铜尾矿废弃地土壤动物多样性特征

土壤动物的恢复、群落演替及其多样性对于铜尾矿废弃地的生态重建具有重要意义.为了解铜尾矿废弃地土壤动物群落多样性特征,在铜陵市铜尾矿区设置4个样地23采样点,共捕获土壤动物4622只个体,隶属5门10纲18目29类.结果表明,铜尾矿自然废弃地与其对照组土壤动物多样性差异明显,自然废弃地土壤动物丰富度指数d、大型土壤动物密度、中小型土壤动物密度、多样性指数H'和D·G指数均小于其对照组且存在显著差异.而复垦废弃地中小型土壤动物密度和D·G指数小于其对照组且存在显著差异,多样性指数H'大于其对照组且差异极显著,其他土壤动物群落指标与其对照组均无显著差异.相似系数q表明,外围林地间土壤动物群落相似性最大,其次是复垦废弃地与外围林地间,自然废弃地与其它3个样地间相似性最小.从垂直分层来看,复垦废弃地土壤动物表聚性强于自然废弃地,尾矿废弃地表聚性强于外围林地.灰色关联分析表明,铜尾矿区土壤理化性质与土壤动物群落结构指标关系密切,其中最重要的因素是土壤含水量和总钾含量,重金属全镉含量也不容忽视,植被因素和土壤全铜含量对土壤动物的影响相对较小.由此可见,土壤含水量、土壤基质的优劣、土壤有机质与营养元素的含量等因素限制了铜尾矿废弃地土壤动物的恢复与重建,而这些因素的改善主要归功于尾矿废弃地的土地复垦和作物种植.所以,尾矿废弃地的复垦与利用有利于土壤动物的恢复与重建.     

科尔沁沙地湖泊消涨对气候变化的响应

湖泊是受气候变化影响显著的地理单元之一,不同地区湖泊消涨与气候变化关系的分析是理解陆地水文过程对未来气候变化响应的关键之一。对干旱、半干旱地区而言,湖泊消涨对气候变化的响应是干旱区生态保护和未来可持续发展的重要指征。气候变化对湖泊的影响研究在不同的区域已有较多的研究,但是针对湖泊群且基于湖泊大小分级和不同降水强度的对应研究还很鲜见。有鉴于此,作者在RS和GIS技术支持下,采用湖泊大小和降水强度分级的方法,分析了科尔沁沙地湖泊群消涨与气候变化的关系。在1971-2010年间,年均气温波动升高和降水量波动减少是该区域的主要气候变化特点。从5年移动平均分析来看,1990年是气温变化的转折点,1991-2010年的平均气温7.36（?0.55）℃,高于全球同期平均增温0.52℃。在1975-2009年间,科尔沁沙地湖泊面积和数量的变化趋势呈抛物线型减少,在1995年湖泊面积与数量最高。进入21世纪,湖泊面积萎缩、数量减少呈明显的加快趋势。到2009年,面积>0.05km2湖泊数量仅为81个,不足高峰期（1995年）的11%;湖泊总面积为4375.0hm2,不到1995年的26%。本研究表明,湖泊消涨主要受到年降水量波动影响,与年内降水分布格局无关,气温变化的影响不显著。     

毛乌素沙地南缘沙丘生物结皮对凝结水形成和蒸发的影响

在水分极度匮乏的荒漠生态系统,凝结水是除降雨之外最重要的水分来源之一,它对荒漠生态系统结构、功能和过程的维持产生重要的影响。为探明半干旱沙区生物结皮表面的凝结水形成和蒸发特征,采用自制的微型蒸渗计(直径7 cm、高5 cm的PVC管)实验观测了不同类型地表(裸沙、浅灰色藻类结皮、黑褐色藻类结皮和苔藓结皮)对凝结水形成和蒸发的影响。结果表明:(1)观测期间共有20次凝结水形成记录,除降雨天气外,几乎每天都能观测到水分凝结现象;(2)不同类型地表凝结水总量依次为(1.998±0.075),(2.326±0.083),(2.790±0.058)和(3.416±0.068) mm,生物结皮表面的凝结水总量显著大于裸沙(P < 0.05);随生物结皮的发育,不同类型生物结皮表面的凝结水总量呈增加的趋势,凝结水总量之间差异显著(P < 0.05);观测期间不同类型地表日平均凝结水量依次为(0.100±0.003),(0.116±0.004),(0.140±0.002)和(0.171± 0.003) mm,不同类型地表日平均凝结水量之间差异极显著(P < 0.01);(3)凝结水形成过程的观测结果显示,凝结水19:00开始形成,23:00-凌晨1:00形成不明显,1:00-7:00继续形成,除浅灰色藻类结皮外,太阳升出后在黑褐色藻类结皮和苔藓结皮表面继续形成少量的凝结水;凝结水7:30开始蒸发,10:30到11:00之间结束蒸发,凝结水在裸沙和浅灰色藻类结皮中的保持时间显著大于黑褐色藻类结皮和苔藓结皮中的保持时间(P < 0.05);(4)凝结水的形成受大气温度、地表温度、空气相对湿度和大气地表温度差等气象因素的影响,但其形成过程不与某一个气象因素呈简单的线性关系。     

生态植被建设对黄土高原农林复合流域景观格局的影响

自1999年以来,黄土高原大规模地实施了退耕还林工程,生态环境呈显著恢复态势。采用2002年和2008年两期Spot5遥感影像,评估了退耕还林工程实施前后黄土高原典型农林复合流域土地利用与景观格局的动态变化。结果表明:在退耕还林工程实施的驱动下,流域土地利用变化剧烈,总变化率高达36.77%,主要变化的土地利用类型包括耕地、果园、幼林地、林地等。28.95%的耕地转为其他土地利用类型,其中48.83%转为果园,44.69%转为幼林地。景观格局变化呈明显的空间分布规律,山腰缓坡区以转化为果园为主,中、高海拔多转化为幼林地。退耕后流域生态景观得以优化,呈现良好发展态势。     

农地保护的外部效益测算——选择实验法在武汉市的应用

农地保护的外部效益是农地保护补偿政策制定的依据.对外部效益进行了理论界定和实证测算,认为农地保护的外部效益是农村集体和农地使用者以外个体从农地保护中得到的收益,通常是非市场收益,对其测算应区分外部效益的内部(外部效益发出者)和外部(外部效益接受者),并确定外部区域的范围.实证利用选择实验模型对武汉市5个区域进行了支付意愿测算,在内外部划分的基础上估算了武汉市农地保护的外部效益并比较了不同方法下外部效益测算结果的差别.结果表明,武汉市耕地、园地、林地和农村水面的外部效益分别为30773.2,653860.0,119267.0和82472.7元/hm2;用行政区域直接代替外部性影响区域的做法会使耕地外部效益的测算结果偏高,也会造成园地、林地和农村水面测算的误差,为避免这类误差,外部性测算及相关补偿、税费政策应考虑内外部区域的划分.     

Deforestation and Reforestation of Latin America and the Caribbean (2001–2010)

Forest cover change directly affects biodiversity, the global carbon budget, and ecosystem function. Within Latin American and the Caribbean region (LAC), many studies have documented extensive deforestation, but there are also many local studies reporting forest recovery. These contrasting dynamics have been largely attributed to demographic and socio‐economic change. For example, local population change due to migration can stimulate forest recovery, while the increasing global demand for food can drive agriculture expansion. However, as no analysis has simultaneously evaluated deforestation and reforestation from the municipal to continental scale, we lack a comprehensive assessment of the spatial distribution of these processes. We overcame this limitation by producing wall‐to‐wall, annual maps of change in woody vegetation and other land‐cover classes between 2001 and 2010 for each of the 16,050 municipalities in LAC, and we used nonparametric Random Forest regression analyses to determine which environmental or population variables best explained the variation in woody vegetation change. Woody vegetation change was dominated by deforestation (?541,835 km²), particularly in the moist forest, dry forest, and savannas/shrublands biomes in South America. Extensive areas also recovered woody vegetation (+362,430 km²), particularly in regions too dry or too steep for modern agriculture. Deforestation in moist forests tended to occur in lowland areas with low population density, but woody cover change was not related to municipality‐scale population change. These results emphasize the importance of quantitating deforestation and reforestation at multiple spatial scales and linking these changes with global drivers such as the global demand for food.     

The catalytic domain CysPc of the DEK1 calpain is functionally conserved in land plants

DEK1, the single calpain of land plants, is a member of the ancient membrane bound TML–CysPc–C2L calpain family that dates back 1.5 billion years. Here we show that the CysPc–C2L domains of land plant calpains form a separate sub‐clade in the DEK1 clade of the phylogenetic tree of plants. The charophycean alga Mesostigma viride DEK1‐like gene is clearly divergent from those in land plants, suggesting that a major evolutionary shift in DEK1 occurred during the transition to land plants. Based on genetic complementation of the Arabidopsis thaliana dek1‐3 mutant using CysPc–C2L domains of various origins, we show that these two domains have been functionally conserved within land plants for at least 450 million years. This conclusion is based on the observation that the CysPc–C2L domains of DEK1 from the moss Physcomitrella patens complements the A. thaliana dek1‐3 mutant phenotype. In contrast, neither the CysPc–C2L domains from M. viride nor chimeric animal–plant calpains complement this mutant. Co‐evolution analysis identified differences in the interactions between the CysPc–C2L residues of DEK1 and classical calpains, supporting the view that the two enzymes are regulated by fundamentally different mechanisms. Using the A. thaliana dek1‐3 complementation assay, we show that four conserved amino acid residues of two Ca²⁺‐binding sites in the CysPc domain of classical calpains are conserved in land plants and functionally essential in A. thaliana DEK1.     

The effects of different vegetation restoration patterns on soil bacterial diversity for sandy land in Hulunbeier

Grassland desertification seriously threatens sustainable economic and social development. Much attention has been paid to the control of grassland desertification, and even to the restoration and reconstruction of the grassland. Vegetation restoration is considered to be a very effective solution. Soil sustains an immense diversity of microbes, and the characteristics of soil microbial communities are sensitive indicators of soil. It is important to understand the relationship between vegetation and soil microbial diversity during the restoration process. Soil microbial, which is the main index to evaluate soil quality, plays a significant role in ecosystem and soil microbial diversity is the important one of global diversity. Exploring the effects of different vegetation patterns on soil microbial diversity can provide scientific bases and technical support for systemic and impersonal assessment of the best vegetation restoration patterns, as well as the vegetation restoration and reconstruction of Hulunbeier sandy land. Based on PCR–DGGE technology, a case study was carried out to investigate the effects of five different vegetation restoration patterns on soil microbial functional diversity after 4 years in sandy land in Hulunbeier, China. The five vegetation restoration patterns included mono-cultivar planting of Agropyron cristatum (UA), mono-cultivar planting of Hedysarum fruticosum (UH), mono-cultivar planting of Caragana korshinskii (UC), mixed-cultivar planting of Agropyron cristatum and Hedysarum fruticosum (AC) and mixed-cultivar planting of Agropyron cristatum, Hedysarum fruticosum, Caragana korshinskii and Elymus nutans (ACHE). Completely degraded sandy land was used as control.The results indicated that the vegetation restoration increased the genetic diversity of soil bacterial community obviously, and the structure of soil bacterial community was changed. The results of phylogenetic analysis suggested that the bacterial community in Hulunbeier sandy land mainly attributed to Proteobacteria, Bacteroidetes, Firmicutes, Actinobacteria, and Acidobacteria. The dominant groups were Proteobacteria and Bacteroidetes. The effects of different vegetation type on soil bacterial community structures were different.     

Inferences of evolutionary history of a widely distributed mangrove species,Bruguiera gymnorrhiza,in the Indo‐West Pacific region

Inference of genetic structure and demographic history is fundamental issue in evolutionary biology. We examined the levels and patterns of genetic variation of a widespread mangrove species in the Indo‐West Pacific region, Bruguiera gymnorrhiza, using ten nuclear gene regions. Genetic variation of individual populations covering its distribution range was low, but as the entire species it was comparable to other plant species. Genetic differentiation among the investigated populations was high. They could be divided into two genetic clusters: the West and East clusters of the Malay Peninsula. Our results indicated that these two genetic clusters derived from their ancestral population whose effective size of which was much larger compared to the two extant clusters. The point estimate of speciation time between B. gymnorrhiza and Bruguiera sexangula was two times older than that of divergence time between the two clusters. Migration from the West cluster to the East cluster was much higher than the opposite direction but both estimated migration rates were low. The past Sundaland and/or the present Malay Peninsula are likely to prevent gene flow between the West and East clusters and function as a geographical or land barrier.     

Effect of spatial and temporal patterns of stress and disturbance intensities in a sub-Mediterranean grassland

Abstract

The present study examined a sub-Mediterranean pastoral system in the central Apennines (Italy) with a long history of grazing, where winter cold stress is alternated with summer drought stress. The research goals were to ascertain whether different floristic structures correspond to different stress conditions (xeric and semimesic), and whether peculiar functional plant traits (such as avoidance and tolerance mechanisms) respond to stress/disturbance intensities, and understand how vegetation reacts to changeable livestock pressure (through floristic and plant trait variations). Cluster analysis indicated that separate communities develop under different stress intensities. Other analyses highlighted how avoidance strategies predominate within the pastoral system. Observations of grazed and ungrazed patches conducted in 10-m transects revealed spiny cushion formation in semimesic grassland, where a brief period of overgrazing occurs in late summer, causing variations in plant community structure. All these results confirm the importance of historical grazing and current land use, showing how small disturbances and stress variations cause ecosystem responses. Best practices for management were identified. In xeric conditions, it is advisable that the intensity of disturbance be lessened, while in semimesic grassland overgrazing should be forbidden during the dry period, because it could facilitate the development of spiny patches, and subsequent spread of Brachypodium rupestre.