长白山天然次生林土壤微生物量对氮沉降的响应

土壤微生物作为土壤养分的生物驱动因素,氮沉降会改变其活性和生物量,从而打破土壤养分循环动态平衡。氮沉降对热带、亚热带森林以及温带原始林生态系统土壤微生物量影响的研究较多,但对温带天然次生林影响的研究鲜有报道。于2016年5月(春)、7月(夏)和9月(秋)分别对长白山模拟10年氮沉降的控制试验样地——白桦山杨次生林进行了野外调查。控制试验分为3个氮添加处理,对照(CK 0 kg N hm~(-2)a~(-1))、低氮(LN 25 kg N hm~(-2)a~(-1))和高氮(HN 50 kg N hm~(-2)a~(-1)),按照土壤层(0—10 cm和10—20 cm)分别测试了不同处理的土壤微生物量碳(MBC)和氮(MBN)、土壤全碳(TC)、全氮(TN)和全磷(TP)、p H、土壤可溶性有机碳(DOC)和氮(DON)等指标。结果表明:1)土壤p H在氮沉降的作用下显著降低;上层土壤TC、TN在氮沉降下变化较小,下层土壤TC、TN的含量显著增加;氮沉降下春、夏两季土壤TP含量上升,LN处理在秋季对TP有抑制作用;氮沉降对DOC、DON的影响不显著。2)上层土壤MBC春季到秋季呈现递减的趋势,下层土壤呈现先升后降的趋势,HN对MBC有抑制作用,LN对下层土壤MBC有促进作用;土壤MBN由春季到秋季呈现递减的趋势,且上、下层土壤MBN差异显著;氮处理对春、秋两季MBN有促进作用,夏季有抑制作用;氮沉降使春、秋两季MBC/MBN降低,夏季土壤MBC/MBN升高。3)氮处理、季节变化和土层深度对MBC、MBN存在显著影响,其交互影响也显著。总之,长期氮沉降在生长季对土壤微生物量的影响具有季节性差异,且受到土层深度的影响。未来研究在重视年际变化的同时,也要注重时空动态对氮沉降作用表现出的差异性。     

土壤食物网中的真菌/细菌比率及测定方法

土壤食物网对有机质的分解有两条途径, 即真菌途径和细菌途径。 在不同的土壤生态系统中, 由于提供能源的有机物其分解的难易程度不同, 这两条途径所起的作用也不同。以细菌分解途径为主导的土壤,有机质降解快,氮矿化率高, 有利于养分供应。以真菌途径为主的土壤,氮和能量转化比较缓慢,有利于有机质存贮和氮的固持。因此,土壤食物网的细菌∕真菌比率, 反映了整个土壤食物网的结构和功能对不同土壤条件的响应。细菌∕真菌比率的常规测定方法有显微镜计数法,选择性呼吸抑制法,麦角固醇法,氨基葡萄糖/胞壁酸法等。磷酸脂肪酸分析法（PLFA）是一种测定微生物群落结构的新方法,所测定的真菌和细菌脂肪酸分子团相对量（摩尔浓度）是一个有用的指标, 但由于真菌与细菌的细胞个体存在很大差异, 要把它换算成真菌与细菌生物量碳的绝对比例, 还存在一定困难。对土壤条件和整个食物网结构的了解有助于确定有关转换参数。     

Quantitative distribution of microbial biomass in the soil profile of a high-mountain grassy ecosystem

The soil microbiota of a grassy ecosystem in the subalpine belt of the Rile Mountain National Park showed greater amounts of fungal biomass. This remained relatively constant throughout the months of sampling while bacterial biomass was a dynamic value fluctuating within a wide range. The two groups of microorganisms also differed in their in-depth distribution in the soil profile: the bacterial biomass was relatively homogeneously distributed while the fungal biomass gradually decreased with depth. Good correlation between the amount of biomass and the values of some abiotic factors of the environment was shown by correlation analysis in a “warm” period of investigation; no distinct correlation between microbial biomass and environmental factors was observed in a “cold” period.     

Variation of soil and biomass carbon pools in beech forests across a precipitation gradient

Temperate forests have recently been identified as being continuing sinks for carbon even in their mature and senescent stages. However, modeling exercises indicate that a warmer and drier climate as predicted for parts of Central Europe may substantially alter the source/sink function of these economically important ecosystems. In a transect study with 14 mature European beech (Fagus sylvatica L.) forests growing on uniform geological substrate, we analyzed the influence of a large reduction of annual precipitation (970–520 mm yr^?1) on the carbon stocks in fast and slow pools, independent of the well‐known aging effect. We investigated the C storage in the organic L, F, H layers, the mineral soil to 100 cm, and in the biomass (stem, leaves, fine roots), and analyzed the dependence of these pools on precipitation. Soil organic carbon decreased by about 25% from stands with > 900 mm yr^?1 to those with < 600 mm yr^?1; while the carbon storage in beech stems slightly increased. Reduced precipitation affected the biomass C pool in particular in the fine root fraction but much less in the leaf biomass and stem fractions. Fine root turnover increased with a precipitation reduction, even though stand fine root biomass and SOC in the organic L, F, and H layers decreased. According to regression analyses, the C storage in the organic layers was mainly controlled by the size of the fine root C pool suggesting an important role of fine root turnover for the C transfer from tree biomass to the SOC pool. We conclude that the long‐term consequence of a substantial precipitation decrease would be a reduction of the mineral soil and organic layer SOC pools, mainly due to higher decomposition rates. This could turn temperate beech forests into significant carbon sources instead of sinks under global warming.     

Application of the chloroform fumigation-incubation method to the estimation of soil microbial biomass in burned and unburned Japanese red pine forests

Abstract Estimation of soil microbial biomass in burned and unburned Japanese red pine forests was attempted using the chloroform fumigation-incubation method. As the amount of CO₂-C evolved from the fumigated soil for 10–20 days after fumigation (designated as F') was always lower than that from the unfumigated soil during the same period (UF'), the formula, microbial biomass-C(M) = the amount of CO₂-C evolved from the fumigated soil for 0–10 days after fumigation, F) − F'/ k _c, was proposed instead of Jenkinson's conventional formula, M = (F − UF')/ k _c. The k _c value was also determined as 0.30 using 3 fungal and 3 bacterial cultured species as internal standards. Microbial biomass-C calculated by (F − F')/0.30 decreased with soil depth at both the burned (Nenoura, 3.5 years after fire) and unburned (Ato) sites, showing the significant correlation with the decrease of soil respiration and organic C content along soil depth. Microbial biomass-C in the 0–2 cm soil layer at the burned site at Nenoura was 130 mg/100 g dry soil and those in the HF horizon and 0–2 cm soil layer at the unburned site at Ato were 686 and 146 mg/100 g dry soil, respectively.     

Root biomass allocation in the world's upland forests

Because the world's forests play a major role in regulating nutrient and carbon cycles, there is much interest in estimating their biomass. Estimates of aboveground biomass based on well-established methods are relatively abundant; estimates of root biomass based on standard methods are much less common. The goal of this work was to determine if a reliable method to estimate root biomass density for forests could be developed based on existing data from the literature. The forestry literature containing root biomass measurements was reviewed and summarized and relationships between both root biomass density (Mg ha⁻¹) and root:shoot ratios (R/S) as dependent variables and various edaphic and climatic independent variables, singly and in combination, were statistically tested. None of the tested independent variables of aboveground biomass density, latitude, temperature, precipitation, temperature:precipitation ratios, tree type, soil texture, and age had important explanatory value for R/S. However, linear regression analysis showed that aboveground biomass density, age, and latitudinal category were the most important predictors of root biomass density, and together explained 84% of the variation. A comparison of root biomass density estimates based on our equations with those based on use of generalized R/S ratios for forests in the United States indicated that our method tended to produce estimates that were about 20% higher. Received: 3 July 1996 / Accepted: 23 January 1997     

Ungulate biomass in relation to feeding strategy within Amazonian forests

Summary The relationship between diet and biomass was examined in the Amazonian ungulates (red brocket deer, grey brocket deer, collared peccary, white-lipped peccary, and lowland tapir) of Northeastern Peru. Tropical forest ungulates have lower biomasses than savanna or grassland ungulates, because in tropical forests the majority of primary production occurs in the canopy, well out of reach from terrestrial herbivores. Within the Amazonian ungulates, species that supplement their diet with animal material, namely the peccaries, obtain a greater crude and metabolic biomass, and higher reproductive rates than the purely herbivorous species. Omnivory appears to help terrestrial herbivores inhabiting closed canopy forests overcome some effects of food limitation.     

Diverse responses of pqqC- and phoD-harbouring bacterial communities to variation in soil properties of Moso bamboo forests

Phosphate-mobilizing bacteria (PMB) play a critical role in the regulation of phosphorus availability in the soil. The microbial genes pqqC and phoD encode pyrroloquinoline quinone synthase and bacterial alkaline phosphatase, respectively, which regulate inorganic and organic phosphorus mobilization, and are therefore used as PMB markers. We examined the effects of soil properties in three Moso bamboo forest sites on the PMB communities that were profiled using high-throughput sequencing. We observed differentiated responses of pqqC- and phoD-harbouring PMB communities to various soil conditions. There was significant variation among the sites in the diversity and structure of the phoD-harbouring community, which correlated with variation in phosphorus levels and non-capillary porosity; soil organic carbon and soil water content also affected the structure of the phoD-harbouring community. However, no significant difference in the diversity of pqqC-harbouring community was observed among different sites, while the structure of the pqqC-harbouring bacteria community was affected by soil organic carbon and soil total nitrogen, but not soil phosphorus levels. Overall, changes in soil conditions affected the phoD-harbouring community more than the pqqC-harbouring community. These findings provide a new insight to explore the effects of soil conditions on microbial communities that solubilize inorganic phosphate and mineralize organic phosphate.     

春季解冻期不同纬度兴安落叶松林的土壤微生物生物量

以移栽自兴安落叶松林自然分布区内4个纬度梯度(塔河、松岭、孙吴和带岭)的8年生兴安落叶松林为对象,于移栽3年后(2007年)的春季土壤解冻期,采用氯仿熏蒸浸提法测定了4个纬度梯度(处理)土壤的微生物生物量碳(C_mic)和微生物生物量氮(N_mic)的时间动态.结果表明：在相似基质和相同气候条件下,移栽自4个纬度梯度的兴安落叶松林春季土壤解冻期的C_mic和N_mic平均值差异显著,呈随纬度升高而减少、随土层加深而下降的分布格局.其中塔河、松岭、孙吴和带岭的C_mic平均为554.63、826.41、874.81和1246.18 mg·kg^-1,而N_mic分别为70.63、96.78、79.76 和119.66mg·kg^-1.C_mic和N_mic在解冻前达到最大值;解冻初期迅速下降;在冻融交替阶段变化不显著,且维持在较低水平;在解冻末期,来自低纬度的带岭和孙吴的C_mic回升较快. 春季冻融期土壤温度和含水量对C_mic和N_mic的影响显著,其影响程度随冻融阶段而变化.土壤微生物生物量与解冻前的土壤温度呈负相关,与整个解冻期间的土壤含水量呈指数关系.     

The annual invasive plant Impatiens glandulifera reduces hyphal biomass of soil fungi in deciduous forests

Soil fungi play a crucial role in ecosystem functioning and there is increasing evidence that exotic plants invading forests can affect soil fungal communities. We examined potential effects of the invasive plant Impatiens glandulifera on hyphal biomass of ectomycorrhizal fungi, their genetic diversity and the diversity of other soil fungi in deciduous forests in Switzerland. We compared invaded patches with patches where I. glandulifera had been removed, by establishing pairs of 3-m long transect lines at the edge of seven areas of either type. Along the transects we assessed the length of ectomycorrhizal fungal hyphae using the ‘ingrowth mesh bag method’, and used terminal restriction fragment length polymorphism (T-RFLP) analysis to examine fungal genetic diversity. The invasive plant reduced fungal hyphal biomass by 30–80%: the reduction was largest in the centre of the patch. I. glandulifera did not alter fungal richness, but affected the composition of fungal communities. This is probably the result of a decrease of mycorrhizal fungi, coupled with an increase of saprotrophic fungi. Our findings demonstrate the adverse impacts of an annual invasive plant species on both fungal hyphal biomass and the composition of soil fungal communities. This may negatively affect forest nutrient and carbon cycling, soil stability and the functionality of the fungal community, with major consequences for forest ecosystem functioning.     

川西亚高山森林土壤呼吸和微生物生物量碳氮对施氮的响应

随着全球大气氮沉降的明显增加,将有可能显著影响我国西部地区受氮限制的亚高山森林生态系统。土壤微生物是生态系统的重要组成部分,是土壤物质循环和能量流动的重要参与者。由于生态系统类型、土壤养分、氮沉降背景值等的差异,土壤呼吸和土壤生物量碳氮对施氮的响应存在许多不确定性。而施氮会不会促进亚高山森林生态系统中土壤呼吸和微生物对土壤碳氮的固定?基于此假设,选择了川西60年生的四川红杉(Larix mastersiana)亚高山针叶林为研究对象,通过4个水平的土壤施氮控制试验(CK:0 g m~(-2) a~(-1)、N1:2 g m~(-2)a~(-1)、N2:5 g m~(-2) a~(-1)、N3:10 g m~(-2)a~(-1)),监测了土壤呼吸及土壤微生物生物量碳氮在一个生长季的动态情况。结果表明:施氮对土壤呼吸各指标和土壤微生物碳氮都有极显著的影响,施氮能促进土壤全呼吸、自养呼吸、异养呼吸通量和土壤微生物生物量碳氮的增长,施氮使土壤呼吸通量提高了11%—15%,土壤微生物量碳提高了5%—9%,土壤微生物量氮提高了23%—34%。在中氮水平下(5 g m~(-2) a~(-1))对土壤呼吸的促进最显著。相关分析发现,土壤呼吸与微生物生物量碳氮和微生物代谢商极呈显著正相关,微生物量碳氮与土壤温度呈极显著的正相关,与土壤湿度呈极显著负相关。通过一般线性回归拟合土壤呼吸速率与土壤10 cm温湿度的关系,发现土壤呼吸速率与土壤温度呈极显著的正相关,与土壤湿度极显著负相关(P0.001),中氮水平下土壤温度敏感性系数Q_(10)值(7.10)明显高于对照(4.26)。     

Fungal and bacterial biomass in tundra soils along an arctic transect from Taimyr Peninsula, central Siberia

Microscopic analyses of tundra soils from northern central Siberia, Taimyr Peninsula (74.5°N, 98.5°E) were performed in order to investigate spatial variation of fungal and bacterial biomass. Biomass figures of fungi and bacteria (µg C g^-1 dry wt.) were measured from 11 permafrost soil pits. Fungal biovolume of up to 3.5 mm³ g^-1 dry wt. (median 0.19 mm³ g^-1 dry wt.) and a maximum hyphal length of 393 m g^-1 dry wt. (median 21 m g^-1 dry wt.) were determined. Fungal biomass was found up to 455 µg C g^-1 dry wt. (median 24 µg C g^-1 dry wt.). The amounts generally decreased with depth but increased within organic horizons. Little fungal biomass was found in the unvegetated soils or deep horizons above the permafrost table. Bacterial counts ranged from 0.16 to 7.38*10⁹ g^-1 dry wt. and bacterial biomass ranged from 0.68 to 20.38 µg C g^-1 dry wt. (median 6.19 µg C g^-1 dry wt.) because of small cell volume (median 0.04 µm³). Microbial biomass was generally dominated by fungi as shown by the ratio of fungal to bacterial biomass, which was between 0 and 174.1 (median 4.5). Plant cover and soil organic matter content were found to be the important keys in understanding microbial ecology in arctic tundra soils.     

退耕还湿后土壤细菌群落结构和生物量变化过程

土壤细菌对湿地生态系统功能和健康维持起着重要作用。以菜子湖原始湿地、不同退耕年限湿地(3a、7a、11a和21a)和仍耕作油菜地土壤为研究对象,应用聚合酶链式反应-变性梯度凝胶电泳(PCR-DGGE)、高通量测序和磷脂脂肪酸(PLFAs)方法分析土壤细菌群落组成和生物量,探讨它们在退耕还湿后的变化过程及其影响因素。结果表明,退耕还湿后土壤变形菌门(α-变形菌纲、β-变形菌纲和δ-变形菌纲)、酸杆菌门(酸杆菌纲和全噬菌纲)、Nitrospinae(Nitrospinia纲)和硝化螺旋菌门(硝化螺旋菌纲)相对丰度先增高后降低;这些参与氮循环的土壤细菌对退耕后湿地生态恢复过程中土壤氮素提升起着重要作用。与农业生产活动密切关联的厚壁菌门(芽孢杆菌纲和梭菌纲)和放线菌门(放线菌纲)相对丰度逐渐降低。湿地土壤细菌多样性在退耕初期(3—7a)上升达到最大,退耕中后期逐渐降低。表层土壤各类群细菌生物量逐渐升高,亚表层土壤各类群细菌生物量则先降后升再降。水分条件和容重是与研究区土壤细菌群落结构和多样性密切相关的土壤因子,而全氮是与土壤细菌生物量密切相关的土壤因子。研究从生态过程视角解析了土壤细菌群落较详...     

Responses of soil microbial biomass and enzymatic activities to different forms of organic nitrogen deposition in the subtropical forests in East China

Numerous studies reported that inorganic nitrogen (N) deposition strongly affected forest ecosystems. However, organic N is also an important component of atmospheric N deposition. The influence of organic N deposition on soil microbial biomass and extracellular enzymatic activities (EEA) in subtropical forests remains unclear. Coniferous forest (CF) and broad-leaved forest (BF) were chosen from the Zijin Mountain in China. Five forms of organic N (urea, glycine, serine, nonylamine, and a mixture of all four) were used to fertilize the soils in CF and BF every month for 1 year. Soil samples were collected every 2 months. Subsequently, soil microbial biomass and EEA were assayed. Results showed that the microbial biomass and EEA of soils fertilized with urea and amino acids increased significantly, whereas those fertilized with nonylamine and mixed N decreased significantly. Urea and amino acid fertilizations had a more positive influence on EEA of BF than on those of CF. Nonylamine fertilization had a more negative influence on EEA of CF than on those of BF. Organic N fertilization shifted soil microbial biomass away from the excretion of N-degrading enzymes and toward the excretion of C-degrading enzymes. These results suggest that organic N type is an important factor that affects soil microbial biomass, EEA, and their relationship. Organic N deposition may seriously affect soil C and N cycling, as well as carbon dioxide releasing from the soils by influencing microbial activities and biomass. This study thereby provides evidence that soil microorganisms have strong feedback to different forms of organic N deposition.     

Divergent biomass partitioning to aboveground and belowground across forests in China

Aims Belowground to aboveground biomass (BGB/AGB) ratio is a highly valued parameter of the terrestrial carbon cycle and productivity. However, it remains far from clear whether plant biomass partitioning to aboveground and belowground is isometric (equal partitioning) or allometric (unequal partitioning) at community levels and what factors are necessary in order to regulate the partitioning. This study aimed to comprehensively find out the patterns of biomass partitioning and their regulatory factors across forests in China.Methods The data of AGB and BGB were compiled from 1542 samples for communities across forests in China. Standardized major axis regression was conducted to examine whether AGB and BGB were allocated isometrically or allometrically at a community level. Redundancy analysis was used to analyze the relationships of BGB/AGB ratio with climatic factors and soil properties.Important findings We found that the slopes of the relationship between logAGB and logBGB were not always comparable to 1.0 (isometric allocation) at community levels, including primary forest, secondary forest, and planted forest. Meanwhile, samples in clay, loam, and sand soil types also presented the same phenomenon. Furthermore, the radically different allocations of AGB and BGB were found in northern and southern China. Environmental factors totally explained 3.86% of the variations in the BGB/AGB ratio at the community level, which include the mean annual precipitation, mean annual temperature, potential water deficit index, soil carbon content, soil nitrogen content, soil clay, soil loam, soil sand, soil pH, and soil bulk density. In addition, the environmental factors also have effects on the BGB/AGB ratio in other categories. The patterns revealed in this study are helpful for better understanding biomass partitioning and spreading the carbon circle models.     

南亚热带森林土壤微生物量碳对氮沉降的响应

研究了鼎湖山自然保护区3种森林生态系统土壤微生物量碳对氮沉降增加的响应.选取南亚热带代表性森林类型马尾松林、混交林和季风常绿阔叶林(季风林)建立野外模拟氮沉降试验样地.2003年7月开始每月进行氮处理.这些处理分别为对照、低氮处理、中氮处理和高氮处理,即0、50、100 kg N hm-2 a-1 和150 kg N hm-2 a-1.在2004年11月和2006年6月用氯仿熏蒸浸提法分别测定土壤微生物量碳和土壤可浸提有机碳.土壤微生物量碳和可浸提有机碳含量均表现为2006年6月高于2004年11月;季风林高于马尾松林和混交林.随着氮沉降增加季风林土壤微生物量碳减少,但可浸提有机碳含量则增加,且此趋势在高氮处理下表现明显.然而,氮沉降增加对马尾松林和混交林土壤微生物量碳和可浸提有机碳含量的影响不显著.以上结果表明,氮沉降增加可能提高季风林土壤有机碳的固持能力.     

云南松林的根系生物量及其分布规律的研究

利用平均标准木机械布点法测定了云南省永仁林业局云南松不同龄组林分的根系生物量及其沿土壤剖面深度的分布规律.结果表明,林分根系总生物量随林龄而增加,幼龄林(15～17年)的根系生物量为8.50 t·hm^-2,中龄林(30～32年)为11.70 t·hm^-2,成熟林为(>62年) 18.91 t·hm^-2.在不同龄组林分中,粗根(>10mm)生物量差异最大（1.5～12.3 t·hm^-2）,而中根（5～10 mm）（1.4～1.6 t·hm^-2）及小根（<5 mm）（5.3～6.2 t·hm^-2）的生物量差异最小.根系生物量沿土壤深度迅速减少,约93%的根系生物量集中分布在0～30 cm土层中,深土层(30～115 cm)的根系生物量仅占7%左右.