Microbial biomass growth, following incorporation of biochars produced at 350 ?C or 700 ?C, in a silty-clay loam soil of high and low pH

Biochar has been widely proposed as a soil amendment, with reports of benefits to soil physical, chemical and biological properties. To quantify the changes in soil microbial biomass and to understand the mechanisms involved, two biochars were prepared at 350 \ub0C (BC350) and 700 \ub0C (BC700) from Miscanthus giganteus, a C4 plant, naturally enriched with 13C. The biochars were added to soils of about pH 4 and 8, which were both sampled from a soil pH gradient of the same soil type. Isotopic (13C) techniques were used to investigate biochar C availability to the biomass. Scanning Electron Microscopy (SEM) was used to observe the microbial colonization, and Attenuated Total Reflectance (ATR) to highlight structural changes at the surface of the biochars. After 90 days incubation, BC350 significantly increased the biomass C concentration relative to the controls in both the low (p < 0.05) and high pH soil (p < 0.01). It declined between day 90 and 180. The same trend occurred with soil microbial ATP. Overall, biomass C and ATP concentrations were closely correlated over all treatments (R2 = 0.87). This indicates that neither the biomass C, nor ATP analyses were affected by the biochars, unless, of course, they were both affected in the same way, which is highly unlikely. About 20% of microbial biomass 13C was derived from BC350 after 90 days of incubation in both low and high pH soils. However, less than 2% of biomass 13C was derived from BC700 in the high pH soil, showing very low biological availability of BC700. After 90 days of incubation, microbial colonization in the charsphere (defined here as the interface between soil and biochar) was more pronounced with the BC350 in the low pH soil. This was consistent with the biomass C and ATP results. The microbial colonization following biochar addition in our study was mainly attributed to biochar C availability and its large surface area. There was a close linear relationship between 13CO2 evolved and biomass 13C, suggesting that biochar mineralization is essentially a biological process. The interactions between non-living and living organic C forms, which are vital in terms of soil fertility and the global C cycle, may be favoured in the charsphere, which has unique properties, distinct from both the internal biochar and the bulk soil. \ua9 2012 Elsevier Ltd

Chromosomal location of the amplified esterase genes conferring resistance to insecticides in Myzus persicae (Homoptera: Aphididae)

A genomic probe encompassing most of an esterase gene (E4) that is amplified in insecticide-resistant Myzus persicae was hybridized in situ to mitotic and meiotic chromosome preparations of aphid clones of known esterase type and resistance level. Binding, which was detected using the biotin-avidin system located both known types of amplified esterase sequences (E4 and FE4). All except one of the E4-producing clones had a single amplified site, on autosome 3 near the break-point of an autosomal 1,3 translocation which previous work had shown to be genetically linked to insecticide resistance. The exceptional clone had two other E4-encoding sites. The most resistant FE4-producing clone (800F) had amplified sequences at five sites (three loci: two homozygous and one heterozygous). Altogether, amplified E4 and/or FE4 sequences were found on four of the five autosome pairs of M. persicae. Possible origins of these multiple loci are discussed