The biogeography and historical ecology of Lobelia urens L.(r)(the heath lobelia) in southern England

This paper examines the past and present ecology and biogeography of Lobelia urens L. (the heath lobelia) which is threatened with extinction in southern England. A survey of the historical and documentary evidence of the distribution of the species is presented. Historical records exist for nineteen sites in the south but nowhere else in England. The status of L. urens is in decline in Britain with ten populations having been lost this century. The six remaining sites have been surveyed to describe the phytosociology of L. urens communities and the variability of the environmental factors controlling its distribution. A total of ninety-five quadrats containing 122 species were recorded and analysed using two-way indicator species analysis. Canonical correspondence analysis was used to assess the correlations between twenty-eight environmental variables and the floristic variation in the ninety-five quadrats. These were reduced to sixteen variables for the final analysis. L. urens is shown to be a member of rough, grass-heath communities (NVC M25 and W23) dominated by Molinia caerulea and situated on seasonally waterlogged, moderately acidic, nutrient-poor soils. The species is suited to both cyclical and sporadic soil disturbance regimes. The final discussion argues that existing populations will only be maintained and expansion of the species distribution occur, if conservationists prevent woodland succession in L. urens sites and periodically disturb the ground in locations where the species survives at present and also where it has been observed in the recent past. This link between historical ecology and present-day conservation management would appear very important. Further demographic and experimental work is needed to explore these predictions and their implications for the future conservation management of L. urens .     

Investigation on arteriosclerosis among population in a rare earth area in South China

An ophthalmofunduscope was used to investigate arteriosclerosis among villagers aged 20–40 yr old in two rare earth areas in Ganzhou, Jiangxi Province. It was noted that the occurrence of arteriosclerosis of the fundus aculi was significantly high (P < 0.05-0.01), the detection of serum cholesterol (CHO) was remarkably increased (P < 0.01), and the level of IgM was also elevated. However, high-density lipoprotein (HDL) remained at a low level. The effect of taking rare earth elements (REE) could be direct or indirect, thus causing an increase in cholesterol and interfering with the synthesis of high-density lipoprotein. Furthermore, rare earth could also cause immunogenic damage to the vascular wall. All of these could facilitate the formation of arteriosclerosis.     

Uptake of Trace Metals and Rare Earth Elements from Hornblende by a Soil Bacterium

Analysis of trace elements released from hornblende between pH 6.5 and 7.5 in the presence of Arthrobacter sp. shows that Fe, Ni, V, Mn, and, to a lesser extent, Co are preferentially released into solution relative to bacteria-free experiments. This enhanced release into solution could be due to contributions from the slightly lowered pH, the presence of low molecular weight organic acids (LMWOAs), or the presence of a catecholate siderophore in experiments with bacteria. The best explanation for enhanced metal release is siderophore complexation at the mineral surface followed by release to solution. However,the relative rates of metal release to solution in these experiments do not strictly follow the trend predicted by the relative ordering of metal hydrolysis, which might be predicted for siderophore-promoted dissolution. For some of these metals, release to solution is fast initially in biotic experiments, but concentrations in solution reach a steady state value or decrease with time as the bacteria cell numbers increase exponentially. Lack of enhanced release to solution for some metals and decreases in release rate with time for others may be explained by uptake into bacteria. Many of the metals predicted to strongly complex with siderophore (including Al, Ti, Fe, Cu) are heavily taken up into cellular material. The relative ordering of organic ligand-element complexation may therefore partially explain the relative ordering of uptake of trace metals and rare earth elements into cell material. Fractionation of heavy rare earth elements taken up into cellular material is also very strong, and increases from Ho to Lu. Strong fractionation in uptake of some elements by bacteria may create biological signatures either in the mineral substrate or in any mineral precipitates associated with the cellular material.     

Genetic diversity and phenotypic variation in marginal populations of the locally endangered speciesHordeum secalinum (Poaceae)

Electrophoresis was used to compare variation in hordein polypeptide patterns and isozymes in five marginal populations ofHordeum secalinum (four Swedish and one Danish population) and four populations along the Atlantic coast from Denmark to Spain. Hordein patterns were uniform within and among Swedish and Danish populations whereas the materials from France and Spain were divergent. The banding patterns for nine isozymes (AAT, IDH, MDH, PGD, GPI, ME, ACP, EST, and PRX) agreed with those reported for otherHordeum species. All putative loci were monomorphic with the exception of PRX, which showed three different phenotypes. The five marginal populations varied in seed set and cultivated plants differed in phenological traits.Dedicated to emer. Univ.-Prof. DrFriedrich Ehrendorfer on the occasion of his 70th birthday     

Phylogenetic diversity and ecological features in the Egyptian flora

Until fairly recently, regional-scale ecological and evolutionarypatterns have tended to be ignored as conservation efforts have been concernedwith species and their habitats. Here we compare frequencies in the Egyptianflora of particular rank sizes (order, family and genus) with patterns ofspecies abundance (classified as very rare, rare, common, or very common) and anarray of life-history attributes. The angiosperm flora of Egypt is representedby 2446 taxa (2088 species), including taxa in 10 subclasses, 51 orders, 120families, and 742 genera. A high degree of monotypism was observed: four ordersare monotypic (each existing as single species), and have very rare overallabundances; 30 families are monotypic (17 of which are very rare or rare); and 354genera are monotypic (over 70% of which are very rare or rare). Fourteenfamilies (in particular the Resedaceae and Zygophyllaceae) have at leastone-fifth of their global species represented in the Egyptian flora. Introducedspecies in general, and tree, aquatic herb and liana life forms all are especially well represented among monotypic genera. Native taxa are highlyrepresented among rare and very rare abundance classes, while introduced taxadid not differ significantly in their abundance patterns, compared to overallflora values. Few large genera (>20 spp.) occur in the flora, with mostspecies concentrated in genera containing 8–19 species per genus.Similarly, few families were highly speciose. Annual and herbaceous species weresignificantly over-represented, mainly among large, speciose genera andfamilies. However, perennials, trees, shrubs, aquatic herbs, lianas and parasiticspecies were found mainly in families and genera having very few taxa.Life-history attributes may have important implications to speciation rates.Taxonomically based results, involving abundances and life-history attributes,are discussed in the context of biodiversity and conservation.