Form and seismic stratigraphy of Halimeda banks in part of the northern Great Barrier Reef Province

Twenty-six percent of the total shelf area in the Northern Region of the Great Barrier Reef Province between latitudes 14°27 and 15°02S is occupied by algal (Halimeda) lithofacies. Sea-bed relief over this bankforming algal lithofacies, which dominates the outer shelf, is generally complex and variable over relatively short distances, but lateral continuity of morphological features near Petricola and Stewart shoals has been demonstrated by parallel profiling. The most prominent subbttom reflector is a pre-Holocene erosion surface, regarded as the Holocene/Pleistocene unconformity. In this area, the maximum thickness of Holocene Halimeda banks above the main subbottom reflector is 19 m. Seismic response suggests three main sequences in the Halimeda bank depostis, which probably relate to changes in environmental conditions, and the recognition of similar seismic characteristics in the deposits beneath the Holocene/Pleistocene unconformity indicates that Halimeda banks may have been a feature of the outer shelf of the Great Barrier Reef in Plesitocene times.     

Preliminary studies of cyanobacteria, picoplankton, and virioplankton in the Salton Sea with special attention to phylogenetic diversity among eight strains of filamentous cyanobacteria

Cyanobacterial diversity in the Salton Sea, a high-salinity, eutrophic lake in Southern California, was investigated using a combination of molecular and morphological approaches. Representatives of a total of 10 described genera (Oscillatoria, Spirulina, Arthrospira, Geitlerinema, Lyngbya, Leptolyngbya, Calothrix, Rivularia, Synechococcus, Synechocystis) were identified in the samples; additionally, the morphology of two cultured strains do not conform to any genus recognized at present by the bacteriological system. Genetic analysis, based on partial 16S rRNA sequences suggested considerable cryptic genetic variability among filamentous strains of similar or identical morphology and showed members of the form-genus Geitlerinema to be distributed among three major phylogenetic clades of cyanobacteria. Cyanobacterial mats, previously described from the Sea were, in fact, composed of both filamentous cyanobacteria and a roughly equivalent biomass of the sulfur-oxidizing bacterium Beggiatoa, indicating their formation in sulfide rich regions of the lake. Flow cytometric analysis of the water samples showed three striking differences between samples from the Salton Sea and representative marine waters: (1) phycoerythrin-containing unicells, while abundant, were much less abundant in the Salton Sea than they were in typical continental shelf waters, (2) Prochlorococcus appears to be completely absent, and (3) small (3–5 m) eukaryotic algae were more abundant in the Salton Sea than in typical neritic waters by one-to-two orders-of-magnitude. Based on flow cytometric analysis, heterotrophic bacteria were more than an order of magnitude more abundant in the Salton Sea than in seawater collected from continental shelf environments. Virus particles were more abundant in the Salton Sea than in typical neritic waters, but did not show increases proportionate with the increase in bacteria, picocyanobacteria, or eukaryotic algae.     

Studies on Halimeda

Large areas of the inter-reefal seabed in the Great Barrier Reef are carpeted with vegetation composed almost entirely of the green calcareous alga Halineda. These meadows occur principally in the northern sections between 11°30 and 15°35S at depths of 20 to 40 m, but there are also some in the central and southern sections, where they have been found at depths down to 96 m. The vegetation is dominated by the same sprawling Halimeda species that are common on coral reefs in this region. However, on reefs these species grow on solid substrata, not soft sediments like the Halimeda-rich gravels that underlie the meadows. A total of 12 Halimeda species, together with two Udotea and one Penicillus species, are characteristic components of the shallow meadows. Below 50 m depth, species composition is restricted to only two major components. One, H. copiosa, is also important shallower, but the other is an unusually large and heavily calcified form of H. fragilis, a species that is normally a minor, fragile component of the shallow meadows. The maximum biomass found in these meadows was 4637 gm² of calcareous algae, although the thean for vegetated areas was 525 gm². These meadows are confined to the nutrient-depleted waters of the outer continental shelf just inside the outer barrier reefs, and are usually associated with distinct shoaling of the seabed caused by accumulation of thick deposits of calcareous Halimeda segments. The meadows are probably supported by very localized upwelling of nutrients from the adjacent Coral Sea onto the shelf, where they enrich the otherwise nutrient-depleted waters.Contribution No.367 from the Australian Institute of Marine Science     

Production of a Gaseous Saturated-hydrocarbon Mixture by Rhizopus japonicus under Aerobic Conditions

The microbial production, by the genus Rhizopus, of a gaseous saturated-hydrocarbon mixture was studied under aerobic conditions. Rhizopus strains, comprising 13 strains of 9 species, were tested as to their ability to produce a gaseous hydrocarbon mixture. Except for one strain, all the strains tested produced more than two kinds of gaseous hydrocarbons simultaneously when grown in nutrient broth containing glucose. Rhizopus japonicus IFO 4758 was selected as being typical of these producers of mixed gaseous hydrocarbons. When this organism was cultivated in a synthetic medium supplemented with l-cysteine under aerobic conditions, the maximum production of the total gaseous hydrocarbon mixture reached ca. 10 nl/ml culture broth/hr. The gaseous hydrocarbon mixture produced was composed mainly of paraffin hydrocarbons, i.e., ca. 74% pentane, ca. 16% propane and a trace amount of methane. The ratios of saturated to unsaturated, and even to odd number hydrocarbons produced by this fungus were 95 : 5 and 90: 10, respectively. The biosynthetic pathways for the production of these gases are discussed in comparison with the biosynthetic pathways for ethylene and isobutene in microorganisms.     

Simulation of the effects of Acanthaster planci on the population structure of massive corals in the genus Porites: evidence of population resilience?

Scleractinian corals in the genus Porites are slow growing, can live for centuries, and can attain great size. In these respects they differ from the majority of coral species, which grow faster and live for years to decades. The predatory starfish Acanthaster planci L. feeds on a wide range of coral species including Porites spp., and during outbreaks in its populations, causes high coral mortality and injury over much of the affected reefs. Because they are slow growing and because recent outbreaks of the starfish occurred only 15 years apart, it may be argued that the Porites populations on affected reefs will be sent into a period of prolonged decline. The present study uses a size stage model of the transition matrix type to predict effects of starfish outbreaks of various frequencies on Porites populations. A transition matrix characterizing the mortality and injury caused in different Porites size classes at John Brewer Reef during an outbreak year was determined from field data. Transition matrices for non-outbreak years were constructed on the basis of realistic growth rates and postulated survivorship and recruitment schedules. The medium term (100 years) effects of outbreaks were simulated by alternation of a single iteration of the outbreak matrix with many iterations of each non-outbreak matrix. By varying the interval between simulated outbreaks it was possible to define combinations of growth rate, survivorship and recruitment which were viable for various outbreak intervals. Simulations based on estimates of the initial size frequency distribution, recruitment rates and colony growth rates for the John Brewer Reef population predicted that the population would remain viable in the face of outbreaks every 15 years only if juvenile and adult survivorship were high. However, within the range of colony growth rates known to occur throughout the Great Barrier Reef and at recruitment rates of the same order as those estimated in the field population, it appears that a much wider range of survivorship schedules could lead to parity or even sustained growth in the face of outbreaks recurring at intervals of from 1 to 3 decades. It is suggested that because the key measurable parameters (initial size structure, damage characteristics, recruitment rate and growth rate) are likely to be very patchy at the scale of whole reefs, no general statement concerning the prognosis for Porites would be meaningful. However the model provides a tool by which a standardized evaluation of this type of field data may be made on a reef by reef basis.     

Genetic control of glucokinase activity in mice

Inbred strains of mice were surveyed for liver glucokinase activity. Mice of all strains studied could be distributed into three groups with high, intermediate, and low levels of enzyme activity. Genetic analysis using crosses and backcrosses with prototype high (C3H/HeJ) and low (RF/J) strains revealed that glucokinase activity was controlled by a single gene. The name glucokinase and gene symbol Gk are suggested for this gene. The Gk ^a allele designates the strain with high glucokinase activity, while Gk ^b represents the allele in the strain with the low enzyme activity. The interaction of fasting and diabetes on the activity of glucokinase in these two strains is described.Supported in part by United States Public Health Service Research Grant CA 05873 from the National Cancer Institute. The Jackson Laboratory is fully accredited by the American Association for the Accreditation of Laboratory Animal Care.     

New record of moss and thermophilic bacteria species and physico-chemical properties of geothermal soils on the northwest slope of Mt. Melbourne (Antarctica)

Four samples of surface soils, one with shoots of an unidentified moss species, were collected from a geothermal site on the northwest slope of volcanic Mt. Melbourne (northern Victoria Land, continental Antarctica) to determine physico-chemical properties, isolate existing strains of heterotrophic microorganisms, and identify the moss species through molecular genetic techniques. Surface soil features such as temperature, grain-size, pH, moisture content, and isolated genera of bacteria, generally corresponded to those previously reported for other geothermal sites in Victoria Land. However, when compared with chemical characteristics of warm substrata from these sites, soils from the northwest slope of Mt. Melbourne showed lower contents of total N and water-extractable PO₄^3– and K⁺, and relatively higher concentrations of Na, Fe, Mn, and of potentially toxic elements such as Cd and Pb. Preliminary results indicate that a new species of thermophilic bacteria growing in Fe-enriched medium was isolated. Although the study area lay only about 1.5 km from Cryptogam Ridge, a geothermal site in the rim of the Mt. Melbourne summit crater with a well-developed population of the moss Campylopus pyriformis, molecular genetic analyses showed that the moss on the volcano slope is Pohlia nutans, a species closely related to populations some 110 km to the north in the Mt. Rittmann fumaroles. It was concluded that physico-chemical features of geothermal grounds may affect the colonisation history and dispersal of microorganisms and mosses.     

SelectingRhizobium phaseoli strains for use with beans (Phaseolus vulgaris L.) in Kenya: Infectiveness and tolerance of acidity and aluminium

Forty strains ofRhizobium phaseoli, isolated from Kenyan soils, were tested for infectiveness on common bean (Phaseolus vulgaris L.). 28 strains were infective and a cultivar × Rhizobium interaction was observed. 48 strains were screened for tolerance of acidity and Al in liquid culture. Assessment of visible turbidity after 14 days indicated 34 strains tolerant of pH 4.5 but none tolerant of pH 3.5. No strain was tolerant of 50 M Al at pH 5.5. Three strains were tolerant of 20 M Al at pH 5.5 and 10 M Al at pH 4.5. Screening on a solid medium identified strains tolerant of 20 and 50 M Al at pH 5.5 and 4.5 which were sensitive to these treatments in liquid culture. Those strains tolerant to 20 M Al at pH 4.5 and 5.5 in liquid culture were correctly identified on the solid medium.     

Phytoplankton biomass and primary production in semi-enclosed reef lagoons of the central Great Barrier Reef,Australia

Phytoplankton biomass and primary production rates within semi-enclosed reef lagoons of the central Great Barrier Reef were compared with adjacent shelf waters. Chlorophyll concentrations and surface primary production rates were usually higher in lagoons although seasonal differences were only significant during the summer. Nitrate concentrations were higher in lagoons than in shelf waters year-round. Nano- (<20 m size fraction) or pico-phytoplankton (<2 m size fraction) dominated phytoplankton biomass and production within reef lagoons throughout the year. Net phytoplankton (>10–20 m size fraction), however, were relatively more important in both reef lagoons and open shelf waters during the summer. Biomass-specific production within lagoons (range 41–90 mg C mg chl^–1 day^–1) was high, regardless of season. Lagoonal phytoplankton production (range 0.2–1.6 g C m^–2 day^–1) was directly correlated with standing crop and inversely related to lagoon flushing rates. Phytoplankton blooms develop within GBR reef lagoons during intermittent calm periods when water residence times exceed phytoplankton generation times.     

Isolation of large linear plasmids from β-lactam producing actinomycete strains

Summary Sixteen -lactam producing actinomycete strains were screened for the presence of large linear plasmids. Among these, four strains contained linear plasmids of 12–450 kb in size. Southern blot analysis using a synthetic oligonucleotide for the isopenicillin N synthase gene and plasmid pBROC137 containing thecefD andcefE genes in the cephalosporin biosynthesis, respectively, showed no hybridization. This result suggests that these linear plasmids are not involved in the biosynthesis of -lactam antibiotics.     

Predicting the Location and Spatial Extent of Submerged Coral Reef Habitat in the Great Barrier Reef World Heritage Area,Australia

Aim

Coral reef communities occurring in deeper waters have received little research effort compared to their shallow-water counterparts, and even such basic information as their location and extent are currently unknown throughout most of the world. Using the Great Barrier Reef as a case study, habitat suitability modelling is used to predict the distribution of deep-water coral reef communities on the Great Barrier Reef, Australia. We test the effectiveness of a range of geophysical and environmental variables for predicting the location of deep-water coral reef communities on the Great Barrier Reef.

Location

Great Barrier Reef, Australia.

Methods

Maximum entropy modelling is used to identify the spatial extent of two broad communities of habitat-forming megabenthos phototrophs and heterotrophs. Models were generated using combinations of geophysical substrate properties derived from multibeam bathymetry and environmental data derived from Bio-ORACLE, combined with georeferenced occurrence records of mesophotic coral communities from autonomous underwater vehicle, remotely operated vehicle and SCUBA surveys. Model results are used to estimate the total amount of mesophotic coral reef habitat on the GBR.

Results

Our models predict extensive but previously undocumented coral communities occurring both along the continental shelf-edge of the Great Barrier Reef and also on submerged reefs inside the lagoon. Habitat suitability for phototrophs is highest on submerged reefs along the outer-shelf and the deeper flanks of emergent reefs inside the GBR lagoon, while suitability for heterotrophs is highest in the deep waters along the shelf-edge. Models using only geophysical variables consistently outperformed models incorporating environmental data for both phototrophs and heterotrophs.

Main Conclusion

Extensive submerged coral reef communities that are currently undocumented are likely to occur throughout the Great Barrier Reef. High-quality bathymetry data can be used to identify these reefs, which may play an important role in resilience of the GBR ecosystem to climate change.     

Significance of <Emphasis Type="Italic">Halimeda</Emphasis> bioherms to the global carbonate budget based on a geological sediment budget for the Northern Great Barrier Reef,Australia

Since the correlation between carbon dioxide (CO₂) levels and global temperatures was established in the ice core records, quantifying the components of the global carbon cycle has become a priority with a view to constraining models of the climate system. The marine carbonate budget is still not adequately constrained and the quantitative significance of the calcareous green alga Halimeda still remains particularly poorly understood. Previously, it has been suggested that Halimeda bioherms on the shelf of the Great Barrier Reef may contain a volume of carbonate equal to or greater than that contained within the shelf edge coral reefs. This study uses published datasets to test this hypothesis in the Northern Great Barrier Reef (NGBR) province. It is estimated that Halimeda bioherms on the outer shelf of the NGBR contain at least as much (and up to four times more) CaCO₃ sediment as the adjacent ribbon reef facies. Globally, if these findings are even only partially applicable, the contribution of shallow water carbonate sediments to the global carbon budget based on coral reefs alone is currently substantially underestimated.     

Decline in condition of gorgonian octocorals on mesophotic reefs in the northern Gulf of Mexico: before and after the Deepwater Horizon oil spill

Hard-bottom ‘mesophotic’ reefs along the ‘40-fathom’ (73 m) shelf edge in the northern Gulf of Mexico were investigated for potential effects of the Deepwater Horizon (DWH) oil spill from the Macondo well in April 2010. Alabama Alps Reef, Roughtongue Reef, and Yellowtail Reef were near the well, situated 60–88 m below floating oil discharged during the DWH spill for several weeks and subject to dispersant applications. In contrast, Coral Trees Reef and Madison Swanson South Reef were far from the DWH spill site and below the slick for less than a week or not at all, respectively. The reefs were surveyed by ROV in 2010, 2011, and 2014 and compared to similar surveys conducted one and two decades earlier. Large gorgonian octocorals were present at all sites in moderate abundance including Swiftia exserta, Hypnogorgia pendula, Thesea spp., and Placogorgia spp. The gorgonians were assessed for health and condition in a before-after-control-impact (BACI) research design using still images captured from ROV video transects. Injury was modeled as a categorical response to proximity and time using logistic regression. Condition of gorgonians at sites near Macondo well declined significantly post-spill. Before the spill, injury was observed for 4–9 % of large gorgonians. After the spill, injury was observed in 38–50 % of large gorgonians. Odds of injury for sites near Macondo were 10.8 times higher post-spill, but unchanged at far sites. The majority of marked injured colonies in 2011 declined further in condition by 2014. Marked healthy colonies generally remained healthy. Background stresses to corals, including fishing activity, fishing debris, and coral predation, were noted during surveys, but do not appear to account for the decline in condition at study sites near Macondo well.     

Isolation and Characterization of Bacteria Capable of Degrading Phenol and Reducing Nitrate Under Low-Oxygen Conditions

Nitrate-reducing bacteria capable of degrading phenol were isolated from natural and contaminated environments under low-oxygen conditions with nitrate-containing media, using phenol as a sole carbon and energy source. A total of 27 bacteria able to degrade phenol and reduce nitrate under low-oxygen conditions were isolated from all of the inoculum samples, regardless of previous phenol contamination. For all of these bacteria, oxygen was an essential requirement for phenol degradation. Nitrate reduction by 19 of the strains was insensitive to 10 mM sodium azide, and these strains were placed into the - and -subclasses of Proteobacteria and two were Gram-positive bacteria. To date, the order of Rhizobiales has hardly been reported to have an ability to degrade aromatic compounds. Interestingly, our study showed that all isolates that were placed into the -subclass of Proteobacteria are in the order of Rhizobiales. Furthermore, the genus Agrobacterium was isolated from most inoculum samples and one genus of Gram-positive bacteria, Staphylococcus, was also isolated. In the case of the remaining eight strains, nitrate reduction was inhibited by 10 mM sodium azide. Of these strains, seven were placed into the -subclass of Proteobacteria.     

Characteristics of 0/129-sensitive motile Aeromonas strains isolated from freshwater on starch-ampicillin agar

Motile Aeromonas hydrophila strains were recovered from several freshwater sources by spread-plating water samples on starch-ampicillin agar, originally described as a medium for recovering Aeromonas hydrophila quantitatively from foods. Starch-ampicillin agar was compared with membrane Aeromonas medium and Rimler-Shotts medium for selectivity for, and recovery of, Aeromonas strains from freshwater. Thirty-four Aeromonas strains thus isolated were identified to species level by their phenotypic characteristics, and the Mol% G+C of representative strains was determined. Although resistant to 10 g of the vibriostatic agent 0/129, all these strains showed sensitivity to 150 g 0/129, which brings into question the use of this agent for distinguishing aeromonads from vibrios. The ability of these strains to produce extracellular virulence factors was generally similar to that reported for environmental strains isolated by other methods from various geographical locations within and beyond Australia. Ten of the 20 A. sobria strains, but none of the A. hydrophila or A. caviae strains, produced enterotoxin as shown by the suckling mouse test. Haemolysin was produced by 9/10 of the enterotoxigenic A. sobria strains and 2/9 A. hydrophila strains. Hemagglutinating activity was detected in 5/20 A. sobria and 7/9 A. hydrophila strains, and was inhibited by fucose and mannose, but not by galactose. The characteristics of these strains were comparable with those of Aeromonas strains isolated from other freshwater environments apart from their sensitivity to 0/129. Send offprint requests to: M. Cahill.     

Separation of multiple genes controlling the T-cell proliferative response to IL-2 and anti-CD3 using recombinant congenic strains

T lymphocytes of the strain BALB/cHeA exhibit a low proliferative response to IL-2 and a high response to the anti-CD3 monoclonal antibodies, while the strain STS/A lymphocyte response to these stimuli is the opposite. We analyzed the genetic basis of this strain difference, using a novel genetic tool: the recombinant congenic strains (RCS). Twenty BALB/c-c-STS/Dem (CcS/Dem) RCS were used, each containing a different random set of approximately 12.5% of the genes from STS and the remainder from BALB/c. Consequently, the genes participating in the multigenic control of a phenotypic difference between BALB/c and STS become separated into different CcS strains where they can be studied individually. The strain distribution patterns of the proliferative responses to IL-2 and anti-CD3 in the CcS strains are different, showing that different genes are involved. The large differences between individual CcS strains in response to IL-2 or anti-CD3 indicate that both reactions are controlled by a limited number of genes with a relatively large effect. The high proliferative response to IL-2 is a dominant characteristic. It is not caused by a larger major cell subset size, nor by a higher level of IL-2R expression. The response to anti-CD3 is known to be controlled by polymorphism in Fc receptor 2 (Fcgr2) and the CcS strains carrying the low responder Fcgr2 allele indeed responded weakly. However, as these strains do respond to immobilized anti-CD3, while the STS strain does not, and as some CcS strains with the BALB/c allele of Fcgr2 are also low responders, additional gene(s) of the STS strain strongly depress the anti-CD3 response. In a backcross between the high responder and the low responder strains CcS-9 and CcS-11, one of these unknown genes was mapped to the chromosome 10 near D10Mit14. The CcS mouse strains which carry the STS alleles of genes controlling the proliferative response to IL-2 and anti-CD3 allow the future mapping, cloning, and functional analysis of these genes and the study of their biological effects in vivo.     

Relationships among isolates of oral haemophili as determined by DNA-DNA hybridization

In order to assess the relationships among strains of the genera Actinobacillus and Haemophilus, DNAs from 50 strains of these genera were isolated and purified. The guanine plus cytosine (G+C) content of DNAs from strains of Haemophilus segnis and Haemophilus para-influenzae were determined by thermal denaturation. DNA-DNA homologies were measured using labelled probes from one strain representing Haemophilus segnis (strain ATCC 10977), and two strains representing Haemophilus parainfluenzae (strains ATCC 9796 and ATCC 7901). Strains isolated as H. segnis had a G+C content of 39.0 to 42.9% and were 49–92% homologous with the ATCC 10977 DNA probe. All of the strains freshly isolated as H. parainfluenzae were 70–81% homologous with the ATCC 9796 DNA probe and had a G+C content of 34.9 to 38.3%. Strain ATCC 7901 was 11% homologous with the ATCC 9796 DNA probe, had a G+C content of 42.4%, and was 65–78% homologous to DNA from strains identified as Haemophilus aphrophilus and Haemophilus paraphrophilus. From these results we conclude that strain ATCC 7901 is a mislabelled strain of H. paraphrophilus. The results of multiple DNA-DNA hybridizations indicated that separate species designations were appropriate for H. segnis, H. parainfluenzae, Actinobacillus actinomycetemcomitans (Haemophilus actinomycetemcomitans), and H. aphrophilus. H. aphrophilus and H. paraphrophilus were closely related organisms and did not fulfill the generally accepted criteria for designation as separate species.     

Development of gene transfer methods forRubrivivax gelatinosus S1: construction, characterization and complementation of apuf operon deletion strain

Gene transfer systems were developed inRubrivivax (Rx.) gelatinosus S1. First, a system for conjugative transfer of mobilizable plasmids fromEscherichia coli toRx. gelatinosus S1 was established. Secondly, optimal conditions for the transformation ofRx. gelatinosus S1 by electroporation were determined. A puf strain was constructed. Complementation with thepuf operon from a wild-type strain cloned in a replicative plasmid restored photosynthetic growth. Two insertion strains were also selected. All the strains constructed were green, due to a change in carotenoid content. Characterization of these strains provides genetic evidence for a superoperon organization in this bacterium.     

Identification and quantitation of near-UV absorbing compounds (S-320) in a hermatypic scleractinian

Reef-building corals from shallow waters are known to contain a suite of water soluble compounds (collectively named S-320) which strongly absorb near-UV light. Compounds of this type have now been isolated from the Pacific staghor coral Acropora formosa and identified as a series of mycosporine-like amino acids including mycosporine-Gly (_max=310nm), palythine (_max=320nm) and palythinol (_max=332nm). These compounds were separated and quantified by high-performance liquid chromatography. Serial extraction efficiencies were calculated using a simple formula which is derived herein. For 12-cm long coral branches collected from a depth of 3 m at Rib Reef, Great Barrier Reef, Australia (146° 53E, 18° 29S) the average concentrations of mycosporine-Gly, palythine, and palythinol were 37.8, 56.4 and 0.895 nmol per mg coral protein, respectively. The coral samples can be stored at-20°C for at least 144 days without degradation of the mycosporinelike amino acids.Contribution number 334 from the Australian Institute of Marine Science     

Cadmium Resistance Mechanism in Acidophilic and Alkalophilic Bacterial Isolates and their Application in Bioremediation of Metal-Contaminated Soil

Acidophilic and alkalophilic cadmium-resistant bacterial strains were isolated from the metal-contaminated soil of Panki thermal power plant, Kanpur, India, and two strains, namely SB21 (acidophilic) and SB20 (alkalophilic), were selected as representative strains on the basis of their high resistance to cadmium as compared to other strains. The phylogenetic analysis of the strains using 16s rDNA sequence revealed the strains to be Pseudomonas putida and Comamonas species strain, respectively. Furthermore, to determine the mechanism involved in cadmium resistance, a czc gene was amplified from the strains and sequenced. Homology of the sequences of the two strains, when compared with the available database using a BLASTn search, showed that the 650bp amplicons possess a partial czcA gene sequence. Moreover, the mechanism was confirmed by the results of atomic absorption spectroscopy and transmission electron microscopy studies, which supported the efflux mechanism in the alkalophilic strain SB20, but the acidophilic strain SB21 showed intracellular and periplasmic accumulation of metal in the cells in spite of the presence of the czcA gene, indicating the presence of multiple mechanisms of metal resistance in strain SB21.

Further, the strains were characterized functionally for their bioremediation potential in cadmium-contaminated soil under acidic and alkaline conditions by performing an in-situ greenhouse experiment using mungbean plants. A marked increase in agronomical parameters was observed under acidic conditions in the presence of strain SB21. Moreover, the concentration of metal decreased in both plants and soil in the presence of these bioinoculants; however, strain SB21 was found to be a better decontaminator than SB20 and thus can further be employed in bioremediation applications.