Authors

Ian Bailey, University of Exeter
Sidney Hemming, Lamont-Doherty Earth Observatory
Brendan T. Reilly, Scripps Institution of Oceanography
Gavyn Rollinson, University of Exeter
Trevor Williams, Texas A&M University
Michael E. Weber, Universität Bonn
Maureen E. Raymo, Lamont-Doherty Earth Observatory
Victoria L. Peck, British Antarctic Survey
Thomas A. Ronge, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Stefanie Brachfeld, Montclair State UniversityFollow
Suzanne O'Connell, Wesleyan University Middletown
Lisa Tauxe, Scripps Institution of Oceanography
Jonathan P. Warnock, Indiana University of Pennsylvania
Linda Armbrecht, Institute for Marine and Antarctic Studies
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
Marga Garcia, CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT)
Anna Glueder, Oregon State University
Michelle Guitard, University of South Florida St. Petersburg
Marcus Gutjahr, Christian-Albrechts-Universität zu 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, University of Tsukuba
Bridget Kenlee, University of California, Riverside
Yasmina M. Martos, NASA Goddard Space Flight Center
Lara F. Pérez, British Antarctic Survey
Osamu Seki, Hokkaido University
Shubham Tripathi, National Centre for Polar and Ocean Research
Xufeng Zheng, South China Sea Institute of Oceanology

Document Type

Article

Publication Date

7-1-2022

Journal / Book Title

Paleoceanography and Paleoclimatology

Abstract

Ice loss in the Southern Hemisphere has been greatest over the past 30 years in West Antarctica. The high sensitivity of this region to climate change has motivated geologists to examine marine sedimentary records for evidence of past episodes of West Antarctic Ice Sheet (WAIS) instability. Sediments accumulating in the Scotia Sea are useful to examine for this purpose because they receive iceberg-rafted debris (IBRD) sourced from the Pacific- and Atlantic-facing sectors of West Antarctica. Here we report on the sedimentology and provenance of the oldest of three cm-scale coarse-grained layers recovered from this sea at International Ocean Discovery Program Site U1538. These layers are preserved in opal-rich sediments deposited ∼1.2 Ma during a relatively warm regional climate. Our microCT-based analysis of the layer's in-situ fabric confirms its ice-rafted origin. We further infer that it is the product of an intense but short-lived episode of IBRD deposition. Based on the petrography of its sand fraction and the Phanerozoic 40Ar/39Ar ages of hornblende and mica it contains, we conclude that the IBRD it contains was likely sourced from the Weddell Sea and/or Amundsen Sea embayment(s) of West Antarctica. We attribute the high concentrations of IBRD in these layers to “dirty” icebergs calved from the WAIS following its retreat inland from its modern grounding line. These layers also sit at the top of a ∼366-m thick Pliocene and early Pleistocene sequence that is much more dropstone-rich than its overlying sediments. We speculate this fact may reflect that WAIS mass-balance was highly dynamic during the ∼41-kyr (inter)glacial world.

Comments

This is an open access article under the terms of the Creative Commons Attribution (CC-BY) License (https://creativecommons.org/licenses/by/4.0/).

DOI

10.1029/2022PA004433

Journal ISSN / Book ISBN

85135079488 (Scopus)

Published Citation

Bailey, I., Hemming, S., Reilly, B. T., Rollinson, G., Williams, T., Weber, M. E., Raymo, M. E., Peck, V. L., Ronge, T. A., Brachfeld, S., O’Connell, S., Tauxe, L., Warnock, J. P., Armbrecht, L., Cardillo, F. G., Du, Z., Fauth, G., Garcia, M., Glueder, A., … Zheng, X. (2022). Episodes of early pleistocene west antarctic ice sheet retreat recorded by iceberg alley sediments. Paleoceanography and Paleoclimatology, 37(7), e2022PA004433. https://doi.org/10.1029/2022PA004433

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