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- W2058128423 abstract "In the Wanganui region of North Island, New Zealand, a record of climate change for the last ca. 500 ka is preserved in a terrestrial cover bed sequence. Eleven loess layers from five major glacial cycles are separated by paleosols and punctuated by both rhyolitic and andesitic tephra layers. The dated rhyolitic tephras, thermoluminescence dates from the loess, and dated marine terraces on which the sequence rests, provide good chronological control. A detailed stratigraphy and the use of four physical and chemical parameters enables a climatic interpretation, and a correlation with the marine oxygen isotope record, to be made. Variations in dry bulk density and potassium content have resulted from weathering of the upper part of each loess unit during a warmer climate than that responsible for generation of the loess. Fluctuations in quartz content and magnetic susceptibility are of sedimentary origin and represent alternating quartzo-feldspathic and andesitic provenance. Fluctuations in potassium content and dry bulk density are caused by weathering of the accumulating sediment. Glacial periods were times of environmental destabilization, loess accumulation, and least weathering, while warm periods saw soil formation and gentle accession of andesitic tephra. The main periods of environmental destabilization were during marine Oxygen Isotope Stages 2, 3 (upper part), 6, 8, 10, and 12, while stages 1, 3 (lower part), 5, 7, 9, 11, and 13 provided most stable conditions and soil formation." @default.
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- W2058128423 date "1996-01-01" @default.
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- W2058128423 title "Record of climatic fluctuations from ca. 500 ka loess deposits and paleosols near Wanganui, New Zealand" @default.
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- W2058128423 doi "https://doi.org/10.1016/1040-6182(95)00080-1" @default.
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