Discovery of Extraterrestrial 244Pu in 2 Million Year Old Fossilized Stromatolites

The rapid neutron capture process ( r -process) is responsible for producing about half of the elements heavier than iron in the Universe through cataclysmic events such as core-collapse supernovae and neutron star mergers (NSMs). Despite extensive research, the exact astrophysical sites of the r -p...

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Main Authors: Shawn Bishop, Iuliana Stanciu, Albert Cabré, Craig Feibel, Doru Pacesila, Alexandru Petre, Paul Mereuta, Livius Trache, Marian Virgolici, Cosmin Pintilie, Andreea Serban, Antonio Petraglia, Filippo Terrasi, Fabio Marzaioli, Giuseppe Porzio, Raffaele Buompane, Lucio Gialanella
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:The Planetary Science Journal
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Online Access:https://doi.org/10.3847/PSJ/adbbd6
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Summary:The rapid neutron capture process ( r -process) is responsible for producing about half of the elements heavier than iron in the Universe through cataclysmic events such as core-collapse supernovae and neutron star mergers (NSMs). Despite extensive research, the exact astrophysical sites of the r -process remain one of the unanswered questions in science. The well-known supernova-produced radioisotope ^60 Fe has been detected in terrestrial reservoirs, providing evidence that material from a nearby supernova reached Earth approximately 2 million years (Ma) ago. Our study reports the detection of ^244 Pu in fossilized stromatolite samples that are 2.0 Ma old, collected from palustrine–lacustrine stratigraphic layers dating back to approximately 5 Ma located at the margins of the present-day Lake Turkana Basin in northern Kenya. We demonstrate that stromatolites can mass-concentrate actinides in the range of 10 ^2 –10 ^3 . Using accelerator mass spectrometry, we isolate ^244 Pu and eliminate the anthropogenic contribution. From our findings, we evaluate a terrestrial fluence between 0.2 and 4.7 × 10 ^3 at ​​​​cm ^−2 , in relative agreement with previous studies. The detection of the r -process ^244 Pu around 2 Ma ago raises the possibility of a common supernova origin with ^60 Fe; however, alternative scenarios, such as the production of ^244 Pu in NSMs or other cosmic events and its transport to Earth alongside ^60 Fe via interstellar debris, cannot be ruled out, highlighting the need to consider multiple mechanisms for isotopic transport in the cosmos.
ISSN:2632-3338