Dr. Mike Philben joined the departments of chemistry and geological and environmental science in 2019. Before starting at 快猫短视频, he worked as a postdoctoral researcher at Memorial University (Canada) and at Oak Ridge National Laboratory in Tennessee. He has conducted field work in the boreal forests of Newfoundland and Labrador, Canada, and the tundra near Nome, Alaska.

See Dr. Philben鈥檚 current research 

Areas of expertise

Mike鈥檚 research focuses on the feedbacks between climate change and the carbon and nitrogen cycles. He is particularly interested in ecosystems such as peat bogs and Arctic tundra that contain vast quantities of organic carbon that could be destabilized and decomposed to CO2 with further warming.

Past and current research projects include:

• Evaluating how peat bogs responded to past climate change
• Improving how climate models represent of the fate of soil organic matter currently stored in permafrost
• Investigating why moss detritus persists in the environment long after its death and contributes to natural carbon sequestration
• Analyzing the stable isotope ratios of individual amino acids to understand how organic nitrogen is transformed in boreal forest soils

Education

• Ph.D., marine science, University of South Carolina, 2014
• B.A., earth and planetary science, Northwestern University, 2010

Published work

• 鈥�Influences of Hillslope Biogeochemistry on Anaerobic Soil Organic Matter Decomposition in a Tundra Watershed,鈥� with  Neslihan Ta艧 et al., Journal of Geophysical Research-Biogeosciences, 2020
• 鈥�Anaerobic respiration pathways and response to increased substrate availability of Arctic wetland soils,鈥� with  Lijie Zhang et al., Environmental Science: Processes and Impacts, 2020
• 鈥�Stimulation of anaerobic organic matter degradation by nitrogen addition in tundra soils,鈥� Soil Biology and Biochemistry, 2019
• 鈥淒ecomposition dynamics and chemical composition of upland boreal forest moss tissues,鈥� Biogeosciences, 2018
• 鈥淐haracterization of Iron Oxide Nanoparticle Films at the Air鈥揥ater Interface in Arctic Tundra Waters,鈥� Science of the Total Environment, 2018
• 鈥淎mino acid 未15N indicates lack of N isotope fractionation during soil organic nitrogen decomposition,鈥� Biogeochemistry, 2018
• 鈥淭he origin of soil organic matter controls its composition and bioreactivity across a mesic boreal forest latitudinal gradient,鈥� Global Change Biology, 2017
• 鈥淐limate warming can accelerate carbon fluxes without changing soil carbon stocks,鈥� Frontiers in Earth Science, 2017
• 鈥淩ates of soil organic nitrogen cycling increase with temperature and precipitation along a boreal forest latitudinal transect,鈥� Biogeochemistry, 2016
• 鈥淭emperature, oxygen, and vegetation controls on decomposition in a James Bay peatland,鈥� Global Biogeochemical Cycles, 2015
• 鈥淒oes oxygen exposure time control the extent of organic matter decomposition in peatlands?鈥� Journal of Geophysical Research-Biogeosciences, 2014
• 鈥淏iochemical evidence for minimal vegetation change in peatlands of the West Siberian Lowland during the Medieval Climate Anomaly and Little Ice Age,鈥� Journal of Geophysical Research-Biogeosciences, 2014
• 鈥淩eactivity of hydroxyproline-rich glycoproteins and their potential as biochemical tracers of plant-derived nitrogen,鈥� Organic Geochemistry, 2013