Abstract
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.
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Acknowledgments
This study was funded by NSFC projects 30725006 and 40730102. We thank many researchers and supporting staff for their sustained contributions in data collections, and the funding support and supervision from the Chinese Ecosystem Research Network (CERN). The authors confirm that all the experiments and studies comply with the current Chinese laws.
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Tang, X., Wang, YP., Zhou, G. et al. Different patterns of ecosystem carbon accumulation between a young and an old-growth subtropical forest in Southern China. Plant Ecol 212, 1385–1395 (2011). https://doi.org/10.1007/s11258-011-9914-2
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DOI: https://doi.org/10.1007/s11258-011-9914-2