Cite
Biogenic silica and organic carbon fluxes provide evidence of enhanced marine productivity in the Upper Ordovician-Lower Silurian of South China.
MLA
Khan, Maliha Zareen, et al. “Biogenic Silica and Organic Carbon Fluxes Provide Evidence of Enhanced Marine Productivity in the Upper Ordovician-Lower Silurian of South China.” Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 534, Nov. 2019, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.palaeo.2019.109278.
APA
Khan, M. Z., Feng, Q., Zhang, K., & Guo, W. (2019). Biogenic silica and organic carbon fluxes provide evidence of enhanced marine productivity in the Upper Ordovician-Lower Silurian of South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 534, N.PAG. https://doi.org/10.1016/j.palaeo.2019.109278
Chicago
Khan, Maliha Zareen, Qinglai Feng, Ke Zhang, and Wei Guo. 2019. “Biogenic Silica and Organic Carbon Fluxes Provide Evidence of Enhanced Marine Productivity in the Upper Ordovician-Lower Silurian of South China.” Palaeogeography, Palaeoclimatology, Palaeoecology 534 (November): N.PAG. doi:10.1016/j.palaeo.2019.109278.