Reduction of the temperature sensitivity of minerotrophic fen methane emissions by simulated glacial atmospheric carbon dioxide starvation
Variations to the global wetland CHâ source strength in response to changes in orbital insolation patterns and atmospheric COâ concentration ([COâ]a) are hypothesized to play an important role in determining glacial-interglacial variations in atmospheric CHâ concentration ([CHâ]a). Here the interactive effects of temperature, a major controlling variable determining wetland CHâ flux, and the low [COâ]a of glacial intervals are investigated for the first time. We measured the temperature dependence of CHâ emissions from replicated mesocosms (n = 8 per COâ treatment) collected from a minerotrophic fen and an ombrotrophic bog incubated in either ambient (c. 400 ppm) or glacial (c. 200 ppm) [COâ]a located in the United Kingdom. CHâ fluxes were measured at 5°C, 10°C, 15°C, 20°C, and 25°C and then in reverse order over a 20 day period under each [COâ]a treatment. Results showed that the Q10 temperature response of CHâ emissions from the Carex/Juncus-dominated fen declined significantly by approximately 39% under glacial [COâ]a (ambient [COâ]a = 2.60, glacial [COâ]a = 1.60; P < 0.01). By contrast, the response of CHâ emissions from the Sphagnum-dominated bog remained unaltered (ambient [COâ]a = 3.67, glacial [COâ]a = 3.67; P > 0.05). This contrasting response may be linked to differences in plant species assemblage and the varying impact of COâ starvation on plant productivity and carbon availability in the rhizosphere. Furthermore, our results provide empirical evidence to support recent model-based indications that glacial-interglacial variations in [CHâ]a may be explained by changes in wetland CHâ source strength in response to orbitally forced changes in climate and [COâ]a.
document
https://n2t.org/ark:/85065/d73j3dtf
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2013-06-01T00:00:00Z
Copyright 2013 American Geophysical Union.
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