Carbon isotopic composition of forest soil respiration in the decade following bark beetle and stem girdling disturbances in the Rocky Mountains

Bark beetle outbreaks are widespread in western North American forests, reducing primary productivity and transpiration, leading to forest mortality across large areas and altering ecosystem carbon cycling. Here the carbon isotope composition (δ¹³C) of soil respiration (δ_J) was monitored in the decade after disturbance for forests affected naturally by mountain pine beetle infestation and artificially by stem girdling. The seasonal mean δ_J changed along both chronosequences. We found (a) enrichment of δ_J relative to controls (<1 ‰) in near‐surface soils in the first 2 years after disturbance; (b) depletion (1‰ or no change) during years 3–7; and (c) a second period of enrichment (1–2‰) in years 8–10. Results were consistent with isotopic patterns associated with the gradual death and decomposition of rhizosphere organisms, fine roots, conifer needles and woody roots and debris over the course of a decade after mortality. Finally, δ_J was progressively more ¹³C‐depleted deeper in the soil than near the surface, while the bulk soil followed the well‐established pattern of ¹³C‐enrichment at depth. Overall, differences in δ_J between mortality classes (<1‰) and soil depths (<3‰) were smaller than variability within a class or depth over a season (up to 6‰).     

Exotic pine plantations and indigenous Lepidoptera in Australia

Temperate regions of Australia have extensive commercial plantations of Monterey pine, Pinus radiata D. Don. Replacement of indigenous forests by P. radiata is likely to have significant effects on assemblages of native Lepidoptera, and has been considered a major threat to native fauna through displacing native species. However, many species of Lepidoptera, including ennomine geometrid moths in the genus Chlenias Guenèe, have adopted P. radiata as a larval host. Comparisons were made of oviposition preferences and nutritional ecology of Chlenias auctaria Guenée on P. radiata and two native host plants [Acacia mearnsii De Wild. (Mimosaceae) and Eucalyptus obliqua LHérit (Myrtaceae)]. Females showed no significant oviposition preference for any of the three hosts. Growth of sixth instar larvae was significantly less on P. radiata than on the native hosts. Pupal weights were significantly lower, suggesting that the fitness of moths reared on P. radiata will be significantly reduced. The life history strategy of C. auctaria, which includes dispersal of first instar larvae by ballooning, may predispose this species to feed on poor quality hosts, and this may be common to other polyphagous species found feeding on P. radiata in southern hemisphere plantations. The impact of P. radiata may have a long term effect on lepidopteran communities, beyond the simple replacement of indigenous host plants leading to extirpations of feeding specialists.     

加勒比松种源苗期DNA甲基化多样性分析

为了解加勒比松(Pinus caribaea)种源的遗传多样性,利用甲基化敏感扩增多态性技术对加勒比松3个变种17个种源的DNA甲基化多样性进行了研究。结果表明,56对引物组合共扩增出425条谱带,其中多态性谱带422条,多态性百分率为99.25%。加勒比松种源幼苗半甲基化比率比全甲基化比率稍高,洪都拉斯加勒比松、古巴加勒比松和巴哈马加勒比松的DNA甲基化率分别为22.39%、22.29%和22.35%,差异不显著。加勒比松的DNA序列遗传多样性(H=0.4376)高于DNA甲基化多样性(H=0.3274),Mantel检验表明,基因组遗传变异与表观遗传变异不存在相关性(r=-0.171,P=0.16)。表观聚类与遗传聚类间存在较大差异,两种聚类分析结果均未将3个加勒比松变种分开。这表明加勒比松变种间的表观遗传变异极为丰富,能为加勒比松遗传改良提供优良种质资源。     

Different effects of supplied ammonium on glutamine synthetase activity in mustard (Sinapis alba) and pine (Pinus sylvestris) seedlings

The activity of glutamine synthetase (GS) in mustard ( Sinapis alba L.) and Scots pine ( Pinus sylvestris L.) seedlings was used as an index to evaluate the capacity to cope with excessive ammonium supply. In these 2 species GS activity was differently affected by the application of nitrogen compounds (NH₄⁺ or NO₃⁻). Mustard seedlings older than 5 days showed a considerable increase in GS activity after NH₄⁺ or NO₃⁻ application. This response was independent of the energy flux, but GS activity in general was positively affected by light. Endogenous NH₄⁺ did not accumulate greatly after nitrogen supply. In contrast, seedlings of Scots pine accumulated NH₄⁺ in cotyledons and roots and showed no stimulation of GS activity after the application of ammonium. In addition, root growth was drastically reduced. Thus, the pine seedlings seem to have insufficient capacity to assimilate exogenously supplied ammonium. NO₃⁻, however, did not lead to any harmful effects.     

阔叶红松混交林林隙内丘坑复合体特征及分布格局

对小兴安岭凉水国家级自然保护区红松阔叶混交林不同大小林隙及郁闭林分内丘坑复合体特征及分布格局进行了对比和分析.结果表明： 大、中、小林隙及郁闭林分中丘坑复合体的丘宽、丘高、丘厚均大于与之对应的坑宽、坑长、坑深.大林隙内丘坑复合体的丘宽、丘高、丘厚、坑宽、坑长、坑深均最大,分别为2.85、0.37、2.00、2.99、2.10、0.39 m;郁闭林分均最小,分别为2.35、0.19、1.60、2.66、1.65、0.21 m.丘的平均体积（1.66 m³）均大于坑的（1.44 m³）.同一大小林隙内绝大多数丘坑复合体之间的特征值差异显著,而郁闭林分内绝大多数丘坑复合体之间的特征值差异不显著.不同大小林隙及郁闭林分丘坑复合体之间的特征值大多差异显著.2012年样地内丘坑复合体大多数特征值显著小于2011年.89.5%和60.5%的丘坑复合体类型为铰链式,形状为半椭圆状,丘坑复合体的分布格局为相对集中.     

Spatial analysis of structural and tree‐ring related parameters in a timberline forest in the Italian Alps

Abstract. We investigated the variability in spatial pattern of some structural, dendrochronological and dendroclimatological features of a mixed Larix decidua‐Pinus cembra forest at the timberline in the eastern Italian Alps at fine geographical and temporal scales. Forest structure variables such as stem diameter, tree height, age and tree‐ring related parameters (yearly growth index, mean sensitivity, first order autocorrelation and some dendroclimatic variables) have been compared at various scale levels. We observed that most of the variables show positive autocorrelated structures due to both forest dynamics and fine‐scale driving forces, probably related to microrelief. Spatial structure of yearly indexed radial growth appears sensitive to extreme climatic events. Secondary succession after past disturbances drives the forest towards a structure governed by a gap regeneration dynamics that seems to ensure the different requirements of the two main tree species present. Small spatial scale studies of forest structures, especially if integrated to dendro‐ecological data, seem an efficient tool to assess the disturbance regime and species sensitivity to environmental change.     

福建万木林天然马尾松林分特征

福建万木林天然马尾松林为以马尾松占绝对优势的松阀混交林,物种多样性与四周的天然阔叶林相近,林分蓄积量高达９８４．２ｍ３ｈｍ－２,是罕见的、典型的天然马尾松丰产林,为珍贵的自然资源。     

Aboveground biomass and litterfall ofPinus pumila scrubs growing on the Kiso mountain range in central Japan

Aboveground biomass and litterfall ofPinus pumila scrubs, growing on the Kiso mountain range in central Japan, were investigated from 1984 to 1985. The biomass of two research plots (P1 and P2) with different scrub heights was estimated by two methods, the stratified clip technique and the allometric method. Aboveground total biomass estimated by the latter method reached 181 ton d.w. ha⁻¹ in P1 and 132 ton d.w. ha⁻¹ in P2. Creeping stems contributed to about half of the total biomass. Although estimates of woody organs differed between the two plots, leaf biomass estimates were almost the same at 15.5 ton d.w. ha⁻¹. The canopies of the twoP. pumila scrubs were characterized by a large mean leaf area density of 5.0 m² m⁻³. Despite this large area density, relatively moderate attenuation of light intensity was observed. Specific leaf area generally increased with reduced leaf height. Annual total litterfall was estimated to be 3.60 ton d.w. ha⁻¹ yr⁻¹ in P1 and 2.39 ton d.w. ha⁻¹ yr⁻¹ in P2. Annual leaf fall in both plots was approximately 2.0 ton d.w. ha⁻¹ yr⁻¹. Leaves fell mainly in early autumn. Annual loss rates of branches, estimated as the sum of annual branch litterfall and the amount of newly formed attached dead branches, were 0.29 ton d.w. ha⁻¹ yr⁻¹ in P1 and 0.37 ton d.w. ha⁻¹ yr⁻¹ in P2.     

Effects of phosphinotricin treatment on glutamine synthetase isoforms in Scots pine seedlings

The occurrence of GS isoenzymes has been investigated in Scots pine (Pinus sylvestris) seedlings. A transient increase of glutamine synthetase (GS, EC 6.3.1.2) activity was observed in the cotyledon whorl of plants treated with the herbicide phosphinotricin (PPT). The increase in GS activity was accompanied by a parallel accumulation of GS1 protein, which remained at high levels throughout the PPT treatment. Two-dimensional SDS-PAGE western analysis showed that pine extracts contained two GS1 polypeptides which differ in their corresponding isoelectric points. Analysis of crude extracts by ion-exchange chromatography led to the separation of two GS isoforms. The first peak (GS1-a) eluted from the columns at a low ionic strength (0.15-0.18 M KCl), whereas the second one (GS1-b) was detected at 0.5 M KCl. A detailed molecular study of both GS holoenzymes confirmed that their subunits were similar in size (about 41 kDa) but different in charge. All these data clearly demonstrate the presence of two GS1 forms in Scots pine cotyledons. Moreover, a comparison of isolated GS isoproteins with the recombinantly expressed Scots pine cytosolic subunit suggests that GS1-a corresponds to the previously characterized cDNA (pGSP114) whereas GS1-b is a minor GS isoenzyme with increased relative abundance in phosphinotricin treated plants.     

Pinus MUTOI (Pinaceae), a new species of permineralized seed cone from the upper Cretaceous of Hokkaido,Japan

Pinus mutoi is described as a new species on the basis of a permineralized seed cone from the Upper Cretaceous of Hokkaido, Japan. The cone is at least 20 cm long and up to 6 cm in diameter, consisting of a cone axis and numerous cone-scale complexes that are arranged helically around the axis. Two winged seeds are borne on the adaxial surface of each ovuliferous scale. Each complex receives a single trace from the vascular cylinder of the cone axis. In the scale base, all the resin canals occur abaxially to the vascular strand. The spatulate bract of the fossil is unique to the specimen among the cones of both living and fossil Pinus. The central umbo, broad sclerotic cortex of cone axis, and absence of serotinous features of the fossil cone suggest affinity with the subsection Sylvestres of the section Pinus, subgenus Pinus. This is the first record of permineralized preserved Pinus cone from the Cretaceous of Eastern Eurasia.