中全新世黄河流域耕地格局重建及对原生植被的影响(英文)

Yangshao culture is the most important mid-Holocene Neolithic culture in the Yellow River catchment,and thus,a study on the impact of human activities on the environment is important.In the current study,the distribution pattern of the cultivated land in late Yangshao culture is reconstructed using GIS tool and site domain analysis(SDA).The results show that the cultivated land during 5.5-5.0 ka BP was mainly distributed in the Weihe River valley,Luohe River valley,northwestern Henan Plain,Fenhe River valley and eastern Gansu region,especially concentrated in the Xi’an-Baoji line of the Weihe River valley.At that time,at least 37,000 km 2 of lands were reclaimed in the middle and lower reaches of the Yellow River,and 132,000 km 2 of lands were affected by agricultural activities.Human activities had become the driving force of land use/land coverage.Charcoal records indicate that the ancestors of Yangshao culture burnt forests for reclamation,leading to the decrease of arbor pollen at 5 ka BP in core areas of the Yangshao culture.The areas that were significantly affected by human activities accounted for 3.2% of the Yangshao culture influenced area,while the moderately affected areas accounted for 20.1% of Yangshao culture influenced area.Meanwhile,92% of the land areas on the edge and outside of the Yangshao culture influenced area were not affected by human activities.The arbor pollen in these areas did not decrease until 4.0 ka BP.     

面向服务架构的文物管理信息系统的设计与实现

本文探讨面向服务架构的文物管理信息系统的实现方法,基于电子地图、影像和三维模型提供的空间信息服务,设计和实现了不可移动文物查询、文物保护、文物空间模型服务等功能。作者以泰州市文物管理为例,实践了一个面向服务架构的文物管理系统,为文物管理提供了精细化、定量化和可视化的技术手段。     

A limnological study of four lakes near Rotorua

Four lakes (Okataina, Rotoehu, Ngapouri and Okaro), near Rotorua, New Zealand, were studied in 1960–66 and their physical features noted. The seasonal changes in water temperature and heat budgets throughout the depth of the lakes were followed through several cycles, and differences between lakes correlated with the altitude and size. The status of the lakes ranged from oligotrophic to eutrophic; changes in values for dissolved oxygen, both diurnal and seasonal, are interpreted in terms of their primary production. The partition of some dissolved substances during thermal stratification and immediately after overturn is described and the biological consquences are noted. The hypolimnetic oxygen deficit, however, was found to be correlated with primary production only when a depth factor was incorporated in the expression.

The data were compared with those from lakes in other parts of the world. The value of various published correlations with biological production is discussed; a possible explanation is put forward for the comparatively high heat budget of Lake Okataina.     

Physico‐chemical features of lake Ototoa,a sand‐dune lake in northern New Zealand

Lake Ototoa is a warm monomictic lake at 36° 31’ S, 174° 14'E. During a year's study (March 1969‐March 1970), the lake became thermally stratified in November, the metalimnion being between depths of 12 m and 16 m. Surface temperatures ranged between 10.2°c (in August) and 25.2°c (in late January), and bottom temperatures between 9.7°c and 17.5°c. The annual heat budget was calculated to be 642 354 KJ.m^‐2 (15 500 cal.cm^‐2) and the work of the wind in distributing the heat income 1.730 KJ.m^‐2 (1766 g.cm.cm^‐2). Secchi disc transparencies ranged between 5 m and 9.2 m (mean 7.07 m) and were greatest in the summer. Light transmission per metre was also high, ranging between 61% and 87%. Surface waters were normally supersaturated with oxygen, but during summer stratification oxygen concentrations in the bottom waters dropped to a minimum of 2.3 mg.litre^‐2 and a positive heterograde distribution of oxygen with depth was found. The oxygen deficit was 0.015 mg.cm^‐2.day^‐1 and showed the lake to be oligotrophic. Mean surface pH was 7.82, and the ionic composition of the waters was similar to that of other small New Zealand and Australian lakes located near the sea. Compared with other New Zealand lakes PO4‐P concentrations (range 1.00–10.20 μg.litre^‐1) were low and NO3—N concentrations (range 0.12–0.60 mg.litre^‐1) high.     

Laboratory culture of Galaxias maculatus and potential applications

Galaxias maculatus has considerable potential as a laboratory animal. Laboratory techniques used to maintain, artificially spawn, hatch, and rear this New Zealand native freshwater fish are described. Potential research applications for the fish, the eggs, and the larvae are outlined. The development of the larvae is described.     

连云港对虾养殖区表层沉积物重金属污染评价

在2010年6月对连云港市对虾养殖区的沉积物环境状况进行这站调查,分析了对虾池养殖区表层沉积物中重金属的含量及分布,并采用海洋沉积物质量国家标准和地积累指数法对该养殖区沉积物中重金属污染进行了评价。结果表明: (1)Cu、Zn、Pb、Cd、Hg、Cr、As的平均浓度分别为22.31 mg/kg、283.9 mg/kg、64.86 mg/kg、0.58 mg/kg、0.0056 mg/kg、89.23 mg/kg、35.58 mg/kg,通过计算单项污染指数表明所有元素的污染指数均在 0～1 之间,属于非污染,表明虾池沉积物属于清洁土壤。(2)利用地积累指数 (Igeo)法对所得到的调查结果进行了评价,发现各样点沉积物呈现出轻洁至中等的污染程度,参与评价的6种重金属的污染程度依次为As> Zn> Pb、Cd> Cr> Cu。进一步的生态风险评价结果表明,所有站位沉积物Cu和Cd（除站位5）的含量皆低于ERL值,说明Cu和Cd很少产生不利的生态效应;全部站位的重金属Zn、Pb和8个站位的Cr的含量均在ERL和ERM之间,表明这三种金属偶尔产生不利的生态效应。     

渤海湾肠道病毒的季节分布及其污染类型分析

肠道病毒是一类水传播胃肠道疾病的重要病原体。为了解感染性肠道病毒在海水环境中的季节分布规律、污染类型以及与流行病学的关系,于2010年12月到2011年10月应用能够提供病毒感染性信息的细胞培养结合实时定量PCR（ICC-qPCR）方法,分4个季节对渤海湾天津近岸海域表层海水中肠道病毒进行了监测。500 mL海水经超滤浓缩,48 h细胞培养,然后用qPCR检测得到四季海水样品中感染性肠道病毒的浓度为0.2~196 PFU/L,平均值为60 PFU/L,其中夏季和秋季肠道病毒浓度较高,其平均值分别为82 PFU/L和110 PFU/L。秋季阳性检出率最高（85.7%）,其次是冬季（71.4%）。经测序分析,其主要污染类型是脊髓灰质炎 Ⅰ 型疫苗株,此外,还检测出危及公众健康的一株类口服脊灰 Ⅰ 型疫苗脊灰和一株脊灰疫苗衍生株。由此可见,肠道病毒的季节分布和主要污染类型与临床上的流行趋势基本一致,海洋作为一个天然的受纳水体为病毒提供了良好的栖息场所和传播机会,对公众健康存在着潜在的威胁。因此,为减少相关疾病的暴发,应重点加强肠道病毒流行季节的海洋水质监测。     

生态补偿机制中的企业责任研究

研究了企业在市场经济体制中的主体地位和企业承担的环境责任,通过对生态补偿的涵义和政策范围进行分析,明确了生态补偿与排污费、资源费之间的区别和联系,提出了完善企业履行生态补偿责任的政策框架、搭建企业履行生态补偿责任的职能体系及创新企业履行生态补偿责任执行形式的建议。     

Field experiments on the role of epibenthic predators in determining prey densities in an estuarine mudflat

A series of caging experiments was performed on an estuarine mudflat at three seasons of the year, in which Carcinus maenas L. and Pomatoschistus microps (Kroyer) were either excluded from, or allowed to prey upon, the benthos in order to determine to what extent infaunal abundance and mortality was a result of predation by epibenthic predators.The difficulties of conducting and interpreting the results of such experiments are recognized. The benthic macrofauna of this mudflat is dominated numerically by small annelids and there is evidence that adult C. maenas can cause significant increases in the oligochaete component of this assemblage, probably as a result of disturbance caused by its burrowing activity. Juvenile C. maenas on the other hand significantly reduced the abundance of small annelids, particularly the dominant polychaete Manayunkia aestuarina (Bourne) and could be responsible for year-to-year variations in abundance of this species. The role of fish predators (in this case P. microps) is more problematical but it is suggested that in the densities at which they occur naturally on the mudflat they have little direct effect on the abundance of prey species. There is no evidence that seasonal mortality of small annelids is reduced in the absence of predation and this is taken to indicate that not all mortality is due to epibenthic predation. Certain changes in relative abundance of the component species of the harpacticoid copepod community were discerned but it is suggested that the plasticity of their reproductive potential is such that the effect of predation on the group as a whole is usually masked.     

FATTY ACIDS PROFILE IN A HIGH CELL DENSITY CULTURE OF ARACHIDONIC ACID-RICH PARIETOCHLORIS INCISA （TREBOUXIOPHYCEAE, CHLOROPHYTA） EXPOSED TO HIGH PFD

The changes in arachidonic acid (AA) and fatty acids profiles along the growth curve ofParietochloris incisa, a coccoid snow green alga, were studied in a 2.8 cm light-path flat photobiorcactor, exposed to strong photon flux density [PFD, 2400 μEmol/(m²·s)]. Sixteen fatty acids were identified by gas chromatography showing that AA was the dominant fatty acid (33%–41%) followed by linoleic acid (17%–21%). AA content was closely investigated with respect to total fatty acids (TFA), ash free dry weight (AFDW) of cell mass as well as total culture content. These parameters were influenced significantly in a similar manner by culture growth phase, i.e., slightly decreasing in the lag period, gradually increasing in the logarithmic phase, becoming maximal at the early stationary phase, starting to decrease at the late stationary phase, sharply dropping at the decline phase. The increase in AA per culture volume during the logarithmic phase was not only associated with the increase in AFDW but also connected with a corresponding increase in AA/TFA, TFA/AFDW as well as AA/AFDW. The sharp decrease in AA content of the culture during the decline phase was mainly due to the decrease in AA/TFA, TFA/AFDW and AA/AFDW, although AFDW declined only a small extent. Maximal AA concentration, obtained at the early stationary phase, was 900 mg/L culture volume, and the average daily net increase of AA during 9 days logarithmic growth was 1.7 g/(m²·day). Therefore, harvesting prior to the decline phase in a batch culture, or at steady state in continuous culture mode seems best for high AA production. The latter possibility was also further confirmed by continuous culture with 5 gradients of harvesting rate. Contribution No. 4138 from the Institute of Oceanology, Chinese Academy of Sciences. Project 39970575 supported by NSFC and A/2786-2 supported by International Foundation for Sciences (IFS).