Evidence for eukaryotic diversification in the ∼1800 million-year-old Changzhougou Formation, North China

By D. M. Lamb, S. Awramik, D. Chapman, S. Zhu. 2009

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Micropaleontology of the lower Mesoproterozoic Roper Group, Australia, and implications for early eukaryotic evolution (2016, unknown): “…of the Roper Group are intermediate in nature between the simple leiosphere-dominated assemblages found in most late Paleoproterozoic shales (e.g., Lamb et al., 2009; Peng et al., 2009) and the slightly more diverse (and taxonomically distinctive) assemblages reported from late Mesoproterozoic…”
Proterozoic phytoplankton and timing of Chlorophyte algae origins (2011, background): “: P R O T E R O Z O I C P H Y T O P L A N K T O N 729 microfossils at c. 1.8 Ga (Javaux and Marshal 2006; Lamb et al. 2009; Peng et al. 2009), and morphologically complex taxa with a cytoskeleton existed by 1.5 Ga (Javaux et al. 2004; Yin et al. 2005).”
The terrestrial biota prior to the origin of land plants (embryophytes): a review of the evidence (2015, background): “…evolution in Proterozoic environments On the basis of the fossil record, most workers consider that stem group eukaryotes had appeared by 1.9–1.7 Ga (Lamb et al. 2009; Peng et al. 2009) and crown group eukaryotes by 1.2 Ga (Butterfield 2000) with a major subsequent diversification at 0.8 Ga (e.g.…”