[1]
Urrutia Fucugauchi, J. 1980. Oceanic circulation changes and continental drift as the main possible causes of palaeoclimatic variations and organic extinctions. Geofisica Internacional. 19, 1 (Jan. 1980), 63–84. DOI:https://doi.org/10.22201/igeof.00167169p.1980.19.1.822.