Elevated temperature may intensify the positive effects of nutrients on microbial decomposition in streams

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Decomposition of Avicennia marina on an iron‐smelting slag substrate

The present study, conducted near Newcastle, Australia, used a blocked analysis of variance experimental design to compare initial nutrient concentrations and decomposition rates of Avicennia marina (grey mangrove) grown on sand and rock blast furnace slag. There were no significant differences ( ANOVA ; P > 0.05) in mean initial nutrient concentrations of total C, N and P for plants grown on the sand and slag substrates. A litterbag technique was used to estimate decomposition rates. After 360 days of incubation, repeated measures analysis did not identify significant differences between the substrates for the interaction term ‘substrate × time’ or the term ‘substrate’ for percentage weight loss or for C, N and P remaining. Avicennia marina on both substrates had nutrient characteristics and decomposition rates comparable to those found in the literature. Results suggest that initial nutrient concentration and decomposition rates are not dramatically influenced by the presence of slag.     

黄土高原樟子松和落叶松与其他树种枯落叶混合分解对土壤的影响

通过采集树木枯落叶与土壤进行室内混合分解培养试验,研究了黄土高原常见的樟子松和落叶松与其他树种枯落叶混合分解对土壤性质的影响及存在的相互作用,从而为不同树木种间关系的探索和该地区人工纯林的混交改造提供科学指导。结果表明:12种枯落叶单一分解均明显提高了土壤脲酶(54%—110%)、脱氢酶(85%—288%)和磷酸酶(81%—301%)活性以及有机质(29%—55%)和碱解N(12%—49%)含量,但对土壤速效P含量和CEC的影响存在较大差异。综合而言,樟子松分别与白桦、刺槐、白榆、柠条和落叶松枯落叶混合分解在对土壤性质的影响中存在相互促进作用,而分别与小叶杨、沙棘、紫穗槐、侧柏和辽东栎枯落叶混合分解在对土壤性质的影响中存在相互抑制作用;落叶松分别与刺槐、白桦、小叶杨和紫穗槐枯落叶混合分解在对土壤性质的影响中存在相互促进作用,而分别与柠条、侧柏、辽东栎、沙棘、油松和白榆枯落叶混合分解在对土壤性质的影响中存在相互抑制作用。     

平果喀斯特山地不同植物群落的土壤质量评价

了解喀斯特山地的土壤环境质量,对其植被恢复和石漠化治理有着重要意义。基于群落土壤肥力分析,采用典范对应分析(CCA)和因子分析相结合的方法,定量评价了广西平果喀斯特山地灌丛、灌木、仪花和蚬木群落的土壤质量。结果表明:土壤物理结构随植被恢复得到改善,土壤容重下降、孔隙增多、持水能力增强。土壤p H值以灌丛最高,仪花和蚬木林的土壤有机质、全氮和碱解氮含量明显高于灌丛和灌木,灌丛、灌木的土壤全磷、全钾和速效钾含量则显著高于次生乔木林;土壤速效磷和交换性钙含量差异不显著。CCA可以有效筛选土壤质量评价指标,土壤质量综合评价分值的大小顺序为:仪花林(0.41)蚬木林(0.27)灌丛(-0.20)灌木林(-0.44)。导致灌丛和灌木林土壤质量较低的原因主要与群落生产力低、土壤有机质等养分积累少有关。     

THE PROCESSING OF UNCONFINED,NATURALLY ENTRAINED LEAVES IN TWO LOW-ORDER SOUTHERN AFRICAN MOUNTAIN STREAMS

Summary

Breakdown of unconfined and confined leaves of the riparian tree Brabejum stellatifolium L. was investigated in two low order mountain streams (Window Stream and Langrivier) in the southwestern Cape, South Africa. At both sites, 5000 unconfined leaves were released in April and another 5000 in December 1990. The leaves were marked and half of them presoaked in river water prior to release. Leaves reaching a net 100 m below the point of release were removed periodically. On termination of the experiments, the study reaches were cleared of the remaining marked leaves. The distance which these leaves had travelled, and the retentive feature at which they were found were recorded. All leaves were weighed after recovery. In December 1990, leaves confined in coarse-mesh bags were placed on the stream beds of the two sites. Decay rates of unconfined leaves differed between streams and seasons but not between wetted and dry leaves or those of contrasting initial size and weight. In winter, breakdown of unconfined leaves was rapid (t₅₀ of 6.6d and 23.9d for Langrivier and Window Stream respectively). In summer, breakdown of unconfined leaves was slower (t₅₀ of 58d, Langrivier), but more rapid than leaves confined in mesh bags (t₅₀ of 77d, Langrivier). Distance travelled downstream had no significant effect on leaf breakdown. Different retentive features resulted in different rates of decay. Leaf weight loss in winter and summer at both sites was greatest in riffles (17–80%) and runs (21–78%). In all cases, stranded (exposed and out of the water) leaves lost the least weight (4–38%).     

Plant diversity does not buffer drought effects on early‐stage litter mass loss rates and microbial properties

Human activities are decreasing biodiversity and changing the climate worldwide. Both global change drivers have been shown to affect ecosystem functioning, but they may also act in concert in a non‐additive way. We studied early‐stage litter mass loss rates and soil microbial properties (basal respiration and microbial biomass) during the summer season in response to plant species richness and summer drought in a large grassland biodiversity experiment, the Jena Experiment, Germany. In line with our expectations, decreasing plant diversity and summer drought decreased litter mass loss rates and soil microbial properties. In contrast to our hypotheses, however, this was only true for mass loss of standard litter (wheat straw) used in all plots, and not for plant community‐specific litter mass loss. We found no interactive effects between global change drivers, that is, drought reduced litter mass loss rates and soil microbial properties irrespective of plant diversity. High mass loss rates of plant community‐specific litter and low responsiveness to drought relative to the standard litter indicate that soil microbial communities were adapted to decomposing community‐specific plant litter material including lower susceptibility to dry conditions during summer months. Moreover, higher microbial enzymatic diversity at high plant diversity may have caused elevated mass loss of standard litter. Our results indicate that plant diversity loss and summer drought independently impede soil processes. However, soil decomposer communities may be highly adapted to decomposing plant community‐specific litter material, even in situations of environmental stress. Results of standard litter mass loss moreover suggest that decomposer communities under diverse plant communities are able to cope with a greater variety of plant inputs possibly making them less responsive to biotic changes.     

长白山红松阔叶混交林紫椴枝条的分解实验

研究了长白山北坡椴树（Tilia amurensis）枝条的分散进程,实验结果揭示,分解率是与各实验地的植被类型,海拔,生长季月平均大于5℃的积温等密切相关。其枝条分解的保存率（Y）与分解年龄（x）的相关,可用指数模型：Y＝e^-kx来拟合,在红松阔叶混交林,红松外叶混交林,岳桦去冷杉林及岳桦林中椴树枝条分解常数K分别为－0.168与－0.127,－0.102和－0.094。枝条原重量50％的分解年龄在上述4个森林中分别是4,5,6和7a。实验还指出,在长白山红松阔叶混交林皆伐迹地的实验条件下适当的蔽荫和浇水对分解有正面影响。而且,枝条的分解率主要是以长白山不同海拔植被类型的温度条件而转移,特别是生长季的积温。     

Recognition of peat-forming plant communities from their peat deposits in two south Swedish bog complexes

Peat samples, 3 015 from 103 boring points, on two mires (Åkhult mire, Store Mosse mire) south Sweden, have been subjected to macrofossil analysis. Based on plant remains, 9 peat groups were distinguished in the field. A further classification using phytosociological methods revealed 29 peat types. The affinities between the peat types were determined from TABORD classification and a Reciprocal Averaging ordination. The primary floristic differentiation is correlated with a gradient from treeless-to wooded stands, which coincides largely with the mire expanse-mire margin gradient. The poor-rich gradient seems to parallel the treeless-wooded gradient as well and may reflect the natural conditions in this mire before it was affected by man. The hummock-mud-bottom gradient is easy to distinguish in peat, formed by bog communities, but is not distinct in peat formed by fen communities and impossible to detect in peat dominated by wood remains. The amount of identifiable remains depends on the decomposition, which is determined by (1) the period of time the plant litter stays in the acrotelm, and (2) the nutrient status. The decomposition is greatest in fen-peat with abundant wood remains. This probably depends on a good supply of oxygen caused by greater horizontal water movements and better nutrient status.     

Functional indicators of stream health: a river‐basin approach

1. The efficacy of leaf‐litter decomposition, sediment respiration, biofilm biomass, growth, chlorophyll a concentration and the autotrophic index (biofilm ash‐free dry mass/chlorophyll a) and fungal biomass for detecting human‐induced change was evaluated using 24 references and 15 disturbed stream sites located in central Portugal. 2. Decomposition rates of alder (Alnus glutinosa) and oak (Quercus robur) leaves and sediment respiration rates were effective in discriminating impairment. Decomposition was negatively correlated with abiotic factors, such as ammonium and nitrite concentrations, connectivity and alterations in the hydrological regime, and positively correlated with nitrate concentration and oxygen concentration. Sediment respiration rates were correlated with organic contamination, land use and morphological changes. 3. Growth rates of biofilm, concentration of chlorophyll a and the autotrophic index, although 41–73% higher at disturbed compared to reference sites, were not significantly different. These three variables were significantly correlated with total organic carbon, oxygen concentration, pH, nitrite and the presence of dams. Fungal biomass on leaves and biofilm biomass on natural substrata did not differ between reference and disturbed sites. 4. Our findings lend support to the use of functional variables like decomposition and sediment respiration in monitoring and when used together with structural variables should give a more holistic measure of stream health.     

Microbial community dynamics alleviate stoichiometric constraints during litter decay

Under the current paradigm, organic matter decomposition and nutrient cycling rates are a function of the imbalance between substrate and microbial biomass stoichiometry. Challenging this view, we demonstrate that in an individual‐based model, microbial community dynamics alter relative C and N limitation during litter decomposition, leading to a system behaviour not predictable from stoichiometric theory alone. Rather, the dynamics of interacting functional groups lead to an adaptation at the community level, which accelerates nitrogen recycling in litter with high initial C : N ratios and thus alleviates microbial N limitation. This mechanism allows microbial decomposers to overcome large imbalances between resource and biomass stoichiometry without the need to decrease carbon use efficiency (CUE), which is in contrast to predictions of traditional stoichiometric mass balance equations. We conclude that identifying and implementing microbial community‐driven mechanisms in biogeochemical models are necessary for accurately predicting terrestrial C fluxes in response to changing environmental conditions.