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泥炭沼泽森林

2002年8月19日婆罗洲的卫星图像,示其燃烧中的泥炭沼泽森林

泥炭沼泽森林Peat swamp forests)为热带潮湿森林,土壤长期浸水,枯叶和木头无法完全分解,逐渐形成厚厚的酸性泥炭层。泥炭沼泽森林大多存在于高海拔地区。

泥炭沼泽森林通常被土壤排水良好的低地雨林,或沿海的半海水或海水红树林包围。

印度尼西亚政府已将婆罗洲大量的泥炭沼泽森林砍伐掉,转变为农业用地。1997年8月和2002年3月旱季的大型山火摧毁了大量泥炭沼泽森林。欧洲航天局研究发现,泥炭沼泽森林是地球重要的碳汇,1997年8月的山火向大气中排放了25亿吨碳,2002年3月的山火则向大气中排放了2亿至10亿吨碳。印度尼西亚拥有世界上50%的热带泥炭沼泽。[1]

泥炭沼泽森林区

参见

参考文献

  1. ^ 存档副本. [2011-06-17]. (原始内容存档于2015-09-23). 

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泥炭沼泽森林
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