Air Flow and Heat Transfer in a Temperature Controlled Open Top Enclosure. ASME International Mechanical Engineering Congress and Exposition.. 2012.
Attaining whole-ecosystem warming using air and deep-soil heating methods with an elevated CO2 atmosphere. Biogeosciences. 14:861-883.. 2017.
Biophysical drivers of seasonal variability in Sphagnum gross primary production in a northern temperate bog. Journal of Geophysical Research: Biogeosciences. 122:1078-1097.. 2017.
A call for international soil experiment networks for studying, predicting, and managing global change impacts. SOIL. 1:575–582.. 2015.
Can Sphagnum leachate chemistry explain differences in anaerobic decomposition in peatlands? Soil Biology and Biochemistry. 86:34-41.. 2015.
Chapter Five - The Sphagnum Genome Project: A New Model for Ecological and Evolutionary Genomics. Genomes and Evolution of Charophytes, Bryophytes, Lycophytes and Ferns. 78:167-187.. 2016.
A comment on Appropriate experimental ecosystem warming methods by ecosystem, objective, and practicality by Aronson and McNulty. AGRICULTURAL AND FOREST METEOROLOGY. 150:497-498.. 2010.
A comprehensive data acquisition and management system for an ecosystem-scale peatland warming and elevated CO2 experiment. Geoscientific Instrumentation, Methods and Data Systems. 4(2):203-213.. 2015.
Deep peat warming increases surface methane and carbon dioxide emissions in a black spruce-dominated ombrotrophic bog. Global Change Biology. 23(12):5398-5411.. 2017.
Dynamic Vertical Profiles of Peat Porewater Chemistry in a Northern Peatland. Wetlands. 36(6):1119-1130.. 2016.
Fine-root growth in a forested bog is seasonally dynamic, but shallowly distributed in nutrient-poor peat. Plant and Soil. 424:123–143.. 2018.
Forecasting responses of a northern peatland carbon cycle to elevated CO2 and a gradient of experimental warming. Journal of Geophysical Research: Biogeosciences. 123(3):1057-1071.. 2018.
Forest phenology and a warmer climate – growing season extension in relation to climatic provenance. Global Change Biology. 18:2008–2025.. 2012.
From systems biology to photosynthesis and whole-plant physiology. Plant Signaling & Behavior. 7(2):260-262.. 2012.
Gaseous mercury fluxes in peatlands and the potential influence of climate change. Atmospheric Environment. 154:247-259.. 2017.
High-throughput fluorometric measurement of potential soil extracellular enzyme activities. Journal of Visualized Experiments. 81(e50961). 2013.
Hydrogenation of organic matter as a terminal electron sink sustains high CO 2 :CH 4 production ratios during anaerobic decomposition. Organic Geochemistry. 112:22-32.. 2017.
Intermediate-scale community-level flux of CO2 and CH4 in a Minnesota peatland: putting the SPRUCE project in a global context. Biogeochemistry. 129(3):255-272.. 2016.
Long-term carbon and nitrogen dynamics at SPRUCE revealed through stable isotopes in peat profiles. Biogeosciences. 14(9):2481-2494.. 2017.
Melanin mitigates the accelerated decay of mycorrhizal necromass with peatland warming. Ecology Letters. 22(3):498-505.. 2019.
A method for experimental heating of intact soil profiles for application to climate change experiments. Global Change Biology. 17:1083–1096.. 2011.
Methylotrophic methanogenesis in Sphagnum -dominated peatland soils. Soil Biology and Biochemistry. 118:156-160.. 2018.
Microbial Community Stratification Linked to Utilization of Carbohydrates and Phosphorus Limitation in a Boreal Peatland at Marcell Experimental Forest, Minnesota, USA. Applied and Environmental Microbiology. 80(11):3518-3530.. 2014.
Microbial Metabolic Potential for Carbon Degradation and Nutrient (Nitrogen and Phosphorus) Acquisition in an Ombrotrophic Peatland. Applied and Environmental Microbiology. 80(11):3531-3540.. 2014.