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BIODIVERSITY OF TROPICAL PEATLAND IN SOUTHEAST ASIA

机译:东南亚热带泥炭地的生物多样性

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Natural lowland peat swamps of Southeast Asia support forest vegetation forming a catena of types from their perimeter to centre, a change that is reflected in variations in canopy height, peat thickness, waterlogging and nutrient availability. Recognition of the biological, environmental and economic importance of tropical peatlands has been a slow process. The earliest interest in the peat swamp forests of Southeast Asia was in the 1930s by British foresters working in the former British Protectorates of Malaya, Sarawak and Brunei and Dutch scientists in Kalimantan and Sumatra. The ecological and taxonomic studies of peat swamp forests of northern Borneo by J.A.R. Anderson became a benchmark for all subsequent research on tropical peatland. Many plant species are restricted to this stressful habitat and some are endemic to it. Several historical accounts of the fauna of tropical peat swamp forests suggested that animal diversity was low but more recent ones, for example in the upper Sg. Sabangau catchment of Central Kalimantan, show the opposite that they are vital habitats for many rare and endangered species of animals and plants including orang utan (Pongo pygmaeus). By the end of the 1980s, extensive areas of peatland in Indonesia, Malaysia and Thailand had been drained and converted to agriculture for a large range of crops including rice and vegetables and plantations of oil palm and paper pulp trees. Associated problems of peat shrinkage, subsidence, nutrient deficiency, toxicity and low plant productivity are also documented. Deforestation, drainage and conversion of tropical peatland to other land uses has continued apace since then over increasingly larger areas with consequent problems of fire, flooding, greenhouse gas emissions and poverty all of which have had negative impacts on biodiversity. These are now regional and global problems some of which will be the subject of other presentations at this congress.
机译:东南亚的天然低地泥炭沼泽支持森林植被从他们的周边到中心形成一个类型的类型,改变,反映在树冠高度,泥炭厚度,涝和养分的变化中。识别热带泥炭地的生物,环境和经济重要性一直是缓慢的过程。在东南亚泥炭沼泽森林中最早的兴趣在20世纪30年代,由英国森林在马来亚,沙捞越和文莱和荷兰科学家在卡利马坦和苏门答腊省的前英国保护区工作。 J.A.R.北北部泥炭沼泽林的生态和分类研究安德森成为对热带泥炭地所有后续研究的基准。许多植物物种都仅限于这种紧张的栖息地,有些人是流行的。热带泥炭沼泽森林的动物群的几个历史账户表明,动物多样性低,但最近的近似值低,例如在上部SG中。卡马曼坦中部的Sabangau集水区表明,对于许多罕见和濒危动物和植物,包括猩猩Utan(Pongo Pygmaeus),它们是重要的栖息地。到20世纪80年代末,印度尼西亚和泰国的广泛的泥炭地区已经排出并转变为农业,为大量作物,包括水稻和棕榈和纸浆树的蔬菜和种植园。还记录了泥炭收缩,沉降,营养缺乏,毒性和低植物生产率的相关问题。热带泥土到其他土地用途的森林砍伐,排水和转化率仍在继续,从那时起,随着越来越大的区域,随后的火灾,洪水,温室气体排放和贫困问题,所有这些都对生物多样性产生了负面影响。这些现在是区域和全球问题,其中一些将成为本国会其他介绍的主题。

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