Environmental effects on photosynthesis of C3 plants : scaling up from electron transport to the canopy (study case: Glycine max L. Merr)
Date
2002
Authors
June, Tania
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Atmospheric CO₂ concentration is expected to rise from its current level of
354 ppm to 530 ppm by the year 2050 and 700 ppm by the year 2100 (Watson et al.,
1990). This change in CO₂ concentration (and other infra-red absorbing gases) in the
atmosphere are expected to produce a greenhouse warming of the global surface of 3
to 4 °C by 2100 (Bretherton et al., 1990). Predicting how plants will respond to these
changes is very important in understanding the impacts of atmospheric change on
both natural ecosystems and crop growth. Photosynthesis is the process by which
plants both sense and respond to change in atmospheric CO₂ concentration, and
hence, understanding how this process is affected by rising atmospheric CO₂ and
accociated climate change is very important.
Farquhar & von Caemmerer (1980) have shown that at steady state, the
responses of C₃ leaf photosynthesis CO₂ uptake to light, temperature and ambient
CO₂ concentration can be described by the biochemical properties of just two steps in
the process, the carboxylation reaction and the regeneration of the acceptor for
carboxylation. This mechanistic model, has been widely validated as an accurate
predictor of photosynthetic carbon uptake by leaves with variation in environmental
conditions. However, the description of the light and temperature dependencies of
most parameters remains empirical and needs parameterisation.
This thesis examines the effects of change in temperature, [CO₂], light
intensity and nitrogen nutrition on photosynthesis, and parameters used in the
modelling of photosynthesis in a C₃ plants, i.e. soybean (Glycine max L. Merr.). The
parameters examined are those used in the mechanistic C₃ leaf-photosynthesis
models of Farquhar et al. (1980) and Farquhar & von Caemmerer (1982), i.e. Vcmax
(maximum rate of Rubisco activity in the leaf), lmax (potential electron transport
rate), Rct (dark respiration), a2 (quantum yield of electron transport) and e (the
curvature factor of the light response curve).
Experiments involved gas exchange and fluorescence techniques on plants
grown at different temperature, [CO₂], light intensity and nitrogen nutrient
concentration in a controlled growth chamber. Short-term responses of
photosynthesis and values for derived parameters from plant material grown at
different controlled environmental conditions, are presented in Chapters 2, 3, and 4 and discussed in terms of methods used and comparison with other published data.
The effect of wall conductance on the derived parameters was examined in quite an
extent in Chapter 5. Long-term acclimation responses to CO₂ concentration and
temperature is examined in Chapter 2 and 3 and the parameter derived from these
analysis are used in Chapter 5 for a simulation of temperature response of the rate of
CO₂ assimilation for various temperature growth acclimation. Chapter 6 shows the
scaling up of models used and parameters obtained at the leaf level to the canopy
level using the sun-shade model of de Pury & Farquhar ( 1997) and big-leaf model of
Lloyd & Farquhar (1996). It presents algorithm for calculating diurnal canopy
assimilation rate given parameters of the single leaf light and CO₂ concentration
responses, the canopy extinction coefficient for light and nitrogen, canopy leaf area
index, nitrogen concentration at the top of the canopy, daily solar irradiance and daily
maximum and minimum temperatures. The simulation was run for Muara
Climatology Station in Bogor, Indonesia (6.67 °S, 106.75 °E), where the fraction of
diffuse irradiance is remarkably high (on average 0.64 for 1978). This chapter
discusses the importance of diffuse fraction of irradiance in canopy assimilation rate
and efficiency. Chapter 7 shows general conclusion of the manuscript and the
applicability of the approach used for further work.
Some important results that can be extracted from the thesis are as follows :
(1) Long-term acclimation of Vcmax and lmax occurred for plants grown at different
temperature. The parameter derived is sensitive to whether wall conductance is
assumed finite or infinite;
(2) The decline in electron transport rate after reaching its optimum temperature and
up to 43 °C is reversible if exposure is of short duration;
(3) A new and simpler empirical formulation for the rate of electron transport as a
function of temperature is developed. This new equation describes the short-term
temperature response quite well, and can be used to analyze acclimation to
growth temperature;
(4) The light gradient developed within the leaf during growth in the chamber affects
the value of the curvature factor of the leaf's light response of photosynthesis
when measured using conventional gas exchange system and hence affects the
derived parameters a2 and Jmax· It is concluded that much of the curvature at the leaf level may result from a 'mismatch' between the profiles of light intensity and
electron transport capacity within the leaf;
(5) The fraction of diffuse irradiance is important in determining canopy assimilation
efficiency. Efficiency (denoted as Light Use Efficiency) increases as the diffuse
fraction of irradiance increases.
(6) The difference between sun-shade and big-leaf model is negligible when canopy
assimilation simulation was run under a high fraction of diffuse irradiance. The
difference was significant under a very bright atmospheric condition.
(7) The estimate of the optimum fraction of diffuse irradiance (fD) for maximum
canopy assimilation rate is possible by using the sun-shade model. It is
impossible to calculate with big-leaf model which would give optimum fD of
zero.
(8) The optimum fraction of diffuse irradiance, which gives highest canopy net
assimilation rate at the chosen site, was around 30 %, with optimum LAI of 4.
Overall, the flow of the work being carried out and reported in this
manuscript is shown in the diagram below. It shows the equations used at the leaf
level, parameterisation at the leaf level and the scaling up to the canopy level.
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