The northern limit of Pinus banksiana Lamb. in Canada: explaining the difference between the eastern and western distributions

Aim Present northern distribution limit of jack pine (Pinus banksiana Lamb.) follows the northern limit of continuous open boreal forest in western Canada, but not in eastern Canada where it is located further south. We tested the hypothesis that fire plays a more important role than climate in explaining the present position of the northern distribution limit of jack pine. Location An experimental jack pine plantation was set up in 1992, c. 300 km north of the present distribution limit of the species, in the Boniface river area of northern Québec (57°43′ N, 76°05′ W). Methods Climate and fire data were used to compare sites at and north of the present distribution limit of jack pine. In 2001, surviving individuals from the plantation were measured (total height, annual shoot elongation, basal diameter, and presence/absence of cones). Results Climate data from the ten weather stations used in this study did not show major differences. The northern limit of jack pine distribution is closely associated with the occurrence of fires larger than 200 ha. Survival of the planted jack pines was 31%. About 25% of the surviving pines qualified as normal, single‐stem individuals; the others were slightly uprooted and/or showed marks of erosion or foraging. Cones were produced, although no viable seeds were found. Main conclusions The low number of degree‐days above 5 °C at the plantation site could explain why the seeds were not viable. However, such climate conditions are not sufficient to prevent growth, as was shown by annual shoot elongation measurements. Most of the surviving jack pines from the Boniface river plantation are relatively healthy and follow a normal developmental programme. Low fire frequency and small fire size are amongst the main factors that prevented P. banksiana from migrating further north or east following deglaciation in northern Québec and Labrador.     

Fire, fuels and restoration of ponderosa pine–Douglas fir forests in the Rocky Mountains, USA

Aim Forest restoration in ponderosa pine and mixed ponderosa pine–Douglas fir forests in the US Rocky Mountains has been highly influenced by a historical model of frequent, low‐severity surface fires developed for the ponderosa pine forests of the Southwestern USA. A restoration model, based on this low‐severity fire model, focuses on thinning and prescribed burning to restore historical forest structure. However, in the US Rocky Mountains, research on fire history and forest structure, and early historical reports, suggest the low‐severity model may only apply in limited geographical areas. The aim of this article is to elaborate a new variable‐severity fire model and evaluate the applicability of this model, along with the low‐severity model, for the ponderosa pine–Douglas fir forests of the Rocky Mountains. Location Rocky Mountains, USA. Methods The geographical applicability of the two fire models is evaluated using historical records, fire histories and forest age‐structure analyses. Results Historical sources and tree‐ring reconstructions document that, near or before ad 1900, the low‐severity model may apply in dry, low‐elevation settings, but that fires naturally varied in severity in most of these forests. Low‐severity fires were common, but high‐severity fires also burned thousands of hectares. Tree regeneration increased after these high‐severity fires, and often attained densities much greater than those reconstructed for Southwestern ponderosa pine forests. Main conclusions Exclusion of fire has not clearly and uniformly increased fuels or shifted the fire type from low‐ to high‐severity fires. However, logging and livestock grazing have increased tree densities and risk of high‐severity fires in some areas. Restoration is likely to be most effective which seeks to (1) restore variability of fire, (2) reverse changes brought about by livestock grazing and logging, and (3) modify these land uses so that degradation is not repeated.     

Hydrolysis of lipid and protein reserves in loblolly pine seeds in relation to protein electrophoretic patterns following imbibition

The correlation between changes in seed protein electrophoretic patterns and the hydrolysis of lipid and protein reserves of loblolly pine ( Pinus taeda L.) seed was studied. Seeds were incubated at 30°C for up to 12 days following stratification, then megagametophytes and embryos were assayed for lipid and protein content after each day of imbibition. The megagametophyte of mature seed was found to contain 20% lipid and 12% storage protein on a fresh weight basis. The embryo contained 26% lipid and 15% protein. Both lipid and protein reserves were depleted constantly following imbibition. Sodium dodecyl sulfate polyacrylamide gel electrophoresis of soluble and insoluble protein fractions showed a 60 kDa protein that was representative of crystalloid-like proteins. These crystalloid-like proteins comprised 85% of the insoluble protein storage reserves. A small number of insoluble storage proteins, including a 47 kDa protein, were distinct in that they were unaffected by 2-mercaptoethanol treatment. The soluble fractions from both tissues were labelled with [³⁵S]-methionine, and incorporation was visualized by two-dimensional electrophoresis. Proteins were found to belong to one of three categories, those synthesized constitutively (comprising the bulk of newly synthesized proteins), those synthesized during germination or those synthesized after radicle emergence. Accompanying seed reserve hydrolysis were developmental shifts in protein pattern and synthesis, suggesting the possibility that control of hydrolysis is at the level of enzyme accumulation.     

Effects of forest management intensity on carbon and nitrogen content in different soil size fractions of a North Florida Spodosol

Pine plantations of the southeastern USA are regional carbon (C) sinks. In spite of large increases in woody biomass due to advanced growing systems, studies have shown little or even negative effects on the C content of the extremely sandy soils of this region. Hence, it is important to understand the mechanisms that determine the impact of intensive forest management on soil organic carbon (SOC) sequestration. This study was conducted to examine the C profile in a 4-year-old loblolly pine (Pinus taeda L.) plantation managed under two levels of management intensity (chemical understory control and fertilizer inputs). Soil organic C and nitrogen (N) pools were evaluated using two size fractionation methods, dry and wet sieving (2000–250 μm, 250–150 μm, 150–53 μm and <53 μm). Dry sieving was preferred over wet sieving for soil size fractionation, as it preserved more structure and water-soluble SOC components such as esters and amides and did not affect the N distribution. Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS) spectra were used to examine the chemical composition of the size fractions, which showed the presence of recently added organic matter in the largest sand fraction, as well as more decomposed organic matter in the <53 μm fraction. Intensive forest management reduced SOC in all three 2000–53 μm fractions, most likely due to reduced root input of understory plants that were controlled using herbicides. The 2000–250 μm fractions contained nearly half of the total SOC and showed a 23% decrease in C content due to the intensive management regime. Results from this study indicated the significance and responsiveness of sand size SOC fractions in Florida Spodosols. Results also showed that reductions in SOC due to intensive management occurred after four years and highlighted the need to understand the long-term impacts and the mechanisms responsible. Responsible Editor: Barbara Wick     

山杨白桦混交次生林与原始阔叶红松林土壤呼吸作用比较

 比较利用静态箱式法测定长白山原始阔叶红松林(Pinus koraiensis)和次生杨桦混交林的土壤呼吸作用表明,两者土壤呼吸作用的日动态均主要受温度影响,次生林土壤呼吸作用的日变化极值出现时间较原始林提前1～2 h;两者具有明显的季节动态,其中8月土壤呼吸速率最大;在生长季,土壤呼吸速率与土壤含水量关系不显著,而与土壤5 cm温度呈显著的指数关系;生长季(5～9月)次生林土壤释放CO₂量(3 449.4 g·m^－2)约为原始林(2 674.4 g·m^－2)的1.3倍,这可能是由于次生林内具有比原始林较高的温度和较低的土壤含水量,更有利于根系生长代谢和土壤微生物的活动引起的。     

Range-wide phylogeography and gene zones in Pinus pinaster Ait. revealed by chloroplast microsatellite markers

Some 1339 trees from 48 Pinus pinaster stands were characterized by five chloroplast microsatellites, detecting a total of 103 distinct haplotypes. Frequencies for the 16 most abundant haplotypes (p(k) > 0.01) were spatially interpolated over a lattice made by 430 grid points. Fitting of spatially interpolated values on raw haplotype frequencies at the same geographical location was tested by regression analysis. A range-wide 'diversity map' based on interpolated haplotype frequencies allowed the identification of one 'hotspot' of diversity in central and southeastern Spain, and two areas of low haplotypic diversity located in the western Iberian peninsula and Morocco. Principal component analysis (PCA) carried out on haplotypes frequency surfaces allowed the construction of a colour-based 'synthetic' map of the first three PC components, enabling the detection of the main range-scale genetic trends and the identification of three main 'gene pools' for the species: (i) a 'southeastern' gene pool, including southeastern France, Italy, Corsica, Sardinia, Pantelleria and northern Africa; (ii) an 'Atlantic' gene pool, including all the western areas of the Iberian peninsula; and (iii) a 'central' gene pool, located in southeastern Spain. Multivariate and AMOVA analyses carried out on interpolated grid point frequency values revealed the existence of eight major clusters ('gene zones'), whose genetic relationships were related with the history of the species. In addition, demographic models showed more ancient expansions in the eastern and southern ranges of maritime pine probably associated to early postglacial recolonization. The delineation of the gene zones provides a baseline for designing conservation areas in this key Mediterranean pine.     

Water transfer via ectomycorrhizal fungal hyphae to conifer seedlings

Little is known about water transfer via mycorrhizal hyphae to plants, despite its potential importance in seedling establishment and plant community development, especially in arid environments. Therefore, this process was investigated in the study reported in this paper in laboratory-based tripartite mesocosms containing the shrub Arctostaphylos viscida (manzanita) and young seedlings of sugar pine (Pinus lambertiana) and Douglas-fir (Pseudotsuga menziesii). The objectives were to determine whether water could be transported through mycorrhizal symbionts shared by establishing conifers and A. viscida and to compare the results obtained using two tracers: the stable isotope deuterium and the dye lucifer yellow carbohydrazide. Water containing the tracers was added to the central compartment containing single manzanita shrubs. The fungal hyphae were then collected as well as plant roots from coniferous seedlings in the other two compartments to determine whether water was transferred via fungal hyphae. In addition, the length of the hyphae and degree of mycorrhizal colonisation were determined. Internal transcribed spacer–restriction fragment length polymorphism (ITS-RFLP) analysis was used to identify the fungal species involved in dye (water) transfer. Results of the stable isotope analysis showed that water is transferred via mycorrhizal hyphae, but isotopically labelled water was only detected in Douglas-fir roots, not in sugar pine roots. In contrast, the fluorescent dye was transported via mycorrhizal hyphae to both Douglas-fir and sugar pine seedlings. Only 1 of 15 fungal morphotypes (identified as Atheliaceae) growing in the mesocosms transferred the dye. Differences were detected in the water transfer patterns indicated by the deuterium and fluorescent dye tracers, suggesting that the two labels are transported by different mechanisms in the same hyphae and/or that different fungal taxa transfer them via different routes to host plants. We conclude that both tracers can provide information on resource transfer between fungi and plants, but we cannot be sure that the dye transfer data provide accurate indications of water transfer rates and patterns. The isotopic tracer provides more direct indications of water movement and is therefore more suitable than the dye for studying water relations of plants and their associated mycorrhizal fungi.     

Pinimenthol ointment in patients suffering from upper respiratory tract infections – A post-marketing observational study

In order to gain further experience regarding the tolerability of Pinimenthol^® ointment¹ in adolescents (⩾12 years) and adults suffering from upper respiratory tract infections, a post-marketing observational study was performed. In this study, data of 3060 patients were collected (64.9% prospectively over an individual observation period of 5–14 days, 35.1% retrospectively). The prospective documentation also comprised data concerning treatment effects.Sample size of the post-marketing observational study was calculated in the way that adverse drug reactions with an event probability of at least 1:1000 would occur within the study at least once with a probability of 95%.Most patients suffered from cold, acute or chronic bronchitis, bronchial catarrh or hoarseness. Pinimenthol^® ointment was prescribed to inunction (29.6%), inhalation (17.3%) or inunction and inhalation (53.1%), respectively. The mean duration of study participation was 8.0±3.4 days.The tolerability was rated as excellent or good by 96.7% of physicians and 95.7% of patients. A total of 22 patients (0.7%) reported adverse drug reactions which mostly affected the skin or mucus membrane and therefore correspond to the expected adverse effects profile of Pinimenthol^® ointment. The treatment effect was mostly judged as excellent or good (physicians: 88.3%; patients: 88.1%).In conclusion, the study confirms Pinimenthol^® ointment as a well tolerated therapy option for upper respiratory tract infections in both adolescents and adults.     

Interactions between soil and tree roots accelerate long-term soil carbon decomposition

Decomposition of soil organic carbon (SOC) is the main process governing the release of CO₂ into the atmosphere from terrestrial systems. Although the importance of soil–root interactions for SOC decomposition has increasingly been recognized, their long-term effect on SOC decomposition remains poorly understood. Here we provide experimental evidence for a rhizosphere priming effect, in which interactions between soil and tree roots substantially accelerate SOC decomposition. In a 395-day greenhouse study with Ponderosa pine and Fremont cottonwood trees grown in three different soils, SOC decomposition in the planted treatments was significantly greater (up to 225%) than in soil incubations alone. This rhizosphere priming effect persisted throughout the experiment, until well after initial soil disturbance, and increased with a greater amount of root-derived SOC formed during the experiment. Loss of old SOC was greater than the formation of new C, suggesting that increased C inputs from roots could result in net soil C loss.