2016 Articles
Impact ejecta at the Paleocene-Eocene boundary
Extraterrestrial impacts have left a substantial imprint on the climate and evolutionary history of Earth. A rapid carbon cycle perturbation and global warming event about 56 million years ago at the Paleocene-Eocene (P-E) boundary (the Paleocene-Eocene Thermal Maximum) was accompanied by rapid expansions of mammals and terrestrial plants and extinctions of deep-sea benthic organisms. Here, we report the discovery of silicate glass spherules in a discrete stratigraphic layer from three marine P-E boundary sections on the Atlantic margin. Distinct characteristics identify the spherules as microtektites and microkrystites, indicating that an extraterrestrial impact occurred during the carbon isotope excursion at the P-E boundary.
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- Schaller+2016+SM.pdf application/pdf 29.8 MB Download File
Also Published In
- Title
- Science
- DOI
- https://doi.org/10.1126/science.aaf5466
More About This Work
- Academic Units
- Lamont-Doherty Earth Observatory
- Biology and Paleo Environment
- Published Here
- October 10, 2018