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Comprehensive vocabulary flashcards reviewing the biochemical pathways of C3, C4, and CAM photosynthesis, photorespiration, anatomical specializations, and the greenhouse effect.
Photorespiration
A metabolic pathway occurring when Rubisco oxygenates RuBP instead of fixing CO2, producing 2-phosphoglycolate; it consumes O2, ATP, and NADPH while releasing CO2 without producing sugar, reducing photosynthetic efficiency by up to 50% on hot, dry days.
2-Phosphoglycolate
A two-carbon product formed when Rubisco reacts with O2 during photorespiration that must be broken down by the plant using O2, ATP, and NADPH.
C3 Plants
Plant species comprising approximately 85% of all plant species (>330,000 species) whose initial carbon fixation product is the 3-carbon molecule 3-phosphoglycerate (3PG); they are prone to photorespiration in hot, dry environments.
3-Phosphoglycerate (3PG)
A 3-carbon (3C) molecule formed in C3 plants when Rubisco combines CO2 with ribulose 1,5-bisphosphate (RuBP).
C4 Plants
A group of over 8,000 plant species (including corn, sugar cane, and some grasses) that evolved independently at least 61 times and utilize anatomical and biochemical adaptations to fix CO2 into a 4-carbon compound, minimizing photorespiration.
Phosphoenolpyruvate (PEP)
A 3-carbon (3C) molecule that acts as the initial carbon acceptor in C4 and CAM mesophyll cells, reacting with CO2 to produce oxaloacetate.
PEP Carboxylase
An enzyme in C4 and CAM plants that catalyzes the addition of CO2 to phosphoenolpyruvate (PEP); it possesses a higher affinity for CO2 than Rubisco and does not bind O2.
Oxaloacetate
The initial 4-carbon (4C) product of carbon fixation synthesized by PEP carboxylase in C4 and CAM photosynthetic pathways.
Malate
A 4-carbon (4C) organic acid formed from oxaloacetate that functions as a "CO2 pump" by transporting carbon to bundle-sheath cells in C4 plants or into vacuoles in CAM plants.
Bundle-Sheath Cells
Specialized cells encircling the vascular bundles of C4 leaves where malate releases concentrated CO2 to Rubisco for the Calvin cycle, away from atmospheric oxygen.
Mesophyll Cells (in C4 Plants)
Photosynthetic leaf cells where initial CO2 fixation by PEP carboxylase takes place to produce oxaloacetate and malate, physically separated from the Calvin cycle.
Spatial Separation of Steps
The structural mechanism in C4 photosynthesis where preliminary carbon fixation by PEP carboxylase occurs in mesophyll cells, whereas decarboxylation and the Calvin cycle occur separately in bundle-sheath cells.
Pyruvate Regeneration (in C4 Pathway)
The transport of 3-carbon (3C) pyruvate from bundle-sheath cells back to mesophyll cells, where it is converted back into PEP using ATP.
Water-Use Efficiency (C4 vs. C3 Plants)
The physiological benefit allowing C4 plants to keep stomata closed more frequently to conserve water in hot/dry environments, requiring 31 less water than C3 plants.
Crassulacean Acid Metabolism (CAM)
An alternate carbon fixation pathway found in approximately 16,000 plant species (mostly succulents and cacti) that uses temporal separation to conserve water, consuming roughly 201 the water of C3 plants.
Temporal Separation of Steps
The timing-based adaptation in CAM plants where stomata open at night to fix CO2 into organic acids, and close during the day to prevent water loss while CO2 is released to the Calvin cycle.
Malic Acid Vacuolar Storage
The nighttime accumulation of malic acid inside cell vacuoles of CAM plants, which is exported during daylight to supply CO2 to the Calvin cycle when ATP and NADPH are available.
Greenhouse Effect
The planetary warming process where the atmosphere allows short-wavelength infrared and visible light to pass through, but greenhouse gases absorb and re-emit trapped long-wavelength infrared radiation back to Earth.
Greenhouse Gases
Atmospheric gases—primarily carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O)—that enhance heat retention by re-radiating thermal energy toward Earth's surface.
Mauna Loa Observatory
A research station in Hawaii whose continuous monitoring through the Scripps CO2 Program documented atmospheric CO2 concentrations rising from around 315ppm in the late 1950s to over 420ppm by May 2024.