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- W1037219219 endingPage "216" @default.
- W1037219219 startingPage "183" @default.
- W1037219219 abstract "This chapter deals with Eolian deposits, consisting of both dune and sheet sand in South and North America. Much of the loess present on both continents, which are derived from glacial outwash sources and deposited during the last glacial maximum. Cold, dry, windy conditions during the last glacial period have favored loess deposition from a variety of sources. Eolian sand is extensive on both the continents. Holocene eolian sand is abundant in the Pampas region of South America. Deep-sea sediment cores, ice cores, and soils contain long-term records of the dust flux. Deposition of loess and eolian sand, from multiple sources during the last glacial period, agrees with pollen records, lake records, and COHMAP (Cooperative Holocene Climate Mapping) climate simulations. In the Pampas region of South America, there is at least fair agreement between summer surface winds simulated by COHMAP and paleowinds as recorded by eolian sand and loess. In mid-continental North America, however, the presence of a strong glacial anticyclone centered over the Laurentide ice sheet generates northeasterly winds in the region immediately to the south of the ice sheet. Both eolian records and lacustrine records indicate that there are multiple periods of relatively dry climate during the late Holocene." @default.
- W1037219219 created "2016-06-24" @default.
- W1037219219 creator A5004231866 @default.
- W1037219219 creator A5055336005 @default.
- W1037219219 date "2001-01-01" @default.
- W1037219219 modified "2023-09-25" @default.
- W1037219219 title "Late Quaternary Eolian Records of the Americas and Their Paleoclimatic Significance" @default.
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