Upside-down swimming behaviour of free-ranging narwhals

Background

Free-ranging narwhals (Monodon monoceros) were instrumented in Admiralty Inlet, Canada with both satellite tags to study migration and stock separation and short-term, high-resolution digital archival tags to explore diving and feeding behaviour. Three narwhals were equipped with an underwater camera pod (Crittercam), another individual was equipped with a digital archival tag (DTAG), and a fifth with both units during August 2003 and 2004.

Results

Crittercam footage indicated that of the combined 286 minutes of recordings, 12% of the time was spent along the bottom. When the bottom was visible in the camera footage, the narwhals were oriented upside-down 80% of the time (range: 61100%). The DTAG data (14.6 hours of recordings) revealed that during time spent below the surface, the two tagged narwhals were supine an average of 13% (range: 9–18%) of the time. Roughly 70% of this time spent in a supine posture occurred during the descent.

Conclusion

Possible reasons for this upside-down swimming behaviour are discussed. No preference for a clockwise or counter-clockwise direction of roll was observed, discounting the possibility that rolling movements contribute to the asymmetric left-handed helical turns of the tusk.     

Speciation of Heavy Metals in Road Runoff and Roadside Total Deposition

The concentrations of Cd, Co, Cu, Pb, W and Zn were measured in road runoff and total deposition at two Swedish field sites during one year. It was found that the concentrations of most elements increased significantly during the winter, up to one order of magnitude. For cobalt and tungsten, it was found that around 90% of the total mass transport occurred during the winter, whereas for Cu, Pb, Cd, Zn and Na, the corresponding figures were 70–90, 40–80, 60–90, 50–70 and ≥99% depending on site specific conditions. The deicing salts (rock salts) did not significantly contribute to the increase in trace element concentrations. Instead, the increased concentrations were due to more intense wearing of the pavement during the winter because of the use of studded tires in combination with the chemical effects caused by the use of deicing salts. New potential elemental markers for roads and traffic are suggested.     

Side Effects of Liming - A Study of Four Dimictic Lakes in Southern Norway

Side effects related to liming have been studied in four dimictic lakes (553–642 m?a.s.l.; 59°57′N) in Finnemarka, a forested area in Southern Norway with poor catchment buffer capacity. Data series from lake profiles have been sampled two decades apart; 10 years prior to liming and after 10 years of liming. Water samples were collected during spring after ice breakup and during summer after the development of thermal stratification. Before liming, there were very low concentrations of bicarbonate (HCO ₃ ^– ; or alkalinity) in the lakes. After 10 years of liming, up to 90% of the ions in hypolimnion originate from lime products. Hence, liming strengthened the chemical stratification and increased the vertical stability. Differences in chemocline developments between lakes were explained by differences in physical properties, i.e. their depth/surface area ratio. The chemocline developments lead to increased concentrations of organic matter in the hypolimnion with a subsequent reduction in oxygen concentrations. Lime additions during late spring, as an alternative to early autumn, lead to pronounced anoxic conditions in the hypolimnion.     

Variability of methane emissions from an old landfill over different time‐scales

Methane (CH₄) emission patterns were investigated at an old landfill in northern Germany during a 2‐year campaign over three different time‐scales (seasonal, daily and diurnal) using modified static chambers. Emissions were not uniformly distributed over the cover soil, but occurred through localized preferential pathways (hotspots). The range of emissions from the 14 investigated hotspots at any one measurement event was large, reflecting large spatial variability of emissions from the landfill. In addition, the individual hotspots showed a large temporal variability of emissions (0–9.7 mol CH₄ day^?1 over a range of 20 months). Environmental variables effectively modified either the biological process of methane oxidation in the soil (temperature) or the physical gas transport process (moisture and atmospheric pressure). During the seasonal campaign, emissions generally were greater in winter (moister and cooler) and smaller during the summer period (dryer and warmer). Under dry conditions, emissions were independent of soil moisture but correlated negatively with soil temperature. A positive correlation of emissions with moisture was found for moisture levels relating to a matric potential of ?30 to ?6 kPa, reflecting impeded diffusive oxygen ingress and hence reduced methanotrophic activity. Under very moist conditions, more than ?6 kPa, emissions were negatively correlated with moisture content because of decreased gas permeability in the soil. In addition, a pressure decrease preceding the measurement was at all time‐scales often related to large emissions, whereas constant or rising pressure prior to measurement resulted in small emissions. The particular importance of the different effects depends on the type of gas transport at the specific emission location and whether it is advective or diffusive gas transport or a mixture of both, and varies at the temporal scale both between and within locations.     

Modification of glutamine and lysine residues in holo and apo alpha-lactalbumin with microbial transglutaminase

The molecular structures determine the physical properties of milk proteins and are important for the texture of many dairy-based foods. Bovine alpha-lactalbumin (alpha-LA) is a globular 123 amino acid Ca(2+) binding milk protein. Modification with microbial Ca(2+) independent transglutaminase (MTGase) was used to modify lysines and glutamines in holo and apo alpha-LA. At 30 degrees C no lysines or glutamines are modified in holo alpha-LA, whereas in apo alpha-LA lysines 13, 16, 108, and 114, and glutamines 39 and 43, are modified. At 50 degrees C lysines 13, 16, 108, and 114, but no glutamines, are modified in holo alpha-LA, whereas in apo alpha-LA lysines 5, 13, 16, 108, and 114, and glutamines 39, 43, 54, 65, and 117, are modified. The methods presented here offer the possibility to manipulate the availabilities of residues in alpha-LA to the MTGase reaction and enable the preparation of alpha-LA species with different degrees of modification and hence with different physical properties.     

Changes in the profile of genistein, daidzein, and their conjugates during thermal processing of tofu.

Profiles of genistein, daidzein, genistin, daidzin, and their acetyl- and malonyl-beta-glycosides were determined in tofu as affected by temperature and time. Tofu was heated in water at 80, 90, and 100 degrees C for 0 (control), 10, 20, 30, and 40 min, and the contents of the isoflavones of interest were quantified using reversed-phase HPLC. Total isoflavone content decreased most likely due to leaching of isoflavones into the water. Because the content of the isoflavones of the genistein series was little affected by the treatments, the decrease in the total isoflavone content was almost exclusively due to a decrease of the daidzein series. Changes in the profile of the daidzein series suggest little decarboxylation of the malonylglycoside to the acetylglycoside, but considerable de-esterification of the malonyl- and acetylglycoside to the beta-glucoside. Strongly temperature dependent decreases of the aglycon suggest possible thermal degradation of daidzein in addition to losses due to leaching.     

Porphyrin-sensitized solar cells with cobalt (II/III)-based redox electrolyte exceed 12 percent efficiency

The iodide/triiodide redox shuttle has limited the efficiencies accessible in dye-sensitized solar cells. Here, we report mesoscopic solar cells that incorporate a Co((II/III))tris(bipyridyl)-based redox electrolyte in conjunction with a custom synthesized donor-π-bridge-acceptor zinc porphyrin dye as sensitizer (designated YD2-o-C8). The specific molecular design of YD2-o-C8 greatly retards the rate of interfacial back electron transfer from the conduction band of the nanocrystalline titanium dioxide film to the oxidized cobalt mediator, which enables attainment of strikingly high photovoltages approaching 1 volt. Because the YD2-o-C8 porphyrin harvests sunlight across the visible spectrum, large photocurrents are generated. Cosensitization of YD2-o-C8 with another organic dye further enhances the performance of the device, leading to a measured power conversion efficiency of 12.3% under simulated air mass 1.5 global sunlight.