植物代谢速率与个体生物量关系研究进展

植物的各项生理生态功能（例如,呼吸、生长和繁殖）都与个体生物量成异速生长关系。West, Brown及Enquist基于分形网络结构理论所提出的WBE模型认为：植物的代谢（呼吸）速率正比于个体生物量的3/4次幂。然而,恒定的“3/4异速生长指数”与实测数据、植物生理生态学等研究之间存在矛盾,引发激烈的争论。论文分析了不同回归方法对代谢指数的影响,重点对植物代谢速率与个体生物量异速生长关系研究进展进行了综述,分析并得出了植物代谢指数在小个体时接近1.0,并随着生物量的增加而系统减小,且其密切依赖于氮含量的调控的结论。据此,提出了进一步深入研究植物代谢速率个体生物量关系需要解决的一些科学问题。     

Divergent scaling of respiration rates to nitrogen and phosphorus across four woody seedlings between different growing seasons

Empirical studies indicate that the exponents governing the scaling of plant respiration rates (R) with respect to biomass (M) numerically vary between three‐fourth for adult plants and 1.0 for seedlings and saplings and are affected by nitrogen (N) and phosphorus (P) content. However, whether the scaling of R with respect to M (or N and P) varies among different phylogenetic groups (e.g., gymnosperms vs. angiosperms) or during the growing and dormant seasons remains unclear. We measured the whole‐plant R and M, and N and P content of the seedlings of four woody species during the growing season (early October) and the dormant season (January). The data show that (i) the scaling exponents of R versus M, R versus N, and R versus P differed significantly among the four species, but (ii), not between the growing and dormant seasons for each of the four species, although (iii) the normalization constants governing the scaling relationships were numerically greater for the growing season compared to the dormant season. In addition, (iv) the scaling exponents of R versus M, R versus N, and R versus P were numerically larger for the two angiosperm species compared to those of the two gymnosperm species, (v) the interspecific scaling exponents for the four species were greater during the growing season than in the dormant season, and (vi), interspecifically, P scaled nearly isometric with N content. Those findings indicate that the metabolic scaling relationships among R, M, N, and P manifest seasonal variation and differ between angiosperm and gymnosperm species, that is, there is no single, canonical scaling exponent for the seedlings of woody species.     

Diel changes in copepod respiration rates

Measurements of respiration in adult copepods at optimum concentrations in a respirometer were made at different hours of day; the amperometric method was used to measure dissolved oxygen. The migratory species from the tropical Indian Ocean and from the Black Sea displayed distinct daily variations in respiration rate and considerable difference between averages recorded in day and night hours. Such vertical migrants as Pleuromamma xiphias (Giesbr.) and Calanus euxinus Hulsemann were found to increase respiration rate late in the evening and early in the morning. No statistically reliable daily differences in the estimates of respiration were observed in copepod species like Acatria clausi (Giesbr.) and Temora discaudata (Giesbr.) which do not make long-distance migrations. In these experimental conditions the respiration rate appeared to represent changes in locomotory activity resulting from the sustained natural migratory rhythm and movements in food search. Using data available from the literature, the feeding rhythm and intensity were compared with respiration rate. This suggested that trophic status of the water may indirectly, through locomotory activity, affect the respiration rate. Increased respiration rate was suggested in the Black Sea copepod species in comparison with data obtained in earlier decades. The possibility of changes in respiration caused by changed food conditions of the environment is discussed.     

稻麦作物呼吸作用与植株氮含量、生物量和温度的定量关系

陆地生态系统碳循环是全球变化研究的重要议题之一,准确估算植被的呼吸作用对于客观评价植被在陆地生态系统碳循环中的作用具有重要意义。为探讨作物生长、植株氮含量和环境温度对呼吸作用的综合影响,研究以盆栽为主并与大田试验相结合,基于逐步收割法和静态暗箱-气相色谱技术,于2 0 0 2年和2 0 0 3年冬小麦和水稻生长季原位测定了作物地上部分CO2 排放速率,并同时测定了作物生物量、氮含量和环境温度。试验处理分为常规管理、不同氮肥水平、不同播种期和不同种植密度。研究结果表明:稻麦作物暗呼吸系数(Rd)不是常数,而是正比于植株氮(N )含量,两者的关系可用方程Rd=4 .74 N - 1.4 5 (R2 =0 .85 ,n=12 2 ,p<0 .0 0 1)来定量表述。用方程RD=(4.74 N - 1.4 5 )×Q( T- 2 5) /1 01 0 ×W模拟的作物暗呼吸量(RD)与大田测定结果一致。用国际上著名的作物模拟模型估算的稻麦作物维持性呼吸与用此方程模拟的结果具有可比性,而采用陆地生态系统模型(TEN)估算的结果则远高于本项研究,TEM用于估算农业植被的呼吸作用可能是不适合的。     

秸秆预处理对土壤微生物量及呼吸活性的影响

冬小麦秸秆经8．0g·L^-1H2O2(pH11．0)溶液、12．5g·L^-1 NaOH溶液或H2SO4溶液浸泡8h并80℃烘干后,与无机N一起加入土壤,进行室内25℃恒温培养试验,在不同时间测定土壤微生物量C、N和CO2释放速率。结果表明,培养前期,秸秆预处理使土壤微生物量C数量增加了1．0～1．4倍,但降低了土壤微生物的呼吸活性;培养后期,NaOH和H2SO4处理使土壤微生物量C分别下降了28％和42％,但增加了土壤微生物的呼吸活性;H2O2处理则使土壤微生物量N增加90％;土壤微生物区系中的真菌比例在不同时刻有所增加,表明将秸秆预处理后施入土壤,将对土壤中微生物数量和呼吸活性产生一定影响。     

Oxygen respiration rates of benthic foraminifera as measured with oxygen microsensors

Oxygen respiration rates of benthic foraminifera are still badly known, mainly because they are difficult to measure. Oxygen respiration rates of seventeen species of benthic foraminifera were measured using microelectrodes and calculated on the basis of the oxygen fluxes measured in the vicinity of the foraminiferal specimens. The results show a wide range of oxygen respiration rates for the different species (from 0.09 to 5.27 nl cell⁻¹ h⁻¹) and a clear correlation with foraminiferal biovolume showed by the power law relationship: R = 3.98 10⁻³ BioVol^0.88 where the oxygen respiration rate (R) is expressed in nl O₂ h⁻¹ and in μm³ biovolume (BioVol) (n = 44, R² = 0.72, F = 114, p < 0.0001). The results expressed per biovolume unit (1.82 to 15.7 nl O₂ 10⁻⁸ μm⁻³ h⁻¹) allow us to compare our data with the previous published data showing similar ranges. A comparison with available data for other microbenthos groups (nematodes, copepods, ostracods, ciliates and flagellates) suggests that benthic foraminifera have a lower oxygen respiration rates per unit biovolume. The total contribution of benthic foraminifera to the aerobic mineralisation of organic matter is estimated for the studied areas. The results suggest that benthic foraminifera play only a minor role (0.5 to 2.5%) in continental shelf environments, which strongly contrasts with their strong contribution to anaerobic organic matter mineralisation, by denitrification, in the same areas.     

植物群落密度调控研究进展

植物群落密度调控是生态学领域的研究热点。从Yoda提出-3/2自疏法则以来,围绕植物群落密度调控规律从自疏线可变性、环境因素对密度调控影响的规律等进行了大量研究。尤其是基于代谢生态学理论建立的WBE自疏规律提出后,密度调控规律的争论和研究更为活跃,其焦点主要是自疏线斜率是否存在相对恒定的α值和值的大小。根据国内外文献,综述了-3/2自疏法则、-4/3自疏法则、质量-密度的等速比例关系和环境对密度调控规律的影响等方面的研究,指出密度调控的机制以及胁迫条件下的密度调控及其应用是未来研究的趋势。     

A relationship between plant responses to cytokinins and cyanide-resistant respiration

Cytokinin bioassay material from six sources ( Amaranthus caudatus L.; Avena sativa L.; Cucumis sativus L.; Funaria hygrometrica Hedw.; Pisum sativum L., cv. Alaska and cv. Progress No. 9; Xanthium pensylvanicum Wallr.) was analyzed for cyanide-resistant oxygen consumption (alternative respiration) during the course of a response to benzyladenine (40 μ M ). In five of the six bioassay systems, the alternative pathway was found to be present but disengaged (ϱ=0) in the cytokinin-treated material while untreated controls continued to fully utilize the pathway (ϱ=1). The moss, Funaria hygrometrica , was the exception to this pattern, with the alternative pathway fully engaged in both treated and untreated protonemata throughout the period of cytokinin-induced bud formation. Respiration via the alternative pathway was not inhibited by benzyladenine in this latter tissue, although titrations with benzyladenine in carrot ( Daucus carota L.) cell suspensions mimicked those obtained using salicylhydroxamic acid, an inhibitor of the alternative pathway. The dwarf pea, Progress No. 9, showed no response to cytokinin application in terms of increased ethylene production, and was also found to lack any capacity for the alternative pathway. Taken together, these results point to a role for the alternative pathway in responses of at least some plant tissues to cytokinins.     

Above- and below-ground biomass relationships across 1534 forested communities

BACKGROUND AND AIMS: Prior work has shown that above- and below-ground dry biomass across individual plants scale in a near isometric manner across phyletically and ecologically diverse species. Allometric theory predicts that a similar isometric scaling relationship should hold true across diverse forest-types, regardless of vegetational composition. METHODS: To test this hypothesis, two compendia for forest-level above- and below-ground dry biomass per hectare (M(A) and M(R), respectively) were examined to test the hypothesis that M(A) vs. M(R) scales isometrically and in the same manner as reported for data from individual plants. Model Type II regression protocols were used to compare the numerical values of M(A) vs. M(R) scaling exponents (i.e. slopes of log-log linear relationships) for the combined data sets (n =1534), each of the two data sets, and data sorted into a total of 17 data subsets for community- and biome-types as well as communities dominated by angiosperms or conifers. KEY RESULTS: Among the 20 regressions examined, 15 had scaling exponents that were indistinguishable from that reported for M(A) vs. M(R) across individual plants. The isometric hypothesis could not be strictly rejected on statistical grounds; four of these 15 exponents had broad 95% confidence intervals resulting from small sample sizes. Significant variation was observed in the y-intercepts of the 20 regression curves, because of absolute differences in M(A) or M(R). CONCLUSIONS: The allometries of forest- and individual plant-level M(A) vs. M(R) relationships share strikingly similar scaling exponents, but differ because of considerable variation in y-intercepts. These results support prior allometric theory and provide boundary conditions for the scaling of M(A) and M(R).     

Comparative assessment of soil microbial biomass determined by the methods of direct microscopy and substrate-induced respiration

The content of microbial biomass (MB) was determined in samples of gray forest, chestnut, and tundra soils with different physicochemical properties (0.4–22.7% C_org; 8.4–26.8% silt particles; pH 4.3–8.4) by the methods of substrate-induced respiration (MB_SIR) and direct microscopy (MB_M). The samples of two upper soil layers, 0–5 and 5–10 cm (without plant litter), from different ecosystems (forest, forest shelter belt, meadow, fallow, and arable) and elements of relief of interfluvial tundra (block/upper land plateau, depression between blocks) have been analyzed. The content of microbial biomass in the 0–5-cm soil layer was 216–8134 and 348–7513 μg C/g soil as measured by the methods of substrate-induced respiration and direct microscopy, respectively. The MB_SIR and MB_M values closely correlated with each other: r = 0.90 and 0.74 for 0–5 and 5–10 cm, respectively. The average MB_SIR/MB_M ratio was 90 and 60% for 0–5 and 5–10 cm, respectively. The portion of microbial carbon in total organic soil carbon was, on average, 4 and 3% (SIR) and 5 and 7% (direct microscopy) for 0–5 and 5–10 cm, respectively. Possible reasons for the differences between MB_SIR and MB_M values in the soils under study are discussed.     

Scaling up calcification,respiration, and photosynthesis rates of six prominent coral taxa

Coral reefs provide a range of important services to humanity, which are underpinned by community‐level ecological processes such as coral calcification. Estimating these processes relies on our knowledge of individual physiological rates and species‐specific abundances in the field. For colonial animals such as reef‐building corals, abundance is frequently expressed as the relative surface cover of coral colonies, a metric that does not account for demographic parameters such as coral size. This may be problematic because many physiological rates are directly related to organism size, and failure to account for linear scaling patterns may skew estimates of ecosystem functioning. In the present study, we characterize the scaling of three physiological rates — calcification, respiration, and photosynthesis — considering the colony size for six prominent, reef‐building coral taxa in Mo''orea, French Polynesia. After a seven‐day acclimation period in the laboratory, we quantified coral physiological rates for three hours during daylight (i.e., calcification and gross photosynthesis) and one hour during night light conditions (i.e., dark respiration). Our results indicate that area‐specific calcification rates are higher for smaller colonies across all taxa. However, photosynthesis and respiration rates remain constant over the colony‐size gradient. Furthermore, we revealed a correlation between the demographic dynamics of coral genera and the ratio between net primary production and calcification rates. Therefore, intraspecific scaling of reef‐building coral physiology not only improves our understanding of community‐level coral reef functioning but it may also explain species‐specific responses to disturbances.     

林木分化对兴安落叶松异速生长方程和生物量分配的影响

林木因对资源竞争而产生分化,从而影响林木的异速生长方程和生物量分配,但其影响程度还不清楚。采用林木相对直径法将38株兴安落叶松(Larix gmelinii)样木在林分中的分化等级分为优势木、中等木和被压木,量化林木分化对林木异速生长方程和生物量分配的影响。结果显示:生物量组分异速生长方程多以胸径(DBH)为自变量为好,但以枝下高处的树干直径为自变量估测其枝、叶生物量时更精确。在一定的胸径范围内,同一胸径下不同林木分化等级的地下部分各组分生物量没有显著差异(P0.05),但优势木分配更多的生物量给枝和叶,中等木比优势木分配更多的生物量给树干,中等木比被压木分配更多的生物量给地上部分,而且被压木和中等木的树高显著高于优势木。除根茎生物量之外,不同林木分化等级的生物量组分(包括枝、叶、树干和根系)的相对分配比例无显著差异(P0.05),根冠比保持相对稳定。这些结果表明,主要由竞争而引起的林木分化改变了兴安落叶松地上生物量组分的异速生长和分配,但其相对分配格局较为保守。     

26年长期施肥对土壤微生物量碳、氮及土壤呼吸的影响

研究长期小麦连作施肥条件下土壤微生物量碳、氮,土壤呼吸的变化及其与土壤养分的相关性。以陕西长武长期定位试验为平台,应用氯仿熏蒸-K2SO4提取法、碱液吸收法和化学分析法分析了长达26a不同施肥处理农田土壤微生物量碳、微生物量氮和土壤呼吸之间的差异及其调控土壤肥力的作用。长期施肥及种植作物,均能提高土壤微生物量碳、氮含量,尤其是施用有机肥,土壤微生物量碳、氮含量高于单施无机肥的处理,土壤呼吸量也提高15.91%—75.73%,而施用无机肥对于土壤呼吸无促进作用。土壤微生物生物量碳氮、土壤呼吸与土壤有机质、全氮呈极显著相关。长期有机无机肥配施可以提高土壤微生物量碳氮、土壤呼吸,氮磷肥与厩肥配施对提高土壤肥力效果最好。微生物量碳氮及土壤呼吸可以反映土壤质量的变化,作为评价土壤肥力的生物学指标。     

Testing metabolic ecology theory for allometric scaling of tree size, growth and mortality in tropical forests

The theory of metabolic ecology predicts specific relationships among tree stem diameter, biomass, height, growth and mortality. As demographic rates are important to estimates of carbon fluxes in forests, this theory might offer important insights into the global carbon budget, and deserves careful assessment. We assembled data from 10 old-growth tropical forests encompassing censuses of 367 ha and > 1.7 million trees to test the theory's predictions. We also developed a set of alternative predictions that retained some assumptions of metabolic ecology while also considering how availability of a key limiting resource, light, changes with tree size. Our results show that there are no universal scaling relationships of growth or mortality with size among trees in tropical forests. Observed patterns were consistent with our alternative model in the one site where we had the data necessary to evaluate it, and were inconsistent with the predictions of metabolic ecology in all forests.     

Soil microbial biomass and respiration measurements: An automated technique based on infra-red gas analysis

An automated system for continuous soil respiration and microbial biomass measurements based on Infra Red Gas Analysis was constructed. The switching device is computer controlled and allows hourly measurements of up to 24 samples when switching intervals of 2.5 min are selected. This allows the use of the substrate-induced respiration method for biomass determination. A software package to run the system was developed.     

Microscale fumigation-extraction and substrate-induced respiration methods for measuring microbial biomass in barley rhizosphere

Changes in microbial biomass in the rhizosphere of young barley seedlings was studied. A fumigation-extraction (FE) method with measurement of ninhydrin-reactive nitrogen (NR-N) and a substrate-induced respiration (SIR) method were applied on a microscale to rhizosphere soil samples of approximately 0.1 g. Rhizosphere soil was defined as the soil adhering to the roots when they were carefully separated from the bulk soil. The rhizosphere soil was gently washed off the roots with either distilled water (FE) or with glucose solution (SIR). Shaking and mild sonication was used to disperse the soil without disrupting the roots. Fumigation was carried out by direct addition of liquid chloroform to the isolated soil. These techniques were proven to give reliable results under the experimental conditions of this investigation. Rhizosphere soil was isolated from segments of the roots representing different distances to the seed different root ages. In the rhizosphere of young barley seedlings, biomass NR-N increased significantly compared to the bulk soil from day 6 after sowing (average increases of 33–97%), especially where adventitious roots had developed. From this time, SIR rates were also significantly higher in the rhizosphere than in bulk soil (average increases 72–170%). The average ratio of SIR rate to biomass NR-N was found to be approximately 50% higher in the rhizosphere than in the bulk soil, which may indicate that a larger fraction of the microbial community is potentially active in the rhizosphere as compared to the bulk soil.     

Algal respiration and the regulation of phytoplankton biomass in a polymictic tropical lake (Lake Xolotlán,Nicaragua)

Community respiration in tropical Lake Xolotlán, Nicaragua, was assessed seasonally and during diurnal cycles, via oxygen consumption in bottle enclosures. Results were analysed in relation to phytoplankton biomass, mixing depth, depth of photic zone and phytoplankton production. A great part of community respiration was associated with the heterotrophic activity of the phytoplankton biomass or its degradation by bacteria and 80% of the variability in oxygen consumption was explained by the variation of chlorophyll-a. Specific rate of respiration was 1.5 mg O2 mg Chla-1 h-1 during diurnal cycles, which corresponded to less than 5% of the specific rate at optimum depth of production. Still, diurnal water column respiratory losses were always of the same magnitude as the total photosynthetic gains in the photic zone, since the mixing depth exceeded the depth of the photic zone. Total column net growth was zero at a ratio between depth of photic zone and mixing depth of 0.19. Water level variations however altered the mixing depth and affected this ratio and net growth. As a consequence, the phytoplankton biomass either increased or decreased until the ratio was re-established through changes of the photic zone depth, which was governed by the phytoplankton biomass itself through the chlorophyll-a light attenuation. This revised version was published online in July 2006 with corrections to the Cover Date.     

广西主要树种(组)异速生长模型及森林生物量特征

基于广西11类主要树种(组)5个龄组(245株样木、345块样地)的生物量实测调查,建立了各树种(组)的生物量优化异速生长模型,探讨广西森林生态系统总生物量及不同森林类型、不同龄组、不同层次的生物量组成与分配。结果表明:(1)广西11类树种(组)叶、枝、干、根、全株生物量(除了杉树叶、桉树叶生物量)、地上-地下、胸径-树高的优化回归模型均为幂函数,经t检验均达到显著水平(P0.05),其中11类树种(组)以全株生物量的模拟效果最好;(2)广西森林总生物量为1425.37 Tg,平均生物量为105.36 Mg/hm2,各森林类型总生物量为松树林(366.14 Tg)硬阔(291.08 Tg)软阔(239.75 Tg)石山林(165.51 Tg)杉木林(164.01 Tg)桉树林(99.55 Tg)栎类(46.34 Tg)八角林(20.21 Tg)油茶林(19.59 Tg)竹林(13.19 Tg),均随年龄的增加而增加,各层次生物量均以乔木层占绝对优势,所占比例为78.30%—97.47%,各龄组地上生物量均大于地下生物量;(3)考虑统计学与实际应用之间的平衡及异速生长模型的可解释量、回归系数的显著性,以胸径为变量的生物量模型能有效估算广西主要树种(组)各器官及总生物量;(4)优化筛选的广西各树种(组)的地上-地下优化异速生长模型及推算的地上-地下生物量比,对于估计广西森林地下生物量具有重要参考价值。