Oligocene climate dynamics
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Date
2004-12
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Publisher
American Geophysical Union
Abstract
A planktonic and benthic foraminiferal stable isotope stratigraphy of the Oligocene equatorial Pacific
(Ocean Drilling Program, Site 1218) was generated at 6 kyr resolution between magnetochrons C9n and
C11n.2n (~26.4–30 Ma on a newly developed astronomically calibrated timescale). Our data allow a detailed
examination of Oligocene paleoceanography, the evolution of the early cryosphere, and the influence of orbital
forcing on glacioeustatic sea level variations. Spectral analysis reveals power and coherency for obliquity (40 kyr
period) and eccentricity (~110, 405 kyr) orbital bands, with an additional strong imprint of the eccentricity and
1.2 Myr obliquity amplitude cycle, driving ice sheet oscillations in the Southern Hemisphere. Planktonic and
benthic foraminifera d18O are used to constrain the magnitude and timing of major fluctuations in ice volume
and global sea level change. Glacial episodes, related to obliquity and eccentricity variations, occurred at 29.16,
27.91, and 26.76 Ma, corresponding to glacioeustatic sea level fluctuations of 50–65 m. Alteration of highlatitude
temperatures and Antarctic ice volume had a significant impact on the global carbon burial and
equatorial productivity, as cyclic variations are also recorded in the carbon isotope signal of planktonic and
benthic foraminifera, the water column carbon isotope gradient, and estimated percent carbonate of bulk
sediment. We also investigate the implications of a close correspondence between oxygen and carbon isotope
events and long-term amplitude envelope extrema in astronomical calculations during the Oligocene, and
develop a new naming scheme for stable isotope events, on the basis of the 405 kyr eccentricity cycle
count.
Description
Copyright 2004 by the American Geophysical Union.
0883-8305/04/2004PA001042
Keywords
Oligocene, stable isotopes, ice volume
Citation
Wade, B. S., and H. Pa¨like (2004), Oligocene climate dynamics, Paleoceanography, 19, PA4019, doi:10.1029/2004PA001042.