华西雨屏带及其对我国生物多样性保育的意义

华西雨屏带为四川盆地西部边缘独特的自然地理区域。东西宽50-70km,南北长400－450km,总面积约2.5万km^2,仅占我国国土总面积的0.26%左右。本区以自然风景优美、天然植被类型丰富、动植物资源种类多样而享誉中外。迄今为止,尚未将华西雨屏带作为相对独立的自然地理单元来研究其生物多样性。本文从当地剧烈的地形、地貌变化,特殊的气候、植被类型与动物栖息环境以及邻近人类聚居区的特点入手,扼要阐述了本区生态系统与环境的多样性状况。进一步通过对当地动植物种类,尤其是种子植物、兽类、鸟类、鱼类物种多样性与珍、稀、特保护物种的数量比重分析,提出了本带作为我国乃至世界上研究与保护生物多样性的热点区域的立论依据。华西雨屏带是一个大尺度、复合性的生态过渡带（ccotone),是我国西部地区以阴湿为主要特征的罕见的气候地理单元,是我国西部生态保护与建设的一道绿色屏障,是我国生物多样性保护与研究不可替代的关键地区之一。     

万木林中亚热带常绿阔叶林物种多样性林隙梯度变化

根据万木林中亚热带常绿阔叶林林隙内外物种的调查数据,研究了林隙各区物种多样性的梯度变化及物种多样性随林隙级的梯度变化.结果表明,从林隙中心区到非林隙区,物种丰富度指数和物种多样性指数逐渐降低;生态优势度呈中间高、两端低的变化趋势;均匀度呈中间低、两端高的变化趋势.林隙各区的物种多样性在林隙面积为200～300 m²时均达到最大.     

华西雨屏区不同恢复阶段湿性常绿阔叶林的土壤微生物多样性

采用时空互代的方法,探讨了崇州市鞍子河自然保护区和邛崃市天台山的常绿阔叶林自然恢复过程中土壤微生物数量、组成、区系和多样性变化,结果表明：（1）不同恢复时期土壤微生物数量存在显著性差异,在植被恢复5～40a期间,土壤细菌和放线菌的数量呈增加趋势,以恢复到40a植被土壤微生物总数、细菌和放线菌的数量较高,分别为1．06×10^6CFUg^-1干土、9．81×10^5CFUg^-1干土和6．8×10^4CFUg^-1干土;真菌以100a次生林较高,为9．01×10^4CFUg^-1干土;植被恢复中细菌占土壤微生物总数的79．06％～93．78％;真菌和放线菌数量分别占4．61％～11．24％和0．52％～15．38％;（2）不同恢复阶段土壤细菌和真菌数量大体上以夏季高,春、秋季较低;放线菌数量为春、秋季较夏季高;（3）植被恢复过程中,土壤微生物群落区系和优势种群组成不同,经鉴定有细菌10个属、真菌7个属、放线菌9个属,细菌以无色细菌属（Achromobater）、棒状杆菌属（Corynebacterium）、短杆菌属（Brevibacterium）和芽孢杆菌属（Bacillus）出现的几率较高;真菌主要是半知菌类和接合菌类,以木霉属（Trichoderma）、腐霉属（Pythium）、青霉属（Penicillium）和犁头霉属（Absidia）分布较为普遍;放线菌9个类群中8个属于链霉菌属（Streptomyces）,仅有1个类群属于小单孢菌属（Micromonospora）,以白孢类群（Albosporus）、金色类群（Aureus）和灰红紫类群（Griseorubroviolaceus）出现几率为较高;（4）细菌属的Shannon—Wiener指数、Simpson指数以恢复初期、30a生次生林和较原始植被为较高。在植被恢复5～50a期间,真菌和放线菌属的多样性呈波动性增加趋势,到50a达到最高;50a以后,呈下降趋势,表明植被恢复的30～50a土壤环境更适合真菌和放线菌的生长。     

季风常绿阔叶林不同恢复阶段藤本植物的物种多样性比较

藤本植物是森林生态系统的重要组成部分,影响群落的恢复与演替。通过对云南普洱地区不同恢复阶段(恢复15a、恢复30a和原始林群落)季风常绿阔叶林群落的野外调查,分析了不同恢复阶段藤本植物的物种丰富度、密度、多度、径级分布、多样性指数及攀援方式,并探讨藤本植物与支持木的关系。结果表明:在0.81hm²的调查样地中,共发现DBH≥0.1cm的藤本植物1292株(分属34科51属64种)。原始林群落的藤本物种丰富度、密度(DBH＜1cm)、胸高断面积和平均胸高断面积都显著高于恢复阶段,原始林和恢复15a群落的密度(DBH≥1cm)、平均胸径和平均长度之间无显著差异,但都显著高于恢复30a。3种群落类型中藤本植物的物种组成和径级分布有显著差异,原始林中藤本植物物种更多,而且大径级(DBH≥10cm)的藤本植物仅出现在原始林及恢复30a的群落。单株藤本攀援的支持木在3种群落类型中均占多数,藤本植物与支持木的胸径存在显著的正相关(P＜0.001),原始林群落中DBH≥15cm的支持木更易被攀援,而恢复阶段则相反。茎缠绕藤本植物对原始林的负面影响要显著少于恢复15a及30a群落,而卷须类藤本植物也反映出原始林正处于一个动态变化的阶段,同时根攀缘和搭靠类藤本植物物种组成和多度变化可以反映出干扰后季风常绿阔叶林的恢复程度。森林砍伐是影响不同恢复阶段藤本植物的物种组成和分布的主要因素。     

Variability of plant species diversity in Swedish natural forest and its relation to atmospheric deposition

Within a subprogram of Integrated Monitoring (IM), understorey vegetation in Swedish natural forests was observed at fifteen reference sites over the country for twelve seasons, 1982–1993. The main task of the subprogram was to assess the impact of atmospheric deposition, mainly sulphur and nitrogen, on natural vegetation through time. The present study is focused on the variability of plant species diversity at community level and the possible impact of sulphur and nitrogen deposition. Species richness, evenness and diversity varied greatly among the sites, and between years within each site. Regarding only coniferous forests the species richness was higher in the north than in the south. But the effects of site condition and atmospheric deposition were not clarified. Changes in species diversity through time differed from site to site. No overall temporal trend was found. The atmospheric deposition of sulphur and nitrogen demonstrated a clear geographical pattern being low in the north-west and high in the south-west. Sulphur deposition declined significantly in Southern Sweden during the period. We concluded that the species diversity of understorey vegetation at the Swedish IM sites was not significantly influenced by atmospheric deposition. The changes observed are explained as natural processes.     

Tree competition and species coexistence in a warm-temperate old-growth evergreen broad-leaved forest in Japan

The growth dynamics and mode of competition between adult trees 5.0cm in diameter at breast height (DBH) of nine abundant treespeciesoccupying ca. 85% of the total basal area were investigated in a 4ha study plot (200 m × 200 m) of awarm-temperate old-growth evergreen broad-leaved forest in the Tatera ForestReserve of Tsushima Island, southwestern Japan. In the plot, adult trees 5.0 cm DBH co-occurred with 35 woody plant species (except forwoody vine species). The most dominant and largest species,Castanopsis cuspidata var. sieboldiiexhibited a bimodal DBH distribution; it was found in both the upper and lowervertical layers. Other tree species had unimodal DBH distributionscorrespondingmostly to the lower vertical layer. We developed a model for individual growthincorporating both intra- and interspecific competition and degree ofcompetitive asymmetry. One-sided interspecific competition was detected in 17cases out of the 66 possible combinations on the scale of the 4 hastudy plot. The direction of interspecific competition was generally one-sidedfrom layer-I species to layer-II and III ones. The effects of two-sidedcompetition were detected only in layer-II and III species. OnlyDistylium racemosum exhibited one-sided intraspecificcompetition. We also found 11 cases of positive interspecific relationships.Generally, competitive relationships prevailed over positive relationshipsbetween adult trees in this warm-temperate evergreen broad-leaved forest.Competition between adult trees 5.0 cm in DBH did not occurinthe same vertical layer, but occurred only between trees in different verticallayers. This suggests that competition between adult trees 5.0cm in DBH plays a key role in the variation in species coexistencebetween different vertical layers on the 4 ha scale of thewarm-temperate evergreen broad-leaved forests. Moreover, it was found bycomparing with three different forest types that interspecific competition ismore intense in warm-temperate forests than in cool-temperate or sub-borealforests. We conclude that, compared to cool-temperate or sub-boreal forests(which have little interspecific competition), warm-temperate forests supportmore complex interspecific relationships and species-specific habitatpreferences that result in higher species diversity.     

模拟氮沉降对华西雨屏区天然常绿阔叶林凋落叶分解过程中基质质量的影响

为理解氮沉降对华西雨屏区天然常绿阔叶林凋落物分解过程的影响,采用立地控制实验和凋落物分解袋法,研究了低氮沉降(L,50 kg N hm~(-2)a~(-1))、中氮沉降(M,150 kg N hm~(-2)a~(-1))和高氮沉降(H,300 kg N hm~(-2)a~(-1))对华西雨屏区天然常绿阔叶林凋落叶分解过程中基质质量的影响。结果表明:N沉降抑制了凋落叶的分解,并随着N沉降量的增加,抑制作用增强。N沉降遏制了凋落叶的C、N释放和纤维素降解,促进了P释放。N沉降提高了凋落叶的C/P比,中氮和高氮处理提高了凋落叶C/N比。N沉降显著增加了凋落叶N、木质素和纤维素的含量,分解1年后,各N沉降处理的木质素/N和纤维素/N均显著高于对照。N沉降提高了质量残留率与C/N、木质素/N和纤维素/N的相关性,降低了与C/P的相关性。可见,模拟N沉降显著影响了华西雨屏区天然常绿阔叶林凋落叶分解过程中的基质质量,进而影响了凋落叶的分解过程。     

种、种的多样性及退化生态系统功能的恢复和维持研究

物种多样性是生态系统的重要特征并维持系统的功能支行,生物种和不同种类构成的群落为人类提供诸如营养物质循环、生物生产力、营养功能等形式的重要生态服务,特种多样性与生态系统抵御逆境和干扰的能力紧密相关,多样性的提高会增加系统的稳定性,与单个种和种类的数量相比,功能群和功能多样性对生态系统功能的影响效应要大得多,且易于被用来测度稳定性和预测群落变化,本文提出并探讨了种对生态系统功能作用的几种形式,理解物种多样性与生态系统的功能关系能指导退化生态系统恢复和维持其功能的实践活动,尤其为恢复的初始阶段进行群落的“种类组装”提供生态理论基础。     

华西雨屏区天然常绿阔叶林土壤可培养微生物数量对模拟氮沉降的响应

为了解氮沉降对华西雨屏区天然常绿阔叶林土壤微生物数量的影响,从2013年11月至2014年12月,通过野外模拟N(NH_4NO_3)沉降,氮沉降水平分别为对照(CK 0 kg N hm~(-2)a~(-1))、低氮沉降(L 50 kg N hm~(-2)a~(-1))、中氮沉降(M 150 kg N hm~(-2)a~(-1))和高氮沉降(H 300 kg N hm~(-2)a~(-1)),研究了氮沉降对天然常绿阔叶林0—10cm和10—20cm土层土壤可培养微生物数量的影响。结果表明:华西雨屏区天然常绿阔叶林0—10cm土层的细菌、真菌和放线菌数量均显著大于10—20cm土层,氮沉降未改变原有垂直分布格局。L处理对0—10cm和10—20 cm土层土壤微生物总量无显著影响,M和H处理则显著降低了土壤微生物总量。氮沉降降低了0—10cm和10—20cm土层的细菌数量,且抑制作用随氮沉降量的增加而增强。氮沉降降低了0—10cm土层的真菌数量,但下降幅度与氮沉降量之间无明显规律;在10—20cm土层,M和H处理在夏季显著增加了真菌数量,表明适量氮沉降能有效缓解夏季土壤真菌的氮限制状态。氮沉降对0—10cm土层放线菌数量的影响表现为先促进再抑制,L和M处理增加了放线菌数量,H处理降低了放线菌数量;氮沉降增加了10—20cm土层的放线菌数量,其中M处理的促进作用最大。氮沉降对土壤微生物数量的影响随土壤深度的增加而减弱。     

模拟氮沉降对华西雨屏区光皮桦林土壤酶活性的影响

在华西雨屏区光皮桦(Betula luminifera)人工林内设置不同氮沉降水平(0、5、15和30 g N·m-2·a-1)的模拟氮沉降试验,研究氮沉降对林地土壤酶活性的影响.结果表明:模拟氮沉降促进了光皮桦人工林土壤中水解酶(蔗糖酶、纤维素酶、酸性磷酸酶和脲酶)活性,抑制了氧化酶(多酚氧化酶和过氧化物酶)活性.土壤水解酶活性的增强预示着在活性氮增加的情况下,光皮桦和土壤微生物对碳、磷元素的需求增加.外源无机氮的增加显著降低了土壤多酚氧化酶和过氧化物酶的活性,可能导致凋落物分解受到抑制,促进凋落物在土壤中的积累,并通过抑制土壤有机质的分解增加土壤中碳的贮存量.     

华西雨屏区苦竹林土壤酶活性对模拟氮沉降的响应

2007年11月-2009年5月,对华西雨屏区苦竹人工林进行了模拟氮沉降试验,氮沉降水平分别为：对照(0 g N·m^-2·a^-1)、低氮(5 g N·m^-2·a^-1)、中氮(15 g N·m^-2·a^-1)和高氮(30 g N·m^-2·a^-1).在氮沉降进行半年后,每月采集各样方0～20 cm土壤样品,测定其土壤酶活性,连续测定1年.结果表明：苦竹人工林样地中6种土壤酶活性的季节变化较明显,蔗糖酶、纤维素酶和酸性磷酸酶活性的高峰期出现在春季,脲酶活性高峰期出现在秋季,而过氧化物酶和多酚氧化酶活性高峰期出现在冬季;氮沉降增加了苦竹林土壤中木质素分解酶和碳、氮、磷分解相关酶（多酚氧化酶、蔗糖酶、酸性磷酸酶和脲酶）的活性,抑制了纤维素酶活性,而对过氧化物酶的影响不显著;苦竹林生态系统处于一种氮限制状态,氮沉降刺激了微生物-酶系统对土壤有机质的分解.     

古田山中亚热带常绿阔叶林群落物种多样性的空间变异特征

古田山常绿阔叶林的群落组成、结构及其维持机制已有许多研究, 但该地区亚热带常绿阔叶林生物多样性空间变异特征还缺乏认识。本文以古田山24 ha大样地(划分为24个1 ha小样地)为基础, 具体分析了α多样性和β多样性在1 ha尺度上的空间变异特征。结果表明: (1)群落第一、二优势物种在各小样地之间变化不大, 但第三优势种变化较大; (2) α多样性变化中, 样地间木本植物个体数量变异最大, 物种丰富度其次, Pielou均匀度指数变异性最小; (3)物种丰富度与植株个体数量、Pielou均匀度指数没有显著的相关性, 与Shannon-Wiener指数呈显著正相关; Shannon-Wiener指数与Pielou均匀度指数呈显著正相关; (4)相邻样地间物种替代速率空间变异较大, 与物种丰富度的空间变化格局有明显差异。这些结果说明尺度对认识群落结构、探讨群落维持机制有重要作用; 由于森林群落是多尺度生态过程作用的结果, 大尺度样地可能有利于更好地揭示森林群落维持机制。     

不同物候时期华西雨屏区四个树种新鲜凋落物可提取腐殖质碳动态

凋落物的可提取腐殖质碳可随着植物生长节律及物候时期的变化而变化,并进而影响物质循环的过程,为深入了解以凋落物为载体的生态系统物质循环特征,该研究以华西雨屏区麻栎(Quercus acutissima)、楠木(Phoebe zhennan)、柳杉(Cryptomeria fortune)和喜树(Camptotheca acuminate)为对象,通过定点动态收集萌芽期、展叶期、盛叶期和落叶期的不同类型凋落物,分析其可提取腐殖质碳(extractable humus carbon,HC)、胡敏酸碳(humic acid carbon,HAC)、富里酸碳(fulvic acid carbon,FAC)以及胡敏酸碳/富里酸碳(humic acid carbon/fulvic acid carbon,HAC/FAC)的差异。结果表明:相对于其他凋落器官,在同一物候时期凋落叶中的HC和HAC含量都最高,大致都表现为凋落叶>凋落枝>凋落果,且在落叶树种中更为显著;相对于其他时期,展叶期四个树种凋落叶均表现出较高的FAC含量,但不同物候期凋落枝和凋落果的HAC含量以及FAC含量受物种的影响较大。尽管HAC/FAC在各器官间差异并不显著,但落叶树种相同器官的HAC/FAC低于常绿树种,表明落叶树种凋落物富里酸相对含量较高,形成速度相对较快,难降解程度也相对较大。统计分析表明关键时期、物种类型、器官类型及其相互作用对凋落物中HC、HAC、FAC含量和HAC/FAC均具有不同程度的影响,这为进一步深入认识区域生态系统以凋落物为载体的物质循环过程提供了理论依据及新的思路。     

华西雨屏区亮叶桦凋落叶分解对模拟氮沉降的响应

从2008年1月至2009年2月, 对华西雨屏区亮叶桦(Betula luminifera)人工林进行了模拟氮(N)沉降试验, N沉降水平分别为对照(CK, 0 g N·m^-2·a^-1)、低N (5 g N·m^-2·a^-1)、中N (15 g N·m^-2·a^-1)和高N (30 g N·m^-2·a^-1)。利用凋落袋法对亮叶桦凋落叶进行原位分解试验, 并在每月下旬定量地对各处理施N (NH₄NO₃)。结果表明, 虽然华西雨屏区大气N沉降量较高, 但模拟N沉降试验表明: 在N沉降继续增加的情况下, 凋落叶分解这一碳(C)循环和养分循环过程仍会受到显著影响。在1年的分解试验中, 模拟N沉降显著抑制了亮叶桦凋落叶的分解, N沉降处理使得凋落叶质量损失95%的时间在2.65年的基础上增加了1.14-1.96年。N沉降抑制凋落叶分解的原因在于无机N的富集对木质素和纤维素的分解造成阻碍。N沉降处理也导致C、N、磷、钾和镁元素在凋落物中的残留量增加, 但N沉降加速了钙元素的释放。凋落物基质化学特性在很大程度上决定了凋落物分解对N沉降的响应方向, 以及凋落物分解过程中各元素的动态变化。     

Study on successions sequence of evergreen broad-leaved forest in Gutian Mountain of Zhejiang, Eastern China:species diversity

Using the widely adopted scheme of space-for-time substitution for investigating 16 typical plots distri-buted as a pattern of contiguous grid quadrates within a sampling plot, the expressions of Shannon-Wiener index (H) for species diversity, Pielou index (Jsw, JSI) for evenness and Simpson index (D) for ecological dominance are employed to investigate the species diversity (SD) of four evergreen broadleaved communities in the successions sequence within the Nature Reserve of the Gutian Mountains. Results showed that in the successions process from the coniferous to the mixed coniferous-broadleaved, then to Schima superba and finally to Castanopsis eyrei forest, the arbor layer SD showed the Shannon-Wiener index (H) as 1.9670, 2.4975, 2.6140 and 2.4356, respectively, characterized by their rise before drop and the shrub (herb) layer SD shows the maximum to be in the mixed coniferous-broadleaved (coniferous) forest (H arriving at 2.8625 (1.5334)). In the vertical structure, on the other hand, for the sequenced coniferous forest, coniferous-broad mixed forest and Castnaopsis eyrei forest, the number of SD ranges in a decreasing order from the shrub, arbor to herb layer in contrast to the SD in a decreasing order of Schima superba forest ranging from the arbor to shrub and then to herb layer, and during the succession, the herb layer exhibits the maximum range of SD change among these layers, with its variation coefficients of 0.1572, 0.0806, 0.0899 and 0.1884 for H, Jsw, JSI and D, in order, in sharp contrast to the minimal SD range in the shrub layer, with the corresponding figures of 0.0482, 0.0385, 0.0142, and 0.1553.     

Study on successions sequence of evergreen broad-leaved forest in Gutian Mountain of Zhejiang, Eastern China: species diversity

Using the widely adopted scheme of space-for-time substitution for investigating 16 typical plots distributed as a pattern of contiguous grid quadrates within a sampling plot, the expressions of Shannon-Wiener index (H) for species diversity, Pielou index (J _sw , J _SI ) for evenness and Simpson index (D) for ecological dominance are employed to investigate the species diversity (SD) of four evergreen broadleaved communities in the successions sequence within the Nature Reserve of the Gutian Mountains. Results showed that in the successions process from the coniferous to the mixed coniferous-broadleaved, then to Schima superba and finally to Castanopsis eyrei forest, the arbor layer SD showed the Shannon-Wiener index (H) as 1.9670, 2.4975, 2.6140 and 2.4356, respectively, characterized by their rise before drop and the shrub (herb) layer SD shows the maximum to be in the mixed coniferous-broadleaved (coniferous) forest (H arriving at 2.8625 (1.5334)). In the vertical structure, on the other hand, for the sequenced coniferous forest, coniferous-broad mixed forest and Castnaopsis eyrei forest, the number of SD ranges in a decreasing order from the shrub, arbor to herb layer in contrast to the SD in a decreasing order of Schima superba forest ranging from the arbor to shrub and then to herb layer, and during the succession, the herb layer exhibits the maximum range of SD change among these layers, with its variation coefficients of 0.1572, 0.0806, 0.0899 and 0.1884 for H, J _SW , J _SI and D, in order, in sharp contrast to the minimal SD range in the shrub layer, with the corresponding figures of 0.0482, 0.0385, 0.0142, and 0.1553. __________ Translated from Chinese Journal of Ecology, 2006, 25(6): 603-C606 [译自: 生态学杂志]     

Changes of vascular plant diversity along a chronosequence of beech coppice stands,central Apennines,Italy

Abstract

This research sought to understand the patterns of vegetation recovery after disturbances because of coppice management in beech forests. Eighty sampling units from the mountain belt of the Marche region (Apennines, Italy) were collected according to a stratified sampling based on their geological setting (limestone, sandstone), elevation classes and age after last coppicing (to represent a chronosequence, from 1 to 90 years). The expected successional trend of decreasing species richness was confirmed, together with some stabilisation processes for older stand ages. However, more complex diversity patterns were found when total species richness was decomposed into the species richness of five social behaviour types (SBTs), defined based on the species' habitat preference. On both bedrocks, temporal gradients explained the observed diversity changes at the stand level: forest specialists increased whereas non-forest species decreased. A relatively long time after coppicing (40–60 years), the contribution of the beech specialist species doubled, whereas non-forest and species from anthropogenic habitats decreased by about 50%. On sandstone, the contribution of gap species also decreased over a long-period, and the beech stands experienced stronger changes over time. We conclude that the decomposition of total species richness in terms of SBT affords the opportunity to identify temporal references for thresholds which can be used to assess plant diversity status in relation to management schedules and conservation policy decisions.     

模拟氮沉降对华西雨屏区苦竹林凋落物基质质量的影响

凋凋落物基质质量是影响凋落物分解速率的决定性因子之一,本研究旨在探究模拟氮沉降对苦竹林凋落物基质质量的影响。2007年11月至2010年12月每月一次连续对华西雨屏区苦竹人工林进行了模拟氮沉降试验,施氮水平分别为：低氮（5 g N?m–2?a–1）,中氮（15 g N?m–2?a–1）和高氮（30 g N?m–2?a–1）。在施氮2 a后,于2010年1月开始收集各样方的凋落物样品,连续收集12个月,分析测定凋落物基质质量。结果表明：施氮显著增加了凋落叶中N、P元素含量,中氮处理显著增加了凋落枝中N元素含量,中氮和高氮处理均显著增加了凋落枝中P元素含量;施氮对凋落物中C元素含量影响很微弱,显著降低了凋落叶中的C/N,中氮处理显著降低了凋落枝中的C/N,对木质素和纤维素含量均未造成显著影响。由于模拟氮沉降增加了苦竹凋落物的N、P含量,降低了其C/N,因此氮沉降可能会促进苦竹凋落物的初期分解速率。