Prolonged 187Os/188Os excursion implies hydrothermal influence after the Chicxulub impact in the Gulf of Mexico

The Cretaceous/Paleogene boundary asteroid impact is recorded globally as a negative <sup>187</sup>Os/<sup>188</sup>Os excursion, including in sediments recovered from the IODP-ICDP drilling within the peak ring of the Chicxulub structure in the Gulf of Mexico. The reconstructed marine <sup>187</sup>Os/<sup>188</sup>Os curves can be used for global age correlations on the ~10 kyr scale. However, the versatility of Os isotope clock between the proximal and distal sites remains unclear. This paper presents <sup>187</sup>Os/<sup>188</sup>Os records from early Paleocene sediments deposited in the Chicxulub impact basin and Mexican sites with biochronological scales. The results for these proximal sites show a recovery timescale of ~700 kyr, which is significantly longer than that of the distal sites (~200 kyr). The interval showing the <sup>187</sup>Os/<sup>188</sup>Os decline coincides with the enrichment of hydrothermally-derived Mn, implying that hydrothermal venting at the Chicxulub structure may have played a role in the marine chemistry and ecosystem of the Gulf of Mexico.

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Publication Details

Journal
Nature Communications
Published
2025-04-08
DOI
https://doi.org/10.1038/s41467-025-58112-x
Citations
1
Primary Topic
Astro and Planetary Science
Type
article
Field-Weighted Citation Impact
1.15

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article

Prolonged 187Os/188Os excursion implies hydrothermal influence after the Chicxulub impact in the Gulf of Mexico

Honami Sato, Ignacio Arenillas, Philippe Claeys, José Antonio Arz et al.
1 citations
Nature Communications
Astro and Planetary Science
1.15
article

Prolonged 187Os/188Os excursion implies hydrothermal influence after the Chicxulub impact in the Gulf of Mexico

Honami Sato, Ignacio Arenillas, Philippe Claeys, José Antonio Arz, Christopher M. Lowery, Steven Goderis, J. Morgan, Vicente Gilabert, S. P. S. Gulick, Akira Ishikawa
article en
1 citations

Abstract

The Cretaceous/Paleogene boundary asteroid impact is recorded globally as a negative <sup>187</sup>Os/<sup>188</sup>Os excursion, including in sediments recovered from the IODP-ICDP drilling within the peak ring of the Chicxulub structure in the Gulf of Mexico. The reconstructed marine <sup>187</sup>Os/<sup>188</sup>Os curves can be used for global age correlations on the ~10 kyr scale. However, the versatility of Os isotope clock between the proximal and distal sites remains unclear. This paper presents <sup>187</sup>Os/<sup>188</sup>Os records from early Paleocene sediments deposited in the Chicxulub impact basin and Mexican sites with biochronological scales. The results for these proximal sites show a recovery timescale of ~700 kyr, which is significantly longer than that of the distal sites (~200 kyr). The interval showing the <sup>187</sup>Os/<sup>188</sup>Os decline coincides with the enrichment of hydrothermally-derived Mn, implying that hydrothermal venting at the Chicxulub structure may have played a role in the marine chemistry and ecosystem of the Gulf of Mexico.

Nature CommunicationsVol. 16(1)
Tokyo Institute of Technology (JP), Planetary Science Institute (US), Japan Agency for Marine-Earth Science and Technology (JP), Vrije Universiteit Brussel (BE), Kyushu University (JP), Universidad de Zaragoza (ES), Planetary Systems (United States) (US), Instituto Aragonés de Ciencias de la Salud (ES), Imperial College London (GB), Universitat de Barcelona (ES), The University of Texas at Austin (US)
National Aeronautics and Space Administration, European Commission, Belgian Federal Science Policy Office, Fonds Wetenschappelijk Onderzoek, Universidad Nacional Autónoma de México, Vlaamse regering, Japan Society for the Promotion of Science, Japan Agency for Marine-Earth Science and Technology, European Regional Development Fund, Agencia Estatal de Investigación
Life below water
Openalex Percentile: Top 20%
Astro and Planetary Science
1.15
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