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The herb layer recovery in post-agricultural woods adjacent to ancient forests has not yet been studied for the wettest European woodlands, like those with black alders (Alnus glutinosa L. (Gaertn.)). Therefore, the studies aimed at: I. checking which herbs from the Polish list of ancient woodland species that are present in the alder woods show an association with these woods (AAWS=Ancient Alder Woodland Species); II. presenting their ecological profile (spectra of life forms, life strategies, dispersal modes, phytosociological affinity, and Ellenberg indicator values), and III. comparing the dispersal potential and other traits of species recorded more often in ancient woods (AAWS) vs the Polish ancient woodland indicators frequently present in ancient and recent alder woods (OAWS = Other Ancient Woodland Species). The survey was carried out in Alnus glutinosa-dominated woodlands, located in south-western Poland. The study sites are located within large forest complexes, where they occupy either periodically waterlogged sites or other places with a high level of groundwater. In the case of ancient woods, wet types of an oak-hornbeam community (Tilio-Carpinetum Tracz. 1962 or Galio-Carpinetum Oberd. 1957) (11 sites), alder-ash carrs (Fraxino-Alnetum W. Mat. 1952) (12 sites) and typical wet alder woods (Ribeso nigri-Alnetum Sol.-Górn. (1975) 1987) (10 sites) were investigated. The ancient woodland sites varied in size from 0.73 ha to 15.54 ha. Recent woods, adjacent to these sites, included black alder stands planted on former meadows. The area of their patches ranged from 0.72 ha to 8.6 ha. Post-agricultural woods represented the following age classes: up to 10 years, 11–20, 21–30, 31–40, and 41–50 years. The process of colonization of recent woods by woodland flora was investigated in 33 transects, approximately 80 m in length by 4 m in width, consisting of 10–12 quadrates, 16 m² each, laid out at intervals of 4 m, perpendicularly across the ancient-recent border. In total 131 quadrates in the ancient wood, 198 in the recent woodland, and 34 in the ecotone zone were investigated. The migration rates (m yr⁻¹) based on the occurrence of the farthest individuals, were calculated for over 50 woodland species. The original lists of species obtained from the transects were completed after detailed inspections of the whole area of adjacent forest sectors where the studies on the colonization process were undertaken. Then, the frequency of herb layer species in ancient and recent woods was compared (Fisher exact probability test). The mean migration rates of species from the AAWS and OAWS groups were calculated. Although 62 herbs from the group of ancient woodland indicators for Poland were recorded in the course of the studies, only 21 of them occurred significantly more often in alder woods. The mean migration rate for herbs from AAWS was significantly lower (0.68 m yr⁻¹) than in the case of the OAWS group (1.54 m yr⁻¹). This indicates that true woodland herbs differ distinctively in their dispersal potential. Species from those two sets also showed some differences in their ecological requirements. Such results allow a conclusion to be reached that in wet and fertile recent forests adjacent to ancient source woods, recolonization of the herbaceous layer by typical woodland flora proceeds faster than in other, less fertile and drier habitats. This in turn explains why many true woodland species do not occur in ancient woodland sites exclusively. They are often recorded in recent woods, as they are able to colonize such sites reasonably fast.
Black alder, an N-fixing tree is considered to accelerate the availability of phosphorus in soils due to the increased production of phosphatase enzymes, which are responsible for the P release from the litter. Acid phosphatase activity plays a pivotal role in organic P mineralization in forest soils and in making P available to plants. In order to check whether Alnus glutinosa stimulates acid phosphomonoesterase (PHACID) activity, we compared enzyme activities, total P concentration (PTOT), plant-available P (PAVAIL), organic P (PORG) and inorganic P (PINORG), and organic matter content in 27 ancient and 27 post-agricultural alder woods (the latter ones representing different age classes: 11-20, 21-40 and 41-60 years) of soil samples taken from the litter and the mineral layers. Phosphomonoesterase activity, organic matter, PTOT, PINORG and PORG concentrations were significantly higher in ancient alder woods than in the soils of post-agricultural forests. Significant differences in the acid phosphatase activity, organic matter and PAVAIL concentration were noted between the litter and mineral layers within the same forest type. In recent stands the amount of organic matter and phosphatase activity increased significantly with the age of alder stands, although only in the mineral layer of their soils. Phosphomonoesterase activity, organic matter and PAVAIL content were higher in a litter layer and decreased significantly at a mineral depth of the soil. The acid phosphatase activity was significantly correlated with organic matter content in both ancient and recent stands. There was no significant relationship between PHACID activity and any P forms.
Tree ring chronologies of Scots pine (Pinus sylvestris L.) and black pine (P. nigra Arnold) from the dry coniferous forest and the fresh mixed coniferous forest, as well as black alder (Alnus glutinosa (L.) Gaertn.) from the alder swamp forest, in the Słowiński National Park and neighbouring forests (Damnica Forest District) are presented. For both pine species 1940, 1956, 1976, and 1996 were the negative signature years, while 1946, 1957, and 1989 were the positive ones. In black alder the diameter increment depressions occurred in 1997 and 1998. The tree ring width in both pine species was positively correlated with the mean monthly air temperatures in February and March, while there was no univocal precipitation-tree growth relationship found. In some cases, in black pine from the fresh mixed coniferous forest and black alder from the alder swamp forest, the statistically significant coefficients describing the precipitation-increment relationship had negative values. The increment depressions, which occurred in both pine species during 1981- -1983, were the result of the nun moth (Lymantria monacha L.) outbreak. Black alder was not attacked by this phyllophagous insect. The positive July precipitation-tree growth relationship was found in both pine species during the nun moth outbreak.
The paper deals with the structural diversity and production of a less frequently studied type of alder stands originated on former agricultural lands in the 1950s, established partly by plantation and partly by natural succession in the area of the Krkonoše Mts. and the Orlické hory Mts. (Czech Republic). Four permanent research plots (PRP) were established at sites where Black alder (Alnus glutinosa L. Gaertn.) and Grey alder (Alnus incana L. Moench.) naturally occurs, each plot of 0.25 ha in size. The aim of the study was to evaluate the structure and development of the alder stands with respect to biodiversity, horizontal, vertical and species structure, diameter increment with emphasis on climate factors, and the quantity and quality of timber production. The results document low diversification of the studied stands in the PRPs. The horizontal structure is defined as random and clumped at sites at the highest altitude with high water table. The number of living trees with DBH ≥ 4 cm ranges between 556 to 828 trees ha-1 with the relative stand density index (SDI) 0.67–0.77. The stand volume ranges from 247 to 393 m3 ha–1, and decreases with higher altitudes. Low temperatures is limiting factor for radial growth in the high mountain areas, respectively low precipitation in the middle lands. Owing to a rather specific site character, as especially the spring area, the stands exhibit only average production, but the production quality is generally high. The quality timber is suitable for industrial use; the rot-affected trunk base parts usable for fuel represent only approximately 16%.
The aim of this study was to specify the above-ground biomass structure of black alder as well as to assess the influence of habitat conditions on biomass size and on allometric relation between biomass and breast height diameter. The empirical material consisted of 67 sample trees in age from 6 to 20 years selected from 17 stands growing on two types of forest habitat. The average share of stem wood in aboveground biomass of trees was 61.04%, branches 18.89%, bark and leaves 11.31% and 8.76% respectively. The fact that the examined stands constituted habitat type did not substantially influence either the biomass size or the relation between biomass and breast height diameter.
Black alder (Alnus glutinosa Gaertn.) is considered a hygrophilous species. The aim of the research was to find out if black alder may play a role of a pioneer species in the habitat of Tilio-Carpinetum typicum Traczyk 1962, i.e. fresh oak-linden-hornbeam forest. The investigation was carried out in Białowieża Forest (East Poland). The vegetation was examined with the Braun-Blanquet (1928) method. Soil diagnosis was based on the analysis of soil profiles and a network of test borings. Ecological differentiation of the phytocoenoses in terms of light, humidity, and fertility factors was analysed by indicator values of vascular plants. Obtained results showed that black alder may play the role of a pioneer species in the habitat of fresh oak-linden-hornbeam forest (Tilio-Carpinetum typicum). This phenomenon may occur on haplic luvisols underlayed with clay, after clear-cuts bigger than 1 hectare. Secondary plant communities with black alder that develop in such conditions reveal characteristics of wet oak-linden-hornbeam forest (Tilio-Carpinetum stachyetosum Traczyk 1962).
Hazel and alder bloom as one of the fi rst plants in climatic conditions of Poland. In the present study, detailed observations were made of the structure of fl owers of Corylus avellana L. and Alnus glutinosa (L.) Gaertn. Pollen yield of the abovementioned species was determined. The number of pollen grains in the theca, anther, fl ower and infl orescence was calculated. A comparison was made of the number of pollen grains of these taxa recorded during the atmospheric pollen seasons analysed over a period of 8 years in the conditions of Lublin. The study demonstrates that pollen yield of the common hazel infl orescence was 66 mg, whereas for black alder it was 120 mg. It was found that the number of pollen grains produced by the alder infl orescence was 2.2 times higher than by the hazel infl orescence. The atmospheric pollen season of the studied plant taxa was recorded at similar dates, but alder pollen was in much larger concentrations.
The different defence strategies of trees against herbivores are very often connected with succession status, leaf life span and the level of secondary metabolites. We examined the effect of simulated leaf grazing on the differences in the leaf life span and defence chemistry of two pioneer tree species that belongs to the same family (Betulaceae), black alder (Alnus glutinosa (L.) Gaertn.) and European white birch (Betula pendula Roth.). At the beginning of the growing season, mature leaves were perforated using a paper punch. The holes removed about 10% of the leaf surface. Each species was represented by six trees – one branch was chosen for perforation and one branch as a control. All leaves were counted every week until their abscission. Additional damages caused by grazing insects were also noted. Undamaged birch leaves were held much longer than those of alder. The average difference in half leaf life span between control and perforated leaves was 28 days in birch and 6 days in alder. The control unperforated alder leaves were significantly (P <0.05) more often grazed by insects than those that were perforated. Leaf perforation in alder increase phenolic concentrations in the new, young leaves. In birch we did not observe these changes. The comparison of alder and birch indicate that the species with similar successional status can have different strategies of leaf defence. The birch leaves were characterized by a longer leaf life span, constitutive defence, a lack of induced defence accumulation of phenolics and earlier shedding of damaged leaves in comparison to the control. The black alder foliage had a shorter leaf life span, induced defence reaction (produced more phenolics after perforation), and only slightly earlier shedding of damaged leaves than the control.
Badania miały na celu określenie patogeniczności zróżnicowanych na 3 podgatunki izolatów Phytophthora alni, otrzymanych z porażonych olszy, gleby oraz wody. W pierwszym doświadczeniu inokulowano krążkami plechy podstawę pędu 2-letnich siewek olszy czarnej. Wszystkie izolaty P. alni subsp. alni powodowały żółknięcie, brązowienie i przedwczesne opadanie liści. Najbardziej patogeniczne okazały się izolaty P. alni subsp. alni otrzymane z gleby oraz izolaty P. alni subsp. alni z Francji. Już po miesiącu od inokulacji podstawy pędu rośliny były całkowicie porażone. W drugim doświadczeniu siewki olszy wysadzano do sztucznie zakażonego podłoża. Wszystkie izolaty P. alni subsp. alni powodowały rozwój choroby, a najbardziej patogeniczne okazały się izolaty P. alni subsp. alni z gleby. Pozostałe dwa podgatunki, tj. subsp. uniformis i subsp. multiformis nie powodowały objawów chorobowych, zarówno w doświadczeniu z inokulacją podstawy pędu jak i z zakażaniem podłoża.
Olsza czarna (Alnus glutinosa) jest drzewem rozpowszechnionym w Polsce, szczególnie wzdłuż rzek, strumieni, jezior i stawów. Korzenie olsz żyją w symbiozie z bakteriami glebowymi, które mogą wiązać azot cząsteczkowy z powietrza i udostępniać go w postaci organicznych związków azotowych warstwie korzeniowej. Z tego powodu nasadzenia olszowe przyczyniają się do poprawy żyzności i uważane są za cenne gatunki pionierskie. Od kilkunastu lat w Polsce obserwuje się liczne zachorowania olsz. W wyniku przeprowadzonych badań z porażonych olsz oraz z ziemi otaczającej chore drzewa otrzymano 133 izolaty rodzaju Phytophthora. Amplifikacja otrzymanego DNA z zastosowaniem starterów ISSR i porównanie z izolatami referencyjnymi 11 gatunków Phytophthora pozwoliło na określenie przynależności gatunkowej patogenów. Dwadzieścia siedem zidentyfikowano jako P. alni subsp. alni, 13 jako P. cactorum oraz 21 jako P. citricola. Przynależność gatunkową potwierdzono za pomocą starterów gatunkowo-specyficznych.
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