Tree species selection and soil tillage in alley cropping systems with Phaseolus vulgaris L. in a humid premontane climate: biomass production,nutrient cycling and crop responses

The development of alley cropping systems is based on the assumption that leguminous trees planted in hedgerows influence the yield of associated crops favourably by means of the additional nutrient pool applied to the soil through tree prunings. An on-station field study (split-plot design in a randomised block design) was conducted on an Eutric Cambisol under humid premontane climate conditions in Costa Rica in order to evaluate the ability of Erythrina poeppigiana, Calliandra calothyrsus and Gliricidia sepium to increase bean (Phaseolus vulgaris) yields compared to sole cropping. Soil tillage was applied as a sub-treatment in order to evaluate if soil preparation would additionally alter soil fertility and bean yield. After seven years with pruning twice per year, the size of both the total N and P pool in the pruned tree material was about three times higher for Erythrina prunings than for Calliandra and Gliricidia prunings. Two and five weeks after mulch application 50–150% higher inorganic N pools were measured in the soil from Erythrina plots, the bean shoot biomass at harvest was increased by 65–100% and the bean yield was 15–50% higher than in plots with beans alone. Hence, of the three tree species, Erythrina was the best choice for alley cropping systems in the pedoclimatic environment studied. Soil tillage reduced bean yield, soil organic matter, total soil N content and soil microbial biomass N in the top soil and is not recommended for similar soils in humid premontane climates.     

水分对土壤呼吸的影响及机理

土壤呼吸是陆地碳循环的重要环节,在全球变化的背景下,研究水分对土壤呼吸的影响,能为探索陆地生态系统在碳循环方面的源—汇功能和揭示碳的失汇之迷提供有力的证据。综述了水分对土壤呼吸的影响及其机理。土壤呼吸是一个复杂的生态学过程,大气降水对土壤呼吸的影响结果是因时、因地而异,在湿润的生态系统或者干湿交替的生态系统中比较湿润的季节．降水事件对土壤呼吸可能会产生比较明显的抑制现象;而在干旱的生态系统或有干湿交替季节的生态系统中比较干旱的季节里,降水事件可能会强烈地激发土壤呼吸。其对土壤呼吸的影响机理包括水分对土壤孔隙中CO2替代、对CO2扩散的阻滞、对微生物活动的刺激和对微生物生物量的影响等。由于实验方法和标准的不一致以及影响土壤呼吸的因素的多样性。水分量的变化对土壤呼吸的影响很难以一个统一的方程来描述,总的来说,最优的水分状况通常是接近最大田间持水力,当土壤处于过于或过湿状态时,土壤呼吸会受到抑制。水分量的变化对土壤呼吸的影响机制在于可溶性有机质、土壤的通透性、微生物与植物根系生命活动等都随土壤水分状况不同而发生相应的改变。关于水分与土壤呼吸的关系研究今后应该主要集中在：(1)水分对根系呼吸和土壤微生物呼吸分别产生的影响;(2)全球变化后水分格局的变化对全球陆地生态系统土壤呼吸格局的潜在影响;(3)人类活动通过直接或间接改变水分状况而对土壤释放CO2的贡献率。     

Fine root distribution of trees and understory in mature stands of maritime pine (Pinus pinaster) on dry and humid sites

Maritime pine (Pinus pinaster) is the main tree cropping species in the Landes of Gascogne forest range in south western France. Soils are nutrient poor, sandy podzosols and site fertility is determined essentially by organic matter content and depth of water table, which is known to limit root growth. We hypothesised, with an ultimate goal of constructing a nutrient uptake model applicable to this region, that the organic top horizons together with the depth of the water table should be the most important parameters related to fine root distribution and presence of associated mycorrhiza. To test this hypothesis, we compared two adult Pinus pinaster stands, contrasting in depth of water table and soil fertility and evaluated fine roots (diameter ≤2 mm) of understory species and fine roots and ectomycorrhizal morphotypes of Pinus pinaster down to 1.2 m, using a soil corer approach. Total fine root biomass of Pinus pinaster was not significantly different between both sites (3.6 and 4.5 t ha⁻¹ for the humid, respectively, dry site), but root distribution was significantly shallower and root diameter increased more with depth at the humid site, presumably due to more adverse soil conditions as related to the presence of a hardpan, higher amount of aluminium oxides and / or anoxia. Fine roots of Pinus pinaster represented only about 30% of total fine root biomass and 15% of total fine root length, suggesting that the understory species cannot be ignored with regards to competition for mineral nutrients and water. A comparison of the ectomycorrhizal morphotypes showed that the humid site could be characterised by a very large proportion of contact exploration types, thought to be more relevant in accessing organic nutrient sources, whereas the dry site had a significantly higher proportion of both long-distance and short-distance exploration types, the latter of which was thought to be more resistant to short-term drought periods. These results partly confirm our hypothesis on root distribution as related to the presence of soil mineral nutrients (i.e. in organic matter), point out the potential role of understory plant species and ectomycorrhizal symbiosis and are a valuable step in building a site-specific nutrient uptake model.     

汶川震区不同气候区受损植被土壤有机碳储量和碳密度分布特征

采用ISSR分子标记技术,对广西特有珍稀濒危植物小花异裂菊6个野生种群的遗传多样性进行了研究。结果表明：10条引物对141个个体共检测到96个位点,其中29个位点具有多态性,多态位点百分率( PPB)为30.21％。在物种水平上,小花异裂菊 PPB 为30.21％, Nei ’ s 基因多样性指数( H )为0.1054, Shannon’s信息指数(I)为0.1546。在种群水平上,PPB 为9％~19％,H 为0.0212~0.0513,I 为0.0339~0.0805。基于Nei’ s遗传多样性分析所得出的种群间基因分化系数Gst＝0.6905,表明种群内的遗传变异为30.95％,种群间的遗传变异为69.05％,小花异裂菊的遗传变异主要存在于种群间。 AMOVA分析结果与前面结果相符。小花异裂菊种群间的基因流( Nm)为0.2242。从遗传距离看,杨堤和兴坪种群的遗传距离最小,为0.0398,白沙和阳朔之间的遗传距离最大,为0.1609。在UPGMA聚类图中,6个种群可分为两组,阳朔和高田为一组,普益、白沙、兴坪、杨堤聚为一组。研究认为小花异裂菊的自交亲和的繁育系统和分布区域的片段化可能是导致种群遗传多样性较低和种群间高遗传分化的主要原因。该研究结果为该物种种质资源的保护提供了科学依据。     

Quantification of soil organic carbon sequestration potential in cropland: A model approach

Agroecosystems have a critical role in the terrestrial carbon cycling process. Soil organic carbon (SOC) in cropland is of great importance for mitigating atmospheric carbon dioxide increases and for global food security. With an understanding of soil carbon saturation, we analyzed the datasets from 95 global long-term agricultural experiments distributed across a vast area spanning wide ranges of temperate, subtropical and tropical climates. We then developed a statistical model for estimating SOC sequestration potential in cropland. The model is driven by air temperature, precipitation, soil clay content and pH, and explains 58% of the variation in the observed soil carbon saturation (n=76). Model validation using independent data observed in China yielded a correlation coefficient R ² of 0.74 (n=19, P<0.001). Model sensitivity analysis suggested that soils with high clay content and low pH in the cold, humid regions possess a larger carbon sequestration potential than other soils. As a case study, we estimated the SOC sequestration potential by applying the model in Henan Province. Model estimations suggested that carbon (C) density at the saturation state would reach an average of 32 t C ha⁻¹ in the top 0–20 cm soil depth. Using SOC density in the 1990s as a reference, cropland soils in Henan Province are expected to sequester an additional 100 Tg C in the future.     

Effect of Soil Texture and Moisture on the Activity of Entomopathogenic Nematodes Against Female Boophilus annulatus Ticks

Soil texture, chemistry and moisture have a profound effect upon the activity and persistence of entomopathogenic nematodes (EPNs). Whereas nematodes’ natural habitat is within the soil, ticks and other arthropod pests prefer to stay on the soil surface and under stones or leaf litter; they spend much of their life cycle in the humid environment of the soil upper layer, therefore consideration of the effect of the soil environment on nematode activity is a pre-requisite for the sucessful use of EPNs against arthropod pests. In the present study we investigated the effects of soil type, and humidity on various nematode strains and on their effectiveness against ticks. Many infective juveniles (IJs) of Steinernema carpocapsae and S. riobrave were found in the uppermost soil layer whereas the heterorhabditid strains were almost absent from the upper 6 cm of the soil profile. The IJs of S. feltiae, and the S. carpocapsae strain S-20, exhibited an intermediate behavior. It was found that the activity of IJs of S. carpocapsae in the soil upper layer (1 cm depth) was strongly affected by soil type: the greatest number of IJs were recorded from sandy loam soil; less were found in the lighter soils – ‘Marine sand’ and ‘Calcareous sandstone’ – and only very few were recovered from heavy soils. Strikingly, even when the soil moisture was low and the number of nematodes found in the upper layer correspondingly low, tick mortality remained high. The results demonstrate: (a) the possible use of the nematodes as an anti-tick agent; (b) the importance of knowing the exact interaction of nematodes with the immediate environment of the pest, in order to optimize the pest-control activity of the nematode.     

Vegetation development in a former orchard under different treatments: A preliminary report

Summary Vegetation development in a former orchard on loamy moist soil after removal of the fruit trees under different treatment is described with the help of multivariate methods. Data on 20 plots over 9 years are treated with a simple classification program and a PCA ordination. Two main groups of plots are involved: one in a relatively moist part of the area where the trees were removed in 1970, one in a slightly drier area where the trees had been removed earlier. The first group is characterized by forbs such as Urtica dioica and Lamium maculatum, the second by grasses, mainly Arrhenatherum elatius.Under a mowing regime the plots of the first group change in the direction of the second group. Under continued fertilization the Urtica vegetation can be maintained. Establishment and/or rapid spread of Urtica can be brought about in Arrhenatherum dominated sites by (re-) introduction of nitrogen fertiliser.Not mowing leads to a dense Urtica-Lamium stand in which Lamium maculatum finds an optimum some years after mowing is stopped.The methods of summarizing the site-time data are discussed and some new ones announced for further research.Nomenclature follows Heukels-van Ooststroom, Flora van Nederland, 18e druk, Wolters-Noordhoff, Groningen, 1975.Vegetation and soil analyses were mainly carried out by students in the framework of their study for the degree of doctorandus in biology: Ineke Opbroek, Ferdinand Baggerman (1970), Carla Veldhuis (1971–1972), the late Doeke Dijken (1971–1973), Jos Rijpert (1972), the Rev. Piet van der Aart, Jo Louppen (1973), Frank Verhoeven (1974), Maurits Heine (1975), Ad Peters (1976), Huub Muyres, Louis Fliervoet (1976, 1977), Emilia Peters (1977), Niek Joanknecht, Thijs Lavrijsen (1977, 1978).     

Shifts in soil organic carbon for plantation and pasture establishment in native forests and grasslands of South America

The replacement of native vegetation by pastures or tree plantations is increasing worldwide. Contradictory effects of these land use transitions on the direction of changes in soil organic carbon (SOC) stocks, quality, and vertical distribution have been reported, which could be explained by the characteristics of the new or prior vegetation, time since vegetation replacement, and environmental conditions. We used a series of paired‐field experiments and a literature synthesis to evaluate how these factors affect SOC contents in transitions between tree‐ and grass‐dominated (grazed) ecosystems in South America. Both our field and literature approaches showed that SOC changes (0–20 cm of depth) were independent of the initial native vegetation (forest, grassland, or savanna) but strongly dependent on the characteristics of the new vegetation (tree plantations or pastures), its age, and precipitation. Pasture establishment increased SOC contents across all our precipitation gradient and C gains were greater as pastures aged. In contrast, tree plantations increased SOC stocks in arid sites but decreased them in humid ones. However, SOC losses in humid sites were counterbalanced by the effect of plantation age, as plantations increased their SOC stocks as plantations aged. A multiple regression model including age and precipitation explained more than 50% (p < 0.01) of SOC changes observed after sowing pastures or planting trees. The only clear shift observed in the vertical distribution of SOC occurred when pastures replaced native forests, with SOC gains in the surface soil but losses at greater depths. The changes in SOC stocks occurred mainly in the silt+clay soil size fraction (MAOM), while SOC stocks in labile (POM) fraction remained relatively constant. Our results can be considered in designing strategies to increase SOC storage and soil fertility and highlight the importance of precipitation, soil depth, and age in determining SOC changes across a range of environments and land‐use transitions.     

Dynamics of soil carbon following destruction of tropical rainforest and the subsequent establishment of Imperata grassland in Indonesian Borneo using stable carbon isotopes

Southeast Asia has the highest rate of tropical rainforest deforestation worldwide, and large deforested areas have been replaced ultimately by the highly invasive grass Imperata cylindrica. However, information on the carbon (C) budget with such land transition is very scarce. This study presents the dynamics of soil C following rainforest destruction and the subsequent establishment of Imperata grassland in the lowland humid tropics of Indonesian Borneo using stable C isotopes. To evaluate the relative contribution of organic matter originating from primary forest (C₃) and grasslands (C₄), we compared soil C stock and natural ¹³C abundance from six sites to a depth of 100 cm using samples with a wide range of soil textures. Twelve years after the first soil sampling in the grasslands, we re‐sampled to examine temporal changes in soil organic matter. The grassland topsoil (0–5 cm) is an active layer with rapid decomposition and incorporation of fresh C (mean residence time: 7.5 year) and a substantial proportion of the stable C pool (37%). The decline in forest‐derived C was slight, even at 5–10 cm depths, and subsoil (20–100 cm depth) forest‐derived C did not change along the forest‐to‐grassland chronosequence. Grassland‐derived C stock increased significantly in the subsurface and subsoils (5–100 cm). Simulation indicated that total soil C stock (0–100 cm) increased by 18.6 Mg ha^?1 from initial primary forest (58.0 Mg ha^?1) to a new equilibrium state of the grassland (76.6 Mg ha^?1) after 30–50 years of grassland establishment. This research indicates that the soil did not function as a CO₂ source when the deforested area was replaced by Imperata grassland on the Ultisols of the Asian humid tropics. Instead, increased soil C stocks offset CO₂ emissions, with the C offset accounting for 6.6–7.4% of the loss of biomass C stock.     

Evaluation of the phosphorus status of P-deficient podzols in temperate pine stands: combining isotopic dilution and extraction methods

Phosphorus (P) is often a limiting factor of forest growth but our knowledge of the processes governing P availability in forest soils is rather limited. In the present work, we combined a isotopic dilution method with extraction methods to evaluate the P status in Pinus pinaster plantation forests on highly P-deficient soils. Total, organic, and inorganic P, dissolved and diffusive P, i.e. ionic P species that can be transferred from the solid phase to the soil solution due a gradient of concentration, were determined to a soil depth of 120 cm in a gradient of 18 forest sites (seven humid sites, five mesic sites, and six dry sites). Our objective was to assess the potential contribution of organic and inorganic P to plant available P. Based on results and our original assumptions, we observed that the contribution of organic P fractions (mineralization of soil organic P) to P availability related to the contribution of inorganic P fractions (diffusive P for durations up to 1 year) was predominant in litter, less important in top soil horizons, and negligible at depths below 30 cm. This was partly due to a decreasing proportion of organic P and an increasing proportion of diffusive P with soil depth. Owing to a very low amount of diffusive P in the top soils in dry sites, the relative contribution of organic P was actually higher in these sites than in humid and mesic sites, despite a lower overall organic P fraction. The combination of extraction and isotopic dilution methods in our study shed new light on P status in this forest range. In particular, these methods enable assessment of both the size of the pools and their dynamic fractions.     

Does the morphology of animal foraging pits influence secondary seed dispersal by ants?

Secondary seed dispersal by ants (myrmecochory) is an important process in semi‐arid environments where seeds are transported from the soil surface to an ant nest. Microsites from which ants often remove seeds are the small pits and depressions made by native and exotic animals that forage in the soil. Previous studies have demonstrated greater seed retention in the pits of native than exotic animals, but little is known about how biotic factors such as secondary seed dispersal by ants affect seed removal and therefore retention in these foraging pits. We used an experimental approach to examine how the morphology of burrowing bettong (Bettongia lesueur), greater bilby (Macrotis lagotis), short‐beaked echidna (Tachyglossus aculeatus) and European rabbit (Oryctolagus cuniculus) foraging pits and ant body size influenced ant locomotion and seed removal from pits along an aridity gradient. Ants took 3.7‐times longer to emerge from echidna pits (19.6 s) and six‐times longer to emerge from bettong pits (30.5 s) than from rabbit pits (5.2 s), resulting in lower seed removal from bettong pits than other pit types. Fewer seeds were removed from pits when cages were used to exclude large body‐sized (>2 mm) ants. Few seeds were removed from the pits or surface up to aridity values of 0.5 (humid and dry sub‐humid), but removal increased rapidly in semi‐arid and arid zones. Our study demonstrates that mammal foraging pit morphology significantly affects ant locomotion, the ability of ants to retrieve seeds, and therefore the likelihood that seeds will be retained within foraging pits.     

干旱沙区生物土壤结皮发育对红砂形态及干物质积累的影响

为了探讨干旱沙区生物土壤结皮发育对红砂形态及干物质积累的影响,以巴丹吉林沙漠南缘已发育不同类型生物土壤结皮并有红砂种群成功定居的区域为研究场所,通过野外监测与室内测定的方法对藻类-地衣、地衣、地衣-藓类结皮上的红砂（当年生、幼株、成株）形态特征及生物量进行了调查研究。结果表明：（1）藻类-地衣结皮演替到地衣-藓类结皮的过程中,当年生红砂形态差异不显著,但5 a以上植株基部分枝长、树冠/侧冠投影面积、主根长均显著减小;同时,地衣-藓类结皮的3-5 a植株基部分枝数明显减少,且5 a以上植株明显矮化。（2）生物土壤结皮发育不仅降低了红砂幼株或成株生物量积累能力,还减小了植株根冠比,且降低/减小程度随结皮演替或株龄的增大逐渐增大。（3）红砂形态、生物量指标与物理或藻类结皮面积百分比呈极显著正相关关系,与藓类结皮面积百分比呈极显著的负相关关系。因此认为,生物土壤结皮的演替导致土壤关键生态因子（如土壤水分）发生变化,进而影响红砂植株生长发育能力,从而使得不同发育阶段结皮上的同龄红砂形态特征及生物量存在差异性。     

Using Soil Water Depletion to Measure Spatial Distribution of Root Activity in Oil Palm (Elaeis guineensis Jacq.) Plantations

Knowledge of where roots are active is crucial for efficient management of nutrients in tree crops but measurement of root activity is problematic. Measurement using soil water depletion is an approach that has not been tested in a humid climate. We hypothesised that the three dimensional distribution of root activity of a tree crop in the humid tropics (a) can be determined by measuring soil water depletion during rain-free periods, and (b) is influenced by environment (soil type and climate) and surface management. A field study was carried out in which soil water content was measured and water uptake calculated (by difference between soil water content at beginning and end of rain-free periods) for different surface management zones and depths (0.1 m intervals to 1.6 m depth) under oil palm (Elaeis guineensis Jacq.) at a loam–clay site and a sandy site. Significant differences were measured between sites and between surface management zones at each site. At both sites water uptake was highest under the weeded zone close to the palm stem, slightly lower under the zone where pruned fronds are placed, and lowest under the path used for removing harvested fruit. Vertical distribution of root activity differed between the sites, with higher activity near the surface at the finer textured site. Total water uptake values were lower than estimates of evapotranspiration made using climate data. The difference was probably largely due to water uptake from deeper than 1.6 m. This study showed that the spatial distribution of tree root activity in a humid climate could be quantified using a relatively simple method.     

亚热带不同树种土壤水源涵养功能

亚热带地区由于大面积的砍伐使天然林被人工林所代替,对森林土壤水源涵养功能造成了很大影响。树种可以通过自身特性来改变土壤物理结构进而影响土壤持水能力,因此合理选择树种对区域水源涵养具有重要意义。然而,立地条件的差异往往会对实验结果产生影响。为减少立地条件的差异,2012年2月在土壤发育和经营历史相同的林地上建立了中亚热带常见树种同质园。2019年8月测定了种植12个树种后不同土层(0—10、10—20、20—30、30—40 cm和40—50 cm)的土壤容重、含水量、总/毛管/非毛管孔隙度、最大/毛管/非毛管持水量和蓄水量。结果表明,种植不同树种7年后,土壤容重、含水量、总/毛管/非毛管孔隙度、最大/毛管/非毛管持水量和蓄水量均在表层(0—20 cm)土壤中差异显著,而在深层(20—50 cm)土壤中差异不显著。土壤孔隙度、持水量和蓄水量均与土壤容重呈显著负相关关系,而与土壤含水量呈显著正相关关系。与其他树种相比,种植鹅掌楸、枫香和全缘叶栾树等落叶阔叶树种可在较短时间内增加土壤孔隙度,提高土壤持水量和蓄水量。因此,在亚热带人工林经营管理中,可在杉木、马尾松纯林中适当引入鹅掌楸、枫香和全缘叶栾树等落叶阔叶树种,提升亚热带森林土壤水源涵养功能。     

Organic matter fraction and pools of phosphorus as indicators of the impact of land use in the Amazonian periphery

The unsustainable use of the soil of the deforested area at the Amazonian border is one of the greatest threats to the rainforest. Among the causes of land degradation in the humid tropics are phosphorus depletion (P), the decrease of soil organic matter (SOM) and the loss of basic cations. The aim of this study was determine the effects of different land uses on the dynamics of soil organic matter and phosphorus, to determine whether and how changes in the P and SOM can be used to assess the degree of land degradation in the humid tropics and whether the use of ecological systems can lessen or mitigate this degradation. Five systems were chosen according to potential use in the region: pasture of 30 years; no-tillage with 5 years of rice–maize rotations; no-tillage in alley cropping systems of 10 years; a newly cleared area; and 20 years of undisturbed secondary forest. Each field was sampled in a “W” pattern, to collect the soil samples from the chosen systems, prior to the chemical analyses. The SOM was separated by physical soil fractionation. The soil P fractionation was performed. All of the soil samples showed a very low pH range. The potential acidity was high under the alley cropping system, with more intensive and continuous use. All of the more labile fractions of organic matter decreased with the continuous use of soil in the alley cropping system. Therefore under alley cropping, most of the P (approximately 95%) was found in an inorganic form, and approximately 60% was found in the less labile fractions. The pasture and secondary forest showed higher contents of the labile fractions of organic matter and organic P. Higher correlations of organic P were found with the silt and clay fractions of organic matter. The results indicate that the fractions of P and organic matter are important indicators to assess changes in the degree of land degradation in the humid tropics. These results indicate also that the intensive and continuous use of annual crops in the soils of the humid tropics must be considered as posing a high risk to the sustainability of the agrosystems, mainly because of the increase of the active and potential acidity, the decrease of the labile organic matter and the depletion of the pools of organic P, leading to land degradation.     

Influence of rainfall amount and livestock grazing on soil respiration in a moist Kenyan savannah

The influence of livestock grazing and changing rainfall patterns on soil respiration (Rs) in the tropical savannah in Lambwe is unclear. Measurements of Rs using chambers were conducted between June and November 2012 in a humid savannah in Western Kenya to determine how simulated rainfall amounts and cattle grazing affected soil respiration. The experimental layout was split plot comprising rainfall simulations which were laid on grazed and fenced blocks, respectively. The rainfall simulations split plots each measured 6 m × 3 m and were covered with rainout gutters above the canopy of the herbaceous layer to either increase or reduce ambient rainfall by 50%. Grazing increased soil bulk density and significantly (p < 0.05) lowered soil respiration rates and soil water content irrespective of the rainfall treatment. The positive correlation between Rs and root biomass in both grazed and fenced plots revealed a significant contribution of root growth activities to Rs. Increased soil water content (SWC) by rainfall addition improved water penetration into deeper soil layers and therefore stimulated root and microbial activities which in turn built up soil respiration. Reduction in SWC by rainfall exclusion lowered microbial contact with the organic substrate and likely caused death and/ or inactivity of roots.     

Influence of humidity and water availability on the survival ofAmblyseius idaeus andA. anonymus (Acarina: Phytoseiidae)

Amblyseius idaeus (Denmark & Muma) andA. anonymus Chant & Baker are morphologically very similar species of phytoseiids inhabiting areas in South America that have very different levels of humidity. Above 60% RH, nearly all eggs of both species hatch successfully, but below 60% RH the egg hatching rate ofA. anonymus is very poor, whereas eggs ofA. idaeus hatch at humidities as low as 30% RH. The mobile stages ofA. idaeus are better able to survive in absence of food and water than those ofA. anonymus. Water availability promotes survival of both species, but its effect onA. idaeus exceeds that onA. anonymus. These differences in low-humidity tolerance and survival ability are consistent with the climatic origin of these phytoseiid species;Amblyseius ideaus has been reported from very dry and humid areas, andA. anonymus from humid areas only.In comparison with other phytoseiid species, the eggs ofA. idaeus have the highest tolerance to low humidities reported to date, and, among the phytoseiids that are shown to be capable of controllingTetranychus spp., this tolerance appears to be exceptionally high. The impact of this result on the scope of biological control ofTetranychus spp. is discussed.     

Paleogeography and historical phytogeography (paleochorology) in the Neophyticum

After presenting the methodological bases of historical phytogeography (paleochorology; Fig. 1), a new paleographic map series is introduced (Fig. 2). They serve for ten examples of paleochorological analyses, in which the major phases of the development of a group in space and time are documented. In addition to purely tropical taxa (Nypa, Ctenolophon), others which originated in the warm and humid N. Tethyan belt (Bombacaceae p.p.,Olacaceae p.p.,Symplocos, Alangium, Nepenthes) or which presently occur as eastern N. American/E. Asian disjuncts (Sarcococca andPachysandra) are discussed (Figs. 3–14). Finally, analyses of two very old angiosperm groups with complicated paleochorological patterns (Restionaceae andAscarina, Chloranthaceae p.p.; Figs. 15–16) are presented.Part I, to be followed by part II in this journal.     

Does salt stress constrain spatial distribution of dune building grasses Ammophila arenaria and Elytrichia juncea on the beach?

Rising sea levels threaten coastal safety by increasing the risk of flooding. Coastal dunes provide a natural form of coastal protection. Understanding drivers that constrain early development of dunes is necessary to assess whether dune development may keep pace with sea‐level rise. In this study, we explored to what extent salt stress experienced by dune building plant species constrains their spatial distribution at the Dutch sandy coast. We conducted a field transplantation experiment and a glasshouse experiment with two dune building grasses Ammophila arenaria and Elytrigia juncea. In the field, we measured salinity and monitored growth of transplanted grasses in four vegetation zones: (I) nonvegetated beach, (II) E. juncea occurring, (III) both species co‐occurring, and (IV) A. arenaria dominant. In the glasshouse, we subjected the two species to six soil salinity treatments, with and without salt spray. We monitored biomass, photosynthesis, leaf sodium, and nutrient concentrations over a growing season. The vegetation zones were weakly associated with summer soil salinity; zone I and II were significantly more saline than zones III and IV. Ammophila arenaria performed equally (zone II) or better (zones III, IV) than E. juncea, suggesting soil salinity did not limit species performance. Both species showed severe winter mortality. In the glasshouse, A. arenaria biomass decreased linearly with soil salinity, presumably as a result of osmotic stress. Elytrigia juncea showed a nonlinear response to soil salinity with an optimum at 0.75% soil salinity. Our findings suggest that soil salinity stress either takes place in winter, or that development of vegetated dunes is less sensitive to soil salinity than hitherto expected.     

Climate,duration, and N placement determine N2O emissions in reduced tillage systems: a meta‐analysis

No‐tillage and reduced tillage (NT/RT) management practices are being promoted in agroecosystems to reduce erosion, sequester additional soil C and reduce production costs. The impact of NT/RT on N₂O emissions, however, has been variable with both increases and decreases in emissions reported. Herein, we quantitatively synthesize studies on the short‐ and long‐term impact of NT/RT on N₂O emissions in humid and dry climatic zones with emissions expressed on both an area‐ and crop yield‐scaled basis. A meta‐analysis was conducted on 239 direct comparisons between conventional tillage (CT) and NT/RT. In contrast to earlier studies, averaged across all comparisons, NT/RT did not alter N₂O emissions compared with CT. However, NT/RT significantly reduced N₂O emissions in experiments >10 years, especially in dry climates. No significant correlation was found between soil texture and the effect of NT/RT on N₂O emissions. When fertilizer‐N was placed at ≥5 cm depth, NT/RT significantly reduced area‐scaled N₂O emissions, in particular under humid climatic conditions. Compared to CT under dry climatic conditions, yield‐scaled N₂O increased significantly (57%) when NT/RT was implemented <10 years, but decreased significantly (27%) after ≥10 years of NT/RT. There was a significant decrease in yield‐scaled N₂O emissions in humid climates when fertilizer‐N was placed at ≥5 cm depth. Therefore, in humid climates, deep placement of fertilizer‐N is recommended when implementing NT/RT. In addition, NT/RT practices need to be sustained for a prolonged time, particularly in dry climates, to become an effective mitigation strategy for reducing N₂O emissions.