The influence of waterlogging at different temperatures on penetration depth and porosity of roots and on stomatal diffusive resistance of pea and maize seedlings

The 8 days old seedlings of pea (cv. Ilowiecki) and maize (cv. Alma F1) were subjected to differentiated aeration conditions (control — with pore water tension about 15 kPa and flooded treatment) for 12 days at three soil temperatures (7, 15 and 25 °C). The shoots were grown at 25 °C while the soil temperature was differentiated by keeping the cylinders with the soil in thermostated water bath of the appropriate temperature. Lowering the root temperature with respect to the shoot temperature caused under control (oxic) conditions a decrease of the root penetration depth, their mass and porosity as well as a decrease of shoot height, their mass and chlorophyll content; the changes being more pronounced in maize as compared to the pea plants. Flooding the soil diminished the effect of temperature on the investigated parameters; the temperature effect remaining significant only in the case of shoot biomass and root porosity of pea plants. Root porosity of pea plants ranged from 2 to 4 % and that of maize plants — from 4 to 6 % of the root volume. Flooding the soil caused an increase in the root porosity of the pea plants in the entire temperature range and in maize roots at lower temperatures by about 1 % of the root volume. Flooding the soil caused a decrease of root mass and penetration depth as well as a decrease of plant height, biomass and leaf chlorophyll content.     

The Effect of Lateral Root Outgrowth on the Structure and Permeability of the Onion Root Exodermis

Lateral root development in onion is accompanied by a variety of anatomical and permeability changes in some cells of the adventitious root. The endodermal Casparian band of the parent root is disrupted early in the development of the lateral but later extends so as to be continuous with the developing Casparian band of the new root. The lateral root emerges through a longitudinal split in the adventitious root exodermis and epidermis. Following this, the cell walls and intercellular air spaces adjacent to the lateral become incrusted with suberin and a small amount of lignin, forming a collar of modified tissue around the lateral. Subsequent radial expansion of the lateral distorts the adjacent cells of the adventitious root and forces a tight association between it and the lateral. The apoplastic permeability of lateral/parent root junctions was tested using Cellufluor, an apoplastic fluorescent dye which binds to cellulose. Prior to lateral root emergence, no dye enters the parent root cortex due to the Casparian band of the exodermis. Immediately after emergence, dye often penetrates through the break in the exodermal Casparian band and diffuses into the first cortical cell layer. However, when the collar of suberized cells develops (two days after lateral root emergence), movement of the dye into an undisturbed adventitious root is usually prevented (i.e., in 77% of the cases examined). In contrast, only 17% of the root systems which were transplanted just prior to treatment excluded the dye. This indicates that the apoplastic seals around the laterals are sensitive to movement and we recommend that only undisturbed root systems be used for permeability studies.     

Feature article

Domesticated maize emerged from human selection, exploitation, and cultivation of natural recombinants between two wild grasses that had novel characteristics desired by humans for food. Crossing experiments reconstructing prototypes of ancient archaeological specimens demonstrate how the simple flowering spike of the wild relatives of maize was transformed into the prolific grain-bearing ear within a few generations of intergenomic recombination between teosinte andTripsacum. The high degree of morphological similarities of segregating intercross progeny to archaeological specimens from Tehuacán, Oaxaca, and Tamaulipas provides strong support for this evolutionary scenario. Comparative genomic analysis of maize, teosinte, andTripsacum confirms that maize has inherited unique polymorphisms from aTripsacum ancestor and other unique polymorphisms from a teosinte progenitor. This supports the hypothesis thatTripsacum introgression provided the mutagenic action for the transformation of the teosinte spike into the maize ear. This model for the origin of maize explains its sudden appearance, rapid evolutionary trajectory, and genesis of its spectacular biodiversity.     

Variation for Root Aerenchyma Formation in Flooded and Non-Flooded Maize and Teosinte Seedlings

Morphological and anatomical factors such as aerenchyma formation in roots and the development of adventitious roots are considered to be amongst the most important developmental characteristics affecting flooding tolerance. In this study we investigated the lengths of adventitious roots and their capacity to form aerenchyma in three- and four-week-old seedlings of two maize (Zea mays ssp. mays, Linn.) inbred accessions, B64 and Na4, and one teosinte, Z. nicaraguensis Iltis & Benz (Poaceae), with and without a flooding treatment. Three weeks after sowing and following a seven day flooding treatment, both maize and teosinte seedlings formed aerenchyma in the cortex of the adventitious roots of the first three nodes. The degree of aerenchyma formation in the three genotypes increased with a second week of flooding treatment. In drained soil, the two maize accessions failed to form aerenchyma. In Z. nicaraguensis, aerenchyma developed in roots located at the first two nodes three weeks after sowing. In the fourth week, aerenchyma developed in roots of the third node, with a subsequent increase in aerenchyma in the second node roots. In a second experiment, we investigated the capacity of aerenchyma to develop in drained soil. An additional three teosinte species and 15 maize inbred lines, among them a set of flooding-tolerant maize lines, were evaluated. Evaluations indicate that accessions of Z. luxurians (Durieu & Asch. Bird) and two maize inbreds, B55 and Mo20W, form aerenchyma when not flooded. These materials may be useful genetic resources for the development of flooding-tolerant maize accessions.     

淹水玉米幼苗根尖分生细胞内Ca2+超微细胞化学定位

采用焦锑酸钾沉淀法,对遭受淹水胁迫的玉米幼苗初生根根尖分生细胞内钙离子分布变化情况进行了电镜细胞化学观察。在正常状态下,根尖分生细胞内Ca^2＋沉淀颗粒的分布较少．主要位于细胞核和细胞质中。在淹水1h后,根尖分生细胞内呈现有大量Ca^2＋沉淀颗粒分布,细胞核和细胞质中分布的Ca^2＋沉淀颗粒密度,远大于正常细胞。随着淹水时间的延长,根尖分生细胞的细胞核和细胞质中分布的Ca^2＋沉淀颗粒呈现不断增多的趋势,而液泡中分布的Ca^2＋沉淀颗粒则逐步明显减少。根据实验结果本文对受淹根尖分生细胞的死亡与Ca^2＋分布变化的关系进行了研究。     

Physiological responses of cotton to a single waterlogging at high and low N-levels

Surface-irrigated cotton (Gossypium hirsutum L.) grown on slowly draining clay soil is subjected to short-term periods of waterlogging at each irrigation which generally results in reduced productivity. The sequence of above- and below-ground plant responses to transient waterlogging and the role of N availability in modifying the immediate responses were studied. Lysimeters of Marah clay loam (a Natrustalf) were instrumented to monitor soil and plant responses to a 7-day waterlogging event beginning 67 days after sowing. Cotton (‘Deltapine 61’) plants (8 per lysimeter) were grown with two levels of added N (300 kg ha⁻¹ and 30 kg ha⁻¹) and two irrigation treatments (flooded and control). Measured soil-O₂ levels decreased rapidly upon surface flooding because water displaced air and root zone respiration consumed O₂. The rate of O₂ consumption was 2.7 times greater in the high-N treatment than the low-N treatment. This difference was associated with a 1.8 fold difference in numbers of observed roots. Root growth was only slightly affected by flooding. Leaf growth decreased by 28%, foliage temperature increased 2.3% and apparent photosynthesis decreased by 16%. It is suggested that flooding reduced photosynthetic activity within 2 days while other stress symptoms became apparent after about 6 days. Although this stress was reflected in a trend for decreased plant productivity, the effect of flooding on boll dry mass at harvest was not significant at the level of replication used. The single waterlogging did not cause yield reductions comparable to those observed elsewhere when several waterlogging events were imposed. Contribution from the CSIRO, Centre for Irrigation Research, Griffith, NSW, Australia and USDA-ARS, Morris, MI, USA, in cooperation with the univ. of Minnesota.     

根系木质素含量影响玉米耐盐性的机制研究

土壤盐度是全球农业生产的主要制约因素,对农业可持续发展和粮食安全造成严重威胁。玉米（Zea mays L.）是我国三大作物之一,而盐碱地是我国极为重要的后备耕地资源。木质素作为植物细胞壁的主要结构成分,研究玉米中木质素的积累及细胞壁增厚对高盐度的响应具有重要意义。选取耐盐玉米自交系（Zhongke4M、Zheng58）和盐敏感玉米自交系（PH4CV、Chang7-2）为研究对象,采用清水对照和200 mmol·L^-1 NaCl处理,分析不同盐浓度下玉米根系的形态变化、细胞学特征,检测相关酶活性、木质素含量和基因表达的差异。甲苯胺蓝染色结果表明,耐盐自交系Zhongke4M和Zheng58在盐胁迫下根皮层和内皮层面积的减少明显低于盐敏感玉米自交系PH4CV、Chang7-2。此外,番红荧光观察显示,耐盐自交系在盐胁迫下木质化程度增强或保持稳定,而盐敏感自交系则木质化程度下降。结果表明,耐盐自交系Zhongke4M和Zheng58在盐胁迫下木质素含量稳定,而盐敏感自交系显著降低。酶活性分析显示,盐胁迫下苯丙氨酸解氨酶（phenylalanine ammonialyase,PAL）和肉桂醇脱氢酶（cinnamyl alcohd dehydrogenase,CAD）在盐敏感自交系中活性降低,而肉桂酸4-羟化酶（cinnamic acid 4-hydroxylase,C4H）在耐盐自交系中活性上升。RNA-seq分析确定了3个与木质素合成相关的基因,其在不同玉米品种中的表达量存在差异。研究结果为深入理解玉米通过调节木质素积累和细胞壁结构应对盐胁迫提供了新视角,有助于揭示玉米的耐盐机制。     

Effect of percolation rate on nutrient kinetics and rice yield in tropical rice soils

A model is presented with which the contribution of longitudinal oxygen diffusion to total oxygen requirement of a root can be estimated. Oxygen transport in and respiration of the soil are taken into account. Given the air-filled root porosity, root diameter, coefficient of oxygen transfer between root and soil, root and soil respiration rate, and the coefficient for oxygen diffusion in the soil, the maximum length a root can attain with an adequate oxygen supply to the root tip can be calculated. Results show the importance of root porosity for root aeration, also in unsaturated soils. For thick roots (radius >0.03 cm), diffusion along the internal pathway can provide 50–75% of the total oxygen requirement even, at modest values of the root porosity.     

Adaptations of Central Amazon Tree Species to Prolonged Flooding: Root Morphology and Leaf Longevity

Abstract: Várzeas are species-rich forest communities of the Central Amazon floodplains, inhabited by highly adapted tree species that can withstand long flooding periods. The leaf shedding behaviour and morphological traits that may contribute to adaptation to low oxygen levels were studied at the Ilha de Marchantaria on the lower Solimoes-Amazonas river, Brazil, and in greenhouse experiments with cuttings of six tree species typical of the Amazon floodplain. Comparison of deciduousness in situ revealed that four of the species under investigation, Salix martiana , Tabernaemontana juruana , Laetia corymbulosa and Pouteria glomerata , are able to maintain their leaf system during the aquatic period. Adventitious roots were formed by S. martiana and T. juruana , but anatomical characteristics differed between the species. Whereas S. martiana developed lysigenous aerenchyma in its roots during aerobic and anaerobic growth, only small intercellular spaces of schizogenous origin were formed in the root cortex of T. juruana . Similar to the latter species, such spaces were constitutively formed in the deciduous species Crateva benthami and Vitex cymosa . Suberin deposits were observed in tangential and radial cell walls of the hypodermis of roots from T. juruana , L. corymbulosa and P. glomerata . Suberin deposits were less pronounced in roots of S. martiana and absent in V. cymosa and C. benthami . The data show that different, almost contrasting, survival mechanisms have evolved in roots of plants with similar life forms in the same habitat. The results further suggest that the morphological traits of the investigated trees are causally linked with the in situ leaf shedding behaviour.     

Oxygen dynamics in submerged rice (Oryza sativa)

Complete submergence of plants prevents direct O(2) and CO(2) exchange with air. Underwater photosynthesis can result in marked diurnal changes in O(2) supply to submerged plants. Dynamics in pO(2) had not been measured directly for submerged rice (Oryza sativa), but in an earlier study, radial O(2) loss from roots showed an initial peak following shoot illumination. O(2) dynamics in shoots and roots of submerged rice were monitored during light and dark periods, using O(2) microelectrodes. Tissue sugar concentrations were also measured. On illumination of shoots of submerged rice, pO(2) increased rapidly and then declined slightly to a new quasi-steady state. An initial peak was evident first in the shoots and then in the roots, and was still observed when 20 mol m(-3) glucose was added to the medium to ensure substrate supply in roots. At the new quasi-steady state following illumination, sheath pO(2) was one order of magnitude higher than in darkness, enhancing also pO(2) in roots. The initial peak in pO(2) following illumination of submerged rice was likely to result from high initial rates of net photosynthesis, fuelled by CO(2) accumulated during the dark period. Nevertheless, since sugars decline with time in submerged rice, substrate limitation of respiration could also contribute to morning peaks in pO(2) after longer periods of submergence.     

Sources of plant-derived carbon and stability of organic matter in soil: implications for global change

Alterations in forest productivity and changes in the relative proportion of above‐ and belowground biomass may have nonlinear effects on soil organic matter (SOM) storage. To study the influence of plant litter inputs on SOM accumulation, the Detritus Input Removal and Transfer (DIRT) Experiment continuously alters above‐ and belowground plant inputs to soil by a combination of trenching, screening, and litter addition. Here, we used biogeochemical indicators [i.e., cupric oxide extractable lignin‐derived phenols and suberin/cutin‐derived substituted fatty acids (SFA)] to identify the dominant sources of plant biopolymers in SOM and various measures [i.e., soil density fractionation, laboratory incubation, and radiocarbon‐based mean residence time (MRT)] to assess the stability of SOM in two contrasting forests within the DIRT Experiment: an aggrading deciduous forest and an old‐growth coniferous forest. In the deciduous forest, removal of both above‐ and belowground inputs increased the total amount of SFA over threefold compared with the control, and shifted the SFA signature towards a root‐dominated source. Concurrently, light fraction MRT increased by 101 years and C mineralization during incubation decreased compared with the control. Together, these data suggest that root‐derived aliphatic compounds are a source of SOM with greater relative stability than leaf inputs at this site. In the coniferous forest, roots were an important source of soil lignin‐derived phenols but needle‐derived, rather than root‐derived, aliphatic compounds were preferentially preserved in soil. Fresh wood additions elevated the amount of soil C recovered as light fraction material but also elevated mineralization during incubation compared with other DIRT treatments, suggesting that not all of the added soil C is directly stabilized. Aboveground needle litter additions, which are more N‐rich than wood debris, resulted in accelerated mineralization of previously stored soil carbon. In summary, our work demonstrates that the dominant plant sources of SOM differed substantially between forest types. Furthermore, inputs to and losses from soil C pools likely will not be altered uniformly by changes in litter input rates.