Three-dimensional structure and cyanobacterial activity within a desert biological soil crust.

Desert biological soil crusts (BSCs) are formed by adhesion of soil particles to polysaccharides excreted by filamentous cyanobacteria, the pioneers and main producers in this habitat. Biological soil crust destruction is a central factor leading to land degradation and desertification. We study the effect of BSC structure on cyanobacterial activity. Micro-scale structural analysis using X-ray microtomography revealed a vesiculated layer 1.5-2.5 mm beneath the surface in close proximity to the cyanobacterial location. Light profiles showed attenuation with depth of 1%-5% of surface light within 1 mm but also revealed the presence of 'light pockets', coinciding with the vesiculated layer, where the irradiance was 10-fold higher than adjacent crust parts at the same depth. Maximal photosynthetic activity, examined by O2 concentration profiles, was observed 1 mm beneath the surface and another peak in association with the 'light pockets'. Thus, photosynthetic activity may not be visible to currently used remote sensing techniques, suggesting that BSCs' contribution to terrestrial productivity is underestimated. Exposure to irradiance higher than 10% full sunlight diminished chlorophyll fluorescence, whereas O2 evolution and CO2 uptake rose, indicating that fluorescence did not reflect cyanobacterial photosynthetic activity. Our data also indicate that although resistant to high illumination, the BSC-inhabiting cyanobacteria function as 'low-light adapted' organisms.

Environmental risk of (heavy) metal release from urns into cemetery soils.

Cremation of the deceased has become the most common funeral type in many countries in the world, including Germany. The ashes of the cremated human body (cremains) are transferred in an urn and most commonly buried in the soil. However, the possible environmental impacts of cremains on soils and groundwater have been rarely studied. In this context, it is still unclear whether or not the release of (heavy) metals like chromium, zinc, copper, nickel and lead from cremains and urns poses an environmental problem in urn grave soils. The aims of the study were to analyze the (heavy) metal content of two cremains from a 74-year-old male and 70-year-old female, and of soils in 6 cemeteries with urn graves in North and West Germany. Soil samples were taken from below the burial depth of 42 urns (upon expiry of the resting time) and from reference soils without urn burials (same cemetery site and depth). The two cremains differed significantly in their heavy metal content (zinc, nickel, copper, chromium), which originated from metal components of the deceased's clothing or burial objects or may have resulted from contrasting occupational exposure during the deceased's lives. Investigations at the cemetery sites revealed a high variability in (heavy) metal contents in the soil samples from below the buried urns. As expected, the accumulation of some element (e.g., lead and tin) in the soil increased with a higher degradation degree of the urns, but an enrichment in copper, chromium, nickel, and iron was also detected below only slightly corroded but not yet perforated urns, which were often made out of copper-bearing material and other alloying agents. This demonstrated that heavy metal releases into cemetery soils originated from both cremains and urn material.

Influence of non-invasive X-ray computed tomography (XRCT) on the microbial community structure and function in soil.

In this study the influence of X-ray computed tomography (XRCT) on the microbial community structure and function in soils has been investigated. Our results clearly indicate that XRCT of soil samples has a strong impact on microbial communities and changes structure and function significantly due to the death of selected microbial groups as a result of the treatment.

Soil microbes and soil respiration of Mongolian Steppe soils under grazing stress.

Soils of Northern China were analysed for their microbiological and soil physical properties with respect to different grazing stress. An important factor for this is soil compaction and related aeration due to pore size shifts. Bulk density increases significantly with increasing grazing intensity and soil carbon contents show decreasing values from top to depth. Organic carbon (LOI) concentrations decrease significantly with increasing grazing intensity. The data on LOI (2-5.8%) approximate 10-30 mg C, our data on glucose show values between 0.4-1.2 mg, i.e. approx. 4% of total carbon. Numbers and biomass of bacteria show generally a decreasing trend of those data at grazed and ungrazed sites, numbers range between 0.4 and 8.7 x10(8) g(-1) d.wt., bacterial biomass between 0.4 and 3.8 microg Cg(-1). This need to be recorded in relation to soil compaction and herewith-hampered aeration and nutrient flow. The temperature-respiration data also allow getting an idea of the Q10-values for soil respiration. The data are between 2.24 (5-15 degrees C) and 1.2 (25-35 degrees C). Our data are presented with a general review of biological properties of Mongolian Steppe soils.