The Department of Geography and Environmental Development, Ben Gurion University of the Negev, David Ben Gurion Blvd 1, Be'er Sheva, P.O.B. 653, Israel.
The Department of Plant and Environmental Sciences, Weizmann Institute of Science, Herzl St 234, Rehovot, P.O.B 26, Israel.
Tree Physiol. 2023 May 12;43(5):794-804. doi: 10.1093/treephys/tpad012.
Phosphorus (P) availability to forest trees is often limited by local soil conditions that increase its fixation to soil minerals. In certain regions, atmospheric-P inputs can compensate for low soil-P availability. Among atmospheric-P sources, desert dust is the most dominant. However, the effects of desert dust on P nutrition and its uptake mechanisms by forest trees are currently unknown. We hypothesized that forest trees that naturally grow on P-poor soils or soils with high soil-P fixation capacity can acquire P from desert dust deposited on their leaves via direct foliar uptake, bypassing the soil, thus promoting tree growth and productivity. We performed a controlled greenhouse experiment with three forest tree species: Palestine Oak (Quercus calliprinos) and Carob (Ceratonia siliqua), native to the NE edge of the Saharan desert, and Brazilian peppertree (Schinus terebinthifolius), native to the Atlantic Forest in Brazil, which is located on the western part of the trans-Atlantic Saharan dust route. To simulate natural dust deposition events, the trees had desert dust applied directly upon their foliage and were monitored for growth and final biomass, P levels, leaf surface pH and the rate of photosynthesis. The dust treatment increased the P concentration significantly by 33-37% in Ceratonia and Schinus trees. On the other hand, trees that received the dust displayed a 17-58% reduction in biomass, probably related to particle coverage of the leaf surface that inhibited photosynthesis by 17-30%. Overall, our findings show that direct P uptake from desert dust can be an alternative P uptake pathway for multiple tree species under P-deficient conditions, with implications for forest trees' P economy.
磷(P)在森林树木中的可用性通常受到增加其与土壤矿物质固定的局部土壤条件的限制。在某些地区,大气 P 输入可以补偿土壤 P 供应不足。在大气 P 来源中,沙漠尘埃是最主要的。然而,沙漠尘埃对 P 营养的影响及其被森林树木吸收的机制目前尚不清楚。我们假设,在 P 贫瘠的土壤或土壤 P 固定能力高的地区自然生长的森林树木,可以通过直接叶片吸收从沉积在叶片上的沙漠尘埃中获取 P,绕过土壤,从而促进树木生长和生产力。我们在三个森林树种中进行了受控温室实验:巴勒斯坦栎(Quercus calliprinos)和角豆(Ceratonia siliqua),原产于撒哈拉沙漠东北边缘,和巴西椒(Schinus terebinthifolius),原产于巴西大西洋森林,位于跨大西洋撒哈拉沙漠尘埃路径的西部。为了模拟自然尘埃沉积事件,将沙漠尘埃直接施用于树木的叶片上,并监测其生长和最终生物量、P 水平、叶片表面 pH 值和光合作用速率。尘埃处理使 Ceratonia 和 Schinus 树木的 P 浓度显著增加了 33-37%。另一方面,接受尘埃处理的树木的生物量减少了 17-58%,这可能与叶片表面的颗粒覆盖有关,该覆盖通过 17-30%抑制了光合作用。总的来说,我们的发现表明,在 P 缺乏的情况下,直接从沙漠尘埃中吸收 P 可能是多种树种吸收 P 的替代途径,这对森林树木的 P 经济具有重要意义。