Late Cenozoic cooling restructured global marine plankton communities

The geographic ranges of marine organisms, including planktonic foraminifera 1 , diatoms, dinoflagellates 2 , copepods 3 and fish 4 , are shifting polewards owing to anthropogenic climate change 5 . However, the extent to which species will move and whether these poleward range shifts represent precursor signals that lead to extinction is unclear 6 . Understanding the development of marine biodiversity patterns over geological time and the factors that influence them are key to contextualizing these current trends. The fossil record of the macroperforate planktonic foraminifera provides a rich and phylogenetically resolved dataset that provides unique opportunities for understanding marine biogeography dynamics and how species distributions have responded to ancient climate changes. Here we apply a bipartite network approach to quantify group diversity, latitudinal specialization and latitudinal equitability for planktonic foraminifera over the past eight million years using Triton, a recently developed high-resolution global dataset of planktonic foraminiferal occurrences 7 . The results depict a global, clade-wide shift towards the Equator in ecological and morphological community equitability over the past eight million years in response to temperature changes during the late Cenozoic bipolar ice sheet formation. Collectively, the Triton data indicate the presence of a latitudinal equitability gradient among planktonic foraminiferal functional groups which is coupled to the latitudinal biodiversity gradient only through the geologically recent past (the past two million years). Before this time, latitudinal equitability gradients indicate that higher latitudes promoted community equitability across ecological and morphological groups. Observed range shifts among marine planktonic microorganisms 1 , 2 , 8 in the recent and geological past suggest substantial poleward expansion of marine communities even under the most conservative future global warming scenarios.