崇明东滩冬季不同管理模式下水稻田水鸟群落特征及其生境分析

崇明东滩是亚太地区候鸟迁徙路线的重要中转站,也是上海地区促淤圈围的重点区域。水稻(Oryza sativa)田作为当地分布广泛且重点改造的人工湿地,研究其是否具有水鸟招引效果具有重要意义。本研究于2013和2014年冬季采用样方法对崇明东滩两种不同管理模式的水稻田,即2013年开始改造的传统模式水稻田和改造多年的机械化模式水稻田,进行了水鸟群落及生境因子调查,以探究不同管理模式下水稻田内生境差异,水鸟对不同生境的利用程度及其不同生境中的关键因子对水鸟分布的影响。调查期间共记录到水鸟5目7科18种1 795只次,其中传统模式水稻田记录到水鸟5目6科17种1 756只次,优势种为绿翅鸭(Anas crecca)、斑嘴鸭(A.poecilorhyncha)、鹤鹬(Tringa erythropus);机械化模式水稻田录到水鸟4目5科6种39只次,优势种为小??(Tachybaptus ruficollis)和凤头麦鸡(Vanellus vanellus)。T检验结果显示,传统模式水稻田对水鸟的招引效果(即多度和物种丰富度)显著优于机械化模式水稻田,2014年改造后传统模式水稻田的水鸟招引效果显著优于2013改造初期。多元回归分析显示,明水面面积比例是影响水稻田水鸟种类、数量分布的最重要因子。结果表明,明水面面积和适合的水位高度是影响冬季水稻田水鸟招引效果的主要因素,为提高冬季水稻田水鸟保育效果,应注重营造、维护冬季水稻田中水文条件。     

Host and environmental influences on the gut bacterial community of carabid beetles in distinct paddy fields

The relationship between the gut bacterial communities of carabid beetles and their habitats holds implications for understanding ecological dynamics. This study examined the gut bacterial communities of two carabid beetle species, Chlaenius pallipes and Pheropsophus jessoensis, in terraced and flat paddy fields. Differences in gut bacterial communities were evident at the species level and were based on habitat. Specifically, P. jessoensis had a greater presence of Firmicutes and Proteobacteria in terraced fields but more Actinobacteria in flatland fields. In comparison, C. pallipes consistently showed high levels of Firmicutes in both habitats. These differences were reflected at class and genus levels, emphasizing the role of host specificity in shaping gut microbiota. Alpha diversity metrics indicated that P. jessoensis hosted a more diverse bacterial community than C. pallipes. Terraced fields, however, showed slightly reduced diversity in P. jessoensis, suggesting environmental effects on microbial populations. Beta diversity analysis using Bray–Curtis distances differentiated the bacterial communities of the two beetles. Multivariate analysis of variance reinforced these findings. Insights from the Sloan neutral model indicate that environmental factors predominantly influence bacterial community assembly through stochastic processes. Functionally, metabolism was highlighted, indicating the role of gut bacteria in beetle metabolic processes. Notably, energy metabolism varied between field types, revealing environmental effects on gut bacterial functions. This study offers in-depth insights into interactions between host-specific and environmental factors influencing gut bacterial communities of carabid beetles, contributing to a broader understanding of microbial ecology and the roles of environment and host in microbiota dynamics.     

Influence of rice cultivar on methane emission from paddy fields

Influence of rice cultivars on CH₄ emissions from a paddy field was studied using four Japonica types, two Indica types, and two Japonica/Indica F₁ hybrids. In addition, the suppression of CH₄ emission by interrupting irrigation at the flowering stage was investigated. Patterns of seasonal variation in CH₄ emission rates were similar among the eight cultivars. Two of the Japonica types showed the maximum and minimum CH₄ emissions among the cultivars investigated. Neither the number of tillers, shoot length, shoot weight, and root weight correlated with the CH₄ emission rates at the tillering and reproductive growth stages. Following temporary interruption of irrigation at the flowering stage, CH₄ emission rates decreased drastically and remained at very low levels until the harvesting stage, indicating its great effectiveness for the suppression of CH₄ emission from rice paddies.     

Storage and sequestration potential of topsoil organic carbon in China's paddy soils

Carbon (C) storage and sequestration in agricultural soils is considered to be an important issue in the study of terrestrial C cycling and global climatic change. The baseline C stock and the C sequestration potential are among the criteria for a region or a state to adopt strategies or policies in response to commitment to the Kyoto Protocol. Paddy soils represent a large portion of global cropland. However, little information on the potential of C sequestration and storage is available for such soils. In this paper, an estimation of the topsoil soil organic carbon (SOC) pool and the sequestration potential of paddy soils in China was made by using the data from the 2nd State Soil Survey carried out during 1979–1982 and from the nationwide arable soil monitoring system established since then. Results showed that the SOC density ranged from 12 to 226 t C ha^?1 with an area‐weighted mean density of 44 t C ha^?1, which is comparable to that of the US grasslands and is higher than that of the cultivated dryland soils in China and the US. The estimated total topsoil SOC pool is 1.3 Pg, with 0.85 Pg from the upper plow layer and 0.45 Pg from the plowpan layer. This pool size is ～2% of China's total storage in the top 1 m of the soil profiles and ～4% of the total topsoil pool, while the area percentage of paddy soil is 3.4% of the total land. The C pool in paddy soils was found predominantly in southeast China geographically and in the subgroups of Fe‐accumulating and Fe‐leaching paddy soils pedogenetically. In comparison with dryland cultivation, irrigation‐based rice cultivation in China has induced significant enrichment of SOC storage (0.3 Pg) in paddy soils. The induced total C sequestration equals half of China's total annual CO₂ emission in the 1990s. Estimates using different SOC sequestration scenarios show that the paddy soils of China have an easily attainable SOC sequestration potential of 0.7 Pg under present conditions and may ultimately sequester 3.0 Pg. Soil monitoring data showed that the current C sequestration rate is 12 Tg yr^?1. The total C sequestration potential and the current sequestration rate of the paddy soils are over 30%, while the area of the paddy soils is 26% that of China's total croplands. Therefore, practicing sustainable agriculture is urgently needed for enhancing SOC storage to realize the ultimate SOC sequestration of rice‐based agriculture of China, as the current C sequestration rate is significantly lower than the potential rate.     

Influence of soil temperature on methane emission from rice paddy fields

Methane emission rates from an Italian rice paddy field showed diel and seasonal variations. The seasonal variations were not closely related to soil temperatures. However, the dieL changes of CH₄ fluxes were significantly correlated with the diel changes of the temperature in a particular soil depth. The soil depths with the best correlations between CH4 flux and temperature were shallow (1–5cm) in May and June, deep (10–15cm) in June and July, and again shallow (1–5 cm) in August. Apparent activation energies (E_a) calculated from these correlations using the Arrhenius model were relatively low (50–150 kJ mol^–1) in May and June, but increased to higher values (80–450 kJ mol^–1) in August. In the laboratory, CH₄ emission from two rice cultures incubated at temperatures between 20 and 38°C showed E . values of 41 and 53 kJ mol^–1) Methane production in anoxic paddy soil suspensions incubated between 7 and 43°C showed E values between 53 and 132 kJ mol^–1 with an average value of 85 kJ mol^–1) and in pure cultures of hydrogenotrophic methanogenic bacteria E _a values between 77 and 173 (average 126) kJ mol^–1. It is suggested that diel changes of soil properties other than temperature affect CH₄ emission rates, e.g. diel changes in root exudation or in efficiency of CH⁴ oxidation in the rhizosphere.     

Application of lidar remote sensing of insects in agricultural entomology on the Chinese scene

Insect pest management is a very important aspect for plant protection in crops production. Remote sensing provides a large number of techniques that are beneficial in entomological research. Although entomological radars have been used for studying migrations of insects for many years, most of entomological radar studies have been vertically tracing high-altitude migration behaviour of insects. Light detection and ranging (lidar) is a counterpart to radar, now operating in the optical part of the electromagnetic spectrum, which has been recently applied for monitoring of insects at low altitude. Such techniques, in particular low-cost continuous-wave (CW) bi-static systems based on the Scheimpflug arrangement, have been rapidly developing during the last decade. As a result, optical methods present new and fascinating possibilities. Based on experience from a 2-week field campaign in rice paddy fields, we here present an overview of lidar remote sensing applied to the Chinese scene. The capability of a CW Scheimpflug lidar system in monitoring the insects was studied. We present results on insect abundance in relation to time of the day and weather conditions. We also identified insect species by analysing wing-beat frequencies and studied their attraction to ultraviolet (UV) lamp located close to the horizontal laser sampling path during night time. Results showed that the insect species were abundant, that insects detected by the lidar system were attracted to light and that light rain increased the insect activity. The lidar detection system had a high read-out frequency, enabling the estimation of insect wing-beat frequencies.     

水稻土中铁氧化物对产甲烷古菌群落结构的影响

产甲烷菌广泛分布在淹水水稻土等各种厌氧环境中,在全球气候变化、碳循环和能源等领域都发挥着重要的作用。研究发现,厌氧条件下,水稻土中铁氧化物的生物还原会抑制产甲烷菌的甲烷合成作用。然而,目前关于铁氧化物对产甲烷菌群落结构的影响报道较少。通过泥浆厌氧培养实验,向采集的水稻土中添加甲酸盐作为甲烷合成的底物(Control,CK处理),并设置添加水铁矿作为体系中唯一电子受体的处理组(Ferrihydrite,Fh处理)。培养结束后,与CK相比,添加水铁矿显著降低了古菌在总微生物群落中的占比,但对古菌群落的物种多样性和均一度没有显著影响;且两组处理中优势种均为操作分类单元(Operational taxonomic unit,OTU)2056和OTU 911(76%—80%)。这说明碳源相同时,产甲烷菌的群落结构不受铁氧化物的影响。本研究为探索土壤中微生物铁还原与碳循环耦合的分子机制奠定基础。     

Microbial mechanism for rice variety control on methane emission from rice field soil

Rice variety is one of the key factors regulating methane (CH₄) production and emission from the paddy fields. However, the relationships between rice varieties and populations of microorganisms involved in CH₄ dynamics are poorly understood. Here we investigated CH₄ dynamics and the composition and abundance of CH₄‐producing archaea and CH₄‐oxidizing bacteria in a Chinese rice field soil planted with three types of rice. Hybrid rice produced 50–60% more of shoot biomass than Indica and Japonica cultivars. However, the emission rate of CH₄ was similar to Japonica and lower than Indica. Furthermore, the dissolved CH₄ concentration in the rhizosphere of hybrid rice was markedly lower than Indica and Japonica cultivars. The rhizosphere soil of hybrid rice showed a similar CH₄ production potential but a higher CH₄ oxidation potential compared with the conventional varieties. Terminal restriction fragment length polymorphism analysis of the archaeal 16S rRNA genes showed that the hydrogenotrophic methanogens dominated in the rhizosphere whereas acetoclastic methanogens mainly inhabited the bulk soil. The abundance of total archaea as determined by quantitative (real‐time) PCR increased in the later stage of rice growth. However, rice variety did not significantly influence the structure and abundance of methanogenic archaea. The analysis of pmoA gene fragments (encoding the α‐subunit of particulate methane monooxygenase) revealed that rice variety also did not influence the structure of methanotrophic proteobacteria, though variable effects of soil layer and sampling time were observed. However, the total copy number of pmoA genes in the rhizosphere of hybrid rice was approximately one order of magnitude greater than the two conventional cultivars. The results suggest that hybrid rice stimulates the growth of methanotrophs in the rice rhizosphere, and hence enhances CH₄ oxidation which attenuates CH₄ emissions from the paddy soil. Hybrid rice is becoming more and more popular in Asian countries. The present study demonstrated that planting of hybrid rice will not enhance CH₄ emissions albeit a higher grain production than the conventional varieties.     

不同施肥对水稻土作物碳同化与土壤碳固定的影响——以太湖地区黄泥土肥料长期试验为例

肥料施用对农田土壤生产力及土壤碳循环的影响是农业与陆地生态系统碳循环及全球变化研究的重要科学问题。以太湖地区黄泥土的长期肥料定位试验为例,研究不同施肥处理对水稻土-作物系统作物碳同化及土壤碳固定的影响。所研究的肥料施用处理包括不施肥(NF)、单施化肥(CF)、化肥与秸秆配施(CFS)以及化肥与猪粪配施(CFM) 4个处理,始于1987年,一直实行稻-油轮作,实行少耕。连续观测水稻和油菜的产量,并于2004年和2005年分别采集了土壤剖面样品和耕作层（0～5cm和5～15cm）土壤,测定土壤总有机碳含量。研究表明,不同施肥处理对水稻产量有显著影响,尤其以配施有机无机肥处理水稻产量显著最高且最为稳定,而对油菜产量的影响不明显。施肥显著提高了耕层土壤碳密度,而对全土碳密度没有显著影响。施肥处理的固碳速率介于0.1～0.4t/(hm^２•a), 配施有机肥处理显著高于单施化肥处理。相关分析表明,土壤固碳速率与作物根茬+有机肥源碳的总碳输入量呈显著的对数关系。这提示土壤有机碳积累主要与作物产量有关,而并非依变于有机肥源碳输入。因此,与作物产量直接关联的作物碳输入的增加是土壤中碳固定提高的重要途径。施入N素对水稻碳同化和土壤碳固定的效应均为化肥配施有机肥处理显著高于单施化肥处理,这揭示化肥配施有机肥是提高与稳定稻田生产力和促进土壤固碳和温室气体减排的双赢措施。当然,不同施肥下上述效应的差异可能与土壤-作物系统中碳分配和土壤生物碳利用的差异有关。