Obliquity disruption and Antarctic ice sheet dynamics over a 2.4-Myr astronomical grand cycle

Marine δ<sup>18</sup>O data reveal astronomical forcing of the climate and cryosphere during the Miocene, when atmospheric <i>P</i>co<sub>2</sub> was on par with emissions scenarios over the next century. This inspired hypotheses for how Milankovitch cycles, ice-ocean interactions, and greenhouse gases influence ice volume. Mass balance controls for marine and terrestrial ice sheets differ, and proxy data collected far from Antarctica provide valuable but limited insight into regional processes. We evaluate clast abundance data from Antarctic marine sedimentary records, observing a strong signal of eccentricity and precession coincident with a terrestrial ice sheet and a clear obliquity signal at the margins of a marine ice sheet. These analyses are integrated with a synthesis of proxy data, and we argue that high variance in obliquity forcing (mediated and enhanced by the ocean and atmosphere) can inhibit ice sheet growth, even when insolation forcing is conducive to glaciation. This "obliquity disruption" explains cryosphere variability before the existence of large northern hemisphere ice sheets.

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Publication Details

Journal
Science Advances
Published
2025-04-25
DOI
https://doi.org/10.1126/sciadv.adl1996
Citations
3
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
3.90
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article

Obliquity disruption and Antarctic ice sheet dynamics over a 2.4-Myr astronomical grand cycle

Fabio Florindo, Tina van de Flierdt, T. Naish, Laura De Santis et al.
3 citations
Science Advances
Geology and Paleoclimatology Research
3.90
article

Obliquity disruption and Antarctic ice sheet dynamics over a 2.4-Myr astronomical grand cycle

Fabio Florindo, Tina van de Flierdt, T. Naish, Laura De Santis, James Marschalek, Robert M. McKay, Nicholas B. Sullivan, Molly O. Patterson, F. Talarico, Richard Levy, David M. Harwood, Stephen R. Meyers, Georgia Grant, Matteo Perotti, L. Zurli
article en
3 citations

Abstract

Marine δ<sup>18</sup>O data reveal astronomical forcing of the climate and cryosphere during the Miocene, when atmospheric <i>P</i>co<sub>2</sub> was on par with emissions scenarios over the next century. This inspired hypotheses for how Milankovitch cycles, ice-ocean interactions, and greenhouse gases influence ice volume. Mass balance controls for marine and terrestrial ice sheets differ, and proxy data collected far from Antarctica provide valuable but limited insight into regional processes. We evaluate clast abundance data from Antarctic marine sedimentary records, observing a strong signal of eccentricity and precession coincident with a terrestrial ice sheet and a clear obliquity signal at the margins of a marine ice sheet. These analyses are integrated with a synthesis of proxy data, and we argue that high variance in obliquity forcing (mediated and enhanced by the ocean and atmosphere) can inhibit ice sheet growth, even when insolation forcing is conducive to glaciation. This "obliquity disruption" explains cryosphere variability before the existence of large northern hemisphere ice sheets.

Science AdvancesVol. 11(17)
University of Siena (IT), University of Nebraska–Lincoln (US), GNS Science (NZ), Binghamton University (US), Pennsylvania State University (US), University of Wisconsin–Madison (US), Istituto Nazionale di Geofisica e Vulcanologia (IT), Victoria University of Wellington (NZ), National Institute of Oceanography and Applied Geophysics (IT), Imperial College London (GB)
Life below water
Openalex Percentile: Top 7%
Geology and Paleoclimatology Research
3.90
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