Literature DB >> 28966889

Diversity of cultivated aerobic poly-hydrolytic bacteria in saline alkaline soils.

Dimitry Y Sorokin1,2, Tatiana V Kolganova3, Tatiana V Khijniak1, Brian E Jones4, Ilya V Kublanov1,5.   

Abstract

Alkaline saline soils, known also as "soda solonchaks", represent a natural soda habitat which differs from soda lake sediments by higher aeration and lower humidity. The microbiology of soda soils, in contrast to the more intensively studied soda lakes, remains poorly explored. In this work we investigate the diversity of culturable aerobic haloalkalitolerant bacteria with various hydrolytic activities from soda soils at different locations in Central Asia, Africa, and North America. In total, 179 pure cultures were obtained by using media with various polymers at pH 10 and 0.6 M total Na+. According to the 16S rRNA gene sequence analysis, most of the isolates belonged to Firmicutes and Actinobacteria. Most isolates possessed multiple hydrolytic activities, including endoglucanase, xylanase, amylase and protease. The pH profiling of selected representatives of actinobacteria and endospore-forming bacteria showed, that the former were facultative alkaliphiles, while the latter were mostly obligate alkaliphiles. The hydrolases of selected representatives from both groups were active at a broad pH range from six to 11. Overall, this work demonstrates the presence of a rich hydrolytic bacterial community in soda soils which might be explored further for production of haloalkalistable hydrolases.

Entities:  

Keywords:  Actinobacteria; Aerobic; Bacillus; Haloalkaliphilic; Hydrolytics; Soda solonchak soils

Year:  2017        PMID: 28966889      PMCID: PMC5619242          DOI: 10.7717/peerj.3796

Source DB:  PubMed          Journal:  PeerJ        ISSN: 2167-8359            Impact factor:   2.984


Introduction

Alkaliphilic aerobic hydrolytic bacteria have already attracted attention for a long time as sources of alkali-stable hydrolases for various industrial applications, primarily enzymatic laundry detergents (reviewed by: Horikoshi, 2004; Horikoshi, 2006; Fujinami & Fujisawa, 2010; Grant & Heaphy, 2010; Sarethy et al., 2011; Zhao, Yan & Chen, 2014; Mamo & Mattiasson, 2016). Most of this research has been conducted with non-halotolerant Bacillus species producing alkalistable proteases, amylases and endoglucanases. In contrast, only a few salt tolerant alkaliphilic hydrolytics have been isolated and characterized from saline alkaline (soda) lakes. So far, the majority of known soda lake hydrolytics belonged to fermentative anaerobic bacteria. A low salt-tolerant Clostridium alkalicellulosi is so far the only truly anaerobic cellulolytic bacterium able to grow on crystalline cellulose found in soda lakes (Zhilina et al., 2005). Pectin utilization for growth at haloalkaline conditions has been demonstrated in two fermentative anaerobic haloalkaliphiles: Natronoflexus pectinovorans (Bacteriodetes) and Natranaerovirga hydrolytica (Clostridia) at moderate and high salinity, respectively (Sorokin et al., 2011; Sorokin et al., 2012a). Two groups of fermentative haloalkaliphilic bacteria, narrowly specialized in the utilization of chitin as a growth substrate, have been found in hypersaline soda lakes. They formed two classes, Chitinivibrionia (high salt-tolerant) and Chitinispirilla (low salt-tolerant) within the phylum Fibrobacteres (Sorokin et al., 2012b; Sorokin et al., 2014; Sorokin et al., 2016). Proteinivorax tanatarense (Clostridiales), isolated from the soda lake decaying phototrophic biomass, represents a so far single example of anaerobic proteolytic haloalkaliphilic microorganism (Kevbrin et al., 2013). Very few examples of aerobic hydrolytic haloalkaliphiles have been characterized from soda lakes, with most of the work done on alkaline protease producers. The low to moderately salt-tolerant organisms are represented by a well-studied salt-tolerant gammaproteobacterium Alkalimonas amylolytica, producing amylase (Ma et al., 2004), Alkalibacillus sp. (Firmicutes), Nesterenkonia sp. (Actinobacteria) and Salinivibrio sp. (Gammaproteobacteria) producing haloalkalitolerant serine proteases (Abdel-Hamed et al., 2016; Gessesse et al., 2003; Lama et al., 2005), as well as several Gammaproteobacteria from the genus Marinimicrobium and a number of Actinobacteria strains, utilizing chitin (Sorokin et al., 2012b). Furthermore, a unique group of aerobic extremely halo(alkali)philic hydrolytic Euryarchaeota is also present in hypersaline soda lakes. The previous findings characterized highly haloalkalistable protease-producing Natronococcus occultus, Natrialba magadii, Natronolimnobius innermongolicus (Studdert et al., 2001; de Castro et al., 2008; Selim et al., 2014) and amylolytic Natronococcus amylolyticus (Kobayashi et al., 1992). Recently we also demonstrated a presence of four novel genus-level groups of natronoarchaea in soda lakes capable of growth on insoluble celluloses and chitin (Sorokin et al., 2015). However, another type of mainly aerobic soda habitats, saline alkaline soils, also called soda solonchaks, remain practically unexplored as a potential source of aerobic haloalkaliphilic hydrolytics. In contrast to the mostly anoxic soda lake sediments, soda soils are well aerated and remain desiccated most of the year. Such conditions should favour predominance of aerobic spore-forming Firmucutes and Actinobacteria, as has been shown in our recent exploration of bacterial nitrogen fixation in such habitats (Sorokin et al., 2008). Soda solonchaks are located in patches in dry steppe and semi-desert areas, such as south Siberia, north-eastern Mongolia, northern China, Egypt, India, Pakistan, Hungary and North American Steppes. In many cases they are hydromorphic and associated with high-standing saline, alkaline ground waters and often occur in the vicinities of saline alkaline (soda) lakes (Bazilevich, 1970; Kondorskaya, 1965). In this paper we describe a previously unexplored culturable diversity of aerobic haloalkalitolerant hydrolytic bacteria recovered from saline alkaline soils of several regions in Central Asia, Africa and North America.

Materials and Methods

Sample characteristics

Surface soil samples (0–5 cm depth) were collected into sterile plastic Petri dishes at five locations in Central Asia, Egypt and California. Each individual sample comprised a composite of 4 subsamples randomly collected in a 3–5 m2 area. Samples from Kenya and Tanzania were collected in sterile plastic bags (Whirl-Pak®; Nasco, Fort Atkinson, WI, USA) and vials using disposable sterile tongue depressors as described previously (Duckworth et al., 1996). The samples were kept at 4 °C before analysis. At most locations, the top soil layer was desiccated at the sampling time with a 20% maximum content of moisture. The selection of the samples was based on an immediate measurement of pH of a 1:5 water extract using a field pH-conductivity meter (model WTW 340i; WTW, Weilheim, Germany). Only those soils showing the pH of the water extract above 9.5 were selected for sampling. In total, more than 70 saline alkaline soil samples were obtained. Some of their characteristics are presented in Table 1. The content of total soluble salts was estimated in the laboratory by gravimetry after extraction of 2 g dry soil homogenized with 5 ml water followed by filtration through 0.2 µm filter and drying at 105 °C. Carbonate alkalinity in the soluble fraction was determined by acid titration monitored by a pH meter, using 5 g dry soil extracted with 20 ml water and after centrifugation at 10,000 × g for 10 min a 10 ml aliquot was titrated to pH 4.5 with 0.1 M HCl providing the value of total soluble carbonate alkalinity (NaHCO3Na2CO3).
Table 1

Characteristics of soda solonchak soils and lacustrine dry soda mud samples.

General informationpH of 1:5 water extractTotal soluble salts (g/kg)Soluble carbonate alkalinity (mM)
Sample codeNumber of samplesYear of samplingSample type
AA101988SS9.45–10.212–38820–1,870
KUS41998SS9.2–9.926–9623–40
BS21998SS9.71–10.7025–6010–502
KS142003SS9.60–10.2153–385150–1,520
MS241999SS9.70–10.8012–12810–1,140
EWN32000SS10.05–10.3085–102750–1,740
MLC42001SLM9.2–9.830–43130–240
KT161988; 1996; 1999SLM9.6–10.743–16045–890

Notes.

Ararate valley Armenia

Barabinskaya Steppe, Novosibirsk region, Russia

Kunkurskay steppe, Buriatia, Russia

Kulunda Steppe, Altai region, Russia

north-eastern Mongolia, Choibalsan province

Wadi al Natrun valley, Libyan Desert, Egypt

Mono Lake, California, USA

Kenya-Tanzania

continental soda solonchak soil

dry soda mad near soda lakes

Notes. Ararate valley Armenia Barabinskaya Steppe, Novosibirsk region, Russia Kunkurskay steppe, Buriatia, Russia Kulunda Steppe, Altai region, Russia north-eastern Mongolia, Choibalsan province Wadi al Natrun valley, Libyan Desert, Egypt Mono Lake, California, USA Kenya-Tanzania continental soda solonchak soil dry soda mad near soda lakes

Enrichment, isolation and cultivation of pure cultures of haloalkaliphilic aerobic hydrolytic bacteria

The general methods for the cultivation of aerobic alkaliphiles have been described elsewhere (Grant, 2006). The basic sodium carbonate mineral medium for cultivation of moderately salt-tolerant alkaliphiles contained 0.6 M total Na+ and 1 g l−1 K2HPO4 and was strongly buffered at pH 10. After sterilization, the medium was supplemented with 1 mM MgSO47H2O and trace metal solution (Pfennig & Lippert, 1966). The enrichments were performed in 20 ml medium contained in 100 ml bottles closed with rubber septa (to prevent evaporation during prolonged incubation) inoculated with 1 g soil. Incubation was performed on a rotary shaker at 100 rpm and 28 °C. After achieving growth and polymer degradation, the cultures were plated on solid media of the same composition. Five different polymers were used as substrates at concentration 1 g l−1: CMC, soluble starch, casein, powdered alpha-keratin and emulsified olive oil prepared according to Sorokin & Jones (2009). Testing of pure cultures also included 3 additional polymers: beech xylan, amorphous cellulose and chitin prepared as described by Sorokin et al. (2015). In the case of CMC, xylan and olive oil, the solid medium was supplemented with 0.2 g l−1 and in the case of chitin and starch—with 20 mg l−1 yeast extract. Growth of the xylanase-positive cultures on xylan was also tested in liquid culture containing 20 mg l−1 yeast extract. The pure cultures were isolated from individual colonies and checked for purity by repeated re-inoculation on to solid media. The culture purity and endospore formation was also checked by phase contrast microscopy (Zeiss Axioplan Imaging 2; Zeiss, Göttingen, Germany) and, finally, by nucleotide sequencing. The pH profiling of growth and hydrolytic activities was performed on solid media containing 0.6 M total Na+ in the form of either NaCl (for pH 5–8) or NaHCO3Na2CO3 (for the pH range 8–11). The media at pH range 5–8 were buffered with a mixture of potassium phosphates (50 mM) and HEPES (50 mM).

Detection of hydrolytic activities

All activities were detected using plate assays. Beta-1,4-endoglucanase and endoxylanase activities were visualized by using sequential flooding of the plates with 0.1% (w/v) Congo Red and 1 M NaCl each with 30 min incubation (Teather & Wood, 1982). The hydrolysis of keratin, emulsified olive oil, and amorphous chitin and cellulose was directly observed by formation of clarification halos around the colonies (Sorokin & Jones, 2009; Sorokin et al., 2015). The hydrolysis of starch was visualized after flooding the plates with 0.05 N J2 solution, containing 1% KJ. The hydrolysis of casein was visualized by flooding the plates with 10% (w/v) trichloroacetic acid. For several strains the pH profile and thermotolerance of endoglucanase activity were measured in culture supernatant by agar diffusion approach and measurements of reducing sugar release with DNS (Miller, 1959).

16S rRNA gene sequence and analysis

Genomic DNA was extracted from colony biomass using alkaline SDS cell lysis at 65 °C for 30 min followed by pH neutralization and DNA purification using the Wizard MaxiPreps Purification resin (Promega, Madison, WI, USA). For this, the following steps were taken: (1) cell material taken from solid medium was resuspended in 100 µl of buffer I; (2) 125 µl of lyzing buffer II was added and the resulted mixture was vortexed and (3) incubated at 65 °C for 30 min; (4) 125 µl neutralizing buffer III was added, the resulted mixture was vortexed, centrifugated at 10,000 g for 10 min; (5) 200 μl of the Wizard MaxiPreps resin (Promega) was added to the supernatant and next purification steps were made according to the Wizard DNA Extraction System manufacturer‘s instructions. The final DNA concentration was generally > 10 m kg ml−1, D260:D280 > 1.8, RNA contamination was less than 1%. Buffer I: 50 mM Tris–HCl, pH 8.0, 10 m M EDTA, 50 µg/ml pancreatic RNAse. Lyzing buffer II: 1% SDS in 0.2 M NaOH. Neutralizing buffer III: 2.5 M CH3COOK, pH 4.5. The 16S rRNA gene was amplified with bacterial forward primer 11f and the reverse universal primer 1495r. Sequencing was performed commercially using standard Sanger sequencing techniques. The obtained sequences were analyzed using SILVAngs web interface (Quast et al., 2013) on 07.03.2017. The Project summary and settings are shown in Table S1. The 16S rRNA gene sequences of 13 isolates, possibly representing novel taxa, together with the most identical sequences from the Ganbank, verified by BLASTn, were aligned in MAFFT 7 (Katoh et al., 2002). The Maximum Likelihood phylogenetic analysis with General Time Reversible model (G + I, 4 categories, Nei & Kumar, 2000) was performed in MEGA 6 (Tamura et al., 2013).

Results

Isolation and identification of pure cultures of aerobic hydrolytics from saline alkaline soils

A total of 179 strains with one of five polymer degrading activities have been isolated. From the general colony morphology and microscopy, the isolates were obviously dominated by two large groups—actinomycetes (formation of aerial or substrate mycelium) and endospore-forming bacilli. Furthermore, isolates obtained with proteins as substrate also included Gram-negative bacteria. The identification by 16S rRNA gene sequencing generally confirmed this conclusion. The two largest groups of isolates from the saline soda soils are typical hydrolytics belonging to the phyla Actinobacteria and Firmicutes (Fig. 1, Table 2) which may reflect a combination of the specific habitat (Table S2), sampling methods and culture conditions (Duckworth et al., 1996).
Figure 1

Distribution of 179 almost complete 16S rRNA gene sequences of hydrolytic haloalkaliphilic bacterial isolates, created by SILVAngs service.

Table 2

Strains of polyhydrolytic aerobic haloalkaliphilic bacteria, isolated from soda solonchak soils.

Candidate new species are highlighted in bold (<97% 16S rRNA gene sequence identity). “ +” and “ −” presence or absence of the feature.

Isolate codeSourceColony morphologyPhylogeny
Sample codeMyceliumPigment aerial/substrateEndo-sporesClosest relative% similarity
Actinobacteria
DS1KUS+Streptomyces sodiiphilus (haloalkaliphile)97
DS7BS+GrayStreptomyces sodiiphilus (haloalkaliphile)97
DS8BS+Streptomyces sodiiphilus (haloalkaliphile)97
DS9BS+GrayStreptomyces alkaliphilus (haloalkaliphile)99
DS16KT+Streptomyces alkalithermotolerans (haloalkaliphile)98
DS31EWN+GrayStreptomyces sp. E-070 (haloalkaliphile)99
DS32EWN+Streptomyces sp. E-070 (haloalkaliphile)99
DS34MLC+GrayStreptomyces sp. YIM 80244 (haloalkaliphile)97
DS35MLC+BeigeStreptomyces sp. E-070 (alkaliphile)99
DS36KS+GrayStreptomyces sodiiphilus YIM 80305 (haloalkaliphile)99
DS37KS+GrayStreptomyces alkaliphilus (haloalkaliphile)99
DS39KS+-/brownStreptomyces sp. E-070 (haloalkaliphile)99
DS42KS+BeigeStreptomyces alkalithermotolerans (haloalkaliphile)97
DS43KS+BeigeStreptomyces sodiiphilus99
DS46KS+GrayStreptomyces sp. E-070 (haloalkaliphile)99
DS55AA+Streptomyces sodiiphilus (haloalkaliphile)97
DS58KS+Streptomyces sodiiphilus YIM 80305 (haloalkaliphile)97
DS59KS+Streptomyces sodiiphilus YIM 80305 (haloalkaliphile)97
DS61KS+BeigeStreptomyces sunnurensis98
DS65AA+GrayStreptomyces alkaliphilus (haloalkaliphile)99
DS70AA+Streptomyces alkalithermophilus (alkaliphile)97
DS71AA+Gray/redStreptomyces alkaliphilus (haloalkaliphile)99
DS177KSGray/violStreptomyces alkaliphilus (haloalkaliphile)99
DS182KT+OliveStreptomyces alkaliphilus (haloalkaliphile)99
DS183KT+Streptomyces sp. E-070 (haloalkaliphile)97
DS2KUS+Nocardiopsis exhalans VTT E-06300199
DS3KUS+Nocardiopsis sp. YIM 80251 (haloalkaliphile)99
DS4KUS+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS10BS+Nocardiopsis exhalans VTT E-06300199
DS12KT+Nocardiopsis sp. YIM 80129 (haloalkaliphile)99
DS13KUS+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS14KT+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS15KT+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS17MS+BeigeNocardiopsis sp. E-143 (haloalkaliphile)99
DS18MS+BeigeNocardiopsis sp. E-143 (haloalkaliphile)99
DS19MS+GrayNocardiopsis sp. E-143 (haloalkaliphile)99
DS21MS+OliveNocardiopsis sp. E-143 (haloalkaliphile)99
DS22MS+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS23MS+BeigeNocardiopsis sp. YIM 80251 (haloalkaliphile)99
DS24MS+BeigeNocardiopsis sp. YIM 80251 (haloalkaliphile)99
DS25MS+BeigeNocardiopsis sp. E-143 (haloalkaliphile)99
DS26MS+BeigeNocardiopsis sp. YIM 80133 (haloalkaliphile)99
DS27MS+BeigeNocardiopsis sp. E-143 (haloalkaliphile)99
DS28MS+-/brownNocardiopsis sp. YIM 80133 (haloalkaliphile)99
DS29MS+Nocardiopsis sp. YIM 80133 (haloalkaliphile)99
DS30MS+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS38KS+Beige/redNocardiopsis sp. E-143 (haloalkaliphile)99
DS40KS+BeigeNocardiopsis sp. YIM 80129 (haloalkaliphile)99
DS41KS+BeigeNocardiopsis sp. AACh2 (haloalkaliphile)99
DS44KS+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS45KS+Nocardiopsis sp. YIM 80129 (haloalkaliphile)100
DS47AA+Nocardiopsis alba99
DS48AA+Nocardiopsis alba98
DS49AA+Nocardiopsis sinuspersici99
DS50AA+Nocardiopsis sp. YIM 80133 (haloalkaliphile)99
DS51AA+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS53AA+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS54AA+-/redNocardiopsis sp. E-143 (haloalkaliphile)99
DS56AA+Nocardiopsis alba99
DS57KS+BeigeNocardiopsis sp. YIM 80133 (haloalkaliphile)99
DS62KS+OliveNocardiopsis sp. E-143 (haloalkaliphile)99
DS63AA+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS64AA+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS66AA+Nocardiopsis sp. YIM 80130 (haloalkaliphile)99
DS67AA+Nocardiopsis sp. AACh2 (haloalkaliphile)99
DS68AA+Nocardiopsis sp. YIM 80130 (haloalkaliphile)99
DS69AA+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS73KUS+Nocardiopsis sp. AACh2 (haloalkaliphile)99
DS74KUS+Nocardiopsis sp. AACh2 (haloalkaliphile)99
DS75KUS+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS76KUS+Nocardiopsis sp. E-143 (haloalkaliphile)99
DS78KUS+Nocardiopsis sp. YIM 80130 (haloalkaliphile)99
DS79KUS+Nocardiopsis sp. AACh2 (haloalkaliphile)99
DS174KS-/redNocardiopsis sp. E-143 (haloalkaliphile)99
DS175KSNocardiopsis sp. E-143 (haloalkaliphile)99
DS176KSNocardiopsis sp. E-143 (haloalkaliphile)99
DS178KSNocardiopsis sp. YIM 80034 (haloalkaliphile)100
DS180KUS+ReddishNocardiopsis ganjiahuensis (haloalkaliphile)100
DS181KUS+Nocardiopsis sp. AACh2 (haloalkaliphile)99
DS20MS+Glycomycetaceae(halophiles)92
DS33EWN+PinkSalinispora arenicola NPS1168494
DS60KS+Isoptericola halotolerans99
DS82KTYellow+Isoptericola halotolerans99
DS88KSYellowIsoptericola halotolerans99
DS91KTYellowIsoptericola halotolerans99
DS92KTYellowIsoptericola halotolerans99
DS97MSYellowIsoptericola halotolerans99
DS99MSIsoptericola halotolerans99
DS111MSYellowIsoptericola halotolerans98
DS164KSYellowIsoptericola halotolerans99
DS149MSOrangeNesterenkonia xinjiangensis100
DS11KUSNitriliruptor alkaliphilus (haloalkaliphile)98
Bacilli
DS6BS++Bacillus horikoshii (alkaliphile)100
DS72KUS+Bacillus sp. E-141 (haloalkaliphile)99
DS81KT+Bacillus okhensis (haloalkalitolerant)99
DS83KT+Bacillus sp. ABCh1 (haloalkaliphile)98
DS84KTYellow+Bacillus cellulolyticus (alkaliphile)99
DS85KT+Bacillus cellulolyticus (alkaliphile)99
DS86KTCream+Bacillus pseudofirmus ( alkaliphile)100
DS87KT+Bacillus polygoni (haloalkaliphile)99
DS89KS+Bacillus daliensis (haloalkaliphile)99
DS90KT+Bacillus halodurans ( haloalkalitolerant)100
DS93KT+Bacillus cellulolyticus (alkaliphile)100
DS94KT+Bacillus vedderi (alkaliphile)98
DS95KT+Bacillus akibai (alkaliphile)98
DS96MSOrangeBacillus halodurans (haloalkaliphile)99
DS100MSOrange+Bacillus daliensis (haloalkaliphile)98
DS101MS+Bacillus akibai (alkaliphile)99
DS102MS+Bacillus alkalisediminis (haloalkaliphile)98
DS103MS+Bacillus akibai (alkaliphile)99
DS104MS+Bacillus alkalisediminis (haloalkaliphile)98
DS105MS+Bacillus akibai (alkaliphile)99
DS106MS+Bacillus alkalisediminis (haloalkaliphile)98
DS107MS+Bacillus akibai (alkaliphile)99
DS108MS+Bacillus alkalisediminis (haloalkaliphile)98
DS109MS+Bacillus alkalisediminis (haloalkaliphile)98
DS110MS+Bacillus akibai (alkaliphile)99
DS112MS+Bacillus pseudofirmus (alkaliphile)99
DS113KSOrangeBacillus daliensis (haloalkaliphile)99
DS114KT+Bacillus bogoriensis (haloalkaliphile)97
DS116KT+Bacillus sp. Z24-11 (haloalkaliphile)100
DS118KT+Bacillus polygoni (alkaliphile)99
DS119KT+Bacillus pseudofirmus (alkaliphile)100
DS120KT+Bacillus pseudofirmus (alkaliphile)99
DS121KT+Bacillus pseudofirmus (alkaliphile)99
DS122KTCream+Bacillus pseudofirmus (alkaliphile)98
DS126BS+Bacillus pseudofirmus (alkaliphile)99
DS127BSOrange+Bacillus pseudofirmus (alkaliphile)99
DS128BSOrange+Bacillus pseudofirmus (alkaliphile)99
DS129BS+Bacillus pseudofirmus (alkaliphile)99
DS131BSOrangeBacillus pseudofirmus (alkaliphile)100
DS132KTCream+Bacillus polygoni (haloalkaliphile)99
DS133KT+Bacillus halodurans (haloalkaliphile)100
DS134KTCream+Bacillus clarkii (alkaliphile)99
DS135KT+Bacillus polygoni (haloalkaliphile)99
DS136KTCream+Bacillus sp. Z24-11 (haloalkaliphile)99
DS137KT+Bacillus pseudofirmus (alkaliphile)99
DS138KT+Bacillus sp. Z24-11 (haloalkaliphile)99
DS139KT+Bacillus polygoni (haloalkaliphile)100
DS140KT+Bacillus alkalisediminis (haloalkaliphile)99
DS141KTYellow+Bacillus alkalinitrilicus (haloalkaliphile)99
DS142KT+Bacillus alkalinitrilicus (haloalkaliphile)99
DS143KT+Bacillus mannanilyticus (alkaliphile)96
DS144MS+Bacillus pseudofirmus (alkaliphile)99
DS148MS+Bacillus alkalinitrilicus (haloalkaliphile)99
DS150MSOrange+Bacillus daliensis (haloalkaliphile)98
DS151MS+Bacillus halodurans (haloalkaliphile)100
DS152MS+Bacillus horikoshii (alkaliphile)99
DS153MS+Bacillus pseudofirmus (alkaliphile)99
DS155MS+Bacillus pseudofirmus (alkaliphile)99
DS158MS+Bacillus pseudofirmus (alkaliphile)99
DS159MS+Bacillus akibai (alkaliphile)99
DS160KSYellow+Bacillus horikoshii (alkaliphile)99
DS161KS+Bacillus horikoshii (alkaliphile)99
DS163KS+Bacillus pseudofirmus (alkaliphile)100
DS165KS+Bacillus pseudofirmus (alkaliphile)99
DS166KS+Bacillus pseudofirmus (alkaliphile)99
DS168KS+Bacillus pseudofirmus (alkaliphile)99
DS169KS+Bacillus pseudofirmus (alkaliphile)99
DS172KS+Bacillus pseudofirmus (alkaliphile)99
DS184KT+Bacillus halodurans (haloalkaliphile)100
DS117KTOrangeAnaerobacillus alkalidiazotrophicus (haloalkaliphile)97
DS123KT+Anaerobacillus alkalidiazotrophicus (haloalkaliphile)97
Gammaproteobacteria
DS115KUSAlkalimonas amylolytica (haloalkaliphile)99
DS125BSAlkalimonas collagenimarina (haloalkaliphile)99
DS130BSAlkalimonas amylolytica (haloalkaliphile)99
DS154MSGreenishAlkalimonas amylolytica (haloalkaliphile)99
DS124BSAliidiomarina maris99
DS145MSAliidiomarina soli (haloalkaliphile)99
DS146MSAliidiomarina soli (haloalkaliphile)99
DS156MSAliidiomarina soli (haloalkaliphile)99
DS157MSAliidiomarina soli (haloalkaliphile)99
DS167KSAliidiomarina soli (haloalkaliphile)99
DS179KSAliidiomarina soli (haloalkaliphile)98
DS162KSYellowXanthomonadaceae ML-122 (haloalkaliphile) Rehaibacterium terrae9795
DS170KSXanthomonadaceae ML-122 (haloalkaliphile)99
DS171KSLysobacterspp.96
DS173KSYellowXanthomonadaceae ML-122 (haloalkaliphile)Lysobacterspp.99 95
DS147MSXanthomonadaceae ML-122 (haloalkaliphile) Lysobacterspp.99 95

Strains of polyhydrolytic aerobic haloalkaliphilic bacteria, isolated from soda solonchak soils.

Candidate new species are highlighted in bold (<97% 16S rRNA gene sequence identity). “ +” and “ −” presence or absence of the feature. The general phylogenetic distribution of the isolates is shown on a Krona diagram, obtained in the course of SILVAngs analysis (Fig. 1) and in the sample-dependent taxa clustering (Table S1). The Actinobacteria were mostly represented by two genera—Nocardiopsis and Streptomyces, and they were closely related to halotolerant alkaliphilic strains and species of these two genera found previously in haloalkaline habitats, in particular in Kenyan and Chinese soda lakes and saline alkaline soils (Grant & Jones, 2016). The relatively low diversity within the otherwise extremely diverse genera of these Actinobacteria indicates that haloalkaline conditions are rather selective for a few highly adapted species. Only two isolates from this group were distantly related to known species. One strain might represent a new genus in the Micromonosporacea with a closest relative from the genus Salinispora, while the second isolate is a distant member in the family Glycomycetaceae (Figs. S1A and S1B, respectively). Notes. CMCase-4 d, Xylanase, protease, amylase-3 d; lipase-10d; amorphous cellulose and chitin-30 d; ϕ col-colony diameter, mm; ϕ zone-hydrolysis zone diameter, mm. Highlights: on the basis of activity to colony diameter ratio: highly active-in bold. Mean values from two biological replicates. Positive on amorphous cellulose. Growth on amorphous cellulose. Growth on amorphous chitin. Same low genetic diversity was also observed in the second largest group represented by the genus Bacillus. Most of the isolates were closely related to the known alkaliphilic (B. pseudofirmus, B. horokoshii and B. akibai), or haloalkaliphilic (B. halodurans, B. daliensis, and B. alkalisediminis) species. The only exception was a single isolate only distantly related (95% sequence similarity) to B. mannanilyticus—a low salt-tolerant alkaliphilic species producing beta-mannanase (Akino, Nakamura & Horikoshi, 1987; Nogi, Takami & Horikoshi, 2005) (Fig. S1C). A relatively minor group of isolates enriched with proteins belonged to the proteobacterial class Gammaproteobacteria. A subgroup of three isolates was closely related (99% sequence similarity) to species of the genus Alkalimonas, a known amylolytic haloalkaliphile (Ma et al., 2004). Four isolates were closely related to a haloalkaliphilic member of the genus Aliidiomarina, A. soli, isolated from a soda soil in Inner Mongolia (Xu & Wu, 2017). The third gammaproteobacterial subgroup is represented by 4 proteolytic strains distantly related to organisms in the genus Lysobacter in the Xanthomonadaceae (95–96% sequence similarity). Three out of four strains of this subgroup clustered with an undescribed haloalkaliphilic isolate from Mono Lake (ML-122, 99% similarity), while the fourth strain was distant (96% similarity to ML-122). Therefore, this subgroup probably consists of two novel species and together with the Mono Lake strain ML-122 might represent a new genus in the family Xanthomonadacea (Fig. S1D). Finally, a significant group of actinobacteria with strong polyhydrolytic potential belonged to the Cellulomonas/Isoptericola clad within the family Promicromonosporaceae (Fig. S1E). The Cellulomonas species are known for their cellulolytic activity and include a haloalkaliphilic isolate from a Kenyan soda lake (Jones et al., 2005), while the genus Isoptericola mostly include halotolarant representatives, although the described neutrophic species apparently have only a limited hydrolytic activity (Schumann & Stackebrandt, 2014). Notes. Solid medium 0.6 M total Na+ buffered with: pH 5–8-0.1 M HEPES/NaCl/NaHCO3; pH 8–11-NaHCO3/Na2CO3. Substrate: 0.1% CMC + yeast extract 0.2 g/l. Growth and activity were estimated by the diameter of colony and zone of hydrolysis, respectively, after four days of plate incubation at 30 °C.

Hydrolytic spectra of the soda soil isolates

Most of the actinobacteria and bacilli isolates enriched with CMC or starch, were polyhydrolytic, being able to degrade all tested polymers, except for the insoluble native cellulose and chitin (Table 3). Only three actinobacterial isolates showed the ability to hydrolyse amorphous cellulose on the plate assay and only one of the three (DS33), a relative of Salinispora, was actually capable of growth with cellulose as substrate. Six isolates showed a potential to grow with amorphous chitin (Table 3). On the other hand, most of the endo-glucanase and endoxylanase positive actinobacteria and bacilli isolates utilized beech xylan as the growth substrate, which indicates that they are rather specialized in the mineralization of soluble hemicelluloses.
Table 3

Polymer hydrolysis and utilization by aerobic haloalkaliphiles from soda soils.

Strain codeEnriched with:CMCXylaneStarchCaseinOlive oil
ActivityGrowthActivityGrowth/activityGrowth/activityActivity
ϕ colϕ zoneϕ colϕ zoneϕ colϕ zoneϕ colϕ zoneϕ colϕ zone
Ds1CMC231943048
Ds11416520
Ds2720+6308227321012
Ds3824+422425630811
Ds4218+6278258301012
Ds180719632828930813
Ds1817236225241035913
Ds6112320425
Ds7214Weak218324522813
Ds8a214+215420320
Ds9412+5255205351013
Ds10617+52872410301517
Ds182c31632432853058
Ds183210312320528
Ds12618+52572410251214
Ds13719+5267256251214
Ds14517+5309255251214
Ds155205317257
Ds16a520+522415223813
Ds17621+6288246221012
Ds18514+52572252479
Ds1971637254281012
Ds2051443418
Ds21717+218932527
Ds224137-415425210
Ds23616+7266305201012
Ds24414+518630428810
Ds25412+7309275221012
Ds262132210325
Ds27515+72610264251011
Ds28414+621815525710
Ds2929349324
Ds306177269285201214
Ds318172255236221013
Ds3241732362222059
Ds33b520+228216220
Ds34312640530523610
Ds35418Weak420320622513
Ds36322+423430425712
Ds37310+31262562869
Ds38515+4257246281314
Ds3921236252121010
Ds40515+723727423911
Ds41616+723523527911
Ds42214223327710
Ds43c224214428332610
Ds44520+730827522912
Ds45315+530725420
Ds46210+220422320810
Ds47521+5237278281014
Ds48315+417420420810
Ds49213+4175231035810
Ds50315726514617810
Ds51315+5237308301013
Ds53318220
Ds54212+6249298301013
Ds5541512342242557
Ds56417+52392972679
Ds81210224524
Ds82321+42462853078
Ds83215Weak2165323
Ds84319Weak315424420
Ds85314Weak415525320
Ds861.5202428530
Ds87216Weak221417312
Ds88422420622320
Ds89312+2233252
Ds90415+3274253
Ds91c520++329524720815
Ds92c523+62873273036
Ds9331831541071537
Ds9421424931535
Ds9528+430423411
Ds96220++326524310
Ds97322514528415
Ds98523+62452531114
Ds9922131442028
Ds100224+2273291
Ds101322+322632112
Ds102523385182
Ds103328+422528110
Ds104218310419412
Ds105327+322534421
Ds106325411618420
Ds107327Weak318428420
Ds1083282518523
Ds109225411418522
Ds110227+320435725
Ds111c326+42032551777
Ds112325+421425720
Ds113213Weak2154232
Ds1845129346254251016
Ds57Casein520+4198265281214
Ds58+417422
Ds59417216
Ds6030Weak423524517
Ds6140310220
Ds6217214324320
Ds114+427528420
Ds115530420410
Ds116217416215
Ds117210520320
Ds118312218611
Ds119330418
Ds120210430224
Ds121+629330324
Ds1225222
Ds123+417415420
Ds124422
Ds125520524
Ds126525218
Ds127428212
Ds128532222
Ds129+313432320
Ds13034052348
Ds131Weak210333415
Ds132314312
Ds133420320725515
Ds134Weak219220
Ds135215315
Ds136420317
Ds137529315
Ds138428214
Ds139318314
Ds140Weak211433522
Ds141214
Ds142317515
Ds143322
Ds144530523
Ds145519
Ds146524
Ds147422
Ds1488320
Ds149328320w
Ds150+ +431525314
Ds151423Weak317725424
Ds152320323
Ds53323220
Ds15443062015
Ds155517312628315911
Ds156515
Ds157517
Ds15859529410
Ds159528+530530212
Ds16020530322
Ds161425228
Ds162315117
Ds163325225
Ds164322+318626425
Ds165328320
Ds166526315
Ds167527420
Ds168526320
Ds169530222
Ds170Keratin420
Ds171523
Ds172532220
Ds173318
Ds1743205259251214
Ds1753308301012
Ds176+8359259301012
Ds17717+22451942579
Ds1785223722830910
Ds179514+83482510301013
Ds63Starch210+5247267251012
Ds64513+62882410331116
Ds6521342752463069
Ds6621235205251015
Ds67+523528322612
Ds68310+6256255251215
Ds695153206286291115
Ds7021526
Ds7118+420525811
Ds725124301030814
Ds7328+5246201032813
Ds74Olive oil313+81873010321014
Ds75820+635103011301014
Ds76518+728725830
Ds7841026205121213
Ds79213+42162481569

Notes.

CMCase-4 d, Xylanase, protease, amylase-3 d; lipase-10d; amorphous cellulose and chitin-30 d; ϕ col-colony diameter, mm; ϕ zone-hydrolysis zone diameter, mm. Highlights: on the basis of activity to colony diameter ratio: highly active-in bold. Mean values from two biological replicates.

Positive on amorphous cellulose.

Growth on amorphous cellulose.

Growth on amorphous chitin.

The isolates enriched with proteins belonged to the Gammaproteobacteria and Firmicutes. All of them, as expected, showed highest hydrolytic potential against casein, and many of them did not have endoglucanase, endoxylanase or lipase activities (Table 3). So, they can be considered as dedicated proteolytics. Indeed, proteolytics are the most well-studied group of alkaliphilic hydrolytics. For the pH profiling, four strains from actinomycetes and from bacilli were selected for test on solid medium containing 0.6 M total Na+ with CMC + yeast extract as substrate. The solid medium is not optimal for the profiling but it was chosen for two reasons: (1) the mycelium-forming actinomycetes do not grow homogenously in liquid media and their growth is often estimated by radial colony increase; (2) test on solid medium permitted simultaneous estimation of both growth and endoglucanase activity. The results (Table 4) demonstrated that the tested actinomycetes are facultative moderate alkaliphiles, while the bacilli isolates are obligate alkaliphiles. The endoglucanase activity of both groups had a very broad pH range from six to 11 with an optimum for actinomycetes from eight to 10 and for the bacilli from nine to 10.5.
Table 4

Influence of pH on growth and endoglucanase activity of soda solonchak alkaliphiles: average profiles estimated from individual results for eight isolates: actinomycetes-Nocardiopsis DS50, 51; Streptomyces DS8,9; Bacillus: DS85, 100, 101, 102.

pH% of maximum
ActinomycetesBacillus ACB
GrowthActivityGrowthActivity
500
620–7030–700
740–10070–1000–100–40
880–10090–10020–6040–100
990–10090–10070–10090–100
1080–10090–10010090–100
10.540–9070–10080–100100
1110–4040–8030–7050–90

Notes.

Solid medium 0.6 M total Na+ buffered with: pH 5–8-0.1 M HEPES/NaCl/NaHCO3; pH 8–11-NaHCO3/Na2CO3. Substrate: 0.1% CMC + yeast extract 0.2 g/l. Growth and activity were estimated by the diameter of colony and zone of hydrolysis, respectively, after four days of plate incubation at 30 °C.

Overall, the results of this study demonstrated that saline alkaline soils represent a potentially valuable resource of aerobic haloalkaliphilic bacteria capable of producing multiple alkalistable hydrolytic enzymes. Most of the haloalkaliphilic polyhydrolytic isolates belong to Actinobacteria (genera Streptomyces and Nocardiopsis) and the genus Bacillus. We consider the actual capability of a large proportion of the soda soil aerobic haloalkaliphilic isolates to utilize xylan and starch as growth substrates as one of the principal findings of this extended screening. Such organisms definitely represent an interesting object for further investigation of their haloalkalistable hydrolases, particularly with a potential for application in laundry detergent production.

Supplemental Tables S1–S2, Supplemental Figure S1

Table S1. SILVAngs Project Summary and Project Settings. Table S2. Site-specific taxonomic distribution of isolates different locations. Figure S1. Unrooted 16S rRNA gene sequence Maximum likelihood phylogenetic trees of the haloalkaliphilic isolates, possibly representing novel taxa, and its nearest relatives. All positions with less than 95 % site coverage were eliminated. There were a total of 1,338 (A), 1,394 (B), 1,442 (C), 1,373 (D) and 1,103 (E) positions in the final datasets. The tree is drawn to scale, with branch lengths measured in the number of substitutions per site with corrections, associated with the model. Bootstrap values as percentages of 1,000 repetitions are shown next to the branches. Type strains of validly published species are underlined. Genbank numbers are indicated at the beginning of each sequence designation. Click here for additional data file.
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