Information om | Engelska ordet UNRADIOGENIC

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• An osmium isotope excursion coeval with OAE2 strongly suggests submarine volcanism as its cause; in the Pacific, an unradiogenic osmium spike began about 350 kyr before the onset of OAE2 and terminated around 240 kyr after OAE2's beginning; the osmium isotope data from a highly expanded OAE2 interval in southern Tibet show multiple osmium excursions with the most pronounced one lagging the onset of OAE2 by ≈50 kyr that was probably related to the ocean connectivity change at ~94.

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