Atmospheric carbon dioxide concentrations are believed to drive climate cha
nges from glacial to interglacial modes', although geological(1-3) and astr
onomical(4-6) mechanisms have been invoked as ultimate causes. Additionally
, it is unclear(7,8) whether the changes between cold and warm modes should
be regarded as a global phenomenon, affecting tropical and high-latitude t
emperatures alike(9-13), or if they are better described as an expansion an
d contraction of the latitudinal climate zones, keeping equatorial temperat
ures approximately constant(14-16). Here we present a reconstruction of tro
pical sea surface temperatures throughout the phanerozoic eon (the past sim
ilar to 550 Myr) from our database(17) of oxygen isotopes in calcite and ar
agonite shells. The data indicate large oscillations of tropical sea surfac
e temperatures in phase with the cold-warm cycles, thus favouring the idea
of climate variability as a global phenomenon. But our data conflict with a
temperature reconstruction using an energy balance model that is forced by
reconstructed atmospheric carbon dioxide concentrations(18). The results c
an be reconciled if atmospheric carbon dioxide concentrations were not the
principal driver of climate variability on geological timescales for at lea
st one-third of the Phanerozoic eon, or if the reconstructed carbon dioxide
concentrations are not reliable.