167 citations as recorded by crossref.

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46. Role of the Summer Monsoon Variability in the Collapse of the Ming Dynasty: Evidences From Speleothem Records J. Zhao et al. 10.1029/2021GL093071
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55. A stalagmite test of North Atlantic SST and Iberian hydroclimate linkages over the last two glacial cycles R. Denniston et al. 10.5194/cp-14-1893-2018
56. Evaluating the timing and structure of the 4.2 ka event in the Indian summer monsoon domain from an annually resolved speleothem record from Northeast India G. Kathayat et al. 10.5194/cp-14-1869-2018
57. Trace element variations in Indian speleothems: Insights into the Holocene climate I. Roy & N. Gandhi 10.1016/j.quaint.2024.08.007
58. Age of the Mt. Ortles ice cores, the Tyrolean Iceman and glaciation of the highest summit of South Tyrol since the Northern Hemisphere Climatic Optimum P. Gabrielli et al. 10.5194/tc-10-2779-2016
59. Speleothem record attests to stable environmental conditions during Neanderthal–modern human turnover in southern Italy A. Columbu et al. 10.1038/s41559-020-1243-1
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62. StalGrowth—A Program to Estimate Speleothem Growth Rates and Seasonal Growth Variations R. Vieten & F. Hernandez 10.3390/geosciences11050187
63. Is Chinese stalagmite δ18O solely controlled by the Indian summer monsoon? D. Li et al. 10.1007/s00382-019-04671-x
64. Local and Regional Indian Summer Monsoon Precipitation Dynamics During Termination II and the Last Interglacial M. Magiera et al. 10.1029/2019GL083721
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68. Climate dynamics during the penultimate glacial period recorded in a speleothem from Kanaan Cave, Lebanon (central Levant) C. Nehme et al. 10.1017/qua.2018.18
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70. Change of marine redox environment in the western Okinawa Trough since the mid-Holocene: Evidence based on geochemical records B. Mi et al. 10.1016/j.jseaes.2023.105731
71. Late Quaternary Climate Variability and Change from Aotearoa New Zealand Speleothems: Progress in Age Modelling, Oxygen Isotope Master Record Construction and Proxy-Model Comparisons A. Lorrey et al. 10.3390/quat3030024
72. Decline in seasonal predictability potentially destabilized Classic Maya societies T. Braun et al. 10.1038/s43247-023-00717-5
73. Intertropical convergence zone variability in the Neotropics during the Common Era Y. Asmerom et al. 10.1126/sciadv.aax3644
74. Chemical weathering patterns driven by solar insolation and Indian monsoon in the southern Bay of Bengal since the last glaciation H. Zhang et al. 10.1016/j.jseaes.2023.105843
75. Holocene Hydroclimate Variability Along the Southern Patagonian Margin (Chile) Reconstructed from Cueva Chica Speleothems C. Nehme et al. 10.2139/ssrn.4172978
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78. The potential of gypsum speleothems for paleoclimatology: application to the Iberian Roman Humid Period F. Gázquez et al. 10.1038/s41598-020-71679-3
79. New advances in the dating of speleothems – An introduction R. Drysdale et al. 10.1016/j.quageo.2012.11.008
80. The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems K. Atsawawaranunt et al. 10.5194/essd-10-1687-2018
81. Climate changes in Northeastern Brazil from deglacial to Meghalayan periods and related environmental impacts G. Utida et al. 10.1016/j.quascirev.2020.106655
82. Extrapolar climate reversal during the last deglaciation Y. Asmerom et al. 10.1038/s41598-017-07721-8
83. Winter hydroclimate contrasts between southern and northern Europe at ∼ 5.2 ka V. Drăgușin et al. 10.1016/j.palaeo.2023.111863
84. Glacial changes in sea level modulated millennial-scale variability of Southeast Asian autumn monsoon rainfall E. Patterson et al. 10.1073/pnas.2219489120
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86. The Indian monsoon variability and civilization changes in the Indian subcontinent G. Kathayat et al. 10.1126/sciadv.1701296
87. Noble gas based temperature reconstruction on a Swiss stalagmite from the last glacial–interglacial transition and its comparison with other climate records E. Ghadiri et al. 10.1016/j.epsl.2018.05.019
88. PRYSM v2.0: A Proxy System Model for Lacustrine Archives S. Dee et al. 10.1029/2018PA003413
89. Hydro-climatic variability in the southwestern Indian Ocean between 6000 and 3000 years ago H. Li et al. 10.5194/cp-14-1881-2018
90. Orchestrated decline of Asian summer monsoon and Atlantic meridional overturning circulation in global warming period J. Zhao et al. 10.59717/j.xinn-geo.2023.100011
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92. A multi-proxy stalagmite record indicates a shift in forcing of twentieth century drought events in Normandy I. Bejarano-Arias et al. 10.1038/s41598-024-77674-2
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98. Megadrought and cultural exchange along the proto-silk road L. Tan et al. 10.1016/j.scib.2020.10.011
99. Timing and Structure of 10.9 and 10.3 ka BP Events Revealed by Annually Laminated Stalagmite Records From Shihua Cave, Northern China M. Li et al. 10.1029/2022PA004459
100. Iberian hydroclimate variability and the Azores High during the last 1200 years: evidence from proxy records and climate model simulations D. Thatcher et al. 10.1007/s00382-022-06427-6
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126. Simple noise estimates and pseudoproxies for the last 21 000 years O. Bothe et al. 10.5194/essd-11-1129-2019
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129. Climate variability in the western Mediterranean between 121 and 67 ka derived from a Mallorcan speleothem record O. Dumitru et al. 10.1016/j.palaeo.2018.06.028
130. Climate history of the southwestern United States based on Estancia Basin hydrologic variability from 69 to 10 ka K. Menking et al. 10.1016/j.quascirev.2018.09.030
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157. An uncertainty-focused database approach to extract spatiotemporal trends from qualitative and discontinuous lake-status histories G. De Cort et al. 10.1016/j.quascirev.2021.106870
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164. Southern hemisphere forced millennial scale Indian summer monsoon variability during the late Pleistocene S. Band et al. 10.1038/s41598-022-14010-6
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