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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>6</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-3093-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/3093/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/3093/2006/acpd-6-3093-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/3093/2006/acpd-6-3093-2006.pdf</fulltext_pdf>
	<start_page>3093</start_page>
	<end_page>3097</end_page>
	<publication_date>2006-04-13</publication_date>
	<article_title content_type="html">Methane production from mixed tropical savanna and forest vegetation in Venezuela</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>P. J. Crutzen</name>
		</author>
		<author numeration="2" affiliations="3">
			<name>E. Sanhueza</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>C. A. M. Brenninkmeijer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Chemistry, Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Scripps Institution of Oceanography, University of California, San Diego, USA</affiliation>
		<affiliation numeration="3" content_type="html">Instituto Venezolano de Investigaciones Cient&amp;iacute;ficas, Caracas, Venezuela</affiliation>
	</affiliations>
	<abstract content_type="html">Measurements of methane concentrations in the boundary layer in the northern
part of the Guayana shield, Venezuela, during the wet season (October 1988),
showed the presence of substantial methane surface emissions. The measuring
site is within the savanna climate region, but is affected by emissions from
savanna and forest vegetation. From day versus night concentration
measurements, with higher concentrations during night, a methane source
strength near the site of 3&amp;ndash;7&amp;times;10&lt;sup&gt;11&lt;/sup&gt; molecules/cm&lt;sup&gt;2&lt;/sup&gt;/s can be
estimated, which includes emissions from small tracts of flooded soils,
termites and especially tropical vegetation. Extrapolated to the entire
savanna, this may imply a methane source of ~30&amp;ndash;60 Tg yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
similar to the one calculated for tropical vegetation on the basis of
recently published in vitro plant emission experiments by Keppler et al.&amp;nbsp;(2006),
which indicate emissions of ~30 Tg yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for tropical
savannas and grasslands and ~78 Tg yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for tropical forests.</abstract>
	<references>
	</references>
</article>

