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Vertical variation in mass and CO2 efflux of litter from the ground to the 40m high canopy in a Bornean tropical rainforest
Agricultural and Forest Meteorology ( IF 5.6 ) Pub Date : 2021-10-06 , DOI: 10.1016/j.agrformet.2021.108659
Ayumi Katayama 1 , Izuki Endo 2, 3 , Naoki Makita 4 , Kazuho Matsumoto 5 , Tomonori Kume 1 , Mizue Ohashi 2
Affiliation  

Litter usually drops to the ground, but some is retained within the canopy. Mass and CO2 efflux from retained litter may play a significant role in carbon cycling in tropical rainforests where emergent trees with complicated canopy structures are observed. This study aimed to show vertical variation in the mass and CO2 efflux (Rlitter) of the retained litter and examined its contribution to carbon cycling in a Bornean tropical rainforest. The retained litter was collected from six 40 m tall columns with a radius of 1.6 m using an 85 m tall crane at six subplots. Dry mass and Rlitter were measured in the laboratory. The mass of the retained litter from the sampling points ranged from 0.35 g to 187.0 g, and Rlitter of the retained litter (42.4 ± 43.4 mg CO2 kg−1 h1) was significantly lower than that of the soil surface litter (85.9 ± 39.2 mg CO2 kg−1 h1) because of the lower water content in the retained litter. The mean mass of the retained litter measured from the ground to the canopy was 40.6 ± 22.2 g m2. The greatest mass was observed at a height of 0–2 m. The ratio of the retained litter mass to the soil surface litter mass ranged from 1.0% to 11.5% with a mean of 5.2%, suggesting that litter retained within the canopy can contribute to carbon storage in this forest. On the other hand, Rlitter did not differ with height, and the ratio of Rlitter to aboveground autotrophic respiration was less than 1%. This study is the first to show that the litter retained within the canopy can sporadically be a moderate hot spot for C storage, but it is not a significant source of released CO2.



中文翻译:

婆罗洲热带雨林中从地面到 40m 高树冠的凋落物质量和 CO2 流出量的垂直变化

垫料通常会掉到地上,但有些会保留在树冠内。来自保留凋落物的质量和 CO 2流出可能在热带雨林中的碳循环中发挥重要作用,在热带雨林中观察到具有复杂冠层结构的挺水树木。本研究旨在显示保留凋落物的质量和 CO 2流出(R凋落物)的垂直变化,并检查其对婆罗洲热带雨林中碳循环的贡献。使用 85 m 高的起重机在六个子地块从半径为 1.6 m 的六个 40 m 高的柱子上收集保留的垃圾。干质量和R凋落物在实验室中测量。采样点残留垃圾的质量范围为 0.35  g至 187.0 g,滞留凋落R凋落物(42.4 ± 43.4 mg CO 2 kg -1 h - 1)显着低于土壤表层凋落物(85.9 ± 39.2 mg CO 2 kg -1 h - 1),因为保留的垫料中较低的水含量。从地面到树冠测量的保留凋落物的平均质量为 40.6 ± 22.2 g m - 2。在 0-2 m 的高度处观察到最大质量。保留的凋落物质量与土壤表面凋落物质量的比率范围为 1.0 %到 11.5%,平均值为 5.2%,这表明保留在树冠内的枯枝落叶有助于该森林的碳储存。另一方面,R凋落物不随高度变化,R凋落物与地上自养呼吸的比值小于 1%。这项研究首次表明,保留在树冠内的凋落物偶尔会成为 C 储存的中等热点,但它不是释放 CO 2的重要来源。

更新日期:2021-10-06
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