Solar UV-B dosimetry in situ with ‘D-dosimeter’: effect of ozone depletion on the Vitamin D synthetic capacity of sunlight

Vitamin D synthesis under solar UV-B radiation (280–315 nm) occurs widely in nature being an inherent characteristic of mammals and plants. Current data suggest that pro-Vitamin D can act as an UV-B receptor in plants, and thus monitoring the Vitamin D synthetic capacity of sunlight should be the subject of UV-B dosimetry. With this aim ‘D-dosimeter’ based on an in vitro model of Vitamin D synthesis has been designed for direct monitoring the Vitamin D synthetic capacity of sunlight in situ. Besides, ‘D-dosimeter’ possesses spectral selectivity that is helpful for detecting mid-latitude UV-B trends which accuracy is hindered by variations of solar UV radiation by clouds and aerosols, that have a comparable effect on UV-B caused by variations in stratospheric ozone.     

Ecosystem UV-B experiments in terrestrial communities: a review of recent findings and methodologies

Ecosystem-level UV-B experiments have revealed a variety of responses in terrestrial communities. These include decreases in the growth of some plant species (usually small changes but occasionally >25%), both decreases and increases in herbivory, occasional altered decomposition patterns, changes in populations of fungi and invertebrates, and morphological changes in the growth patterns of mosses. These field experiments have been pursued both with solar UV-B exclusion using selective filters and with supplementation of UV-B using lamps. For UV-B-exclusion studies it is critical that the UV-B-excluding and UV-B-transmitting filters pass the same amount of photosynthetically active radiation (PAR, 400–700 nm) and also infrared. Canopy photosynthesis models indicate that even small differences in PAR transmittance can, under many circumstances, have significant effects on plant carbon gain. It is also important that filters in UV-B-exclusion studies allow precipitation to pass uniformly to the plots unless there is some form of irrigation underneath the filters. For UV-B-supplementation studies with lamps, many factors are involved in the realism of the ozone depletion simulation. We believe the major lamp-system error is excessive supplementation of UV-B by timer-controlled lamps when weather conditions (primarily clouds) decrease ambient solar UV-B irradiance. The choice of biological spectral weighting functions (BSWF) used in adjusting lamp flux is also critical in determining the level of ozone depletion simulated. In addition, shading by the lamp arrays influences plant growth and becomes particularly important when BSWF with substantial weighting in the UV-A are employed.     

Spatial patterns of variation in the composition and structure of nematode communities in relation to different microhabitats: a case study of Quercus dalechampii Ten. forest

Variability in the spatial distribution of nematode communities in relation to the structural heterogeneity of the environment was studied in nine different microhabitats within a relatively small area of a natural oak forest in Bulgaria. Maturity and diversity indices, trophic structure and the distribution of colonizer-persister groups were applied to analyze the quality of substrate and ecological processes involved from a functional point of view. Two main groups of nematode communities, below- and above-ground, were distinguished in terms of the location of the microhabitats. Our results indicated a higher percentage similarity between nematode communities inhabiting microhabitats with a higher resemblance in substrate structure, and abiotic and biotic conditions than between microhabitats with more dissimilar microenvironmental conditions. The application of Detrended Correspondence Analysis helped to reveal two ecological gradients. The first one was from microhabitats characterized by smaller fluctuations in microclimatic conditions and nutrient supply to microhabitats with more adverse abiotic conditions and dynamics of food resources. Along this gradient from below- to above-ground microhabitats, the proportion of general opportunists (cp 2 taxa) increased, whereas the diversity, MI and the proportions of persisters (cp (3-5) taxa), decreased. Along the second gradient a gradual decrease in the decomposition rate within above-ground microhabitats was revealed, which was indicated by the proportion of enrichment opportunists (cp 1 taxa). The nematode communities of decaying wood had the most specific cp groups' distribution characterized by a high proportion of enrichment opportunists (colonizers). Each microhabitat has developed nematode communities with a characteristic trophic structure that was related to the relative importance of primary production and decomposition processes occurring within the microhabitat. The nematode communities of mosses growing on soil, stones and tree trunks had similar trophic structure dominated by bacterial-feeding nematode taxa. Our results supported the role of nematode communities as potential indicators of environmental conditions.     

Response of microbial community composition and activity in agricultural and grassland soils after a simulated rainfall

Rainfall in Mediterranean climates may affect soil microbial processes and communities differently in agricultural vs. grassland soils. We explored the hypothesis that land use intensification decreases the resistance of microbial community composition and activity to perturbation. Soil carbon (C) and nitrogen (N) dynamics and microbial responses to a simulated Spring rainfall were measured in grassland and agricultural ecosystems. The California ecosystems consisted of two paired sets: annual vegetable crops and annual grassland in Salinas Valley, and perennial grass agriculture and native perennial grassland in Carmel Valley. Soil types of the respective ecosystem pairs were derived from granitic parent material and had sandy loam textures. Intact cores (30 cm deep) were collected in March 1999. After equilibration, dry soil cores (approx. −1 to −2 MPa) were exposed to a simulated Spring rainfall of 2.4 cm, and then were measured at 0, 6, 24, and 120 h after rewetting. Microbial biomass C (MBC) and inorganic N did not respond to rewetting. N₂O and CO₂ efflux and respiration increased after rewetting in all soils, with larger responses in the grassland than in the agricultural soils. Phospholipid fatty acid (PLFA) profiles indicated that changes in microbial community composition after rewetting were most pronounced in intensive vegetable production, followed by the relict perennial grassland. Changes in specific PLFA markers were not consistent across all sites. There were more similarities among microbial groups associated with PLFA markers in agricultural ecosystems than grassland ecosystems. Differences in responses of microbial communities may be related to the different plant species composition of the grasslands. Agricultural intensification appeared to decrease microbial diversity, as estimated from numbers of individual PLFA identified for each ecosystem, and reduce resistance to change in microbial community composition after rewetting. In the agricultural systems, reductions in both the measures of microbial diversity and the resistance of the microbial community composition to change after a perturbation were associated with lower ecosystem function, i.e. lower microbial responses to increased moisture availability.