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1.
1963年在小兴安岭丰林自然保护区红松林及有关的皆伐迹地上设置了61组,325个实验样方,定期观察到1965年,以研究死、活地被物对人工播种的红松林伴生树种种子发芽和幼苗初期存活、生长的影响。实验表明死、活地被物,特别是死地被物的干湿变化剧烈,影响幼苗的成活,甚至使种子或幼根无法接触土壤,因而种粒越小,或轻而带翅,受影响越大。此外本文还指出了桦树种子的强迫休眠和延迟发芽现象。讨论了实验结果在红松林演替和人工促进天然更新中的意义。 相似文献
2.
红松混交林是中国东北地区最重要的植被类型,在缓解全球气候变化、保证木质产品供给和维护生物多样性中扮演重要角色。该研究以吉林东大坡自然保护区第52林班的水曲柳-红松混交林和第54林班的核桃楸-红松混交林为例,采用林分结构参数一元分布(UDSSP)、二元分布(BDSSP)和非线性模型(NLM)分析了它们的针叶树和阔叶树的结构特征,以探讨混交林中针、阔树种组之间的关系,为低效次生林的改造提供参考。结果显示:(1)多数针叶树同时处于高混交和优势状态,仅有极少数个体处于中庸或劣势;多数阔叶树亦处于高混交状态,且不同优势的树木总数几乎相等。(2)大部分树木都同时处于高度混交和随机分布状态,少量针叶树略偏向规则分布。(3)大部分针叶树同时处于随机分布和优势状态,且不同优势的阔叶树皆倾向随机分布,而处于规则或聚集分布的数量很少。(4)针叶树和阔叶树的径阶分布均能够较好地通过指数函数或幂函数描述。这些特征充分展示了空间格局和径阶分布在不同群落类型之间差异很小,但在不同树种组之间存在明显差异。 相似文献
3.
水分利用效率是反映植物水分利用的客观指标,对其研究有助于了解陆地生态系统的碳水耦合机制.本研究利用稳定碳同位素技术分析了长白山阔叶红松林演替序列下3种林分(中龄杨桦林、成熟杨桦林、阔叶红松林)中优势树种的水分利用效率.结果 表明:3种林分的水分利用效率在不同演替阶段存在阔叶红松林>中龄杨桦林>成熟杨桦林的大小顺序,且同... 相似文献
4.
Stand-scale gap-phase dynamics is generally viewed as the main driver of development in mesic deciduous forests of the temperate biome. Soil charcoal of temperate forests in eastern North America are unnoticed in most surveys, thus explaining why fire is undervalued as a driver of forest succession. The extent to which gap-phase, fire, or other processes are responsible for the regeneration and maintenance of mesic deciduous forests is unknown because paleoecological evidence is lacking. We tested the fire-driven succession hypothesis on the development of this major forest type. Based on charcoal 14C dates of two sites, 44 and 55 fires occurred since early Holocene, with a mean interval of 170 to 215 years. The vegetation of both sites followed comparable post-glacial trajectories consisting of three distinct periods. Conifers dominated the two first periods during 5200–6000 years and were replaced by hardwoods–conifers over the last 3500 years. The first period was represented by boreal conifers, whereas the second period, dominated by white pine (Pinus strobus) forests, persisted during 3000–4300 years. The third period marked the development of hardwood (sugar maple, Acer saccharum) forests. Fires occurred continuously on the sites since early Holocene likely under dry conditions during the conifer periods and cooler and moister conditions during the hardwood–conifer period. Recurrent fires appear with climate as key drivers of the long-term dynamics of several temperate forests in eastern North America. Similar studies on other temperate forests should be pursued to test the hypothesis of climate–fire interactions influencing tree composition change. 相似文献
5.
阔叶红松林是我国东北重要的原生群落,其土壤团聚体在森林生态系统碳固定中具有重要作用.本研究采用空间代替时间的方法,选取白桦幼龄林、白桦中龄林、白桦成熟林、阔叶红松成熟林和阔叶红松过熟林5个不同演替序列,通过湿筛法研究长白山天然针阔混交林群落恢复演替中土壤团聚体粒径组成及有机碳含量的变化.结果表明: 土壤团聚体粒径组成受演替过程影响较大,不同演替阶段下土壤团聚体各粒级所占比例差异显著.团聚体平均质量直径随演替的进行表现为先升高再降低的单峰形式,且最高点出现在白桦成熟林阶段.土壤中不同粒级的团聚体内有机碳含量随着演替的进行呈先增加后略有下降的趋势,且团聚体内有机碳含量最大值出现在阔叶红松成熟林阶段.在同一演替阶段下,0~5和5~10 cm土层(除演替末期的阔叶红松过熟林外)中的各粒径团聚体内有机碳含量都随着粒径的减小而增加,而10~20 cm土层中的各粒径团聚体内有机碳含量都随着粒径的减小而减小.从演替初期的白桦幼龄林到演替末期的阔叶红松过熟林,每个样地内的同一粒径团聚体内有机碳含量均具有明显的垂直分布特性,均随着土层深度的增加而显著降低. 相似文献
6.
运用LANDIS Pro 7.0模型,模拟了2000—2200年小兴安岭地区10个阔叶树种地上部分生物量在当前气候条件和不同气候变化情景下的变化状况,并结合各树种的含碳率计算各树种的地上部分固碳速率.结果表明: 在模拟初始年份,水曲柳、黄檗、蒙古栎、春榆、色木槭的生物量低所占比例小,枫桦、白桦、山杨生物量较大所占比例较高.先锋树种白桦和山杨的固碳速率在模拟中后期出现先下降后上升的过程;其他阔叶树种的固碳速率变化规律较复杂,蒙古栎和紫椴的固碳速率在整个模拟阶段分别在-0.05~0.25和0.16~1.29 t·hm -2·(10 a) -1范围内波动,水曲柳、春榆、色木槭和枫桦的固碳速率在模拟中后期呈先上升后下降的趋势.在模拟的第2(2050—2100年)和第4阶段(2150—2200年),黄檗、黑桦在不同气候变化情景间的固碳速率存在显著差异,其他树种的固碳速率在不同气候条件间无显著差异.小兴安岭地区阔叶树种地上部分固碳速率对未来气候的敏感性存在差异.不同气候变化情景的不确定性对大多数森林乔木树种地上部分固碳速率不会造成显著差异,且气候对森林固碳速率的影响存在时滞效应. 相似文献
7.
研究了中国东北小兴安岭地区阔叶红松林的更新和红松的生长及其影响因素。研究结果表明由于成树树冠的遮蔽作用所导致的光照减少是制约幼树生长和存活的关键因素。阔叶红松林是该区最典型和稳定的植被类型,但是在过去的50a中,由于皆伐和更新不良导致了它的分布面积和蓄积量的减少。阔叶红松林是地带性“顶极”植被,并通过具有连续性年龄结构的树种有规律的替代和演替过程中不同阔叶树种组成而处于优势地位。这种林型无疑应作为一种重要的基因库加以保护。次生阔叶林是在阔叶红松林受干扰后出现的,但它的种类组成简单,而且结构也很不稳定。因此,必须对现有的林分结构加以调整以利于林分的长期稳定和高产。同时,提出了红松阔叶林的恢复和重建的经营方式。 相似文献
8.
选择处于全球变化中国东北样带东部典型生态系统的长白山阔叶红松林作为研究区,采用动态气室-CO 2红外分析法测定了森林生态系统不同退化阶段的土壤呼吸作用.结果表明:在生长季,长白山阔叶红松林不同退化阶段的土壤呼吸动态变化呈单峰型曲线,在7-8月达到最大值;不同退化阶段林地土壤呼吸大小顺序为:杨桦林>蒙古栎林>阔叶红松林>硬阔叶林>裸地.其中,杨桦林和蒙古栎林样地的碳释放量分别为对照阔叶红松林的1.4和1.3倍,硬阔叶林和裸地的碳释放量分别为对照阔叶红松林的88%和78%. 相似文献
9.
Aim Predictions of ecosystem responses to climate warming are often made using gap models, which are among the most effective tools for assessing the effects of climate change on forest composition and structure. Gap models do not generally account for broad‐scale effects such as the spatial configuration of the simulated forest ecosystems, disturbance, and seed dispersal, which extend beyond the simulation plots and are important under changing climates. In this study we incorporate the broad‐scale spatial effects (spatial configurations of the simulated forest ecosystems, seed dispersal and fire disturbance) in simulating forest responses to climate warming. We chose the Changbai Natural Reserve in China as our study area. Our aim is to reveal the spatial effects in simulating forest responses to climate warming and make new predictions by incorporating these effects in the Changbai Natural Reserve. Location Changbai Natural Reserve, north‐eastern China. Method We used a coupled modelling approach that links a gap model with a spatially explicit landscape model. In our approach, the responses (establishment) of individual species to climate warming are simulated using a gap model (linkages ) that has been utilized previously for making predictions in this region; and the spatial effects are simulated using a landscape model (LANDIS) that incorporates spatial configurations of the simulated forest ecosystems, seed dispersal and fire disturbance. We used the recent predictions of the Canadian Global Coupled Model (CGCM2) for the Changbai Mountain area (4.6 °C average annual temperature increase and little precipitation change). For the area encompassed by the simulation, we examined four major ecosystems distributed continuously from low to high elevations along the northern slope: hardwood forest, mixed Korean pine hardwood forest, spruce‐fir forest, and sub‐alpine forest. Results The dominant effects of climate warming were evident on forest ecosystems in the low and high elevation areas, but not in the mid‐elevation areas. This suggests that the forest ecosystems near the southern and northern ranges of their distributions will have the strongest response to climate warming. In the mid‐elevation areas, environmental controls exerted the dominant influence on the dynamics of these forests (e.g. spruce‐fir) and their resilience to climate warming was suggested by the fact that the fluctuations of species trajectories for these forests under the warming scenario paralleled those under the current climate scenario. Main conclusions With the spatial effects incorporated, the disappearance of tree species in this region due to the climate warming would not be expected within the 300‐year period covered by the simulation. Neither Korean pine nor spruce‐fir was completely replaced by broadleaf species during the simulation period. Even for the sub‐alpine forest, mountain birch did not become extinct under the climate warming scenario, although its occurrence was greatly reduced. However, the decreasing trends characterizing Korean pine, spruce, and fir indicate that in simulations beyond 300 years these species could eventually be replaced by broadleaf tree species. A complete forest transition would take much longer than the time periods predicted by the gap models. 相似文献
10.
【目的】研究我国最大的林区之一——大兴安岭森林火烧后不同演替阶段土壤细菌多样性动态,为天然林保护工程对于生物多样性的影响增添新的认识。【方法】以空间替代时间的方法分析大兴安岭森林演替对于土壤细菌多样性动态的影响。大兴安岭森林火烧后典型的自然演替序列为火烧迹地(LG-BA)、灌丛(SHR)、白桦林(BP)、白桦落叶松混交林(BP-LG)、落叶松林(LG-OM)。在演替序列的每个典型样地上采集0-10 cm土样,采用Illumina Mi Seq高通量测序技术测定土壤细菌群落组成及其多样性。【结果】细菌操作分类单位(OTU)数量从少到多的顺序为火烧迹地落叶松白桦混交林灌丛落叶松林白桦林。随着森林演替,多样性指数Simpson先增高后降低;Shannon指数先增加后减少再增加;OTU的丰度变化比较平缓,表明物种变化较小。在各演替阶段中,土壤细菌种类主要有变形菌门(Proteobacteria)、酸杆菌门(Acidobacteria)、放线菌门(Actinobacteria)和浮霉菌门(Planctomycetes),4个门的种类含量随演替顺序都呈现先增加后减少的趋势。主成分分析表明不同演替阶段土壤细菌群落存在一定的差异性。冗余分析表明有机质(SOM)、全氮(TN)、全磷(TP)和p H对于土壤细菌群落变化有影响。【结论】随着森林演替,大兴安岭地区土壤细菌种类和生物多样性会发生变化,其变化与土壤化学成分和p H有关。 相似文献
11.
Fire is a primary driver of boreal forest dynamics. Intensifying fire regimes due to climate change may cause a shift in boreal forest composition toward reduced dominance of conifers and greater abundance of deciduous hardwoods, with potential biogeochemical and biophysical feedbacks to regional and global climate. This shift has already been observed in some North American boreal forests and has been attributed to changes in site conditions. However, it is unknown if the mechanisms controlling fire‐induced changes in deciduous hardwood cover are similar among different boreal forests, which differ in the ecological traits of the dominant tree species. To better understand the consequences of intensifying fire regimes in boreal forests, we studied postfire regeneration in five burns in the Central Siberian dark taiga, a vast but poorly studied boreal region. We combined field measurements, dendrochronological analysis, and seed‐source maps derived from high‐resolution satellite images to quantify the importance of site conditions (e.g., organic layer depth) vs. seed availability in shaping postfire regeneration. We show that dispersal limitation of evergreen conifers was the main factor determining postfire regeneration composition and density. Site conditions had significant but weaker effects. We used information on postfire regeneration to develop a classification scheme for successional pathways, representing the dominance of deciduous hardwoods vs. evergreen conifers at different successional stages. We estimated the spatial distribution of different successional pathways under alternative fire regime scenarios. Under intensified fire regimes, dispersal limitation of evergreen conifers is predicted to become more severe, primarily due to reduced abundance of surviving seed sources within burned areas. Increased dispersal limitation of evergreen conifers, in turn, is predicted to increase the prevalence of successional pathways dominated by deciduous hardwoods. The likely fire‐induced shift toward greater deciduous hardwood cover may affect climate–vegetation feedbacks via surface albedo, Bowen ratio, and carbon cycling. 相似文献
12.
应用林窗模型-FAREAST,模拟未来气候变化对中国东北主要类型森林演替动态的影响.根据大气环流模型ECHAM5-OM和HadCM3预测的气候变化资料,模拟选择了目前气候情景、增暖情景、增暖且降水变化情景3种气候情景.结果表明:维持目前气候不变,东北森林树种组成和森林生物量基本维持动态平衡.气候增暖不利于东北主要森林类型生长,主要针叶树种比例下降,阔叶树比例增加;温带针阔混交林垂直分布带有上移的趋势;增暖幅度越大,变化越明显.气候增暖基础上考虑降水变化,东北森林水平分布带有北移的趋势,降水对低海拔温带针阔混交林影响不大. 相似文献
13.
应用Simpson和Shannon多样性指数及其相应的均匀度,对阔叶红松林及其次生白桦林的高等植物物种多样性进行了对比研究.结果表明,对于木本植物,次生白桦林物种多样性高于阔叶红松林;而对于草本植物,情况正好相反.但在次生白桦林中,无论木本植物还是草本植物,占优势的物种都是一些常见种,而许多阔叶红松林中的珍稀或特有物种在次生白桦林中数量很少,有些甚至完全消失.对群落各种群多度分布的检验表明,2种森林类型中,无论木本植物还是草本植物,各种群的多度分布都遵从对数级数分布. 相似文献
14.
选择长白山阔叶红松林、白桦林和落叶松林3种林型,对各林型蛾类的群落结构和多样性进行了比较。结果表明:蛾类各科(亚科)在3种林型中的比例分配明显不同。阔叶红松林中尺蛾科数量占优绝对优势,占47.0%,其次是舟蛾科,为9.3%。优势种为台褥尺蛾,占17.2%;从蛾类总种数和蛾类个体总数上看,白桦林中蛾类物种丰富度、多度和多样性指数明显高于阔叶红松林和落叶松林,优势度指数则最低;白桦林的优势种有尘尺蛾、枞灰尺蛾和双星白枝尺蛾;在落叶松林中,灯蛾科、波纹蛾科和枯叶蛾科的多度都比阔叶红松林和白桦林高,其优势种为阿泊波纹蛾。 相似文献
15.
Montane forests of western China provide an opportunity to establish baseline studies for climate change. The region is being impacted by climate change, air pollution, and significant human impacts from tourism. We analyzed forest stand structure and climate-growth relationships from Jiuzhaigou National Nature Reserve in northwestern Sichuan province, along the eastern edge of the Tibetan plateau. We conducted a survey to characterize forest stand diversity and structure in plots occurring between 2050 and 3350 m in elevation. We also evaluated seedling and sapling recruitment and tree-ring data from four conifer species to assess: 1) whether the forest appears in transition toward increased hardwood composition; 2) if conifers appear stressed by recent climate change relative to hardwoods; and 3) how growth of four dominant species responds to recent climate. Our study is complicated by clear evidence of 20 th century timber extraction. Focusing on regions lacking evidence of logging, we found a diverse suite of conifers ( Pinus, Abies, Juniperus, Picea, and Larix) strongly dominate the forest overstory. We found population size structures for most conifer tree species to be consistent with self-replacement and not providing evidence of shifting composition toward hardwoods. Climate-growth analyses indicate increased growth with cool temperatures in summer and fall. Warmer temperatures during the growing season could negatively impact conifer growth, indicating possible seasonal climate water deficit as a constraint on growth. In contrast, however, we found little relationship to seasonal precipitation. Projected warming does not yet have a discernible signal on trends in tree growth rates, but slower growth with warmer growing season climates suggests reduced potential future forest growth. 相似文献
16.
应用林窗模型LINKAGES对小兴安岭红松针阔混交林在不同季节增温方式下的未来演替过程进行了模拟预测.以温度增加5℃、降水无明显变化作为未来变暖气候的模拟假设,共设计3种气候变暖方式预案,分别为冬季增温幅度大于夏季、冬季与夏季增温幅度相同以及冬季增温幅度小于夏季.模拟结果表明,当冬季增温幅度大于夏季时,小兴安岭现存林分的演替受气候变暖的影响相对最小,树种组成仍然能够保持较为稳定的针阔混交林状态;当冬季增温幅度小于夏季时,现存林分的演替受气候变暖的影响最显著,树种衰退最迅速.可见,小兴安岭针阔混交林的演替与未来的增温方式关系密切,上限温度是现存树种能否继续存活的重要决定因子. 相似文献
17.
木腐真菌在森林生态系统中具有丰富的物种多样性, 并在倒木的降解过程中发挥重要的生态功能。针叶树是大小兴安岭森林生态系统的优势树种, 因此研究针叶树倒木木腐真菌物种多样性和影响其物种分布的相关环境因子有助于揭示大小兴安岭森林生态系统物质循环的机理。本研究收集了近16年对大小兴安岭地区冷杉属( Abies)、落叶松属( Larix)、云杉属( Picea)和松属( Pinus) 4类针叶树倒木上1,561份木腐真菌标本的采集信息, 统计了物种种类及其腐朽类型, 并选取具有代表性的地点开展木腐真菌群落多样性及其与环境因子的相关性分析。结果显示, 大小兴安岭针叶树倒木木腐真菌有166种, 隶属于70属, 其中白腐真菌有111种, 占所有种类的66.9%, 褐腐真菌为55种, 占所有种类的33.1%。在4类针叶树倒木上均能生长的真菌种类有19种, 占所有种类的11.5%, 其中柔丝干酪孔菌( Oligoporus sericeomollis)是各类倒木上木腐真菌群落中的优势种。大兴安岭地区落叶松属为优势寄主, 其倒木上生长的木腐真菌种类数和个体数在4类倒木中均为最高; 而小兴安岭地区松属倒木上木腐真菌种类数和个体数比其他3类倒木高, 是该地区的优势寄主。对6个代表性地区木腐真菌群落的研究显示, 有11种真菌在6个地区均有分布, 小兴安岭地区木腐真菌多样性普遍高于大兴安岭地区; 聚类分析显示树种比地理位置对木腐真菌物种分布的影响更大。 相似文献
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2003年10月~2004年4月,在黑龙江省小兴安岭凉水国家级自然保护区,应用跟踪观察法、样线调查法、样方调查法等研究方法,采用Vanderploeg和scavia选择系数Wi和选择指数Ei作为衡量指标,对松鼠贮食红松种子生境选择进行了研究。研究表明,松鼠贮食对生境具有选择性:以主要林型为划分标准,松鼠偏爱贮食生境依次为:原始红松林,云杉林,人工云杉林,针叶混交林,人工落叶松林,针阔混交林,阔叶混交林,次生白桦林和人工红松林。在原始红松林内,松鼠对微生境的利用存在选择性差异:松鼠对郁闭良好(郁闭度大于0.6)、灌丛密度中等、倒木和枯立木密度中等(1~5个)、盗食动物活动较弱(大林姬鼠Apodemus peninsulae为主要盗食动物)的原始红松林生境表现出较强的选择性(Ei>0.2);而对坡度小于5°、基质为霉菌土、倒木和枯立木密度较高(大于5个)、草本盖度较高、盗食动物活动中等(花鼠Eutamias sibiricus为主要盗食动物)的原始红松林生境表现出较强的负选择性(Ei<-0.2),对阴坡表现出强烈的回避性(Ei=-0.5368)。 相似文献
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用森林演替模型BKPF研究黑龙江省伊春地区红松针阔叶混交林采伐迹地上森林演替在未来50年气候变化和CO 2浓度增加的反应得出:伊春地区采伐迹地演替50年后红松和硬阔叶树的数量增加,落叶松、山杨与白桦减少;林分密度略有降低;林分生产力增加约7%~28%;林分地上部分总生物量增加15%~24%;叶面积指数增加约5%~8%.气候变化有利于采伐迹地阔叶红松林恢复. 相似文献
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通过样地调查对不同干扰方式产生的过伐天然林、次生白桦林和人工落叶松林等群落的结构组成进行分析和分类探讨,并选取能够表征结构完整性和稳定性的一些指标因子,利用健康距离法对长白山阔叶红松林区的森林生态系统健康进行了评估实践,结果按顺序依次为:原始阔叶类0.14<结构转换型0.23<结构保留型0.32<结构破坏型0.33<严重干扰类型0.44<次生白桦林0.53<人工落叶松林0.68.以期对阔叶红松林生态系统的恢复和区域林业可持续发展提供参考. 相似文献
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