La. Frakes et al., LATITUDINAL DISTRIBUTION OF PALEOTEMPERATURE ON LAND AND SEA FROM EARLY CRETACEOUS TO MIDDLE MIOCENE, Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 318(9), 1994, pp. 1209-1218
Paleotemperature data from the oceans and the continents are summarize
d for the interval from the early Cretaceous through the middle Miocen
e. The data are contoured on diagrams of age vs latitude after adjustm
ents for the known occurrences of seasonal ice and for estimated ice v
olumes. Separate plots for oceans and continents indicate the warmest
times for the oceans were the late Paleocene and the late Eocene and t
he coolest were the early Oligocene and the early Cretaceous. Continen
ts were warmest in the late Cretaceous and the late Eocene and coolest
during the early Oligocene and the late Maastrichtian. Oceans were ch
aracterized by cooler tropics and warmer higher latitudes than present
and continents by strikingly higher temperatures than present over al
l latitudes.