Effect of open-air fumigation with sulphur dioxide and ozone on phyllosphere and endophytic fungi of conifer needles

The phyllosphere microbial populations inhabiting the needles of three conifer species, Scots pine (Pinus sylvestris L.), Sitka spruce (Picea sitchensis L.) and Norway spruce (Picea abies (L.) Karst.), exposed to SO₂ and O₃, in an open-air fumigation experiment were analysed over a 3 year period using serial dilution after washing, direct plating and a fluorescein diacetate (FDA) enzyme assay. Total fungal populations ranged from 10² to 10⁵ colonyforming units (CPU) g^?1 fresh weight of needles. The dominant fungi isolated from needles varied with tree species and isolation technique; Aureobasidium pullulans (de Bary) Arnaud was most common on Scots pine and Norway spruce and white yeasts on Sitka spruce using the dilution plating method. However, direct plating of needle segments onto culture media indicated that Sclerophoma pythiophila (Corda) Hohnel was dominant on Scots pine and A. pullulans on Sitka and Norway spruce. Green needles of Sitka spruce were found to be endophytically colonized by Rhizosphaera kalkhoffii Bubak, but seldom by Lophodermium piceae (Fuckel) Hohn during extensive sampling in 1990. Statistical analyses revealed significant differences (P<0.05) between plots in the 3 year mean of the total fungal populations or the fungal biomass (FDA assay) on all three tree species. Differences between plots were also observed for a number of dominant component species. Data were also analysed for treatment effects. A significant effect of SO₂ treatment was observed on the total fungal populations on Sitka spruce (P<0.05) which were reduced markedly by the low-SO₂ treatment, while the O₃ treatment caused a significant increase in total fungal numbers on Scots pine (P<0.05). The FDA activity on needles of both Scots pine and Sitka spruce was noticeably higher in the 0₃-only treatment plot, but the overall O₃ effect was not significant. Treatment effects were also detected on the occurrence of component species. The serial dilution method revealed an SO₂ effect (P<0.05) of a reduction in the occurrence of pink yeasts on Sitka spruce and an O₃ effect (P<0.05) of an increase in the occurrence of S. pythiophila on Sitka spruce (P<0.01) but a decrease of Epicoccum nigrum Link and Cladosporium spp. on Scots pine. The direct-plating method revealed an SO₂ effect of an increase in S. pythiophila on Norway spruce (P<0.05). Ozone treatment caused a significant increase in the isolation of a black strain of A. pullulans on Norway spruce (P<0.05). Endophytic colonization of Sitka spruce needles by R. kalkhoffii was found to be increased on two occasions by O₃ exposure.     

15N-ammonium and 15N-nitrate uptake of a 15-year-old Picea abies plantation

Throughfall nitrogen of a 15-year-old Picea abies (L.) Karst. (Norway spruce) stand in the Fichtelgebirge, Germany, was labeled with either ¹⁵N-ammonium or ¹⁵N-nitrate and uptake of these two tracers was followed during two successive growing seasons (1991 and 1992). ¹⁵N-labeling (62 mg ¹⁵N m^-2 under conditions of 1.5 g N m^-2 atmospheric nitrogen deposition) did not increase N concentrations in plant tissues. The ¹⁵N recovery within the entire stand (including soils) was 94%±6% of the applied ¹⁵N-ammonium tracer and 100%±6% of the applied ¹⁵N-nitrate tracer during the 1st year of investigation. This decreased to 80%±24% and 83%±20%, respectively, during the 2nd year. After 11 days, the ¹⁵N tracer was detectable in 1-year-old spruce needles and leaves of understory species. After 1 month, tracer was detectable in needle litter fall. At the end of the first growing season, more than 50% of the ¹⁵N taken up by spruce was assimilated in needles, and more than 20% in twigs. The relative distribution of recovered tracer of both ¹⁵N-ammonium and ¹⁵N-nitrate was similar within the different foliage age classes (recent to 11-year-old) and other compartments of the trees. ¹⁵N enrichment generally decreased with increasing tissue age. Roots accounted for up to 20% of the recovered ¹⁵N in spruce; no enrichment could be detected in stem wood. Although ¹⁵N-ammonium and ¹⁵N-nitrate were applied in the same molar quantities (¹⁵NH ₄ ⁺ : ¹⁵NO ₃ ^- =1:1), the tracers were diluted differently in the inorganic soil N pools (¹⁵NH ₄ ⁺ /NH ₄ ⁺ : ¹⁵NO ₃ ^- /NO ₃ ^- =1:9). Therefore the measured ¹⁵N amounts retained by the vegetation do not represent the actual fluxes of ammonium and nitrate in the soil solution. Use of the molar ammonium-to-nitrate ratio of 9:1 in the soil water extract to estimate ¹⁵N uptake from inorganic N pools resulted in a 2–4 times higher ammonium than nitrate uptake by P. abies.     

灵芝孢子粉中氨基酸和微量元素的分析

本文用氨基酸自动分析仪测定了灵芝孢子粉中的19种氨基酸,其总含量为7.20g/100g,其中牛磺酸(含0.02g/100g)为作者首次测得。我们还用电感耦合等离子体发射光谱法(ICP-AES法)测定了灵芝孢子粉中14种微量元素和8种常量元素,其中Ge的含量为5.9mg/kg,Hg、As、Pb的含量依次为<0.01、1.5、2.2mg/kg,而P、Fe、Zn等有益元素的含量介于0.12×10~3mg/kg与6.22×10~3mg/kg之间。     

Numerical analysis of vegetation complexes and community diversity of major coastal dinaric mountains

Abstract. This study includes 24 transects on slopes of the Velebit, Biokovo and Orjen mountains, the tallest coastal mountains along the Adriatic Sea, with a very high species richness according to European standards and having the largest regional concentrations of endemics. Within each transect the presence or absence of phytosociological alliances, according to the Zürich-Montpellier School, was interpreted from local studies. The alliance composition of the transects was compared with methods used in numerical syntaxonomy. Three types of vegetation complexes (N. Dinaric inland, transitional and S. Dinaric coastal) were derived from a numerical classification of the transects; they were defined on the basis of their characteristic alliances. The maritime impact affecting the mountains through the river canyons reduces the contrast in vegetation between inland and coastal slopes. The existence of a climatic macrogradient is indicated by seriation of the basic alliance/transect data matrix leading to a diagonal structure, by a gradual shift of the alliance composition within the same vegetational type, and by the distribution of the transects and alliances along the first axis of a Correspondence Analysis ordination. Transect scores on the second ordination axis are negatively correlated with transect vegetational diversity (number of alliances per transect); this axis may reflect a decrease in humidity and temperature range. This interpretation is supported by the result of a comparison of the total mountain vegetational diversity (Mann-Whitney test), which showed that Orjen is the most diverse mountain ridge. The expected correlation between plant community diversity and altitude of the transects is blurred, probably due to the impact of the cold Bora wind and subsequent compression of vegetational zones.     

广西龙虎山猕猴种群生态特征

１９８８～１９９５年,采用定点观察法和绝对计数与相对计数结合法对龙虎山猕猴种群生态作了调查研究。１９９０年核心区有猕猴１４群,５００只左右,猴群密度１．６群／ｋｍ２,种群密度５５．６只／ｋｍ２．猴群大小平均３３．８±２３．１（ｎ＝６）只。一般每隔４～５年分群一次,猴群群体年均增长率１４．８％,种群年均增长率为９．７％。猴群中成年猴性比为７．６±６．５（ｎ＝１２）,１～３岁组的性比为０．７４±０．６１（ｎ＝４）,群内未成年猴比例为６７．７±３．１％（ｎ＝１２）。发情交配期最早１１月１２日,最晚次年１月２０日,高峰期１２月上旬,持续３个月．产仔期最早４月１日,最晚８月１４日,高峰期５月上旬,持续时间４个半月．繁殖率４５．５％～１００％,平均７５．４±１３．２％（ｎ＝２１）。新生猴死亡率较低,新生猴性比（雌：雄）平均０．７４±０．３４（ｎ＝５）。     

盘县大洞的发育与演化

盘县大洞是一个形态和成因复杂的大型喀斯特洞穴系统,本文通过对喀斯特作用与坡立谷结构,古水系变迁与洞穴形成等动力地貌－洞穴过程分析,探讨区域喀斯特及洞穴形成演化的水动力成因,结合岩相古地理环境等推测指出,关牛洞形成早更新世和中更新世早期,大洞洞厅,阴河坡,消洞和水洞形成于更新世早期至中更新世中期,十里坪坡立谷的形成始于中更新世早期,并经历后来反复积水－消水,侵蚀－堆积过程直至全新世。     

Carbohydrate distribution and cellular injuries in acid rain and cold-treated spruce needles

Summary The cellular structures of acid rain-irrigated needles of several provenances of Norway spruce (Picea abies L. Karst) seedlings were studied after winter experimental freezing. Frost injuries and recovery were characterized by visual damage scoring and classification of mesophyll cell alterations, also using histochemical methods for carbohydrate fluorescent staining. The treatment with-30° C during the late dormancy period was sufficient to cause significant injuries and intracellular degradation in the tissues of the green needles. The most affected seedlings in terms of visual injury scoring were found among those treated with clean water or at pH 3, while freezing injury, defined as an occlusion of phenolic substances in the central vacuole of the mesophyll cells, was most abundant in the needles from spruces irrigated either with clean water or at pH 4 or pH 3. Electron microscopy revealed the details of the injury, e. g. thinning out of the cytoplasm and chloroplast stroma, darkening of the chloroplasts and eventually swelling of the chloroplasts and protoplast. PAS and ConA reactions in the needle tissue revealed intense starch accumulation in the mesophyll and transfusion tissues as early as in March, with a tendency to increase, especially in the untreated needles during the recovery period. Plasma membrane disturbances were indicated by histochemical identification of callose deposits in the mesophyll cell walls, these being most abundant in the acid rain-treated needles. All these findings suggest that freezing at –30° C was more deleterious to the seedlings pretreated with acid or clean water than to those not given additional irrigation.     

The effect of ozone on the yellowing process of magnesium-deficient clonal Norway spruce grown under defined conditions

During two vegetation periods, young clonal spruce trees (Picea abies (L.) Karst.) with sufficient and poor magnesium (Mg) supply were exposed in the environmental chambers of the GSF phytotron to three levels of ozone (daily means: 18-22, 88-130, and 135-190 microg m(-3); 10% reduction at night). Previous year's needles were examined at 4-week intervals with respect to their contents of Mg, Ca, K, Mn, N, P, and chlorophyll (Chl), various parameters of Chl fluorescence, and the stability of the isolated light-harvesting Chl-a/b-protein complex LHC II. The needles of the two nutrition variants contained more than 0.53 or less than 0.27mg Mg g(-1) needle dry matter, respectively. The ratio of variable to maximal Chl-a fluorescence of the dark-adapted needles, Fv/Fm, and the photoinhibitory quenching of Fv after light treatment, SVi.v, were affected by the Mg content of the needles rather than the ozone levels. Changes of the Chl content and the behavior of the LHC II allowed differentiating between a slow process of needle yellowing occurring under Mg deficiency only, and a rapid process of needle yellowing occurring under the combined action of Mg deficiency and ozone pollution. Only the rapid yellowing process was accompanied by destabilization of the LHC II, and the degree of destabilization was correlated with the ozone concentration present in the days before sampling. The results are consistent with observations obtained at a research site in the Central Black Forest (J Plant Physiol 161 (2004) 423).     

喀斯特山地城市内山体绿地对城市热岛的减温效应——以安顺市西秀区为例

山体绿地是喀斯特山地城市内典型的城市绿地景观类型,其对于改善城市生态环境、提升喀斯特山地城市生态服务功能具有重要作用。以黔中典型喀斯特山地城市安顺市为研究对象,运用2011年和2016年两期热红外遥感影像和城市景观结构空间数据,在反演分析城市热岛效应及其强度时空分布特征的基础上,运用冷热点分析剖析了山体绿地与城市热岛效应冷点分布区的关系,揭示山体绿地对城市热岛的减温效应。结果表明:基于Landsat热红外遥感数据反演地表温度结果显示,2011—2016年,安顺市西秀区平均反演地表温度升高约4℃;主城区一带热岛效应呈现加剧趋势,但总体热岛面积呈下降趋势,绿岛区多分布于水体和山体绿地中,且山体绿地对热岛效应减缓作用逐年增大;热/冷聚集面积呈现上升趋势,约40%~50%的冷聚集区由山体绿地贡献,热聚集区主要由建筑用地和其他用地构成;500 m格网尺度下,山体绿地面积与地表温度呈显著负相关,表现为山体绿地面积占格网比例每增加10%,地表温度将降低0.17~0.27℃。研究结果可为喀斯特山地城市山体绿地管理、城市绿地空间规划和城市热环境缓解提供科学依据。     

Direct response of tree growth to soil water and its implications for terrestrial carbon cycle modelling

Wood growth constitutes the main process for long‐term atmospheric carbon sequestration in vegetation. However, our understanding of the process of wood growth and its response to environmental drivers is limited. Current dynamic global vegetation models (DGVMs) are mainly photosynthesis‐driven and thus do not explicitly include a direct environmental effect on tree growth. However, physiological evidence suggests that, to realistically model vegetation carbon allocation under increased climatic stressors, it is crucial to treat growth responses independently from photosynthesis. A plausible growth response function suitable for global simulations in DGVMs has been lacking. Here, we present the first soil water‐growth response function and parameter range for deciduous and evergreen conifers. The response curve was calibrated against European larch and Norway spruce in a dry temperate forest in the Swiss Alps. We present a new data‐driven approach based on a combination of tree ring width (TRW) records, growing season length and simulated subdaily soil hydrology to parameterize ring width increment simulations. We found that a simple linear response function, with an intercept at zero moisture stress, used in growth simulations reproduced 62.3% and 59.4% of observed TRW variability for larch and spruce respectively and, importantly, the response function slope was much steeper than literature values for soil moisture effects on photosynthesis and stomatal conductance. Specifically, we found stem growth stops at soil moisture potentials of ?0.47 MPa for larch and ?0.66 MPa for spruce, whereas photosynthesis in trees continues down to ?1.2 MPa or lower, depending on species and measurement method. These results are strong evidence that the response functions of source and sink processes are indeed very different in trees, and need to be considered separately to correctly assess vegetation responses to environmental change. The results provide a parameterization for the explicit representation of growth responses to soil water in vegetation models.