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Global climate forcing on late Miocene establishment of the Pampean aeolian system in South America

Author

Listed:
  • Blake Stubbins

    (University of South Carolina)

  • Andrew L. Leier

    (University of South Carolina)

  • David L. Barbeau

    (University of South Carolina)

  • Alex Pullen

    (Clemson University)

  • Jordan T. Abell

    (University of Arizona
    Lehigh University)

  • Junsheng Nie

    (Lanzhou University)

  • Marcelo A. Zárate

    (CONICET Universidad Nacional de La Pampa)

  • Mary Kate Fidler

    (Clemson University)

Abstract

Wind-blown dust from southern South America links the terrestrial, marine, atmospheric, and biological components of Earth’s climate system. The Pampas of central Argentina (~33°–39° S) contain a Miocene to Holocene aeolian record that spans an important interval of global cooling. Upper Miocene sediment provenance based on n = 3299 detrital-zircon U-Pb ages is consistent with the provenance of Pleistocene–Holocene deposits, indicating the Pampas are the site of a long-lived fluvial-aeolian system that has been operating since the late Miocene. Here, we show the establishment of aeolian sedimentation in the Pampas coincided with late Miocene cooling. These findings, combined with those from the Chinese Loess Plateau (~33°–39° N) underscore: (1) the role of fluvial transport in the development and maintenance of temporally persistent mid-latitude loess provinces; and (2) a global-climate forcing mechanism behind the establishment of large mid-latitude loess provinces during the late Miocene.

Suggested Citation

  • Blake Stubbins & Andrew L. Leier & David L. Barbeau & Alex Pullen & Jordan T. Abell & Junsheng Nie & Marcelo A. Zárate & Mary Kate Fidler, 2023. "Global climate forcing on late Miocene establishment of the Pampean aeolian system in South America," Nature Communications, Nature, vol. 14(1), pages 1-10, December.
    • Handle: RePEc:nat:natcom:v:14:y:2023:i:1:d:10.1038_s41467-023-42537-3
    DOI: 10.1038/s41467-023-42537-3
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    References listed on IDEAS

    as
    1. Alex Pullen & David L. Barbeau & Andrew L. Leier & Jordan T. Abell & Madison Ward & Austin Bruner & Mary Kate Fidler, 2022. "A westerly wind dominated Puna Plateau during deposition of upper Pleistocene loessic sediments in the subtropical Andes, South America," Nature Communications, Nature, vol. 13(1), pages 1-8, December.
    2. Junsheng Nie & Thomas Stevens & Martin Rittner & Daniel Stockli & Eduardo Garzanti & Mara Limonta & Anna Bird & Sergio Andò & Pieter Vermeesch & Joel Saylor & Huayu Lu & Daniel Breecker & Xiaofei Hu &, 2015. "Loess Plateau storage of Northeastern Tibetan Plateau-derived Yellow River sediment," Nature Communications, Nature, vol. 6(1), pages 1-10, December.
    3. Jasper F. Kok & Daniel S. Ward & Natalie M. Mahowald & Amato T. Evan, 2018. "Global and regional importance of the direct dust-climate feedback," Nature Communications, Nature, vol. 9(1), pages 1-11, December.
    4. Z. T. Guo & William F. Ruddiman & Q. Z. Hao & H. B. Wu & Y. S. Qiao & R. X. Zhu & S. Z. Peng & J. J. Wei & B. Y. Yuan & T. S. Liu, 2002. "Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China," Nature, Nature, vol. 416(6877), pages 159-163, March.
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