APA (7th ed.) Citation

Kobashi, T. (2001). Paleogene cooling (55-30 MA) as inferred from oxygen isotope variation within mollusc shells. [publisher not identified].

Chicago Style (17th ed.) Citation

Kobashi, Takuro. Paleogene Cooling (55-30 MA) as Inferred from Oxygen Isotope Variation Within Mollusc Shells. [Place of publication not identified]: [publisher not identified], 2001.

MLA (9th ed.) Citation

Kobashi, Takuro. Paleogene Cooling (55-30 MA) as Inferred from Oxygen Isotope Variation Within Mollusc Shells. [publisher not identified], 2001.