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Title: SPRUCE Stability of Peatland Carbon to Rising Temperatures: Supporting Data

Abstract

This data set reports the results of extensive field measurements and laboratory analyses of samples from the SPRUCE experiment. Results indicate that ecosystem-scale warming of over 2 m of peat exponentially increased CH4 emissions —but not ecosystem respiration of CO2. Multiple lines of evidence, including incubations and in situ analyses of 14C, dissolved gases, and microbial community metabolic potential, indicate that CH4 emissions increased due to surface processes and not degradation of deeper buried carbon. The supporting data provided include the summarized and aggregated data used to generate the six figures in the main text of the paper and the 12 supplementary figures.

Authors:
; ; ; ; ; ; ; ; ; ; ;
  1. Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tennessee, U.S.A
  2. USDA Forest Service
Publication Date:
DOE Contract Number:  
AC05-00OR22725
Research Org.:
ORNLTESSFA (Oak Ridge National Lab's Terrestrial Ecosystem Science Scientific Focus Area (ORNL TES SFA))
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23). Climate and Environmental Sciences Division
Subject:
54 ENVIRONMENTAL SCIENCES; SPRUCE Experiment, ORNL TES SFA, U.S. DOE Office of Science, Marcell Experimental Forest, Northern Research Station, U.S. Forest Service, Radiocarbon, CH4 production rates, methane, soil warming
OSTI Identifier:
1415751
DOI:
https://doi.org/10.3334/cdiac/spruce.026

Citation Formats

Wilson, R. M., Hopple, A. M., Tfaily, M. M., Sebestyen, S. D., Schadt, C. W., Pfeifer-Meister, L., Medvedeff, C., McFarlane, K J., Kostka, J. E., Kolton, M, Kolka, R., and Kluber, L. A. SPRUCE Stability of Peatland Carbon to Rising Temperatures: Supporting Data. United States: N. p., 2016. Web. doi:10.3334/cdiac/spruce.026.
Wilson, R. M., Hopple, A. M., Tfaily, M. M., Sebestyen, S. D., Schadt, C. W., Pfeifer-Meister, L., Medvedeff, C., McFarlane, K J., Kostka, J. E., Kolton, M, Kolka, R., & Kluber, L. A. SPRUCE Stability of Peatland Carbon to Rising Temperatures: Supporting Data. United States. doi:https://doi.org/10.3334/cdiac/spruce.026
Wilson, R. M., Hopple, A. M., Tfaily, M. M., Sebestyen, S. D., Schadt, C. W., Pfeifer-Meister, L., Medvedeff, C., McFarlane, K J., Kostka, J. E., Kolton, M, Kolka, R., and Kluber, L. A. 2016. "SPRUCE Stability of Peatland Carbon to Rising Temperatures: Supporting Data". United States. doi:https://doi.org/10.3334/cdiac/spruce.026. https://www.osti.gov/servlets/purl/1415751. Pub date:Fri Jan 01 04:00:00 UTC 2016
@article{osti_1415751,
title = {SPRUCE Stability of Peatland Carbon to Rising Temperatures: Supporting Data},
author = {Wilson, R. M. and Hopple, A. M. and Tfaily, M. M. and Sebestyen, S. D. and Schadt, C. W. and Pfeifer-Meister, L. and Medvedeff, C. and McFarlane, K J. and Kostka, J. E. and Kolton, M and Kolka, R. and Kluber, L. A.},
abstractNote = {This data set reports the results of extensive field measurements and laboratory analyses of samples from the SPRUCE experiment. Results indicate that ecosystem-scale warming of over 2 m of peat exponentially increased CH4 emissions —but not ecosystem respiration of CO2. Multiple lines of evidence, including incubations and in situ analyses of 14C, dissolved gases, and microbial community metabolic potential, indicate that CH4 emissions increased due to surface processes and not degradation of deeper buried carbon. The supporting data provided include the summarized and aggregated data used to generate the six figures in the main text of the paper and the 12 supplementary figures.},
doi = {10.3334/cdiac/spruce.026},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Fri Jan 01 04:00:00 UTC 2016},
month = {Fri Jan 01 04:00:00 UTC 2016}
}