17 citations as recorded by crossref.

1. A novel application of triple oxygen isotope ratios of speleothems L. Sha et al. 10.1016/j.gca.2019.12.003
2. Variations of the global annual mean surface temperature during the past 2000 years: results from the CESM1 Z. Wang et al. 10.1007/s00704-019-02775-2
3. The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records . Zhang et al. 10.3390/quat2030026
4. Precipitation variability over Northwest Himalaya from ∼4.0 to 1.9 ka BP with likely impact on civilization in the foreland areas B. Kotlia et al. 10.1016/j.jseaes.2017.11.025
5. East Asian Monsoon Variability Since the Sixteenth Century N. Goodkin et al. 10.1029/2019GL081939
6. New insights on Chinese cave δ18O records and their paleoclimatic significance X. Liu et al. 10.1016/j.earscirev.2020.103216
7. Modern aragonite formation at near-freezing conditions in an alpine cave, Carnic Alps, Austria C. Spötl et al. 10.1016/j.chemgeo.2016.04.017
8. High-resolution δ18O and δ13C records of an AMS 14C and 230Th/U dated stalagmite from Xinya Cave in Chongqing: Climate and vegetation change during the late Holocene J. Li et al. 10.1016/j.quaint.2017.06.075
9. High-resolution δ 18 O and δ 13 C records during the past 65 ka from Fengyu Cave in Guilin: Variation of monsoonal climates in south China H. Li et al. 10.1016/j.quaint.2016.08.048
10. The first high-resolution stalagmite record from Taiwan: Climate and environmental changes during the past 1300 years H. Li et al. 10.1016/j.jseaes.2015.07.025
11. Sedimentary rhythm of Mn-carbonate laminae induced by East Asian summer monsoon variability and human activity in Lake Ohnuma, southwest Hokkaido, northern Japan N. Katsuta et al. 10.1016/j.quascirev.2020.106576
12. δ 18 O, δ 13 C, elemental content and depositional features of a stalagmite from Yelang Cave reflecting climate and vegetation changes since late Pleistocene in central Guizhou, China M. Zhao et al. 10.1016/j.quaint.2016.07.022
13. Changes in climate and vegetation of central Guizhou in southwest China since the last glacial reflected by stalagmite records from Yelang Cave M. Zhao et al. 10.1016/j.jseaes.2015.07.021
14. Are aragonite stalagmites reliable paleoclimate proxies? Tests for oxygen isotope time-series replication and equilibrium M. Lachniet 10.1130/B31161.1
15. A framework for triple oxygen isotopes in speleothem paleoclimatology T. Huth et al. 10.1016/j.gca.2021.11.002
16. Variations of monsoonal rain and vegetation during the past millennium in Tiangui Mountain, North China reflected by stalagmite δ18O and δ13C records from Zhenzhu Cave J. Yin et al. 10.1016/j.quaint.2017.06.039
17. Role of the Summer Monsoon Variability in the Collapse of the Ming Dynasty: Evidences From Speleothem Records J. Zhao et al. 10.1029/2021GL093071