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1.
苔藓结皮是地表重要的活性覆盖物,具有改善土壤性状、固土持水、固碳固氮等多种生态功能,微生物群落是苔藓结皮发挥生态功能的主要成分。为了探究湿润区石生苔藓结皮的微生物群落组成及其多样性特征,揭示其发育形成机制以及功能机理,该研究以秦岭北麓的泥峪、车峪、骆峪5个样地的石生苔藓结皮为研究对象,利用高通量测序技术,分析了石生苔藓结皮层的微生物群落组成、丰度、多样性,并测定分析养分与微生物群落的关系,为裸露岩石创面的生态修复提供理论依据。结果表明:(1)秦岭石生苔藓结皮层的全氮和有机质含量在4.16~8.26 g/kg、89.44~131.05 g/kg之间,且样点间均差异显著;全磷和全钾含量较低,分别为0.88~1.21 g/kg和13.50~18.10 g/kg。(2)秦岭石生苔藓结皮层中细菌占微生物群落组成的80%以上,且细菌的多样性也远高于真菌;其中细菌优势菌群为变形菌门(Proteobateria)、拟杆菌门(Bateroidetes)、放线菌门(Actinobacteria)和酸杆菌门(Acidobacteria),真菌优势菌群为子囊菌门(Ascomycota)和被孢霉菌门(Mortierellomycota)。(3)冗余分析(RDA)显示,全钾和有机质对优势细菌群落结构影响显著,变形菌和拟杆菌适宜生活在湿度大、营养状况良好的基质中;全磷和有机质对优势真菌群落结构影响显著,被孢霉菌门在低磷基质中更具生长优势。研究发现,细菌是秦岭石生苔藓结皮层的优势菌群,与旱区土生状况相比,秦岭石生苔藓结皮层的放线菌和酸杆菌的含量有所下降,而拟杆菌含量显著增加;对于真菌而言,子囊菌门和担子菌门的相对丰度明显减少,被孢菌门丰度显著增加;有机质是影响结皮层微生物群落组成最主要的养分因子,丰富的养分使湿润区石生苔藓结皮层的微生物群落结构更加复杂多样、物种组成更加丰富。 相似文献
2.
Ana Giraldo‐Silva Corey Nelson Cory Penfold Nichole N. Barger Ferran Garcia‐Pichel 《Restoration Ecology》2020,28(Z2):S187-S193
Biological soil crusts are complex communities of organisms that develop on the top layer of dryland soils where they enhance important ecosystem services, including soil fertility and protection from erosion. Regrettably, a range of human activities such as cattle grazing, off‐road driving, hiking, and global warming result in significant deterioration of biocrust cover and their associated services. This scenario has prompted efforts to develop effective biocrust restoration strategies, which often involve the production of biocrust inoculum, both in greenhouse and in laboratory settings. Sometimes this inoculum is preconditioned in a process of “hardening” at considerable expense and effort in order to improve its fitness under harsh field conditions. But the positive effects of such hardening procedures have yet to be rigorously demonstrated. Here, we compared the growth performance of 20 cultured strains of biocrust cyanobacteria in outdoor tests on native soils as a function of preconditioning regimes consisting of increasingly high exposure to solar radiation, temperature and illumination daily variability, and recurrent wet‐dry cycles. Preconditioning improved performance in 13 out of 20 strains, particularly among pioneer crust‐forming Microcoleus spp. (eight out of eight). Improvements were variable among heterocystous strains (three out of four Scytonema spp., two out of four Tolypothrix spp., and none out of four Nostoc spp.). Based on these results, we recommend the inclusion of preconditioning treatments to increase inoculum survival rate and speed of cyanobacterial biocrust recovery in restoration of dryland soils. 相似文献
3.
4.
Ana Giraldo‐Silva Corey Nelson Nichole N. Barger Ferran Garcia‐Pichel 《Restoration Ecology》2019,27(4):793-803
Biological soil crusts (biocrust) are microbial communities that develop at the soil surface of drylands and play an important role in erosion control and fertility. Soil surface disturbance from a broad range of natural and human processes (e.g. fire, livestock grazing, off‐road traffic) cause significant losses in biocrust cover and associated ecosystems services. Hence, biocrust restoration is emerging as an important intervention strategy to rehabilitate degraded dryland soils. In a multistep process, we designed protocols for the establishment of “microbial nurseries” to produce photosynthetic cyanobacterial inoculum for biocrust seeding at scale. We first report on the strategy for isolation, directly from the target site, of a large culture collection of cyanobacteria that included multiple representatives of the five most common biocrust taxa. After genetic pedigreeing of these isolates, we could select those that best matched field populations genetically for scale‐up cultivation. We then developed protocols for effective cyanobacterial biomass production to obtain sufficient inoculum. This was followed by conditioning treatments (hardening off) to preacclimate this inoculum to the stressful conditions expected in the field. Finally, we show that the inoculum obtained was fit to thrive in its original soil under natural outdoor conditions if sufficient water was available. We repeated this process successfully for four sites, two in the hot Chihuanuan desert and two in the cooler Great Basin Desert, and on two textural types of soils in each. The cyanobacterial biocrust nursery approach represents a versatile, viable, and safe tool for the rehabilitation of dryland soils. 相似文献
5.
人工生物土壤结皮（BSCs）是目前沙化土地治理的新方法和新模式,播撒天然BSCs碎片是培养人工BSCs的有效方法之一。降雨显著影响人工BSCs的拓殖和发育,已有的研究多集中于探讨降雨总量和频次对单一类别的人工BSCs的影响。而单次降雨量如何影响不同类别的人工BSCs生长发育,仍鲜见报道。以腾格里沙漠东南缘的天然藓类（N-M）、天然蓝藻-地衣（N-CL）、天然蓝藻（N-C）和人工蓝藻（A-C）结皮碎片作为培养人工BSCs的材料,探讨了1 mm、2 mm和5 mm的单次降雨量与不同类别BSCs碎片对人工BSCs的影响。结果表明,在3种单次降雨量处理下使用3种天然BSCs碎片和A-C结皮碎片均可成功培养人工BSCs,2 mm单次降雨量处理下人工BSCs的发育效果最好,而N-C和A-C较其他类别在培养早期具有较高的盖度（32.5%）和叶绿素a含量（11.39 μg/cm2）。回归分析发现,人工BSCs的盖度与单次降雨量呈二项式相关;N-M和N-CL的厚度与单次降雨量呈二项式相关,N-C和A-C与单次降雨量呈对数相关;N-C的叶绿素a含量和单次降雨量呈线性正相关;N-M的松散结合胞外多糖含量和单次降雨量呈线性负相关;N-M和A-C的紧密结合胞外多糖含量和单次降雨量分别呈线性负相关和指数相关（P<0.05）。研究证明了单次降雨量和BSCs类别显著影响人工BSCs的拓殖和发育。同时发现A-C较N-C发育更稳定。因此,建议在使用人工BSCs进行大规模生态恢复时,应选择适宜的BSCs类别并优先选择人工BSCs碎片作为培养材料。 相似文献
6.
Anita Antoninka Matthew A. Bowker Nichole N. Barger Jayne Belnap Ana Giraldo‐Silva Sasha C. Reed Ferran Garcia‐Pichel Michael C. Duniway 《Restoration Ecology》2020,28(Z2):S150-S159
Methods to reduce soil loss and associated loss of ecosystem functions due to land degradation are of particular importance in dryland ecosystems. Biocrusts are communities of cyanobacteria, lichens, and bryophytes that are vulnerable to soil disturbance, but provide vital ecosystem functions when present. Biocrusts stabilize soil, improve hydrologic function, and increase nutrient and carbon inputs. Methods to reestablish biocrust rapidly, when lost from ecosystems, have the potential to restore important dryland ecosystem functions and thereby increase probability of successful rehabilitation. The aim of this study was to identify habitat ameliorations to enhance the success of biocrust inoculation by: (1) reducing physiological stress on biocrusts and increasing resource availability (using shade, soil surface roughening, and watering), and (2) stabilizing mobile soils (using straw borders, three soil tackifiers [soil stabilizers], and a combination of shade, water, roughening, and tackifier). In the Great Basin Desert on the Utah Test and Training Range near Salt Lake City, we applied field‐harvested biocrust material to experimental plots on coarse‐ and fine‐textured soils with the top 2 cm of soil and biocrust removed. Habitat ameliorations were applied with and without biocrust addition. Shade provision increased biocrust cover 50% over controls. Biocrust cover and soil stability were 65% lower in straw border plots relative to controls. Soil tackifiers, alone and in combination with resource augmentation and stress reduction, did not improve cover and stabilization over inoculated controls. We found variability in recovery by time and between soil types. These results suggest plausible strategies to improve success of biocrust inoculation. 相似文献
7.
Efforts are being made to upscale restoration of New Zealand's native ecosystems. Success depends, however, on consideration of several key issues that need to be built into restoration planning, implementation and monitoring. This study makes eight recommendations to improve the prospect of obtaining the hoped‐for biodiversity conservation outcomes. 相似文献
8.
Corrine Duncan Megan K. Good Ian Sluiter Simon Cook Nick L. Schultz 《Restoration Ecology》2020,28(Z1):A35-A43
The biogeochemical properties of soils drive ecosystem function and vegetation dynamics, and hence soil restoration after mining should aim to reinstate the soil properties and hydrological dynamics of remnant ecosystems. The aim of this study is to assess soil structure in two vegetation types in an arid ecosystem, and to understand how these soil properties compare to a reconstructed soil profile after mining. In an arid ecosystem in southeast Australia, soil samples were collected at five depths (to 105 cm) from remnant woodland and shrubland sites, and sites either disturbed or totally reconstructed after mining. We assessed soil physico‐chemical properties and microbial activity. Soils in the remnant arid ecosystem had coarse‐textured topsoils that overlay clay horizons, which allows water to infiltrate and avoid evaporation, but also slows drainage to deeper horizons. Conversely, reconstructed soils had high sand content at subsoil horizons and high bulk density and compaction at surface layers (0–20 cm). Reconstructed soils had topsoils with higher pH and electrical conductivity. The reconstructed soils did not show increased microbial activity with time since restoration. Overall, the reconstructed soil horizons were not organized in a way that allowed rainfall infiltration and water storage, as is imperative to arid‐zone ecosystem function. Future restoration efforts in arid ecosystems should focus on increasing sand content of soils near the surface, to reduce evaporative water loss and improve soil quality and plant health. 相似文献
9.
Until recently, parameters from microorganisms were generally not included in risk assessment at a comparable level to animals and plants. However, the major part of global biomass, biodiversity, and ecosystem processes is present in the microbial world and microbiological techniques applicable to risk assessment are becoming available. Two microbial indicators are described based on the usage of multiwell plates with different substrates and a redox indicator for monitoring mineralisation. With both techniques autochthonous microbial communities are analysed. Producing functional fingerprints of the microbial community gives insights into the composition of different functions. This is equivalent to observations of ecological abundance and species composition. When lack of reference sites or reference data renders risk assessment difficult, measurement of the pollution-induced community tolerance (PICT) can provide useful information. 相似文献
10.
Akasha M. Faist Anita J. Antoninka Jayne Belnap Matthew A. Bowker Michael C. Duniway Ferran Garcia‐Pichel Corey Nelson Sasha C. Reed Ana Giraldo‐Silva Sergio Velasco‐Ayuso Nichole N. Barger 《Restoration Ecology》2020,28(Z2):S96-S105
As dryland degradation continues, it is increasingly important to understand how to effectively restore biocrust communities. Potential techniques include the addition of biocrust inoculum to accelerate biocrust recovery. Enhanced erosion typical of degraded environments creates a challenge for these approaches, due to loss by wind or water and burial by saltating particles. To retain and protect added inoculum, the inclusion of habitat‐amelioration techniques can improve recovery rates. This study tested three different types of inoculum (field‐collected, greenhouse‐cultivated, and laboratory‐cultivated biocrust) coupled with two treatments to augment soil stability and ameliorate habitat limitations: soil surface polyacrylamide additions and installation of straw barriers. This was done across two deserts (Great Basin and Chihuahuan) and separated into generally coarse‐ or finer‐textured soils in each desert, with results monitored for 3 years (2015, 2016, 2017). While the inoculum type, coupled with habitat ameliorations, occasionally enhanced biocrust growth across years and treatments, in other cases, it made no difference compared to natural recovery rates. Rather, the desert location and soil texture groupings were the most prominent factors in determining recovery trajectories. Recovery proportions were similar in the finer‐textured sites in both the Great Basin and the Chihuahuan deserts, while the coarser‐textured site in the Great Basin did show some recovery over time and the Chihuahuan coarser‐textured site did not. This study demonstrates the importance of understanding site potential and identifying key limitations to biocrust recovery for successful restoration projects. 相似文献
11.
Arbuscular mycorrhizae and terrestrial ecosystem processes 总被引：2，自引：0，他引：2
Matthias C. Rillig 《Ecology letters》2004,7(8):740-754
Arbuscular mycorrhizal fungi (AMF; phylum Glomeromycota) are ubiquitous in terrestrial ecosystems. Despite their acknowledged importance in ecology, most research on AMF has focused on effects on individual plant hosts, with more recent efforts aimed at the level of the plant community. Research at the ecosystem level is less prominent, but potentially very promising. Numerous human‐induced disturbances (including global change and agro‐ecosystem management) impinge on AMF functioning; hence study of this symbiosis from the ecosystem perspective seems timely and crucial. In this paper, I discuss four (interacting) routes via which AMF can influence ecosystem processes. These include indirect pathways (through changes in plant and soil microbial community composition), and direct pathways (effects on host physiology and resource capture, and direct mycelium effects). I use the case study of carbon cycling to illustrate the potentially pervasive influence of AMF on ecosystem processes. A limited amount of published research on AMF ecology is suited for direct integration into ecosystem studies (because of scale mismatch or ill‐adaptation to the ‘pools and flux’ paradigm of ecosystem ecology); I finish with an assessment of the tools (experimental designs, response variables) available for studying mycorrhizae at the ecosystem scale. 相似文献
12.
为揭示不同人工植被修复模式对喀斯特土壤微生物群落的影响,采用氯仿熏蒸提取法和磷脂脂肪酸(phospholipid fatty acid, PLFA)法研究人工构建的降香黄檀(Dalbergia odorifera)纯林(PDOP)、顶果木(Acrocarpus fraxinifolius)纯林(PAFP)、顶果木×降香黄檀混交林(MADP)对土壤微生物生物量及土壤微生物群落结构的影响。结果表明:(1)PDOP的土壤微生物生物量碳(MBC)和微生物生物量氮(MBN)含量显著高于PAFP和MADP,PAFP显著高于MADP。(2)三种人工林土壤真菌、丛枝菌根真菌和总PLFA含量无显著差异,但PDOP土壤细菌、放线菌、丛枝菌根真菌和总PLFA含量均高于PAFP和MADP,PAFP高于MADP。PDOP的土壤细菌、革兰氏阳性菌、革兰氏阴性菌、放线菌的PLFA含量显著高于MADP。MADP的真菌细菌比显著高于PDOP,但与PAFP无显著差异。(3)冗余分析表明,土壤阳离子交换量、pH和C:N是影响土壤微生物群落组成的最主要影响因子。从三种人工林的土壤微生物生物量及微生物群落结构来看,在喀斯特地区MADP并未显示出酸性土地区混交林提高土壤微生物生物量、改善土壤微生物群落结构的优势,但混交林的真菌细菌比最高,更有利于提高土壤生态系统的稳定性。 相似文献
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Frederick A. Dadzie Angela T. Moles Todd E. Erickson Nathali Machado de Lima Miriam Muñoz-Rojas 《Restoration Ecology》2024,32(2):e14025
Restoration managers inoculate microorganisms to enhance soil function and improve restoration success, but the efficacy of these inoculations in real-world conditions is still unclear. We conducted a field experiment to test whether applying extruded seed pellets inoculated with native microbes affected soil properties related to ecosystem function in severely degraded mine soil. We found that inoculating with bacteria did not affect soil carbon, metabolic quotient (a measure of microbial stress), or basal respiration, but increased soil nitrogen by 75%, substrate-induced respiration by 147% and reduced carbon-to-nitrogen ratio by 44% compared to the control. This suggests that the bacteria inoculant contained free-living N fixers that increased the soil N content. Thus, inoculating with bacteria could supplement nitrogen fertilizers in degraded soils during soil restoration. However, we found that inoculating with a mix of bacteria and cyanobacteria did not affect any of the soil properties. This finding is counter to results in laboratory studies, suggesting that field tests are critical for understanding real-world outcomes of microbial inoculation. Finally, we found that soil microbial composition was changed by the inoculation with a mix of bacteria and cyanobacteria. None of the treatments significantly changed the diversity of soil microbial communities. Our data suggest that microbial inoculation could improve some aspects of ecosystem function and thus provide beneficial effects that might facilitate restoration of degraded sites. 相似文献
14.
David G. Chandler Natalie Day Matthew D. Madsen Jayne Belnap 《Restoration Ecology》2019,27(2):289-297
In most drylands, biological soil crusts (biocrusts), an assemblage of lichens, bryophytes, fungi, green algae, and cyanobacteria, are critical to healthy ecosystem function. However, they are extremely sensitive to disturbance and attempts to facilitate their recovery have had variable success. In this study, we applied soil amendments designed to improve soil surface stability and accelerate biocrust recovery on an area disturbed by oil/gas exploration vehicles. Treatments included: (1) control (one time water only); (2) biocrust‐only: biocrust inoculum + nutrients in water; (3) polyacrylamide gels (which are known to stabilize soils) + biocrust inoculum + nutrients in water; (4) gypsum + biocrust inoculum + nutrients in water; and (5) saline (NaCl) solution + biocrust inoculum + nutrients in water. Only the NaCl treatment showed any effects on soil properties and these were only short term. These effects included an increase in soil strength and a reduction in soil aggregate stability, unsaturated hydraulic conductivity (Kh), and cyanobacterial biomass. The inoculated biocrust material failed to develop and even after 10 years, there was only a very low natural recolonization of the plots. These results show that inoculating soils or applying these levels of soil amendments does not guarantee recovery of soil stability or biocrust, and that some sites are unlikely to recover without assistance. Thus, there is a need for more research into ways to enhance soil stability and identify the factors limiting biocrust establishment. 相似文献
15.
Melissa Chua Todd E. Erickson David J. Merritt Angela M. Chilton Mark K. J. Ooi Miriam Muoz‐Rojas 《Restoration Ecology》2020,28(Z2):S168-S176
Cyanobacteria are photosynthetic bacteria that form a fundamental part of soil biocrusts, enhance soil function and structure, and can promote plant growth. We assessed the potential of cyanobacteria as a seed bio‐primer for mine‐site restoration in an arid region in Western Australia, examining its effects on native plant growth and the characteristics of mine soil substrates used in dryland restoration. Cyanobacteria strains indigenous to the study region (Leptolyngbya sp., Microcoleus sp., Nostoc sp., and Scytonema sp.) were used to create an inoculant. Seeds of seven native plant species were bio‐primed with the inoculant, and their germination and growth assessed in a laboratory experiment. Seedling growth after bio‐priming was assessed in a glasshouse experiment for a subset of three species, in two different substrates (topsoil and mine waste). Soil properties related to soil function, e.g. total organic carbon, total nitrogen, and microbial activity, were also measured. Minor effects on germination were recorded with only significantly higher germination rates reported in E. gamophylla. Soil parameters were generally higher in topsoil than in mine waste, regardless of bio‐priming treatment. However, bio‐priming resulted in seedlings of four species producing longer radicles and/or shoots. For example, seedling root lengths of bio‐primed G. wickhamii were 57% larger than the control treatment (30.1 ± 4.3 and 13.0 ± 1.6 mm, respectively); and shoots of T. wiseana were 54% longer in the bio‐primed treatment (18.6 ± 1.6 mm) compared to the control (8.53 ± 1.4 mm). Overall, our results highlight that bio‐priming with cyanobacteria may improve plant growth for some species commonly used in dryland restoration. 相似文献
16.
栽培植物是人类赖以生存和发展的重要物质基础。全球人口与人均需求量的持续增长导致对植物资源的需求与日俱增。栽培植物较低的遗传多样性是限制其产量增长和质量提高的主要因素。栽培植物野生近缘种在自然环境中积累了丰富的遗传变异, 并在应对环境变化的过程中产生了很多新的适应性状, 是栽培植物种质创新和品种改良的重要遗传资源。然而, 栽培植物野生近缘种的存续和自然进化因生境破坏以及全球气候变化等正面临严重威胁, 需要采取有效的措施进行保护。本文总结了国内外对栽培植物野生近缘种进行原生境保护与迁地保护所取得的进展, 并基于我国实际情况提出了栽培植物野生近缘种的保护建议。此外, 本文还对栽培植物野生近缘种利用技术进行了梳理, 探讨了栽培植物野生近缘种遗传资源可持续利用的新思路。最后, 我们以长江流域几种代表性栽培植物为例, 对主要作物类型的保护与利用情况进行了讨论。 相似文献
17.
荒漠生态系统中生物结皮广泛分布并蕴含丰富的土壤微生物,但不同生物结皮类型间真菌与细菌群落特征及其影响因素的对比研究相对不足,制约了对生物结皮生态功能的深入理解。以毛乌素沙地西南缘广泛分布的藻、地衣与苔藓结皮为研究对象,采集不同类型生物结皮土壤样品,通过高通量测序与土壤理化性质的测定,探究不同生物结皮间真菌与细菌群落特征差异及其影响因素。结果显示:(1)不同类型生物结皮间真菌与细菌的α多样性无显著差异,但β多样性差异显著;(2)不同生物结皮间真菌与细菌门水平上物种组成稳定,目水平上的部分物种存在显著差异;(3)网络分析显示,苔藓结皮的微生物网络最为复杂,真菌网络结构的复杂性远低于细菌网络结构;(4)不同类型生物结皮显著影响了真菌营养型丰度,但对细菌潜在功能特征无显著影响;(5)交换性钙离子与硝态氮是生物结皮中微生物群落结构的主要影响因子。综上所述,不同生物结皮间真菌与细菌群落特征呈现出显著差异,其群落结构受到多种环境因子的综合调控。研究结果有助于深入理解生物结皮的生态功能,为荒漠化防治与生态修复提供科学依据。 相似文献
18.
土壤微生物是反映土壤质量状况的重要指标,研究侵蚀地植被恢复后土壤微生物群落结构的变化对深入认识土壤质量的演变具有重要意义。对比分析了未治理地(Y0)、治理13年(Y13)和31年(Y31)的马尾松林(Pinus massoniana)林下芒萁(Dicranopteris dichotoma)覆盖地(NRd)、去除芒萁覆盖地(Rd)与林下裸地(CK)土壤微生物生物量和群落结构差异,结果表明:林下裸地土壤微生物生物量碳(MBC)、微生物生物量氮(MBN)和总微生物磷脂脂肪酸量(总PLFAs)的含量均显著低于芒萁覆盖地,且去除芒萁4个月后,MBC和总PLFAs均有降低趋势,表明芒萁覆盖对土壤微生物生物量具有重要影响;林下芒萁覆盖地土壤革兰氏阳性菌(GP)、革兰氏阴性菌(GN)、丛植菌根真菌(VAM)、真菌(Fungi)、放线菌(ACT)的PLFAs含量显著高于林下裸地(Y13例外),去除芒萁4个月后,各值均有有接近林下裸地的趋势;芒萁覆盖地真菌/细菌的比值(F/B)均显著高于林下裸地(P0.05),芒萁覆盖地革兰氏阳性菌/革兰氏阴性菌的比值(GP/GN)、饱和直链脂肪酸/单不饱和脂肪酸的比值(sat/mono)和(cy17:0+cy19:0ω8c)/(16:1ω7c+18:1ω7c)(cy/pre)显著小于林下裸地(P0.05),去除芒萁4个月后,芒萁覆盖地土壤cy/pre显著升高(P0.05)(Y13例外),意味着芒萁覆盖地土壤生态系统更稳定,土壤的养分可利用性更高,微生物生物量和群落结构更丰富,活性更强;皮尔逊相关分析和冗余分析发现,土壤理化性质与土壤微生物生物量和群落结构关系密切,土壤C/N、p H和氮素水平是调控芒萁覆盖下土壤微生物生物量和群落结构的主要生态因子。 相似文献
19.
川西亚高山不同林龄云杉人工林土壤微生物群落结构 总被引：4，自引：0，他引：4
以川西亚高山云杉人工林林地土壤为对象,采用磷脂脂肪酸(PLFA)法研究了4种不同林龄(50、38、27和20年)的人工林土壤微生物多样性和群落结构特征.结果表明: 随着林龄的增加,土壤有机碳和全氮含量逐步增加;土壤微生物Shannon多样性和Pielou均匀度指数则呈现先增后减的趋势.土壤微生物总PLFAs量、细菌PLFAs量、真菌PLFAs量、放线菌PLFAs量以及丛枝菌根真菌PLFAs量均表现为随林龄的增加而增加.主成分分析(PCA)表明,不同林龄人工林的土壤微生物群落结构之间存在显著差异,其中,第1主成分(PC1)和第2主成分(PC2)共同解释了土壤微生物群落结构总变异的66.8%.冗余分析(RDA)表明,对土壤微生物群落结构产生显著影响的环境因子分别为土壤有机碳、全氮、全钾以及细根生物量.随着人工造林时间的延长,土壤肥力和微生物生物量增加,森林生态系统的恢复进程稳定. 相似文献
20.
全球变暖对陆地生态系统造成一系列生态问题,使这些问题将随着全球平均气温的升高而进一步加剧。海拔梯度变化是研究气候变暖对陆地生态系统影响的一种重要手段。目前为止利用海拔梯度对微生物影响的研究尚未定论,其主要原因是忽略了植被类型的影响。因此,以中亚热带戴云山的3个海拔(1300、1450、1600 m)的黄山松(Pinus taiwanensis)林为研究对象,探究沿海拔梯度的变化,森林土壤微生物生物量和微生物群落结构的响应变化。结果表明:土壤碳氮磷养分(SOC、TN、TP)、微生物生物量氮(MBN)、微生物生物量磷(MBP)和丛枝菌根真菌(AMF)、革兰氏阴性菌(GN)、真菌(Fungi)、总磷脂脂肪酸(T_(PLFA)),细菌∶真菌(F∶B)均随海拔升高显著下降,而革兰氏阳性菌∶革兰氏阴性菌(GP∶GN)随海拔升高呈相反的趋势。冗余分析(RDA)表明,温度(T)和可溶性有机氮(DON)是影响微生物群落结构的最重要的环境因子。研究表明:与1600 m海拔相比,1300 m海拔温度较高,土壤有机质矿化作用较强,土壤速效养分及微生物生物量随之增加,从而提高(Fungi)、细菌(Bacteria)等。因此,未来气候变暖将通过改变土壤碳氮磷养分来影响本区域微生物群落组成结构。这对进一步深入了解气候变化对山地生态系统土壤养分循环过程具有重要意义。 相似文献