best evidence of seafloor spreading?

Kirschvink noted that reappeared in the geological record during the possible Snowball Earth times, after vanishing about a billion years earlier. Kirschvink noted that iron cannot increase to levels where they would create BIFs if the global ocean was oxygenated. Kirschvink proposed that the sea ice not only killed the photosynthesizers, but it also separated the ocean from the atmosphere so that the global ocean became anoxic. Iron from volcanoes on the ocean floor would build up in solution during the , and during the greenhouse phase the oceans would become oxygenated and the iron would fall out in BIFs. Other geological evidence for the vacillating icehouse and greenhouse conditions was the formation of cap carbonates over the glacial till. It was a global phenomenon; wherever the Snowball Earth till was, cap carbonates were atop them. In geological circles, deposited during the past 100 million years are considered to be of tropical origin, so scientists think that the cap carbonates reflected a tropical environment. The fact of cap carbonates atop glacial till is one of the strongest pieces of evidence for the Snowball Earth hypothesis. Kirschvink finished his paper by noting that the eon of complex life came on the heels of the Snowball Earth, and scouring the oceans of life would have presented virgin oceans for the rapid spread of life in the greenhouse periods, and this could have initiated the evolutionary novelty that led to complex life.

By contrast, along the mid-ocean ridges, the seafloor is spreading,creating new oceanic crust.

At the mid-ocean spreading zones, the mantle partially melts during decompression, and the melted rocks are pushed out to form the oceanic crust – the seafloor.

The Continental Drift and Seafloor Spreading Theory

The red curves are areas ofcollision, whereas the blue lines are those where the seafloor was spreading.

Tectonic plates are able to move because the Earth's lithosphere has a higher strength and lower density than the underlying . Lateral density variations in the mantle result in . Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topography and density of the crust, which result in ) and , downward , at the subduction zones. Another explanation lies in the different forces generated by the rotation of the globe and the tidal forces of the and the . The relative importance of each of these factors is unclear, and is still subject to debate (see also below).