Human Influence on the Atmospheric Vertical Temperature Structure: Detection and Observations

Recent work suggests a discernible human influence on climate. This finding is supported, with less restrictive assumptions than those used in earlier studies, by a 1961 through 1995 data set of radiosonde observations and by ensembles of coupled atmosphere-ocean simulations forced with changes in greenhouse gases, tropospheric sulfate aerosols, and stratospheric ozone. On balance, agreement between the simulations and observations is best for a combination of greenhouse gas, aerosol, and ozone forcing. The uncertainties remaining are due to imperfect knowledge of radiative forcing, natural climate variability, and errors in observations and model response.     

Mammalian ribosomal protein: analysis by electrophoresis on polyacrylamide gel

Ribosomal protein from five mammalian tissues when analyzed by discontinuous electrophoresis on polyacrylamide gel at pH 4.5 yielded 24 bands. Densitometric tracings indicated that the patterns of the basic ribosomal proteins from the several tissues were qualitatively similar. Protein from Escherichia coli ribosomes analyzed at pH 4.5 gave 29 bands, and the pattern was different from that of mammalian ribosomal protein. No distinct band was found when mammalian ribosomal protein was analyzed at pH 8.3 (acidic proteins). Ribosomal protein from Escherichia coli gave eight bands at pH 8.3. Thus, the structure of the genes responsible for synthesis of ribosomal protein in several mammalian tissues is the same, and different genes direct synthesis of ribosomal protein in bacteria.     

Effects of Hydrogen Peroxide (H2O2) on Fresh and Cryopreserved Buffalo Sperm Functions During Incubation at 37°C In Vitro

The magnitude of damage to buffalo spermatozoa during incubation with different levels of H₂O₂ was assessed. A total number of 24 ejaculates from four Murrah buffalo bulls were analysed in the study. Each ejaculate was split into two parts (part I and II). Part I was extended in Tris–egg yolk–citrate extender (20% egg yolk:7% glycerol), equilibrated (4 h at 5°C) and cryopreserved in 0.5‐ml French straws and stored in liquid nitrogen. The other part was utilized for fresh semen studies. The sperm in fresh, equilibrated and frozen–thawed semen was separated by centrifugation (1500 g ; 15 min) and were washed with sperm TALP. The sperm cells were re‐suspended in incubation TALP at the rate of 10⁸ sperm cells per millilitre and incubated with 0, 10, 25, and 50 μm H₂O₂ per ml at 37°C. Sperm motility, viability and intact acrosome percentages were assessed at 15‐min intervals up to 60 min of incubation. Lipid peroxidation levels of sperm were assessed at 0 and 60 min of incubation. The results of the experiment revealed that sperm motility decreased drastically during incubation with H₂O₂. Among the different levels of H₂O₂, the 50‐μm H₂O₂‐incorporated group had significantly (p < 0.05) higher malonaldehyde (MDA) level than the other groups. In the 50‐μm H₂O₂‐incorporated group, the MDA levels in fresh, equilibrated and frozen–thawed semen after incubation for 60 min were 961.6 ± 12.7, 991.8 ± 10.3 and 1234.9 ± 9.6 nm per 10⁹ spermatozoa respectively. An inverse relationship was observed between sperm motility, viability, intact acrosome percentages and concentration of H₂O₂ and duration of incubation. The decrease in sperm functions with duration of incubation and concentration of H₂O₂ was significantly (p < 0.05) higher in frozen–thawed than fresh and equilibrated spermatozoa.     

Tetravalent uranium in calcite

X-ray absorption spectroscopy and x-ray fluorescence microprobe studies of 35-million-year-old calcite from a Mississippi Valley-type zinc ore deposit indicate substitution of tetravalent uranium for divalent calcium. Thus, tetravalent uranium has a stable location in calcite deposited under reducing conditions. This result validates uranium-series dating methods (including uranium/lead dating) for ancient calcite and shows that calcite provides a sink for uranium in deep groundwater aquifers and anoxic lacustrine and marine basins.