石羊河下游盐渍化弃耕地植被演替与土壤养分相关性分析

以石羊河下游不同年代盐渍化弃耕地自然群落为对象,利用优势种群的消长和土壤养分的动态变化进行相关性分析,研究退耕地群落演替与土壤养分之间的动态变化以及相互关系。结果表明:1)植被类型一般经历3个阶段:田间杂草→荒漠草本→荒漠灌木,但群落演替可分为4个阶段:藜+田旋花群落(1～2年)→骆驼蒿群落(3～10年)→苏枸杞+黄毛头群落(10～40年)→黄毛头群落(顶极群落);2)土壤养分在整个植被演替过程中一般经历消耗-积累-消耗3个阶段,但速效钾不存在初期消耗阶段,演替后期土壤养分处于消耗状态,并逐渐接近本区域自然植被土壤养分;3)由于前期土壤养分处于消耗阶段,骆驼蒿种群对土壤养分的贡献不明显,其中与速效磷之间呈显著负相关,与速效钾呈显著正相关;苏枸杞种群与土壤养分呈正相关,其中与有机质、全氮、30～60cm速效钾相关性显著;而黄毛头种群与土壤养分之间呈显著负相关。黄毛头具有较强的适应性,可作为盐渍化弃耕地上的适宜引种物种,以调控和加速植物群落演替。     

Foliar nutrient dynamics in tidal and non-tidal freshwater forested wetlands

Foliar nutrient dynamics were studied at 8 forest stands (three non-tidal and five tidal) along the lower 30 km of the Apalachicola River system in Florida, USA, during 2008. At each site, we sampled canopy foliage and litterfall from three to four trees representative of the dominant overstory species. Foliage and litterfall were analyzed for a variety of elements including N and P and these data were used to examine differences in element concentrations, nutrient ratios (C:P, C:N, and N:P), nutrient use efficiency, and nutrient proficiency. Measurements of tree diameter at basal height (DBH) at each plot were used with species allometric equations to estimate forest litterfall dry weight and N and P flux in non-tidal and tidal wetlands. Both non-tidal and tidal wetlands showed evidence of P limitation based on N:P ratios, but absolute levels of P were determined to be extremely low in tidal wetlands based on higher nutrient use efficiencies (measures of both P resorption efficiency and proficiency). Differences in P concentrations and fluxes between tidal and non-tidal wetlands are probably related to longer inundation and hydrologic export observed in tidal wetlands. Using estimations of annual litterfall dry weight and nutrient concentrations, N and P flux in non-tidal swamps were 2-4 times greater than in tidal wetlands. This study demonstrates the change in nutrient dynamics as wetlands shift from tidal to non-tidal conditions.     

Effect of great-horned owl trapping on chick survival in piping plovers

We studied the effect of great-horned owl (Bubo virginianus) removal on piping plover (Charadrius melodus) hatchling survival on Missouri River sandbars (2008–2009). Owl removal increased daily survival of piping plover chicks in 2008 (β = 2.03, 95% CI: 0.04–4.02), but this effect decreased with increasing age of the chick (β = −0.42, 95% CI: −0.81 to −0.03). Results for 2009 were similar in direction but not significant. Survival was higher in 2008 than in 2009, regardless of owl capture, indicating that even if owl capture consistently were effective at increasing survival, overall survival resulting from trapping may vary annually. Owl trapping was a successful means to raise chick survival on the Missouri River in ≥1 year and could be used at other sites experiencing depressed chick survival due to avian predators. © 2011 The Wildlife Society.     

Simulating the rice yield change in the middle and lower reaches of the Yangtze River under SRES B2 scenario

As one of the most important crops in China, rice accounts for 18% of the country’s total cultivated area. Increasing atmospheric CO₂ concentration and associated climate change may greatly affect the rice productivity. Therefore, understanding the impacts of climate change on rice production is of great significance. This paper aims to examine the potential impacts of future climate change on the rice yield in the middle and lower reaches of the Yangtze River, which is one of the most important food production regions in China. Climate data generated by the regional climate Model PRECIS for the baseline (1961–1990) and future (2021–2050) period under IPCC SRES B2 scenario were employed as the input of the rice crop model ORYZA2000. Four experimental schemes were carried out to evaluate the effects of future climate warming, CO₂ fertilization and water managements (i.e., irrigation and rain-fed) on rice production. The results indicated that the average rice growth duration would be shortened by 4 days and the average rice yield would be declined by more than 14% as mean temperature raised by 1.5 °C during the rice growing season in 2021–2050 period under B2 scenario. This negative effect of climate warming was more obvious on the middle and late rice than early rice, since both of them experience higher mean temperature and more extreme high temperature events in the growth period from July to September. The significance effect of the enhanced CO₂ fertilization to rice yield was found under elevated CO₂ concentrations in 2021–2050 period under B2 scenario, which would increase rice yield by more than 10%, but it was still not enough to offset the negative effect of increasing temperature. As an important limiting factor to rice yield, precipitation contributed less to the variation of rice yield than either increased temperature or CO₂ fertilization, while the spatial distribution of rice yield depended on the temporal and spatial patterns of precipitation and temperature. Compared to the rain-fed rice, the irrigated rice generally had higher rice yield over the study area, since the irrigated rice was less affected by climate change. Irrigation could increase the rice yield by more than 50% over the region north of the Yangtze River, with less contribution to the south, since irrigation can relieve the water stress for rice growing in the north region of the study area. The results above indicated that future climate change would significantly affect the rice production in the middle and lower reaches of the Yangtze River. Therefore, the adverse effect of future climate change on rice production will be reduced by taking adaptation measures to avoid disadvantages. However, there is uncertainty in the rice production response prediction due to the rice acclimation to climate change and bias in the simulation of rice yield with uncertainty of parameters accompanied with the uncertainty of future climate change scenario.     

Activity budget of inshore Indo‐Pacific bottlenose dolphins (Tursiops aduncus): A critical evaluation of methods and comparison among other populations

Activity budgets are widely used to compare behavior patterns but sampling methods vary, rendering comparisons difficult. The two main methods used are instantaneous and continuous sampling. Their comparability was examined by applying them to data obtained from bottlenose dolphins in the Port River estuary, South Australia. They gave comparable results for activity budgets, but instantaneous sampling did not detect most of the behavioral events. Individual differences in behavior and/or follow duration influenced results. Variability in activity definitions and categories among studies makes comparative analysis difficult. Comparison of the Port River dolphin's activity budget with other inshore populations indicated the former spent more time feeding and resting, and less time traveling. The greater feeding time seemed to be due to small prey size rather than reduced abundance or unpredictable distribution. The reduced traveling time, possibly the result of low predation pressure and/or evenly distributed prey, gave them more time to rest. They traveled mostly at 2.5 kn or less, consistent with studies from other shallow areas. Most feeding was individual, probably on demersal species. Surface feeding incorporated physical barriers rather than cooperative behavior. Activity durations ranged from 2 s to 2.9 h, with mean durations varying from 7.8 to 22.9 min.     

1967—2006年太子河流域径流系数的变化特征

利用太子河流域6个主要支流（海城河、南沙河、北沙河、兰河、细河、太子河南支）1967—2006年日均降水和径流资料,分析了各支流径流系数的变化趋势及其与降水的关系.结果表明：1967—2006年,位于高山丘陵区的太子河南支的年均径流系数较大,而人类活动影响较多的海城河流域的年均径流系数较小;除南沙河的年径流系数总体呈上升趋势外,其余各条支流的年径流系数均呈下降趋势,以南支和兰河的下降趋势尤为明显;除细河流域的年径流系数没有发生突变外,其余各条支流的年径流系数都发生了突变,且突变出现的年份各不相同;年降水量对年径流系数的影响极显著.     

海河流域生态功能区划

从海河流域自身的特征出发,运用RS、GIS技术,采用定性和定量分析相结合的方法,对海河流域生态功能区进行划分.结果表明:海河流域可划分为5个生态区、24个生态亚区和114个生态功能区;以流域尺度上占主导地位的4项生态功能(水源涵养、水土保持、防风固沙和生物多样性保护)为依据,确定了对海河流域具有重要意义的11个重要生态功能区域.该区划结果明确了对海河流域生态安全具有重要意义的区域,可用于指导海河流域自然资源的有序开发利用和产业的合理布局,为海河流域生态环境保护提供了科学依据,对维护海河流域生态安全具有重要意义.     

Postfire energy exchange in arctic tundra: the importance and climatic implications of burn severity

Fires produce land cover changes that have consequences for surface energy balance and temperature. Three eddy covariance towers were setup along a burn severity gradient (i.e. Severely, Moderately, and Unburned tundra) to determine the effect of fire and burn severity on arctic tundra surface energy exchange and temperature for three growing seasons (2008–2010) following the 2007 Anaktuvuk River fire. The three sites were well matched before the fire, experienced similar weather, and had similar energy budget closure, indicating that the measured energy exchange differences between sites were largely attributable to burn severity. Increased burn severity resulted in decreased vegetation and moss cover, organic layer depth, and the rate of postfire vegetation recovery. Albedo and surface greenness steadily recovered with Moderately matching Unburned tundra by the third growing season. Decreased albedo increased net radiation and partly fueled increased latent and ground heat fluxes, soil temperatures, and thaw depth. Decreases in moss cover and the organic layer also influenced the ground thermal regime and increased latent heat fluxes. These changes either offset or decreased the surface warming effect from decreased albedo, resulting in a small surface warming in Severely and a small surface cooling in Moderately relative to Unburned tundra. These results indicate that fires have a significant impact on surface energy balance and highlight the importance of moss and permafrost thaw in regulating arctic surface energy exchange and temperature.     

珠江口城市段近岸表层水体浮游细菌分离方法比较

为了更好地分离珠江口未/难培养的浮游细菌,本研究以珠江河口三个样点的水体为研究对象,同时采用了纯培养和免培养的方法,对不同培养基的分离效果进行了探索。在纯培养实验中,本研究选择了7种不同的分离培养基,共分离获得153株菌;同时,将扩增子分析结果作为分离效果的参考,所有环境样品中共包含3 553个操作分类单元（operational taxonomic units,OTUs）。对三个样点微生物类群的多样性进行比较,纯培养结果显示珠江口下游珠海样点多样性最高,其次为中大和虎门样点;免培养则显示虎门样点多样性最高;对比7种不同的分离培养基,Z7（R₂A）培养基的分离效果最好,分离菌株数和分离类群的α多样性最高,Z1（改良ISP 2）次之;主坐标分析结合韦恩图的结果表明相比其余的培养基,Z1和Z7培养基分离获得的菌群兼具普遍性和特异性,进一步证明了这两种培养基的分离效果较佳;冗余分析结果表明K₂HPO₄、酵母粉、可溶性淀粉、MgSO₄·7H₂O、麦芽膏和葡萄糖与特定类群的分离有相关关系,其中K₂HPO₄的影响最为显著（P<0.05）。本文通过7种不同培养基对河口微生物分离效果的探究,有助于我们在研究未知微生物的营养特性时,选择成分和组成更合理的培养基来提升河口微生物纯培养的分离效率。     

汉江中下游浮游植物群落结构及水质评价

南水北调中线工程调水后,汉江中下游水华频发引起社会关注。为掌握调水后汉江中下游浮游植物的群落结构特征,于2017年11月、2018年2月、4月和8月在汉江中下游的8个断面对浮游植物进行了定量调查。调查结果显示:共鉴定浮游植物163种,群落组成以硅藻门(Bacillariophyta)、绿藻门(Chlorophyta)为主,其次是蓝藻门(Cyanophyta)。浮游植物优势种主要为硅藻门的梅尼小环藻(Cyclotella meneghiniana)、颗粒直链藻最窄变种(Melosira granulata var.)、变异直链藻(Melosira varians)、颗粒直链藻(Melosira granulata),隐藻门的卵形隐藻(Cryptomonas ovata),蓝藻门的弯曲颤藻(Oscillatoria sp.)和伪鱼腥藻(Pseudoanabaena sp.),且都有较高的优势度。浮游植物密度和生物量的季节变化范围分别为0. 33×106cells/L～1. 82×106cells/L和0. 49 mg/L～7. 38 mg/L。基于Shannon-Weaver多样性指数和Pielou均匀度指数以及优势种评价法对汉江中下游的水质进行评价,判断汉江中下游水质整体处于中污状态。