A new European study has found that soil carbon loss is more sensitive to climate change compared to carbon taken up by plants. In drier regions, soil carbon loss decreased but in wetter regions soil carbon loss increased. This could result in a positive feedback to the atmosphere leading to an additional increase of atmospheric CO2 levels.
Scientists analysed data from seven climate change experiments across Europe to show how European shrubland plant biomass and soil carbon loss is affected by summer drought and year-around warming.
The research was led by Dr Sabine Reinsch and Professor Bridget Emmett from the UK-based Centre for Ecology & Hydrology (CEH) in collaboration with European and US climate scientists and published in the Nature journal Scientific Reports.
The authors showed that soil carbon loss is most responsive to change in soil water. Soil water plays a critical role in wet soils where water logging limits decomposition processes by soil biota resulting in a build-up of soil carbon as peat. Drying of the soil removes this limitation resulting in soil carbon loss. In contrast in drier soils, reduced rainfall reduces soil water below the optimum for soil biota resulting in a decrease in soil carbon loss.
Most of the earth's terrestrial carbon is stored in soil. The world's soil carbon stocks are estimated to be circa 2000 gigatonnes (1 gigatonne = 1 000 000 000 000 kilograms) of carbon. The researchers showed that drought decreases and increases soil carbon more predictably than warming.
Data was provided from CEH's climate change manipulation experiment, which has been running for 18 years in Cloceanog forest, a wet Welsh upland site with a peat layer resulting from seasonal waterlogging. At the field site, increasing temperature and drought were imposed on the vegetation to study the effects of climate change on various ecosystem processes.
Dr Sabine Reinsch, the lead author on the paper and a Soil Ecologist at the Centre for Ecology & Hydrology, said, "This cross-European study enabled us, for the first, time to investigate plant and soil responses to climate change beyond single sites.
"Putting ecosystem responses to climate change into the wider context of natural climate gradients helps us to understand the observed responses of plants and soils better."
Professor Claus Beier, the Head of Department of Geosciences and Natural Resource Management in Denmark and co-author on the paper, said, "The study highlights and illustrates new and fundamental understanding related to the response of ecosystems to climate change.
"By conducting the same experiment at different moisture and temperature conditions across the European continent, it has become clear and visible how the pressure from climate change factors may act differently, and sometimes even opposite, across these conditions.
"These differences are important for our overall assessment of future ecosystem responses to climate change, but the study also shows that they can be understood and to some extent predicted."
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