Climate change is caused by an imbalance in the global carbon cycle - human activity has increased the concentration of carbon in the atmosphere. To predict and mitigate the effects of climate change, we need to understand how carbon flows between the atmosphere and its two other major reservoirs on land: plants and soils. The Waring Ecology Lab at Imperial College London investigates how the ecology of plant and soil microbial communities influences the carbon cycle and its feedbacks on climate change.
Averill C, Waring B, 2018, Nitrogen limitation of decomposition and decay: How can it occur?, Global Change Biology, Vol:24, ISSN:1354-1013, Pages:1417-1427
et al., 2017, Historical climate controls soil respiration responses to current soil moisture, Proceedings of the National Academy of Sciences, Vol:114, ISSN:0027-8424, Pages:6322-6327
et al., 2016, Scale-dependent variation in nitrogen cycling and soil fungal communities along gradients of forest composition and age in regenerating tropical dry forests, New Phytologist, Vol:209, ISSN:0028-646X, Pages:845-854