Ehleringer James
Department of Biology, University of Utah, 84112, Salt Lake City, UT, USA.
Oecologia. 1983 Mar;57(1-2):107-112. doi: 10.1007/BF00379568.
Basic photosynthetic and water relations characteristics in relation to soil water availability were investigated in Amaranthus palmeri, a common C summer annual of the Sonoran Desert. Under conditions of high soil water availability, photosynthetic capacity exceeded 70 μmol CO m s at a leaf temperature optimum of 42°C, and photosynthesis was not light saturated at an irradiance of 2.0 mmol m s (400-700 nm). Leaves of A. palmeri exhibited diaheliotropic movements, allowing them to take advantage of their high photosynthetic capacity. In response to a long term drought cycle, both photosynthetic rate and leaf conductance to water vapor decreased, reaching minima at an approximate leaf water potential of-2.9 MPa. Active leaf osmotic adjustment appeared to play an important role in allowing leaves to maintain gas exchange activities down to these low leaf water potentials. The photosynthetic rate became light saturated at the lower leaf water potentials. Although the two parameters decreased in concert, the decreased photosynthetic rate was not due to increased stomatal diffusion limitations, since intercellular CO concentrations remained constant over the range of leaf water potentials. Instead it appeared that during the drought cycle, both intrinsic photosynthetic capacity and leaf protein content decreased as well. These results suggested a coordination of gas exchange parameters during long term drought such that the intercellular CO concentration remained constant.
对索诺兰沙漠常见的C4一年生夏季植物帕尔默苋(Amaranthus palmeri)与土壤水分有效性相关的基本光合和水分关系特征进行了研究。在高土壤水分有效性条件下,叶片温度最适为42°C时,光合能力超过70 μmol CO₂ m⁻² s⁻¹,且在2.0 mmol m⁻² s⁻¹(400 - 700 nm)的辐照度下光合作用未达到光饱和。帕尔默苋的叶片表现出向日运动,使其能够利用其高光合能力。响应长期干旱周期,光合速率和叶片对水蒸气的导度均下降,在叶片水势约为 -2.9 MPa时达到最小值。活跃的叶片渗透调节似乎在使叶片在这些低叶片水势下维持气体交换活动中起重要作用。在较低的叶片水势下光合速率达到光饱和。尽管这两个参数协同下降,但光合速率下降并非由于气孔扩散限制增加,因为在叶片水势范围内细胞间CO₂浓度保持恒定。相反,在干旱周期中,内在光合能力和叶片蛋白质含量似乎也下降了。这些结果表明在长期干旱期间气体交换参数的协调,使得细胞间CO₂浓度保持恒定。