高寒草甸放牧扰动与两种植物的反应研究

对不同放牧强度下矮嵩草草甸植物垂穗披碱草和鹅绒委陵菜的生长和繁殖特性进行了5年研究。结果表明,垂穗披碱草株高、分蘖数、地上物量、地下生物量、有性繁殖效力在不放牧或轻度放牧下最大,营养生长效力在重度放牧中最大,而贮藏效力在重度放牧中最小。鹅绒委陵菜叶数、匍匐茎长度、地上生物量、匍匐茎生物量、开花数、生殖生物量、有性繁殖效力及营养繁殖效力在放牧区显著高于不放牧的对照区。说明适当的放牧干扰有利于垂穗披碱草营养生长,但放牧过重会抑制其有性繁殖;由于放牧采食减少了种间竞争影响,从而提高了鹅绒委陵菜营养,生长效力和有性繁殖效力。两物种地下贮藏物的比例随着放牧强度增加显著减少。放牧强度对高寒草甸的群落演替方向有显著影响。     

紫茎泽兰和飞机草的形态、生物量分配和光合特性对氮营养的响应

比较研究了紫茎泽兰(Ageratina adenophora)和飞机草(Chromolaena odorata)的形态、生物量分配、生长和光合特性对氮营养的可塑性反应,探讨其与入侵性的关系。结果表明:1) 两种入侵植物对氮营养变化表现出很高的可塑性。随供氮量的增加,两种植物的根冠比、根生物量比降低,叶生物量比(LMR)、叶面积比和叶根比升高。低氮时,增加吸收器官的生物量分配,有利于养分吸收;高氮时,更多的生物量投入同化器官,有利于碳积累。相比之下紫茎泽兰对氮素的适应性更强。2) 两种入侵植物偏好较高的氮营养环境,土壤氮含量升高利于紫茎泽兰和飞机草的入侵。在较大的氮范围内,其相对生长速率(RGR)、总生物量、株高、分枝数、叶面积指数、最大净光合速率和光合色素含量都随供氮量的增加而显著增加,过量氮素对上述参数的抑制不显著。在本地种基本停止生长的干季,紫茎泽兰和飞机草仍维持较高的RGR,这与它们的入侵性密切相关。3) 在决定RGR对氮营养的响应过程中,平均叶面积比和净同化速率同等重要。LMR对两种植物的RGR有重要的影响,是决定处理间和种间RGR差异的重要因素。随氮素的增加,紫茎泽兰的比叶面积(SLA)降低,飞机草的SLA升高,但在所有氮水平下,前者的SLA都高于后者,紫茎泽兰SLA的变化规律更利于植物适应氮环境。     

祁连山冷龙岭南坡移地植物叶片的碳氮特征

在祁连山冷龙岭南麓坡地进行不同海拔高度土壤(0～40(30)cm土层)和植被的整体双向移地实验,以探讨气候变化对主要物种和群落碳、氮特征的影响。结果表明,3 200 m的麻花艽移地至高海拔时,叶片碳、氮含量分别呈现出先增加后减少和一直增加的趋势,而碳/氮值下降明显。3 400 m的兰石草、珠芽蓼、垂穗披碱草、金露梅和鹅绒委陵菜5种植物大部分叶片碳、氮素含量及碳/氮呈现出随海拔增高而下降的趋势。3 600 m的矮嵩草、雪白委陵菜和重齿风毛菊3种植物叶片碳、氮含量及碳/氮在各海拔之间变化不明显。3 800 m的矮嵩草和矮火绒草的叶片碳、氮含量随海拔高度增加而增加,碳/氮下降。整个群落来讲碳含量随海拔升高而降低,氮含量和碳/氮比变化较小。研究发现,各群落和物种对移地的响应方式因物种组成、原生状态不同而存在差异;温度条件(以海拔升降模拟温度降升)对植被群落及主要植物叶片碳、氮含量和碳/氮比有一定影响,尤其是当高海拔稀疏植被移地到低海拔时,其叶片碳、氮和碳氮比与原生状况的植被群落及主要植物种相对变化较大。     

增温对窄叶鲜卑花高寒灌丛生物量碳和氮分配的影响

文章以青藏高原东部窄叶鲜卑花灌丛为研究对象,采用开顶式生长室(OTCs)模拟增温实验(+1.2℃),分析增温对灌木层和草本层各器官碳、氮分配的影响及其影响因素,以揭示青藏高原东部高寒灌丛灌木层和草本层碳、氮分配对增温的响应策略。结果显示:(1)增温使窄叶鲜卑花灌木层叶、粗根、细根碳库显著增加18.8%、7.7%和139.4%,使灌木层细根氮库显著增加153.9%;增温使草本层地上和地下部分碳库显著增加60.4%和130.5%,使草本层地上和地下部分氮库显著增加46.1%和124.0%。(2)增温使灌木层茎和粗根碳分配比例显著降低18.9%和16.2%,使灌木层叶、茎和粗根氮分配比例显著降低25.2%、23.3%和14.4%,使灌木层细根碳、氮分配比例显著增加86.5%和96.2%;增温使草本层地上部分碳、氮分配比例显著降低19.5%和18.9%,使草本层地下部分碳、氮分配比例显著增加15.6%和24.8%。(3)Pearson相关分析和多元线性回归分析结果表明,空气温度和土壤微生物生物量是影响灌木层地上碳、氮分配的主要因子,能解释其变异的72.0%以上;土壤温度、土壤有机碳含量和土壤脲酶活性是影响灌木层地下碳、氮分配的主要因子,能解释其变异的92.0%以上;土壤有机碳含量、土壤转化酶和脲酶活性是影响草本层地上和地下碳、氮分配的主要因子,能解释其变异的92.8%以上。(4)土壤氮素有效性对灌木层和草本层生物量碳、氮分配的影响不显著。研究表明,气候变暖情景下,青藏高原东部窄叶鲜卑花高寒灌丛的灌木层和草本层植物通过提高地下部分碳、氮分配,进而更好地适应外界环境温度的提高。     

围封对天山高寒草原4种植物叶片和土壤化学计量学特征的影响

以中国科学院巴音布鲁克草原生态系统研究站长期围栏内外的羊茅(Festuca ovina)、天山赖草(Leymus tiansecalinus)、二裂委陵菜(Potentilla bifurca)和鹅绒委陵菜(Potentilla anserine)4种植物叶片和土壤为研究对象,分析了放牧与围封对植物叶片和土壤C、N、P的化学计量特征的影响。结果表明,围封样地土壤养分浓度整体高于放牧样地(P0.05),全氮(TN)浓度除外。围封显著增加羊茅叶片C、N浓度(P0.05),对P浓度影响不显著;围封显著增加鹅绒委陵菜叶片的C浓度,但是显著降低叶片的N和P浓度(P0.05),围封对天山赖草和二裂委陵菜养分含量影响不显著。围封显著增加鹅绒委陵菜C∶N和C∶P(P0.05);围封显著降低羊茅C∶N、C∶P和增加N∶P(P0.05);围封显著降低二裂委陵菜C∶N(P0.05),对天山赖草的化学计量特征影响不显著。不同植物对围封的响应不同,意味着长期围封可能会改变天山高寒草原生态系统的结构。围封降低优势种(羊茅)的固碳能力,增加退化期出现的代表性植物(鹅绒委陵菜)的固碳能力,表明在长期围封下植物凋落物中的杂类草(鹅绒委陵菜)可能更多的为土壤提供碳来源,也能促进优势禾本科物种的氮含量和碳含量的增加。     

间伐对川西亚高山粗枝云杉人工林细根生物量及碳储量的影响

以川西亚高山50年生粗枝云杉(Picea asperata)人工林为研究对象, 探讨了间伐对粗枝云杉人工林1-5级细根生物量及碳储量的影响。结果表明: 粗枝云杉人工林细根生物量和碳储量随根序等级的增加而显著增加(p < 0.05), 5级根序中1级根生物量及碳储量最小, 5级根生物量及碳储量最大。与对照(间伐0%)相比, 间伐对粗枝云杉人工林林分细根生物量及碳储量有显著影响(p < 0.05); 而对单株细根生物量影响不一, 间伐10%和20%与对照没有显著性差异(p > 0.05)。间伐显著影响生物量在各根序中的分配, 随着间伐强度的增加, 1、2级细根中生物量分配比例增加, 1级细根的生物量增加幅度最大; 3-5级细根的生物量分配比例减小, 5级细根减少幅度最大。其中, 间伐50%显著减少了细根在下层(20-40 cm)土壤中的生物量比例(p < 0.05), 但与间伐20%和30%无显著差异(p > 0.05)。     

岷江上游华山松林冬季土壤呼吸对模拟增温的短期响应

冬季的土壤呼吸是生态系统呼吸的重要组成部分, 对气候变化的响应可能更为敏感。该文采用红外辐射加热器模拟土壤增温, 研究了岷江上游华山松(Pinus armandii)人工林冬季的土壤呼吸、微生物生物量及无机氮库对模拟增温的响应。结果表明: 在冬季(2009年11月-翌年3月), 模拟增温往往能显著提高土壤呼吸速率, 平均增幅达31.4%; 同样模拟增温使土壤微生物生物量碳、氮分别增加23.2%和22.7%, 而对微生物生物量碳氮比没有影响, 温度升高显著促进了微生物的生长, 但没有改变微生物的群落结构; 增温样地土壤的NO₃ ^--N和NH₄ ⁺-N浓度较对照分别增加了38.5%和12.3%, 增温显著提高了土壤的可溶性无机氮含量。综上所述, 该区针叶林冬季土壤呼吸、微生物生长和养分矿化对未来气候变暖非常敏感。     

黑河中游荒漠草地地上和地下生物量的分配格局

草地生态系统中地上和地下生物量的分配方式对于研究生态系统碳储量和碳循环有着重要的意义。为了解黑河中游荒漠草地的地上和地下生物量分配格局, 从群落和个体两个水平对黑河中游的地上和地下生物量进行了调查。结果表明: 群落水平上地上生物量介于3.2-559.2 g·m^-2之间, 地下生物量介于3.3-188.2 g·m^-2之间, 个体水平上地上生物量介于6.1-489.0 g·株^-1之间, 地下生物量介于2.4-244.2 g·株^-1之间, 群落水平上的根冠比(R/S)为0.10-2.49, 个体水平上为0.07-1.55, 地下生物量均小于地上生物量, 群落水平上R/S值大于个体水平。群落和个体水平地上和地下生物量的拟合斜率分别为1.1001和0.9913, 与1没有显著差异, 说明地上与地下生物量呈等速生长关系。群落和个体水平土壤表层0-20 cm和0-30 cm的根系生物量分别占全部根系生物量的89.81%、96.95%和81.42%、93.62%, 表明地下生物量主要集中在0-20 cm和0-30 cm土壤表层。     

四种不同生活型植物幼苗对喀斯特生境干旱的生理生态适应性

喀斯特石漠化是我国西南喀斯特地区最严重的生态环境问题, 生境干旱是限制该地区植物生长的主要因素之一, 掌握喀斯特植被不同演替阶段不同生活型植物对干旱胁迫的适应策略有助于提高植被恢复的成功率。通过人工模拟4种干旱强度, 测定叶片水势、气体交换、叶绿素荧光、光合色素含量、渗透调节物质浓度、抗氧化酶活性以及生物量, 研究了喀斯特地区4种不同生活型植物幼苗对干旱胁迫的适应策略。这4种植物为常绿灌木火棘(Pyracantha fortuneana)、落叶灌木小果蔷薇(Rosa cymosa)、常绿乔木猴樟(Cinnamomum bodinieri)和落叶乔木圆果化香树(Platycarya longipes)。结果表明: 随着干旱程度的加深, 4种植物幼苗的叶片水势、光合能力、叶绿素含量、生物量增长、叶重比(LMR)、叶面积比(LAR)和比叶面积(SLA)逐渐下降, 而热耗散(NPQ)、类胡萝卜素与叶绿素含量比值、丙二醛含量和根重比(RMR)逐渐上升; 圆果化香树和猴樟的水分利用效率(A_n/g_s)、渗透调节物质浓度和抗氧化酶活性呈先升高后降低的趋势, 而火棘和小果蔷薇的A_n/g_s、脯氨酸含量和超氧化物歧化酶活性呈上升趋势。严重干旱下, 火棘和小果蔷薇幼苗的叶片水势和叶绿素含量下降较少, 具有较高的光合能力和生物量增长, 这主要是由于它们具有较低的SLA和LAR、较高的NPQ和A_n/g_s以及较高的渗透调节能力和抗氧化保护能力。中度干旱下, 猴樟幼苗叶片水势下降很少, LMR和LAR也较高, 脯氨酸含量和抗氧化酶活性非常高。但在严重干旱下, 其叶片水势、LMR、LAR和生物量增长大幅度下降, 最大光化学效率和光合速率也非常低, 渗透调节能力与抗氧化酶活性大幅度下降至正常水平以下。水分好的条件下, 圆果化香树幼苗具有较高的RMR以吸收充足的水分, 具有较高的LAR和叶绿素含量, 保证了生物量的大量积累。然而, 干旱胁迫致使其生物量大幅度下降, 主要是由于LMR、LAR、气体交换和叶绿素含量的大量下降以减少蒸腾面积、水分散失和对光能的吸收。研究结果表明, 火棘、小果蔷薇和猴樟幼苗主要采用耐旱策略, 其中猴樟抗严重干旱的能力较弱; 圆果化香树幼苗对干旱胁迫更为敏感, 主要采取避旱策略。     

水稻光合碳在植物-土壤系统中的分配及其对CO2升高和施氮的响应

采用¹³C-CO₂进行连续标记,研究水稻分蘖期和孕穗期光合碳在植株-土壤系统中的分配及其对大气CO₂浓度升高(800 μL·L^-1)和施氮(100 mg·kg^-1)的响应.结果表明: CO₂浓度升高显著提高分蘖期根系生物量和孕穗期地上部生物量,并使生物量根冠比在分蘖期增加,而在孕穗期减小.CO₂浓度升高条件下,施氮使水稻地上部分生物量增加,却显著降低了孕穗期水稻根系生物量.CO₂浓度升高使光合¹³C在孕穗期向土壤的输入显著增加,然而施肥并没有促进由CO₂浓度升高驱动的光合¹³C在土壤中的积累,而且还降低了土壤中的光合¹³C的分配比例.综上,CO₂浓度升高显著提高了稻田土壤光合碳输入,促进稻田有机碳周转;施氮促进了水稻地上部的生长,却降低了光合碳向地下的分配比例.     

模拟增温和功能群去除对岷江冷杉幼苗存活和生长的影响

通过模拟增温和功能群去除试验,研究不同功能群的草本植物在岷江冷杉幼苗更新定植过程的作用,分析其在温度升高条件下生理指标的变化.结果表明:增温提高了岷江冷杉幼苗的存活率和植物体内非结构性碳水化合物含量,但抑制了幼苗的生长和根冠比.岷江冷杉幼苗的非结构性碳水化合物含量,尤其是可溶性糖含量与存活率呈显著正相关.不增温处理中,草本植物降低了幼苗的存活率,促进幼苗的株高生长和地上生物量积累,禾本科植物和杂类草抑制了幼苗根系生长和地下生物量的积累;增温处理中,杂类草的存在提高了幼苗的存活率,莎草科则显著抑制了幼苗根系生长和地下生物量的积累,禾本科植物和杂类草抑制了幼苗的高生长和地上生物量积累.模拟增温提高了林线树种岷江冷杉幼苗的存活率,但使其面临来自草本植物更剧烈的竞争,抑制其生长.     

Phenotypic plasticity of lianas in response to altered light environment

The growth, morphology and biomass allocation of 11 liana species (six light-demanding and five shade-tolerant) were investigated by growing plants in three contrasting light environments (i.e., field, forest edge and forest interior). Our objectives were to determine: (1) changes in plant traits at the species level; and (2) differences in light-demanding and shade-tolerant species in response to altered light environment. We found that all seedlings of liana species increased in total biomass, total leaf area, relative growth rate (RGR), net assimilation rate (NAR), height, basal diameter, root length, leaf number, root mass/total plant mass (RMR) and root-to-shoot dry biomass (R/S ratio), and decreased in leaf area ratio (LAR), specific leaf area (SLA), leaf size, stem mass-to-total plant mass ratio (SMR) and leaf mass-to-total plant mass ratio (LMR) with increasing light availability. Under the three light environments, the two types of species differed significantly in total biomass, total leaf area, RGR, NAR, LAR, SLA and leaf number, and not in leaf area. Only light-demanding species differed significantly in height, root length, basal diameter, RMR, SMR, LMR and R/S ratio. The mean plasticity index of growth and biomass allocation were relatively higher than the morphological variables, with significant differences between the two groups. Our results showed that liana species respond differently to changing light environments and that light-demanding species exhibit higher plasticity. Such differences may affect the relative success of liana species in forest dynamics.     

Effects of experimental warming on growth,biomass allocation,and needle chemistry of <Emphasis Type="Italic">Abies faxoniana</Emphasis> in even-aged monospecific stands

The response and adaption mechanisms of seedlings under long-term warming have remained largely unknown. In this study, we investigated the effects of warming for 6 years on growth, and needle carbon, nitrogen, chlorophyll, and carbohydrate levels in a coniferous tree species, Abies faxoniana. Seedlings were grown in even-aged monospecific stands under ambient and warming (ambient +2.2°C) temperature in climate control chambers. Warming caused statistically significant increases in the specific leaf area, leaf area ratio, root biomass, leaf biomass, branch biomass, stem biomass, and total mass of the seedlings, and reduced the root/shoot ratio. Warming also increased total chlorophyll concentrations, specific chlorophyll pigments, and Chlorophyll a/b ratios in both studied needle age classes. In addition, C/N ratios of current-year and 1-year-old needles increased by warming. In contrast, warming decreased the levels of N, sugar, cellulose, and starch in needles, while warming had no effect on the height, stem diameter, needle mass ratio, root mass ratio, and root/needle ratio. We conclude that warming increases branch growth and changes needle chemistry, which enhances the light capture potential of seedlings.     

青藏高原高寒草甸两种优势植物的生长及其CNP化学计量特征对模拟增温的响应

以青藏高原高寒草甸和高寒沼泽中的两种优势物种小嵩草(Kobresia pygmaea)和藏嵩草(Kobresia tibetica)为研究对象,采用开顶式增温室(OTCs)模拟气候变暖,对比分析两种植物叶片形态和解剖结构特征、根活性及地上—地下部分化学计量特征对增温的响应差异。结果表明:增温显著增加了小嵩草叶片的长度和叶片的数量,也显著增加了藏嵩草株高和叶片长度;增温没有明显改变小嵩草和藏嵩草的叶片上表皮厚度、下表皮厚度、下表皮细胞角质层厚度、叶肉细胞长和叶肉细胞宽;增温增加了小嵩草根系活跃吸收面积,对小嵩草和藏嵩草其他根系活性指标没有显著影响;增温降低了小嵩草地上部分N含量,对小嵩草地上部分C、P含量没有影响;增温降低了藏嵩草地上部分C、N含量,对P含量没有影响;增温增加了小嵩草和藏嵩草地上部分C/N比,提高了两种优势植物对氮素的长期利用效率;增温对小嵩草地下部分化学计量学特征没有影响,而降低了藏嵩草地下部分C含量和C/N比。     

Responses of phenology and biomass production of boreal fens to climate warming under different water‐table level regimes

Climate change affects peatlands directly through increased air temperatures and indirectly through changes in water‐table level (WL). The interactions of these two still remain poorly known. We determined experimentally the separate and interactive effects of temperature and WL regime on factors of relevance for the inputs to the carbon cycle: plant community composition, phenology, biomass production, and shoot:root allocation in two wet boreal sedge‐dominated fens, “southern” at 62°N and “northern” at 68°Ν. Warming (1.5°C higher average daily air temperature) was induced with open‐top chambers and WL drawdown (WLD; 3–7 cm on average) by shallow ditches. Total biomass production varied from 250 to 520 g/m², with belowground production comprising 25%–63%. Warming was associated with minor effects on phenology and negligible effects on community composition, biomass production, and allocation. WLD clearly affected the contribution of different plant functional types (PFTs) in the community and the biomass they produced: shrubs benefited while forbs and mosses suffered. These responses did not depend on the warming treatment. Following WLD, aboveground biomass production decreased mainly due to reduced growth of mosses in the southern fen. Aboveground vascular plant biomass production remained unchanged but the contribution of different PFTs changed. The observed changes were also reflected in plant phenology, with different PFTs showing different responses. Belowground production increased following WLD in the northern fen only, but an increase in the contributions of shrubs and forbs was observed in both sites, while sedge contribution decreased. Moderate warming alone seems not able to drive significant changes in plant productivity or community composition in these wet ecosystems. However, if warming is accompanied by even modest WL drawdown, changes should be expected in the relative contribution of PFTs, which could lead to profound changes in the function of fens. Consequently, hydrological scenarios are of utmost importance when estimating their future function.     

Density-dependent responses of Picea purpurea seedlings for plant growth and resource allocation under elevated temperature

This study was conducted to determine whether plants in the presence or absence of competition differ in their responses to warming, and whether density modifies the effect of warming. Picea purourea seedlings were grown under ambient and warming (ambient +2.2 °C) conditions in climate control chambers with two different planting densities. After 4 years, seedlings were harvested and measured for height, stem diameter, leaf area, structural biomass, carbon, nitrogen, chlorophyll and carbohydrate levels of needles, branches, stem and roots. At low density, warming increased height, stem diameter, total leaf area biomass production and carbohydrate concentration per seedling, while it decreased C/N ratio for all plant parts, but did not affect chlorophyll content. By contrast, at high density, although warming increased biomass and total leaf area, it did not affect plant height and stem diameter. At the same time, it had different effects on chlorophyll content, C/N ratio and carbohydrate levels among plant parts. On the other hand, high density limited plant growth and altered resource allocation pattern. Our study demonstrates that planting densities decreased the temperature-induced growth enhancement of P. purpurea seedlings and the effects of warming on resource allocation not only showed density-dependence, but also vary with tissue age classes and root diameter; the responses of plants to elevated temperature, acquired from plants growing as individuals, may not be applicable to plants grown under intraspecific competition as typically found in the field.     

光照和氮交互作用对水曲柳幼苗生长、生物量和氮分配的影响

采用温室沙培方式,对水曲柳幼苗进行了不同光强（2个水平）和氮浓度（4个水平）处理,分析了其生长、生物量和氮分配对环境变化的响应.结果表明：与全光照处理相比,低光处理下水曲柳幼苗冠根比（S/R）和净氮吸收速率（NNUR）极显著提高（P<0.01）,但相对生长速率（RGR）和净同化速率（NAR）极显著下降（P<0.01）;低光处理下的幼苗根、茎、叶和整株生物量分别较全光照处理降低了36.8%（P<0.01）、1.7%、12.7%（P<0.05）和24.3%（P<0.01）;低光处理使幼苗分配到根系的氮比例明显下降,而叶片的分配比例增加.无论光强大小,氮对幼苗生长都具有十分明显的促进作用,而且幼苗S/R和叶片的氮分配比例都随氮供给浓度的增加而明显提高.光强和氮浓度对水曲柳幼苗的基径、S/R、RGR和生物量（根和叶）分配比例具有显著的交互作用（P<0.05）.     

Effects of Warming and Nitrogen Addition on Plant Photosynthate Partitioning in an Alpine Meadow on the Tibetan Plateau

Quantifying plant carbon (C) allocation among different pools is critical for understanding and predicting how C turnover responds to global climate change in terrestrial ecosystems. A field experiment with increasing warming and nitrogen (N) was established to investigate interactive effects on plant C allocation in alpine meadows. Open-top chambers (OTCs) were used to simulate warming. In OTCs, daytime air and soil temperature at 5 cm depth increased by 2.0 and 1.6 °C, respectively, compared with ambient conditions, but soil moisture at 5 cm depth decreased by 4.95% (v/v) from 2012 to 2014. Warming reduced aboveground biomass by 38, 36, and 43% in 2012, 2013, and 2014, respectively, and increased belowground biomass by 64% and 29% in 2013 and 2014, respectively, and the root-to-shoot ratio was significantly increased. Specifically, warming increased the proportion of plant roots in the deep layers (10–20 cm). Both N addition and its combination with warming substantially enhanced belowground biomass. Pulse-labeling experiments for ¹³C revealed that warming reduced the translocation of assimilated C to shoots by 8.8% (38.7% in warming, and 47.5% in the control [CK]), and increased the allocation to root by 12.2% (55.5% in warming, and 43.3% in CK) after 28 days labeling. However, N addition increased the proportion of assimilated C allocated to shoots by 6.5% (54.0% in N addition, and 47.5% in CK), whereas warming combined with N addition reduced this proportion by 10.9%. A decline in soil water content in the surface layer may be the main cause of plants allocating more newly fixed photosynthate to roots. Therefore, plants promoted root growth to draw water from deeper soil layers (10–20 cm). We concluded that climate warming will change the allocation patterns of plant photosynthates by affecting soil water availability, whereas N addition will increase plant photosynthates aboveground in alpine meadows and thus will significantly affect C turnover under future climate change scenarios.

     

狭叶红景天幼苗对水分及遮阴的生长及生理生化响应

研究植物对水分和遮阴胁迫的响应及其生理机制对制定合理的栽培管理措施十分必要。以红景天属植物为研究对象,设置土壤含水量分别为田间持水量的80%(过湿水分)、70%(正常水分)、60%(轻度干旱)、40%(中度干旱)、20%(重度干旱)5个水分梯度;设置2个遮阴处理,以全光照(遮阴率为0)为对照、黑色遮阴网遮阴(遮阴率为85%),研究狭叶红景天生长及生理生化指标的变化特征。结果表明:在不同水分处理下,与对照相比,叶绿素含量、茎干重和茎重比(SMR)显著增加(P0.05),株高、总生物量、叶面积、叶干重、叶重比(LMR)、比叶面积(SLA)、叶面积比(LAR)和叶面积根干重比(LARMR)增加,根冠比和根重比(RMR)减少;随着干旱程度加剧,丙二醛(MDA)、脯氨酸(Pro)和可溶性糖(Ss)含量增加,超氧化物歧化酶(SOD)活性总体呈先增加后减小的趋势。在遮阴处理下,株高、SMR、SLA、LAR和LARMR显著增加(P0.05),叶绿素SPAD值和叶面积增加,总生物量、根干重、根冠比和LMR显著减少(P0.05),茎干重和叶干重减少,MDA含量显著增加,Pro含量略有下降,Ss含量减少。在水分胁迫下,狭叶红景天中度干旱时通过增加酶活性抵御伤害,重度干旱超过其阈值,SOD活性下降,植物体受到伤害,Ss可能是主要的渗透调节物质。在遮阴处理下,狭叶红景天通过增加SLA避免遮阴伤害。狭叶红景天在受到环境胁迫时会通过形态改变、调节MDA含量、抗氧化酶活性和渗透调节物质来保证自身正常的生长发育。