Projet Innovation du Geotop
Volcanoes are a major hazard to vulnerable communities and fragile ecosystems but understanding their behaviour can be difficult. The behaviour and hazards of a particular volcano can sometimes be forecast based on its eruptive history. However, recorded volcanic histories are typically short and contain gaps. Not all eruptions leave geological deposits behind, and many pre-eruptive phases include gas emissions which are infrequently measured and are difficult to trace over decadal or centennial timescales.
Trees record environmental change as variations in the isotopic composition of their wood. Studies have shown that anthropogenic SO2 pollution can impair leaf stomata function, causing a stable carbon fractionation of ~ 3‰. In a recent study by D’Arcy et al (in review), concentrated volcanic SO2 emissions were inferred to have a similar effect, but tree uptake of volcanic CO2 complicates this interpretation. Volcanic CO2 has an isotopic signature that is enriched in 13C relative to atmospheric CO2, which will also affect the isotopic composition of the tree rings, making quantitative estimates at the scale of past degassing difficult, based on 13C measurements alone. In this study, we propose to combine radiocarbon analysis with stable carbon isotope analysis, which will allow us to distinguish between (a) carbon fractionation due to the SO2 damage to the leaves and (b) the added volcanic CO2 signature from the volcano.
Volcanic CO2 contains no 14C, while atmospheric CO2 has relatively high amounts of 14C derived from natural cosmogenic nuclide production and atomic weapons testing, and therefore 14C is a very sensitive measure of plant uptake of volcanic CO2. Radiocarbon in tree rings has been used to infer magmatic CO2 emissions in geothermally active regions, and we aim to use these methods to similarly calculate magmatic CO2 uptake in tree rings two volcanic regions. Then, we will apply a stable carbon isotopic approach to estimate past volcanic SO2 degassing, with any influence of volcanic CO2 accounted for. In this way, we can reconstruct the degassing history of a volcano.