“to revisit the ocean’s paleotemperatures now, we need to carefully quantify this re-equilibration, which has been overlooked for too long.
“to revisit the ocean’s paleotemperatures now, we need to carefully quantify this re-equilibration, which has been overlooked for too long.
paleothermometer:22
temperature has been estimated (to varying degrees of fidelity) using leaf physiognomy for late cretaceous and cenozoic leaf floras, principally using two main approaches: a univariate approach that is based on the observation that the proportion of woody dicot species with smooth (i.e.