The latest Accretionary Wedge, being hosted at Geology Happens, asks: what are you working on? This seemed to me to be a good excuse to finally write something about this whole Snowball Earth thing that I’m currently researching. More musings will hopefully follow in the future.
Why did visit I Oman last year? Because in Oman you can find Late Neoproterozoic rocks, between about 750 and 600 million years in age, that contain sequences like this:


There are two very different rock units in this outcrop. The lower part consists of a diamicite: a sedimentary rock that contains both very fine particles (the dark grey matrix) and also large pebbles, cobbles and even occasionally boulders, and possibly everything in between (this range of different grain sizes means that is a poorly sorted sediment).


The buff coloured unit deposited directly above this is a carbonate rock, more specifically dolomite; it is crystalline, and generally quite fine grained.

This is not just an outcrop of extremes because of the obvious lithological differences between the two units. Diamictites are often interpreted as having being deposited in a glacial environment*. Bedrock underneath a glacier is very efficiently ground up into fine powder by the slowly moving ice, while larger rock fragments are also swept along, frozen within the main body of the glacier itself. Thus, when the ice melts at the end of a glacier, fine and coarse material will all get mixed up in the same deposit. However, whilst this suggests that the lowermost unit was deposited in a very cold, icy climate, the carbonate appears to have been directly chemically precipitated from seawater, something which only happens in warm, tropical conditions – think the Bahamas. There is no sign of a large time gap between the formation of these two units, so if these interpretations are correct, this outcrop records an extremely abrupt climatic shift from very cold conditions to very warm ones.










