Ali Nejidat

Assessment of the spatial distribution of soil microbial communities in patchy arid and semi‐arid landscapes of the Negev Desert using combined PLFA and DGGE analyses

Arid and semi-arid ecosystems are often characterized by vegetation patchiness and variable availability of resources. Phospholipid fatty acid (PLFA) and 16S rRNA gene fragment analyses were used to compare the bulk soil microbial community structure at patchy arid and semi-arid landscapes. Multivariate analyses of the PLFA data and the 16S rRNA gene fragments were in agreement with each other, suggesting that the differences between bulk soil microbial communities were primarily related to shrub vs intershrub patches, irrespective of climatic or site differences. This suggests that the mere presence of a living shrub is the dominant driving factor for the differential adaptation of the microbial communities. Lipid markers suggested as indicators of Gram-positive bacteria were higher in soils under the shrub canopies, while markers suggested as indicators of cyanobacteria and anaerobic bacteria were elevated in the intershrub soils. Secondary differences between soil microbial communities were associated with intershrub characteristics and to a lesser extent with the shrub species. This study provides an insight into the multifaceted nature of the factors that shape the microbial community structure in patchy desert landscapes. It further suggests that these drivers not only act in concert but also in a way that is dependent on the aridity level.

The Identification and Characterization of Osmotolerant Yeast Isolates from Chemical Wastewater Evaporation Ponds

Ramat Hovav is a major chemical industrial park manufacturing pharmaceuticals, pesticides, and various aliphatic and aromatic halogens. All wastewater streams are collected in large evaporation ponds. Salinity in the evaporation ponds fluctuates between 3% (w/v) and saturation and pH values range between 2.0 and 10.0. We looked for microorganisms surviving in these extreme environmental conditions and found that 2 yeast strains dominate this biotope. 18S rDNA sequence analysis identified the isolates as Pichia guilliermondii and Rhodotorula mucilaginosa. Both isolates grew in NaCl concentrations ranging up to 3.5 M and 2.5 M, respectively, and at a pH range of 2-10. There was a distinct difference between the Rhodotorula and Pichia strains and S. cerevisiae RS16 that served as a control strain with respect to accumulation of osmoregulators and internal ion concentrations when exposed to osmotic stress. The Pichia and Rhodotorula strains maintained high glycerol concentration also in media low in NaCl. Utilization of various carbon sources was examined. Using a tetrazolium-based assay we show that the Rhodotorula and Pichia strains are capable of utilizing a wide range of different carbon sources including anthracene, phenanthrene, and other cyclic aromatic hydrocarbons.

Effect of organic and inorganic nitrogenous compounds on RDX degradation and cytochrome P-450 expression in Rhodococcus strain YH1.

We hypothesized that biodegradation of hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX)—a widely used explosive contaminating soil and groundwater—by Rhodococcus strain YH1 is controlled by the presence of external nitrogen sources. This strain is capable of degrading RDX while using it as sole nitrogen source under aerobic conditions. Both inorganic and organic nitrogen sources were found to have a profound impact on RDX-biodegradation activity. This effect was tested in growing and resting cells of strain YH1. Nitrate and nitrite delayed the onset of RDX degradation by strain YH1, while ammonium inhibited it almost completely. In addition, 2,4,6-trinitrotoluene (TNT) inhibited RDX degradation and growth of strain YH1. On the other hand, tetrahydrophthalamide did not influence biodegradation or growth. Growth on RDX induced the expression of a cytochrome P-450 enzyme that is suggested to be involved in the first step in the aerobic pathway of RDX degradation, as identified by SDS-PAGE analysis. Ammonium and nitrite strongly repressed cytochrome P-450 expression. Our findings suggest that effective RDX bioremediation by strain YH1 requires the design of a treatment scheme that includes initial removal of ammonium, nitrite, nitrate and TNT before RDX degradation can take place.

DNA markers for sex: Molecular evidence for gender dimorphism in dioecious Mercurialis annua L.

Male specific Random Amplified Polymorphic DNA (RAPD) markers, OPB01-1562 and OPC07-303, were identified and sequenced in dioecious Mercurialis annua. Sequence Characterized Amplified Region (SCAR) primers were designed. Several internal segments of OPB01-1562 were amplified as male specific SCAR markers. These markers were PCR amplified from strong, intermediate and weak male subtypes selected according to their resistance to feminization by cytokinin. Nucleotide sequence of OPB01-1562 isolated from three male subtypes were near identical. The OPB01-1562 and derived SCAR markers were absent in females as well as hexaploid Mercurialis male and monoecious individuals. The gender relationship of the markers was maintained in all ecotypes tested. There were 2 internal fragments of OPB01-1562, which were PCR amplified from all genotypes of diploid and hexaploid Mercurialis. It is argued that identification of gender specific DNA suggests a dimorphic differentiation of the genome of dioecious Mercurialis annua.

Spatial and temporal diversity and abundance of ammonia oxidizers in semi-arid and arid soils: indications for a differential seasonal effect on archaeal and bacterial ammonia oxidizers

Besides water, nitrogen is the limiting factor for biomass production in arid ecosystems. Global climatic changes are exacerbating aridity levels, and the response of nitrogen-transforming microorganisms to these changes is not clear yet. Using semi-arid and arid ecosystems as surrogates for conditions of increased aridity, we investigated the activity, abundance, and diversity of ammonia-oxidizing bacteria (AOB) and archaea (AOA) in arid and semi-arid soils. Ammonia oxidation potentials were higher during the winter in both sites than in the summer, and higher nitrate concentrations were measured in the arid soil than in the semi-arid soil. Denaturing gradient gel electrophoresis (DGGE) patterns of AOB 16S rRNA gene fragments were similar for the arid and semi-arid soils with no seasonal variations. In contrast, the DGGE patterns of the AOA amoA gene fragments differed between the sites and a soil transfer experiment suggested that these differences are possibly associated with soil type. AOB numbers were higher during the winter than in the summer, while AOA numbers were higher during the summer. The results indicate the resistance of AOB and AOA community structure to arid conditions, albeit with seasonal variations in their abundance. Together, the results suggest the resilience of nitrification activity to increased aridity level.

Soil nitrifying enrichments as biofilter starters in intensive recirculating saline water aquaculture

Abstract Intensive recirculating aquaculture relies on biofilters to sustain satisfactory water quality in the ponds. Establishment of new biofilters in aquaculture ponds without a start-up culture requires a long period of time and may therefore cause significant losses and environmental harm due to discharge of nitrogen-rich effluents. A laboratory scale setup (7-l aquaria with shrimp and fish) demonstrated that an external start-up nitrifying enrichment culture performed similarly to the natural bacterial population of an established pond biofilter, and superior to the performance of similar biofilters without a start-up culture (control). Ammonia concentration in the control treatment increased daily and reached 18 mg l −1 during a 14-day experiment, whereas in the treated aquaria, it averaged less than 2 mg l −1 . Fish growth and survival were similar in the treated aquaria (average growth of 0.45 g/14 days, and 95% survival) and significantly higher than in the control (average growth of 0.0 g/14 days, and 80% survival). The source for the enrichment cultures was soil samples collected from the region where the farm is situated. This approach may lead to the development of bacterial amendments (probiotic products) that can be used as start-up cultures for new operations or damaged filters, and potentially enhance nitrification in established filters. As the cultures are collected from soils, it is unlikely that they will be contaminated with fish disease-causing agents. This will improve water quality and consequently aquatic animal production.

Activity and survival of tribromophenol-degrading bacteria in a contaminated desert soil

A strain of bromophenol degrading bacteria was isolated from a contaminated desert soil. The isolate identified as Achromobacter piechaudii and designated as strain TBPZ was able to metabolize both 2,4,6-tribromophenol and chlorophenols. The degradation of halophenols resulted in the stechiometric release of bromide or chloride. Growth and degradation of bromophenol were enhanced in the presence of yeast extract. To follow the survival of an introduced bacteria in the contaminated soil, TBPZ was transformed with a plasmid carrying a gene for kanamycin resistance and the lux CDABE operon from the luminescent bacteria Vibrio fischeri under the control of a constitutive promoter producing strain TBPZ-N61. The activity of the transformed bacteria was not affected by the insertion of the plasmid. Specific detection of the introduced isolate in the contaminated soil samples was achieved by selection on kanamycin. Survival of the introduced bacteria, TBPZ-N61, in the contaminated soil was influenced by soil moisture. Biodegradation of TBP occurred only in soil with at least 25% water content. Addition of yeast extract increased the survival and the activity of the introduced bacteria. The current study demonstrated that the limiting factors controlling pollutant degradation in a contaminated desert soil are water content, nutrient availability and the bioaugmentation of an appropriate microbial population.

Polymorphism and DNA markers for asparagus cultivars identified by random amplified polymorphic DNA

SummaryDNA polymorphism among five Asparagus officinalis L. cultivars-Imperial, Snow, Steline, UC-157 and Larac, as detected by random amplified polymorphic DNA (RAPD), is reported. Thirty one decamer primers were tested. and twenty six of them yielded amplification products. Fourteen primers gave products with at least one polymorphic DNA fragment. Among a total of 119 amplified fragments 33 were polymorphic. These RAPD markers enabled the identification of asparagus cultivars. Unique markers for cultivars were: Snow-bands 475 bp, 772 bp, 412 bp, 935 bp and 820 bp amplified by primers D5, OPA-07, OPA-09, OPA-10 and OPA-18, respectively. Steline-bands 645 bp, 680 bp and 997 bp amplified by primers A32, OPA-03 and OPA-09, respectively. A band 903 bp, amplitied by primer OPA-12, is a marker for Imperial, and a band 420 bp, amplified by primer D52, is a marker for Larac. Cultivar UC-157 could be identified by a combination of shared polymorphic bands. The pairwise marker difference between cultivars ranged from 0.08 to 0.17. A phenogram of the genetic relationship based on RAPD fits with the known origin of the cultivars.

Alterations in protein synthesis and levels of heat shock 70 proteins in response to salt stress of the halotolerant yeast Rhodotorula mucilaginosa.

Responses of the halotolerant yeast Rhodotorula mucilaginosa YRH2 to salt stress was studied. Strain YRH2 was isolated from chemical industry park wastewater evaporation ponds that are characterized by large fluctuations in salinity and pH. Upon shift to high salt medium there is a shutdown of protein synthesis. Radiolabeling and separation of proteins from salt stressed and non-stressed cells identified down-regulated heat shock 70 proteins Ssb1/2p, by N-terminal sequencing and Western blotting. Ssb’s role in salt stress in both R. mucilaginosa and S. cerevisiae was examined and we show that its response to salt stress and amino acid limitation is similar. Other proteins such as the heat shock 70 protein Kar2p/BiP and Protein Disulfide Isomerase were strongly induced in response to a shift to high salt in R. mucilaginosa and reacted in a manner similar to the effect of tunicamycin, a known unfolded protein response inducer. Also, assaying carboxypeptidase Y, we showed that high salt medium reduces the specific activity of the enzyme in R. mucilaginosa. It is suggested that the changes in the expression of the heat shock 70 proteins is a part of a mechanism which alleviates the damaging effects of high salt on protein folding in the yeast Rhodotorula mucilaginosa.

Ammonia transformations and abundance of ammonia oxidizers in a clay soil underlying a manure pond

Unlined manure ponds are constructed on clay soil worldwide to manage farm waste. Seepage of ammonia-rich liquor into underlying soil layers contributes to groundwater contamination by nitrate. To identify the possible processes that lead to the production of nitrate from ammonia in this oxygen-limited environment, we studied the diversity and abundance of ammonia-transforming microorganisms under an unlined manure pond. The numbers of ammonia-oxidizing bacteria and anammox bacteria were most abundant in the top of the soil profile and decreased significantly with depth (0.5 m), correlating with soil pore-water ammonia concentrations and soil ammonia concentrations, respectively. On the other hand, the numbers of ammonia-oxidizing archaea were relatively constant throughout the soil profile (10(7) amoA copies per g(soil)). Nitrite-oxidizing bacteria were detected mainly in the top 0.2 m. The results suggest that nitrate accumulation in the vadose zone under the manure pond could be the result of complete aerobic nitrification (ammonia oxidation to nitrate) and could exist as a byproduct of anammox activity. While the majority of the nitrogen was removed within the 0.5-m soil section, possibly by combined anammox and heterotrophic denitrification, a fraction of the produced nitrate leached into the groundwater.