A molecular timescale for the origin of red algal-derived plastids

In modern oceans, eukaryotic phytoplankton is dominated by lineages with red algal-derived plastids such as diatoms, dinoflagellates, and coccolithophores. These lineages and countless others representing a huge diversity of forms and lifestyles all belong to four algal groups: cryptophytes, ochrophytes, haptophytes, and myzozoans. Despite the ecological importance of these groups, we still lack a comprehensive understanding of their evolution and how they obtained their plastids. Over the last years, new hypotheses have emerged to explain the acquisition of red algal-derived plastids by serial endosymbiosis, but the chronology of these putative independent plastid acquisitions remains untested. Here, we have established a timeframe for the origin of red algal-derived plastids under scenarios of serial endosymbiosis, using a taxon- and gene-rich phylogenomic dataset combined to Bayesian molecular clock analyses. We find that the hypotheses of serial endosymbiosis are chronologically possible, as the stem lineages of all red plastid-containing groups overlapped in time. This period in the Meso- and Neoproterozoic Eras set the stage for the later expansion to dominance of red algal-derived primary production in the contemporary oceans, which has profoundly altered the global geochemical and ecological conditions of the Earth.