Evidence left in rock from the Neoproterozoic age that indicates glaciers: The presence of "Cap Carbonates" suggests that glaciers must have been present at low latitudes at some point in the past. This is further explained below.
Generally, It was during the Neoproterozoic Era (1000–543 Ma) that the microbial world transitioned to a more sophisticated animal life form known as the Phanerozoic.
In conclusion, Glaciers were likely present throughout the Neoproterozoic epoch based on the following evidence found in rocks: Glaciers must have been at low latitudes at one point in time in order for there to be evidence of "Cap Carbonates," which indicates that they did.
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