Rapid loss of an ecosystem engineer: Sphagnum decline in an experimentally warmed bog. Ecology and Evolution. 9(22):12571-12585.. 2019.
Uncertainty in Peat Volume and Soil Carbon Estimated Using Ground-Penetrating Radar and Probing. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL. 76:1911-1918.. 2012.
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.
Representing northern peatland microtopography and hydrology within the Community Land Model. Biogeosciences. 12:6463–6477.. 2015.
Novel climates reverse carbon uptake of atmospherically dependent epiphytes: Climatic constraints on the iconic boreal forest lichen Evernia mesomorpha. American Journal of Botany. 105(2):266-274.. 2018.
Organic matter transformation in the peat column at Marcell Experimental Forest: Humification and vertical stratification. Journal of Geophysical Research: Biogeosciences. 119:661–675.. 2014.
Vertical Stratification of Peat Pore Water Dissolved Organic Matter Composition in a Peat Bog in Northern Minnesota. Journal of Geophysical Research: Biogeosciences. 123:479-494.. 2018.
Simulation of carbon cycling, including dissolved organic carbon transport, in forest soil locally enriched with 14C. Biogeochemistry. 108:91-107.. 2012.
Biophysical drivers of seasonal variability in Sphagnum gross primary production in a northern temperate bog. Journal of Geophysical Research: Biogeosciences. 122:1078-1097.. 2017.
Molybdenum-Based Diazotrophy in a Sphagnum Peatland in Northern Minnesota. [collaborator contribution]. Applied and Environmental Microbiology. 83:e01174-17.. 2017.
Sphagnum physiology in the context of changing climate: emergent influences of genomics, modelling and host–microbiome interactions on understanding ecosystem function. Plant, Cell & Environment. 38:1737–1751.. 2015.
From systems biology to photosynthesis and whole-plant physiology. Plant Signaling & Behavior. 7(2):260-262.. 2012.
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.
Stability of peatland carbon to rising temperatures. Nature Communications. 7:13723.. 2016.
Small differences in ombrotrophy control regional-scale variation in methane cycling among Sphagnum-dominated peatlands. Biogeochemistry. 139:155-177.. 2018.
Methylotrophic methanogenesis in Sphagnum -dominated peatland soils. Soil Biology and Biochemistry. 118:156-160.. 2018.