Relationships of reproductive performance indicators in black rhinoceros (Diceros bicornis michaeli) with plant available moisture,plant available nutrients and woody cover

Plant available moisture and plant available nutrients in soils influence forage quality and availability and subsequently affect reproductive performance in herbivores. However, the relationship of soil moisture, soil nutrients and woody forage with reproductive performance indicators is not well understood in mega‐browsers yet these three are important in selecting suitable areas for conservation of mega‐browsers. Here, the eastern black rhinoceros (Diceros bicornis michaeli), a mega‐browser, was studied in seven geographically distinct populations in Kenya to understand the relationships between its reproductive performance indicators and plant available moisture, plant available nutrients and woody cover. Reproductive parameters showed a complex relationship with plant available moisture and plant available nutrients. We found an increase in the predicted yearly percentage of females calving as plant available nutrients decreased in areas of high levels of plant available moisture but no relationship with plant available nutrients in areas of low plant available moisture. Age at first calving was earlier, inter‐calving interval was longer and yearly percentage of females calving was higher at higher woody cover. Woody plant cover contributes positively to black rhino reproduction performance indicators, whereas plant available moisture and plant available nutrients add to the selection of conservation areas, in more subtle ways.     

Gaseous fluxes of peroxyacetyl nitrate (PAN) into plant leaves

Peroxyactyl nitrate (PAN) is the most abundant of the gaseous organic nitrates produced from the photochemistry of hydrocarbons and NO_x (i.e. ozone and smog production). PAN is known to be toxic to plants and also as a reservoir for the transport nitrogen dioxide in the troposphere. Here, the effect of vegetation on PAN deposition was investigated in four plant species by measuring leaf fluxes of PAN in a dynamic leaf chamber using atmospheric PAN fumigations between 0.7 and 18 nmol mol^?1. A linear relationship was observed between PAN flux and ambient PAN mixing ratio for all species. Depending on the species, measured PAN flux varied between 11 and 24 pmol m^?2 s^?1. Measured fluxes of PAN accounted for 12–48% of the PAN flux predicted solely from modelled stomatal conductance to PAN, suggesting the presence of a mesophyllic resistance to PAN uptake. The brief (approximately 5–10 min) exposure to PAN during uptake measurements did not affect photosynthesis, transpiration or conductance to water vapour. Increasing stomatal resistance by varying the vapour pressure gradient between the leaf chamber and leaf internal air space led to a corresponding drop in PAN uptake. Varying leaf nitrogen and total leaf–ascorbate concentrations did not appear to influence PAN uptake as had been reported for other reactive odd‐nitrogen gases. Measured and model‐predicted PAN fluxes were offset, but correlated suggesting that PAN flux could be estimated using established stomatal conductance algorithms.     

Nutrient enrichment increases plant biomass and exotic plant proportional cover independent of warming in freshwater wetland communities

Anthropogenic environmental change can increase exotic species performance and reduce native biodiversity. Nutrient enrichment may favor exotic plants with higher growth rates. Warming may increase the performance of exotic species from warmer native ranges and/or decrease the performance of locally adapted native species. However, community level impacts of nutrient enrichment and warming may depend on their combined effects on individual species and species interactions. We conducted a factorial 11-month field experiment that manipulated 1) plant origin: native, exotic (species from warmer and nutrient rich habitats), or native-&-exotic; 2) nutrients: ambient or high; and 3) temperature: ambient, +1 °C, or +2 °C. Elevated nutrients increased biomass and exotic plant proportional cover. Exotic diversity was higher with elevated nutrients. Native and exotic biomass responses to elevated nutrients were smaller in native-&-exotic treatments. Elevated nutrients increased the relative abundance of two exotic and decreased one exotic and three native species in native-&-exotic treatments. The predicted exotic to native biomass ratio was higher than the observed ratio, indicating that native plants reduced the potential growth of exotic plants in native-&-exotic treatments. Warming had no effect on plant biomass or diversity. These results suggest that nutrient enrichment increases the performance of some exotic plants and that it is critical to consider native and exotic plant interactions when assessing anthropogenic factor and exotic plant effects on native plant communities.     

不同放牧强度草原休牧后土壤养分和植物群落变化特征

在内蒙古典型草原,对不同放牧率草地休牧3a后的土壤养分空间异质性和植物群落的数量变化特征进行了研究,结果表明：不同放牧率草地休牧3a后,由于维持土壤养分或植被空间格局的匀质化条件消失,土壤养分的空间异质性呈不同程度的增大趋势,随机性因素所占比例增加,其中土壤有机碳、全氮、无机氮、有效磷和有效硫的空间异质性均以0．00羊/hm^2区最大,4．00羊／hm^2区（中牧区）最小,其它样地不同土壤养分指标表现不同的变化特征;群落生物量和群落盖度均表现增加趋势,但群落盖度增加不显著（P〉0．05）,与1998年相比,群落生物量除对照区外均达到了显著性差异（P〈0．05）,与1．33羊／hm^2、4．00羊／hm^2和6．67羊／hm^2相比,O．00羊／hm^2优势植物出现多样化特征;群落的灌丛化与牧压和恢复演替的时间序列高度相关,牧压越小,恢复演替的时间序列越大,群落灌丛化的趋势越明显;1年生植物、羊草、克氏针茅、木地肤、冷蒿（除6．67羊／hm^2）和扁蓿豆（除O．00羊／hm^2）均表现增加趋势,星毛委陵菜则均表现降低趋势;植物群落的生物量、群落高度、群落盖度和群落物种多样性与土壤养分分布均表现一致的正相关关系,但只有植物群落生物量和群落高度与土壤有机碳、全氮、无机氮、土壤有效磷和有效硫相关显著（P〈0．05）。     

Multiple trade‐offs regulate the effects of woody plant removal on biodiversity and ecosystem functions in global rangelands

Woody plant encroachment is a major land management issue. Woody removal often aims to restore the original grassy ecosystem, but few studies have assessed the role of woody removal on ecosystem functions and biodiversity at global scales. We collected data from 140 global studies and evaluated how different woody plant removal methods affected biodiversity (plant and animal diversity) and ecosystem functions (plant production, hydrological function, soil carbon) across global rangelands. Our results indicate that the impact of removal is strongly context dependent, varying with the specific response variable, removal method, and traits of the target species. Over all treatments, woody plant removal increased grass biomass and total groundstorey diversity. Physical and chemical removal methods increased grass biomass and total groundstorey biomass (i.e., non‐woody plants, including grass biomass), but burning reduced animal diversity. The impact of different treatment methods declined with time since removal, particularly for total groundstorey biomass. Removing pyramid‐shaped woody plants increased total groundstorey biomass and hydrological function but reduced total groundstorey diversity. Environmental context (e.g., aridity and soil texture) indirectly controlled the effect of removal on biomass and biodiversity by influencing plant traits such as plant shape, allelopathic, or roots types. Our study demonstrates that a one‐size‐fits‐all approach to woody plant removal is not appropriate, and that consideration of woody plant identity, removal method, and environmental context is critical for optimizing removal outcomes. Applying this knowledge is fundamental for maintaining diverse and functional rangeland ecosystems as we move toward a drier and more variable climate.     

What controls plant nutrient use in high elevation ecosystems?

The importance of rock-derived mineral nutrients (P, K, Mn, Mg, and Ca) in plant physiological function is well established. However, one important and relatively unexplored question is whether or not the same rules of plant nutrient use efficiency apply to these essential elements even if they are not limiting to primary production. We examined conifer growth and nutrient use dynamics across sites with contrasting geologies (sedimentary and volcanic) that vary in both rock-derived mineral nutrient and N availability. Differences in bedrock geochemistry generally corresponded to differences in available soil nutrients, such that the volcanic site tended to have greater available nutrients. Foliar nutrient concentrations reflected both differences in bedrock chemistry and indices of available soil nutrients for P, K, and Mn. Aboveground biomass production did not follow expected patterns and was greater for trees growing on low nutrient sites, but only with respect to the annual woody increment. Fine litter production did not differ between sites. Finally, we found evidence for trade-offs between two commonly examined components of nutrient use efficiency (NUE): nutrient productivity (A _n) and mean residence time of nutrients. However, we did not find evidence for higher plant NUE in soils with lower nutrient availability for N or rock-derived nutrients.     

The effects of temporal variation in soil carbon inputs on resource allocation in an annual plant

Aims Resource allocation in plants can be strongly affected by competition. Besides plant–plant interactions, terrestrial plants compete with the soil bacterial community over nutrients. Since the bacterial communities cannot synthesize their own energy sources, they are dependent on external carbon sources. Unlike the effect of overall amounts of carbon (added to the soil) on plant performance, the effect of fine scale temporal variation in soil carbon inputs on the bacterial biomass and its cascading effects on plant growth are largely unknown. We hypothesize that continuous carbon supply (small temporal variance) will result in a relatively constant bacterial biomass that will effectively compete with plants for nutrients. On the other hand, carbon pulses (large temporal variance) are expected to cause oscillations in bacterial biomass, enabling plants temporal escape from competition and possibly enabling increased growth. We thus predicted that continuous carbon supply would increase root allocation at the expense of decreased reproductive output. We also expected this effect to be noticeable only when sufficient nutrients were present in the soil.Methods Wheat plants were grown for 64 days in pots containing either sterilized or inoculated soils, with or without slow-release fertilizer, subjected to one of the following six carbon treatments: daily (1.5mg glucose), every other day (3mg glucose), 4 days (6mg glucose), 8 days (12mg glucose), 16 days (24mg glucose) and no carbon control.Important findings Remarkably, carbon pulses (every 2–16 days) led to increased reproductive allocation at the expense of decreased root allocation in plants growing in inoculated soils. Consistent with our prediction, these effects were noticeable only when sufficient nutrients were present in the soil. Furthermore, soil inoculation in plants subjected to low nutrient availability resulted in decreased total plant biomass. We interpret this to mean that when the amount of available nutrients is low, these nutrients are mainly used by the bacterial community. Our results show that temporal variation in soil carbon inputs may play an important role in aboveground–belowground interactions, affecting plant resource allocation.     

The use of sewage sludge and horticultural waste to develop artificial soil for plant cultivation in Singapore

Greenhouse pot experiments were performed with Ipomoea aquatica (Kang Kong) to evaluate artificial soil produced from poor fertility subsoil, horticultural compost, and sewage sludge. The addition of horticultural compost and sewage sludge to subsoil substantially improved plant growth, improved the physical properties of subsoil and enriched subsoil by essential nutrients for plants. The effect was enhanced when the two ingredients were added to subsoil together. The highest yield of biomass of I. aquatica was observed in artificial soil prepared by mixing subsoil with 4% (wet weight/wet weight) of horticultural compost and 2% (dry weight/wet weight) of sewage sludge. The contents of heavy metals in plants, grown in the artificial soil, were significantly lower than toxic levels. The artificial soil could be recommended for urban landscaping and gardening in Singapore.     

Spatial variation in vegetation structure coupled to plant available water determined by two-dimensional soil resistivity profiling in a Brazilian savanna

Tropical savannas commonly exhibit large spatial heterogeneity in vegetation structure. Fine-scale patterns of soil moisture, particularly in the deeper soil layers, have not been well investigated as factors possibly influencing vegetation patterns in savannas. Here we investigate the role of soil water availability and heterogeneity related to vegetation structure in an area of the Brazilian savanna (Cerrado). Our objective was to determine whether horizontal spatial variations of soil water are coupled with patterns of vegetation structure across tens of meters. We applied a novel methodological approach to convert soil electrical resistivity measurements along three 275-m transects to volumetric water content and then to estimates of plant available water (PAW). Structural attributes of the woody vegetation, including plant position, height, basal circumference, crown dimensions, and leaf area index, were surveyed within twenty-two 100-m² plots along the same transects, where no obvious vegetation gradients had been apparent. Spatial heterogeneity was evaluated through measurements of spatial autocorrelation in both PAW and vegetation structure. Comparisons with null models suggest that plants were randomly distributed over the transect with the greatest mean PAW and lowest PAW heterogeneity, and clustered in the driest and most heterogeneous transect. Plant density was positively related with PAW in the top 4 m of soil. The density-dependent vegetation attributes that are related to plot biomass, such as sum of tree heights per plot, exhibited spatial variation patterns that were remarkably similar to spatial variation of PAW in the top 4 m of soil. For PAW below 4 m depth, mean vegetation attributes, such as mean height, were negatively correlated with PAW, suggesting greater water uptake from the deep soil by plants of larger stature. These results are consistent with PAW heterogeneity being an important structuring factor in the plant distribution at the scale of tens of meters in this ecosystem.     

科尔沁沙地封育恢复过程中植物群落特征变化及影响因素

封育是退化沙地植被恢复与生态重建的重要措施, 理解长期处于封育状态下不同类型沙地植物群落特征变化及其影响因素有利于沙地植被恢复和生态重建。该文基于对科尔沁沙地长期封育的流动沙丘(2005年封育)、固定沙丘(1985年封育)和沙质草地(1997年封育)连续多年(2005-2017年)的植物群落调查, 结合土壤种子库、土壤养分以及气象数据, 分析了植物群落特征变化及其对环境变化的响应。研究结果表明流动沙丘植被盖度显著增加, 群落生物量和物种多样性年际间波动变化, 但无明显趋势; 固定沙丘植物群落存在逆行演替趋势, 具体表现为群落生物量、灌木和半灌木以及豆科优势度显著下降, 而一年生和多年生杂类草优势度显著增加; 沙质草地群落物种丰富度和多年生禾草优势度存在降低趋势, 并且一年生杂类草优势度明显高于其他功能群, 群落存在退化现象。3类沙地土壤种子密度变化不显著, 而种子丰富度在流动沙丘显著增加, 在固定沙丘和沙质草地有下降趋势, 土壤养分仅有有效氮和有效磷含量增加。回归分析结果表明气温和降水是影响年内生物量积累的主要因素, 但对年际间群落生物量和物种丰富度变化影响不大。除趋势对应分析结果显示土壤种子库与植物群落之间存在很高的相似性, 典型相关分析结果表明沙质草地植物群落与土壤养分紧密相关, 而固定沙丘群落主要与土壤水分紧密相关。综合以上结果可知, 封育33年的固定沙丘群落和封育21年的沙质草地群落都存在退化现象, 而封育11年的流动沙丘群落正在缓慢恢复, 因此封育年限的设定对退化沙地植被恢复至关重要, 封育时间过长不仅不利于植物群落恢复, 反而会使群落发生逆行演替, 建议封育年限的设定应综合考虑植被退化程度、土壤养分状况、土壤种子库基础以及气候条件等因素的影响。     

桉树与红锥混交对土壤养分及林下植物功能群的影响

桉树人工林对生态环境的影响一直是全球性争议的热点问题,桉树与珍贵乡土树种混交的生态环境效应备受关注。为探究桉树混交营林措施对林地土壤养分及林下植物功能群的影响,该研究以桉树纯林(PE)、桉树×红锥混交林(MEC)和红锥纯林(PCH)为对象,开展了林下植物群落及环境因子的调查测定。研究结果显示：不同林分的土壤理化性质具有显著差异,混交林的土壤pH、有效氮(AN)和有效磷(AP)含量显著高于纯林;而土壤含水量(SMC)、有机碳(SOC)、总氮(TN)含量及C∶N和C∶P在混交林中没有显著优势,并呈现PEMEC>PCH的趋势。混交林显著增加林下木本植物功能群(WFG)的物种丰富度,而PCH显著增加蕨类植物功能群(FeFG)的物种丰富度。混交林的WFG和禾草植物功能群(GFG)的重要值均显著高于红锥纯林,而红锥纯林FeFG的重要值显著高于混交林。主坐标分析结果表明,MEC与PE的林下植物功能群组成差异不显著,但与PCH的差异显著;冗余分析结果揭示了AN和AP是WFG占优势的主要影响因子,SMC、TN...     

Modelling below- and above-ground biomass for non-woody and woody plants

BACKGROUND AND AIMS: Intraspecific relationships between below- and above-ground biomass (MB and MA, respectively) have been studied extensively to evaluate environmental effects on growth and development at the level of the individual plant. However, no current theoretical model for this relationship exists for broad interspecific trends. The aims of this paper are to provide a model and to test its predictions using a recently assembled, large database (1406 data entries for 257 species). METHODS: An allometric model was derived to predict the relationship between MB and MA for non-woody and woody plants based on previously developed scaling relationships for leaf, stem and root standing biomass and annual growth rates. The predictions of this model were tested by comparing the numerical values of predicted scaling exponents (the slopes of log-log regression curves) with those observed for the database. KEY RESULTS AND CONCLUSIONS: For non-woody plants and the juveniles of woody species, the model predicts an isometric scaling relationship (i.e. MB proportional, variant MA). For woody plants, a complex scaling function is predicted. But, for a particular set of biologically reasonable conditions, the model predicts MB proportional, variant MA across woody plants. These predictions accord reasonably well with observed statistical trends when non-woody and woody plants are studied separately (n=1061 and 345 data entries, respectively). Although the reliability of regression formulas to estimate MB based on MA measurements increased with increasing plant size, estimates of MB can be as much as two orders of magnitude off, even when using regression formulas with r2 >0.90 and F >53,000.     

Tundra plant structure and production in relation to the environment

The alpine and polar climatic limit for growth of woody plants is very much dependent on the mean temperatures of the warmest three or four summer months. Tundra plants with perennating buds close to the ground are sheltered by insulating snow cover. Many tundra plants can grow at temperatures 5–10°C below 0°C and also have low optimum temperatures. Total net production of tundra plants may be as high as 900 g/m²/yr as dry weight in moist and eutrophic low alpine shrub tundra and in antarctic moss mats. The variation in tundra plant production is often observed to be greater between different stands (communities) within one locality than between localities, because of very important variation in soil moisture and nutrients between the stands. On a global scale the biomass of vascular plants increases by an order of magnitude from the climatic severe polar desert to semidesert and again from there to moist shrub tundra. The cryptogam biomass increases only 2–10 fold from polar desert to low arctic shrub tundra. To a certain limit unfavourable climatic conditions are worse to above- than to belowground plant parts. Highest root biomass compared to top (up to 20 times higher) is observed in wet monocotyledonous polar and alpine communities. In polar desert root biomass is small again, as compared to tops and also in lower latitudes and altitudes of temperate regions.Presented at he Eighth International Congress of Biometeorology, 9–14 September 1979, Shefayim, Israel.     

Plant-pollinator interactions and the assembly of plant communities

Most studies of plant community assembly have focused on how the abiotic aspects of a habitat (e.g. soil moisture or mineral composition) or direct interactions among plants in a community (e.g. competition for space or nutrients) influence which species establish and persist, but they have tended to neglect indirect interactions such as those mediated by pollinators. We address three types of plant-pollinator interactions--filtering, facilitation and competitive exclusion--and their predicted impacts on communities. The few available studies that address how pollinator-mediated interactions limit or promote plant species establishment and persistence provide support for many of these predictions. An integrated framework for understanding plant community assembly needs to incorporate abiotic and biotic interactions, including plant-pollinator and other plant-animal interactions.     

连续施用保水材料对旱作条件下土壤特性及燕麦生长的影响

以坝莜一号为材料,研究连续4a施用保水材料聚丙烯酰胺(PAM)与聚丙烯酸钾(PAM-K),对旱作农田不同土层土壤微生物量变化与相应土层土壤含水量、容重、电导率、养分及燕麦生长的影响。结果表明,旱区农田施用PAM-K和PAM的微生态效应存在时空差异,以连续施用4a效果最佳,其大小顺序表现为连续施用4a施用3a2a1a对照。连续施用4a PAM-K和PAM,0—60 cm土层土壤含水量平均增加了27.18%和34.40%;土壤容重、土壤电导率分别平均降低了2.33%和6.64%、29.50%和22.70%;相对显著增加了耕层土壤养分(有机质、碱解氮、有效磷、速效钾)含量;土壤微生物生物量碳、氮、磷增幅平均达24.11%、31.89%、46.52%和69.96%、35.21%、52.70%,尤其是连续施用4a PAM,10—20cm土层土壤微生物量氮增幅达98.95%及0—10cm、20—40cm土层土壤微生物生物量碳和土壤微生物量磷的增加最明显,增幅分别达31.13%和74.49%、62.27%和49.91%。连续施用4a PAM-K和PAM,植株鲜重、干重、株高、籽粒产量,分别增加了90.53%和146.91%、101.56%和128.13%、33.67%和76.39%、19.27%和22.40%。可见,连续多年施用PAM-K和PAM对施入层(0—20 cm)和近施入层(20—40 cm)改善效果显著;PAM对旱区土壤的适宜性优于PAM-K,可改善土壤质量,提高作物产量。     

Asynchronous fluctuation of soil microbial biomass and plant litterfall in a tropical wet forest

Carbon availability often controls soil microbial growth and there is evidence that at regional scales soil microbial biomass is positively correlated with aboveground forest litter input. We examined the influence of plant litterfall on annual variation of soil microbial biomass in control and litter-excluded plots in a tropical wet forest of Puerto Rico. We also measured soil moisture, soil temperature, and plant litterfall in these treatment plots. Aboveground plant litter input had no effect on soil microbial biomass or on its pattern of fluctuation. Monthly changes in soil microbial biomass were not synchronized with aboveground litter inputs, but rather preceeded litterfall by one month. Soil microbial biomass did not correlate with soil temperature, moisture, or rainfall. Our results suggest that changes in soil microbial biomass are not directly regulated by soil temperature, moisture, or aboveground litter input at local scales within a tropical wet forest, and there were asynchronous fluctuation between soil microbial biomass and plant litterfall. Potential mechanisms for this asynchronous fluctuation include soil microbial biomass regulation by competition for soil nutrients between microorganisms and plants, and regulation by below-ground carbon inputs associated with the annual solar and drying-rewetting cycles in tropical wet forests.     

Variation in plant species richness of different life forms along a subtropical elevation gradient in the Himalayas, east Nepal

Aim To explore the variation in species richness along a subtropical elevation gradient, and evaluate how climatic variables explain the richness of the different life forms such as trees, shrubs, climbers, herbs and ferns. Location The study was made in a subtropical to warm temperate region in the south‐eastern part of Nepal, between 100 and 1500 m above sea level (a.s.l.). Methods The number of species was counted in six plots (50 × 20 m) in each of the 15 100 m elevation bands covering the main physiognomic structures along an imaginary transect. Each species recorded was assigned to a life form. Potential evapotranspiration (PET, i.e. energy), mean annual rainfall (MAR), and their ratio (MI = moisture index) were evaluated as explanatory variables by means of generalized linear models (GLM). Each variable was tested individually, and in addition MAR and PET were used to test the water‐energy dynamics model for each life form. Results The richness of herbaceous species, including herbaceous climbers, was unrelated to any of the climate variables. PET was strongly negatively correlated with elevation, and the following relationships were found between increasing PET and richness: (i) shrubs, trees and total species (sum of all life forms) showed unimodal responses (ii) ferns decreased monotonically, and (iii) woody climbers increased monotonically. Richness of all woody groups increased monotonically with MAR and MI. The water‐energy dynamics model explained 63% of the variation in shrubs, 67% for trees and 70% for woody species combined. Main conclusions For the various herbaceous life forms (forbs, grasses, and herbaceous climbers) we found no significant statistical trends, whereas for woody life forms (trees, shrubs, and woody climbers) significant relationships were found with climate. E.M. O’Brien's macro‐scale model based on water‐energy dynamics was found to explain woody species richness at a finer scale along this elevational‐climatic gradient.     

黄土高原典型草原群落结构和土壤水分对划破的响应

划破是草原改良的基础措施之一，划破强度是划破措施的关键环节，划破对草原健康持续管理有重要意义。目前的研究主要集中在划破对植物群落结构和生产力的影响上，然而草原植物群落与土壤水分对划破强度的响应尚不清楚。在黄土高原典型草原开展不同程度的草地划破试验，探究不同划破强度（27.4%、46.3%和61.9%）对草地植物群落物种多样性、生物量和土壤水分的影响。结果表明：3个划破强度下划破带物种丰富度显著低于未划破带1-3种/m²，划破带和未划破带群落相似性分别低于整区23.85%-119.23%和44.43%-84.55%。地上生物量随物种丰富度的增加而增大，且地上生物量与Simpson指数和Shannon Weiner指数显著负相关。3个划破强度下未划破带地下生物量和总生物量分别高于划破带88.2%-134.6%、52.4%-67.8%、2.5%-16.6%和103.9%-152.9%、59.3%-75.8%、9.1%-22.6%。植物群落物种丰富度和地上生物量随划破强度的增加呈"驼峰"型曲线变化，当划破强度分别为43.7%-55.3%和43.8%-45.7%时，植物群落物种丰富度和生物量均最高。本试验阐明了划破对典型草原植物群落特征和土壤水分的作用机制，研究结果为采用划破措施实现草地培育和草原修复提供了科学依据，对保护草地生物多样性和提高生产力具有重要意义。     

CO2 enrichment accelerates successional development of an understory plant community

Aims Rising concentrations of atmospheric carbon dioxide ([CO₂]) may influence forest successional development and species composition of understory plant communities by altering biomass production of plant species of functional groups. Here, we describe how elevated [CO₂] (eCO₂) affects aboveground biomass within the understory community of a temperate deciduous forest at the Oak Ridge National Laboratory sweetgum (Liquidambar styraciflua) free-air carbon dioxide enrichment (FACE) facility in eastern Tennessee, USA. We asked if (i) CO₂ enrichment affected total understory biomass and (ii) whether total biomass responses could be explained by changes in understory species composition or changes in relative abundance of functional groups through time.Materials and Methods The FACE experiment started in 1998 with three rings receiving ambient [CO₂] (aCO₂) and two rings receiving eCO₂. From 2001 to 2003, we estimated species-specific, woody versus herbaceous and total aboveground biomass by harvesting four 1 × 0.5-m subplots within the established understory plant community in each FACE plot. In 2008, we estimated herbaceous biomass as previously but used allometric relationships to estimate woody biomass across two 5 × 5-m quadrats in each FACE plot.Important findings Across years, aboveground biomass of the understory community was on average 25% greater in eCO₂ than in aCO₂ plots. We could not detect differences in plant species composition between aCO₂ and eCO₂ treatments. However, we did observe shifts in the relative abundance of plant functional groups, which reflect important structural changes in the understory community. In 2001–03, little of the understory biomass was in woody species; herbaceous species made up 94% of the total understory biomass across [CO₂] treatments. Through time, woody species increased in importance, mostly in eCO₂, and in 2008, the contribution of herbaceous species to total understory biomass was 61% in aCO₂ and only 33% in eCO₂ treatments. Our results suggest that rising atmospheric [CO₂] could accelerate successional development and have longer term impact on forest dynamics.     

Comparative analysis of plant carbohydrate active enZymes and their role in xylogenesis

Background

Carbohydrate metabolism is a key feature of vascular plant architecture, and is of particular importance in large woody species, where lignocellulosic biomass is responsible for bearing the bulk of the stem and crown. Since Carbohydrate Active enZymes (CAZymes) in plants are responsible for the synthesis, modification and degradation of carbohydrate biopolymers, the differences in gene copy number and regulation between woody and herbaceous species have been highlighted previously. There are still many unanswered questions about the role of CAZymes in land plant evolution and the formation of wood, a strong carbohydrate sink.

Results

Here, twenty-two publically available plant genomes were used to characterize the frequency, diversity and complexity of CAZymes in plants. We find that a conserved suite of CAZymes is a feature of land plant evolution, with similar diversity and complexity regardless of growth habit and form. In addition, we compared the diversity and levels of CAZyme gene expression during wood formation in trees using mRNA-seq data from two distantly related angiosperm tree species Eucalyptus grandis and Populus trichocarpa, highlighting the major CAZyme classes involved in xylogenesis and lignocellulosic biomass production.

Conclusions

CAZyme domain ratio across embryophytes is maintained, and the diversity of CAZyme domains is similar in all land plants, regardless of woody habit. The stoichiometric conservation of gene expression in woody and non-woody tissues of Eucalyptus and Populus are indicative of gene balance preservation.

Electronic supplementary material

The online version of this article (doi:10.1186/s12864-015-1571-8) contains supplementary material, which is available to authorized users.