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[31]Li, D., Zhang, X.*, Hu, D., Li, D., Zhang, G., Zhang, X., Ling, H-F., Xu, Y., Shen, Y., 2020. Multiple S-isotopic constraints on paleo-redox and sulfate concentrations across the Ediacaran-Cambrian transition in South China. Precambrian Research 349, 105500.
[32]Gao, Y., Zhang, X.*, Xu, Y., Fang, C., Gong, Y., Shen, Y., 2020. High primary productivity during the Ediacaran Period revealed by the covariation of paired C-isotopic records from South China. Precambrian Research 349, 105411.
[33]Li, D.*, Zhang, X.*, Zhang, X., Zhu, H., Peng, S, Sun, L., Shen, Y., 2020. A paired carbonate–organic δ13C approach to understanding the Cambrian Drumian carbon isotope excursion (DICE). Precambrian Research 349, 105503.
[34]Chen, K., Hu, D., Zhang, X., Zhu, H., Sun, L., Li, M., Shen, Y.*, 2020. Minor Δ33S anomalies coincide with biotic turnover events during the Great Ordovician Biodiversification Event (GOBE) in South China. Global and Planetary Change 184, 103069.
[35]Zhang, X.*, Gao, Y., Chen, X., Hu, D., Li, M., Wang, C., Shen, Y., 2019. Nitrogen isotopic composition of sediments from the eastern Tethys during Oceanic Anoxic Event 2. Palaeogeography, Palaeoclimatology, Palaeoecology 515, 123-133.
[36]Liu, X., Zhan, T.*, Zhou, X., Wu, H., Li, Q., Zhao, C., Qiao, Y., Jiang, S., Tu, L., Ma, Y., Zhang, J., Jiang, X., Lou, B., Zhang, X.*, Zhou, X.*, 2019. Late onset of the Holocene rainfall maximum in northeastern China inferred from a pollen record from the sediments of Tianchi Crater Lake. Quaternary Research 92, 133-145.
[37]Zhou, X.*, Liu, Z., Yan, Q., Zhang, X., Yi, L., Yang, W., Xiang, R., He, Y., Hu, B., Liu, Y., Shen, Y., 2019. Enhanced tropical cyclone intensity in the western North Pacific during warm periods over the last two millennia. Geophysical Research Letters 46, 9145-9153.
[38]Rao, X., Sha, J.*, Peng, B., Zhang, X., Cai, H., 2019. Constraints of bipolar and tropical bivalve on the northward drifting of the Indian Plate. Journal of Asian Earth Sciences 175, 68-73.
[39]Li, D., Zhang, X., Hu, D., Chen, X., Huang, W., Zhang, X., Li, M., Qin, L., Peng, S., Shen, Y.*, 2018. Evidence of a large δ13Ccarb and δ13Corg depth gradient for deep‑water anoxia during the late Cambrian SPICE event. Geology 46, 631-634.
[40]Jiang, S., Luo, W., Tu, L., Yu, Y., Fang, F., Liu, X., Zhan, T., Fang, L., Zhang, X.*, Zhou, X.*, 2018. The Holocene optimum (HO) and the response of human activity: A case study of the Huai River Basin in eastern China. Quaternary International 493, 31-38.
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