for
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45 s, annealing at 55°C for 45 s, and elongation at 72°C for 30 sec. A final elongation
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step at 72°C for 5 min was included. If needed, the DNase treatment was repeated until
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the RNA was free of any contaminating DNA as confirmed by PCR. DNA-free RNA was
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then precipitated using Lithium Chloride Precipitation Solution (Ambion, Carlsbad, CA)
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according to manufacturer’s instructions to remove any contaminating small RNAs.
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High-quality RNA preparations were stored at -80ºC until used. Total RNA reverse
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transcription (cDNA construction) was conducted on 1 µg of RNA preparations using
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Superscript III first strand synthesis kit (Invitrogen) with random hexamers (Invitrogen).
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To study the expression levels of genes involved in trehalose synthesis in
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Haladaptatus paucihalophilus, Reverse Transcription qPCR (RT-qPCR) was conducted
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on the cDNA obtained using primers shown in Table S2. Levels of expression of
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different genes were compared to Glyceraldehyde-3-Phosphate dehydrogenase gene
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expression. qPCR was conducted using a MyIQ thermocycler (Bio-Rad Laboratories,
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Hercules, CA) and Sybr GreenER qPCR mix (Invitrogen). The 20-µl reaction contained 2
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µl of cDNA, 0.5 µM each of the forward and reverse primers, and 10 µl of the qPCR mix.
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The reactions were heated at 50°C for 2 min, followed by heating at 95ºC for 8.5 min.
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This was followed by 65 cycles, with one cycle consisting of 15 sec at 95°C, 60 sec at
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52°C, and 30 sec at 72°C.
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Phylogenetic analysis. RpoB′ protein sequences from publicly available Halobacteriales
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genomes (n=82) were aligned in ClustalX (Larkin et al 2007 ) and used to construct a
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maximum likelihood tree in Mega (Tamura et al 2011) using a WAG model with Γ
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distribution of rates among sites as previously suggested (Minegishi et al 2010). Support
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values were obtained using 1000 bootstrapping events. To examine the evolutionary
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history of trehalose synthesis, Halobacteriales OtsA (trehalose-6-phosphate synthase),
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and OtsB (trehalose-6-phosphatase) protein sequences, as well as those from reference
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bacterial and archaeal taxa were aligned using ClustalX (Larkin et al 2007 ). The
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alignment was used to predict the best protein substitution model in Mega (Tamura et al
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2011) using maximum likelihood. The predicted model was applied in maximum
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likelihood tree construction and support values were obtained using 1000 bootstrapping
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events.
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Ecological distribution of otsAB-harboring genera. We examined the correlation
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between the presence/absence of trehalose synthesis otsAB genes in a genome and the
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respective salt minimum, maximum and optimum concentrations. We used χ2
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Contingency tables for correlation (Plackett 1983), since the dependent variable is
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nominal (dichotomous). The independent variable was converted to nominal values as
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follows. Values of salt minimum, maximum and optimum concentrations were ranked
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and grouped into 6 categories: (very low (ranks 1-14), low (ranks 15-27), moderate
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(ranks 28-40), moderate-high (ranks 41-53), high (ranks 54-66), and very high (ranks 67-
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81)). With the two variables (dependent and independent) being nominal, χ2 Contingency
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correlation was calculated, and the χ2 values obtained were compared to the tabulated χ2
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value at α = 0.05. The probability of the result being due to chance (i.e. p-value) was
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evaluated using the Chi-square calculator http://www.fourmilab.ch/rpkp/experiments
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/analysis/chiCalc.html. Only in cases where the correlation was significant (p<0.05), the
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obtained χ2 value was used to calculate Cramer's V statistics;
, where χ2 is the calculated χ2 value, n is the number of
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Halobacteriales species with sequenced genomes (n=81), M is the number of rows (or
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dependent variables, dichotomous), and N is the number of columns (or independent
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variables), to measure the degree of association between the two variables.
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To study the correlation between otsAB presence and the ecological distribution
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of various genera, we reexamined the relative abundance of various Halobacteriales
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genera in 13 different environments with salinities ranging from permanently hypersaline
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(n=9), saline and fluctuating salinity habitats (where salinity is usually lower than 250 g.l-
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diverse prokaryotic community) (n=3), and mostly non-saline with only occasional
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development of temporal and spatial pockets (n=1, Zodletone spring). Relative
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abundances of Halobacteriales genera with and without the OtsAB system in their
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genome were compared between various groups of environments using Student t test.
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Values were considered significantly different if the P-value associated with the t test
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was <0.0038 (equivalent to an α value of 0.05 corrected for 13 pairwise comparisons
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using the Bonferroni correction). The relative abundances values obtained were also used
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in a principal-component analysis to evaluate the differences in genera composition
, exhibits fluctuation, and the Halobacteriales community is usually a fraction of a more
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between the environments using the R statistical package (R Development Core Team
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2011).
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Results: Genes for Na+ extrusion, K+ uptake, and chloride homeostasis in
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Haladaptatus paucihalophilus genome.
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At least two Na+ extrusion mechanisms employing the proton electrochemical
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gradient as the driving force for exporting Na+ exist in the genome: A Na+:H+ antiporter
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of the NhaC family, and a multisubunit Na+:H+ antiporter similar to MnhABCDEFG. As
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for potassium uptake, 2 clusters similar to the ATP-dependent low affinity K+ transporter
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(Trk) exist in the genome, each consisting of the membrane component TrkH and the
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NAD-binding component TrkA. A voltage-gated K+ channel of the Kef-type, most
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probably functioning as a facilitated diffusion K+ uniporter driven by the membrane
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potential, was also identified in the genome. Two voltage-gated Cl- channels of the EriC-
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type exist in tandem in the genome upstream of a universal stress family protein. It is not
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clear whether these would be employed in Cl- uptake or extrusion. However, two Na+-
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dependent transporters of the neurotransmitter:Na+ symporter, NSS family, exist in the
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genome in tandem. Some of these are known to co-transport Cl-, and could potentially act
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as an energy-dependent inward chloride pump.
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Cui H-L, Gao X, Sun F-F, Dong Y, Xu X-W, Zhou Y-G et al (2010). Halogranum
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rubrum gen. nov., sp. nov., a halophilic archaeon isolated from a marine solar saltern. Int
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J Syst Evol Microbiol 60: 1366-1371.
References
251
252
Desmarais D, Jablonski PE, Fedarko NS, Roberts MF (1997). 2-Sulfotrehalose, a novel
253
osmolyte in haloalkaliphilic archaea. J Bacteriol 179: 3146-3153.
254
255
Dulaney EL, Dulaney DD, Rickes EL (1968). Factors in yeast extract which relieve
256
growth inhibition of bacteria in defined medium of high osmolarity. Dev Ind Microbiol 9:
257
260-269.
258
259
Falicia Goh, Young Jae Jeon, Kevin Barrow, Brett A. Neilan, Burns BP (2011).
260
Osmoadaptive strategies of the archaeon Halococcus hamelinensis Isolated from a
261
hypersaline stromatolite environment. Astrobiology 11: 529-536.
262
263
Grieve CM, Grattan SR (1983). Rapid assay for determination of water soluble
264
quaternary ammonium compounds. Plant Soil 70: 303-307.
265
266
Larkin MA, Blackshields G, Brown NP, Chenna R, McGettigan PA, McWilliam H et al
267
(2007 ). Clustal W and Clustal X version 2.0. Bioinformatics 23 2947–2948.
268
13
269
Lundquist P, Mårtensson J, Sörbo B, Ohman S (1980). Turbidimetry of inorganic sulfate,
270
ester sulfate, and total sulfur in urine. Clin Chem 26: 1178-1181.
271
272
Markowitz VM, Chen I-MA, Palaniappan K, Chu K, Szeto E, Grechkin Y et al (2012).
273
IMG: the integrated microbial genomes database and comparative analysis system.
274
Nucleic Acid Res 40: D115-D122.
275
276
Minegishi H, Kamekura M, Itoh T, Echigo A, Usami R, Hashimoto T (2010). Further
277
refinement of the phylogeny of the Halobacteriaceae based on the full-length RNA
278
polymerase subunit B' (rpoB') gene. Int J Syst Evol Microbiol 60: 2398-2408.
279
280
Morgan JK, Luedtke BE, Thompson HA, Shaw EI (2010). Coxiella burnetii type IVB
281
secretion system region I genes are expressed early during the infection of host cells.
282
FEMS Microbiol Lett 311: 61-69.
283
284
Mori H, Lee J-H, Okuyama M, Nishimoto M, Ohguchi M, Kim D et al (2009). Catalytic
285
reaction mechanism based on alpha-secondary deuterium isotope effects in hydrolysis of
286
trehalose by European Honeybee trehalase. Biosci Biotechnol Biochem 73: 2466-2473.
287
288
Neves MJ, Terenzi HF, Leone FA, Jorge JA (1994). Quantification of trehalose in
289
biological samples with a conidial trehalase from the thermophilic fungus Humicola
290
grisea var. thermoidea. World Journal of Microbiology & Biotechnology 10: 17-19.
291
14
292
Ocon, Aurora, Hampp, Rudiger, Requena, Natalia (2007). Trehalose turnover during
293
abiotic stress in arbuscular mycorrhizal fungi. New Phytol 174: 879-891.
294
295
Plackett RL (1983). Karl Pearson and the Chi-Squared Test. Int Statist Rev 51: 59-72.
296
297
R Development Core Team (2011). R: A Language and Environment for Statistical
298
Computing. Reference Index., 2.13.2 edn. R Foundation for Statistical Computing:
299
Vienna, Austria.
300
301
Savage KN, Krumholz LR, Oren A, Elshahed MS (2007). Haladaptatus paucihalophilus
302
gen. nov., sp. nov., a halophilic archaeon isolated from a low-salt, sulfide-rich spring. Int
303
J Syst Evol Microbiol 57: 19-24.
304
305
Sluiter A, Hames B, Ruiz R, Scarlata C, Sluiter J, Templeton D et al (2008).
306
Determination of structural carbohydrates and lignin in biomass. National Renewable
307
Energy Laboratory (NREL): Golden, CO.
308
309
Takagi M, Nakamura H, Sanui Y, Ueno K (1981). Spectrophotometric determination of
310
sodium by ion-pair extraction with crown ether complexes and monoanionic dyes. Analyt
311
Chim Acta 126: 185-190.
312
15
313
Tamura K, Peterson D, Peterson N, Stecher G, Nei M, Kumar S (2011). MEGA5:
314
Molecular Evolutionary Genetics Analysis Using Maximum Likelihood, Evolutionary
315
Distance, and Maximum Parsimony Methods. Mol Biol Evol 28: 2731-2739.
316
317
Uzawa H, Nishida Y, Sasaki K, Nagatsuka T, Hiramatsu H, Kobayashi K (2004).
318
Sulfatase-catalyzed assembly of regioselectively O-sulfonated p-nitrophenyl α-d-gluco-
319
and α-d-mannopyranosides. Carbohyd Res 339: 1597-1602.
320
321
Widdel F, Pfennig N (1981). Studies on dissimilatory sulfate-reducing bacteria that
322
decompose fatty acids. Arch Microbiol 129: 395-400.
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Table S1. Microorganisms used in this study and their growth media showing the carbon source, salt concentration used in culturing
experiments, carbon sources in growth media, and yeast extract content in these media.
Strain
Growth medium
Culture
Salt concentration g.l-1
Carbon source(s)
Yeast extract
collection
(g.l-1)
Low Opt
High
Haloferax mediterranei
DSM 372
125
175
225
YE, CAA, Na citrate, Na glutamate 5
Halovivax ruber
DSM 514
125
175
225
YE, Peptone
1
Halogeometricum borinquense
DSM 372
125
225
275
YE, CAA, Na citrate, Na glutamate 5
Halostagnicola larsenii
DSM 1138
175
225
275
YE
5
Halococcus saccharolyticus
DSM 372
125
225
275
YE, CAA, Na citrate, Na glutamate 5
Halorhabdus utahensis
DSM 927
125
225
275
YE, glucose
1
Halorubrum lacusprofundi
DSM 372
125
175
275
YE, CAA, Na citrate, Na glutamate 5
Halosarcina pallida
JCM 645
75
175
225
YE, CAA
0.1
Natrialba magadii
DSM 371
125
175
275
YE, CAA, Na glutamate
5
Natrinema pellirubrum
DSM 372
125
175
275
YE, CAA, Na citrate, Na glutamate 5
Natronobacterium gregoryi
DSM 371
125
175
275
YE, CAA, Na glutamate
5
Natronococcus occultus
DSM 371
125
175
275
YE, CAA, Na glutamate
5
Halalkalicoccus jeotgali
DSM 954
125
175
275
YE, CAA
5
Halogranum rubrum
MR2A
125
225
275
YE, CAA, Na citrate, Na glutamate, 0.5
Na pyruvate, glucose, peptone
Haloterrigena turkmenica
DSM 372
125
175
275
YE, CAA, Na citrate, Na glutamate 5
Natronorubrum tibetense
DSM 371
125
175
275
YE, CAA, Na glutamate
5
Halobacterium salinarum
DSM 372
175
225
275
YE, CAA, Na citrate, Na glutamate 5
Haladaptatus paucihalophilus
DSM 1125
75
125, 175 225, 275
Na pyruvate
0
Eschericia coli K12
10
YE, tryptone
5
YE: yeast extract; CAA: casamino acid
M2RA: modified R2A medium as described in (Cui et al 2010), LB contains (g.l-1): yeast extract, 5; tryptone, 10; NaCl, 10.
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Table S2. Primers used for RT-PCR.
Gene
Accession number qPCR primers
otsA1
EFW91797
F: 5’-GTGGGACGTGTTTCGAAGTT-3’
R: 5’-TAGCGAATCACTCCCGTTTC-3’
otsA2
EFW92049
F: 5’-AACTCACGGACGAGCAAGTT-3’
R: 5’-CCCGAGATGGTAATCCTGAA-3’
otsB
EFW92050
F: 5’-CAAGAACGAGTCGATGTGGA-3’
R: 5’-GAATCGAGAGTTGCGGAGAG-3’
treT
EFW90639
F: 5’-ACCGTCTGGATGGTGAACTC-3’
R: 5’-GTGCAGGAGGTTGTGAATCC-3’
GAPDH
EFW92006
F: 5’-TAACGGGTACGGGACTATCG-3’
R: 5’-ATAGCGGCGTAGAGTGGGTA-3’
328
329
330
331
332
333
334
335
336
337
338
339
340
341
342
343
344
345
346
347
348
349
350
351
352
353
354
355
18
356
357
Table S3. General genomic features as well as protein properties of Haladaptatus
paucihalophilus genome.
DNA, total number of bases
4,284,805
DNA coding number of bases
3,650,099 (85.2%)
DNA G+C number of bases
2,648,659 (61.8%)
DNA scaffolds
32
Genes total number
4,496
Protein coding genes
4,443
with function prediction
2,528
Average pI of all protein-coding genes
5.12
Percentage of acidic (D+E) residues
15.95
Percentage of basic (K+R) residues
8.79
Percentage of large hydrophobic residues (I+L+M+F)
18.98
RNA genes
53
rRNA genes
6
5S rRNA
2
16S rRNA
3
23S rRNA
1
tRNA genes
47
358
359
360
361
362
363
364
365
366
367
368
369
370
371
372
373
374
375
19
376Table S4. Comparison of average pI values of cytoplasmic versus membrane proteins in
377different halophilic archaeal and bacterial strains.
Microroganism
Average pI of proteins
Cytoplasmic
Membrane
Haladaptatus paucihalophilus
4.69
6.88
Haloarcula marismortui
4.1
6.89
Halobacterium salinarum
4.29
7.22
Halorubrum locusprofundii
4.23
6.56
Haloterigena turkmenica
4.42
5.53
Halopiger xanaduensis
4.44
5.36
Halostagnicola larsenii
4.44
5.44
Halovivax ruber
4.42
5.57
Halogeometricum borinquense
4.55
6.06
Halalkalicoccus jeotgali
4.57
6.19
Halomicrobium mukohataei
4.42
5.84
Haloferax sulfurifontis
4.49
6.11
Halorhabdus utahenesis
4.34
5.75
Haloquadratum walsbyi
4.56
6.04
Natrinema pellirubrum
4.51
5.63
Natronobacterium gregoryi
4.49
5.44
Natronococcus occultus
4.4
5.61
Natrialba magadii
4.44
5.38
Natronomonas pharonis
4.38
6.45
Salinibacter ruber
4.36
7.92
Halorhodospira halophila
5.12
8.56
20
378
Table S5. Intracellular levels of trehalose/2-sulfotrehalose, glycine betaine, and potassium in the strains tested.
Species
Salt conc
Osmolytes measuresa
(g.l-1)
Tre (µmol.mg STre (µmol SO4: GB (µmol.mg K+ (µmol.mg
protein-1)
µmol Tre)
protein-1)
protein-1)
Haloferax mediterranei
175
BDL
NA
8.02
16.26
Halovivax ruber
125
2.56
0
BDL
9.62
175
2.83
0
BDL
8.37
225
2.42
0
BDL
9.48
Halogeometricum borinquense
125
BDL
NA
BDL
7.67
225
BDL
NA
0.98
9.38
Halostagnicola larsenii
175
BDL
NA
BDL
4.19
225
BDL
NA
BDL
24.44
275
BDL
NA
BDL
29.7
Halococcus saccharolyticus
175
3.14
0
1.69
6.24
225
3.17
0
1.81
7.8
275
1.84
0
2.82
5.61
Halorhabdus utahensis
225
BDL
NA
0
9.07
275
BDL
NA
1.23
11.5
Halorubrum lacusprofundi
125
BDL
NA
0
6.5
175
BDL
NA
1.45
8.9
275
BDL
NA
2.74
22.9
Halosarcina pallida
75
3.07
0
0
3.92
225
3.02
0
1.73
5.6
Natrialba magadii
125
3.38
0.13
BDL
4.33
175
2.11
0.16
BDL
6.61
275
1.67
0.18
BDL
5.53
Natrinema pellirubrum
125
1.62
0.28
BDL
2.42
21
379
380
381
175
1.17
0.17
BDL
2.11
275
1.25
0.26
0.54
2.76
Natronobacterium gregoryi
125
5.88
0.28
BDL
4.36
175
2.43
0.27
BDL
6.62
275
1.66
0.13
BDL
5.12
Natronococcus occultus
125
3.31
0.74
0
4.69
175
1.70
0.31
2.85
3.75
275
1.22
0.27
3.63
3.83
Halalkalicoccus jeotgali
125
3.11
0.28
BDL
4.82
175
2.41
0.18
BDL
4.11
275
2.13
0.32
BDL
4.75
Halogranum rubrum
125
5.80
0
0.56
8.56
225
3.00
0
1.22
5.32
275
2.30
0
1.64
6.75
Haloterrigena turkmenica
125
2.32
0
0.23
3.17
175
2.19
0
1.47
4.67
275
1.28
0
2.05
3.86
Halobacterium salinarum
125
BDL
NA
1.58
6.1
175
BDL
NA
ND
8.88
225
BDL
NA
2.43
11.05
275
BDL
NA
2.65
12.5
Natronorubrum tibetense
125
3.62
0
BDL
5.24
175
2.09
0
0.82
4.54
275
1.49
0
0.9
4.37
A: osmolytes for which intracellular concentrations were measured in cell-free PCA extracts; trehalose (Tre), glycine betaine (GB),
and potassium are all shown in µmoles.mg protein-1. For 2-sulfotrehalose (STre), values shown are µmoles SO42-: µmoles trehalose.
BDL: below detection limit, NA: not applicable, BDL: Below detection limit, ND: not determined
22
382
383
23
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