Field measurements on the exchange of carbonyl sulfide between lichens and the atmosphere

The exchange of carbonyl sulfide (COS) between lichens and the atmosphere was investigated under natural field conditions. Using dynamic enclosures flushed with ambient air, we demonstrate that lichens act as a major sink for atmospheric COS in the investigated ecosystem. Diel courses of the exchange are shown in an open oak woodland ecosystem at a rural site in central California. The measurements were distributed over a variety of weather conditions during the dry (May/June) and the wet season (Nov/Dec). The physiological parameters (CO2 exchange and thallus hydration status) plus environmental variables (temperature, irradiance, atmospheric humidity and ambient COS mixing ratio) were recorded. Lichens are capable of continuous uptake of COS in the dark as well as in the light, depending mainly on their moisture status. Results indicate that the uptake is additionally dependent on temperature and COS ambient mixing ratio. Enzyme inactivation by high temperature denaturation demonstrate that the uptake is under physiological control. Light and thus photosynthetic activity do not have a direct influence on the uptake rate. Under these field investigations the COS uptake on a dry weight basis ranged between 0.015 and 0.071 pmol g−1 s−1. On a thallus surface area basis the sink strength is comparable to the uptake by higher vegetation.