Cave selection and use by swarming bat species

Caves are an important resource to a large proportion of temperate bat species, primarily as mating and hibernation sites. However, information on bat use exists for only a small fraction of caves in many parts of the temperate world, in part because current survey methods are inappropriate for many species. We surveyed the UK’s largest karst landscape, the Yorkshire Dales, by monitoring autumn swarming (mating) activity at 53 caves using automated echolocation call loggers, followed by trapping. Over 60% of caves surveyed were used by bats, but there was considerable variation in activity. Swarming activity was positively correlated with chamber development and negatively correlated with the amount of water the cave carried: together these two predictors explained 45% of the variance. Entrance orientation and shelter explained a further 10%. Activity was not correlated with entrance size, altitude or connectivity to the nearest summer habitat. All five resident swarming species were caught at most sites: Myotis brandtii, Myotis daubentonii, Myotis mystacinus, Myotis nattereri and Plecotus auritus. Behaviour, species composition and sex and age ratios were typical of swarming reported in other studies. Bat populations and catchment sizes were large and despite the proximity of other suitable caves, bats showed high fidelity to single sites. Our results show that the national importance of these caves has been overlooked. We suggest that survey for swarming activity is a quick and effective method of identifying underground bat sites and is likely to uncover many previously unknown and important sites throughout the temperate world.     

Re-examining the glomalin-purity of glomalin-related soil protein fractions through immunochemical,lectin-affinity and soil labelling experiments

Due to analytical similarities with the mycorrhizal glycoprotein glomalin, ubiquitous citrate and heat-extractable soil protein fractions have been assumed to be predominantly glomalin-stabilised within soil. Often termed glomalin-related soil protein (GRSP), little however is actually known of the “glomalin-purity” of these soil fractions. We undertook western and lectin blots and crossed immuno/lectin affinity electrophoresis (CIE/CLAE) analysis of “easily extractible” GRSP fractions, as well as liquid chromatography-tandem mass spectrometry (LC–MS/MS) of “total” GRSP fractions. To further test whether soil saprobes contribute to GRSP production, we amended soil with ¹⁴C-sucrose and examined whether ¹⁴C could be traced in the GRSP pool over a 500-day incubation period.While only four of six bands on SDS–PAGE profiles of easily extracted GRSP reacted with anti-glomalin MAb32B11 and the lectin Con A under our blotting conditions, CIE/CLAE indicated the presence of a single protein moiety in the easily extractible GRSP pool. LC–MS/MS analysis of total GRSP pooled from various soils also showed that although traces of protein tentatively assignable to soil bacteria were present in GRSP, their concentrations were low. Additionally, specific activity of total GRSP in ¹⁴C-labelled soil was relatively depleted compared to the bulk soil and soil microbial biomass. This suggests that little GRSP of heterotrophic origin was laid down over the incubation period, although the potential presence of a pre-existing ¹⁴C-free GRSP background, as well as of low microbial dynamics in the absence of any further substrate inputs to the soil warrant caution with this inference.     

Genetic and environmental impact on iron, zinc, and phytate in food sorghum grown in Benin

Seventy-six farmers' varieties of sorghum from Benin were distinguished by amplified fragment length polymorphism (AFLP) and clustered into 45 distinct genotypes. The genotype clusters were evaluated for their Fe, Zn, and phytate concentrations to assess the impact of genetic and environmental effects on the composition of the grains and to identify farmers' varieties with high potential Fe and Zn availability. The Fe concentration of the grains ranged from 30 to 113 mg/kg with an average of 58 mg/kg. The Zn concentration ranged from 11 to 44 mg/kg with an average of 25 mg/kg. The phytate concentration of the grain ranged from 0.4 to 3.5% with a mean of 1.2%. The grain-Fe and grain-Zn did not show consistent linkage to genetic variation, but varied significantly across field locations, suggesting a predominant environmental impact. The phytate concentration of the grains appeared to be environmentally as well as genetically determined. No varieties provide adequate Zn to meet nutritional requirements of sorghum consumers. The most promising varieties for Fe supply were tokogbessenou, mahi swan, biodahu, sa? ma?, mare dobi, sakarabokuru, and chabicouma, as they showed a [phytate]/[Fe] ratio of <14, which is the critical value above which Fe availability is strongly impaired. These varieties could therefore be recommended for the preparation of food products such as dibou, in which processing methods have only a slight diminishing effect on phytate levels. Further research is needed to test these varieties for the stability of [phytate]/[Fe] molar ratio across various environmental conditions.