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Influence of Carbonic Anhydrase Activity in Terrestrial Vegetation on the 18O Content of Atmospheric CO2
Jim Gillon,Dan Yakir*
The oxygen-18 (18O) content of atmospheric carbon
dioxide (CO2) is an important indicator of
CO2 uptake on land. It has generallybeen assumed that
during photosynthesis, oxygen in CO2 reachesisotopic
equilibrium with oxygen in 18O-enriched water in leaves. We
show, however, large differencesin the activity of carbonic anhydrase
(which catalyzes CO2 hydrationand 18O exchange
in leaves) among major plant groups that cause variationsin the extent
of 18O equilibrium (eq). A clear distinction
in eq between C3 treesand shrubs, and
C4 grasses makes atmospheric C18OO a
potentially sensitive indicator to changes in C3 and
C4 productivity.We estimate a global mean
eq value of ~0.8, which reasonablyreconciles
inconsistencies between 18O budgets of atmospheric
O2 (Dole effect) and CO2.
Department of Environmental Science and Energy Research, Weizmann
Institute of Science, Rehovot 76100, Israel.
*
To whom correspondence should be addressed. E-mail:
dan.yakir{at}weizmann.ac.il
The editors suggest the following Related Resources on Science sites:
In Science Magazine
PERSPECTIVES
F. I. Woodward (30 March 2001) Science291 (5513), 2562.
[DOI: 10.1126/science.1059472] |Summary »|Full Text »
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