黄土丘陵沟壑区森林生态系统生态化学计量特征

为了阐明黄土丘陵沟壑区森林生态系统植物与土壤之间的养分循环关系,明确叶片与乔木层整体生态化学计量特征差异性,采用野外调查与室内分析相结合的方法对研究区内主要森林生态系统不同乔木器官和土壤C、N、P含量进行了测定,分析了叶片、乔木层和土壤化学计量特征及之间的关系。结果表明:研究区内森林生态系统乔木层平均C、N、P含量均显著低于叶片水平,表层土壤(0—10 cm)C、N含量以及C∶P、N∶P值均显著高于土壤(0—100 cm)平均值;叶片与乔木层及二者与土壤间的生态化学计量特征关系不同;乔木层平均C含量与降水呈显著正相关,乔木层平均P含量仅与海拔呈显著正相关,影响本地区植物生长状态的主要因素是降水。土壤平均C、N含量仅受土壤容重的影响,土壤平均P含量主要受土壤容重、温度和降水的影响。研究结果可以为黄土丘陵沟壑区人工林的建设和管理提供理论依据。     

林窗对格氏栲天然林更新层物种多样性和稳定性的影响

采用物种多样性指数和改进的M.Godron稳定性法研究林窗干扰对格氏栲(Castanopsis kawakamii)自然保护区天然林更新层物种多样性和稳定性的影响.结果表明:林窗干扰改善了微环境,表现在林窗和林下乔灌层树种重要值和多样性存在差异.林窗乔木层中丰富度指数R、优势度指数D、Shannon-Wiener指数H、均优多指数Z均高于林下,均匀度指数Js和群落优势度指数C低于林下;灌木层中R、D、H、Js、Z指数均高于林下,群落优势度指数C低于林下,林窗物种多样性更为丰富,生态优势种不明显,群落向复杂化和均匀化方向发展.林窗与林下乔木层Jaccard相似性系数Cj、Sorenson相似性系数CS、Bray-Curtis指数CN相对较低,Morista-Horn指数CmH较高,林窗对树种更新具有促进作用;灌木层相似性系数Cj、Cs、CN、CmH均较高,物种组成基本一致.根据M.Godron稳定性原理拟合出稳定性模型,林窗和林下乔木层分别为对数模型与二次函数模型,林窗和林下灌木层最佳拟合模型均为对数模型.林窗乔木层植物处于稳定状态,林下乔木层植物不稳定;林窗和林下灌木层植物均处于稳定状态.林窗和林下乔木层树种中以桂北木姜子(Litsea subcoriacea)重要值最高,说明其在森林更新中占有重要地位,可能对格氏栲种群更新产生较大影响.林下乔木层中格氏栲重要值较低,格氏栲更新存在困难,而林窗干扰促进了格氏栲的向上生长和重要值的提升,可有效实现格氏栲种群的更新和恢复.     

林下植被的生物量分布特征及其作用

林下植被是森林生态系统的重要组成部分。研究林下植被的生物量特征及其生态作用对深入研究森林生态系统结构和功能有重要意义。本文归纳了森林林下植被的生物量分布特征与森林的类型、龄级和林分特征等因子之间的变化关系,分析了林下植被在维持森林生态系统营养元素循环、保持水土、指示森林环境状态变化、影响森林林分的生理生态特征和森林演替、保护动物的栖息地以及维持生态平衡等方面的主要生态作用。     

Drivers of understorey biomass: tree species identity is more important than richness in a young forest

林下生物量影响因素：幼龄林树种特性比丰富度更重要 生物多样性与生态系统功能的正相关关系已被广泛报道,其主要来源于对草原生态系统的研究。然而,该结论并不一定适用于更复杂的环境,例如具有不同垂直层次的森林。举例而言,已有研究表明上层乔木树种丰富度与林下生产力降低有关。树种丰富度是否会通过增加(由于生境异质性)或降低(通过增强竞争)资源的可利用性进而影响林下生产力,以及林下生产力是否受树种特性的影响更大,这些影响机制都可能会随着时间的推移而改变。此外,研究还表明,丰富度-生产力关系随着环境背景的变化而改变。本研究利用可以操控树种丰富度的实验林场研究了这些不同垂直层位里的时间和环境动态。在中国亚热带森林生物多样性与生态系统功能(BEF-China)研究计划的框架下,我们在3年时间里沿树种丰富度梯度反复采集林下生物量样本,研究了不同环境处理中树种丰富度、树种特性和时间对林下生物量的影响。尽管我们发现乔木层特性对林下生物量有显著和一致的影响,但是树种丰富度对后者却不具有这种影响。另外,在森林结构层之间,可能并不存在单一的、具有普遍性的上层乔木树种丰富度与林下生产力的相关关系,并且与上层乔木相关的环境因素(如透光率)对林下生产力的贡献程度会随着时间而变化。总体而言,我们的结果表明,在研究森林结构层之间的关系时应将时间动态变化考虑在内。     

喀斯特风水林和荒山生态系统碳储量的研究

所研究的风水林和荒山属于喀斯特地貌。喀斯特森林是一种脆弱的低生物量生态系统,土壤贫瘠,自我修复能力低,易受人为因素干扰。风水林指人们居住地附近的一片茂盛的森林,认为有神居住而崇拜,严禁被砍伐和破坏。荒山是喀斯特森林植被在人为干扰后出现岩石裸露产生的石漠化现象。该研究通过野外调查、实验室分析、数理统计等对广西罗城喀斯特风水林和荒山生态系统碳储量进行对比性研究。结果表明:喀斯特风水林植被、土壤和枯落物碳储量分别是荒山的7.42倍、5.9倍和1.1倍,风水林和荒山生态系统碳储量分别为137.06、93.73 t·hm~(-2),其中土壤碳库贡献率最高,而林下植被和枯落物却较低,表明风水林森林生态系统碳储量明显高于荒山。通过风水林和荒山的碳储量比较研究,为评价风水林碳汇提供依据,为制定森林管理政策、保护村社水平的植被提供数据参考。此外,还探讨了少数民族朴素的生态伦理思想在保护森林和增汇方面的作用,丰富了生态伦理学内容,对传承和弘扬少数民族传统文化、恢复生态具有重要意义。     

坝上地区不同年代退耕还林生境的草本层植物多样性及影响因子

退耕还林是坝上地区重要的生态修复工程,其生态效益日益受到广泛关注,但针对林下植物多样性保护功能的研究还较少,虽然草本层植被是森林生态系统服务功能的重要指标之一。为评估不同年代退耕还林生境的生物多样性,调查了20世纪70年代至21世纪初共4个年代退耕还林生境的草本层植物多样性,并与弃耕生境及自然林生境进行了对比。为进一步分析林下草本层植物多样性的影响因子,还分析了乔灌层植被、土壤理化性质与林下草本植物多样性的关系。结果显示,不同年代退耕还林的林下草本植物多样性未有显著差异,且均显著低于弃耕生境与自然林生境。草本层物种丰富度对土壤碱解氮含量、灌木层丰富度、灌木层密度具有显著的正响应,Simpson多样性主要与乔木层林木密度呈显著负相关。研究表明,不同年代退耕还林后的林下草本层植物多样性保护功能低于预期,而改善林分空间结构与建设模式可能利于提升其生物多样性保护功能。未来植被修复中需充分权衡生态系统不同服务功能之间的关系,因地制宜,宜林则林,宜草则草,重视自然恢复与多元化生态修复方式,以实现更好生态效益。     

油松(Pinus tabulaeformis)人工林林下植被发育对油松生长节律的响应

林下植被作为森林生态系统的一个重要组成部分,对维持林分结构和土壤质量起着重要作用.不同年龄树种对林下植被发育的影响已有所涉及,但这些为数不多的研究往往割裂了林木种群的生长规律与其林下植被间的相互作用,以林龄为尺度探讨林下植被发育的差异必然掩盖了林分种群对林下植被作用的异质性.采用时序研究法,按照油松(Pinus tabulaeformis)高速生期、径速生期、材积慢生期和材积速生期等不同发育时期,探讨林下植被组成、多样性、生物量和元素积累量的差异性.结果表明,高速生期阶段油松与林下植被竞争最为激烈,林下植被物种丰富度、多样性、生物量、元素积累量均最低.因此,高速生期阶段应及时对油松采取较大强度的抚育间伐以缓和油松种群与林下植被剧烈竞争的关系.径速生阶段林下植被与油松竞争最为缓和,草本层Gleason、Shannon-Wiener、Pielow指数由高生长阶段的7.817、2.222和0.769剧增到19.978、3.470和0.907,灌木层、草本层地上部分生物量、元素积累量也均达到最大.径速生阶段对油松林分的管理可相对粗放一些.进入材积阶段,油松与林下植被的关系日趋紧张.材积慢生阶段灌木层、草本层生物量由径速生期的2 262.61、461.92 kg/hm2分别下降至1 549.85、 220.84 kg/hm2,而灌木层Gleason、Shannon-Wiener指数均达到峰值.相对于材积慢生期,材积速生期灌木层、草本层物种多样性指数、元素积累量进一步下降,而生物量略有上升,材积速生期阶段应对油松林分适度间伐或主伐.可见,林下植被可作为人工纯林乔木生长规律的指示剂,根据林下植被发育状况选择林分经营方式具有一定的参考价值.     

林下密集蕨类层生态学研究进展

林下密集蕨类层在森林尤其是受干扰森林中广泛存在,对森林更新具有强烈的过滤效应,能够改变林下层的多样性,影响群落的结构、功能和动态,林下密集蕨类层的生态学研究,对揭示森林群落物种分布格局和群落构建机制具有重要意义.结合国内外最新研究,论述了林下密集蕨类层的特征,从机制上解释了林下密集蕨类层形成的主要原因;分类阐述了林下密...     

环境因子对山西太岳山典型森林类型物种多样性及其功能多样性的影响

该研究采用典型样地法,调查群落内物种分布并测量植物功能性状(叶面积和植株高度),对山西太岳山不同坡位华北落叶松-白桦混交林以及辽东栎次生林物种多样性及其功能多样性进行比较分析,探究环境因子对不同群落层次(乔木、灌木、草本)物种多样性及其功能多样性的影响机制,以及环境因子与群落构建之间的联系,为森林生态系统多样性研究以及经营管理提供理论依据。结果显示:(1)华北落叶松-白桦混交林的物种分布更加均匀,物种多样性和功能多样性(乔木层)均显著高于辽东栎次生林。(2)华北落叶松-白桦混交林乔木层功能均匀度与功能分散指数显著高于辽东栎次生林,但灌木草本层低于辽东栎次生林。(3)不同群落层次的物种多样性与功能多样性均呈正相关关系,影响物种分布和性状分布的环境因子存在差异,物种多样性受多种环境因子的综合影响,而单个环境因子对功能多样性影响较大,环境解释力与林分类型和群落层次相关。(4)乔木层物种多样性主要受土壤pH、冠层结构(MLA、林分开度)以及光照影响,灌木层物种多样性与土壤pH和MLA密切相关,林下总辐射、土壤养分(SOC、STN)、土壤相对含水率是影响草本层物种分布的主要环境因子;冠层结构(MLA、林分开度)是影响乔木层功能多样性最主要的环境因子,土壤pH和坡位分别是华北落叶松-白桦混交林和辽东栎次生林灌木层功能多样性的主要影响因子,影响草本层功能多样性的主要环境因子是土壤相对含水率与LAI。研究表明,在垂直分层的森林生态系统中,不同群落层次竞争的主要环境资源存在差异,乔木层通过改变冠层结构和林内环境限制林下物种分布和性状分布。     

树种组成对北亚热带11年生常绿阔叶人工林碳储量的影响

以中国北亚热带退化灌木林改造而来的木荷-青冈栎混交林和杜英纯林为对象,研究树种组成对常绿阔叶人工林生态系统碳储量的影响。结果表明:(1)退化灌木林改造成两种人工林生长11年后,生态系统植被、土壤碳储量均显著增加;植被碳储量的增加主要来自乔木层。(2)两种人工林碳积累能力有差异。杜英林植被碳储量比木荷-青冈栎林高99.4%,其中杜英林的乔木层碳储量比木荷-青冈栎林高27.75t·hm-2,是后者的2倍;杜英林土壤有机碳储量(0~50cm)显著高于木荷-青冈栎林10.17t·hm-2,其中在0~10、20~30cm土层杜英林均显著高于木荷-青冈栎林。研究表明,退化灌木林人工改造成常绿阔叶林后生态系统碳储量显著增加,杜英纯林碳蓄积能力明显高于木荷-青冈栎混交林,说明在以增加碳储量为目的的退化生态系统改造过程中,树种选择非常重要。     

Hydraulic architecture of evergreen broad-leaved woody plants at different successional stages in Tiantong National Forest Park,Zhejiang Province,China

Aims Hydraulic architecture is a morphological strategy in plants to transport water in coping with environmental conditions. Change of hydraulic architecture for plants occupying different canopy layers within community and for the same plant at different successional stages reflect existence and adaptation in plant's water transportation strategies. The objective of this study was to examine how hydraulic architecture varies with canopy layers within a community and with forest succession.Methods The study site is located in Tiantong National Forest Park, Zhejiang Province, China. Hydraulic architectural traits studied include sapwood-specific hydraulic conductivity, leaf-specific hydraulic conductivity, Huber value, sapwood channel area of twigs, total leaf area per terminal twig, and water potential of twigs. We measured those traits for species that occur in multiple successional stages (we called it "overlapping species") and for species that occur only in one successional stage (we called it "turnover species") along a successional series of evergreen broadleaved forests. For a given species, we sampled both overstory and understory trees. Hydraulic architectural traits between overstory and understory trees in the same community and at successional stages were compared. Pearson correlation was used to exam the relationship between hydraulic architectural traits and the twig/leaf traits.Important findings Sapwood-specific hydraulic conductivities and leaf-specific hydraulic conductivities were significantly higher in overstory trees than those in understory trees, but did not significantly differ from successional stages. Huber value decreased significantly for understory trees, but did not change for overstory trees through forest successional stages. For overstory trees, a trend of decreasing sapwood-specific hydraulic conductivity was observed for overlapping species but not for turnover species with successional stages. In contrast, for understory trees, a trend of decreasing Huber values was observed for turner species but not for overlapping species with successional stages. Across tree species, sapwood-specific hydraulic conductivity was positively correlated with sapwood channel area and total leaf area per terminal twig size. Huber value was negatively correlated to water potential of twigs and total leaf area per terminal twig size. These results suggest that water transportation capacity and efficiency are higher in overstory trees than in understory trees across successional stages in evergreen broadleaved forests in Tiantong region. The contrasting trends of sapwood-specific hydraulic conductivity between overlapping species and turnover species indicate that shift of microenvironment conditions might lead to changes of hydraulic architecture in overstory trees, whereas species replacement might result in changes of hydraulic architecture in understory trees.     

浙江天童常绿阔叶林不同演替阶段木本植物的水力结构特征

水力结构是植物应对环境形成的与水分运输相关的形态策略.探索不同演替阶段和群落不同高度层植物的水力结构特征, 有助于理解植物的水分运输和利用策略.该研究以浙江天童常绿阔叶林演替前中后期群落的上层木(占据林冠层的树种)和下层木(灌木层物种)为对象, 测定了演替共有种(至少存在于两个演替阶段的物种)和更替种(仅存在于某一演替阶段的物种)的枝边材比导率,叶比导率和胡伯尔值, 以及边材疏导面积,末端枝总叶面积和枝条水势, 分析植物水力结构在群落上层木和下层木间以及在演替阶段间的差异, 及其与枝叶性状的相关关系.结果显示: (1)上层木植物边材比导率和叶比导率显著高于下层木植物(p < 0.05); (2)上层木和下层木的边材比导率与叶比导率在演替阶段间均无显著差异(p > 0.05); 上层木的胡伯尔值在演替阶段间无显著差异, 下层木的胡伯尔值随演替显著下降(p < 0.05); (3)上层木共有种仅边材比导率随演替进行显著降低(p < 0.05), 更替种的3个水力结构参数在演替阶段间无显著差异; 下层木共有种水力结构参数在演替阶段间无明显差异, 更替种仅胡伯尔值随演替减小(p < 0.05); (4)植物边材比导率与枝疏导面积和末端枝所支撑的总叶面积显著正相关(p < 0.01), 胡伯尔值与枝条水势及末端枝总叶面积显著负相关(p < 0.01).以上结果表明: 天童常绿阔叶林演替各阶段上层木比下层木具有更大的输水能力和效率; 随着演替进行, 上层木与下层木的共有种和更替种边材比导率的相反变化表明上层木水力结构的变化可能由微生境变化引起, 而下层木水力结构特征的变化可能由物种更替造成.     

Spatial and seasonal heterogeneity in understory light conditions caused by differential leaf flushing of deciduous overstory trees

In a deciduous broad-leaved forest, we investigated the seasonality and heterogeneity of understory light conditions in relation to the leaf phenology of overstory trees. Fisheye photographs were taken from spring to autumn to estimate direct and indirect light conditions above the understory. Spatial variation in daily direct photosynthetic photon flux density (PPFD) was highest in late May, when the early and the intermediate-flushing trees had finished flushing and the late-flushing trees had just started flushing. After whole canopy closure, spatial variation in direct PPFD became low. Thus, asynchronous overstory leaf flushing in spring resulted in spatial heterogeneity in understory light conditions. These results suggest that the leaf phenological patterns of overstory trees are an important factor in the formation of the understory community.     

Tree species growth response to climate warming varies by forest canopy position in boreal and temperate forests

Reports of forest sensitivity to climate change are based largely on the study of overstory trees, which contribute significantly to forest growth and wood supply. However, juveniles in the understory are also critical to predict future forest dynamics and demographics, but their sensitivity to climate remains less known. In this study, we applied boosted regression tree analysis to compare the sensitivity of understory and overstory trees for the 10 most common tree species in eastern North America using growth information from an unprecedented network of nearly 1.5 million tree records from 20,174 widely distributed, permanent sample plots across Canada and the United States. Fitted models were then used to project the near-term (2041–2070) growth for each canopy and tree species. We observed an overall positive effect of warming on tree growth for both canopies and most species, leading to an average of 7.8%–12.2% projected growth gains with climate change under RCP 4.5 and 8.5. The magnitude of these gains peaked in colder, northern areas for both canopies, while growth declines are projected for overstory trees in warmer, southern regions. Relative to overstory trees, understory tree growth was less positively affected by warming in northern regions, while displaying more positive responses in southern areas, likely driven by the buffering effect of the canopy from warming and climate extremes. Observed differences in climatic sensitivity between canopy positions underscore the importance of accounting for differential growth responses to climate between forest strata in future studies to improve ecological forecasts. Furthermore, latitudinal variation in the differential sensitivity of forest strata to climate reported here may help refine our comprehension of species range shift and changes in suitable habitat under climate change.     

Deciduousness Influences the Understory Community in a Semideciduous Tropical Forest

We investigated how deciduousness of overstory tree species influences the community structure and species composition in the understory. The results suggest that deciduous overstory trees have positive effects on light‐demanding species, and that the processes underlying such effects may involve reduced competition for light or facilitation through increased water availability.     

林火干扰对北方针叶林林下植被的影响

林下植被在北方针叶林植被群落中的物种多样性最高, 且具有较高的生物量周转率和地上部分净初级生产力, 对北方针叶林生态系统功能起着重要作用。火干扰是决定北方针叶林林下植被结构与功能的一个重要景观过程。该文综述了火干扰是如何通过与地形、火前林冠组成的交互作用而影响环境资源和林下植被的。最近的研究表明: 林下植被能够影响火后树木更新苗的定植、重建速率及森林演替轨迹; 林下植被还会通过影响元素的生物地球化学过程(凋落物降解和养分循环)影响林下环境资源的数量与异质性。因此, 研究火后初期北方针叶林林下植被的动态变化, 对于物种多样性保护和森林管理具有重要意义。     

Community Comparison and Determinant Analysis of Understory Vegetation in Six Plantations in South China

Plantations cover large areas in many countries, and the enhancement of plantation biodiversity is an increasingly important ecological concern. Many studies have demonstrated that overstory composition is important because it influences understory regeneration. To compare the understory vegetation and analyze its determinant factors, six typical plantations in South China were investigated: Acacia mangium plantation, Schima superba plantation, Eucalyptus citriodora plantation, E. exserta plantation, mixed‐coniferous plantation, and mixed native species plantation. The results show that native species plantations shaded out more grasses and herbs than exotic species plantations, mixed‐species plantations recruited more understory species than monoculture plantations, the leguminous species plantation had higher soil nitrogen than nonleguminous species plantations, and understory vegetation in the mixed‐coniferous plantation was similar to that of mixed, native broadleaf species plantation. Although light is the crucial environmental factor affecting the understory community and diversity among the 14 measured factors, other environmental variables such as soil nutrients and soil moisture are also important.     

Contributions of Understory and/or Overstory Vegetations to Soil Microbial PLFA and Nematode Diversities in Eucalyptus Monocultures

Ecological interactions between aboveground and belowground biodiversity have received many attentions in the recent decades. Although soil biodiversity declined with the decrease of plant diversity, many previous studies found plant species identities were more important than plant diversity in controlling soil biodiversity. This study focused on the responses of soil biodiversity to the altering of plant functional groups, namely overstory and understory vegetations, rather than plant diversity gradient. We conducted an experiment by removing overstory and/or understory vegetation to compare their effects on soil microbial phospholipid fatty acid (PLFA) and nematode diversities in eucalyptus monocultures. Our results indicated that both overstory and understory vegetations could affect soil microbial PLFA and nematode diversities, which manifested as the decrease in Shannon–Wiener diversity index (H′) and Pielou evenness index (J) and the increase in Simpson dominance index (λ) after vegetation removal. Soil microclimate change explained part of variance of soil biodiversity indices. Both overstory and understory vegetations positively correlated with soil microbial PLFA and nematode diversities. In addition, the alteration of soil biodiversity might be due to a mixing effect of bottom-up control and soil microclimate change after vegetation removal in the studied plantations. Given the studied ecosystem is common in humid subtropical and tropical region of the world, our findings might have great potential to extrapolate to large scales and could be conducive to ecosystem management and service.     

Species richness and soil properties in Pinus ponderosa forests: A structural equation modeling analysis

Question: How are the effects of mineral soil properties on understory plant species richness propagated through a network of processes involving the forest overstory, soil organic matter, soil nitrogen, and understory plant abundance? Location: North‐central Arizona, USA. Methods: We sampled 75 0.05‐ha plots across a broad soil gradient in a Pinus ponderosa (ponderosa pine) forest ecosystem. We evaluated multivariate models of plant species richness using structural equation modeling. Results: Richness was highest at intermediate levels of understory plant cover, suggesting that both colonization success and competitive exclusion can limit richness in this system. We did not detect a reciprocal positive effect of richness on plant cover. Richness was strongly related to soil nitrogen in the model, with evidence for both a direct negative effect and an indirect non‐linear relationship mediated through understory plant cover. Soil organic matter appeared to have a positive influence on understory richness that was independent of soil nitrogen. Richness was lowest where the forest overstory was densest, which can be explained through indirect effects on soil organic matter, soil nitrogen and understory cover. Finally, model results suggest a variety of direct and indirect processes whereby mineral soil properties can influence richness. Conclusions: Understory plant species richness and plant cover in P. ponderosa forests appear to be significantly influenced by soil organic matter and nitrogen, which are, in turn, related to overstory density and composition and mineral soil properties. Thus, soil properties can impose direct and indirect constraints on local species diversity in ponderosa pine forests.     

Linking dominant Hawaiian tree species to understory development in recovering pastures via impacts on soils and litter

Large areas of tropical forest have been cleared and planted with exotic grass species for use as cattle pasture. These often remain persistent grasslands after grazer removal, which is problematic for restoring native forest communities. It is often hoped that remnant and/or planted trees can jump‐start forest succession; however, there is little mechanistic information on how different canopy species affect community trajectories. To investigate this, I surveyed understory communities, exotic grass biomass, standing litter pools, and soil properties under two dominant canopy trees—Metrosideros polymorpha (‘ōhi‘a) and Acacia koa (koa)—in recovering Hawaiian forests. I then used structural equation models (SEMs) to elucidate direct and indirect effects of trees on native understory. Native understory communities developed under ‘ōhi‘a, which had larger standing litter pools, lower soil nitrogen, and lower exotic grass biomass than koa. This pattern was variable, potentially due to historical site differences and/or distance to intact forest. Koa, in contrast, showed little understory development. Instead, data suggest that increased soil nitrogen under koa leads to high grass biomass that stalls native recruitment. SEMs suggested that indirect effects of trees via litter and soils were as or more important than direct effects for determining native cover. It is suggested that diverse plantings which incorporate species that have high carbon to nitrogen ratios may help ameliorate the negative indirect effects of koa on natural understory regeneration.