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991.
Northern peatlands have accumulated one third of the Earth's soil carbon stock since the last Ice Age. Rapid warming across northern biomes threatens to accelerate rates of peatland ecosystem respiration. Despite compensatory increases in net primary production, greater ecosystem respiration could signal the release of ancient, century‐ to millennia‐old carbon from the peatland organic matter stock. Warming has already been shown to promote ancient peatland carbon release, but, despite the key role of vegetation in carbon dynamics, little is known about how plants influence the source of peatland ecosystem respiration. Here, we address this issue using in situ 14C measurements of ecosystem respiration on an established peatland warming and vegetation manipulation experiment. Results show that warming of approximately 1 °C promotes respiration of ancient peatland carbon (up to 2100 years old) when dwarf‐shrubs or graminoids are present, an effect not observed when only bryophytes are present. We demonstrate that warming likely promotes ancient peatland carbon release via its control over organic inputs from vascular plants. Our findings suggest that dwarf‐shrubs and graminoids prime microbial decomposition of previously ‘locked‐up’ organic matter from potentially deep in the peat profile, facilitating liberation of ancient carbon as CO2. Furthermore, such plant‐induced peat respiration could contribute up to 40% of ecosystem CO2 emissions. If consistent across other subarctic and arctic ecosystems, this represents a considerable fraction of ecosystem respiration that is currently not acknowledged by global carbon cycle models. Ultimately, greater contribution of ancient carbon to ecosystem respiration may signal the loss of a previously stable peatland carbon pool, creating potential feedbacks to future climate change.  相似文献   
992.
In the desert locust, Schistocerca gregaria (Forskål) (Orthoptera: Acrididae), the threshold density inducing the gregarization phenomenon has never been determined under natural conditions. The influence of environmental factors on this phenomenon has been studied mostly in controlled environments. Based on data collected during several years by the survey teams of the National Center for Locust Control in Mauritania, we analyzed the influence of locust density, vegetation cover, and vegetation status on the probability of observing gregarious locusts. We assumed that a probability to observe gregarious locusts of 0.5 corresponded to the density threshold of gregarization. The results showed in detail the change in the threshold of gregarization according to the cover and status of the vegetation. Low cover and dry vegetation led to a low density threshold of gregarization probably due to high probability of individuals to touch each other. Dense and green vegetation favored a high threshold of gregarization probably due to a dispersion of the individuals and a low probability of individual encounters. These findings should help the management of locusts and decision making during control operations.  相似文献   
993.
对用海藻酸钙包埋胡萝卜体细胞胚(0.6—2mm)制作的人工种子进行贮藏研究,发现低温及干燥均能在一定程度上抑制人工种子萌发。失水率达67%的种子,2℃贮藏60天后, 在发芽培养基上发芽率为100%,7天内的成苗率达80%。未经贮藏的对照种子发芽率为100%,成苗率为76%。无论在“种皮”还是在胚胎悬浮培养液中加入脱落酸或香豆素,都能抑制胚的生长,但也促进了胚的衰老。铝箔袋内密闭贮藏期间种子不萌发,但活力下降快。随着贮藏时间的延长,种子的活力指数、脱氢酶活性、氧吸收率都呈下降趋势。  相似文献   
994.
深圳市大鹏半岛土地利用变化对植被覆盖动态的影响   总被引:1,自引:0,他引:1  
城市化背景下的植被覆盖动态研究对于区域生态保护工作具有重要的指导意义.利用深圳市1995-2007年的遥感数据以及1996和2007年土地变更调查资料,基于归一化植被指数轨迹追踪分析和叠图代数计算方法,对大鹏半岛植被覆盖动态类型及其空间分异、土地利用变化结构和格局特征以及土地利用变化与植被覆盖动态之间的响应关系进行研究.结果表明:1995-2007年,研究区65%的地区植被覆盖发生显著改变,植被覆盖状况总体趋于好转;城市化和商品农业发展是该区土地利用动态变化的主要成因,研究时段内31%的地表发生了用地功能转变;土地利用变化是区内植被覆盖发生改变的重要成因之一,约35%的植被覆盖出现退降过程区域与土地功能转变有关;55%的用地功能转变区域因机械干扰导致植被覆盖退化,但至研究期末,大多数退化区域已经进入植被覆盖显著改善阶段.  相似文献   
995.
植被覆盖度是衡量地表植被状况和指示生态环境变化的一个重要指标。基于像元二分模型,利用Landsat5/8遥感影像和DEM数据,对岷江汶川-都江堰段植被覆盖动态变化进行了监测,并结合高程、坡度和坡向数据,分析了汶川地震前后植被受损与恢复的空间动态格局变化。研究表明:植被覆盖总体良好,大部分区域的植被覆盖度均在中、高度以上,空间格局上呈现由汶川县东部、都江堰市西北部的龙门山区向两侧减少的总体趋势;地震造成植被受损面积达63808.7 hm~2,且集中分布于海拔567—4331 m、坡度26—51°的范围以及东坡、北坡、南坡和西坡;震后5a,植被恢复面积17786.47 hm~2,主要分布在海拔576—2180 m与3256—3793 m、坡度小于9°和26—51°以及东坡、东南坡和和南坡;高程和坡度对植被损毁与恢复的影响明显高于坡向。  相似文献   
996.

Questions

What are the syntaxonomic and synchorological patterns of the xerothermic chasmophytic vegetation in the central part of the Mediterranean Basin? What are the diagnostic species of the high‐rank syntaxa of Asplenietalia glandulosi, Onosmetalia frutescentis and Centaureo dalmaticae‐Campanuletalia pyramidalis?

Location

Mediterranean coastal and subcoastal areas of southern France, Italy, Malta, Slovenia, Croatia, Bosnia and Herzegovina, Montenegro, Albania and of mainland Greece.

Methods

The data set of 1,261 published relevés was analysed using hierarchical clustering (Flexible Beta method), involving a series of data transformations. Indicator species analysis was used to select the best dendrogram solution and identify diagnostic taxa of the main clusters. The dendrogram was interpreted from a syntaxonomic point of view, using nomenclatural type relevés as a basis. The NMDS ordination was performed in order to visualize the floristic relationships among associations and high‐rank syntaxa. MRPP was used to test for differences among alliances.

Results

The classification revealed four main clusters of relevés representing the chasmophytic vegetation of southern France, Sardinia and the northwestern part of Italy (Asplenienalia glandulosi/Asplenietalia glandulosi), the southwestern part of Italy and Malta (Tinguarrenalia siculae/Asplenietalia glandulosi), the Adriatic Basin area (Centaureo dalmaticae‐Campanuletalia pyramidalis) and the southern Balkans (Onosmetalia frutescentis). The NMDS ordination confirmed the overall pattern, while MRPP showed significant differences among the alliances of the above‐mentioned orders and suborders. The lists of diagnostic taxa of the high‐rank syntaxa were revised according to a supra‐national perspective.

Conclusions

The new syntaxonomic scheme provides a comprehensive overview of the chasmophytic vegetation of the central part of the Mediterranean Basin. This scheme mostly matches the recently published EuroVegChecklist, but also exhibits important novelties concerning the syntaxonomic position of some alliances (Dianthion rupicolae, Centaureion pentadactyli, Arenarion bertolonii and Caro‐Aurinion), and the floristic and chorological relationships among high‐rank syntaxa, with new revised sets of diagnostic taxa. This revision might be useful for further small‐scale phytosociological studies.
  相似文献   
997.
Over the last century the Northern Hemisphere has experienced rapid climate warming, but this warming has not been evenly distributed seasonally, as well as diurnally. The implications of such seasonal and diurnal heterogeneous warming on regional and global vegetation photosynthetic activity, however, are still poorly understood. Here, we investigated for different seasons how photosynthetic activity of vegetation correlates with changes in seasonal daytime and night‐time temperature across the Northern Hemisphere (>30°N), using Normalized Difference Vegetation Index (NDVI) data from 1982 to 2011 obtained from the Advanced Very High Resolution Radiometer (AVHRR). Our analysis revealed some striking seasonal differences in the response of NDVI to changes in day‐ vs. night‐time temperatures. For instance, while higher daytime temperature (Tmax) is generally associated with higher NDVI values across the boreal zone, the area exhibiting a statistically significant positive correlation between Tmax and NDVI is much larger in spring (41% of area in boreal zone – total area 12.6 × 10km2) than in summer and autumn (14% and 9%, respectively). In contrast to the predominantly positive response of boreal ecosystems to changes in Tmax, increases in Tmax tended to negatively influence vegetation growth in temperate dry regions, particularly during summer. Changes in night‐time temperature (Tmin) correlated negatively with autumnal NDVI in most of the Northern Hemisphere, but had a positive effect on spring and summer NDVI in most temperate regions (e.g., Central North America and Central Asia). Such divergent covariance between the photosynthetic activity of Northern Hemispheric vegetation and day‐ and night‐time temperature changes among different seasons and climate zones suggests a changing dominance of ecophysiological processes across time and space. Understanding the seasonally different responses of vegetation photosynthetic activity to diurnal temperature changes, which have not been captured by current land surface models, is important for improving the performance of next generation regional and global coupled vegetation‐climate models.  相似文献   
998.
子午岭植被恢复对土壤饱和导水率的影响   总被引:11,自引:0,他引:11  
梁向锋  赵世伟  张扬  华娟 《生态学报》2009,29(2):636-642
通过对子午岭林区不同植被的土壤性质进行实验室测定和野外调查,对饱和土壤水分运动的重要参数之一土壤饱和导水率(Ks)及其相关因子进行了多元分析和通径分析,揭示了植被恢复提高土壤水分传输性能的机理,主要结论如下:土壤有机质是子午岭林区九种植被下土壤饱和导水率提高的主要驱动因子.不同植被下的土壤饱和导水率均随深度的增加而迅速降低,尽管草地和先锋草地在5~10cm深度有一强透水层.土壤饱和导水率在剖面上的平均值,从辽东栎、早期森林、灌丛、先锋草地、弃耕地到草地依次降低.灌丛与草地、弃耕地的差异达到显著水平,辽东栎顶级群落的饱和导水率最高,植被的恢复明显提高了土壤饱和导水率.土壤容重、毛管孔隙度、>0.25mm团聚体含量及粘粒含量直接影响土壤饱和导水率.土壤有机质含量的提高能够改善容重、毛管孔隙度、团聚体含量等物理性质.  相似文献   
999.
喀斯特山区不同植被类型土壤有机碳的变化   总被引:7,自引:0,他引:7  
Liao HK  Long J 《应用生态学报》2011,22(9):2253-2258
研究了贵州西南部典型喀斯特山区不同植被类型下常规土壤及小生境土壤中有机碳及不同粒径土壤颗粒有机碳的变化.结果表明:不同植被类型下,常规及小生境土壤有机碳含量均表现为:裸地<草丛<灌木林<乔木林,常规土壤变幅在7.18 ~43.42 g·kg-1,土面和石坑土壤有机碳变幅分别为6.62 ~46.47 g· kg-1和9.01 ~52.07 g·kg-1;颗粒有机碳(POC)/矿物结合态有机碳( MOC)值均为:裸地<草丛<乔木林<灌木林,同一植被类型下,与常规及土面相比,石坑中土壤POC/MOC值最高;植被在由裸地-草丛-灌木林-乔木林的变化过程中,不同粒径土壤颗粒有机碳含量增加,而土壤有机碳主要以砂粒及粉砂粒有机碳形式存在,说明喀斯特地区土壤的固碳能力及有机碳稳定性较弱,土壤易受外界干扰而引发有机碳流失,土壤质量存在下降或退化的风险.  相似文献   
1000.
人发角蛋白人工腱材料体内降解及生物相容性研究   总被引:11,自引:0,他引:11  
目的研究人发角蛋白人工腱(humanhairkeratinartificaltendon,HHKAT)材料在体内的可降解性及其生物相容性.方法对12只日本大耳白兔随机分组,在脊旁肌埋藏不同处理时间的人发角蛋白人工腱试件F及Z,用正常人发O做对照,分别在2、6、12、24周取材,观察人发角蛋白的降解吸收过程及其周围的组织反应.结果动物植入实验中发现不同时间处理的材料其降解速度不同,其中降解最快的F组在24周已完全吸收,而Z组在24周只有部分降解,O组未见降解.HHKAT及人发在肌肉组织内无明显的炎症排斥反应,随着HHKAT材料的降解吸收,其周围的组织反应逐渐降低.结论本研究表明人发角蛋白人工腱材料具有良好的生物相容性,在体内能够被降解吸收,可根据不同的需要调节其降解速度,是良好的肌腱替代材料.  相似文献   
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