No detectable aerobic methane efflux from plant material, nor from adsorption/desorption processes

In early 2006, Keppler et al. (Nature, 439:187–191) reported a novel finding that plant leaves, and even simple organic materials, can release methane under aerobic conditions. We investigated here whether the reported methane release might simply arise from methane desorption from sample surfaces a...

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Main Authors: M. U. F. Kirschbaum, A. Walcroft
Format: Article
Language:English
Published: Copernicus Publications 2008-11-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/5/1551/2008/bg-5-1551-2008.pdf
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spelling doaj-3bf430c1b8e8455d8f0c259ccac60e942020-11-25T01:09:23ZengCopernicus PublicationsBiogeosciences1726-41701726-41892008-11-015615511558No detectable aerobic methane efflux from plant material, nor from adsorption/desorption processesM. U. F. KirschbaumA. WalcroftIn early 2006, Keppler et al. (Nature, 439:187–191) reported a novel finding that plant leaves, and even simple organic materials, can release methane under aerobic conditions. We investigated here whether the reported methane release might simply arise from methane desorption from sample surfaces after prior exposure to higher methane concentrations. We exposed standard cellulose filter papers (i.e. organic material with a high surface area) to atmospheric methane concentration and then transferred them to a low-methane atmosphere. Our results suggest that any desorption flux was extremely small (−0.0001±0.0019 ngCH<sub>4</sub> kgDW<sup>−1</sup> s<sup>−1</sup>) and would play no quantitatively significant role in modifying any measured methane fluxes. <br> <br> We also incubated fresh detached leaves of several species and intact <i>Zea mays</i> seedlings under aerobic and low-light conditions. After correcting for a small measured methane influx into empty chambers, measured rates of methane emission by plant materials were zero or, at most, very small, ranging from −0.25±1.1 ngCH<sub>4</sub> kgDW<sup>−1</sup> s<sup>−1</sup> for <i>Zea mays</i> seedlings to 0.10±0.08 ngCH<sub>4</sub> kgDW<sup>−1</sup> s<sup>−1</sup> for a mixture of freshly detached grasses. These rates were much smaller than the rates originally reported by Keppler et al. (2006). http://www.biogeosciences.net/5/1551/2008/bg-5-1551-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. U. F. Kirschbaum
A. Walcroft
spellingShingle M. U. F. Kirschbaum
A. Walcroft
No detectable aerobic methane efflux from plant material, nor from adsorption/desorption processes
Biogeosciences
author_facet M. U. F. Kirschbaum
A. Walcroft
author_sort M. U. F. Kirschbaum
title No detectable aerobic methane efflux from plant material, nor from adsorption/desorption processes
title_short No detectable aerobic methane efflux from plant material, nor from adsorption/desorption processes
title_full No detectable aerobic methane efflux from plant material, nor from adsorption/desorption processes
title_fullStr No detectable aerobic methane efflux from plant material, nor from adsorption/desorption processes
title_full_unstemmed No detectable aerobic methane efflux from plant material, nor from adsorption/desorption processes
title_sort no detectable aerobic methane efflux from plant material, nor from adsorption/desorption processes
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2008-11-01
description In early 2006, Keppler et al. (Nature, 439:187–191) reported a novel finding that plant leaves, and even simple organic materials, can release methane under aerobic conditions. We investigated here whether the reported methane release might simply arise from methane desorption from sample surfaces after prior exposure to higher methane concentrations. We exposed standard cellulose filter papers (i.e. organic material with a high surface area) to atmospheric methane concentration and then transferred them to a low-methane atmosphere. Our results suggest that any desorption flux was extremely small (−0.0001±0.0019 ngCH<sub>4</sub> kgDW<sup>−1</sup> s<sup>−1</sup>) and would play no quantitatively significant role in modifying any measured methane fluxes. <br> <br> We also incubated fresh detached leaves of several species and intact <i>Zea mays</i> seedlings under aerobic and low-light conditions. After correcting for a small measured methane influx into empty chambers, measured rates of methane emission by plant materials were zero or, at most, very small, ranging from −0.25±1.1 ngCH<sub>4</sub> kgDW<sup>−1</sup> s<sup>−1</sup> for <i>Zea mays</i> seedlings to 0.10±0.08 ngCH<sub>4</sub> kgDW<sup>−1</sup> s<sup>−1</sup> for a mixture of freshly detached grasses. These rates were much smaller than the rates originally reported by Keppler et al. (2006).
url http://www.biogeosciences.net/5/1551/2008/bg-5-1551-2008.pdf
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