Bornman J F, Barnes P W, Robinson S A, Ballaré C L, Flint S D, Caldwell M M
International Institute of Agri-Food Security (IIAFS), Curtin University, Building 408, PO Box U1987, Perth, WA 6845, Australia.
Photochem Photobiol Sci. 2015 Jan;14(1):88-107. doi: 10.1039/c4pp90034k.
In this assessment we summarise advances in our knowledge of how UV-B radiation (280-315 nm), together with other climate change factors, influence terrestrial organisms and ecosystems. We identify key uncertainties and knowledge gaps that limit our ability to fully evaluate the interactive effects of ozone depletion and climate change on these systems. We also evaluate the biological consequences of the way in which stratospheric ozone depletion has contributed to climate change in the Southern Hemisphere. Since the last assessment, several new findings or insights have emerged or been strengthened. These include: (1) the increasing recognition that UV-B radiation has specific regulatory roles in plant growth and development that in turn can have beneficial consequences for plant productivity via effects on plant hardiness, enhanced plant resistance to herbivores and pathogens, and improved quality of agricultural products with subsequent implications for food security; (2) UV-B radiation together with UV-A (315-400 nm) and visible (400-700 nm) radiation are significant drivers of decomposition of plant litter in globally important arid and semi-arid ecosystems, such as grasslands and deserts. This occurs through the process of photodegradation, which has implications for nutrient cycling and carbon storage, although considerable uncertainty exists in quantifying its regional and global biogeochemical significance; (3) UV radiation can contribute to climate change via its stimulation of volatile organic compounds from plants, plant litter and soils, although the magnitude, rates and spatial patterns of these emissions remain highly uncertain at present. UV-induced release of carbon from plant litter and soils may also contribute to global warming; and (4) depletion of ozone in the Southern Hemisphere modifies climate directly via effects on seasonal weather patterns (precipitation and wind) and these in turn have been linked to changes in the growth of plants across the Southern Hemisphere. Such research has broadened our understanding of the linkages that exist between the effects of ozone depletion, UV-B radiation and climate change on terrestrial ecosystems.
在本次评估中,我们总结了关于紫外线B辐射(280 - 315纳米)以及其他气候变化因素如何影响陆地生物和生态系统的知识进展。我们确定了关键的不确定性因素和知识空白,这些因素限制了我们全面评估臭氧消耗和气候变化对这些系统的交互作用的能力。我们还评估了平流层臭氧消耗对南半球气候变化产生影响的方式所带来的生物学后果。自上次评估以来,出现了一些新的发现或见解,或者这些发现或见解得到了强化。其中包括:(1)人们越来越认识到紫外线B辐射在植物生长和发育中具有特定的调节作用,进而通过对植物抗逆性的影响、增强植物对食草动物和病原体的抵抗力以及提高农产品质量,对植物生产力产生有益影响,随后对粮食安全产生影响;(2)紫外线B辐射与紫外线A(315 - 400纳米)和可见光(400 - 700纳米)一起,是全球重要的干旱和半干旱生态系统(如草原和沙漠)中植物凋落物分解的重要驱动因素。这是通过光降解过程发生的,这对养分循环和碳储存有影响,尽管在量化其区域和全球生物地球化学意义方面存在相当大的不确定性;(3)紫外线辐射可通过刺激植物、植物凋落物和土壤中的挥发性有机化合物来促进气候变化,尽管目前这些排放的规模、速率和空间格局仍高度不确定。紫外线诱导的植物凋落物和土壤中的碳释放也可能导致全球变暖;(4)南半球的臭氧消耗通过对季节性天气模式(降水和风)的影响直接改变气候,而这些又与南半球各地植物生长的变化有关。此类研究拓宽了我们对臭氧消耗、紫外线B辐射和气候变化对陆地生态系统影响之间存在的联系的理解。
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