An open-air system for exposing forest-canopy branches to ozone pollution

We developed a chamberless system to expose branches to elevated concentrations of ozone with little alteration of micro-meteorological conditions. In a 35-year-old stand of sugar maple (Acer saccharum Marsh.), scaffolding and a platform (14 m in height) provided access to 10 branches and ten paired controls within the canopy. Ozone was delivered to the canopy through a manifold and an array of loops (38 cm in diameter) of teflon tubing individually fitted to each branch. Ozone-enriched air was discharged through numerous small holes in each loop positioned beneath the exposed foliage. A sampling system controlled by a microcomputer monitored ozone concentrations for each loop by means of composite air samples from 12 leaves, drawn through small teflon tubes (1.65 mm diameter) attached to the petioles. On average, coefficients of variation for ozone concentrations for the sample points within each branch loop were less than 50%. Between 0900 and 1700 h for 68 d of exposure, the mean hourly ozone concentrations among the branches averaged 95nmol mol⁻¹ (±13SD), about twice the ambient mean. Frequency distributions of mean hourly concentrations during exposure were unimodal and approximately log-normal, comparable to ambient ozone concentrations. The open-air loop system enables exposure of branches to gaseous pollutants under relatively natural conditions.     

Rooting down the aphid's tree – the oldest record of the Aphidomorpha lineage from Palaeozoic (Insecta: Hemiptera)

The new genus and species Lutevanaphis permiana gen.n. et sp.n. , represents the oldest Aphidomorpha, new superfamily Lutevanaphidoidea superfam.n. and new family Lutevanaphididae. This taxon is described from the Middle Permian of the Lodève Basin, southern France. The presence of very small Aphidomorpha in the Middle Permian contradicts the hypothesis of the ‘Lilliput effect’ that is presumed to have affected the insect fauna during the Early to Middle Triassic, after the end‐Permian crisis. Very small insects were present well before the end of the Permian; their relative rarity is attributable probably to taphonomic biases.