Oligocene - Climate

Climate

The Paleogene Period general temperature decline is interrupted by an Oligocene 7 million year stepwise climate change. A deeper 8.2 °C, 400,000 year temperature depression leads the 2 °C, 7 million year stepwise climate change 33.5 Ma (Million years ago). The stepwise climate change began 32.5Ma and lasted through to 25.5Ma, as depicted in the PaleoTemps chart. The Oligocene climate change was a global increase in ice volume and a 55 M (181 feet) decrease in sea level (35.7-33.5 Ma) with a closely related (25.5-32.5 Ma) temperature depression. The 7 million year depression abruptly terminated within 1-2 million years of the La Garita Caldera eruption at 28-26 Ma. A deep 400,000 year glaciated Oligocene Miocene boundary event is recorded at McMurdo Sound and King George Island.

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