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• W2037974327 abstract "A micromorphologically based pedosedimentary reconstruction of a 40-m loess–palaeosol sequence from the western part of the Chinese Loess Plateau provides a sensitive proxy record of changing processes and associated environmental conditions in this region between ca. 150 000 and 10 000 yr BP. Depth functions of more traditional climate proxies, such as magnetic susceptibility, calcium carbonate content and median grain size, support the broad pattern of environmental changes inferred from the micromorphology, although the bulk properties sometimes lag behind or are out of phase with each other and do not match all the fluctuations in the micromorphological record. The reasons for the disparities are probably complex, although they partly reflect differences in response rates and sensitivities of proxies to different climate parameters, as well as genuine out-of-phase changes in strength of monsoonal climate controls. This work illustrates the sensitivity of micromorphology in detecting past environmental changes within rapidly aggrading landscapes, and emphasises the need to understand more fully the local and regional significance of bulk proxies currently used in global correlations with marine- and ice-core records. Copyright © 1999 John Wiley & Sons, Ltd." @default.
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• W2037974327 date "1999-02-01" @default.
• W2037974327 modified "2023-09-27" @default.
• W2037974327 title "Comparison of proxy records of Late Pleistocene climate change from a high-resolution loess-palaeosol sequence in north-central China" @default.
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• W2037974327 doi "https://doi.org/10.1002/(sici)1099-1417(199902)14:1<91::aid-jqs440>3.0.co;2-1" @default.
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