The Mesoproterozoic Era is the second era in the Proterozoic Eon, occurring after the Paleoproterozoic Era, and before the Neoproterozoic Era.
1,600–1,000 million years ago
This time is marked by robust tectonic activity
The breakup of the supercontinent Columbia (Zhao et al., 2004)
Formation of the supercontinent Rodinia (Li et al., 2008).
Oxygen levels are 0.1% of current levels
Maximum diversity of stromatolites
Clear evidence of photosynthetic eukaryotes on Earth
Origin of major groups, such as the red and green algae, and clear evidence of their ability to become multicellular (Knoll et al., 2006; Bai, 2015).
The red algae or rhodophytes probably originated by at least 1.6 Ga, and the green alga lineage probably originated by 1.5 Ga (Yoon et al., 2004)
Rafatazmia and Ramnathallus, are two genera from 1.6 Ga with features aligning them with rhodophytes (Bengtson et al., 2017)
The earliest fossils attributed to green algae from the Stenian-Ectasian boundary at 1,200 Ma (Tappan, 1980; Knoll, 2003). The nature of these early fossils is controversial (Cavalier-Smith, 2006)
All major algal groups were present by at least the late Mesoproterozoic (Taylor et al., 2009).
Sexual Reproduction and the Evolution of Sex (Nature.com)
Lack of oxygen delayed rise of animals (YaleNews, 2014)