Zhu Jinfang, Liu Jingtao, Li Junsheng, Zhao Caiyun, Sun Jingkuan
State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing, China.
Shandong Provincial Key Laboratory of Eco-Environmental Science for Yellow River Delta, Binzhou University, Binzhou, China.
Front Plant Sci. 2022 Jun 23;13:935025. doi: 10.3389/fpls.2022.935025. eCollection 2022.
and are two dominant shrub species on Chenier Island in the Yellow River Delta, China. Water is a restrictive factor determining the plant growth, vegetation composition, and community succession in this coastal zone. We investigated how water uptake tradeoffs of the two shrub species responded to soil water fluctuations caused by seasonal variations of precipitation. The soil water content, salinity and δO values of potential water sources (soil water in 0-20, 20-40, 40-60, and 60-100 cm soil layers, and groundwater) and plant xylem water were measured in wet (July 2013) and dry (July 2014) seasons. The IsoSource model was employed to calculate the contributions of different water sources to plant xylem water. The results showed that δO values of soil water decreased significantly with soil depth in the dry season, while increased significantly with soil depth in the wet season. In the wet season, when the soil water was abundant, mostly used the soil water from the 60-100 cm layer, while took up a mixture of groundwater and soil water from the 60-100 cm layer. In the dry season, when the soil water was depleted because of low precipitation, mainly took up a mixture of the soil water from 20 to 100 cm soil layers, while mainly used groundwater. and showed different ecological amplitudes of water sources during dry and wet seasons. The niche differentiation of major water sources for and demonstrated their adaptabilities to the fluctuations of soil moisture in water-limited ecosystems. Water niche differentiations of coexisting shrub species were expected to minimize their competition for limited water sources, contributing to successful coexistence and increasing the resilience of the coastal wetland ecosystem to drought.
[物种名称1]和[物种名称2]是中国黄河三角洲陈ier岛的两种优势灌木物种。水是决定该沿海地区植物生长、植被组成和群落演替的限制因素。我们研究了这两种灌木物种的水分吸收权衡如何响应降水季节变化引起的土壤水分波动。在湿润季节(2013年7月)和干旱季节(2014年7月)测量了潜在水源(0 - 20、20 - 40、40 - 60和60 - 100厘米土层的土壤水分以及地下水)和植物木质部水的土壤水分含量、盐度和δO值。采用IsoSource模型计算不同水源对植物木质部水的贡献。结果表明,干旱季节土壤水分的δO值随土壤深度显著降低,而湿润季节随土壤深度显著增加。在湿润季节,当土壤水分充足时,[物种名称1]主要利用60 - 100厘米土层的土壤水分,而[物种名称2]吸收60 - 100厘米土层的地下水和土壤水的混合物。在干旱季节,由于降水少土壤水分耗尽时,[物种名称1]主要吸收20至100厘米土层的土壤水混合物,而[物种名称2]主要利用地下水。[物种名称1]和[物种名称2]在干湿季节表现出不同的水源生态幅度。[物种名称1]和[物种名称2]主要水源的生态位分化表明它们对水分受限生态系统中土壤水分波动的适应性。共存灌木物种的水分生态位分化有望使它们对有限水源的竞争最小化,有助于成功共存并提高沿海湿地生态系统对干旱的恢复力。