土地利用对崇明岛围垦区土壤有机碳库和土壤呼吸的影响

土地利用方式是影响农业土壤碳固持和温室气体减排的关键因子之一,而准确地评价土地利用变化的影响往往因土壤本底的不均一和土地利用历史多变而复杂化。为此,在崇明东滩湿地围垦区选取了本底均匀、利用历史简单的几种土地利用类型(水-旱轮作农田、人工林、鱼塘撂荒地),研究其土壤有机碳库和土壤呼吸的变化及其与土壤环境间的关系,以期评价其各自的固碳和温室气体减排潜力。农田土壤的表层(20cm)有机碳和微生物生物量碳含量最高,分别为12.62g/kg和225.34mg/kg,包括苗圃栾树林、水杉林带以及桔园在内的人工林地次之,鱼塘撂荒地最低;但撂荒地深层土壤(40—100cm)的有机碳含量高于其它类型,反映了围垦前湿地土壤有机碳累积的残留影响。土壤呼吸强度的顺序则为鱼塘撂荒地农田桔园苗圃栾树林水杉林带。农耕地在前作小麦收割种植水稻后,土壤CO2通量显著下降,不及旱作时的10%。除农田和撂荒地以外,土壤表层5 cm深处温度可以很好地解释土壤呼吸速率的变化,但在高温高湿季节呼吸速率较为离散。研究表明:在有机质含量较低的土壤中,水-旱轮作可增加土壤有机碳的储量;受人类活动干扰较小的林地土壤,有机碳含量反而有可能低于农田土壤。在中国南方湿润亚热带地区,水旱轮作可较好地协调农业土壤的碳固持和释放过程的矛盾,可能具有相当大的农业减排潜力。     

General Relationships between Abiotic Soil Properties and Soil Biota across Spatial Scales and Different Land-Use Types

Very few principles have been unraveled that explain the relationship between soil properties and soil biota across large spatial scales and different land-use types. Here, we seek these general relationships using data from 52 differently managed grassland and forest soils in three study regions spanning a latitudinal gradient in Germany. We hypothesize that, after extraction of variation that is explained by location and land-use type, soil properties still explain significant proportions of variation in the abundance and diversity of soil biota. If the relationships between predictors and soil organisms were analyzed individually for each predictor group, soil properties explained the highest amount of variation in soil biota abundance and diversity, followed by land-use type and sampling location. After extraction of variation that originated from location or land-use, abiotic soil properties explained significant amounts of variation in fungal, meso- and macrofauna, but not in yeast or bacterial biomass or diversity. Nitrate or nitrogen concentration and fungal biomass were positively related, but nitrate concentration was negatively related to the abundances of Collembola and mites and to the myriapod species richness across a range of forest and grassland soils. The species richness of earthworms was positively correlated with clay content of soils independent of sample location and land-use type. Our study indicates that after accounting for heterogeneity resulting from large scale differences among sampling locations and land-use types, soil properties still explain significant proportions of variation in fungal and soil fauna abundance or diversity. However, soil biota was also related to processes that act at larger spatial scales and bacteria or soil yeasts only showed weak relationships to soil properties. We therefore argue that more general relationships between soil properties and soil biota can only be derived from future studies that consider larger spatial scales and different land-use types.     

Developing X-ray Computed Tomography to non-invasively image 3-D root systems architecture in soil

Background

The positive relationship between biodiversity and ecosystem functioning (BEF) is due mainly to complementarity between species. Most BEF studies primarily focused on plant interactions; however, plants are embedded in a dense network of multitrophic interactions above and below the ground, which are likely to play a crucial role in BEF relationships.

Scope

In the present review I point out the relevance of aboveground–belowground interactions as a source of complementarity effects in grassland biodiversity experiments. A review of the current knowledge on the role of decomposers, arbuscular mycorrhizal fungi, rhizobia, plant growth promoting rhizobacteria, invertebrate ecosystem engineers, herbivores, pathogens and predators in biodiversity experiments, indicates that soil biota can drive both positive and negative complementarity between plant species via a multitude of mechanisms.

Conclusions

I pose four main processes by which aboveground–belowground interactions determine positive complementarity effects: enlarging biotope space, mediating legume effects, increasing plant community resistance, and maintaining plant diversity. By contrast, soil biota may also reinforce negative complementarity effects by competing with plants for nutrients or by exerting herbivore or pathogen pressure, thereby reducing community productivity. Thus, considering aboveground–belowground interactions as well as interactions between antagonistic and mutualistic consumers may improve the mechanistic understanding of complementarity effects in plant diversity–ecosystem functioning experiments and should inspire future research.     

Single introductions of soil biota and plants generate long‐term legacies in soil and plant community assembly

Recent demonstrations of the role of plant–soil biota interactions have challenged the conventional view that vegetation changes are mainly driven by changing abiotic conditions. However, while this concept has been validated under natural conditions, our understanding of the long‐term consequences of plant–soil interactions for above‐belowground community assembly is restricted to mathematical and conceptual model projections. Here, we demonstrate experimentally that one‐time additions of soil biota and plant seeds alter soil‐borne nematode and plant community composition in semi‐natural grassland for 20 years. Over time, aboveground and belowground community composition became increasingly correlated, suggesting an increasing connectedness of soil biota and plants. We conclude that the initial composition of not only plant communities, but also soil communities has a long‐lasting impact on the trajectory of community assembly.     

Land-use and soil depth affect resource and microbial stoichiometry in a tropical mountain rainforest region of southern Ecuador

Global change phenomena, such as forest disturbance and land-use change, significantly affect elemental balances as well as the structure and function of terrestrial ecosystems. However, the importance of shifts in soil nutrient stoichiometry for the regulation of belowground biota and soil food webs have not been intensively studied for tropical ecosystems. In the present account, we examine the effects of land-use change and soil depth on soil and microbial stoichiometry along a land-use sequence (natural forest, pastures of different ages, secondary succession) in the tropical mountain rainforest region of southern Ecuador. Furthermore, we analyzed (PLFA-method) whether shifts in the microbial community structure were related to alterations in soil and microbial stoichiometry. Soil and microbial stoichiometry were affected by both land-use change and soil depth. After forest disturbance, significant decreases of soil C:N:P ratios at the pastures were followed by increases during secondary succession. Microbial C:N ratios varied slightly in response to land-use change, whereas no fixed microbial C:P and N:P ratios were observed. Shifts in microbial community composition were associated with soil and microbial stoichiometry. Strong positive relationships between PLFA-markers 18:2n6,9c (saprotrophic fungi) and 20:4 (animals) and negative associations between 20:4 and microbial N:P point to land-use change affecting the structure of soil food webs. Significant deviations from global soil and microbial C:N:P ratios indicated a major force of land-use change to alter stoichiometric relationships and to structure biological systems. Our results support the idea that soil biotic communities are stoichiometrically flexible in order to adapt to alterations in resource stoichiometry.     

Introduced earthworms in agricultural and reclaimed land: their ecology and influences on soil properties, plant production and other soil biota

Accidental and deliberate introductions of earthworms into agricultural and reclaimed land are natural experiments that provide opportunities to understand the attributes of successful invaders and their impacts on local biota and ecosystem processes. We consider various case studies (e.g., earthworm invasions in agricultural soils in Australia and Brazil) and deliberate introductions of earthworms into reclaimed mine sites, landfills and cutaway peat in the U.K. and Ireland. Invasions of exotic earthworms, such as European Lumbricidae in Australia, have been geographically extensive, but remain very patchy at regional and field scales. Their impacts on soil properties, plant production and other biota are therefore also likely to be patchy. Various methods have been developed to deliberately inoculate exotic earthworms into disturbed lands, with varying degrees of success. The factors controlling success are, in general, poorly understood. A broad range of impacts of invasive earthworms on soil properties (e.g., soil structure, nutrient availability, burial of surface materials, incidence of root diseases) and plant yield and quality have been reported. Less is known of the impacts of invasive earthworms on other soil fauna, but they are likely to occur due to alterations in food availability and habitat structure. Influences on other biota are likely to extend to aboveground communities as well as those belowground. Introductions of earthworms to disturbed lands can yield substantial benefits in agricultural productivity and amelioration of soil degradation. However, the potential impact of the promotion or control of such introductions on non-target biota and ecosystem processes in pristine ecosystems nearby should be considered.     

外来植物入侵对土壤生物多样性和生态系统过程的影响

随着科学家对生态系统地下部分的重视,评价外来植物入侵对土壤生态系统的影响成为当前入侵生态学领域的研究热点之一。本文综述了外来植物入侵对土壤微生物、土壤动物以及土壤碳、氮循环动态影响的研究,并探讨了其影响机制。已有的研究表明,植物入侵对土壤生物多样性及相关生态系统过程的影响均存在不一致的格局,影响机制也是复杂多样的。外来植物与土著植物凋落物的质与量、根系特征、物候等多种生理生态特性的差异可能是形成格局多样性和影响机制复杂性的最主要原因。今后,加强多尺度和多生态系统的比较研究、机制性研究、生物多样性和生态系统过程的整合性研究及土壤生态系统对植物入侵的反馈研究是评价外来植物入侵对土壤生态系统影响的发展趋势。     

Possible role of soil microorganisms in aggregation in soils

In many soils, roots and fungal hyphae, especially those of vesicular arbuscular mycorrhizal (VAM) fungi, stabilize macroaggregates (>250 μm diameter); organic residues, bacteria, polysaccharides and inorganic materials stabilize microaggregates (<250 μm). This review discusses the factors (including other organisms) which affect VAM hyphae and their extracellular polysaccharides in soil, and the subsequent effect on stability of aggregates. The review also discusses the possible role of other organisms, including ectomycorrhizal fungi, in the stability of soil, and suggests future research.     

重金属污染土壤中生物间相互作用及其协同修复应用

土壤是人类赖以生存的物质基础。我国土壤重金属污染状况不容乐观,给人类健康构成严重威胁。生物修复重金属污染土壤被广泛认为是可持续的修复技术,但当前仍存在修复效率不高的科学瓶颈问题。土壤中生活着丰富的微生物、植物和动物,且这些生物之间存在着复杂的相互作用,并且通过物质循环和能量传递形成了错综复杂的食物网联系。土壤生物间的相互作用能深刻影响土壤中污染物的迁移转化和生物修复的效率,多元生物协同的修复技术集合了单一生物修复方法的优势,具有强化生物修复效果的巨大潜力。文中综述了土壤中微生物-植物-动物之间的相互作用,及其对土壤重金属迁移转化和生物修复效果的影响,并对定向调控土壤食物网结构、提高重金属污染土壤的生物修复效果、建立基于食物网的多元生物协同修复技术进行了展望。     

A framework for modelling soil structure dynamics induced by biological activity

Soil degradation is a worsening global phenomenon driven by socio‐economic pressures, poor land management practices and climate change. A deterioration of soil structure at timescales ranging from seconds to centuries is implicated in most forms of soil degradation including the depletion of nutrients and organic matter, erosion and compaction. New soil–crop models that could account for soil structure dynamics at decadal to centennial timescales would provide insights into the relative importance of the various underlying physical (e.g. tillage, traffic compaction, swell/shrink and freeze/thaw) and biological (e.g. plant root growth, soil microbial and faunal activity) mechanisms, their impacts on soil hydrological processes and plant growth, as well as the relevant timescales of soil degradation and recovery. However, the development of such a model remains a challenge due to the enormous complexity of the interactions in the soil–plant system. In this paper, we focus on the impacts of biological processes on soil structure dynamics, especially the growth of plant roots and the activity of soil fauna and microorganisms. We first define what we mean by soil structure and then review current understanding of how these biological agents impact soil structure. We then develop a new framework for modelling soil structure dynamics, which is designed to be compatible with soil–crop models that operate at the soil profile scale and for long temporal scales (i.e. decades, centuries). We illustrate the modelling concept with a case study on the role of root growth and earthworm bioturbation in restoring the structure of a severely compacted soil.     

Macroecological patterns in soil communities

Aim To review published evidence regarding the factors that influence the geographic variation in diversity of soil organisms at different spatial scales. Location Global. Methods A search of the relevant literature was conducted using the Web of Science and the author's personal scientific database as the major sources. Special attention was paid to include seminal studies, highly cited papers and/or studies highlighting novel results. Results Despite their significant contribution to global biodiversity, our taxonomic knowledge of soil biota is still poor compared with that of most above‐ground organisms. This is particularly evident for small‐bodied taxa. Global patterns of soil biodiversity distribution have been poorly documented and are thought to differ significantly from what is reported above‐ground. Based on existing data, it appears that microorganisms do not respond to large‐scale environmental gradients in the same way as metazoans. Whereas soil microflora seem to be mainly represented by cosmopolitan species, soil animals respond to altitudinal, latitudinal or area gradients in the same way as described for above‐ground organisms. At local scales, there is less evidence that local factors regulate above‐ and below‐ground communities in the same way. Except for a few taxa, the humpbacked response to stress and disturbance gradients doesn't seem to apply underground. Soil communities thus appear weakly structured by competition, although competitive constraints may account for assembly rules within specific taxa. The main factor constraining local soil biodiversity is the compact and heterogeneous nature of soils, which provides unrivalled potential for niche partitioning, thus allowing high levels of local biodiversity. This heterogeneity is increased by the impact of ecosystem engineers that generate resource patchiness at a range of spatio‐temporal scales.     

城市化对土壤动物群落结构和多样性的影响

城市化进程加快带来的环境挑战正威胁着地球上的生物多样性。土壤动物是生物多样性的重要组成部分, 对维持土壤健康及城市生态系统稳定性具有重要意义。近年来, 城市土壤动物群落结构和多样性的研究已经取得了一定进展, 但是仍缺乏系统的总结和综述。基于此, 本文梳理归纳了国内外已有的相关文献, 总结了城市化影响土壤动物的主要途径, 并阐述了城市中不同体型大小的优势土壤动物类群对城市化的响应。本文建议未来应利用分子生物学手段深入解析城市土壤动物多样性, 明晰城市土壤食物网的结构与功能, 关注土壤动物群落的保护与恢复, 揭示城市土壤动物肠道微生物组特征, 并挖掘城市土壤动物抑制人类致病菌的潜力, 以期为城市生物多样性保护、生态系统稳定和人类健康维持提供相关科学依据。     

Local vs. landscape controls on diversity: a test using surface-dwelling soil macroinvertebrates of differing mobility

Aim A better understanding of the processes driving local species richness and of the scales at which they operate is crucial for conserving biodiversity in cultivated landscapes. Local species richness may be controlled by ecological processes acting at larger spatial scales. Very little is known about the effect of landscape variables on soil biota. The aim of our study was to partly fill this gap by relating the local variation of surface‐dwelling macroarthropod species richness to factors operating at the habitat scale (i.e. land use and habitat characteristics) and the landscape scale (i.e. composition of the surrounding matrix). Location An agricultural landscape with a low‐input farming system in Central Hesse, Germany. Methods We focused on five taxa significantly differing in mobility and ecological requirements: ants, ground beetles, rove beetles, woodlice, and millipedes. Animals were caught with pitfall traps in fields of different land use (arable land, grassland, fallow land) and different habitat conditions (insolation, soil humidity). Composition of the surrounding landscape was analysed within a radius of 250 m around the fields. Results Factors from both scales together explained a large amount of the local variation in species richness, but the explanatory strength of the factors differed significantly among taxa. Land use particularly affected ground beetles and woodlice, whereas ants and rove beetles were more strongly affected by habitat characteristics, namely by insolation and soil characteristics. Local species richness of diplopods depended almost entirely on the surrounding landscape. In general, the composition of the neighbouring landscape had a lower impact on the species richness of most soil macroarthropod taxa than did land use and habitat characteristics. Main conclusions We conclude that agri‐environment schemes for the conservation of biodiversity in cultivated landscapes have to secure management for both habitat quality and heterogeneous landscape mosaics.     

土壤生物及其对土壤生态学发展的影响

土壤生物区系、土壤生物多样性和全球变化已成为土壤生态学研究的肖沿领域,土壤生物以不同的方式改变着土壤的物理、化学和生物学特性,某一等级层次上的土壤生物群落的组成和结构可以对其它等级层次上的资源空间异质性产生影响,而这种空间异质性受到许多生物圈层－－土壤功能区域所维持。本文评价了土壤生物区系在土壤生态系统过程中的作用,论述了土壤生物多样性与生态系统功能的关系,讨论了土壤生态系统对全球变化的影响。     

土壤生物与可持续农业研究进展

农业的可持续发展是人类文明持续繁荣的重要保障。从原始农业到工业化农业的发展历程,是"自然力"不断削弱,"人为调控力"不断加强的过程。新兴的可持续农业,则希望将人为调控和自然过程协调融合,建立近自然的高效的现代农业体系。但是,面对土壤生物极高的多样性、生物和非生物过程的复杂互作及其高度的时空异质性,基于还原论的传统科学研究方法探究地下生态系统的"自然过程"困难重重。人为管理措施对农田生态过程调控的针对性和调控效果受到极大限制。尽管如此,土壤生物在生态系统服务中的作用已在世界范围内得到空前重视。如何充分发挥土壤生物在可持续农业中的作用,已成为现代农业研究领域的重要突破口。简述了土壤生物与可持续农业研究的学科发展历史,总结了农业管理措施对土壤生物及土壤食物网特征的影响,突出了土壤生物群落在可持续农业模式中土壤结构改善、土壤肥力提高和化肥农药减施等方面的积极作用;最后探讨了当前的研究难点和未来的研究方向,并对如何充分发挥土壤生物在现代农业中的贡献进行了初步的思考。认为:土壤有机质,土壤结构和土壤食物网以及三者的内在联系是可持续农业研究的关键。土壤有机质管理是调控土壤结构、土壤食物网及生态系统生产力的重要支点,但也是可持续农业模式不确定性的重要来源。基于同位素示踪等整体性分析方法,开展典型农田生态系统土壤食物网特征及其生态功能的系统研究,揭示农业模式、土壤食物网特征及生态系统生产力的关键联系,是充分发挥土壤生物在可持续农业中的积极作用的基础。     

毛乌素沙地半固定沙丘油蒿种群对土壤湿度空间异质性的响应

将统计学和地统计学方法相结合,探讨了毛乌素沙地半固定沙丘土壤湿度空间异质性与油蒿种群空间异质性之间的关系. 结果表明,在块尺度（80 m×80 m）上,油蒿密度和生物量的空间异质性受制于土壤湿度的空间异质性,尤其油蒿生物量的空间异质性与土壤湿度的空间异质性呈显著正相关关系.表明在半固定沙丘阶段,土壤湿度的空间异质性决定油蒿种群的空间异质性. 由于沙丘地形对降水量的再分配在土壤湿度分布中的作用,土壤湿度和油蒿种群空间异质性相互作用的结果为地形的缀块性→土壤湿度分布的缀块性→油蒿种群分布的缀块性→油蒿生物量和密度的缀块性.     

土壤动物群落空间格局和构建机制研究进展

群落空间格局和构建机制一直是生态学研究的核心内容。在生物多样性严重丧失的背景下, 揭示群落空间格局及其构建机制, 有助于深刻理解生物多样性丧失的原因, 更有助于应对生物多样性保护等重大生态环境问题。然而, 陆地生态系统的研究多集中于地上生物群落, 对地下生态系统, 尤其是土壤动物空间格局和构建机制的研究尚不充分。事实上, 土壤动物多样性是全球生物多样性的关键组成之一, 是地下生态系统结构和功能维持的重要部分。对土壤动物空间格局和构建机制的研究, 能明确不同空间尺度条件下土壤动物多样性的维持机制。土壤动物群落常在多种空间尺度形成复杂的空间分布格局, 因此, 本文首先介绍了不同空间尺度主要土壤动物群落的空间自相关性特征, 阐述了土壤动物群落斑块和孔隙镶嵌分布的复杂空间格局。继而阐明这种空间格局主要受生物间作用、环境过滤和随机扩散的调控, 并说明这三个过程对土壤动物群落的调控能力和作用方式。作者提出, 这三个过程仍是今后土壤动物群落空间格局和构建机制研究的重点内容, 需要进一步加强以土壤动物为研究对象的群落构建理论的验证和发展。我国土壤动物群落空间格局和构建机制起步较晚, 希望本文能够促进我国土壤动物生态学相关领域的研究。     

Exogenous carbon turnover within the soil food web strengthens soil carbon sequestration through microbial necromass accumulation

Exogenous carbon turnover within soil food web is important in determining the trade-offs between soil organic carbon (SOC) storage and carbon emission. However, it remains largely unknown how soil food web influences carbon sequestration through mediating the dual roles of microbes as decomposers and contributors, hindering our ability to develop policies for soil carbon management. Here, we conducted a ¹³C-labeled straw experiment to demonstrate how soil food web regulated the residing microbes to influence the soil carbon transformation and stabilization process after 11 years of no-tillage. Our work demonstrated that soil fauna, as a “temporary storage container,” indirectly influenced the SOC transformation processes and mediated the SOC sequestration through feeding on soil microbes. Soil biota communities acted as both drivers of and contributors to SOC cycling, with 32.0% of exogenous carbon being stabilizing in the form of microbial necromass as “new” carbon. Additionally, the proportion of mineral-associated organic carbon and particulate organic carbon showed that the “renewal effect” driven by the soil food web promoted the SOC to be more stable. Our study clearly illustrated that soil food web regulated the turnover of exogenous carbon inputs by and mediated soil carbon sequestration through microbial necromass accumulation.     

古尔班通古特沙漠土壤水分与化学性质的空间分布

区域尺度上,气象和水文状况是影响植被分布格局和土壤性状的主要因子,当然,局部的地貌特征及植被分布对土壤性质的影响也是不能忽视的。以古尔班通古特沙漠为研究对象,对其南缘至腹地约25 km的土壤水分与化学性质的空间分布及其相互关系进行研究,结果显示:水平方向上,从沙漠南缘至腹地,土壤水分在丘底呈减小趋势,尤其是距边缘10 km以外,且在距边缘6—7 km出现1个峰值。同时土壤pH值和电导率的大小以及有机碳,全氮,有效氮,全磷和有效磷含量与土壤水分的变化状况相似,在丘底呈减小趋势,而在丘坡和丘顶上均呈波动分布。这说明丘底土壤性质的空间格局受到气象和水文状况的显著影响,而丘坡和丘顶土壤性质并没有受到气象和水文状况的显著影响,这种波动分布主要由采样点的设置及植物的分布状况所引起。丘底土壤水分及化学性质均显著高于丘坡和丘顶,这说明地貌特征对土壤性质的空间分布有显著影响。垂直方向上,不同深度土层土壤性质也存在显著差异,土壤水分,pH值和电导率随着土层深度增加而增加,而土壤养分随土层深度增加而减小。相关分析结果表明:仅4、5月份的土壤含水量及年平均土壤含水量与丘底土壤化学性质显著正相关,这可能由于冬季积雪的融化导致了土壤水分在4、5月份的聚集比较明显,使土壤水分对土壤化学性质发挥作用。总之,土壤空间异质性是由气象和水文以及地貌特征共同影响的,而土壤空间异质性的变异进而影响到植被的分布,植被的分布反过来又影响土壤的空间分布,因此土壤的空间分布和植被的空间分布是相互影响,共同作用的。