<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">AiM</journal-id><journal-title-group><journal-title>Advances in Microbiology</journal-title></journal-title-group><issn pub-type="epub">2165-3402</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/aim.2016.66041</article-id><article-id pub-id-type="publisher-id">AiM-66455</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Biomedical&amp;Life Sciences</subject></subj-group></article-categories><title-group><article-title>
 
 
  Cultivable Nitrogen Fixing Bacteria from Extremely Alkaline-Saline Soils
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>endi</surname><given-names>E. Navarro-Noya</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Marco</surname><given-names>Luna-Guido</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Luc</surname><given-names>Dendooven</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref></contrib></contrib-group><aff id="aff1"><addr-line>CONACYT-Tlaxcala Autonomous University, Tlaxcala, Mexico</addr-line></aff><aff id="aff2"><addr-line>Laboratory of Soil Ecology, ABACUS-Cinvestav, Mexico City, Mexico</addr-line></aff><pub-date pub-type="epub"><day>11</day><month>05</month><year>2016</year></pub-date><volume>06</volume><issue>06</issue><fpage>412</fpage><lpage>423</lpage><history><date date-type="received"><day>10</day>	<month>March</month>	<year>2016</year></date><date date-type="rev-recd"><day>accepted</day>	<month>8</month>	<year>May</year>	</date><date date-type="accepted"><day>13</day>	<month>May</month>	<year>2016</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  Three soils with different Electrolytic Conductivity (EC) from the former Lake Texcoco (soil with low EC 1.2 dS
  &#183;
  m<sup>-1</sup>, medium with EC 83.1 - 107.8 dS
  &#183;
  m<sup>-1</sup>, and high with EC 137.3 - 152.5 dS
  &amp;bull;m<sup>-1</sup>) were used to isolate nitrogen-fixing bacterial strains through enrichment cultures in nitrogen-free media. The medium and high EC in the soil affected negatively the nitrogen-fixing activity, which was generally ten times lower compared to the activity in the soil with low EC. Twenty-one bacterial strains were isolated, identified and characterized for their nitrogen fixation capacity. The diazotrophic genetic potential of all isolates was confirmed by amplification and sequencing of partial nifH and nifD genes and diazotrophic activity quantified by the acetylene reduction assay. Azospirillum brasilense, and several species of Paenibacillus (P. fujiensis, P. durus, P. borealis, P. graminis, P. massiliensis and P. wynnii) were identified. Isolates belonging to the Paenibacillus genus were found in the three soils. Paenibacillus fujiensis and P. durus showed a high nitrogenase activity. The phylograms based on nifH and nifD gene sequences were consistent with 16S rRNA gene phylogeny.
 
</p></abstract><kwd-group><kwd>Diazotrophs</kwd><kwd> Extremophyles</kwd><kwd> Haloalkaline</kwd><kwd> Halotolerant</kwd><kwd> &lt;i&gt;Paenibacillus&lt;/i&gt;</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Globally, saline soils or solonchaks cover between 260 million and 340 million ha [<xref ref-type="bibr" rid="scirp.66455-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref2">2</xref>] . Antropogenic activities, such as irrigation and excessive use of fertilizer, have increased salt contents in important agriculture production areas affecting soil processes and limiting crop production. Excessive amounts of salts often result in poor soil structure and affect chemical and biological processes [<xref ref-type="bibr" rid="scirp.66455-ref3">3</xref>] - [<xref ref-type="bibr" rid="scirp.66455-ref6">6</xref>] . Saline soils are of particular interest as they allow investigating the effect of high salt contents on microbial activity in a natural environment [<xref ref-type="bibr" rid="scirp.66455-ref6">6</xref>] - [<xref ref-type="bibr" rid="scirp.66455-ref9">9</xref>] .</p><p>Biological nitrogen fixation controls soil fertility as it represents the most important input of nitrogen into an ecosystem. Activity of nitrogen fixating bacteria, however, is often inhibited by large concentrations of salts [<xref ref-type="bibr" rid="scirp.66455-ref10">10</xref>] - [<xref ref-type="bibr" rid="scirp.66455-ref13">13</xref>] . Nevertheless, Sorokin et al. [<xref ref-type="bibr" rid="scirp.66455-ref12">12</xref>] demonstrated that diazotrophs might still be active in soda soils with moderate salinity and alkalinity. Isolation of pure cultures of haloalkaliphilic diazotrophs from several locations in Central Asia and Egypt through micro-oxic enrichments of soils yielded the aerotolerant fermentative haloalkaliphilic bacterium Amphibacillus tropicus and the obligately anaerobic haloalkaliphile Bacillus arseniciselenatis. Apparently, nitrogen fixing activity in alkaline saline soils can be attributed to free-living fermentative low- GC gram-positive bacteria [<xref ref-type="bibr" rid="scirp.66455-ref10">10</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref13">13</xref>] - [<xref ref-type="bibr" rid="scirp.66455-ref15">15</xref>] .</p><p>Most studies on nitrogen ﬁxation activity in soils with high salinity have focused on Rhizobium-legume symbioses. Nodule formation on legumes is more sensitive to salt or osmotic stress than the rhizobia. Salt stress inhibits the initial steps of Rhizobium-legume symbioses or affects legume root-hair morphology [<xref ref-type="bibr" rid="scirp.66455-ref11">11</xref>] . Another group of diazotrophs well described in salt stressed environments are the haloalkaliphile cyanobacteria found to be responsible for nitrogen fixation in soda lakes and soils [<xref ref-type="bibr" rid="scirp.66455-ref16">16</xref>] - [<xref ref-type="bibr" rid="scirp.66455-ref18">18</xref>] . Only a few obligate anaerobes isolated from soda lakes, such as Clostridium alkalicellum [<xref ref-type="bibr" rid="scirp.66455-ref19">19</xref>] and Geoalkalibacter ferrihydritucus [<xref ref-type="bibr" rid="scirp.66455-ref20">20</xref>] , have been described as diazotrophs.</p><p>The soil of the former Lake Texcoco located in the valley of Mexico City (Mexico) can be classified as soda solonchaks. Its pH ranges from 8.3 to 10.2, electrolytic conductivities (EC) in saturation extracts from 1.2 to 200 dS・m<sup>−1</sup>, exchangeable sodium percentages from 75% to 98% and sodium adsorption ratio from 103 to 1718 mM [<xref ref-type="bibr" rid="scirp.66455-ref21">21</xref>] . High evaporation rate and low precipitation (700 mm・y<sup>−1</sup>) increase the concentration of salts. Dynamics of C and N have been investigated intensively [<xref ref-type="bibr" rid="scirp.66455-ref22">22</xref>] , and although the bacterial and archaeal communities have been studied [<xref ref-type="bibr" rid="scirp.66455-ref21">21</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref23">23</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref24">24</xref>] , no potential diazotrophs have been identified. It can be speculated, however, that nitrogen fixation represents an important input of nitrogen into the environment so diazotrophs should be present. The aim of this work was to determine the nitrogen fixing activity in soils with different electrolytic conductivity, and to identify the cultivable diazotrophic community and to evaluate their potential of nitrogen fixing capacity.</p></sec><sec id="s2"><title>2. Materials and Methods</title><sec id="s2_1"><title>2.1. Sampling and Sample Description</title><p>Three soils from the former Lake Texcoco (19˚30'N, 98˚59'W) with different electrolytic conductivity (EC) were sampled in triplicate. As such, nine soil samples were obtained. Soil was sampled by augering the 0 - 10 cm layer of a 1 m<sup>2</sup>-delimited area 20 times while the 0 - 2 cm layer was discarded. Soil samples were transported to the laboratory in black polyethylene bags on ice, 5 mm sieved separately and stored at −20˚C pending analysis.</p><p>Soil physicochemical characteristics were determined as described previously [<xref ref-type="bibr" rid="scirp.66455-ref25">25</xref>] . The EC was measured in a saturated solution extract and pH was measured in 1:2.5 soil-H<sub>2</sub>O suspensions using a glass electrode (<xref ref-type="table" rid="table1">Table 1</xref>). The first soil had a low EC of 1.2 dS・m<sup>−1</sup> (considered the Tex-Low soil), the second soil had an EC ranging from 83.1 to 107.8 dS・m<sup>−1</sup> (considered the Tex-Med soil), while the third sample had EC ranging from 137.3 to 152.5 dS・m<sup>−1</sup> (considered the Tex-High soil). According to the FAO soil classification, a very strong saline soil has an electrolytic conductivity (EC) &gt; 16 dS・m<sup>−1</sup> [<xref ref-type="bibr" rid="scirp.66455-ref26">26</xref>] .</p></sec><sec id="s2_2"><title>2.2. Culture Enrichments and Isolation of Free Living Nitrogen-Fixing Bacterial Cultures</title><p>Diazotrophic enrichment cultures were obtained by adding subsamples of 0.5 g soil to 125 ml serum-flasks containing 100 ml N-free semisolid medium [<xref ref-type="bibr" rid="scirp.66455-ref27">27</xref>] . The medium contained (g・l<sup>−1</sup>): 0.1, MgSO<sub>4</sub>・7H<sub>2</sub>O; 0.5, sodium thioglycolate; 0.008, ferric citrate; 0.008, Na<sub>2</sub>MoO<sub>4</sub>・2H<sub>2</sub>O, and agar 0.1% (w/v). The medium was autoclaved at 121˚C for 15 min. After sterilization, the medium was supplemented with 55 mM filter-sterilized glucose and phosphate buffer (36 mM K<sub>2</sub>HPO<sub>4</sub> and 16 mM NaH<sub>2</sub>PO<sub>4</sub>). Serum flasks were stoppered with cotton plugs and incubated statically at 22˚C for several days. When turbidity appeared, the flasks were closed with sterile rubber stoppers, acetylene added and nitrogenase activity measured after one day. Positive cultures were stabilized by repeated transfers (1% inoculum) with an interval of two weeks.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Nitrogen fixation activity in soils of the former Lake Texcoco with different electrolytic conductivity</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Soil</th><th align="center" valign="middle"  rowspan="2"  >EC<sup>a</sup> (dS・m<sup>−1</sup>)</th><th align="center" valign="middle"  colspan="3"  >Acetylene reduction assay (nmol C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・g<sup>−1</sup> soil)</th></tr></thead><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" >Tex-Low</td><td align="center" valign="middle" >1.2</td><td align="center" valign="middle" >172 (69)<sup>b</sup></td><td align="center" valign="middle" >296 (55)</td><td align="center" valign="middle" >255 (57)</td></tr><tr><td align="center" valign="middle" >Tex-Med</td><td align="center" valign="middle" >83 - 108</td><td align="center" valign="middle" >47 (33)</td><td align="center" valign="middle" >16 (6)</td><td align="center" valign="middle" >16 (6)</td></tr><tr><td align="center" valign="middle" >Tex-High</td><td align="center" valign="middle" >137 - 153</td><td align="center" valign="middle" >30 (12)</td><td align="center" valign="middle" >8 (4)</td><td align="center" valign="middle" >30 (10)</td></tr></tbody></table></table-wrap><p><sup>a</sup>EC: Electrolytic conductivity. <sup>b</sup>Values between parenthesis are standard deviations of the mean.</p><p>Nitrogen fixing bacteria were isolated in solid N-free culture medium. Serial decimal dilutions of enrichment cultures in sterile water were done and 10<sup>−5</sup> to 10<sup>−9</sup> dilutions were spread onto N-free Bridges agar and incubated in an atmosphere enriched with GasPack<sup>&#174;</sup> system at 28˚C for five days. Five representative colonies of each morphotype obtained were used to confirm nitrogenase activity by the acetylene reduction assay. The positives were conserved in 25% v/v glycerol at −70˚C.</p></sec><sec id="s2_3"><title>2.3. Differentiation of Pure Cultures and 16S rRNA Gene Sequence Analysis</title><p>Random amplification polymorphic DNA (RAPD) fingerprints were obtained to distinguish morphologically similar strains. Briefly, genomic DNA from the isolates was obtained from 48 h bacterial cultures with a QIAamp DNA minikit (Qiagen Inc., Valencia, CA) on the QIAcube&#174; apparatus (Qiagen). Extracted bacterial DNA was eluted from the columns with 200 &#181;l elution buffer and stored at −20˚C.</p><p>The RAPD fingerprints were generated using the primer OPB01 (5’-GTT TCG CTC C-3’) and the reaction conditions were used as previously reported [<xref ref-type="bibr" rid="scirp.66455-ref28">28</xref>] . The RAPD products were electrophoresed in 1.5% agarose gels in 1 &#180; TAE (40 mM Tris, pH 8.3; 20 mM acetic acid; 1 mM EDTA) and stained with SYBR&#174; Gold (Invitrogen Corporation, Carlsbad, CA).</p><p>At least two isolates of each group were selected for identification by a similitude and phylogenetic analysis of the 16S rRNA gene partial sequence. The amplification of 16S rRNA genes was done using the universal bacterial primer 8 forward and 1492 reverse [<xref ref-type="bibr" rid="scirp.66455-ref29">29</xref>] . The PCR products were purified using the QIAquick PCR purification kit according to manufacturer’s instructions (Qiagen Inc., Valencia, CA). Sequencing was done by Macrogen Inc. (DNA Sequencing Service, Seoul, Korea).</p></sec><sec id="s2_4"><title>2.4. Molecular Analyses of nifH and nifD Genes</title><p>The nifH and nifD genes fragments were amplified from chromosomal DNA samples using primers designed for this work. These primers were chosen from conserved regions detected in multiple sequence (nucleotidic and aminoacidic) alignments of a broad collection of nifH and nifD genes and design degenerate primer pairs. The designed primers correspond to N19-N38 (5’-TAY GGI AAR GGI GGI ATH GG-3’) and N378-N398 (5’-GGI GAY GTI GTI TGY GGI GGI-3’) of nifH Methanocaldococcus jannaschii MJ-4000-136 (DQ516852), and N181-N200 (5’-CGC GGC TGC GCC TAY GCM GG-3’) and N1309-N1328 (5’-CCK TTC CGY CAG ATG CAY TC-3’) of nifD Klebsiella pneumoniae (X13303). The PCR reactions were done with an initial denaturation step at 94˚C for 10 min, 35 cycles at 94˚C for 60s, at 55˚C for 60 s, and at 72˚C for 60 s and a final extension at 72˚C for 10 min. Reactions contained 20 ng template DNA, 1&#180; reaction buffer, 50 mM MgCl<sub>2</sub>, 0.25 mM of each dNTP, 10 pM of each primer and 1 U Taq polymerase, adjusted to 25 ml. Purified PCR products were sequenced by Macrogen Inc.</p></sec><sec id="s2_5"><title>2.5. Phylogenetic Analysis</title><p>Taxonomic assignations were done with the RDP classifier 2.2 at an 80% confidence threshold [<xref ref-type="bibr" rid="scirp.66455-ref30">30</xref>] and based on the Greengenes reference database (version 1210). A collection of taxonomically related sequences obtained from the national center for biotechnology information (NCBI) taxonomy homepage (http://www.ncbi.nlm.nih.gov/Taxonomy/taxonomyhome.html/) and Ribosomal Database Project-II Release 10 (http://rdp.cme.msu.edu) were used for a multiple alignment analyses with CLUSTAL X [<xref ref-type="bibr" rid="scirp.66455-ref31">31</xref>] . Only common 16S rRNA gene regions were included in the phylogenetic analyses. Maximum likelihood analyses were done using MEGA version 5 [<xref ref-type="bibr" rid="scirp.66455-ref32">32</xref>] . “Find best model” tool were used to evaluate the substitution models. For each model, AICc value (Akaike Information Criterion, corrected), Maximum Likelihood value (lnL), and the number of parameters (including branch lengths) were calculated [<xref ref-type="bibr" rid="scirp.66455-ref33">33</xref>] . The confidence at each node was assessed by 500 bootstrap replicates [<xref ref-type="bibr" rid="scirp.66455-ref34">34</xref>] . The similitude percentages were obtained by subtracting p-distance from one.</p></sec><sec id="s2_6"><title>2.6. Acetylene Reduction Assay</title><p>The nitrogen-fixation (NF) activity of the enrichment-cultures and pure cultures was examined by means of the acetylene reduction activity assay (ARA) as reported by Navarro-Noya et al. [<xref ref-type="bibr" rid="scirp.66455-ref28">28</xref>] . Briefly, strains were grown in 10 ml vials containing 5 ml N-free semisolid medium to determine their nitrogenase activity. A single colony of each bacterial strain was incubated at 30˚C for 72 h. The vials were sealed with rubber stoppers and acetylene was injected to a final concentration of 5% (v/v) by replacing an identical volume of air. The test tubes were incubated at 30˚C for 12 or 24 h. The produced ethylene was measured with an Agilent 4890-D GC-17 gas chromatograph (USA). The gas chromatograph was fitted with a 0.2 ml sample loop on the injector port, a 50/80 Porapak N column (182.88 cm by 3.175 mm) and a flame ionization detector. The temperature of the injector was 40˚C, the detector 250˚C and the oven 55˚C. Concentrations of ethylene were calculated every time samples were analysed by comparing peak areas against a standard curve prepared from a standard concentration of 250 ppm ethylene. Reference strain Klebsiella variicola ATCC BAA-830T was included as positive and Escherichia coli DH10b as negative control.</p><p>Total cell protein concentration in the semisolid medium used to determine ARA was measured by the coomassie brilliant blue assay [<xref ref-type="bibr" rid="scirp.66455-ref35">35</xref>] . Bovine serum albumin (sigma no. A5503, Grade V, 99% purity) was used as standard. Prior to the protein determination, the sample was incubated with 10% (w/v) trichloroacetic acid at 90˚C for 20 min, then cooled to room temperature and centrifuged at 8000&#180; g for 15 min [<xref ref-type="bibr" rid="scirp.66455-ref36">36</xref>] . The insoluble protein was disolved in 0.1 M NaOH at 55˚C for 1 h. Semisolid medium without inoculum were processed as control.</p></sec><sec id="s2_7"><title>2.7. Determination of Tolerance to NaCl</title><p>Tolerance to NaCl was determined by broth microdilution according to the CLSI document M27-A2 (2002). NaCl concentrations were varied from 0% to 25% with 1% increments. Briefly, an inoculum suspension was adjusted to a 0.5 McFarland standard and diluted first 1:50 and then 1:20 in R2A medium. Medium R2A contained (g・l<sup>−1</sup>): 0.5, yeast extract; 0.5, proteose peptone (Difco no. 3); 0.5, casamino acids; 0.5 g, glucose; 0.5, soluble starch; 0.3, sodium pyruvate; 0.3, K<sub>2</sub>HPO<sub>4</sub>; 0.05, MgSO<sub>4</sub>・7H<sub>2</sub>O; pH 7.2 [<xref ref-type="bibr" rid="scirp.66455-ref37">37</xref>] . The minimum inhibitory concentration (MIC) microplates were incubated at 28˚C until growth in the medium without NaCl.</p></sec><sec id="s2_8"><title>2.8. Sequence Accession Numbers</title><p>The sequence data reported in this paper have been deposited in the GenBank database, under accession numbers from JQ436863-JQ436919.</p></sec></sec><sec id="s3"><title>3. Results</title><sec id="s3_1"><title>3.1. Measurements of Nitrogen Fixation Activity in Enrichment Cultures</title><p>Nitrogen fixation rate in the Tex-Low soil varied from 172 to 296 nmol C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・g<sup>−1 </sup>soil, while in the Tex-High soil from 7.4 to 30.4 nmol C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・g<sup>−1</sup> soil (<xref ref-type="table" rid="table1">Table 1</xref>). Stabilized cultures were obtained after six transfers in N-free medium. Nitrogenase activity in the stabilized cultures of the Tex-Low was 14.2 C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・culture<sup>−1</sup>, in Tex-Med 4.3 C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・culture<sup>−1</sup> and in Tex-High 4.8 nmol C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・culture<sup>−1</sup> (data not shown). Gram-positive spore-forming bacilli dominated in all the enrichment cultures.</p></sec><sec id="s3_2"><title>3.2. Isolation and Identification of Diazotrophic Strains</title><p>A total of 39 strains with positive AR activity were isolated from the enrichment cultures. However, after RAPD screening 21 different RAPD-profiles were found (Data not shown). Seven different profiles were found in the Tex-Low soil, 10 in the Tex-Med soil and four in the Tex-High soil.</p><p>Strains Tex01-S1, Tex01-S2, Tex01-S3, Tex01-S5, Tex22-S1, Tex02-S4, Tex03-P3, Med01-S2 and Hgh02- P1 were isolated in consortium with negative NF isolates. Consortiums were more frequent in soil with low EC.</p><p>Approximately 1430 nucleotides of 16S rRNA gene sequence of each isolate were used for identification based on pair alignments with sequences from databases and relationships in a phylogenetic tree. A majority of the isolates belonged to the genus Paenibacillus (P. durus, P. graminis, P. wynnii, P. massiliensis, P. borealis and P. fujiensis), with similarity percentages of 99.1 - 100 (<xref ref-type="table" rid="table2">Table 2</xref>). Only three of the isolates were identified as Azospirillum brasilense (Tex03-P3, Tex02-S3 and Tex02-S3c) and were detected in the Tex-Low sample soil. Paenibacillus durus and P. fujiensis were isolated from the Tex-Low soil, P. durus and P. graminis from Tex- Med and P. borealis, P. massiliensis and P. wynii from Tex-High soil.</p><p>Consortium members with negative NF activity were also analyzed for identification. Thus, Agrobacterium tumefaciens, Celullomonas hominis, Bacillus circulans, Achromobacter xylosoxidans and Pantoea agglomerans were found (<xref ref-type="table" rid="table2">Table 2</xref>).</p></sec><sec id="s3_3"><title>3.3. Characterization of the Nitrogen-Fixing Isolates</title><p>Nitrogen fixation capacity of the isolates was investigated by PCR-amplification of nifH and nifD genes and quantified by ARA (<xref ref-type="table" rid="table3">Table 3</xref>). Except for the Hgh03-P4 isolate, nif genes were detected in all strains. In general, higher NF activities were found in isolates from the Tex-Low soil. Strains with a high activity (2811 - 4358 nmol C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・mg・protein<sup>−1</sup>) were Tex01-S5 and Tex02-S5 identified as P. fujiensis (first two) and Md01-S1 as P. durus. Strains Tex01-S4, Tex02-P4 and Tex02-S4 showed an NF activity of approximately 1500 nmol C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・mg・protein<sup>−1</sup>.</p><p>The isolates grew in medium containing 2% - 10% NaCl. Isolates with a tolerance to 10% NaCl were Hgh02- S1, Hgh02-S1 and Tex01-S5. There was no relationship between source of isolation (soil with low, medium or</p><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Phylogenetic afﬁliation of nitrogen-fixing isolates from soils of the former Lake Texcoco</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Soil</th><th align="center" valign="middle" >Bacterial strain (GenBank accession number)</th><th align="center" valign="middle" >Best match<sup>a</sup> (GenBank accession number)</th><th align="center" valign="middle" >Similarity<sup>b</sup> (%)</th></tr></thead><tr><td align="center" valign="middle" >Tex-Low</td><td align="center" valign="middle" >Tex01-S4 (JQ436894); Tex02-S4 (JQ436895)</td><td align="center" valign="middle" >Paenibacillus durus (NR_037017)</td><td align="center" valign="middle" >100</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex01-S5 (JQ436893); Tex02-S5 (JQ436897); Tex02-P4 (JQ436896)</td><td align="center" valign="middle" >Paenibacillus fujiensis (AB092351)</td><td align="center" valign="middle" >100</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex03-P3 (JQ436891); Tex02-S3 (JQ436890); Tex02-S3c (JQ436892)</td><td align="center" valign="middle" >Azospirillum brasilense (EF634031)</td><td align="center" valign="middle" >99 - 99.2</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex03-P3c (JQ436912); Tex01-S2c (JQ436913); Tex01-S3c (JQ436914)</td><td align="center" valign="middle" >Bacillus circulans (JN644554)</td><td align="center" valign="middle" >99.1</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex01-S5c (JQ436888); Tex01-S3b (JQ436889)</td><td align="center" valign="middle" >Agrobacterium tumefaciens (AJ389909)</td><td align="center" valign="middle" >98.7</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex02-S1c (JQ436918)</td><td align="center" valign="middle" >Pantoea agglomerans (AM184264)</td><td align="center" valign="middle" >100</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex01-S2a (JQ436919)</td><td align="center" valign="middle" >Achromobacter xylosoxidans (FJ796451)</td><td align="center" valign="middle" >100</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex01-S1c (JQ436916)</td><td align="center" valign="middle" >Celullomonas hominis (AB480700)</td><td align="center" valign="middle" >99 - 100</td></tr><tr><td align="center" valign="middle" >Tex-Med</td><td align="center" valign="middle" >Md01-S1 (JQ436900); Md01-S4 (JQ436898); Md01-S5 (JQ436899)</td><td align="center" valign="middle" >Paenibacillus durus (NR_037017)</td><td align="center" valign="middle" >99.5 - 99.8</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Md02-S1 (JQ436905); Md02-S3 (JQ436901); Md03-S1 (JQ436902); Md03-S2 (JQ436907); Md03-S3 (JQ436904); Md03-S5 (JQ436903); Md03-S6 (JQ436906)</td><td align="center" valign="middle" >Paenbacillus graminis (AM745263)</td><td align="center" valign="middle" >99.6</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Med01-S2c (JQ436915)</td><td align="center" valign="middle" >Bacillus circulans (JN644554)</td><td align="center" valign="middle" >99.9</td></tr><tr><td align="center" valign="middle" >Tex-High</td><td align="center" valign="middle" >Hgh02-S4 (JQ436909); Hgh02-P4 (JQ436908)</td><td align="center" valign="middle" >Paenibacillus borealis (AB073364)</td><td align="center" valign="middle" >99.1 - 99.6</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Hgh02-S1 (JQ436911); Hgh02-S2 (JQ436910)</td><td align="center" valign="middle" >Paenibacillus massiliensis (AY912109)</td><td align="center" valign="middle" >100</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Hgh02-P1c (JQ436917)</td><td align="center" valign="middle" >Celullomonas hominis (AB480700)</td><td align="center" valign="middle" >97.5 - 99.8</td></tr></tbody></table></table-wrap><p><sup>a</sup>The best match was selected using the closest sequence from the phylogenetic tree. <sup>b</sup>Similarity percentage was estimated by considering the number of nucleotide-substitutions between a pair of sequences divided by the total number of compared bases &#215;100.</p><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Acetylene reduction activity and NaCl tolerance in nitrogen-fixing isolates from soil of the former Lake Texcoco</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Soil</th><th align="center" valign="middle" >Bacterial strain</th><th align="center" valign="middle" >Acetylene reduction activity (nmol C<sub>2</sub>H<sub>4</sub>/h/mg protein)</th><th align="center" valign="middle" >NaCl tolerance<sup>a</sup> (%)</th></tr></thead><tr><td align="center" valign="middle" >Tex-Low</td><td align="center" valign="middle" >Tex01-S4</td><td align="center" valign="middle" >1960 &#177; 56</td><td align="center" valign="middle" >2</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex01-S5</td><td align="center" valign="middle" >4358 &#177; 143</td><td align="center" valign="middle" >10</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex02-S2</td><td align="center" valign="middle" >429 &#177; 78</td><td align="center" valign="middle" >2</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex02-S3</td><td align="center" valign="middle" >484 &#177; 46</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex02-S3c</td><td align="center" valign="middle" >97 &#177; 4</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex02-S4</td><td align="center" valign="middle" >1722 &#177; 76</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex02-S5</td><td align="center" valign="middle" >2811 &#177; 190</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex02-P4</td><td align="center" valign="middle" >1835 &#177; 24</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tex03-P3</td><td align="center" valign="middle" >124 &#177; 7</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" >Tex-Med</td><td align="center" valign="middle" >Md01-S1</td><td align="center" valign="middle" >2982 &#177; 699</td><td align="center" valign="middle" >7</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Md01-S5</td><td align="center" valign="middle" >574 &#177; 44</td><td align="center" valign="middle" >4</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Md02-S1</td><td align="center" valign="middle" >435 &#177; 36</td><td align="center" valign="middle" >2</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Md02-S3</td><td align="center" valign="middle" >399 &#177; 29</td><td align="center" valign="middle" >2</td></tr><tr><td align="center" valign="middle" >Tex-High</td><td align="center" valign="middle" >Hgh02-P4</td><td align="center" valign="middle" >638 &#177; 75</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Hgh02-S1</td><td align="center" valign="middle" >234 &#177; 53</td><td align="center" valign="middle" >10</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Hgh02-S2</td><td align="center" valign="middle" >324 &#177; 78</td><td align="center" valign="middle" >10</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Hgh02-S4</td><td align="center" valign="middle" >175 &#177; 12</td><td align="center" valign="middle" >4</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >Hgh03-P2</td><td align="center" valign="middle" >184 &#177; 56</td><td align="center" valign="middle" >3</td></tr></tbody></table></table-wrap><p><sup>a</sup>NaCl tolerance was determined in R2A medium amended with NaCl.</p><p>high EC) and NaCl tolerance.</p></sec><sec id="s3_4"><title>3.4. Phylogenetic Analyses</title><p>Maximum-likelihood phylogenetic trees of 16S rRNA, nifH, and nifD genes were constructed to determine relationships between the sequences of the isolates and related organisms from the GenBank database. Phylogenetic trees obtained with 16S rRNA sequences of the diazotrophic isolates and negative NF co-isolates showed that nitrogen-fixing species of the genus Paenibacillus were grouped in three different clusters (<xref ref-type="fig" rid="fig1">Figure 1</xref>). Cluster A grouped Tex-Low and Tex-Med isolates, cluster B grouped Tex-Med and Tex-High isolates and cluster C grouped Tex-High isolates. The 16S rRNA phylogram also included sequences belonging to the Proteobacteria and the Actinobacteria phyla, which corresponded to ribosomal sequences of the negative NF co-isolates.</p><p>Topology of the Maximum-Likelihood nifH tree displays a similar tendency with isolate sequences grouped in three phylogenetic clusters (<xref ref-type="fig" rid="fig2">Figure 2</xref>). Cluster A was formed by 7 nifH gene sequences of isolates from the Tex-Med soil and was related to P. graminis nifH gene (84% of identity). Cluster B grouped 3 nifH gene sequences of isolates from the Tex-High soil and were related to P. wynnii nifH (Hgh02-S4 and Hgh02-P4) and P. massiliensis nifH (Hgh02-S2). Cluster C comprised five isolate sequences from the Tex-Low soil and two from the Tex-Med soil. These nifH sequences were related to a compressed group formed by P. forsythia, P. sabinae, P. durus, P. zanthoxyli and P. fujiensis.</p></sec></sec><sec id="s4"><title>4. Discussion</title><p>Nitrogen fixation is a key process that is, in part, directly correlated with the primary production of many environments [<xref ref-type="bibr" rid="scirp.66455-ref38">38</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref39">39</xref>] . Together with other processes of the N cycle (e.g. ammonification, nitrification and denitrification), nitrogen fixation is affected by environmental factors, such as temperature, pH, oxygen, heavy metals and mineral nutrients [<xref ref-type="bibr" rid="scirp.66455-ref40">40</xref>] - [<xref ref-type="bibr" rid="scirp.66455-ref42">42</xref>] . Our study documents nitrogen-fixing cultivable bacteria obtained by enrichment</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> Maximum-likelihood phylogenetic tree showing the position of the 16S rRNA gene fragments amplified from the nitrogen-fixing isolates and consortium coisolates from soils of the former Lake Texcoco. The scale bars indicate the nucleotide substitutions per site. Numbers at the branches indicate the bootstrap values of 500 resamplings. Only values above 50% are shown. Actinobacteria phylum served as outgroup</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-2270736x7.png"/></fig><p>cultures in nitrogen-free media occurring in soils with a different degree of salinity.</p><p>N<sub>2</sub> fixation rates were obtained (296 nmol C<sub>2</sub>H<sub>4</sub> h<sup>−1</sup>・g<sup>−1</sup> dry soil or 48.5 mg・N・day<sup>−1</sup>・g<sup>−1</sup> soil), similar to those found in other terrestrial environments, such as in soda solonchak soils and the rhizosphere of some plants [<xref ref-type="bibr" rid="scirp.66455-ref12">12</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref14">14</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref40">40</xref>] . In this work, the high EC, however, affected negatively the nitrogen fixation activity, as it was ten-times lower in Tex-High compared to the Tex-Low soil (<xref ref-type="table" rid="table1">Table 1</xref>). Different effects of salinity on N<sub>2</sub> fixing have been reported. Some studies have found that concentrations of NaCl as low as 75 mM had a negative effect on nitrogenase activity in symbiotic nitrogen fixers [<xref ref-type="bibr" rid="scirp.66455-ref41">41</xref>] . In mangroves, nitrogen fixation was also reduced when pH and salinity increased [<xref ref-type="bibr" rid="scirp.66455-ref43">43</xref>] . However, others have reported no negative effects of high salinity on nitrogen</p><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Maximum-likelihood phylogenetic tree showing the position of the nifH gene fragments amplified from the nitrogen-fixing isolates from soils of the former Lake Texcoco. The scale bars indicate the nucleotide substitutions per site. Numbers at the branches indicate the bootstrap values of 500 resamplings. Only values above 50% are shown. nifH of Cyanob- acteria group served as outgroup</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-2270736x8.png"/></fig><p>fixation activity [<xref ref-type="bibr" rid="scirp.66455-ref44">44</xref>] .</p><p>pH is also an important factor that affects nitrogen fixation [<xref ref-type="bibr" rid="scirp.66455-ref12">12</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref43">43</xref>] reported that in soda solonchak soils maximum nitrogen fixation activity was obtained at pH 9.8, but at pH 7.3 and 10.5 it decreased 80%. Microorganisms involved in key processes of important biochemical cycles are probably well adapted to extreme conditions. It is possible that the decrease in nitrogen fixation activity in Tex-Med and Tex-High was a synergistic effect of a high salinity and pH.</p><p>Isolation of nitrogen-fixing bacteria through enrichment in nitrogen-free media allowed us to identify different species of the Paenibacillus genus and Azospirillum brasilense. Paenibacillus spp. are ubiquitous, and frequently isolated from the rhizosphere of maize, wheat, sugarcane, and pioneer plants growing on mine tailings [<xref ref-type="bibr" rid="scirp.66455-ref28">28</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref45">45</xref>] - [<xref ref-type="bibr" rid="scirp.66455-ref47">47</xref>] . Nitrogen fixing species are also characterized by their capacity to produce phytohormones, solubilize phosphorous and control the access of phytopathogens in plants [<xref ref-type="bibr" rid="scirp.66455-ref45">45</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref46">46</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref48">48</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref49">49</xref>] . In other salt stressed environments, some genera phylogenetically related with Paenibacillus have been isolated, e.g. Amphibacillus tropicus, Bacillus arseniciselenatis in solonchak soils and Bacillus spp. in coastal arable saline soils [<xref ref-type="bibr" rid="scirp.66455-ref12">12</xref>] [<xref ref-type="bibr" rid="scirp.66455-ref15">15</xref>] . In mangrove ecosystem other N<sub>2</sub> fixing bacteria have been isolated, e.g. Azospirillum, Azotobacter, Rhizobium, Clostridium, Klebsiella, Vibrio, and Phyllobacterium [<xref ref-type="bibr" rid="scirp.66455-ref50">50</xref>] . This is probably due to the specific physicochemical characteristics of this environment. nifH genes related with P. durus were also detected in solochak soils [<xref ref-type="bibr" rid="scirp.66455-ref12">12</xref>] . Particularly, A. brasilense was found only in the soil with low EC indicating its sensitivity to high salt concentrations. Nitrogen fixation activity of isolates Tex01-S4, Tex01-S5, Tex02-P4, Tex02-S4, and Med01-S1 identified as P. durus and P. fujiensis was high and similar to that of other free-living diazotrophs [<xref ref-type="bibr" rid="scirp.66455-ref51">51</xref>] .</p><p>Bacillus circulans was co-isolated in consortium with several strains. However, to our knowledge, no reports exist of this species as being a diazotroph or any of the other coisolates Achromobacter, Cellulomonas and Patoea. In this study, no nitrogen fixation activity of these bacteria was observed under the conditions tested.</p><p>Halotolerant strains of Bacillus and Paenibacillus were previously isolated from salt mining soils of Russia. However, their nitrogen fixation ability was not tested [<xref ref-type="bibr" rid="scirp.66455-ref52">52</xref>] . Most strains isolated in this work were not able to grow in high or moderate concentrations of NaCl. Isolates Tex01-S5 and Hgh02-S1 identified as P. fujiensis and P. massiliensis, however, tolerated up to 10% NaCl.</p><p>Phylogeny of the 16S rRNA and nifH genes showed a clear effect of EC on the distribution of the Paenibacillus spp. Apparently there is a gradient along soils with low, moderate and high EC. Thus, A. brasilense, P. fujiensis, P. durus, P. graminis, P. wynnii, P. borealis, and P. massiliensis were isolated in that order in the soils from low to high EC. However, their NaCl tolerance profile did not match this observation. It is possible that other characteristics than salinity affected the bacterial community, especially in the nitrogen fixing guild.</p><p>Phylogeny of the 16S rRNA gene showed a clear relationship between sequences from the databases and sequences of the isolates, with percentages of similitude ranging from 99% to 100%. nifH and nifD phylogenies agreed with the ribosomal relationships. Nevertheless, similarity and identity were in the range of 84% - 95% and 86% - 99%, respectively. Ribosomal phylogram showed a close relationship between the cluster formed by P. fujiensis and P. durus sequences from the database and sequences of the isolates (<xref ref-type="fig" rid="fig1">Figure 1</xref>). However, nifH and nifD phylograms showed a close-fitting group formed by P. zanthoxyli, P. forsythia, P. durus and P. fujiensis, and relatively distant related isolates (<xref ref-type="fig" rid="fig2">Figure 2</xref>, <xref ref-type="fig" rid="fig3">Figure 3</xref>). This suggests that they might be different ecotypes of this species and selected by the extreme conditions of this soil.</p></sec><sec id="s5"><title>5. Conclusion</title><p>The results of this investigation concluded that despite extreme salinity and pH conditions, an active bacterial population with a nitrogen fixation potential was found in the soil of the former Lake Texcoco. The cultivable nitrogen-fixing guild in this environment was mainly represented by Paenibacillus spp.</p><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Maximum-likelihood phylogenetic tree showing the position of the nifD gene fragments amplified from the nitrogen-fixing isolates from soils of the former Lake Texcoco. The scale bars indicate the nucleotide substitutions per site. Numbers at the branches indicate the bootstrap values of 500 resamplings. Only values above 50% are shown. nifD of Cyanobacteria group served as outgroup</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-2270736x9.png"/></fig></sec><sec id="s6"><title>Acknowledgements</title><p>This research was funded by Centro de Investigaci&#243;n y de Estudios Avanzados (CINVESTAV) and Y. E. Navarro-Noya received a postdoctoral grant BM11-132 from Instituto de Ciencia y Tecnolog&#237;a del Distrito Federal (ICyTDF, Mexico).</p></sec><sec id="s7"><title>Cite this paper</title><p>Yendi E. Navarro-Noya,Marco Luna-Guido,Luc Dendooven, (2016) Cultivable Nitrogen Fixing Bacteria from Extremely Alkaline-Saline Soils. Advances in Microbiology,06,412-423. doi: 10.4236/aim.2016.66041</p></sec><sec id="s8"><title>NOTES</title></sec></body><back><ref-list><title>References</title><ref id="scirp.66455-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Dudal, R. 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