My research focuses on multi-scale effects of global change on ecosystem structure and function. In the past, I have investigated the influence of drought, permafrost thaw or warming on above and belowground plant dynamics, greenhouse gas fluxes and litter decomposition. I am also interested in regional to global-scale drivers of carbon sequestration. My toolkit draws from ecosystem ecology, biogeochemistry, plant ecology and systems thinking and I specialize in carbon-rich systems such as northern peatlands and permafrost features.
My postdoctoral research in the Jackson lab focuses on 1) greenhouse gas fluxes of peatlands and northern ecosystems and 2) the fate of root-derived carbon in soils.
Doctor of Philosophy, McGill University (2016)
Master of Science, Villanova University (2010)
Bachelor of Science, York University (2007)
Peatland warming strongly increases fine-root growth.
Proceedings of the National Academy of Sciences of the United States of America
Belowground climate change responses remain a key unknown in the Earth system. Plant fine-root response is especially important to understand because fine roots respond quickly to environmental change, are responsible for nutrient and water uptake, and influence carbon cycling. However, fine-root responses to climate change are poorly constrained, especially in northern peatlands, which contain up to two-thirds of the world's soil carbon. We present fine-root responses to warming between +2 °C and 9 °C above ambient conditions in a whole-ecosystem peatland experiment. Warming strongly increased fine-root growth by over an order of magnitude in the warmest treatment, with stronger responses in shrubs than in trees or graminoids. In the first year of treatment, the control (+0 °C) shrub fine-root growth of 0.9 km m-2 y-1 increased linearly by 1.2 km m-2 y-1 (130%) for every degree increase in soil temperature. An extended belowground growing season accounted for 20% of this dramatic increase. In the second growing season of treatment, the shrub warming response rate increased to 2.54 km m-2 °C-1 Soil moisture was negatively correlated with fine-root growth, highlighting that drying of these typically water-saturated ecosystems can fuel a surprising burst in shrub belowground productivity, one possible mechanism explaining the "shrubification" of northern peatlands in response to global change. This previously unrecognized mechanism sheds light on how peatland fine-root response to warming and drying could be strong and rapid, with consequences for the belowground growing season duration, microtopography, vegetation composition, and ultimately, carbon function of these globally relevant carbon sinks.
View details for DOI 10.1073/pnas.2003361117
View details for PubMedID 32661144
- Thaw Transitions and Redox Conditions Drive Methane Oxidation in a Permafrost Peatland JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES 2020; 125 (3)
- Fast plants in deep water: introducing the whole-soil column perspective. The New phytologist 2020; 225 (1): 7–9
- Peatland warming strongly increases fine-root growth PNAS 2020
- Rapid Net Carbon Loss From A Whole-Ecosystem Warmed Peatland AGU Advances 2020
Large loss of CO2 in winter observed across the northern permafrost region.
Nature Climate Change
2019; 9: 852-857
View details for DOI 10.1038/s41558-019-0592-8
The landscape of soil carbon data: emerging questions, synergies and databases
Progress in Physical Geography
View details for DOI 10.1177/0309133319873309
- Reviews and syntheses: Changing ecosystem influences on soil thermal regimes in northern high-latitude permafrost regions BIOGEOSCIENCES 2018; 15 (17): 5287–5313
- Post-thaw variability in litter decomposition best explained by microtopography at an ice-rich permafrost peatland ARCTIC ANTARCTIC AND ALPINE RESEARCH 2018; 50 (1)
The Fate of Root Carbon in Soil: Data and Model
View details for DOI 10.1029/2018EO112593
Networking our science to characterize the state, vulnerabilities, and management opportunities of soil organic matter.
Global change biology
2018; 24 (2): e705–e718
Soil organic matter (SOM) supports the Earth's ability to sustain terrestrial ecosystems, provide food and fiber, and retains the largest pool of actively cycling carbon. Over 75% of the soil organic carbon (SOC) in the top meter of soil is directly affected by human land use. Large land areas have lost SOC as a result of land use practices, yet there are compensatory opportunities to enhance productivity and SOC storage in degraded lands through improved management practices. Large areas with and without intentional management are also being subjected to rapid changes in climate, making many SOC stocks vulnerable to losses by decomposition or disturbance. In order to quantify potential SOC losses or sequestration at field, regional, and global scales, measurements for detecting changes in SOC are needed. Such measurements and soil-management best practices should be based on well established and emerging scientific understanding of processes of C stabilization and destabilization over various timescales, soil types, and spatial scales. As newly engaged members of the International Soil Carbon Network, we have identified gaps in data, modeling, and communication that underscore the need for an open, shared network to frame and guide the study of SOM and SOC and their management for sustained production and climate regulation.
View details for PubMedID 28981192
- Temporal and Spatial Variation in Peatland Carbon Cycling and Implications for Interpreting Responses of an Ecosystem-Scale Warming Experiment SOIL SCIENCE SOCIETY OF AMERICA JOURNAL 2017; 81 (6): 1668–88
- Biophysical drivers of seasonal variability in Sphagnum gross primary production in a northern temperate bog JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES 2017; 122 (5): 1078–97
A New Platform for Managing Soil Carbon and Soil Health
View details for DOI 10.1029/2017EO080753
- Ecohydrological feedbacks in peatlands: an empirical test of the relationship among vegetation, microtopography and water table ECOHYDROLOGY 2016; 9 (7): 1346–57
- Environmental correlates of peatland carbon fluxes in a thawing landscape: do transitional thaw stages matter? BIOGEOSCIENCES 2015; 12 (10): 3119–30