Continuous soil carbon storage of old permanent pastures in Amazonia

Amazonian forests continuously accumulate carbon (C) in biomass and in soil, representing a carbon sink of 0.42–0.65 GtC yr^?1. In recent decades, more than 15% of Amazonian forests have been converted into pastures, resulting in net C emissions (~200 tC ha^?1) due to biomass burning and litter mineralization in the first years after deforestation. However, little is known about the capacity of tropical pastures to restore a C sink. Our study shows in French Amazonia that the C storage observed in native forest can be partly restored in old (≥24 year) tropical pastures managed with a low stocking rate (±1 LSU ha^?1) and without the use of fire since their establishment. A unique combination of a large chronosequence study and eddy covariance measurements showed that pastures stored between ?1.27 ± 0.37 and ?5.31 ± 2.08 tC ha^?1 yr^?1 while the nearby native forest stored ?3.31 ± 0.44 tC ha^?1 yr^?1. This carbon is mainly sequestered in the humus of deep soil layers (20–100 cm), whereas no C storage was observed in the 0‐ to 20‐cm layer. C storage in C4 tropical pasture is associated with the installation and development of C3 species, which increase either the input of N to the ecosystem or the C:N ratio of soil organic matter. Efforts to curb deforestation remain an obvious priority to preserve forest C stocks and biodiversity. However, our results show that if sustainable management is applied in tropical pastures coming from deforestation (avoiding fires and overgrazing, using a grazing rotation plan and a mixture of C3 and C4 species), they can ensure a continuous C storage, thereby adding to the current C sink of Amazonian forests.     

Influence of living plants on immobilization of nitrogen in permanent pastures

Summary The presence of plants has a negative effect on the net nitrogen mineralization rate in samples of turf from permanent grassland. This effect is probably caused by root excretions and dead roots which lead to the immobilization of mineralized nitrogen. When the plants of a turf sample have been killed by repeated cutting and removal of the shoots the mineral nitrogen immobilized due to the presence of plants is subsequently more readily mobilized than that immobilized in the greater part of the soil organic matter. The constant presence of plants is responsible for the accumulation of nitrogen in the organic matter of the soil of permanent grassland.     

The invertebrate population and response to pesticide treatment of two permanent and two temporary pastures

During 1979 and 1980 the herbage yields of two permanent pastures and two temporary swards were compared. All four swards received 250 kg N/ha per yr. The invertebrate population of all four swards was studied. Pot-worms (Enchytraeidae) and some species with long life cycles, e.g. wireworms (Agriotes spp.) were more numerous in the permanent swards, but aerial species were more numerous in the temporary swards. A range of pesticide treatments was applied. At one temporary sward site, application of the broad-spectrum pesticide aldicarb increased total annual yield of herbage by 16% in 1979 and 33% in 1980. Insecticide application at the same site resulted in no increase in herbage yield in 1979 and 12% yield increase in 1980. At the other three sites no significant increases in total annual yield were recorded in either year, but there were significant responses at one harvest or more at every site.     

Seasonal vegetation changes in mountain pastures due to simulated effects of cattle grazing

Cattle influence grassland dynamics in three ways: herbage removal, dung deposition and trampling. The objective of this study was to assess the effects of these factors, separately or in combination, and to compare them with cattle grazing over a one year period in a field experiment conducted in the Jura Mountains of northwestern Switzerland. A set of controlled treatments simulating the three factors was applied in a fenced area: (1) repeated mowing — three levels; (2) intensive trampling — two levels; (3) manuring with a liquid mixture of dung and urine — three levels. All treatments were applied homogeneously to the entire surface of each of the 40 plots inside the exclosure. Additionally, ten plots outside the fenced area represented reference plots with regular cattle pasturing. The multivariate response of species composition was assessed three times with the point‐intercept method: in spring before the treatments, in autumn after one season of treatments and at the beginning of the following year after winter rest. Multivariate analyses of vegetation data in the first year showed an overwhelming seasonal shift and significant differences induced by treatments. Abandoned and manured plots showed the largest deviation from the cattle grazed reference. Herbage removal, simulated by repeated mowing, appeared to be the most important factor for maintaining vegetation texture. Seasonal treatment effects were only partially carried over to the next spring, showing an unexpected resilience of the plant community, probably due to life‐history traits and competition release following climatic disturbance in winter.     

Conversion from forests to pastures in the Colombian Amazon leads to contrasting soil carbon dynamics depending on land management practices

Strategies to mitigate climate change by reducing deforestation and forest degradation (e.g. REDD+) require country‐ or region‐specific information on temporal changes in forest carbon (C) pools to develop accurate emission factors. The soil C pool is one of the most important C reservoirs, but is rarely included in national forest reference emission levels due to a lack of data. Here, we present the soil organic C (SOC) dynamics along 20 years of forest‐to‐pasture conversion in two subregions with different management practices during pasture establishment in the Colombian Amazon: high‐grazing intensity (HG) and low‐grazing intensity (LG) subregions. We determined the pattern of SOC change resulting from the conversion from forest (C3 plants) to pasture (C4 plants) by analysing total SOC stocks and the natural abundance of the stable isotopes ¹³C along two 20‐year chronosequences identified in each subregion. We also analysed soil N stocks and the natural abundance of ¹⁵N during pasture establishment. In general, total SOC stocks at 30 cm depth in the forest were similar for both subregions, with an average of 47.1 ± 1.8 Mg C ha^?1 in HG and 48.7 ± 3.1 Mg C ha^?1 in LG. However, 20 years after forest‐to‐pasture conversion SOC in HG decreased by 20%, whereas in LG SOC increased by 41%. This net SOC decrease in HG was due to a larger reduction in C3‐derived input and to a comparatively smaller increase in C4‐derived C input. In LG both C3‐ and C4‐derived C input increased along the chronosequence. N stocks were generally similar in both subregions and soil N stock changes during pasture establishment were correlated with SOC changes. These results emphasize the importance of management practices involving low‐grazing intensity in cattle activities to preserve SOC stocks and to reduce C emissions after land‐cover change from forest to pasture in the Colombian Amazon.     

Viruses occurring in white clover (Trifolium repens L.) from permanent pastures in Britain

The uptake of captan from aqueous solution by conidia of Neurospora crassa can be markedly reduced by pretreatment of the cells with thiol reagents such as iodoacetic acid (IOA). The nature of this reaction has been investigated and it is shown that IOA largely reacts with the soluble thiol pool of the spores. Captan, however, reacts with both soluble and insoluble thiols and it is suggested that whilst the former is a detoxication process the latter may provide the key to its toxic action. Using glutathione as a model soluble thiol the molar ratio and pH dependence of the captan detoxication process has been determined and compared with the cellular reactions. Assay of ³⁵S-labelled captan has shown that captan is almost completely decomposed by the spores and that one-third of the accumulated captan is converted to sulphur compounds fixed to insoluble cell entities.     

Grassland structure in native pastures: links to soil surface condition

Summary When grassland is grazed by livestock, the structure of the sward changes in a patchy manner. With continuous selective grazing there is a mosaic of short and tall patches but as grazing intensifies the area of short‐grazed patch increases until the paddock has a lawn‐like appearance. This mosaic of patch structures can be stable, as short patches tend to attract repeated grazing and tall patches tend to be avoided. Because heavy grazing can detrimentally affect soil and water functions in grassland (ultimately resulting in erosion), we aimed to assess how well the physical structure of the sward reflects soil surface condition. We described four grassland patch structures that were assumed to reflect different levels of present grazing, and to some extent, past grazing pressure. We assessed patch structure and two other grass‐related variables (basal area of a ‘large tussock’ functional group and basal area of all perennial grass) as possible indicators of soil surface condition. Three indices of condition were measured in the field. The infiltration and nutrient cycling index declined progressively across patch structures, consistent with increasing grazing pressure. The stability index was found to be reduced only for the most heavily grazed grass structure (short patches). We found the ‘large tussock’ grass functional group to be a more sensitive indicator of soil surface condition than the group consisting of all perennial grasses. We found no evidence of sudden soil surface condition decline beyond a certain level of grass basal area, that is, there was no evidence of thresholds, rather, incremental loss of condition accompanied grass decline. We are thus not able to further refine an earlier proposed management recommendation ‘Graze conservatively to maintain dominance of large and medium tussock grasses over 60–70% of the native pastures’, except to suggest the use of short patches as a more practical indicator, rephrasing the recommendation as ‘Graze conservatively to allow a maximum of 30% short‐grazed patches in native pastures’.     

Field method for isolation of trichostrongyle larvae from vegetation of natural pastures of Arctic ruminants

The extent to which wild ruminant populations are exposed to infective helminth larvae on their natural pastures is relatively undetermined. In the present study, a modified method for sampling of herbage and isolation of trichostrongyle infective third-stage larvae from natural pastures was used successfully in a muskox habitat in low-Arctic Greenland. The method, a revision of the Macro-Baermann method, is particularly aimed at fieldwork under primitive conditions.     

Mercuric reductase gene transfer from soil to rumen bacteria

Conjugal transfer between soil bacterial population and microorganisms isolated from the rumen of herbivores from mercury-polluted area was investigated. The transfer of merA encoding mercury-resistance plasmids from soil bacteria Enterobacter cloacae and Enterococcus durans into two ruminal isolates Citrobacter freundii and Bacillus subtilis was observed. Approximately the same frequency of mobilization in mating experiments was observed for both Gram-negative (approximately 2.5 x 10(-8), transconjugants-to-recipient ratio) and Gram-positive (approximately 1.3 x 10(-8)) bacteria.     

Floristic composition and structure of vegetation under isolated trees in neotropical pastures

Abstract. Large isolated trees are a common feature of the agricultural landscape in humid tropical regions originally covered by rain forest. These isolated trees are primarily used as a source of shade for cattle and people. 13 pastures (totalling ca. 80 ha) currently used as cattle pasture were studied. In them, we registered 265 isolated trees belonging to 57 species. 50 trees of the most frequent species (Ficus spp. n = 30 and Nectandra ambigens n = 20) were selected to examine the influence of isolated trees on floristic composition and vegetation structure in the pastures. At each tree, three 4–m² quadrats were sampled: under the canopy, directly under the canopy perimeter, and beyond the canopy in the open pasture. Under-canopy vegetation was structurally and floristically different from the other two sampling sites. Mean species richness per quadrat was significantly higher under the canopy (17.8 ± 4.3 SD) than at the canopy perimeter (11.2 ± 3.4) and in the open pasture (10.6 ± 3.6) sites. Stem density was higher at under-canopy sites, where greater proportions of endozoochorous and rain-forest species were found. Isolated trees function as nursery plants for rain-forest species by facilitating the establishment of zoochorous species whose seeds are deposited under the tree canopies by frugivorous birds or bats. Our results imply that isolated trees may play a major role in seed dispersal and establishment of native species, which is of consequence for the preservation of rain-forest species in these fragmented landscapes.     

Effects of soil water content on soil respiration in forests and cattle pastures of eastern Amazonia

The effect of soil water content on efflux of CO₂ from soils has been described by linear, logarithmic, quadratic, and parabolic functions of soil water expressed as matric potential, gravimetric and volumetric water content, water holding capacity, water-filled pore space, precipitation indices, and depth to water table. The effects of temperature and water content are often statistically confounded. The objectives of this study are: (1) to analyze seasonal variation in soil water content and soil respiration in the eastern Amazon Basin where seasonal temperature variation is minor; and (2) to examine differences in soil CO₂ emissions among primary forests, secondary forests, active cattle pastures, and degraded cattle pastures. Rates of soil respiration decreased from wet to dry seasons in all land uses. Grasses in the active cattle pasture were productive in the wet season and senescent in the dry season, resulting in the largest seasonal amplitude of CO₂ emissions, whereas deep-rooted forests maintained substantial soil respiration during the dry season. Annual emissions were 2.0, 1.8, 1.5, and 1.0 kg C m^-2 yr^-1 for primary forest, secondary forest, active pasture, and degraded pasture, respectively. Emissions of CO₂ were correlated with the logarithm of matric potential and with the cube of volumetric water content, which are mechanistically appropriate functions for relating soil respiration at below-optimal water contents. The parameterization of these empirical functions was not consistent with those for a temperate forest. Relating rates of soil respiration to water and temperature measurements made at some arbitrarily chosen depth of the surface horizons is simplistic. Further progress in defining temperature and moisture functions may require measurements of temperature, water content and CO₂ production for each soil horizon.     

Prairie vegetation and soil nutrient responses to ungulate carcasses

The impact of large ungulate carcasses on grassland dynamics was investigated by monitoring vegetation and soil nutrients in 50-cm circular zones around the center of bison (Bos bison), cattle (B. taurus), and deer (Odocoileus virginianus) carcasses. An ungulate carcass creates an intense localized disturbance that varies with animal size and the season of death. Unlike other natural disturbances, carcasses deposit a concentrated pulse of nutrients into the soil. One year after death, inorganic nitrogen concentrations were significantly higher in the inner 50 cm at both adult and juvenile carcass sites than in surrounding prairie. Areas around a carcass became zones of fertility that favored different components of the vegetation and stimulated biomass production. Species richness and diversity at the center of carcass sites were lowest 1 year after death, but increased significantly in subsequent years. However, warm-season perennial grasses declined near the center of carcass sites and did not recover. Five years after death, ungulate carcass sites remained disturbed patches that harbored vegetation characteristically different in composition and stature from surrounding prairie. By providing a niche for species not normally found in undisturbed prairie, carcasses increased community heterogeneity and may play an important role in adding spatial complexity to grassland ecosytems. Received: 12 April 1999 / Accepted: 7 September 1999     

黄土丘陵沟壑区三种豆科人工草地的植被与土壤特征

在黄土高原丘陵沟壑区以 4龄苜蓿 (Medicago sativa)、沙打旺 (Astragalus adsurgens)和甘草 (Giycyrrhiza uralensis)单播人工草地为材料 ,人工牧草、杂草和土壤 3方面研究了其生产性能和生态特性。在相同的管理条件下 ,沙打旺种群高度平均高于苜蓿 33.8% ,是甘草的 6 .2倍 ;苜蓿的密度分别是甘草和沙打旺的 5 .9倍和 2 .6倍 ;沙打旺盖度最大 ,苜蓿次之 ,甘草最小。三种牧草的地上生物量及其占群落生物量的比例依次是苜蓿 >沙打旺 >甘草 ;苜蓿种群生物量占群落的比例接近沙打旺 ,二者远高于甘草。甘草人工草地的杂草种数、杂草生物量及其生物量占群落的比例均最大。0～ 10 0 cm土层内三种人工草地的地下生物量依次为甘草 >苜蓿 >沙打旺。 0～ 10 0 cm土层内营养物质含量 :全 P,苜蓿 >甘草 >沙打旺 ;全 N,苜蓿与甘草接近 ,高于沙打旺 ;速效 P、速效 N都是甘草最高 ;有机质含量 ,苜蓿接近甘草、高于沙打旺。讨论了管理措施与人工草地的关系 ,加大投入是维持人工草地群落稳定的前提之一     

Biosorption of cobalt by fungi from serpentine soil of Andaman

Fungi belonging to Aspergillus, Mortierella, Paecilomyces, Penicillium, Pythium, Rhizopus and Trichoderma, isolated from serpentine soil of Andaman (India) were screened for cobalt-resistance. Eleven out of total 38 isolated fungi which tolerated > 6.0 mM Co(II) were evaluated for cobalt biosorption using dried mycelial biomass. Maximum Co(II)-loading (1036.5 microM/g, 60 min) was achieved with Mortierella SPS 403 biomass, which removed almost 50% of 4.0 mM cobalt from the aqueous solution. Co(II)-sorption kinetics of Mortierella SPS 403 biomass was fast and appreciable quantities of metal [562.5 microM/g] was adsorbed during first 10 min of incubation. The metal biosorption capacity of the isolate was accelerated with increasing cobalt concentration, while it was reverse with increase of initial biomass. The optimum pH and temperature for Co(II) removal were 7.0 and 30 degrees C, respectively. However, Co(II)-uptake was inhibited in presence of other metals (Pb, Cd, Cu, Ni, Cr and Zn). Freundlich adsorption isotherm appropriately describes Mortierella SPS 403 biomass as an efficient Co(II)-biosorbent.     

Effects of vegetation on the emission of methane from submerged paddy soil

Summary Methane emission rates from rice-vegetated paddy fields followed a seasonal pattern different to that of weed-covered or unvegetated fields. Presence of rice plants stimulated the emission of CH₄ both in the laboratory and in the field. In unvegetated paddy fields CH₄ was emitted almost exclusively by ebullition. By contrast, in rice-vegetated fields more than 90% of the CH₄ emission was due to plant-mediated transport. Rice plants stimulated methanogenesis in the submerged soil, but also enhanced the CH₄ oxidation rates within the rhizosphere so that only 23% of the produced CH₄ was emitted. Gas bubbles in vegetated paddy soils contained lower CH₄ mixing ratios than in unvegetated fiels. Weed plants were also efficient in mediating gas exchnage between submerged soil and atmosphere, but did not stimulate methanogenesis. Weed plants caused a relatively high redox potential in the submerged soil so that 95% of the produced CH₄ was oxidized and did not reach the atmosphere. The emission of CH₄ was stimulated, however, when the cultures were incubated under gas atmospheres containing acetylene or consisting of O₂-free nitrogen.     

植被砍伐对土壤养分的影响

研究了不同砍伐频率下,香港、深圳和鹤山研究样地山坡地Ｎ、Ｐ、Ｋ含量的差异．不同采样地之间,养分全量和有效量差异显著．在尚未砍伐的山坡地,土壤养分含量显著高于经常砍伐的山坡地．未伐土壤的Ｎ含量顺序为香港样地＞深圳样地＞鹤山样地．下层土壤Ｐ的含量高于上层土壤．深圳样地常代土壤养分含量高于鹤山．结果建议采用最适砍伐频率和在最适季节砍伐,以便减少砍伐产生的不利影响．     

Sampling techniques and disturbance of algal vegetation in permanent quadrats

Summary In studying permanent quadrats established in an algal vegetation by means of sampling in the quadrat itself, the vegetation is exposed to the risk of disturbance by the sampling. By taking small samples (microsampling or reduced size sampling) this risk is reduced considerably. The quantitative minimal area of vegetation units ofVaucheria, filamentous green algae and Oscillatoriaceae is less than 20 mm². InVaucheria components, however, often the viability for cultivation purposes is the limiting factor for the size of a sample suitable for a complete analysis of the permanent quadrat. The minimum size of a viableVaucheria sample is 1 cm². The disturbance of the algal layer by other external factors is often more intense than that caused by sampling. Nomenclature follows Polderman (1975b). Contribution to the Symposium of the Working Group for Succession Research on Permanent Plots, held at Yerseke, The Netherlands, October 1975. The author thanks Dr. Ir. W. G. Beeftink for helpful criticism and Mrs. R.A. Polderman-Hall for correcting the English text. The investigation of the algal communities of saltmarshes in the Wadden area is a project of the Netherlands Organisation for the Advancement of Pure Research.