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101.
20000~15000a.B.P.间气候最冷,生长喜冷的针叶林和干旱草原植被.在14780±700a.B.P.出现了最低海面(-154m);15000~13500a.B.P.,气候较暖湿,海面上升,生长阔叶混交林;13500~10500a.B.P.,气候有2次温暖和3次较冷,在暖期生长针阔叶混交林.较冷期则出现森林草原和草原.最低的温度比现在低5~7;一万多年来的冰后期,气候变化分为5个新冰期(包括小冰期)和5个新高温期(包括小气候最宜期).最高气温比现在高2~3℃,出现在5000~4000a.B.P.之间;最低温度比现在低3~5℃最高海面在6500~6300a.B.P.,高出现在海面4~5m.在温暖期中生长常绿一落叶阔叶林中亚热带针阔混交林;在较冷期间,生长落叶阔叶林,针叶林或草原草地.在人类影响或自然发展之结果,未来环境变化有可能向干暖气候和高海面演变,或向干冷气候和海面下降转变.这些变化将对长江中下游带来意外的灾难. 相似文献
102.
103.
生态工业园区是按照工业生态学原理,通过模拟自然生态系统,建立工业系统中“生产者-消费者-分解者”的循环途径,实现物质闭路循环和能量多级利用。文中介绍了生态工业园区的概念、分类和中国工业生态园区的建设进展。结合无锡新区生态工业园区的建设现状,提出新区的生态工业链网设计思路,通过园区成员企业之间的协同管理,以取得资源、环境与经济、社会效益的增长最大化。 相似文献
104.
I studied the ecology of parental care behaviors displayed by two closely related sympatric species of microhylid frogs in Papua New Guinea that occupy different microhabitats. Adult removal experiments on the terrestrial frog Hylophorbus rufescens and the undescribed arboreal frog Oreophryne sp. A demonstrate a significant positive effect of parental attendance on offspring survivorship and differential causes of egg mortality between microhabitats. Desiccation was the primary cause of egg mortality for the arboreal frog, whereas predation was the main source of mortality for the terrestrial frog. These selection pressures (desiccation and predation) are comparable to two of Wilsons prime movers of the evolution of parental care (harsh environment and predation) and may have driven and/or are maintaining the evolution of parental care behaviors in these Papuan microhylid frogs. These results highlight microhabitat-specific selection pressures in the evolution and maintenance of parental care behaviors.Communicated by A. Mathis 相似文献
105.
浦东新区土壤—食物链中的铜锌 总被引:1,自引:0,他引:1
本文调查了浦东新区污灌区、吹泥区和一般区三种处理土壤中Cu、Zn的水平和垂直分布,Cu、Zn分层现象不明显,水平差异较大,但三种关型土壤差异不显著。Cu在食物链中累积系数铰小,一般小于1.0,而Zn的累积程度较大,尤其是以人为消费者的食物链中,累积系数最高达到18。 相似文献
106.
This paper examines the determination of effort levels, the rental price of quotas and the number of participants in a fishery managed with a total allowable catch and individual transferable quotas. How these variables change is determined for three phases of the management process. Potential participants in the fishery are assumed to be heterogeneous in their catching capabilities so that almost all active fishers earn positive net profits from fishing activities. It is shown that these quasirents are reduced during any of the management phases considered here. The impact of free allocations of permanent quota rights on fishers’ welfare is also considered. This may increase the welfare of all fishers if the allocation is based on catch history. However, an example is provided where the welfare of some highliners is reduced when the allocation is based on effort history. 相似文献
107.
Mercy Varghese Parakkatt Parambil Leena Palani Murugavel Shivdas Bankar Kiran Todekar Subharthi Chowdhuri 《毒物与环境化学》2020,102(7-8):305-333
Abstract This study reports on new particle formation (NPF) and characteristic features observed from a rural site falling in the rainshadow of the Western Ghats in peninsular India. A total of 35 NPF events observed during August 2018 - January 2019 are classified and analyzed here. The apparent formation rates ranged from 0.2 to 10.0?cm–3 s–1, while the growth rates of nucleation mode particles ranged from 1.2 to 13.8?nm h–1. The frequency of occurrence was least during August (core monsoon) and highest during post-monsoon. The local winds were calm and southeasterly to easterly (from the urban centre) supplying the essential precursor gases during October and November, leading to a frequent occurrence of nucleation events. Observations suggest that an increased condensation sink could limit the NPF while promoting Aitken mode growth. The newly formed particles accounted for about 10–80% of the total aerosol concentration. These newly formed particles were able to act as cloud condensation nuclei after growing to approximately 50?nm with an average activation fraction of 0.4. 相似文献
108.
109.
Beryllium and aluminium contents in uncontaminated soils from six countries are reported. The means and ranges of beryllium in the surface soils were as follows: 1.43(0.20–5.50)g g–1 in Thailand (n=28), 0.7 (0.31–1.03) g g–1 in Indonesia (n=12), 0.99(0.82–1.32) g g–1 in New Zealand (n=3), 0.58(0.08-1.68)g g–1 in Brazil (n=16), 3.52(2.49–4.97)g g–1 in the former Yugoslavia (n=10), and 1.56(1.01–2.73) g g–1 in the former USSR (n=8). The mean and range of beryllium contents of the surface soils in Japan (1.17(0.27–1.95)g g–1
n=27) are situated within the values of the soils from these countries except for the Yugoslav soils derived from limestones. The mean of the mean beryllium contents of the surface soils in all these countries is 1.42 g g–1 which will be used as a tentative average content of beryllium in uncontaminated surface soils, except for the soils derived from parent materials high in beryllium content. The beryllium contents of the subsoils were higher than those of the surface soils in New Zealand and Yugoslavia as is the case with Japan. The correlation coefficient between the contents of beryllium and aluminium in all the soil samples (n=113) including surface soils and subsoils was 0.505 (p < 0.001). 相似文献
110.