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Solar System chaos and the Paleocene–Eocene boundary age constrained by geology and astronomy - MaRDI portal

Solar System chaos and the Paleocene–Eocene boundary age constrained by geology and astronomy

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Publication:5218601

DOI10.1126/SCIENCE.AAX0612zbMATH Open1431.85003arXiv1909.00283OpenAlexW3100624638WikidataQ92994061 ScholiaQ92994061MaRDI QIDQ5218601

Lucas J. Lourens, Richard E. Zeebe

Publication date: 4 March 2020

Published in: Science (Search for Journal in Brave)

Abstract: Astronomical calculations reveal the solar system's dynamical evolution, including its chaoticity, and represent the backbone of cyclostratigraphy and astrochronology. An absolute, fully calibrated astronomical time scale has hitherto been hampered beyond sim50 Ma, because orbital calculations disagree before that age. Here we present geologic data and a new astronomical solution (ZB18a), showing exceptional agreement from sim58 to 53 Ma. We provide a new absolute astrochronology up to 58 Ma and a new Paleocene-Eocene boundary age (56.01 pm 0.05 Ma). We show that the Paleocene-Eocene Thermal Maximum (PETM) onset occurred near a 405-kyr eccentricity maximum, suggesting an orbital trigger. We also provide an independent PETM duration (170 pm 30 kyr) from onset to recovery inflection. Our astronomical solution requires a chaotic resonance transition at sim50 Ma in the solar system's fundamental frequencies.


Full work available at URL: https://arxiv.org/abs/1909.00283











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