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51.
玉米转录因子zmCBF1的凝胶阻滞分析 总被引:2,自引:0,他引:2
凝胶阻滞试验是分析核酸与蛋白质相互作用的有效方法,在转录因子的功能分析中得到了广泛应用。以玉米转录因子zmCBF1与顺式元件CRT的结合为例,建立了用于转录因子分析的GRA/EMSA实验体系,并对其在应用中可能出现的问题进行了分析。 相似文献
52.
大兴安岭森林草原过渡带白桦及主要草本植物生态位关系的研究 总被引:10,自引:3,他引:10
以白桦、日阴菅及其它主要草本植物的个体数量为指标,分析了各植物种群在土壤有机质,速效P和pH值3个资源维上的生态位宽度和生态位重叠及其在不同海拔条件下的变化规律。日阴菅生态位宽度随海拔升高而增大,其余植物种类在有机质资源维上的生态位宽度,大都是以中等海拔(800m)的样带最宽,而在速效P资源维上,又以中等海拔的样带为最窄,由于高海拔及相应低气温在某种程度上限制了植物种群在土壤有机质和速效P的利用,主要植物种对之间在这两个资源维上的生态位重叠以高海拔(950m)样带为最小,在土壤pH值资源维上,溪荪与其它主要植物种间的生态位重叠皆以低海拔(650m)样带为最小,可能是其特殊的环境组合迫使溪荪发生了生态位移动,大多数种对在土壤有机质,速效P和pH值3个资源维上都以海拔800m的样带生态位重叠最大。 相似文献
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54.
Shrubline but not treeline advance matches climate velocity in montane ecosystems of south‐central Alaska
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Roman J. Dial T. Scott Smeltz Patrick F. Sullivan Christina L. Rinas Katriina Timm Jason E. Geck S. Carl Tobin Trevor S. Golden Edward C. Berg 《Global Change Biology》2016,22(5):1841-1856
Tall shrubs and trees are advancing into many tundra and wetland ecosystems but at a rate that often falls short of that predicted due to climate change. For forest, tall shrub, and tundra ecosystems in two pristine mountain ranges of Alaska, we apply a Bayesian, error‐propagated calculation of expected elevational rise (climate velocity), observed rise (biotic velocity), and their difference (biotic inertia). We show a sensitive dependence of climate velocity on lapse rate and derive biotic velocity as a rigid elevational shift. Ecosystem presence identified from recent and historic orthophotos ~50 years apart was regressed on elevation. Biotic velocity was estimated as the difference between critical point elevations of recent and historic logistic fits divided by time between imagery. For both mountain ranges, the 95% highest posterior density of climate velocity enclosed the posterior distributions of all biotic velocities. In the Kenai Mountains, mean tall shrub and climate velocities were both 2.8 m y?1. In the better sampled Chugach Mountains, mean tundra retreat was 1.2 m y?1 and climate velocity 1.3 m y?1. In each mountain range, the posterior mode of tall woody vegetation velocity (the complement of tundra) matched climate velocity better than either forest or tall shrub alone, suggesting competitive compensation can be important. Forest velocity was consistently low at 0.1–1.1 m y?1, indicating treeline is advancing slowly. We hypothesize that the high biotic inertia of forest ecosystems in south‐central Alaska may be due to competition with tall shrubs and/or more complex climate controls on the elevational limits of trees than tall shrubs. Among tall shrubs, those that disperse farthest had lowest inertia. Finally, the rapid upward advance of woody vegetation may be contributing to regional declines in Dall's sheep (Ovis dalli), a poorly dispersing alpine specialist herbivore with substantial biotic inertia due to dispersal reluctance. 相似文献
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Greenhouse gas buildup, sardines, submarine eruptions and the possibility of abrupt degradation of intense marine upwelling ecosystems 总被引:1,自引:1,他引:1
Widespread hypoxia and massive eruptions of noxious, radiatively active gases currently characterize the world's strongest eastern ocean upwelling zone. Theory, modelling results and observations suggest that the world's coastal upwelling zones will undergo progressive intensification in response to greenhouse gas buildup. This presents the prospect of progressive development of similarly degraded marine ecosystems in additional regions and of a contributing feedback loop involving associated additions to the global buildup rate of greenhouse gases, resulting further increases in upwelling intensity, creation of additional sources of greenhouse gas emissions, and so on. Abundant sardine stocks might be a mitigating factor opposing the process. 相似文献
57.
黄孢原毛平革菌(Phanerochaetechrysosporium)能产生降解木质素的胞外木质素过氧化物酶(LIP) 和锰过氧化物酶( MnP)同工酶。为研究LIP基因的转录调控机理, 对LIP基因( GLG3 和GLG6) 的5′端上游序列进行亚克隆, 获得6 个亚克隆DNA 片段, 然后应用凝胶迁移率变动分析技术筛选能与菌体蛋白质专一性结合的DNA片段。结果表明: LIP基因GLG6 的5′端上游有一个约670 bp 的DNA 片段能与总蛋白质组分专一性结合, 其核苷酸序列分析表明该片段可能含有蛋白质结合的序列特征。研究结果初步显示, 黄孢原毛平革菌可能存在有与LIP基因上游某些顺式调控元件相互作用的蛋白质, 调控着LIP基因的转录表达。 相似文献
58.
在神农架山地不同海拔高度进行领春木(Euptelea pleiospermum)种子萌发实验和萌发后实生幼苗的存活状况研究,模拟气候变化对领春木分布的潜在影响.结果显示:(1)林窗内种子萌发率显著高于林下,林下的幼苗全部死亡;(2)在领春木的分布上限(2090 m)和以上区域种子萌发率高,且幼苗死亡率低,在领春木的分布下限(900 m)和以下区域种子萌发率低,且除620 m阳坡林下以外,幼苗均全部死亡;(3)种源对领春木种子萌发率和幼苗死亡率均无显著影响;(4)冬季播种的种子比春季播种种子萌发率低,萌发后幼苗死亡率高.研究结果表明,珍稀植物领春木具备向高海拔地区迁移的潜能,但向高海拔的迁移扩散可能会受到一定的限制;在低海拔区域,领春木幼苗更新受到威胁,但一些小生境可以缓冲气候变暖带来的威胁. 相似文献
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60.
Hydrological regulation drives regime shifts: evidence from paleolimnology and ecosystem modeling of a large shallow Chinese lake 总被引:2,自引:0,他引:2
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Xiangzhen Kong Qishuang He Bin Yang Wei He Fuliu Xu Annette B. G. Janssen Jan J. Kuiper Luuk P. A. van Gerven Ning Qin Yujiao Jiang Wenxiu Liu Chen Yang Zelin Bai Min Zhang Fanxiang Kong Jan H. Janse Wolf M. Mooij 《Global Change Biology》2017,23(2):737-754
Quantitative evidence of sudden shifts in ecological structure and function in large shallow lakes is rare, even though they provide essential benefits to society. Such ‘regime shifts’ can be driven by human activities which degrade ecological stability including water level control (WLC) and nutrient loading. Interactions between WLC and nutrient loading on the long‐term dynamics of shallow lake ecosystems are, however, often overlooked and largely underestimated, which has hampered the effectiveness of lake management. Here, we focus on a large shallow lake (Lake Chaohu) located in one of the most densely populated areas in China, the lower Yangtze River floodplain, which has undergone both WLC and increasing nutrient loading over the last several decades. We applied a novel methodology that combines consistent evidence from both paleolimnological records and ecosystem modeling to overcome the hurdle of data insufficiency and to unravel the drivers and underlying mechanisms in ecosystem dynamics. We identified the occurrence of two regime shifts: one in 1963, characterized by the abrupt disappearance of submerged vegetation, and another around 1980, with strong algal blooms being observed thereafter. Using model scenarios, we further disentangled the roles of WLC and nutrient loading, showing that the 1963 shift was predominantly triggered by WLC, whereas the shift ca. 1980 was attributed to aggravated nutrient loading. Our analysis also shows interactions between these two stressors. Compared to the dynamics driven by nutrient loading alone, WLC reduced the critical P loading and resulted in earlier disappearance of submerged vegetation and emergence of algal blooms by approximately 26 and 10 years, respectively. Overall, our study reveals the significant role of hydrological regulation in driving shallow lake ecosystem dynamics, and it highlights the urgency of using multi‐objective management criteria that includes ecological sustainability perspectives when implementing hydrological regulation for aquatic ecosystems around the globe. 相似文献