Differential 18O enrichment of leaf cellulose in C3 versus C4 grasses
Brent R. Helliker and James R. Ehleringer
Abstract
We show that differences in the oxygen isotope ratio of leaf water between
C3 and C4 grasses (five species of
each photosynthetic type) become less distinct as relative humidity increases,
and that 18O leaf water differences translate directly
to the oxygen isotope ratio of leaf cellulose. A conceptual model is presented
that is based on grass blade growth characteristics and observed patterns of
progressive enrichment in grasses. The Barbour and Farquhar (2000) model was
capable of explaining the oxygen isotope ratio of bulk leaf cellulose of
C3 and C4 grasses grown under a
variety of growth conditions.
Keywords: C
Functional Plant Biology 29(4) 435 - 442
(2002) doi:10.1071/PP01122





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