This APEX has been supported by National Science Foundation grants (DEB-0425328, DEB-0724514 and DEB-0830997) to M.R.T, A.D.M, J.H., E.E. and E.S.K., the Bonanza Creek Long-Term Ecological Research program (funded jointly by NSF Grant DEB-0620579, an USDA Forest Service Pacific Northwest Research Grant PNW01-JV11261952-231) and U.S. Geological Survey Climate and Land Use Change Program and Climate Science Center grant funds to J.H., A.D.M., M.W. and E.E. During manuscript compilation and writing, D.O. was supported by a Campus Alberta Innovates Program grant. Any use of trade, firm or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. We thank all collaborators and students who have contributed over the years to the APEX project, namely Bill Cable, Colin Edgar, Michael Waddington, Jamie Hollingsworth, Teresa Hollingsworth, Rebecca Finger, Amy Churchill, Nicole McConnell and Molly Chivers. The authors claim no conflicts of interest.
Department of Integrative Biology, University of Guelph, Science Complex, Guelph, ON, Canada; Department of Renewable Resources, University of Alberta, Edmonton, AB, Canada; Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, AK, United States; U.S. Geological Survey, Menlo Park, CA, United States; School of Forest Resources and Environmental Sciences, and USDA Forest Service, Michigan Tech University, Northern Research Station, Houghton, MI, United States; U.S. Geological Survey, Alaska Cooperative Fish and Wildlife Research Unit, University of Alaska Fairbanks, Fairbanks, AK, United States
Recommended Citation:
Olefeldt D.,Euskirchen E.S.,Harden J.,et al. A decade of boreal rich fen greenhouse gas fluxes in response to natural and experimental water table variability[J]. Global Change Biology,2017-01-01,23(6)