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- W2003876298 abstract "Fine quartz silt (1–10μm dia, important in aerosol dust) isolated from a large number of soils, as well as Phanerozoic shales, sandstones and recent sands of the southern African stratigraphie column (Carboniferous, Permian and Triassic) exhibits a mean δ18O of 12.2 ± 2.1%0. These values are similar to those reported for South Pacific pelagic sediments and adjacent land areas of similar latitude but are lower than those reported for this size fraction of 30 Mesozoic and Paleozoic shales (20.7 ± 1.8%.) and soils from mid-continental U.S.A., for aerosol quartz in the North Pacific pelagic sediments, and for eolian caps in high-elevation soils of Hawaii. The lower oxygen isotopic ratios in fine quartz silt of southern Africa reinforces the earlier indication that Southern Hemisphere detritai sedimentary reservoirs contain a higher proportion of igneous and metamorphic quartz (lower δ18O) and less lowtemperature authigenic quartz (higherδ18O) than Northern Hemisphere detritai sediments. The difference reflects climates, as continents drifted in latitude." @default.
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- W2003876298 date "1980-03-01" @default.
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- W2003876298 title "Oxygen isotopic ratios in fine quartz silt from sediments and soils of southern Africa" @default.
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- W2003876298 doi "https://doi.org/10.1016/0016-7037(80)90049-6" @default.
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