Atmospheric CO₂ over 800,000 years — with photosynthesis thresholds
Ice-core + instrumental record. Shaded zones show where photosynthesis is impaired or impossible.
Photosynthesis reference levels (plant physiology, not claims)
~150 ppm (red dashed) —
C3 photosynthesis severe impairment threshold.
Below ~150–200 ppm most C3 plants cannot sustain net photosynthesis.
Source: Ward et al. 2005, PNAS; Sage 1995; Wikipedia “CO₂ in Earth’s atmosphere” citing peer-reviewed literature.
~50 ppm (orange dashed) —
C3 CO₂ compensation point. Below this, respiration exceeds photosynthesis —
net carbon loss even in full sunlight. Affects ~85% of plant species (wheat, rice, most trees).
Source: Standard plant physiology; Taiz & Zeiger, Plant Physiology.
~5 ppm (green dashed) —
C4 plant CO₂ compensation point. C4 plants (corn, sugarcane, many grasses)
evolved a CO₂-concentrating mechanism ~7–5 Ma ago partly in response to
declining CO₂. They can sustain photosynthesis at near-zero atmospheric CO₂.
Source: Osborne & Beerling 2006, Phil. Trans. R. Soc. B.
Ice-core minimum ~180 ppm —
The glacial troughs sit in the C3 stress zone (150–200 ppm): plants were
severely stressed but still above the shutdown floor.
Antarctic composite: Bereiter et al. (2015) via NOAA NCEI •
Instrumental: NOAA GML Mauna Loa •
Generated by generate_photo_chart.py