林隙干扰对森林生态系统的影响

林隙干扰通过改变森林微生境异质性和群落演替进程,对森林物种组成、林分结构和系统功能产生重要影响。本研究评述了有关林隙干扰对森林生态系统影响的最新研究进展,从物种生物学特性和环境因素两个方面分析了林隙干扰对森林物种组成变化的影响规律,基于群落组件和群落架构阐述了林隙干扰对森林结构的作用关系,梳理了林隙干扰对森林生态系统功能的影响机制。基于已有研究的分析和目前森林生态系统经营亟需解决的问题,提出未来研究所需关注的重点领域和问题: 林隙面积阈值确定方法;林隙闭合机制;林隙干扰对森林生态系统过程的影响;林隙干扰与森林生产力的关系。林隙干扰在促进物种更新和提升森林结构复杂性等方面具有优势,因此本研究可为我国低产低效人工林改造提供科学依据。     

林窗干扰与森林群落演替

林窗干扰是影响森林群落演替的一个重要因素。该文从林窗干扰和森林群落演替理论及林窗对森林群落微环境、植物入侵和定居、群落结构、群落演替的影响等方面简要介绍了当前国内外有关林窗干扰与森林群落演替的研究现状和研究前景。     

干扰对动物传播森林植物种子有效性影响的研究进展

干扰在森林生态系统中普遍存在,并影响森林的更新和演替.动物传播种子是种子更新的必经阶段,其对森林干扰的响应在一定程度上能够预测未来的森林群落组成和结构变化,对于明确森林演替方向具有重要意义.本文论述了森林干扰对动物传播种子有效性(包括动物传播种子的数量和质量)影响研究的生态学意义,全面揭示了自然干扰(火干扰、林窗干扰等)和人为干扰(生境破碎化、狩猎、采伐等)对动物传播种子数量、传播距离以及传播后幼苗更新影响的研究进展,指出干扰通过影响动物种群动态,进而造成动物传播种子数量发生了改变,动物传播种子的距离对干扰的响应基本表现出轻微负相关;干扰对传播后幼苗更新的影响结果因干扰类型的不同而复杂多变,干扰迹地环境因子的变化也影响着传播后的种子萌发和幼苗更新.干扰对动物传播种子有效性影响研究中存在的问题,主要表现为火干扰迹地恢复过程、增益性的干扰(如抚育、间伐、林窗)等对种子传播有效性影响研究的匮乏,以及忽略了温带森林内的干扰对动物传播种子的影响等.今后,应开展干扰对种子传播有效性的长期研究;对于干扰多发地带的森林,应高度重视增益性干扰影响动物传播植物种子的研究.     

林窗干扰研究

林窗是森林生态系统中一种普遍存在的现象,无论是健康的系统还是已经受到过度干扰的系统,林窗作为森林生态系统发展的重要驱动力,影响着森林的物种组成、结构以及森林的演替方向。因此,林窗研究能够为受干扰森林生态系统的恢复提供理论指导,并为森林生态系统的管理提供科学依据。本文从总结有关林窗的基本理论入手,重点介绍了近年来对林窗概念、基本特征、林窗产生后的生境条件变化以及生物对林窗环境变化的响应等研究概况,并对目前林窗研究的手段以及热点问题进行了总结,以期为今后的相关研究提供参考。     

热带次生林森窗平均气温空间分布特征的初步分析

森林群落演替更新作为生态学研究的核心问题 ,一直是研究热点 ,而群落演替更新的重要生态动力乃是自然或人为的干扰。国内外关于大尺度干扰对不同森林类型演替更新已有较详细的研究 ;从 2 0世纪 80年代初开始 ,小尺度的林窗干扰开始受到广泛重视。由于林窗是群落演替的起始地 ,其大小和环境变化程度决定了林窗发展的方向和速度 ,并且林窗的更新状况直接影响到顶级森林的结构、种类组成和种群动态。对于世界范围内的各种森林类型的更新和演替均有重要作用 [17] ,而在热带雨林中的作用更加显著和重要[15] ,因此 ,国外学者十分重视林窗的研究。…     

南亚热带森林演替过程中土壤线虫群落结构变化

森林演替会通过改变植物群落组成和土壤环境影响土壤生物群落, 反过来, 土壤生物群落的变化也会对生态系统的演替产生反馈作用, 但迄今南亚热带森林演替过程中土壤生物群落的变化特征尚不清晰。本研究以广东省鼎湖山的南亚热带森林演替序列(马尾松(Pinus massoniana)林-针阔叶混交林-季风常绿阔叶林)为对象, 研究了森林演替过程中土壤线虫多样性和群落结构的动态变化及其影响因素。通过采集不同演替阶段的土壤样品, 分析和比对了不同演替阶段土壤线虫的多度、多样性、群落组成、土壤线虫生态指数以及土壤理化性质的差异。结果表明: (1)在南亚热带森林演替过程中, 针阔叶混交林和季风常绿阔叶林土壤线虫的α多样性显著高于马尾松林, 但土壤线虫总数和各营养类群多度及其相对丰度并无显著变化; (2)针阔叶混交林中土壤线虫富集指数显著高于马尾松林, 表明其土壤养分状况要好于马尾松林, 而季风常绿阔叶林土壤线虫结构指数较高, 表明其受干扰程度较低; (3)针阔叶混交林的土壤含水量和土壤理化性质(除土壤总磷含量)已达到季风常绿阔叶林的水平, 但两者的土壤pH值均显著低于马尾松林, 而土壤pH值和土壤含水量是影响土壤线虫群落动态变化的主要因素。综上所述, 南亚热带森林中土壤线虫多度、多样性和群落结构对森林演替的响应略有不同, 演替过程中土壤环境因素的趋同是导致针阔叶混交林和季风常绿阔叶林中土壤线虫多样性和群落特征相似的主要原因。     

南亚热带森林不同演替阶段植物与土壤中N、P的化学计量特征

选择南亚热带森林演替过程3个阶段(初期、中期和后期)的典型森林生态系统为研究对象,在测定植物与土壤中全N、全P含量的基础上,阐明了森林演替过程中植物与土壤的N、P化学计量特征。结果显示:1)土壤中全N含量随演替进行而增加,马尾松(Pinus massoniana)林(初期)、混交林(中期)和季风林(后期)0–10cm土层中全N含量分别为0.440、0.843和1.023g·kg–1;混交林0–10cm土层中全P的含量最为丰富,为0.337g·kg–1,马尾松林和季风林土壤全P含量分别为0.190和0.283g·kg–1。2)植物叶片中全N、全P的含量随演替呈减少的趋势,但根系中全N、全P的含量都以马尾松林为最多,混交林和季风林含量彼此相当。3)各土层中N:P随演替的进行呈现明显增加趋势,马尾松林、混交林和季风林0–10cm土层中N:P分别为2.3、2.5和3.6;植物各器官中N:P随演替的进行也呈增加趋势,且叶片和根系中的N:P相近,马尾松林、混交林和季风林叶片中N:P分别为22.7、25.3和29.6。基于上述结果,探讨了南亚热带森林生态系统植物与土壤中N:P特征、森林演替过程中植物与土壤中N:P变化规律以及P对南亚热带森林生态系统的限制作用。结果表明,P已经成为南亚热带森林生态系统生物生长和重要生态过程的限制因子。     

林火干扰对森林生态系统土壤有机碳的影响研究进展

林火干扰是森林生态系统特殊而重要的生态因子,可改变生态系统的养分循环与能量传递。研究林火干扰对森林生态系统土壤有机碳的影响,有助于理解森林生态系统中土壤碳固持和碳循环过程,为制定科学合理的旨在减缓全球变化的林火管理策略具有重要意义。从4个方面阐述了林火干扰对森林生态系统土壤有机碳的影响及内在机制:分别从大尺度和小尺度两个方面阐述了林火干扰对土壤有机碳的影响及对森林生态系统碳循环与碳平衡的作用机制;探讨了不同林火干扰类型和林火干扰强度下,土壤活性有机碳对林火干扰的响应机制;阐明了林火干扰对土壤惰性有机碳的影响及作用机制;论述了林火干扰主要通过改变土壤有机碳的输入和输出过程进而影响土壤有机碳的稳定性及内在机制。最后提出了提高林火干扰对森林生态系统土壤有机碳影响定量化研究的4种路径选择:(1)全面比较研究不同林火干扰类型对土壤有机碳循环及其碳素再分配过程的功能特征;(2)进一步阐明林火干扰通过改变植被结构进而影响土壤生物群落结构,剖析土壤碳库循环的内在机制;(3)完善不同时空尺度下林火干扰对森林生态系统土壤碳库周转过程的定量化研究;(4)加强不同林火干扰类型土壤碳库稳定性差异的研究。     

亚高山森林生态系统过程研究进展

亚高山森林是以冷、云杉属为建群种或优势种的暗针叶林为主体的森林植被。亚高山森林在庇护邻近脆弱生态系统、保育生物多样性、涵养水源、碳吸存和指示全球气候变化等方面具有十分重要且不可替代的作用和地位,其多样化的植被和土壤组合为研究生态系统过程提供了天然的实验室。亚高山森林的群落演替与更新、生物多样性保育、水文生态过程、生物元素的生物地球化学循环以及亚高山森林生态过程对气候变化的响应等研究已取得了明显的进展。但有关全球变化条件下的亚高山森林土壤生物多样性和冬季生态学过程等研究明显不足。全球气候变化背景下的冬季生态学过程、极端灾害事件对亚高山森林生态系统过程的影响、亚高山森林生物多样性的保育机制、亚高山森林土壤生物多样性与生态系统过程的耦合机制等可能是未来研究的前沿科学问题。     

中国西南地区热带森林演替序列碳动态

热带森林的破坏是全球性问题,我国西双版纳森林覆盖率受砍伐、火烧和短期耕种丢荒后,面积不断减少,取而代之的是大面积的不同演替状态的次生林。次生林演替过程中的碳储量和碳平衡的变化目前还鲜有研究,为了进一步揭示我国西南地区热带森林演替对于碳蓄积的影响,并制定更科学的热带森林经营管理措施,以结构复杂、生物多样和生物量巨大的热带森林为研究对象,并利用3个热带次生林的样地的实测数据,探讨了不同演替状态的热带次生林的碳储量变化,以及森林的净碳蓄积,死亡碳损失和更新碳增长等碳动态规律,分析表明:(1)在森林的演替过程中,森林的胸径分布频度从近正态分布逐渐向小径级的偏态分布发展,也就是随着演替的进展,小径级林木所占的比例越来越高。(2)热带次生林在森林固碳方面发挥着不可忽略的作用。(3)小的干扰,会波及森林的碳动态;大的干扰,如火灾和砍伐,将导致森林的次生演替,对森林的碳动态产生不可逆转的改变。(4)干旱事件是影响凋落物的季节和年间动态的原因,也是短时间尺度上影响碳平衡的一个重要因子。(5)不论原生林还是次生林,大树在生态系统碳动态方面皆扮演着重要的角色,因此本研究推荐注重大树的研究。     

林窗模型及其在全球气候变化研究中的应用

林窗模型是基于个体的广泛应用于森林长期动态变化的模拟与预测的模型,是研究森林生态系统对气候变化响应的有效工具。本文把林窗模型的发展与演变过程概括为3个阶段:萌芽阶段、飞速发展阶段和提高阶段;展望了林窗模型的未来发展趋势;简要阐述了在全球气候变化背景下应用模型研究森林与气候间关系的可行性与必要性;对国际上相关的研究热点和前沿问题进行了探讨;综述了国内的研究现状,指出国内林窗模型的预测研究应以改进现有模型、构建新模型、耦合多模型作为未来的发展方向。     

Changes in tree phenology along natural regeneration in a seasonally dry tropical forest

The applicability of succession models from temperate and tropical wet forests to threatened seasonally dry tropical forests (SDTFs) is questioned. Plant phenology affects ecosystem functions and changes along forest regeneration gradient. To investigate the recovery of ecological functions after disturbances in a SDTF, we recorded the vegetative and reproductive phenologies for trees (DBH >5 cm) for 17 months in southeast Brazil in three successional stages: early (10–15 years after clearing), intermediate (25–30) and late (>50). The vegetative phenology of the 523 individuals was strongly seasonal, with 3% of individuals presenting green leaves in a deciduous dry season. Besides structural and floristic differences, phenological trends were similar between the later stages. Reproduction occurred with higher intensities in the early stage and in the advanced stages only in the dry season, providing key resources to local fauna. The studied SDTF is resilient to ecological functions, rapidly recovering functional processes. The integration of structural and functional knowledge of succession of STDFs may lead to better management of its secondary remnants. Our study suggests that classical forest succession theory developed for other ecosystems may not fully reflect the pattern of SDTF succession, an ecosystem that originally covered 42% of the earth's tropical and subtropical landmass.     

Simulation of moss and tree dynamics in the boreal forests of interior Alaska

We used a simulation model of forest dynamics to examine the ecological significance of the complex interactions among site conditions, tree growth, and the development of a thick forest floor moss layer found in many boreal forests. To examine the effect of site conditions on moss growth and forest dynamics, we simulated the dynamics of several different forest sites in the uplands of interior Alaska. Then we used a cold, wet permafrost site to examine the ecological consequences of direct moss and tree interactions. Our analyses revealed a tightly coupled system in which forest succession was highly sensitive to the interactions among site conditions, mosses, and trees. The effect of mosses on the soil thermal regime was a particularly important feedback. Direct interactions between mosses and trees that affected the development of a thick forest floor layer were also important. In particular, shading of moss by trees, reduced tree regeneration on moss-covered soils, and reduced moss growth with open forest canopies were also important determinants of forest succession. These complex feedbacks ensure that an ecosystem approach is needed to understand the ecology of boreal forests.     

Quantifying ecological memory during forest succession: A case study from lower subtropical forest ecosystems in South China

The concept of ecological memory provides a new perspective for research on forest succession by including historical factors and the initial state of ecological processes. However, there are still significant gaps between the concept and its application. We selected nine proxy indicators (plant species, soil seed banks, soil microbes, soil animals, birds, soil age, soil pollen, soil mineral distribution, and light environment) and developed a method to quantify ecological memory and succession in a subtropical forest succession in South China. Taking the climax-monsoon evergreen broad-leaved forest as the reference ecosystem, we found that ecological memory increased nonlinearly and accumulated following a specific assembly rule during succession. Memory concerning major soil microbes and soil animals, which improve the soil substrate, mainly accumulated from the initial to the early successional stage. Memory concerning the number of bird species and the availability of light, which ensure a source of regenerative seeds and the survival of understory seedlings, mainly accumulated from the early to middle successional stages. Memory concerning vegetation and soil seed banks mainly accumulated late in succession, guaranteeing that the ecosystem would reach the regional climax stage. Prospective memory was greater than retrospective memory in every successional stage except the late stage, which indicated that all stages but the late stage were undergoing progressive succession. Our study demonstrates that the concept of ecological memory and the proposed evaluation framework are useful for guiding research on succession and restoration, and especially for assessing how “far” a restored ecosystem is from a reference ecosystem or how far a restored ecosystem has deviated from its natural succession trajectory.     

庐山森林景观格局变化的长期动态模拟

在以植被格局为基础的森林景观动态分析中,可通过森林演替推断景观格局的动态变化以及相应的景观生态过程。运用空间直观景观模型LANDIS,以庐山风景区为案例地,模拟森林植被在未来300 a的自然演替动态,在此基础上选取斑块面积比、聚集度、分维数、多样性指数和均匀度指数等景观格局指数,分析森林景观格局随森林演替的动态变化。结果表明：（1）阔叶林树种的绝对优势地位保证其斑块面积比呈现持续增长的稳定趋势,森林植被将朝着地带性常绿阔叶林方向演替;（2）景观聚集度特征方面,阔叶林树种在前150 a缓慢增长,而后150 a保持相对稳定,杉木林一直保持平稳,毛竹林在整个模拟阶段一直在不断下降直至演替结束;（3）各优势树种植被斑块的分维数都保持在1-1.1之间,说明各景观斑块的边缘相对较规则且变化较小;（4）景观多样性指数呈现出先上升后缓慢下降的趋势,而均匀度指数则呈现出先下降后上升再缓慢下降的变化态势。景观格局指数的变化特征与植被向顶极群落演替的趋势相吻合,该模拟结果可运用到庐山森林景观的管理实践中。从长远来看,应该继续实行严格的封山育林政策。     

Effects of Natural and Human-Assisted Regeneration on Landscape Dynamics in a Korean Pine Forest in Northeast China

Improper forest harvesting can potentially degrade forest ecosystem functions and services. Human-assisted regeneration (e.g., planting) is often used to increase the rate of forest recovery and thereby reduce regeneration failure. Seed dispersal is a fundamental ecological process that can also influence spatio-temporal patterns of forest regeneration. In this study, we investigated the relative contribution of planting and seed dispersal on forest regeneration at landscape scales. Because such influences can be further complicated by timber harvest intensity and seed availability within and around harvested area, we also evaluated the effects of those factors on forest landscape dynamics. We used the forest landscape model LANDIS to simulate the dynamics of Korean pine-broadleaf mixed forests in Northeast China. We considered three factors: timber harvest intensity (3 levels), seed dispersal and whether or not planting was used. The results showed that planting was more important in maintaining the abundance of Korean pine (Pinus koraiensis), a climax keystone species in this region, under the high-intensity harvesting option during early succession. In contrast, seed dispersal was more important during late succession. Korean pine can be successfully regenerated through seed dispersal under low and medium harvest intensities. Our results also indicated that effective natural regeneration will require protecting seed-production trees (seed rain). This study results provide a basis for more effectively managing Chinese temperate forests and possibly other similar ecosystems.     

基于植物多样性的生态系统恢复动力学原理

生态系统恢复动力学是生态学的重要问题.本研究利用岛屿生物地理学、植物群落演替、生物多样性维持机制及生态系统功能等有关理论,推导了生态系统恢复动力学模型,并用半湿润常绿阔叶林次生演替阶段数据作了初步验证.基于动力学模型讨论了动力学原理.结果表明,生态系统恢复的动力学过程决定于生态系统恢复力F1、干扰力F2和环境阻力F3的综合作用.植物多样性恢复速度的变率与植物种丰富度呈反比,与生态系统恢复总动力F呈正比.生态系统恢复力F1和环境阻力F3是初始物种丰富度s0、特定地理区域资源环境状况的函数.干扰力是干扰强度系数b和物种丰富度s的函数.当生态系统存在有害干扰的条件下,物种丰富度不能达到生态系统最高物种丰富度sm.动力学模型显示,初始物种丰富度s0越小,生态系统恢复过程越具有逻辑斯蒂性.建立了生态系统恢复力、环境阻力和干扰力的计算模型和植物多样性、干扰对生态系统恢复的作用模型.生态系统恢复动力模型显示,植物多样性能增加生态系统恢复力,促进生态系统稳定性.     

Altered dynamics of forest recovery under a changing climate

Forest regeneration following disturbance is a key ecological process, influencing forest structure and function, species assemblages, and ecosystem–climate interactions. Climate change may alter forest recovery dynamics or even prevent recovery, triggering feedbacks to the climate system, altering regional biodiversity, and affecting the ecosystem services provided by forests. Multiple lines of evidence – including global‐scale patterns in forest recovery dynamics; forest responses to experimental manipulation of CO₂, temperature, and precipitation; forest responses to the climate change that has already occurred; ecological theory; and ecosystem and earth system models – all indicate that the dynamics of forest recovery are sensitive to climate. However, synthetic understanding of how atmospheric CO₂ and climate shape trajectories of forest recovery is lacking. Here, we review these separate lines of evidence, which together demonstrate that the dynamics of forest recovery are being impacted by increasing atmospheric CO₂ and changing climate. Rates of forest recovery generally increase with CO₂, temperature, and water availability. Drought reduces growth and live biomass in forests of all ages, having a particularly strong effect on seedling recruitment and survival. Responses of individual trees and whole‐forest ecosystems to CO₂ and climate manipulations often vary by age, implying that forests of different ages will respond differently to climate change. Furthermore, species within a community typically exhibit differential responses to CO₂ and climate, and altered community dynamics can have important consequences for ecosystem function. Age‐ and species‐dependent responses provide a mechanism by which climate change may push some forests past critical thresholds such that they fail to recover to their previous state following disturbance. Altered dynamics of forest recovery will result in positive and negative feedbacks to climate change. Future research on this topic and corresponding improvements to earth system models will be a key to understanding the future of forests and their feedbacks to the climate system.