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• W4385522924 endingPage "108255" @default.
• W4385522924 startingPage "108255" @default.
• W4385522924 abstract "Substantial stratigraphic evidence from the Late Quaternary at orbital- and millennial‒scales indicates that the formation and evolution of aeolian‒sand landscapes results from the interaction between regional aeolian and fluvial‒lacustrine activity. In many deserts (sandy lands) across the planet, fluvial‒aeolian interplay at the glacial‒interglacial scale since the Late Quaternary has been responsive to monsoonal precipitation, and linked to atmospheric CO2 and periodic variations in insolation. However, the patterns of fluvial‒aeolian interplay and their relationship with climate change are not always consistent over a given timescale during the Late Pleistocene. The paucity of studies on fluvial‒aeolian interplay in the Mu Us Desert (MUD) during the Last Glacial Period (LGP) hinders our understanding of the relationships between the dynamics of aeolian and fluvial‒lacustrine landscapes and their drivers. Here, based on a comprehensive field survey and stratigraphic dating of a typical fluvial‒aeolian sequence in the MUD, we synthesized the chronology of fluvial‒lacustrine and aeolian strata during the LGP. Our results show that extensive development of a fluvial‒lacustrine environment in the MUD during the LG mainly occurred during the late Last Glacial Maximum (LGMa, 20.1–18.4 ka BP) and Bølling/Allerød interstadial (14.8–12.6 ka BP), while thicker aeolian sands extensively accumulated during the Heinrich Stadial 2, Heinrich Stadial 1, and Younger Dryas periods. However, the development of fluvial‒lacustrine environments showed considerable spatial heterogeneity, mainly occurring on the southern and eastern margins of the desert, while they were extremely rare in the central and western parts of the desert owing to strong wind erosion. Comparisons with other high-resolution geological records from the Asian monsoon region reveal that the fluvial‒aeolian interplay in the MUD during the LGP was highly consistent with the evolution pattern of the East Asian summer monsoon (EASM) on the millennial‒centennial scale, and indicate that the development of fluvial‒lacustrine environments was mainly controlled by an increase in monsoonal precipitation during strengthening of the EASM. Consistency with other broad changes at high latitudes in the Northern Hemisphere suggests that fluvial‒aeolian interplay during the LGP in northern Chinese deserts, as represented by the MUD, was mainly controlled by changes in high-northern-latitude ice volume and the Atlantic Meridional Overturning Circulation." @default.
• W4385522924 created "2023-08-04" @default.
• W4385522924 creator A5001713727 @default.
• W4385522924 creator A5014348411 @default.
• W4385522924 creator A5054837807 @default.
• W4385522924 creator A5065037394 @default.
• W4385522924 date "2023-09-01" @default.
• W4385522924 modified "2023-10-12" @default.
• W4385522924 title "High-northern-latitude forcing modulated fluvial‒aeolian interplay during the Last Glacial Period in the Mu Us Desert, northern central China" @default.
• W4385522924 cites W1440478720 @default.
• W4385522924 cites W1507513809 @default.
• W4385522924 cites W1870614584 @default.
• W4385522924 cites W1943346833 @default.
• W4385522924 cites W1964883926 @default.
• W4385522924 cites W1966207504 @default.
• W4385522924 cites W1966746778 @default.
• W4385522924 cites W1972892880 @default.
• W4385522924 cites W1975223521 @default.
• W4385522924 cites W1978299336 @default.
• W4385522924 cites W1980498694 @default.
• W4385522924 cites W1980860342 @default.
• W4385522924 cites W1992192360 @default.
• W4385522924 cites W1994007098 @default.
• W4385522924 cites W1997350491 @default.
• W4385522924 cites W1999956578 @default.
• W4385522924 cites W2002717773 @default.
• W4385522924 cites W2004368305 @default.
• W4385522924 cites W2006364543 @default.
• W4385522924 cites W2010516453 @default.
• W4385522924 cites W2011622086 @default.
• W4385522924 cites W2013878295 @default.
• W4385522924 cites W2016349369 @default.
• W4385522924 cites W2017547727 @default.
• W4385522924 cites W2018471515 @default.
• W4385522924 cites W2019558782 @default.
• W4385522924 cites W2024720828 @default.
• W4385522924 cites W2027385173 @default.
• W4385522924 cites W2029233754 @default.
• W4385522924 cites W2030362765 @default.
• W4385522924 cites W2035304876 @default.
• W4385522924 cites W2041006844 @default.
• W4385522924 cites W2044941373 @default.
• W4385522924 cites W2048891927 @default.
• W4385522924 cites W2048950463 @default.
• W4385522924 cites W2049610925 @default.
• W4385522924 cites W2050311837 @default.
• W4385522924 cites W2054158006 @default.
• W4385522924 cites W2054856491 @default.
• W4385522924 cites W2057138816 @default.
• W4385522924 cites W2061330514 @default.
• W4385522924 cites W2061780966 @default.
• W4385522924 cites W2068072860 @default.
• W4385522924 cites W2072446525 @default.
• W4385522924 cites W2073350984 @default.
• W4385522924 cites W2075733243 @default.
• W4385522924 cites W2076592609 @default.
• W4385522924 cites W2079049818 @default.
• W4385522924 cites W2080101287 @default.
• W4385522924 cites W2083790636 @default.
• W4385522924 cites W2084428435 @default.
• W4385522924 cites W2085838653 @default.
• W4385522924 cites W2086192317 @default.
• W4385522924 cites W2086853516 @default.
• W4385522924 cites W2089177966 @default.
• W4385522924 cites W2089956949 @default.
• W4385522924 cites W2093032081 @default.
• W4385522924 cites W2094173026 @default.
• W4385522924 cites W2094408279 @default.
• W4385522924 cites W2106123297 @default.
• W4385522924 cites W2109489043 @default.
• W4385522924 cites W2116331566 @default.
• W4385522924 cites W2136065747 @default.
• W4385522924 cites W2142021968 @default.
• W4385522924 cites W2161679449 @default.
• W4385522924 cites W2163819305 @default.
• W4385522924 cites W2170494697 @default.
• W4385522924 cites W2178183697 @default.
• W4385522924 cites W2198517330 @default.
• W4385522924 cites W2199849620 @default.
• W4385522924 cites W2204290202 @default.
• W4385522924 cites W2308666877 @default.
• W4385522924 cites W2366526863 @default.
• W4385522924 cites W2464339816 @default.
• W4385522924 cites W2599502281 @default.
• W4385522924 cites W2607017642 @default.
• W4385522924 cites W2765180760 @default.
• W4385522924 cites W2767351345 @default.
• W4385522924 cites W2790236092 @default.
• W4385522924 cites W2791482603 @default.
• W4385522924 cites W2886337500 @default.
• W4385522924 cites W2899343070 @default.
• W4385522924 cites W2903389357 @default.
• W4385522924 cites W2912460194 @default.
• W4385522924 cites W2914349082 @default.
• W4385522924 cites W2945706793 @default.
• W4385522924 cites W2953555491 @default.
• W4385522924 cites W2973933799 @default.
• W4385522924 cites W2987868251 @default.

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