Advances in biogeography of the tropical rain forest in southern Yunnan, southwestern China

Zhu Hua^1
1 Xishuangbanna Tropical botanical Garden, the Chinese Academy of Sciences, Kunming, 650223. E-mail: [email protected]

Abstract The tropical rainforest of southern Yunnan, which is similar to the equatorial rainforest of Asia in floristic composition and physiognomy, is a type of tropical Asian rainforest. Its tropical floristic elements contribute more than 90% at the generic level and more than 80% at the specific level to the total flora. Those of typical tropical Asian distribution contribute about 75% of the species. Occurring at the northern edge of the tropical zone (up to 24°40' N), the tropical rainforest of Yunnan differs from the equatorial rainforest in having deciduous trees in the canopy layer and fewer megaphanerophytes and epiphytes, but more abundant lianas as well as more plants with microphyllous leaves. It is suggested that the tropical rainforest did not emerge until the late Tertiary in the region, and that the rainforest is more dependent on topography and local habitats than on the regional climate. Key words: Tropical rain forest, plant diversity, biogeography, southern Yunnan, China 摘要 摘要 中国云南的热带雨林具有与亚洲赤道热带雨林类似的生态外貌特征和植物区系组成，是热带亚洲雨林的一个类型.云南的热带雨林中有多于90%的属和多于80%的种为热带植物区系成分，其中约75%的种为热带亚洲成分。由于发生在季风热带北缘山地(up to 24°40' N)，云南热带雨林在其林冠层中有落叶树种存在，大高位芽植物和附生植物较逊色而藤本植物和在叶级谱上的小叶植物更丰富，这些特征又有别于赤道低地的热带雨林. 云南热带雨林是在晚第三纪以后才发展起来, 它们的分布主要受制于局部生境，并非地区性气候条件. 关键词：云南，热带雨林，生物地理

Received: 16 January, 2008, Accepted: 18 February, 2008, Published: 3 March, 2008

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Cite this paper as: Zhu Hua. 2008. Advances in biogeography of the tropical rain forest in southern Yunnan, southwestern China. Tropical Conservation Science 1(1):34-42. Available online: tropicalconservationscience.org.

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Introduction

The tropical area of southern China located at the northern edge of tropical Asia, including southeastern Xizang (Tibet), southern Yunnan, southwestern Guangxi, southern Taiwan and Hainan Island between 86° and 123° E, 18°21' and 24°40' N with a disjunct site at c. 29° N in southeastern Xizang [1]. The largest tropical area still covered by forests is in southern Yunnan.



Fig 1. Province of Yunnan, China

The tropical areas in southern Yunnan are those of valleys and lower montane generally below 900 m asl. between 21°01' and 24°40' N [2]. The main tropical rainforests of the world are in tropical lowlands with a mean annual temperature generally more than 24°deg;C and mean annual rainfall of more than 2,000 mm [3]. By comparison, the tropical area of southern Yunnan is at a higher latitude (500-900 m asl.) with relatively lower annual mean temperature (c. 22°deg;C) and lower annual mean precipitation (1,500 mm). The tropical forests in southern Yunnan were first mentioned by Wang in 1939 [4]. Between 1955 and 1960, these forests were surveyed by Sino-Russian expeditions and Yunnan University. It was then suggested that tropical rainforests existed in southern Yunnan, but these were considered to be a type different from the ones in Indo-Malaya [5] because of the lack of representatives of Dipterocarpaceae, which dominates the rainforests of tropical Asia. However, a dipterocarp forest was found in southernmost Yunnan in the 1970s, which indicated that the Indo-Malayan tropical rainforest existed in the region. It was later confirmed by Whitmore [6, 7], after a short visit to southern Yunnan, that there are true evergreen rainforests present in the southern fringes of China. Further biogeographical and ecological studies on the vegetation and flora of southern Yunnan revealed that the tropical rainforest in southern Yunnan, with physiognomic and floristic similarities to the Indo-Malayan rainforests, is a type of tropical Asian rainforest at the climatic limit of the northern edge of the tropical zone. It is identified as "tropical seasonal rainforest" [8-16].

Physiognomy and species diversity of the tropical rain forest in southern Yunnan

The tropical seasonal rainforest in southern Yunnan, occurring on lower montane and valleys between 500-900 m asl., has a profile of three tree layers, of which the top layer is composed of emergent trees, and the second layer is the main canopy with the most density of individuals. This is the typical profile of equatorial lowland rainforests [17, 18]. In life forms, phanerophytes contribute 87.5-89.7% of the total species in the tropical seasonal rainforest. Of these, liana phanerophytes contribute 18.3-20.3%, megaphanerophytes 7.2-9.7%, mesophanerophytes 27-28%, microphanerophytes 12-15%, nanophanerophytes 8.3-9.7%, and herbaceous phanerophytes 4.2-4.6%. In leaf-scale spectra, mesophyllous leaves make up 71%, microphyllous leaves 20-23%, and macrophyllous leaves 5.5-7.5% of the total woody plants. In leaf types, compound leaves make up 21.4-24.5% of the total tree species [19].

In species diversity, 150-200 vascular plant species were recorded from a single sampling plot based on 10 sampling plots of 0.25 ha, of which 44-63 species were trees (if saplings and seedlings are included, it was 80-90 species), 30-40 species were lianas, 15-20 species were herbaceous plants, and 5-20 were epiphytes [20]. Shannon-Wiener's diversity indexes (base:2.718283) are 3.1594-3.599. A survey of 1 ha sampling plot yielded 150 tree species with DBH > 5 cm, and 119 species with DBH > 10 cm, respectively [15].

The long-tailed rank/abundance diagrams of the tropical seasonal rainforest indicate that the species with small population sizes make up an unusually large proportion of the total species composition [8, 16]. The frequency patterns also revealed that 40%-60% of tree species have only one individual, and 30%-40% of tree species two to five individuals. Fewer than 15% have 6-10 individuals and fewer than 10% have more than 10 individuals, from a 0.25 ha sampling plot [20].


Fig 2. The tropical seasonal rain forest in southern Yunnan, China

Floristic composition and geographical elements

The families with most species richness in the tropical seasonal rainforest were ranked as Rubiaceae, Lauraceae, Annonaceae, Moraceae, Orchidaceae, Meliaceae, Vitaceae, Apocynaceae, Urticaceae, Rutaceae, Fagaceae, Acanthaceae, and Papilionaceae. Some families have only a small number of species, but they are the dominant families in phytosociological importance (dominant in individuals), such as Sapindaceae, Anacardiaceae, Burseraceae, Ebenaceae, Combretaceae, Ulmaceae, and Myrtaceae. The families Dipterocarpaceae, Barringtoniaceae, Tetrameleaceae, Myristicaceae, Guttiferae, Icacinaceae, Ixonanthaceae, and Sapotaceae have even fewer species, but have high phytosociological importance.

At the generic level, Ficus has the highest species richness. Other genera with high species richness include Piper, Syzygium, Litsea, Lasianthus, Lithocarpus, Millettia, Pilea, Castanopsis, and Tetrastigma. Pometia, Terminalia, Antiaris, Girroniera, Pouteria, and Tetrameles have fewer species but high phytosociological importance in the dominant tree layer, as do Lasiococca, Garcinia, Mitrephora, Alphonsea, Cleidion, Sumbaviopsis, and Pittosporops is in the lower tree layer of the tropical seasonal rainforest.

Based on the study of the distribution patterns of Chinese genera [21] and the studies on species distribution of the flora in southern Yunnan [10], 12 distribution types at generic level and 8 distribution types at specific level were recognized in the flora of the tropical seasonal rainforest. The genera of tropical distribution contribute 94% of the total genera; of these, the genera of tropical Asian distribution have the highest percentage among all distribution types, contributing 33-42%, while the genera of pantropical distribution contribute 20-25% of the total genera. The species of strictly tropical distribution contribute 76-80% of the total flora, and of these the species of tropical Asian distribution also show the highest percentage among all distribution types of species. These data indicate that the tropical seasonal rainforest has strong tropical Asiatic affinity floristically and is a type of tropical Asian rainforest.

Comparison to tropical rain forests in equatorial Asia

The tropical seasonal rainforest in southern Yunnan, which is similar to equatorial Asian lowland rainforests in profile, life-form spectra and leaf-scale spectra, was classified as a type of lowland rainforest, although it occurs at mountain habitats with higher altitude [2]. It differs from the latter only in having some deciduous trees in the canopy layer, more abundant woody lianas, fewer megaphanerophytes, and a relatively higher percentage of microphylls. It is a type of semi-evergreen rainforest at altitudinal and latitudinal limits.

In species richness, the tropical seasonal rainforest of Yunnan has a relatively lower number of species per unit area than typical lowland rainforests in equatorial Asia. For example, in a 1 ha sampling area, 119 tree species with DBH > 10 cm were recorded from the tropical seasonal rainforest in southern Yunnan [15], while 214-223 tree species with DBH > 10 cm were recorded in Sarawak, Malaysia [22], 129-149 tree species in Kalimantan, Indonesia [23], and 145-184 tree species in Papua New Guinea [24].

In floristic composition, most of the dominant families from the tropical seasonal rainforest of southern Yunnan are dominant in the tropical rainforests in Malaysia. However, the tropical seasonal rainforest occurs on the margin of tropical Asia. Although tropical families and genera make up the majority of its total flora, the taxa of strictly tropical distribution are still under-represented in species richness compared to the Malaysian flora. For example, Dipterocarpaceae, Melastomaceae, Gutifferae, Myrtaceae, Myristicaceae, and Sapotaceae, which are dominant families in the tropical rainforests in Malaysia, have fewer species or less species richness in southern Yunnan.

Geological history and factors resulting in formation of southern Yunnan rain forest

During the Tertiary, southern Yunnan was covered by a subtropical evergreen broad-leaved forest characterized by Fagaceae species, and the climate was cooler and drier than the present day [25-27]. Current distribution patterns of the vegetation in southern Yunnan, shows deciduous forests dominated by tree species such as Anogeissus acuminata and Bombax ceiba on the banks and lower mountain slopes of the Mekong valley. The forest dominated by the palm species Livistona saribus, which usually occurs in drier habitats, is patchily distributed on lower mountains. The usual savanna species, such as Woodfordia fruticosa, Phyllanthus emblica, Cipadessa cinerascens, Lannea coromandelica, Bauhinia variegata, Grewia eriocarpa, Dalbergia obtusifolia, Helicteres angustifolia, Helicteris isora, Lagerstroemia tomentosa, Albizzia, Eriolaena, and Acacia, and the species that prefer dry habitats, such as Pistacia weinmanifolia, Cycas, and Dracaena, are frequently found in the tropical forests in southern Yunnan. These data indicate that the region did experience drier climate in the historical past [28].

The fundamental topography and climate of southern Yunnan have been strongly affected by the uplift of the Himalayas and the formation of the monsoon climate of East Asia [29]. It has been suggested that the moist tropical climate in southern Yunnan did not form until the Himalaya lifted to a certain elevation after the late Tertiary, allowing the development of the tropical rainforest in the region [2]. The Hengduan Mountains, which are situated north of southern Yunnan, form a barrier keeping out the cold air in winter, resulting, in southern Yunnan, in dense fog during the whole dry season to supplement the insufficient precipitation and in keeping the ground warm by reducing radiation cooling or long-wave effective radiation, conditions that seemed to have allowed for the presence of the tropical rain forest.

A direct land connection between mainland SE Asia and Western Malesia existed until the early Pliocene (5 million years ago) and there was no geographical barrier to natural distribution of plants between mainland Southeast Asia and Western Malesia during most of the Tertiary [30]. The geological history of Southeast Asia could explain the Malaysian floristic affinity of the tropical seasonal rainforest in southern Yunnan.


Fig 3. Left: people of the village of Yao. Right: Village and people of Dai. Southern Yunnan, China.

Discussion and implications for conservation

The tropical seasonal rainforest in southern Yunnan has almost the same forest profile and physiognomic characteristics as equatorial lowland rainforests. It is undoubtedly a type of truly tropical rainforest. As the tropical seasonal rainforest occurs at the northern edge of the tropical zone and at the extreme limit of rainfall and temperature usually required by tropical rainforest, it differs from lowland rainforests in equatorial areas in having deciduous trees in the canopy layer, fewer megaphanerophytes and epiphytes, but more abundant lianas as well as more plants with microphylls. Abundant lianas could be a characteristic of rainforest in a monsoon climate. Fewer megaphanerophytes and a relatively higher percentage of microphylls may be a result of the fact that this occurs at climatic limits at the northern edge of the tropical zone and is influenced by seasonal dryness and the relatively low temperature.

The flora of the tropical seasonal rainforest consists mainly of tropical floristic elements, which contribute more than 90 % at the generic level and more than 80% at the specific level to its total flora. The most dominant floristic elements at both the generic and specific levels are the ones of tropical Asian distribution. Most of the dominant families from the tropical seasonal rainforest are also dominant in the Indo-Malayan rain forests. This reveals that the flora of the rainforest of Yunnan is of tropical nature with a strong tropical Asian affinity.

The tropical seasonal rainforest of southern Yunnan, in terms of physiognomy, is similar to the evergreen seasonal forest of the tropical America of Beard [31], or the moist evergreen type of African tropical rainforest of Hall and Swaine [32], or the Mesophyll vine forest of the Australian rainforest of Webb [33], as well as the semi-evergreen rainforest of Walter [34]. However, it is most equivalent to Whitmore's [7] semi-evergreen rainforests of Southeast Asia. The tropical seasonal rainforest in southern Yunnan nonetheless belongs to the tropical rainforest formation of Southeast Asia and is a type of semi-evergreen rainforest.

Tropical rainforests occur at c. 27°31' N in northeastern India [35] and Burma [36]. The tropical rainforest in southern Yunnan, although it is not the northernmost type of tropical rainforest, occurs really at the climatic limits of tropical rainforest due to its high altitude. The occurrence of the tropical rainforest in southern Yunnan was more influenced by local habitats and microclimates than by regional climate.


Fig 4. Left: Village of Dai with rubber plantation behind.
Right: Rubber plantation. Southern Yunnan, China.

The tropical seasonal rainforest in southern Yunnan conspicuously decreased from a cover of 10.9% of the total area of the region in 1976 down to 3.6% in 2003, mainly due to rubber planting [37]. The high price of rubber has continued to promote the expansion of rubber plantations in the region (Fig. 3, 4). Rubber plantations, by replacing this unique type of tropical rainforest, are resulting in a loss of biodiversity. In the last 2,000 years, southern Yunnan reportedly has experienced six periods of climate change marked by alternating warm-wet and cool-dry conditions and 11 drought events and cold events, as well as 12 periods of fire damage [38]. Rubber is a strictly tropical species and the climatic conditions in southern Yunnan may not be suitable for its growth in the long-term, given the geological history of the area. Limiting further expansion of rubber plantations is the only way to conserve the tropical seasonal rainforest in southern Yunnan.

Acknowledgements

This project was funded by The National Natural Science Foundation of China (30570128, 30770158). I thank three anonymous reviewers very much for their important and constructive comments. I am very grateful to Tropical Conservation Science for assistance in improving the English and for other technical improvements in preparing this article.

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