Research Fellow, University of Waikato
Charlotte is a soil microbial ecologist, biogeochemist, and science communicator. Her work uses trait-based ecological approaches to link soil microbial activity to ecosystem function and biogeochemical cycling, particularly in response to anthropogenic environmental change. Charlotte is an expert in characterising temperature responses of microbial communities and the won the Gene E. Likens Biogeosciences Junior Scientist Outstanding Publication Award from the Ecological Society of America, for her 2020 Global Change Biology paper "Embracing a new paradigm for temperature sensitivity of soil microbes”. Charlotte moved to Aotearoa in 2021 from the U.S. to work as a research fellow at the University of Waikato and recently joined the Soil and Physical Sciences Department at Lincoln University as a Lecturer in Soil Microbiology.
Aotearoa as a model system to understand soil microbial responses to climate warming
Soils contain the largest reservoir of carbon in the terrestrial biosphere and this carbon is vulnerable to degradation by soil microbial communities. As the climate warms microbial activity will increase, leading to acceleration of soil carbon losses. Despite its major importance for climate modelling and for understanding of ecosystem responses to climate change, the relationship between warming and soil microbial activity remains poorly constrained. This is due to a number of factors, but primarily because of methodological and conceptual limitations. In this presentation, I aim to provide a background on the temperature responses of soil microbial activity and present a theoretical framework to progress this area of research. I will explore experimental data collected from a range of soil temperatures across Aotearoa, including from along a unique soil geothermal gradient, to make predictions about soil microbial responses to warming. Using this data, I quantified adaptation rates of soil microbial respiration and found that it is decoupled from warming. This work highlights the exceptional opportunity we have here in Aotearoa to study large thermal gradients across relatively controlled environmental conditions. We can use this information to estimate potential for soil carbon losses with warming and generate novel hypotheses about evolutionary adaptation of soil microbial communities.