Metabolic adaptations of mullet Rhinomugil corsula (Hamilton) with special reference to energy utilization

While the respiratory quotient (R.Q.) of Rhinomugil corsula in air-saturated water remains near unity at all levels of random activity, the ammonia quotient (A.Q. = volume or mole: mole relation of ammonia excreted to oxygen consumed) is higher at lower levels of activity, indicating relatively higher protein utilization in less active fish. The mean routine R.Q. values of R. corsula in air-saturated water at temperatures of 30 and 35°C are 0.91 and 0.95 respectively. Assuming that the major sources of ammonia excreted are certain predominant free amino acids, an estimate of caloric break-up of routine meta-bolism of R. corsula suggests that the fish is completely aerobic in air-saturated water and that it derives 14, 44 and 42% of energy from proteins, carbohydrates and fats respectively from a total of 567 cal/kg fish/h at 30°C (15, 55 and 30% at 35°C). At oxygen concentrations below air saturation, R.Q. and A.Q. values of R. corsula increase with decrease in ambient oxygen indicating an increase in anaerobic metabolism and protein utilization. The correlation between the trends of R.Q. and A.Q. levels are similar to that observed earlier in Tilapia mossambica. During hypoxia (1.6 mg O₂/l at 30°C) R. corsula derives about half its energy for sustenance and activity anaerobically. The mullet does not appear to accumulate an oxygen debt during hypoxia.     

Threatened deer of the world: Research programmes for conservation

This paper is the sequel to an earlier publication (see Biological Conservation, Vol. 5, No. 4 pp. 243–250, October 1973) on the conservation status of deer and describes an IUCN programme for the conservation of world-threatened deer. Research requirements for conservation of deer that are currently threatened with extinction are discussed. The immediate conservation objective is to ensure the species' or subspecies' survival, and the long-term objective is to restore their productive status in the wild. A framework for research to provide data to guide conservation practices is outlined. It comprises a set of research questions, to aid the planning of studies, and statements of the conservation action potential of the results of these investigations. The proposed organization of the IUCN programme and its current status is described. University and other research institutions that would be interested in participating or co-operating in the programme are invited to write to IUCN.     

Burial of vegetation by erosion debris near ski lifts on Cairngorm,Scotland

The extent of accelerated erosion from ground damaged near ski lifts was found to have reached a peak in about 1969, with a marked decline since then. This decline was attributable to reseeding of damaged ground, provision of drains and grading of dirt roads. Burial experiments showed that where erosion debris had covered vegetation, recovery at best took several years, and with depths above about 7 cm, was almost negligible.     

The relative-intensity method of x-ray fluorescence analysis and its application to soils and rocks

The relative-intensity X-ray fluorescence method of analysis of rock and soil samples has been investigated and compared with the net-intensity method. Strong, coherently scattered radiation originating from the X-ray tube is shown to be preferable to background radiation as an internal standard, and scattered radiation measured at one wavelength can usefully be applied in the determination of several elements. When the concentrations of an element in two soil samples of different composition (for example concretions and the soil adjacent to them) are compared, the ratio of the relative intensities may be different from the ratio of net intensities by a factor of about two. The concentrations of manganese in thirteen standard rock samples determined by the relative-intensity method are within or very close to the ranges of values reported previously.     

Thermal decomposition of protein in soil organic matter

Infrared spectroscopy and nitrogen analyses suggest that secondary amide groups in protein-like components of soil clay-organic complexes and extracted organic matter decompose above 100°C to yield ammonia which is retained as NH₄⁺ by acid-washed clay-organic complexes. Above about 400°C, other volatile nitrogenous decomposition products are released. Clay surfaces in the clay-organic complexes may catalyse the decomposition.