<p>Chlorophyll fluorescence is a commonly used indicator of photosynthetic capacity. Crassulacean acid metabolism (CAM) plants absorb CO<sub>2</sub> during the night, but nighttime gas exchange alone does not readily represent CAM. This study was conducted to determine how light levels, daytime electron transport rate (ETR), and nighttime CO<sub>2</sub> uptake are related. <i>Phalaenopsis</i> Queen Beer ‘Mantefon’ clones were treated with a combination of three light intensity levels of 50, 100, and 200 µmol∙m<sup>-2</sup>∙s<sup>-1</sup> and three daylengths: 8&#xa0;h, 12&#xa0;h, 16&#xa0;h, resulting in daily light integrals (DLI) between 1.44 and 11.52&#xa0;mol∙m<sup>-2</sup>∙d<sup>-1</sup>. Daytime ETR linearly increased with increasing DLI levels; however, nighttime CO<sub>2</sub> uptake reached saturation point around 6&#xa0;mol∙m<sup>-2</sup>∙d<sup>-1</sup>, and then decreased. As a result, daytime ETR and nighttime CO<sub>2</sub> uptake were linearly correlated within 1.44 to 5.76&#xa0;mol∙m<sup>-2</sup>∙d<sup>-1</sup> DLI levels in this study. Under 12&#xa0;h of daylength, despite the higher DLI level and ETR values, the amounts of nighttime malic acid accumulation in 200 µmol∙m<sup>-2</sup>∙s<sup>-1</sup> treatment were similar to those in 100 µmol∙m<sup>-2</sup>∙s<sup>-1</sup> treatment. On the following day, when all plants were exposed to uniform light conditions of 100 µmol∙m<sup>-2</sup>∙s<sup>-1</sup>, they exhibited identical ETR values, despite significant differences in CO<sub>2</sub> uptake rates observed in some plants the previous night. These results indicated that the daytime DLI level is a major factor for nighttime CO<sub>2</sub> uptake, but DLI levels over a specific range have minimal effects on the carbon-gaining of CAM orchid <i>Phalaenopsis</i>.</p>

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Diel cycle of crassulacean acid metabolism in response to daily light integral levels in Phalaenopsis

  • Su Yong Shim,
  • Nam Hyun Im,
  • Hyo Beom Lee

摘要

Chlorophyll fluorescence is a commonly used indicator of photosynthetic capacity. Crassulacean acid metabolism (CAM) plants absorb CO2 during the night, but nighttime gas exchange alone does not readily represent CAM. This study was conducted to determine how light levels, daytime electron transport rate (ETR), and nighttime CO2 uptake are related. Phalaenopsis Queen Beer ‘Mantefon’ clones were treated with a combination of three light intensity levels of 50, 100, and 200 µmol∙m-2∙s-1 and three daylengths: 8 h, 12 h, 16 h, resulting in daily light integrals (DLI) between 1.44 and 11.52 mol∙m-2∙d-1. Daytime ETR linearly increased with increasing DLI levels; however, nighttime CO2 uptake reached saturation point around 6 mol∙m-2∙d-1, and then decreased. As a result, daytime ETR and nighttime CO2 uptake were linearly correlated within 1.44 to 5.76 mol∙m-2∙d-1 DLI levels in this study. Under 12 h of daylength, despite the higher DLI level and ETR values, the amounts of nighttime malic acid accumulation in 200 µmol∙m-2∙s-1 treatment were similar to those in 100 µmol∙m-2∙s-1 treatment. On the following day, when all plants were exposed to uniform light conditions of 100 µmol∙m-2∙s-1, they exhibited identical ETR values, despite significant differences in CO2 uptake rates observed in some plants the previous night. These results indicated that the daytime DLI level is a major factor for nighttime CO2 uptake, but DLI levels over a specific range have minimal effects on the carbon-gaining of CAM orchid Phalaenopsis.