An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite.

MLA

Hermoso, M., et al. “An Explanation for the 18O Excess in Noelaerhabdaceae Coccolith Calcite.” Geochimica et Cosmochimica Acta, vol. 189, Sept. 2016, pp. 132–42. EBSCOhost, https://doi.org/10.1016/j.gca.2016.06.016.

APA

Hermoso, M., Minoletti, F., Aloisi, G., Bonifacie, M., McClelland, H. L. O., Labourdette, N., Renforth, P., Chaduteau, C., & Rickaby, R. E. M. (2016). An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite. Geochimica et Cosmochimica Acta, 189, 132–142. https://doi.org/10.1016/j.gca.2016.06.016

Chicago

Hermoso, M., F. Minoletti, G. Aloisi, M. Bonifacie, H.L.O. McClelland, N. Labourdette, P. Renforth, C. Chaduteau, and R.E.M. Rickaby. 2016. “An Explanation for the 18O Excess in Noelaerhabdaceae Coccolith Calcite.” Geochimica et Cosmochimica Acta 189 (September): 132–42. doi:10.1016/j.gca.2016.06.016.