Comment on "A 12-million-year temperature history of the tropical Pacific Ocean".

Zhang et al. (Reports, 4 April 2014, p. 84) interpret TEX86 and U(37)(K') paleotemperature data as providing a fundamentally new view of tropical Pacific climate during the warm Pliocene period. We argue that, within error, their Pliocene data actually support previously published data indicating average western warm-pool temperature similar to today and a reduced zonal gradient, referred to as a permanent El Niño-like state.