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1“... maximum in benthic foraminiferal δ18O (Zone Mi6 of Miller et al. [1991]), which has been interpreted...”
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2“... and occur at the end of the Miocene cooling events Mi5 (about 11.5 Ma) and Mi6 (about 10.5 Ma). Both cooling...”
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3by Heinrich, Sonja“... to the Miocene cooling events, Mi-5 and Mi-6. At about 11.1 Ma, productivity increased and the polar species...”
Published 2012
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4by Browning, Emily“...). The complementary Miocene oxygen isotope events Mi1, Mi1a, Mi1aa, Mi2, Mi2b, Mi3a, Mi3, Mi4, Mi5a, Mi5, and Mi6...”
Published 2012
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5by Browning Emily“...). The complementary Miocene oxygen isotope events Mi1, Mi1a, Mi1aa, Mi2, Mi2b, Mi3a, Mi3, Mi4, Mi5a, Mi5, and Mi6...”
Published 2012
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Thesis -
6by Cooke, Penelope J., Nelson, Campbell S., Crundwell, Martin P., Field, Brad D., Elkington, E. Shirley, Stone, Harold H.“... providing the mechanism to increase watermass flow. Miocene glacial zones Mi1b-Mi6 are identified...”
Published in New Zealand Journal of Geology and Geophysics (2004)
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7by Browning, Emily“...). The complementary Miocene oxygen isotope events Mi1, Mi1a, Mi1aa, Mi2, Mi2b, Mi3a, Mi3, Mi4, Mi5a, Mi5, and Mi6...”
Published 2012
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