Aeolian process and climatic changes in loess records from the eastern Tibetan Plateau: Implications for paleoenvironmental dynamics since MIS 3

[1]  XiangJun Liu,et al.  Distribution and fate of Tibetan Plateau loess , 2023, CATENA.

[2]  Fahu Chen,et al.  The northern boundary of the Asian summer monsoon and division of westerlies and monsoon regimes over the Tibetan Plateau in present-day , 2023, Science China Earth Sciences.

[3]  Shengli Yang,et al.  Westerly Variations in the Eastern Tibetan Plateau since the Last Interglacial Revealed by the Grain-Size Records of the Ganzi Loess , 2023, Atmosphere.

[4]  E. Mosley‐Thompson,et al.  Use of δ18Oatm in dating a Tibetan ice core record of Holocene/Late Glacial climate , 2022, Proceedings of the National Academy of Sciences of the United States of America.

[5]  P. Valdes,et al.  A distinctive Eocene Asian monsoon and modern biodiversity resulted from the rise of eastern Tibet. , 2022, Science bulletin.

[6]  Hai-ping Hu,et al.  Amplified and suppressed regional imprints of global warming events on the southeastern Tibetan Plateau during MIS 3–2 , 2022, Quaternary Science Reviews.

[7]  Shengli Yang,et al.  Variation of luminescence sensitivity of quartz grains from loess in eastern Tibetan Plateau and its provenance significance , 2022, Frontiers in Earth Science.

[8]  Jian-biao Zhou,et al.  Effects of the size of the test dose on the SAR protocol for quartz optically stimulated luminescence dating of loess in the eastern Tibetan Plateau , 2022, Quaternary Geochronology.

[9]  Yue Zheng,et al.  Accumulation of aeolian sediments around the Tengger Desert during the late Quaternary and its implications on interpreting chronostratigraphic records from drylands in north China , 2022, Quaternary Science Reviews.

[10]  David S. G. Thomas,et al.  A tale of two signals: Global and local influences on the Late Pleistocene loess sequences in Bulgarian Lower Danube , 2021, Quaternary Science Reviews.

[11]  S. Clemens,et al.  Abrupt Indian summer monsoon shifts aligned with Heinrich events and D-O cycles since MIS 3 , 2021, Palaeogeography, Palaeoclimatology, Palaeoecology.

[12]  S. Clemens,et al.  Persistent orbital influence on millennial climate variability through the Pleistocene , 2021, Nature Geoscience.

[13]  Jingran Zhang,et al.  Regional hydroclimates regulate the Holocene aeolian accumulation processes of the Qinghai Lake basin on the northeastern Tibetan plateau , 2021, CATENA.

[14]  Fahu Chen,et al.  Direct astronomical influence on abrupt climate variability , 2021, Nature Geoscience.

[15]  G. Guérin,et al.  Optically stimulated luminescence dating using quartz , 2021, Nature Reviews Methods Primers.

[16]  Shengli Yang,et al.  Stepwise Weakening of Aeolian Activities During the Holocene in the Gannan Region, Eastern Tibetan Plateau , 2021, Frontiers in Earth Science.

[17]  Shengli Yang,et al.  Chronology and dust mass accumulation history of the Wenchuan loess on eastern Tibetan Plateau since the last glacial , 2021, Aeolian Research.

[18]  Yan Yan,et al.  High-sedimentation-rate loess records: A new window into understanding orbital- and millennial-scale monsoon variability , 2021 .

[19]  Shengli Yang,et al.  Comparisons of topsoil geochemical elements from Northwest China and eastern Tibetan Plateau identify the plateau interior as Tibetan dust source. , 2021, The Science of the total environment.

[20]  Shi-chang Kang,et al.  Hf-Nd-Sr Isotopic Composition of the Tibetan Plateau Dust as a Fingerprint for Regional to Hemispherical Transport. , 2021, Environmental science & technology.

[21]  R. Orozbaev,et al.  Spatio-temporal distribution of Quaternary loess across Central Asia , 2021 .

[22]  J. Elser,et al.  Aeolian dust transport, cycle and influences in high-elevation cryosphere of the Tibetan Plateau region: New evidences from alpine snow and ice , 2020 .

[23]  Shengli Yang,et al.  Quartz OSL chronology of the loess deposits in the Western Qinling Mountains, China, and their palaeoenvironmental implications since the Last Glacial period , 2020, Boreas.

[24]  Kun Yang,et al.  Climate change, vegetation history, and landscape responses on the Tibetan Plateau during the Holocene: A comprehensive review , 2020 .

[25]  S. Sarkar,et al.  Paleoenvironment of the Central Himalaya during late MIS 3 using stable isotopic compositions of lacustrine organic matter occluded in diatoms and sediments , 2020 .

[26]  M. Prange,et al.  Stability of the Atlantic overturning circulation under intermediate (MIS3) and full glacial (LGM) conditions and its relationship with Dansgaard-Oeschger climate variability , 2020, Quaternary Science Reviews.

[27]  Xiaoqiang Yang,et al.  Sensitivity of altitudinal vegetation in southwest China to changes in the Indian summer monsoon during the past 68000 years , 2020 .

[28]  Fahu Chen,et al.  Spatiotemporal complexity of the "Greatest Lake Period" in the Tibetan Plateau. , 2020, Science bulletin.

[29]  H. Birks,et al.  Evolution of vegetation and climate variability on the Tibetan Plateau over the past 1.74 million years , 2020, Science Advances.

[30]  J. Niu,et al.  Geochemical record of rapid climate change and chemical weathering in a semi-arid area, northeastern Tibetan Plateau , 2020, Geosciences Journal.

[31]  Weijian Zhou,et al.  The deficiency of organic matter 14C dating in Chinese Loess-paleosol sample , 2020 .

[32]  Xiaoqiang Yang,et al.  Synchronous change of temperature and moisture over the past 50 ka in subtropical southwest China as indicated by biomarker records in a crater lake , 2019, Quaternary Science Reviews.

[33]  Fahu Chen,et al.  Optical dating of Holocene paleosol development and climate changes in the Yili Basin, arid central Asia , 2019, The Holocene.

[34]  S. Hou,et al.  Apparent discrepancy of Tibetan ice core δ18O records may be attributed to misinterpretation of chronology , 2019, The Cryosphere.

[35]  U. Mikolajewicz,et al.  Heinrich events show two-stage climate response in transient glacial simulations , 2019, Climate of the Past.

[36]  F. Lehmkuhl,et al.  Quartz OSL dating of late quaternary Chinese and Serbian loess: A cross Eurasian comparison of dust mass accumulation rates , 2019, Quaternary International.

[37]  Shi-Yong Yu,et al.  Late‐Quaternary history of ‘great lakes’ on the Tibetan Plateau and palaeoclimatic implications – A review , 2018, Boreas.

[38]  F. Eynaud,et al.  Monsoonal Forcing of European Ice‐Sheet Dynamics During the Late Quaternary , 2018, Geophysical Research Letters.

[39]  J. Vandenberghe,et al.  Palaeoenvironmental implication of grain-size compositions of terrace deposits on the western Chinese Loess Plateau , 2018, Aeolian Research.

[40]  M. Frey,et al.  Greenland records of aerosol source and atmospheric lifetime changes from the Eemian to the Holocene , 2018, Nature Communications.

[41]  Yougui Song,et al.  Radiometric dating of late Quaternary loess in the northern piedmont of South Tianshan Mountains: Implications for reliable dating , 2018 .

[42]  Jimin Sun,et al.  Fake age hiatus in a loess section revealed by OSL dating of calcrete nodules , 2017 .

[43]  Z. An,et al.  Abrupt climatic events recorded by the Ili loess during the last glaciation in Central Asia: Evidence from grain-size and minerals , 2017 .

[44]  J. Bassis,et al.  Heinrich events triggered by ocean forcing and modulated by isostatic adjustment , 2017, Nature.

[45]  R. Edwards,et al.  The Asian monsoon over the past 640,000 years and ice age terminations , 2016, Nature.

[46]  Thomas Stevens,et al.  Mass accumulation rate and monsoon records from Xifeng, Chinese Loess Plateau, based on a luminescence age model , 2016 .

[47]  Z. An,et al.  Mass accumulation rate changes in Chinese loess during MIS 2, and asynchrony with records from Greenland ice cores and North Pacific Ocean sediments during the Last Glacial Maximum , 2015 .

[48]  Tao Chen,et al.  Comparison between luminescence and radiocarbon dating of late Quaternary loess from the Ili Basin in Central Asia , 2015 .

[49]  Chao Zhao,et al.  Holocene aeolian activity and climatic change in Qinghai Lake basin, northeastern Qinghai–Tibetan Plateau , 2015 .

[50]  G. A. T. Duller,et al.  The Analyst software package for luminescence data: overview and recent improvements , 2015 .

[51]  Weijian Zhou,et al.  Variability of stalagmite-inferred Indian monsoon precipitation over the past 252,000 y , 2015, Proceedings of the National Academy of Sciences.

[52]  Wa-Tat Yan,et al.  Magnetostratigraphy of a Loess‐Paleosol Sequence from Higher Terrace of the Daduhe River in the Eastern Margin of the Tibetan Plateau and Its Geological Significance , 2015 .

[53]  H. Fischer,et al.  A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: refining and extending the INTIMATE event stratigraphy , 2014 .

[54]  C. Buizert,et al.  Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint , 2014 .

[55]  G. Dong,et al.  Reliability of radiocarbon dating on various fractions of loess-soil sequence for Dadiwan section in the western Chinese Loess Plateau , 2014, Frontiers of Earth Science.

[56]  Zhongping Lai,et al.  Paleoenvironmental implications of new OSL dates on the formation of the “Shell Bar” in the Qaidam Basin, northeastern Qinghai-Tibetan Plateau , 2014, Journal of Paleolimnology.

[57]  A. Wintle,et al.  On natural and laboratory generated dose response curves for quartz of different grain sizes from Romanian loess , 2013 .

[58]  Yan-chou Lu,et al.  Quartz OSL chronology and dust accumulation rate changes since the Last Glacial at Weinan on the southeastern Chinese Loess Plateau , 2013 .

[59]  Jef Vandenberghe,et al.  Grain size of fine-grained windblown sediment: A powerful proxy for process identification , 2013 .

[60]  H. Oeschger,et al.  North Atlantic climatic oscillations revealed by deep Greenland ice cores , 2013 .

[61]  Zhongping Lai,et al.  A comparison of natural- and laboratory-generated dose response curves for quartz optically stimulated luminescence signals from Chinese Loess , 2012 .

[62]  V. Masson‐Delmotte,et al.  Spatial gradients of temperature, accumulation and δ 18 O-ice in Greenland over a series of Dansgaard-Oeschger events , 2012 .

[63]  Yan-chou Lu,et al.  The estimation of basic experimental parameters in the fine-grained quartz multiple-aliquot regenerative-dose OSL dating of Chinese loess , 2012 .

[64]  L. Thompson,et al.  Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings , 2012 .

[65]  J. Christen,et al.  Flexible paleoclimate age-depth models using an autoregressive gamma process , 2011 .

[66]  W. Balsam,et al.  Magnetic susceptibility as a proxy for rainfall: Worldwide data from tropical and temperate climate , 2011 .

[67]  P. Clark,et al.  Ice-shelf collapse from subsurface warming as a trigger for Heinrich events , 2011, Proceedings of the National Academy of Sciences.

[68]  Zhuolun Li,et al.  High lake levels on Alxa Plateau during the Late Quaternary , 2011 .

[69]  Soon-Chang Yoon,et al.  Dust cycle: An emerging core theme in Earth system science , 2011 .

[70]  T. Dokken,et al.  A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events , 2010 .

[71]  M. Bierkens,et al.  Climate Change Will Affect the Asian Water Towers , 2010, Science.

[72]  F. Lehmkuhl,et al.  Timing and provenance of loess in the Sichuan Basin, southwestern China , 2010 .

[73]  J. King,et al.  Differences between East Asian and Indian monsoon climate records during MIS3 attributed to differences in their driving mechanisms: Evidence from the loess record in the Sichuan basin, southwestern China and other continental and marine climate records , 2010 .

[74]  Joseph M. Prospero,et al.  Global connections between aeolian dust, climate and ocean biogeochemistry at the present day and at the last glacial maximum , 2010 .

[75]  S. Planton,et al.  Northern hemisphere storm tracks during the last glacial maximum in the PMIP2 ocean-atmosphere coupled models: energetic study, seasonal cycle, precipitation , 2009 .

[76]  H. Roberts The development and application of luminescence dating to loess deposits: a perspective on the past, present and future , 2008 .

[77]  Shi-chang Kang,et al.  Shifts of dust source regions over central Asia and the Tibetan Plateau: Connections with the Arctic oscillation and the westerly jet , 2008 .

[78]  P. Brantingham,et al.  Age constraints on the late Quaternary evolution of Qinghai Lake, Tibetan Plateau , 2008, Quaternary Research.

[79]  H. Brückner,et al.  Alpha efficiency determination for OSL of quartz extracted from Chinese loess , 2008 .

[80]  A. Murray,et al.  Optical dating of Chinese loess using sand-sized quartz: Establishing a time frame for Late Pleistocene climate changes in the western part of the Chinese Loess Plateau , 2008 .

[81]  T. Stocker,et al.  Four Climate Cycles of Recurring Deep and Surface Water Destabilizations on the Iberian Margin , 2007, Science.

[82]  R. Röthlisberger,et al.  Ice core evidence for a very tight link between North Atlantic and east Asian glacial climate , 2007 .

[83]  J. Torrent,et al.  Review of recent developments in mineral magnetism of the Chinese loess , 2007 .

[84]  R. Edwards,et al.  High-resolution absolute-dated Indian Monsoon record between 53 and 36 ka from Xiaobailong Cave, southwestern China , 2006 .

[85]  A. Murray,et al.  A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols , 2006 .

[86]  Kam‐biu Liu,et al.  Pollen records and time scale for the RM core of the Zoige Basin, northeastern Qinghai-Tibetan Plateau , 2005 .

[87]  J Schwander,et al.  High-resolution record of Northern Hemisphere climate extending into the last interglacial period , 2004, Nature.

[88]  X. Fang,et al.  Millennial-scale climate change since the last glaciation recorded by grain sizes of loess deposits on the northeastern Tibetan Plateau , 2004 .

[89]  Xiaoye Zhang,et al.  Dust storms and loess accumulation on the Tibetan Plateau: A case study of dust event on 4 March 2003 in Lhasa , 2004 .

[90]  G. Duller Distinguishing quartz and feldspar in single grain luminescence measurements , 2003 .

[91]  Sandy P. Harrison,et al.  DIRTMAP: the geological record of dust , 2001 .

[92]  Ge Yu,et al.  Reconstruction of the 30–40 ka bp enhanced Indian monsoon climate based on geological records from the Tibetan Plateau , 2001 .

[93]  Jef Vandenberghe,et al.  Rapid climatic changes recorded in loess successions , 2001 .

[94]  A. Murray,et al.  Luminescence dating of quartz using an improved single aliquot regenerative-dose protocol , 2000 .

[95]  T. Yao,et al.  A very strong summer monsoon event during 30–40 kaBP in the Qinghai-Xizang (Tibet) Plateau and its relation to precessional cycle , 1999 .

[96]  G. Laslett,et al.  OPTICAL DATING OF SINGLE AND MULTIPLE GRAINS OF QUARTZ FROM JINMIUM ROCK SHELTER, NORTHERN AUSTRALIA: PART I, EXPERIMENTAL DESIGN AND STATISTICAL MODELS* , 1999 .

[97]  X. Fang,et al.  Rock magnetic and grain size evidence for intensified Asian atmospheric circulation since 800,000 years B.P. related to Tibetan uplift , 1999 .

[98]  L. D. Meeker,et al.  Major features and forcing of high‐latitude northern hemisphere atmospheric circulation using a 110,000‐year‐long glaciochemical series , 1997 .

[99]  E. Mosley‐Thompson,et al.  Tropical Climate Instability: The Last Glacial Cycle from a Qinghai-Tibetan Ice Core , 1997 .

[100]  Fang Xiaomin THE ORIGIN AND PROVENANCE OF MALAN LOESS ALONG THE EASTERN MARGIN OF QINGHAI-XIZANG (TIBETAN) PLATEAU AND ITS ADJACENT AREA , 1995 .

[101]  A. Zhisheng,et al.  Correlation between climate events in the North Atlantic and China during the last glaciation , 1995, Nature.

[102]  J. Prescott,et al.  Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths and long-term time variations , 1994 .

[103]  R. Alley,et al.  Global Younger Dryas , 1993 .

[104]  G. Kukla,et al.  Late quaternary dust flow on the chinese Loess Plateau , 1991 .

[105]  J. T. Wang,et al.  Partly pedogenic origin of magnetic variations in Chinese loess , 1990, Nature.

[106]  N. Pisias,et al.  A direct link between the China loess and marine δ18O records: aeolian flux to the north Pacific , 1989, Nature.

[107]  B. Maher,et al.  Formation of ultrafine-grained magnetite in soils , 1988, Nature.

[108]  H. Heinrich,et al.  Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years , 1988, Quaternary Research.

[109]  J. Vandenberghe Paleoenvironment and Stratigraphy during the Last Glacial in the Belgian-Dutch Border Region , 1985, Quaternary Research.

[110]  Jun Qin,et al.  Recent climate changes over the Tibetan Plateau and their impacts on energy and water cycle: A review , 2014 .

[111]  Aifeng Zhou,et al.  Peatland initiation and carbon accumulation in China over the last 50,000 years , 2014 .

[112]  Christopher Bronk Ramsey,et al.  BAYESIAN ANALYSIS OF RADIOCARBON DATES , 2009 .

[113]  Zhao Jing-dong The Special Warm-Humid Climate and Environment in China during 40~30 ka BP:Discovery and Review , 2009 .

[114]  U. Herzschuh Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years , 2006 .

[115]  J. Mason,et al.  Pedogenic response to millennial summer monsoon enhancements on the Tibetan Plateau , 2003 .

[116]  J. Southon,et al.  Stepped-Combustion 14C Dating of Sediment: A Comparison with Established Techniques , 2001, Radiocarbon.

[117]  Z. An,et al.  Pleistocene magnetic susceptibility and paleomagnetism of the Tibetan loess and its implications on large climatic change events , 2001 .

[118]  W. Jian LOESS DEPOSIT IN EASTERN PART OF QINGHAI XIZANG PLATEAU: ITS CHARACTERISTICS AND ENVIRONMENT , 1997 .