The multi-element content of the lichen Parmelia sulcata, soil, and oak bark in relation to acidification and climate.

Understanding how biodiversity is influenced by changing atmospheric conditions is important for conservation, public policy and environmental health. In a recent study, an impact on two of the most abundant lichens in Europe (Parmelia sulcata and Hypogymnia physodes) was recorded at Burnham Beeches lying 40 km west of London (UK) during unusual atmospheric conditions whilst other species remained unaffected. Bark and soil chemistry also influence lichen vitality and community composition. Correlations between element concentrations and element ratios in different samples help understand element cycling. To study this further, the multi-element content of the lichen P. sulcata and bark sampled in 2000 from 16 oak (Quercus robur) trees at Burnham Beeches was compared with the same elements determined in 24 surface soils sampled in 2005 from beneath the same trees. Soil pH ranged from 4.1 to 6.7. Highly significant correlations (p<0.001) for Mn/Ca ratios in lichen versus bark, soil versus bark and soil versus lichen samples confirmed cycling via the soil-tree-lichen system. Similar Mn/Ca ratios were reported in coniferous forests where high Mn concentrations were shown to limit epiphytic lichen abundance. Soil acidification influences element bioavailability and bark chemistry in Burnham Beeches with implications for lichen diversity and health. Recovery was recorded in P. sulcata, including regeneration within monitoring quadrats. Biological systems are well known to be influenced by pollution episodes.

Biogeochemical signatures in the lichen Hypogymnia physodes in the mid Urals.

Multi-element content and uranium (U) isotopes were investigated in the lichen Hypogymnia physodes (native and transplants) sampled across a 60-km transect, centred on Karabash smelter town, from Turgoyak Lake (SW) to Kyshtym (NE) to investigate the origin of U. Kyshtym was the site of a major nuclear accident in 1957. (234)U/(238)U activity ratios in native thalli sampled during July 2001 were within the natural isotopic ratio in minerals. Uranium/thorium (U/Th) ratios were higher in native thalli towards the NE (average 0.73) than those in the SW (average 0.57). Element signatures in native thalli and transplants suggest U was derived from fossil fuel combustion from Karabash and sources lying further to the east. Systematic and significant U enrichment indicative of a nuclear fuel cycle source was not detected in any sample. Element signatures in epiphytic lichen transplants and native thalli provide a powerful method to evaluate U deposition.

Biomonitoring using the lichen Hypogymnia physodes and bark samples near Zlatna, Romania immediately following closure of a copper ore-processing plant.

Lichen transplants were established along a 40km transect centred on a large mine waste dump close to Zlatna town centre, two weeks after closure of a major industrial source, to compare spatial patterns of element concentrations in lichen and bark samples. After 3 months of exposure, spatial patterns of 4 element concentrations (Pb, Cu, Zn and Fe) in transplants confirmed deposition due to a point source 'Zlatna influence'. Cu and Pb reached concentrations 8 and 4 times, respectively, higher than samples transplanted in the 'background' site, and over 200 (Cu) and 2000 (Pb) times higher relative to 'background' bark. Ten out of 15 elements analysed reached highest concentrations in bark. Spatial patterns confirmed long-term pollution for 6 elements (Pb, S, Fe, Cu, Zn and Ba). The study provides a model baseline to monitor recovery following closure of major industrial sources and highlights the importance of considering biogeochemical processes when interpreting metal concentrations.