
SPRUCE
Spruce and Peatland Responses
Under Changing Environments
Publications
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. 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. Characterizing Peatland Microtopography Using Gradient and Microform-Based ApproachesAbstract. Ecosystems. 23(7):1464-1480.
.
2020. 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. Ecosystem warming extends vegetation activity but heightens vulnerability to cold temperatures. Nature. 560:371.
.
2018. 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.