Soil Methane Uptake Increases under Continuous Throughfall Reduction in a Temperate Evergreen,Broadleaved Eucalypt Forest

Soils in temperate forests ecosystems are the greatest terrestrial CH₄ sink globally. Global and regional circulation models predict decreased average rainfall, increased extreme rainfall events and increased temperatures for many temperate ecosystems. However, most studies of soil CH₄ uptake have only considered extended periods of drought rather than an overall decrease in rainfall amount. We measured soil CH₄ uptake from March 2010 to March 2012 after installing passive rainfall reduction systems to intercept approximately 40% of throughfall in a temperate broadleaf evergreen eucalypt forest in south-eastern Australia. Throughfall reduction caused an average reduction of 15.1 ± 6.4% (SE) in soil volumetric water content, a reduction of 19.8 ± 6.9% in soil water-filled pore space (%WFPS) and a 20.1 ± 6.8% increase in soil air-filled porosity. In response to these changes, soil CH₄ uptake increased by 54.7 ± 19.3%. The increase in soil CH₄ uptake could be explained by increased diffusivity in drier soils, whilst the activity of methanotrophs remained relatively unchanged. It is likely that soil CH₄ uptake will increase if rainfall reduces in temperate broadleaf evergreen forests of Australia as a consequence of climate change.     

广西猫儿山中山森林共生的常绿和落叶阔叶树光合特性的季节变化

研究分析了广西猫儿山中山森林中3种落叶阔叶树（亮叶水青冈Fagus lucida;青榨槭Acer davidti;缺萼枫香Lktuidambar acalycina）和4种常绿阔叶树（铁椎栲Castanopsis lainontii;曼青冈Cyclobalanopsis oxyodon;桂南木莲Manglietia chingii;银木荷Schima argentea）光合特性的季节性变化。除青榨槭外,在雨季饱和光照下,落叶树与常绿树的最大净光合速率（P-）差异不明显,而落叶树的最大气孔导度（G-）要比常绿树高;在旱季,落叶树的P-和Gmax下降幅度远大于常绿树,这伴随前者暗呼吸速率和光补偿点的大幅提高。常绿树和落叶树的表观量子效率（AQY）和凌晨光系统II潜在最大光化学效率（Fv／Fm-predawn）在雨季差异不明显;在旱季,落叶树的AQY和Fv／Fm-predawn小于常绿树,说明前者遭受较严重的光抑制。此外,光合速率与气孔导度呈显著直线相关,但常绿树的直线斜率要比落叶树大,说明前者光合水分利用效率较高,这有利于常绿植物在干旱和低温条件下生存。光合速率与电子传递速率和温度也呈显著直线相关,但常绿树的直线斜率都小于落叶树,这说明常绿植物可以调节电子传递速率的变化来适应温度的宽幅的季节性变化。总之,落叶阔叶树需要相对较高的温度和水分供应才能满足光合作用的需要,而在干旱和低温条件下,落叶阔叶树尽管可以通过气孔和光系统II的调节来适应环境的变化,但还是无法避免严重的光抑制从而导致叶片脱落;与之相反,常绿植物却可以通过气孔调节提高水分利用效率和通过电子分配耗散多余能量来适应干旱和低温的胁迫而使叶片维持四季常绿。     

Soil Nematode Responses to Increases in Nitrogen Deposition and Precipitation in a Temperate Forest

The environmental changes arising from nitrogen (N) deposition and precipitation influence soil ecological processes in forest ecosystems. However, the corresponding effects of environmental changes on soil biota are poorly known. Soil nematodes are the important bioindicator of soil environmental change, and their responses play a key role in the feedbacks of terrestrial ecosystems to climate change. Therefore, to explore the responsive mechanisms of soil biota to N deposition and precipitation, soil nematode communities were studied after 3 years of environmental changes by water and/or N addition in a temperate forest of Changbai Mountain, Northeast China. The results showed that water combined with N addition treatment decreased the total nematode abundance in the organic horizon (O), while the opposite trend was found in the mineral horizon (A). Significant reductions in the abundances of fungivores, plant-parasites and omnivores-predators were also found in the water combined with N addition treatment. The significant effect of water interacted with N on the total nematode abundance and trophic groups indicated that the impacts of N on soil nematode communities were mediated by water availability. The synergistic effect of precipitation and N deposition on soil nematode communities was stronger than each effect alone. Structural equation modeling suggested water and N additions had direct effects on soil nematode communities. The feedback of soil nematodes to water and nitrogen addition was highly sensitive and our results indicate that minimal variations in soil properties such as those caused by climate changes can lead to severe changes in soil nematode communities.     

Responses of Tree Transpiration and Growth to Seasonal Rainfall Redistribution in a Subtropical Evergreen Broad-Leaved Forest

Precipitation changes such as more frequent drought and altered precipitation seasonality may impose substantial impacts on the structure and functioning of forest ecosystems. A better understanding of tree responses to precipitation changes can provide fundamental information for the conservation and management of forests under future climate regimes. We conducted a 2-year seasonal rainfall redistribution experiment to assess the responses of tree transpiration and growth to manipulated precipitation changes in a subtropical evergreen broad-leaved forest. Three precipitation treatments were administered including a drier dry season and wetter wet season treatment (DD), an extended dry season and wetter wet season treatment (ED), and an ambient control treatment, with the total amount of annual rainfall being kept the same among the three treatments. Our results showed that the DD and ED treatments reduced daily transpiration of Schima superba by 8–16 and 13–25%, respectively. The ED treatment also reduced the DBH increment of larger S. superba individuals. In contrast, neither treatment showed obvious effects on the transpiration and DBH increment of another dominant species Michelia macclurei. However, the transpiration of both species showed clear inter-annual differences between the 2 years with contrasting annual rainfall (2094 vs 1582 mm). S. superba had a lower transpiration-to-precipitation ratio (T/P) compared to M. macclurei and showed decreased sensitivities to total solar radiation and vapor pressure deficit under the DD and ED treatments. These results indicate the deep-rooted S. superba may be suppressed with a lower ability to obtain water and assimilate carbon compared to the shallow-rooted M. macclurei under the precipitation seasonality changes, which could potentially cause shifts in species dominance within the forest community.     

Seasonal Photochemical Transformations of Nitrogen Species in a Forest Stream and Lake

The photochemical release of inorganic nitrogen from dissolved organic matter is an important source of bio-available nitrogen (N) in N-limited aquatic ecosystems. We conducted photochemical experiments and used mathematical models based on pseudo-first-order reaction kinetics to quantify the photochemical transformations of individual N species and their seasonal effects on N cycling in a mountain forest stream and lake (Plešné Lake, Czech Republic). Results from laboratory experiments on photochemical changes in N speciation were compared to measured lake N budgets. Concentrations of organic nitrogen (N_org; 40–58 µmol L⁻¹) decreased from 3 to 26% during 48-hour laboratory irradiation (an equivalent of 4–5 days of natural solar insolation) due to photochemical mineralization to ammonium (NH₄ ⁺) and other N forms (N_x; possibly N oxides and N₂). In addition to N_org mineralization, N_x also originated from photochemical nitrate (NO₃ ⁻) reduction. Laboratory exposure of a first-order forest stream water samples showed a high amount of seasonality, with the maximum rates of N_org mineralization and NH₄ ⁺ production in winter and spring, and the maximum NO₃ ⁻ reduction occurring in summer. These photochemical changes could have an ecologically significant effect on NH₄ ⁺ concentrations in streams (doubling their terrestrial fluxes from soils) and on concentrations of dissolved N_org in the lake. In contrast, photochemical reactions reduced NO₃ ⁻ fluxes by a negligible (<1%) amount and had a negligible effect on the aquatic cycle of this N form.     

The Inhibitory Effects of Nitrogen Deposition on Asymbiotic Nitrogen Fixation are Divergent Between a Tropical and a Temperate Forest

Ecosystems - Asymbiotic nitrogen (N) fixation (ANF) is an important source of N in pristine forests and is predicted to decrease with N deposition. Previous studies revealing N fixation in response...     

Landscape-Scale Implications of the Edge Effect on Soil Fauna Activity in a Temperate Forest

Although studies on edge effects on species richness and abundance are numerous, the responses of ecosystem processes to these effects have received considerably less attention. How ecosystem processes respond to edge effects is particularly important in temperate forests, where small fragments and edge habitats form a considerable proportion of the total forest area. Soil fauna are key contributors to decomposition and soil biogeochemical cycling processes. Using the bait lamina technique, we quantified soil fauna feeding activity, and its dependence on soil moisture and distance to the edge in a broad-leaved forest in Southern England. Feeding activity was 40% lower at the forest edge than in the interior, and the depth of edge influence was approximately 75 m. A watering treatment showed that moisture limitation was the main driver of the reduced feeding activity at the edge. In England, only 33% of the forest area is greater than 75 m from the edge. Therefore, assuming that the results from this single-site study are representative for the landscape, it implies that only one- third of the forest area in England supports activity levels typical for the forest core, and that edge effects reduce the mean feeding activity across the landscape by 17% (with lower and upper 90% confidence intervals of 1.3 and 23%, respectively). Changing climatic conditions, such as summer droughts may exacerbate such effects as edges lose water faster than the forest interior. The results highlight the importance of taking edge effects into account in ecological studies and forest management planning in highly fragmented landscapes.     

武夷山常绿阔叶林土壤微生物多样性的季节动态

为了解武夷山自然保护区常绿阔叶林土壤微生物群落特征和季节变化,采用Illumina Miseq高通量测序技术分析了土壤微生物多样性的季节响应。结果表明,武夷山常绿阔叶林土壤为典型的南方酸性土壤,有效钾、土壤温度四季内存在显著差异,其他理化指标均无显著差异。土壤中的微生物多样性比较丰富,已鉴定出23门206属细菌和2门17属的古菌。夏季反映细菌总数的Chao指数最高,但反映细菌多样性的Shannon指数比春季低0.21,夏季古菌的Chao指数和Shannon指数分别比冬季高21.7%和0.27%。4个季节共有的细菌和古菌分别占总数的83.1%和70.0%,说明武夷山常绿阔叶林土壤不同季节的核心微生物组成具有很好的稳定性。在门和属水平的聚类树分析表明,春季和冬季的细菌和古菌群落组成最为接近,而夏季与其他3个季节的差异最大。冗余分析和热图分析结果表明,土壤p H是决定和影响细菌和古菌多样性的主要环境因子,有效钾、有效碳和总氮对微生物群落组成均有很大的影响。因此,随季节变化武夷山常绿阔叶林土壤微生物多样性呈现出规律性变化。     

Precipitation Pattern Regulates Soil Carbon Flux Responses to Nitrogen Addition in a Temperate Forest

Ecosystems - Changes in precipitation frequency and intensity are predicted to be more intense and frequent accompanying climate change and may have immediate or potentially prolonged effects on...     

Nitrogen Fixation and Nitrogen Assimilation in a Temperate Saline Ecosystem

As nitrogen is known to be a limiting factor for plant growth, we were interested in the relationship between soil microbial activity and the nitrogen assimilation of 5 different halophytes from 4 saline sites near the lake “Neusiedlersee”, Austria. The following were studied between May and October 1985: nitrogen fixation (¹⁵N₂ and acetylene reduction): N-mineralization; several soil characteristics and in vivo nitrate reductase activity of roots and shoots of these plants. NO^?₃, org. N- and carboxylate contents of both roots and shoots, as well as the effect of NO^?₃-fertilization on the amounts of these substances, were determined on plants growing in the field during a 3-day period in September 1985. Fertilization led to a decrease in acetylene reduction activity at most sites, and an increase in the nitrate reductase activity of the shoots of all plants. Overall, carboxylate and organic nitrogen contents of these halophytes did not change in response to fertilization. Only in the roots of Aster tripolium and Atriplex hastata was there a marked increase in the nitrate reductase activity in response to fertilization. Species growing at the same site, such as Plantago maritima and Lepidium crassifolium showed contrasting levels of assimilatory activity. Apparent low rates of ammonification and nitrification were detected in soils from the 4 sites. The results are discussed in relation to the nitrogen and carbon economies of the microorganisms and plants.     

模拟降水分配季节变化对南亚热带常绿阔叶林凋落物的影响

为探讨降水季节分配的变化对南亚热带常绿阔叶林凋落物的影响,在广东省鹤山国家野外生态观测站模拟干季更干(DD)和延长干季(ED)的野外降水控制实验,对森林生态系统中凋落物变化进行了分析研究。结果表明,该试验林年凋落物总量为9.24 t hm–2,在不同时期均以叶凋落物为主,约占50.7%~69.3%。DD处理显著减少了干季(10–3月)叶凋落物量(P0.01)。虽然DD处理下全年总凋落物量比对照降低了10.3%,但差异不显著。ED处理也减少了春季(4–5月)的叶和花果及总凋落物量,全年总凋落物量则比对照增加了11.3%,但ED处理对春季和全年凋落物量的影响均差异不显著。两种干旱处理对凋落物叶质量总体上影响不明显,但DD处理显著减小了火力楠(Michelia macclurei)凋落叶的木质素含量。因此,降水格局的变化可能会影响南亚热带森林土壤的碳汇能力。     

Nitrogen Fixation in the Canopy of Temperate Forest Trees: A Re-examination

¹⁵N₂ studies and acetylene reduction assays of leaves and shootsof Douglas fir and other forest trees do not confirm previousreports that extensive nitrogen fixation occurs on leaf surfacesand it is concluded that the importance of nitrogen fixationin the canopy of forest trees has been exaggerated. The presenceof nitrogen-fixing bacteria on the leaves of trees is confirmed,however, and they have been identified as Enterobacter agglomerans,Clostridium butyricum and Bacillus sp. Their distribution onleaves is fortuitous since dead oak leaves and artificial leavesbecome colonized to the same extent as living oak leaves. nitrogen fixation, acetylene reduction, Enterobacter agglomerans, Clostridium butyricum, Bacillus sp, Douglas fir, Pseudotsuga menziensii, larch, Larix x oak, Quercus petraea.     

氮添加对温带森林细根长期分解的影响

细根分解是森林生态系统碳循环的重要过程之一,其分解速率受到大气氮沉降增加的潜在影响。利用长期模拟氮沉降样地（2009年至今）,采用凋落物分解袋方法,研究了氮添加对温带常见的5个森林树种长期细根分解的影响。结果表明：细根分解呈现先快后慢的趋势,在分解第516天质量损失达30%~50%,之后质量残留率变化较为平缓。总体上,渐近线分解模型可以更准确的反应各处理细根分解速率。氮添加对细根分解具有阶段性影响,分解前期促进细根分解,分解后期抑制分解。在细根分解后期氮添加减缓分解速率,一方面是因为木质素等较难分解的物质所占比例升高所带来的直接影响,另一方面,是因为氮添加改变了微生物活动所带来的间接影响。     

Temporal Changes in the Ectomycorrhizal Community in Two Soil Horizons of a Temperate Oak Forest

The species structure of an ectomycorrhizal (ECM) community was assessed monthly for 15 months in the two horizons (A1 and A2) of an oak temperate forest in northeastern France. Ectomycorrhizal species were identified each month by internal transcribed spacer sequencing. Seventy-five fungal symbionts were identified. The community was dominated by Tomentellaceae, Russulaceae, Cortinariaceae, and Boletales. Four species are abundant in the study site: Lactarius quietus, Tomentella sublilacina, Cenococcum geophilum, and Russula sp1. The relative abundance of each species varied depending on the soil horizon and over time. Some species, such as L. quietus, were present in the A1 and A2 horizons. C. geophilum was located particularly in the A2 horizon, whereas T. sublilacina was more abundant in A1. Some species, such as Clavulina sp., were detected in winter, while T. sublilacina and L. quietus were present all year long. Our results support the hypothesis that a rapid turnover of species composition of the ECM community occurs over the course of a month. The spatial and temporal unequal distribution of ECM species could be explained by their ecological preferences, driven by such factors as root longevity, competition for resources, and resistance to environmental variability.     

Seasonal Dynamics of Nitrogenous Compounds in a Nitrophilic Weed I. Changes in Inorganic and Organic Nitrogen Fractions of the Different Plant Parts of Urtica dioica

The seasonal dynamics of nitrogenous compounds in the differentplant parts of Urtica diocia, a perennial nitrophilic weed,were investigated under natural conditions during the courseof a year. In the below ground plant parts (roots and rhizomes)a nitrogen store was built up during summer and autumn, consistingmainly of free amino acids. In the seeds, however, proteinswere of major importance as nitrogen reserve. In early springthe below ground nitrogen store was quickly mobilized, translocatedto the upper plant parts and used for the protein synthesisof the shoots, enabling them a rapid growth prior to the developmentof their own capacity for nitrogen assimilation. (Received September 3, 1984; Accepted November 2, 1984)     

Methane Consumption in Temperate and Subarctic Forest Soils: Rates, Vertical Zonation, and Responses to Water and Nitrogen

Rates of methane consumption were measured in subarctic coniferous and temperate mixed-hardwood forest soils, using static chambers and intact soil cores. Rates at both sites were generally between 1 and 3 mg of CH₄ m^-2 day^-1 and decreased with increasing soil water contents above 20%. Addition of ammonium (1 μmol g of soil^-1) strongly inhibited methane oxidation in the subarctic soils; a lesser inhibition was observed for temperate forest samples. The response to nitrogen additions occurred within a few hours and was probably due to physiological changes in the active methane-consuming populations. Methane consumption in soils from both sites was stratified vertically, with a pronounced subsurface maximum. This maximum was coincident with low levels of both nitrate and ammonium in the mixed-hardwood forest soil.     

Seasonal Energetic Stress in a Tropical Forest Primate: Proximate Causes and Evolutionary Implications

Animals facing seasonal variation in food availability experience selective pressures that favor behavioral adjustments such as migration, changes in activity, or shifts in diet. Eclectic omnivores such as many primates can process low-quality fallback food when preferred food is unavailable. Such dietary flexibility, however, may be insufficient to eliminate constraints on reproduction even for species that live in relatively permissive environments, such as moist tropical forests. Focusing on a forest-dwelling primate with a flexible diet (Cercopithecus mitis) we investigated whether females experience seasonal energetic stress and how it may relate to reproductive seasonality. We used fecal glucocorticoids (fGCs) as an indicator of energetic stress, controlling for the potentially confounding effects of social interactions and reproductive state. We modeled within-female fGC variation with General Linear Mixed Models, evaluating changes in feeding behavior and food availability as main effects. Regardless of reproductive state, fGCs increased when females shifted their diet towards fallback foods (mature leaves and other non-preferred items) and when they spent more time feeding, while fGCs decreased with feeding time on preferred items (insects, fruits, young leaves) and with the availability of young leaves. Changes in fruit availability had no general effects on fGCs, likely because fruits were sought out regardless of availability. As predicted, females in the energetically demanding stages of late pregnancy and early lactation showed greater increases in fGCs between periods of low versus high availability of fruits and young leaves than females in other reproductive states. Potential social stressors had no measurable effects on fGCs. Preliminary evidence suggests that seasonal energetic stress may affect the timing of infant independence from mothers and contribute to unusually long inter-birth intervals compared to closely related species of similar body size. Our findings highlight how the study of stress responses can provide insights into the proximate control of reproductive strategies.     

Seasonal Changes of Nitrogen Storage Compounds in a Rhizomatous Grass Calamagrostis epigeios

The seasonal dynamics in content and distribution of N-rich compounds between overwintering organs of Calamagrostis epigeios were examined. Samples were taken both from plants grown in natural conditions and in containers with controlled nutrient supply. There were significant changes in content of nitrate, free amino acids and soluble protein in all investigated plant parts during the course of a year. Amino acids showed both the highest maximum and seasonal fluctuation among the all N compounds observed and, therefore, appear to have a central role in N storage. Their content rises in the autumn, remains stable during winter and declines quickly at the beginning of spring. The most abundant amino acids in the end of winter storage period - asparagine, arginine and glutamine - constituted about 90 % of N in fraction of free amino acids. The portion of N stored in soluble proteins, however, was considerably smaller compare to both amino acids and nitrate. The amount of N stored in rhizomes of C. epigeios was smaller than in roots and stubble base before the onset of spring re-growth. This indicates that roots and stubble base are particularly important for winter N storage in this species.     

Ecological life history of Polymnia canadensis,a monocarpic species of the North American Temperate Deciduous Forest: Demography

A demographic investigation was conducted to assess variation in life history of Polymnia canadensis (Asteraceae), a geographically-widespread, herbaceous species of deciduous forests in eastern North America. During 1985-1994, 23,063 seedlings of P. canadensis were monitored at five central Kentucky study sites. Numbers at the end were: biennials, 554; triennials, 142; winter annuals, 16; monocarpic perennials, 2; tricarpic perennials (three years), 3; and dicarpic perennials (some skipped years) that matured in the first year of life, 23; in the second year, 60; and in the third year, 9. Weekly cohorts of P. canadensis generally exhibited Deevey Type III survivorship with highest seedling mortality in summer associated with low soil moisture. Wide spatial variation in life history was displayed by the fact that fall germination cohorts at dry sites generally had greater germination and survivorship than at mesic sites during seedling establishment, while the reverse was true for spring cohorts. This led to more reproductive individuals in fall germination cohorts than spring cohorts at dry sites and generally the opposite case at mesic sites. Forest shade in mesic sites caused slower growth and a greater frequency of longer-lived reproductive individuals than in open, dry sites, but it also resulted in higher survivorship than at dry sites during moderate drought. Annual population growth rate averaged across four years was not significantly different between a dry site and mesic site, indicating that despite forest shade, P. canadensis persisted in the mesic site as well as it did in the dry site. Population structure varied among years, seasons, and study sites; at two study plots, a 2-year flowering cycle of mass seeding and senescence persisted for 4 years. At a smaller scale, there was little difference in survivorship between study plots within sites or between quadrats within study plots, while in a few instances there were large differences in the number of reproductive individuals. Weekly cohorts that germinated early within seasonal cohorts had greater number of reproductive individuals than later weekly cohorts, but not consistently greater survivorship. Several droughts induced temporal variation that was as important as spatial variation. During these droughts, the population size of all cohorts that germinated prior to the droughts declined to zero at all sites, and biennials were the longest lived type of reproductive individuals. During drought, Deevey Type I survivorship was prevalent, and lack of seed rain led to dependence on persistent seed banks for recruitment in some seasonal cohorts.     

Net Primary Production and Canopy Nitrogen in a Temperate Forest Landscape: An Analysis Using Imaging Spectroscopy, Modeling and Field Data

Understanding spatial patterns of net primary production (NPP) is central to the study of terrestrial ecosystems, but efforts are frequently hampered by a lack of spatial information regarding factors such as nitrogen availability and site history. Here, we examined the degree to which canopy nitrogen can serve as an indicator of patterns of NPP at the Bartlett Experimental Forest in New Hampshire by linking canopy nitrogen estimates from two high spectral resolution remote sensing instruments with field measurements and an ecosystem model. Predicted NPP across the study area ranged from less than 700 g m⁻² year⁻¹ to greater than 1300 g m⁻² year⁻¹ with a mean of 951 g m⁻² year⁻¹. Spatial patterns corresponded with elevation, species composition and historical forest management, all of which were reflected in patterns of canopy nitrogen. The relationship between production and elevation was nonlinear, with an increase from low- to mid-elevation deciduous stands, followed by a decline in upper-elevation areas dominated by evergreens. This pattern was also evident in field measurements and mirrored an elevational trend in foliar N concentrations. The increase in production from low-to mid-elevation deciduous stands runs counter to the generally accepted pattern for the northeastern U.S. region, and suggests an importance of moisture limitations in lower-elevation forests. Field measurements of foliar N, wood production and leaf litterfall were also used to evaluate sources of error in model estimates and to determine how predictions are affected by different methods of acquiring foliar N input data. The accuracy of predictions generated from remotely sensed foliar N approached that of predictions driven by field-measured foliar N. Predictions based on the more common approach of using aggregated foliar N for individual cover types showed reasonable agreement in terms of the overall mean, but were in poor agreement on a plot-by-plot basis. Collectively, these results suggest that variation in foliar N exerts an important control on landscape-level spatial patterns and can serve as an integrator of other underlying factors that influence forest growth rates.