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[1] Liu, P., Liu, Y.*, Gu, S., Hoffman, P., & Li, S. (2023). A positive cooling feedback for the Neoproterozoic snowball Earth initiation due to weakening of ocean ventilation. Geophysical Research Letters, 50(4), e2022GL102020.
[2] Liu, P., Liu, J., Ji, A., Reinhard, C. T., Planavsky, N. J., Babikov, D., Najjar, R. G., & Kasting, J. F. (2021). Triple oxygen isotope constraints on atmospheric O2 and biological productivity during the mid-Proterozoic. Proceedings of the National Academy of Sciences, 118(51), e2105074118.
[3] Liu, P., Liu, Y., Peng, Y., Lamarque, J.-F., Wang, M., & Hu, Y. (2020). Large influence of dust on the Precambrian climate. Nature communications, 11(1), 1-8.
[4] Liu, P., Harman, C. E., Kasting, J. F., Hu, Y., & Wang, J. (2019). Can organic haze and O2 plumes explain patterns of sulfur mass-independent fractionation during the Archean? Earth and Planetary Science Letters, 526, 115767.
[5] Liu, P., Liu, Y., Hu, Y., Yang, J., & Pisarevsky, S. A. (2019). Warm climate in the “Boring Billion” era. Acta Geologica Sinica‐English Edition, 93(S3), 40-43.
[6] Liu, Y., Liu, P., Li, D., Peng, Y., & Hu, Y. (2021). Influence of Dust on the Initiation of Neoproterozoic Snowball Earth Events. Journal of Climate, 34(16), 6673-6689.
[7] Zhou, C., Liu, P., Huang, G., Lin, J., Hu, K., Chen, L., Wang, J., Li, S., Wang, S., & Ni, R. (2020). The impact of secondary inorganic aerosol emissions change on surface air temperature in the Northern Hemisphere. Theoretical and Applied Climatology, 141(3), 857-868.
[8] Lin, J., Zhou, C., Chen, L., Huang, G., Lamarque, J.-F., Nie, J., Yang, J., Hu, K., Liu, P., & Wang, J. (2022). Sulfur emissions from consumption by developed and developing countries produce comparable climate impacts. Nature Geoscience, 15(3), 184-189.
[9] Shang, Y., Liu, P., Wu, S., 2023. Responses of the Pacific and Atlantic decadal variabilities under global warming by using CMIP6 models. Ocean Dynamics. 74(1), 67-75.
[10] Zhang, Z., Yang, J., Feng, X., Guo, X., Liu, P., Wei, H., Liu, S., Zhao, Y., Zhang, G., Li, S., Zhang, Y., Li, D., 2024. Redox evolution in the subtropical Northwest Pacific across the Middle Miocene Climate Transition. Journal of Asian Earth Sciences, 259, 105916.
[11] 毋宇斌, 刘永岗, 易朝路, & 刘鹏 (2019). 末次冰盛期青藏高原冰川变化对亚洲气候的影响. 北京大学学报 (自然科学版), 1.
[12] 刘永岗, 张铭, 林琪凡, 刘鹏, & 胡永云 (2022). 古气候中的沙尘变化及其气候影响. 地学前缘, 29(5), 285.
[13] 李三忠, 刘丽军, 索艳慧, 李玺瑶, 周洁, 姜兆霞, 管红香, 孙国正, 于雷, 刘鹏, 戴黎明, 李晓辉, 陈龙, 赵彦彦, 王誉桦, 许博超. (2023). 碳构造: 一个地球系统科学新范式. 科学通报, 68(4), 309-338.
[14] 李三忠,索艳慧,周洁,钟世华,孙国正,刘洁,王光增,朱俊江,姜素华,李玺瑶,郭晓玉,刘丽军,刘永江,曹现志,郭玲莉,赵淑娟,王鹏程,关庆彬,陈龙,刘勃然,周建平,姜兆霞,刘琳,曹花花,戴黎明,于胜尧,刘博,王秀娟,王程程,王玺,刘泽,管红香,李晓辉,胡军,段威,于雷,刘晓光,王誉桦,钟源,刘鹏,张文超,李洛阳,赵彦彦,许淑梅. (2022).微板块与大板块:基本原理与范式转换.地质学报,96(10): 3541-3558.