glaciers at low and mid-latitudes. Recently compiled geological data of 200-million-year-outdated lake sediments in the jap United States present a sequence of cycles of approximately the same intervals as the present orbital cycles, spanning a interval of forty-million-years.
Variations within the oxygen isotope (18 /16O) ratio with depth in a sediment core are extensively interpreted as indicating complete land-ice volume as a perform of time.
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