闽江河口红树林土壤微生物群落对互花米草入侵的响应

采用磷脂脂肪酸标记法(PLFA)研究外来入侵植物互花米草对闽江河口湿地红树林土壤微生物群落结构的影响,并探讨其主要影响因素。结果表明:从3种不同植被群落土壤(红树林群落MC、红树林-互花米草混生群落MS、互花米草群落SC)共检测到22种PLFA生物标记,MS土壤微生物PLFA生物标记总量明显高于其他植被群落,3种植被群落土壤理化性质和酶活性的变化趋势为:MCMSSC,表明互花米草入侵后土壤微生物量增加,而理化性质和酶活性均有明显下降,红树林湿地土壤质量发生了明显退化。3种植被群落土壤中含量最高的PLFA生物标记是16:0,16:1w7c,9Me15:0w,18:1w12c。土壤中特征微生物相对生物量存在明显差异,细菌分布量最大,其次是真菌和放线菌,原生动物分布量最小。群落多样性指数呈相似规律,MS土壤微生物类群多样性指数均小于MC,表明互花米草入侵后土壤微生物群落多样性指数均有下降。通过主成分分析,基本能区分出3种不同植被群落微生物群落的特征。土壤理化性质、酶活性间存在相关性,有机碳、全氮、蔗糖酶、过氧化氢酶与革兰氏阴性菌、放线菌呈显著或极显著正相关。研究结果表明互花米草入侵在一定程度上具有影响红树林群落土壤营养代谢循环的潜力,特别是关于碳、氮、磷等的循环及酶活性,改变部分有利于自身生长的土壤环境相关的微生物类群含量,竞争有利环境,迅速扩张实现入侵。     

黄顶菊对不同入侵地植物群落及土壤微生物群落的影响

为明确不同入侵地植物群落和土壤生态对黄顶菊入侵的反馈机制,选取天津静海(JH)、河北沧州(CZ)、河北衡水(HS)及河南安阳(AY)4个黄顶菊入侵典型区域,研究黄顶菊对不同入侵地植物群落多样性、土壤理化及土壤微生物群落结构的影响,并进一步揭示植物群落、土壤养分和土壤微生物之间的相关关系。结果表明,黄顶菊入侵显著降低了JH、CZ和HS的植物群落多样性指数(P0.05),改变了四个地区的土壤理化性质,显著升高了不同入侵地真菌PLFA的含量、总PLFA的含量、真菌/细菌和革兰氏阴性菌/革兰氏阳性菌(P0.05),降低了土壤微生物的Margalef丰富度指数(P0.05),但均存在地区间差异;RDA和相关分析的结果表明,硝态氮、全氮的含量对植物群落的影响较大,而铵态氮的含量对土壤微生物群落结构的影响较大,除丰富度指数外,植物群落与土壤微生物群落的多样性指数之间存在显著的负相关关系(P0.05)。总之,黄顶菊改变了入侵地植物群落多样性,并且对入侵地土壤理化性质和土壤微生物群落结构产生了显著影响,且存在地区差异。本研究将为更好的理解外来植物的入侵机制及制定相应的防控策略提供理论依据。     

贺兰山不同海拔植被下土壤微生物群落结构特征

为明确海拔变化对干旱区山地森林土壤微生物群落的影响,揭示环境因子改变后土壤微生物群落结构特征及影响因素。对贺兰山5个海拔梯度土壤理化性质进行测定,同时采用磷酸脂肪酸(PLFA)图谱法分析土壤微生物群落组成,通过主成分分析、冗余分析(RDA)探究土壤理化性质与土壤微生物群落相对丰度之间的相关关系。结果表明:土壤养分含量在不同海拔之间差异性显著(P<0.05),土壤有机碳和全氮含量随海拔的升高而升高,全磷含量随海拔升高先升高再降低再升高;土壤微生物量随海拔升高先升高后降低,土壤微生物的相对丰度在不同海拔之间存在差异(P<0.05);主成分分析表明,与第1主成分相关性较强的微生物类群为革兰氏阳性细菌(G~+)、革兰氏阴性细菌(G~-)和真菌;与第2主成分相关性较强的微生物类群为放线菌、原生动物和非特异性细菌。非特异性细菌和真菌与各土壤因子之间均有显著相关关系,而放线菌、G~+和G~-与各土壤因子相关性较弱,原生动物与土壤全磷含量的关系密切。海拔是影响特征微生物分布的重要因素,特征微生物的含量和相对丰度随海拔的升高先升高后降低,符合山地生态学中的"中部膨胀"理论。探明了贺兰山不同海...     

羊草基因型数目与氮添加对土壤微生物群落的交互影响

物种多样性(或同一物种遗传多样性)减少和氮富集都是影响陆地生态系统进程的主要因素,它们之间的交互作用是否对土壤微生物群落产生显著影响已成为研究者关心的主要科学问题。研究羊草基因型数目(1、2、4三种基因型数目组合)和氮添加(无氮添加、低氮添加和高氮添加3种水平)对土壤微生物群落的总磷脂脂肪酸(PLFA,Phospholipid Fatty Acid)含量、细菌PLFA生物标记含量、真菌PLFA生物标记含量、真菌/细菌比、以及基于每个PLFA生物标记相对含量百分比所得微生物群落的Shannon-Wiener多样性指数和Simpson优势度指数的影响。结果表明:氮添加对细菌PLFA生物标记含量,以及土壤微生物PLFA生物标记的Shannon-Wiener多样性指数和Simpson优势度指数具有显著影响(P0.05);基因型数目对所测变量无显著影响(P0.05),但基因型数目和氮添加的交互作用对细菌PLFA生物标记含量和真菌/细菌比具有显著影响(P0.05)。研究结果为全球变化背景下氮沉降及重要物种种群数量减少对土壤微生物群落的影响提供了科学数据,为合理解释群落动态变化提供了数据支持。     

脂肪酸甲酯法检测空心莲子草入侵影响土壤微生物群落结构的初步研究

空心莲子草是我国2003年公布的第一批外来入侵物种。为了进一步了解该植物的入侵机制,采集湖北咸宁、仙桃和武汉三地的土样,采用土壤脂肪酸甲酯谱图分析的方法探讨该植物入侵对土壤微生物的影响。结果显示：空心莲子草入侵后土壤可培养细菌、真菌的数量显著增加,而放线菌的数量显著下降。脂肪酸分析表明土壤微生物群落结构发生一定程度的改变,但其变化因土壤的不同而有差异。     

紫茎泽兰(Ageratina adenophora)入侵对土壤微生物群落和理化性质的影响

外来入侵植物与入侵地土壤微生物群落的互作关系是影响外来植物入侵力和生态系统可入侵性的一个重要领域。因此,研究外来植物入侵对入侵地土壤微生物群落及其理化性质的影响不仅可以全面地评估入侵植物对生态系统的影响,而且对于探索外来植物入侵的土壤微生物学机制尤为重要。采用磷脂脂肪酸(PLFAs)和传统培养相结合的方法研究了外来入侵植物紫茎泽兰对入侵地土壤微生物群落结构的影响;同时研究了紫茎泽兰入侵对11种土壤理化因子的影响。结果表明紫茎泽兰入侵改变了土壤微生物群落结构,提高了土壤自生固氮菌、氨氧化细菌和真菌的数量;同时,显著地提高了土壤的有效磷、速效钾、硝态氮、氨态氮和土壤有机碳含量,降低了土壤总钾含量和pH值。土壤微生物不同生理类群的变化与土壤中植物可直接吸收利用养分的变化显著相关。紫茎泽兰在入侵地成功定殖后,可能通过改变土壤微生物群落结构,特别是增加了与土壤养分循环相关的微生物功能类群数量,进而提高了土壤可利用的养分水平,创造对自身生长有利的土壤环境。紫茎泽兰改变土壤微生物群落是其入侵的一部分,这种改变进而加速了土壤养分循环,可能增强了紫茎泽兰的养分吸收,进而促进其生长、竞争和扩张。     

黄顶菊入侵对土壤氨氧化细菌群落结构及多样性的影响

入侵植物通常会改变入侵地土壤微生物群落,进而影响到土壤养分循环以及物种之间的竞争格局。研究入侵植物对入侵地土壤微生物群落的影响不仅可以评估其对入侵地生态系统的影响,也为探明外来植物入侵的土壤微生物学机制提供理论依据。本文利用聚合酶链式反应变性梯度凝胶电泳(PCR-DGGE)技术及序列分析方法研究了入侵植物黄顶菊对入侵地土壤氨氧化细菌(AOB)多样性和系统发育的影响。结果表明:未入侵土壤(CK)、入侵地根围土(BS)和入侵地根际土(RPS)土壤AOB主要为亚硝化螺菌属(Nitrosospira sp.)、亚硝化弧菌属(Nitrosovibrio)、不可培养的亚硝化单胞菌属(Nitrosomonas)和不可培养的氨氧化细菌。其中,亚硝化螺菌群和不可培养的氨氧化细菌为各样地的优势类群。各样地AOB的Shannon指数(H)变化趋势为:RPSCKBS,土壤硝化潜势变化趋势与之一致,而影响H的关键理化因子分别是土壤硝态氮和铵态氮含量。黄顶菊入侵降低了BS的AOB活性,并表现出明显的根际效应,暗示黄顶菊可能通过加速自身根际氮素周转实现其成功入侵。     

外来植物火炬树(Rhus typhina L.)入侵对不同林型土壤性质的影响

生物入侵在世界范围内广泛发生,严重威胁当地生物多样性和生态系统稳定性。植物与土壤之间的相互作用在决定植物的竞争力以及分布格局中起着重要作用,是影响外来植物入侵力和生态系统可入侵性的一个重要方面。目前,有关研究已成为植被生态学与入侵生态学的研究热点。引自北美的外来植物火炬树(Rhus typhina L.)已成为我国北方主要的入侵木本植物之一。比较了火炬树单优林型、火炬树+刺槐(Robinia pseudoacacia L.)混交林、火炬树+麻栎(Quercus acutissima Carruth.)混交林、火炬树+银白杨(Populus alba L.)混交林4种不同林型的土壤微生物群落结构、土壤酶活性和土壤养分含量特征。结果表明:火炬树单优林土壤细菌、放线菌数量明显高于各混交林型,而真菌数量无显著差异;土壤酶活性方面,火炬树单优林脲酶、过氧化氢酶活性高,土壤磷酸酶活性低;火炬树的入侵显著提高了土壤全碳、全氮、全磷和硝态氮含量,同时明显降低了土壤铵态氮含量。硝态氮含量的增高可能与火炬树入侵造成土壤微生物群落组成变化、土壤硝化速率高有关;而火炬树入侵降低了土壤铵态氮含量,说明该物种可能更易于吸收利用铵态氮。以上研究结果表明,火炬树可以改变土壤生态系统的微生物群落组成和土壤酶活性并影响土壤相关营养元素循环,从而可能使其在与当地植物的竞争中获得优势,为自身的入侵创造有利条件。     

外来种湿地松凋落物对土壤微生物群落结构和功能的影响

外来种湿地松是我国亚热带地区大面积造林树种,研究其凋落物影响下土壤微生物群落结构和功能的变化,对于全面科学的评价湿地松的生态影响具有重要的理论与实践意义。通过凋落物袋 小盆模拟试验研究,分两个时期(分解5个月和18个月)比较了外来种湿地松与本地种马尾松的凋落物对土壤微生物群落结构(磷脂脂肪酸)和功能(碳代谢)的影响,结果表明：(1)外来种湿地松凋落物的C:N高于本地种马尾松;(2)两个时期,湿地松凋落物处理土壤细菌和放线菌的磷脂脂肪酸含量均低于马尾松,18个月时湿地松凋落物处理土壤真菌含量和群落真菌/细菌显著高于马尾松处理;(3)湿地松凋落物影响下土壤微生物群落功能多样性显著低于马尾松;(4)土壤微生物群落的结构显著影响微生物的活性和功能多样性：土壤微生物群落碳源代谢的强度、多样性及丰富度与细菌磷脂脂肪酸含量呈极显著正相关,细菌特征脂肪酸14:0、15:0、a15:0、i16:0、16:1ω7c、a17:0和cy19:0的含量显著影响土壤微生物群落碳代谢功能。上述结果表明：与本地种马尾松相比,引进种湿地松的凋落物显著改变了土壤微生物群落结构,降低了微生物群落的功能。     

紫茎泽兰入侵对土壤细菌的群落组成和多样性的影响

外来生物入侵可能对生物群落结构和生态系统功能产生多种影响, 但入侵植物与土壤微生物群落组成和多样性的关系尚不清楚。为了揭示外来植物紫茎泽兰(Eupatorium adenophorum)入侵对土壤化学性质和细菌群落组成及多样性的影响, 本研究利用第二代高通量测序技术, 比较了紫茎泽兰不同入侵程度的生境(本地植物群落、紫茎泽兰与本地植物混生群落、紫茎泽兰单优群落)土壤中细菌群落的差异。土壤化学性质分析表明, 土壤pH值、有机质、全N和全K随着紫茎泽兰的入侵而逐渐降低, 而土壤全P则在入侵程度最高的生境土壤中最高。通过测序共获得7,755个细菌OUT (operational taxonomic unit)。结果表明, 紫茎泽兰入侵对土壤的细菌多样性影响较小, ACE和Chao指数在3种不同生境间的差异不显著。细菌在紫茎泽兰与本地植物混生群落中的Shannon指数最低, 即细菌的多样性在中等入侵程度的生境最低。此外, 紫茎泽兰入侵改变了土壤细菌组成和结构, 酸杆菌门(Acidobacteria)和疣微菌门(Verrucomicrobia)的相对丰度, 从本地植物群落、混合群落到紫茎泽兰单优群落, 呈现出先增加后减少的趋势。可见, 紫茎泽兰入侵一定程度上改变了土壤微生物的多样性和群落结构, 并改变了土壤的化学性质。     

No consistent legacy effects of invasion by giant goldenrod (Solidago gigantea) via soil biota on native plant growth

Aims Changes in soil microbial communities after occupation by invasive alien plants can represent legacy effects of invasion that may limit recolonization and establishment of native plant species in soils previously occupied by the invader. In this study, for three sites in southern Germany, we investigated whether invasion by giant goldenrod (Solidago gigantea) leads to changes in soil biota that result in reduced growth of native plants compared with neighbouring uninvaded soils.Methods We grew four native plant species as a community and treated those plants with soil solutions from invaded or uninvaded soils that were sterilized, or live, with live solutions containing different fractions of the soil biota using a decreasing sieve mesh-size approach. We measured aboveground biomass of the plants in the communities after a 10-week growth period.Main Findings Across all three sites and regardless of invasion, communities treated with <20 μm soil biota or sterilized soil solutions had significantly greater biomass than communities treated with the complete soil biota solution. This indicates that soil biota>20 μm are more pathogenic to the native plants than smaller organisms in these soils. Across all three sites, there was only a non-significant tendency for the native community biomass to differ among soil solution types, depending on whether or not the soil was invaded. Only one site showed significant differences in community biomass among soil solution types, depending on whether or not the soil was invaded; community biomass was significantly lower when treated with the complete soil biota solution than with soil biota <20 μm or sterilized soil solutions, but only for the invaded soil. Our findings suggest that efforts to restore native communities on soils previously invaded by Solidago gigantea are unlikely to be hindered by changes in soil microbial community composition as a result of previous invasion.     

Microbial community responses reduce soil carbon loss in Tibetan alpine grasslands under short‐term warming

Changes in labile carbon (LC) pools and microbial communities are the primary factors controlling soil heterotrophic respiration (R_h) in warming experiments. Warming is expected to initially increase R_h but studies show this increase may not be continuous or sustained. Specifically, LC and soil microbiome have been shown to contribute to the effect of extended warming on R_h. However, their relative contribution is unclear and this gap in knowledge causes considerable uncertainty in the prediction of carbon cycle feedbacks to climate change. In this study, we used a two‐step incubation approach to reveal the relative contribution of LC limitation and soil microbial community responses in attenuating the effect that extended warming has on R_h. Soil samples from three Tibetan ecosystems—an alpine meadow (AM), alpine steppe (AS), and desert steppe (DS)—were exposed to a temperature gradient of 5–25°C. After an initial incubation period, soils were processed in one of two methods: (a) soils were sterilized then inoculated with parent soil microbes to assess the LC limitation effects, while controlling for microbial community responses; or (b) soil microbes from the incubations were used to inoculate sterilized parent soils to assess the microbial community effects, while controlling for LC limitation. We found both LC limitation and microbial community responses led to significant declines in R_h by 37% and 30%, respectively, but their relative contributions were ecosystem specific. LC limitation alone caused a greater R_h decrease for DS soils than AMs or ASs. Our study demonstrates that soil carbon loss due to R_h in Tibetan alpine soils—especially in copiotrophic soils—will be weakened by microbial community responses under short‐term warming.     

Interaction between the Microbial Community and Invading Escherichia coli O157:H7 in Soils from Vegetable Fields

The survival of Escherichia coli O157:H7 in soils can contaminate vegetables, fruits, drinking water, etc. However, data on the impact of E. coli O157:H7 on soil microbial communities are limited. In this study, we monitored the changes in the indigenous microbial community by using the phospholipid fatty acid (PLFA) method to investigate the interaction of the soil microbial community with E. coli O157:H7 in soils. Simple correlation analysis showed that the survival of E. coli O157:H7 in the test soils was negatively correlated with the ratio of Gram-negative (G⁻) to Gram-positive (G⁺) bacterial PLFAs (G⁻/G⁺ ratio). In particular, levels of 14 PLFAs were negatively correlated with the survival time of E. coli O157:H7. The contents of actinomycetous and fungal PLFAs in the test soils declined significantly (P, <0.05) after 25 days of incubation with E. coli O157:H7. The G⁻/G⁺ ratio declined slightly, while the ratio of bacterial to fungal PLFAs (B/F ratio) and the ratio of normal saturated PLFAs to monounsaturated PLFAs (S/M ratio) increased, after E. coli O157:H7 inoculation. Principal component analysis results further indicated that invasion by E. coli O157:H7 had some effects on the soil microbial community. Our data revealed that the toxicity of E. coli O157:H7 presents not only in its pathogenicity but also in its effect on soil microecology. Hence, close attention should be paid to the survival of E. coli O157:H7 and its potential for contaminating soils.     

Exogenous application of plant defense hormones alters the effects of live soils on plant performance

The overall effect of a live soil inoculum collected from nature on plant biomass is often negative. One hypothesis to explain this phenomenon is that the overall net pathogenic effect of soil microbial communities reduces plant performance. Induced plant defenses triggered by the application of the plant hormones jasmonic acid (JA) and salicylic acid (SA) may help to mitigate this pathogenic effect of live soil. However, little is known about how such hormonal application to the plant affects the soil and how this, in turn, impacts plant growth. We grew four plant species in sterilized and inoculated live soil and exposed their leaves to two hormonal treatments (JA and SA). Two species (Jacobaea vulgaris and Cirsium vulgare) were negatively affected by soil inoculation. In these two species foliar application of SA increased biomass in live soil but not in sterilized soil. Two other species (Trifolium repens and Daucus carota) were not affected by soil inoculum and for these two species foliar application of SA reduced plant biomass in both the sterilized and live soil. Application of JA reduced plant biomass in both soils for all species. We subsequently carried out a multiple generation experiment for one of the plant species, J. vulgaris. In each generation, the live soil was a mixture of 10% soil from the previous generation and 90% sterilized soil and the same hormonal treatments were applied. The negative effects of live soil on plant biomass were similar in all four generations, and this negative effect was mitigated by the application of SA. Our research suggests that the application of SA can mitigate the negative effects of live soil on plant growth. Although the inoculum of soil containing a natural live soil microbial community had a strong negative effect on the growth of J. vulgaris, we found no evidence for an increase or decrease in negative plant-soil feedback in either the control or the SA treated plants. Also plant performance did not decrease consistently with succeeding generations.     

Establishment and effectiveness of inoculated arbuscular mycorrhizal fungi in agricultural soils

Arbuscular mycorrhizal fungi (AMF) are promoted as biofertilizers for sustainable agriculture. So far, most researchers have investigated the effects of AMF on plant growth under highly controlled conditions with sterilized soil, soil substrates or soils with low available P or low inoculum potential. However, it is still poorly documented whether inoculated AMF can successfully establish in field soils with native AMF communities and enhance plant growth. We inoculated grassland microcosms planted with a grass–clover mixture (Lolium multiflorum and Trifolium pratense) with the arbuscular mycorrhizal fungus Rhizoglomus irregulare. The microcosms were filled with eight different unsterilized field soils that varied greatly in soil type and chemical characteristics and indigenous AMF communities. We tested whether inoculation with AMF enhanced plant biomass and R. irregulare abundance using a species specific qPCR. Inoculation increased the abundance of R. irregulare in all soils, irrespective of soil P availability, the initial abundance of R. irregulare or the abundance of native AM fungal communities. AMF inoculation had no effect on the grass but significantly enhanced clover yield in five out of eight field soils. The results demonstrate that AMF inoculation can be successful, even when soil P availability is high and native AMF communities are abundant.     

An invasive aster (Ageratina adenophora) invades and dominates forest understories in China: altered soil microbial communities facilitate the invader and inhibit natives

Exotic plant invasion may alter underground microbial communities, and invasion-induced changes of soil biota may also affect the interaction between invasive plants and resident native species. Increasing evidence suggests that feedback of soil biota to invasive and native plants leads to successful exotic plant invasion. To examine this possible underlying invasion mechanism, soil microbial communities were studied where Ageratina adenophora was invading a native forest community. The plant–soil biota feedback experiments were designed to assess the effect of invasion-induced changes of soil biota on plant growth, and interactions between A. adenophora and three native plant species. Soil analysis showed that nitrate nitrogen (NO₃⁻-N), ammonium nitrogen (NH₄⁺-N), and available P and K content were significantly higher in a heavily invaded site than in a newly invaded site. The structure of the soil microbial community was clearly different in all four sites. Ageratina adenophora invasion strongly increased the abundance of soil VAM (vesicular-arbuscular mycorrhizal fungi) and the fungi/bacteria ratio. A greenhouse experiment indicated that the soil biota in the heavily invaded site had a greater inhibitory effect on native plant species than on A. adenophora and that soil biota in the native plant site inhibited the growth of native plant species, but not of A. adenophora. Soil biota in all four sites increased A. adenophora relative dominance compared with each of the three native plant species and soil biota in the heavily invaded site had greater beneficial effects on A. adenophora relative dominance index (20% higher on average) than soil biota in the non-invaded site. Our results suggest that A. adenophora is more positively affected by the soil community associated with native communities than are resident natives, and once the invader becomes established it further alters the soil community in a way that favors itself and inhibits natives, helping to promote the invasion. Soil biota alteration after A. adenophora establishment may be an important part of its invasion process to facilitate itself and inhibit native plants.     

基于梯度稀释法分析细菌多样性对土壤碳代谢的影响

为探究土壤微生物多样性对土壤碳代谢过程的影响,利用梯度稀释法(处理D1、D3和D5分别为稀释10-1、10-3和10-5倍)改变土壤样品中原始土壤微生物群落的多样性,以探究土壤微生物群落多样性减少对土壤碳代谢的影响。进行为期6周的预培养实验,以消除梯度稀释法对土壤样品中微生物群落丰度的影响,并通过Q-PCR和高通量测序测定预培养结束后3种土壤样品中细菌丰度及其基因多样性指数(ACE、Chao1、Shannon),以验证预培养实验结果。后加入等量葡萄糖(0.5g/100g干土)继续培养,并于培养期间测定3种处理土壤的碳矿化速率,进行biolog ECO板实验,分析计算各土壤样品中细菌的功能多样性指数(Shannon指数(H)、Simpson指数(D)、McIntosh指数(U))及碳源代谢强度。结果表明:(1)3种处理土壤样品碳矿化速率及累积碳矿化量大小排序为:D1> D3> D5,且D1与D3、D5处理均有显著差异(P<0.05)。(2)D1处理下土壤样品中微生物群落的孔平均颜色变化率(AWCD)、功能多样性指数(Shannon指数(H)、McIntosh指数(U))均显著高于D3、D5处理(P<0.05)。(3)对31种碳源吸光度做主成分分析(PCA)分析,发现3种稀释处理下土壤样品的碳源利用模式存在差异,且D1处理下的土壤微生物群落对碳源的代谢功能大于D3、D5处理。因此,该研究表明土壤微生物多样性的减少会降低土壤的碳矿化速率及其碳源代谢强度,对土壤碳代谢过程产生一定程度的不利影响。     

Shifts in priming partly explain impacts of long‐term nitrogen input in different chemical forms on soil organic carbon storage

Input of labile organic carbon can enhance decomposition of extant soil organic carbon (SOC) through priming. We hypothesized that long‐term nitrogen (N) input in different chemical forms alters SOC pools by altering priming effects associated with N‐mediated changes in plants and soil microbes. The hypothesis was tested by integrating field experimental data of plants, soil microbes and two incubation experiments with soils that had experienced 10 years of N enrichment with three chemical forms (ammonium, nitrate and both ammonium and nitrate) in an alpine meadow on the Tibetan Plateau. Incubations with glucose–¹³C addition at three rates were used to quantify effects of exogenous organic carbon input on the priming of SOC. Incubations with microbial inocula extracted from soils that had experienced different long‐term N treatments were conducted to detect effects of N‐mediated changes in soil microbes on priming effects. We found strong evidence and a mechanistic explanation for alteration of SOC pools following 10 years of N enrichment with different chemical forms. We detected significant negative priming effects both in soils collected from ammonium‐addition plots and in sterilized soils inoculated with soil microbes extracted from ammonium‐addition plots. In contrast, significant positive priming effects were found both in soils collected from nitrate‐addition plots and in sterilized soils inoculated with soil microbes extracted from nitrate‐addition plots. Meanwhile, the abundance and richness of graminoids were higher and the abundance of soil microbes was lower in ammonium‐addition than in nitrate‐addition plots. Our findings provide evidence that shifts toward higher graminoid abundance and changes in soil microbial abundance mediated by N chemical forms are key drivers for priming effects and SOC pool changes, thereby linking human interference with the N cycle to climate change.     

氮肥添加对高寒藏嵩草(Kobresia tibetica)沼泽化草甸和土壤微生物群落的影响

以藏嵩草沼泽化草甸为研究对象,利用磷脂脂肪酸(PLFA)技术,研究连续6年N素添加对地上植被群落数量特征、土壤微生物群落结构的影响。结果表明:①藏嵩草沼泽化草甸群落生物量、枯枝落叶对施肥处理无明显响应,且莎草科植物对土壤氮素的吸收和利用率较低。②施肥增加了0-10 cm土壤微生物类群PLFAs丰富度尤其细菌和革兰氏阳性菌PLFAs,降低了10-20 cm PLFAs丰富度;③磷脂脂肪酸饱和脂肪酸/单烯不饱和脂肪酸、细菌PLFAs/真菌PLFAs的比值随土壤层次增加而增加;④0-10 cm土层革兰氏阳性菌、真菌PLFAs含量与pH、土壤速效磷、速效氮、土壤有机质显著正相关(P0.05或P0.01);10-20 cm土层,细菌、革兰氏阳性菌、真菌和总PLFAs含量与土壤有机质含量显著正相关(P0.05或P0.01)。表明藏嵩草沼泽化草甸微生物PLFAs含量和丰富度对施肥的响应存在明显的土层梯度效应,土壤微生物PLFAs含量和丰富度主要受表层土壤初始养分含量的影响。