
Mikael Elfman
Researcher

Globally distributed iridium layer preserved within the Chicxulub impact structure
Author
Summary, in English
The Cretaceous-Paleogene (K-Pg) mass extinction is marked globally by elevated concentrations of iridium, emplaced by a hypervelocity impact event 66 million years ago. Here, we report new data from four independent laboratories that reveal a positive iridium anomaly within the peak-ring sequence of the Chicxulub impact structure, in drill core recovered by IODP-ICDP Expedition 364. The highest concentration of ultrafine meteoritic matter occurs in the post-impact sediments that cover the crater peak ring, just below the lowermost Danian pelagic limestone. Within years to decades after the impact event, this part of the Chicxulub impact basin returned to a relatively low-energy depositional environment, recording in unprecedented detail the recovery of life during the succeeding millennia. The iridium layer provides a key temporal horizon precisely linking Chicxulub to K-Pg boundary sections worldwide.
Department/s
- Nuclear physics
Publishing year
2021
Language
English
Publication/Series
Science Advances
Volume
7
Issue
9
Document type
Journal article
Publisher
American Association for the Advancement of Science (AAAS)
Topic
- Geology
Status
Published
ISBN/ISSN/Other
- ISSN: 2375-2548