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Tectonic and climatic implications of the Aleutian Arc initiation ≥56 million years ago
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  • Published: 30 May 2026

Tectonic and climatic implications of the Aleutian Arc initiation ≥56 million years ago

  • K. Hoernle  ORCID: orcid.org/0000-0002-3165-34801,
  • B. Jicha  ORCID: orcid.org/0000-0002-1228-515X2,
  • M. Portnyagin  ORCID: orcid.org/0000-0001-5197-65621,
  • S. Zahirovic  ORCID: orcid.org/0000-0002-6751-49763,
  • D. Müller  ORCID: orcid.org/0000-0002-3334-57643,
  • F. Hauff  ORCID: orcid.org/0000-0001-9503-97141,
  • C. Timm  ORCID: orcid.org/0000-0002-5889-16651,
  • T. W. Höfig4,
  • G. Yogodzinski  ORCID: orcid.org/0000-0003-4166-33215,
  • M. Guillong  ORCID: orcid.org/0000-0002-6920-33626,
  • C. Berndt  ORCID: orcid.org/0000-0001-5055-01801,
  • D. Savelyev  ORCID: orcid.org/0000-0001-9867-77977,
  • R. Bezard  ORCID: orcid.org/0000-0002-3818-88848 &
  • …
  • B. Baranov  ORCID: orcid.org/0000-0002-1965-320X9 

Nature Communications (2026) Cite this article

We are providing an unedited version of this manuscript to give early access to its findings. Before final publication, the manuscript will undergo further editing. Please note there may be errors present which affect the content, and all legal disclaimers apply.

Subjects

  • Geochemistry
  • Geodynamics
  • Solid Earth sciences

Abstract

The timing and origin of Aleutian subduction initiation remain poorly constrained, yet they are central to understanding late Paleocene to early Eocene plate tectonic reorganization in the Pacific and its possible climatic consequences. Here, we use geochronologic and geochemical data obtained on western Aleutian arc samples from four basal submarine sequences, spanning ~700 km, to constrain Aleutian subduction initiation to ≥56 Ma. Early forearc lavas have similar compositions to forearc basalts erupted during the initial stages of Izu-Bonin-Mariana subduction in the western Pacific. Collision of the Olyutorsky Arc with Kamchatka-Koryak margin and subduction of the Izanagi-Pacific Ridge are likely to have triggered Aleutian subduction initiation and a change in absolute Pacific plate motion from WNW to N between 57 and 55 Ma, as shown with a GPlates model. Our study shows that Aleutian subduction initiation is a key event at the beginning of a major ~10 Myr plate reorganization in the circum-Pacific ending with Hawaii-Emperor-Bend formation. These tectono-magmatic events may have contributed to contemporaneous global climatic events in the late Paleocene and early Eocene.

Acknowledgements

Reinhard Werner is thanked for help obtaining funding and carrying out the cruises; S. Jung for providing XRF and D. Garbe-Schönberg for ICP-MS data; S. Hauff, K. Junge and U. Westernströer for analytical support; and Deep Sea Drilling Project (DSDP) and International Ocean Discovery Program (IODP) for sediment and IBM forearc reference samples.

Funding

K.H., M.P., and F.H. disclose support for the research of this work from the German Federal Ministry of Research, Technology and Space (BMFTR) [grants KALMAR 03G0640A and Bering 03G0249]; BJ from the National Science Foundation (NSF) [grants EAR-1753492 and OCE-1551657]; G.Y. from NSF [grants OCE-1551640 and EAR 1753518]; S.Z. from the Australian Research Council (ARC) [grant DE210100084]; D.M. and S.Z. from the AuScope National Collaborative Research Infrastructure System (NCRIS) program and GPlates Development. The remaining co-authors declare no relevant funding. Open Access funding enabled and organized by Projekt DEAL.

Author information

Authors and Affiliations

  1. Research Division 4, GEOMAR Helmholtz Center for Ocean Research Kiel, Kiel, Germany

    K. Hoernle, M. Portnyagin, F. Hauff, C. Timm & C. Berndt

  2. Department of Geoscience, University of Wisconsin-Madison, Madison, Wisconsin, USA

    B. Jicha

  3. EarthByte Group, School of Geosciences, The University of Sydney, Sydney, Australia

    S. Zahirovic & D. Müller

  4. Projektträger Jülich, Forschungszentrum Jülich GmbH, Rostock, Germany

    T. W. Höfig

  5. School of Earth, Ocean, and Environment, University of South Carolina, Columbia, SC, USA

    G. Yogodzinski

  6. Department of Earth and Planetary Sciences, ETH Zurich, Zurich, Switzerland

    M. Guillong

  7. Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia

    D. Savelyev

  8. Laboratoire de Planétologie et Géosciences, Nantes Université, Nantes, France

    R. Bezard

  9. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia

    B. Baranov

Authors
  1. K. Hoernle
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  2. B. Jicha
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  3. M. Portnyagin
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  4. S. Zahirovic
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  5. D. Müller
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  6. F. Hauff
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  7. C. Timm
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  8. T. W. Höfig
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  9. G. Yogodzinski
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  10. M. Guillong
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  11. C. Berndt
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  12. D. Savelyev
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  13. R. Bezard
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  14. B. Baranov
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Corresponding author

Correspondence to K. Hoernle.

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Hoernle, K., Jicha, B., Portnyagin, M. et al. Tectonic and climatic implications of the Aleutian Arc initiation ≥56 million years ago. Nat Commun (2026). https://doi.org/10.1038/s41467-026-73363-y

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  • Received: 21 April 2025

  • Accepted: 07 May 2026

  • Published: 30 May 2026

  • DOI: https://doi.org/10.1038/s41467-026-73363-y

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