丹霞地貌山顶生态效应

首次探讨了丹霞地貌山顶生态效应现象,揭示特殊的地貌、形态所产生的特殊生态现象.测定广东省丹霞山宝珠峰和海螺峰的山顶的生态因子特征、群落结构特征和物种生态型特征,并与山脚的群落与种群以及相近非丹霞地貌区作比较.结果表明,山顶的平均温度高于山脚沟谷,平均湿度小于山脚沟谷,群落物种数和物种多样性均小于山脚沟谷.相比山顶而言,山脚沟谷的植物有很强的热带性.这些特征都有别于一般非丹霞地貌山地.另外,在山顶和山脚调查的几个种群在叶面积、比叶面积、树皮、枝下高和冠幅等方面,均出现了生态型的差异.讨论了丹霞地貌山顶对生态型研究、岛屿理论研究和适应性进化研究的科学意义.     

山东茶山高等植物资源及群落结构

目的:为有效保护和合理利用山东茶山国家级生态示范区植物资源提供科学依据.方法:对茶山进行了植物物种综合普查,调查范围涉及植物物种及野外分布、群落结构和区系组成.结果:记录到高等植物352种,隶属90科250属,其中国家二级重点保护植物4种.本区地带性植被为黑松人工林及次生杂木林,主要森林植被为黑松群落Pinus thunbergii community.其植物区系以热带分布类型和温带分布类型为主,纬度因素和"岛屿效应"应是形成该格局的主要成因.受强烈人为活动干扰,该区域原生植被类型已遭严重破坏,珍稀植物灭绝风险很高.结论:调查表明该区域群落结构简单,灌木层和层间结构不发达,群落演替时间短.     

丹霞山风景地貌的植物区系研究

描述了丹霞山植物区系的特征,对其科、属、种进行系统分析,并与邻近地区植物区系作了对比研究,探讨了丹霞地貌对本区植物区系组成成分的影响。丹霞山植物区系体现了华夏植物区系的特征,其表征科有不少同时也是华夏区系的表征科。从属的地理分布区类型来看,以泛热带分布局的比例最高,其次为热带亚洲分布属、东亚分布局及北温带分布属。丹霞山植物区系相对其纬度来说热带性较强,这与其特定的地貌特征有关。另外,本区的苦藓植物较为丰富,据初步统计共有27科70属,其中石生性苔藓分布尤其广泛。     

云南热带雨林:特征、生物地理起源与演化北大核心CSCD

云南热带雨林具有与东南亚低地热带雨林类似的群落结构、生态外貌特征和物种多样性,是亚洲热带雨林的一个类型。它的植物区系组成中有90%的属和多于80%的种为热带分布成分,其中约40%的属和70%的种为热带亚洲分布型,它含属种较多的优势科和在群落中重要值较大的科也与亚洲热带雨林相似,是亚洲热带雨林和植物区系的热带北缘类型。云南西南部、南部与东南部的热带雨林在群落结构和生态外貌上类似,但在南部与东南部之间有明显的植物区系分异,它们经历了不同的起源背景和演化历程。云南的热带雨林在很大程度上由西南季风维持。喜马拉雅隆升导致西南季风气候形成和加强,在云南热带局部地区产生了湿润气候,发育了热带雨林植被。现在的云南热带雨林里或其分布地区有落叶物种或热带落叶林存在,这不仅是季节性气候的影响,推测在晚第三纪或第四纪更新世云南热带地区曾经历了干旱气候。云南热带雨林的分布主要受制于局部生境,并非地区性气候条件。     

海南岛坝王岭热带山地雨林陆均松-线枝蒲桃群系的区系特点

初步探讨了海南坝王岭自然保护区热带山地雨林的代表群落类型即陆均松－线枝蒲桃群系的种子植物区系组成及其地理分布特点。此群落含有61科、137属、326种,热带分布特别是热带－亚洲分布的成分占有明显优势,其次是泛热带分布,热带性很强,中国特有的分布的种属所占比例极低。单、寡种属极为丰富是该地区植物区系组成的另一特点。     

江西井冈山地区沟谷季雨林及其超地带性特征

江西井冈山地区位于中国东部中亚热带地区南缘,属北半球湿润区。该地区地处罗霄山脉中段,地势高耸,沟谷深切,生境极富多样化,在其沟谷地区保存有典型亚热带季风常绿阔叶,常称季雨林。选择6个典型沟谷季雨林群落,开展群落生态学和生物地理学的研究,结果表明:(1)群落组成以典型的热带性科属为特征,如樟科Lauraceae、壳斗科Fagaceae、山茶科Theaceae、茜草科Rubiaceae、金缕梅科Hamamelidaceae等;种子植物属的地理成分以热带-亚热带成分占优势,占总属数的64.71%—77.94%,高于同纬度地区其他山体,接近甚至高于南亚热带季风常绿阔叶林中的热带性成分。(2)群落结构具有多优势种及明显的特征性标志种,与具单优势种或少数优势种的亚热带常绿阔叶林有明显差异。(3)Shannon-Wiener指数为4.44—5.46之间,物种多样性较丰富,表现出明显的南亚热带植被特征。(4)其它热带雨林性质的特征还包括:大型木质藤本,板根现象,绞杀现象,滴水叶尖,丰富的寄生、附生植物、兰科植物、树蕨等。整体上,井冈山地区亚热带沟谷季雨林群落具有热带雨林向亚热带常绿阔叶林过渡的明显特征,与南亚热带季雨林性质相似,在演替上常被称为侵入群落,或为历史时期长期演化形成的超地带性植物群落。     

湖南崀山丹霞地貌区维管植物区系特征分析及对比

采用线路与标准地相结合的调查方法,对湖南崀山丹霞地貌区维管植物的区系特征(组成、主要类群和种子植物属的分布区类型)进行了统计分析,并与舜皇山非丹霞地貌区维管植物区系特征进行了对比.崀山丹霞地貌区有维管植物185科689属1 464种(含变种),其中,蕨类植物25科49属84种,裸子植物5科8属8种,被子植物155科632属1 372种.蕨类植物和裸子植物绝大多数为种类数在10种以下的小科;被子植物中含30种以上的科有12个,种类数在50种以上的科为菊科(Compositae)、蔷薇科(Rosaceae)、蝶形花科(Papilionaceae)和禾本科(Gramineae);被子植物中含6种及6种以上的属有52属,种类数最多的是薹草属(Carex L.)(15种).崀山丹霞地貌区种子植物属的分布区类型具有热带、温带分布交会的特点,热带成分、温带成分和中国特有成分分别占总属数(不包括世界广布型属)的47.62%、47.79%和4.59%,其中泛热带分布型属、热带亚洲分布型属、北温带分布型属、东亚-北美间断分布型属、东亚分布型属以及中国特有分布型属具有重要地位.崀山丹霞地貌区的植物区系具有古老残遗性和丰富的特有成分,分布有新宁毛莨(Ranunculus xinningensis W. T. Wang)和崀山唇柱苣苔(Chirita langshanica W. T. Wang)2个特有种.崀山丹霞地貌区的植物区系与舜皇山非丹霞地貌区具有种类相对丰富、热带和温带成分所占比例相近等共同特点,但各分布区类型所占比例以及中国特有成分的组成及数量有一定差异,且崀山丹霞地貌区维管植物属和种的丰富度低于舜皇山非丹霞地貌区(维管植物792属2 232种).研究结果显示,崀山丹霞地貌区的生境狭窄,特有现象明显;丹霞地貌对种类分化、新物种形成、植物分布区类型比例和物种丰富度产生影响.     

云南中山湿性常绿阔叶林起源的探讨

云南中山湿性常绿阔叶林广泛分布于海拔1800~3400 m的山地,这类常绿阔叶林在生态外貌上具有亚热带常绿阔叶林特征,但其分布生境却是暖温带-温带气候,且植物区系组成与热带植物区系有古老的渊源。该文以研究得比较深入的哀牢山中山湿性常绿阔叶林为例,对其植物区系与其气候条件的不协调进行剖析。哀牢山的中山湿性常绿阔叶林记录了种子植物110科386属821种。在植物区系科的地理成分上,无论是含种数多的科,还是所有科的分布区类型,都是以热带分布科为主,体现了它的远古热带起源背景。在该种子植物区系中,热带分布属占总属数的47.75%,热带分布种占总种数的33.45%,在近代演化上仍体现出明显的热带亲缘特征。按照哀牢山中山湿性常绿阔叶林分布地区的暖温带-温带气候条件,它相当于中国东部的暖温带落叶阔叶林地区。在中国东部地区类似气候条件的地带性植被的植物区系中,热带分布属通常只占总属数的25%~27%,云南中山湿性常绿阔叶林植物区系的地理成分与所在地的温带气候明显不协调。对这种现象的解释,笔者认为结合哀牢山地区曾经是低海拔夷平面,在第四纪以来才迅速抬升形成的地质历史,可能这里曾经在第四纪以前的热带-亚热带性质的植物区系和常绿阔叶林随着地形的迅速抬升,逐渐适应了因海拔上升而形成的温带气候,成为在云南高海拔山地存在的所谓中山湿性常绿阔叶林,其植物区系和植被的热带-亚热带性质及常绿阔叶生态外貌并未因气候改变而发生改变。     

东北地区蒙古栎群落区系地理成分分析

分析了东北地区蒙古栎群落192个属分布区类型,其中温带分布属占72%,热带分布属占9.7%.也比较了东北地区10个地点和河北省1个地点的蒙古栎群落物种所在属的分布区类型,统计了不同地点属的分布区类型占总属的比例,计算了温带属与热带属(T/R)的比值,结果发现蒙古栎群落的温带分布属和T/R值(温带属和热带属之比值)不仅受纬度地带性影响,也受垂直地带性影响;在海拔相差不大的情况下蒙古栎群落T/R值随着纬度的递增而递增,热带分布属随着纬度递增而减少。垂直地带性对T/R之比率也有较大的影响,使得T/R值随纬度变化时出现波动。并给出了T/R值、纬度和海拔三者关系的回归方程,结果表明T/R值与纬度、海拔有着比较精确的数量关系。最后对这种分布格局产生的原因进行了解释.     

桂西地区南亚热带落叶栎林群落组成及物种多样性研究北大核心CSCD

落叶栎林是桂西地区南亚热带的典型次生林,也是该区域落叶阔叶林的重要群系组。该研究采用典型样方法对桂西地区落叶栎林群落进行调查,分析了该区域落叶栎林群落的物种组成、区系成分、物种多样性特征及其与地形因子的关系,为桂西地区南亚热带植物多样性保护与恢复提供依据。结果显示:(1)研究区落叶栎林群落维管束植物共计269种,隶属80科178属。(2)种子植物区系以热带成分为主,同时表现出一定程度的温带过渡性质。(3)聚类分析表明,调查的落叶栎林群落可分为云南波罗栎林、栓皮栎林、白栎林、麻栎林4种林分类型,其中以白栎林群落的物种多样性最高,且灌木层的物种多样性显著高于乔木层和草本层。(4)RDA分析显示,落叶栎林群落不同层次物种多样性的差异受地形因子的影响,多样性指标与经度、纬度、海拔之间具有明显的相关性(P<0.05),其中乔木层物种多样性主要与经度、纬度呈显著的相关性,灌木层物种多样性与纬度、海拔相关,草本层物种多样性与经度、纬度、海拔之间均有相关性。     

Special ecological effects of ravines in Danxia Landform, China

Danxia Mountain in Guangdong Province was investigated on the special ecological effects of ravines in Danxia Landform. The results showed that its geomorphologic ecological effects could be manifested in the following two aspects. Firstly, multitudinous ridgy stone peaks and hollow ravines were shaped in the forming process of Danxia Landform. Ecological factors were different between the ravines and other open regions. Relatively close microclimate and high moisture condition in ravines could provide suitable living environment for tropical species which preferred hot and humid environment. Geomorphologic environment in ravines, like smooth degree of surrounding cliffs, would affect intensity of light reflected into ravines. All the aspects had influence on the temperature and humidity in ravines. Secondly, the special ecological effects of ravines in Danxia Landform provided a possibility to gestate a group of taxa with greater tropical characteristics. There, tropical plant flora was markedly increased in comparison with other vegetations at similar latitude. Tropical plant distributions were obvious in most ravines of Danxia Landform. Its proportion was 10% more than that of other regions at the similar latitude. The ravines in Danxia Landform were rich in liana, ferns and other plants with high water-logging resistance. Collectively, the phenomena that some typical species in south subtropical regions appeared in mid-subtropical regions revealed latitudinal shift of plant distribution. This kind of climax communities, which were coordinated and balanced with their geomorphologic environments due to the special ecological effects of ravines in Danxia Landform, could be called geo-climax communities.     

Ecological effect on the hilltop of Danxia Landform

The hilltop ecological effect of Danxia Landform generated by the distinct physiognomy and topography was investigated. The characteristic differences in ecological factors, community structure and species ecotype between hilltop and foot gulch and those of adjacent non-Danxia Landform were determined. The results showed that the mean daily temperature on the hilltop was higher than that at the foot gulch. But the average relative humidity and community diversity on the hilltop were lower than those at the foot gulch. In contrast to those on the hilltop, plants at the foot gulch showed stronger tropical character. All of the characteristics above were different from those in other landforms. In addition, ecotypic differentiations in leaf area, specific leaf area, bark, height under branch and crown width were found in the studied species between the hilltop and the foot gulch. Moreover, the hilltop of Danxia Landform was thought to be of significance in the scientific research of ecotype, island biogeography and adaptive evolution. Further studies are needed in order to better understand the universality of ecological effect on the hilltop of Danxia Landform.     

论丹霞地貌区生态演替特征及其科学价值

论述了丹霞地貌区生态演替的特征及其科学价值.认为植被演替由于时间漫长、过程复杂而对其研究具极大的难度,时空互代成为演替研究的重要手段,而这需要有完整的空间序列.丹霞地貌区存在着完整的原生演替与次生演替系列.典型丹霞地貌的山顶为原生演替的矮灌木林和乔木林,周围斜坡仍然受季节性降水侵蚀、风化、重力崩塌等作用,原生演替不断从裸露的岩石开始,故形成原生演替早期的苔藓、草本群落,随着岩石的进一步风化和苔藓、地衣等植物的作用,土壤层增厚,将原生演替继续往前推进.特殊的地质地貌过程使之不断有新的崩塌,从裸露的岩石开始的新的原生演替,如此形成不同时间系列的原生演替阶段.丹霞地貌区也存在着完整的次生演替系列,同时存在演替先锋林、演替过渡林和演替基本稳定林.这两个演替系列提供了一个非常难得的理想场所,使得生态学工作者在一个地点就可以观察到一个完整的植被演替系列.其研究可为该区域植被的经营管理和保护措施提供必要的依据.作为生态恢复参照系,对区域的植被生态恢复具有重要的指导意义.＃     

Characteristics and scientific values of ecological succession in Danxia Landform of China

The characteristics and scientific values of ecological succession in Danxia Landform of China were discussed. It was known that research on vegetation succession was quite difficult for its long-term and intricate process. Space-time substitution is an important method to study the succession, while it needs intact spatial succession series. In Danxia Landform, there are such primary and secondary succession series. On the hilltops, there are typical low shrubberies and arboreal forests of primary succession. The surrounding slopes are subjected to seasonal rainfall erosion, weathering action, gravitational collapse and so on. The primary succession constantly starts from bare rocks, and then moss and herbal communities of early primary succession are formed. With further weathering of rocks and effects of moss and lichen, soil layers are getting thicker and thicker, which pushes primary succession ahead. New collapses are ceaselessly induced by the special geological geomorphological process, and then a new primary succession starts from bare rocks. Thus, different stages of primary succession are formed in Danxia Landform. In addition, the secondary succession series exist in Danxia Landform, including the pioneer forests, transitional forests and steady forests. Danxia Landform provides ideal sites for vegetation succession study. The relative studies would be helpful for the vegetation management and protection in this area. As ecological restoration reference, it is also meaningful for the vegetation restoration.     

Species richness in tropical fresh waters of Australia

General ecological expectations about the relationship between latitude and species richness are that at low latitudes (the tropics) species richness is greater than at higher latitudes (temperate and polar regions). Recent work suggests that this may not be the case for several habitat types and biological groups in Australia. Results are conflicting: on present evidence (admittedly sparse) it appears that in Australian tropical fresh waters species richness is generally depressed in zooplankton and littoral microfaunal communities, but not in macroinvertebrate communities in typical streams and in fish communities (and perhaps also in amphibian and reptile communities). The situation is indeterminate for tropical phytoplankton and macrophyte communities.     

Vegetative Community Compositional Gradients of Tropical Hardwood Hammocks along the Florida Keys

Tropical hardwood hammocks, among the rarest and most threatened vegetative communities in the United States, occur throughout the 225-km Florida Keys archipelago as it extends toward the Caribbean from the southeast tip of peninsular Florida. Compounding their critical conservation status, tropical hardwood hammocks and the dynamics that support their peculiar species diversity in the region are poorly understood. The goal of this study was to explore the dynamics of the species compositional gradient of the hammocks along the Florida Keys, and to identify significant ecological units within the gradient. The primary data for this research were assembled from the Institute for Regional Conservation's floristic database of South Florida. We were able to extract presence/absence data for 295 species from comprehensive surveys of 23 study sites. Nonmetric multidimensional scaling was used to deconstruct the compositional trends into a reduced ordination space. Cluster analysis was subsequently used to identify discrete ecological units. Additionally, we used vector fitting to interpret the significant correlated ancillary variables. Our main results were three well-fitted nonmetric multidimensional scaling axes with three nonoverlapping ecological units. Of the ancillary variables, latitude, longitude, percent composition from biogeographical regions, richness, and area were correlated to the nonmetric multidimensional scaling results. These results increase our understanding of the community structure of the hammocks along the Florida Keys, and can contribute to increasing our ability to adequately protect and restore tropical hardwood hammocks and other similar tropical dry forest communities throughout the Caribbean.     

Comparative analysis of the floristic richness of alpine communities in the Caucasus and the Central Alps

Abstract. Species richness of selected alpine plant communities in the Teberda Biosphere Reserve (Northwestern Caucasus) and the Davos area (Central Alps) was compared in series of plots from 0.0025 to 100 m². Communities developing under similar ecological conditions and with similar syntaxonomic positions were compared in order to estimate the role of recent environment versus regional historical factors in determining plant community structure and diversity. The floristic richness of the Caucasian and Alpic fens was very similar. The Grasslands and Meadows were quite similar as to floristic richness for plots > 25 cm × 25 cm, but the Caucasian communities had fewer species in smaller plots. The Lichen heath at Teberda was richer than the Caricetum curvulae cetrarietosum for all plot sizes, except the two smallest ones. On the other hand, the plots of the Salix Snowbed community were richer in species than the Caucasian snowbeds for all plot sizes. The Rhododendron Shrubland plots were very similar as to floristic richness in larger plots (4 — 100 m²). Generally, most Alpic communities near Davos were richer in species at small plot sizes than the corresponding communities from Teberda. Caucasian communities were floristically less similar to each other — and thus more discrete — than the Alpic ones. The possible role of different factors controlling floristic richness of the communities is discussed. Our results suggest that recent ecological conditions have a big influence on local floristic diversity and may lead to high similarities between ecologically similar communities from different regions. In addition, the general floristic richness of a regions as well as island effects should be taken into account.     

广东优势群落甜槠林多样性研究

采用每木调查法,对广东粤北石门台和粤中象头山地区甜槠（Castanopsis eyrie（Champ.） Tutch.）林样方内胸径≥ 1 cm的乔、灌木进行测量,记录其种名、胸径、高度和在样方中的坐标位置等指标,对群落的植物组成、区系成分、优势种及物种多样性进行分析。结果显示：石门台样地有维管植物112种,隶属36科54属;象头山样地有维管植物109种,隶属36科59属。两个群落均具有明显的热带向亚热带过渡的性质。其中,石门台样地与华东、华中地区联系紧密;象头山样地则与中国台湾、日本的岛屿联系更多。比较两个地区的群落特征发现,他们的相似性较高,物种多样性指数接近,纬度并不是决定群落植物多样性高低的因素,小环境、群落演替进程及人为因素对群落植物多样性的影响更大。     

Potential warm-stage microrefugia for alpine plants: Feedback between geomorphological and biological processes

During interglacial stages, microrefugia are sites that support locally favorable climates within larger areas with unfavorable warmer climates. Despite recent theoretical representations of microrefugia, an appropriate ecological characterization is still lacking, mostly for warm periods. Across mountain/alpine areas, cold-adapted plant species could adopt different strategies to manage the effects of climate warming: (A) migration toward higher elevations and summits; (B) in situ resilience of communities and species populations within microrefugia; and C) adaptation and evolution by genetic differentiation. This review aims to distinguish and characterize from an ecological perspective glacial, nival, periglacial and composite landforms and deposits that may function as potential microrefugia during interglacial warm periods.We conducted a literature screening related to the geomorphological processes and landforms associated with vegetation and plant communities in alpine/mountain environments of Europe. They include glacial deposits rock glaciers, debris-covered glaciers, composite cones and channels. In Alpine regions, geomorphologic niches that constantly maintain cold-air pooling and temperature inversions are the main candidates for microrefugia. Within such microrefugia, microhabitat diversity modulates the responses of plants to disturbances caused by geomorphologic processes and supports their aptitude for surviving under extreme conditions on unstable surfaces in isolated patches. Currently, European marginal mountain chains may be considered as examples of macrorefugia where relict boreo-alpine species persist within peculiar geomorphological niches that act as microrefugia.This review contributes to identifying potential warm-stage microrefugia areas across alpine and mountain regions and determining certain landforms that play or may play such role under global-change scenarios. The occurrence of warm-stage microrefugia within these locations may be of great importance for the modeling of future distributions of species and assessing the risk of extinction for alpine species. Microrefugia may have important implications in micro-evolutionary processes that occur across alternating climatic phases.