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Leaf litter decomposition in a tropical peat swamp forest in Peninsular Malaysia

机译:马来西亚半岛热带泥炭沼泽森林中的凋落物分解

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It has long been assumed that the peat underlying tropical peat swamp forests accumulates because the extreme conditions (water logged, nutrient poor, anaerobic and acidic—pH 2.9–3.5) impede microbial activity. Litterbag studies in a tropical Malaysian peat swamp (North Selangor peat swamp forest) showed that although the sclerophyllous, toxic leaves of endemic peat forest plants (Macaranga pruinosa, Campnosperma coriaceum, Pandanus atrocarpus, Stenochlaena palustris) were barely decomposed by bacteria and fungi (decay rates of only 0.0006–0.0016 k day−1), leaves of M. tanarius, a secondary forest species were almost completely decomposed (decay rates of 0.0047–0.005 k day−1) after 1 year. Thus it is intrinsic properties of the leaves (that are adaptations to deter herbivory in the nutrient poor environment) that impede microbial breakdown. The water of the peat swamp was very high in dissolved organic carbon (70–84 mg l−1 DOC). Laboratory studies revealed initial rapid leaching of DOC from leaves (up to 1,720 mg l−1 from 4 g of leaves in 7 days), but the DOC levels then fell rapidly. The leaching of DOC resulted in weight loss but the physical structure of the leaves remained intact. It is suggested that the DOC is used as a substrate for microbial growth hence lowering the concentration of DOC in the water and transferring energy from the leaves to other trophic levels. This would explain how nutrient poor tropical peatswamps support diverse, abundant flora and fauna despite low nutrient levels and lack of rapid litter cycling such as occurs in other types of tropical rainforests.
机译:长期以来,人们一直认为热带泥炭沼泽森林下面的泥炭会积累,因为极端条件(水淹,营养缺乏,厌氧和酸性,pH值为2.9-3.5)会阻碍微生物的活动。在热带马来西亚泥炭沼泽(北雪兰莪泥炭沼泽森林)进行的垃圾袋研究表明,尽管地方性泥炭森林植物(Macaranga pruinosa,Campnosperma coriaceum,Pandanus atrocarpus,Stenochlaena palustris)的硬毛病,有毒叶子几乎没有被细菌和真菌分解(仅次生林种的塔纳罗非鱼(M. tanarius)的叶片几乎被完全分解(衰减率为0.0047–0.0016 k day -1 ),仅0.0006–0.0016 k day -1 ) >)1年后。因此,阻碍微生物分解的是叶片的固有特性(适应于在营养不良的环境中抑制食草动物)。泥炭沼泽中的水溶解有机碳含量很高(70-84 mg l -1 DOC)。实验室研究表明,最初的DOC从叶片中快速浸出(7天之内从4 g的叶片中提取出1,720 mg l -1 ),但是DOC的含量随后迅速下降。 DOC的浸出导致重量减轻,但是叶片的物理结构保持完整。建议将DOC用作微生物生长的基质,从而降低水中的DOC浓度并将能量从叶片转移到其他营养级。这可以解释营养不足的热带泥炭沼泽如何尽管营养水平低和缺乏像其他类型的热带雨林那样快速的凋落物循环,却支持多样化,丰富的动植物。

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