沙棘对中国亚湿润干旱区的杨树人工林养分分布及生物循环影响

通过将沙棘（ＨｉｐｐｏｐｈａｅｒｈａｍｎｏｉｄｅｓＬ．）与三种杨树品种（小黑杨（Ｐｏｐｕｌｕｓ‘Ｘｉａｏｈｅｉ’）昭林６号杨（Ｐ．‘Ｚａｏｌｉｎ０６’）和欧美杨６４号（Ｐ．ｅｕｒａｍｅｒｉｃａｎｅｃｖ．‘Ｎ３０１６’）的人工林分别按株混和行混两种方式进行混交实验,研究了固氮植物沙棘对亚湿润干旱区的杨树人工林养分分布和循环的影响,连续３ａ的观测研究得以下结果,沙棘叶片的氮,磷和钾的元素粪土了高于杨树     

黄土残塬沟壑区刺槐人工林生态系统的养分循环通量与平衡分析

根据养分平衡原理测算了黄土高原残塬沟壑区刺槐人工林生态系统的生物化学循环和生物地球化学循环通量及循环率,以相对聚散度反映了养分循环通径上的各养分元素的相对富集化或稀释化程度,结果表明了刺槐人工林生态系统的养分循环为土壤亏损,系统积累型的总流动趋势。     

Simulated effects of low atmospheric CO2 on structure and composition of North American vegetation at the Last Glacial Maximum

1. Physiological experiments have indicated that the lower CO₂ levels of the last glaciation (200 μmol mol^?1) probably reduced plant water-use efficiency (WUE) and that they combined with increased aridity and colder temperatures to alter vegetation structure and composition at the Last Glacial Maximum (LGM). 2. The effects of low CO₂ on vegetation structure were investigated using BIOME3 simulations of leaf area index (LAI), and a two-by-two factorial experimental design (modern/LGM CO₂, modern/LGM climate).3. Using BIOME3, and a combination of lowered CO₂ and simulated LGM climate (from the NCAR-CCM1 model), results in the introduction of additional xeric vegetation types between open woodland and closed-canopy forest along a latitudinal gradient in eastern North America.4. The simulated LAI of LGM vegetation was 25–60% lower in many regions of central and eastern United States relative to modern climate, indicating that glacial vegetation was much more open than today.5. Comparison of factorial simulations show that low atmospheric CO₂ has the potential to alter vegetation structure (LAI) to a greater extent than LGM climate.6. If the magnitude of LAI reductions simulated for glacial North America were global, then low atmospheric CO₂ may have promoted atmospheric warming and increased aridity, through alteration of rates of water and heat exchange with the atmosphere.     

Characteristics of Plant Communities and Element Contents in Plants at Mengentaoligai Ag,Pb, Zn Mine area in Inner Mongolia

The types of plant communities in Mengentaoligai mine area are disscussed. Arenaria juncea, densely grown in the phytocommunities of the mineralized zone, is found closely related to the presence of Pb and Zn mineral deposits. Analytical results of seven element contents (in ash) for 34 species (or part of plant) show that: levels of element contents in sequence in. the plants are Fe>Mn > Zn > Pb > Cu > Ni>Co; variable ranges of element contents in the plants are Pb, Zn>Fe,Mn> Cu> Co > Ni; and variable ranges of Pb, Zn contents in the same species at different sites are respectively larger than that among species. For example, Pb and Zn contents of Arenaria juncea, l145ppm and 3087ppm respectively, are the highest; the difference among Pb contents of Ulmus macrocarpa, Arenaria ?uncea and PotentiUa chinensis at different sites are more than 10 folds. The difference of Co and Ni contents in the species is less than two to one- Striking correlation is found between elements in plants and in soils, such as the Pb and Zn contents between leaves and twigs of Ulmus macrocarpa, twigs of Prunus sibirica, Artemisia halodendron and soils (lrl≤α 0.05 or≤α 0.01). It is found that Pb and Zn phytogeochemical anomalies, correlate closely with Pb and Zn mining deposits. In addition, analysis of principal component was conducted among seven elements contents of 14 species (or part of plant) in the mineralized zone and 12 species in the unmineralized zone.     

The Origin,Dispersal and Formation of the Distribution Pattern of Swertia L. (Gentianaceae)

The genus Swertia is one of the large genera in Gentianaceae, including 154 species, 16 series and 11 sections. It is disjunctly distributed in Europe, Asia, Africa and N. America, but entirely absent from Oceania and S. America. According to Takhtajan’s (1978) regionalization of the world flora, Swertia is found in 14 regions. Eastern Asiatic region with 86 species, of which 58 are local endemics, 13 series and 9 sections, ranks the first among all the regions. The highest concentration of the taxa and endemics in Eastern Asiatic region occurs in SW China-Himalayan area (Sikang-Yunnan P. , W. Sichuan, W. Yunnan-Guichou Plateau of China and NE. Burma, N. Burmense P. , E. Himalayan P. and Khasi-Manipur P. ). In this area there are 74 species (48 endemics), 12 series, and 9 sections; thus about half species of the world total, three quarters of series and 82% of sections occur in this small area. Besides, the taxa at different evolutionary stages in Swertia also survive here. It is an indication that SW. China-Himalayan area is a major distribution centre of the genus Swertia. In addition, Sudan-Zambezian Region in Africa, with 22 species, 4 series and 2 sections, is a second distribution centre. The primitive type of the genus Swertia is Sect. Rugosa which consists of 2 series and 23 species. It is highly centred in the mountains of SW. China (Yunnan, Sichuan, Guizhou and SE. Xizang) where 2 series and 16 species occur. Among them 15 species of Ser. Rugosae were considered as the most primitive groups in this genus. From our study, the outgroup of Swertia is the genus Latouchea Frahch. , which is distributed in Yunnan, Sichuan, Guizhou, Hunan, Guangdong, Guangxi and Fujian. The two groups overlap in distribution in SW. China. According to the principle of common origin, the ancestor of two genera ap peared most probably in this overlapping area. It was inferred that SW. China Was the birth-place of the genus Swertia. Four sections of Swertia have different disjunct distribution patterns: Sect. Ophelia is of Tropic Asia, Africa and Madagascar disjunct distribution; sect. Swertia is of north temperate distribution; sect. Spinosisemina is in Tropical Asia (Trop. India to S. China and Philipines); sect. Platynema also is in Tropical Asia (Java, Sumatra, Himalayas to SW. China). These disjunct patterns indicate that the Swertia floras between the continents or between continent and islands have a connection with each other. From paleogeographical analysis, Swertia plants dispersed to Madagascar before the Late Cretaceous, to SE. Asian Islands in the Pleistocene, to North America in the Miocene. The distribution of Swertia in Madagascar might be later than that in Asia. Therefore the origin time of the genus Swertia was at least not later than the Late Cretaceous, and might be back to the Mid-Cretaceous. The genus Swertia first fully developed and differentiated, forming some taxa at different evolutionary stages (Rugosa, Swertia, Poephila, Ophelia and Platynema etc. ) in the original area, and these taxa quickly dispersed in certain directions during the Late Cretaceous-Middle Tertiary when the global climate was warm and no much change. There seem to be three main dispersal routes from the origin area to different continents; (1) The westward route i. e. from SW. China, along the Himalayas area to Kashmir, Pakistan, Afghanistan and Iran, and then southwestwards into Africa throuth Arabia. Four sections (Poephila, Macranthos, Kingdon-Wardia and Ophelia) took this dispersal route. Most species of sect. Ophelia dispersed along this route, but a few along southern route and north ern route. Sect. Ophelia greatly differentiated in Africa and the African endemic sectionSect. Montana was derived from it. The two sections form there a second distribution center of Swertia. (2) The southward route, i. e. towards S. India through the Himalayas, and towards SE. Asian islands through C. and S. China, Indo-China. Along this dispersal route sect. Platynema, Sect. Spinosisemina and a few species of Sect. Ophelia dispersed; (3) The northward rout, i. e. northwards across N. China, C. Asia to a high latitude of Euasia, and also through E. Asia into N. America. The following groups took this route: sect. Rugosa, sect. Swertia, sect. Frasera, sect. Heteranthos and sect. Ophelia ser. Dichotomae. Therefore, it seems that the genus Swertia originated in SW. China and then dispersed from there to N. and S. Asia, Africa, Europe and North America and formed the moderndistribution pattern of this genus.     

中国东亚飞蝗新类型蝗区——海南热带稀树草原蝗区的生态地理特征及其与大沙河蝗区比较

本文系统地对海南热带稀树草原蝗区的生态地理结构特征进行了分析,说明本蝗区是 Uvarov(1936)提出的飞蝗两类蝗区理论中,由于森林破坏而形成的一类蝗区,作者将它定名为“热带稀树草原蝗区”。这类蝗区在我国过去尚缺乏研究。文中进而根据本蝗区的成因、生态特征以及对蝗区的生态控制对策,分别与我国大陆的东亚飞蝗大沙河类型蝗区进行了比较。     

森林公园在我国自然保护区系统中的地位

本文针对我国森林公园建设发展迅速的现状,阐述了“森林公园”的自然保护性质和作用,提出“国家自然保护区系统”的概念,将森林公园与自然保护区、风景名胜区三个体系同视为“国家自然保护区系统”中的三个组成部分,并阐述了这三个体系各自的特点、地位及其相互关系。同时,还提出进一步加强森林公园管理的建议。     

海岸带复合梨园的光能分布与利用规律

采用方格法和分层法相结合的技术对江苏省如东县棉花原种场林网保护区内13年生梨园的树冠结构特征和光能分布与利用规律进行了系统研究。结果表明:梨树叶幕光能分布状况直接受叶面积系数、树冠结构、太阳位置及光强的影响。各层叶幕中的光合有效辐射(PAR)分布随自然光照条件的变化而改变,其日平均透光率大小和PAR日变化范围均从叶幕外围向内膛随累积叶面积系数(LAI)的增加而减弱;不同生长时期及不同天气变化下树冠光能分布存在明显的差异性;树冠结构与累积LAI对PAR的分布及利用率具有决定性的影响。在生产实践中,通过密度调控、整形修剪等农业技术措施,维持成年梨园盛果期高效光合生产的叶幕厚度在2.5m以上,有效LAI为4左右,是增强梨树光合生产能力、提高产量和品质的有效措施。     

冬小麦农田中净辐射的研究

本文对陕西泾阳地区冬小麦田净辐射进行了分段和分层模拟,取得了较好的拟合效果,相对误差在１０％以内。确定了麦田相对叶面积函数最大值的出现高度为４．５／７Ｈ,介于高粱（４／７Ｈ）和谷子（５／７Ｈ）之间。计算了不同发育期、不同层次至冠层顶部累积叶片的消光系数,结果表明,消光系数因发育期和叶片层次而异,拔节期,由旗叶向下,消光系数增大,乳熟期旗叶的消光系数最大,比拔节期大一倍,倒二叶以上两个层次叶片消光系数较小。就平均而言,冬小麦消光系数拔节期为０．５１,乳熟期为０．５６。本项成果为进一步开展麦田小气候研究提供了有意义的数据和方法。     

菜豆属（Phaseolus L.）两种食用作物的核型研究

作者研究了红花菜豆品种大白芸豆和菜豆品种珍珠豆的核型。大白芸豆和珍珠豆的核型公式分别为;２ｎ＝２ｘ＝２２＝１４ｍ（２ＳＡＴ）＋６ｓｍ＋２ｓｔ;２ｎ＝２ｘ＝２２＝６ｍ（２ＳＡＴ）＋１４ｓｍ＋２ｓｔ。这两处品种的核型存在明显差异,但也有相似之处。