Carbon isotopic record of terrestrial ecosystems spanning the Late Miocene extinction of Oreopithecus bambolii, Baccinello Basin (Tuscany, Italy)

Oreopithecus bambolii is a Late Miocene hominoid with an extensive fossil record in the Baccinello Basin (Tuscany, Italy), and was the only western European hominoid to survive a major extinction event ca. 9.6 Ma (millions of years ago). Oreopithecus lived in the insular Tusco-Sardinian paleobioprovince, where it evolved many unique anatomical specializations that make it important for understanding the mechanisms and history of Late Miocene hominoid evolution. The eventual extinction of Oreopithecus and its associated fauna ca. 6.5 Ma has generally been attributed to interaction with species that arrived from continental Europe following tectonic collision of the Tusco-Sardinian province with mainland Italy, but palynological, paleontological, and sedimentological records indicate an environmental shift toward more variable climate across the extinction event.To explore the possibility of environmental change as a contributing factor in the extinction of Oreopithecus, we developed a stable carbon and oxygen isotope record from organic matter in paleosols from the Baccinello Basin. These data show very low temporal and spatial variability (indicating plant ecosystem stability through time and space) and provide no evidence for ecologically significant changes in floral composition spanning the extinction event, suggesting that environmental change was not an underlying cause for the extinction of Oreopithecus and its associated fauna. The carbon isotope values fall entirely within the range of isotopic variability for modern plants following the C₃ photosynthetic pathway (trees, shrubs, cool-season grasses), indicating that C₄ vegetation (warm-season grasses) was not an important component of biomass. When corrected for temporal variation in the carbon isotopic composition of atmospheric carbon dioxide, the paleosol carbon isotope values are consistent with predicted values based on modern plants and the Baccinello palynoflora, supporting the reliability of paleosol isotopic records as paleoecological proxies.     

大比例尺土壤保持服务制图分级方法研究

科学地编制生态系统服务空间分布图,有助于识别生态系统优先保护热点及空缺,能够为国土安全规划提供基础信息。但由于缺乏统一科学的生态系统服务分级方法,生态系统服务分布图的展示效果和制图效率都受到限制。不恰当的分级制图会误导决策者对生态系统服务空间分布特征的判断,增加生态保护决策的不确定性。以构建生态服务制图分级标准为目标,对我国6个典型县区的土壤保持服务数据展开1：25万比例尺制图分级案例研究。采用分级精度、面积均衡性、极差一致性、空间自相关一致性4个分级质量评价指标评价并比较了目前地图编制中常用的自然断点法、几何间隔法、累积比例法、等差法、分位数法5种分级算法的分级制图效果。结果表明,6个县区有相似的土壤保持服务分布特征：低值区覆盖面积大,高值区覆盖面积小。各县区土壤保持服务制图最优分级方法有差异：延庆区、丰满区最优分级方法为自然断点法;永靖县、天山区、安宁市最优分级方法为累积比例法;富阳区最优分级方法为几何间隔法。各分级方法中,累积比例法在6个县区综合制图效果最优或接近最优,适用性最好,能够较好的刻画各县区的土壤保持服务空间分布特征。本文提出的分级评价方法及其结果,可为生态系统土壤保持服务制图规范化和自动化提供科学依据。     

Multiple Scales of Temporal Variability in Ecosystem Metabolism Rates: Results from 2 Years of Continuous Monitoring in a Forested Headwater Stream

Headwater streams are key sites of nutrient and organic matter processing and retention, but little is known about temporal variability in gross primary production (GPP) and ecosystem respiration (ER) rates as a result of the short duration of most metabolism measurements in lotic ecosystems. We examined temporal variability and controls on ecosystem metabolism by measuring daily rates continuously for 2 years in Walker Branch, a first-order deciduous forest stream. Four important scales of temporal variability in ecosystem metabolism rates were identified: (1) seasonal, (2) day-to-day, (3) episodic (storm-related), and (4) inter-annual. Seasonal patterns were largely controlled by the leaf phenology and productivity of the deciduous riparian forest. Walker Branch was strongly net heterotrophic throughout the year with the exception of the open-canopy spring when GPP and ER rates were co-equal. Day-to-day variability in weather conditions influenced light reaching the streambed, resulting in high day-to-day variability in GPP particularly during spring (daily light levels explained 84% of the variance in daily GPP in April). Episodic storms depressed GPP for several days in spring, but increased GPP in autumn by removing leaves shading the streambed. Storms depressed ER initially, but then stimulated ER to 2–3 times pre-storm levels for several days. Walker Branch was strongly net heterotrophic in both years of the study, with annual GPP being similar (488 and 519 g O₂ m⁻² y⁻¹ or 183 and 195 g C m⁻² y⁻¹) but annual ER being higher in 2004 than 2005 (−1,645 vs. −1,292 g O₂ m⁻² y⁻¹ or −617 and −485 g C m⁻² y⁻¹). Inter-annual variability in ecosystem metabolism (assessed by comparing 2004 and 2005 rates with previous measurements) was the result of the storm frequency and timing and the size of the spring macroalgal bloom. Changes in local climate can have substantial impacts on stream ecosystem metabolism rates and ultimately influence the carbon source and sink properties of these important ecosystems.     

京津唐城市生态系统能值比较

运用能值(emergy)分析方法,以京津冀地区的北京、天津、唐山为研究对象,建立了复合生态系统与可持续发展的能值指标,对3个城市1991～2005年自然环境与社会经济可持续发展状况进行了比较分析.研究结果表明:1991～2005年期间,由于北京、天津的本地资源能值对经济发展的驱动力不足,城市发展对外部输入能值的依赖程度越来越高;北京、天津、唐山社会子系统的能值指标均呈上升趋势,城市居民生活水平和经济发展水平不断提高;北京经济子系统的各项指标均优于天津和唐山,但环境子系统和能值可持续指标体现出,北京的环境压力最大、可持续发展能力低于天津和唐山.在此分析基础上,对北京、天津、唐山的可持续发展提出了几点建议,为制定城市发展策略和产业调整提供科学依据.     

森林生态系统土壤CO2释放随海拔梯度的变化及其影响因子

联合国气候框架公约的签署提升了人们对全球变暖、碳循环的关注。土壤CO₂释放作为土壤-大气CO₂交换的主要途径之一,成为了各国生态学家研究的重点内容。通过对1800~2155m海拔梯度上森林生态系统土壤CO₂释放进行研究,揭示了较小空间尺度上土壤CO₂释放的变化规律及其控制机制。在研究区域内,随着海拔梯度的增加,森林土壤CO₂释放由(1.94±006) μmol m^-2 s^-1逐渐增加至(2.22±0.07) μ mol m^-2 s^-1。土壤温度、土壤水分、土壤有机碳（SOC）、全N、全P与土壤CO₂释放呈显著正相关（n=14, P<0.05）;土壤容重与土壤CO₂释放速率呈显著负相关（n=14,P<0.05）;土壤pH对土壤CO₂释放影响不显著。作为一个复杂的生态学过程,环境因子及其交互作用对土壤CO₂释放产生影响,为了减少因子共线性影响,逐步降低因子维数,采用主成分分析（PCA）揭示了土壤温度、土壤水分、SOC、全N、全P、容重6个因子的联合作用,其累积贡献率达到了57％以上;进一步运用逐步回归分析方法,探讨了影响土壤CO₂释放沿海拔梯度分布的主导因子,结果表明土壤水分是研究区域森林生态系统土壤CO₂释放沿海拔梯度变化的主导因子。     

Aquo-pentamine Co(III) complexes as models for carbonic anhydrase

The hydrolysis of 4-nitrophenyl acetate by metal complexes Co(en)2(imH)H2O3+, Co(en)2(bzmH)H2O3+, and Co(en)2(imCH3)H2O3+ (imH = imidazole, bzmH = benzimodazole, imCH3 = methyl imidazole) has been investigated in the pH range 5.4-8.9. The small difference in nucleophilic reactivity in the pH range 5.4-6.7 is assumed to be due to hydrogen bonding abilities of the imidazole and substituted imidazole ligands and small pKa differences (k2(imH) = 2.2 X 10(-2) M-1 sec-1, k2(bzmH) = 5.68 X 10(-2) M-1 sec-1, k2(imCH3) = 1.35 X 10(-2) M-1 sec-1, 40 degrees C, 1 = 0.3 NaClO4, pKa(imH) = 6.2, pKa(imCH3) = 6.2 and pKa(bzmH) = 5.9). In the pH range 7.8-8.9, the differences in nucleophilic reactivity (k3(imH) = 85.5 X 10(-2) M-1 sec-1, k3(bzmH) = 33.4 X 10(-2) M-1 sec-1, 40 degrees C, I = 0.3 NaClO4) are reconciled with a significant steric factor outweighing the acidity of the benzimidazole complex. In the pH region 6.7-7.7, the deviation from linearity is presumably due to both hydroxo and imido ligands functioning as nucleophiles, the latter being about 40 times stronger than the former.     

Nitrogen vs. phosphorus limitation across an ecotonal gradient in a mangrove forest

Mangrove forests are characterized by distinctive tree-height gradientsthat reflect complex spatial, within-stand differences in environmentalfactors,including nutrient dynamics, salinity, and tidal inundation, across narrowgradients. To determine patterns of nutrient limitation and the effects ofnutrient availability on plant growth and within-stand nutrient dynamics, weused a factorial experiment with three nutrient treatment levels (control, N,P)and three zones along a tree-height gradient (fringe, transition, dwarf) onoffshore islands in Belize. Transects were laid out perpendicular to theshoreline across a mangrove forest from a fringe stand along the seaward edge,through a stand of intermediate height, into a dwarf stand in the interior ofthe island. At three sites, three trees were fertilized per zone for 2yr. Although there was spatial variability in response, growth byR. mangle was generally nitrogen (N) -limited in thefringe zone;phosphorus (P) -limited in the dwarf zone; and, N- and/or P-limited in thetransition zone. Phosphorus-resorption efficiency decreased in all three zones,and N-resorption efficiency increased in the dwarf zone in response to Penrichment. The addition of N had no effect on either P or N resorptionefficiencies. Belowground decomposition was increased by P enrichment in allzones, whereas N enrichment had no effect. This study demonstrated thatessential nutrients are not uniformly distributed within mangrove ecosystems;that soil fertility can switch from conditions of N to P limitation acrossnarrow ecotonal gradients; and, that not all ecological processes respondsimilarly to, or are limited by, the same nutrient.     

IPBES的建立、前景及应对策略

生物多样性和生态系统服务政府间科学-政策平台(IPBES)是一个类似于气候变化专门委员会(IPCC)的独立的政府间机构,其目标是建立科学界和决策者之间的沟通平台,推动全球生物多样性和生态系统服务的保护.从2008年11月到2010年6月,联合国环境规划署(UNEP)主持召开了三次政府间谈判会议.在最后一次会议上各国同意建立IPBES,并形成了一份《釜山成果》文件,确定其基本职能主要是开展评估,还确定IPBES的决策机构是全体会议,向联合国所有会员国和区域经济一体化组织开放,政府间组织和其他利益相关方可作为观察员.IPBES的建立将会在国际社会产生深刻的影响,但其未来走向也有一定的不确定性:一是如何保持科学独立性的问题,二是评估尺度可能会影响其成功,三是能否促进发展中国家的广泛参与.为使我国能在IPBES中发挥重要作用,建议今后应加强对IPBES运作模式的研究,加强评估工具和方法的开发以及加强生物多样性的监测.     

城市生态系统中AM真菌侵染与群落结构特征

丛枝菌根(AM)真菌作为土壤微生物的重要成员之一,对城市生态系统可持续发展具有重要意义.本文系统总结了城市生态系统中AM真菌着生状况和群落结构特点,探讨了城市生态因子,如人类行为、植被重建与维护、城市土壤状况等对AM真菌着生状况和群落结构的影响,认为今后应加强城市生态系统中AM真菌群落结构与功能的研究,如关键城市生态因子(如水资源匮乏、热岛效应等)改变AM真菌群落结构的效应与机制.     

Dispersal frequency affects local biomass production by controlling local diversity

Dispersal is a major factor regulating the number of coexisting species, but the relationship between species diversity and ecosystem processes has mainly been analysed for communities closed to dispersal. We experimentally investigated how initial local diversity and dispersal frequency affect local diversity and biomass production in open benthic microalgal metacommunities. Final local species richness and local biomass production were strongly influenced by dispersal frequency but not by initial local diversity. Both final local richness and final local biomass showed a hump-shaped pattern with increasing dispersal frequency, with a maximum at intermediate dispersal frequencies. Consequently, final local biomass increased linearly with increasing final richness. We conclude that the general relationship between richness and ecosystem functioning remains valid in open systems, but the maintenance of ecosystem processes significantly depends on the effects of dispersal on species richness and local interactions.