15 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. 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