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Effect of shrub coverage on grassland ecosystem carbon pool in southwestern China
XUE Jing-Yue, WANG Li-Hua, XIE Yu, GAO Jing, HE Jun-Dong, WU Yan
Chin J Plant Ecol    2019, 43 (4): 365-373.   DOI: 10.17521/cjpe.2017.0062
Abstract   (1245 HTML135 PDF(pc) (1105KB)(1179)  

AimsThe grassland in southwestern China is mainly warm and tropical grass and shrub grassland, accounting for approximately one-tenth of the national grassland area. Analysis of the relationship between shrub coverage and the grassland carbon pool and its composition is of great significance for accurately assessing carbon storage in the southwestern grassland, which grassland is still in the secondary succession stage.
MethodsIn a field investigation, 41 representative plots of different geomorphic types in southwestern China were divided into three types according to shrub coverage: no shrub grassland community (shrub coverage is 0), low shrub coverage grassland community (shrub coverage is 0-10%) and high shrub coverage grassland community (shrub coverage is 10%-30%). Carbon density was calculated by measuring the aboveground and underground biomass and litter biomass of grassland communities at different shrub coverage levels, as well as plant and soil carbon content.
Important findings The results showed that with increasing shrub coverage and species richness in grasslands, the ecosystem vegetation carbon density increased from 0.304 kg·m -2 to 1.574 kg·m -2, and the roots and litter carbon density also showed growth trends. The soil carbon density increased from 7.215 kg·m -2 to 9.735 kg·m -2, and the ecosystem carbon density increased from 7.519 kg·m -2 to 11.309 kg·m -2, with increasing shrub coverage. Regarding the composition of the grassland carbon pool, the soil carbon pool of the low shrub coverage grassland accounted for the smallest proportion of the ecosystem carbon pool. In summary, the increase in shrub coverage changes the composition of the grassland ecosystem carbon pool and leads to an increase in the amount of ecosystem carbon. Therefore, when estimating the grassland ecosystem carbon pool, it is necessary to overall plan for and take into account the changes in grassland shrub coverage in southern China.


Fig. 2 Soil carbon pool in grassland community with different shrub coverage in southwestern China. I, II, and III represent no shrub grassland, low shrub coverage grassland, and high shrub coverage grassland, respectively. The data are the means ± SE (I, II, n = 18; III, n = 5). Different uppercase letters indicate that the soil carbon pool at 0-100 cm was significantly different among different shrub coverage grassland communities (p < 0.05), and different lowercase letters indicate significant differences in the carbon pool at different soil layers (p < 0.05).
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从无灌木植物草地群落到高灌木植物盖度草地群落, 草地土壤碳库未呈现显著的变化趋势。就土壤碳库而言, 无灌木植物草地群落与低灌木植物盖度和高灌木植物盖度草地群落差异不显著(F = 1.610, p = 0.213)。这说明, 草地群落中灌木植物盖度的大小并没有对土壤碳库造成显著影响。在垂直剖面上, 高灌木植物盖度草地群落的土壤表层(0-10 cm)碳库显著大于低灌木植物盖度草地群落(F = 4.475, p = 0.018); 但在10-20 cm和30-50 cm土层, 不同灌木植物盖度草地群落土壤碳库无显著差异(F = 1.914, p = 0.161; F = 0.093, p = 0.912); 在20-30 cm土层无灌木植物草地群落碳库显著大于高灌木植物盖度草地群落(F = 4.777, p = 0.014), 低灌木植物盖度草地群落与二者差异均不显著; 在50-100 cm土层, 不同灌木植物盖度草地群落的土壤碳库差异显著(F = 4.149, p = 0.023), 从无灌木植物草地群落、低灌木植物盖度草地群落到高灌木植物盖度草地群落, 土壤碳库逐渐增加, 且高灌木植物盖度草地群落显著大于无灌木植物草地群落(图2)。总体来看, 一方面, 草地土壤碳库并没有因为灌木植物盖度增加发生显著变化; 另一方面, 不同灌木植物盖度草地群落土壤碳库的空间分层变化明显, 表层和底层灌木多的样地土壤碳相对较高, 而中间的过渡土层的土壤碳库则呈现多样性趋势。
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