From the mass extinction at the end of the Ordovician period to the Pleistocene glaciations, everything affects the climate system, and climate affects everything. At the center of this central system is the earth’s paradigmatic biogeochemical loop: the carbon cycle. Carbon builds the whole biosphere, flows through the oceans, sediments, and atmosphere, and in its atmospheric phase decisively inflects the quantity and distribution of energy around the surface of the earth.