Faculty of Agriculture and Environment, The University of Sydney, Sydney, NSW, 2570, Australia,
Oecologia. 2013 Oct;173(2):375-85. doi: 10.1007/s00442-013-2640-9. Epub 2013 Mar 27.
The definition of photosynthetically active radiation (Q) as the visible waveband (λ 400-700 nm) is a core assumption of much of modern plant biology and global models of carbon and water fluxes. On the other hand, much research has focused on potential mutation and damage to leaves caused by ultraviolet (UV) radiation (280-400 nm), and anatomical and physiological adaptations that help avoid such damage. Even so, plant responses to UV-A are poorly described and, until now, photosynthetic utilization of UV-A has not been elucidated under full light conditions in the field. We found that the UV-A content of sunlight increased photosynthetic rates in situ by 12% in Pimelea ligustrina Labill., a common and indigenous woody shrub of alpine ecosystems of the Southern Hemisphere. Compared to companion shrubs, UV-A-induced photosynthesis in P. ligustrina resulted from reduced physical and chemical capacities to screen UV-A at the leaf surface (illustrated by a lack of cuticle and reduced phenol index) and the resulting ability of UV-A to excite chlorophyll (Chl) a directly, and via energy provided by the carotenoid lutein. A screening of 55 additional sub-alpine species showed that 47% of the plant taxa also display Chl a fluorescence under UV-A. If Chl a fluorescence indicates potential for photosynthetic gain, continued exclusion of UV-A from definitions of Q in this ecosystem could result in underestimates of measured and modeled rates of photosynthesis and miscalculation of potential for carbon sequestration. We suggest that carbon gain for alpine environs across the globe could be similarly underestimated given that UV-A radiation increases with altitude and that the frequently dominant herb and grass life-forms often transmit UV-A through the epidermis.
光合有效辐射(Q)的定义为可见光波段(λ 400-700nm),这是现代植物生物学和全球碳和水通量模型的核心假设。另一方面,许多研究集中在紫外线(UV)辐射(280-400nm)对叶片可能造成的突变和损伤上,以及帮助避免这种损伤的解剖和生理适应。即便如此,植物对 UV-A 的反应仍描述不足,到目前为止,在野外的全光照条件下,尚未阐明植物对 UV-A 的光合利用。我们发现,在南半球高山生态系统中常见的本土木本灌木 Pimelea ligustrina Labill. 中,阳光中的 UV-A 含量使原地光合作用速率提高了 12%。与伴生灌木相比,P. ligustrina 中由 UV-A 诱导的光合作用是由于叶片表面减少了对 UV-A 的物理和化学屏蔽能力(表现为缺乏角质层和降低的酚指数),以及由此产生的 UV-A 直接激发叶绿素(Chl)a 的能力,以及叶黄素提供的能量。对 55 种额外的亚高山物种的筛选表明,47%的植物类群在 UV-A 下也显示出 Chl a 荧光。如果 Chl a 荧光表明有潜在的光合增益,那么在这个生态系统中继续将 UV-A 排除在 Q 的定义之外,可能会导致对光合作用的实测和模拟速率的低估,以及对碳封存潜力的错误计算。我们认为,由于 UV-A 辐射随海拔升高而增加,并且频繁占主导地位的草本和草类生命形式通常通过表皮传递 UV-A,因此全球高山环境的碳增益也可能被低估。