1. Anagnostou, E., Sherrell, R. M., Gagnon, A., LaVigne, M., Field, M. P., and McDonough, W. F., 2011. Seawater nutrient and carbonate ion concentrations recorded as P/Ca, Ba/Ca, and U/Ca in the deep-sea coral Desmophyllum dianthus. Geochimica et Cosmochimica Acta, 75: 2529–2543.
2. Armid, A., Asami, R., Fahmiati, T., Sheikh, M. A., Fujimura, H., Higuchi, T., Taira, E., Shinjo, R., and Oomori, T., 2011. Sea-water temperature proxies based on DSr, DMg, and DU from culture experiments using the branching coral Porites cylindrical. Geochimica et Cosmochimica Acta, 75: 4273–4285.
3. Bachtel, S. L., Kissling, R. D., Martono, D., Rahardjanto, S. P., Dunn, P. A., and MacDonald, B. A., 2004. Seismic stratigraphic evolution of the Miocene-Pliocene Segitiga Platform, East Natuna Sea, Indonesia: The origin, growth, and demise of an isolated carbonate platform. In: Seismic Imaging of Carbonate Reservoirs and Systems. Erberli, G. P., et al., eds., American Association of Petroleum Geologists, Tulsa, Oklahoma, 309–328.
4. Bi, D. J., Zhang, D. J., Zhai, S. K., Liu, X. Y., Xiu, C., Zhang, A. B., and Cao, J. Q., 2017. The coupling relationships among the Qinghai-Tibet Plateau uplifting, the Qiongdongnan Basin subsiding and the Xisha Islands’ reefs developing. Haiyang Xuebao, 39(1): 52–63 (in Chinese with English abstract).
5. Brand, U., and Veizer, J., 1980. Chemical diagenesis of a multi-component carbonate system-1: Trace elements. Journal of Sedimentary Research, 50(4): 1219–1236.