鄂尔多斯高原生态过渡带的判定及生物群区特征

本文用Holdridge生命地带方法对鄂尔多斯高原的生物群区进行了分类研究,研制了用于生态过渡带判定的计算机模型,模拟结果与实际情况基本吻合。鄂尔多斯高原的生物群区可分为草原、荒漠灌丛和荒漠3大类,草原群区以本氏针茅(Stipa bungeana)群落为主,荒漠灌丛群区以冷蒿(Artemisia frigida),狭叶锦鸡儿(Caragana stenophylla)群落为主,荒漠群区以红砂(Reaumuria soongorica)群落为主。鄂尔多斯高原的地带性植被在传统上分为典型草原、荒漠草原和草原化荒漠3部分,在典型草原的边界划分上,传统划分与本文结果一致。而在荒漠草原和草原化荒漠的边界方面,模拟结果与传统划分有一定的差异。荒漠灌丛和荒漠草原以及荒漠和草原化荒漠在生物群落特征上具有一定的相似性,荒漠灌丛和荒漠在生态特征上较荒漠草原和草原化荒漠更为旱化,在地理位置上更为靠西部。该计算机模型结合了地理空间分析,能准确地确定生态过渡带的位置和宽度,为研究鄂尔多斯高原生态过渡带的特征提供了较可靠的技术手段。     

小叶、中间和柠条三种锦鸡儿的分布式样及其生态适应

确定了小叶锦鸡儿、中间锦鸡儿和柠条锦鸡儿3种植物的分布式样:小叶锦鸡儿为蒙古高原东部-F松辽平原西部-华北山地分布种,中间锦鸡儿为东戈壁-鄂尔多斯高原-黄土高原北部分布种,柠条锦鸡儿为南阿拉善-西鄂尔多斯分布种。小叶锦鸡儿适应分布于蒙古高原典型草原带和森林草原带以及华北山地落叶阔叶林带,在草原带高平原上可形成灌丛化草原的景观,在草原带的沙地上可形成以小叶锦鸡儿为建群种的沙地灌丛植被;中间锦鸡儿适应分布于蒙古高原的荒漠化草原及草原化荒漠带、鄂尔多斯高原的典型草原和荒漠化草原带的沙地及梁地上、黄土高原北部的黄土丘坡上,常形成以中间锦鸡儿为建群种的沙地灌丛植被;柠条锦鸡儿则适应分布于草原化荒漠和典型荒漠带的固定和半固定沙地上。近缘的3种锦鸡儿的地带性分布从东至西或从北向南形成明显的有规律的地理替代分布格局。     

鄂尔多斯高原植物群落多样性时空变化特点

作者利用1999年和2000年野外植物群落调查资料,结合李博(1990)的植物群落调查结果,分析了鄂尔多斯高原植物群落多样性的时空变化特点。鄂尔多斯高原主要植物群落类型有23类,不同植被类型的群落多样性表现出一定的差异性,其中丰富度指数的差异不显著,而Simpson指数和Shannon-Wiener指数及群落盖度的差异明显。中东部典型草原表现为高多样性高盖度;西鄂尔多斯荒漠草原和草原化荒漠物种多样性较高,但盖度较低;毛乌素沙地植物群落物种多样性低,但盖度较高。从1986年到2000年,该地区典型草原群落、荒漠草原和沙地植被的群落多样性指数都有下降趋势;典型草原和草原化荒漠的群落盖度有所增加,荒漠草原有所下降。以上结果表明,沙地植被和草原化荒漠生物多样性已经得到了一定的保护,但还有待加强,而荒漠草原的保护亟待引起重视。     

人工灌丛化对荒漠草原生态系统碳储量的影响

宁夏盐池县从20世纪70年代开始在荒漠草原上人工种植柠条灌木用以防风固沙和生态恢复,这一人为措施极大地改变了区域生态系统的植被结构和碳循环,而定量评估人工灌丛化对荒漠草原生态系统碳储量的影响,不仅能够揭示人类活动的碳循环反馈机制,而且可为地方政府生态治理提供理论指导。结合Biome-BGC模型和Logistics生长模型模拟了1958—2017年间荒漠草原人工灌丛化前后的碳储量变化,定量分析了人工灌丛化对生态系统碳储量和组分的影响。结果表明:(1)结合Biome-BGC模型和Logistics生长模型可以较准确地模拟出荒漠草原人工灌丛化过程中生态系统碳储量的变化。(2)人工灌丛化会快速改变荒漠草原的碳储量累积特征,柠条灌木种植后的快速生长阶段极大增强了生态系统的总碳储量,导致生态系统的碳储量特征由草地型向灌木型转变。(3)人工灌丛化改变了生态系统各类型碳储量的组分结构,其对地上植被和枯落物碳储量的影响非常明显,灌丛化后生态系统的植被和枯落物碳分别增加了6倍和1.76倍;因植被碳向土壤碳转化过程较慢,故人工灌丛化对地下土壤碳储量的影响在短期内较为微弱。以上结果显示,荒漠草原人工灌丛化能显...     

小叶锦鸡儿(Caragana microphylla)灌丛对草本群落特征的影响

基于干旱、半干旱草原灌丛化现象的发展，探究灌木与草本之间的关系对深刻理解灌丛化对草原植物群落特征的影响机制具有重要意义。然而，很少有研究考虑草地类型和灌丛斑块大小对灌木和草本植物之间关系的影响。在内蒙古典型草原和荒漠草原的自由放牧草地上选择了18个小叶锦鸡儿灌丛化样地进行野外采样，并调查了不同大小灌丛和周围草地的植物群落特征。运用单因素方差分析(one-way ANOVA)和最小显著差异法(LSD)来检验不同大小灌丛斑块内外的植被群落特征(高度、密度、地上生物量、凋落物量)和植物多样性指数(Shannon-Wiener指数、Pielou指数、丰富度指数、群落Sprensen相似性系数)的差异性。结果表明：(1)与草地相比，两种草原类型的灌丛产生、捕获了更多的凋落物，灌丛的保育作用显著提高了斑块内草本植物的高度，但灌丛占用了生存空间和资源，从而降低了斑块内草本植物的密度和地上生物量。(2)灌丛对多年生草本植物的地上生物量有明显的抑制作用，但对两种草原类型的一、二年生草本植物没有显著影响(典型草原中的小灌丛除外)。(3)两种草原类型的灌丛对草本植物多样性的影响存在差异。典型草原灌丛内多样性...     

荒漠草原人工灌丛化对蒸散发及其组分的影响——以盐池县为例

我国西北防沙治沙工程中大量的种植中间锦鸡儿(Caragana intermedia)会导致荒漠草原发生灌丛化现象,研究人工灌丛化对荒漠草原蒸散发的影响,不仅能够揭示半干旱区人为活动对生态系统水循环的影响机理,还可以指导区域生态治理实践。以宁夏盐池县荒漠草原为例,基于植被的生理生态参数和荒漠草原水热条件,采用生物地球化学模型(Biome Bio-Geochemical Cycles,Biome-BGC)和地球呼吸系统模拟模型(Breathing Earth System Simulator,BESS)结合的方法,模拟荒漠草原生态系统人工灌丛引入前后蒸散发及其组分的变化,定量研究荒漠草原人工灌丛化对区域生态水文循环中蒸散发的影响。结果表明,人工灌丛的引入使植被结构及特征发生了变化,叶面积指数(Leaf Area Index,LAI)年最大值由0.20增加为0.67,改变了植被年内与年际变化特征。荒漠草原人工灌丛化后,生态系统年均蒸散发由251.74 mm增加到了281.42 mm;人工灌丛化对生长季的蒸散发增强明显,8月蒸散发峰值时,日均蒸散发由1.27 mm/d增加到1.56 mm/d。灌丛化过程使生态系统蒸腾量平均增加了1.35倍,蒸发量增加了1.06倍,改变了生态系统蒸散发的组分结构,导致蒸发比例降低、蒸腾比例增高。由此可知,荒漠草原在防沙治沙和生态治理中大量种植灌木的现象,加大了区域生态系统的蒸散发,并改变了水分耗散结构,从而对生态系统地气水汽交换有较大影响,研究结论对荒漠草原生态治理及未来的植被重建有一定的借鉴意义。     

气候变暖与荒漠-草原过渡带植物动态响应灰色分析--以美国新墨西哥州Sevilleta生态过渡带为例

在当前全球气候变暖的形势下,地表生态系统表现出不同的响应。干旱-半干旱地区的生态过渡带的生物反应更为敏感。美国新墨西哥州中部的荒漠-草原生态过渡带是监测全球气候变化和人类活动对生物影响的重要区域之一。本文以Sevilleta荒漠．草原生态过渡带为例,运用灰色系统分析方法．研究在当前全球气候变暖的条件下,1989～1998年10年间该生态过渡带的两种共存的植物优势种(Bouteloua eripoda)和(Bouteloua grncilis)历年的种群密度、组合形式和变化趋势,分析引起这些变化的主要气候因子。结果表明,Sevilleta生态过渡带中来自荒漠草原的优势物种Bouteloua eripoda的密度有上升的趋势,来自大草原的优势物种Bouteloua gracilis的密度有下降的趋势,它们的密度比大于1且有上升的趋势;在影响种群密度变化的降水、最高温度、最低温度、湿度的4个气候因子中,温度因子起着重要的作用。由此可以认为,随着气候的变暖,本区来自荒漠地区的优势植物种在荒漠-草原群落过渡带中将逐渐处于强优势地位,生态过渡带将有可能被荒漠草原所替代。     

小叶锦鸡儿灌丛化对典型草原群落结构与生态系统功能的影响

草原灌丛化是全球干旱半干旱地区面临的重要生态问题。灌丛化对草原生态系统结构与功能的影响较为复杂, 有待于在更广泛的区域开展研究。该研究在内蒙古锡林郭勒典型草原选择轻度、中度和重度灌丛化草地, 通过群落调查, 结合植物功能性状和土壤理化性质观测, 研究了小叶锦鸡儿(Caragana microphylla)灌丛化对草原群落结构(物种多样性、功能多样性和功能群组成)和生态系统功能(初级生产力、植被和土壤养分库)的影响。结果表明: 1)不同程度灌丛化草地的物种丰富度、功能性状多样性和群落加权性状平均值差异显著, 其中, 中度灌丛化草地的物种多样性和功能多样性较高, 表明一定程度的灌丛化有利于生物多样性维持。2)重度灌丛化草地的地上净初级生产力(ANPP)显著高于轻度和中度灌丛化草地, 其原因主要是随着灌丛化程度加剧, 群落内一/二年生草本植物显著增加, 而多年生禾草和多年生杂类草显著减少。三个灌丛化草地的植被叶片和土壤碳、氮库差异均不显著。3)灌丛化对草原生态系统功能包括ANPP、植被和土壤养分库均没有直接的影响, 而是通过影响功能群组成、土壤理化性质和功能多样性, 间接地影响生态系统功能; 灌丛化导致功能群发生替代和土壤旱碱化是最重要的生物和非生物因素。     

小叶锦鸡儿灌丛化对典型草原群落结构与生态系统功能的影响

草原灌丛化是全球干旱半干旱地区面临的重要生态问题。灌丛化对草原生态系统结构与功能的影响较为复杂,有待于在更广泛的区域开展研究。该研究在内蒙古锡林郭勒典型草原选择轻度、中度和重度灌丛化草地,通过群落调查,结合植物功能性状和土壤理化性质观测,研究了小叶锦鸡儿(Caragana microphylla)灌丛化对草原群落结构(物种多样性、功能多样性和功能群组成)和生态系统功能(初级生产力、植被和土壤养分库)的影响。结果表明:1)不同程度灌丛化草地的物种丰富度、功能性状多样性和群落加权性状平均值差异显著,其中,中度灌丛化草地的物种多样性和功能多样性较高,表明一定程度的灌丛化有利于生物多样性维持。2)重度灌丛化草地的地上净初级生产力(ANPP)显著高于轻度和中度灌丛化草地,其原因主要是随着灌丛化程度加剧,群落内一/二年生草本植物显著增加,而多年生禾草和多年生杂类草显著减少。三个灌丛化草地的植被叶片和土壤碳、氮库差异均不显著。3)灌丛化对草原生态系统功能包括ANPP、植被和土壤养分库均没有直接的影响,而是通过影响功能群组成、土壤理化性质和功能多样性,间接地影响生态系统功能;灌丛化导致功能群发生替代和土壤旱碱化是最重要的生物和非生物因素。     

基于茎流-蒸渗仪法的荒漠草原带人工灌丛群落蒸散特征

中国西北地区通过大量种植中间锦鸡儿(Caragana liouana)进行生态治理, 在荒漠草原带上形成人工灌丛景观, 改变了生态系统的结构和功能, 影响到地-气水汽循环过程, 研究该人工灌丛群落的蒸散特征, 对揭示其生态水文效应和指导地方生态治理实践具有重要意义。该文以宁夏盐池荒漠草原带上的人工灌丛群落为例, 利用茎流-蒸渗仪法测定了2018年5-8月的灌木蒸腾和丛下蒸散, 并分析了环境因子对人工灌丛群落蒸散的影响。结果表明: (1)茎流-蒸渗仪法所测的群落蒸散与水量平衡法、涡度相关法得到的群落蒸散有较好的一致性, 茎流-蒸渗仪法能适用于荒漠草原带人工灌丛群落蒸散及其组分结构的测定; (2)观测期内晴天的灌木蒸腾速率和丛下蒸散速率日变化趋势相近, 均为单峰曲线, 群落蒸散主要发生在日间, 但灌丛最大蒸腾速率的出现时间比丛下蒸散最大速率的出现时间晚1 h; (3) 5-8月间灌木累积蒸腾为83.6 mm, 日平均蒸腾量为0.7 mm·d^-1, 季节变化呈抛物线状; 同期丛下累积蒸散为182.5 mm, 日平均蒸散量为1.5 mm·d^-1; 丛下蒸散明显大于灌木蒸腾; (4)观测期间人工灌丛群落累积蒸散266.1 mm, 而同期的降水量为222.6 mm, 陆面水分收支处于亏缺状态; (5)净辐射是影响蒸散最主要、最直接的驱动因素, 且能够影响其他因子进而对人工灌丛群落蒸散产生作用。综上, 人工灌丛引发荒漠草原地带陆面水分收支亏缺的现象, 在生态恢复与重建中须引起注意。     

锦鸡儿属植物在鄂尔多斯高原区系和植被中的作用

锦鸡儿属植物在鄂尔多斯高原分布有9种。是物种多样性相对丰富的一个地区。其中中间锦鸡儿Caragana korshinskii var. intermedia,在鄂尔多斯高原东部和毛乌素沙地被当作优选的、广泛栽培的、习见的固沙和水土保持灌木树种。从植物区系成分上分析,主要是中亚成分和东亚成分,中亚成分有蒙古高原分布,阿拉善分布,戈壁-蒙古分布,内蒙古草原-黄土高原分布;东亚成分有华北分布,华北-青藏高原分布,以及蒙古高原南部-青藏高原成分。这些成分充分反映出这一地区与相邻地区的联系和过渡性。形成明显替代现象是本区东部的C. korshinskii var. intermedia与西部的C. korshinskii之间的替代。灌木种类是鄂尔多斯高原的优势生活型植物。在鄂尔多斯高原分布的14个主要灌木群落中,其中有4个重要的锦鸡儿群落,即中间锦鸡儿群系Form. Caragana korshinskii var. intermedia,狭叶锦鸡儿群系Form. Caragana stenophylla,柠条锦鸡儿群系Form. Caragana korshinskii,藏锦鸡儿群系Form. Caragana tibetica。中间锦鸡儿群系为优良的固沙和水土保持灌木。藏锦鸡儿群系则主要分布在西鄂尔多斯,为自然分布。在硬地及覆沙梁地形成高达40~80 cm的小沙丘包,在灌丛中占绝对优势,是锦鸡儿属植物在鄂尔多斯高原最典型的景观之一。这些锦鸡儿属植物群落对于揭示植被从东到西典型草原-荒漠化草原-荒漠的地带性分布具有典型的表征意义。     

An Ecogeographical Regionalization for Biodiversity in China

Ecogeographical regionalization is the basis for spatial differentiation of biodiversity research. In view of the principle of international ecogeographical regionalization, this study has applied multivariate analysis and GIS method and based on some ecogeographical attributes limited to the distribution of plant and vegetation, including climatic factors, such as minimum temperature, mean temperature of the coldest month, mean temperature of the wannest month, annual average temperature, precipitation of the coldest month, precipitation of the wannest month, annual precipitation, CV of annual precipitation, biological factors such as vegetation types, vegetation division types, NPP, fiorisitic types, fauna types, abundance of plant species, genus and endemic genus; soil factors such as soil types, soil pH;topographical factors as longitude, latitude and altitude etc. The ecogeographical regionalization for biodiversity in China was made synthetically by using fuzzy cluster method. Four classes of division were used, viz., biodomain, subbiodomain, biome and bioregion. Five biodomains, seven subbiodomains and eighteen biomes were divided in China as follows: Ⅰ Boreal forest biodomain. Ⅰ A Eurasian boreal forest subbiodomain. Ⅰ A1 Southern Taiga mountain cold-temperate coniferous forest biome; Ⅰ A2 North Asian mixed coniferous-broad-leaved forest biome. Ⅱ Northern steppe and desert biodomain. Ⅱ B Eurasian steppe subbiodomain. Ⅱ BI Inner Asian temperate grass steppe biome; Ⅱ B2 Loess Plateau warm-temperate forest/shmb steppe biome. Ⅱ C Asia-Mrica desert subbiodomain. Ⅱ C1 Mid-Asian temperate desert biome; Ⅱ C2 Mongolian/Inner Asian temperate desert biome. Ⅲ East Asian biodomain. Ⅲ D East Asian deciduous broad-leaved forest subbiodomain. Ⅲ D1 East Asian deciduous broad-leaved forest biome, Ⅲ E East Asian evergreen broad-leaved forest subbiodomain. Ⅲ El East Asian mixed deciduous-evergreen broad-leaved forest biome; Ⅲ E2 East Asian evergreen broad-leaved forest biome; Ⅲ E3 East Asian monsoon evergreen broad-leaved forest biome; Ⅲ FA Western East Asian mountain evergreen broadleaved forest biome. Ⅳ Palaeotropical subdomain. IV F India-Malaysian tropical forest subbiodomain.Ⅳ Fl Northern tropical rain forest/seasonal rain forest biome; Ⅳ F2 Tropical island coral reef vegetation biome. Ⅴ Asian plateau biodomain. Ⅴ G Tibet Plateau subbiodomain. Ⅴ G1 Tibet alpine highcold shrub meadow biome;Ⅴ G2 Tibet alpine high-cold steppe biome; Ⅴ G3 Tibet alpine high-cold desert biome; Ⅴ G4 Tibet alpine temperate steppe biome; Ⅴ G5 Tibet alpine temperate desert biome.     

Vegetation responses along environmental gradients on the Ordos plateau, China

The Ordos plateau is a unique ecotone and is a focal region for the campaign to reduce or reverse desertification in China. This paper explores the relationship between vegetation and environmental gradients on the Ordos plateau based on a field survey of species distribution, vegetation distribution patterns, plant community structure, ecophysiological properties, and soil water content along an environmental gradient. The vegetation on the Ordos plateau may be divided into three types from east to west: steppe (eastern part), desert steppe (middle part) and steppe desert (western part). From east to west, precipitation declines significantly (from 400 mm to 150 mm). The spatial distribution pattern of vegetation at different sites was random. The density of shrub islands decreased from east to west, and their height and diameter were negatively correlated with precipitation. From east to west, the transpiration rate increased as temperature increased. Stomatal conductance was positively correlated with percentage of sunshine hours and negatively correlated with temperature. Water-use efficiency was positively correlated with average annual precipitation but negatively correlated with increasing percentage of sunshine hours. The results suggest that for effective revegetation, highly drought-tolerant species, such as Caragana tibetica and C. stenophylla, should be used and a lower percentage of vegetation cover expected (30–40%) in the western half of the Ordos plateau. In the eastern half, moderately drought-tolerant species, such as Artemisia ordosica and C. korshinskii, could be used and a higher percentage vegetation cover expected (40–50%).     

Simulated distribution of vegetation types in response to climate change on the Tibetan Plateau

Abstract. Questions: What is the relationship between alpine vegetation patterns and climate? And how do alpine vegetation patterns respond to climate changes? Location: Tibetan Plateau, southwestern China. The total area is 2500000 km² with an average altitude over 4000 m. Methods: The geographic distribution of vegetation types on the Tibetan Plateau was simulated based on climatology using a small set of plant functional types (PFTs) embedded in the biogeochemistry‐biography model BIOME4. The paleoclimate for the early Holocene was used to explore the possibility of simulating past vegetation patterns. Changes in vegetation patterns were simulated assuming continuous exponential increase in atmospheric CO concentration, based on a transient ocean‐atmosphere simulation including sulfate aerosol effects during the 21st century. Results: Forest, shrub steppe, alpine steppe and alpine meadow extended while no desert vegetation developed under the warmer and humid climate of the early Holocene. In the future climate scenario, the simulated tree line is farther north in most sectors than at present. There are also major northward shifts of alpine meadows and a reduction in shrub‐dominated montane steppe. The boundary between montane desert and alpine desert will be farther to the south than today. The area of alpine desert would decrease, that of montane desert would increase. Conclusions: The outline of changes in vegetation distribution was captured with the simulation. Increased CO2 concentration would potentially lead to big changes in alpine ecosystems.     

Characteristics of desert flora and vegetation in lower reach of Shiyang River论Basin

石羊河下游位于干草原向荒漠过渡区域,有天然种子植物23个科,73个属,123个种,不仅有典型的戈壁荒漠成分,也渗入一些草原化荒漠植物种类.其荒漠植被特征更明显,群落层片结构简单,群丛建群种的74.4%是灌木和半灌木,构成了灌木、半灌木旱生群落;1年生草本植物随季节性降雨可形成＂灌草丛＂,成为荒漠植被的重要组成部分.在植物地理区系成分上,温带成分属占优势,其中地中海至中亚分布型及其变型最多,其次为北温带分布及其变型.整个区域内植物的分布集中在生境较适宜的区域,空间结构的成群性高,但在小区域内植物种的分布则较单一.植被可划分为4个植被型,5个植被亚型,13个群系组,23个群系,38个群丛.地域性植被以绿洲为中心,成环状分布,可分为3个带.     

Ecology of a steppe-tundra gradient in interior Alaska

Abstract. Subarctic steppe is currently restricted in interior Alaska and the Yukon Territory to steep, south-facing river bluffs. Paleoecological and biogeographic evidence suggests that some steppe taxa may have been more widespread during the Full-Glacial. We examined factors controlling the distribution of steppe taxa on an elevation gradient across a steppetundra ecotone; such analyses may help define potential Full-Glacial distributions of these taxa. Multivariate analyses suggest that species can be divided into four spatially distinct groups, but individualistic species distributions create considerable overlap among these groups. The steppe-tundra ecotone comprises a broad zone of mixing between steppe taxa and drought-tolerant alpine tundra taxa, followed by an abrupt shift to alpine shrub tundra. The transition from low steppe to tundra vegetation is primarily associated with a gradient of decreasing soil temperature. The more abrupt transition from mixed steppe-tundra to alpine shrub tundra vegetation is primarily associated with changes in soil depth and soil moisture. Variation in vegetation within steppe is associated with gradients in soil phosphorus and moisture. Greenhouse experiments on drought tolerance of two steppe and two tundra taxa suggest that the individualistic distribution of species along the ecotone is partly a function of physiological differences among species. Our analyses of vegetation-environment relationships support the hypothesis that some components of the steppe community could have been more widespread during the colder Full-Glacial.     

鄂尔多斯高原地区昆虫物种多样性研究

鄂尔多斯高原有特殊生境类型,本文研究了该地区的昆虫物种多样性变化及影响因素,得到以下结果：（1）利用巴氏罐诱法得到昆虫标本约5159号,其他无脊椎动物标本291号,鞘翅目为优势昆虫类群,其数量占昆虫标本总数的45．8％,其中拟步甲和步甲个体数量较多,占所有甲虫总数92．8％;（2）根据甲虫的物种多样性和丰富度的特点将4个调查地点分为两组：一组为以荒漠灌丛为主的杭锦旗和植被类型多样化的石灰庙,物种多样性指数,丰富度和个体数量较高;另一组为以人工植被区为主的石龙庙和新街镇,物种均匀度指数较高;（3）主成分排序（PCA）可以将该地区的甲虫群落分为人工植被区和荒漠植被区2种类型,反映降水和植被类型是决定甲虫群落组成的关键因素;（4）降水梯度对甲虫物种多样性有很大影响,物种多样性指数,均匀度指数与降水梯度呈显著的正相关关系;个体数量与降水梯度呈显著的负相关关系;物种的丰富度与降水梯度没有相关关系。以上结果表明,在鄂尔多斯高原地区,只有减少人为干扰,加强保护脆弱的原有植被,才能保护特有的昆虫种类;只有大力开展固沙造林植草,才能改善环境,提高该地区的昆虫物种多样性。     

内蒙古高原针茅草原群落土壤水分和碳、氮分布的小尺度空间异质性

用地统计学的方法,研究比较了内蒙古高原4类地带性针茅草原群落,贝加尔针茅（Stipa baicalensis)群落,大针茅（S.grandis)群落,克氏针茅（S.krylovii)群落和小针茅（S.kelemenzii)群落0-20cm土壤水分和碳,氮的小尺度空间异质性特征,结果表明;4类群落土壤水分,有机碳和全氮均表现出显著的小尺度空间结构特征。自相关尺度为1.91m-10.81m,结构性方差占样本方差的35.31%-99.74%。从贝加尔针茅群落到小针茅群落空间自相关的尺度逐渐增大,纹理有逐渐变粗的趋势,土壤水分,碳和氮的小尺度空间格局共同作用于群落的生态学过程,即土壤水分格局→植物种群格局（基本斑块的大小）→土壤碳空间格局→土壤氮空间格局,同时,由于生态学过程的反馈作用,土壤氮空间格局→种群格局→土壤水分格局,土壤属性空间自相关尺度的改变可能是导致群落演替的驱动力,草原退化可能与土壤异质性尺度的改变相关。