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	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>7</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/bg-7-333-2010</doi>
	<article_url>http://www.biogeosciences.net/7/333/2010/</article_url>
	<abstract_html>http://www.biogeosciences.net/7/333/2010/bg-7-333-2010.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/7/333/2010/bg-7-333-2010.pdf</fulltext_pdf>
	<start_page>333</start_page>
	<end_page>341</end_page>
	<publication_date>2010-01-28</publication_date>
	<article_title content_type="html">A kinetic analysis of leaf uptake of COS and its relation to transpiration, photosynthesis and carbon isotope fractionation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>U. Seibt</name>
			<email>ulli@atmos.ucla.edu</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. Kesselmeier</name>
		</author>
		<author numeration="3" affiliations="2,4">
			<name>L. Sandoval-Soto</name>
		</author>
		<author numeration="4" affiliations="2,5">
			<name>U. Kuhn</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>J. A. Berry</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">UniversitÃ© Pierre et Marie Curie Paris 6, UMR BioEmco, Campus ParisAgroTech, 78850 Thiverval-Grignon, France</affiliation>
		<affiliation numeration="2" content_type="html">Max Planck Institute for Chemistry, Biogeochemistry Dept., Joh.-J.-Becher-Weg 27, 55128 Mainz, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Carnegie Institution for Science, Department of Global Ecology, 260 Panama St., Stanford, CA 94305-1297, USA</affiliation>
		<affiliation numeration="4" content_type="html">now at: Fachhochschule Nordwestschweiz, Hochschule fÃ¼r Life Sciences, Institut fÃ¼r Ecopreneurship, GrÃ¼ndenstraÃŸe 40, 4132 Muttenz, Switzerland</affiliation>
		<affiliation numeration="5" content_type="html">now at: Agroscope Reckenholz-TÃ¤nikon Research Station ART, ReckenholzstraÃŸe 191, 8046 ZÃ¼rich, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">Carbonyl sulfide (COS) is an atmospheric trace gas that holds great promise
for studies of terrestrial carbon and water exchange. In leaves, COS follows
the same pathway as CO&lt;sub&gt;2&lt;/sub&gt; during photosynthesis. Both gases are taken up in
enzyme reactions, making COS and CO&lt;sub&gt;2&lt;/sub&gt; uptake closely coupled at the leaf
scale. The biological background of leaf COS uptake is a hydrolysis reaction
catalyzed by the enzyme carbonic anhydrase. Based on this, we derive and test
a simple kinetic model of leaf COS uptake, and relate COS to CO&lt;sub&gt;2&lt;/sub&gt; and water
fluxes at the leaf scale. The equation was found to predict realistic leaf
COS fluxes compared to observations from field and laboratory chambers. We
confirm that COS uptake at the leaf level is directly linked to stomatal
conductance. As a consequence, the ratio of normalized uptake rates (uptake
rates divided by ambient mole fraction) for leaf COS and CO&lt;sub&gt;2&lt;/sub&gt; fluxes can
provide an estimate of &lt;i&gt;C&lt;sub&gt;i&lt;/sub&gt;&lt;/i&gt;/&lt;i&gt;C&lt;sub&gt;a&lt;/sub&gt;&lt;/i&gt;, the ratio of intercellular to atmospheric
CO&lt;sub&gt;2&lt;/sub&gt;, an important plant gas exchange parameter that cannot be measured
directly. The majority of published normalized COS to CO&lt;sub&gt;2&lt;/sub&gt; uptake ratios
for leaf studies on a variety of species fall in the range of 1.5 to 4,
corresponding to &lt;i&gt;C&lt;sub&gt;i&lt;/sub&gt;&lt;/i&gt;/&lt;i&gt;C&lt;sub&gt;a&lt;/sub&gt;&lt;/i&gt; ratios of 0.5 to 0.8. In addition, we utilize the
coupling of &lt;i&gt;C&lt;sub&gt;i&lt;/sub&gt;&lt;/i&gt;/&lt;i&gt;C&lt;sub&gt;a&lt;/sub&gt;&lt;/i&gt; and photosynthetic &lt;sup&gt;13&lt;/sup&gt;C discrimination to derive an
estimate of 2.8&amp;plusmn;0.3 for the global mean normalized uptake ratio. This
corresponds to a global vegetation sink of COS in the order of
900&amp;plusmn;100 Gg S yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. COS can now be implemented in the same model framework as
CO&lt;sub&gt;2&lt;/sub&gt; and water vapour. Atmospheric COS measurements can then provide
independent constraints on CO&lt;sub&gt;2&lt;/sub&gt; and water cycles at ecosystem, regional and
global scales.</abstract>
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</article>

