Climate of the Past
Climate of the Past
CP
Articles | Volume 17, issue 3
Articles | Volume 17, issue 3
https://doi.org/10.5194/cp-17-1385-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-1385-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 17, issue 3
Research article
 | 
23 Jun 2021
Research article |  | 23 Jun 2021

A revised mid-Pliocene composite section centered on the M2 glacial event for ODP Site 846

Timothy D. Herbert, Rocio Caballero-Gill, and Joseph B. Novak

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Cited articles

Ahn, S., Khider, D., Lisiecki, L. E., and Lawrence, C. E.: A probabilistic Pliocene–Pleistocene stack of benthic δ18O using a profile hidden Markov model, Dynamics and Statistics Climate Sys., 2, dzx002, https://doi.org/10.1093/climsys/dzx002, 2017. 
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Duplessy, J.-C., Shackleton, N. J., Matthews, R. K., Prell, W., Ruddiman, W. F., Caralp, M., and Hendy, C. H.: 13C record of benthic foraminifera in the last interglacial ocean: implications for the carbon cycle and the global deep water circulation, Quaternary Res., 21, 225–243, 1984. 
Hagelberg, T. K., Pisias, N. G., Shackleton, N. J., Mix, A. C., and Harris, S. E.: Refinement of a high-resolution, continuous sedimentary section for studying equatorial Pacific Ocean paleoceanography Leg 138, in: Proceedings of the Ocean Drilling Program, edited by: Pisias, N. G., Mayer, L. A., Janecek, T. R., Palmer-Julson, A., and van Andel, T. H., Scientific Results, 138, 31–46, 1995. 
Harris, S. E., Shackleton, N. J., Hagelberg, T. K., Pisias, N. G., and Mix, A. C.: Sediment depths determined by comparison of grape and logging density data during Leg 138, in: Proceedings of the Ocean Drilling Program, edited by: Pisias, N. G., Mayer, L. A., Janecek, T. R., Palmer-Julson, A., and van Andel, T. H., Scientific Results of the Proceedings of the Ocean Drilling Program, vol. 138, College Station, TX (Ocean Drilling Program), 47–57, 1995. 
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The Pliocene represents a geologically warm period with polar ice restricted to the Antarctic. Nevertheless, variability and ice volume persisted in the Pliocene. This work revisits a classic site on which much of our understanding of Pliocene paleoclimate variability is based and corrects errors in data sets related to ice volume and ocean surface temperature. In particular, it generates an improved representation of an enigmatic glacial episode in Pliocene times (circa 3.3 Ma).
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