2000年以来,国家在中国西南喀斯特地区开展一系列生态治理工程,该地区退化生态系统得到一定程度的恢复,而2008年开展石漠化综合治理工程以来该地区的植被覆盖和生产力如何变化尚不清楚。本研究利用遥感增强型植被指数(EVI)和总初级生产力(GPP)数据,研究2000—2015年西南喀斯特地区植被EVI年均值和GPP年总量的时空变化特征,重点探讨2008年以来石漠化综合治理工程、气候变化等因素对植被覆盖及生长的影响,进而评估石漠化综合治理工程的成效。结果表明,2000—2015年西南喀斯特地区植被EVI总体显著增加,其中2008—2015年植被EVI均值和变化率分别比2000—2007年高6.9%和85.7%,EVI显著增加的区域占西南喀斯特地区的13.4%;该区域GPP年总量亦呈显著增加趋势(20.58 g C m-2a-1)。2008—2015年气温和降水对植被EVI变化趋势的贡献仅占28.3%,退耕还林还草等生态恢复措施、大气CO2浓度、大气氮沉降的增加可能是该区域植被覆盖显著增加的主要贡献因子。在100个首批石漠化综合治理试点县中,大部分试点县植被EVI的变化趋势受非气候因子的影响,其中治理面积大的县受非气候因子的影响显著高于治理面积小的县,表明石漠化综合治理工程的实施有效地促进了试点县植被覆盖的增加。 相似文献
水分利用效率是深入理解生态系统水碳循环耦合关系的重要指标。西南高山地区是响应气候变化的重点区域,研究西南高山地区水分利用效率动态及其对气候变化的响应,对于评估区域碳水耦合关系及对全球气候变化的响应具有重要意义。应用生态系统模型CEVSA(Carbon Exchange between Vegetation,Soil,and the Atmosphere)估算了1954—2010年西南高山地区水分利用效率(Water use efficiency,WUE)的时空变化,分析了其对气候变化的响应。结果表明:(1)西南高山地区1954—2010年水分利用效率均值为1.13 g C mm-1m-2。3种主要植被类型草地、常绿针叶林和常绿阔叶林的WUE分别为1.35、1.14、0.99 g C mm-1m-2。在空间分布上,WUE与海拔显著正相关(r=0.156,P0.05),而与温度则显著负相关(r=-0.386,P0.01)。(2)在时间尺度上,1954—2010年西南高山地区整体WUE降低趋势显著(P0.01),变动区间为0.83-1.46g C mm-1m-2,平均每年下降0.006g C mm-1m-2。整体WUE年际变化与温度呈显著负相关(r=-0.727,P0.01),与降水量相关性不显著;整体WUE下降主要原因是温度上升引起的ET增加速率大于NPP增加速率。(3)1954—2010年西南高山地区3种主要植被类型草地、常绿针叶林及常绿阔叶林WUE均显著下降(P0.01),下降速度分别为-1.03×10-2、-6.17×10-3、-1.37×10-3g C mm-1m-2a-1。西南高山地区76.3%格点WUE年际变化与温度显著负相关(P0.05),34.1%格点WUE年际变化与降水量显著正相关(P0.05)。草地和常绿针叶林WUE年际变化与温度显著负相关(r=-0.889,P0.01;r=-0.863,P0.01),与降水量相关性不显著。由于西南高山地区降水较为丰富,且过去57年降水变化不显著,因此该地区WUE的时空格局主要受温度变化的影响。1954—2010年期间温度升高造成的ET增加显著高于NPP的增加是该地区WUE下降的主要原因。未来需要获取更高空间分辨率的气候、土壤、植被数据,从而更加准确和精确地模拟西南高山地区水碳循环及其耦合关系对气候变化的响应。 相似文献
Human activity has a profound effect on the global environment and caused frequent occurrence of climatic fluctuations. To survive, plants need to adapt to the changing environmental conditions through altering their morphological and physiological traits. One known mechanism for phenotypic innovation to be achieved is environment-induced rapid yet inheritable epigenetic changes. Therefore, the use of molecular techniques to address the epigenetic mechanisms underpinning stress adaptation in plants is an important and challenging topic in biological research. In this study, we investigated the impact of warming, nitrogen (N) addition, and warming+nitrogen (N) addition stresses on the cytosine methylation status of Leymus chinensis Tzvel. at the population level by using the amplified fragment length polymorphism (AFLP), methylation-sensitive amplified polymorphism (MSAP) and retrotransposon based sequence-specific amplification polymorphism (SSAP) techniques.
Methodology/Principal Findings
Our results showed that, although the percentages of cytosine methylation changes in SSAP are significantly higher than those in MSAP, all the treatment groups showed similar alteration patterns of hypermethylation and hypomethylation. It meant that the abiotic stresses have induced the alterations in cytosine methylation patterns, and the levels of cytosine methylation changes around the transposable element are higher than the other genomic regions. In addition, the identification and analysis of differentially methylated loci (DML) indicated that the abiotic stresses have also caused targeted methylation changes at specific loci and these DML might have contributed to the capability of plants in adaptation to the abiotic stresses.
Conclusions/Significance
Our results demonstrated that abiotic stresses related to global warming and nitrogen deposition readily evoke alterations of cytosine methylation, and which may provide a molecular basis for rapid adaptation by the affected plant populations to the changed environments. 相似文献
Chemical 2,3-butanediol is an important platform compound possessing diverse industrial applications. So far, it is mainly produced by using petrochemical feedstock which is associated with high cost and adverse environmental impacts. Hence, finding alternative routes (e.g., via fermentation using renewable carbon sources) to produce 2,3-butanediol are urgently needed. In this study, we report a wild-type Klebsiella sp. strain XRM21, which is capable of producing 2,3-butanediol from a wide variety of carbon sources including glucose, sucrose, xylose, and glycerol. Among them, fermentation of sucrose leads to the highest production of 2,3-butanediol. To maximize the production of 2,3-butanediol, fermentation conditions were first optimized for strain XMR21 by using response surface methodology (RSM) in batch reactors. Subsequently, a fed-batch fermentation strategy was designed based on the optimized parameters, where 91.2 g/L of 2,3-butanediol could be produced from substrate sucrose dosing in 100 g/L for three times. Moreover, random mutagenesis of stain XMR21 resulted in a highly productive mutant strain, capable of producing 119.4 and 22.5 g/L of 2,3-butanediol and ethanol under optimized fed-batch fermentation process within 65 h with a total productivity of 2.18 g/L/h, which is comparable to the reported highest 2,3-butanediol concentration produced by previous strains. This study provides a potential strategy to produce industrially important 2,3-butanediol from low-cost sucrose. 相似文献
Hyaluronan lyase from Streptococcus pneumoniae can degrade hyaluronic acid, which is one of the major components in the extracellular matrix. Hyaluronan can regulate water balance, osmotic pressure, and act as an ion exchange resin. Followed by our recent work on the catalytic reaction mechanism and substrate binding mode, we in this work further investigate the functional role of active site arginine residue, R462, in the degradation of hyaluronan. The site directed mutagenesis simulation of R462A and R462Q were modeled using a combined quantum mechanical and molecular mechanical method. The overall substrate binding features upon mutations do not have significant changes. The energetic profiles for the reaction processes are essentially the same as that in wild type enzyme, but significant activation barrier height changes can be observed. Both mutants were shown to accelerate the overall enzymatic activity, e.g., R462A can reduce the barrier height by about 2.8 kcal mol–1, while R462Q reduces the activation energy by about 2.9 kcal mol–1. Consistent with the active site model calculated using density functional theory, our results can support that the positive charge on R462 guanidino side chain group plays a negative role in the catalysis. Finally, the functional role of R462 was proposed to facilitate the formation of initial enzyme-substrate complex, but not in the subsequent catalytic degradation reaction.
The NOx input terrestrial ecosystems are increasing significantly induced by human activities, yet the understanding of the responses of carbon cycle to nitrogen deposition is still poor. The northern temperate forest ecosystems have seen the greatest changes in nitrogen inputs from atmosphere. It is necessary for us to understand how the carbon cycle would change under the nitrogen addition in temperate forests, as an important carbon sink. In this study, we present a biogeochemical process model, CEVSA2, and use this model to elucidate the key processes that may strongly influence the carbon budget response to anthropogenic nitrogen addition. The CEVSA2 model has included the effect of nitrogen on photosynthesis, carbon allocation, soil organic matter decomposition, etc. Our simulations show nitrogen addition stimulates the photosynthesis, net carbon sequestration, carbon accumulation in vegetation and soil, by contrary, the low level of nitrogen addition decreases the heterotrophical and total respiration. The long-term chronic nitrogen addition experiments show that the low and high level nitrogen addition would reduce the carbon sequestration and accumulation. The model failed to simulate the effect of nitrogen addition on plant mortality, the de-coupling of nitrogen and photosynthesis when nitrogen saturates. In addition, the responses of soil respiration to nitrogen deposition involve so many complex biochemical processes; however, we have little knowledge about them. Sequentially, there is large uncertainty of model simulation on the effect of nitrogen deposition on soil respiration. With increasing rates of anthropogenic nitrogen deposition, there is a strong need to understand links between nitrogen inputs and carbon cycle. 相似文献
