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Forest structure and carbon dynamics in Amazonian tropical rain forests

机译:亚马孙热带雨林的森林结构和碳动态

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摘要

Living trees constitute one of the major stocks of carbon in tropical forests. A better understanding of variations in the dynamics and structure of tropical forests is necessary for predicting the potential for these ecosystems to lose or store carbon, and for understanding how they recover from disturbance. Amazonian tropical forests occur over a vast area that encompasses differences in topography, climate, and geologic substrate. We observed large differences in forest structure, biomass, and tree growth rates in permanent plots situated in the eastern (near Santarém, Pará), central (near Manaus, Amazonas) and southwestern (near Rio Branco, Acre) Amazon, which differed in dry season length, as well as other factors. Forests at the two sites experiencing longer dry seasons, near Rio Branco and Santarém, had lower stem frequencies (460 and 466 ha−1 respectively), less biodiversity (Shannon–Wiener diversity index), and smaller aboveground C stocks (140.6 and 122.1 Mg C ha−1) than the Manaus site (626 trees ha−1, 180.1 Mg C ha−1), which had less seasonal variation in rainfall. The forests experiencing longer dry seasons also stored a greater proportion of the total biomass in trees with >50 cm diameter (41–45 vs 30% in Manaus). Rates of annual addition of C to living trees calculated from monthly dendrometer band measurements were 1.9 (Manaus), 2.8 (Santarém), and 2.6 (Rio Branco) Mg C ha−1 year−1. At all sites, trees in the 10–30 cm diameter class accounted for the highest proportion of annual growth (38, 55 and 56% in Manaus, Rio Branco and Santarém, respectively). Growth showed marked seasonality, with largest stem diameter increment in the wet season and smallest in the dry season, though this may be confounded by seasonal variation in wood water content. Year-to-year variations in C allocated to stem growth ranged from nearly zero in Rio Branco, to 0.8 Mg C ha−1 year−1 in Manaus (40% of annual mean) and 0.9 Mg C ha−1 year−1 (33% of annual mean) in Santarém, though this variability showed no significant relation with precipitation among years. Initial estimates of the C balance of live wood including recruitment and mortality as well as growth suggests that live wood biomass is at near steady-state in Manaus, but accumulating at about 1.5 Mg C ha−1 at the other two sites. The causes of C imbalance in living wood pools in Santarém and Rio Branco sites are unknown, but may be related to previous disturbance at these sites. Based on size distribution and growth rate differences in the three sites, we predict that trees in the Manaus forest have greater mean age (~240 years) than those of the other two forests (~140 years).
机译:活树是热带森林中主要的碳储量之一。必须更好地了解热带森林的动态和结构变化,才能预测这些生态系统丧失或储存碳的潜力,并了解它们如何从干扰中恢复。亚马孙热带森林遍布广阔的地区,涵盖了地形,气候和地质基质的差异。我们观察到位于亚马逊东部(圣帕伦附近,帕拉附近),中部(马瑙斯附近,亚马逊河)和西南地区(里约布兰科,英亩附近)的永久性地块的森林结构,生物量和树木生长率存在很大差异,而干旱地区则有所不同季节长度以及其他因素。里约布兰科和圣塔伦附近的两个干旱季节较长的森林的茎干频率较低(分别为460和466 ha-1 ),生物多样性较低(香农-维纳多样性指数),地上碳储量较小(比Manaus站点(626棵树ha-1 ,180.1 Mg C ha-1 )高140.6和122.1 Mg C ha-1 ),降雨的季节变化较小。干旱季节较长的森林在直径大于50厘米的树木中也存储了更大比例的总生物量(41–45,而马瑙斯为30%)。根据月度树突仪带测量得出的每年向活树中添加C的速率分别为1.9(Manaus),2.8(Santarém)和2.6(Rio Branco)Mg C ha-1 year-1 。在所有地点,直径在10至30厘米的树种在年增长率中所占比例最高(玛瑙斯,里约布兰科和圣塔伦分别为38%,55%和56%)。生长表现出明显的季节性,在潮湿季节茎干直径增加最大,而在干燥季节最小,尽管这可能与木材含水量的季节性变化混淆。分配给茎生长的碳的年变化范围从里约布兰科的几乎为零,到马瑙斯的C ha-1 年-1 (年均值的40%)和0.9 Mg圣塔伦的C ha-1 year-1 (年平均数的33%),尽管这种变化与年份之间的降水没有显着关系。对活木碳平衡的初步估计(包括募集和死亡率以及生长)表明,玛瑙斯的活木生物量处于稳定状态,但在其他两个地点积累了约1.5 Mg C ha-1 。在圣塔伦和里奥布兰科站点的活木池中碳平衡失调的原因尚不清楚,但可能与这些站点先前的干扰有关。根据这三个地点的大小分布和生长率差异,我们预测马瑙斯森林中的树木平均年龄(〜240岁)比其他两个森林中的树木(〜140岁)长。

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