Fast Microbial Processes and the Long-Term Soil Carbon-Climate Feedback |
Bernhard Ahrens,
Alexander J. Winkler,
Thomas Wutzler,
Markus Reichstein
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Project descriptionFast microbial processes, such as microbial acclimation or substrate depletion may play a crucial role in how soils respond to climate change. These processes could provide a self-regulating feedback controlling soil carbon losses in a warmer world - but they are often poorly explored in current soil carbon models, in part due to limited integration of experimental data from soil warming studies and global soil carbon databases.At the same time, increased vegetation productivity due to the CO2 fertilization effect may increase carbon inputs to the soil. While this could offset soil carbon losses due to climate change via increased carbon inputs, it might also stimulate priming effects, accelerating the microbial decomposition of existing soil carbon. Understanding these competing mechanisms is essential for improving predictions of how soil carbon contributes to the global carbon-climate feedback. In this project we aim to understand how fast microbial processes affect the long-term soil carbon-climate feedback by combining soil microbial models and vegetation models with machine learning from large-scale soil warming datasets and global soil carbon databases. Your profileWe welcome applications from curious and motivated students from any country who have
Working group and planned collaborationsThe Max Planck Institute for Biogeochemistry in Jena offers an exceptionally dynamic, creative, international, and multidisciplinary working environment. You will join the Modeling Interactions in Soil Systems Group, focusing on the persistence and sensitivity of organic carbon in soils and interactions between biogeochemical cycles of carbon, nutrients, and water. The project is embedded in the MC3 4 Earth Max Planck Center - a collaboration between:
For further information, please contact Bernhard Ahrens Alexander Winkler Thomas Wutzler Markus Reichstein |