Mycorrhizal suppression and phosphorus addition influence the stability of plant community composition and function in a temperate steppe

Nutrient enrichment can reduce ecosystem stability, typically measured as temporal stability of a single function, e.g. plant productivity. Moreover, nutrient enrichment can alter plant–soil interactions (e.g. mycorrhizal symbiosis) that determine plant community composition and productivity. Thus, it is likely that nutrient enrichment and interactions between plants and their soil communities co-determine the stability in plant community composition and productivity. Yet our understanding as to how nutrient enrichment affects multiple facets of ecosystem stability, such as functional and compositional stability, and the role of above–belowground interactions are still lacking. We tested how mycorrhizal suppression and phosphorus (P) addition influenced multiple facets of ecosystem stability in a three-year field study in a temperate steppe. Here we focused on the functional and compositional stability of plant community; functional stability is the temporal community variance in primary productivity; compositional stability is represented by compositional resistance, turnover, species extinction and invasion. Community variance was partitioned into population variance defined as community productivity weighted average of the species temporal variance in performance, and species synchrony defined as the degree of temporal positive covariation among species. Compared to treatments with mycorrhizal suppression, the intact AM fungal communities reduced community variance in primary productivity by reducing species synchrony at high levels of P addition. Species synchrony and population variance were linearly associated with community variance with the intact AM fungal communities, while these relationships were decoupled or weakened by mycorrhizal suppression. The intact AM fungal communities promoted the compositional resistance of plant communities by reducing compositional turnover, but this effect was suppressed by P addition. P addition increased the number of species extinctions and thus promoted compositional turnover. Our study shows P addition and AM fungal communities can jointly and independently modify the various components of ecosystem stability in terms of plant community productivity and composition.     

陆地生态系统环境控制实验的研究方法及技术体系

生物及生态系统与环境变化间的反馈关系及其过程机制是生态学研究的重要内容。不同类型的生物环境因素控制实验以及大尺度的联网野外控制实验被认为是认识生态系统响应和适应环境变化过程机制、精细定量表达的有效手段及认知过程的加速器。近年来发展了大型野外物理模拟实验装置网络(如ECOTRON)、生态系统分析与实验平台(AnaEE)、国际干旱实验研究网络(Drought Network)、氮沉降联合实验网络(Nutrient Network),以及基于各区域性生态观测实验站的联网控制实验(如USA-ILTER)。发展大陆尺度联网实验研究平台事业正日益受到学术界的重视,将会在认知生态系统环境响应过程机制方面发挥更重要的作用。基于以上背景,本文综述了生态系统环境控制实验的研究方法和实验体系的发展,明确指出各种类型的生物环境控制实验需要形成联合协作体系,共同解决生态系统对环境变化的响应及适应的基本科学问题。目前的控制实验包括: 1) 实验室封闭装置内的生物生理生态学控制实验;2) 野外实验场的半开放部分环境要素控制实验;3) 近自然状态的野外环境控制实验;以及4) 基于野外生态站的联网控制实验。进而,本文还深入讨论了陆地生态系统的环境响应及适应过程机制实验系统设计的发展趋势,分析了基于大尺度自然环境梯度实验及生态站尺度的要素控制实验的优势,提出了整合两种实验技术、发展新一代的野外联网实验体系的科学设想,讨论了基于野外联网控制实验的研究体系,论证了研究生态系统对环境变化短期响应和长期适应的规律和机制、生态系统环境响应定量表达的技术途径。若本文提出的控制实验体系设计方案能够得以实施,必将大大促进我国乃至全球生态系统和环境变化科学的研究水平,对我国应对气候变化和生态环境建设具有重要的科学意义。     

既主内政, 又辖外交——以PHR为中心的基因网络调控植物-菌根真菌的共生

磷是植物生长发育必需的大量矿质营养元素, 但自然界大部分土壤都存在严重缺磷的问题。为了适应这一营养逆境, 植物演化出一系列低磷胁迫应答反应。通过改变基因的转录水平调控低磷胁迫应答反应, 而转录因子PHR1在调控植物对低磷胁迫的转录响应中起关键作用。此外, 大部分陆生植物还能与丛枝菌根真菌建立共生关系, 通过丛枝菌根真菌更有效地从土壤中获取磷元素。最近, 中国科学院分子植物科学卓越创新中心王二涛研究组发现, 以PHR为中心的转录调控网络控制植物-丛枝菌根真菌共生的建立。因此, PHR不但在维持植物细胞自身的磷稳态中发挥作用, 而且参与植物与外界微生物的相互作用, 为植物有效地从环境中获得磷元素提供了另外一条途径。     

国家公园陆地自然生态系统完整性与原真性评价方法探索: 以钱江源国家公园体制试点为例

中国建立国家公园的目的是保护自然生态系统的完整性和原真性, 促进生物多样性保护。国家公园的完整性和原真性评价是国家公园的布局规划、边界范围确定以及功能区划等研究的前提条件。为了评估国家公园自然生态系统完整性和原真性状态, 本文基于陆地自然生态系统的结构和功能, 通过指标筛选、专家咨询、指标量化和建立综合评价模型, 构建了陆地自然生态系统完整性与原真性的评价指标体系及其量化评价方法。该评价方法包括5个自然生态系统完整性指标、5个自然生态系统原真性指标和2个综合评价指标。以浙江省钱江源国家公园体制试点为例, 本文初步评估了其生态系统完整性与原真性状态, 并对评价结果进行了分级。按照本研究的评价方法, 钱江源国家公园体制试点的自然生态系统完整性评价结果为52.83%, 评价等级为较差; 自然生态系统原真性评价结果为87.06%, 评价等级为好。钱江源国家公园体制试点有待关注和提升的指标有保护区域完整性指数(27.00%)和旗舰种适宜生境完整性指数(53.04%)。最后, 本文结合研究区域评价结果对生态系统完整性和原真性领域应关注的问题进行了讨论。该自然生态系统完整性和原真性评价方法可提供一种评价指标覆盖较全面、数据易获取, 且评价结果易被决策者和管理者理解的评价思路。     

基于指数施肥法的一年生油松菌根化容器苗的供N研究

为了探讨一年生菌根化油松容器苗的最适苗木供N量和供N速率,采用4种不同指数施肥量进行了试验.通过测定苗木生物量和N含量,显示总供N量为80 mg·株-1的处理组在生物量积累和苗木N含量上显著优于其它各组（P〈0.05）;在100 d时,该处理可获得0.47 mg·株-1·d-1的N最适添加速率;在该速率下,苗木生物量、N含量分别可以达到845.60 mg·株-1和6.51 mg·株-1.根据生物量和N含量随着供N量增加的回归拟合结果,在107 d的生长过程中,67.96 mg·株-1至84.15 mg·株-1的供N总量可以使得一年生油松幼苗获得较高的生物量积累水平和N含量.     

A Novel Alveolate in Bivalves with Chemosynthetic Bacteria Inhabiting Deep‐Sea Methane Seeps

It has recently been unveiled that a wide variety of microbial eukaryotes (protists) occur in chemosynthetic ecosystems, such as hydrothermal vents and methane seeps. However, there is little knowledge regarding protists associated with endemic animals inhabiting these environments. In the present study, utilizing PCR techniques, we detected fragments of the small subunit ribosomal RNA gene (SSU rRNA gene) from a particular protist from gill tissues of a significant fraction of the vesicomyid clams Calyptogena soyoae and C. okutanii complex and of the mussel Bathymodiolus platifrons and B. japonicus, all of which harbor chemosynthetic endosymbiont bacteria and dominate methane seeps in Sagami Bay, Japan. Based on the phylogeny of SSU rRNA gene, the organism in question was shown to belong to Alveolata. It is noteworthy that this protist did not affiliate with any known alveolate group, although being deeply branched within the lineage of Syndiniales, for which the monophyly was constantly recovered, but not robustly supported. In addition, the protist detected using PCR followed by sequencing was localized within gill epithelial cells of B. platifrons with whole‐mount fluorescence in situ hybridization. This protist may be an endoparasite or an endocommensal of Calyptogena spp. and Bathymodiolus spp., and possibly have physiological and ecological impacts on these bivalves.     

Symbiotic fungi in roots of Artemisia annua with special reference to endophytic colonizers

Abstract

Advances on plant–fungal interactions reveal that root symbiotic fungi actively modulate host growth, resistance response and secondary metabolism. Artemisia annua has been widely recognized as an important medicinal plant for artemisinin production, yet little is known about the fungal consortium associated with roots of A. annua. In this article, microscopic and culture-dependant methods were used to evaluate the identity and taxonomic affinities of root symbiotic fungi. Morphological evidence confirmed that arbuscular mycorrhizal fungi were dominant fungal group in naturally regenerated roots, but low colonization frequency in planted roots. Dark septate endophytes (DSEs) were easily found, which were characterized with dark pigmented hypha and a sclerotium-like structure in root cortex, and other endophytic fungi also occurred. A total of 36 isolates were recovered. Combined morphological and molecular identification (based on ITS sequences) determined 21 fungal taxa (genotype), which were placed into numerous lineages of Ascomycota. The best BLAST match indicated that almost half of total taxa were closely related to undescribed fungi, some of them may act as novel DSEs but experimental data were warranted. Interestingly, remarkable difference of fungal community associated with two types of roots was examined and no culturable fungi overlapped. Our findings provide some additional evidence that DSEs and other root endophytes may be as common as mycorrhizal fungi. Recovered fungi as raw materials for bioassay of endophytes-mediated promotion of artemisinin content in A. annua will be conducted in further research.     

Impacts of 3 years of elevated atmospheric CO2 on rhizosphere carbon flow and microbial community dynamics

Carbon (C) uptake by terrestrial ecosystems represents an important option for partially mitigating anthropogenic CO₂ emissions. Short‐term atmospheric elevated CO₂ exposure has been shown to create major shifts in C flow routes and diversity of the active soil‐borne microbial community. Long‐term increases in CO₂ have been hypothesized to have subtle effects due to the potential adaptation of soil microorganism to the increased flow of organic C. Here, we studied the effects of prolonged elevated atmospheric CO₂ exposure on microbial C flow and microbial communities in the rhizosphere. Carex arenaria (a nonmycorrhizal plant species) and Festuca rubra (a mycorrhizal plant species) were grown at defined atmospheric conditions differing in CO₂ concentration (350 and 700 ppm) for 3 years. During this period, C flow was assessed repeatedly (after 6 months, 1, 2, and 3 years) by ¹³C pulse‐chase experiments, and label was tracked through the rhizosphere bacterial, general fungal, and arbuscular mycorrhizal fungal (AMF) communities. Fatty acid biomarker analyses and RNA‐stable isotope probing (RNA‐SIP), in combination with real‐time PCR and PCR‐DGGE, were used to examine microbial community dynamics and abundance. Throughout the experiment the influence of elevated CO₂ was highly plant dependent, with the mycorrhizal plant exerting a greater influence on both bacterial and fungal communities. Biomarker data confirmed that rhizodeposited C was first processed by AMF and subsequently transferred to bacterial and fungal communities in the rhizosphere soil. Over the course of 3 years, elevated CO₂ caused a continuous increase in the ¹³C enrichment retained in AMF and an increasing delay in the transfer of C to the bacterial community. These results show that, not only do elevated atmospheric CO₂ conditions induce changes in rhizosphere C flow and dynamics but also continue to develop over multiple seasons, thereby affecting terrestrial ecosystems C utilization processes.     

Predicting species‐specific responses of fungi to climatic variation using historical records

Although striking changes have been documented in plant and animal phenology over the past century, less is known about how the fungal kingdom's phenology has been changing. A few recent studies have documented changes in fungal fruiting in Europe in the last few decades, but the geographic and taxonomic extent of these changes, the mechanisms behind these changes, and their relationships to climate are not well understood. Here, we analyzed herbarium data of 274 species of fungi from Michigan to test the hypotheses that fruiting times of fungi depend on annual climate and that responses depend on taxonomic and functional groups. We show that the fungal community overall fruits later in warmer and drier years, which has led to a shift toward later fruiting dates for autumn‐fruiting species, consistent with existing evidence. However, we also show that these effects are highly variable among species and are partly explained by basic life‐history characteristics. Resulting differences in climate sensitivities are expected to affect community structure as climate changes. This study provides a unique picture of the climate dependence of fungal phenology in North America and an approach for quantifying how individual species and broader fungal communities will respond to ongoing climate change.     

The impacts of climate change and human activities on biogeochemical cycles on the Qinghai‐Tibetan Plateau

With a pace of about twice the observed rate of global warming, the temperature on the Qinghai‐Tibetan Plateau (Earth's ‘third pole’) has increased by 0.2 °C per decade over the past 50 years, which results in significant permafrost thawing and glacier retreat. Our review suggested that warming enhanced net primary production and soil respiration, decreased methane (CH₄) emissions from wetlands and increased CH₄ consumption of meadows, but might increase CH₄ emissions from lakes. Warming‐induced permafrost thawing and glaciers melting would also result in substantial emission of old carbon dioxide (CO₂) and CH₄. Nitrous oxide (N₂O) emission was not stimulated by warming itself, but might be slightly enhanced by wetting. However, there are many uncertainties in such biogeochemical cycles under climate change. Human activities (e.g. grazing, land cover changes) further modified the biogeochemical cycles and amplified such uncertainties on the plateau. If the projected warming and wetting continues, the future biogeochemical cycles will be more complicated. So facing research in this field is an ongoing challenge of integrating field observations with process‐based ecosystem models to predict the impacts of future climate change and human activities at various temporal and spatial scales. To reduce the uncertainties and to improve the precision of the predictions of the impacts of climate change and human activities on biogeochemical cycles, efforts should focus on conducting more field observation studies, integrating data within improved models, and developing new knowledge about coupling among carbon, nitrogen, and phosphorus biogeochemical cycles as well as about the role of microbes in these cycles.