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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Bibliographic Details
Main Authors: Wilson, G S, Pekar, S F, Nash, T R, Passchier, S, Deconto, Robert M
Format: Text
Language:unknown
Published: SelectedWorks 2008
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Online Access:https://works.bepress.com/robert_deconto/16
http://www.sciencedirect.com/science/article/pii/S1571919708000098