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Pre One: 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 d13Ccarb and d13Corg depth gradient for deep-water anoxia during the late Cambrian SPICE event. Geology 46: 631-634.
Next One: Hu, D., Li, M., Zhang, X., Turchyn, A.V., Gong, Y., Shen, Y., 2020. Large mass-independent sulphur isotope anomalies link stratospheric volcanism to the Late Ordovician mass extinction. Nature Communications 11: 2297.