Department of Ecology, Key Laboratory for Earth Surface Processes of the Ministry of Education, Peking University, Beijing 100871, China.
Sci China Life Sci. 2010 Jul;53(7):851-7. doi: 10.1007/s11427-010-4027-z. Epub 2010 Aug 10.
Above- and belowground biomass allocation not only influences growth of individual plants, but also influences vegetation structures and functions, and consequently impacts soil carbon input as well as terrestrial ecosystem carbon cycling. However, due to sampling difficulties, a considerable amount of uncertainty remains about the root: shoot ratio (R/S), a key parameter for models of terrestrial ecosystem carbon cycling. We investigated biomass allocation patterns across a broad spatial scale. We collected data on individual plant biomass and systematically sampled along a transect across the temperate grasslands in Inner Mongolia as well as in the alpine grasslands on the Tibetan Plateau. Our results indicated that the median of R/S for herbaceous species was 0.78 in China's grasslands as a whole. R/S was significantly higher in temperate grasslands than in alpine grasslands (0.84 vs. 0.65). The slope of the allometric relationship between above- and belowground biomass was steeper for temperate grasslands than for alpine. Our results did not support the hypothesis that aboveground biomass scales isometrically with belowground biomass. The R/S in China's grasslands was not significantly correlated with mean annual temperature (MAT) or mean annual precipitation (MAP). Moreover, comparisons of our results with previous findings indicated a large difference between R/S data from individual plants and communities. This might be mainly caused by the underestimation of R/S at the individual level as a result of an inevitable loss of fine roots and the overestimation of R/S in community-level surveys due to grazing and difficulties in identifying dead roots. Our findings suggest that root biomass in grasslands tended to have been overestimated in previous reports of R/S.
地上和地下生物量分配不仅影响个体植物的生长,还影响植被结构和功能,从而影响土壤碳输入以及陆地生态系统碳循环。然而,由于采样困难,根冠比(R/S)仍然存在相当大的不确定性,R/S 是陆地生态系统碳循环模型的关键参数。我们在广泛的空间尺度上研究了生物量分配模式。我们收集了单个植物生物量的数据,并在内蒙古温带草原和青藏高原高寒草原的一条横截线上系统地进行了采样。我们的结果表明,中国草原草本植物的 R/S 中位数为 0.78。温带草原的 R/S 明显高于高寒草原(0.84 比 0.65)。地上和地下生物量之间的异速生长关系的斜率在温带草原比在高寒草原更陡峭。我们的结果不支持地上生物量与地下生物量等比例缩放的假设。中国草原的 R/S 与年平均温度(MAT)或年平均降水量(MAP)没有显著相关性。此外,我们的结果与先前的研究结果进行比较,表明个体植物和群落之间的 R/S 数据存在很大差异。这可能主要是由于在个体水平上不可避免地损失细根而低估了 R/S,以及在群落水平调查中由于放牧和难以识别死根而高估了 R/S。我们的研究结果表明,在以前关于 R/S 的报告中,草原根生物量可能被高估了。