46 citations as recorded by crossref.

1. A detailed East Asian monsoon history of Greenland Interstadial 21 in southeastern China X. Zhang et al. 10.1016/j.palaeo.2020.109752
2. The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records . Zhang et al. 10.3390/quat2030026
3. Sign-switching ecological changes in the Mediterranean Basin at 4.2 ka BP F. Di Rita et al. 10.1016/j.gloplacha.2021.103713
4. Hydroclimatic variation over central China during the 4.2 ka event and its implications for cultural transformation W. Zhang et al. 10.1016/j.palaeo.2023.111441
5. Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans F. Duan et al. 10.5194/cp-16-475-2020
6. The impact and implications of aragonite-to-calcite transformation on speleothem trace element composition M. He et al. 10.1016/j.sedgeo.2021.106010
7. Genomic investigation of the Chinese alligator reveals wild‐extinct genetic diversity and genomic consequences of their continuous decline S. Yang et al. 10.1111/1755-0998.13702
8. El Niño/Southern Oscillation during the 4.2 ka event recorded by growth rates of corals from the North South China Sea S. Dang et al. 10.1007/s13131-019-1520-5
9. Isotope composition of daily precipitation from 2019 to 2020 in Sanming, southeastern China J. Cai et al. 10.3389/fenvs.2022.1061882
10. Climate and sea-level fluctuations on the western coast of Bohai Bay during the 4.2 ka event: Multi-proxy evidence from the Nandagang area of Cangzhou, China H. You et al. 10.1016/j.quascirev.2023.108467
11. 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
12. Climate–human–environment interactions in the middle Yangtze Basin (central China) during the middle Holocene, based on pollen and geochemical records from the Sanfangwan Site M. Jia et al. 10.1016/j.catena.2021.105357
13. Hydroclimatic changes in south-central China during the 4.2 ka event and their potential impacts on the development of Neolithic culture T. Wang et al. 10.1017/qua.2022.11
14. Considering change with archaeological data: Reevaluating local variation in the role of the ~4.2k BP event in Northwest China Y. Jaffe & A. Hein 10.1177/0959683620970254
15. Collapse of the Liangzhu and other Neolithic cultures in the lower Yangtze region in response to climate change H. Zhang et al. 10.1126/sciadv.abi9275
16. Abrupt Drying on the Southeast Coast of China During the Mid‐to‐Late Holocene Transition X. Wang et al. 10.1029/2022GL100257
17. Holocene development and human use of mangroves and limestone forest at an ancient hong lagoon in the Tràng An karst, Ninh Binh, Vietnam S. O’Donnell et al. 10.1016/j.quascirev.2020.106416
18. Climate as a factor for Neolithic cultural collapses approximately 4000 years BP in China Q. Sun et al. 10.1016/j.earscirev.2019.102915
19. 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
20. Chinese stalagmite paleoclimate researches: A review and perspective H. Cheng et al. 10.1007/s11430-019-9478-3
21. Expression of the “4.2 ka event” in the southern Rocky Mountains, USA D. Liefert & B. Shuman 10.5194/cp-18-1109-2022
22. A gradual transition into Greenland interstadial 14 in southeastern China based on a sub-decadally-resolved stalagmite record X. Zhang et al. 10.1016/j.quascirev.2020.106769
23. Seasonal and Inter-Annual Variations of Stable Isotopic Characteristics of Rainfall and Cave Water in Shennong Cave, Southeast China, and Its Paleoclimatic Implication Y. Tian et al. 10.3389/feart.2021.794762
24. Middle-late Holocene environment change induced by climate and human based on multi-proxy records from the middle and lower reaches of Yangtze River, eastern China R. Ke et al. 10.1007/s11430-022-1101-2
25. 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
26. Human settlement distribution patterns during the Longshan and Xinzhai-Erlitou periods and their hydrogeomorphic contexts in the Central Plains, China K. Li & W. Gao 10.1016/j.catena.2021.105433
27. The East Asian summer monsoon, the Indian summer monsoon, and the midlatitude westerlies at 4.2 ka BP H. Weiss 10.1073/pnas.2200796119
28. 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
29. 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
30. Spatial and temporal characteristics of the precipitation response to the 4.2 ka event in the Asian summer monsoon region D. Wang et al. 10.1016/j.gloplacha.2022.103854
31. Climate changes in Northeastern Brazil from deglacial to Meghalayan periods and related environmental impacts G. Utida et al. 10.1016/j.quascirev.2020.106655
32. New insights towards an integrated understanding of NE Asian monsoon during mid to late Holocene J. Zhao et al. 10.1016/j.quascirev.2020.106793
33. Antipodal pattern of millet and rice demography in response to 4.2 ka climate event in China K. He et al. 10.1016/j.quascirev.2022.107786
34. Mismatches of scale in the application of paleoclimatic research to Chinese archaeology Y. Jaffe et al. 10.1017/qua.2020.60
35. 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
36. A high-resolution stalagmite record from Luoshui Cave, Central China over the past 23.5 kyr Z. Wang et al. 10.1016/j.quascirev.2022.107443
37. Climatic implication of stalagmite δ13C in the middle reaches of the Yangtze River since the Last Glacial Maximum and coupling with δ18O Z. Wang et al. 10.1016/j.palaeo.2022.111290
38. SISALv2: a comprehensive speleothem isotope database with multiple age–depth models L. Comas-Bru et al. 10.5194/essd-12-2579-2020
39. The Spatiotemporal Patterns of Human Settlement during the Longshan and Erlitou Periods in Relation to Extreme Floods and Subsistence Strategy in the Upper and Middle Qin River Reaches, Central China W. Gao et al. 10.3390/land11071088
40. Evidence from giant-clam <i>δ</i><sup>18</sup>O of intense El Ninõ–Southern Oscillation-related variability but reduced frequency 3700 years ago Y. Hu et al. 10.5194/cp-16-597-2020
41. Complex Pathways Towards Emergent Pastoral Settlements: New Research on the Bronze Age Xindian Culture of Northwest China Y. Jaffe et al. 10.1007/s10963-021-09160-w
42. 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
43. A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon H. Zhang et al. 10.1016/j.quascirev.2021.106911
44. Role of the Summer Monsoon Variability in the Collapse of the Ming Dynasty: Evidences From Speleothem Records J. Zhao et al. 10.1029/2021GL093071
45. Stalagmite-based long-term and multi-centennial hydroclimatic variations in southwestern China during the Holocene and relations to global climate change F. Duan et al. 10.1016/j.quascirev.2023.108327
46. Double-plunge structure of the East Asian summer monsoon during Heinrich stadial 1 recorded in Xianyun Cave, southeastern China W. Qiu et al. 10.1016/j.quascirev.2022.107442