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. 2012 Sep;5(5):595–607. doi: 10.1242/dmm.009613

Fig. 2.

Fig. 2.

Isotopic trends over the last 5 million years. Oxygen-18 (18O) isotope levels are directly equivalent to average global temperature. As the world became steadily cooler, shorter-term climate stochasticity also increased substantially, indicating less stable ecological conditions. Based on published data (Lisiecki and Raymo, 2005). BP, before present.