长江中游(以湖北湖南为主)的植物生物多样性及其保护对策

在对植物调查研究的基础上,对长江中游(湖北、湖南为主)的植物区系、植被、生物多样性保护及保护对策进行了系统的论述。根据两省土著种子植物名录统计,本区共有202科1476属7037种(包括种下等级),其中裸子植物7科30属64种;被子植物196科1445属6973种。以鄂湘为代表的华中区分布类型复杂、物种丰富、起源古老,而且特有的科、属、种多,特有度高。北温带木本植物属高度集中,体现了长江中游具有古第三纪．泛北极植物区系的代表性。拥有众多的东亚特有属、东亚．北美间断分布属和中国特有属,它们既是本地植物区系的特色,也代表了中国植物区系的核心。本地中山以亮叶水青冈(Fagus lucida)为主的阔叶林系第三纪．泛北中生落叶阔叶林的后裔。在植被区划上,本区属于常绿阔叶林区域,包括北亚热带常绿阔叶．落叶阔叶混交林地带及中亚热带常绿阔叶林两个植被地带。后者分为北部典型常绿阔叶林亚地带,南部含华南植物区系成分的常绿阔叶林亚地带。本区主要的自然植被类型(以原生类型为主)有171个类型(相当于群系formations)。从生物多样性保护的三个层次上(物种、群落、景观)对保护现状、特点、保护方针和策略等进行了探讨并提出了建议。     

河南植被水平地带性的分布规律

河南植被纬向性分布与气温有关。北部属温带落叶林区域,典型植被,山地为落叶阔叶林和常绿针叶林,东部平原的农作物为一年两作或两年三作。南部为亚热带常绿阔叶林区域的常绿、落叶阔叶混交林地带,典型植被为含有常绿成分的落叶阔叶林,针叶林由马尾松、黄山松和杉木林组成。河南植被的经向性分布职决于干燥度引起的地带性变化,东部大别山的植被由黄山松林和茶园来表征,南部的桐柏山地带则没有黄山松林和茶园。     

湖北植被地理分布的规律性(上)

湖北植被的地理分布明显地受水热因素的规律性的控制,植被的纬向性分布规律十分明显;北部为北亚热常绿阔叶落叶阔叶混交林地带,典型植被以含有青冈、柯、楠木、冬青的栎类林,枫香林以及马尾松林,台湾松林和巴山松林为代表,南部为中热带常绿阔叶林地带,典型植被以含有栲类林、润楠林、梓树林,水丝梨林和杉木林、马尾松林为表征。植被的经向地带性规律显而易见,东部植被基本为华中成分,与华东区系有密切联系,西部则为典型的     

山西吕梁山南段植物群落的生态梯度

吕梁山南段在中国植被区划上属暖温带南部落叶阔叶林亚地带向暖温带北部落叶阔叶林亚地带的过渡地带.采用TWINSPAN分类和DCCA排序法,从植物种、植物群落与环境因子之间的相互关系,对吕梁山南段植物群落的生态梯度进行了研究.结果表明:(1)TWINSPAN分类将74个样方划分为18个群丛.其中4个群丛为森林群落,14个群丛为灌丛.这18个群丛属南暖温带性质的次生植被类型,代表了吕梁山南段植物群落的主要类型,这些群丛都不同程度受到人类活动的干扰;(2)样方的DCCA排序较好地揭示了该区域植物群落的分布格局与海拔、坡度、土层厚度、枯枝落叶层厚度、坡向和人类干扰6个因子的关系,其中制约植物群落结构及分布格局的主导因子是海拔高度和人类干扰,另外,坡向和土层厚度也对植物群落特征产生一定的影响;(3)对环境因子的相关分析表明,海拔、人类干扰、土层厚度和枯枝落叶层厚度之间存在着极显著的相关性,是影响分布格局的主导因子;(4)结合TWINSPAN和DCCA的分析表明,吕梁山南段植物群落表现出明显的垂直分布格局,在海拔690～1 100 m的低山和沟谷中主要分布着荆条和酸枣灌丛;海拔1 100～1 300 m阳坡和半阳坡主要分布着灌木状檀子栎林,并伴生有少量的侧柏和鹅耳枥;在1 300～1 570 m主要分布着以辽东栎为建群种的森林群落;(5)灌木状檀子栎林的分布,是该地区处于暖温带南部落叶阔叶林亚地带向暖温带北部落叶阔叶林亚地带的交错区的主要标志.     

安徽植被带的划分

安徽各地种子植物分布型的统计结果显示其植物区系基本属于温带性质．地理联系广泛．与东亚关系密切。通过对大别山不同区域3个山头(天堂寨、多枝尖和陀尖)的种子植物数目和结构．及属种相似性系数两方面的研究,认为整个大别山植物应归同一植物区系,其植被应归为亚热带常绿阔叶林．在划分亚热带与暖温带的分界线时,大别山应作为一个整体考虑。同时结合对黄山、板桥、天堂寨、琅琊山和皇藏峪的植物区系和生活型谱的统计结果分析,提出暖温带落叶阏叶林与常绿、落叶阔叶混交林的分界线,位于淮河一线;而亚热带常绿阔叶林与暖温带的常绿、落叶阏叶混交林的分界线位于叶集、六安、舒城、庐江、铜陵、宣城至广德一线。     

中国东部森林植被带划分之我见

简要回顾了中国东部森林植被带划分研究的历史及当前存在的争论。提出了中国东部植被带划分应以植被本身的特征,特别是地带性的生物群落集为主要依据,同时参照它们的区系组成和气候指标。根据上述原则将中国东部划分为6个植被带∶北方针叶林带、凉温带针阔混交林带、温带落叶阔叶林带、暖温带常绿落叶阔叶混交林带、亚热带常绿阔叶林带和热带雨林、季雨林带,并对各植被带的特征作了简要的描述。阐述了对一些植被带名称、界线改动的原因,特别讨论了我国常绿落叶阔叶混交林以及常绿阔叶林生物气候带的归属问题,认为前者归属于暖温带植被,后者归属于亚热带植被为宜。     

中国东部森林植被带划分之我见

简要回顾了中国东部森林植被带划分研究的历史及当前存在的争论。提出了中国东部植被带划分应以植被本身的特征，特别是地带性的生物群落集为主要依据，同时参照它们的区系组成和气候指标。根据上述原则将中国东部划分为６个植被带∶北方针叶林带、凉温带针阔混交林带、温带落叶阔叶林带、暖温带常绿落叶阔叶混交林带、亚热带常绿阔叶林带和热带雨林、季雨林带，并对各植被带的特征作了简要的描述。阐述了对一些植被带名称、界线改动的原因，特别讨论了我国常绿落叶阔叶混交林以及常绿阔叶林生物气候带的归属问题，认为前者归属于暖温带植被，后者归属于亚热带植被为宜。     

北京东灵山主要森林植被中苔藓植物的物种多样性

通过对北京东灵山地区32个样地植被及苔藓植物的调查,对主要森林植被中苔藓植物物种多样性进行分析。结果表明:东灵山主要森林植被中共有苔藓植物16科33属79种,优势科为青藓科(Brachytheciaceae)和绢藓科(Entodontaceae)等。密叶绢藓(Entodoncompressus)、小牛舌藓(Anomodon minor)等为优势种。地面生苔藓植物物种丰富度以落叶阔叶混交林中最大,白桦林中最小,苔藓植物群落相似性以辽东栎林与落叶阔叶林之间最高,以山杨林与油松林之间最低。树附生苔藓植物物种丰富度以落叶阔叶混交林中最大,油松林中最小;苔藓植物群落相似性以油松林和山杨林之间最高,华北落叶松林与白桦林之间最低。地面生和树附生苔藓植物多样性与林型、树种及其所形成的林内微环境相关。     

无样地法在暖温带落叶阔叶林群落调查中的应用

本文以秦岭太白山自然保护区内锐齿栎(Quercus atiena var. acuteserrota)为优势的暖温带落叶阔叶林为对象,采用与大样地(0.5公顷)实测结果的比较,研究了无样地法中的中点四分法取样技术在暖温带落叶阔叶林中的应用。认为中点四分法取样技术,具有较高的精度和效率,可适用于暖温带落叶阔叶林。并用种点数曲线确定了暖温带落叶阔叶林的最小点数为15个。     

东灵山林区不同森林植被水源涵养功能评价

森林植被发挥着涵养水源的作用,主要表现在以下几个方面:对降水的截留与再分配;调节河川径流,调节林内小气候,减小林内地表蒸发,改善土壤结构,减少地表侵蚀等. 通过对几种林分各层拦蓄降水和保土功能指标定性评价的基础上,用综合评定法对不同林分水源涵养和保土功能进行综合评价,选择出综合功能最好的林分,以期为北京山区的生态环境建设、植被恢复与保护提供一定的依据。在测定东灵山4种森林植被林冠层、枯枝落叶层和土壤层蓄水和土壤保持功能指标的基础上,采用综合评定法对4种森林植被水源涵养和土壤保持功能进行了评价。结果表明:各植被类型的林冠层截留各不相同,在雨季(6-9 月份) 辽东栎林的截留率最大,华北落叶松的最小;枯落物最大持水深以辽东栎林的最大,油松的最小;土壤水文特性各异,0-80 cm 土层平均容重以落叶阔叶林的最小,华北落叶松的最大;稳渗速率以落叶阔叶林的最大,油松的最小,初渗速率以辽东栎林的最大,油松的最小。不同林分水源涵养和土壤保持综合能力由大到小顺序为落叶阔叶混交林、辽东栎林、华北落叶松林、油松林。常绿阔叶灌丛水源涵养和土壤保持综合能力评价值(0.1039) 比其它植被类型少3个数量级,说明其水源涵养和土壤保持功能明显优于其它植被类型。由此可见,树种组成丰富、林下灌草盖度高、枯落物储量多的落叶阔叶混交林水源涵养和土壤保持能力最强,优于单一的阔叶林,而油松林最差。     

秦岭太白山桦林的稳定性

本文论述了桦林的稳定性。文中认为桦林地质时期和现代都可形成地带性森林,它是凉温湿润气候的顶极群落,分布在暖温带落叶阔叶林与湿冷生针叶林之间的凉温湿润地带。因此这类林的区系组成无论地质时期或现代,都是以暖温带落叶阔叶林和寒温带针叶林的混合成分为特征。     

秦岭太白山桦林的稳定性

本文论述了桦林的稳定性。文中认为桦林地质时期和现代都可形成地带性森林,它是凉温湿润气候的顶极群落,分布在暖温带落叶阔叶林与湿冷生针叶林之间的凉温湿润地带。因此这类林的区系组成无论地质时期或现代,都是以暖温带落叶阔叶林和寒温带针叶林的混合成分为特征。     

Pollen-based reconstructions of biome distributions for Australia, Southeast Asia and the Pacific (SEAPAC region) at 0, 6000 and 18,000 14C yr BP

Aim This paper documents reconstructions of the vegetation patterns in Australia, Southeast Asia and the Pacific (SEAPAC region) in the mid‐Holocene and at the last glacial maximum (LGM). Methods Vegetation patterns were reconstructed from pollen data using an objective biomization scheme based on plant functional types. The biomization scheme was first tested using 535 modern pollen samples from 377 sites, and then applied unchanged to fossil pollen samples dating to 6000 ± 500 or 18,000 ± 1000 ¹⁴C yr bp . Results 1. Tests using surface pollen sample sites showed that the biomization scheme is capable of reproducing the modern broad‐scale patterns of vegetation distribution. The north–south gradient in temperature, reflected in transitions from cool evergreen needleleaf forest in the extreme south through temperate rain forest or wet sclerophyll forest (WSFW) and into tropical forests, is well reconstructed. The transitions from xerophytic through sclerophyll woodlands and open forests to closed‐canopy forests, which reflect the gradient in plant available moisture from the continental interior towards the coast, are reconstructed with less geographical precision but nevertheless the broad‐scale pattern emerges. 2. Differences between the modern and mid‐Holocene vegetation patterns in mainland Australia are comparatively small and reflect changes in moisture availability rather than temperature. In south‐eastern Australia some sites show a shift towards more moisture‐stressed vegetation in the mid‐Holocene with xerophytic woods/scrub and temperate sclerophyll woodland and shrubland at sites characterized today by WSFW or warm‐temperate rain forest (WTRF). However, sites in the Snowy Mountains, on the Southern Tablelands and east of the Great Dividing Range have more moisture‐demanding vegetation in the mid‐Holocene than today. South‐western Australia was slightly drier than today. The single site in north‐western Australia also shows conditions drier than today in the mid‐Holocene. Changes in the tropics are also comparatively small, but the presence of WTRF and tropical deciduous broadleaf forest and woodland in the mid‐Holocene, in sites occupied today by cool‐temperate rain forest, indicate warmer conditions. 3. Expansion of xerophytic vegetation in the south and tropical deciduous broadleaf forest and woodland in the north indicate drier conditions across mainland Australia at the LGM. None of these changes are informative about the degree of cooling. However the evidence from the tropics, showing lowering of the treeline and forest belts, indicates that conditions were between 1 and 9 °C (depending on elevation) colder. The encroachment of tropical deciduous broadleaf forest and woodland into lowland evergreen broadleaf forest implies greater aridity. Main conclusions This study provides the first continental‐scale reconstruction of mid‐Holocene and LGM vegetation patterns from Australia, Southeast Asia and the Pacific (SEAPAC region) using an objective biomization scheme. These data will provide a benchmark for evaluation of palaeoclimate simulations within the framework of the Palaeoclimate Modelling Intercomparison Project.     

北京山区的栎林

 本文叙述了北京山区的主要栎林——辽东栎林、槲栎林、槲树林和栓皮栎林的群落学特征。栎林是由温带植物区系所组成的落叶阔叶林。组成栎林的植物以菊科、蔷薇科、禾本科和豆科植物种类为最丰富。在群落结构中有重要作用的植物,乔木层以壳斗科的栎属为主,灌木层以蔷薇科的绣线菊属、李属、豆科的胡枝子属,马鞭草科的荆条属和虎耳草科的溲疏属占有重要地位。草本层常以莎草科的苔草属,禾本科的隐子草属、大油芒属、野古草属和白草属植物为优势种或常见种。栎林的植物生活型谱,从种类成分分析是以地面芽植物为主,高位芽植物次之,地下芽植物亦占一定比例,但从各类生活型植物的优势度分析,显然以高位芽植物占有优势。组成栎林植物的叶级,是以小型叶植物为主,中型叶植物次之,大型叶植物为罕见。就各类栎林种类成分的相似性分析,以槲树林与槲栎林最为相似,辽东栎林与栓皮栎林差异较大。     

Evaluating Spatial-Temporal Dynamics of Net Primary Productivity of Different Forest Types in Northeastern China Based on Improved FORCCHN

An improved individual-based forest ecosystem carbon budget model for China (FORCCHN) was applied to investigate the spatial-temporal dynamics of net primary productivity of different forest types in northeastern China. In this study, the forests of northeastern China were categorized into four ecological types according to their habitats and generic characteristics (evergreen broadleaf forest, deciduous broadleaf forest, evergreen needleleaf forest and deciduous needleleaf forest). The results showed that distribution and change of forest NPP in northeastern China were related to the different forest types. From 1981 to 2002, among the forest types in northeastern China, per unit area NPP and total NPP of deciduous broadleaf forest were the highest, with the values of 729.4 gC/(m²•yr) and 106.0 TgC/yr, respectively, followed by mixed broadleaf- needleleaf forest, deciduous needleleaf forest and evergreen needleleaf forest. From 1981 to 2002, per unit area NPP and total NPP of different forest types in northeastern China exhibited significant trends of interannual increase, and rapid increase was found between the 1980s and 1990s. The contribution of the different forest type’s NPP to total NPP in northeastern China was clearly different. The greatest was deciduous broadleaf forest, followed by mixed broadleaf- needleleaf forest and deciduous needleleaf forest. The smallest was evergreen needleleaf forest. Spatial difference in NPP between different forest types was remarkable. High NPP values of deciduous needleleaf forest, mixed broadleaf- needleleaf forest and deciduous broadleaf forest were found in the Daxing’anling region, the southeastern of Xiaoxing’anling and Jilin province, and the Changbai Mountain, respectively. However, no regional differences were found for evergreen needleleaf NPP. This study provided not only an estimation NPP of different forest types in northeastern China but also a useful methodology for estimating forest carbon storage at regional and global levels.     

辽东次生林木腐菌的物种多样性及其分布特征

2013年7—9月,以清原林场、老秃顶子国家级自然保护区和宽甸白石砬子自然保护区为研究区域,对辽东次生林中木腐菌的物种多样性及其分布特征进行了研究.经过野外调查,共采集和记录木腐菌1062份,经鉴定为92种,隶属于48个属;其中白石砬子国家级自然保护区木腐真菌物种最丰富,Shannon多样性指数为4.04.从物种的地理成分来看,辽东地区的木腐菌以世界性广布和北温带分布为主,具有明显的北温带特征.白腐真菌是该地区倒木的主要分解者;该地区的木腐菌主要生长在腐烂等级为2、3的倒木上,主要优势寄主为槭属倒木,有243份真菌采集于槭属倒木,占总数的23.2%.     

再论中国植被分区的原则和方案

 本文首先提出中国植被分区的原则和依据以及高级分区单位的标志,将全国划分为八大植被区,其中有五个区包括两个亚区,因作者主张亚区与区作为同一级的辅助单位看待,所以实际上把全国分为13个高级植被分区单位。除少数例外,每一植被区或亚区都分为一过渡带和典型带。全文以植被区或亚区、植被地带或亚地带为单位,论述其植被特点。     

中国主要森林生态系统水文功能的比较研究(英文)

 基于中国不同区域生态站的观测资料,着重从降雨截留（林冠截留、枯枝落叶层截持和土壤蓄水）、调节径流和蒸散等3个方面对我国主要森林生态系统的水文生态功能进行了比较研究。各生态系统林冠年截留量在134～626 mm间变动,由大到小排列为：热带山地雨林,亚热带西部山地常绿针叶林,热带半落叶季雨林,温带山地落叶与常绿针叶林,寒温带、温带山地常绿针叶林,亚热带竹林,亚热带、热带东部山地常绿针叶林,寒温带、温带山地落叶针叶林,温带、亚热带落叶阔叶林,亚热带山区常绿阔叶林,亚热带、热带西南山地常绿针叶林,南亚热带常绿阔叶林,亚热带山地常绿阔叶林。枯落物持水量可以达到自身干重的2～5倍,但也因林型而异。土壤非毛管持水量变动在36～142 mm之间,平均89 mm。常绿阔叶林的非毛管持水量通常高于100 mm,而寒温带/温带落叶阔叶林和常绿针叶林通常低于100 mm. 土壤的非毛管持水量通常占生态系统中截持水量的90%,其次是枯落物和林冠层。这说明,森林土壤在调节降雨截留中占有重要地位,其水文功能的大小取决于土壤结构和空隙度,而这些恰恰又受枯落物和森林植被特征的影响。森林皆伐后,一般地表径流会显著地增加,而适当抚育措施则对地表径流影响不大。流域径流受诸多因素的影响,包括植被、土壤、气候、地形、地貌以及人类影响导致的流域景观变化,比较研究表明森林变化对流域径流的影响尚未得到一致的规律性的结果。通过对比研究不同森林的蒸散变化,发现随降雨量的增加,森林蒸散量略有增加,而相对蒸散率却在下降,相对蒸散率在40%～90%间变动。     

Latitudinal patterns of magnitude and interannual variability in net ecosystem exchange regulated by biological and environmental variables

Over the last two and half decades, strong evidence showed that the terrestrial ecosystems are acting as a net sink for atmospheric carbon. However the spatial and temporal patterns of variation in the sink are not well known. In this study, we examined latitudinal patterns of interannual variability (IAV) in net ecosystem exchange (NEE) of CO₂ based on 163 site-years of eddy covariance data, from 39 northern-hemisphere research sites located at latitudes ranging from ∼29°N to ∼64°N. We computed the standard deviation of annual NEE integrals at individual sites to represent absolute interannual variability (AIAV), and the corresponding coefficient of variation as a measure of relative interannual variability (RIAV). Our results showed decreased trends of annual NEE with increasing latitude for both deciduous broadleaf forests and evergreen needleleaf forests. Gross primary production (GPP) explained a significant proportion of the spatial variation of NEE across evergreen needleleaf forests, whereas, across deciduous broadleaf forests, it is ecosystem respiration (Re). In addition, AIAV in GPP and Re increased significantly with latitude in deciduous broadleaf forests, but AIAV in GPP decreased significantly with latitude in evergreen needleleaf forests. Furthermore, RIAV in NEE, GPP, and Re appeared to increase significantly with latitude in deciduous broadleaf forests, but not in evergreen needleleaf forests. Correlation analyses showed air temperature was the primary environmental factor that determined RIAV of NEE in deciduous broadleaf forest across the North American sites, and none of the chosen climatic factors could explain RIAV of NEE in evergreen needleleaf forests. Mean annual NEE significantly increased with latitude in grasslands. Precipitation was dominant environmental factor for the spatial variation of magnitude and IAV in GPP and Re in grasslands.     

外来树种日本落叶松对森林土壤质量及细菌多样性的影响

以甘肃小陇山林区8～30年林龄日本落叶松林（外来树种）、油松林（乡土树种）及次生林为研究对象,研究了不同树种森林的土壤质量和细菌多样性变化.结果表明: 不同树种森林土壤pH无明显变化;林龄越长,土壤含水量越高.土壤总氮与有机质含量以次生林最高,其次为日本落叶松,油松最低.不同林龄森林土壤总氮与有机质含量无明显变化,表明树种是影响土壤质量的主要因素.与乡土树种油松相比,外来树种日本落叶松显著提高了土壤全氮及土壤有机质含量.变性梯度凝胶电泳(DGGE)图谱显示,次生林土壤细菌多样性最高,而外来树种日本落叶松土壤细菌多样性最低.对DGGE图谱的聚类分析发现,小陇山不同森林土壤细菌类群分属变形杆菌、噬纤维黄杆菌和高G+C含量革兰氏阳性细菌类,其中分属变形杆菌为主要类群.进一步分析发现,日本落叶松的细菌群落组成具有更高的相似度,说明日本落叶松正在使该地区土壤细菌多样性发生变化.