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A sedimentological proxy indicator linking changes in loess and deserts in the Quaternary
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1016/0031-0182(89)90143-0openalex-snapshot
Loess stratigraphy in Central China
inferredcites →https://doi.org/10.1016/0031-0182(92)90120-topenalex-snapshot
A coupled environmental system formed at about 2.5 Ma in East Asia
inferredcites →https://doi.org/10.1016/0341-8162(91)90012-mopenalex-snapshot
Late quaternary dust flow on the chinese Loess Plateau
inferredcites →https://doi.org/10.1016/0341-8162(94)90077-9openalex-snapshot
Last glacial maximum in China: comparison between land and sea
inferredcites →https://doi.org/10.1038/366552a0openalex-snapshot
Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores
inferredcites →https://doi.org/10.1130/0091-7613(1997)025<0035:natsft>2.3.co;2openalex-snapshot
New absolute time scale for the Quaternary climate in the Chinese Loess region by grain-size analysis
inferredcites →https://doi.org/10.1144/gsl.sp.1987.035.01.10openalex-snapshot
The mechanics and geological implications of dust transport and deposition in deserts with particular reference to loess formation and dune sand diagenesis in the northern Negev, Israel
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.1002/gj.2795openalex-snapshot
History of moisture change derived from slope sediments of the eastern Gonghe Basin (northeastern Qinghai–Tibetan Plateau) during the last 17 ka
inferred← citeshttps://doi.org/10.1002/gj.3184openalex-snapshot
Multiproxy records of Holocene millennial‐scale climatic variations from the aeolian deposit in eastern Horqin dune field, northeastern China
inferred← citeshttps://doi.org/10.1007/bf02911994openalex-snapshot
Tectonic-climatic events in eastern Qilian Mountains over the past 0.83 Ma
inferred← citeshttps://doi.org/10.1007/bf03182815openalex-snapshot
A 1.5 Ma sporopollen record of paleoecologic environment evolution in the central Chinese Loess Plateau
inferred← citeshttps://doi.org/10.1007/bf03183320openalex-snapshot
Extension of drylands in northern China around 250 kaBP linked with the uplift of the southeast margin of Tibetan Pla-teau
inferred← citeshttps://doi.org/10.1007/s00531-014-1042-5openalex-snapshot
Spatial–temporal differences in climate change at different altitudes, northeastern Qinghai-Tibetan Plateau during the Holocene period
inferred← citeshttps://doi.org/10.1007/s00704-010-0252-4openalex-snapshot
An indicator of sand storms in the south of the Tengger Desert
inferred← citeshttps://doi.org/10.1007/s00704-018-2725-9openalex-snapshot
Reconstruction of dust storm frequency in China using the SST signals recorded in coral reefs
inferred← citeshttps://doi.org/10.1007/s11430-007-0040-xopenalex-snapshot
Instability characteristics of the East Asian Monsoon recorded by high-resolution loess sections from the last interglacial (MIS5)
inferred← citeshttps://doi.org/10.1007/s11430-008-0057-9openalex-snapshot
Optically stimulated luminescence dating of aeolian sand in the Otindag dune field and Holocene climate change
inferred← citeshttps://doi.org/10.1007/s11434-006-2003-6openalex-snapshot
Variations of organic carbon isotopic composition and its environmental significance during the last glacial on western Chinese Loess Plateau
inferred← citeshttps://doi.org/10.1007/s12303-010-0015-3openalex-snapshot
Loess record of the evolution history of severe sandstorms in the Tengger Desert during the Last Interglacial Period (MIS5)
inferred← citeshttps://doi.org/10.1007/s12665-020-8897-5openalex-snapshot
A 7-ka climatic variability record inferred from peat bog sediments in the north of Bayan Har Mountains, northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.aeolia.2014.03.006openalex-snapshot
Holocene moisture change revealed by the Rb/Sr ratio of aeolian deposits in the southeastern Mu Us Desert, China
inferred← citeshttps://doi.org/10.1016/j.catena.2024.107963openalex-snapshot
Origin and depositional background of the Holocene black soil in Northeast China: Evidence from grain-size analysis and optically stimulated luminescence dating
inferred← citeshttps://doi.org/10.1016/j.crte.2010.01.012openalex-snapshot
Pattern of abrupt climatic fluctuation in the East Asian Monsoon during the Last Glacial: Evidence from Chinese loess records
inferred← citeshttps://doi.org/10.1016/j.earscirev.2013.02.003openalex-snapshot
Investigation of the sand sea with the tallest dunes on Earth: China's Badain Jaran Sand Sea
inferred← citeshttps://doi.org/10.1016/j.geomorph.2023.108780openalex-snapshot
The largest deflation basin in Asia reveals that the Miocene basin-filling sediments in the eastern Gobi Desert are an important dust source
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104621openalex-snapshot
Quantitative contributions of different atmospheric circulation systems to Holocene aeolian activity in northwestern China: Evidence from a closed interdune lake in the Tengger Desert hinterland
inferred← citeshttps://doi.org/10.1016/j.gsf.2017.03.005openalex-snapshot
Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia
inferred← citeshttps://doi.org/10.1016/j.jseaes.2017.09.013openalex-snapshot
Loess deposits since early Pleistocene in northeast China and implications for desert evolution in east China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.03.029openalex-snapshot
Timing and significance of the initiation of present day deserts in the northeastern Hexi Corridor, China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.08.025openalex-snapshot
Intensification of aridity in the eastern margin of the Tibetan Plateau since 300ka BP inferred from loess-soil sequences, western Sichuan Province, southwest China
inferred← citeshttps://doi.org/10.1016/j.quaint.2008.07.007openalex-snapshot
Differences among sub-orbital time scale events recorded in two high-resolution loess sections, China, during the last deglaciation
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.05.003openalex-snapshot
Holocene climatic change revealed by aeolian deposits from the Gonghe Basin, northeastern Qinghai–Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.quaint.2019.02.026openalex-snapshot
Formation age of Jiudong Sandy Land, in the western Hexi Corridor, NW China
inferred← citeshttps://doi.org/10.1016/j.quaint.2019.12.022openalex-snapshot
History of moisture change indicated by aeolian deposit in the Horqin sandy land, Northeastern China since the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108275openalex-snapshot
BrGDGTs-based temperature and hydrological reconstruction from loess-paleosol deposits in the Eastern European Plain since 200 ka
inferred← citeshttps://doi.org/10.1016/j.quascirev.2026.109957openalex-snapshot
Aeolian processes and their dynamics in the desert-loess transition zone of northwestern China since 20 ka: A synthesis of paleoenvironmental records
inferred← citeshttps://doi.org/10.1016/j.revpalbo.2017.04.002openalex-snapshot
Late Pleistocene changes in vegetation and the associated human activity at Beiyao Site, Central China
inferred← citeshttps://doi.org/10.1016/j.yqres.2011.06.015openalex-snapshot
Luminescence sensitivities of quartz grains from eolian deposits in northern China and their implications for provenance
inferred← citeshttps://doi.org/10.1017/qua.2020.113openalex-snapshot
Provenance and paleoclimatic implications of loess deposits in Shandong Province, eastern China
inferred← citeshttps://doi.org/10.1029/2006jd007316openalex-snapshot
Response of East Asian climate to Dansgaard/Oeschger and Heinrich events in a coupled model of intermediate complexity
inferred← citeshttps://doi.org/10.1029/2007gl031716openalex-snapshot
Link between European and North Atlantic abrupt climate changes over the last glaciation
inferred← citeshttps://doi.org/10.1111/1755-6724.13326openalex-snapshot
Intensification of the East Asian Monsoon in Southern China at about 300-400 kaBP Inferred from Eolian Deposits in the Middle-lower Reaches of the Yangtze River
inferred← citeshttps://doi.org/10.1594/pangaea.962970openalex-snapshot
Pre-industrial Holocene (pi-HOL) paleo-dust record
inferred← citeshttps://doi.org/10.1594/pangaea.962971openalex-snapshot
Last Glacial Maximum (LGM) paleo-dust record
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