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71.
The susceptibility of shelled corn to invasion by storage fungi was assessed using a carbon dioxide (CO2) test kit. Shelled corn samples were rewetted to either 16 or 21% wb moisture content (MC) and incubated ≤80 hr at either 24 or 30°C in sealed glass jars. CO2 concentration in the jars was quantified using the color number (0–5) of an indicator gel, which was determined either by visual comparison to a color card (VR) or using a Digital Color Reader (DCR). Plots of DCR color numbers versus time were smoother than those for VR color numbers. The DCR was better able to distinguish differences among samples, especially when color numbers were <2.0. The highest coefficients of determination (r2) for linear regressions of color number versus ergosterol difference were 0.75 for the DCR readings and 0.73 for the VR readings. Rankings of fungal susceptibility were similar at all four temperature‐MC combinations and many r2 values for linear regressions comparing readings at other conditions with those at 21% MC and 24°C were statistically significant (α ≤ 0.05). Incubation conditions and time of prior storage had a noticeable yet relatively minor effect on which fungi infected the kernels. 相似文献
72.
Deep-Sea coral evidence for rapid change in ventilation of the deep north atlantic 15,400 years Ago 总被引:1,自引:0,他引:1
Coupled radiocarbon and thorium-230 dates from benthic coral species reveal that the ventilation rate of the North Atlantic upper deep water varied greatly during the last deglaciation. Radiocarbon ages in several corals of the same age, 15.41 +/- 0.17 thousand years, and nearly the same depth, 1800 meters, in the western North Atlantic Ocean increased by as much as 670 years during the 30- to 160-year life spans of the samples. Cadmium/calcium ratios in one coral imply that the nutrient content of these deep waters also increased. Our data show that the deep ocean changed on decadal-centennial time scales during rapid changes in the surface ocean and the atmosphere. 相似文献
73.
DH Sandweiss H McInnis RL Burger A Cano B Ojeda R Paredes MC Sandweiss MD Glascock 《Science (New York, N.Y.)》1998,281(5384):1830-1832
Excavations at Quebrada Jaguay 280 (QJ-280) (16 degrees30'S) in south coastal Peru demonstrated that Paleoindian-age people of the Terminal Pleistocene (about 11,100 to 10,000 carbon-14 years before the present or about 13,000 to 11,000 calibrated years before the present) in South America relied on marine resources while resident on the coast, which extends the South American record of maritime exploitation by a millennium. This site supports recent evidence that Paleoindian-age people had diverse subsistence systems. The presence of obsidian at QJ-280 shows that the inhabitants had contact with the adjacent Andean highlands during the Terminal Pleistocene. 相似文献
74.
It is shown that lagged correlations for and cross-correlations between observed hemispheric-mean temperature data differ markedly from those for unforced (control-run) climate model simulations. The differences can be explained adequately by assuming that the observed data contain a significant externally forced component involving both natural (solar) and anthropogenic influences and that the global climate sensitivity is in the commonly accepted range. Solar forcing alone cannot reconcile the differences in autocorrelation structure between observations and model control-run data. 相似文献
75.
S Chen RS Ingram MJ Hostetler JJ Pietron RW Murray TG Schaaff JT Khoury MM Alvarez RL Whetten 《Science (New York, N.Y.)》1998,280(5372):2098-2101
A transition from metal-like double-layer capacitive charging to redox-like charging was observed in electrochemical ensemble Coulomb staircase experiments on solutions of gold nanoparticles of varied core size. The monodisperse gold nanoparticles are stabilized by short-chain alkanethiolate monolayers and have 8 to 38 kilodaltons core mass (1.1 to 1.9 nanometers in diameter). Larger cores display Coulomb staircase responses consistent with double-layer charging of metal-electrolyte interfaces, whereas smaller core nanoparticles exhibit redox chemical character, including a large central gap. The change in behavior is consistent with new near-infrared spectroscopic data showing an emerging gap between the highest occupied and lowest unoccupied orbitals of 0.4 to 0.9 electron volt. 相似文献
76.
The Canadian Basin of the Arctic Ocean, largely ice covered and isolated from deep contact with the more dynamic Eurasian Basin by the Lomonosov Ridge, has historically been considered an area of low productivity and particle flux and sluggish circulation. High-sensitivity mass-spectrometric measurements of the naturally occurring radionuclides protactinium-231 and thorium-230 in the deep Canada Basin and on the adjacent shelf indicate high particle fluxes and scavenging rates in this region. The thorium-232 data suggest that offshore advection of particulate material from the shelves contributes to scavenging of reactive materials in areas of permanent ice cover. 相似文献