Einfluss organischer Substanz auf die Reproduktion, Biomasse und Akkumulation hydrophober Schadstoffe in Lumbriculus variegatus

Background, aim, and scope Sediment-Water Toxicity Tests are an important instrument for the environmental risk assessment of native, contaminated sediments within the European Water Framework Directive. Thus, it must be guaranteed to distinguish between natural and anthropogenic adverse effects. The content of particulate (POC) and dissolved (DOC) organic carbon can affect the mobility of sediment pollutants. Different studies demonstrated that the DOC-content can influence the bioavailability of contaminants and can directly affect aquatic organisms. The aim of this study was to investigate the influence of increasing sediment organic matter on reproduction and growth of the benthic oligochaete Lumbriculus variegatus. Furthermore, the accumulation factors of the hydrophobic substances 1,1-dichloro-2,2-bis(p-chlorphenyl)ethylene (p,p'-DDE), 2´, 3, 4, 4´, 5´-Hexachlorbiphenyl (PCB 138) und 2, 2´, 4, 4´, 5, 5´-Hexachlorbiphenyl (PCB 153) were calculated considering the TOC-content and the uptake route (water-only exposure or sediment ingestion). Materials and methods The test was performed according to the OECD Guideline 225 (2007) using artificial sediment with different peat concentrations. The effect of an increasing TOC-concentration was studied in three different testmodifications with and without spiked sediment. The nominal concentration of the contaminants in spiked sediment was 50?µg/kg. Results The results showed maximum accumulation factors of 13 for both, PCB 138 and 153 and 11 for p,p'-DDE in sediments with low organic carbon content. With increasing peat content accumulation factors decreased. Thereby the ingestion of sediment was the main exposure route. Moreover preponderantly negative correlations between the organic carbon content in unspiked sediments and reproduction as well as growth of the testorganisms were detected. In combination with the test substances reproduction and growth increased with increasing organic carbon content. Discussion Hence it can be assumed that organic matter, especially humic substances, directly effected the testorganisms in the tests without spiked sediment. Due to the decrease of accumulation factors in spiked sediment with increasing TOC-content it might be possible that the availability of humic substances was reduced by conglomeration with the tested chemicals. Conclusions Therefore the possible influence of dissolved organic matter on the testorganism should be considered when assessing the results of toxicity tests and bioaccumulation studies with Lumbriculus variegatus. Recommendations and perspectives To receive detailed information about a critical DOC-concentration influencing the testorganisms further investigations about the amount of organic matter in the sediment and the DOC-concentration in the overlaying water are recommended.     

Determining Minimum Habitat Areas and Habitat Corridors for Cougars

I simulated population dynamics of cougars to predict the minimum areas and levels of immigration needed to avoid population extinction caused by demographic and environmental stochasticity for a period of 100 years. Under most plausible parameter values, the model predicted very low extinction risk in areas as small as 2200 km², and (in the absence of immigration) increasing risk as area decreased below 2200 km². If as few as one to four animals per decade could immigrate into a small population, the probability of population persistence increased markedly. Thus a corridor for immigration will benefit a small population in an area where further loss of habitat will occur. The model was applied to the cougar population in the Santa Ana Mountain Range of southern California (2070 km², with about 20 adults). Field data support the model’s conclusion that this population is demographically unstable. There will be a high risk of extinction if the habitat is reduced to currently protected and connected areas (1114 km²). A movement corridor allowing immigration from the adjacent population and intra-range corridors would greatly enhance the prognosis. However, the last corridor for immigration has been degraded by recent human activity. Within the mountain range, cougars recently became extinct in a 75 km² habitat fragment recently isolated by development, and cougars will become extinct in another 150 km² of habitat if a proposed housing project occludes a critical corridor. Radio tracking has confirmed use of this and other important corridors. Neither the model nor the field data alone would have much influence in the face of development pressure; together they have stimulated interest in restoring and protecting critical corridors in this range. Nonetheless, the long-term prognosis for this populations is bleak, because 22 local governments review potential impact on a case-by-case basis. Effective land-use planning must be spatially explicit and regional in scope. Because cougars need corridors and because telemetered cougars can quickly identify movement corridors, cougar research is an efficient and appropriate way to inject biological data into such planning efforts.     

Effects of Climate and Ecosystem Disturbances on Biogeochemical Cycling in a Semi-Natural Terrestrial Ecosystem

The effects of increased temperature and potential ecosystem disturbances on biogeochemical cycling were investigated by manipulation of temperature in a mixed Calluna/grass heathland in Denmark. A reflective curtain covered the vegetation during the night to reduce the heat loss of IR radiation from the ecosystem to the atmosphere. This `night time warming' was done for 3 years and warmed the air and soil by 1.1 °C. Warming was combined with ecosystem disturbances, including infestation by Calluna heather beetles (Lochmaea suturalis Thompson) causing complete defoliation of Calluna leaves during the summer 2000, and subsequent harvesting of all aboveground biomass during the autumn. Small increases in mineralisation rates were induced by warming and resulted in increased leaching of nitrogen from the organic soil layer. The increased nitrogen leaching from the organic soil layer was re-immobilised in the mineral soil layer as warming stimulated plant growth and thereby increased nitrogen immobilisation. Contradictory to the generally moderate effects of warming, the heather beetle infestation had very strong effects on mineralisation rates and the plant community. The grasses completely out-competed the Calluna plants which had not re-established two years after the infestation, probably due to combined effects of increased nutrient availability and the defoliation of Calluna. On the short term, ecosystem disturbances may have very strong effects on internal ecosystem processes and plant community structure compared to the more long-term effects of climate change.     

A method for classifying multidimensional data with respect to uncertainties of measurement and its application to archaeometry

This study was supported by the Bundesministerium für Forschung und Technologie (BMFT), core program Einsatz neuer Technologien in den Geisteswissenschaften.     

Synthetische Nanopartikel — Entwicklungschancen im Dialog

This article provides an overview on the opportunities and risks of nanotechology. It is the outcome of a first national stakelholder dialogue carried out by the Federal Environment Ministry in October 2005. Recommendations are provided for further risk communication.     

Altersklassierung von Gew?ssersedimenten Messung der radioaktivit?t von isotopen

Ziel dieser Untersuchung war die Beantwortung der Frage, in wieweit mit Hilfe der Messung der Radioaktivit?t von Umweltisotopen eine Aussage zum Alter von Einzelproben des Gew?ssersediments m?glich ist. Voraussetzung ist, da? die Sedimente n?herungsweisegleichf?rmig abgelagerte Schwebstoffe sind, und sei es auch nur in gewissen Zeitabschnitten (Zeitfenstern). Proben chaotisch wechselnder Sedimentation und Erosion sind z.Zt. nicht beurteilbar im Hinblick auf ihr Alter. Folgerung aus den Messungen von Umweltisotopen: Die Einzelproben werden mitReferenzschwebstoffen der 0 bis 38 μm Feinkornfraktion hinsichtlich ihrer Radioaktivit?tskonzentration verglichen. Dann werden sie grob in vier Altersklassen eingeteilt:

Pathway of CH4 formation in anoxic rice field soil and rice roots determined by 13C-stable isotope fractionation

In anoxic rice fields methane is produced by either reduction of CO2 or cleavage of acetate. We measured the delta 13C-values of CH4 and CO2, acetate and organic carbon during time course experiments with anoxic methanogenic soil and root samples and used these values to calculate the fractions of CH4 (and acetate) produced from CO2 reduction. Comparison with radiotracer and/or inhibitor studies constrained the kinetic fractionation factors used for calculation. The fractionation factors for the conversion of CO2 to CH4 and of acetate to CH4 were on the order of alpha = 1.07 (epsilon = -70%) and epsilon > or = - 20%, respectively. The pathway of CH4 production changed with time of anoxic incubation. Anoxic slurries of rice field soil first produced CH4 predominantly (>50%) from CO2, then predominantly (>80%) from acetate and finally (after about one month) according to the theoretically expected ratio (33% CO2 and 67% acetate). Anoxic rice roots, on the other hand, initially produced CH4 exclusively from CO2, followed by contribution of acetate of about 40-60%. Rice roots also produced acetate that partially originated (< or = 1 30%) from reduction of CO2 as determined by calculation of isotopic fractionation using fractionation factors from the literature. The results demonstrate that there is quite some variability in pathways of CH4 production, and also indicate that isotopic fractionation factors may be different in different habitats and change with time.