Carbon Assimilation Calculators
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Calvin Cycle (C3 Carbon Fixation)
3 stages: Carboxylation: CO₂ + RuBP (5C) → 2 × 3-PGA (3C); catalyzed by Rubisco. Reduction: 3-PGA → G3P using ATP + NADPH from light reactions. Regeneration: G3P → RuBP using ATP. Net: 3 CO₂ + 9 ATP + 6 NADPH → 1 G3P (triose phosphate).
C4 Photosynthesis
CO₂ first fixed by PEP carboxylase in mesophyll → 4-carbon acids → transferred to bundle sheath cells → decarboxylated → high local CO₂ → Rubisco operates efficiently with minimal photorespiration. Examples: maize, sorghum, sugarcane. Higher WUE and NUE than C3.
CAM Plants
Stomata open at night → CO₂ fixed by PEP carboxylase → stored as malate → released to Rubisco in daytime with closed stomata. Minimizes water loss. Examples: cacti, agave, pineapple.
Measurement
LICOR-6800 gas exchange system: measures net assimilation rate A (μmol CO₂ m⁻² s⁻¹). C3 A_max: 20–30 μmol m⁻² s⁻¹; C4: 40–60 μmol m⁻² s⁻¹.
Glossary
Frequently Asked Questions
Carbon assimilation = conversion of atmospheric CO₂ into organic carbon by photosynthesis. Calvin cycle (C3 pathway): (1) Carboxylation: Rubisco catalyzes CO₂ + RuBP (5C) → 2 molecules of 3-phosphoglycerate (3-PGA, 3C). (2) Reduction: 3-PGA reduced to G3P (glyceraldehyde-3-phosphate) using ATP and NADPH from light reactions. (3) Regeneration: most G3P regenerates RuBP using ATP, maintaining the cycle. Net: 6 turns fix 6 CO₂ → 1 net glucose; requires 18 ATP + 12 NADPH per glucose.
C3 (most plants — wheat, rice, soybeans, most trees): CO₂ fixed directly by Rubisco → first stable product is 3-PGA (3-carbon). Rubisco's oxygenase activity causes photorespiration, wasting energy, especially at high temperatures and low CO₂. C4 (maize, sorghum, sugarcane): CO₂ first fixed by PEP carboxylase in mesophyll → 4-carbon compounds → transported to bundle sheath cells → released at high concentration near Rubisco. Virtually eliminates photorespiration. Better in hot, bright, dry conditions. CAM (cacti, agave, pineapple, orchids): stomata open at night to fix CO₂ as malate (stored in vacuoles); stomata closed during day; stored CO₂ released to Rubisco during daylight. Extremely water-efficient — suited to deserts.
Gas exchange analysis using an infrared gas analyzer (IRGA): The LICOR-6800 or LI-6400 clamps around a leaf in a cuvette; CO₂ and H₂O concentrations measured in air flowing into and out of the chamber. Net assimilation rate (A) = CO₂ fixed per unit leaf area per second (μmol CO₂ m⁻² s⁻¹). Simultaneously measures transpiration (E) and stomatal conductance (gs). A/Ci curve: vary CO₂ concentration inside the chamber → reveals Rubisco capacity (Vcmax) and electron transport capacity (Jmax). Typical A_max: C3 crops 20–30 μmol CO₂ m⁻² s⁻¹; C4 crops 40–60. At ecosystem scale: eddy covariance towers measure net ecosystem exchange (NEE) of CO₂.
Photorespiration occurs when Rubisco fixes O₂ instead of CO₂ (its oxygenase activity). Rubisco + O₂ + RuBP → phosphoglycolate (2C) + 3-PGA; phosphoglycolate is toxic and must be recycled in a multi-step process (the photorespiratory pathway) involving the chloroplast, peroxisome, and mitochondria. Energy cost: photorespiration releases previously fixed CO₂ and consumes ATP + NADPH without net carbon gain. At current atmospheric CO₂ levels (420 ppm) and 25°C: photorespiration reduces C3 photosynthesis by ~25%. At higher temperatures: O₂ competes more effectively → larger loss. C4 and CAM plants avoid photorespiration by concentrating CO₂ near Rubisco, making them far more efficient under heat and water stress.