Integrated chronostratigraphic calibration of the Oligocene-Miocene boundary at 24.0 +/- 0.1 MA from the CRP-2A drill core, Ross Sea, Antarctica

An expanded Oligocene-Miocene boundary interval recovered in the Cape Roberts Project CRP-2A core from beneath the Ross Sea, Antarctica, has yielded a high-resolution integrated chrono stratigraphy that has, in turn, enabled a new, more direct, calibra tion of magnetic polarity and biostratigraphic...

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Bibliographic Details
Main Authors: Wilson, Gary S., Lavelle, Mark, McIntosh, William C., Roberts, Andrew P., Harwood, David M., Watkins, David K., Villa, Giuliana, Bohaty, Steven M., Fielding, Chris R., Florindo, Fabio, Sagnotti, Leonardo, Naish, Timothy R., Scherer, Reed P., Verosub, Kenneth L.
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America 2002
Subjects:
Marine Sciences
Earth Sciences
Ross Sea
Cape Roberts
Antarc*
Antarctica
Online Access:http://nora.nerc.ac.uk/id/eprint/17519/
http://geology.gsapubs.org/content/30/11/1043.full.pdf+html
Description
Summary:An expanded Oligocene-Miocene boundary interval recovered in the Cape Roberts Project CRP-2A core from beneath the Ross Sea, Antarctica, has yielded a high-resolution integrated chrono stratigraphy that has, in turn, enabled a new, more direct, calibra tion of magnetic polarity and biostratigraphic events. The Oligocene-Miocene boundary interval in the CRP-2A core comprises three ∼60-m-thick, rapidly deposited (>0.5 m/k.y.) sedimentary sequences (sequences 9, 10, and 11). In sequences 10 and 11, single-crystal, laser-fusion 40Ar/39Ar analyses of anorthoclase phenocrysts from two tephra horizons independently calibrate the CRP-2A magnetic-polarity stratigraphy and age model. Sequences 10 and 11 encompass subchron C6Cn.3n, which is dated as 24.3 ± 0.1 to 24.16 ± 0.1 Ma. Sequence 9 is interpreted to encompass subchron C6Cn.2n and the Oligocene-Miocene boundary, which is dated as 24.0 ± 0.1 Ma. These ages are ∼0.2 m.y. older than those of the geomagnetic polarity time scale calibrated from seafloor-spreading ridges and ∼0.9–1.3 m.y. older than the newly proposed astronomically calibrated ages. We contend that the discrepancy with the astronomically calibrated ages arises from a mismatch of three 406 k.y. eccentricity cycles or a 1.2 m.y. modulation of obliquity amplitude in the astronomical calibration of the Oligocene–Miocene time scale.

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