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- W2034911751 abstract "Initial interpretation of the sediments from the Burmester core (Eardley et al. (1973). Geological Society of America Bulletin 84, 211–216) indicated that 17 deep-lake cycles, separated by shallow-lake and soil-forming intervals, occurred in the Bonneville basin during the Brunhes Chron (the last 780 × 10 3 yr). Our re-examination of the core, along with new sedimentological, geochronological, and paleontological data, indicate that only four deep-lake cycles occurred during this period, apparently correlative with marine oxygen-isotope stages 2, 6, 12, and 16. This interpretation suggests that large lakes formed in the Bonneville basin only during the most extensive of the Northern Hemisphere glaciations." @default.
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- W2034911751 date "1999-09-01" @default.
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- W2034911751 title "Reinterpretation of the Burmester Core, Bonneville Basin, Utah" @default.
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- W2034911751 doi "https://doi.org/10.1006/qres.1999.2058" @default.
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