Orbital‐ to millennial‐scale variation of the speleothem δ18O record during Marine Isotope Stages 5 to 3 on the southeast Chinese Loess Plateau and its climatic and environmental implications
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R. Edwards | Z. An | Haiwei Zhang | Hanying Li | Y. Cai | Ting Wang | Le Ma | Zhengguo Shi | C. Pérez-Mejías | Yanbin Lu | Yingying Wei | Xing Cheng | G. Xue | Hai Cheng | YANBIN LU | CARLOS PÉREZ‐MEJÍAS | HAIWEI ZHANG | Mei He | Hai Cheng | R. Edwards | Yanjun Cai
[1] R. Edwards,et al. Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics , 2021, Communications Earth & Environment.
[2] A. Berger,et al. Insolation triggered abrupt weakening of Atlantic circulation at the end of interglacials , 2021, Science.
[3] Z. An,et al. Variation of summer precipitation δ18O on the Chinese Loess Plateau since the last interglacial , 2021, Journal of Quaternary Science.
[4] R. Edwards,et al. Holocene variability of East Asian summer monsoon as viewed from the speleothem δ18O records in central China , 2021 .
[5] R. Edwards,et al. Speleothem‐Based Hydroclimate Reconstructions During the Penultimate Deglaciation in Northern China , 2021, Paleoceanography and Paleoclimatology.
[6] H. Cheng,et al. Orbital-scale Asian summer monsoon variations: Paradox and exploration , 2021, Science China Earth Sciences.
[7] Fahu Chen,et al. New insights on Chinese cave δ18O records and their paleoclimatic significance , 2020 .
[8] J. Fohlmeister,et al. Main controls on the stable carbon isotope composition of speleothems , 2020, 2005.02787.
[9] Chuan‐Chou Shen,et al. Variation of the Asian summer monsoon since the last glacial-interglacial recorded in a stalagmite from southwest China , 2020 .
[10] R. Edwards,et al. Inter-relationship and environmental significance of stalagmite δ13C and δ18O records from Zhenzhu Cave, north China, over the last 130 ka , 2020 .
[11] T. Miller,et al. Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP , 2020, Nature Communications.
[12] H. Chiang,et al. On the glacial-interglacial variability of the Asian monsoon in speleothem δ18O records , 2020, Science Advances.
[13] R. Edwards,et al. Orbital-to-millennial scale climate variability during Marine Isotope Stages 5 to 3 in northeast Iberia , 2019, Quaternary Science Reviews.
[14] Gregory S. Springer,et al. Eastern North American climate in phase with fall insolation throughout the last three glacial-interglacial cycles , 2019, Earth and Planetary Science Letters.
[15] R. Edwards,et al. A new speleothem record of the penultimate deglacial: Insights into spatial variability and centennial-scale instabilities of East Asian monsoon , 2019, Quaternary Science Reviews.
[16] Weijian Zhou,et al. Diverse manifestations of the mid-Pleistocene climate transition , 2019, Nature Communications.
[17] A. Delgado-Huertas,et al. Transference of isotopic signal from rainfall to dripwaters and farmed calcite in Mediterranean semi-arid karst , 2018, Geochimica et Cosmochimica Acta.
[18] J. Grimalt,et al. Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial , 2018, Nature Communications.
[19] Weijian Zhou,et al. A 550,000-year record of East Asian monsoon rainfall from 10Be in loess , 2018, Science.
[20] Xiao-dong Liu,et al. Distinct responses of East Asian and Indian summer monsoons to astronomical insolation during Marine Isotope Stages 5c and 5e , 2017, Palaeogeography, Palaeoclimatology, Palaeoecology.
[21] Long Ma,et al. Registration of Precession Signal in the Last Interglacial Paleosol (S1) on the Chinese Loess Plateau , 2017 .
[22] G. Haug,et al. Climatic and in-cave influences on δ18O and δ13C in a stalagmite from northeastern India through the last deglaciation , 2017, Quaternary Research.
[23] Fei Liu,et al. Continued obliquity pacing of East Asian summer precipitation after the mid-Pleistocene transition , 2017 .
[24] R. Edwards,et al. Strong coupling of Asian Monsoon and Antarctic climates on sub-orbital timescales , 2016, Scientific Reports.
[25] R. Edwards,et al. The Asian monsoon over the past 640,000 years and ice age terminations , 2016, Nature.
[26] R. Edwards,et al. Indian monsoon variability on millennial-orbital timescales , 2016, Scientific Reports.
[27] J. Kutzbach,et al. Astronomical and glacial forcing of East Asian summer monsoon variability , 2015 .
[28] Keith M. Prufer,et al. Aerosol forcing of the position of the intertropical convergence zone since ad 1550 , 2015 .
[29] 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.
[30] I. Fung,et al. Role of seasonal transitions and westerly jets in East Asian paleoclimate , 2015 .
[31] Fahu Chen,et al. Evolving history of the East Asian summer monsoon intensity during the MIS5: inconsistent records from Chinese stalagmites and loess deposits , 2015, Environmental Earth Sciences.
[32] L. Lisiecki,et al. A Late Pleistocene sea level stack , 2014 .
[33] D. Battisti,et al. Coherent pan‐Asian climatic and isotopic response to orbital forcing of tropical insolation , 2014 .
[34] Ge Yu,et al. Chinese cave records and the East Asia Summer Monsoon , 2014 .
[35] M. Tan. Circulation effect: response of precipitation δ18O to the ENSO cycle in monsoon regions of China , 2014, Climate Dynamics.
[36] R. Edwards,et al. Improvements in 230Th dating, 230Th and 234U half-life values, and U–Th isotopic measurements by multi-collector inductively coupled plasma mass spectrometry , 2013 .
[37] Norbert Marwan,et al. COnstructing Proxy Records from Age models (COPRA) , 2012 .
[38] C. Frankenberg,et al. Asian monsoon hydrometeorology from TES and SCIAMACHY water vapor isotope measurements and LMDZ simulations: Implications for speleothem climate record interpretation , 2012 .
[39] F. Liang,et al. The Holocene Indian monsoon variability over the southern Tibetan Plateau and its teleconnections , 2012 .
[40] R. Edwards,et al. The Global Paleomonsoon as seen through speleothem records from Asia and the Americas , 2012, Climate Dynamics.
[41] J. Kutzbach,et al. Distinct responses of East Asian summer and winter monsoons to astronomical forcing , 2011 .
[42] C. Bitz,et al. Chinese stalagmite δ 18 O controlled by changes in the Indian monsoon during a simulated Heinrich event , 2011 .
[43] J. Schewe,et al. A critical humidity threshold for monsoon transitions , 2011 .
[44] M. Ziegler,et al. Precession phasing offset between Indian summer monsoon and Arabian Sea productivity linked to changes in Atlantic overturning circulation , 2010 .
[45] R. Edwards,et al. Large variations of oxygen isotopes in precipitation over south-central Tibet during Marine Isotope Stage 5 , 2010 .
[46] R. Edwards,et al. The variation of summer monsoon precipitation in central China since the last deglaciation , 2010 .
[47] M. Siddall,et al. Controls on the East Asian monsoon during the last glacial cycle, based on comparison between Hulu Cave and polar ice-core records , 2009 .
[48] W. Broecker,et al. Ice Age Terminations , 2009, Science.
[49] Hermann Held,et al. Basic mechanism for abrupt monsoon transitions , 2009, Proceedings of the National Academy of Sciences.
[50] B. A. Maher,et al. Holocene variability of the East Asian summer monsoon from Chinese cave records: a re-assessment , 2008 .
[51] Yihui Ding,et al. Inter‐decadal variation of the summer precipitation in East China and its association with decreasing Asian summer monsoon. Part I: Observed evidences , 2008 .
[52] J. Kutzbach,et al. Simulation of the evolutionary response of global summer monsoons to orbital forcing over the past 280,000 years , 2008 .
[53] Xiaohua Shao,et al. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years , 2008, Nature.
[54] Jerry F. McManus,et al. Evolution and demise of the Last Interglacial warmth in the subpolar North Atlantic , 2006 .
[55] B. Soden,et al. Robust Responses of the Hydrological Cycle to Global Warming , 2006 .
[56] J. Hellstrom,et al. Timing and dynamics of the last deglaciation from European and North African δ13C stalagmite profiles—comparison with Chinese and South Hemisphere stalagmites , 2006 .
[57] R. Edwards,et al. High-resolution absolute-dated Indian Monsoon record between 53 and 36 ka from Xiaobailong Cave, southwestern China , 2006 .
[58] R. Edwards,et al. High resolution characterization of the Asian Monsoon between 146,000 and 99,000 years B.P. from Dongge Cave, China and global correlation of events surrounding Termination II , 2006 .
[59] G. Vecchi,et al. Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing , 2006, Nature.
[60] S. Clemens,et al. Astronomical timescale and palaeoclimatic implication of stacked 3.6-Myr monsoon records from the Chinese Loess Plateau , 2006 .
[61] J. Chan,et al. The East Asian summer monsoon: an overview , 2005 .
[62] Z. Feng,et al. Pedogenic factors affecting magnetic susceptibility of the last interglacial palaeosol S1 in the Chinese Loess Plateau , 2004 .
[63] J Schwander,et al. High-resolution record of Northern Hemisphere climate extending into the last interglacial period , 2004, Nature.
[64] R. Edwards,et al. Timing, Duration, and Transitions of the Last Interglacial Asian Monsoon , 2004, Science.
[65] F. McDermott,et al. Palaeo-climate reconstruction from stable isotope variations in speleothems: a review , 2004 .
[66] Li Bao-sheng,et al. Major element records in Salawusu River Valley responding to global change in the last interglacial period , 2004 .
[67] Fahu Chen,et al. Stable East Asian monsoon climate during the Last Interglacial (Eemian) indicated by paleosol S1 in the western part of the Chinese Loess Plateau , 2003 .
[68] W. Broecker,et al. Last Interglacial Climates , 2002, Quaternary Research.
[69] S. John,et al. Comparison of oxygen isotope records from the GISP 2 and GRIP Greenland ice cores , 2002 .
[70] Guangjian Wu,et al. Loess record of climatic changes during MIS5 in the Hexi Corridor, northwest China , 2002 .
[71] R. L. Edwards,et al. A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China , 2001, Science.
[72] J. Kirchner,et al. Spatial and temporal variability in the stable isotope systematics of modern precipitation in China: implications for paleoclimate reconstructions , 2001 .
[73] Z. An,et al. The δ18O variation of a stalagmite from Qixing Cave, Guizhou Province and indicated climate change during the Holocene , 2001 .
[74] Bin Wang,et al. Pacific–East Asian Teleconnection: How Does ENSO Affect East Asian Climate? , 2000 .
[75] G. Kukla. The Last Interglacial , 2000, Science.
[76] Z. Ding,et al. Climate instability during the penultimate glaciation: Evidence from two high‐resolution loess records, China , 1999 .
[77] Fahu Chen,et al. East Asian monsoon variations during Oxygen Isotope Stage 5: evidence from the northwestern margin of the Chinese loess plateau , 1999 .
[78] Z. An,et al. Variation of Rb/Sr Ratios in the Loess-Paleosol Sequences of Central China during the Last 130,000 Years and Their Implications for Monsoon Paleoclimatology , 1999, Quaternary Research.
[79] Gonzalez,et al. Climate and vegetation history of the midcontinent from 75 to 25 ka: A speleothem record from crevice cave, missouri, USA , 1998, Science.
[80] J. Bloemendal,et al. High resolution climate record from the Beijing area during the Last Glacial‐Interglacial Cycle , 1998 .
[81] Uffe Andersen,et al. The δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability , 1997 .
[82] E. Brook,et al. CH4 and δ18O of O2 records from Antarctic and Greenland ice: A clue for stratigraphic disturbance in the bottom part of the Greenland Ice Core Project and the Greenland Ice Sheet Project 2 ice cores , 1997 .
[83] Sang-Tae Kim,et al. Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates , 1997 .
[84] A. Zhisheng,et al. Millennial-scale climatic oscillations during the last interglaciation in central China , 1997 .
[85] E. Jansen,et al. Rapid changes in ocean circulation and heat flux in the Nordic seas during the last interglacial period , 1996, Nature.
[86] M. Leuenberger,et al. δ18O of atmospheric oxygen measured on the GRIP Ice Core Document Stratigraphic disturbances in the lowest 10% of the core , 1996 .
[87] A. Zhisheng,et al. Correlation between climate events in the North Atlantic and China during the last glaciation , 1995, Nature.
[88] W. Dansgaard,et al. The Eem Stable Isotope Record along the GRIP Ice Core and Its Interpretation , 1995, Quaternary Research.
[89] E. Cortijo,et al. Eemian cooling in the Norwegian Sea and North Atlantic ocean preceding continental ice-sheet growth , 1994, Nature.
[90] S. Lehman,et al. The role of the deep ocean in North Atlantic climate change between 70 and 130 kyr ago , 1994, Nature.
[91] W. Broecker,et al. High-resolution climate records from the North Atlantic during the last interglacial , 1994, Nature.
[92] J. Jouzel,et al. Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores , 1993, Nature.
[93] R. Alley,et al. Electrical conductivity measurements from the GISP2 and GRIP Greenland ice cores , 1993, Nature.
[94] J. Jouzel,et al. Evidence for general instability of past climate from a 250-kyr ice-core record , 1993, Nature.
[95] Greenland Ice-core Project Members. Climate instability during the last interglacial period recorded in the GRIP ice core , 1993, Nature.
[96] G. Wasserburg,et al. 238U234U230Th232Th systematics and the precise measurement of time over the past 500,000 years , 1987 .
[97] J. Kutzbach,et al. Monsoon Climate of the Early Holocene: Climate Experiment with the Earth's Orbital Parameters for 9000 Years Ago , 1981, Science.
[98] C. Hendy,et al. The isotopic geochemistry of speleothems—I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators , 1971 .
[99] R. Edwards,et al. U-234 U _ 230 Th-232 Th systematics and the precise measurement of time over the past 500 , 000 years , 2022 .