BIO211H5 Lecture Notes - Superheated Water, Seafloor Spreading, Oceanic Crust

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A week from wednesday is your first exam. Fill in the correct bubble on the scantron sheet. There s a lot of material in the book that is not covered in the class. Oxygen is so good at measuring temperatures that we can actually get exact numbers. We can get the average temperature of the oceans at a given point in time. What we know by looking at sedimentary rock records is that there have been multiple episodes where there has been no ice, as well long periods where there has been ice. When we have polar ice, we call it an icehouse climate. When there is no polar ice, it is a greenhouse climate. Sea levels rise and fall as we go to and from icehouse and greenhouse environments. Yeah, warming is normal, but you just don t lose as much polar ice as we have naturally within a few decades.

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