中晚全新世泰国湾Chanthaburi海岸Welu河口区沉积物的敏感粒级组分及其对季风气候变化的指示意义

对泰国湾Chanthaburi海岸Welu河口区三根沉积物柱样(WLE08、WLE10和WLE12)进行了210Pb测年分析、AMS14C测年分析和粒度分析.粒度分析结果表明,研究区三根柱样的沉积物类型均属于粘土质粉砂,包含部分贝壳及生物碎屑,分选差,呈正偏态,属于中晚全新世以来形成的沉积物.通过粒级-标准偏差方法对沉...     

Bridging information domains to improve ecological understanding of biological invasions in a marine ecosystem

We devised a practical method for integrating information on 2 marine invasive species using 3 different approaches: standardized ecological monitoring, online-reporting databases, and surveys of anglers and crabbers. Focusing on 2 recently introduced species with different characteristics, the Asian shore crab (Hemigrapsus sanguineus) and Chinese mitten crab (Eriocheir sinensis), in the Hudson-Raritan watershed of New York and New Jersey, we used sensitivity analyses to explore the relative contribution of each information source to knowledge of species abundance and distribution. All 3 information sources contributed something unique to understanding abundance and distribution of the introduced crabs. Online and survey data on Asian shore crabs significantly affected predictions of abundance, whereas monitoring data did not. When survey data were omitted, abundance estimates were unchanged over time, but when they were included, the model predicted an increased abundance in 2012. All 3 data sets for the Asian shore crab significantly affected estimates of species coverage; surveys had the biggest influence, increasing range size by 4097.25 km². For the catadromous Chinese mitten crab, ecological monitoring data collected in freshwater shortly after the original sighting significantly shaped model estimates for abundance and documented the establishment phase of the mitten crab in an area outside the spatial scope of the surveyed resource users. However, the survey data significantly enlarged mitten crab range-size estimates by 6498.01 km². By demonstrating that data integration produced an image of the invasion process that would not have emerged had we used any 1 method individually, model results provide evidence for the advantages of an interdisciplinary approach.     

Agroecology in the tropics: Achieving a balance between land use and preservation

Agroecology is the application of ecological concepts and principles to the design and management of sustainable agricultural systems. An agroecological approach to agriculture has special importance in the humid tropics where agricultural development and the preservation of tropical forests are most often in direct conflict. It is proposed that a more sustainable approach to development is needed, where agroecosystems depend on low external inputs, function more on the use of locally available and renewable resources, have benign impacts on the environment, and are based on the knowledge and culture of the local inhabitants. Examples of traditional agroecosystem management in Mesoamerica that can provide this basis are presented. The preservation of both biological and cultural diversity are integral to the long-term sustainable management of natural resources in the tropics.     

2010年亚运会对广州市可持续发展的影响

2010年举办的第16届亚运会将是广州有史以来承办的最大型的综合性体育赛事。分析了亚运会的举办将对广州市经济、社会发展、城市与环境建设等方面的影响,并提出了全面贯彻可持续发展思想,进一步办好亚运会的建议:立足长远,社会效益与经济效益并重;加大生态环境建设力度;加大宣传力度,推动公众参与;加强区域合作,协调区域发展。     

Geophagy in the tropics: an appraisal of three geophagical materials

Geophagy, the deliberate consumption of soil, is a common practice amongst the world's poorer or more tribally oriented people of the tropics. An appraisal of three geophagical samples suggests that Fe is a mineral nutrient which can be supplied to humans in significant amounts via ingested soil. Geophagy provides a direct link between the geochemistry of soils and human health, but as yet this association has only a limited awareness amongst research workers.     

青藏高原隆升对我国西南地区气候的影响——从季风角度研究

青藏高原隆升作为新生代最重要的地质事件,对亚洲乃至全球气候演化产生了深刻的影响。我国西南地区因紧邻青藏高原、地形地貌复杂,该区青藏高原隆升的气候效应至今仍存在许多需要探讨的问题。本文通过整理总结青藏高原隆升与亚洲季风各子系统形成与发展的相关性,从季风的角度分析了高原隆升对西南地区气候的影响。主要结论如下：（1）对西南地区气候起控制性作用的东亚季风、南亚季风以及高原季风的形成与青藏高原的隆升密切相关。虽然东亚夏季偏南风在约22 Ma就因海陆差异形成,但冬季风却是在约7.2 Ma因青藏高原隆升才出现;南亚夏季风（西南季风）约在12 Ma因喜马拉雅山脉及临近山脉形成而出现,而其冬季风形成时间及原因与东亚冬季风相似,同样离不开青藏高原的隆升;高原季风形成的直接因素就是高原隆升,其约在36 Ma青藏高原主体隆升至约1500 m时才开始形成。（2）亚洲季风各子系统对西南地区的气候演变有重要影响。尽管东亚冬季风不能直接影响西南地区,但青藏高原隆升增强了海陆差异及其热源作用,在一定程度上扩大了东亚夏季风的影响范围,并给西南地区带来水汽;南亚冬季风使得西南地区变得相对寒冷干燥,而南亚夏季风因青藏高原的隆升得到进一步加强,其通过形成南北向的水汽通道成为西南地区温暖湿润气候的主导者;高原冬、夏季风随着青藏高原隆升使得西南地区季节性干冷与湿润气候的差异更加显著。     

Effects of Asian dust events on atmospheric bacterial communities at different distances downwind of the source region

Aeolian dust particles arising from arid and semiarid zones are known to carry microbes by air currents. The effect of wind-borne bacteria on atmospheric bacterial population at various downwind distances from the dust source regions must be clarified, but has not yet been reported. This study monitored the bacterial abundance and community composition in outdoor aerosol samples in Beijing, China, which is close to the Asian dust source regions, and compared them with the results obtained in a distant region(Osaka, Japan).The Asian dust collected in Beijing contained(4 ± 3) × 10~4 bacterial cells/m~3, approximately~4 times higher than in Osaka. On 15 April 2015, Beijing experienced severe Asian dust events with a 1000-fold increase in bacterial abundance, relative to non-Asian dust days. Dominant bacterial phyla and classes in Asian dust collected in Beijing were Actinobacteria, Bacilli and Acidobacteria, and the bacterial community composition varied more widely than in Osaka.The bacterial community compositions differed between the Beijing and Osaka dusts, even for the same Asian dust events. These results indicated that aerosol bacterial communities nearer the dust source are more affected by eolian dust than their distant counterparts.     

亚青会期间南京大气PM_(2.5)中重金属来源及风险

为探究亚青会期间南京奥体中心附近大气PM2.5中重金属来源及潜在的健康风险,于2013年8月3~28日对PM2.5中重金属元素V、Cr、Mn、Fe、Co、Ni、Cu、Zn、As、Cd、Sn、Sb和Pb进行了观测分析.结果表明:受亚青会污染源调控和气象要素影响,亚青会前、中、后不同时期重金属浓度存在差异,亚青会期间各重金属的浓度均值低于亚青会前期.富集因子分析显示Cu、Zn、Cd、Sn、Sb和Pb为重度富集元素,污染程度为CdCuZnPbSbSn.聚类分析表明工业排放、燃煤、道路尘和机动车尾气排放是这些重金属的主要来源.亚青会期间,PM2.5中各重金属通过呼吸途径对运动员造成的非致癌风险均小于1,5种致癌重金属的风险指数均低于致癌风险阈值范围.     

Incorporating uncertainty in a chemical leaching assessment

Pesticide leaching models are being used to assist in the regulation and management of pesticides by indicating their potential for leaching to groundwater. Uncertainty in model input data is not, regrettably, included in most pesticide leaching assessments. In the work described here, we use logarithmic transformations of the attenuation factor (AF), a simple process-based index model, to represent uncertainty in a pesticide leaching assessment. Characterization of a wide range of pesticides as `leachers' or `non-leachers' for a specific Hawaii hydrogeological setting is facilitated by comparing the log-transformed AF, designated AFR, for each chemical with two reference chemicals for which leaching behavior in Hawaii is known. Defining a mean and uncertainty interval for the AFR index of each chemical being ranked provides a practical method of incorporating data uncertainty into a regulatory protocol.     

Dry deposition of PM10 over the Yellow Sea during Asian dust events from 2001 to 2007

Dry deposition velocities and fluxes of PM10during Asian dust events over the Yellow Sea from 2001 to 2007 were investigated using observation data in Qingdao, China and Jeju, Korea. The dry deposition velocities of PM10 during dust events over the Yellow Sea ranged from 0.19 to 8.17 cm/sec, with an average of 3.38 cm/sec. Dry deposition fluxes of PM10during dust events over the Yellow Sea were in the range of 68.5–2647.1 mg/(m2·day), with an average of 545.4 mg/(m2·day), which is 2–10 times higher than those reported by other studies for both dust and non-dust periods. It was estimated that 2.6 × 1011–48.7 × 1011g dust particles deposit to the Yellow Sea during dust events through dry deposition every year. Compared with the results in previous studies, it was found that the dry deposition of PM10over the Yellow Sea during dust events in the years with high frequency of dust could account for a large or overwhelming fraction of the annual total dry deposition. Backward air mass trajectory analysis showed that dust events influenced Jeju mainly originated from the desert regions located in Mongolia and Inner Mongolia, China. There were 119 backward trajectories influenced both Qingdao and Jeju during 15 dust events from 2001 to 2007, accounting for 61.3% of the total trajectories of 194, indicating that Qingdao and Jeju were usually on the same pathway of dust transport downwind from source areas.