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Nitrogen (N) and sulphur (S) are essential for plant growth and development. Cysteine (Cys) and methionine (Met) are N- and S-containing amino acids in soi
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A method is presented for determining both the average turnover rate and the standard deviation of the average turnover rate of the adenine nucleotide (AN) pool within a population of microorganisms. The method requires the calculation of the initial slope and curvature of a plot of AN specific activity versus time following the introduction of [ 3 H]adenine. An analysis of noise-corrupted data indicated that the method is capable of detecting a lack of uniformity in the turnover rate when the coefficient of variation of the turnover rate exceeds 39%. An analysis of field data revealed a significant lack of uniformity in the turnover rates of microbial communities in a marine sediment sample and freshwater pond but no significant nonuniformity in the turnover rates of microbial communities in a seawater sample and in a second freshwater pond. Although the method has been applied only to the analysis of AN turnover rates, it is applicable to any intracellular pool for which a suitable radioactive precursor exists.
Soil organic matter is known to directly influence nutrient capture and affect the growth of arbuscular mycorrhizal fungi (AMF). The effect of organic-rich patches in soil on subsequent sporulation and the persistence of spores will have important implications for sustainable agricultural practices particularly as AMF spores are likely to play a significant role in soil carbon dynamics and ecosystem productivity. We have used a mesh-exclusion approach to quantify the temporal dynamics of AMF sporulation in organic-rich patches following host shoot excision. Wheat plants were grown in pots, filled with sterile sand inoculated with Glomus intraradices, Glomus mosseae or a non-mycorrhizal control. Each pot contained three 25cm3 mesh bags (35μm), filled with either farmyard manure (FYM), soil or sand. At 6 weeks post-emergence the host shoot was excised and AMF spores were quantified in each of the mesh bags and again at 24, 52, 66 and 80 days after host excision. Spore numbers were far higher in FYM than in patches of soil, although by 24 days after shoot excision the number of spores had dramatically decreased in patches of both FYM and soil; however this was followed by a significant increase in spore numbers of G. intraradices in the FYM patches. Extractable P, NO3 − and NH4 + in the mesh bags were all significantly higher in the FYM patches than in the patches of soil, although there were no differences between the control and the mycorrhizal treatments. However, the concentration of soluble phenolics in the FYM colonised by both of the AMF species significantly decreased between 0 and 24 days after host excision compared to the control. This finding provides novel insights into the nature of asymbiotic sporulation in organic-rich patches and has important implications for sustainable agricultural practices, including FYM application enhancing the ‘mycorrhizal potential’ of soil following a harvest, by increasing the amount of early colonisation in the next crop.
<p>Peatlands cover three percent of the global land surface. However, they store significant amounts of carbon (C), approximately 30%. Peatlands are drained to support agricultural production. It’s estimated that agriculture exploits approximately 20% of peatlands worldwide. The exploited peatlands are significant emitters of carbon dioxide (CO<sub>2</sub>) and nitrous oxide (N<sub>2</sub>O). In Europe, agriculture is the second largest contributor of greenhouse gas (GHG) emissions. In addition to GHG emissions, we are fast losing productive peatlands; it’s estimated by 2050, a third of productive peatlands will be lost. Loss of productive peatlands will affect productivity and food security.</p><p>To prolong use of peatlands, ploughing in of crop residue, either from the previous season or specially grown crop, is often considered a mitigation option. Nevertheless, there is concern that fresh organic matter (FOM) might accelerate decomposition of existing organic. This study assesses effects of FOM on the emissions of CO<sub>2</sub>, methane (CH<sub>4</sub>) and N<sub>2</sub>O in a cultivated peatland. A mesocosm experiment was carried out using intact cores with added FOM and manipulated water table (WT), -20 and -50 cm.</p><p>The results show there is an effect of both WT and FOM on emissions. CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O emissions differ in the different WT treatments. The -20 cm cores produced more methane than the -50 cm.  It is evident that leaving crop residue and then ploughing it in does not have the desired effect as it led to increased emissions.</p>
No abstract is provided for this article.
SUMMARY Using the scanning electron microscope with microprobe analysis, observations have been made on the weathering of rock‐forming minerals—feldspars, ferromagnesian minerals, quartz and serpentine—principally by crustose lichens. A variety of phenomena can be recognized, namely, etching patterns, decomposition features and secondary products which can be related to differences in mineral structure and composition. Such weathering has been proved to involve the chelating effects of oxalic acid in certain lichens, although lichen acids could also be implicated.