Vol. 11 (2021)

Christopher Poeplau
Hildesheim: Universitätsverlag Hildesheim, 2021. - 353 p.
Zugl. Hildesheim, Univ., Habl., 2021

DOI 10.18442/198

ISBN 978-3-96424-055-2

Soil organic carbon (SOC) is the largest terrestrial carbon pool, holding a manifold of atmospheric carbon. The agricultural management of soils exerts a strong influence on this pool and thereby also on carbon fluxes between biosphere and atmosphere. Historically, land-use changes have caused large CO2 emissions from soils, which significantly contributed to global warming. The latter is expected to cause strong fluxes of CO2 from soils, due to enhanced microbial activity – the climate-carbon cycle feedback loop. This cumulative habilitation thesis focuses on the two major anthropogenic impacts on soil organic carbon as the largest terrestrial carbon pool: land use and global warming due to greenhouse gas emissions. Both have been steadily increasing with the expansion of human population and activity on the planet and are thus considered specific for the ‘Anthropocene’ as a synonym for the period in world history in which human activity leaves irreversible traces. Due to the importance of SOC and its management for climate change, but also for soil fertility and ecosystem resilience, it is crucial to understand i) which management options can maintain and increase SOC, ii) what are the mechanisms leading to SOC losses and stabilization, iii) how shall global net primary production (NPP) as a resource be used in a climate-smart and sustainable way, iv) how will global warming affect SOC dynamics. Together with several methodological aspects related to measuring, calculating and modelling SOC, the research presented in this thesis focuses on those four key questions.