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However, in-depth molecular clock studies utilizing this dataset have thus far been lacking.

Here, we present molecular clock analyses of the Philippe et al. Our results confirm previous molecular-clock estimates of an early-mid Neoproterozoic (Tonian; 1000–720 Ma) origin of crown-group Metazoa, before the onset of long-lasting global glaciations, the Sturtian and Marinoan “Snowball Earths” of the Cryogenian (720–635 Ma).

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So far, thorough molecular clock studies focusing specifically on Metazoa as a whole have been based on relatively small datasets or incomplete representation of the main non-bilaterian lineages (such as sponges and ctenophores), which are fundamental for understanding early metazoan evolution.Astrid Rommetveit is a Journalist with the Norwegian Broadcasting Corporation NRK.As a journalist, she specializes on weather and climate, committing herself to tell important stories to a broad public.Astrid Rommetveit was nominated for the Journalist Award on the basis of three recent articles published on the popular Norwegian websites and Yr is a cooperation between NRK and the Norwegian Meteorological Institute, and NRK has the full editorial responsibility.

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