甜槠凋落叶分解中土壤节肢动物群落结构动态及其对森林片段化的响应

选取浙、闽、赣交界山地5个不同的常绿阔叶林群落(1处连续森林和4处片段化森林),对优势种甜槠凋落叶分解过程中土壤节肢动物动态进行了研究.5个研究样地共获得土壤节肢动物899头,分属9纲25目,其中鳞翅目占个体总数的10%以上,为优势类群;膜翅目、弹尾目、双翅目、前气门亚目和地蜈蚣目为常见类群.凋落叶分解速率与土壤节肢动物的类群数、个体数随季节动态呈现相一致的变化趋势.8月凋落物分解最快,土壤节肢动物类群和个体数最多;而4至6月和12月情况与之相反.片段化森林和连续森林在土壤节肢动物的类群数、个体数和物种多样性方面均显示出差异,面积效应和边缘效应在其中都起了一定的作用.     

亚热带森林凋落叶分解过程土壤节肢动物群落的变化特征

土壤动物群落结构和多样性可能随凋落物分解进程和基质质量的变化不断改变。为了解亚热带森林凋落叶分解过程中土壤节肢动物群落变化特征,以四川盆地亚热带森林麻栎（Quercus acutissima）和柳杉（Cryptomeria fortunei）凋落叶为对象,于2011-2015年采用分解袋法研究了2种凋落叶分解过程中土壤节肢动物组成、结构和多样性动态变化。整个研究期间,柳杉和麻栎凋落叶分解袋中共捕获土壤节肢动物3855只,分属于16目51科,且均以等节跳科和棘跳科为优势类群;麻栎凋落叶中土壤节肢动物的个体密度随分解进程呈现增加趋势,在分解的1079天达最高值后降低,而柳杉凋落叶则在分解的156天急剧增加后快速降低,2种凋落叶中土壤节肢动物类群数量具有相似的动态变化过程;2种凋落叶中土壤节肢动物总体以菌食性数量比例最高,腐食性最低,且随凋落叶分解进程,植食性土壤节肢动物占比明显下降,菌食性则上升;非度量多维尺度（NMDS）分析显示,2种凋落叶中土壤节肢动物群落组成具有显著差异,聚类分析表明,2种凋落叶土壤节肢动物群落结构相似性随分解进程不断降低。亚热带森林凋落叶分解过程中土壤节肢动物群落组成、结构和多样性受凋落叶类型影响。     

热带季节雨林凋落叶分解过程中的中小型土壤节肢动物的群落结构及动态

2000年5月-2001年4月,采用尼龙网袋法,以西双版纳热带季节雨林混合凋落叶作为分解基质,在3个季节雨林样地开展分解实验,对实验过程中分解袋内的中小型土壤节肢动物(meso—microarthropod)进行取样调查。根据所获数据探讨了中小型土壤节肢动物群落在分解过程中的结构和动态。结果显示：(1)在季节雨林凋落叶分解过程中,中小型土壤节肢动物群落组成始终以弹尾目和蜱螨目相对数量较高(均在30％以上),成为优势类群。(2)分解中期,土壤节肢动物群落多样性指数,类群、个体及重要类群的数量均处于整个分解过程中的较高水平,分解初期和后期相对较低,且波动性大,其中分解初期各多样性指标在波动过程中呈逐步增长趋势,而后期逐步降低,其变化过程受凋落叶数量和质量、林地降雨量变化的影响。土壤动物群落类群和个体相对密度(每克凋落叶干重的类群数和个体数)的变化可在一定程度上反映土壤动物与凋落物质量的动态关系。(3)不同样地间,土壤节肢动物群落结构及动态差异在分解前期不明显,而分解后期差异有所增加,但3样地凋落叶分解物质损失率没有明显差异。     

哀牢山不同类型亚热带森林地表凋落物及土壤节肢动物群落特征

分别于2005年4月（干热季）、6月（雨季）和12月（干热季）,采用样线法对哀牢山中山湿性常绿阔叶林、山顶苔藓矮林和滇山杨次生林地表凋落物及其中的土壤节肢动物群落进行了调查.结果表明： 凋落物现存总量、C储量和C/N在干、湿季均表现为苔藓矮林＞滇山杨林＞常绿阔叶林,N储量差异不大.蜱螨目和弹尾目是3林地凋落物层节肢动物群落的优势类群,双翅目幼虫、鞘翅目、蚁类和同翅目为常见类群,3林地凋落物层土壤节肢动物群落相似性系数极高.3林地凋落物层土壤节肢动物群落密度(ind·m^-2)没有显著差异,但相对密度(ind·g^-1)呈现出常绿阔叶林和滇山杨林显著高于苔藓矮林;土壤节肢动物密度季节变化呈现干季（4月和12月）显著高于雨季（6月）,群落香农多样性指数差异不显著.干热季(4月)3林地枯枝落叶现存量与其土壤节肢动物群落和主要类群密度呈显著正相关关系,而在干冷季(12月)凋落物总现存量与其土壤节肢动物群落及蜱螨目相对密度则呈显著负相关关系;弹尾目和鞘翅目密度与地表凋落物层的N储量也有显著的正相关关系.哀牢山亚热带森林凋落物及其土壤节肢动物群落的发展与森林植被结构密切相关, 其群落个体数量和多样性受森林地表凋落物的调控, 但林内其他环境因素如温湿度对森林凋落物层土壤动物个体数的季节变动也有明显影响.     

不同演替阶段热带森林地表凋落物和土壤节肢动物群落特征

为了解不同演替阶段热带森林土壤节肢动物群落结构特征及其与地表凋落物的关系, 2001年9月采用样线调查法对西双版纳23年次生林、35年次生林、季节雨林地表凋落物及其中的土壤节肢动物进行了调查。所获数据表明, 地表凋落物数量(现存量干重)和质量(N和C/N)总体上表现为35年次生林最好, 23年次生林次之; 蜱螨目和弹尾目为3林地地表凋落物土壤节肢动物群落优势类群, 膜翅目蚂蚁、马陆目、鞘翅目、双翅目和半翅目为常见类群。土壤节肢动物个体密度和个体相对密度均表现为35年次生林>季节雨林>23年次生林。群落的丰富度指数以季节雨林最高, 多样性和均匀度指数显示为23年次生林最高, 35年次生林的优势度指数最高, 3林地土壤节肢动物群落类群组成相似性达到较好水平。相关分析表明, 3种不同演替阶段热带森林土壤节肢动物个体密度与林地地表凋落物现存量呈正相关, 而现存凋落物N元素储量与土壤节肢动物的相关性仅表现在23年次生林和季节雨林。研究认为, 热带森林土壤节肢动物群落的发展与森林植被演替密切相关, 其群落个体数量和多样性受森林地表凋落物数量、质量的调控, 但其他环境因素如捕食效应、人为干扰等影响亦不可忽视。     

北京市海淀区土壤节肢动物群落特征

掌握城市土壤节肢动物的群落结构和物种组成对保护城市物种多样性具有重要意义.用手拣法和干漏斗法对北京市土壤节肢动物进行调查,共得土壤节肢动物样本4 984个,隶属6纲16目,共36个类群,其中蜱螨目、蚁科和弹尾目是优势类群,分别占个体总数的32.60%,27.83%,26.91%.不同功能区土壤节肢动物群落特征不同,平均密度为公园＞机关单位＞校园＞工业区＞交通干线＞住宅区,丰富度为公园＞交通干线＞校园＞工业区＞机关单位＞住宅区.不同地表植被状况下,土壤节肢动物的平均密度、丰富度和多样性指数排序均为林地＞草地＞行道树＞裸地.另外土壤节肢动物的个体数和类群数随着土层的加深而减少.北京市土壤节肢动物群落组成与同地带森林生态系统土壤节肢动物群落组成基本相同.     

森林-草原交错带土壤节肢动物群落多样性

在河北北部的塞罕坝森林草原交错区进行了土壤节肢动物群落组成与多样性调查,共获得土壤节肢动物25类,10420头,分属于6纲24目.交错区地带土壤节肢动物群落优势类群为弹尾目和蜱螨目,常见类群有8类,稀有类群15类.群落的多样性分析表明,森林带的多样性指数(H′)、密度-类群指数(DG)和均匀度指数较大,而草甸草原带各种指数较小.pH值与土壤节肢动物的类群数关联度较大,而温度和含水量与土壤节肢动物的个体数关联度较大.     

土壤节肢动物对箭竹凋落叶分解过程中酶活性的影响

为了解凋落物分解过程中土壤节肢动物与土壤酶活性的相互联系,以川西亚高山森林箭竹(Fargesia spathacea)凋落叶为对象,通过原位控制实验,于2016年4月至2018年4月研究了土壤节肢动物对凋落叶分解过程中碳、氮和磷转化相关酶活性的影响。结果表明:生物抑制剂施用降低了分解袋中土壤节肢动物49.7%～66.8%的个体密度和19.2%～46.3%的类群数量;对照和处理分解袋中凋落叶碳、氮和磷转化相关酶活性随分解过程呈现相似的动态;与处理相比,土壤节肢动物参与(对照)显著提高了凋落叶分解过程中蔗糖酶、β-葡聚糖苷酶、纤维素酶、多酚氧化酶、过氧化物酶、N-乙酰-β-D-氨基葡萄糖苷酶和酸性磷酸酶活性;土壤节肢动物对凋落叶分解过程中酶活性的贡献率在达到一个明显的峰值后快速降低;土壤温度和土壤节肢动物类群数量与蔗糖酶活性呈显著正相关,与β-葡聚糖苷酶、纤维素酶、多酚氧化酶、过氧化物酶、N-乙酰-β-D-氨基葡萄糖苷酶和酸性磷酸酶活性呈显著负相关。土壤节肢动物对凋落叶分解过程中酶活性促进效应随酶类型和分解时间变化存在差异,与土壤节肢动物群落结构和分解环境密切相关。     

土壤节肢动物对箭竹凋落叶分解过程中酶活性的影响

为了解凋落物分解过程中土壤节肢动物与土壤酶活性的相互联系,以川西亚高山森林箭竹(Fargesia spathacea)凋落叶为对象,通过原位控制实验,于2016年4月至2018年4月研究了土壤节肢动物对凋落叶分解过程中碳、氮和磷转化相关酶活性的影响。结果表明:生物抑制剂施用降低了分解袋中土壤节肢动物49.7%~66.8%的个体密度和19.2%~46.3%的类群数量;对照和处理分解袋中凋落叶碳、氮和磷转化相关酶活性随分解过程呈现相似的动态;与处理相比,土壤节肢动物参与(对照)显著提高了凋落叶分解过程中蔗糖酶、β-葡聚糖苷酶、纤维素酶、多酚氧化酶、过氧化物酶、N-乙酰-β-D-氨基葡萄糖苷酶和酸性磷酸酶活性;土壤节肢动物对凋落叶分解过程中酶活性的贡献率在达到一个明显的峰值后快速降低;土壤温度和土壤节肢动物类群数量与蔗糖酶活性呈显著正相关,与β-葡聚糖苷酶、纤维素酶、多酚氧化酶、过氧化物酶、N-乙酰-β-D-氨基葡萄糖苷酶和酸性磷酸酶活性呈显著负相关。土壤节肢动物对凋落叶分解过程中酶活性促进效应随酶类型和分解时间变化存在差异,与土壤节肢动物群落结构和分解环境密切相关。     

下辽河平原不同土地利用方式下土壤微节肢动物群落结构研究

2000年10月～2001年10月对下辽河平原地区撂荒、林地、旱田、水田4种不同土地利用方式的土壤微节肢动物进行了调查。应用个体数密度、类群丰富度、多样性指数和均匀度4个群落参数,研究了土壤微节肢动物的群落结构和季节变化。结果表明,撂荒中土壤微节肢动物的4个群落参数均为最高,旱田均为最低,季节变化影响土壤微节肢动物的群落结构,但土地利用方式不影响群落结构的季节变化型,下辽河平原地区不同土地利用方式共鉴定出土壤微节肢动物12个类群,撂荒、林地、旱田中弹尾目(Collembola)和蜱螨目(Acarina)为优势类群,双翅目(Diptera)、鞘翅目(Coleoptera)和膜翅目(Hymenoptera)为常见类群,水田中弹尾目、蜱螨目和双翅目为优势类群,鞘翅目为常见类群,各土地利用方式、各季节均在表层土壤出现的类群最多、密度最高,中层次之,底层最少。     

三种相思人工林和木荷林凋落叶分解的动态分析

对3种相思（Acacia Mill．）人工林和木荷（Schima superba Gardn．et．Champ．）林凋落叶的分解速率及磷和钾的动态变化进行了研究。结果表明,在分解过程中,卷荚相思（A．cincinnata F．Muell．）林、黑木相思（A．melanoxylon R．Br．）林、马占相思（A．magium Willd．）林和木荷林凋落叶干质量残留率分别为24．37％、13．51％、12．49％和41．86％,其中马占相思林的年分解系数最大,木荷林最小。凋落叶的磷含量大多呈上升趋势,其中黑木相思林和马占相思林表现为磷的净释放;卷荚相思林则在分解过程的前180d内表现为净固持,180d后表现为净释放;木荷林基本表现为磷的净固持。凋落叶的钾含量均为单调下降,且各林分均呈现出钾的净释放,分解末期各林分的钾释放率达90．14％～98．72％。与木荷林相比,3种相思人工林对土壤养分含量,特别是磷含量的维持非常有益。     

Leaf litter decomposition rates in degraded and fragmented tropical rain forests of Borneo

Previously extensive tracts of primary rain forest have been degraded by human activities, and we examined how the effects of forest disturbance arising from habitat fragmentation and commercial selective logging affected ecosystem functioning in these habitats by studying leaf litter decomposition rates in litter bags placed on the forest floor. The rain forests of Borneo are dominated by trees from the family Dipterocarpaceae, and we compared leaf litter decomposition rates of three dipterocarp species at eight forest fragment sites (area 3–3529 ha) that had different histories of disturbance pre‐fragmentation: four fragments had been selectively logged prior to fragmentation and four had been formed from previously undisturbed forest. We compared these logged and unlogged forest fragments with sites in continuous forest that had been selectively logged (two sites) and fully protected and undisturbed (two sites). After 120 d, undisturbed continuous forest sites had the fastest rates of decomposition (52% mass loss). Forest fragments formed from unlogged forest (32% mass loss) had faster decomposition rates than logged forest fragments (28% mass loss), but slower rates than continuous logged forest (39% mass loss). Leaves of a light‐demanding species (Parashorea malaanonan) decomposed faster than those of a shade‐tolerant species (Hopea nervosa), but decomposition of all three dipterocarp species that we studied responded similarly to logging and fragmentation effects. Reduced decomposition rates in logged and fragmented forest sites may affect nutrient cycling and thus have detrimental consequences for forest regeneration. Conservation management to improve forest quality should be a priority, particularly in logged forest fragments.     

Species-specific characteristics of trees can determine the litter macroinvertebrate community and decomposition process below their canopies

This paper tests whether individual trees in a mature forest stand influence the process of litter decomposition and the macroinvertebrate communities in the soil underneath their canopies, as a result of species-specific characteristics. A field decomposition experiment was performed in a mature forest stand of tropical montane cloud forest in Mexico. The areas under the canopies of Quercus laurina Humbl. & Bompl., Oreopanax xalapensis (Kunth) Decne. & Planchon and Beilschmedia ovalis (Blake) C. K. Allen trees were used as experimental units. The natural soil and litter macroinvertebrate communities were monitored and compared to the community that invaded decomposition boxes with reciprocally transplanted leaf litter. The abundances of four macroinvertebrate taxa in natural litter differed among tree species independently of season. No differences were found in the soil community. The response to experimental litter by macroinvertebrate taxa suggests that the production of a specific quality of litter is an important mechanism by which a tree influences the litter macroinvertebrate community that develops under its canopy. However, not all differences in community composition naturally found between tree species can be explained by differences in litter quality during the first year of decomposition. Differences in nutrient release that occur after the first year, and physical properties of litter also probably play an important role. Independently of the canopy tree, the initial chemical quality (N, P, Ca, Mg and lignin) of experimental litter largely determined the decomposition rate and nutrient dynamics of decomposing leaves. However, it was found that under O. xalapensis trees the breakdown of lignin from the litter produced by the same species of tree was particularly effective. This suggests that a feedback has developed between this tree species and the decomposer community prevailing under its canopy.     

不同起源时间的植物叶凋落物在中亚热带的分解特性

选择9种起源时间不同的植物的凋落叶,采用分解袋法,在浙江千岛湖地区从2006年6月到2008年6月进行了分解试验,试图探索植物进化过程中凋落物分解特性的演变趋势.所选的9种植物分属于4个类群,按起源时间由早到晚依次为蕨类植物(芒萁和桫椤)、裸子植物(苏铁、水杉、杉木和马尾松)、双子叶植物(木荷和青冈)及单子叶植物(毛竹).每隔一个月取样,每种凋落物3次重复.结果表明:不同植物类群凋落物基质的氮(N)、木质素(Lignin)含量及Lignin/N比值与分解速率具有良好的相关性.起源时间越晚的植物凋落物的基质N含量越高,为单子叶植物>双子叶植物>裸子植物>蕨类植物.Lignin含量和Lignin/N比值的趋势一致,均为起源时间越晚而值越低,即蕨类植物>裸子植物>双子叶植物>单子叶植物.凋落物分解系数k值的范围在0.25～0.63之间,表现出毛竹>青冈>木荷>水杉>马尾松>杉木>苏铁>桫椤>芒萁的趋势.4个植物类群的凋落物分解速率的均值为单子叶植物>双子叶植物>裸子植物>蕨类植物.试验结果初步表明:植物凋落物分解的进化趋势是由分解缓慢逐渐演变为分解较快.     

全球气候变暖对凋落物分解的影响

凋落物分解作为生态系统核心过程,参与生态系统碳的周转与循环,影响生态系统碳的收支平衡,调控生态系统对全球气候变暖的反馈结果。全球气候变暖通过环境因素、凋落物数量和质量以及分解者3个方面,直接或间接地作用于凋落物分解过程,并进一步影响土壤养分周转和碳库动态。气候变暖可通过升高温度和改变实际蒸散量等环境因素直接作用于凋落物分解。气候变暖可引起植物物种短期内碳、氮和木质素等化学性质的改变以及群落中物种组成的长期变化从而改变凋落物质量。在凋落物分解过程中,土壤分解者亚系统作为主要生命组分(土壤动物和微生物)彼此相互作用、相互协调共同参与调节凋落物的分解过程。凋落物分解可以通过改变土壤微生物量、微生物活动和群落结构来加快微生物养分的固定或矿化,以形成新的养分利用模式来改变土壤有机质从而对气候变化做出响应。未来凋落物分解的研究方向应基于大尺度跨区域分解实验和长期实验,关注多个因子交互影响下,分解过程中碳、氮养分释放、地上/地下凋落物分解生物学过程与联系、分解者亚系统营养级联效应等方面。     

青冈林土壤动物群落结构在落叶分解过程中的演替变化

１９９３年５月－１９９５年４月,采用落叶袋法研究了中亚热带青冈（Ｃｙｃｌｏｂａｌａｎｏｐｓｉｓｇｌａｕｃａ）林土壤动物在落叶分离过程中的演替,变化,用多样性指数,演替指数,相似系数分析土壤动物群落结构的季节变化和在落叶分解过程中的演替,分解出现的类群,密度最高的为蜱螨目（Ａｃａｒｉｎａ）其次为弹尾目（Ｃｏｌｌｅｍｂｏｌａ）,二者个体数之和占总数的９２．７％,其他依次为：双翅目（Ｄｉｐｔｅｒａ）膜翅     

Fungal community composition in neotropical rain forests: the influence of tree diversity and precipitation

Plant diversity is considered one factor structuring soil fungal communities because the diversity of compounds in leaf litter might determine the extent of resource heterogeneity for decomposer communities. Lowland tropical rain forests have the highest plant diversity per area of any biome. Since fungi are responsible for much of the decomposition occurring in forest soils, understanding the factors that structure fungi in tropical forests may provide valuable insight for predicting changes in global carbon and nitrogen fluxes. To test the role of plant diversity in shaping fungal community structure and function, soil (0-20?cm) and leaf litter (O horizons) were collected from six established 1-ha forest census plots across a natural plant diversity gradient on the Isthmus of Panama. We used 454 pyrosequencing and phospholipid fatty acid analysis to evaluate correlations between microbial community composition, precipitation, soil nutrients, and plant richness. In soil, the number of fungal taxa increased significantly with increasing mean annual precipitation, but not with plant richness. There were no correlations between fungal communities in leaf litter and plant diversity or precipitation, and fungal communities were found to be compositionally distinct between soil and leaf litter. To directly test for effects of plant species richness on fungal diversity and function, we experimentally re-created litter diversity gradients in litter bags with 1, 25, and 50 species of litter. After 6?months, we found a significant effect of litter diversity on decomposition rate between one and 25 species of leaf litter. However, fungal richness did not track plant species richness. Although studies in a broader range of sites is required, these results suggest that precipitation may be a more important factor than plant diversity or soil nutrient status in structuring tropical forest soil fungal communities.     

Distinct Bacterial Communities Dominate Tropical and Temperate Zone Leaf Litter

Little is known of the bacterial community of tropical rainforest leaf litter and how it might differ from temperate forest leaf litter and from the soils underneath. We sampled leaf litter in a similarly advanced stage of decay, and for comparison, we also sampled the surface layer of soil, at three tropical forest sites in Malaysia and four temperate forest sites in South Korea. Illumina sequencing targeting partial bacterial 16S ribosomal ribonucleic acid (rRNA) gene revealed that the bacterial community composition of both temperate and tropical litter is quite distinct from the soils underneath. Litter in both temperate and tropical forest was dominated by Proteobacteria and Actinobacteria, while soil is dominated by Acidobacteria and, to a lesser extent, Proteobacteria. However, bacterial communities of temperate and tropical litter clustered separately from one another on an ordination. The soil bacterial community structures were also distinctive to each climatic zone, suggesting that there must be a climate-specific biogeographical pattern in bacterial community composition. The differences were also found in the level of diversity. The temperate litter has a higher operational taxonomic unit (OTU) diversity than the tropical litter, paralleling the trend in soil diversity. Overall, it is striking that the difference in community composition between the leaf litter and the soil a few centimeters underneath is about the same as that between leaf litter in tropical and temperate climates, thousands of kilometers apart. However, one substantial difference was that the leaf litter of two tropical forest sites, Meranti and Forest Research Institute Malaysia (FRIM), was overwhelmingly dominated by the single genus Burkholderia, at 37 and 23 % of reads, respectively. The 454 sequencing result showed that most Burkholderia species in tropical leaf litter belong to nonpathogenic “plant beneficial” lineages. The differences from the temperate zone in the bacterial community of tropical forest litter may be partly a product of its differing chemistry, although the unvarying climate might also play a role, as might interactions with other organisms such as fungi. The single genus Burkholderia may be seen as potentially playing a major role in decomposition and nutrient cycling in tropical forests, but apparently not in temperate forests.