Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia,China

Studying the responses of soil respiration (R_s) to soil management changes is critical for enhancing our understanding of the global carbon cycle and has practical implications for grassland management. Therefore, the objectives of this study were (1) quantify daily and seasonal patterns of R_s, (2) evaluate the influence of abiotic factors on R_s, and (3) detect the effects of soil management changes on R_s. We hypothesized that (1) most of daily and seasonal variation in R_s could be explained by soil temperature (T_s) and soil water content (S_w), (2) soil management changes could significantly affect R_s, and (3) soil management changes affected R_s via the significant change in abiotic and biotic factors. In situ R_s values were monitored in an agropastoral ecotone in Inner Mongolia, China, during the growing seasons in 2009 (August to October) and 2010 (May to October). The soil management changes sequences included free grazing grassland (FG), cropland (CL), grazing enclosure grassland (GE), and abandoned cultivated grassland (AC). During the growing season in 2010, cumulative R_s for FG, CL, GE, and AC averaged 265.97, 344.74, 236.70, and 226.42 gC m^?2 year^?1, respectively. The T_s and S_w significantly influenced R_s and explained 66%–86% of the variability in daily R_s. Monthly mean temperature and precipitation explained 78%–96% of the variability in monthly R_s. The results clearly showed that R_s was increased by 29% with the conversion of FG to CL and decreased by 35% and 11% with the conversion of CL to AC and FG to GE. The factors impacting the change in R_s under different soil management changes sequences varied. Our results confirm the tested hypotheses. The increase in Q₁₀ and litter biomass induced by conversion of FG to GE could lead to increased R_s if the climate warming. We suggest that after proper natural restoration period, grasslands should be utilized properly to decrease R_s.     

高寒草地土壤温室气体排放对放牧的响应研究进展

高寒草地生态系统具有独特的地理环境和气候特征,对放牧干扰十分敏感,在全球温室气体通量中贡献突出,研究高寒草地放牧对土壤温室气体排放的影响机制具有重要意义。本文总结高寒草地温室气体源/汇特征、不同放牧方式对土壤微环境和微生物群落结构的影响,发现高寒草地主要是CO₂源、CH₄汇、N₂O源。放牧通过家畜选择性采食、践踏和排泄物返还等多重机制作用于地上植物、土壤结构、温度、湿度和养分,进而影响地下微生物及温室气体通量。本文旨在为高寒草地生态系统健康发展和管理及缓解全球气候变化提供科学依据,并对未来研究方向进行展望。     

Responses of the functional structure of soil microbial community to livestock grazing in the Tibetan alpine grassland

Microbes play key roles in various biogeochemical processes, including carbon (C) and nitrogen (N) cycling. However, changes of microbial community at the functional gene level by livestock grazing, which is a global land‐use activity, remain unclear. Here we use a functional gene array, GeoChip 4.0, to examine the effects of free livestock grazing on the microbial community at an experimental site of Tibet, a region known to be very sensitive to anthropogenic perturbation and global warming. Our results showed that grazing changed microbial community functional structure, in addition to aboveground vegetation and soil geochemical properties. Further statistical tests showed that microbial community functional structures were closely correlated with environmental variables, and variations in microbial community functional structures were mainly controlled by aboveground vegetation, soil C/N ratio, and NH₄⁺‐N. In‐depth examination of N cycling genes showed that abundances of N mineralization and nitrification genes were increased at grazed sites, but denitrification and N‐reduction genes were decreased, suggesting that functional potentials of relevant bioprocesses were changed. Meanwhile, abundances of genes involved in methane cycling, C fixation, and degradation were decreased, which might be caused by vegetation removal and hence decrease in litter accumulation at grazed sites. In contrast, abundances of virulence, stress, and antibiotics resistance genes were increased because of the presence of livestock. In conclusion, these results indicated that soil microbial community functional structure was very sensitive to the impact of livestock grazing and revealed microbial functional potentials in regulating soil N and C cycling, supporting the necessity to include microbial components in evaluating the consequence of land‐use and/or climate changes.     

Asymmetric effects of grazing intensity on macroelements and microelements in grassland soil and plants in Inner Mongolia Grazing alters nutrient dynamics of grasslands

Grazing is a traditional grassland management technique and greatly alters ecosystem nutrient cycling. The effects of grazing intensity on the nutrient dynamics of soil and plants in grassland ecosystems remain uncertain, especially among microelements. A 2‐year field grazing experiment was conducted in a typical grassland with four grazing intensities (ungrazed control, light, moderate, and heavy grazing) in Inner Mongolia, China. Nutrient concentration was assessed in soil and three dominant plant species (Stipa krylovii, Leymus chinensis, and Cleistogenes squarrosa). Assessed quantities included four macroelements (carbon (C), nitrogen (N), phosphorus (P), and magnesium (Mg)) and four microelements (copper (Cu), iron (Fe), manganese (Mn), and zinc (Zn)). Soil total C, total N, total P, available N, and available P concentrations significantly increased with grazing intensity but soil Mg, Cu, Fe, Mn, Zn concentrations had no significant response. Plant C concentration decreased but plant N, P, Mg, Cu, Fe, Mn, and Zn concentrations significantly increased with grazing intensity. In soil, macroelement dynamics (i.e., C, N, and P) exhibited higher sensitivity with grazing intensity, conversely in plants, microelements were more sensitive. This result indicates macroelements and microelements in soil and plants had asymmetric responses with grazing intensity. The slopes of nutrient linear regression in C. squarrosa were higher than that of S. krylovii and L. chinensis, indicating that C. squarrosa had higher nutrient acquisition capacity and responded more rapidly to heavy grazing. These findings indicate that short‐term heavy grazing accelerates nutrient cycling of the soil–plant system in grassland ecosystems, elucidate the multiple nutrient dynamics of soil and plants with grazing intensity, and emphasize the important function of microelements in plant adaptation in grazing management.     

克氏针茅草原土壤生态化学计量特征对放牧强度的响应

生态化学计量学是研究生态系统中各元素间平衡的科学,对于探究土壤有机碳（C）、全氮（N）、全磷（P）元素循环以及土壤养分限制状况具有重要意义。为了解克氏针茅（Stipa kirschnii）草原土壤生态化学计量特征,以内蒙古克氏针茅草原区为研究对象,在不同放牧强度草场进行采样分析。结果表明：随着放牧强度的增加,C、P含量先降低后升高,N含量先升高后降低;土壤C/N先降低后升高、C/P逐渐升高、N/P先升高后降低。C/N随着放牧强度的增加与有机碳相关性逐渐增大、与全氮的相关性逐渐减小;轻牧区的C/P受有机碳作用有所增强;中牧区N/P受全氮作用增强。C/N主要限制因素是有机碳含量,C/P和N/P主要限制因素是全磷含量。不同放牧强度会影响土壤化学计量比与其他物质的关系,也会改变土壤化学计量比各制约因素的强度。     

放牧对荒漠草原克氏针茅种群和土壤生态化学计量特征的影响

该研究选取内蒙古荒漠草原,设计无牧区(NG)、中度放牧(MG)、重度放牧(HG)3个处理,测定分析不同放牧强度处理5年后,优势植物克氏针茅以及土壤的C、N、P营养元素的化学计量特征及其协同关系,以揭示放牧生态系统养分循环的影响机制,为区域草地的利用以及修复提供理论依据。结果表明:(1)轻度放牧下荒漠草原的物种多样性均显著高于中度和重度放牧条件(P<0.05)。(2)土壤中C、N含量以及C∶N、N∶P、C∶P,均随着放牧强度的增加呈先升高后降低的变化趋势,土壤P含量随放牧强度的增加而升高。(3)随放牧强度增加,克氏针茅地上部分C含量降低,N、P含量以及N∶P先升高后降低,C∶P则先减少后升高;克氏针茅地下部分的C、N含量以及N∶P一直呈增加的趋势,P含量先减少后升高,而C∶N、C∶P则是与P含量规律相反。(4)与地上部分各元素含量相比,克氏针茅地下部分各元素含量及其比值与土壤中各元素含量的相关性更高,说明放牧条件下荒漠草原优势植物的根系与其所处的土壤环境具有一定的协同变化能力。     

Recent decline of the critically endangered Plains‐wanderer (Pedionomus torquatus), and the application of a simple method for assessing its cause: major changes in grassland structure

A monitored population of the critically endangered Plains‐wanderer (Pedionomus torquatus) on Victoria's Northern Plains declined by over 90% between 2010 and 2012 following an unusually wet year which led to flooding, excess grass growth and a major change in the structure of native grasslands. The Plains‐wanderer population remained very low on private land during 2013 and 2014 when dry conditions prevailed and domestic stock overgrazed most of its favoured grasslands on red soil. Numbers also remained very low on public reserves despite grassland structure gradually improving there by 2014. In 2015, the population partially recovered in some grasslands protected from overgrazing. Grassland structure is critically important for Plains‐wanderer conservation. The ‘golf ball technique’ proved to be a quick and effective method for measuring grassland structure; it offers a means of accelerating responses to habitat change because it can be easily used by land managers.     

放牧后自然恢复沙质草地土壤节肢动物群落结构与多样性

以中国科学院奈曼沙漠化研究站为依托,对不同放牧强度后自然恢复沙质草地土壤节肢动物群落进行了调查,分析了土壤节肢动物群落结构及其多样性变化,探讨了植被和土壤环境对土壤节肢动物群落的影响.结果表明: 无牧草地土壤动物种类丰富,个体数量较多,多样性最高;中牧后恢复草地土壤动物个体数量少,但主要类群较多,分布较均匀,多样性较高;重牧后恢复草地土壤动物主要类群少,但个体数量多,多样性较高;而轻牧后恢复草地土壤动物分布均匀性最差,多样性最低.植物个体数、高度及盖度和土壤酸碱度是影响不同放牧强度后恢复草地土壤动物种类和个体数量分布的主要因素.说明沙质草地经过12年的围封可以一定程度上恢复土壤动物群落,而放牧干扰对土壤动物群落的负面影响是长期的.     

Plant and soil microbial responses to defoliation in temperate semi-natural grassland

There is much interest in understanding the nature of feedback mechanisms between plants and soil organisms in grazed ecosystems. In this study, we examine the effects of different intensities of defoliation on the growth of three dominant grass species, and observe how these plant responses relate to the biomass and activity of the microbial community in the root zone. Our data show that grassland plants with varying tolerances to grazing have markedly different growth responses to defoliation, and that these responses vary with the intensity of cutting. Defoliation of grasses which are tolerant to grazing, namely Festuca rubra and Cynosurus cristatus, leads to a reduction in root mass and an increase in the allocation of resources to shoots. In contrast, defoliation of a grass with low tolerance to grazing, Anthoxanthum odoratum, had little effect on root mass, but increased the relative allocation of resources below-ground. In all plant species, defoliation led to an increase in soil microbial biomass and C use efficiency in the root zone. This response was greatest in the root zone of A. odoratum and is likely to be related to changes in root exudation pattern following defoliation. The significance of these changes in relation to soil nutrient dynamics and plant nutrient uptake during regrowth require further exploration. This revised version was published online in June 2006 with corrections to the Cover Date.     

Response of a Native Perennial Grass Stand to Disturbance in California's Coast Range Grassland

To assess the potential for enhancing an existing stand of native perennial grasses on a California Coast Range Grassland site, we experimentally manipulated the seasonal timing and presence of grazing for 3 years (1994 through 1996) and of autumn burning for 2 years (1994 and 1995) and measured species cover for 6 years (1993 through 1998). We subjected the species matrix to classification (TWINSPAN) and ordination (CCA) and tested the ordination site scores as well as diversity indices with linear mixed effects models. Four distinct plant community groups emerged from the classification. Two of these were dominated by annual grasses and two by perennial grasses. No treatment effects were observed on diversity. For composition, temporal and spatial random effects were important mixed effects model parameters, as was the fixed effect covariate, pre‐treatment CCA site score, indicating the importance of random environmental variation and initial starting conditions. Incorporation of these random effects and initial condition terms made for more powerful tests of the fixed effects, grazing season, and burning. We found no significant burning effects. Grazing removal imparted a shift in plant community from more annual‐dominated toward more perennial‐dominated vegetation. Individual perennial grass species responded differently according to genus and species. Nassella spp. increased gradually over time regardless of grazing treatment. Nassella pulchra (purple needlegrass) increase was greatest under spring grazing and N. lepida (foothill needlegrass) was greatest with grazing removal. Danthonia californica (California oatgrass) had little response over time under seasonal grazing treatments, but increased with grazing removal. Under relatively mesic weather conditions it appears that grazing removal from Coast Range Grasslands with existing native perennial grass populations can increase their cover. However if N. pulchra is the sole existing population, spring season‐restricted grazing should be equally effective at enhancing cover of the native grass species.     

藏北高寒草地植被和土壤对不同放牧强度的响应

放牧压力在时间和空间的不均衡分布导致局部土地过度利用和生态退化,然而当前对放牧强度的量化多采用替代性指标或对照试验,缺乏直接监测数据,也缺乏不同草地类型对放牧强度变化的响应差异性研究。以西藏自治区那曲市为研究区,利用佩戴式GPS牛羊定位器构建高精度放牧轨迹数据集模拟放牧强度,构建栅格尺度放牧强度空间分布和划分方法,结合草地群落样方调查,通过Duncan法（Duncan''s multiple comparative analysis）进行多重比较分析,探究自由放牧模式下高寒草甸和高寒草原两类区域植被和土壤对不同放牧强度的响应方式及差异性。本研究可为放牧行为环境效应监测提供新思路,并根据不同草地状况因地制宜提出放牧优化管理策略,助力高寒传统牧区的可持续发展。主要结论有：1）随着放牧强度的增大,高寒草原地上生物量先升高后降低,高强度放牧对高寒草原植被的影响大于高寒草甸。2）高放牧强度下,高寒草原土壤水分显著高于中低强度,高寒草甸土壤容重显著低于低强度。可能原因是放牧压力多集聚于水源附近。高寒草原区土壤的砂粒含量随放牧强度的增大而增加。放牧强度的增大导致草甸上层土壤有机质增加,草甸下层、草原上层、草原下层土壤有机质先增加后减小。草甸上下层土壤全磷含量在低放牧强度下显著低于中高强度。3）植被土壤变化受到自然因子和放牧活动的共同影响。高寒草甸更加耐牧,高强度放牧对高寒草原的负面影响更大,而中度放牧有利于草地尤其是高寒草原的放牧利用。4）放牧生态系统是一个环境-植物-家畜自适应系统。在放牧管理中不能仅通过控制载畜量缓解草地超载,还需要综合考虑生态系统的弹性及各营养级的适应性,合理配置放牧强度,控制季节性超载和局部超载。     

Response of soil bacterial communities to moisture and grazing in the Tibetan alpine steppes on a small spatial scale

As the Third Pole of the world, the Tibetan Plateau provides a typical alpine grassland environment for soil bacteria with its unique frigid and arid climate. Owing to clear changes in spatial moisture and increased grazing intensity, moisture and livestock grazing have become key factors influencing the microbial communities. Accordingly, we investigated the diversity and composition of soil bacteria in a selected alpine grassland within the dual gradients of moisture and grazing using high-throughput sequencing. Our results showed that grazing changed the soil bacterial diversity and composition, whereas moisture only influenced the relative abundance of the segmental community at the small spatial scale. Species richness was found to be increased by moderate grazing compared with that by high or low-grazing intensity. The relative abundance of dominant species and β-diversity of soil bacteria both showed differences with heavy, moderate, and low grazing. Some dominant bacteria were altered with the moisture content. However, there were no significant differences according to the moisture gradient in terms of the overall bacterial β diversity and composition. These results might be taken account into the small spatial scale as well as the compensation of grazing to moisture on this scale. This work provides new insights into the soil bacterial response to moisture gradients and grazing intensity in alpine steppe habitat.     

自然保护区退牧还草生态补偿标准——以向海国家级自然保护区为例

我国部分自然保护区中拥有大面积草原,但由于过度放牧,面临草原面积减少、质量下降等问题,其重要原因之一是缺少合理的补偿标准导致牧民生计得不到有效保障,偷牧行为屡禁不止。研究制定自然保护区的退牧还草生态补偿标准、完善补偿机制,对于提高我国自然保护区内草原的生态环境质量、改善牧民生计具有重要意义。以我国自然保护区草原生态环境破坏的典型案例--吉林向海国家级自然保护区为例,构建自然保护区退牧还草生态补偿标准制定框架,包括识别影响保护区牧民退牧还草意愿的关键因素,遴选生态补偿标准计算方法;根据草原承包经营权、保护区功能分区、草原利用情况等对补偿客体进行分类;制定针对不同客体的多种补偿标准方案,并提出其优先序。研究结果显示：影响向海国家级自然保护区牧民退牧还草的关键因素为文化程度、务农人口比例、原有牲畜数量和已退养牲畜数量。核心区、缓冲区内未承包草原放牧的牧民的最佳补偿标准为833元 羊单位^-1 a^-1;核心区、缓冲区内承包草原放牧的牧民的最佳补偿标准为913元 羊单位^-1 a^-1;核心区、缓冲区内承包草原未放牧的牧民的最佳补偿标准为120元 羊单位^-1 a^-1;实验区牧民的最佳补偿标准则在核心区、缓冲区三类牧民的补偿基础上扣除牧民承包草原的理论载畜量后进行计算。建议完善牧民基本情况统计制度、拓展补偿资金来源、创新多元化补偿方式并建立动态化补偿标准调整机制。     

Population augmentation had no effect on the abundance or body condition of conspecifics and co‐occurring lizard species in a native grassland community

Wildlife translocations have been historically plagued by failure. As more species gain endangered status, we must increase the success rate through use of pre‐emptive empirical, evidence‐based research. The main ecological risk is the potential for the relocated individuals to have competitive advantage at the recipient site, acting invasively and, potentially, outcompeting the native fauna for food, shelter or other resources. Here we investigated the ecological risk of increased population density, following a population augmentation of the pygmy bluetongue lizard (Tiliqua adelaidensis) an endangered lizard, endemic to South Australia. We experimentally increased T. adelaidensis density to ascertain if a sudden increase in T. adelaidensis density would negatively affect the abundance or body condition of the resident conspecifics and co‐existing lizard species found at the recipient site. Twenty‐four individuals, from two populations, were relocated into previously built enclosures at a recipient site in grassland habitat, north of Adelaide, South Australia. For one activity‐season pre and post the augmentation, co‐existing lizard species were sampled in an effort to detect any changes inabundance or body condition. Comparisons were also made between experimental enclosures, containing residents and translocated individuals and control enclosures, containing only residents. Using Menetia greyii as a proxy for all of the competing species, our results show there was no reduction in abundance or body condition post augmentation. Our lack of evidence indicating a negative impact of the T. adelaidensis translocation on the body condition and abundance of the resident lizard species is a positive outcome for future conservation of this species. This study provides a new way of approaching wildlife movements, through identification of potential risks using small‐scale translocations in an enclosed area before conducting large‐scale releases into unfenced areas; the results are intended to facilitate higher translocation success rates and limit the negative effects upon the wider ecological community at recipient sites.     

土壤纤毛虫群落对退牧还草生态恢复的响应——以玛曲县为例

为研究退牧还草对土壤纤毛虫群落特征的影响、退牧还草后土壤环境变化以及如何利用原生动物纤毛虫群落特征来评价退还效果的可行性,于2015年5月至2016年3月在甘肃省甘南藏族自治州玛曲县选取3个不同恢复年限的草地样点和1个未经过退牧还草对照样点,采用"非淹没培养皿法"、活体观察法和培养直接计数法对土壤纤毛虫的物种数和密度进行测定,同时测定了土壤温度、pH值、含水量、土壤孔隙度、速效钾、速效氮、速效磷、全氮、全钾、全磷和有机质含量,并分析了在生态逐渐恢复条件下,土壤纤毛虫群落特征与土壤环境因子间的相关性。研究共鉴定到纤毛虫95种,隶属9纲15目21科28属。研究发现,退牧还草样地与未退牧还草样地的土壤纤毛虫的物种分布存在明显差异:退牧还草后的3个样点间的物种相似性减小,群落组成复杂化,纤毛虫丰度、丰富度指数、均匀度指数和物种多样性指数增高。相关性分析结果表明,退牧还草后,对纤毛虫群落结构稳定性影响最主要的是土壤有机质、含水量和土壤全氮、全磷和全钾的含量,不同恢复年限样点的土壤纤毛虫群落组成差异较大。土壤纤毛虫群落对退牧还草生态恢复过程中土壤环境条件的变化有较好的响应。     

Grassland to shrubland state transitions enhance carbon sequestration in the northern Chihuahuan Desert

The replacement of native C₄‐dominated grassland by C₃‐dominated shrubland is considered an ecological state transition where different ecological communities can exist under similar environmental conditions. These state transitions are occurring globally, and may be exacerbated by climate change. One consequence of the global increase in woody vegetation may be enhanced ecosystem carbon sequestration, although the responses of arid and semiarid ecosystems may be highly variable. During a drier than average period from 2007 to 2011 in the northern Chihuahuan Desert, we found established shrubland to sequester 49 g C m^?2 yr^?1 on average, while nearby native C₄ grassland was a net source of 31 g C m^?2 yr^?1 over this same period. Differences in C exchange between these ecosystems were pronounced – grassland had similar productivity compared to shrubland but experienced higher C efflux via ecosystem respiration, while shrubland was a consistent C sink because of a longer growing season and lower ecosystem respiration. At daily timescales, rates of carbon exchange were more sensitive to soil moisture variation in grassland than shrubland, such that grassland had a net uptake of C when wet but lost C when dry. Thus, even under unfavorable, drier than average climate conditions, the state transition from grassland to shrubland resulted in a substantial increase in terrestrial C sequestration. These results illustrate the inherent tradeoffs in quantifying ecosystem services that result from ecological state transitions, such as shrub encroachment. In this case, the deleterious changes to ecosystem services often linked to grassland to shrubland state transitions may at least be partially offset by increased ecosystem carbon sequestration.     

草原矿区土壤环境损害基线评估判定的应用研究——以内蒙古草原矿区为例

草原生态环境损害评估鉴定中,土壤基线是重要的评价标准。如何确定土壤基线,寻找适宜的基线判定方法,进而判定草原土壤的受损害程度,已成为草原生态系统损害评估鉴定、生态系统保护及修复工作中的关键。基于科学、务实、准确的原则,对内蒙古2个草原矿区土壤的总有机质（TOM）、N、P、K含量进行采样分析,采用历史数据法、参考点位法和统计点位法来判定土壤基线。结果表明,胜利矿区土壤养分均值与参考点位法基线值差异较小,采矿对胜利矿区土壤养分含量未见直接的影响。宝日希勒矿区土壤中TOM含量均值明显低于3种方法得出的基线值,N、K均值与参考点位法基线值相似,P均值位于3种基线值之间。可见采矿对宝日希勒矿区土壤中TOM的含量造成了直接影响,对N、P、K含量未见直接的影响。最适宜该地区的方法取决于样本质量和评估尺度,建议以参考点位法为主,历史数据法和统计点位法作为验证工具,3种方法共同使用。