16 citations as recorded by crossref.

1. Archaeal ammonia oxidation plays a part in late Quaternary nitrogen cycling in the South China Sea L. Dong et al. 10.1016/j.epsl.2018.12.023
2. Significant SST differences between peak MIS5 and MIS1 along the low-latitude western North Pacific margin M. Wang & Y. Zong 10.1016/j.quascirev.2019.106060
3. Quantitative reconstruction of paleoclimate in central Japan for the past 158,000 years based on a modern analogue technique of pollen composition T. Kigoshi et al. 10.1016/j.quaint.2017.05.015
4. Asynchronous Variation in the Quaternary East Asian Winter Monsoon Associated With the Tropical Pacific ENSO‐Like System D. Zhao et al. 10.1029/2019GL083033
5. A Transient Modeling Study of the Latitude Dependence of East Asian Winter Monsoon Variations on Orbital Timescales X. Xie et al. 10.1029/2019GL083060
6. 200,000 years of monsoonal history recorded on the lower Bengal Fan - strong response to insolation forcing M. Weber et al. 10.1016/j.gloplacha.2018.04.003
7. A global database of Holocene paleotemperature records D. Kaufman et al. 10.1038/s41597-020-0445-3
8. Eustatic, Climatic and Tectonic Controls on the Evolution of a Middle to Late Holocene Coastal Dune System in Shimokita, Northeast Japan K. Minoura & N. Nakamura 10.3390/geosciences10100410
9. BAYSPLINE: A New Calibration for the Alkenone Paleothermometer J. Tierney & M. Tingley 10.1002/2017PA003201
10. Hemipelagic and turbiditic deposits constrain lower Bengal Fan depositional history through Pleistocene climate, monsoon, and sea level transitions M. Weber & B. Reilly 10.1016/j.quascirev.2018.09.027
11. Shrinkage of East Asia Winter Monsoon Associated With Increased ENSO Events Since the Mid‐Holocene J. Wu et al. 10.1029/2018JD030148
12. New insights into upper MOW variability over the last 150kyr from IODP 339 Site U1386 in the Gulf of Cadiz S. Kaboth et al. 10.1016/j.margeo.2015.08.014
13. Hydrographic variability in the northern South China Sea over the past 45,000 years: New insights based on temperature reconstructions by U k’ 37 and TEX H 86 proxies from a marine sediment core (MD972146) D. Lin et al. 10.1016/j.quaint.2017.09.029
14. Glacial cooling as inferred from marine temperature proxies TEXH86 and UK′37 S. Ho & T. Laepple 10.1016/j.epsl.2014.10.033
15. CO 2 ‐Induced Decoupling of Tropical Surface and Thermocline Water Temperature at the Onset of Interglacials L. Dong et al. 10.1029/2020GL088805
16. Glacial changes in tropical climate amplified by the Indian Ocean P. DiNezio et al. 10.1126/sciadv.aat9658