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 ecosys...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.展开更多
在沙地环境中,沙埋是影响植物幼苗存活的一个重要因素。中间锦鸡儿(C arag ana interm ed ia)是浑善达克沙地和毛乌素沙地固定和半固定沙丘上常见的一种沙生灌木。为了研究沙埋对其幼苗存活以及生长的影响,对出土后生长了1个月的中间锦...在沙地环境中,沙埋是影响植物幼苗存活的一个重要因素。中间锦鸡儿(C arag ana interm ed ia)是浑善达克沙地和毛乌素沙地固定和半固定沙丘上常见的一种沙生灌木。为了研究沙埋对其幼苗存活以及生长的影响,对出土后生长了1个月的中间锦鸡儿实生苗进行沙埋实验,实验处理:TC为对照,T1为沙埋幼苗地上部的1/3,T2为沙埋幼苗地上部的1/2,T3为沙埋到幼苗的近顶端。实验持续4周,每周收获1次。结果表明:TC、T1和T2没有幼苗死亡,T3有20%的幼苗死亡;沙埋对中间锦鸡儿幼苗的生物量、根冠比、根生物量比和茎生物量比有显著影响,叶片生物量比各处理没有显著差异,沙埋对幼苗的叶面积没有显著影响,在第1周T2和T3的小叶片面积显著大于TC,在其余3周,TC与T1、T2的小叶片面积没有显著差异,与全埋则有显著差异;沙埋对幼苗的相对生长速率(RGR)和净同化速率(N AR)产生显著影响,实验结束时,T3处理幼苗的RGR和N AR显著地小于其它3个处理。上述结果表明,部分沙埋(T1、T2)对沙生灌木中间锦鸡儿幼苗的生长发育没有显著的影响,而全部沙埋(T3)对其幼苗的生长发育产生显著的抑制,中间锦鸡儿是一个比较耐沙埋的物种。展开更多
Quantifying forest carbon(C) storage and distribution is important for forest C cycling studies and terrestrial ecosystem modeling.Forest inventory and allometric approaches were used to measure C density and allocati...Quantifying forest carbon(C) storage and distribution is important for forest C cycling studies and terrestrial ecosystem modeling.Forest inventory and allometric approaches were used to measure C density and allocation in six representative temperate forests of similar stand age(42-59 years old) and growing under the same climate in northeastern China.The forests were an aspen-birch forest,a hardwood forest,a Korean pine plantation,a Dahurian larch plantation,a mixed deciduous forest,and a Mongolian oak forest.There were no significant differences in the C densities of ecosystem components(except for detritus) although the six forests had varying vegetation compositions and site conditions.However,the differences were significant when the C pools were normalized against stand basal area.The total ecosystem C density varied from 186.9 tC hm-2 to 349.2 tC hm-2 across the forests.The C densities of vegetation,detritus,and soil ranged from 86.3-122.7 tC hm-2,6.5-10.5 tC hm-2,and 93.7-220.1 tC hm-2,respectively,which accounted for 39.7% ± 7.1%(mean ± SD),3.3% ± 1.1%,and 57.0% ± 7.9% of the total C densities,respectively.The overstory C pool accounted for 】 99% of the total vegetation C pool.The foliage biomass,small root(diameter 【 5mm) biomass,root-shoot ratio,and small root to foliage biomass ratio varied from 2.08-4.72 tC hm-2,0.95-3.24 tC hm-2,22.0%-28.3%,and 34.5%-122.2%,respectively.The Korean pine plantation had the lowest foliage production efficiency(total biomass/foliage biomass:22.6 g g-1) among the six forests,while the Dahurian larch plantation had the highest small root production efficiency(total biomass/small root biomass:124.7 g g-1).The small root C density decreased with soil depth for all forests except for the Mongolian oak forest,in which the small roots tended to be vertically distributed downwards.The C density of coarse woody debris was significantly less in the two plantations than in the four naturally regenerated forests.The variability of C allocation patterns in a specific fore展开更多
基金supported by the National Natural Science Foundation of China (Grant No. 30870381)the Key Project of Scientific and Technical Supporting Programs Funded by the Ministry of Science & Technology of China (Grant No. 2007BAC06B01)
文摘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.
文摘在沙地环境中,沙埋是影响植物幼苗存活的一个重要因素。中间锦鸡儿(C arag ana interm ed ia)是浑善达克沙地和毛乌素沙地固定和半固定沙丘上常见的一种沙生灌木。为了研究沙埋对其幼苗存活以及生长的影响,对出土后生长了1个月的中间锦鸡儿实生苗进行沙埋实验,实验处理:TC为对照,T1为沙埋幼苗地上部的1/3,T2为沙埋幼苗地上部的1/2,T3为沙埋到幼苗的近顶端。实验持续4周,每周收获1次。结果表明:TC、T1和T2没有幼苗死亡,T3有20%的幼苗死亡;沙埋对中间锦鸡儿幼苗的生物量、根冠比、根生物量比和茎生物量比有显著影响,叶片生物量比各处理没有显著差异,沙埋对幼苗的叶面积没有显著影响,在第1周T2和T3的小叶片面积显著大于TC,在其余3周,TC与T1、T2的小叶片面积没有显著差异,与全埋则有显著差异;沙埋对幼苗的相对生长速率(RGR)和净同化速率(N AR)产生显著影响,实验结束时,T3处理幼苗的RGR和N AR显著地小于其它3个处理。上述结果表明,部分沙埋(T1、T2)对沙生灌木中间锦鸡儿幼苗的生长发育没有显著的影响,而全部沙埋(T3)对其幼苗的生长发育产生显著的抑制,中间锦鸡儿是一个比较耐沙埋的物种。
基金supported by the grants from the National Natural Science Foundation of China (Grant No.30625010)the Special Research Program for Public-welfare Forestry (Grant No.200804001)the Ministry of Science and Technology of China (Grant No.2006BAD03A0703)
文摘Quantifying forest carbon(C) storage and distribution is important for forest C cycling studies and terrestrial ecosystem modeling.Forest inventory and allometric approaches were used to measure C density and allocation in six representative temperate forests of similar stand age(42-59 years old) and growing under the same climate in northeastern China.The forests were an aspen-birch forest,a hardwood forest,a Korean pine plantation,a Dahurian larch plantation,a mixed deciduous forest,and a Mongolian oak forest.There were no significant differences in the C densities of ecosystem components(except for detritus) although the six forests had varying vegetation compositions and site conditions.However,the differences were significant when the C pools were normalized against stand basal area.The total ecosystem C density varied from 186.9 tC hm-2 to 349.2 tC hm-2 across the forests.The C densities of vegetation,detritus,and soil ranged from 86.3-122.7 tC hm-2,6.5-10.5 tC hm-2,and 93.7-220.1 tC hm-2,respectively,which accounted for 39.7% ± 7.1%(mean ± SD),3.3% ± 1.1%,and 57.0% ± 7.9% of the total C densities,respectively.The overstory C pool accounted for 】 99% of the total vegetation C pool.The foliage biomass,small root(diameter 【 5mm) biomass,root-shoot ratio,and small root to foliage biomass ratio varied from 2.08-4.72 tC hm-2,0.95-3.24 tC hm-2,22.0%-28.3%,and 34.5%-122.2%,respectively.The Korean pine plantation had the lowest foliage production efficiency(total biomass/foliage biomass:22.6 g g-1) among the six forests,while the Dahurian larch plantation had the highest small root production efficiency(total biomass/small root biomass:124.7 g g-1).The small root C density decreased with soil depth for all forests except for the Mongolian oak forest,in which the small roots tended to be vertically distributed downwards.The C density of coarse woody debris was significantly less in the two plantations than in the four naturally regenerated forests.The variability of C allocation patterns in a specific fore
