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1.
Site-dependent N uptake from N-form mixtures by arctic plants,soil microbes and ectomycorrhizal fungi 总被引:1,自引:0,他引:1
Soil microbes constitute an important control on nitrogen (N) turnover and retention in arctic ecosystems where N availability
is the main constraint on primary production. Ectomycorrhizal (ECM) symbioses may facilitate plant competition for the specific
N pools available in various arctic ecosystems. We report here our study on the N uptake patterns of coexisting plants and
microbes at two tundra sites with contrasting dominance of the circumpolar ECM shrub Betula nana. We added equimolar mixtures of glycine-N, NH4+–N and NO3−–N, with one N form labelled with 15N at a time, and in the case of glycine, also labelled with 13C, either directly to the soil or to ECM fungal ingrowth bags. After 2 days, the vegetation contained 5.6, 7.7 and 9.1% (heath
tundra) and 7.1, 14.3 and 12.5% (shrub tundra) of the glycine-, NH4+- and NO3−–15N, respectively, recovered in the plant–soil system, and the major part of 15N in the soil was immobilized by microbes (chloroform fumigation-extraction). In the subsequent 24 days, microbial N turnover
transferred about half of the immobilized 15N to the non-extractable soil organic N pool, demonstrating that soil microbes played a major role in N turnover and retention
in both tundra types. The ECM mycelial communities at the two tundras differed in N-form preferences, with a higher contribution
of glycine to total N uptake at the heath tundra; however, the ECM mycelial communities at both sites strongly discriminated
against NO3−. Betula nana did not directly reflect ECM mycelial N uptake, and we conclude that N uptake by ECM plants is modulated by the N uptake
patterns of both fungal and plant components of the symbiosis and by competitive interactions in the soil. Our field study
furthermore showed that intact free amino acids are potentially important N sources for arctic ECM fungi and plants as well
as for soil microorganisms.
Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users. 相似文献
2.
The influence of plants grown under elevated CO2 and N fertilization on soil nitrogen dynamics 总被引:1,自引:0,他引:1
We investigated the effects of spring barley growth on nitrogen (N) transformations and rhizosphere microbial processes in a controlled system under elevated carbon dioxide (CO2) at two levels of N fertilization (applied with 15N labelling). After 25 d, elevated CO2 (twice ambient) increased plant growth (dry weight, DW) by 141% at low‐N fertilization and by 60% at high‐N fertilization, but its positive effect on the root‐to‐shoot ratio was only significant at low‐N input. As a result of this plant response, elevated CO2 caused a greater soil CO2 efflux, rhizosphere soil DW, and soil microbial biomass under N‐limiting conditions than under high N availability. Elevated CO2 also caused a significant (P < 0.001) increase in the N recovered by the plant from both the labelled (Nf) and unlabelled (Ns + Nuf) N pools. The dynamics of N in the system as affected by elevated CO2 were driven principally by mineralization–immobilization turnover, with little loss by denitrification. Under N‐limiting conditions, there is evidence to suggest enhanced nutrient release from soil organic matter (SOM) pools—a process which could be defined as priming. The results of our experiment did not indicate a direct plant‐mediated effect of elevated CO2 on nitrous oxide (N2O) fluxes or denitrification activity. 相似文献
3.
Off-season uptake of nitrogen in temperate heath vegetation 总被引:3,自引:0,他引:3
In this field study we show that temperate coastal heath vegetation has a significant off-season uptake potential for nitrogen,
both in the form of ammonium and as glycine, throughout winter. We injected 15N-ammonium and 15N 2×(13C)-glycine into the soil twice during winter and once at spring. The winter temperatures were similar to those of an average
winter in the northern temperate region of Europe, with only few days of soil temperatures below zero or above 5°C. The vegetation,
consisting of the evergreen dwarf shrub Calluna vulgaris, the deciduous dwarf shrub Salix arenaria, and the graminoids Carex arenaria and Deschampsia flexuosa, showed high root uptake of both forms of nitrogen, both 1 day after labelling and after a month, in species specific temporal
patterns. Plant uptake of 13C was not significant, providing no further evidence of intact uptake of glycine. Translocation of the labelled nitrogen to
shoots was generally evident after 1 month and increased as spring approached, with different translocation strategies in
the three plant functional types. Furthermore, only the graminoids showed shoot growth during winter. Increasing plant nitrogen
concentration from fall to spring at temperate heaths may, hence, be due to nitrogen uptake. Our results suggest that the
potential for nitrogen uptake in plants at winter is of the same order of magnitude as at summer. Hence, winter nitrogen uptake
in ecosystems in the temperate/boreal region should be considered when making annual nitrogen budgets of heath ecosystems,
and the view of plant nutrient uptake as low in this climatic region during winter should be revised. 相似文献
4.
Gorka Erice Juan J. Irigoyen Pilar Prez Rafael Martínez-Carrasco Manuel Snchez-Díaz 《Plant science》2006,170(6):1059-1067
The rising atmospheric CO2 concentration resulting from industrial development may enhance photosynthesis and plant growth. However, there is a lack of research concerning the effect of combined factors such as CO2, temperature and water availability on plant regrowth following cutting or grazing, which represent the usual methods of managing forage legumes like alfalfa. Elevated CO2, temperature and drought can interact with cutting factors (e.g. cutting frequency or height), and source-sink balance differences before and after defoliation can modify photosynthetic behaviour and dry matter accumulation, as well as dry matter partitioning between above- and belowground organs. The aim of our study was to determine the interactive effect of CO2 (ambient, around 350 μmol mol−1 versus 700 μmol mol−1), temperature (ambient versus ambient + 4 °C) and water availability (well-irrigated versus partially irrigated) on dry matter partitioning and photosynthesis in nodulated alfalfa after vegetative normal growth and during regrowth. At the end of vegetative normal growth, CO2 enhanced dry matter accumulation despite photosynthesis being down-regulated at the end of this period. Photosynthesis was stimulated by elevated CO2 and resulted in greater dry matter accumulation during the regrowth period. Aboveground organs were affected more by drought than belowground organs during the entire experiment, particularly during vegetative normal growth. The higher drought tolerance (greater growth) observed during the regrowth period may be related to higher mass and greater reserves accumulated in the roots of plants. 相似文献
5.
Effects of elevated CO2 , temperature and N fertilization on nitrogen fluxes in a temperate grassland ecosystem 总被引:2,自引:0,他引:2
The soil nitrogen cycle was investigated in a pre‐established Lolium perenne sward on a loamy soil and exposed to ambient and elevated atmospheric CO2 concentrations (350 and 700 μL L?1) and, at elevated [CO2], to a 3 °C temperature increase. At two levels of mineral nitrogen supply, N– (150 kgN ha?1 y?1) and N+ (533 kgN ha?1 y?1), 15N‐labelled ammonium nitrate was supplied in split applications over a 2.5‐y period. The recovery of the labelled fertilizer N was measured in the harvests, in the stubble and roots, in the macro‐organic matter fractions above 200 μm in size (MOM) and in the aggregated organic matter below 200 μM (AOM). Elevated [CO2] reduced the total amount of N harvested in the clipped parts of the sward. The harvested N derived from soil was reduced to a greater extent than that derived from fertilizer. At both N supplies, elevated [CO2] modified the allocation of the fertilizer N in the sward, in favour of the stubble and roots and significantly increased the recovery of fertilizer N in the soil macro‐organic matter fractions. The increase of fertilizer N immobilization in the MOM was associated with a decline of fertilizer N uptake by the grass sward, which supported the hypothesis of a negative feedback of elevated [CO2] on the sward N yield and uptake. Similar and even more pronounced effects were observed for the native N mineralized in the soil. At N–, a greater part of the fertilizer N organized in the root phytomass resulted in an underestimation of N immobilized in dead roots and, in turn, an underestimation of N immobilization in the MOM. The 3 °C temperature increase alleviated the [CO2] effect throughout much of the N cycle, increasing soil N mineralization, N derived from soil in the harvests, and the partitioning of the assimilated fertilizer N to shoots. In conclusion, at ambient temperature, the N cycle was slowed down under elevated [CO2], which restricted the increase in the aboveground production of the grass sward, and apparently contributed to the sequestration of carbon belowground. In contrast, a temperature increase under elevated [CO2] stimulated the soil nitrogen cycle, improved the N nutrition of the sward and restricted the magnitude of the soil C sequestration. 相似文献
6.
大气CO2浓度升高对土壤氮素转化过程产生重要影响,研究其变化有助于更好地预测陆地生态系统的固碳潜力.氮同位素自然丰度作为生态系统氮素循环过程的综合指标能够有效地指示CO2浓度升高对土壤氮素转化过程的影响.本研究采用开顶箱CO2 熏蒸法研究连续10年的大气CO2 浓度升高对我国东北地区蒙古栎及其土壤和微生物生物量碳、氮同位素自然丰度的影响.结果表明: 大气CO2浓度升高改变了土壤氮循环过程,增加了土壤微生物和植物叶片δ15N;促进了富13C土壤有机碳分解,中和了贫13C植物光合碳输入的效果,导致土壤可溶性有机碳和微生物碳δ13C在CO2升高条件下没有发生显著变化.这些结果表明,CO2浓度升高很可能促进了土壤有机质矿化过程,并加剧了系统氮限制的状态. 相似文献
7.
KIRSTEN S. HOFMOCKEL † WILLIAM H. SCHLESINGER ROBERT B. JACKSON‡ 《Global Change Biology》2007,13(9):1950-1959
Rising atmospheric carbon dioxide (CO2) is expected to increase forest productivity, resulting in greater carbon (C) storage in forest ecosystems. Because elevated atmospheric CO2 does not increase nitrogen (N) use efficiency in many forest tree species, additional N inputs will be required to sustain increased net primary productivity (NPP) under elevated atmospheric CO2. We investigated the importance of free amino acids (AAs) as a source for forest N uptake at the Duke Forest Free Air CO2 Enrichment (FACE) site, comparing its importance with that of better‐studied inorganic N sources. Potential proteolytic enzyme activity was monitored seasonally, and individual AA concentrations were measured in organic horizon extracts. Potential free AA production in soils ranged from 190 to 690 nmol N g−1 h−1 and was greater than potential rates of soil NH4+ production. Because of this high potential rate of organic N production, we determined (1) whether intact AA uptake occurs by Pinus taeda L., the dominant tree species at the FACE site, (2) if the rate of cycling of AAs is comparable with that of ammonium (NH4+), and (3) if atmospheric CO2 concentration alters the aforementioned N cycling processes. A field experiment using universally labeled ammonium (15NH4+) and alanine (13C3H715NO2) demonstrated that 15N is more readily taken up by plants and heterotrophic microorganisms as NH4+. Pine roots and microbes take up on average 2.4 and two times as much NH4+ 15N compared with alanine 15N 1 week after tracer application. N cycling through soil pools was similar for alanine and NH4+, with the greatest 15N tracer recovery in soil organic matter, followed by microbial biomass, dissolved organic N, extractable NH4+, and fine roots. Stoichiometric analyses of 13C and 15N uptake demonstrated that both plants and soil microorganisms take up alanine directly, with a 13C : 15N ratio of 3.3 : 1 in fine roots and 1.5 : 1 in microbial biomass. Our results suggest that intact AA (alanine) uptake contributes substantially to plant N uptake in loblolly pine forests. However, we found no evidence supporting increased recovery of free AAs in fine roots under elevated CO2, suggesting plants will need to acquire additional N via other mechanisms, such as increased root exploration or increased N use efficiency. 相似文献
8.
The natural abundance of 15N in plant biomass has been used to infer how N dynamics change with elevated atmospheric CO2 and changing water availability. However, it remains unclear if atmospheric CO2 effects on plant biomass 15N are driven by CO2-induced changes in soil moisture. We tested whether 15N abundance (expressed as δ15N) in plant biomass would increase with increasing soil moisture content at two atmospheric CO2 levels. In a greenhouse experiment we grew sunflower (Helianthus annuus) at ambient and elevated CO2 (760 ppm) with three soil moisture levels maintained at 45, 65, and 85% of field capacity, thereby eliminating potential
CO2-induced soil moisture effects. The δ15N value of total plant biomass increased significantly with increased soil moisture content at both CO2 levels, possibly due to increased uptake of 15N-rich organic N. Although not adequately replicated, plant biomass δ15N was lower under elevated than under ambient CO2 after adjusting for plant N uptake effects. Thus, increases in soil moisture can increase plant biomass δ15N, while elevated CO2 can decrease plant biomass δ15N other than by modifying soil moisture. 相似文献
9.
Shuijin Hu Jiansheng Wu Kent O. Burkey† Mary K. Firestone‡ 《Global Change Biology》2005,11(2):213-223
The impact of elevated CO2 on terrestrial ecosystem C balance, both in sign or magnitude, is not clear because the resulting alterations in C input, plant nutrient demand and water use efficiency often have contrasting impacts on microbial decomposition processes. One major source of uncertainty stems from the impact of elevated CO2 on N availability to plants and microbes. We examined the effects of atmospheric CO2 enrichment (ambient+370 μmol mol?1) on plant and microbial N acquisition in two different mesocosm experiments, using model plant species of annual grasses of Avena barbata and A. fatua, respectively. The A. barbata experiment was conducted in a N‐poor sandy loam and the A. fatua experiment was on a N‐rich clayey loam. Plant–microbial N partitioning was examined through determining the distribution of a 15N tracer. In the A. barbata experiment, 15N tracer was introduced to a field labeling experiment in the previous year so that 15N predominantly existed in nonextractable soil pools. In the A. fatua experiment, 15N was introduced in a mineral solution [(15NH4)2SO4 solution] during the growing season of A. fatua. Results of both N budget and 15N tracer analyses indicated that elevated CO2 increased plant N acquisition from the soil. In the A. barbata experiment, elevated CO2 increased plant biomass N by ca. 10% but there was no corresponding decrease in soil extractable N, suggesting that plants might have obtained N from the nonextractable organic N pool because of enhanced microbial activity. In the A. fatua experiment, however, the CO2‐led increase in plant biomass N was statistically equal to the reduction in soil extractable N. Although atmospheric CO2 enrichment enhanced microbial biomass C under A. barbata or microbial activity (respiration) under A. fatua, it had no significant effect on microbial biomass N in either experiment. Elevated CO2 increased the colonization of A. fatua roots by arbuscular mycorrhizal fungi, which coincided with the enhancement of plant competitiveness for soluble soil N. Together, these results suggest that elevated CO2 may tighten N cycling through facilitating plant N acquisition. However, it is unknown to what degree results from these short‐term microcosm experiments can be extrapolated to field conditions. Long‐term studies in less‐disturbed soils are needed to determine whether CO2‐enhancement of plant N acquisition can significantly relieve N limitation over plant growth in an elevated CO2 environment. 相似文献
10.
以CO2浓度升高为主要标志的全球气候变化及由其引起的极端气候变化对陆地生态系统产生了重要的影响。利用步入式CO2生长室模拟研究了CO2浓度变化(400和700μL/L)和干旱胁迫(水分充足CK:100%FC(田间持水量);中度干旱MS:40%FC;重度干旱SS:20%FC)的交互作用对草本植物网果酸模(Rumex chalepensis)、野豌豆(Vicia sepium)、泥胡菜(Hemmistepta lyrata)、风轮菜(Clinopodium chinense)、藜(Chenopodium album)和玉米石(Sedum album)生长特性的影响。结果表明:CO2浓度升高总体上刺激了网果酸模、野豌豆、泥胡菜、风轮菜和藜这5种C3植物在任何水分条件下的生长,也刺激了玉米石在水分条件较好下的生长;干旱胁迫总体上抑制了所有6种植物的生长,但中度干旱胁迫有刺激CAM植物玉米石生长的趋势。CO2浓度升高能否缓解干旱的负面影响具有明显的种间差异:CO2浓度升高减缓了干旱胁迫对泥胡菜和风轮菜的负面影响,这种缓解作用在网果酸模和野豌豆中显著降低,对藜没有明显的促进作用,对干旱下的玉米石的生长却起到了抑制作用。CO2浓度升高总体上增加了根质量分数和干物质含量;干旱胁迫明显提高了6种草本植物的根生物量的分配比例,降低了干物质含量;但CO2浓度升高和干旱胁迫的交互作用可导致不同的物种产生不同的响应,说明植物能够通过调节生物量分配和植株本身的水分含量保持能力来适应CO2浓度和干旱胁迫的交互影响,这种调节能力取决于植物在碳的吸收和水分散失之间的平衡"trade-off"。研究结果有助于增进草本植物对未来气候变化的适应性理解,为评估和预测全球气候和水文变化对植物的生理生态影响提供理论依据。 相似文献
11.
Mineralization of organically bound nitrogen in soil as influenced by plant growth and fertilization
L. H. Sørensen 《Plant and Soil》1982,65(1):51-61
Summary A loam soil containing an organic fraction labelled with15N was used for pot experiments with spring barley, rye-grass and clover. The organically bound labelled N was mineralized
at a rate corresponding to a half-life of about 9 years.
Fertilization with 106 and 424 kgN/ha of unlabelled N in the form of KNO3 significantly increased uptake of labelled N from the soil in barley and the first harvest of rye-grass crops. The fertilized
plants removed all the labelled NH4 and NO3 present in the soil, whereas the unfertilized plants removed only about 80%.
The second, third and fourth harvests of the unfertilized rye-grass took up more labelled N than the fertilized rye-grass.
The total uptake in the four harvests was similar whether the plants were fertilized or not.
Application of KCl to barley plants in amounts equivalent to that of KNO3 resulted in a small but insignificant increase in uptake of labelled N.
The uptake of labelled N in the first harvest of clover which was not fertilized but inoculated with Rhizobium was similar
to that of the fully fertilized rye-grass indicating that the biological fixation of N had the same effect as addition of
N-fertilizer. N uptake in the following harvests was lower and the total uptake by four harvests of clover was similar to
that of rye-grass.
There was no indication that fertilization with KNO3 accelerated the mineralization of the organically bound labelled N. The observed apparent ‘priming effect’ of the fertilizer
on the uptake of labelled N was compensated by subsequent crops and harvests, and it seems to arise from a more thorough search
of the soil volume by a better developed root system of the fertilized plants. 相似文献
12.
鼎湖山苗圃和主要森林土壤CO2排放和CH4吸收对模拟N沉降的短期响应 总被引:16,自引:0,他引:16
研究了鼎湖山生物圈保护区苗圃(幼苗)、马尾松、混交林和季风常绿阔叶林(季风林)土壤CO2排放和CH4吸收的一些特征及其对模拟N沉降增加的响应.结果表明,土壤CO2日(白天)平均排放量的大小顺序为(平均值±标准误)苗圃(258±62mg·m-2·h-1)>季风林(177±42 mg·m-2·h-1)>马尾松林(162±39 mg·m-2·h-1)>混交林(126±30 mg·m-2·h-1).土壤CH4日(白天)平均吸收量的大小顺序为马尾松林(-0.15±0.02 mg·m-2·h-1)>季风林(-0.08±0.01 mg·m-2·h-1)>混交林(-0.07±0.01 mg·m-2·h-1)>苗圃(-0.05±0.01 mg·m-2·h-1).低N(50 kg N·hm-2·a-1)和中N(100kg N·hm-2·a-1)处理对苗圃、马尾松林和混交林样地土壤CO2日平均排放量的影响均不明显,高N(150 kg N·hm-2·a-1)处理对苗圃土壤CO2的日平均排放量也无显著影响,但倍高N(300kg N·hm-2·a-1)处理显著促进苗圃样地土壤CO2的排放.然而,所有N(低N、中N和高N)处理均显著促进季风林土壤CO2日平均排放量,且这种促进作用随N处理水平的升高而增加.N处理显著促进季风林和马尾松林土壤对CH4吸收速率,但对混交林土壤CH4吸收则无明显的影响.在苗圃样地,除倍高N外,N处理对土壤CH4吸收速率也无显著作用,但倍高N处理使苗圃土壤发生功能转变,即从CH4汇转变为CH4源. 相似文献
13.
增温和CO2浓度加倍对川西亚高山针叶林土壤可溶性氮的影响 总被引:1,自引:0,他引:1
采用全自动微气候控制的"人工模拟气候实验系统"研究了增温和CO2浓度加倍对川西亚高山针叶林土壤硝态氮(NO_3~--N)、铵态氮(NH_4~+-N)、游离氨基酸(FAA)、可溶性有机氮(DON)和可溶性总氮(TSN)的影响。结果表明:1在种植油松苗木组,增温处理显著降低了土壤NO_3~--N含量,不同处理0—15 cm土层NO_3~--N含量均显著小于15—30 cm层;而在未种树组,增温处理显著增加了土壤NO_3~--N含量,0—15 cm土层NO_3~--N含量显著高于15—30 cm层,这表明增温促进了油松苗对NO_3~--N的吸收。2在种植油松苗木组,增温(ET)、增CO_2(EC)及两者的共同作用(ETC)均显著增加了土壤NH_4~+-N、DON和TSN含量;在未种树组,ET显著增加了土壤NH_4~+-N、FAA、DON和TSN含量,EC和ETC对NH_4~+、FAA、DON和TSN含量具有微弱影响或没有显著影响。不同处理0—15cm层土壤NH_4~+-N、FAA、DON和TSN的含量显著大于15—30 cm层。3种植油松苗木组土壤NO_3~--N、NH_4~+-N、FAA、DON和TSN含量均显著低于未种树组,这是由植物对氮素的吸收消耗造成的。研究结果表明,EC、ETC主要通过植物根系作用促进了NH_4~+-N、DON和TSN含量增加,而ET处理通过影响土壤微生物和植物根系来促进NH_4~+-N、FAA、DON和TSN含量的增加。 相似文献
14.
应用自控、封闭、独立的生长室系统,研究川西亚高山林线复合群落根际、非根际土壤微生物数量以及根际、非根际土壤酶活性对大气CO2浓度升高(环境CO2浓度+350(±25)μmol.mol-1,EC)和温度升高(环境温度+2.0(±0.5)℃,ET)及其两者同时升高(ECT)的响应。结果表明:(1)与对照(CK)相比,EC、ET和ECT处理能够增加土壤根际微生物数量,但不同微生物种类对EC、ET和ECT的反应有所差异。(2)不同种类的根际土壤酶对EC、ET和ECT的响应不同。(3)与CK相比,EC、ET和ECT的非根际土壤微生物数量以及非根际土壤酶活性均无显著提高。(4)EC、ET和ECT处理对复合群落土壤微生物总数的根际效应明显;除ET处理的转化酶为负根际效应,其余处理的过氧化氢酶,脲酶及转化酶均表现为正根际效应。 相似文献
15.
Intact amino acid uptake by northern hardwood and conifer trees 总被引:1,自引:0,他引:1
Anne Gallet-Budynek Edward Brzostek Vikki L. Rodgers Jennifer M. Talbot Sharon Hyzy Adrien C. Finzi 《Oecologia》2009,160(1):129-138
Empirical and modeling studies of the N cycle in temperate forests of eastern North America have focused on the mechanisms
regulating the production of inorganic N, and assumed that only inorganic forms of N are available for plant growth. Recent
isotope studies in field conditions suggest that amino acid capture is a widespread ecological phenomenon, although northern
temperate forests have yet to be studied. We quantified fine root biomass and applied tracer-level quantities of U–13C2–15N-glycine, 15NH4
+ and 15NO3
− in two stands, one dominated by sugar maple and white ash, the other dominated by red oak, beech, and hemlock, to assess
the importance of amino acids to the N nutrition of northeastern US forests. Significant enrichment of 13C in fine roots 2 and 5 h following tracer application indicated intact glycine uptake in both stands. Glycine accounted for
up to 77% of total N uptake in the oak–beech–hemlock stand, a stand that produces recalcitrant litter, cycles N slowly and
has a thick, amino acid-rich organic horizon. By contrast, glycine accounted for only 20% of total N uptake in the sugar maple
and white ash stand, a stand characterized by labile litter and rapid rates of amino acid production and turnover resulting
in high rates of mineralization and nitrification. This study shows that amino acid uptake is an important process occurring
in two widespread, northeastern US temperate forest types with widely differing rates of N cycling. 相似文献
16.
Usue Prez-Lpez Anabel Robredo Maite Lacuesta Amaia Mena-Petite Alberto Muoz-Rueda 《Environmental and Experimental Botany》2009,66(3):463-470
With the changing climate, plants will be facing increasingly harsh environmental conditions marked by elevated salinity in the soils and elevated concentrations of CO2 in the atmosphere. These two factors have opposite effects on water status in plants. Therefore, our objective was to determine the interaction between these two factors and to determine whether elevated [CO2] might alleviate the adverse effects of salt stress on water status in two barley cultivars, Alpha and Iranis, by studying their relative water content and their water potential and its components, transpiration rate, hydraulic conductance, and water use efficiency. Both cultivars maintained their water status under salt stress, increasing water use efficiency and conserving a high relative water content by (1) reducing water potential via passive dehydration and active osmotic adjustment and (2) decreasing transpiration through stomatal closure and reducing hydraulic conductance. Iranis showed a greater capacity to achieve osmotic adjustment than Alpha. Under the combined conditions of salt-stress and elevated [CO2], both cultivars (1) achieved osmotic adjustment to a greater extent than at ambient [CO2], likely due to elevated rates of photosynthesis, and (2) decreased passive dehydration by stomatal closure, thereby maintaining a greater turgor potential, relative water content, and water use efficiency. Therefore, we found an interaction between salt stress and elevated [CO2] with regard to water status in plants and found that elevated [CO2] is associated with improved water status of salt-stressed barley plants. 相似文献
17.
植物病害是降低植物产量和产品品质的重要因素,但对其在气候变化情景下如何影响植物的研究鲜见报道。利用封闭式人工气候室模拟不同环境处理,探讨了大气CO2浓度增加和温度升高情况下白粉菌(Podosphaera xanthii)侵染对西葫芦(Cucurbita pepo)生长发育的影响。结果表明,单独CO2加富(EC)增强了西葫芦光合作用(P<0.05),促进了植株生长和果实生产;CO2浓度和温度同时升高(ECT)也促进了光合作用(P<0.05),加速了植株器官发育,但限制了叶片叶绿素合成和叶片面积生长,最终明显降低了植株地上部分干物质积累和果实产量(P<0.05)。和对照相比,EC处理下白粉菌的生长繁殖没有明显变化,但由于西葫芦植株的抗病性有所改善,植株病情指数略有下降;而ECT处理下白粉菌的发育繁殖明显改善,P. xanthii菌落规模和产孢能力极大提高(P<0.01),植物病情指数显著加重(P<0.01),作物严重减产(P<0.01)。可见,在未来以CO2浓度和温度升高为特征的气候变化条件下,白粉菌倾向于加重对西葫芦的侵染。这个结论对其他葫芦科白粉病的防治管理也有借鉴作用。 相似文献
18.
SVEN MARHAN ELLEN KANDELER STEFANIE REIN† REAS FANGMEIER† PASCAL A. NIKLAUS‡ 《Global Change Biology》2010,16(1):469-483
Increased plant productivity under elevated atmospheric CO2 concentrations might increase soil carbon (C) inputs and storage, which would constitute an important negative feedback on the ongoing atmospheric CO2 rise. However, elevated CO2 often also leads to increased soil moisture, which could accelerate the decomposition of soil organic matter, thus counteracting the positive effects via C cycling. We investigated soil C sequestration responses to 5 years of elevated CO2 treatment in a temperate spring wheat agroecosystem. The application of 13C‐depleted CO2 to the elevated CO2 plots enabled us to partition soil C into recently fixed C (Cnew) and pre‐experimental C (Cold) by 13C/12C mass balance. Gross C inputs to soils associated with Cnew accumulation and the decomposition of Cold were then simulated using the Rothamsted C model ‘RothC.’ We also ran simulations with a modified RothC version that was driven directly by measured soil moisture and temperature data instead of the original water balance equation that required potential evaporation and precipitation as input. The model accurately reproduced the measured Cnew in bulk soil and microbial biomass C. Assuming equal soil moisture in both ambient and elevated CO2, simulation results indicated that elevated CO2 soils accumulated an extra ~40–50 g C m?2 relative to ambient CO2 soils over the 5 year treatment period. However, when accounting for the increased soil moisture under elevated CO2 that we observed, a faster decomposition of Cold resulted; this extra C loss under elevated CO2 resulted in a negative net effect on total soil C of ~30 g C m?2 relative to ambient conditions. The present study therefore demonstrates that positive effects of elevated CO2 on soil C due to extra soil C inputs can be more than compensated by negative effects of elevated CO2 via the hydrological cycle. 相似文献
19.
Kees-Jan Van Groenigen Johan Six David Harris‡ Herbert Blum§ Chris Van Kessel 《Global Change Biology》2003,9(12):1751-1762
Reduced soil N availability under elevated CO2 may limit the plant's capacity to increase photosynthesis and thus the potential for increased soil C input. Plant productivity and soil C input should be less constrained by available soil N in an N2‐fixing system. We studied the effects of Trifolium repens (an N2‐fixing legume) and Lolium perenne on soil N and C sequestration in response to 9 years of elevated CO2 under FACE conditions. 15N‐labeled fertilizer was applied at a rate of 140 and 560 kg N ha?1 yr?1 and the CO2 concentration was increased to 60 Pa pCO2 using 13C‐depleted CO2. The total soil C content was unaffected by elevated CO2, species and rate of 15N fertilization. However, under elevated CO2, the total amount of newly sequestered soil C was significantly higher under T. repens than under L. perenne. The fraction of fertilizer‐N (fN) of the total soil N pool was significantly lower under T. repens than under L. perenne. The rate of N fertilization, but not elevated CO2, had a significant effect on fN values of the total soil N pool. The fractions of newly sequestered C (fC) differed strongly among intra‐aggregate soil organic matter fractions, but were unaffected by plant species and the rate of N fertilization. Under elevated CO2, the ratio of fertilizer‐N per unit of new C decreased under T. repens compared with L. perenne. The L. perenne system sequestered more 15N fertilizer than T. repens: 179 vs. 101 kg N ha?1 for the low rate of N fertilization and 393 vs. 319 kg N ha?1 for the high N‐fertilization rate. As the loss of fertilizer‐15N contributed to the 15N‐isotope dilution under T. repens, the input of fixed N into the soil could not be estimated. Although N2 fixation was an important source of N in the T. repens system, there was no significant increase in total soil C compared with a non‐N2‐fixing L. perenne system. This suggests that N2 fixation and the availability of N are not the main factors controlling soil C sequestration in a T. repens system. 相似文献
20.
Christian Kampichler Ellen Kandeler† Richard D. Bardgett‡ T. Hefin Jones§ Lindsey J. Thompson§ 《Global Change Biology》1998,4(3):335-346
Although soil organisms play an essential role in the cycling of elements in terrestrial ecosystems, little is known of the impact of increasing atmospheric CO2 concentrations on soil microbial processes. We determined microbial biomass and activity in the soil of multitrophic model ecosystems housed in the Ecotron (NERC Centre for Population Biology, Ascot, UK) under two atmospheric CO2 concentrations (ambient vs. ambient + 200 ppm). The model communities consist of four annual plant species which naturally co-occur in weedy fields and disturbed ground throughout southern England, together with their herbivores, parasitoids and soil biota. At the end of two experimental runs lasting 9 and 4.5 months, respectively, root dry weight and quality showed contradictory responses to elevated CO2 concentrations, probably as a consequence of the different time-periods (and hence number of plant generations) in the two experiments. Despite significant root responses no differences in microbial biomass could be detected. Effects of CO2 concentration on microbial activity were also negligible. Specific enzymes (protease and xylanase) showed a significant decrease in activity in one of the experimental runs. This could be related to the higher C:N ratio of root tissue. We compare the results with data from the literature and conclude that the response of complex communities cannot be predicted on the basis of oversimplified experimental set-ups. 相似文献