四川省峨眉山森林植被垂直分布的初步研究

本文对四川省峨眉山森林植被的垂直分布特点进行了初步研究。文中,采用数量分类的方法,结合对群落生态外貌特点和区系组成的分析,以及群落所处海拔高度,划分出森林植被的垂直带如下：1．常绿阔叶林带 1900米以下;2．常绿、落叶阔叶混交林带 1500米至2000米;3．针阔混交林带 2000米至2500米;4．寒温性针叶林带 2500米至3099米。     

Altitudinal distribution of evergreen broad-leaved trees and their leaf-size pattern on a humid subtropical mountain,Mt. Emei,Sichuan, China

Altitudinal distribution of evergreen broad-leaved trees and changes in their leaf sizes were studied on a humid subtropical mountain, Mt. Emei (3099 m a.s.l., 29°34.5 N, 103°21.5 E), Sichuan, China. Among the total woody flora of ca. 540 species, evergreen broad-leaved trees account for 88 species in 39 genera and 23 families, corresponding to the northern limit of subtropical evergreen broad-leaved trees. The number of evergreen broad-leaved tree species greatly decreased from the low-altitudinal, evergreen broad-leaved forest zone (600–1500 m) to the mid-altitudinal, mixed forest zone (1500–2500 m), and to the high-altitudinal, coniferous forest zone (2500–3099 m). The overall trend of reduced leaf size toward upper zones was analyzed and documented in detail. The 88 species were assigned to three leaf-size classes: notophylls (48%), microphylls (36%), and mesophylls (16%). The leaf size was relatively small and the specific leaf weight (SLW, mg cm^–2) was much larger in high altitude as compared to low altitude. No overall correlation was found between leaf size and SLW, but leaf size decreased as SLW increased toward high altitude for certain species having relatively wide altitudinal ranges. Moreover, leaf size varied with forest stratification: canopy trees were predominantly notophyllous species, while subcanopy and understorey trees were mainly microphyllous species. The tendency is compatible with the trend found in other mountains of East Asia.     

陕西省化龙山森林植被垂直分布的初步研究

 本文对陕西省化龙山植被的垂直分布特点进行了初步研究。文中采用了数量分类结合对群落生态特点及区系组成的分析,划分出森林植被垂直带如下：常绿、落叶阔叶混交林带,海拔1600m以下;落叶阔叶林带,海拔1600—2200m;亚高山针叶林带,海拔2200—2917m。     

Ecology of the pteridophytes on the southern slopes of Mt. Kilimanjaro – I. Altitudinal distribution

140 taxa of 61 genera in 24 families of pteridophytes were recorded on the southern slopes of Mt. Kilimanjaro. These represent about one third of the entire pteridophyte flora of Tanzania. The families richest in species are the Aspleniaceae, the Adiantaceae, the Dryopteridaceae, the Thelypteridaceae and the Hymenophyllaceae. Due to its luxuriant montane rain forest, which receives a precipitation of up to over 3000 mm, Mt. Kilimanjaro is distinctly richer in pteridophyte species than other volcanoes in East Africa. However, compared with the mountains of the Eastern Arc, the number of pteridophytes on Mt. Kilimanjaro is smaller. This can be explained by the widely destroyed submontane (intermediate) forest rather than by the higher age of the Eastern Arc Mts.The altitudinal distribution of all ferns was investigated in 24 transects. On the southern slopes of Mt. Kilimanjaro they were found in an altitudinal range of 3640 m. Cyclosorus quadrangularis, Azolla nilotica, Azolla africana andMarsilea minuta are restricted to the foothills, while Polystichum wilsonii, Cystopteris nivalis and Asplenium adiantum-nigrum are species found in the highest altitudes.Based on unidimensionally constrained clustering and on the analysis of the lowermost and uppermost occurrence of species, floristic discontinuities within the transects were determined. From these data and from an evaluation of the distribution of ecological groups and life forms, 11 altitudinal zones could be distinguished: a colline zone (–900 m asl), a submontane zone (900–1600 m asl) with lower and upper subzones, a montane zone (1600-2800 m asl) divided into 4 subzones, a subalpine zone (2800–3900 m asl) with lower, middle and upper subzones, and finally a (lower) alpine zone above 3900 m. The highest species numbers were observed in the lower montane forest belt between 1600 and 2000 m altitude. The zonation of ferns found at Mt. Kilimanjaro corresponds well with the vegetational zonation described by other authors using bryophytes as indicators in different parts of the humid tropics.     

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。     

Forest vegetation as related to climate and soil conditions at varying altitudes on a humid subtropical mountain, Mount Emei, Sichuan, China

Altitudinal variations in temperature and soils were analysed on a humid subtropical mountain, Mt Emei (3,099 m a.s.l., 29°34.5N, 103°21.5E), in Sichuan, China, to see how the vegetation varies with the environmental factors. As a principal finding, the coldest mean monthly temperature –1°C, rather than the warmth index of 85°C·months, emerged as the primary factor that delimited the evergreen broadleaved forest. With regard to soils, properties such as organic C, total N, available P, exchangeable K tended to increase with altitude. The highest values in organic C (26.6%), total N (1.34%) and available P (45.39 ppm) were recorded in surface soils of the mixed forest (2,210 m a.s.l.) including all three tree life forms, i.e. evergreen/deciduous broadleaved and coniferous trees. The high pH and contents of exchangeable Ca and Mg in the surface soils derived from the parent material, limestone and dolomite, between 900 and 1,200 m, where several Tertiary tree species existed. The C/N ratios of surface soils in the coniferous forests (2,500–3,099 m) were higher than those of the evergreen broadleaved forests (600–1,500 m) and the mixed forests (1,500–2,500 m).     

Characteristic and representativeness of the vertical vegetation zonation along the altitudinal gradient in Shennongjia Natural Heritage北大核心CSCD

Aims Mountains contain broad environmental gradients, which are to be an outstanding universal value representing significant on-going ecological and biological processes in the evolution and development of zonal vegetation along the elevation gradients. Exploring the biological and ecological value of the vegetation zonation along the elevation gradients of Chinese mountain natural heritage site is important for biodiversity conservation and management. Methods Based on the community survey data of the six vegetation zonation along the elevational gradients in Shennongjia, the global land use dataset, and the literature data of the communities along the altitudinal gradients of other natural heritage sites and the nominated world natural heritage sites in Oriental Deciduous Forest Biogeographic Province by Udvardy, we explored the outstanding universal value of the zonal vegetation along the altitude gradients by the methods of spatial analysis. Important findings Shennongjia heritage site preserves the intact vegetation zonation of the typical Oriental Deciduous Forest Biogeographical Province in the Classification of the Biogeographical Provinces of the World by Udvardy, including evergreen broad-leaved forests (South Slope of the Heritage Site), evergreen deciduous broad-leaved mixed forests, deciduous broad-leaved forests, coniferous and broad-leaved mixed forests, coniferous forests and subalpine shrub and meadow along the elevation gradients. The altitudinal zonation of vegetation in the Shennongjia heritage site represented a variety of bio-ecological processes, such as the turnover of the dominant trees along the altitudinal gradients, and is an outstanding example of the ongoing ecological processes occurring in the development of intact subtropical mixed broadleaved evergreen and deciduous forest in the Northern Hemisphere. © 2018 Editorial Office of Chinese Journal of Plant Ecology. All Rights Reserved.     

Tertiary relic deciduous forests on a humid subtropical mountain, Mt. Emei, Sichuan, China

The floristic characteristics, age structure and survival modes of Tertiary-relic deciduous forests were analyzed at 1600 m on Mt. Emei (3099 m), Sichuan, China. Three plots were selected to represent typical topographies: Plot 1 at 1620 m on a scree slope, Plot 2 at 1640 m on a slope with moderately rocky soils, and Plot 3 at 1616 m on a gentle slope with less rocky soils. At Plot 1, on the scree slope, the forest was rich in species and dominated by Tertiary remnants and other deciduous trees (Davidia involucrata, Styrax hemsleyana, Cercidiphyllum japonicum var.sinense, Pterocarya hupehensis, Prunus brachypoda, Prunus padus, Tetracentron sinense andStaphylea holocarpa). The relic deciduous tree taxaDavidia, Cercidiphyllum, Tetracentron andEuptelea occupied the unstable concave slopes, where evergreen broad-leaved trees (Castanopsis platycantha andMachilus pingii) were rarely able to survive. On the relatively stable convex slopes of this plot, evergreen trees with small diameter mainly appeared in the subcanopy and shrub layers.Davidia involucrata was the dominant species in this forest. On the slope with moderately rocky soils (Plot 2), the forest was co-dominated by relicDavidia and other deciduous (Styrax andPterocarya), and evergreen trees (Castanopsis andMachilus). On the gentle slope with less rocky soils (Plot 3),Davidia trees were found only in the subcanopy and shrub layers, and the forest was dominated byMachilus, Castanopsis, Styrax andPrunus trees. Regeneration ofDavidia occurs mainly on the scree slope where landslides are most common. The age structure of theDavidia stands indicates that this species is able to survive on the unstable scree habitat due to its strong sprouting ability. The Tertiary-relic deciduous forest on the scree slope is seen to be a topographic climax forest.     

Characteristic and representativeness of the vertical vegetation zonation along the altitudinal gradient in Shennongjia Natural Heritage

Aims Mountains contain broad environmental gradients, which are to be an outstanding universal value representing significant on-going ecological and biological processes in the evolution and development of zonal vegetation along the elevation gradients. Exploring the biological and ecological value of the vegetation zonation along the elevation gradients of Chinese mountain natural heritage site is important for biodiversity conservation and management.Methods Based on the community survey data of the six vegetation zonation along the elevational gradients in Shennongjia, the global land use dataset, and the literature data of the communities along the altitudinal gradients of other natural heritage sites and the nominated world natural heritage sites in Oriental Deciduous Forest Biogeographic Province by Udvardy, we explored the outstanding universal value of the zonal vegetation along the altitude gradients by the methods of spatial analysis.Important findings Shennongjia heritage site preserves the intact vegetation zonation of the typical Oriental Deciduous Forest Biogeographical Province in the Classification of the Biogeographical Provinces of the World by Udvardy, including evergreen broad-leaved forests (South Slope of the Heritage Site), evergreen deciduous broad-leaved mixed forests, deciduous broad-leaved forests, coniferous and broad-leaved mixed forests, coniferous forests and subalpine shrub and meadow along the elevation gradients. The altitudinal zonation of vegetation in the Shennongjia heritage site represented a variety of bio-ecological processes, such as the turnover of the dominant trees along the altitudinal gradients, and is an outstanding example of the ongoing ecological processes occurring in the development of intact subtropical mixed broadleaved evergreen and deciduous forest in the Northern Hemisphere.     

Altitudinal zonation of human-disturbed vegetation on Mt. Tianmu,eastern China

Much of the primary vegetation at low altitudes has been greatly altered or destroyed by a long history of human activities. This is particularly true in eastern China, where low-altitude areas are now dominated by secondary forests or plantations. Altitudinal vegetation zonation of this region is often based on these secondary forests, resulting in seral vegetation with an obscure zonal sequence. Here, we deduced the potential climax vegetation according to the regeneration patterns of the dominant species of the secondary forests at low altitudes (below 1,000 m a.s.l.) on Mt. Tianmu (1,506 m a.s.l., 30°18′30″–30°21′37″N, 119°24′11″–119°27′11″E). Based on the potential climax vegetation combined with the floristic composition and community structure, three vegetation zones were identified, viz: (1) evergreen broad-leaved forest zone (400–950 m a.s.l.); (2) evergreen and deciduous broad-leaved mixed forest zone (950–1,100 m a.s.l.); (3) deciduous broad-leaved forest zone (1,100–1,506 m a.s.l.). The altitudinal vegetation zones identified in this study correspond with the thermal conditions on Mt. Tianmu. The distribution of vegetation on Mt. Tianmu was limited by lower temperatures in winter, and the altitudinal thermal vegetation zones on this mountain were more similar to the thermal vegetation of Japan than to that of China. The vertical distributions and roles of conifers were different between the eastern and the western regions along 30°N latitude in humid East Asia. Cryptomeria fortunei formed the emergent layer, towering above the broad-leaved canopy at middle altitudes as C. japonica on Yakushima, but disappeared at high altitudes with hydrothermal limitation on Mt. Tianmu.     

Leaf size zonation pattern of woody species along an altitudinal gradient on Mt. Pulog,Philippines

Leaf size zonation along an altitudinal gradient from 2000–2700 m a.s.l. on Mt. Pulog, Cordillera mountain range, Luzon Is., Philippines was examined using the Raunkiaer-Webb classification system. The entire altitudinal range studied was dominated by the small leaf size classes which possess thick, lustrous, pubescent leaves adapted to high evapotranspiration, cold temperature and other stressful conditions. Altitudinal leaf size zonation was identified as follows: (1) pure needle leaved zone from 2000–2300 m a.s.l., (2) mixed needle leaved/microphyllous zone from 2300–2400 m a.s.l., (3) microphyllous zone from 2400–2600 m a.s.l. and, (4) microphyllous/nanophyllous zone from 2600–2700 m a.s.l., coinciding with the altitudinal vegetation zonation. This pattern is different from that in other tropical mountains, which usually show a gradual shift from a mesophyllous zone in the lowland to a nanophyllous zone in the upper subalpine. Stressful conditions such as steep topography (1200–2300 m a.s.l.), cloud cover, decrease of temperature, strong winds (2600–2700 m a.s.l.) could have influenced the altitudinal leaf size zonation on Mt. Pulog. The complex phytogeographical position of Mt. Pulog as a transition region between the tropics and subtropics have also influenced leaf size zonation as in eastern Himalaya, southwestern China and Taiwan.     

Aquatic and terrestrial vegetation of the Prespa area

We studied the vegetation of the aquatic ecosystems ofLake Mikri Prespa. The lacustrine vegetationcomprises three distinct forms: floating plants,benthic hydrophytes and helophytes, which aredescribed and classified from the phytosociologicalpoint of view, as follows: (a) the vegetation of thefloating plants belong to the Lemnetea class and isrepresented by two plant communities; (b) thevegetation of the benthic hydrophytes, belongs to thePotametea class consisting of two differentcategories, namely the submersed formations and theemergent formations of the hydrophytes. Various plantcommunities were recognised in this type of vegetationand three among them are considered as the mostrepresentative; (c) the vegetation of helophytes, theprevailing life form in this wetland, belongs to thePhragmitetea class and is represented mainly by sevenwell organised plant communities. The respectivevegetation of two of the five more important wetlandsites is described.The terrestrial vegetation is composed of forestand meadow vegetation. The forest vegetation of theNational Park belongs to the class Querco-Fagetea andshows the following zonation: (a) in the vicinity ofthe lake, at the elevation of 860–1000 m, twoassociations have been found: the mixed deciduous andevergreen forests of Ostryo-Carpinion orientalis andthe evergreen forests of Ostryo-Carpinion adriaticum;(b) the deciduous oak forests surround the previouszone at the altitude of 900–1300 m with two principalassociations, namely the Quercetum frainetto and theQuercetum petraeae; (c) in the upper forest layerbetween 1200–1800 m asl, dominate beech forests of theassociation Fagion moesiacum and the less extensiveoccurrence of the mixed beech-fir stands (Ass.Abieti-Fagetum moesiacum).The zone above the tree limit is distinguished by itssubalpine character semi-shrub vegetation extendinghigher than the forest (1800–2000 m), whereas alpine meadowscover the vegetation at higheraltitudes. On the plains and in the forest clearingsexist herbaceous meadow formations of variablestructure, in parallel with the vegetation of specifichabitats, such as nitrophilous and ammophilousplants.     

Pattern of changes in species diversity,structure and dynamics of forest ecosystems along latitudinal gradients in East Asia

We examined effects of seasonality of climate and dominant life form (evergreen/deciduous, broad-leaf/coniferous) together with energy condition on species diversity, forest structure, forest dynamics, and productivity of forest ecosystems by comparing the patterns of changes in these ecosystem attributes along altitudinal gradients in tropical regions without seasonality and along a latitudinal gradient from tropical to temperate regions in humid East Asia. We used warmth index (temperature sum during growing season, WI) as an index of energy condition common to both altitudinal and latitudinal gradients. There were apparent differences in patterns of changes in the ecosystem attributes in relation to WI among four forest formations that were classified according to dominant life form and climatic zone (tropical/temperate). Many of the ecosystem attributes—Fishers alpha of species-diversity indices, maximum tree height and stem density, productivity [increment rate of aboveground biomass (AGB)], and population and biomass turnover rates—changed sharply with WI in tropical and temperate evergreen broad-leaved forests, but did not change linearly or changed only loosely with WI in temperate deciduous broad-leaved and evergreen coniferous forests. Values of these ecosystem attributes in temperate deciduous broad-leaved and evergreen coniferous forests were higher (stem density was lower) than those in tropical and temperate evergreen broad-leaved forests under colder conditions (WI below 100°C). Present results indicate that seasonality of climate and resultant change in dominant life form work to buffer the effects of energy reduction on ecosystem attributes along latitudinal gradients.     

Structural comparison of tropical montane rain forests along latitudinal and altitudinal gradients in south and east Asia

Geographical patterns of altitudinal zonation, floristic composition, and structural features of tropical montane rain forests were examined along latitudinal gradients in south and east Asia. On equatorial mountains, the tropical montane rain forests occur above 1000 m. Toward middle latitudes, they come farther down and reach sea level at c. 35° N. Thus, the forests are equivalent to the subtropical rain forests of the latitudinal, horizontal zonation series. They exhibit gradual changes in floristic composition and structure along both altitudinal and latitudinal gradients. On equatorial mountains, they are divided into three types, i.e. tropical lower montane, upper montane, and subalpine forests. The three tree regeneration types, having emergent, sporadic and inverse-J type stem-diameter class frequency distributions, coexist in the lower montane forests, but the upper and subalpine forests display only the inverse-J type species with a few species of the sporadic type. Toward the northern latitudinal limit, the distinction between the three tropical montane forest zones in equatorial mountains becomes less clear. This can be explained by temperature conditions: on equatorial mountains, a temperature sum of 85° C months which controls the upper limit of the lower montane forests, and a coldest month mean temperature of-1° C which controls the evergreen broad-leaved trees, appear at c. 2500 and c. 4000 m respectively. The altitudinal range between 2500 m and 3800 m, which is the upper forest limit, is covered by upper montane and subalpine forests. On the other hand, at the latitudinal northern limit, the tropical upper montane and subalpine forests cannot exist because the above mentioned two temperature conditions occur at nearly the same point. Thus, at the northern latitudinal limit of the tropical montane forests, the three zones of equatorial mountains amalgamate into a single subtropical lowland forest community. This is due to the seasonal temperature climate in middle latitudes in, e.g., central Japan and central China.A part of this paper was presented as an oral presentation at the Vth International Congress of Ecology, Yokohama 23–30.8.1990.     

峨眉山常绿落叶阔叶混交林的生物多样性及植物区系初探

对峨眉山常绿落叶阔叶混交林的群落结构﹑组成﹑生物多样性及植物区系等几方面进行了研究分析。结果显示峨眉山阔叶混交林由226种维管束植物组成,其中被子植物73科137属207种, 占总种数的91.6%,是峨眉山阔叶混交林的重要组成部分;群落分层现象明显,为乔木层﹑灌木层﹑草本层和层外植物4层,其中草本层发育情况差;科分布型是以热带—亚热带﹑热带—温带为主,各占22.7%, 在属的水平上则以温带分布占绝对优势(52.9%),揭示了峨眉山阔叶混交林的区系性质是以温带为主的亚热带类型;生物多样性指数处于较低的水平,在经过人为干扰后,群落处于稳定的恢复阶段。     

Altitudinal zonation of montane Quercus forests along two transects in Chirripó National Park,Costa Rica

Abiotic and vegetation data were collected along two altitudinal transects through mature montane Quercus forests on the Pacific and Atlantic slopes of Costa Rica's Chirripó Massif. Between 2000 and 3200 m asl twenty-four 0.05 ha forest plots were selected at altitudinal intervals of 100 m, and eight soil profiles were described at intervals of 200 m. A TWINSPAN classification aided in the determination of eight zonal forest communities on the basis of their floristic composition. They are grouped in two sets of four: (i) the palm-rich lauraceous-fagaceous Lower Montane Mollinedia-Quercus Forests (2000–2600 m asl) and (ii) the bamboo-rich myrsinaceous-fagaceous Upper Montane Schefflera-Quercus Forests (2500–3200 m asl), respectively. Vegetation changes seem correlated with two major climatic gradients: (i) a temperature gradient (altitude), and (ii) a moisture gradient (wet Atlantic vs. moist Pacific slope). Most soils are Andepts, and residual, colluvial or derived from volcanic material. Humus layers are thicker on the wetter Atlantic slope. A total of 431 vascular plant species consisted of 86 pteridophytes, 1 gymnosperm, 296 dicots and 48 monocots. Species richness, canopy height and stem diameter decrease with increasing altitude, while the canopy surface becomes more flattend. A comparison with other studies shows that Chirripó's montane Quercus forests fit within the environmental ranges known from altitudinal zonations elsewhere in the Tropics.Abbreviations asl above sea level - dbh diameter at breast height - LM Lower Montane - Mt. Mountain - TWINSPAN two way indicator species analysis - UM Upper Montane - VU code referring to soil profiles as presented in Van Uffelen (1991) This paper is dedicated to the memory of Alwyn H. Gentry, an outstanding and inspiring tropical botanist who tragically died in a plane crash in the mountains of Ecuador on August 3 1993, when surveying possible boundaries for a new tropical cloud forest reserve.     

短尾猴栖息地的季节变化

本文阐述了短尾猴栖息地的季节变化。春季,主要利用海拔570-1600米的常绿阔叶林、常绿、落叶阔叶混交林和落叶阔叶林;夏季,限于海拔1000米以上的落叶阔叶林。秋季的栖息地,在海拔650-1200米常绿阔叶林和常绿、落叶阔叶混交林;冬季仅利用海拔600-900米的常绿阔叶林。此外还报道了短尾猴四季的食物组成。并对栖息地的变化原因,做了初步探讨。     

Coexistence mechanisms of evergreen,deciduous and coniferous trees in a mid-montane mixed forest on Mt. Emei,Sichuan, China

Structure and regeneration of a mid-montane (2200 m a.s.l.)mixed forest codominated by evergreen (Lithocarpuscleistocarpus), deciduous (Acer flabellatum)andconiferous (Tsuga chinensis, Abies fabri, andTaxus chinensis) trees were analyzed in a 40m× 60 m plot on Mt. Emei, Sichuan, China. Plant communitystructure and composition varied depending on topographic micro-habitat withinthe plot. Four topographic communities (topo-communities) were distinguishedwith dominant species corresponding to topography: (1)Abies – valley bank, (2) Acer– lower steep slope, (3) Lithocarpus – uppergentle slope, and (4) Tsuga – ridge. The coexistencemechanisms of the evergreen, deciduous, and coniferous trees were determined byidentifying the regeneration process characteristic of each dominant species,asrepresented by their seedling dispersion patterns and seedling establishmentalong the topographic gradients. The saplings and seedlings of the dominantswere distributed differently according to the topography:Lithocarpus under the canopy of parent trees and in gapsofthe upper gentle slope and ridge, Acer mainly in bothwell-lit and shady sites on the lower steep slope and on fallen logs,Abies on the valley bank but only in well-lit sites,Tsuga on the ridge, Taxus mostly onrock and well-lit sites on the slopes. Distribution of surviving saplings andseedlings was also related to the species of nearby canopy trees. We suggestthat Lithocarpus, Tsuga and Acer tendto be self-replacing in their own topographic habitats, andAbies survives as a fugitive by occupying occasionalsuitable gaps. The variation in soil conditions, particularly nutrients, withtopography affected seedling establishment and the growth of trees. Thesuccessional change of quantitative species composition, as predicted by theMarkovian model, shows the mixed forest to be in a sustained climax stage.     

An altitudinal transect study of the vegetation on Mount Kinabalu,Borneo

A quantitative transect analysis of altitudinal sequences of forest canopy species from 600 to 3400 m asl on Mt. Kinabalu (4101 m), Borneo, resulted in four discrete altitudinal vegetation zones. These were made up of mutually exclusive species groups for lowland (<1200 m asl), lower montane (1200 to 2000–2350 m asl), upper montane (2000–2350 to 2800 m asl), and subalpine (2800 to the forest line, 3400 m asl) zones. Zonal soil types were correlated with the vegetation zones. In upslope sequence, these were: lowland Oxisols, montane Histosol/Spodosol complex, and subalpine Inceptisols. The highest contents of organic carbon, extractable phosphorus, and exchangeable magnesium and potassium were recorded in the lower and upper montane zones. The upper boundaries of the lowland, upper montane and subalpine zones coincided with thermal thresholds of latitudinal bioclimatic zones: 18°C TMIN (Köppen's tropical), WI 85 (Kira's warm temperate), and WI 45 (Kira's cool temperate), respectively. The upper limit of the lower montane zone was correlated with an abrupt increase of water surplus estimated from the annual rainfall minus annual potential evaporation. These climatic characteristics appear to define ecological altitudinal turnover points, so called critical altitudes, where groups of associated species are displaced by other groups.Abbreviations asl = above sea level - DBH = diameter at breast height - PHQ = Park headquarters - TMAX = Mean daily maximum air temperature - TMIN = Mean daily minimum air temperature - TWINSPAN = Two-way indicator species analysis - WI = Warmth index