Trade-off between road avoidance and attraction by roadside salt pools in moose: An agent-based model to assess measures for reducing moose-vehicle collisions

Moose-vehicle collisions are a frequent traffic-safety issue, particularly in northern regions where moose are attracted to the near-road areas because they can consume sodium from de-icing salts that accumulate in pools at snowmelt. Moose that find salt pools near roads tend to remember their location and to re-visit them to get the sodium they need in their diet. This study investigated the trade-off between road avoidance and salt pool spatial memory in the movement behaviour of moose using an agent-based model to determine how the interplay of these two factors influences the frequency of road crossings in the Laurentides Wildlife Reserve (Québec, Canada). Mitigation measures studied were the removal of roadside salt pools and the construction of compensatory salt pools away from the road shoulder. A GPS telemetry program of moose in the study area was used to validate our model. The model moose with both road avoidance and salt pool spatial memory activated produced the best results when comparing to the real moose data. Results show that both road avoidance and salt pool spatial memory significantly affect moose road crossings, but that road avoidance explains most of the variance. Road avoidance tended to decrease the number of moose crossings, but this decrease was partly compensated by the spatial memory of salt pools which typically increased the likelihood that moose will cross the road. The trade-off between road avoidance and salt pool memory was largest when original salt pools were maintained. In simulations where road avoidance and salt pool memory were both turned off, the impact of mitigation measures on the number of road crossings was lowest. For the most realistic moose behavior, the management scenarios resulted in reductions in road crossings between 22% and 79%, and the best scenario is to completely remove roadside salt pools. If compensation salt pools are used, they should be located as far as possible from the roads (beyond 500 m) to have an impact on moose road crossings.     

Photoactive titanium dioxide nanoparticles modify heterotrophic microbial functioning

Environmental Science and Pollution Research - Nanoparticulate titanium dioxide (nTiO2) is frequently applied, raising concerns about potential side effects on the environment. While various...     

Herbicides: A new threat to the Great Barrier Reef

The runoff of pesticides (insecticides, herbicides and fungicides) from agricultural lands is a key concern for the health of the iconic Great Barrier Reef, Australia. Relatively low levels of herbicide residues can reduce the productivity of marine plants and corals. However, the risk of these residues to Great Barrier Reef ecosystems has been poorly quantified due to a lack of large-scale datasets. Here we present results of a study tracing pesticide residues from rivers and creeks in three catchment regions to the adjacent marine environment. Several pesticides (mainly herbicides) were detected in both freshwater and coastal marine waters and were attributed to specific land uses in the catchment. Elevated herbicide concentrations were particularly associated with sugar cane cultivation in the adjacent catchment. We demonstrate that herbicides reach the Great Barrier Reef lagoon and may disturb sensitive marine ecosystems already affected by other pressures such as climate change.     

Inputs of nutrients and fecal bacteria to freshwaters from irrigated agriculture: case studies in Australia and New Zealand

Increasing demand for global food production is leading to greater use of irrigation to supplement rainfall and enable more intensive use of land. Minimizing adverse impacts of this intensification on surface water and groundwater resources is of critical importance for the achievement of sustainable land use. In this paper we examine the linkages between irrigation runoff and resulting changes in quality of receiving surface waters and groundwaters in Australia and New Zealand. Case studies are used to illustrate impacts under different irrigation techniques (notably flood and sprinkler systems) and land uses, particularly where irrigation has led to intensification of land use. For flood irrigation, changes in surface water contaminant concentrations are directly influenced by the amount of runoff, and the intensity and kind of land use. Mitigation for flood irrigation is best achieved by optimizing irrigation efficiency. For sprinkler irrigation, leaching to groundwater is the main transport path for contaminants, notably nitrate. Mitigation measures for sprinkler irrigation should take into account irrigation efficiency and the proximity of intensive land uses to sensitive waters. Relating contaminant concentrations in receiving groundwaters to their dominant causes is often complicated by uncertainty about the subsurface flow paths and the possible pollutant sources, viz. drainage from irrigated land. This highlights the need for identification of the patterns and dynamics of surface and subsurface waters to identify such sources of contaminants and minimize their impacts on the receiving environments.     

Hysteresis in Reversal of Central European Mountain Lakes from Atmospheric Acidification

Extremely high emissions of S and N compounds in Central Europe (both 280 mmol m^-2 yr^-1) declined by 70and 35%, respectively, during the last decade. Decreaseddeposition rates of SO₄ ^-2, NO₃ ^-, and NH₄ ⁺ in the region paralleled emission declines. The reduction in atmospheric inputs of S and N to mountain ecosystemshas resulted in a pronounced reversal of acidification in the Tatra Mountains and Bohemian Forest lakes. Between the 1987–1990and 1997–1999 periods, concentrations of SO₄ ^-2 and NO₃ ^- decreased (average ± standard deviation) by 22±7 and 12±7 mol L^-1, respectively, in theTatra Mountains, and by 19±7 and 15±10 mol L^-1, respectively, in the Bohemian Forest. Their decrease was compensated in part (1) by a decrease in Ca²⁺ + Mg²⁺ (17±7 mol L^-1) and H⁺ (4±6 mol L^-1), and an increase in HCO₃ ^-(10±10 mol L^-1) in the Tatra Mountains lakes, and (2) by a decrease in Al (7±4 mol L^-1), Ca²⁺ + Mg²⁺ (9±6 mol L^-1), and H⁺ (6±5 mol L^-1), in Bohemian Forest lakes. Despite the rapid decline in lake water concentrations of SO₄ ^-2 and NO₃ ^- in response to reduced S and N emissions, their present concentrations in some lakes are higher than predictionsbased on observed concentrations at comparable emission rates during development of acidification. This hysteresis in chemical reversal from acidification has delayed biological recovery of the lakes. The only unequivocal sign of biological recovery hasbeen observed in erné Lake (Bohemian Forest) where a cladoceran species Ceriodaphnia quadrangular has recentlyreached its pre-acidification abundance.     

The territorial flight of male houseflies (Fannia canicularis L.)

Summary The heart rate (HR) of three male and five female European blackbirds (Turdus merula) was monitored by radiotelemetry under three conditions: in a dark cage, in a lighted cage, and in an outdoor aviary. In all three, the response to recorded bird song was tested.The resting HR in the cage ranged from 4.8 to 6.3 beats per second. The HR of all the birds changed in response to playback of conspecific song as well as of the songs of other species. In 68% of trials a typical biphasic HR curve was obtained, with acceleration followed by deceleration (Fig. 2). The time from stimulus onset to the second curve inflection (t _iII) averaged 15–18 s; this was significantly longer for conspecific than for heterospecific song. The parameter t _iII was used as a basic measure of the response.The reaction of the males was longer-lasting than that of the females. The possibility that this reflects the territorial role of the songs is discussed. Response durations were longest in the dark cage, and shortest in the aviary. The reason is thought to be the gradation in total stimulus input available to the bird.The results suggest that the HR response consists of an unspecific component (acceleration) plus a component specific to bird sounds (deceleration). At this fundamental level of stimulus processing it is possible to study reactions to single strophes not only in males, as with more traditional methods, but also in females and young birds.     

Lethal fighting between honeybee queens and parasitic workers (<Emphasis Type="Italic">Apis mellifera</Emphasis>)

Pheromonal signals associated with queen and worker policing prevent worker reproduction and have been identified as important factors for establishing harmony in the honeybee (Apis mellifera) colony. However, "anarchic workers", which can evade both mechanisms, have been detected at low frequency in several honeybee populations. Worker bees of the Cape honeybee, Apis mellifera capensis, also show this anarchistic trait but to an extreme degree. They can develop into so called "pseudoqueens", which release a pheromonal bouquet very similar to that of queens. They prime and release very similar reactions in sterile workers to those of true queens (e.g. suppress ovary activation; release retinue behavior). Here we show in an experimental bioassay that lethal fights between these parasitic workers and the queen (similar to queen–queen fights) occur, resulting in the death of either queen or worker. Although it is usually the queen that attacks the parasitic workers and kills many of them, in a few cases the workers succeeded in killing the queen. If this also occurs in a parasitized colony where the queen encounters many parasitic workers, she may eventually be killed in one of the repeated fights she engages in.     

Mantle buffering of the early oceans

Archean calcites and dolomites, if compared to their Phanerozoic counterparts, are enriched in Sr²⁺, Ba²⁺, Mn²⁺, Fe²⁺, depleted in ¹⁸O, (Na⁺), and contain mantle-like ⁸⁷Sr/⁸⁶Sr and, in associated S phases, mantle-like ³⁴S/³²S. This may be a consequence of massive seawater pumping through, and equilibration with, the coeval basaltic oceanic crust. The exponential decline of oceanic geothermal gradient in the course of terrestrial evolution led to a waning of this “mantle” flux and to the enhancement of the continental river discharge as the controlling factor of seawater composition; the major transition occurring probably during the late Archean — early Proterozoic time interval. Such evolution is consistent with the observed tectonic, sedimentological, geochemical and metallogenic secular patterns and may also provide an alternative, or complementary, inorganic explanation for the development of the post-Archean oxygenic atmosphere.