Imaging resource flow in soil-plant systems remains central to understanding plant development and interactions with the environment. Typically, subcellular resolution is required to fully elucidate the compartmentation, behavior, and mode of action of organic compounds and mineral elements within plants. For many situations this has been limited by the poor spatial resolution of imaging techniques and the inability to undertake studies in situ. Here we demonstrate the potential of Nanoscale Secondary Ion Mass Spectrometry (NanoSIMS), which is capable of the quantitative high-resolution spatial imaging of stable isotopes (e.g. 12C, 13C, 14N, 15N, 16O, 18O, 31P, 34S) within intact plant-microbial-soil systems. We present examples showing how the approach can be used to investigate competition for 15N-labeled nitrogen compounds between plant roots and soil microorganisms living in the rhizosphere and the spatial imaging of 31P in roots. We conclude that NanoSIMS has great potential to elucidate the flow of isotopically-labeled compounds in complex media (e.g. soil) and opens up countless new opportunities for studying plant responses to abiotic stress (e.g. 18O3, elevated 13CO2), signal exchange, nutrient flow and plant-microbial interactions.
The rate of organic matter turnover in soil is a critical component of the terrestrial carbon cycle and is frequently estimated from measurements of respiration. For estimates to be reliable requires that isotopically labelled substrate uptake into the soil microbial biomass and its subsequent mineralization occurs almost simultaneously (i.e. no time delay). Here we investigated this paradigm using glucose added to an agricultural soil. Immediately after collection from the field, various concentrations of 14C-labeled glucose (1μM to 10mM) were added to soil and the depletion from the soil solution measured at 1–60min after substrate addition. 14CO2 production from the mineralization of glucose was simultaneously measured. The microbial uptake of glucose from soil solution was concentration-dependent and kinetic analysis suggests the operation of at least two distinct glucose transport systems of differing affinity. At glucose concentrations reflecting those naturally present in the soil solution (54±10μM), the half-time (t 1/2) of exogenous glucose was extremely rapid at ca. 30s. At higher glucose concentrations (100μM to 10mM), the t 1/2 values for the high-affinity carrier were altered little, but increasing proportions of glucose were taken up by the low affinity transport system. Glucose mineralization by the soil microbial community showed a significant delay after its uptake into the microbial biomass suggesting a decoupling of glucose uptake and subsequent respiration, possibly by dilution of glucose in labile metabolite pools. By fitting a double first order kinetic equation to the mineralization results we estimated the t 1/2 for the first rapid phase of respiration at natural soil solution glucose concentrations to be 6–8min, but at least 87% of the added glucose was retained in the microbial biomass prior to mineralization. Our results suggest that in this soil the soil solution glucose pool turns over 100–1000 times each day, an order of magnitude faster than when determined from measurements of mineralization. These results imply that traditional isotopic based measurements of substrate turnover measured using CO2 may vastly underestimate their rate of cycling in soil.
Journal Article A quantitative risk assessment for the safety of carcase storage systems for scrapie infected farms Get access A. Adkin, A. Adkin Department of Epidemiological Sciences, Animal Health and Veterinary Laboratories Agency Weybridge UK Correspondence Amie Adkin, Senior Risk Analyst, Epidemiology, Surveillance and Risk Group, Woodham land, Addlestone, Surrey, KT15 3NB, UK. E‐mail: Amie.adkin@ahvla.gsi.gov.uk Search for other works by this author on: Oxford Academic Google Scholar D.L. Jones, D.L. Jones School of the Environment, Natural Resources and Geography Bangor University Bangor Gwynedd UK Search for other works by this author on: Oxford Academic Google Scholar R.L. Eckford, R.L. Eckford Veterinary Advisor, Office of the Chief Veterinary Officer Welsh Government Wales UK Search for other works by this author on: Oxford Academic Google Scholar G. Edwards‐Jones, G. Edwards‐Jones School of the Environment, Natural Resources and Geography Bangor University Bangor Gwynedd UK Search for other works by this author on: Oxford Academic Google Scholar A.P. Williams A.P. Williams School of the Environment, Natural Resources and Geography Bangor University Bangor Gwynedd UK Search for other works by this author on: Oxford Academic Google Scholar Journal of Applied Microbiology, Volume 117, Issue 4, 1 October 2014, Pages 940–948, https://doi.org/10.1111/jam.12596 Published: 01 October 2014 Article history Received: 26 February 2014 Revision received: 13 June 2014 Accepted: 04 July 2014 Published: 01 October 2014
The influx and efflux of sugar-C and the cycling of C within intact maize roots (Zea mays L.) was studied in sterile solution culture. Using metabolic inhi
Amino acids represent one of the largest inputs of dissolved organic nitrogen to soil and consequently they constitute a major component of the organic N cycle. The effect of agricultural management on the rate of amino acid turnover in soil, however, remains largely unknown. The aim of this study was to evaluate in long-term field experiments the effect of fertilizer addition (N, P and K), grazing, pH manipulation (lime addition), vegetation cover and shifts (grassland versus arable) and drainage on the mineralization of 14C-labelled amino acids in agricultural topsoils. Our results showed that the intrinsic rate of amino acid mineralization was rapid for all management regimes, irrespective of the tested soil type. The average (±SEM) half-life of the amino acids in all soils (n=155) was calculated to be 2.3±0.5h. The relative amount of amino acid-C partitioned into respiration (25% of total C) versus biomass production (75% of total C) was also unaffected by management strategy. The rate of amino acid mineralization was shown to be slightly sensitive to soil pH, peaking at around pH ( CaCl 2 ) 5.0with an approximate twofold reduction at the pH extremes (pH 3.8 and 6.4). We conclude that management regime has little effect on the intrinsic rate of amino acid mineralization in agricultural soils. We propose therefore that total microbial activity rather than microbial diversity or community structure is likely to be the key determinant governing amino acid turnover in agricultural soils.
poultry industries, with approximately 1,000 E. coli O157 cases reported in
What controls the rate of growth of roots? Behind this deceptively simple question lie a very complex set of processes within the plant and a wide range of environmental variables that affect root growth. To begin to answer it, we will simplify by making the...