Articles | Volume 18, issue 8
Biogeosciences, 18, 2449–2463, 2021
Biogeosciences, 18, 2449–2463, 2021

Research article 19 Apr 2021

Research article | 19 Apr 2021

Biogeochemical and plant trait mechanisms drive enhanced methane emissions in response to whole-ecosystem warming

Genevieve L. Noyce and J. Patrick Megonigal

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Cited articles

Al-Haj, A. N. and Fulweiler, R. W.: A synthesis of methane emissions from shallow vegetated coastal ecosystems, Global Change Biol., 26, 2988–3005,, 2020. 
Bardgett, R. D., Bowman, W. D., Kaufmann, R., and Schmidt, S. K.: A temporal approach to linking aboveground and belowground ecology, Trends Ecol. Evol., 20, 634–641,, 2005. 
Basiliko, N., Stewart, H., Roulet, N. T., and Moore, T. R.: Do root exudates enhance peat decomposition?, Geomicrobiol. J., 29, 374–378,, 2012. 
Bianchi, T. S.: Biogeochemistry of Estuaries, Oxford University Press, New York, USA, 720 pp., 2006. 
Blaser, M. and Conrad, R.: Stable carbon isotope fractionation as tracer of carbon cycling in anoxic soil ecosystems, Curr. Opin. Biotech., 41, 122–129,, 2016. 
Short summary
Methane (CH4) is a potent greenhouse gas that contributes to global radiative forcing. A mechanistic understanding of how wetland CH4 cycling will respond to global warming is crucial for improving prognostic models. We present results from the first 4 years of a novel whole-ecosystem warming experiment in a coastal wetland, showing that warming increases CH4 emissions and identifying four potential mechanisms that can be added to future modeling efforts.
Final-revised paper