Abstract

Peatland rewetting aims at stopping the emissions of carbon dioxide (CO2) and establishing net carbon sinks. However, in times of global warming, restoration projects must increasingly deal with extreme events such as drought periods. Here, we evaluate the effect of the European summer drought 2018 on vegetation development and the exchange of methane (CH4) and CO2 in two rewetted minerotrophic fens (Hütelmoor—Hte and Zarnekow—Zrk) including potential carry-over effects in the post-drought year. Drought was a major stress factor for the established vegetation but also promoted the rapid spread of new vegetation, which will likely gain a lasting foothold in Zrk. Accordingly, drought increased not only respiratory CO2 losses but also photosynthetic CO2 uptake. Altogether, the drought reduced the net CO2 sink in Hte, while it stopped the persistent net CO2 emissions of Zrk. In addition, the drought reduced CH4 emissions in both fens, though this became most apparent in the post-drought year and suggests a lasting shift towards non-methanogenic organic matter decomposition. Occasional droughts can be beneficial for the restoration of the peatland carbon sink function if the newly grown vegetation increases CO2 sequestration in the long term. Nonetheless, care must be taken to prevent extensive peat decay.This article is part of the theme issue ‘Impacts of the 2018 severe drought and heatwave in Europe: from site to continental scale'.

Highlights

  • Peatlands constitute the largest terrestrial carbon (C) stocks and exert distinct feedback mechanisms on the climate system [1,2]

  • We investigated the impact of the European summer drought 2018 on vegetation development, CH4 and net CO2 exchange including possible carry-over effects in the year after the drought

  • The resilience of restored peatlands to global warming is critical for future prospects of climate mitigation through peatland rewetting

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Summary

Introduction

Peatlands constitute the largest terrestrial carbon (C) stocks and exert distinct feedback mechanisms on the climate system [1,2]. Reducing CO2 emissions and restoring the natural C sink function are such a high priority for peatland rewetting, little is known about the consequences of hydroclimatic droughts for achieving climate mitigation goals. We aim to provide an integrated understanding of drought effects on vegetation development and the evolving GHG dynamics in rewetted minerotrophic fens and further assess the prospects of peatland rewetting as mitigation measure under climate change. The study was conducted in two degraded rewetted fens in Northeast Germany Both sites feature comprehensive datasets on vegetation dynamics and GHG exchange dating back to 2014 so that the patterns occurring during the drought and the post-drought year can be compared against a profound reference record

Methods
Conclusion
22. Johnson WC et al 2010 Prairie wetland complexes
Findings
15. Pachauri RK et al 2014 Climate change 2014
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