Predicting leaf gas exchange and δ13C responses to the past 30000 years of global environmental change
Article first published online: 28 APR 2006
Volume 128, Issue 3, pages 425–433, November 1994
How to Cite
BEERLING, D. J. (1994), Predicting leaf gas exchange and δ13C responses to the past 30000 years of global environmental change. New Phytologist, 128: 425–433. doi: 10.1111/j.1469-8137.1994.tb02988.x
- Issue published online: 28 APR 2006
- Article first published online: 28 APR 2006
- (Received 10 May 1994; accepted 1 July 1994)
- stomatal conductance;
- stable carbon isotopes;
- global change
Theoretical developments in our understanding of leaf gas exchange processes and carbon isotope composition (δ13C) mean that it should now be possible to model their responses to global environmental change. Such a model would be of use for process-based interpretations of historical changes in leaf δ13C and for understanding the global stable carbon isotope balance. This paper describes the development and validation of a model towards this aim. The resulting model is used to simulate changes in leaf photosynthesis, stomatal conductance and δ13C of limber pine (Pinus flexilis) in response to the past 30000 y of global environmental change. The predictions of needle δ13C are in line with reported measurements of δ13C from fossilized Pinus flexilis needles preserved in packrat middens in western USA. Leaf gas exchange predictions show that the increased water use efficiency (WUE) of these trees growing in present-day environments, relative to the past, was brought about through an increase in photosynthetic rates and a decrease in stomatal conductance. This contrasts with the explanation of the recent (past 200 y) increase in the WUE of temperate and Mediterranean ecosystems inferred from δ13C measurements which are predicted by the model to have arisen largely by a decrease in stomatal conductance in response to increases in the concentration of atmospheric CO2 since the pre-industrial era.
The model as described offers the potential to contribute to our understanding of vegetation effects on the global carbon isotope balance during the glacial periods, and therefore to provide a further constraint on the carbon cycle models used to explain the low concentrations of atmospheric CO2 at these times.