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Variability of stalagmite-inferred Indian monsoon precipitation over the past 252,000 y

https://doi.org/10.1073/pnas.1424035112
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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

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Coherent pan‐Asian climatic and isotopic response to orbital forcing of tropical insolation
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On the time-varying trend in global-mean surface temperature
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The Global Paleomonsoon as seen through speleothem records from Asia and the Americas
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238U234U230Th232Th systematics and the precise measurement of time over the past 500,000 years
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Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years
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Insolation values for the climate of the last 10 million years
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A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China
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Lessons learned from oxygen isotopes in modern precipitation applied to interpretation of speleothem records of paleoclimate from eastern Asia
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The Holocene Indian monsoon variability over the southern Tibetan Plateau and its teleconnections
inferredcites →https://doi.org/10.1016/j.epsl.2013.04.006openalex-snapshot
Improvements in 230Th dating, 230Th and 234U half-life values, and U–Th isotopic measurements by multi-collector inductively coupled plasma mass spectrometry
inferredcites →https://doi.org/10.1016/j.quascirev.2004.06.005openalex-snapshot
Periodicities of palaeoclimatic variations recorded by loess-paleosol sequences in China
inferredcites →https://doi.org/10.1016/j.quascirev.2006.04.012openalex-snapshot
Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman and Yemen (Socotra)
inferredcites →https://doi.org/10.1016/s0009-2541(01)00404-1openalex-snapshot
Uranium and thorium isotopic and concentration measurements by magnetic sector inductively coupled plasma mass spectrometry
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Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates
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A 350,000 year summer-monsoon multi-proxy stack from the Owen Ridge, Northern Arabian Sea
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Analysis of the global distribution of water isotopes using the NCAR atmospheric general circulation model
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Water isotopes during the Last Glacial Maximum: New general circulation model calculations
inferredcites →https://doi.org/10.1029/2010pa001926openalex-snapshot
Orbital-scale timing and mechanisms driving Late Pleistocene Indo-Asian summer monsoons: Reinterpreting cave speleothem δ 18 O
inferredcites →https://doi.org/10.1029/2010pa002083openalex-snapshot
The response of the Walker circulation to Last Glacial Maximum forcing: Implications for detection in proxies
inferredcites →https://doi.org/10.1029/2011jd017133openalex-snapshot
Asian monsoon hydrometeorology from TES and SCIAMACHY water vapor isotope measurements and LMDZ simulations: Implications for speleothem climate record interpretation
inferredcites →https://doi.org/10.1029/98jd00423openalex-snapshot
Water isotope module of the ECHAM atmospheric general circulation model: A study on timescales from days to several years
inferredcites →https://doi.org/10.1029/jd092id07p08411openalex-snapshot
Monsoon variability over the past 150,000 years
inferredcites →https://doi.org/10.1038/31750openalex-snapshot
Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years
inferredcites →https://doi.org/10.1038/364322a0openalex-snapshot
Century-scale events in monsoonal climate over the past 24,000 years
inferredcites →https://doi.org/10.1038/nature01340openalex-snapshot
Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean
inferredcites →https://doi.org/10.1038/nature06692openalex-snapshot
Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years
inferredcites →https://doi.org/10.1038/ngeo1169openalex-snapshot
Chinese stalagmite δ18O controlled by changes in the Indian monsoon during a simulated Heinrich event
inferredcites →https://doi.org/10.1073/pnas.0701020104openalex-snapshot
On the trend, detrending, and variability of nonlinear and nonstationary time series
inferredcites →https://doi.org/10.1126/science.1064618openalex-snapshot
A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China
inferredcites →https://doi.org/10.1126/science.1177840openalex-snapshot
Ice Age Terminations
inferredcites →https://doi.org/10.1126/science.1203752openalex-snapshot
Glacial-Interglacial Indian Summer Monsoon Dynamics
inferredcites →https://doi.org/10.1126/science.214.4516.59openalex-snapshot
Monsoon Climate of the Early Holocene: Climate Experiment with the Earth's Orbital Parameters for 9000 Years Ago
inferredcites →https://doi.org/10.1126/science.272.5270.1930openalex-snapshot
Pore Fluid Constraints on the Temperature and Oxygen Isotopic Composition of the Glacial Ocean
inferredcites →https://doi.org/10.1130/0091-7613(2001)029<0063:maaocc>2.0.co;2openalex-snapshot
Modulation and amplification of climatic changes in the Northern Hemisphere by the Indian summer monsoon during the past 80 k.y
inferredcites →https://doi.org/10.1130/g21498.1openalex-snapshot
Variability of Southwest Indian summer monsoon precipitation during the Bølling-Ållerød
inferredcites →https://doi.org/10.1130/g22567.1openalex-snapshot
High-resolution absolute-dated Indian Monsoon record between 53 and 36 ka from Xiaobailong Cave, southwestern China
inferredcites →https://doi.org/10.1130/g30306.1openalex-snapshot
Large variations of oxygen isotopes in precipitation over south-central Tibet during Marine Isotope Stage 5
inferredcites →https://doi.org/10.1142/s1793536909000047openalex-snapshot
ENSEMBLE EMPIRICAL MODE DECOMPOSITION: A NOISE-ASSISTED DATA ANALYSIS METHOD
inferredcites →https://doi.org/10.1146/annurev.earth.31.100901.141251openalex-snapshot
The Indian Monsoon and Its Variability
inferredcites →https://doi.org/10.1146/annurev.earth.32.082503.144359openalex-snapshot
GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE
inferredcites →https://doi.org/10.1175/jcli3748.1openalex-snapshot
Last Glacial Maximum and Holocene Climate in CCSM3
inferredcites →https://doi.org/10.1177/0959683608095569openalex-snapshot
Holocene variability of the East Asian summer monsoon from Chinese cave records: a re-assessment
inferredcites →https://doi.org/10.5194/cp-3-261-2007openalex-snapshot
Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 1: experiments and large-scale features
inferredcites →https://doi.org/10.5194/cp-5-441-2009openalex-snapshot
Sources of Holocene variability of oxygen isotopes in paleoclimate archives

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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The Optimized Late Pleistocene Chronology of a Lacustrine Sedimentary Core from Heqing Basin by Geomagnetic Paleointensity, and its Paleoclimate Significance
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Distinct impacts of the Mongolian and Tibetan Plateaus on the evolution of the East Asian monsoon
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Interannual controls on oxygen isotope variability in Asian monsoon precipitation and implications for paleoclimate reconstructions
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Rapid northward shift of the Indian Monsoon on the Tibetan Plateau at the end of the Little Ice Age
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Formation, mechanism and significance of alluvial‐dammed lakes in Golmud River catchment, north‐eastern Qinghai‐Tibetan Plateau
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The Pleistocene geoarchaeology and geochronology of Con Moong Cave, North Vietnam: Site formation processes and hominin activity in the humid tropics
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High‐resolution scanning XRF investigation of Chinese loess and its implications for millennial‐scale monsoon variability
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Glacial fluctuations around the Karola Pass, eastern Lhagoi Kangri Range, since the Last Glacial Maximum
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Variation of summer precipitation δ18O on the Chinese Loess Plateau since the last interglacial
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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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Regional Description: South and Southeast Asia
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Changes of Köppen Climate Zones over China in Simulated Interglacial and Future Warm Intervals
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Decreasing monsoon precipitation in southwest China during the last 240 years associated with the warming of tropical ocean
inferred← citeshttps://doi.org/10.1007/s00382-018-4456-0openalex-snapshot
Reconstructing the western boundary variability of the Western Pacific Subtropical High over the past 200 years via Chinese cave oxygen isotope records
inferred← citeshttps://doi.org/10.1007/s00382-019-04629-zopenalex-snapshot
Tree rings reveal hydroclimatic fingerprints of the Pacific Decadal Oscillation on the Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/s00382-019-04671-xopenalex-snapshot
Is Chinese stalagmite δ18O solely controlled by the Indian summer monsoon?
inferred← citeshttps://doi.org/10.1007/s00382-019-04935-6openalex-snapshot
Relationship between the Asian summer monsoon circulation and speleothem δ18O of Xiaobailong cave
inferred← citeshttps://doi.org/10.1007/s00382-020-05429-6openalex-snapshot
Similarities and differences in driving factors of precipitation changes on the western Loess Plateau and the northeastern Tibetan Plateau at different timescales
inferred← citeshttps://doi.org/10.1007/s00382-025-07812-7openalex-snapshot
Annually laminated stalagmite inferred variations of precipitation and temperature in northern China over the last 150 years
inferred← citeshttps://doi.org/10.1007/s10346-024-02392-9openalex-snapshot
Spatiotemporal distribution of mass movements: insights into regional changes in climate and geological environments
inferred← citeshttps://doi.org/10.1007/s10933-025-00365-zopenalex-snapshot
Response of middle and late Pleistocene ostracod δ18O and δ13C values to Indian summer monsoon and lake productivity on the southeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/s11430-015-5500-5openalex-snapshot
On the timing of the East Asian summer monsoon maximum during the Holocene—Does the speleothem oxygen isotope record reflect monsoon rainfall variability?
inferred← citeshttps://doi.org/10.1007/s11430-018-9344-2openalex-snapshot
Application of Avaatech X-ray fluorescence core-scanning in Sr/Ca analysis of speleothems
inferred← citeshttps://doi.org/10.1007/s11430-019-9478-3openalex-snapshot
Chinese stalagmite paleoclimate researches: A review and perspective
inferred← citeshttps://doi.org/10.1007/s11430-019-9649-1openalex-snapshot
A multiple-proxy stalagmite record reveals historical deforestation in central Shandong, northern China
inferred← citeshttps://doi.org/10.1007/s11430-020-9720-yopenalex-snapshot
Orbital-scale Asian summer monsoon variations: Paradox and exploration
inferred← citeshttps://doi.org/10.1007/s11430-020-9833-3openalex-snapshot
Lake-level records support a mid-Holocene maximum precipitation in northern China
inferred← citeshttps://doi.org/10.1007/s11430-022-1054-xopenalex-snapshot
An annually laminated stalagmite from the eastern Qinghai-Tibetan Plateau provides evidence of climate instability during the early MIS5e in the Asian summer monsoon
inferred← citeshttps://doi.org/10.1007/s11430-022-1190-0openalex-snapshot
Centennial-scale monsoon collapses during Marine Isotope Stage (MIS)7e detected in a northern Chinese stalagmite record
inferred← citeshttps://doi.org/10.1007/s11430-025-1772-1openalex-snapshot
A 25,000-yr-long integrated large earthquake record of the Xiaojiang Fault zone, southeastern Tibetan Plateau: New paleoseismic evidence from Yangzong Lake
inferred← citeshttps://doi.org/10.1007/s11430-025-1860-0openalex-snapshot
Phase contrast in Asian summer monsoon rainfall between marine and terrestrial records on precessional timescales and their driving mechanisms
inferred← citeshttps://doi.org/10.1007/s11442-021-1908-yopenalex-snapshot
Impact of changes in precipitation pattern on food supply in a monsoon interlacing area and its mechanism: A case study of Yunnan Province
inferred← citeshttps://doi.org/10.1007/s11442-026-2501-1openalex-snapshot
Rapid Bølling-Allerød Interstadial deglaciation in the southeastern Tibetan Plateau: Evidence from 10Be chronology of the glacially polished bedrock surfaces in the Haizishan Plateau
inferred← citeshttps://doi.org/10.1007/s12040-025-02520-6openalex-snapshot
Western equatorial Indian Ocean surface hydrographic variations inferred from isotopic record of planktic foraminifera Globigerinoides ruber during last ~412,000 years
inferred← citeshttps://doi.org/10.1007/s12520-022-01540-3openalex-snapshot
Investigating the palaeoenvironmental context of Late Pleistocene human dispersals into Southeast Asia: a review of stable isotope applications
inferred← citeshttps://doi.org/10.1007/s12520-023-01928-9openalex-snapshot
Technological diversity in the tropical-subtropical zone of Southwest China during the terminal Pleistocene: excavations at Fodongdi Cave
inferred← citeshttps://doi.org/10.1007/s12583-024-0005-4openalex-snapshot
Half-Precessional Cycle Revealed by Environment Magnetism of Stalagmite in Shizhu Cave from Southwestern China during the Last Glacial
inferred← citeshttps://doi.org/10.1007/s12665-021-09946-3openalex-snapshot
Palaeo-notch sediments as reliable proxy records for climate change and anthropogenic activities: a short review
inferred← citeshttps://doi.org/10.1016/b978-0-12-822698-8.00007-xopenalex-snapshot
Paleoclimate evidence of Indian Ocean variability across a range of timescales
inferred← citeshttps://doi.org/10.1016/b978-0-12-822869-2.00001-3openalex-snapshot
Teleconnection between Arctic climate and tropical Indian monsoon during the Holocene
inferred← citeshttps://doi.org/10.1016/b978-0-323-99762-1.00029-2openalex-snapshot
Geochemical approaches to reconstructing Earth's hydroclimates
inferred← citeshttps://doi.org/10.1016/b978-0-323-99931-1.00234-8openalex-snapshot
Monsoon reconstructions for South and East Asia
inferred← citeshttps://doi.org/10.1016/j.agrformet.2021.108687openalex-snapshot
Spatial synchrony in δ18O time-series from a tree-ring network are driven by synchronous hydroclimate variability in the transitional zone of the Asian summer monsoon
inferred← citeshttps://doi.org/10.1016/j.apgeochem.2022.105305openalex-snapshot
Subannual-to-biannual-resolved travertine record of Asian Summer Monsoon dynamics in the early Holocene at the eastern margin of Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.atmosres.2024.107602openalex-snapshot
Response of Northern Hemispheric climate and Asian monsoon to dust darkened snow cover changes during the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1016/j.catena.2020.105002openalex-snapshot
Significant influence of Northern Hemisphere high latitude climate on appeared precession rhythm of East Asian summer monsoon after Mid-Brunhes Transition interglacials recorded in the Chinese loess
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Determination of the optimized late Pleistocene chronology of a lacustrine sedimentary core from the Heqing Basin by geomagnetic paleointensity and its paleoclimate significance
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Aeolian process and climatic changes in loess records from the eastern Tibetan Plateau: Implications for paleoenvironmental dynamics since MIS 3
inferred← citeshttps://doi.org/10.1016/j.catena.2023.107721openalex-snapshot
Climate-driven formation of mass movements across the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.catena.2024.108446openalex-snapshot
Early-mid Holocene vegetation and diversity evolution on the Ningshao Plain, eastern China
inferred← citeshttps://doi.org/10.1016/j.catena.2024.108569openalex-snapshot
Hydroclimate variability in southeastern Tibetan Plateau since the late Quaternary: Insights from hydrogen isotopes in sedimentary leaf waxes
inferred← citeshttps://doi.org/10.1016/j.catena.2025.109161openalex-snapshot
Paleoenvironmental changes in the northeastern margin of the Tibetan Plateau since MIS 3: Magnetic evidence from the second terrace of the Yellow River
inferred← citeshttps://doi.org/10.1016/j.earscirev.2017.07.006openalex-snapshot
The global monsoon across time scales: Mechanisms and outstanding issues
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103216openalex-snapshot
New insights on Chinese cave δ18O records and their paleoclimatic significance
inferred← citeshttps://doi.org/10.1016/j.earscirev.2021.103731openalex-snapshot
High-sedimentation-rate loess records: A new window into understanding orbital- and millennial-scale monsoon variability
inferred← citeshttps://doi.org/10.1016/j.earscirev.2026.105478openalex-snapshot
Dominant control of precipitation on paleofire activity in the Asian Monsoon region over the past 20 ka
inferred← citeshttps://doi.org/10.1016/j.earscirev.2026.105483openalex-snapshot
Response of water chemistry and boron resources in boron-rich salt lakes to a warming–wetting climate on the Tibetan Plateau: modern processes and geological records
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Climatic-hydrological-geothermal coupled mechanism drives lake evolution and Li-B enrichment from mega-lakes to salt lakes on the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.epsl.2016.09.044openalex-snapshot
Heterodynes dominate precipitation isotopes in the East Asian monsoon region, reflecting interaction of multiple climate factors
inferred← citeshttps://doi.org/10.1016/j.epsl.2017.06.006openalex-snapshot
Orbitally-paced variations of water availability in the SE Asian Monsoon region following the Miocene Climate Transition
inferred← citeshttps://doi.org/10.1016/j.epsl.2017.09.012openalex-snapshot
Tropical and high latitude forcing of enhanced megadroughts in Northern China during the last four terminations
inferred← citeshttps://doi.org/10.1016/j.epsl.2018.04.046openalex-snapshot
Precession and glacial-cycle controls of monsoon precipitation isotope changes over East Asia during the Pleistocene
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.01.043openalex-snapshot
Timing and structure of Termination II in north China constrained by a precisely dated stalagmite record
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.115794openalex-snapshot
Regional controls on daily to interannual variations of precipitation isotope ratios in Southeast China: Implications for paleomonsoon reconstruction
inferred← citeshttps://doi.org/10.1016/j.epsl.2021.116758openalex-snapshot
Holocene variability of East Asian summer monsoon as viewed from the speleothem δ18 O records in central China
inferred← citeshttps://doi.org/10.1016/j.epsl.2022.117912openalex-snapshot
Determining key upstream convection and rainout zones affecting δ18O in water vapor and precipitation based on 10-year continuous observations in the East Asian Monsoon region
inferred← citeshttps://doi.org/10.1016/j.fmre.2026.06.001openalex-snapshot
Spatial heterogeneity of Holocene hydroclimatic variations and their driving mechanisms in the South Asian summer monsoon region
inferred← citeshttps://doi.org/10.1016/j.gca.2019.12.003openalex-snapshot
A novel application of triple oxygen isotope ratios of speleothems
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.04.003openalex-snapshot
200,000 years of monsoonal history recorded on the lower Bengal Fan - strong response to insolation forcing
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103700openalex-snapshot
General characteristics of climate change over China and associated dynamic mechanisms during the Last Interglacial based on PMIP4 simulations
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104132openalex-snapshot
Milankovitch-paced South Asian monsoons during Marine Isotope Stage 5
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104639openalex-snapshot
Stalagmite records of spatiotemporal hydroclimatic variations in monsoonal China during 47–12 ka BP
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104680openalex-snapshot
Evolution of the Asian summer monsoon during the Heinrich events 1–6
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104733openalex-snapshot
Nonlinear feedback of Asian summer monsoon to abrupt events in North Atlantic: Evidence from a precisely dated speleothem record during late MIS3
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104739openalex-snapshot
Variations of Asian summer monsoon and regional hydroclimate between the MIS 7.1 and 6.5
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104968openalex-snapshot
Monsoon and hydroclimate evolution during Heinrich Stadial 3 as revealed by stalagmite from Central China
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105017openalex-snapshot
A strong influence of the precession and northern high latitudinal climate on the monsoon seasonality and productivity in the Andaman Sea
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105092openalex-snapshot
Indian summer monsoon variability across the last 9000 years: New evidence from stalagmites of southwestern China
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105127openalex-snapshot
Orbital-scale precipitation oxygen isotope variations at Northern Hemisphere mid-low latitudes: Characteristics and causes
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105187openalex-snapshot
Hydroclimate changes during the last deglaciation in Central China inferred from speleothem multiple proxies
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105228openalex-snapshot
Millennial-scale precipitation isotope variability reveals spatial heterogeneity in Asian monsoon moisture during the last glacial period
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105445openalex-snapshot
Contrasting response of the Asian Summer monsoon to bipolar climates and implications for ice core chronology during Marine Isotope Stages 5c-a inferred from stalagmite record, Central China
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105736openalex-snapshot
Rapid vegetation reorganization in southern Hengduan Mountains driven by high climatic oscillations
inferred← citeshttps://doi.org/10.1016/j.gr.2021.08.008openalex-snapshot
HIRM variation in the Ganzi loess of the eastern Tibetan Plateau since the last interglacial period and its paleotemperature implications for the source region
inferred← citeshttps://doi.org/10.1016/j.heliyon.2023.e13075openalex-snapshot
Isolation and Characterization of Crude-Oil-Dependent Bacteria from the Coast of Ghana Using Oxford Nanopore Sequencing
inferred← citeshttps://doi.org/10.1016/j.jas.2021.105535openalex-snapshot
High-precision U-series dating of the late Pleistocene – early Holocene rock paintings at Tiger Leaping Gorge, Jinsha River valley, southwestern China
inferred← citeshttps://doi.org/10.1016/j.jas.2023.105922openalex-snapshot
Past rainfall patterns in Southeast Asia revealed by microanalysis of δ18O values in human teeth
inferred← citeshttps://doi.org/10.1016/j.jas.2025.106416openalex-snapshot
Cave site formation processes, climate change and hominin activities: A high-resolution microstratigraphic investigation on the terminal Pleistocene deposits at Fodongdi Cave, Yunnan Province, South China
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Different moisture regimes during the last 150 years inferred from a tree-ring δ18O network over the transitional zone of the Asian summer monsoon
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Oxygen isotope variability in precipitation, dripwater, and modern calcite responding to ENSO based on 11 years’ monitoring in Yuhua Cave, Southeast China
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Hydroclimate changes related to thermal state of the tropical Pacific in the northern coast of the South China Sea since ∼8000 cal yr B.P.
inferred← citeshttps://doi.org/10.1016/j.jseaes.2017.11.008openalex-snapshot
Hydroclimatic variability in loess δDwax records from the central Chinese Loess Plateau over the past 250 ka
inferred← citeshttps://doi.org/10.1016/j.jseaes.2019.04.024openalex-snapshot
Changes in the Asian monsoon climate during the late last interglacial recorded in oxygen isotopes of a stalagmite from the Yongxing Cave, central China
inferred← citeshttps://doi.org/10.1016/j.jseaes.2022.105435openalex-snapshot
Millennial-scale climate oscillations over the last two climatic cycles revealed by a loess–paleosol sequence from central Asia
inferred← citeshttps://doi.org/10.1016/j.jseaes.2023.105951openalex-snapshot
Changes of provenance of loess deposits in Nyingchi, southeastern Tibetan Plateau: Implications for paleoclimates since the last glacial
inferred← citeshttps://doi.org/10.1016/j.jseaes.2024.106121openalex-snapshot
Sediment provenance variations driven by sea level in the eastern Arabian Sea since the MIS 9 period: Evidence from geochemical proxies
inferred← citeshttps://doi.org/10.1016/j.margeo.2019.05.006openalex-snapshot
Sedimentary responses to the sea level and Indian summer monsoon changes in the central Bay of Bengal since 40 ka
inferred← citeshttps://doi.org/10.1016/j.margeo.2023.107010openalex-snapshot
Sedimentary modulation of magnetic mineral records in the Central Bengal Fan
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.06.013openalex-snapshot
Reconciliation of hydroclimate sequences from the Chinese Loess Plateau and low-latitude East Asian Summer Monsoon regions over the past 14,500years
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.02.005openalex-snapshot
Grain size of Lake Qinghai sediments: Implications for riverine input and Holocene monsoon variability
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.07.003openalex-snapshot
Indian summer monsoon variability in southern India during the last deglaciation: Evidence from a high resolution stalagmite δ18O record
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.11.032openalex-snapshot
Vegetation responses to late Quaternary climate change in a biodiversity hotspot, the Three Parallel Rivers region in southwestern China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.12.029openalex-snapshot
Distinct responses of East Asian and Indian summer monsoons to astronomical insolation during Marine Isotope Stages 5c and 5e
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.11.040openalex-snapshot
Indian Summer Monsoon variations and competing influences between hemispheres since ~35 ka recorded in Tengchongqinghai Lake, southwestern China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109445openalex-snapshot
Stable isotope proxy records in tropical terrestrial environments
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109879openalex-snapshot
Reconstruction of the East Asian Summer monsoon rainfall distribution at centennial scale during the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110390openalex-snapshot
Centennial- to millennial-scale Asian summer monsoon changes during the MIS 5/4 transition revealed by high-resolution stalagmite records from southwestern China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110658openalex-snapshot
Abrupt Indian summer monsoon shifts aligned with Heinrich events and D-O cycles since MIS 3
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110720openalex-snapshot
Spatio-temporal expressions of precessional-scale stalagmite δ18O variations from the Asian monsoon area
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110798openalex-snapshot
Influences on Asian summer monsoon during Dansgaard-Oeschger events 19 to 25 (70–115 kyr B.P.)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.110852openalex-snapshot
Climatic controls on travertine deposition in southern Tibet during the late Quaternary
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111047openalex-snapshot
Chronological constraints on the late Quaternary Beihai wetland deposits in southwestern China and its depositional history linked to hydroclimate change
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111230openalex-snapshot
Timing and climatic drivers for the MIS 6 glaciation in the central Himalaya: 10Be surface exposure dating of hummocky moraine northwest of Mt. Gang Benchhen, Paiku Gangri
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111265openalex-snapshot
Chinese Interstadials 14–17 recorded in a precisely U-Th dated stalagmite from the northern edge of the Asian summer monsoon during the MIS 4/3 boundary
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111290openalex-snapshot
Climatic implication of stalagmite δ13C in the middle reaches of the Yangtze River since the Last Glacial Maximum and coupling with δ18O
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111336openalex-snapshot
Modeling the timing and extent of glaciations over southeastern Tibet during the last glacial stage
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111380openalex-snapshot
Centennial-scale variability of the Indian Summer Monsoon during the middle to late Holocene and its links with ENSO activity
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111441openalex-snapshot
Hydroclimatic variation over central China during the 4.2 ka event and its implications for cultural transformation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111698openalex-snapshot
Millennial-scale changes in the Asian monsoon during the MIS12 period as recorded by a Chinese stalagmite
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111875openalex-snapshot
Chronological features of Heinrich Stadial 2 based on a high-resolution analysis of δ18O stalagmite records from China, and possible links to changes in Atlantic Meridional Overturning Circulation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111898openalex-snapshot
Atmospheric CO2 controls on the MIS 6 glaciation: 10Be chronology of moraines in the Haizishan area, southeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111959openalex-snapshot
Repeated glacial fluctuations during the Last Glacial Maximum in the southeastern Tibetan Plateau: 10Be surface exposure dating of moraines in the Lahaku Valley, Haizishan Plateau, China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111961openalex-snapshot
The centennial-resolution loess δDwax record indicates summer precipitation variations in the marginal region of the East Asian monsoon during the last deglaciation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112016openalex-snapshot
Indian summer monsoon variability during the past ~75 ka based on stable isotope records of sediments from NW India
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112067openalex-snapshot
Magnetostratigraphy and relative paleointensity study of a late Quaternary lacustrine sediment sequence from Southwest China and its chronological significance
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112593openalex-snapshot
Indian summer monsoon history during the last glacial cycle revealed by a loess sequence from the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112702openalex-snapshot
Millennial-scale hydroclimate dynamics in the Southeastern Tibetan Plateau: linkages with atmospheric circulation changes during the last glacial period
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112814openalex-snapshot
Magnetic proxy in the Heqing drill core revealed Indian Summer Monsoon variations linked with AMOC at the orbital -scale during the late Pleistocene
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112874openalex-snapshot
MIS 3 climate transitions revealed by high-resolution loess records from the eastern margin of the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113004openalex-snapshot
Paleo-productivity reconstruction in Bay of Bengal during the past 1.3 Ma: Implications for glacial-interglacial dynamics and southern hemispheric processes
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113114openalex-snapshot
Hydroclimate changes in southwestern China from Dark Age Cold Period to Medieval Climate Anomaly and their global teleconnections
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113374openalex-snapshot
Decoupling of silicate weathering and Asian monsoon evolution during the penultimate glacial and interglacial
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113406openalex-snapshot
Initiation, evolution and variability of the Asian Monsoon through the Cenozoic Era: Insights from the successions of the Weihe Basin and Loess Plateau of central China, and beyond
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113577openalex-snapshot
Regular and mechanism of millennial scale weak monsoon events during the late MIS7 to early MIS6.5 period
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113642openalex-snapshot
Different coercivity magnetic components in a lacustrine sequence from Heqing Basin and its linkage with millennial Indian summer monsoon variability since 52 ka
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113682openalex-snapshot
Variability of sea surface temperature regulated millennial-scale transition of hydroclimate in mid- and low-latitude Asia
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113764openalex-snapshot
A 5200-year record of vegetation dynamics and variations in the Indian Summer Monsoon from the Garhwal Himalaya, India
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113814openalex-snapshot
Orbital-scale Asian monsoon variability and its forcing mechanisms: A new conceptual model
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.114102openalex-snapshot
Two-stage pattern of Dansgaard–Oeschger 19.2 during MIS 4: Evidence from a high-resolution stalagmite δ18O record in southwestern China and its global correlations
inferred← citeshttps://doi.org/10.1016/j.quageo.2024.101497openalex-snapshot
An integrated study of constraining the initial 230Th of a stalagmite and its implications
inferred← citeshttps://doi.org/10.1016/j.quaint.2015.12.088openalex-snapshot
The age of human remains and associated fauna from Zhiren Cave in Guangxi, southern China
inferred← citeshttps://doi.org/10.1016/j.quaint.2016.05.013openalex-snapshot
Highly negative oxygen isotopes in precipitation in southwest China and their significance in paleoclimatic studies
inferred← citeshttps://doi.org/10.1016/j.quaint.2017.05.038openalex-snapshot
A tentative study of the relationship between annual δ18O & δD variations of precipitation and atmospheric circulations—A case from Southwest China
inferred← citeshttps://doi.org/10.1016/j.quaint.2017.08.072openalex-snapshot
Multi-scale variability of the Asian monsoon recorded in an annually-banded stalagmite during the Neoglacial from Qixing Cave, Southwestern China
inferred← citeshttps://doi.org/10.1016/j.quaint.2017.10.050openalex-snapshot
Microcodium in Chinese loess as a recorder for the oxygen isotopic composition of monsoonal rainwater
inferred← citeshttps://doi.org/10.1016/j.quaint.2018.12.007openalex-snapshot
Response of the Himalayan glacial cycles to multiple equilibrium of climate system: A review
inferred← citeshttps://doi.org/10.1016/j.quaint.2020.05.039openalex-snapshot
Millennial-scale summer monsoon oscillations over the last 260 ka revealed by high-resolution elemental results of the Mangshan loess-palaeosol sequence from the southeastern Chinese Loess Plateau
inferred← citeshttps://doi.org/10.1016/j.quaint.2020.06.050openalex-snapshot
Taxonomic reassessment of large mammals from the Pleistocene Homo-bearing site of Tham Wiman Nakin (Northeast Thailand): relevance for faunal patterns in mainland Southeast Asia
inferred← citeshttps://doi.org/10.1016/j.quaint.2021.08.001openalex-snapshot
Probing the impact of Solar System dynamics on Holocene North Atlantic cold events at the millennial-scale
inferred← citeshttps://doi.org/10.1016/j.quaint.2024.04.008openalex-snapshot
Late Holocene vegetation diversity change and potential response to climate variations on the northern Qinghai-Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.quascirev.2014.11.009openalex-snapshot
Role of seasonal transitions and westerly jets in East Asian paleoclimate
inferred← citeshttps://doi.org/10.1016/j.quascirev.2015.03.009openalex-snapshot
Astronomical and glacial forcing of East Asian summer monsoon variability
inferred← citeshttps://doi.org/10.1016/j.quascirev.2015.11.003openalex-snapshot
Changes in dominant moisture sources and the consequences for hydroclimate on the northeastern Tibetan Plateau during the past 32 kyr
inferred← citeshttps://doi.org/10.1016/j.quascirev.2016.08.009openalex-snapshot
Disentangling the impacts of climate and human colonization on the flora and fauna of the Australian arid zone over the past 100 ka using stable isotopes in avian eggshell
inferred← citeshttps://doi.org/10.1016/j.quascirev.2016.12.014openalex-snapshot
Holocene moisture changes in western China, Central Asia, inferred from stalagmites
inferred← citeshttps://doi.org/10.1016/j.quascirev.2017.02.003openalex-snapshot
Stalagmite-inferred centennial variability of the Asian summer monsoon in southwest China between 58 and 79 ka BP
inferred← citeshttps://doi.org/10.1016/j.quascirev.2017.06.009openalex-snapshot
Timing of fluvial terrace formation and concomitant travertine deposition in the upper Sutlej River (Tirthapuri, southwestern Tibet) and paleoclimatic implications
inferred← citeshttps://doi.org/10.1016/j.quascirev.2018.03.025openalex-snapshot
Response of the Asian summer monsoons to idealized precession and obliquity forcing in a set of GCMs
inferred← citeshttps://doi.org/10.1016/j.quascirev.2018.05.035openalex-snapshot
Precession-paced thermocline water temperature changes in response to upwelling conditions off southern Sumatra over the past 300,000 years
inferred← citeshttps://doi.org/10.1016/j.quascirev.2018.06.004openalex-snapshot
Late Middle Pleistocene ecology and climate in Northeastern Thailand inferred from the stable isotope analysis of Khok Sung herbivore tooth enamel and the land mammal cenogram
inferred← citeshttps://doi.org/10.1016/j.quascirev.2018.07.021openalex-snapshot
High resolution monsoon precipitation changes on southeastern Tibetan Plateau over the past 2300 years
inferred← citeshttps://doi.org/10.1016/j.quascirev.2018.09.027openalex-snapshot
Hemipelagic and turbiditic deposits constrain lower Bengal Fan depositional history through Pleistocene climate, monsoon, and sea level transitions
inferred← citeshttps://doi.org/10.1016/j.quascirev.2019.02.023openalex-snapshot
A new speleothem record of the penultimate deglacial: Insights into spatial variability and centennial-scale instabilities of East Asian monsoon
inferred← citeshttps://doi.org/10.1016/j.quascirev.2019.04.003openalex-snapshot
Synchronous change of temperature and moisture over the past 50 ka in subtropical southwest China as indicated by biomarker records in a crater lake
inferred← citeshttps://doi.org/10.1016/j.quascirev.2019.06.006openalex-snapshot
Abrupt changes in Indian summer monsoon strength during the last deglaciation and early Holocene based on stable isotope evidence from Lake Chenghai, southwest China
inferred← citeshttps://doi.org/10.1016/j.quascirev.2019.106127openalex-snapshot
Landscape dynamics and human-environment interactions in the northern foothills of Cho Oyu and Mount Everest (southern Tibet) during the Late Pleistocene and Holocene
inferred← citeshttps://doi.org/10.1016/j.quascirev.2020.106218openalex-snapshot
Millennial-scale Asian monsoon variability during MIS 9 revealed by a high-resolution stalagmite δ18O record in Luoshui Cave, central China
inferred← citeshttps://doi.org/10.1016/j.quascirev.2020.106261openalex-snapshot
Variation of the Asian summer monsoon since the last glacial-interglacial recorded in a stalagmite from southwest China
inferred← citeshttps://doi.org/10.1016/j.quascirev.2020.106359openalex-snapshot
Sensitivity of altitudinal vegetation in southwest China to changes in the Indian summer monsoon during the past 68000 years
inferred← citeshttps://doi.org/10.1016/j.quascirev.2020.106619openalex-snapshot
Glacial-interglacial variation in catchment weathering and erosion paces the Indian summer monsoon during the Pleistocene
inferred← citeshttps://doi.org/10.1016/j.quascirev.2020.106699openalex-snapshot
East Asian monsoon changes early in the last deglaciation and insights into the interpretation of oxygen isotope changes in the Chinese stalagmite record
inferred← citeshttps://doi.org/10.1016/j.quascirev.2020.106745openalex-snapshot
Planktic foraminiferal δ18O values indicate precipitation variability in the southeastern South China Sea over the last 175 ka BP
inferred← citeshttps://doi.org/10.1016/j.quascirev.2020.106793openalex-snapshot
New insights towards an integrated understanding of NE Asian monsoon during mid to late Holocene
inferred← citeshttps://doi.org/10.1016/j.quascirev.2021.106911openalex-snapshot
A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon
inferred← citeshttps://doi.org/10.1016/j.quascirev.2021.106947openalex-snapshot
Variability of PDO identified by a last 300-year stalagmite δ18O record in Southwest China
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107403openalex-snapshot
Indian Summer Monsoon variability 140–70 thousand years ago based on multi-proxy records from the Bay of Bengal
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107443openalex-snapshot
A high-resolution stalagmite record from Luoshui Cave, Central China over the past 23.5 kyr
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107499openalex-snapshot
A new stalagmite oxygen isotope record over the last 1350 years: Insights into spatial variation in Asian summer monsoon and temperature forcing
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107593openalex-snapshot
A review of orbital-scale monsoon variability and dynamics in East Asia during the Quaternary
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107658openalex-snapshot
Orbital-scale hydroclimate variations in the southern Tibetan Plateau over the past 414,000 years
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107736openalex-snapshot
Amplified and suppressed regional imprints of global warming events on the southeastern Tibetan Plateau during MIS 3–2
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107761openalex-snapshot
A strong influence of the mid-Pleistocene transition on the monsoon and associated productivity in the Indian Ocean
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107808openalex-snapshot
Structural similarity between Termination III and I
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107844openalex-snapshot
Spatial pattern of orbital-to millennial-scale East Asian stalagmite δ18O variations during MIS 3
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108193openalex-snapshot
The spatio-temporal pattern of Asian summer monsoon during glacial Termination II recorded by Chinese stalagmite δ18O
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108291openalex-snapshot
Enhanced summer extreme precipitation over the Asian-African land monsoon regions during past warm periods: A modelling perspective from CESM2
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108327openalex-snapshot
Stalagmite-based long-term and multi-centennial hydroclimatic variations in southwestern China during the Holocene and relations to global climate change
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108434openalex-snapshot
Synchronous anti-phase variations between the East Asian summer monsoon and South America Summer Monsoon during Heinrich stadial 2
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108441openalex-snapshot
Vertical biome shifts and climate changes since the last glacial maximum in the southeastern margin of the Tibetan plateau, Southwest China
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108482openalex-snapshot
Enhanced Asian hydroclimate instability during early MIS 6.5
inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.108723openalex-snapshot
Millennial to orbital scale Indian summer monsoon evolution inferred from grain size end-members in Tengchongbeihai wetland, southwestern China
inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.108946openalex-snapshot
Distinct response of Asian summer monsoon circulation and precipitation to orbital forcing during six Heinrich events
inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.108971openalex-snapshot
The LGM termination in the southeastern Tibetan plateau: View from high-frequency LGM glacier fluctuations in the Boshula mountain range
inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.109069openalex-snapshot
Transitions between Chinese dynasties influenced by spatial-patterned precipitation
inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.109152openalex-snapshot
A high-resolution multiproxy speleothem record of Eastern China hydroclimate variation during last glacial maximum
inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.109179openalex-snapshot
Climate-controlled distribution of erosion over the Himalaya in the late Quaternary: Evidence from Sr-Nd isotope variability in paleo-Yamuna channel sediments
inferred← citeshttps://doi.org/10.1016/j.quascirev.2025.109231openalex-snapshot
Mid-to-late Holocene temperature variability in southwestern China
inferred← citeshttps://doi.org/10.1016/j.quascirev.2025.109267openalex-snapshot
Elevated equilibrium line altitude over High Mountain Asia during the Last Interglacial
inferred← citeshttps://doi.org/10.1016/j.quascirev.2025.109268openalex-snapshot
Hydroclimate variability in southwest China during Marine Isotope Stage 9: Insights from multi–proxy stalagmite records
inferred← citeshttps://doi.org/10.1016/j.quascirev.2025.109298openalex-snapshot
Magnetotactic bacterial activity indicates redox conditions in an upland lake in southwest China since the last glaciation
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