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Different patterns of ecosystem carbon accumulation between a young and an old-growth subtropical forest in Southern China

机译:中国南方的幼龄和老生长的亚热带森林之间生态系统碳积累的不同模式

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摘要

Using long-term (22 years) measurements from a young and an old-growth subtropical forest in southern China, we found that both forests accumulated carbon from 1982 to 2004, with the mean carbon accumulation rate at 227 +/- 59 g C m(-2) year(-1) for young forest and 115 +/- 89 g C m(-2) year(-1) for the old-growth forest. Allocation of the accumulated carbon was quite different between these two forests: the young forest accumulated a significant amount of carbon in plant live biomass, whereas the old-growth forest accumulated a significant amount of carbon in the soil. From 1982 to 2004, net primary productivity (NPP) increased for the young forest, and did not change significantly for the old-growth forest. The increase in NPP of the young forest resulted from recruitment of some dominant tree species characteristic of the subtropical mature forest in the region and an increase in tree density; decline of NPP of the old-growth forest was caused by increased mortality of the dominant trees.
机译:通过对中国南部的一个年轻的和古老的亚热带森林进行的长期(22年)测量,我们发现这两个森林在1982年至2004年期间都积累了碳,平均碳积累速率为227 +/- 59 g C m (-2)年幼林(-1)和115 +/- 89 g C m(-2)年林(-1)年(-1)。这两种森林之间的累积碳分配有很大不同:年轻森林的植物活生物量中积累了大量碳,而老龄森林的土壤中积累了大量碳。从1982年到2004年,幼林的净初级生产力(NPP)有所增加,而老林则没有显着变化。幼林NPP的增加是由于该地区亚热带成熟林的一些优势树种的征募和树木密度的增加所致;老龄林NPP的下降是由优势树的死亡率增加引起的。

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