Eradication of populations of an invasive ant in northern Australia: successes, failures and lessons for management

Eradication is the most difficult management goal for exotic species, and successes are rare and even more rarely published. The lack of publication of the methodology and outcomes of eradication programs severely limits the transfer of knowledge to programs elsewhere that target the same or similar species. Here I detail the successes and failures of eradication efforts on six populations of African big headed ant Pheidole megacephala in northern Australia, covering a combined area of almost 9 ha. Two years post-treatment, assessment criteria for successful eradication were met for four of the six populations, whereas eradication failed in the remaining two, resulting in the need for ongoing management. Positive outcomes are attributed to eight criteria being met: (1) a single line of project management authority; (2) over-arching legal authority; (3) susceptibility of the target organism to control procedures; (4) sufficient resources; (5) detectibility of the target organism at low densities; (6) early intervention; (7) prevention of reinvasion; and (8) prevention of invasive succession. Reasons for one of the failures remain unclear, but eradication failed in the other because a part of the population was not treated. In both cases, the eradication failures could have been detected and managed much earlier than was the case. The successes and lessons documented here, coupled with the now large number of small-scale eradications of this ant, warrant the implementation of larger and more ambitious management programs against this significant invader, especially within areas of high conservation value.     

Recovery of fish and crustacean communities during remediation of tidal wetlands affected by leachate from acid sulfate soils in north-eastern Australia

In the 1970s, acid sulfate soils (ASS) distributed within about 720 ha of predominantly mangrove and salt pan wetlands at East Trinity in north Queensland were developed after the area was isolated from tidal flooding by a surrounding seawall and the installation of tidal gates on major drainage creeks. Following drainage and oxidation of these estuarine acidic sediments, resultant acid leachate caused considerable, ongoing environmental problems including regular fish kills. A rehabilitation program covering much of these former tidal wetlands commenced in 2000 using a lime-assisted tidal exchange management regime. Changes in the established populations of estuarine fish and crustaceans were monitored in the two creeks (Firewood and Hills Creeks) where tidal flows were reinstated. In Firewood Creek between 2001 and 2005, there was a progressive increase in fish species richness, diversity and abundance. The penaeid prawn Fenneropenaeus merguiensis was a major component of the cast net catches in the lower sections of both Firewood and Hills Creeks but its relative abundance decreased upstream of the tidal gates on the seawall. Well established stocks of predominantly juvenile, male Scylla serrata resident upstream of the tidal gates indicated suitable habitats with acceptable water and sediment quality and adequate availability of food. The regular fish kills that occurred prior to the management regime abated and, overall, the implementation of the rehabilitation program is yielding positive benefits for the local fisheries.     

Nitric oxide and iron: effect of iron overload on nitric oxide production in endotoxemia

The amount of iron within the cell is carefully regulated in order to provide an adequate level of micronutrient while preventing its accumulation and toxicity. Iron excess is believed to generate oxidative stress, understood as an increase in the steady-state concentration of oxygen radical intermediates. Nitric oxide (NO) is an inorganic free-radical gaseous molecule which has been shown over the last decade to play an unprecedented variety of roles in biological systems. The effect of nitrogen reactive species may explain the iron sequestration pattern that characterizes macrophages under inflammatory conditions. From a patho-physiological viewpoint, further studies are required to assess the usefulness of this mechanism to minimize formation and release of free radicals in diseased tissues. However, contrary to the deleterious effects of the reactive nitrogen oxide species formed from either NO/O(2) and NO/O(2)(-), it has been pointed out that NO shows antioxidant properties. A number of studies have described the complex relationships between iron and NO, but controversy remains as to the influence and significance of iron on inflammatory NO production. To explore the initial steps of the effects triggered by LPS administration in the presence of excess iron, male Wistar rats were treated with: lipopolysaccharide from Escherichia coli (serotype 0127:B8) (LPS); iron-dextran; or iron-dextran plus LPS and liver samples were taken after 6 h. EPR spectra of NO-Hb in the venous blood were determined at 77 K. Iron-dextran administered to rats intraperitoneally resulted predominantly in iron uptake by the liver Kupffer cells and led to an increased NO level in blood in the presence of LPS. Further studies will be required to assess the complex role of the Kupffer cells on iNOS induction and NO production.     

Influence of fulvic acid on transport of iron in soils and uptake by paddy seedlings

The influence of fulvic acid (FA) on the porous system self diffusion coefficient (Dp) of Fe in Calciorthent soils of Bihar, India, was determined with the half cell technique. Significantly higher values of Dp were observed when Fe was applied as Fe–FA to the soil compared to FeCl₃. The capacity factor of Fe decreased considerably due to its complexation by fulvic acid, resulting in an increase in the Dp of Fe. The organic carbon content of the soils correlated positively with Dp of Fe while it showed a negative relationship with active CaCO₃ and the clay content of soils. A soil culture system simulating acquisition of Fe by rice was developed to investigate transport of Fe from the soil solution to the surface of the plant roots through diffusion and mass flow. Mass flow contributed only 5–9% of the total Fe uptake by rice, with the remainder being ascribed to diffusion and root interception. A significant relationship ( r =0.96^**) between Dp- and Fe-uptake by rice was observed. The uptake of Fe by the crop and the percentage of tissue iron content derived from fertilizer were higher in the case of Fe–FA in comparison with FeCl₃, indicating the superiority of organically complexed Fe fertilizers over inorganic salts.     

Abiotic factors regulating nitrogen transformations in the organic layer of acid forest soils: Moisture and pH

The relationships between nitrogen transformations and moisture and pH in coniferous forest litter were determined using laboratory incubation experiments. A linear relation between gravimetric moisture content and nitrification was found within the whole studied range of moisture conditions (10–290% ODW). Net nitrogen mineralization increased linearly with moisture content up to 140% ODW. At higher moisture contents, net mineralization was found to be independent of moisture. Relative nitrification was found to be a linear function of moisture content. The dependence of the CO₂ production rates on moisture in the coniferous litter decreased from low to high moisture availability. Due to a nearly linear relationship between gravimetric moisture content and log-(water potential) within the investigated moisture range, the same type of relationships were found with this latter parameter as well. The relationship between nitrogen transformations and pH was studied by means of the addition of different amounts of HCl and NaOH during short incubation experiments (1 week). Nitrification was found to be a negative linear function of the H-ion concentration within the range of 0.04 (pH 4.40) and 0.36 (pH 3.45) mmol H-ion L^?1. At a higher H-ion concentration and thus at a lower pH than 3.45, no nitrate was produced any more. No relationship between net mineralization and pH was found.     

Supplement comprising of laccase and citric acid as an alternative for antibiotics: In vitro triggers of melanin production

An indiscriminate use of antibiotics in humans and animals has led to the widespread selection of antibiotic‐resistance, thus constricting the use of antibiotics. A possible solution to counter this problem could be to develop alternatives that can boost the host immunity, thus reducing the quantity and frequency of antibiotic use. In this work, for the first time, citric acid and laccase were used as extracellular inducers of melanin production in yeast cells and human cell lines. It is proposed that the formulation of laccase and citric acid together could further promote melatonin‐stimulated, melanocyte‐derived melanin production. Melanization as a probe of immunity described in this study, is an easy and a rapid test compared to other immunity tests and it allows performing statistical analyses. The results showed the synergistic effect of citric acid and laccase on melanin production by yeast cells, with significant statistical differences compared to all other tested conditions (p: 0.0005–0.005). Laccase and citric acid together boosted melanin production after 8 days of incubation. An increase in melanin production by two human colon cells lines (Cacao‐2/15 and HT‐29) was observed on supplementation with both laccase and citric acid in the cell growth medium. Produced melanin showed antimicrobial properties similar to antibiotics. Therefore, a formulation with citric acid and laccase may prove to be an excellent alternative to reduce the antibiotic use in human and animal subjects.     

Growth of oil palm (Elaeis guineensis) seedlings on acid sulfate soils as affected by water regime and aluminium

In Malaysia, acid sulfate soils contain high amounts of aluminium and are usually utilized for oil palm cultivation. As these soils are frequently flooded during rainy periods, it is thought that this may affect the growth performance of the oil palm. A glasshouse experiment was, therefore, conducted to study the effects of water regime and aluminium on the growth of oil palm seedlings. Soils used in the experiment were Typic Sulfaquepts and Sulfic Tropaquepts from Pulau Lumut Island, Malaysia. Best growth was observed on a non-jarositic freely drained topsoil. Oil palm seedlings were found the be moderately tolerant to soil acidity. Growth was only affected if Al³⁺ and Al_sum activities in the soil solutions were above 100 and 700 M, respectively. Root length was found to be one of the better parameters to predict crop growth, while others included plant height, fron length and LAI. Soil solution attributes which could be used as indices of soil acidity for oil palm growth were pH and activities of Al³⁺, AlSO₄ ⁺ and Al_sum.     

Association of cation and organic anion accumulation with iron chlorosis of Scots pine on prairie soils

Summary Iron chlorosis of 4 year old Scots pine (Pinus sylvestris L.) in comparison to areas of adjacent healthy growth on calcareous prairie soil, was associated with slight increases in the soluble ion content of the saturation paste extract. Such increases in soluble ions (mainly calcium sulphate) were associated with significant increases in ash, cation (including iron) and organic anion content of the chlorotic needles. Increasing levels of available soil nitrate were also related to increase in organic anions. Nitrogen and phosphorus assimilation was adversely affected under conditions of iron chlorosis. These observations support the theory of induced iron deficiency associated with elevated levels of organic anions or translocated cations and are applicable to plantings of conifers on prairie soils.     

Binding and direct electrochemistry of OmcA, an outer-membrane cytochrome from an iron reducing bacterium, with oxide electrodes: A candidate biofuel cell system

Dissimilatory iron-reducing bacteria transfer electrons to solid ferric respiratory electron acceptors. Outer-membrane cytochromes expressed by these organisms are of interest in both microbial fuel cells and biofuel cells. We use optical waveguide lightmode spectroscopy (OWLS) to show that OmcA, an 85 kDa decaheme outer-membrane c-type cytochrome from Shewanella oneidensis MR-1, adsorbs to isostructural Al₂O₃ and Fe₂O₃ in similar amounts. Adsorption is ionic-strength and pH dependent (peak adsorption at pH 6.5-7.0). The thickness of the OmcA layer on Al₂O₃ at pH 7.0 [5.8 ± 1.1 (2σ) nm] from OWLS is similar, within error, to that observed using atomic force microscopy (4.8 ± 2 nm). The highest adsorption density observed was 334 ng cm⁻² (2.4 × 10¹² molecules cm⁻²), corresponding to a monolayer of 9.9 nm diameter spheres or submonolayer coverage by smaller molecules. Direct electrochemistry of OmcA on Fe₂O₃ electrodes was observed using cyclic voltammetry, with cathodic peak potentials of −380 to −320 mV versus Ag/AgCl. Variations in the cathodic peak positions are speculatively attributed to redox-linked conformation change or changes in molecular orientation. OmcA can exchange electrons with ITO electrodes at higher current densities than with Fe₂O₃. Overall, OmcA can bind to and exchange electrons with several oxides, and thus its utility in fuel cells is not restricted to Fe₂O₃.     

Association with pedogenic iron and aluminum: effects on soil organic carbon storage and stability in four temperate forest soils

Soil organic carbon (SOC) can be stabilized via association with iron (Fe) and aluminum (Al) minerals. Fe and Al can be strong predictors of SOC storage and turnover in soils with relatively high extractable metals content and moderately acidic to circumneutral pH. Here we test whether pedogenic Fe and Al influence SOC content and turnover in soils with low Fe and Al content and acidic pH. In soils from four sites spanning three soil orders, we quantified the amount of Fe and Al in operationally-defined poorly crystalline and organically-complexed phases using selective chemical dissolution applied to the soil fraction containing mineral-associated carbon. We evaluated the correlations of Fe and Al concentrations, mean annual precipitation (MAP), mean annual temperature (MAT), and pH with SOC content and ¹⁴C-based turnover times. We found that poorly crystalline Fe and Al content predicted SOC turnover times (p < 0.0001) consistent with findings of previous studies, while organically-complexed Fe and Al content was a better predictor of SOC concentration (p < 0.0001). Greater site-level MAP (p < 0.0001) and colder site-level MAT (p < 0.0001) were correlated with longer SOC turnover times but were not correlated with SOC content. Our results suggest that poorly crystalline Fe and Al effectively slow the turnover of SOC in these acidic soils, even when their combined content in the soil is less than 2% by mass. However, in the strongly acidic Spodosol, organo-metal complexes tended to be less stable resulting in a more actively cycling mineral-associated SOC pool.     

Effect of desferrioxamine, rhodotorulic acid and cholylhydroxamic acid on transferrin and iron exchange with hepatocytes in culture

The mechanism of action of the hydroxamate iron chelators desferrioxamine (DFO), rhodotorulic acid (RHA) and cholylhydroxamic acid (CHA) was studied using rat hepatocytes in culture. Each chelator affected both the uptake and, to a much smaller extent, the release of transferrin-125I-59Fe from the cells. All chelators reduced the 59Fe uptake and incorporation into ferritin in a concentration-dependent manner. Uptake of 59Fe into the membrane (stromal-mitochondrial) fraction was also decreased by DFO and RHA but increased by CHA. Transferrin-125I binding was reduced slightly by DFO and RHA and increased by CHA. All chelators released 59Fe transferrin-125I from hepatocytes prelabelled by incubation with rat transferrin-125I-59Fe and washed before reincubation in the presence of the chelators. DFO decreased membrane 59Fe but had little effect on ferritin-59Fe. RHA decreased 59Fe in both membrane and ferritin fractions. CHA decreased hepatocyte-59Fe but increased 59Fe in the hepatocyte membrane fraction. Higher concentrations of the chelators had little further effect on 59Fe release but promoted transferrin-125I release from hepatocytes. All chelators appeared to act on kinetically important iron pools of limited size and hence are likely to be most effective when given by continuous infusion rather than bolus injection.     

Surface modification of iron oxide nanoparticles with polyarginine as a highly positively charged magnetic nano-adsorbent for fast and effective recovery of acid proteins

Polyarginine has been successfully bound onto iron oxide nanoparticles via carbodiimide activation as a highly positively charged magnetic nano-adsorbent for protein separation. They were nearly superparamagnetic with a mean diameter of 10.3 ± 2.36 nm, and the binding process did not change the spinel structure of iron oxide. From the analyses of FTIR spectra and zeta potential, the binding of polyarginine on the surface of iron oxide was confirmed and the resultant polyarginine-coated magnetic nanoparticles (PA-MNPs) were positively charged even up to pH 11. By thermogravimetric analysis, the typical product contained about 7.1 wt% of polyarginine. From the adsorption of the proteins with different pI values, the resultant PA-MNPs were found to be quite efficient for the fast and effective adsorption of acid proteins. For the typical acid protein, bovine serum albumin (BSA), the adsorption equilibrium was achieved within few minutes and obeyed the Langmuir isotherm equation. At pH 7 and 25 °C, the maximum adsorption capacity and equilibrium constant were 67.6 mg/g and 0.0623 L/mg, respectively. Moreover, by SDS–polyacrylamide gel electrophoresis, the capability of PA-MNPs for the separation of BSA-lysozyme mixture and egg white was further confirmed. Accordingly, the PA-MNPs were useful for the fast and effective magnetic recovery of acid proteins.     

Restoration of a deciduous woodland in Western Norway formerly used for fodder production: effects on tree canopy and field layer

The rich deciduous woodland at Loi, Luster, Inner Sogn, 61° 20 N., was traditionally used for fodder production from both tree and field layer. After more than nearly 40 years of disuse and secondary forest succession, experimental efforts were made to restore the traditional agricultural meadow woodland. Following a detailed preliminary registration of the vegetation the following measures were taken:

The apoptotic inducible effects of salicylic acid on hepatoma cell line: relationship with nitric oxide signaling

Clinical and experimental data suggest that salicylic acid (SA) is tumor preventive and NO has a multitude of effects on tumor biology. Therefore, firstly, the aim of our study is to explore the important role of SA in apoptotic induction of liver cancer cells. Secondly, we investigate whether SA mediates the anti-tumor effects by NO signaling pathway. The liver cancer cell line was treated with different concentrations of SA. Cell proliferation was tested using MTS assay and cell apoptosis was assessed by flow cytometry. NO content and NOS activities were measured by biochemical assay. The anti- or pro-apoptotic regulator gene expressions were analyzed by real-time PCR. Our data illustrated that high concentration of SA significantly inhibited liver cancer cell proliferation accompanied by apoptosis induction. In addition, SA led to the release of NO and the increase of NOS activities in above process. Importantly, SA up-regulated a series of apoptosis-related gene expression and reduced the mRNA level of HMGB1. Meanwhile, we also found that NOS inhibitor L-NAME and NO scavenger cPTIO attenuated the above SA-induced effects. Thus, we provided the evidence that SA exerted anti-tumor effects in liver cancer cell in part mediated by the NO pathway.     

Intracellular free iron in liver tissue and liver homogenate: studies with electron paramagnetic resonance on the formation of paramagnetic complexes with desferal and nitric oxide.

Treatment of intact liver and liver homogenate with sodium nitrite, or desferal, brings about the appearance of g = 2.03 and g = 4.3 electron paramagnetic resonance spectroscopy (EPR) signals, respectively. The g = 2.03 signal is conditioned by the formation of dinitrosyl complexes of Fe(II); the g = 4.3 signal is related to the appearance of paramagnetic desferal-Fe(III) complexes. Desferal and sodium nitrite were administered successively into liver homogenate, resulting in only a g = 4.3 EPR signal. And, vice versa, if desferal was administered after sodium nitrite, there appeared only the signal with g = 2.03. These data testify to the fact that one and the same endogenous free iron is included in both paramagnetic centers. The concentration of iron ions was measured in intact tissue according to the formation of dinitrosyl-iron complexes and desferal-iron complexes. It was 33.2 +/- 4.6 and 20.3 +/- 4.0 nmol/g of tissue weight, respectively. The data obtained testify to the fact that free endogenous iron is present in intact tissue. Possibilities of the EPR method for estimation of the content of intracellular free iron are discussed.     

Consequences of liming and gypsum top-dressing on nitrogen and carbon dynamics in acid forest soils with different humus forms

The aim of this study was to understand the effects of lime and gypsum on nitrogen and carbon turnover of the soil. A pot experiment was conducted in parallel with a field experiment which was set up in 1989 in a declining forest of the French Ardennes. A dystric cambisol, associated with a moder and mull humus separately, was used to study changes in the soil chemistry as a result of added lime and gypsum top-dressing.The lime was applied to the surface of an acid mull humus of an oak (Quercus petraea) stand and of a moder humus of a spruce (Picea abies) stand. A quantity of 2.8 t ha^-1 equivalent CaO was supplied as CaCO₃, CaCO₃+MgO and CaSO₄.2H₂O. The experiment was installed in an open-air nursery for 20 months, during which the organic carbon and nitrogen in the solution were analysed monthly. They were analysed in the solid phase after 20 months. At the end of this period the changes in the soil and leachate depended mainly on the type of the material added.The leachate was enriched with nitrogen from the third month of the experiment under lime treatments and in the control. The same pattern was found under the two humus types but the magnitude was higher in soil with a mull humus. The nitrogen was mostly leached as NO₃ ^--N in the carbonate treatments and in the control, whereas it was predominantly NH₄ ⁺-N under gypsum. The NO₃ ^--N was 50% higher than NH₄ ⁺-N in the control and CaCO₃, CaCO₃+MgO treatments. In the CaSO₄ treatment this phenomenon was reversed. The leaching of organic carbon was greater under gypsum than under the other treatments whatever the humus.In the solid phase of the soil (organic layers) the organic carbon and nitrogen concentration decreased significantly after liming, especially in the mull humus. Consequently it induced a decrease in C:N ratio of about 18% with respect to the control.     

Color transformation and fluorescence of Prussian blue-positive cells: implications for histologic verification of cells labeled with superparamagnetic iron oxide nanoparticles

Superparamagnetic iron oxide (SPIO) nanoparticles, either modified or in combination with other macromolecules, are being used for magnetic labeling of stem cells and other cells to monitor cell trafficking by magnetic resonance imaging (MRI) in experimental models. The correlation of histology to MRI depends on the ability to detect SPIO-labeled cells using Prussian blue (PB) stain and fluorescent tags to cell surface markers. Exposure of PB-positive sections to ultraviolet light at a wavelength of 365 nm commonly used fluorescence microscopy can result in color transformation of PB-positive material from blue to brown. Although the PB color transformation is primarily an artifact that may occur during fluorescence microscopy, the transformation can be manipulated using imaging process software for the detection of low levels of iron labeled cells in tissues samples.