Paleotseeni-Eotseeni termaalne maksimum
, Rea, D. K. & Owen, R. M. 1995 Dissociation of oceanic
methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene.
Paleoceanography 10, 965971.
Haywood, A.M., Ridgwell, A., lunt, D.J. 2011. Are there pre-Quaternary geological analogues
for a future greenhouse warming? Phil Trans R Soc A, March 13, 2011, v. 369, p. 933-956.
Koch, P.L.; Zachos, J.C.; Gingerich, P.D. (1992). "Correlation between isotope records in marine
and continental carbon reservoirs near the Palaeocene/Eocene boundary". Nature 358: 319322.
Kelly, D.C., Nielsen, T.M.J., McCarren, H.K., Zachos, J.C., & Röhl, U., 2010: Spatiotemporal
patterns of carbonate sedimentation in the South Atlantic: Implications for carbon cycling during
the PaleoceneEocene thermal maximum. Paleogeogr., Paleoclimatol., Paleoecol., 293, 30-40.
Kent, D. V., Cramer, B. S., Lanci, L., Wang, D., Wright, J. D. & Van der Voo, R. 2003 A case