南中国海地区红树林的利用和保护

南中国海具有丰富的浅海和热带的生物多样性,是全球红树林分布的中心之一.南中国海地区红树林面积大约占全球的28%,该区红树植物的多样性为世界最高,共有46种真红树分布于此.由于受人口增加和经济发展的巨大压力,南中国地区红树林资源破坏严重,退化趋势明显.虽然南中国海周边国家过去都实施了相应的海洋环境保护行动计划,然而缺乏区域协调措施大大降低了这些行动的有效性.本文在对南中国海地区红树林资源的利用现状和退化原因进行分析的基础上,提出南中国海地区红树林资源保护与管理的建议,以期能在双边或区域的层面上共同协作,采取适当的措施去扭转南中国海地区红树林生境退化趋势.     

Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence

Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon （SOC） of paddy soils of China under warming. SOC mineralization of three major types of China＇s paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C： very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied.     

A method to estimate pre-exploitation population size

Antarctic fur seals (Arctocephalus gazella) were commercially exploited on the subantarctic island of South Georgia for over 100 years and nearly driven to extinction. Since the cessation of harvesting, however, their populations have rebounded, and they are now often considered a nuisance species whose impact on the terrestrial landscape should be mitigated. Any evaluation of their current population requires the context provided by their historic, pre-exploitation abundance, lest ecologists fall prey to shifting baseline syndrome in which their perspective on current abundance is compared only with an altered state resulting from past anthropogenic disturbance. Estimating pre-exploitation abundance is critical to defining species recovery and setting recovery targets, both of which are needed for the International Union for the Conservation of Nature's recent efforts to develop a green list of recovering species. To address this issue, we reconstructed the South Georgia fur seal harvest from 1786 to 1908 from ship logbooks and other historical records and interpolated missing harvest data as necessary with a generalized linear model fit to the historical record. Using an approximate Bayesian computation framework, harvest data, and a stochastic age-structured population model, we estimated the pre-exploitation abundance of Antarctic fur seals on South Georgia was 2.5 million females (95% CI 1.5–3.5 million). This estimate is similar to recent abundance estimates, and suggests current populations, and the ecological consequences of so many fur seals on the island, may be similar to conditions prior to human harvest. Although the historic archive on the fur sealing era is unavoidably patchy, the use of archival records is essential for reconstructing the past and, correspondingly, to understanding the present. Article impact statement: Defining species recovery requires an understanding of baseline population state, which can be estimated through statistical methods.     

1991年华南地区热带气旋灾害概况

本文介绍了1991年在我国登陆的6个热带气旋灾害的特点及其所造成的人员伤亡与经济损失。     

Flood policy reversal in australia

In 1977 the Government of New South Wales introduced a flood prone lands policy which attempted to break with the past emphasis on structural works. Cornerstones of the policy were the preparation of floodplain maps, and use of the 1:100 (100 year or 1%) flood to delineate floodplains and 1:20 flood for floodway definition. The fiscal and regulatory elements of the policy were to be applied more or less uniformly within the two zones. At first there was little effective opposition to the program, but this changed when large areas of Sydney, which had not been inundated since development, were mapped. Local government concern over issues of legal liability led to decisions which in turn prompted opposition to the policy from residents' action groups and property development interests. A perceived drop in property values provided the main motivation for action by residents. This pressure for change, which intensified just before the 1984 state election, saw the policy overturned.
The new policy gives local government greater responsibility for floodplain management. State authorities have withdrawn from floodplain mapping, although technical advice will continue to be provided, and there are no longer any uniform floodplain or floodway definitions. Policy implementation is to be guided by a Manual which attempts to define flood hazard in terms of both physical and social criteria.     

西太平洋添加营养盐培养实验中挥发性卤代烃含量动态变化

于2018年10月9日~11月1日采集西太平洋表层海水，通过营养盐添加船基培养实验，研究了不同营养盐条件下浮游植物的生长及其释放挥发性卤代烃（VHCs）含量的动态变化规律.结果表明，与对照组相比，氮磷营养盐的添加对叶绿素a（Chl-a）的含量和三氯乙烯（C₂HCl₃），四氯乙烯（C₂Cl₄），一氯二溴甲烷（CHBr₂Cl），三溴甲烷（CHBr₃）的释放量表现出显著促进作用，但促进程度与添加氮磷营养盐的浓度及比值密切相关.高浓度氮更有利于浮游植物的生长及C₂HCl₃和C₂Cl₄的释放.N/P比符合Redfield比值更有利于CHBr₂Cl和CHBr₃的释放.相比NO₃^--N，NH₄⁺-N的添加更有利于4种VHCs释放.     

“苏南模式”与可持续发展

“苏南模式”是我国目前经济发展模式之一，取得了巨大的成就，也面临着严峻的挑战。实施可持续发展战略是“苏南模式”摆脱传统再创辉煌的必然选择，可将苏南地区建成我国可持续发展示范区。     

Preliminary studies on methane flux from the ornithogenic soils on Xi-Sha atoll, South China Sea

IntroductionMethane ( CH4) is a radiatively active trace gas ,contributing approximately 20 % to global warming(Bouwman, 1990) . An increasing concentration in theatmosphere, and ill-defined sink and source strengths haveled to a proliferation of the stud…     

青藏高原东北部气候变化的异质性及其成因

利用1961-2016年西宁等青藏高原东北部13个气象台站气温、降水等气象资料以及国家气候中心发布的南海季风指数、西伯利亚高压指数等大气环流特征量数据,分析近56年来气候变化与高原主体的差异性及其可能的气候成因。研究表明：近56年来青藏高原东北部气候变暖趋势十分显著,年平均气温气候倾向率高达0.39 ℃/10 a,呈现出三次明显的阶梯性增高态势,并于1994年前后发生了由冷到暖的突变,同时具有明显的空间差异性;年降水量及四季降水量均没有明显变化趋势,虽然经历了2002年左右由少到多的变化,但并未出现明显突变,年降水量具有3年、5年的准周期,而年降水日数微弱减少,降水强度呈增加趋势;该区域气候变化的年际波动主要受到东亚季风、高原季风和南海季风的年际振荡及其相互作用的影响,而西风环流的作用并不明显,植被覆盖的恢复既是对2002年以来降水量增加的具体反应,同时也对于气候变暖趋势起到了一定的缓和作用。     

“中国南方喀斯特”世界自然遗产申报战略研究

中国南方喀斯特地区面积大,自然资源丰富,生态环境脆弱,在世界喀斯特地区中极具代表性。文章依据中国南方喀斯特地区独特的自然特征和社会、经济功能,借助申报自然遗产机遇,为实现该区人口、资源、环境与社会的可持续发展,提出了一系列针对中国南方喀斯特地区的保护策略及措施。