Niedrige Ei- und Körpertemperatur („Hypothermie“) bei brütenden Gelbschnabelsturmtauchern (Calonectris diomedea)
Body and egg temperatures of Cory's Shearwater were recorded in an Aegean colony. Body temperatures of breeding birds were 2 ° C lower than those of non-breeding, resting adults and accounted for 36.7±0.41 ° C in ♂ and 37.6±0.59 ° C in ♀. Incubation temperature, determined telemetrically inside incubated eggs, was 29.6±0.6° C.
Body Temperatures of Petrels
During the course of a study of the development rates of albatrosses, shearwaters, and other petrels (Warham MS), the existing data on body temperatures of birds in the order Procellariiformes were examined. These suggested that petrels have unusually low body temperatures and that these might provide clues to the birds' unusually long incubation and nestling periods. Subsequently it became possible to extend the data to cover a much wider range of species during visits to the Campbell, Antipodes, and Snares Islands, south of New Zealand. Figures for 31 species are now available.
Soil organic matter and microbiological development of technosols in the South Wales Coalfield
Abstract Degraded land (formerly ‘reclaimed’) after surface-coal-mining is a serious problem in South Wales. This project uses forestation to foster soil development on opencast coal-mine spoil technosols. It compares records of humification and the soil microbiological system (microcoenosis) using paired data from the same plantings in 1998 and 2018. Statistical analysis finds no significant difference between samples collected under trees planted by the pit-planting versus trench planting method or trees planted using organic or mineral fertilizer. However, there are strong significant differences in both soil organic matter and microflora components and significant correlations with time since tree planting. Most components of the soil organic carbon (TOC) and the microflora increase, often significantly. However, compared to 2018, 1998 samples contain significantly greater maximum levels of Insoluble Carbon while the microflora had significantly more Ammonifying bacteria. Decreases in Insoluble Carbon explain the relatively small increase in TOC between 1998 and 2018. The % extracted with 0.1 N H2SO4 is significantly larger in 2018, suggesting active weathering. Similarly, both the maxima and minima of total Humic and Fulvic acids content, extracted with 0.1 M Na4P2O7 + 0.1 M NaOH, are significantly greater in 2018. Total microflora shows significant positive correlations with time-since-tree-planting as do the proportions of bacilli and actinomycetes but the correlation with ammonifying bacteria is negative. In 1998, the microflora was dominated by non-spore-forming bacteria while, in 2018, bacilli and actinomycetes prevail; both are involved in the transformation of complex organic compounds and humification. This indicates active transformation of more complex organic compounds and advancing humification. In sum, forestation of these degraded, formerly reclaimed, opencast coal-mine spoils has resulted in a massive increase in both the size and functioning of the soil organic system.