Authors

Brendan T. Reilly, Scripps Institution of Oceanography
Lisa Tauxe, Scripps Institution of Oceanography
Stefanie Brachfeld, Montclair State UniversityFollow
Maureen Raymo, Lamont-Doherty Earth Observatory
Ian Bailey, University of Exeter
Sidney Hemming, Lamont-Doherty Earth Observatory
Michael E. Weber, Universität Bonn
Trevor Williams, Texas A&M University
Marga Garcia, CSIC - Centro Oceanográfico de Cádiz (COCAD-IEO)
Michelle Guitard, University of South Florida St. Petersburg
Yasmina M. Martos, NASA Goddard Space Flight Center
Lara F. Pérez, British Antarctic Survey
Xufeng Zheng, South China Sea Institute of Oceanology
Linda Armbrecht, The University of Adelaide
Fabricio G. Cardillo, Servicio de Hidrografia Naval
Zhiheng Du, Northwest Institute of Eco-Environment and Resources
Gerson Fauth, Universidade do Vale do Rio dos Sinos
Anna Glueder, Oregon State University
Marcus Gutjahr, GEOMAR - Helmholtz-Zentrum für Ozeanforschung Kiel
Iván Hernández-Almeida, ETH Zürich
Frida S. Hoem, Universiteit Utrecht
Ji Hwan Hwang, Korea Basic Science Institute
Mutsumi Iizuka, Tokyo City University
Yuji Kato, Kochi University
Bridget Kenlee, University of California, Riverside
Suzanne O’Connell, Wesleyan University Middletown
Victoria Peck, British Antarctic Survey
Thomas A. Ronge, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Osamu Seki, Hokkaido University
Shubham Tripathi, National Centre for Polar and Ocean Research
Jonathan Warnock, Indiana University of Pennsylvania

Document Type

Article

Publication Date

2-1-2021

Journal / Book Title

Paleoceanography and Paleoclimatology

Abstract

International Ocean Discovery Program (IODP) Expedition 382 in the Scotia Sea’s Iceberg Alley recovered among the most continuous and highest resolution stratigraphic records in the Southern Ocean near Antarctica spanning the last 3.3 Myr. Sites drilled in Dove Basin (U1536/U1537) have well-resolved magnetostratigraphy and a strong imprint of orbital forcing in their lithostratigraphy. All magnetic reversals of the last 3.3 Myr are identified, providing a robust age model independent of orbital tuning. During the Pleistocene, alternation of terrigenous versus diatomaceous facies shows power in the eccentricity and obliquity frequencies comparable to the amplitude modulation of benthic δ18O records. This suggests that variations in Dove Basin lithostratigraphy during the Pleistocene reflect a similar history as globally integrated ice volume at these frequencies. However, power in the precession frequencies over the entire ∼3.3 Myr record does not match the amplitude modulation of benthic δ18O records, suggesting Dove Basin contains a unique record at these frequencies. Comparing the position of magnetic reversals relative to local facies changes in Dove Basin and the same magnetic reversals relative to benthic δ18O at North Atlantic IODP Site U1308, we demonstrate Dove Basin facies change at different times than benthic δ18O during intervals between ∼3 and 1 Ma. These differences are consistent with precession phase shifts and suggest climate signals with a Southern Hemisphere summer insolation phase were recorded around Antarctica. If Dove Basin lithology reflects local Antarctic ice volume changes, these signals could represent ice sheet precession-paced variations not captured in benthic δ18O during the 41-kyr world.

Comments

© 2021 American Geophysical Union. All Rights Reserved. This article is being shared in accordance with the AGU self-archiving policy.

DOI

10.1029/2020PA003994

Journal ISSN / Book ISBN

85101734471 (Scopus)

Published Citation

Reilly, B. T., Tauxe, L., Brachfeld, S., Raymo, M., Bailey, I., Hemming, S., Weber, M. E., Williams, T., Garcia, M., Guitard, M., Martos, Y. M., Pérez, L. F., Zheng, X., Armbrecht, L., Cardillo, F. G., Du, Z., Fauth, G., Glueder, A., Gutjahr, M., … Warnock, J. (2021). New magnetostratigraphic insights from iceberg alley on the rhythms of antarctic climate during the plio‐pleistocene. Paleoceanography and Paleoclimatology, 36(2), e2020PA003994. https://doi.org/10.1029/2020PA003994

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