Abstract
Closely related taxa are, on average, more similar in terms of their physiology, morphology and ecology than distantly related ones. How this biological similarity affects geochemical signals, and their interpretations, has yet to be tested in an explicitly evolutionary framework. Here we compile and analyze planktonic foraminiferal size-specific stable carbon and oxygen isotope values (δ(13)C and δ(18)O, respectively) spanning the last 107 million years. After controlling for dominant drivers of size-δ(13)C and size-δ(18)O trends, such as geological preservation, presence of algal photosymbionts, and global environmental changes, we identify that shared evolutionary history has shaped the evolution of species-specific vital effects in δ(13)C, but not in δ(18)O. Our results lay the groundwork for using a phylogenetic approach to correct species δ(13)C vital effects through time, thereby reducing systematic biases in interpretations of long-term δ(13)C records-a key measure of holistic organismal biology and of the global carbon cycle.