“…The above-mentioned and other peculiarities of the Precambrian tectonics (including, first of all, the activity of mantle plumes (Gargaud et al, 2012;Gerya, 2014)) likely influenced global sea-level change on a large scale; possible changes in the crust production may also induce a cyclic pattern of these changes (Eriksson et al, 2004(Eriksson et al, , 2005(Eriksson et al, , 2012. For the earliest times, this second line of evidence is most uncertain, because the onset of the plate tectonics on the Earth remains debatable (e.g., Hamilton, 2011;Gargaud et al, 2012;Griffin et al, 2014;Turner et al, 2014). Thirdly, the amount of water on the Earth did not remain constant at the earliest stages of the planetary evolution (Gargaud et al, 2012), which also means significant global sea-level changes (although the latter, probably, will never be modelled).…”