Plutonium-244 has a half-life of 81 million years, which means it takes 81 million years for half of it to disappear naturally. Scientists say this type of plutonium cannot be made inside normal stars. It is created in an event called a kilonova, which happens when two extremely dense dead stars called neutron stars collide and explode.
The kilonova that produced this plutonium happened somewhere in our galaxy within the last billion years. When the explosion occurred, it scattered heavy elements including gold, platinum, and plutonium through space. Some of this material eventually reached Earth and settled on the ocean floor, where it has been preserved in the rock layers.
Researchers from a European-Australian collaboration published a study in Nature Astronomy confirming the detection of extraterrestrial plutonium-244 (Pu-244) in ferromanganese crusts recovered from the Pacific Ocean floor. Ferromanganese crusts grow at a rate of just 1 to 10 millimetres per million years, making them extraordinarily precise archives of the materials that settled from the water column over geological time. By sampling different depth layers within the crust, the team was able to assign approximate dates to the plutonium signal, narrowing the kilonova event to within the last billion years but more than 100 million years ago.
The key evidence distinguishing a kilonova origin from a supernova origin was the absence of curium-247 (Cm-247). Both kilonova and supernova events produce Pu-244, but only supernovae produce Cm-247 in comparable quantities. The absence of Cm-247 alongside the presence of Pu-244 therefore indicates that the source event was a kilonova, a merger of two neutron stars. This r-process nucleosynthesis, in which neutron-rich atomic nuclei rapidly capture free neutrons to build heavy elements, is the primary pathway for creating elements heavier than iron that cannot be made inside ordinary stars.
The significance of the discovery lies in its confirmation that kilonovae are a realistic source of r-process heavy elements reaching the inner solar system. Previous evidence for kilonova-produced material in the geological record was largely theoretical or based on isotopic anomalies in meteorites. Finding Pu-244 in a slowly accumulated terrestrial archive provides a new and sensitive tool for dating and localising past nucleosynthetic events in the Milky Way's history.
A research consortium spanning European and Australian institutions has reported in Nature Astronomy the detection of live extraterrestrial Pu-244 in ferromanganese crust samples dredged from the Pacific Ocean floor. With a half-life of 80.8 million years, Pu-244 is the longest-lived superheavy nuclide short of primordial uranium and thorium. Its detection as a live radioisotope (meaning measurable activity remains rather than purely stable daughter products) constrains the production event to within approximately one to three half-lives prior to deposition, placing the kilonova within the last billion years but no more recently than roughly 100 million years ago, a window inferred from the co-absence of shorter-lived r-process nuclides such as Cm-247 (t1/2 = 15.6 Myr).
The forensic discrimination between kilonova and core-collapse supernova origin rests on the differential r-process yield ratios of the actinide series. Core-collapse supernovae, particularly those with very neutron-rich ejecta from the neutrino-driven wind mechanism, produce both Pu-244 and Cm-247, whereas neutron star mergers favour the third r-process peak through a higher neutron-to-seed ratio, producing large quantities of Pu-244 while yielding Cm-247 below detection thresholds. The observed ratio (Pu-244 present, Cm-247 undetected) is thus a robust kilonova fingerprint. The absolute abundance of Pu-244 in the crust layers further constrains the event distance to within approximately 300 parsecs of the pre-solar nebula, consistent with ejecta reaching the inner solar system at the dilution levels observed.
Beyond the immediate result, the study demonstrates that ferromanganese crusts function as a novel class of cosmic ray and interstellar medium detector, complementing established archives such as deep-sea nodules and Antarctic micrometeorite collections. The growth rate of 1-10 mm per million years and the capacity for continuous accretion over hundreds of millions of years allow sub-million-year temporal resolution for late Phanerozoic events and Myr-scale resolution deeper in the stratigraphic column. Future surveys coupling Pu-244 measurements with I-129, Fe-60, and Mn-53 profiles from the same crust layers could disentangle multiple nucleosynthetic episodes, offering a window into the stochastic history of massive star and compact object mergers in the Galactic thin disk over the last few billion years.
Scientists studying deep-sea ferromanganese crusts have identified plutonium-244 of stellar origin in samples from the Pacific Ocean floor, providing direct physical evidence that a nearby kilonova event scattered heavy elements across the solar system within the last billion years.

Scientists have found something very special buried deep under the Pacific Ocean. They discovered tiny amounts of a material called plutonium-244 on the ocean floor. This type of plutonium does not come from Earth. It came from space.
The plutonium was made in a huge explosion in space called a kilonova. A kilonova happens when two very dense dead stars crash into each other. This explosion creates heavy materials like gold, silver, and plutonium.
The plutonium then fell to Earth and settled on the bottom of the ocean. Scientists can study these tiny amounts of material to learn more about stars and space events that happened a very long time ago.
1Where did scientists find the plutonium?
2What is a kilonova?
3What kinds of materials does a kilonova create?
4Where did the plutonium-244 originally come from?
5What is the ocean floor?
6The plutonium-244 found on the ocean floor was made on Earth.
7A kilonova happens when two dead stars crash into each other.
8Kilonova explosions can create gold.
9Scientists found the plutonium in the atmosphere.
10Plutonium-244 is a radioactive material.
11Scientists found plutonium-244 on the ___ Ocean floor.
12A kilonova happens when two neutron ___ collide.
13The kilonova creates heavy materials including gold and ___.