黄龙山白桦桦木醇与桦木酸含量研究

为了阐明黄龙山白桦不同生境、不同径级、不同器官桦木醇与桦木酸含量,系统采集了陕北黄土高原黄龙山林场阳坡、阴坡、林缘、孤立木4种生境下的白桦不同径级植株的树皮、树枝和树叶样品,采用超声波辅助提取法提取样品,用高效液相色谱法测定了不同生境、不同径级白桦各器官桦木醇、桦木酸含量。结果表明：（1）不同生境下白桦各器官桦木醇、桦木酸含量均存在显著差异（P＜0.05）,白桦树皮中桦木醇与桦木酸含量、白桦树枝中桦木酸含量在4种生境下均表现为阴坡＞孤立木＞林缘＞阳坡,白桦树叶中桦木醇与桦木酸含量及树枝中桦木醇含量均表现为阴坡＞林缘＞孤立木＞阳坡,总体来看阴坡生境下白桦各器官桦木醇与桦木酸含量都是最高的。（2）在白桦各器官中,桦木醇、桦木酸含量均表现为树皮＞树枝＞树叶。（3）不同生境下白桦各器官桦木醇、桦木酸含量随着胸径的增大均先增大后减小,均在第Ⅱ径级即胸径10.1~20 cm达到最大。研究认为,阴坡生境有利于白桦各器官积累桦木醇、桦木酸;白桦各器官中桦木醇含量较高,桦木酸含量比较低,而以桦木酸为原料的生物制剂已进入临床应用阶段,因此,以桦木醇为原料制取桦木酸是解决桦木酸在天然植物中含量低、提取困难的有效途径;对白桦各器官的采收应注意把握时机,于白桦生长到胸径10.1~20 cm时为最佳采收期。     

The contribution of trees to ecosystem methane emissions in a temperate forested wetland

Wetland‐adapted trees are known to transport soil‐produced methane (CH₄), an important greenhouse gas to the atmosphere, yet seasonal variations and controls on the magnitude of tree‐mediated CH₄ emissions remain unknown for mature forests. We examined the spatial and temporal variability in stem CH₄ emissions in situ and their controls in two wetland‐adapted tree species (Alnus glutinosa and Betula pubescens) located in a temperate forested wetland. Soil and herbaceous plant‐mediated CH₄ emissions from hollows and hummocks also were measured, thus enabling an estimate of contributions from each pathway to total ecosystem flux. Stem CH₄ emissions varied significantly between the two tree species, with Alnus glutinosa displaying minimal seasonal variations, while substantial seasonal variations were observed in Betula pubescens. Trees from each species emitted similar quantities of CH₄ from their stems regardless of whether they were situated in hollows or hummocks. Soil temperature and pore‐water CH₄ concentrations best explained annual variability in stem emissions, while wood‐specific density and pore‐water CH₄ concentrations best accounted for between‐species variations in stem CH₄ emission. Our study demonstrates that tree‐mediated CH₄ emissions contribute up to 27% of seasonal ecosystem CH₄ flux in temperate forested wetland, with the largest relative contributions occurring in spring and winter. Tree‐mediated CH₄ emissions currently are not included in trace gas budgets of forested wetland. Further work is required to quantify and integrate this transport pathway into CH₄ inventories and process‐based models.     

Long‐term experimental manipulation of climate alters the ectomycorrhizal community of Betula nana in Arctic tundra

Climate warming is leading to shrub expansion in Arctic tundra. Shrubs form ectomycorrhizal (ECM) associations with soil fungi that are central to ecosystem carbon balance as determinants of plant community structure and as decomposers of soil organic matter. To assess potential climate change impacts on ECM communities, we analysed fungal internal transcribed spacer sequences from ECM root tips of the dominant tundra shrub Betula nana growing in treatments plots that had received long‐term warming by greenhouses and/or fertilization as part of the Arctic Long‐Term Ecological Research experiment at Toolik Lake Alaska, USA. We demonstrate opposing effects of long‐term warming and fertilization treatments on ECM fungal diversity; with warming increasing and fertilization reducing the diversity of ECM communities. We show that warming leads to a significant increase in high biomass fungi with proteolytic capacity, especially Cortinarius spp., and a reduction of fungi with high affinities for labile N, especially Russula spp. In contrast, fertilization treatments led to relatively small changes in the composition of the ECM community, but increased the abundance of saprotrophs. Our data suggest that warming profoundly alters nutrient cycling in tundra, and may facilitate the expansion of B. nana through the formation of mycorrhizal networks of larger size.     

Reproducibility of vegetation cover estimates in south‐central Alaska forests

Abstract. Reproducibility of vegetation measurements is critical for large‐scale or long‐term studies, where numerous observers collect data, but past studies have questioned repro‐ducibility of some techniques. Five methods of evaluating understory composition were appraised for reproducibility among six observers in two forest types in south‐central Alaska: ocular estimates in quadrats, overall community species rank and cover estimates, nested rooted frequency, horizontal‐vertical profiles, and pin drop (systematic points). One forest type was selected to represent structure of coastal communities, another to represent structure of interior Alaska communities. Three general methods of evaluating reproducibility were considered: standard deviations (precision among observers), components of variance (percentage of total variance attributable to observers), and analysis of variance (significance of observer variance). Observer variances were generally similar among techniques and significant in most cases. No technique stood out as being more reproducible than others. Features of techniques other than reproducibility may be more important when selecting a technique. Management decisions based on vegetation cover data should consider the observer errors involved as well as biological significance.     

The influence of vegetation type,soil properties and precipitation on the composition of soil mite and microbial communities at the landscape scale

Aim We used a landscape‐scale study of birch invasion onto heather moorland to determine the consistency of changes in vegetation type and soil properties and in the community composition of five soil organism groups. Our aim was to determine whether the degree to which soil organisms respond to natural changes and/or induced changes (e.g. changes in land‐use type and climate) in habitat is consistent across trophic and taxonomic groups in the context of conservation policies for birch woodland and heather moorland. Location Mainland Scotland. Methods We sampled mesostigmatid mites, oribatid mites, fungi, bacteria and archaea in adjacent patches of birch woodland (dominated by Betula pubescens) and heather moorland (dominated by Calluna vulgaris) at 12 sites for which annual rainfall ranged between 713 and 2251 mm. Differences in community composition were visualized using non‐metric multidimensional scaling based on Bray–Curtis dissimilarities. The factors contributing to differences between habitats within sites were explored using general linear models and those among sites using redundancy analysis. Results The communities of all groups differed between habitats within sites, but only the oribatid mites and fungi differed consistently between habitats across sites. Within sites, dissimilarity in fungal communities was positively related to the difference in C. vulgaris cover between habitats, whereas dissimilarities in bacteria and archaea were positively related to differences in soil pH and C:N ratio between habitats, respectively. Main conclusions The influence of vegetation type and soil properties differed between groups of soil organisms, albeit in a predictable manner, across the 12 sites. Organisms directly associated with plants (fungi), and organisms with microhabitat and resource preferences (Oribatida) were strongly responsive to changes in habitat type. The response of organisms not directly associated with plants (bacteria, archaea) depended on differences in soil properties, while organisms with less clear microhabitat and resource preferences (Mesostigmata) were not strongly responsive to either vegetation type or soil properties. These results show that it is possible to predict the impact of habitat change on specific soil organisms depending on their ecology. Moreover, the community composition of all groups was related to variation in precipitation within the study area, which shows that external factors, such as those caused by climate change, can have a direct effect on belowground communities.     

光皮桦6个南方天然群体的遗传多样性

为揭示中国特有珍贵用材树种光皮桦(Betula luminifera)天然群体的遗传多样性和遗传结构, 采用AFLP分子标记, 分析了采自浙江、福建、江西、广西和贵州5个省区6个天然群体的120份样品。9对引物获得了355个位点, 其中多态性位点323个。分析结果表明光皮桦天然群体具有较高的遗传多样性, 多态位点百分率(PPL)达90.99%, 各群体的PPL和Nei’s基因多样性(h_j)分别为93.20-98.60%和0.3143-0.3645; 总群体遗传多样性指数(H_t)为0.3616, 群体间遗传分化系数(F_st)为0.0650, 群体间总的基因流较高(N_m= 3.5962)。AMOVA分析表明群体间的遗传变异占总变异的11.49%, 浙江临安群体和贵州修文群体间的遗传距离最大(0.0665), 江西龙南群体和广西龙胜群体间的遗传距离最小(0.0173), 且遗传结构分析显示这两个群体的部分个体可能来自同一近祖。Mantel检测发现, 群体间的遗传距离与地理距离没有显著相关性(r = 0.423, P = 0.113), 而与两两群体所在地的均温差呈显著相关(r = 0.449, P = 0.017)。结合群体实地调查, 可以得出光皮桦天然群体的遗传多样性和遗传结构的形成不仅与其广域分布、自然杂交、种子特性以及生活史有关, 而且与群体被人为砍伐、生境片断化等因素有重要关系。基于上述结果我们提出了光皮桦天然种群的保护策略。     

青藏高原东缘林线交错带糙皮桦幼苗光合特性对模拟增温的短期响应

采用开顶式生长室(OTC)模拟增温对植被影响的研究方法, 研究了青藏高原东缘林线交错带糙皮桦(Betula utilis)光合特性对模拟增温的响应。结果表明: 与对照样地相比, OTC内日平均气温(1.2 m)在植物生长季中增加2.9 ℃, 5 cm土壤温度增加0.4 ℃。增温使糙皮桦幼苗叶片的净光合速率(P_n)、蒸腾速率(T_r)和气孔导度(G_s)分别增加17.4%、21.4%和33.9%, 但对糙皮桦幼苗叶片的水分利用率(WUE)却没有明显影响, 而对糙皮桦的叶氮浓度却表现为显著的负效应。同时, 增温能显著增加糙皮桦幼苗的最大同化速率(P_nmax) (+19.6%)、暗呼吸速率(R_d) (+14.3%)、表观量子效率(AQY) (+7.9%), 但对其光补偿点(LCP)和光饱和点(LSP)却没有明显的影响。此外, 增温使糙皮桦幼苗叶片的最大羧化速率(V_cmax)和电子传递速率(J)分别增加了12.3%和11.7%, 而磷酸丙糖利用率(TPU)和CO₂补偿点(CCP)对增温却并不敏感。该研究表明, 模拟增温对林线糙皮桦光合生理总体上表现为正效应, 这有可能帮助该物种对未来气候变化更快更好地适应。