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• W1560418462 abstract "Dust lifted from arid and semiarid continental surfaces, commonly by large spring and summer storms, travels transoceanic distances and forms an important component of deep-sea sediments. That sedimentary record provides a history of continental aridity in the dust flux data, a history of the intensity of the prevailing winds in the dust grain-size data, and a record of provenance in the geochemistry of the dust grains. Furthermore, identification of eolian source regions permits reconstruction of transport pathways via the zonal winds. All these aspects of the sedimentary dust record have been brought to bear on fundamental problems of climate and climate change during Cenozoic times." @default.
• W1560418462 created "2016-06-24" @default.
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• W1560418462 date "2013-01-01" @default.
• W1560418462 modified "2023-10-14" @default.
• W1560418462 title "EOLIAN RECORDS, DEEP-SEA SEDIMENTS" @default.
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• W1560418462 doi "https://doi.org/10.1016/b978-0-444-53643-3.00155-2" @default.
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