Tree rings reveal long-term changes in growth resilience in Southern European riparian forests

The gradual increase in temperature over the last few decades is one of the major consequences of global change. It is also projected that drought frequency and intensity in the Mediterranean region will increase, promoting changes in plant responses to environmental conditions and ultimately species distribution. Studying past growth trends can help understand future impacts of climate change on species-function and predict alterations in how species are distributed. This study sought to evaluate growth trends in riparian tree species to assess both their resistance and resilience responses to, and their complementary strategies in the face of, climatic and hydrological changes. Their supporting ecosystem role in riverine ecosystems and their representativeness in the study region led to the selection of the species Alnus glutinosa (L.) Gaertn. and Fraxinus angustifolia Vahl for this purpose.Yearly growth curves were obtained for coexisting A. glutinosa and F. angustifolia, sampled in 2009 in a riparian forest in a Southern Portuguese river basin. Standardized Precipitation Evapotranspiration Index (SPEI) was calculated to select drought events, identified as years of extreme and severe drought combined with adverse river discharge conditions. Temporal trends in Basal Area Increments (BAI) were explored for both species across 1970–2009, particularly during drought years. Tree growth response was associated with long-term SPEI, minimum temperature, rainfall and discharge.Both species presented an increase in BAI until the 1980s, apparently triggered by the rise in minimum temperatures, which lengthened the growing season. However, after the 80′s this trend in tree growth has been reversed due to the reduced precipitation associated with increased drought intensity. Similar tree growth responses to drought were observed in both species, but responses to extreme drought events were species-specific. Distinct long-term resilience trends between species suggest that under the current climate change scenario, mesic species (e.g. A. glutinosa) will gradually be replaced by more drought-tolerant species, such as F. angustifolia.Finally, further research should be undertaken to provide information on physiological and anatomical changes of riparian tree species in the Mediterranean region.     

Black alder (Alnus Glutinosa (L.) Gaertn.) trees mediate methane and nitrous oxide emission from the soil to the atmosphere

Three-year-old seedlings of black alder (Alnus glutinosa (L.) Gaertn.), a common European wetland tree species, were grown in native soil taken from an alder swamp. Fluxes of methane (CH₄) and nitrous oxide (N₂O) between the tree stem and the atmosphere were determined under controlled conditions. Both CH₄ and N₂O were emitted through the bark of the stem into the atmosphere when the root zone exhibited higher-than-ambient CH₄ and N₂O gas mixing ratios. Flooding of the soil caused a decreased N₂O emission but an increased CH₄ efflux from the stem. Immediately after flooding of the soil, N₂O was emitted from the seedlings' bark at a rate of 350 mol N₂O m^-2 h^-1 whereas CH₄ flux could not be detected. After more than 40 days of flooding CH₄ fluxes up to 3750 mol CH₄ m^-2 h^-1 from the stem were measured, while N₂O emission had decreased below the limit of detection. Gas efflux decreased with increasing stem height and correlated with gas mixing ratios in the soil, indicating diffusion through the aerenchyma as the major path of gas transport. From these results it is assumed that woody species with aerenchyma can serve as conduits for soil-derived trace gases into the atmosphere, to date only shown for herbaceous plants. This, yet unidentified, woody plant pathway contributes to the total greenhouse gas source strength of wetlands.     

Chloroplast DNA phylogeography of Alnus glutinosa (L.) Gaertn.

Traditionally, information on the postglacial history of plant species has been gained from the analysis of fossil pollen data. More recently, surveys of present patterns of genetic variation have given valuable insights into species phylogeography. The genus Alnus , based on fossil data, is known to have had at least four glacial refugia. A survey of chloroplast DNA (cpDNA) diversity in populations of black alder ( A. glutinosa ) was undertaken in order to gain more insight into its postglacial history. This revealed a high degree of structuring of 13 cpDNA haplotypes on a European scale which indicated that most of northern and central Europe was colonized from a refuge in the Carpathian Mountains. Based on the distribution of two common cpDNA haplotypes, colonization routes from this refuge can be determined. The locations of other previously identified refugia are confirmed and two formerly unconfirmed refugial areas for alder (southern Spain and Turkey) are proposed.     

Ectomycorrhizas of Cortinarius helodes and Gyrodon monticola with Alnus acuminata from Argentina

Field ectomycorrhizas of Cortinarius helodes Moser, Matheny & Daniele (sp. nov) and Gyrodon monticola Sing. on Alnus acuminata Kunth (Andean alder, aliso del cerro) are described based on morphological and anatomical features. Ectomycorrhizal roots were sampled beneath fruitbodies of C. helodes and G. monticola from two homogeneous A. acuminata forest sites located in Tucumán and Catamarca Provinces in Argentina. C. helodes ectomycorrhizas showed a thick white to beige mantle exuding a milky juice when injured, were bluish toward the apex, and had hyphal strands in the mantle. G. monticola ectomycorrhizas showed some conspicuous features like highly differentiated rhizomorphs, inflated brown cells on the mantle surface, and hyaline and brown emanating hyphae with dolipores. Restriction fragment length polymorphism analysis of the nuclear rDNA internal transcribed spacer provided a distinctive profile for each of the collections of fruitbodies and the mycorrhizal morphotypes.     

Biotic versus hydrologic control over seasonal nitrate leaching in a floodplain forest

Strong seasonal increases in aquatic (stream, ground and hyporheic water) nitrate have been observed in a variety of ecosystems. In most cases, changes in hydrological and vegetative activity occur contemporaneously, making it difficult to determine whether soil leaching is being driven by increases in the availability of leachable N or is simply due to flushing of N that has accumulated over longer periods. Three studies were conducted to better determine controls on soil nitrate leaching in a near-pristine temperate floodplain ecosystem receiving large N inputs via N-fixation by red alder: 1) an artificial rainfall experiment was conducted to estimate N-leaching potential during the summer, when plant uptake is high and new inputs of organic matter are low; 2) soil solution, groundwater and surface water were sampled during a major autumn storm to document exchanges at the seasonal transition, when plant uptake is low and inputs of senescent organic matter are high; and 3) monthly samples of soil and aquatic nitrogen were collected in 1997 and 1998 to document seasonal patterns of N exchanges. Collectively, these studies demonstrate the importance of hydrologic factors in controlling N flux. Nitrate was rapidly leached from soils during actual and simulated rainstorms. Two pathways of nitrate leaching were identified. Localized flooding and direct leaching of streamside soils into surface waters contributed to high solute concentrations in peak flows. Nitrate that leached into interstitial waters was subject to various factors that could delay or reduce its delivery to surface waters. Greater residence time may increase the influence of this component of stormflow on ecosystem productivity. While soil nitrate pools were rapidly depleted during rainstorms, accumulation of soil nitrate occurred over summer dry periods. Large differences in soil and aquatic nitrate concentrations between two years with contrasting rainfall highlight the potential for inter-annual hydrologic variability to affect ecosystem nutrient cycling.     

The effect of the meteorological factors on the Alnus pollen season in Lublin (Poland)

Alder pollen seasons and the effect of meteorological conditions on daily average pollen counts in the air of Lublin (Poland) were analysed. Alnus pollen grains reach very high concentrations in the atmosphere of this city during the early spring period and the parameters of pollen seasons were very different in the particular years studied. The pollen season lasted on average one month. The highest variation was observed for the peak value and the Seasonal Pollen Index (SPI). The pollen seasons, which started later, had shorter duration. Peak daily average pollen counts and SPI value were higher during the shorter seasons. Similarities in the stages of pollen seasons designated by the percentage method depended on the start date of the pollen season. Season parameters were mainly correlated with thermal conditions at the beginning of the year. Regression analysis was used to predict certain characteristics of the alder pollen season. The highest level of explanation of the variation in Alnus pollen season start and peak dates was obtained in the model using mean temperature in February. The obtained regression models may predict 82% of the variation in the pollen season start date, 73% of the variation in the duration, and 62% in the peak date.     

Growth,nitrogen accumulation,and symbiotic dinitrogen fixation in pure and mixed plantings of hybrid poplar and black alder

Summary Growth and N accumulation were assessed in pure and mixed plantings (2 years old) of hybrid poplar and black alder in southern Québec. Symbiotic dinitrogen fixation was evaluated by natural¹⁵N dilution. Growth of hybrid poplar plants and N accumulation in their tissues increased with their decreasing contribution to species ratio whereas no differences among treatments were measured for black alder. Yield and N content per hectare of aboveground components increased with the proportion of black alder in the plantation. Symbiotic dinitrogen fixation was estimated at 68% of alder nitrogen in both pure and mixed treatments. The maximum rate of N-fixation was 53kg ha^–1 yr^–1 in pure alder plots. The amount of nitrogen accumulated in entire plants of black alder from symbiotic fixation could be sufficient to balance the N export in harvested stems and branches of short-rotation plantations containing at least 33% of alder.     

Callus regeneration from Alnus incana protoplasts isolated from cell suspensions

Nagata and Takebe's (NT) medium, supllementedte with 2.5 μm 2,4-dichlorphenoxyacetic acid (2,4-D), induced development of friable calluses from leaves of axenic shoot cultures of Alnus incana. Fast-growing cell suspensions were established in the same medium without agar. Suspensions gave high yields of viable protoplasts after an overnight incubation in an enzyme mixture consisting of 1% (w/v) Onozuka R-10, 0.5% (w/v) Rhozyme HP-150, 0.03% (w/v) Macerase, CPW salts, and 13% (w/v) mannitol (pH 5.8). Protoplasts cultured on K8p medium underwent cell wall regeneration within 24 h. The optimum protoplast-derived colony formation and growth was obtained on the NT medium supplemented, as was the K8p medium, with glucose as the osmoticum, growth regulators, coconut milk and casein hydrolysate. Compared with other culture techniques, the agarose bead technique of Shillito et al. (Plant Cell Reports, 2 (1983) 244) improved cell division and colony formation frequency. Protoplast-derived macrocalluses grew under the same conditions as those used for leaf calluses.     

Carbon and Nitrogen Dynamics of Boreal Jack Pine Stands With and Without a Green Alder Understory

We compared the species composition, structure and selected components of the carbon (C) and nitrogen (N) budgets of similar-aged, mature boreal jack pine (Pinus banksiana Lamb.) forests with and without green alder [Alnus crispa (Ait.) Pursh.] in two different boreal environments. The C and N content of the overstory biomass components (for example, stem, branch, and foliage), total vegetation, forest floor, and mineral soil were greater (P= 0.05 to P= 0.10) for jack pine with alder (JPA) stands than for jack pine without alder (JP) stands at both study areas. Jack pine foliage N isotopic discrimination (δ¹⁵N) and annual litterfall N content were significantly greater (P < 0.05) in the JPA than the JP stands at both study areas, suggesting that alder was fixing N and that N availability was greater in the JPA than the JP stands. The greater leaf area index (LAI) and overstory C accumulation in the JPA than the JP stands (P < 0.05) is likely because of the greater N availability in the JPA stands, but the effect of soil texture discontinuity on water availability in the JPA stands can not be dismissed. Percent ground cover by feathermoss varied among the jack pine communities and was positively correlated with overstory LAI (r ²= 0.83, P< 0.05). One index of N-use efficiency (NUE), defined as aboveground net primary productivity (ANPP) per litterfall N, was significantly greater (P < 0.05) for the JP than the JPA stands, but a second index of NUE, ANPP/N uptake, did not differ between the two jack pine communities. Jack pine trees growing without alder produced more organic matter per unit of N, but percent N retranslocation from senescing foliage and N mean residence time in the overstory did not differ between the JPA and the JP stands. A conceptual model is presented that illustrates the potential influence of alder on the species composition, structure, and function of boreal jack pine forests. Received 6 January 1998; accepted 15 April 1998.