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Neogene explosive volcanicity, temperature and glaciation

Abstract

Recent theoretical1–6 and observationa7–10 demonstrations of depression in surface temperature of the Earth due to explosive volcanic eruptions have provided a more exact basis for speculations that explosive volcanicity may have had a climatic impact11–15 during periods over the past 2 Myr. In this letter, broad volcanic–climate relationships are assessed over a longer period by comparing the dates of global explosive phases and of volcanic–plutonic phases with paleotemperature and glaciation records from the Neogene. Analysis of these records indicates significant relationships between the explosive and volcanic–plutonic phases and Neogene temperature decline and also a correspondence between the three greatest explosive and volcanic-plutonic phases and glacial expansion. The second highest global explosive peak was coincident with recently suggested dates of around 3.2 Myr for the initiation of the late Cenozoic glacial age. Further testing of these relationships is necessary to resolve inconsistencies in the late-middle to early-late Miocene and in the late Pliocene.

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Bray, J. Neogene explosive volcanicity, temperature and glaciation. Nature 282, 603–605 (1979). https://doi.org/10.1038/282603a0

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