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

Abstract

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.