Zhu Hua, Ashton Peter, Gu Bojian, Zhou Shisun, Tan Yunhong
Center for Integrative Conservation, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, Yunnan 666303, PR China.
Arnold Arboretum, Harvard University and Royal Botanic Gardens, Kew, UK.
Plant Divers. 2021 Jan 16;43(6):444-451. doi: 10.1016/j.pld.2021.01.001. eCollection 2021 Dec.
In the southern mountain ranges of Yunnan province, China, deep valleys of several large rivers create rain shadows with hot dry summers, and are locally designated tropical; towards the north, notably in the Lancang (Upper Mekong) valley, these regions may experience frost during winter. The woody forest canopy of these valleys is predominantly deciduous, with evergreen elements in the north, where the canopy is open and the forest savanna-like. However, we here present tall forest with a closed deciduous canopy and semi-evergreen subcanopy observed in hot dry valleys of these rivers and their tributaries in the tropical south. The structure and physiognomy of these forests resemble the tall (moist) deciduous forest formation widespread in South Asia and Indo-Burma. Furthermore, these forests are largely composed of tropical elements at both the generic (80%) and the species level (>70%), indicating that these forests are indeed tropical. We originally hypothesized that these isolated forests represent refugia of a pre-Holocene extension of tall (moist) deciduous forest formation of South Asia and Indo-Burma. The sample plot we established to test this hypothesis confirmed that these forests share the structure and physiognomy of the tall (moist) deciduous forest formation; however, the plots also showed that these forests lack the characteristic and dominant species of the formation's Indo-Burmese range. The tree flora, in particular, indicates that both deciduous and evergreen elements are instead mostly derived from the adjacent tropical semi-evergreen forests of tropical southern China; yet they also include an important endemic element, which implies that these forests have survived as refuges possibly since the Pliocene. The exceptional representation of evergreen elements in these forests indicates that they have rarely been subject to hot fires or domestic cattle browsing, adding to the unique nature of the forests and further justifying their strict conservation.
在中国云南省南部山区,几条大河的深切河谷形成了雨影区,夏季炎热干燥,当地被划定为热带地区;向北,尤其是在澜沧江(湄公河上游)流域,这些地区冬季可能会出现霜冻。这些河谷的木本森林冠层主要为落叶林,北部有常绿成分,冠层开阔,类似森林稀树草原。然而,我们在此展示的是在这些河流及其支流位于热带南部的炎热干燥河谷中观察到的具有封闭落叶冠层和半常绿亚冠层的高大森林。这些森林的结构和外貌类似于在南亚和印度 - 缅甸广泛分布的高大(湿润)落叶林。此外,这些森林在属级(80%)和种级(>70%)层面上大多由热带成分组成,表明这些森林确实是热带森林。我们最初假设这些孤立的森林是南亚和印度 - 缅甸高大(湿润)落叶林形成的全新世前延伸的避难所。我们为验证这一假设而设立的样地证实,这些森林具有高大(湿润)落叶林的结构和外貌;然而,样地也显示这些森林缺乏该林型在印度 - 缅甸分布范围内的特征性和优势物种。特别是树木植物区系表明,落叶和常绿成分大多反而源自中国热带南部相邻的热带半常绿森林;但它们也包含一个重要的特有成分,这意味着这些森林可能自上新世以来就作为避难所幸存下来。这些森林中常绿成分的特殊表现表明它们很少遭受热火灾或家畜啃食,这增加了森林的独特性,并进一步证明了对其进行严格保护的合理性。