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@ARTICLE{Seibt:13369,
author = {Seibt, U. and Kesselmeier, J. and Sandoval-Soto, L. and
Kuhn, U. and Berry, J.A.},
title = {{A} kinetic analysis of leaf uptake of {COS} and its
relation to transpiration, photosynthesis and carbon isotope
fractionation},
journal = {Biogeosciences},
volume = {7},
issn = {1726-4170},
address = {Katlenburg-Lindau [u.a.]},
publisher = {Copernicus},
reportid = {PreJuSER-13369},
pages = {333 - 341},
year = {2010},
note = {We are grateful to Parv Suntharalingam, Graham Farquhar,
and the two referees for discussions, helpful comments and
suggestions. The research leading to these results has
received funding from the European Research Council under
the European Community's Seventh Framework Programme
(FP7/2007-2013)/ERC Grant Agreement no. 202835 "COSIRIS".},
abstract = {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
CO2 during photosynthesis. Both gases are taken up in enzyme
reactions, making COS and CO2 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 CO2 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 CO2 fluxes can provide an estimate of
C-i/C-a, the ratio of intercellular to atmospheric CO2, an
important plant gas exchange parameter that cannot be
measured directly. The majority of published normalized COS
to CO2 uptake ratios for leaf studies on a variety of
species fall in the range of 1.5 to 4, corresponding to
C-i/C-a ratios of 0.5 to 0.8. In addition, we utilize the
coupling of C-i/C-a and photosynthetic C-13 discrimination
to derive an estimate of 2.8 +/- 0.3 for the global mean
normalized uptake ratio. This corresponds to a global
vegetation sink of COS in the order of 900 +/- 100 Gg S
yr(-1). COS can now be implemented in the same model
framework as CO2 and water vapour. Atmospheric COS
measurements can then provide independent constraints on CO2
and water cycles at ecosystem, regional and global scales.},
keywords = {J (WoSType)},
cin = {IEK-8},
ddc = {570},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {Atmosphäre und Klima / COSIRIS - Investigating the
terrestrial carbon and water cycles with a multi-tracer
approach (202835)},
pid = {G:(DE-Juel1)FUEK491 / G:(EU-Grant)202835},
shelfmark = {Ecology / Geosciences, Multidisciplinary},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000274058100026},
url = {https://juser.fz-juelich.de/record/13369},
}