机构地区:[1]中国农业科学院草原研究所,呼和浩特010018 [2]内蒙古农业大学生命科学学院,呼和浩特010018 [3]内蒙古农业大学生态与环境学院,呼和浩特010018
出 处:《生态学报》2016年第21期6909-6918,共10页Acta Ecologica Sinica
基 金:内蒙古自治区自然科学基金资助项目(2015MS0305);中国科学院西部之光"人才培养"项目;中国农业科学院草原研究所科技创新工程资助项目
摘 要:为探究全球变暖对温带荒漠草原地上种群的遗传影响,对已经接受模拟增温处理6年的短花针茅草原4种不同生活型植物,即半灌木、多年生禾草、多年生杂类草和一年生植物,应用AFLP分子标记方法研究了其遗传多样性和遗传结构。结果显示,对照处理与增温处理下的木地肤、短花针茅、细叶葱、猪毛菜4种植物的多态位点百分率(PPB)分别为11.32%,11.32%;40.83%,39.91%;14.29%,13.10%;19.85%,19.12%。Nei's基因多样性指数(He)分别为0.0274,0.0259;0.0812,0.0899;0.0131,0.0084;0.0506,0.0456。Shannon's信息指数值(I)分别为0.0447,0.0430;0.1354,0.1466;0.0267,0.0182;0.0811,0.0733。分子方差分析(AMOVA)显示4种植物的变异主要来源于实验处理内部,木地肤为85.03%,短花针茅为66.35%,细叶葱为70.00%,猪毛菜为66.52%;增温处理间的变异分别占-2.81%,-5.47%,-3.60%,2.53%(P>0.05)。4种植物增温处理与变异程度之间在统计学上并无相关性。研究表明虽然短时间的模拟增温并不足以使4种生活型植物种群遗传多样性和遗传结构发生显著变化,但相对于3种多年生植物,一年生植物猪毛菜更容易受到增温影响。多年生和一年生植物对增温具有不同的遗传响应。Climate is the most important factor that determines vegetation types and the distribution of species, and, accordingly, these features are two of the most prominent indicators of climate change. Currently, scientists generally agree that climate change will inevitably lead to changes in plant community structure and function, and if this change continues, the effects will be profound and enduring. Existing research shows that simulated warming causes an increase in biomass in Deschampsia caespitosa, Carex alrofusca, and Leymus chinensis ; as climates change, these constructive species and their main companion species within a Kobresia humilis meadow have experienced an advancement in their spring phenology and a delay in their autumn phenophase. In addition, the photosynthetic rate of Deschampsia caespitosa in a Northwest Sichuan alpine meadow has increased. Although the change in stomatal conductance was irregular, a significant decrease has also been observed in the sodium, potassium, and phosphorus content of leaves. However, relatively little research has been conducted on the effects of simulated warming on the genetic structure and diversity of plant populations. Against the background of global climate change, the temperatures of the Inner Mongolian desert steppe have become unevenly elevated, with average annual temperatures increasing from 8.1℃ in the 1950s to 9.0℃ in the 1990s. The present study explores the effects of global warming on the genetics of wild forage plant populations with different life forms in desert steppe habitat, in an effort to elucidate their potential to adapt to environmental change. The study site was located in the desert steppe in Siziwangqi territory of Inner Mongolia. Suspension infrared radiators were used to create a controlled warming experiment under otherwise natural field conditions. Warming began on May 3, 2006. The average soil temperature at depths of 0, 7.5, 15, 30, and 50 cm increased by 1.32, 0.92, 0.88, 0.80, and 0.74℃, respectively, after warming for 1 y
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