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Dryad

Quantifying the global biodiversity of Proterozoic eukaryotes

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Nov 04, 2024 version files 3.74 MB

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Abstract

The global diversity of Proterozoic eukaryote fossils is poorly quantified despite its fundamental importance to the understanding of macroevolutionary patterns and dynamics on the early Earth. Here we report a new construction of fossil eukaryote diversity from the Paleoproterozoic to early Cambrian based on a comprehensive data compilation and quantitative analyses. The resulting taxonomic richness curve verifies Cryogenian glaciations as a major divide that separates the “Boring Billion” and Ediacaran Period, with the former characterized by a remarkable stasis and the latter by greater diversity, more rapid turnover, and multiple radiations and extinctions. These contrasting evolutionary patterns and dynamics provide a framework to test competing hypotheses on biosphere and geosphere co-evolution in the Proterozoic Eon.