64 citations as recorded by crossref.

1. Low-latitude forcing on 4.2 ka event indicated by records in the Asian monsoon region X. Zhou et al. 10.1016/j.gloplacha.2024.104401
2. Geoscientific and Geoheritage Value of Waterfall Calc Tufa and Speleothem Deposits from Semi-arid Upland Deccan Traps, India M. Ukey & R. Pardeshi 10.1007/s12371-023-00828-7
3. Environmental variability at the margin of the South American monsoon system recorded by a high-resolution sediment record from Lagoa Dourada (South Brazil) B. Zolitschka et al. 10.1016/j.quascirev.2021.107204
4. Reply to Weiss: Tree-ring stable oxygen isotopes suggest an increase in Asian monsoon rainfall at 4.2 ka BP B. Yang et al. 10.1073/pnas.2204067119
5. Climatic and hydrological variations on the southwestern Tibetan Plateau during the last 30,000 years inferred from a sediment core of Lake Zabuye M. Li et al. 10.1016/j.quaint.2022.10.015
6. Late Quaternary record of Indian summer monsoon‐induced stratification and productivity collapse in the Andaman Sea A. Sijinkumar et al. 10.1002/jqs.3278
7. Monitoring hydroecology and climatic variability since ~4.6 ka from palynological, sedimentological and environmental perspectives in an Ox-bow lake, Central Ganga Plain, India A. Farooqui et al. 10.1177/09596836231183067
8. Controls on Speleothem Initial 234U/238U Ratios in a Monsoon Climate J. Oster et al. 10.1029/2023GC010899
9. Mid-late Holocene climatic reconstruction from coastal dunes of the western Kachchh, India M. Dabhi et al. 10.1016/j.quaint.2021.09.011
10. The late Holocene hydroclimate variability in the Northwest Himalaya: Sedimentary clues from the Wular Lake, Kashmir Valley A. Lone et al. 10.1016/j.jseaes.2022.105184
11. Trace element variations in Indian speleothems: Insights into the Holocene climate I. Roy & N. Gandhi 10.1016/j.quaint.2024.08.007
12. A 17,000-year multi-proxy study of the Indian Summer Monsoon from Lake Dian, Yunnan, China A. Hillman et al. 10.1016/j.palaeo.2021.110292
13. The centennial-resolution loess δDwax record indicates summer precipitation variations in the marginal region of the East Asian monsoon during the last deglaciation Z. Wang et al. 10.1016/j.palaeo.2023.111961
14. Diatom-based indications of an environmental regime shift and droughts associated with seasonal monsoons during the Holocene in Biển Hồ maar lake, the Central Highlands, Vietnam H. Đào-Trung et al. 10.1177/09596836241236342
15. Increase in summer monsoon rainfall over the northeast India during El Niño years since 1600 P. Kiran Kumar & A. Singh 10.1007/s00382-021-05743-7
16. Atmospheric blocking induced by the strengthened Siberian High led to drying in west Asia during the 4.2 ka BP event – a hypothesis A. Perşoiu et al. 10.5194/cp-15-781-2019
17. Abrupt changes in the southwest monsoon during Mid-Late Holocene in the western Bay of Bengal P. Govil et al. 10.1016/j.jseaes.2022.105100
18. Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology S. Helama & M. Oinonen 10.1016/j.quascirev.2019.04.013
19. The ‘4.2 ka drought event’ and the fall of the Harappan Civilization: A critical review T. Jahan & M. Quamar 10.1016/j.revpalbo.2024.105187
20. The Indian Summer Monsoon from a Speleothem δ18O Perspective—A Review N. Kaushal et al. 10.3390/quat1030029
21. Larger floods of Himalayan foothill rivers sustained flows in the Ghaggar–Hakra channel during Harappan age A. Singh et al. 10.1002/jqs.3320
22. Hydroclimate change in the Garhwal Himalaya, India at 4200 yr BP coincident with the contraction of the Indus civilization E. Niederman et al. 10.1038/s41598-021-02496-5
23. Investigating possible links between Holocene environmental changes and cultural transitions across India D. Behera & P. Chauhan 10.1177/09596836231157060
24. A Holocene history of the Indian monsoon from Qilu Lake, southwestern China A. Hillman et al. 10.1016/j.quascirev.2019.106051
25. Debris flow events of 4000 a BP and its resulting archaeological site destruction in Qian River gorge, the upper reach of Wei River, central China S. Fan et al. 10.1002/gj.3879
26. Abrupt changes in Indian summer monsoon strength during the last ~900 years and their linkages to socio-economic conditions in the Indian subcontinent A. Gupta et al. 10.1016/j.palaeo.2019.109347
27. Chinese stalagmite paleoclimate researches: A review and perspective H. Cheng et al. 10.1007/s11430-019-9478-3
28. Formal subdivision of the Quaternary System/Period: Present status and future directions M. Head 10.1016/j.quaint.2019.05.018
29. Holocene climate events and associated land use changes in the eastern coast of India: Inferences from the Chilika Lagoon R. Ahmad Shah et al. 10.1177/09596836221106964
30. Sign-switching ecological changes in the Mediterranean Basin at 4.2 ka BP F. Di Rita et al. 10.1016/j.gloplacha.2021.103713
31. Weakening monsoon event during 2.8 ka BP in East China linked to the North Atlantic cooling X. Jin et al. 10.1016/j.quascirev.2023.108037
32. Tropical Indian Ocean basin hydroclimate at the Mid- to Late-Holocene transition and the double drying hypothesis N. Scroxton et al. 10.1016/j.quascirev.2022.107837
33. Mismatches of scale in the application of paleoclimatic research to Chinese archaeology Y. Jaffe et al. 10.1017/qua.2020.60
34. Fossil leaf wax hydrogen isotopes reveal variability of Atlantic and Mediterranean climate forcing on the southeast Iberian Peninsula between 6000 to 3000 cal. BP J. Schirrmacher et al. 10.1371/journal.pone.0243662
35. Regional Character of the “Global Monsoon”: Paleoclimate Insights from Northwest Indian Lacustrine Sediments Y. Dixit 10.5670/oceanog.2020.206
36. A substantial meltwater event on the northeastern Tibetan Plateau during the middle to late Holocene transition Z. Wang et al. 10.1016/j.quascirev.2024.108996
37. Indian summer monsoon variability in northeastern India during the last two millennia S. Dutt et al. 10.1016/j.quaint.2020.10.021
38. Response of trace and rare earth elements to environmental changes in a stalagmite from southern India for the last deglaciation W. Raza et al. 10.1016/j.quaint.2023.09.003
39. Recurring summer and winter droughts from 4.2-3.97 thousand years ago in north India A. Giesche et al. 10.1038/s43247-023-00763-z
40. Subdividing the Holocene Series/Epoch: formalization of stages/ages and subseries/subepochs, and designation of GSSPs and auxiliary stratotypes M. WALKER et al. 10.1002/jqs.3097
41. Reconstruction of the late Holocene climate variability from the summer monsoon dominated Bhagirathi valley, western Himalaya I. Roy et al. 10.1016/j.jseaes.2022.105080
42. SISALv2: a comprehensive speleothem isotope database with multiple age–depth models L. Comas-Bru et al. 10.5194/essd-12-2579-2020
43. Spatially diverse hydroclimatic response to the 4.2 ka event in the Asian monsoon region J. Lin et al. 10.1016/j.quascirev.2022.107809
44. Mid–late Holocene event registered in organo-siliciclastic sediments of Lagoa Salgada carbonate system, southeast Brazil A. Soares Cruz et al. 10.5194/cp-15-1363-2019
45. Additional multi-proxy stalagmite evidence from northeast Namibia supports recent models of wetter conditions during the 4.2 ka Event in the Southern Hemisphere L. Railsback et al. 10.1016/j.palaeo.2021.110756
46. Is bat guano a potential pollen trap? A comparative assessment from conventional soil and moss substrates from Eraaning Cave of Meghalaya, India S. Basumatary & S. Tripathi 10.1016/j.revpalbo.2021.104539
47. High-frequency shifts in the Indian summer monsoon following termination of the YD event A. Gupta et al. 10.1016/j.quascirev.2021.106888
48. Holocene Monsoon Change and Abrupt Events on the Western Chinese Loess Plateau as Revealed by Accurately Dated Stalagmites L. Tan et al. 10.1029/2020GL090273
49. Middle to late Holocene hydroclimate instability in the Yangtze River Delta region of China inferred from phytolith records, and its implications for societal disruption L. Xueming et al. 10.1016/j.palaeo.2024.112079
50. A stalagmite δ18O record from Jinfo Cave, southern China reveals early-mid holocene variations in the East Asian Summer Monsoon X. Yang et al. 10.1016/j.quaint.2020.01.002
51. Landscape evolution of the NW Himalayan rivers during the late Quaternary and their non-contemporaneity to the Harappan Civilization I. Khan et al. 10.1016/j.quascirev.2024.108622
52. Last 10 millennial history of Indian summer monsoon in the Bengal region – a multi-proxy reconstruction from a lacustrine archive R. Ghosh et al. 10.1016/j.palaeo.2022.111308
53. Evidence for Seawater Retreat With Advent of Meghalayan Era (∼4200 a BP) in a Coastal Harappan Settlement A. Das et al. 10.1029/2021GC010264
54. Pastoralism, climate change, and the transformation of the Indus Civilization in Gujarat: Faunal analyses and biogenic isotopes B. Chase et al. 10.1016/j.jaa.2020.101173
55. Local hydrology control of radiocarbon in stalagmites from the Kyusendo Cave, Kumamoto, Japan S. Hirabayashi et al. 10.1016/j.qsa.2024.100232
56. A Bayesian change point analysis re-examines the 4.2 ka BP event in southeast Europe and southwest Asia Z. Bora Ön 10.1016/j.quascirev.2023.108163
57. Surface oceanographic changes from ∼ 25,000 to 3500 cal yr BP in the eastern Arabian Sea J. Majumder et al. 10.1016/j.gloplacha.2024.104397
58. New definition for the subdivision of the Holocene Epoch and climate S. Hirabayashi & Y. Yokoyama 10.4116/jaqua.59.129
59. Mid–late Holocene palaeoclimate and biogeochemical evolution of Wular Lake, Kashmir Valley, India R. Shah et al. 10.1002/jqs.3565
60. Paleoenvironmental reconstruction in La Paz Bay, Gulf of California: Evidence from δ18O in Chione californiensis F. Arenas et al. 10.1177/09596836211066594
61. A Bayesian test for the 4.2 ka BP abrupt climatic change event in southeast Europe and southwest Asia using structural time series analysis of paleoclimate data Z. Ön et al. 10.1007/s10584-021-03010-6
62. Impact of Indian Summer Monsoon Change on Ancient Indian Civilizations During the Holocene A. Laskar & A. Bohra 10.3389/feart.2021.709455
63. Timing and structure of the Younger Dryas event and its underlying climate dynamics H. Cheng et al. 10.1073/pnas.2007869117
64. Imprints of Holocene aridity variability in the Aegean Sea and interconnections with north-latitude areas A. Noti et al. 10.1177/09596836241247300