Heterotrophic bicarbonate assimilation is the main process of de novo organic carbon synthesis in hadal zone of the Hellenic Trench, the deepest part of Mediterranean Sea.

MLA

Yakimov, Michail M., et al. “Heterotrophic Bicarbonate Assimilation Is the Main Process of de Novo Organic Carbon Synthesis in Hadal Zone of the Hellenic Trench, the Deepest Part of Mediterranean Sea.” Environmental Microbiology Reports, vol. 6, no. 6, Dec. 2014, pp. 709–22. EBSCOhost, https://doi.org/10.1111/1758-2229.12192.

APA

Yakimov, M. M., La Cono, V., Smedile, F., Crisafi, F., Arcadi, E., Leonardi, M., Decembrini, F., Catalfamo, M., Bargiela, R., Ferrer, M., Golyshin, P. N., & Giuliano, L. (2014). Heterotrophic bicarbonate assimilation is the main process of de novo organic carbon synthesis in hadal zone of the Hellenic Trench, the deepest part of Mediterranean Sea. Environmental Microbiology Reports, 6(6), 709–722. https://doi.org/10.1111/1758-2229.12192

Chicago

Yakimov, Michail M, Violetta La Cono, Francesco Smedile, Francesca Crisafi, Erika Arcadi, Marcella Leonardi, Franco Decembrini, et al. 2014. “Heterotrophic Bicarbonate Assimilation Is the Main Process of de Novo Organic Carbon Synthesis in Hadal Zone of the Hellenic Trench, the Deepest Part of Mediterranean Sea.” Environmental Microbiology Reports 6 (6): 709–22. doi:10.1111/1758-2229.12192.