Wood as a model material for medical biomaterials. In vivo and in vitro studies with bone and Betula pubescens Ehrh

Novel biomaterials are needed to fill the demand of tailored bone substitutes required by an ever‐expanding array of surgical procedures and techniques. Wood, a natural fiber composite, modified with heat treatment to alter its composition, may provide a novel approach to the further development of hierarchically structured biomaterials. The suitability of wood as a model biomaterial as well as the effects of heat treatment on the osteoconductivity of wood was studied by placing untreated and heat‐treated (at 220 C , 200 degrees and 140 degrees for 2 h) birch implants (size 4 x 7mm) into drill cavities in the distal femur of rabbits. The follow‐up period was 4, 8 and 20 weeks in all in vivo experiments. The flexural properties of wood as well as dimensional changes and hydroxyl apatite formation on the surface of wood (untreated, 140 degrees C and 200 degrees C heat‐treated wood) were tested using 3‐point bending and compression tests and immersion in simulated body fluid. The effect of premeasurement grinding and the effect of heat treatment on the surface roughness and contour of wood were tested with contact stylus and non‐contact profilometry. The effects of heat treatment of wood on its interactions with biological fluids was assessed using two different test media and real human blood in liquid penetration tests. The results of the in vivo experiments showed implanted wood to be well tolerated, with no implants rejected due to foreign body reactions. Heat treatment had significant effects on the biocompatibility of wood, allowing host bone to grow into tight contact with the implant, with occasional bone ingrowth into the channels of the wood implant. The results of the liquid immersion experiments showed hydroxyl apatite formation only in the most extensively heat‐treated wood specimens, which supported the results of the in vivo experiments. Parallel conclusions could be drawn based on the results of the liquid penetration test where human blood had the most favorable interaction with the most extensively heat‐treated wood of the compared materials (untreated, 140 degrees C and 200 degrees C heat‐treated wood). The increasing biocompatibility was inferred to result mainly from changes in the chemical composition of wood induced by the heat treatment, namely the altered arrangement and concentrations of functional chemical groups. However, the influence of microscopic changes in the cell walls, surface roughness and contour cannot be totally excluded. The heat treatment was hypothesized to produce a functional change in the liquid distribution within wood, which could have biological relevance. It was concluded that the highly evolved hierarchical anatomy of wood could yield information for the future development of bulk bone substitutes according to the ideology of bioinspiration. Furthermore, the results of the biomechanical tests established that heat treatment alters various biologically relevant mechanical properties of wood, thus expanding the possibilities of wood as a model material, which could include e.g. scaffold applications, bulk bone applications and serving as a tool for both mechanical testing and for further development of synthetic fiber reinforced composites.

Substâncias químicas com atividades alelopáticas presentes nas folhas de Parkia pendula (Leguminosae)

Os objetivos deste trabalho foram isolar, identificar e caracterizar a atividade alelopática de substâncias químicas produzidas por Parkia pendula. Os efeitos alelopáticos foram avaliados sobre a germinação de sementes e o desenvolvimento da radícula das plantas daninhas malícia (Mimosa pudica) e mata-pasto (Senna obtusifolia). O processo de isolamento das substâncias envolveu a extração com solvente em ordem crescente de polaridade, e a elucidação estrutural foi realizada via Ressonância Magnética Nuclear, espectro de COSY e de HETCOR. Os bioensaios foram desenvolvidos em condições controladas de 25 ºC de temperatura e fotoperíodo de 12 (germinação) e 24 horas (desenvolvimento da radícula). Foram isolados e identificados nas folhas da P. pendula os seguintes aleloquímicos: ácido 3,4,5-trimetoxibenzóico (S1), ácido 3,4-dimetoxibenzóico (S2) e o Blumenol A (S3). Comparativamente, S1 e S2 apresentaram maior atividade alelopática. Os efeitos promovidos sobre o desenvolvimento da radícula foram de maior magnitude do que aqueles verificados sobre a germinação das sementes. As substâncias isoladas mostraram baixo potencial inibitório da germinação das sementes, especialmente as sementes de mata-pasto. Os efeitos alelopáticos inibitórios estiveram positivamente associados à concentração das substâncias, embora em alguns casos esses efeitos não tenham correspondido às diferenças estatísticas.

Actividad alelopática de compuestos aislados de dos comelináceas:Rhoeo spathacea (Sw.) Stearn y Zebrina pendula Schinzlein.

Tesis (Maestría en Ciencias con Especialidad en Química de Productos Naturales) UANL

Crystallization and preliminary x-ray analysis of Parkia pendula lectin

Lectins are proteins important in various biological processes such as infection, cell differentiation and metastasis. The Parkia pendula lectin has been crystallized using the hanging-drop vapour diffusion method. X-ray diffraction data were collected using a Rigaku RU300 rotating anode generator and R-AXIS IV diffractometer. The cell parameters for P. pendula lectin are a=93.7 Angstrom b=161.1 Angstrom, c=80.0 Angstrom and space group C222. The maximum resolution was of 2.98 Angstrom. These data showed a R-sym=12.8%.

Substâncias químicas com atividades alelopáticas presentes nas folhas de Parkia pendula (Leguminosae)

Os objetivos deste trabalho foram isolar, identificar e caracterizar a atividade alelopática de substâncias químicas produzidas por Parkia pendula. Os efeitos alelopáticos foram avaliados sobre a germinação de sementes e o desenvolvimento da radícula das plantas daninhas malícia (Mimosa pudica) e mata-pasto (Senna obtusifolia). O processo de isolamento das substâncias envolveu a extração com solvente em ordem crescente de polaridade, e a elucidação estrutural foi realizada via Ressonância Magnética Nuclear, espectro de COSY e de HETCOR. Os bioensaios foram desenvolvidos em condições controladas de 25 ºC de temperatura e fotoperíodo de 12 (germinação) e 24 horas (desenvolvimento da radícula). Foram isolados e identificados nas folhas da P. pendula os seguintes aleloquímicos: ácido 3,4,5-trimetoxibenzóico (S1), ácido 3,4-dimetoxibenzóico (S2) e o Blumenol A (S3). Comparativamente, S1 e S2 apresentaram maior atividade alelopática. Os efeitos promovidos sobre o desenvolvimento da radícula foram de maior magnitude do que aqueles verificados sobre a germinação das sementes. As substâncias isoladas mostraram baixo potencial inibitório da germinação das sementes, especialmente as sementes de mata-pasto. Os efeitos alelopáticos inibitórios estiveram positivamente associados à concentração das substâncias, embora em alguns casos esses efeitos não tenham correspondido às diferenças estatísticas.

Holocene climate, fire and vegetation dynamics at the treeline in the Northwestern Swiss Alps

Treelines are expected to rise to higher elevations with climate warming; the rate and extent however are still largely unknown. Here we present the first multi-proxy palaeoecological study from the treeline in the Northwestern Swiss Alps that covers the entire Holocene. We reconstructed climate, fire and vegetation dynamics at Iffigsee, an alpine lake at 2,065 m a.s.l., by using seismic sedimentary surveys, loss on ignition, visible spectrum reflectance spectroscopy, pollen, spore, macrofossil and charcoal analyses. Afforestation with Larix decidua and tree Betula (probably B. pendula) started at ~9,800 cal. b.p., more than 1,000 years later than at similar elevations in the Central and Southern Alps, indicating cooler temperatures and/or a high seasonality. Highest biomass production and forest position of ~2,100–2,300 m a.s.l. are inferred during the Holocene Thermal Maximum from 7,000 to 5,000 cal. b.p. With the onset of pastoralism and transhumance at 6,800–6,500 cal. b.p., human impact became an important factor in the vegetation dynamics at Iffigsee. This early evidence of pastoralism is documented by the presence of grazing indicators (pollen, spores), as well as a wealth of archaeological finds at the nearby mountain pass of Schnidejoch. Human and fire impact during the Neolithic and Bronze Ages led to the establishment of pastures and facilitated the expansion of Picea abies and Alnus viridis. We expect that in mountain areas with land abandonment, the treeline will react quickly to future climate warming by shifting to higher elevations, causing drastic changes in species distribution and composition as well as severe biodiversity losses.

Morphological differentiation of Betula (birch) pollen in northwest North America and its palaeoecological application

Lake sediments from arcto-boreal regions commonly contain abundant Betula pollen. However, palaeoenvironmental interpretations of Betula pollen are often ambiguous because of the lack of reliable morphological features to distinguish among ecologically distinct Betula species in western North America. We measured the grain diameters and pore depths of pollen from three tree-birch species (B. papyrifera, B. kenaica and B. neoalaskana) and two shrub-birch species (B. glandulosa and B. nana), and calculated the ratio of grain diameter to pore depth (D/P ratio). No statistical difference exists in all three parameters between the shrub-birch species or between two of the tree-birch species (B. kenaica and B. papyrifera), and B. neoalaskana is intermediate between the shrub-birch and the other two tree-birch species. However, mean pore depth is significantly larger for the tree species than for the shrub species. In contrast, mean grain diameter cannot distinguish tree and shrub species. Mean D/P ratio separates tree and shrub species less clearly than pore depth, but this ratio can be used for verification. The threshold for distinguishing pollen of tree versus shrub birch lies at 2.55 μm and 8.30 for pore depth and D/P ratio, respectively. We'applied these thresholds to the analysis of Betula pollen in an Alaskan lake-sediment core spanning the past 800 years. Results show that shrub birch increased markedly at the expense of tree birch during the‘Little Ice Age’; this patten is not discernible in the profile of total birch pollen.

Betula humilis Schrank in Westpreußen

Von Hans Preuss

Pedology, geochronology, palynology and macrofossils of soil profiles in the Altdarss area, german Baltic Sea coast

A new site with Lateglacial palaeosols covered by 0.8 - 2.4 m thick aeolian sands is presented. The buried soils were subjected to multidisciplinary analyses (pedology, micromorphology, geochronology, dendrology, palynology, macrofossils). The buried soil cover comprises a catena from relatively dry ('Nano'-Podzol, Arenosol) via moist (Histic Gleysol, Gleysol) to wet conditions (Histosol). Dry soils are similar to the so-called Usselo soil, as described from sites in NW Europe and central Poland. The buried soil surface covers ca. 3.4 km**2. Pollen analyses date this surface into the late Aller0d. Due to a possible contamination by younger carbon, radiocarbon dates are too young. OSL dates indicate that the covering by aeolian sands most probably occurred during the Younger Dryas. Botanical analyses enables the reconstruction of a vegetation pattern typical for the late Allerod. Large wooden remains of pine and birch were recorded.

Palynological records of sediments from the Odderade type locality, north Germany

Reinvestigation of the Odderade Interstadial in its type locality led to an augmentation of the flora list and correction of some misinterpretations (e.g. Omorica, Frangula). The Eemian, stadials FW 1 and 3, and the interstadials Amersfoort/Broerup and Odderade have been manifested by pollen analyses. FW 1 and FW 3 are probably not completely free from forested areas. The new pollen diagrams considered with older data from Odderade, and in comparison with other regions in Central Europe, fit essentially with the classification and development of Vegetation during the Early Weichselian in Oerel by Behre & Lade (1986).