The Oligocene–Miocene Boundary – Antarctic Climate Response to Orbital Forcing
Recent high-resolution Oligocene–Miocene oxygen isotopic records revealed a relatively transient, ca. 2 myr period, 1m amplitude cyclicity in isotopic values (Oi and Mi events, respectively). Intriguingly, it has been suggested that these isotopic excursions in oceanic d18O were linked to ephemeral...
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2008
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Online Access: | https://works.bepress.com/robert_deconto/16 http://www.sciencedirect.com/science/article/pii/S1571919708000098 |